{"pageNumber":"2406","pageRowStart":"60125","pageSize":"25","recordCount":184617,"records":[{"id":79100,"text":"sir20055049 - 2006 - Hydraulic and solute-transport properties and simulated advective transport of contaminated ground water in a fractured-rock aquifer at the Naval Air Warfare Center, West Trenton, New Jersey, 2003","interactions":[],"lastModifiedDate":"2024-09-23T22:07:50.229414","indexId":"sir20055049","displayToPublicDate":"2006-09-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5049","title":"Hydraulic and solute-transport properties and simulated advective transport of contaminated ground water in a fractured-rock aquifer at the Naval Air Warfare Center, West Trenton, New Jersey, 2003","docAbstract":"Volatile organic compounds, predominantly trichloroethylene and its degradation products, have been detected in ground water at the Naval Air Warfare Center (NAWC), West Trenton, New Jersey. An air-stripping pump-and-treat system has been in operation at the NAWC since 1998. An existing ground-water-flow model was used to evaluate the effect of a change in the configuration of the network of recovery wells in the pump-and-treat system on flow paths of contaminated ground water.\r\n\r\nThe NAWC is underlain by a fractured-rock aquifer composed of dipping layers of sedimentary rocks of the Lockatong and Stockton Formations. Hydraulic and solute-transport properties of the part of the aquifer composed of the Lockatong Formation were measured using aquifer tests and tracer tests. The heterogeneity of the rocks causes a wide range of values of each parameter measured. Transmissivity ranges from 95 to 1,300 feet squared per day; the storage coefficient ranges from 9 x 10-5 to 5 x 10-3; and the effective porosity ranges from 0.0003 to 0.002.\r\n\r\nThe average linear velocity of contaminated ground water was determined for ambient conditions (when no wells at the site are pumped) using an existing ground-water-flow model, particle-tracking techniques, and the porosity values determined in this study. The average linear velocity of flow paths beginning at each contaminated well and ending at the streams where the flow paths terminate ranges from 0.08 to 130 feet per day. As a result of a change in the pump-and-treat system (adding a 165-foot-deep well pumped at 5 gallons per minute and reducing the pumping rate at a nearby 41-foot-deep well by the same amount), water in the vicinity of three 100- to 165-foot-deep wells flows to the deep well rather than the shallower well.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055049","usgsCitation":"Lewis-Brown, J.C., Carleton, G.B., and Imbrigiotta, T., 2006, Hydraulic and solute-transport properties and simulated advective transport of contaminated ground water in a fractured-rock aquifer at the Naval Air Warfare Center, West Trenton, New Jersey, 2003: U.S. Geological Survey Scientific Investigations Report 2005-5049, vi, 32 p., https://doi.org/10.3133/sir20055049.","productDescription":"vi, 32 p.","numberOfPages":"38","temporalStart":"2003-01-01","temporalEnd":"2003-12-31","costCenters":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":462158,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_77630.htm","linkFileType":{"id":5,"text":"html"}},{"id":8533,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5049/","linkFileType":{"id":5,"text":"html"}},{"id":191194,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"New Jersey","city":"Trenton","otherGeospatial":"Naval Air Warfare Center","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.915771484375,\n              40.1095880747414\n            ],\n            [\n              -74.61090087890625,\n              40.1095880747414\n            ],\n            [\n              -74.61090087890625,\n              40.271143686084194\n            ],\n            [\n              -74.915771484375,\n              40.271143686084194\n            ],\n            [\n              -74.915771484375,\n              40.1095880747414\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a311","contributors":{"authors":[{"text":"Lewis-Brown, Jean C.","contributorId":46991,"corporation":false,"usgs":true,"family":"Lewis-Brown","given":"Jean","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":289089,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carleton, Glen B. 0000-0002-7666-4407 carleton@usgs.gov","orcid":"https://orcid.org/0000-0002-7666-4407","contributorId":3795,"corporation":false,"usgs":true,"family":"Carleton","given":"Glen","email":"carleton@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":289088,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Imbrigiotta, Thomas E. 0000-0003-1716-4768 timbrig@usgs.gov","orcid":"https://orcid.org/0000-0003-1716-4768","contributorId":2466,"corporation":false,"usgs":true,"family":"Imbrigiotta","given":"Thomas E.","email":"timbrig@usgs.gov","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":false,"id":289087,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":79096,"text":"fs20063054 - 2006 - Interdisciplinary science in support of environmental health along the United States-Mexico border","interactions":[{"subject":{"id":70296,"text":"fs20043140 - 2004 - Internet Map Service for Environmental Health in the U.S.-Mexico Border Region","indexId":"fs20043140","publicationYear":"2004","noYear":false,"title":"Internet Map Service for Environmental Health in the U.S.-Mexico Border Region"},"predicate":"SUPERSEDED_BY","object":{"id":79096,"text":"fs20063054 - 2006 - Interdisciplinary science in support of environmental health along the United States-Mexico border","indexId":"fs20063054","publicationYear":"2006","noYear":false,"title":"Interdisciplinary science in support of environmental health along the United States-Mexico border"},"id":1}],"lastModifiedDate":"2016-08-11T16:41:56","indexId":"fs20063054","displayToPublicDate":"2006-09-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-3054","title":"Interdisciplinary science in support of environmental health along the United States-Mexico border","docAbstract":"<p>The diverse, fragile ecosystems of the borderlands have been pushed beyond sustainable levels due to rapid population growth and land-use changes. Water shortages and pollution, poor air quality, increased soil salinities, residual pesticides and heavy metal contaminants are some of the many stressors that are degrading the quality of life in the borderlands. The relationship between human health and environmental quality challenges public officials, medical professionals, and resource managers on both sides of the border in their efforts to provide for and maintain healthy communities. To help understand the relationship between environmental and human health, the U.S. Geological Survey's (USGS) Border Environmental Health Initiative (BEHI) created an Internet Map Service (IMS) with binational georeferenced data. The goal is to have seamless integration of borderwide datasets at regional and local scales that can lend understanding of the linkages between the condition of the physical environment and public health issues.</p>","language":"English","publisher":"U.S Geological Survey","publisherLocation":"Reston, Virginia","doi":"10.3133/fs20063054","usgsCitation":"Papoulias, D., Parcher, J., Stefanov, J., and Page, R., 2006, Interdisciplinary science in support of environmental health along the United States-Mexico border (English Version 1.0, Supersedes FS 2004-3140): U.S. Geological Survey Fact Sheet 2006-3054, 2 p., https://doi.org/10.3133/fs20063054.","productDescription":"2 p.","numberOfPages":"2","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":124953,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3054.jpg"},{"id":8528,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2006/3054/","linkFileType":{"id":5,"text":"html"}}],"edition":"English Version 1.0, Supersedes FS 2004-3140","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e091c","contributors":{"authors":[{"text":"Papoulias, Diana","contributorId":22046,"corporation":false,"usgs":true,"family":"Papoulias","given":"Diana","email":"","affiliations":[],"preferred":false,"id":289073,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parcher, Jean","contributorId":31841,"corporation":false,"usgs":true,"family":"Parcher","given":"Jean","affiliations":[],"preferred":false,"id":289074,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stefanov, Jim","contributorId":15705,"corporation":false,"usgs":true,"family":"Stefanov","given":"Jim","email":"","affiliations":[],"preferred":false,"id":289072,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Page, Ric","contributorId":86861,"corporation":false,"usgs":true,"family":"Page","given":"Ric","email":"","affiliations":[],"preferred":false,"id":289075,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":79102,"text":"sir20065168 - 2006 - A comparison of approaches for estimating bottom-sediment mass in large reservoirs","interactions":[],"lastModifiedDate":"2012-03-08T17:16:24","indexId":"sir20065168","displayToPublicDate":"2006-09-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5168","title":"A comparison of approaches for estimating bottom-sediment mass in large reservoirs","docAbstract":"Estimates of sediment and sediment-associated constituent loads and yields from drainage basins are necessary for the management of reservoir-basin systems to address important issues such as reservoir sedimentation and eutrophication. One method for the estimation of loads and yields requires a determination of the total mass of sediment deposited in a reservoir. This method involves a sediment volume-to-mass conversion using bulk-density information. A comparison of four computational approaches (partition, mean, midpoint, strategic) for using bulk-density information to estimate total bottom-sediment mass in four large reservoirs indicated that the differences among the approaches were not statistically significant. However, the lack of statistical significance may be a result of the small sample size. Compared to the partition approach, which was presumed to provide the most accurate estimates of bottom-sediment mass, the results achieved using the strategic, mean, and midpoint approaches differed by as much as ?4, ?20, and ?44 percent, respectively. It was concluded that the strategic approach may merit further investigation as a less time consuming and less costly alternative to the partition approach.","language":"ENGLISH","doi":"10.3133/sir20065168","usgsCitation":"Juracek, K.E., 2006, A comparison of approaches for estimating bottom-sediment mass in large reservoirs: U.S. Geological Survey Scientific Investigations Report 2006-5168, iv, 13 p., https://doi.org/10.3133/sir20065168.","productDescription":"iv, 13 p.","numberOfPages":"17","onlineOnly":"Y","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":195776,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8535,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5168/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -102,37 ], [ -102,40 ], [ -95,40 ], [ -95,37 ], [ -102,37 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b1005","contributors":{"authors":[{"text":"Juracek, Kyle E. 0000-0002-2102-8980 kjuracek@usgs.gov","orcid":"https://orcid.org/0000-0002-2102-8980","contributorId":2022,"corporation":false,"usgs":true,"family":"Juracek","given":"Kyle","email":"kjuracek@usgs.gov","middleInitial":"E.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":289091,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":79098,"text":"sir20065074 - 2006 - Methodology to evaluate the effect of sorption in the unsaturated zone on the storage of nitrate and other ions and their transport across the water table, southern New Jersey","interactions":[],"lastModifiedDate":"2020-01-26T16:30:39","indexId":"sir20065074","displayToPublicDate":"2006-09-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5074","title":"Methodology to evaluate the effect of sorption in the unsaturated zone on the storage of nitrate and other ions and their transport across the water table, southern New Jersey","docAbstract":"A new field-based approach for determining sorption in the unsaturated zone and its effect on the storage of ions and their transport in recharge to ground water has been demonstrated for a small agricultural watershed in the Coastal Plain of southern New Jersey. Moisture-content and chemical-concentration data obtained from unsaturated-zone-core and shallow-ground-water samples were used to estimate the mass flux of chemical constituents across the water table, as well as sorption coefficients (Kd). The selectivity order of the Kd values for cations is consistent with the expected selectivity order: for example, Na+ > Mg++ > Ca++ for sands. Although calculated sorption coefficients, as expected, were greater for cations than for anions, sorption had a substantial effect on the transport of anions through the unsaturated zone; in particular, average Kd values for NO3- were 0.22 liters per milligram for sands and 0.62 liters per milligram for finer grained sediments. The unsaturated zone in the study area is a large reservoir for nitrogen. Models that do not account for sorption are likely to result in unrealistic predictions of contaminant transport rate and provide overly optimistic expectations for natural cleansing in this watershed and those in other similar hydrogeologic settings.