{"pageNumber":"2940","pageRowStart":"73475","pageSize":"25","recordCount":184582,"records":[{"id":39941,"text":"wri024166 - 2002 - Detection of fresh ground water and a contaminant plume beneath Red Brook Harbor, Cape Cod, Massachusetts, 2000","interactions":[],"lastModifiedDate":"2023-04-07T19:57:49.365507","indexId":"wri024166","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2002-4166","title":"Detection of fresh ground water and a contaminant plume beneath Red Brook Harbor, Cape Cod, Massachusetts, 2000","docAbstract":"Trichloroethene and tetrachloroethene were detected in ground water in a vertical interval from about 68 to 176 feet below sea level beneath the shoreline where the contaminant plume emanating from a capped landfill on the Massachusetts Military Reservation intersects Red Brook Harbor. The highest concentrations at the shoreline, about 15 micrograms per liter of trichloroethene and 1 microgram per liter of tetrachloroethene, were measured in samples from one well at about 176 feet below sea level. The concentrations of nutrients, such as nitrate and ammonium, and trace metals, such as iron and manganese, in these same samples are typical of uncontaminated ground water on Cape Cod. Fresh ground water (bulk electrical conductance less than 100 millisiemens per meter) is present beneath the harbor at 40 of 48 locations investigated within about 250 feet of the shoreline. Fresh ground water also was detected at one location approximately 450 feet from shore. The harbor bottom consists of soft sediments that range in thickness from 0 to greater than 20 feet and overlie sandy aquifer materials. Trichloroethene was detected at several locations in fresh ground water from the sandy aquifer materials beneath the harbor. The highest trichloroethene concentration, about 4.5 micrograms per liter, was measured about 450 feet from shore.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri024166","usgsCitation":"McCobb, T.D., and LeBlanc, D.R., 2002, Detection of fresh ground water and a contaminant plume beneath Red Brook Harbor, Cape Cod, Massachusetts, 2000: U.S. Geological Survey Water-Resources Investigations Report 2002-4166, iv, 36 p., https://doi.org/10.3133/wri024166.","productDescription":"iv, 36 p.","costCenters":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":3639,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024166/","linkFileType":{"id":5,"text":"html"}},{"id":415462,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52728.htm","linkFileType":{"id":5,"text":"html"}},{"id":165036,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Cape Cod, Red Brook Harbor","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -70.6728,\n              41.6814\n            ],\n            [\n              -70.6728,\n              41.65\n            ],\n            [\n              -70.5778,\n              41.65\n            ],\n            [\n              -70.5778,\n              41.6814\n            ],\n            [\n              -70.6728,\n              41.6814\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6679f9","contributors":{"authors":[{"text":"McCobb, Timothy D. 0000-0003-1533-847X tmccobb@usgs.gov","orcid":"https://orcid.org/0000-0003-1533-847X","contributorId":2012,"corporation":false,"usgs":true,"family":"McCobb","given":"Timothy","email":"tmccobb@usgs.gov","middleInitial":"D.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":222657,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LeBlanc, Denis R. 0000-0002-4646-2628 dleblanc@usgs.gov","orcid":"https://orcid.org/0000-0002-4646-2628","contributorId":1696,"corporation":false,"usgs":true,"family":"LeBlanc","given":"Denis","email":"dleblanc@usgs.gov","middleInitial":"R.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":222656,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39934,"text":"wri024148 - 2002 - Metal concentrations and sources in the Miller Creek watershed, Park County, Montana, August 2000","interactions":[],"lastModifiedDate":"2020-02-20T06:25:52","indexId":"wri024148","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2002-4148","title":"Metal concentrations and sources in the Miller Creek watershed, Park County, Montana, August 2000","docAbstract":"Miller Creek is a tributary of Soda Butte Creek in south-central Montana near the northeast corner of Yellowstone National Park. Surface-water and streambed-sediment samples were collected from streams and seeps throughout the Miller Creek watershed during low-flow conditions on August 28-31, 2000, to characterize metal concentrations and identify possible sources contributing metal to Miller Creek. \r\n\r\nMost water in Miller Creek appears to be unaffected by mining disturbances or natural weathering of mineralized rocks, although such effects are common elsewhere in the New World Mining District. Values for pH were near neutral to basic. Total-recoverable copper, lead, and zinc concentrations were low, relative to State of Montana water-quality standards, with many concentrations less than the analytical minimum reporting levels. Metal concentrations in Miller Creek during this study ranged from 1 to 6 micrograms per liter (?g/L) for total-recoverable copper, <1 to 5 ?g/L for total-recoverable lead, and <1 to 26 ?g/L for total-recoverable zinc. Concentrations of cadmium, copper, lead, and zinc in all samples from Miller Creek were less than the chronic aquatic-life criteria, except for one total-recoverable lead value (5 ?g/L) just downstream from the Black Warrior Mine inflow. \r\n\r\nLeachable lead and zinc concentrations in streambed-sediment samples collected during this study were highest at the Black Warrior Mine inflow. Leachable concentrations at this site were about 20 times greater for lead and 11 times greater for zinc than concentrations in the streambed-sediment sample collected from Miller Creek upstream from this inflow. However, these elevated concentrations had little effect on the leachable metal concentrations in the streambed-sediment sample collected downstream from the Black Warrior Mine inflow. \r\n\r\nMetal loading to Miller Creek during this low-flow study was relatively small. Three small left-bank inflows having elevated copper concentrations entered Miller Creek near the middle of the study reach and their combined total-recoverable copper load accounted for about 96 percent of the copper load in Miller Creek. Small loads of lead (about 2 micrograms per second) entered Miller Creek from the Black Warrior Mine inflow and a right bank inflow. None of the loads entering Miller Creek had an appreciable effect on mainstem metal concentrations. In addition, substantial differences between mining related areas and areas influenced by local geology could not be determined.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri024148","usgsCitation":"Cleasby, T., and Nimick, D.A., 2002, Metal concentrations and sources in the Miller Creek watershed, Park County, Montana, August 2000: U.S. Geological Survey Water-Resources Investigations Report 2002-4148, 32 p. , https://doi.org/10.3133/wri024148.","productDescription":"32 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":164738,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3634,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024148","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Montana","county":"Park County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-110.2821,46.1847],[-110.2815,46.1596],[-110.2816,46.1348],[-110.2901,46.1344],[-110.2904,46.0447],[-110.29,45.9595],[-110.2908,45.9289],[-110.2916,45.8708],[-110.2912,45.7852],[-110.2207,45.7842],[-110.2182,45.6072],[-110.2145,45.5523],[-110.2175,45.4824],[-110.2166,45.37],[-110.2167,45.3494],[-110.2297,45.3494],[-110.2286,45.2946],[-110.2275,45.259],[-110.2276,45.2306],[-110.227,45.2051],[-110.2271,45.1763],[-110.059,45.1758],[-109.7977,45.1729],[-109.7977,45.1665],[-109.7979,45.0939],[-109.7969,45.003],[-109.8524,45.0029],[-109.9988,45.0026],[-110.1325,45.0022],[-110.133,45.0021],[-110.2006,44.9942],[-110.3717,44.9972],[-110.4021,44.9921],[-110.4302,44.9921],[-110.5806,44.9925],[-110.7072,44.9929],[-110.7756,45.0019],[-110.7823,45.0018],[-110.8004,45.0017],[-111.0418,45],[-111.0411,45.078],[-111.0427,45.0773],[-111.0429,45.1024],[-111.0424,45.1307],[-111.042,45.1599],[-111.0422,45.1791],[-111.0364,45.1791],[-111.0355,45.234],[-111.0357,45.2614],[-111.0351,45.3495],[-110.9366,45.349],[-110.9145,45.3486],[-110.9146,45.3619],[-110.9164,45.451],[-110.9174,45.4953],[-110.9175,45.5245],[-110.859,45.5247],[-110.8568,45.5896],[-110.7943,45.5902],[-110.7937,45.6113],[-110.794,45.6657],[-110.7935,45.6977],[-110.7942,45.7132],[-110.7945,45.7864],[-110.7886,45.7864],[-110.7888,45.8299],[-110.7884,45.8871],[-110.7893,45.9301],[-110.7887,45.9452],[-110.7889,46.1425],[-110.7836,46.1425],[-110.7825,46.1933],[-110.5789,46.1913],[-110.55,46.1913],[-110.5264,46.1913],[-110.4062,46.1904],[-110.4068,46.1844],[-110.3031,46.1852],[-110.2821,46.1847]]]},\"properties\":{\"name\":\"Park\",\"state\":\"MT\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db6256ee","contributors":{"authors":[{"text":"Cleasby, Thomas E. 0000-0003-0694-1541","orcid":"https://orcid.org/0000-0003-0694-1541","contributorId":21993,"corporation":false,"usgs":true,"family":"Cleasby","given":"Thomas E.","affiliations":[],"preferred":false,"id":222647,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nimick, David A. dnimick@usgs.gov","contributorId":421,"corporation":false,"usgs":true,"family":"Nimick","given":"David","email":"dnimick@usgs.gov","middleInitial":"A.","affiliations":[{"id":573,"text":"Special Applications Science