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20065074","usgsCitation":"Reilly, T.J., and Baehr, A.L., 2006, Methodology to evaluate the effect of sorption in the unsaturated zone on the storage of nitrate and other ions and their transport across the water table, southern New Jersey: U.S. Geological Survey Scientific Investigations Report 2006-5074, vi, 22 p., https://doi.org/10.3133/sir20065074.","productDescription":"vi, 22 p.","numberOfPages":"28","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":8530,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5074/","linkFileType":{"id":5,"text":"html"}},{"id":192387,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"New Jersey","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.981689453125,\n              40.027614437486655\n            ],\n            [\n              -75.322265625,\n              39.86758762451019\n            ],\n            [\n              -75.5859375,\n              39.66491373749128\n            ],\n            [\n              -75.552978515625,\n              39.46164364205549\n            ],\n            [\n              -75.12451171875,\n              39.18117526158749\n            ],\n            [\n              -74.915771484375,\n              39.172658670429946\n            ],\n            [\n              -75.03662109375,\n              38.92522904714054\n            ],\n            [\n              -74.90478515625,\n              38.89103282648846\n            ],\n            [\n              -74.46533203125,\n              39.342794408952365\n            ],\n            [\n              -74.091796875,\n              39.9434364619742\n            ],\n            [\n              -74.981689453125,\n              40.027614437486655\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a017","contributors":{"authors":[{"text":"Reilly, Timothy J. 0000-0002-2939-3050 tjreilly@usgs.gov","orcid":"https://orcid.org/0000-0002-2939-3050","contributorId":1858,"corporation":false,"usgs":true,"family":"Reilly","given":"Timothy","email":"tjreilly@usgs.gov","middleInitial":"J.","affiliations":[{"id":34983,"text":"Contaminant Biology Program","active":true,"usgs":true},{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"preferred":true,"id":289080,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baehr, Arthur L.","contributorId":104523,"corporation":false,"usgs":true,"family":"Baehr","given":"Arthur","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":289081,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":79103,"text":"ofr20061185 - 2006 - Seismicity of Afghanistan and vicinity","interactions":[],"lastModifiedDate":"2012-02-02T00:14:21","indexId":"ofr20061185","displayToPublicDate":"2006-09-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-1185","title":"Seismicity of Afghanistan and vicinity","docAbstract":"This publication describes the seismicity of Afghanistan and vicinity and is intended for use in seismic hazard studies of that nation. Included are digital files with information on earthquakes that have been recorded in Afghanistan and vicinity through mid-December 2004. Chapter A provides an overview of the seismicity and tectonics of Afghanistan and defines the earthquake parameters included in the 'Summary Catalog' and the 'Summary of Macroseismic Effects.' Chapter B summarizes compilation of the 'Master Catalog' and 'Sub-Threshold Catalog' and documents their formats. The 'Summary Catalog' itself is presented as a comma-delimited ASCII file, the 'Summary of Macroseismic Effects' is presented as an html file, and the 'Master Catalog' and 'Sub-Threshold Catalog' are presented as flat ASCII files. Finally, this report includes as separate plates a digital image of a map of epicenters of earthquakes occurring since 1964 (Plate 1) and a representation of areas of damage or strong shaking from selected past earthquakes in Afghanistan and vicinity (Plate 2).","language":"ENGLISH","doi":"10.3133/ofr20061185","usgsCitation":"Dewey, J.W., 2006, Seismicity of Afghanistan and vicinity (Version 1.0): U.S. Geological Survey Open-File Report 2006-1185, v, 55 p.; CD-ROM, https://doi.org/10.3133/ofr20061185.","productDescription":"v, 55 p.; CD-ROM","numberOfPages":"60","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":194574,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8536,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1185/","linkFileType":{"id":5,"text":"html"}},{"id":8537,"rank":9999,"type":{"id":23,"text":"Spatial Data"},"url":"https://pubs.usgs.gov/of/2006/1185/downloads/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa902","contributors":{"authors":[{"text":"Dewey, James W. 0000-0001-8838-2450 jdewey@usgs.gov","orcid":"https://orcid.org/0000-0001-8838-2450","contributorId":5819,"corporation":false,"usgs":true,"family":"Dewey","given":"James","email":"jdewey@usgs.gov","middleInitial":"W.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":289092,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":79093,"text":"ofr20061182 - 2006 - Storms and flooding in California in December 2005 and January 2006 — A preliminary assessment","interactions":[],"lastModifiedDate":"2022-01-26T19:57:00.515952","indexId":"ofr20061182","displayToPublicDate":"2006-09-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-1182","title":"Storms and flooding in California in December 2005 and January 2006 — A preliminary assessment","docAbstract":"<p>A series of storms beginning before Christmas 2005 and ending after New Year’s Day 2006 produced significant runoff over much of northern California. The storms resulted in an estimated $300 million in damages and Federal disaster declarations in 10 counties. Several precipitation stations in the Sierra Nevada had precipitation totals greater than 20 inches for the period December 24 through January 3, and several stations in the Coastal Range had precipitation totals greater than 18 inches. The peak stream discharges resulting from the storms in the north coast area generally had recurrence intervals in the 10- to 25-year range, although the recurrence interval for peak discharge at one station on Sonoma Creek near Agua Caliente was greater than 100 years. In the San Francisco Bay area, peak discharges also generally had recurrence intervals in the 10- to 25-year range. Further south along the central coast and in southern California, peak discharges had smaller recurrence intervals, in the 2- to 5-year range. Upper Sacramento River tributaries draining from the west had peak flows with recurrence intervals in the 2- to 5-year range, whereas upper tributaries draining from the east side had recurrence intervals in the 5- to 10-year range. Further south, Sacramento River tributaries such as the Yuba and American Rivers had peak discharges with recurrence intervals in the 10- to 25-year range. On the east side of the central Sierra around Lake Tahoe, peak discharges had recurrence intervals in the 10- to 25-year range. Further south in the Sierra, streams draining into the San Joaquin River Basin had flows with recurrence intervals ranging from 2 to 5 years.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061182","usgsCitation":"Parrett, C., and Hunrichs, R.A., 2006, Storms and flooding in California in December 2005 and January 2006 — A preliminary assessment: U.S. Geological Survey Open-File Report 2006-1182, iv, 8 p., https://doi.org/10.3133/ofr20061182.","productDescription":"iv, 8 p.","numberOfPages":"12","onlineOnly":"Y","temporalStart":"2005-12-01","temporalEnd":"2006-01-31","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":191556,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":394906,"rank":3,"type":{"id":36,"text":"NGMDB Index 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,{"id":79097,"text":"fs20063054S - 2006 - Ciencia Interdisciplinaria en Apoyo a la Salud Ambiental a lo largo de la Frontera de Mexico-Estados Unidos","interactions":[{"subject":{"id":70299,"text":"fs20043140S - 2004 - Servicio de Mapas en Internet para la Salud Ambiental en la Region Fronteriza Entre los Estados Unidos y Mexico","indexId":"fs20043140S","publicationYear":"2004","noYear":false,"title":"Servicio de Mapas en Internet para la Salud Ambiental en la Region Fronteriza Entre los Estados Unidos y Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":79097,"text":"fs20063054S - 2006 - Ciencia Interdisciplinaria en Apoyo a la Salud Ambiental a lo largo de la Frontera de Mexico-Estados Unidos","indexId":"fs20063054S","publicationYear":"2006","noYear":false,"title":"Ciencia Interdisciplinaria en Apoyo a la Salud Ambiental a lo largo de la Frontera de Mexico-Estados Unidos"},"id":1}],"lastModifiedDate":"2026-01-29T20:57:16.959784","indexId":"fs20063054S","displayToPublicDate":"2006-09-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-3054","title":"Ciencia Interdisciplinaria en Apoyo a la Salud Ambiental a lo largo de la Frontera de Mexico-Estados Unidos","language":"Spanish","publisher":"U.S. Geological Survey","doi":"10.3133/fs20063054S","usgsCitation":"Papoulias, D., Parcher, J., Stefanov, J., and Page, R., 2006, Ciencia Interdisciplinaria en Apoyo a la Salud Ambiental a lo largo de la Frontera de Mexico-Estados Unidos (Spanish Version 1.0, Supersedes FS 2004-3140): U.S. Geological Survey Fact Sheet 2006-3054, 2 p., https://doi.org/10.3133/fs20063054S.","productDescription":"2 p.","numberOfPages":"2","costCenters":[{"id":139,"text":"Border Environmental Health Initiative","active":false,"usgs":true}],"links":[{"id":8529,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2006/3054/","linkFileType":{"id":5,"text":"html"}},{"id":121010,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3054.jpg"}],"edition":"Spanish Version 1.0, Supersedes FS 2004-3140","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dde4b07f02db5e1fc6","contributors":{"authors":[{"text":"Papoulias, Diana","contributorId":22046,"corporation":false,"usgs":true,"family":"Papoulias","given":"Diana","email":"","affiliations":[],"preferred":false,"id":289077,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parcher, Jean","contributorId":31841,"corporation":false,"usgs":true,"family":"Parcher","given":"Jean","affiliations":[],"preferred":false,"id":289078,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stefanov, Jim","contributorId":15705,"corporation":false,"usgs":true,"family":"Stefanov","given":"Jim","email":"","affiliations":[],"preferred":false,"id":289076,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Page, Ric","contributorId":86861,"corporation":false,"usgs":true,"family":"Page","given":"Ric","email":"","affiliations":[],"preferred":false,"id":289079,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":79104,"text":"fs20063063 - 2006 - Monitoring changes in the Platte River riparian corridor with serial LiDAR surveys","interactions":[],"lastModifiedDate":"2012-02-02T00:14:21","indexId":"fs20063063","displayToPublicDate":"2006-09-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-3063","title":"Monitoring changes in the Platte River riparian corridor with serial LiDAR surveys","docAbstract":"The Platte River in central Nebraska is a wide, sand-bedded river that provides habitat for migratory water birds along the North American flyway. The central Platte River functions as critical habitat for the endangered whooping crane (Grus americana) and also is an important habitat for the endangered least tern (Sterna antillarum) and the threatened piping plover (Charadrius melodus). Upstream water-resource development over the last century has decreased the water and sediment supplied to the central Platte River. This has resulted in vegetation encroachment and narrowing of Platte River channels. The National Academy of Sciences' National Research Council, in a recent review of these critical habitat designations, concluded that the current morphology of Platte River channels is limiting the recovery of the endangered and threatened avian species.\r\n\r\nHabitat-enhancement efforts along the Platte River currently (2006) are focused on the clearing of vegetation from in-channel and riparian areas, whereas future plans propose the release of water from upstream dams as a means to prevent vegetation from encroaching on the active river channel. For this reason, monitoring the physical response of the river channel to these management treatments is an important component of a proposed habitat recovery program. Understanding the effects of management strategies on Platte River riparian habitat also is a key objective of the U.S. Geological Survey's Platte River Priority Ecosystem Program (http://mcmcweb.er.usgs.gov/platte/). This fact sheet describes applications of LiDAR to monitor changes in the Platte River riparian corridor.","language":"ENGLISH","doi":"10.3133/fs20063063","usgsCitation":"Kinzel, P.J., Nelson, J.M., and Wright, C.W., 2006, Monitoring changes in the Platte River riparian corridor with serial LiDAR surveys (Version 1.0): U.S. Geological Survey Fact Sheet 2006-3063, 4 p., https://doi.org/10.3133/fs20063063.","productDescription":"4 p.","numberOfPages":"4","onlineOnly":"Y","costCenters":[{"id":534,"text":"Platte River Priority Ecosystem Program","active":false,"usgs":true}],"links":[{"id":126814,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3063.jpg"},{"id":8538,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2006/3063/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db62739f","contributors":{"authors":[{"text":"Kinzel, Paul J. 0000-0002-6076-9730 pjkinzel@usgs.gov","orcid":"https://orcid.org/0000-0002-6076-9730","contributorId":743,"corporation":false,"usgs":true,"family":"Kinzel","given":"Paul","email":"pjkinzel@usgs.gov","middleInitial":"J.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":289093,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, Jonathan M. 0000-0002-7632-8526 jmn@usgs.gov","orcid":"https://orcid.org/0000-0002-7632-8526","contributorId":2812,"corporation":false,"usgs":true,"family":"Nelson","given":"Jonathan","email":"jmn@usgs.gov","middleInitial":"M.","affiliations":[{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":289094,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wright, C. Wayne wwright@usgs.gov","contributorId":57422,"corporation":false,"usgs":true,"family":"Wright","given":"C.","email":"wwright@usgs.gov","middleInitial":"Wayne","affiliations":[],"preferred":false,"id":289095,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":79101,"text":"sir20065088 - 2006 - An update of hydrologic conditions and distribution of selected constituents in water, Snake River Plain aquifer, Idaho National Laboratory, Idaho, Emphasis 1999-2001","interactions":[],"lastModifiedDate":"2012-03-08T17:16:21","indexId":"sir20065088","displayToPublicDate":"2006-09-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5088","title":"An update of hydrologic conditions and distribution of selected constituents in water, Snake River Plain aquifer, Idaho National Laboratory, Idaho, Emphasis 1999-2001","docAbstract":"Radiochemical and chemical wastewater discharged since 1952 to infiltration ponds, evaporation ponds, and disposal wells at the Idaho National Laboratory (INL) has affected water quality in the Snake River Plain aquifer underlying the INL. The U.S. Geological Survey (USGS), in cooperation with the U.S. Department of Energy, maintains ground-water monitoring networks at the INL to determine hydrologic trends, and to delineate the movement of radiochemical and chemical wastes in the aquifer. This report presents an analysis of water-level and water-quality data collected from wells in the USGS ground-water monitoring networks during 1999-2001.\r\n\r\nWater in the Snake River Plain aquifer moves principally through fractures and interflow zones in basalt, generally flows southwestward, and eventually discharges at springs along the Snake River. The aquifer is recharged principally from infiltration of irrigation water, infiltration of streamflow, ground-water inflow from adjoining mountain drainage basins, and infiltration of precipitation. Water levels in wells rose in the northern and west-central parts of the INL by 1 to 3 feet, and declined in the southwestern parts of the INL by up to 4 feet during 1999-2001.\r\n\r\nDetectable concentrations of radiochemical constituents in water samples from wells in the Snake River Plain aquifer at the INL generally decreased or remained constant during 1999-2001. Decreases in concentrations were attributed to decreased rates of radioactive-waste disposal, radioactive decay, changes in waste-disposal methods, and dilution from recharge. Tritium concentrations in water samples decreased as much as 8.3 picocuries per milliliter (pCi/mL) during 1999-2001, ranging from 0.43?0.14 to 13.6?0.6 pCi/mL in October 2001. Tritium concentrations in five wells near the Idaho Nuclear Technology and Engineering Center (INTEC) increased a few picocuries per milliliter from October 2000 to October 2001. Strontium-90 concentrations decreased or remained constant during 1999-2001, ranging from 2.1?0.6 to 42.4?1.4 pCi/L in October 2001. During 1999-2001, concentrations of cesium-137, plutonium-238, and plutonium-239, -240 (undivided) were less than the reporting level in water samples from all wells sampled at the INL. The concentration of americium-241 in one sample was 0.003?0.001 pCi/L, the reporting level for that constituent. Cobalt-60 was not detected in any samples collected during 1999-2001.\r\n\r\nChanges in detectable concentrations of nonradioactive chemical constituents in water from the Snake River Plain aquifer at the INL varied during 1999-2001. In October 2001, water from one well south of the Reactor Technology Complex (RTC) [known as the Test Reactor Area (TRA) until 2005] contained 139 micrograms per liter (?g/L) of chromium, a decrease from the concentration of 168 ?g/L detected in October 1998. Other water samples contained from less than 16.7 to 21.3 ?g/L of chromium. In October 2001, concentrations of sodium in water samples from most of the wells in the southern part of the INL were larger than the background concentration of 10 mg/L, but were similar to or slightly less than October 1998 concentrations. The largest sodium concentration was 75 milligrams per liter (mg/L) in water from well USGS 113.\r\n\r\nIn 2001, chloride concentrations in most water samples from the INTEC and the Central Facilities Area (CFA) exceeded ambient concentrations of 10 and 20 mg/L, respectively. Chloride concentrations in water from wells near the RTC were less than 20 mg/L. At the Radioactive Waste Management Complex (RWMC), chloride concentrations in water from wells USGS 88, 89, and 120 were 81, 40, and 23 mg/L, respectively. Concentrations of chloride in all other wells near the RWMC were less than 19 mg/L. During 2001, concentrations of sulfate in water from two wells near the RTC, two wells near the RWMC, and one well near the CFA exceeded 40 mg/L, the estimated background concentration of sulfate in the Snake River","language":"ENGLISH","doi":"10.3133/sir20065088","usgsCitation":"Davis, L.C., 2006, An update of hydrologic conditions and distribution of selected constituents in water, Snake River Plain aquifer, Idaho National Laboratory, Idaho, Emphasis 1999-2001: U.S. Geological Survey Scientific Investigations Report 2006-5088, viii, 48 p., https://doi.org/10.3133/sir20065088.","productDescription":"viii, 48 p.","numberOfPages":"56","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":190733,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8534,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5088/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a84aa","contributors":{"authors":[{"text":"Davis, Linda C. lcdavis@usgs.gov","contributorId":2539,"corporation":false,"usgs":true,"family":"Davis","given":"Linda","email":"lcdavis@usgs.gov","middleInitial":"C.","affiliations":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"preferred":true,"id":289090,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":79105,"text":"wdrCT051 - 2006 - Water resources data, Connecticut, water year 2005","interactions":[],"lastModifiedDate":"2012-03-08T17:16:24","indexId":"wdrCT051","displayToPublicDate":"2006-09-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CT-05-1","title":"Water resources data, Connecticut, water year 2005","docAbstract":"This report includes records on both surface and ground water in the State. Specifically, it contains: (1) discharge records for 52 streamflow-gaging stations and for 38 partial-record streamflow stations and miscellaneous sites; (2) stage-only records for 4 tidal-gaging stations; (3) water-quality records for 17 streamflow-gaging stations, for 18 ungaged stream sites, and temperature at 1 reservoir site; and (4) water-level records for 73 observation wells. Additional water-quality data are published for 16 miscellaneous surface-water sites and for 19 miscellaneous ground-water sites, which were not part of the systematic data-collection program.","language":"ENGLISH","doi":"10.3133/wdrCT051","usgsCitation":"Morrison, J., Sargent, T., Martin, J., and Norris, J., 2006, Water resources data, Connecticut, water year 2005: U.S. Geological Survey Water Data Report CT-05-1, 380 p., https://doi.org/10.3133/wdrCT051.","productDescription":"380 p.","numberOfPages":"380","additionalOnlineFiles":"Y","temporalStart":"2004-10-01","temporalEnd":"2005-09-30","costCenters":[{"id":196,"text":"Connecticut Water Science Center","active":true,"usgs":true}],"links":[{"id":194375,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8539,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/2005/wdr-ct-05-1/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49b8e4b07f02db5ccda7","contributors":{"authors":[{"text":"Morrison, Jonathan 0000-0002-1756-4609 jmorriso@usgs.gov","orcid":"https://orcid.org/0000-0002-1756-4609","contributorId":2274,"corporation":false,"usgs":true,"family":"Morrison","given":"Jonathan","email":"jmorriso@usgs.gov","affiliations":[{"id":196,"text":"Connecticut Water Science Center","active":true,"usgs":true}],"preferred":true,"id":289096,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sargent, T.C.","contributorId":24428,"corporation":false,"usgs":true,"family":"Sargent","given":"T.C.","email":"","affiliations":[],"preferred":false,"id":289097,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Martin, J.W.","contributorId":71510,"corporation":false,"usgs":true,"family":"Martin","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":289099,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Norris, J.R.","contributorId":67153,"corporation":false,"usgs":true,"family":"Norris","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":289098,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":79095,"text":"sir20065089 - 2006 - Estimated flood-inundation mapping for the Lower Blue River in Kansas City, Missouri, 2003-2005","interactions":[],"lastModifiedDate":"2023-03-20T21:24:32.411936","indexId":"sir20065089","displayToPublicDate":"2006-09-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5089","title":"Estimated flood-inundation mapping for the Lower Blue River in Kansas City, Missouri, 2003-2005","docAbstract":"The U.S. Geological Survey, in cooperation with the city of Kansas City, Missouri, began a study in 2003 of the lower Blue River in Kansas City, Missouri, from Gregory Boulevard to the mouth at the Missouri River to determine the estimated extent of flood inundation in the Blue River valley from flooding on the lower Blue River and from Missouri River backwater. Much of the lower Blue River flood plain is covered by industrial development. Rapid development in the upper end of the watershed has increased the volume of runoff, and thus the discharge of flood events for the Blue River. Modifications to the channel of the Blue River began in late 1983 in response to the need for flood control. By 2004, the channel had been widened and straightened from the mouth to immediately downstream from Blue Parkway to convey a 30-year flood.\r\n\r\nA two-dimensional depth-averaged flow model was used to simulate flooding within a 2-mile study reach of the Blue River between 63rd Street and Blue Parkway. Hydraulic simulation of the study reach provided information for the design and performance of proposed hydraulic structures and channel improvements and for the production of estimated flood-inundation maps and maps representing an areal distribution of water velocity, both magnitude and direction.\r\n\r\nFlood profiles of the Blue River were developed between Gregory Boulevard and 63rd Street from stage elevations calculated from high water marks from the flood of May 19, 2004; between 63rd Street and Blue Parkway from two-dimensional hydraulic modeling conducted for this study; and between Blue Parkway and the mouth from an existing one-dimensional hydraulic model by the U.S. Army Corps of Engineers. Twelve inundation maps were produced at 2-foot intervals for Blue Parkway stage elevations from 750 to 772 feet. Each map is associated with National Weather Service flood-peak forecast locations at 63rd Street, Blue Parkway, Stadium Drive, U.S. Highway 40, 12th Street, and the Missouri River at the Hannibal railroad bridge in Kansas City. The National Weather Service issues peak-stage forecasts for these locations during times of flooding. Missouri River backwater inundation profiles were developed using interpolated Missouri River stage elevations at the mouth of the Blue River. Twelve backwater-inundation maps were produced at 2-foot intervals for the mouth of the Blue River from 730.9 to 752.9.\r\n\r\nTo provide public access to the information presented in this report, a World Wide Web site (http://mo.water.usgs.gov/indep/kelly/blueriver/index.htm) was created that displays the results of two-dimensional modeling between 63rd Street and Blue Parkway, estimated flood-inundation maps, estimated backwater-inundation maps, and the latest gage heights and National Weather Service stage forecast for each forecast location within the study area. In addition, the full text of this report, all tables, and all plates are available for download at http://pubs.water.usgs.gov/sir2006-5089.","language":"English","doi":"10.3133/sir20065089","usgsCitation":"Kelly, B.P., and Rydlund, P.H., 2006, Estimated flood-inundation mapping for the Lower Blue River in Kansas City, Missouri, 2003-2005: U.S. Geological Survey Scientific Investigations Report 2006-5089, Report: vi, 28 p.; Appendix, https://doi.org/10.3133/sir20065089.","productDescription":"Report: vi, 28 p.; Appendix","numberOfPages":"34","onlineOnly":"Y","temporalStart":"2003-01-01","temporalEnd":"2005-12-31","costCenters":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"links":[{"id":414390,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_77609.htm","linkFileType":{"id":5,"text":"html"}},{"id":8527,"rank":3,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/sir/2006/5089/appendix-index.htm","linkFileType":{"id":5,"text":"html"}},{"id":192716,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8526,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5089/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Missouri","city":"Kansas City","otherGeospatial":"Lower Blue River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -94.5375,\n              39.1333\n            ],\n            [\n              -94.5375,\n              38.9917\n            ],\n            [\n              -94.4567,\n              38.9917\n            ],\n            [\n              -94.4567,\n              39.1333\n            ],\n            [\n              -94.5375,\n              39.1333\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad0e4b07f02db6809d1","contributors":{"authors":[{"text":"Kelly, Brian P. 0000-0001-6378-2837 bkelly@usgs.gov","orcid":"https://orcid.org/0000-0001-6378-2837","contributorId":897,"corporation":false,"usgs":true,"family":"Kelly","given":"Brian","email":"bkelly@usgs.gov","middleInitial":"P.","affiliations":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true},{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":289070,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rydlund, Paul H. Jr. 0000-0001-9461-9944 prydlund@usgs.gov","orcid":"https://orcid.org/0000-0001-9461-9944","contributorId":3840,"corporation":false,"usgs":true,"family":"Rydlund","given":"Paul","suffix":"Jr.","email":"prydlund@usgs.gov","middleInitial":"H.