Center","active":true,"usgs":true},{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":true,"id":222646,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39986,"text":"wri024115 - 2002 - Water-quality assessment of the Great Salt Lake basins, Utah, Idaho, and Wyoming: Environmental setting and study design","interactions":[],"lastModifiedDate":"2022-12-19T22:04:44.149183","indexId":"wri024115","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2002-4115","title":"Water-quality assessment of the Great Salt Lake basins, Utah, Idaho, and Wyoming: Environmental setting and study design","docAbstract":"The Great Salt Lake Basins, Utah, Idaho, and Wyoming is one of 51 study units in the United States where the status and trends of water quality, and the factors controlling water quality, are being studied by the National Water-Quality Assessment Program of the U.S. Geological Survey. The 14,500-square-mile Great Salt Lake Basins study unit encompasses three major river systems that enter Great Salt Lake: the Bear, the Weber, and the Utah Lake/Jordan River systems. The environmental setting of the study unit includes natural and human-related factors that potentially influence the physical, chemical, and/or biological quality of the surface- and ground-water resources. Surface- and ground-water components of the planned assessment activities are designed to evaluate the sources of natural and human-related factors that affect the water quality in the Great Salt Lake Basins study unit.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/wri024115","usgsCitation":"Baskin, R.L., Waddell, K.M., Thiros, S.A., Giddings, E.M., Hadley, H.K., Stephens, D.W., and Gerner, S.J., 2002, Water-quality assessment of the Great Salt Lake basins, Utah, Idaho, and Wyoming: Environmental setting and study design: U.S. Geological Survey Water-Resources Investigations Report 2002-4115, viii, 47 p., https://doi.org/10.3133/wri024115.","productDescription":"viii, 47 p.","numberOfPages":"57","costCenters":[{"id":610,"text":"Utah Water Science 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K.","contributorId":101654,"corporation":false,"usgs":true,"family":"Hadley","given":"Heidi","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":222756,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Stephens, Doyle W.","contributorId":40195,"corporation":false,"usgs":true,"family":"Stephens","given":"Doyle","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":222757,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Gerner, Steven J. 0000-0002-5701-1304 sjgerner@usgs.gov","orcid":"https://orcid.org/0000-0002-5701-1304","contributorId":972,"corporation":false,"usgs":true,"family":"Gerner","given":"Steven","email":"sjgerner@usgs.gov","middleInitial":"J.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":222753,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":39858,"text":"fs05502 - 2002 - USGS capabilities for interdisciplinary investigations in coastal and nearshore ecosystems of the Great Lakes","interactions":[],"lastModifiedDate":"2017-02-06T11:05:18","indexId":"fs05502","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","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":"055-02","title":"USGS capabilities for interdisciplinary investigations in coastal and nearshore ecosystems of the Great Lakes","docAbstract":"<p>People choose to reside, work, and vacation in coastal areas of the Great Lakes because of the lakes' scenic beauty and their historic and cultural features. Great Lakes nearshore areas also constitute a valuable economic resource. Two million anglers added \\$1 billion to the region's economy in 1996. More than 300 million tons of goods were transported out of major Great Lakes ports at a value of \\$3 billion in 1996. A 1998 survey of Lake Erie beaches estimated contributions of $5 million per year to each local economy with a public beach. More than 70 million people yearly visit national, state and provincial parks in the Great Lakes area. </p><p>Uncontrolled land development, recreational development, invasive species, climate change, water availability, and water-level changes and fluctuations lead a long list of current and potential issues in coastal and nearshore areas. To be effectively addressed, these complex issues require an interdisciplinary approach. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs05502","usgsCitation":"Myers, D.N., 2002, USGS capabilities for interdisciplinary investigations in coastal and nearshore ecosystems of the Great Lakes: U.S. Geological Survey Fact Sheet 055-02, 6 p., https://doi.org/10.3133/fs05502.","productDescription":"6 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":3572,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://mi.water.usgs.gov/pubs/FS/FS055-02/","linkFileType":{"id":5,"text":"html"}},{"id":67735,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2002/0055/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120267,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2002/0055/report-thumb.jpg"}],"country":"Canada, United States","otherGeospatial":"Great Lakes","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db610f71","contributors":{"authors":[{"text":"Myers, Donna N.","contributorId":63027,"corporation":false,"usgs":true,"family":"Myers","given":"Donna","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":222443,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39991,"text":"ofr2002117 - 2002 - Aerial Magnetic, Electromagnetic, and Gamma-ray Survey, Berrien County, Michigan","interactions":[],"lastModifiedDate":"2018-11-05T11:04:34","indexId":"ofr2002117","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","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":"2002-117","title":"Aerial Magnetic, Electromagnetic, and Gamma-ray Survey, Berrien County, Michigan","docAbstract":"This publication includes maps, grids, and flightline databases of a detailed aerial survey and maps and grids of satellite data in Berrien County, Michigan. The purpose of the survey was to map aquifers in glacial terrains. This was accomplished by using a DIGHEMVRES mufti-coil, mufti-frequency electromagnetic system supplemented by a high sensitivity cesium magnetometer and 256-channel spectrometer. The information from these sensors was processed to produce maps, which display the conductive, magnetic and radioactive properties of the survey area. A GPS electronic navigation system ensured accurate positioning of the geophysical data.\r\n\r\nThis report also includes data from the advanced spaceborne thermal emission and reflection (ASTER) radiometer.  ASTER measures thermal emission and reflection data for 14 bands of the spectrum.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr2002117","usgsCitation":"Duval, J.S., Pierce, H., Daniels, D.L., Mars, J.L., Webring, M.W., and Hildenbrand, T.G., 2002, Aerial Magnetic, Electromagnetic, and Gamma-ray Survey, Berrien County, Michigan: U.S. Geological Survey Open-File Report 2002-117, Available online and on CD-ROM, https://doi.org/10.3133/ofr2002117.","productDescription":"Available online and on CD-ROM","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":248,"text":"Eastern Region Minerals Program","active":false,"usgs":true}],"links":[{"id":171993,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":12960,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/of02-117/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -86.6,41.8 ], [ -86.6,42.1 ], [ -86.25,42.1 ], [ -86.25,41.8 ], [ -86.6,41.8 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db697217","contributors":{"authors":[{"text":"Duval, Joseph S.","contributorId":22314,"corporation":false,"usgs":true,"family":"Duval","given":"Joseph","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":222773,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pierce, Herbert A.","contributorId":83093,"corporation":false,"usgs":true,"family":"Pierce","given":"Herbert A.","affiliations":[],"preferred":false,"id":222775,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Daniels, David L. 0000-0003-0599-8036 dave@usgs.gov","orcid":"https://orcid.org/0000-0003-0599-8036","contributorId":1792,"corporation":false,"usgs":true,"family":"Daniels","given":"David","email":"dave@usgs.gov","middleInitial":"L.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":222771,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mars, John L. jmars@usgs.gov","contributorId":3428,"corporation":false,"usgs":true,"family":"Mars","given":"John","email":"jmars@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":false,"id":222772,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Webring, Michael W. mwebring@usgs.gov","contributorId":1221,"corporation":false,"usgs":true,"family":"Webring","given":"Michael","email":"mwebring@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":222770,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hildenbrand, Thomas G.","contributorId":61787,"corporation":false,"usgs":true,"family":"Hildenbrand","given":"Thomas","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":222774,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":39937,"text":"wri024155 - 2002 - Simulation of ground-water flow and delineation of areas contributing recharge within the Mt. Simon-Hinckley aquifer to well fields in the Prairie Island Indian Community, Minnesota","interactions":[],"lastModifiedDate":"2022-12-15T22:40:32.903136","indexId":"wri024155","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2002-4155","title":"Simulation of ground-water flow and delineation of areas contributing recharge within the Mt. Simon-Hinckley aquifer to well fields in the Prairie Island Indian Community, Minnesota","docAbstract":"<p>The Prairie Island Indian Community in east-central Minnesota uses ground water from the Mt. Simon-Hinckley aquifer as its source of water supply. Tribal officials implemented a Source Water Protection Program to protect the quality of this water. Areas of contributing recharge were delineated for two community well fields. At well field A are two wells 325 m apart, and at well field B are two wells 25 m apart.</p>\n<p>A steady state single layer, two-dimensional ground-water flow model constructed with the computer program MODFLOW,combined with the particle-tracking computer program MODPATH, was used to track water particles (upgradient) from the two well fields. A withdrawal rate of 625 m<sup>3</sup>/d was simulated for each well field. The ground-water flow paths delineated areas of contributing recharge that are 0.38 and 0.65 km<sup>2</sup>&nbsp;based on 10- and 50-year travel times, respectively. The flow paths that define these areas extend for maximum distances of about 350 and 450 m, respectively, from the wells. At well field A the area of contributing recharge was delineated for each well as separate withdrawal points. At well field B the area of contributing recharge was delineated for the two wells as a single withdrawal point. Delineation of areas of contributing recharge to the well fields from land surface would require construction of a multi-layer ground-water flow model.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View, MN","doi":"10.3133/wri024155","collaboration":"Prepared in cooperation with the Prairie Island Indian Community","usgsCitation":"Ruhl, J.F., 2002, Simulation of ground-water flow and delineation of areas contributing recharge within the Mt. Simon-Hinckley aquifer to well fields in the Prairie Island Indian Community, Minnesota: U.S. Geological Survey Water-Resources Investigations Report 2002-4155, iv, 11 p., https://doi.org/10.3133/wri024155.","productDescription":"iv, 11 p.","numberOfPages":"15","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":319950,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri024155.JPG"},{"id":410593,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52076.htm","linkFileType":{"id":5,"text":"html"}},{"id":3636,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024155/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Minnesota, Wisconsin","otherGeospatial":"Prairie Island Indian Community","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  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F.","contributorId":81866,"corporation":false,"usgs":true,"family":"Ruhl","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":222652,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39855,"text":"fs03502 - 2002 - Estimated flood flows in the Lake Tahoe basin, California and Nevada","interactions":[],"lastModifiedDate":"2022-08-24T19:12:13.823055","indexId":"fs03502","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","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":"035-02","title":"Estimated flood flows in the Lake Tahoe basin, California and Nevada","docAbstract":"<p>Lake Tahoe, the largest alpine lake in North America, covers about 192 square miles (mi<sup>2</sup>) of the 506-mi<sup>2</sup> Lake Tahoe Basin, which straddles the border between California and Nevada (Fig. 1). In cooperation with the Nevada Department of Transportation (NDOT), the U.S. Geological Survey (USGS) estimates the flood frequencies of the streams that enter the lake. Information about potential flooding of these streams is used by NDOT in the design and construction of roads and highways in the Nevada portion of the basin. The stream-monitoring network in the Lake Tahoe Basin is part of the Lake Tahoe Interagency Monitoring Program (LTIMP), which combines the monitoring and research efforts of various Federal, State, and regional agencies, including both USGS and NDOT. The altitude in the basin varies from 6,223 feet (ft) at the lake's natural rim to over 10,000 ft along the basin's crest. Precipitation ranges from 40 inches per year (in/yr) on the eastern side to 90 in/yr on the western side (Crippen and Pavelka, 1970). Most of the precipitation comes during the winter months as snow. Precipitation that falls from June through September accounts for less than 20 percent of the annual total.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs03502","usgsCitation":"Crompton, E.J., Hess, G.W., and Williams, R.P., 2002, Estimated flood flows in the Lake Tahoe basin, California and Nevada: U.S. Geological Survey Fact Sheet 035-02, 2 p., https://doi.org/10.3133/fs03502.","productDescription":"2 p.","costCenters":[],"links":[{"id":126237,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_035_02.bmp"},{"id":3569,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/fs-035-02/","linkFileType":{"id":5,"text":"html"}},{"id":405544,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52040.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California, Nevada","otherGeospatial":"Lake Tahoe basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.234375,\n              38.846125291387025\n            ],\n            [\n              -119.82238769531251,\n              38.846125291387025\n            ],\n            [\n              -119.82238769531251,\n              39.43831424149678\n            ],\n            [\n              -120.234375,\n              39.43831424149678\n            ],\n            [\n              -120.234375,\n              38.846125291387025\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd3b2","contributors":{"authors":[{"text":"Crompton, E. James","contributorId":78771,"corporation":false,"usgs":true,"family":"Crompton","given":"E.","email":"","middleInitial":"James","affiliations":[],"preferred":false,"id":222436,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hess, Glen W.","contributorId":19136,"corporation":false,"usgs":true,"family":"Hess","given":"Glen","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":222435,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Williams, Rhea P.","contributorId":87114,"corporation":false,"usgs":true,"family":"Williams","given":"Rhea","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":222437,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":39988,"text":"ofr022 - 2002 - Geological framework data from Long Island Sound, 1981-1990: A digital data release","interactions":[],"lastModifiedDate":"2024-05-10T14:44:12.177578","indexId":"ofr022","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","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":"02-002","title":"Geological framework data from Long Island Sound, 1981-1990: A digital data release","docAbstract":"<h1>Introduction</h1><p>Since 1980 the <a href=\"http://marine.usgs.gov\" data-mce-href=\"http://marine.usgs.gov\"> Coastal and Marine Geology Program</a> of the <a href=\"http://www.usgs.gov\" data-mce-href=\"http://www.usgs.gov\"> U.S. Geological Survey</a> and <a href=\"http://dep.state.ct.us\" data-mce-href=\"http://dep.state.ct.us\"> Connecticut Department of Environmental Protection</a> have conducted a joint program of cooperative geologic research in Long Island Sound and its vicinity. As part of this program, a highly successful regional-scale study of the geologic framework was completed. Reconnaissance high-resolution seismic reflection data were collected and used to establish the basic stratigraphy within the Sound and to map the major geologic units; field verification of the geologic interpretations of the seismic profiles was primarily accomplished with vibratory cores. These interpretations were in turn used to produce basin-wide syntheses of the late Quaternary depositional history.</p><p>Unfortunately, the original seismic records and core logs were generated only in analog form. These unique paper documents, which are still under demand for industrial applications and academic research, are fragile and have become ragged from frequent use. The purpose of this report is to preserve these data by converting the seismic profiles, core descriptions, and ancillary reports into digital form, and to organize these files into a product that can be more readily accessed and disseminated.</p><p>Not all of the existing high-resolution seismic-reflection surveys, collected in Long Island Sound through cooperatives with the U.S. Geological Survey and the Connecticut Department of Environmental Protection, have been incorporated into this report. These surveys, whose records are still in need of preprocessing and annotation, generally cover smaller areas along the Connecticut coast and were originally intended to provide additional detail to the larger, more regional data sets presented herein. The digital release of the omitted data sets is planned as part of a future product.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr022","collaboration":"Prepared in cooperation with the Connecticut Department of Environmental Protection","usgsCitation":"Poppe, L., Paskevich, V., Lewis, R.S., and DiGiacomo-Cohen, M., 2002, Geological framework data from Long Island Sound, 1981-1990: A digital data release: U.S. Geological Survey Open-File Report 02-002, https://doi.org/10.3133/ofr022.","costCenters":[],"links":[{"id":3672,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0002/index.htm","linkFileType":{"id":5,"text":"html"},"description":"OFR 2002-02 HTML"},{"id":171886,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2002/0002/coverthb.jpg"},{"id":406562,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52734.