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true},{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true},{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"preferred":true,"id":289071,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70161680,"text":"70161680 - 2006 - Salinity tolerance of goldfish, <i>Carassius auratus</i>, a non-native fish in the United States","interactions":[],"lastModifiedDate":"2016-01-05T13:45:06","indexId":"70161680","displayToPublicDate":"2006-09-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1672,"text":"Florida Scientist","active":true,"publicationSubtype":{"id":10}},"title":"Salinity tolerance of goldfish, <i>Carassius auratus</i>, a non-native fish in the United States","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Florida Academy of Sciences","usgsCitation":"Schofield, P., Brown, M.E., and Fuller, P.L., 2006, Salinity tolerance of goldfish, <i>Carassius auratus</i>, a non-native fish in the United States: Florida Scientist, v. 69, no. 4, p. 258-268.","productDescription":"11 p.","startPage":"258","endPage":"268","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":313818,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":313816,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.floridaacademyofsciences.org/pdf/FLSC-69-04.pdf"}],"volume":"69","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568cf749e4b0e7a44bc0f187","contributors":{"authors":[{"text":"Schofield, Pamela J. 0000-0002-8752-2797 pschofield@usgs.gov","orcid":"https://orcid.org/0000-0002-8752-2797","contributorId":127812,"corporation":false,"usgs":true,"family":"Schofield","given":"Pamela J.","email":"pschofield@usgs.gov","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":false,"id":587587,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, Mary E. 0000-0002-5580-137X mbrown@usgs.gov","orcid":"https://orcid.org/0000-0002-5580-137X","contributorId":5688,"corporation":false,"usgs":true,"family":"Brown","given":"Mary","email":"mbrown@usgs.gov","middleInitial":"E.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":587588,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fuller, Pamela L. 0000-0002-9389-9144 pfuller@usgs.gov","orcid":"https://orcid.org/0000-0002-9389-9144","contributorId":3217,"corporation":false,"usgs":true,"family":"Fuller","given":"Pamela","email":"pfuller@usgs.gov","middleInitial":"L.","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":false,"id":587589,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70161470,"text":"70161470 - 2006 - A standard protocol for describing individual-based and agent-based models","interactions":[],"lastModifiedDate":"2016-01-05T12:58:57","indexId":"70161470","displayToPublicDate":"2006-09-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1458,"text":"Ecological Modelling","active":true,"publicationSubtype":{"id":10}},"title":"A standard protocol for describing individual-based and agent-based models","docAbstract":"<p><span>Simulation models that describe autonomous individual organisms (individual based models, IBM) or agents (agent-based models, ABM) have become a widely used tool, not only in ecology, but also in many other disciplines dealing with complex systems made up of autonomous entities. However, there is no standard protocol for describing such simulation models, which can make them difficult to understand and to duplicate. This paper presents a proposed standard protocol, ODD, for describing IBMs and ABMs, developed and tested by 28 modellers who cover a wide range of fields within ecology. This protocol consists of three blocks (Overview, Design concepts, and Details), which are subdivided into seven elements: Purpose, State variables and scales, Process overview and scheduling, Design concepts, Initialization, Input, and Submodels. We explain which aspects of a model should be described in each element, and we present an example to illustrate the protocol in use. In addition, 19 examples are available in an Online Appendix. We consider ODD as a first step for establishing a more detailed common format of the description of IBMs and ABMs. Once initiated, the protocol will hopefully evolve as it becomes used by a sufficiently large proportion of modellers.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.ecolmodel.2006.04.023","usgsCitation":"Grimm, V., Berger, U., Bastiansen, F., Eliassen, S., Ginot, V., Giske, J., Goss-Custard, J., Grand, T., Heinz, S.K., Huse, G., Huth, A., Jepsen, J.U., Jorgensen, C., Mooij, W.M., Muller, B., Pe’er, G., Piou, C., Railsback, S.F., Robbins, A.M., Robbins, M.M., Rossmanith, E., Ruger, N., Strand, E., Souissi, S., Stillman, R.A., Vabo, R., Visser, U., and DeAngelis, D., 2006, A standard protocol for describing individual-based and agent-based models: Ecological Modelling, v. 198, no. 1-2, p. 115-126, https://doi.org/10.1016/j.ecolmodel.2006.04.023.","productDescription":"12 p.","startPage":"115","endPage":"126","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"links":[{"id":313617,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"198","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568cf73be4b0e7a44bc0f12b","contributors":{"authors":[{"text":"Grimm, Volker","contributorId":89656,"corporation":false,"usgs":true,"family":"Grimm","given":"Volker","email":"","affiliations":[],"preferred":false,"id":586426,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berger, Uta","contributorId":59552,"corporation":false,"usgs":true,"family":"Berger","given":"Uta","email":"","affiliations":[],"preferred":false,"id":586427,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bastiansen, Finn","contributorId":151645,"corporation":false,"usgs":false,"family":"Bastiansen","given":"Finn","email":"","affiliations":[],"preferred":false,"id":586428,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Eliassen, Sigrunn","contributorId":151646,"corporation":false,"usgs":false,"family":"Eliassen","given":"Sigrunn","email":"","affiliations":[],"preferred":false,"id":586429,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ginot, Vincent","contributorId":151647,"corporation":false,"usgs":false,"family":"Ginot","given":"Vincent","email":"","affiliations":[],"preferred":false,"id":586430,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Giske, Jarl","contributorId":18498,"corporation":false,"usgs":true,"family":"Giske","given":"Jarl","email":"","affiliations":[],"preferred":false,"id":586431,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Goss-Custard, John","contributorId":151648,"corporation":false,"usgs":false,"family":"Goss-Custard","given":"John","email":"","affiliations":[],"preferred":false,"id":586432,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Grand, Tamara","contributorId":151649,"corporation":false,"usgs":false,"family":"Grand","given":"Tamara","email":"","affiliations":[],"preferred":false,"id":586433,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Heinz, Simone K.","contributorId":151650,"corporation":false,"usgs":false,"family":"Heinz","given":"Simone","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":586434,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Huse, Geir","contributorId":151651,"corporation":false,"usgs":false,"family":"Huse","given":"Geir","email":"","affiliations":[],"preferred":false,"id":586435,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Huth, Andreas","contributorId":151652,"corporation":false,"usgs":false,"family":"Huth","given":"Andreas","email":"","affiliations":[],"preferred":false,"id":586437,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Jepsen, Jane U.","contributorId":151653,"corporation":false,"usgs":false,"family":"Jepsen","given":"Jane","email":"","middleInitial":"U.","affiliations":[],"preferred":false,"id":586438,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Jorgensen, Christian","contributorId":151654,"corporation":false,"usgs":false,"family":"Jorgensen","given":"Christian","email":"","affiliations":[],"preferred":false,"id":586439,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Mooij, Wolf M.","contributorId":94169,"corporation":false,"usgs":true,"family":"Mooij","given":"Wolf","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":586440,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Muller, Birgit","contributorId":100161,"corporation":false,"usgs":true,"family":"Muller","given":"Birgit","email":"","affiliations":[],"preferred":false,"id":586441,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Pe’er, Guy","contributorId":151655,"corporation":false,"usgs":false,"family":"Pe’er","given":"Guy","email":"","affiliations":[],"preferred":false,"id":586442,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Piou, Cyril","contributorId":151656,"corporation":false,"usgs":false,"family":"Piou","given":"Cyril","email":"","affiliations":[],"preferred":false,"id":586443,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Railsback, Steven F.","contributorId":147528,"corporation":false,"usgs":false,"family":"Railsback","given":"Steven","email":"","middleInitial":"F.","affiliations":[{"id":16859,"text":"Lang, Railsback, and Associates","active":true,"usgs":false}],"preferred":false,"id":586444,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Robbins, Andrew M.","contributorId":151657,"corporation":false,"usgs":false,"family":"Robbins","given":"Andrew","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":586445,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"Robbins, Martha M.","contributorId":76599,"corporation":false,"usgs":true,"family":"Robbins","given":"Martha","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":586446,"contributorType":{"id":1,"text":"Authors"},"rank":20},{"text":"Rossmanith, Eva","contributorId":151658,"corporation":false,"usgs":false,"family":"Rossmanith","given":"Eva","email":"","affiliations":[],"preferred":false,"id":586447,"contributorType":{"id":1,"text":"Authors"},"rank":21},{"text":"Ruger, Nadja","contributorId":151659,"corporation":false,"usgs":false,"family":"Ruger","given":"Nadja","email":"","affiliations":[],"preferred":false,"id":586448,"contributorType":{"id":1,"text":"Authors"},"rank":22},{"text":"Strand, Espen","contributorId":91280,"corporation":false,"usgs":true,"family":"Strand","given":"Espen","email":"","affiliations":[],"preferred":false,"id":586449,"contributorType":{"id":1,"text":"Authors"},"rank":23},{"text":"Souissi, Sami","contributorId":151660,"corporation":false,"usgs":false,"family":"Souissi","given":"Sami","email":"","affiliations":[],"preferred":false,"id":586450,"contributorType":{"id":1,"text":"Authors"},"rank":24},{"text":"Stillman, Richard A.","contributorId":151661,"corporation":false,"usgs":false,"family":"Stillman","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":586451,"contributorType":{"id":1,"text":"Authors"},"rank":25},{"text":"Vabo, Rune","contributorId":151662,"corporation":false,"usgs":false,"family":"Vabo","given":"Rune","email":"","affiliations":[],"preferred":false,"id":586452,"contributorType":{"id":1,"text":"Authors"},"rank":26},{"text":"Visser, Ute","contributorId":151663,"corporation":false,"usgs":false,"family":"Visser","given":"Ute","email":"","affiliations":[],"preferred":false,"id":586453,"contributorType":{"id":1,"text":"Authors"},"rank":27},{"text":"DeAngelis, Donald L. 0000-0002-1570-4057 don_deangelis@usgs.gov","orcid":"https://orcid.org/0000-0002-1570-4057","contributorId":147289,"corporation":false,"usgs":true,"family":"DeAngelis","given":"Donald L.","email":"don_deangelis@usgs.gov","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":false,"id":586454,"contributorType":{"id":1,"text":"Authors"},"rank":28}]}}
,{"id":70161549,"text":"70161549 - 2006 - Comment on \"Asymmetric coevolutionary networks facilitate biodiversity maintenance\"","interactions":[],"lastModifiedDate":"2016-01-05T13:04:15","indexId":"70161549","displayToPublicDate":"2006-09-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Comment on \"Asymmetric coevolutionary networks facilitate biodiversity maintenance\"","docAbstract":"<p><span>Bascompte&nbsp;</span><i>et al</i><span>. (Reports, 21 April 2006, p. 431) used network asymmetries to explain mathematical conditions necessary for stability in historic models of mutualism. The Lotka-Volterra equations they used artificially created conditions in which some factor, such as asymmetric interaction strengths, is necessary for community coexistence. We show that a more realistic model incorporating nonlinear functional responses requires no such condition and is consistent with their data.</span></p>","language":"English","publisher":"AAAS","doi":"10.1126/science.1129547","usgsCitation":"Holland, J.N., Okuyama, T., and DeAngelis, D., 2006, Comment on \"Asymmetric coevolutionary networks facilitate biodiversity maintenance\": Science, v. 313, no. 5795, https://doi.org/10.1126/science.1129547.","productDescription":"1 p.","startPage":"1887","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"links":[{"id":313674,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"313","issue":"5795","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568cf73ee4b0e7a44bc0f141","contributors":{"authors":[{"text":"Holland, J. Nathaniel","contributorId":49912,"corporation":false,"usgs":true,"family":"Holland","given":"J.","email":"","middleInitial":"Nathaniel","affiliations":[],"preferred":false,"id":586798,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Okuyama, Toshinori","contributorId":151776,"corporation":false,"usgs":false,"family":"Okuyama","given":"Toshinori","email":"","affiliations":[],"preferred":false,"id":586799,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"DeAngelis, Donald L. 0000-0002-1570-4057 don_deangelis@usgs.gov","orcid":"https://orcid.org/0000-0002-1570-4057","contributorId":147289,"corporation":false,"usgs":true,"family":"DeAngelis","given":"Donald L.","email":"don_deangelis@usgs.gov","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":false,"id":586800,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":79099,"text":"sir20065122 - 2006 - A conceptual model of ground-water flow in the eastern Snake River Plain aquifer at the Idaho National Laboratory and vicinity with implications for contaminant transport","interactions":[],"lastModifiedDate":"2012-03-08T17:16:21","indexId":"sir20065122","displayToPublicDate":"2006-09-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5122","title":"A conceptual model of ground-water flow in the eastern Snake River Plain aquifer at the Idaho National Laboratory and vicinity with implications for contaminant transport","docAbstract":"Ground-water flow in the west-central part of the eastern Snake River Plain aquifer is described in a conceptual model that will be used in numerical simulations to evaluate contaminant transport at the Idaho National Laboratory (INL) and vicinity. The model encompasses an area of 1,940 square miles (mi2) and includes most of the 890 mi2 of the INL. A 50-year history of waste disposal associated with research activities at the INL has resulted in measurable concentrations of waste contaminants in the aquifer. A thorough understanding of the fate and movement of these contaminants in the subsurface is needed by the U.S. Department of Energy to minimize the effect that contaminated ground water may have on the region and to plan effectively for remediation.