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Connecticut, New York","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.883056640625,\n              40.78054143186033\n            ],\n            [\n              -73.51776123046875,\n              40.90313381465847\n            ],\n            [\n              -73.21563720703125,\n              40.89275342420696\n            ],\n            [\n              -72.5262451171875,\n              40.99855696412671\n            ],\n            [\n              -72.20489501953125,\n              41.178653972331674\n            ],\n            [\n              -72.25433349609375,\n              41.29844430929419\n            ],\n            [\n              -72.7734375,\n              41.283998505385924\n            ],\n            [\n              -72.96844482421875,\n              41.292253642159466\n            ],\n            [\n              -73.32000732421875,\n              41.151774298444984\n            ],\n            [\n              -73.67431640625,\n              41.025499378313754\n            ],\n            [\n              -73.84185791015625,\n              40.85537053192494\n            ],\n            [\n              -73.90502929687499,\n              40.79925662005228\n            ],\n            [\n              -73.883056640625,\n              40.78054143186033\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p>Director, <a href=\"https://woodshole.er.usgs.gov/index.html\" data-mce-href=\"https://woodshole.er.usgs.gov/index.html\">Woods Hole Science Center</a><br>384 Woods Hole Road<br>Quissett Campus<br>Woods Hole, MA 02543</p><p><a href=\"https://pubs.usgs.gov/contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","tableOfContents":"<ul><li>Introduction</li><li>Seismic Data</li><li>Core Data</li><li>Photo Gallery</li><li>Data Catalog</li><li>References</li><li>Related Websites</li><li>Acknowledgments</li><li>Contacts</li><li>Disclaimer</li><li>Readme</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db68759e","contributors":{"authors":[{"text":"Poppe, L.J.","contributorId":72782,"corporation":false,"usgs":true,"family":"Poppe","given":"L.J.","affiliations":[],"preferred":false,"id":222763,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Paskevich, V.F.","contributorId":96285,"corporation":false,"usgs":true,"family":"Paskevich","given":"V.F.","email":"","affiliations":[],"preferred":false,"id":222764,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lewis, R. S.","contributorId":19951,"corporation":false,"usgs":true,"family":"Lewis","given":"R.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":222761,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"DiGiacomo-Cohen, M. L.","contributorId":55465,"corporation":false,"usgs":true,"family":"DiGiacomo-Cohen","given":"M. L.","affiliations":[],"preferred":false,"id":222762,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":39936,"text":"wri20024153 - 2002 - Hydrogeology and water quality of the Upper Three Runs aquifer in the vicinity of the Gibson Road Landfill, Fort Gordon, Georgia, June-November 1999","interactions":[],"lastModifiedDate":"2022-01-12T12:19:34.148998","indexId":"wri20024153","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2002-4153","title":"Hydrogeology and water quality of the Upper Three Runs aquifer in the vicinity of the Gibson Road Landfill, Fort Gordon, Georgia, June-November 1999","docAbstract":"<p>Fort Gordon military installation, a U.S. Department of the Army facility, is located in east-central Georgia southwest of Augusta. The military base operates a three-phase unlined landfill—Gibson Road Landfill— to store a variety of wastes. Phases I and II stored only household wastes, and these phases were discontinued during the mid–1990s. Fort Gordon currently (1999) operates Phase III of the landfill that stores only construction and demolition debris. Water-quality monitoring detected selected trace elements and organic compounds exceeding the maximum contaminant levels of the U.S. Environmental Protection Agency, National Primary Drinking Water Standards. The selected trace elements and organic compounds detected showed that contamination of ground water had occurred in the vicinity of the landfill. In 1999, the U.S. Geological Survey, in cooperation with the Environmental and Natural Resources Management Office of the U.S. Army Signal Center and Fort Gordon, Georgia, began an assessment of the hydrogeology and water quality in shallow ground water in the vicinity of the Gibson Road Landfill to delineate the extent of a ground-water contamination plume in the vicinity of the landfill.</p><p>Hydrogeologic units in the Augusta area include the Upper Three Runs aquifer, the Gordon aquifer, the Millers Pond aquifer, and the Dublin aquifer. Only the shallowest aquifer, Upper Three Runs, was penetrated during this study. The Upper Three Runs aquifer is composed of sediments of the Barnwell Group. Mostly, these sediments are highly permeable fine to medium, well-sorted sand with lenses of clay.</p><p>Ground-water flow is from northwest to southeast and generally was unaffected by seasonal variation during the period of study (June–November 1999). Water-table altitudes in the landfill area for the study period ranged from 394 feet (ft) to 445 ft above sea level. Ground-water samples analyzed for organic compounds and selected trace elements by a U. S. Environmental Protection Agency (USEPA) approved statistical test revealed that increases in contaminant concentrations above the detection limits had occurred during March and September 1999 in five wells—one of which is located upgradient. These organic compounds, respective increases in concentration, and the wells in which they were detected are: methylene chloride—wells 28AA29 (24 parts per billion [ppb] and 46 ppb), 28AA30 (86 ppb and 130 ppb), and 28AA31 (240 ppb and 140 ppb); 1,1-dichloroethene—well 28AA31 (10 ppb and 5.7 ppb); 1,1-dichloroethane— wells 28AA30 (81 ppb and 140 ppb) and 28AA31 (200 ppb and 130 ppb); and 1,1,1-trichloroethane—well 28AA31 (61 ppb and 37 ppb). Although in some wells the concentration decreased from March to September, the median concentrations were still higher in certain groups. Trace element compounds, their respective increases in concentration, and the wells in which they were detected are: chromium—well 28AA30 (1,190 ppb), vanadium—well 28AA30 (104 ppb); barium—wells 28AA27 (42.2 ppb) and 28AA32 (140 ppb), and beryllium—well 28AA30 (6.3 ppb). These increases occurred in September, with the exception of chromium in well 28AA30, which occurred in March. Although a statistical test indicated increases in contaminant concentrations had occurred, water from wells 28AA27, 28AA30, 28AA31, and 28AA32 had a decrease in contaminant concentrations from February 1998 to September 1999.</p><p>U.S. Environmental Protection Agency, National Primary Drinking Water Regulations Maximum Contaminant Levels (PMCLs), formerly (MCLs) were exceeded in water from four wells for organic compounds and in five wells by selected trace elements during the February 1998, March 1999, and September 1999 sampling periods. The concentrations for the following organic compounds and the associated wells are: methylene chloride (PMCL is 5 ppb)—wells 28AA27 (February, 37 ppb; March, 24 ppb; and September, 9.6 ppb), 28AA29 (February, 20 ppb; March, 24 ppb; and September, 46 ppb), 28AA30 (February, 50 ppb; March, 86 ppb; and September, 130 ppb), and 28AA31 (February, 330 ppb; March 240 ppb; and September, 140 ppb); vinyl chloride (PMCL is 2 ppb)—well 28AA29 (March, 3.6 ppb; and September, 4.4 ppb); 1,1-dichloroethene (PMCL is 7 ppb)—wells 28AA30 (March 10 ppb; and September, 17 ppb) and 28AA31 (February, 13 ppb; and March, 10 ppb); and 1,1,2-trichloroethane (PMCL is 5 ppb)—well 28AA30 (March, 33 ppb). Contaminant concentrations decreased in well 28AA31 from March to September 1999; however, concentrations still exceeded the PMCL. The concentrations for the following selected trace elements exceeding PMCL and the associated wells during the sampling periods February 1998, March 1999, and September 1999 are: mercury (PMCL is 2 ppb)—well 28AA24 (September, 2.82 ppb), well 28AA25 (February, 3.1 ppb; March, 2.11 ppb; and September, 2.28 ppb), and well 28AA30 (September, 2.82 ppb); arsenic (PMCL is 50 ppb)—well 28AA30 (February, 90 ppb; and September, 114 ppb); thallium (PMCL is 2 ppb)—wells 28AA27 (March, 2.08 ppb) and 28AA29 (February, 2.56); barium (PMCL is 2,000 ppb)—well 28AA30 (March, 4,490 ppb); chromium (PMCL is 30 ppb)—well 28AA30 (February, 630 ppb; and March, 1,190 ppb); and beryllium (PMCL is 4 ppb)—well 28AA30 (September, 6.3 ppb). Water from seven wells, three of which are upgradient of the landfill, contained organic compounds and/or selected trace elements exceeding PMCLs during the period February 1998 to September 1999 according to private consultants. Contaminants present in upgradient wells most likely were caused by chemical dispersion, leachate migration, incorrectly defined landfill area, or natural ground-water flow beneath the landfill.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri20024153","usgsCitation":"Priest, S., and McSwain, K., 2002, Hydrogeology and water quality of the Upper Three Runs aquifer in the vicinity of the Gibson Road Landfill, Fort Gordon, Georgia, June-November 1999 (Version 1.0: 2002; Version 1.1: January 11, 2022): U.S. Geological Survey Water-Resources Investigations Report 2002-4153, v, 22 p., https://doi.org/10.3133/wri20024153.","productDescription":"v, 22 p.","temporalStart":"1999-06-01","temporalEnd":"1999-11-30","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":393893,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52211.htm"},{"id":394189,"rank":4,"type":{"id":25,"text":"Version History"},"url":"https://pubs.usgs.gov/wri/wri02-4153/versionHist.txt","text":"Version History","size":"1 KB","linkFileType":{"id":2,"text":"txt"},"description":"Version History"},{"id":164831,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/wri02-4153/coverthb2.jpg"},{"id":394215,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/wri02-4153/wrir024153.pdf","text":"Report","size":"3.23 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 02-4153"}],"country":"United States","state":"Georgia","otherGeospatial":"Fort Gordon, Gibson Road Landfill, Upper Three Runs Aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.31463432312012,\n              33.34702063231064\n            ],\n            [\n              -82.28279113769531,\n              33.34702063231064\n            ],\n            [\n              -82.28279113769531,\n              33.37598230011142\n            ],\n            [\n              -82.31463432312012,\n              33.37598230011142\n            ],\n            [\n              -82.31463432312012,\n              33.34702063231064\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0: 2002; Version 1.1: January 11, 2022","contact":"<p><a href=\"https://pubs.er.usgs.gov/contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","tableOfContents":"<ul><li>ABSTRACT</li><li>INTRODUCTION</li><li>HYDROGEOLOGY</li><li>GROUND-WATER QUALITY</li><li>SUMMARY AND CONCLUSIONS</li><li>REFERENCES CITED</li></ul>","revisedDate":"2022-01-12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e7fe","contributors":{"authors":[{"text":"Priest, Sherlyn","contributorId":23994,"corporation":false,"usgs":true,"family":"Priest","given":"Sherlyn","email":"","affiliations":[],"preferred":false,"id":222650,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McSwain, Kristen Bukowski","contributorId":104458,"corporation":false,"usgs":true,"family":"McSwain","given":"Kristen Bukowski","affiliations":[],"preferred":false,"id":222651,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39863,"text":"fs09702 - 2002 - U.S. Department of the Interior investigations of irrigation-induced contamination of water, sediment, and biota","interactions":[],"lastModifiedDate":"2012-02-02T00:10:32","indexId":"fs09702","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","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":"097-02","title":"U.S. Department of the Interior investigations of irrigation-induced contamination of water, sediment, and biota","language":"ENGLISH","doi":"10.3133/fs09702","usgsCitation":"Seiler, R.L., and Skorupa, J.P., 2002, U.S. Department of the Interior investigations of irrigation-induced contamination of water, sediment, and biota: U.S. Geological Survey Fact Sheet 097-02, 4 p., https://doi.org/10.3133/fs09702.","productDescription":"4 p.","costCenters":[],"links":[{"id":125235,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2002/0097/report-thumb.jpg"},{"id":67737,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2002/0097/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696290","contributors":{"authors":[{"text":"Seiler, R. L.","contributorId":87546,"corporation":false,"usgs":true,"family":"Seiler","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":222456,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Skorupa, J. P.","contributorId":93002,"corporation":false,"usgs":false,"family":"Skorupa","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":222457,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39992,"text":"ofr02120 - 2002 - Archive of sidescan-sonar data and DGPS navigation data collected during USGS cruise DIAN97011 Long Island, NY inner shelf-Fire Island, NY, 5 May-26 May, 1997","interactions":[],"lastModifiedDate":"2012-02-02T00:10:53","indexId":"ofr02120","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","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":"2002-120","title":"Archive of sidescan-sonar data and DGPS navigation data collected during USGS cruise DIAN97011 Long Island, NY inner shelf-Fire Island, NY, 5 May-26 May, 1997","language":"ENGLISH","doi":"10.3133/ofr02120","usgsCitation":"Capone, M., Hammar-Klose, E., Hill, J.C., and Schwab, W.C., 2002, Archive of sidescan-sonar data and DGPS navigation data collected during USGS cruise DIAN97011 Long Island, NY inner shelf-Fire Island, NY, 5 May-26 May, 1997: U.S. Geological Survey Open-File Report 2002-120, 6 DVD-ROMs : ill. (some col.), col. maps ; 4 3/4 in. , https://doi.org/10.3133/ofr02120.","productDescription":"6 DVD-ROMs : ill. (some col.), col. maps ; 4 3/4 in. ","costCenters":[],"links":[{"id":171994,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac0e4b07f02db676d49","contributors":{"authors":[{"text":"Capone, M.K.","contributorId":17670,"corporation":false,"usgs":true,"family":"Capone","given":"M.K.","email":"","affiliations":[],"preferred":false,"id":222776,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hammar-Klose, E. S.","contributorId":68380,"corporation":false,"usgs":true,"family":"Hammar-Klose","given":"E. S.","affiliations":[],"preferred":false,"id":222777,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hill, J. C.","contributorId":100878,"corporation":false,"usgs":true,"family":"Hill","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":222779,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schwab, W. C.","contributorId":78740,"corporation":false,"usgs":true,"family":"Schwab","given":"W.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":222778,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":39905,"text":"ofr00183 - 2002 - Flood-prone areas and waterways, Edwards Air Force Base, California","interactions":[],"lastModifiedDate":"2012-02-02T00:10:17","indexId":"ofr00183","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","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":"2000-183","title":"Flood-prone areas and waterways, Edwards Air Force Base, California","docAbstract":"Edwards Air Force Base (EAFB) is in the Mojave Desert region of southern California. Although the climate in the study area is arid, occasional intense storms result in flooding on the base, damaging roads and buildings. To plan for anticipated development at EAFB, the U.S. Department of the Air Force (USAF) and the U.S. Geological Survey (USGS) began a cooperative study to locate flood-prone areas on the base. This report describes flood hazards and shows flood-prone areas of the base.","language":"ENGLISH","doi":"10.3133/ofr00183","usgsCitation":"Meyer, R.W., and Bowers, J.C., 2002, Flood-prone areas and waterways, Edwards Air Force Base, California: U.S. Geological Survey Open-File Report 2000-183, 1 over-size sheet., https://doi.org/10.3133/ofr00183.","productDescription":"1 over-size sheet.","costCenters":[],"links":[{"id":170553,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3610,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/ofr00183/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e64ec","contributors":{"authors":[{"text":"Meyer, Robert W.","contributorId":69601,"corporation":false,"usgs":true,"family":"Meyer","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":222564,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bowers, James C. jcbowers@usgs.gov","contributorId":4185,"corporation":false,"usgs":true,"family":"Bowers","given":"James","email":"jcbowers@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":222563,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39990,"text":"ofr02103 - 2002 - Archive of sidescan-sonar data and DGPS navigation data collected during USGS cruise ATSV99044, South Carolina coast, 29 October-14 November, 1999","interactions":[],"lastModifiedDate":"2012-02-02T00:10:53","indexId":"ofr02103","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","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":"2002-103","title":"Archive of sidescan-sonar data and DGPS navigation data collected during USGS cruise ATSV99044, South Carolina coast, 29 October-14 November, 1999","language":"ENGLISH","doi":"10.3133/ofr02103","usgsCitation":"Roberts, C., Hammar-Klose, E., and Schwab, W.C., 2002, Archive of sidescan-sonar data and DGPS navigation data collected during USGS cruise ATSV99044, South Carolina coast, 29 October-14 November, 1999: U.S. Geological Survey Open-File Report 2002-103, 5 DVD-ROMs : ill. (some col.), col. maps ; 4 3/4 in. , https://doi.org/10.3133/ofr02103.","productDescription":"5 DVD-ROMs : ill. (some col.), col. maps ; 4 3/4 in. ","costCenters":[],"links":[{"id":171992,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abee4b07f02db675029","contributors":{"authors":[{"text":"Roberts, C.S.","contributorId":71240,"corporation":false,"usgs":true,"family":"Roberts","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":222768,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hammar-Klose, E. S.","contributorId":68380,"corporation":false,"usgs":true,"family":"Hammar-Klose","given":"E. S.","affiliations":[],"preferred":false,"id":222767,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schwab, W. C.","contributorId":78740,"corporation":false,"usgs":true,"family":"Schwab","given":"W.