\r\n\r\nThree hydrogeologic units were used to represent the complex stratigraphy of the aquifer in the model area. Collectively, these hydrogeologic units include at least 65 basalt-flow groups, 5 andesite-flow groups, and 61 sedimentary interbeds. Three rhyolite domes in the model area extend deep enough to penetrate the aquifer. The rhyolite domes are represented in the conceptual model as low permeability, vertical pluglike masses, and are not included as part of the three primary hydrogeologic units. Broad differences in lithology and large variations in hydraulic properties allowed the heterogeneous, anisotropic basalt-flow groups, andesite-flow groups, and sedimentary interbeds to be grouped into three hydrogeologic units that are conceptually homogeneous and anisotropic. Younger rocks, primarily thin, densely fractured basalt, compose hydrogeologic unit 1; younger rocks, primarily of massive, less densely fractured basalt, compose hydrogeologic unit 2; and intermediate-age rocks, primarily of slightly-to-moderately altered, fractured basalt, compose hydrogeologic unit 3. Differences in hydraulic properties among adjacent hydrogeologic units result in much of the large-scale heterogeneity and anisotropy of the aquifer in the model area, and differences in horizontal and vertical hydraulic conductivity in individual hydrogeologic units result in much of the small-scale heterogeneity and anisotropy of the aquifer in the model area.\r\n\r\nThe inferred three-dimensional geometry of the aquifer in the model area is very irregular. Its thickness generally increases from north to south and from west to east and is greatest south of the INL. The interpreted distribution of older rocks that underlie the aquifer indicates large changes in saturated thickness across the model area.\r\n\r\nThe boundaries of the model include physical and artificial boundaries, and ground-water flows across the boundaries may be temporally constant or variable and spatially uniform or nonuniform. Physical boundaries include the water-table boundary, base of the aquifer, and northwest mountain-front boundary. Artificial boundaries include the northeast boundary, southeast-flowline boundary, and southwest boundary. Water flows into the model area as (1) underflow (1,225 cubic feet per second (ft3/s)) from the regional aquifer (northeast boundary-constant and nonuniform), (2) underflow (695 ft3/s) from the tributary valleys and mountain fronts (northwest boundary-constant and nonuniform), (3) precipitation recharge (70 ft3/s) (constant and uniform), streamflow-infiltration recharge (95 ft3/s) (variable and nonuniform), wastewater return flows (6 ft3/s) (variable and nonuniform), and irrigation-infiltration recharge (24 ft3/s) (variable and nonuniform) across the water table (water-table boundary-variable and nonuniform), and (4) upward flow across the base of the aquifer (44 ft3/s) (uniform and constant). The southeast-flowline boundary is represented as a no-flow boundary. Water flows out of the model area as underflow (2,037 ft3/s) to the regional aquifer (southwest boundary-variable and nonuniform) and as ground-water withdrawals (45 ft3/s) (water table boundary-variable and nonuniform).\r\n\r\nGround-water flow i","language":"ENGLISH","doi":"10.3133/sir20065122","usgsCitation":"Ackerman, D.J., Rattray, G.W., Rousseau, J.P., Davis, L.C., and Orr, B.R., 2006, A conceptual model of ground-water flow in the eastern Snake River Plain aquifer at the Idaho National Laboratory and vicinity with implications for contaminant transport: U.S. Geological Survey Scientific Investigations Report 2006-5122, vi, 62 p., https://doi.org/10.3133/sir20065122.","productDescription":"vi, 62 p.","numberOfPages":"68","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":190703,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8531,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5122/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,43 ], [ -114,44.5 ], [ -112,44.5 ], [ -112,43 ], [ -114,43 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b0901","contributors":{"authors":[{"text":"Ackerman, Daniel J.","contributorId":9286,"corporation":false,"usgs":true,"family":"Ackerman","given":"Daniel","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":289084,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rattray, Gordon W. 0000-0002-1690-3218 grattray@usgs.gov","orcid":"https://orcid.org/0000-0002-1690-3218","contributorId":2521,"corporation":false,"usgs":true,"family":"Rattray","given":"Gordon","email":"grattray@usgs.gov","middleInitial":"W.","affiliations":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"preferred":true,"id":289082,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rousseau, Joseph P.","contributorId":22030,"corporation":false,"usgs":true,"family":"Rousseau","given":"Joseph","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":289086,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Davis, Linda C. lcdavis@usgs.gov","contributorId":2539,"corporation":false,"usgs":true,"family":"Davis","given":"Linda","email":"lcdavis@usgs.gov","middleInitial":"C.","affiliations":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"preferred":true,"id":289083,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Orr, Brennon R.","contributorId":18747,"corporation":false,"usgs":true,"family":"Orr","given":"Brennon","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":289085,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70242045,"text":"70242045 - 2006 - Catastrophe, recovery and range limitation in NE Pacific kelp forests: a large-scale perspective","interactions":[],"lastModifiedDate":"2023-04-05T14:05:17.595285","indexId":"70242045","displayToPublicDate":"2006-08-29T08:53:01","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2636,"text":"MEPS","active":true,"publicationSubtype":{"id":10}},"title":"Catastrophe, recovery and range limitation in NE Pacific kelp forests: a large-scale perspective","docAbstract":"<p><span>The 1997–98 El Niño was one of the strongest on record and resulted in widespread losses of the giant kelp&nbsp;</span><i>Macrocystis pyrifera</i><span>&nbsp;(Agardh) along the west coast of North America. Drawing on a rich history of studies that have shown abnormally large waves and warm nutrient-poor water associated with El Niños to negatively impact giant kelp populations at some locations in southern and Baja California, we examined (1) how these impacts scale up when considered across the species’ geographic range in the NE Pacific Ocean and (2) if these impacts are generalizable over broad spatial scales. Working at 56 sites in 14 study locations over a 3 yr period (1997 to 2000), we examined how giant kelp populations were impacted by and recovered following the 1997–98 El Niño over a ~1500 km span along the west coast of North America. Our results indicate that while nearly all giant kelp disappeared from the southern one-third of the species’ range along the coast of Baja California, Mexico, and heavy losses occurred throughout the central one-third of the species’ range in southern California, USA, only minor impacts were observed throughout the northern one-third of the species’ range in central California. Further, although highly variable among regions, these impacts were similar and generalizable among locations within each region. Our results also suggest that, as has been observed in local-scale studies, this large-scale variability in giant kelp mortality was driven by large-scale patterns in ocean temperature (nutrient concentration) and wave intensity. Recovery following El Niño, in contrast, was variable at multiple spatial scales and although not directly tested here, presumably influenced by numerous factors such as proximity to upwelling areas, competition with other algae, grazing, and propagule availability. Further, variability in the rates of recovery among locations resulted in a generally slow recovery of giant kelp throughout most of Baja California, and residual large-scale impacts of the El Niño were still evident 2 yr after the El Niño ended. As global climate change may lead to increases in the frequency and intensity of El Niños, our findings have broad implications for the ways in which ecosystems might be expected to respond to them and provide a measure by which their impacts to giant kelp ecosystems may be compared among events.</span></p>","language":"English","publisher":"Inter-research Science Publisher","doi":"10.3354/meps320079","usgsCitation":"Edwards, M., and Estes, J.A., 2006, Catastrophe, recovery and range limitation in NE Pacific kelp forests: a large-scale perspective: MEPS, v. 320, p. 79-87, https://doi.org/10.3354/meps320079.","productDescription":"9 p.","startPage":"79","endPage":"87","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":477317,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3354/meps320079","text":"Publisher Index Page"},{"id":415228,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico, United States","otherGeospatial":"Pacific Ocean","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -113.90206252929181,\n              26.93094746896577\n            ],\n            [\n              -114.67166568069763,\n              27.662790573703916\n            ],\n            [\n              -113.9608437206309,\n              27.89072172650296\n            ],\n            [\n              -114.11835149746376,\n              28.671108944957027\n            ],\n            [\n              -115.65081281043813,\n              29.844869047267252\n            ],\n            [\n              -117.020006532164,\n              32.527864990612954\n            ],\n            [\n              -117.5958661248973,\n              33.62479806113656\n            ],\n            [\n              -118.48046528982154,\n              34.20260681727105\n            ],\n            [\n              -120.39217160783527,\n              34.59948659241695\n            ],\n            [\n              -120.71543441789687,\n              35.10449911869162\n            ],\n            [\n              -121.84920107488243,\n              36.3907045697502\n            ],\n            [\n              -121.79003067031844,\n              36.86030284506636\n            ],\n            [\n              -122.30373224598206,\n              37.13219674532428\n            ],\n            [\n              -122.66821292412838,\n              38.21062794517695\n            ],\n            [\n              -123.67348855772319,\n              39.00685957982992\n            ],\n            [\n              -124.30516118931818,\n              40.35184362323267\n            ],\n            [\n              -128.4195484715151,\n              40.01922675644212\n            ],\n            [\n              -124.36941509517033,\n              34.13294893416567\n            ],\n            [\n              -117.80640147383887,\n              27.848723477337685\n            ],\n            [\n              -113.87499943643222,\n              25.87023809119225\n            ],\n            [\n              -113.90206252929181,\n              26.93094746896577\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"320","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Edwards, Matthew S.","contributorId":53293,"corporation":false,"usgs":true,"family":"Edwards","given":"Matthew S.","affiliations":[],"preferred":false,"id":868696,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Estes, James A. jim_estes@usgs.gov","contributorId":53325,"corporation":false,"usgs":true,"family":"Estes","given":"James","email":"jim_estes@usgs.gov","middleInitial":"A.","affiliations":[{"id":6949,"text":"University of California, Santa Cruz","active":true,"usgs":false},{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":868697,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":78888,"text":"ofr20061198 - 2006 - Applicability of terrestrial LIDAR scanning for scientific studies in Grand Canyon National Park, Arizona","interactions":[],"lastModifiedDate":"2014-10-09T15:45:51","indexId":"ofr20061198","displayToPublicDate":"2006-08-28T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-1198","title":"Applicability of terrestrial LIDAR scanning for scientific studies in Grand Canyon National Park, Arizona","docAbstract":"<p>In November 2004, an experimental high flow release of water from Glen Canyon Dam into the Colorado River through Grand Canyon National Park in Arizona was conducted. The goal of the experiment was to evaluate the use of high flow events as a management tool for the preservation and restoration of natural resources in the Colorado River below Glen Canyon Dam. The U.S. Geological Survey (USGS), Grand Canyon Monitoring and Research Center (GCMRC) located in Flagstaff, Arizona performed oversight of all aspects of scientific data collection including suspended sediment transport studies, biological population variations, effects on archaeological resources, and morphological studies of river sand bars.</p>\n<br>\n<p>As part of the experimental high flow studies, the USGS Coastal and Marine Geology (CMG) team was invited to participate to test the effectiveness of utilizing terrestrial LIDAR technology for gathering morphological data on sand bars, biological habitats, and archaeological sites. The CMG is equipped with a terrestrial LIDAR unit and has used the technique in a variety of terrains to gather high-resolution morphological data. A three-member team from CMG participated in the experiment, joining a GCMRC team on a river trip from November 18 to November 21, 2004.