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":222769,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70179830,"text":"70179830 - 2002 - Ecological resource management: A call to arms","interactions":[],"lastModifiedDate":"2018-01-12T12:28:05","indexId":"70179830","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5268,"text":"Ecological Society Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Ecological resource management: A call to arms","docAbstract":"<div class=\"t m0 x10 h5 yb3 ff2 fs5 fc0 sc0 ls8 ws470\"><span class=\"current-selection\">As the human population enlarges,&nbsp;</span><span class=\"current-selection\">it becomes increasingly difficult to </span><span class=\"ls9 current-selection\">sus</span><span class=\"current-selection\">tain valued ecological resources. Hu</span><span class=\"current-selection\">man use of resources, whether it is </span><span class=\"current-selection\">t</span><span class=\"current-selection\">h</span><span class=\"current-selection\">e&nbsp;</span><span class=\"current-selection\">harvest of ocean fisheries, logging of&nbsp;</span><span class=\"current-selection\">forests, or farming of arable lands, has&nbsp;</span><span class=\"current-selection\">resulted in significant population de</span><span class=\"current-selection\">clines i</span><span class=\"current-selection\">n </span><span class=\"ls2b ws0\"><span class=\"current-selection\">many </span> <span class=\"ls9 ws4c1 current-selection\">wildlife species. The&nbsp;</span></span><span class=\"current-selection\">growth of urban areas and the exp</span><span class=\"current-selection\">ansion of impermeable surfaces alter&nbsp;</span><span class=\"current-selection\">landscape diversity and modify hydro</span><span class=\"current-selection\">logic patterns in ways </span><span class=\"lsa current-selection\">that decrease&nbsp;</span><span class=\"current-selection\">habitat quality for many desired plant,&nbsp;</span><span class=\"current-selection\">fish, and wildlife species. Impaired wa</span><span class=\"current-selection\">ter, </span><span class=\"ls9 ws40a current-selection\">air, and soil quality related to in</span><span class=\"current-selection\">dustrial, municipal, and agricultural ac</span><span class=\"current-selection\">tivities </span> <span class=\"ls9 ws33e current-selection\">have altered the composition&nbsp;</span><span class=\"current-selection\">of aquatic and terrestrial communities.</span></div>","language":"English","publisher":"Wiley ","doi":"10.1890/0012-9623(2002)083[0260:C]2.0.CO;2","usgsCitation":"Emlen, J., Kapustka, L., Barnthouse, L., Beyer, N., Biddinger, G., Kedwards, T., Landis, W., Menzie, C., Munns, W., Sorenson, M., and Wentsel, R., 2002, Ecological resource management: A call to arms: Ecological Society Bulletin, v. 83, p. 269-271, https://doi.org/10.1890/0012-9623(2002)083[0260:C]2.0.CO;2.","productDescription":"3 p. ","startPage":"269","endPage":"271","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":333391,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"83","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58808d9ae4b01dfadfff15b7","contributors":{"authors":[{"text":"Emlen, J.M.","contributorId":63979,"corporation":false,"usgs":true,"family":"Emlen","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":658862,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kapustka, Lawrence","contributorId":178433,"corporation":false,"usgs":false,"family":"Kapustka","given":"Lawrence","email":"","affiliations":[],"preferred":false,"id":658863,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barnthouse, L.","contributorId":178434,"corporation":false,"usgs":false,"family":"Barnthouse","given":"L.","email":"","affiliations":[],"preferred":false,"id":658864,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Beyer, N.","contributorId":15737,"corporation":false,"usgs":true,"family":"Beyer","given":"N.","email":"","affiliations":[],"preferred":false,"id":658865,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Biddinger, G.","contributorId":178435,"corporation":false,"usgs":false,"family":"Biddinger","given":"G.","affiliations":[],"preferred":false,"id":658866,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kedwards, T.","contributorId":178436,"corporation":false,"usgs":false,"family":"Kedwards","given":"T.","email":"","affiliations":[],"preferred":false,"id":658867,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Landis, W.","contributorId":178437,"corporation":false,"usgs":false,"family":"Landis","given":"W.","email":"","affiliations":[],"preferred":false,"id":658868,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Menzie, C.","contributorId":37431,"corporation":false,"usgs":true,"family":"Menzie","given":"C.","affiliations":[],"preferred":false,"id":658869,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Munns, W.","contributorId":178438,"corporation":false,"usgs":false,"family":"Munns","given":"W.","email":"","affiliations":[],"preferred":false,"id":658870,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Sorenson, M.","contributorId":178439,"corporation":false,"usgs":false,"family":"Sorenson","given":"M.","affiliations":[],"preferred":false,"id":658871,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Wentsel, R.","contributorId":81219,"corporation":false,"usgs":true,"family":"Wentsel","given":"R.","email":"","affiliations":[],"preferred":false,"id":658872,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":49206,"text":"wri014240 - 2002 - Standard errors of annual discharge and change in reservoir content data from selected stations in the lower Colorado River streamflow-gaging station network, 1995-99","interactions":[],"lastModifiedDate":"2014-06-12T09:22:29","indexId":"wri014240","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4240","title":"Standard errors of annual discharge and change in reservoir content data from selected stations in the lower Colorado River streamflow-gaging station network, 1995-99","docAbstract":"<p>The Bureau of Reclamation is currently (1995–2001) testing the Lower Colorado River Accounting\nSystem as a method to estimate the consumptive use of Colorado River water by diverters from Hoover\nDam to Mexico. Consumptive use is estimated in the Lower Colorado River Accounting System method,\nin part, on the basis of the annual discharge or annual change in reservoir contents, as well as the variance\nof estimate of the annual discharge or the annual change in reservoir contents at several surface-water\ngaging stations in the lower Colorado River stream-gaging network. The standard error and the variance\nof estimate were determined for the annual discharge at 14 streamflow-gaging stations and for the annual\nchange in content at 2 reservoir-content gaging stations used in the Lower Colorado River Accounting\nSystem for calendar years 1995–99.</p>\n<br>\n<p>The standard error of the annual discharge was determined by using modifications to an existing\nmethod that assumes that the uncertainty in the discharge-rating shift is the main source of uncertainty in\ncomputed discharges and that the discharge-rating shift behaves as a first-order Markovian process. The\nmethod uses Kalman filtering of a first-order Markovian process as a statistical analogy to computing\nstreamflow with a shifted discharge rating. Temporally unbiased residuals from a discharge rating are used\nas a surrogate for the actual shifts used to compute discharge. The standard error of the annual discharge is\ndetermined by using Kalman-filter theory and estimates of four parameters: (1) the measurement variance\nof the discharge measurements used to determine the discharge-rating shift, (2) the process variance of the\ndischarge-rating residuals, (3) the serial correlation of the discharge-rating residuals, and (4) the\nfrequency of the discharge measurements. The existing methodology was improved by estimating the\nmeasurement variance from a semivariogram of the discharge-rating residuals, rather than on the basis of\nempirically derived error estimates for discharge measurements. The process variance and serial\ncorrelation of the discharge-rating residuals are estimated from the semivariogram, rather than a\nvariogram, of the discharge-rating residuals. The empirically derived estimates are based on\ncharacteristics of the discharge measurements such as number of depth and velocity observation sections,\ntype of current meter, and bed material composition and stability. Measurement variance determined from\nthe semivariograms was site specific and is therefore considered a better estimate than measurement\nvariance determined from the empirically-derived estimates. The method of estimating the standard error\nof the annual discharge requires the assumption of unbiased discharge-rating residuals, and for this\nreason, the standard errors presented in this report only represent the random error in the annual discharge\ndata. Estimates of the standard error of the annual change in reservoir content were determined on the\nbasis of the reservoir-surface area and the standard error of reservoir-stage readings.</p>\n<br>\n<p>The standard error of the annual discharge, as a percentage, ranged from 0.11 percent for the All-\nAmerican Canal near Imperial Dam in 1998 to 12.3 percent for the Colorado River below Imperial Dam\nin 1996. The standard error of the annual discharge was less than 2 percent for all 5 years for 11 of the\n14 streamflow-gaging stations. In terms of flow volume, the standard error of the annual discharge ranged\nfrom 97 acre-feet for the Mittry Lake Diversions in 1995 to 77,000 acre-feet for the Colorado River at the\nnortherly international boundary with Mexico in 1998. In general, the standard error of the annual\ndischarge, as a percentage, was smallest at streamflow-gaging stations on the main stem of the Colorado\nRiver; however, the standard error of the annual discharge in acre-feet was largest at these stations\nbecause of the large annual discharge on the main stem. The standard error of the annual change in\ncontent for the two reservoirs ranged from 1,590 acre-feet for Lake Havasu in 1996 to 2,790 acre-feet for\nLake Mohave in 1995.