</p>\n<br>\n<p>This report begins with a brief description of the LIDAR technique and then outlines the data collected, processing required, and results for three study areas located within the Grand Canyon. Specifically, studies were performed at the Mile 30 Sand Bar, at Vaseys Paradise (Mile 32), and at the Mile 66 Palisades Archaeological Site. Conclusions and recommendations for utilizing terrestrial LIDAR for future studies at each of these sites are also included.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20061198","usgsCitation":"Collins, B., and Kayen, R., 2006, Applicability of terrestrial LIDAR scanning for scientific studies in Grand Canyon National Park, Arizona (Version 1.0): U.S. Geological Survey Open-File Report 2006-1198, v, 27 p., https://doi.org/10.3133/ofr20061198.","productDescription":"v, 27 p.","numberOfPages":"32","costCenters":[{"id":322,"text":"Grand Canyon Monitoring and Research Center","active":false,"usgs":true}],"links":[{"id":192528,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20061198.PNG"},{"id":8509,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1198/","linkFileType":{"id":5,"text":"html"}},{"id":295194,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2006/1198/of2006-1198.pdf"}],"country":"United States","state":"Arizona","otherGeospatial":"Grand Canyon National Park","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67abbc","contributors":{"authors":[{"text":"Collins, Brian D.","contributorId":71641,"corporation":false,"usgs":true,"family":"Collins","given":"Brian D.","affiliations":[],"preferred":false,"id":289000,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kayen, Robert","contributorId":12030,"corporation":false,"usgs":true,"family":"Kayen","given":"Robert","affiliations":[],"preferred":false,"id":288999,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":78918,"text":"ofr20061165 - 2006 - Preliminary surficial geologic map database of the Amboy 30 x 60 minute quadrangle, California","interactions":[],"lastModifiedDate":"2012-02-10T00:11:37","indexId":"ofr20061165","displayToPublicDate":"2006-08-28T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-1165","title":"Preliminary surficial geologic map database of the Amboy 30 x 60 minute quadrangle, California","docAbstract":"The surficial geologic map database of the Amboy 30x60 minute quadrangle presents characteristics of surficial materials for an area approximately 5,000 km2 in the eastern Mojave Desert of California. This map consists of new surficial mapping conducted between 2000 and 2005, as well as compilations of previous surficial mapping. Surficial geology units are mapped and described based on depositional process and age categories that reflect the mode of deposition, pedogenic effects occurring post-deposition, and, where appropriate, the lithologic nature of the material.\r\n\r\nThe physical properties recorded in the database focus on those that drive hydrologic, biologic, and physical processes such as particle size distribution (PSD) and bulk density. This version of the database is distributed with point data representing locations of samples for both laboratory determined physical properties and semi-quantitative field-based information. Future publications will include the field and laboratory data as well as maps of distributed physical properties across the landscape tied to physical process models where appropriate.\r\n\r\nThe database is distributed in three parts: documentation, spatial map-based data, and printable map graphics of the database. Documentation includes this file, which provides a discussion of the surficial geology and describes the format and content of the map data, a database 'readme' file, which describes the database contents, and FGDC metadata for the spatial map information. Spatial data are distributed as Arc/Info coverage in ESRI interchange (e00) format, or as tabular data in the form of DBF3-file (.DBF) file formats. Map graphics files are distributed as Postscript and Adobe Portable Document Format (PDF) files, and are appropriate for representing a view of the spatial database at the mapped scale. ","language":"ENGLISH","doi":"10.3133/ofr20061165","usgsCitation":"Bedford, D., Miller, D., and Phelps, G., 2006, Preliminary surficial geologic map database of the Amboy 30 x 60 minute quadrangle, California: U.S. Geological Survey Open-File Report 2006-1165, v, 28 p.; 1 map sheet, 60 x 29 in., https://doi.org/10.3133/ofr20061165.","productDescription":"v, 28 p.; 1 map sheet, 60 x 29 in.","numberOfPages":"33","additionalOnlineFiles":"Y","costCenters":[{"id":647,"text":"Western Earth Surface Processes","active":false,"usgs":true}],"links":[{"id":110669,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_77605.htm","linkFileType":{"id":5,"text":"html"},"description":"77605"},{"id":192876,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8513,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1165/","linkFileType":{"id":5,"text":"html"}},{"id":8515,"rank":9999,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/2006/1165/of06-1165_1a.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":8516,"rank":9999,"type":{"id":23,"text":"Spatial Data"},"url":"https://pubs.usgs.gov/of/2006/1165/of06-1165_3.zip"},{"id":8514,"rank":9999,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2006/1165/of06-1165_1d.html","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","projection":"UTM Zone 11 NAD 27","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116,34.5 ], [ -116,35 ], [ -115,35 ], [ -115,34.5 ], [ -116,34.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aabe4b07f02db669aa7","contributors":{"authors":[{"text":"Bedford, David R.","contributorId":26352,"corporation":false,"usgs":true,"family":"Bedford","given":"David R.","affiliations":[],"preferred":false,"id":289004,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, David M. 0000-0003-3711-0441 dmiller@usgs.gov","orcid":"https://orcid.org/0000-0003-3711-0441","contributorId":1707,"corporation":false,"usgs":true,"family":"Miller","given":"David M.","email":"dmiller@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":289002,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Phelps, Geoffrey A.","contributorId":17262,"corporation":false,"usgs":true,"family":"Phelps","given":"Geoffrey A.","affiliations":[],"preferred":false,"id":289003,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":78920,"text":"ofr20061197 - 2006 - Gravity, magnetic, and physical property data in the Smoke Creek Desert area, northwest Nevada","interactions":[],"lastModifiedDate":"2012-02-10T00:11:41","indexId":"ofr20061197","displayToPublicDate":"2006-08-28T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-1197","title":"Gravity, magnetic, and physical property data in the Smoke Creek Desert area, northwest Nevada","docAbstract":"The Smoke Creek Desert, located approximately 100 km (60 mi) north of Reno near the California-Nevada border, is a large basin situated along the northernmost parts of the Walker Lane Belt (Stewart, 1988), a physiographic province defined by northwest-striking topographic features and strike-slip faulting. Because geologic framework studies play an important role in understanding the hydrology of the Smoke Creek Desert, a geologic and geophysical effort was begun to help determine basin geometry, infer structural features, and estimate depth to Pre-Cenozoic rocks, or basement.\r\n\r\nIn May and June of 2004, and June of 2005, the U.S. Geological Survey (USGS) collected 587 new gravity stations, more than 160 line-kilometers (100 line-miles) of truck-towed magnetometer data, and 111 rock property samples in the Smoke Creek Desert and vicinity in northwest Nevada, as part of an effort to characterize its hydrogeologic framework. In the Smoke Creek Desert area, gravity highs occur over rocks of the Skedaddle Mountains, Fox Range, Granite Range, and over portions of Tertiary volcanic rocks in the Buffalo Hills. These gravity highs likely reflect basement rocks, either exposed at the surface or buried at shallow depths. The southern Smoke Creek Desert corresponds to a 25-mGal isostatic gravity low, which corresponds with a basin depth of approximately 2 km.\r\n\r\nMagnetic highs are likely due to granitic, andesitic, and metavolcanic rocks, whereas magnetic lows are probably associated with less magnetic gneiss and metasedimentary rocks in the region. Three distinctive patterns of magnetic anomalies occur throughout the Smoke Creek Desert and Squaw Creek Valley, likely reflecting three different geological and structural settings.","language":"ENGLISH","doi":"10.3133/ofr20061197","usgsCitation":"Tilden, J.E., Ponce, D.A., Glen, J., Chuchel, B.A., Tushman, K., and Duvall, A., 2006, Gravity, magnetic, and physical property data in the Smoke Creek Desert area, northwest Nevada (Version 1.0): U.S. Geological Survey Open-File Report 2006-1197, ii, 33 p.; , https://doi.org/10.3133/ofr20061197.","productDescription":"ii, 33 p.; ","numberOfPages":"35","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":305,"text":"Geology Division","active":false,"usgs":true}],"links":[{"id":190518,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8517,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1197/","linkFileType":{"id":5,"text":"html"}},{"id":8518,"rank":9999,"type":{"id":23,"text":"Spatial Data"},"url":"https://pubs.usgs.gov/of/2006/1197/data/","linkFileType":{"id":5,"text":"html"}},{"id":8519,"rank":9999,"type":{"id":25,"text":"Version History"},"url":"https://pubs.usgs.gov/of/2006/1197/version_history.txt","linkFileType":{"id":2,"text":"txt"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.11805555555554,40.13444444444444 ], [ -120.11805555555554,40.918055555555554 ], [ -119.25111111111111,40.918055555555554 ], [ -119.25111111111111,40.13444444444444 ], [ -120.11805555555554,40.13444444444444 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671fbe","contributors":{"authors":[{"text":"Tilden, Janet E. 0000-0002-4759-3814","orcid":"https://orcid.org/0000-0002-4759-3814","contributorId":20423,"corporation":false,"usgs":true,"family":"Tilden","given":"Janet","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":289008,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ponce, David A. 0000-0003-4785-7354 ponce@usgs.gov","orcid":"https://orcid.org/0000-0003-4785-7354","contributorId":1049,"corporation":false,"usgs":true,"family":"Ponce","given":"David","email":"ponce@usgs.gov","middleInitial":"A.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":289005,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Glen, Jonathan M. G.","contributorId":45756,"corporation":false,"usgs":true,"family":"Glen","given":"Jonathan M. G.","affiliations":[],"preferred":false,"id":289009,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chuchel, Bruce A. chuchel@usgs.gov","contributorId":2415,"corporation":false,"usgs":true,"family":"Chuchel","given":"Bruce","email":"chuchel@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":289006,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Tushman, Kira","contributorId":70065,"corporation":false,"usgs":true,"family":"Tushman","given":"Kira","email":"","affiliations":[],"preferred":false,"id":289010,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Duvall, Alison","contributorId":7780,"corporation":false,"usgs":true,"family":"Duvall","given":"Alison","affiliations":[],"preferred":false,"id":289007,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":78917,"text":"ofr20061238 - 2006 - Geologic map of the Kings Mountain and Grover quadrangles, Cleveland and Gaston Counties, North Carolina, and Cherokee and York Counties, South Carolina","interactions":[],"lastModifiedDate":"2012-02-10T00:11:45","indexId":"ofr20061238","displayToPublicDate":"2006-08-28T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-1238","title":"Geologic map of the Kings Mountain and Grover quadrangles, Cleveland and Gaston Counties, North Carolina, and Cherokee and York Counties, South Carolina","docAbstract":"This geologic map of the Kings Mountain and Grover 7.5-minute quadrangles, N.C.-S.C., straddles a regional geological boundary between the Inner Piedmont and Carolina terranes. The Kings Mountain sequence (informal name) on the western flank of the Carolina terrane in this area includes the Neoproterozoic Battleground and Blacksburg Formations. The Battleground Formation has a lower part consisting of metavolcanic rocks and interlayered schist, and an upper part consisting of quartz-sericite phyllite and schist interlayered with quartz-pebble metaconglomerate, aluminous quartzite, micaceous quartzite, manganiferous rock, and metavolcanic rocks. The Blacksburg Formation consists of phyllitic metasiltstone interlayered with thinner units of marble, laminated micaceous quartzite, hornblende gneiss, and amphibolite. Layered metamorphic rocks of the Inner Piedmont terrane include muscovite-biotite gneiss, muscovite schist, and amphibolite. The Kings Mountain sequence has been intruded by metatonalite and metatrondhjemite (Neoproterozoic), metadiorite and metagabbro (Paleozoic), and High Shoals Granite (Pennsylvanian). Layered metamorphic rocks of the Inner Piedmont in this area have been intruded by Toluca Granite (Ordovician?), Cherryville Granite and associated pegmatite (Mississippian), and spodumene pegmatite (Mississippian). Diabase dikes (early Jurassic) are locally present throughout the area. Ductile fault zones of regional scale include the Kings Mountain and Kings Creek shear zones. In this area, the Kings Mountain shear zone forms the boundary between the Inner Piedmont and Carolina terranes, and the Kings Creek shear zone separates the Battleground Formation from the Blacksburg Formation. Structural styles change across the Kings Mountain shear zone from steeply-dipping layers, foliations, and folds on the southeast to gently- and moderately-dipping layers, foliations, and recumbent folds on the northwest. Mineral assemblages in the Kings Mountain sequence show a westward decrease from upper amphibolite facies (sillimanite zone) near the High Shoals Granite on the east side of the map to greenschist (epidote-amphibolite) facies in the south-central part of the area near the Kings Mountain shear zone. Amphibolite-facies mineral assemblages in the Inner Piedmont terrane increase in grade from the kyanite zone near the Kings Mountain shear zone to the sillimanite zone in the northwest part of the map. Surficial deposits include alluvium in the stream valleys and colluvium along ridges and steep slopes. These quadrangles are unusual in their richness and variety of mineral deposits, which include spodumene (lithium), cassiterite (tin), mica, feldspar, silica, clay, marble, kyanite and sillimanite, barite, manganese, sand and gravel, gold, pyrite, and iron. (Abstract from pamphlet.)","language":"ENGLISH","doi":"10.3133/ofr20061238","usgsCitation":"Horton, J., 2006, Geologic map of the Kings Mountain and Grover quadrangles, Cleveland and Gaston Counties, North Carolina, and Cherokee and York Counties, South Carolina (Version 1.0): U.S. Geological Survey Open-File Report 2006-1238, 1 map sheet, 60 x 35.5 in.; pamphlet, 17 p., https://doi.org/10.3133/ofr20061238.","productDescription":"1 map sheet, 60 x 35.5 in.; pamphlet, 17 p.","numberOfPages":"17","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":305,"text":"Geology Division","active":false,"usgs":true}],"links":[{"id":110670,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_77607.htm","linkFileType":{"id":5,"text":"html"},"description":"77607"},{"id":8510,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1238/","linkFileType":{"id":5,"text":"html"}},{"id":195752,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8511,"rank":9999,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2006/1238/metadata.zip"},{"id":8512,"rank":9999,"type":{"id":23,"text":"Spatial Data"},"url":"https://pubs.usgs.gov/of/2006/1238/shapefiles.zip"}],"scale":"24000","projection":"UTM Zone 17 NAD 27","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -81.5,35.11694444444444 ], [ -81.5,35.25 ], [ -81.25,35.25 ], [ -81.25,35.11694444444444 ], [ -81.5,35.11694444444444 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696662","contributors":{"authors":[{"text":"Horton, J. Wright Jr. 0000-0001-6756-6365 whorton@usgs.gov","orcid":"https://orcid.org/0000-0001-6756-6365","contributorId":423,"corporation":false,"usgs":true,"family":"Horton","given":"J. Wright","suffix":"Jr.","email":"whorton@usgs.gov","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":false,"id":289001,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":78581,"text":"sir20065142 - 2006 - Occurrence, distribution, loads, and yields of selected pesticides in the Little River basin, Kentucky, 2003-04","interactions":[],"lastModifiedDate":"2012-03-08T17:16:24","indexId":"sir20065142","displayToPublicDate":"2006-08-24T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5142","title":"Occurrence, distribution, loads, and yields of selected pesticides in the Little River basin, Kentucky, 2003-04","docAbstract":"Water resources in the Little River Basin are potentially vulnerable to applications of pesticides associated with both agricultural and nonagricultural activities, because much of the basin is characterized by karst topography. Concerns about water quality resulting from pesticide use in karst areas and lack of data on concentrations of pesticides in surface water led to further investigation of water quality in the Little River Basin, which includes about 600 square miles in Christian and Trigg Counties and a portion of Caldwell County in western Kentucky. Water samples were collected in streams in the Little River Basin, Kentucky during 2003-04 as part of a study conducted in cooperation with the Kentucky Department of Agriculture. The objectives of the study were to assess the occurrence and distribution of pesticides, to evaluate the spatial and seasonal variability of pesticides, and to evaluate loads and yields of selected pesticides in the basin. A total of 91 water samples was collected at 4 fixed-network sites from March through November 2003 and from February through November 2004. An additional 20 samples were collected at 5 synoptic-network sites within the same period.\r\n\r\nTwenty-four pesticides were detected of the 127 pesticides analyzed in the stream samples. Of the 24 detected pesticides, 15 were herbicides, 7 were insecticides, and 2 were fungicides. The most commonly detected pesticides-atrazine, simazine, metolachlor, and acetochlor-were those most heavily used on crops during the study. Atrazine and simazine were detected in 100 percent of all surface-water samples, and metolachlor and acetochlor were detected in more than 45 percent. The pesticide degradate, deethylatrazine, was detected in 100 percent of the samples. Only one nonagricultural herbicide, prometon, was detected in more than 50 percent of the samples. Diazinon, the most commonly detected insecticide, was found in 25 percent of all samples and was found at all sites except Casey Creek. Metalaxyl was the most commonly detected fungicide (14 percent); most detections were in samples from the Sinking Fork subbasin.\r\n\r\nConcentrations of herbicides were highest following application in the spring (March-May). In contrast, insecticides typically were present during the summer (June-August). The most commonly detected pesticides in the Little River Basin were found at low concentrations in streams year-round. Atrazine and simazine (row-crop herbicides) had the highest measured concentrations (22 and 6.1 micrograms per liter (?g/L), respectively) and were the most heavily applied herbicides in the basin. Metolachlor also was heavily applied in the basin, but measured concentrations did not exceed 0.32 ?g/L. The insecticide, Malathion, was only detected in 4 percent of the samples, although it was heavily applied in the basin during 2003-04. Most detections of pesticides were at low concentrations in relation to drinking-water standards and guidelines established for the protection of aquatic life. Only two pesticide compounds--atrazine and simazine--exceeded the U.S. Environmental Protection Agency (USEPA) standards for drinking water. Atrazine exceeded the USEPA's maximum contaminant level (MCL) 19 times in 111 detections; simazine exceeded the established MCL 2 times in 111 detections. These exceedences occurred in the spring. Concentrations of atrazine also exceeded the established aquatic-life criterion (1.8 ?g/L) in 32 samples collected from all sites.\r\n\r\nConcentrations of deethylatrazine, an herbicide-transformation compound, tended to follow the same monthly concentration pattern as its parent compound (atrazine), but concentrations of deethylatrazine were lower than those of atrazine. Atrazine may have been present in the soil much longer at these sites, which might have allowed microbial populations to transform atrazine into deethylatrazine.\r\n\r\nA statistical comparison of concentrations of selected pesticides among four fixed-network sites ","language":"ENGLISH","doi":"10.3133/sir20065142","usgsCitation":"Crain, A.S., 2006, Occurrence, distribution, loads, and yields of selected pesticides in the Little River basin, Kentucky, 2003-04: U.S. Geological Survey Scientific Investigations Report 2006-5142, vi, 25 p., https://doi.org/10.3133/sir20065142.","productDescription":"vi, 25 p.","numberOfPages":"31","temporalStart":"2003-01-01","temporalEnd":"2004-12-31","costCenters":[{"id":354,"text":"Kentucky Water Science Center","active":true,"usgs":true}],"links":[{"id":195751,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8499,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5142/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88,36.7 ], [ -88,37 ], [ -87.33333333333333,37 ], [ -87.33333333333333,36.7 ], [ -88,36.7 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db69209c","contributors":{"authors":[{"text":"Crain, Angela S. 0000-0003-0969-6238 ascrain@usgs.gov","orcid":"https://orcid.org/0000-0003-0969-6238","contributorId":3090,"corporation":false,"usgs":true,"family":"Crain","given":"Angela","email":"ascrain@usgs.gov","middleInitial":"S.","affiliations":[{"id":27231,"text":"Indiana-Kentucky Water Science Center","active":true,"usgs":true},{"id":354,"text":"Kentucky Water Science Center","active":true,"usgs":true}],"preferred":true,"id":288964,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":78578,"text":"sir20065159 - 2006 - Monitoring and modeling to predict Escherichia coli at Presque Isle Beach 2, City of Erie, Erie County, Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-06T14:06:27","indexId":"sir20065159","displayToPublicDate":"2006-08-22T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5159","title":"Monitoring and modeling to predict Escherichia coli at Presque Isle Beach 2, City of Erie, Erie County, Pennsylvania","docAbstract":"The Lake Erie shoreline in Pennsylvania spans nearly 40 miles and is a valuable recreational resource for Erie County. Nearly 7 miles of the Lake Erie shoreline lies within Presque Isle State Park in Erie, Pa. Concentrations of Escherichia coli (E. coli) bacteria at permitted Presque Isle beaches occasionally exceed the single-sample bathing-water standard, resulting in unsafe swimming conditions and closure of the beaches.\r\n\r\nE. coli concentrations and other water-quality and environmental data collected at Presque Isle Beach 2 during the 2004 and 2005 recreational seasons were used to develop models using tobit regression analyses to predict E. coli concentrations. All variables statistically related to E. coli concentrations were included in the initial regression analyses, and after several iterations, only those explanatory variables that made the models significantly better at predicting E. coli concentrations were included in the final models. Regression models were developed using data from 2004, 2005, and the combined 2-year dataset. Variables in the 2004 model and the combined 2004-2005 model were log10 turbidity, rain weight, wave height (calculated), and wind direction. Variables in the 2005 model were log10 turbidity and wind direction. Explanatory variables not included in the final models were water temperature, streamflow, wind speed, and current speed; model results indicated these variables did not meet significance criteria at the 95-percent confidence level (probabilities were greater than 0.05). The predicted E. coli concentrations produced by the models were used to develop probabilities that concentrations would exceed the single-sample bathing-water standard for E. coli of 235 colonies per 100 milliliters. Analysis of the exceedence probabilities helped determine a threshold probability for each model, chosen such that the correct number of exceedences and nonexceedences was maximized and the number of false positives and false negatives was minimized. Future samples with computed exceedence probabilities higher than the selected threshold probability, as determined by the model, will likely exceed the E. coli standard and a beach advisory or closing may need to be issued; computed exceedence probabilities lower than the threshold probability will likely indicate the standard will not be exceeded. Additional data collected each year can be used to test and possibly improve the model. This study will aid beach managers in more rapidly determining when waters are not safe for recreational use and, subsequently, when to issue beach advisories or closings.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, Virginia","doi":"10.3133/sir20065159","usgsCitation":"Zimmerman, T.M., 2006, Monitoring and modeling to predict Escherichia coli at Presque Isle Beach 2, City of Erie, Erie County, Pennsylvania: U.S. Geological Survey Scientific Investigations Report 2006-5159, iv, 15 p., https://doi.org/10.3133/sir20065159.","productDescription":"iv, 15 p.","numberOfPages":"19","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":190977,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8492,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5159/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Pennsylvania","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.83333333333333,42 ], [ -80.83333333333333,42.833333333333336 ], [ -80,42.833333333333336 ], [ -80,42 ], [ -80.83333333333333,42 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624c17","contributors":{"authors":[{"text":"Zimmerman, Tammy M. 0000-0003-0842-6981 tmzimmer@usgs.gov","orcid":"https://orcid.org/0000-0003-0842-6981","contributorId":2359,"corporation":false,"usgs":true,"family":"Zimmerman","given":"Tammy","email":"tmzimmer@usgs.gov","middleInitial":"M.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":false,"id":288958,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":78580,"text":"ds199 - 2006 - Digital geologic map and GIS database of Venezuela","interactions":[],"lastModifiedDate":"2012-02-02T00:14:14","indexId":"ds199","displayToPublicDate":"2006-08-22T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"199","title":"Digital geologic map and GIS database of Venezuela","docAbstract":"The digital geologic map and GIS database of Venezuela captures GIS compatible geologic and hydrologic data from the 'Geologic Shaded Relief Map of Venezuela,' which was released online as U.S. Geological Survey Open-File Report 2005-1038. Digital datasets and corresponding metadata files are stored in ESRI geodatabase format; accessible via ArcGIS 9.X. Feature classes in the geodatabase include geologic unit polygons, open water polygons, coincident geologic unit linework (contacts, faults, etc.) and non-coincident geologic unit linework (folds, drainage networks, etc.). Geologic unit polygon data were attributed for age, name, and lithologic type following the Lexico Estratigrafico de Venezuela. All digital datasets were captured from source data at 1:750,000. Although users may view and analyze data at varying scales, the authors make no guarantee as to the accuracy of the data at scales larger than 1:750,000.","language":"ENGLISH","doi":"10.3133/ds199","collaboration":"See also OFR 2005-1038","usgsCitation":"Garrity, C.P., Hackley, P.C., and Urbani, F., 2006, Digital geologic map and GIS database of Venezuela (Version 1.0): U.S. Geological Survey Data Series 199, Spatial database, https://doi.org/10.3133/ds199.","productDescription":"Spatial database","onlineOnly":"Y","costCenters":[],"links":[{"id":190978,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8496,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/2006/199/","linkFileType":{"id":5,"text":"html"}},{"id":8497,"rank":9999,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/ds/2006/199/README.txt","linkFileType":{"id":2,"text":"txt"}},{"id":8498,"rank":9999,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/ds/2006/199/USGS_06_DS_199.zip"}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a97e4b07f02db65ade2","contributors":{"authors":[{"text":"Garrity, Christopher P. 0000-0002-5565-1818 cgarrity@usgs.gov","orcid":"https://orcid.org/0000-0002-5565-1818","contributorId":644,"corporation":false,"usgs":true,"family":"Garrity","given":"Christopher","email":"cgarrity@usgs.gov","middleInitial":"P.","affiliations":[{"id":5061,"text":"National Cooperative Geologic Mapping and Landslide Hazards","active":true,"usgs":true},{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":288962,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hackley, Paul C. 0000-0002-5957-2551 phackley@usgs.gov","orcid":"https://orcid.org/0000-0002-5957-2551","contributorId":592,"corporation":false,"usgs":true,"family":"Hackley","given":"Paul","email":"phackley@usgs.gov","middleInitial":"C.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true},{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"preferred":true,"id":288961,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Urbani, Franco","contributorId":67163,"corporation":false,"usgs":true,"family":"Urbani","given":"Franco","email":"","affiliations":[],"preferred":false,"id":288963,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":78579,"text":"sir20055250 - 2006 - Sources of water to wells in updip areas of the Wenonah-Mount Laurel aquifer, Gloucester and Camden Counties, New Jersey","interactions":[],"lastModifiedDate":"2012-03-08T17:16:18","indexId":"sir20055250","displayToPublicDate":"2006-08-22T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5250","title":"Sources of water to wells in updip areas of the Wenonah-Mount Laurel aquifer, Gloucester and Camden Counties, New Jersey","docAbstract":"Since 1996, when the New Jersey Department of Environmental Protection (NJDEP) restricted ground-water withdrawals from the Potomac-Raritan-Magothy aquifer system in the southern New Jersey Coastal Plain as a result of excessive drawdown, Coastal Plain communities have been interested in developing alternate sources of water supply for their residents. The use of ground water from areas near the updip parts of the overlying confined aquifers where withdrawals are not restricted is being considered to meet the demand for drinking water. Concerns have arisen, however, regarding the potential effects of increased withdrawals from these areas on ground-water flow to streams and wetlands as well as to the deeper, confined parts of the aquifers. Therefore, the U.S. Geological Survey, in cooperation with the NJDEP, conducted a study to investigate the sources of water to currently inactive wells in the updip part of the Wenonah-Mount Laurel aquifer in Gloucester and Camden Counties, New Jersey. Of particular interest is whether the primary source of the increased withdrawals is likely to be the aquifer outcrop or the downdip, confined part of the aquifer.\r\n\r\nThe outcrop of the Wenonah-Mount Laurel aquifer covers nearly 8 mi2 (square miles), or about 46 percent of Deptford Township's 17.56-mi2 area. The Deptford Township Municipal Utilities Authority owns six currently (2005) inactive wells in the Wenonah-Mount Laurel aquifer at the southeastern boundary of Deptford Township, 1.25 mi (miles) from the outcrop. For the purposes of this study, an existing ground-water-flow model of the New Jersey Coastal Plain aquifers was used to simulate ground-water-flow conditions in Gloucester and Camden Counties in 1998.\r\n\r\nTwo alternative withdrawal scenarios were superimposed on the results of the 1998 simulation. In the first (the 'full-allocation' scenario), full-allocation withdrawal rates established by the NJDEP were applied to 45 existing wells in the Deptford Township area. In the second (the 'additional-withdrawal' scenario), the full-allocation scenario was modified by adding an additional withdrawal of 1.62 million gallons per day from the six inactive Deptford Township withdrawal wells.\r\n\r\nSimulated drawdown for the full-allocation scenario is zero to near zero in Deptford Township. Changes are greatest downdip from Deptford Township, where a broad area of 5- to 10-ft (feet) drawdowns is simulated; maximum drawdown at the center of the cone of depression is 20 ft. Water levels declined as much as 10 ft around individual wells whose current withdrawals are only a small percentage of their allotted allocation.\r\n\r\nSimulated drawdown for the additional-withdrawal scenario exceeds 40 ft and is centered around the six inactive Deptford Township withdrawal wells. The area in which the simulated drawdown is 5 ft extends approximately 3.75 mi downdip from the wells and 2 mi updip, into the outcrop.\r\n\r\nWater budgets based on the simulation results for the full-allocation and additional-withdrawal scenarios were calculated and compared, with particular focus on a 75-mi2 area in and around Deptford Township that includes the outcrop of the Wenonah-Mount Laurel aquifer and part of the area downdip from the outcrop (budget zone 2). The comparison of the two water budgets for zone 2 shows that 46 percent of the withdrawals from the six inactive Deptford Township wells would result from reduced stream base flow in the outcrop of the Wenonah-Mount Laurel aquifer and 35 percent would result from increased downward flow from the overlying Vincentown aquifer. Four percent would result from increased flow from the downdip areas of the Wenonah-Mount Laurel aquifer, 5 percent would result from decreased flow to the downdip areas of the Wenonah-Mount Laurel aquifer, and 5 percent would result from decreased flow to the underlying Englishtown aquifer system. The remaining 4 percent was attributed to decreased upward flow to the overlying Vincentown aquifer.\r\n\r","language":"ENGLISH","doi":"10.3133/sir20055250","usgsCitation":"Watt, M.K., and Voronin, L.M., 2006, Sources of water to wells in updip areas of the Wenonah-Mount Laurel aquifer, Gloucester and Camden Counties, New Jersey: U.S. Geological Survey Scientific Investigations Report 2005-5250, vi, 34 p., https://doi.org/10.3133/sir20055250.","productDescription":"vi, 34 p.","numberOfPages":"40","costCenters":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"links":[{"id":191564,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8495,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5250/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db6985cf","contributors":{"authors":[{"text":"Watt, Martha K. 0000-0001-5651-3428 mwatt@usgs.gov","orcid":"https://orcid.org/0000-0001-5651-3428","contributorId":3275,"corporation":false,"usgs":true,"family":"Watt","given":"Martha","email":"mwatt@usgs.gov","middleInitial":"K.","affiliations":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"preferred":true,"id":288960,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Voronin, Lois M. 0000-0002-1064-1675 lvoronin@usgs.gov","orcid":"https://orcid.org/0000-0002-1064-1675","contributorId":1475,"corporation":false,"usgs":true,"family":"Voronin","given":"Lois","email":"lvoronin@usgs.gov","middleInitial":"M.","affiliations":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"preferred":true,"id":288959,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70209653,"text":"70209653 - 2006 - Performance of Bromus tectorum L. in relation to soil properties, water additions, and chemical amendments in calcareous soils of southeastern Utah, USA","interactions":[],"lastModifiedDate":"2020-04-17T16:49:26.272358","indexId":"70209653","displayToPublicDate":"2006-08-21T11:45:21","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3089,"text":"Plant and Soil","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Performance of <i>Bromus tectorum</i> L. in relation to soil properties, water additions, and chemical amendments in calcareous soils of southeastern Utah, USA","title":"Performance of Bromus tectorum L. in relation to soil properties, water additions, and chemical amendments in calcareous soils of southeastern Utah, USA","docAbstract":"<p><span>In drylands of southeastern Utah, USA, the invasive exotic grass&nbsp;</span><i>Bromus tectorum</i><span>&nbsp;L. occurs in distinct spatial patterns suggesting soil control of ecosystem susceptibility to invasion. To improve our understanding of these patterns, we examined performance of&nbsp;</span><i>B. tectorum</i><span>&nbsp;in relation to additions of water, KCl, MgO, and CaO at seventeen 1600&nbsp;m</span><sup>2</sup><span>&nbsp;sites distributed across a calcareous soil gradient in Canyonlands National Park. Water additions resulted in a 57% increase in&nbsp;</span><i>B. tectorum</i><span>&nbsp;establishment. Fall establishment was significantly correlated with silt and clay content in wet plots but not in dry plots, suggesting that texture effects on&nbsp;</span><i>B. tectorum</i><span>&nbsp;establishment patterns may be greater in wet years than in dry years. Applications of MgO resulted in a 49% decrease in&nbsp;</span><i>B. tectorum</i><span>&nbsp;establishment, although MgO had no effect on whole-plot biomass at the end of the growing season.&nbsp;</span><i>B. tectorum</i><span>–soil relations were strongest during winter (December–March) when relative growth rates were negatively related to soil acid-neutralizing potential, sand and CaCO</span><sub>3</sub><span>&nbsp;content, and a measure of bioavailable Mg; and positively related to silt and clay content, total N, measures of bioavailable Mn, P, and K, and a measure of magnetite indicating distributional patterns of eolian dust. As soils were persistently moist during this period, we attribute strong&nbsp;</span><i>B. tectorum</i><span>–soil patterns in winter to effects of low temperature on diffusion, microbial activity, and/or production of root exudates important for nutrient mobilization and uptake. In spring, there was a reversal in&nbsp;</span><i>B. tectorum</i><span>–soil relations such that loamy soils with higher&nbsp;</span><i>B. tectorum</i><span>&nbsp;densities were unfavorable for growth relative to sandy soils with higher warm-season water potentials. We conclude that resource limitations for&nbsp;</span><i>B. tectorum</i><span>&nbsp;in this study area shift seasonally, from water limitation of fall establishment, to nutrient limitation of winter growth, and back to water limitation of spring growth. Because study sites generally were arrayed along a hillslope gradient with downslope trends in soil vtexture and nutrient content, close&nbsp;</span><i>B. tectorum</i><span>–soil relations documented in this study indicate that a geomorphic framework is useful for understanding and predicting&nbsp;</span><i>B. tectorum</i><span>&nbsp;invasion patterns in dryland ecosystems of this region.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s11104-006-0058-4","usgsCitation":"Miller, M.E., Belnap, J., Beatty, S.W., and Reynolds, R.L., 2006, Performance of Bromus tectorum L. in relation to soil properties, water additions, and chemical amendments in calcareous soils of southeastern Utah, USA: Plant and Soil, v. 288, p. 1-18, https://doi.org/10.1007/s11104-006-0058-4.","productDescription":"18 p.","startPage":"1","endPage":"18","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":374097,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Canyonlands National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.25741577148438,\n              37.94419750075404\n            ],\n            [\n              -109.63668823242188,\n              37.94419750075404\n            ],\n            [\n              -109.63668823242188,\n              38.50089258896462\n            ],\n            [\n              -110.25741577148438,\n              38.50089258896462\n            ],\n            [\n              -110.25741577148438,\n              37.94419750075404\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"288","noUsgsAuthors":false,"publicationDate":"2006-08-21","publicationStatus":"PW","contributors":{"authors":[{"text":"Miller, Mark E.","contributorId":91580,"corporation":false,"usgs":false,"family":"Miller","given":"Mark","email":"","middleInitial":"E.","affiliations":[{"id":6959,"text":"National Park Service Southeast Utah Group","active":true,"usgs":false}],"preferred":false,"id":787395,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Belnap, Jayne 0000-0001-7471-2279 jayne_belnap@usgs.gov","orcid":"https://orcid.org/0000-0001-7471-2279","contributorId":1332,"corporation":false,"usgs":true,"family":"Belnap","given":"Jayne","email":"jayne_belnap@usgs.gov","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":787396,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Beatty, Susan W.","contributorId":70530,"corporation":false,"usgs":true,"family":"Beatty","given":"Susan","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":787397,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Reynolds, Richard L. 0000-0002-4572-2942 rreynolds@usgs.gov","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":139068,"corporation":false,"usgs":true,"family":"Reynolds","given":"Richard","email":"rreynolds@usgs.gov","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":787398,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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