</p>\n<br>\n<p>The variance of estimate of the annual discharge for a streamflow-gaging station can be reduced by\nmaking additional discharge measurements; either by increasing the number of discharge measurements\nmade per site visit, or by increasing the frequency of site visits. Measurement error can be reduced by\nusing the average shift for two or more discharge measurements made during a site visit. For a\nstreamflow-gaging station where measurement error is much greater than process error and the serial\ncorrelation of the discharge-rating residuals is high, an improved gaging strategy would involve making\nmultiple discharge measurements per site visit. In contrast, for a streamflow-gaging station where process\nerror is much greater than measurement error and the serial correlation of discharge-rating residuals is\nlow, the gaging strategy would consist of several single discharge-measurement site visits. For a given\noperating cost or for a given variance of estimate of the annual discharge at a streamflow-gaging station,\nthe optimal site-visit and discharge-measurement strategy can be determined, providing that the travel\ncosts as well as the measurement variance, process variance, and serial correlation of discharge-rating\nresiduals are known.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Tucson, AZ","doi":"10.3133/wri014240","collaboration":"Prepared in cooperation with Bureau of Reclamation","usgsCitation":"Anning, D.W., 2002, Standard errors of annual discharge and change in reservoir content data from selected stations in the lower Colorado River streamflow-gaging station network, 1995-99: U.S. Geological Survey Water-Resources Investigations Report 2001-4240, x, 81 p., https://doi.org/10.3133/wri014240.","productDescription":"x, 81 p.","numberOfPages":"92","costCenters":[],"links":[{"id":288432,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288431,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2001/4240/report.pdf"}],"country":"United States","state":"Arizona;California","otherGeospatial":"Colorado River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.0,32.0 ], [ -116.0,37.0 ], [ -113.0,37.0 ], [ -113.0,32.0 ], [ -116.0,32.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478fe4b07f02db48a18a","contributors":{"authors":[{"text":"Anning, David W. dwanning@usgs.gov","contributorId":432,"corporation":false,"usgs":true,"family":"Anning","given":"David","email":"dwanning@usgs.gov","middleInitial":"W.","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":true,"id":239304,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39974,"text":"wri024064 - 2002 - Concentrations of Escherichia coli in streams in the Ohio River Watershed in Indiana, May—August 2000","interactions":[],"lastModifiedDate":"2019-04-15T08:43:42","indexId":"wri024064","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2002–4064","displayTitle":"Concentrations of Escherichia coli in streams in the Ohio River Watershed in Indiana, May—August 2000","title":"Concentrations of Escherichia coli in streams in the Ohio River Watershed in Indiana, May—August 2000","docAbstract":"<p>Water samples collected from 40 stream sites in the Ohio River Watershed in Indiana from May through August 2000 were analyzed for concentrations of <i>Escherichia coli (E. coli)</i> bacteria. Each site was sampled five times in a 30-day period. Concentrations of E. coli in 72 of the 200 samples exceeded the State of Indiana single-sample standard of 235 colonies per 100 milliliters for waters used for recreation.</p><p>A five-sample geometric mean of concentrations was computed for each site. Concentrations in samples from 24 of the 40 sites exceeded the State of Indiana standard for a five-sample geometric mean of 125 colonies per 100 milliliters for waters used for recreation. Samples collected from 34 sites had <i>E. coli</i> concentrations that exceeded either or both the single-sample standard and the five-sample geometric mean standard.</p><p>Five of the 40 sampling sites were at or near U.S. Geological Survey streamflowgaging stations. On the basis of records from these stations, 16 percent of the samples from these sites were collected at streamflows above the median daily mean discharge for each station.</p><p><i>E. coli</i> concentrations and turbidity measurements collected during 2000 were analyzed in concert with <i>E. coli</i> concentration and turbidity data collected in 1999 at streams within the Kankakee and Lower Wabash River Watersheds in Indiana and in 1998 at streams within the Upper Wabash River Watershed in Indiana. These data were grouped together to investigate the relation between concentrations of bacteria and turbidity. The resulting analysis indicated a statistically significant correlation between concentrations of <i>E. coli</i> and turbidity.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri024064","usgsCitation":"Silcox, C.A., Robinson, B.A., and Willoughby, T.C., 2002, Concentrations of Escherichia coli in streams in the Ohio River Watershed in Indiana, May—August 2000: U.S. Geological Survey Water-Resources Investigations Report 2002–4064, Report: vi, 45 p., https://doi.org/10.3133/wri024064.","productDescription":"Report: vi, 45 p.","numberOfPages":"51","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":3663,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4064/wri20024064.pdf","text":"Report","size":"2.22 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 2002-4064"},{"id":170209,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2002/4064/coverthb.jpg"}],"country":"United States","state":"Indiana","otherGeospatial":"Ohio River watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.011474609375,\n              38.272688535980976\n            ],\n            [\n              -88.13232421875,\n              37.931200459333716\n            ],\n            [\n              -88.1048583984375,\n              37.76202988573211\n            ],\n            [\n              -87.95654296875,\n              37.75334401310656\n            ],\n            [\n              -87.8961181640625,\n              37.78808138412046\n            ],\n            [\n              -87.8961181640625,\n            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    -84.81994628906249,\n              39.605688178320825\n            ],\n            [\n              -87.5555419921875,\n              38.839707613545144\n            ],\n            [\n              -88.011474609375,\n              38.272688535980976\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/oki-water/\" data-mce-href=\"https://www.usgs.gov/centers/oki-water/\">Director, Indiana Water Science Center</a><br>U.S. Geological Survey<br>5957 Lakeside Blvd.<br>Indianapolis, IN 46278</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Study Methods</li><li>Concentrations of Escherichia coli</li><li>Quality-Assurance Results</li><li>Summary</li><li>References Cited</li><li>Supplemental Data</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a54a8","contributors":{"authors":[{"text":"Silcox, Cheryl A. casilcox@usgs.gov","contributorId":5080,"corporation":false,"usgs":true,"family":"Silcox","given":"Cheryl","email":"casilcox@usgs.gov","middleInitial":"A.","affiliations":[{"id":27231,"text":"Indiana-Kentucky Water Science Center","active":true,"usgs":true}],"preferred":true,"id":222722,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, Bret A. barobins@usgs.gov","contributorId":3897,"corporation":false,"usgs":true,"family":"Robinson","given":"Bret","email":"barobins@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":222721,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Willoughby, Timothy C.","contributorId":49404,"corporation":false,"usgs":true,"family":"Willoughby","given":"Timothy","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":222723,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":38172,"text":"fs05702 - 2002 - The Lake Olathe watershed: Understanding an important resource","interactions":[],"lastModifiedDate":"2022-07-11T18:35:53.866621","indexId":"fs05702","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","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":"057-02","title":"The Lake Olathe watershed: Understanding an important resource","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs05702","usgsCitation":"Mau, D.P., and Adams, C.S., 2002, The Lake Olathe watershed: Understanding an important resource: U.S. Geological Survey Fact Sheet 057-02, 4 p., https://doi.org/10.3133/fs05702.","productDescription":"4 p.","costCenters":[],"links":[{"id":403423,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52026.htm","linkFileType":{"id":5,"text":"html"}},{"id":64471,"rank":298,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2002/0057/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119571,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2002/0057/report-thumb.jpg"}],"country":"United States","state":"Kansas","otherGeospatial":"Lake Olathe watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.96994018554688,\n              38.7519413494709\n            ],\n            [\n              -94.79827880859375,\n              38.7519413494709\n            ],\n            [\n              -94.79827880859375,\n              38.91668153637508\n            ],\n            [\n              -94.96994018554688,\n              38.91668153637508\n            ],\n            [\n              -94.96994018554688,\n              38.7519413494709\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bfdf","contributors":{"authors":[{"text":"Mau, David P. dpmau@usgs.gov","contributorId":457,"corporation":false,"usgs":true,"family":"Mau","given":"David","email":"dpmau@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":219255,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adams, Carly S.","contributorId":53442,"corporation":false,"usgs":true,"family":"Adams","given":"Carly","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":219256,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39982,"text":"wri024111 - 2002 - Statistical analysis of stream water-quality data and sampling network design near Oklahoma City, central Oklahoma, 1977-1999","interactions":[],"lastModifiedDate":"2016-04-08T15:17:35","indexId":"wri024111","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2002-4111","title":"Statistical analysis of stream water-quality data and sampling network design near Oklahoma City, central Oklahoma, 1977-1999","docAbstract":"<p>Water-quality data collected from 1993-99 at five sites on Bluff, Deer, and Chisholm Creeks and from 1988-99 at five sites in the North Canadian River indicated that there were significant differences in constituent values among sites for water properties, major ions, trace elements, nutrients, turbidity, pesticides, and bacteria. Concentrations of dissolved solids and sulfate generally decreased as streams flowed through the Oklahoma City urban area. Concentrations of organic carbon, nitrogen and phosphorus compounds, lindane, and 2,4-D, and frequencies of detection of pesticides increased in the North Canadian River as it flowed through the urban area. Volatile organic compounds were not detected in samples collected quarterly from 1988-90 at sites on the North Canadian River. Concentrations of some compounds, including dissolved oxygen, sulfate, chloride, ammonia, manganese, diazinon, dieldrin, and fecal coliform bacteria periodically exceeded Federal or state water-quality standards at some sites.</p>\n<p>Regression analyses were used to identify trends in constituent concentrations related to streamflow, season, and time. Trends for some constituents were indicated at all sites, but most trends were sitespecific. Seasonal trends were evident for several constituents: suspended solids, organic nitrogen, and biochemical oxygen demand were greatest during summer. Dissolved oxygen, ammonia, and nitrite plus nitrate-nitrogen were greatest during winter. Concentrations of dissolved oxygen, fluoride, sulfate, total suspended solids, iron, and manganese generally increased with time. Concentrations of chloride, nitrite plus nitrate-nitrogen, dissolved phosphorus, dissolved orthophosphate, biochemical oxygen demand, dieldrin, and lindane decreased with time. There was relatively little change in land use from the late 1970s to the mid-1990s due to relatively modest rates of population growth in the study area during that period. Most changes in water quality in these streams and rivers may be due to changes in chemical use and wastewater treatment practices.</p>\n<p>The sampling network was evaluated with respect to areal coverage, sampling frequency, and analytical schedules. Areal coverage could be expanded to include one additional watershed that is not part of the current network. A new sampling site on the North Canadian River might be useful because of expanding urbanization west of the city, but sampling at some other sites could be discontinued or reduced based on comparisons of data between the sites. Additional real-time or periodic monitoring for dissolved oxygen may be useful to prevent anoxic conditions in pools behind new low-water dams. The sampling schedules, both monthly and quarterly, are adequate to evaluate trends, but additional sampling during flow extremes may be needed to quantify loads and evaluate water-quality during flow extremes. Emerging water-quality issues may require sampling for volatile organic compounds, sulfide, total phosphorus, chlorophyll-<i>a</i>, <i>Esherichia coli</i>, and enterococci, as well as use of more sensitive laboratory analytical methods for determination of cadmium, mercury, lead, and silver.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Oklahoma City, OK","doi":"10.3133/wri024111","collaboration":"Prepared in cooperation with the City of Oklahoma City","usgsCitation":"Brigham, M.E., Payne, G.A., Andrews, W.J., and Abbott, M.M., 2002, Statistical analysis of stream water-quality data and sampling network design near Oklahoma City, central Oklahoma, 1977-1999: U.S. Geological Survey Water-Resources Investigations Report 2002-4111, vi, 125 p., https://doi.org/10.3133/wri024111.","productDescription":"vi, 125 p.","numberOfPages":"133","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":97427,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4111/report.pdf","size":"17531","linkFileType":{"id":1,"text":"pdf"}},{"id":172681,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2002/4111/report-thumb.jpg"}],"country":"United States","state":"Oklahoma","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.25,\n              35.92\n            ],\n            [\n              -97.1,\n              35.92\n            ],\n            [\n              -97.1,\n              35.3\n            ],\n            [\n              -98.38,\n              35.3\n            ],\n            [\n              -98.38,\n              35.6\n            ],\n            [\n              -98.4,\n              35.6\n            ],\n            [\n              -98.4,\n              35.8\n            ],\n            [\n              -98.25,\n              35.8\n            ],\n            [\n              -98.25,\n              35.92\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dde4b07f02db5e2222","contributors":{"authors":[{"text":"Brigham, Mark E. 0000-0001-7412-6800 mbrigham@usgs.gov","orcid":"https://orcid.org/0000-0001-7412-6800","contributorId":1840,"corporation":false,"usgs":true,"family":"Brigham","given":"Mark","email":"mbrigham@usgs.gov","middleInitial":"E.","affiliations":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":222739,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Payne, Gregory A.","contributorId":43819,"corporation":false,"usgs":true,"family":"Payne","given":"Gregory","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":222740,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Andrews, William J. 0000-0003-4780-8835 wandrews@usgs.gov","orcid":"https://orcid.org/0000-0003-4780-8835","contributorId":328,"corporation":false,"usgs":true,"family":"Andrews","given":"William","email":"wandrews@usgs.gov","middleInitial":"J.","affiliations":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"preferred":true,"id":222738,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Abbott, Marvin M.","contributorId":89106,"corporation":false,"usgs":true,"family":"Abbott","given":"Marvin","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":222741,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":40009,"text":"ofr02399 - 2002 - Chemical analyses of soils, soil leaches, rocks, and stream sediments from Guam and the Western United States and sample location maps of Guam","interactions":[],"lastModifiedDate":"2012-02-02T00:09:50","indexId":"ofr02399","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","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":"2002-399","title":"Chemical analyses of soils, soil leaches, rocks, and stream sediments from Guam and the Western United States and sample location maps of Guam","language":"ENGLISH","doi":"10.3133/ofr02399","usgsCitation":"Miller, W.R., Sanzolone, R.F., Lamothe, P.J., and Ziegler, T.L., 2002, Chemical analyses of soils, soil leaches, rocks, and stream sediments from Guam and the Western United States and sample location maps of Guam: U.S. Geological Survey Open-File Report 2002-399, 72 p., https://doi.org/10.3133/ofr02399.","productDescription":"72 p.","costCenters":[],"links":[{"id":3522,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0399/","linkFileType":{"id":5,"text":"html"}},{"id":165263,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4a02","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":222826,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sanzolone, Richard F.","contributorId":88007,"corporation":false,"usgs":true,"family":"Sanzolone","given":"Richard","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":222827,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lamothe, Paul J. plamothe@usgs.gov","contributorId":1298,"corporation":false,"usgs":true,"family":"Lamothe","given":"Paul","email":"plamothe@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":222824,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ziegler, Thomas L.","contributorId":20381,"corporation":false,"usgs":true,"family":"Ziegler","given":"Thomas","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":222825,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":32696,"text":"fs13001 - 2002 - The USGS role in TMDL assessments","interactions":[],"lastModifiedDate":"2020-12-02T14:56:43.086176","indexId":"fs13001","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","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":"130-01","displayTitle":"The USGS Role in TMDL Assessments","title":"The USGS role in TMDL assessments","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs13001","usgsCitation":"Shipp, A.A., and Cordy, G.E., 2002, The USGS role in TMDL assessments: U.S. Geological Survey Fact Sheet 130-01, 4 p., https://doi.org/10.3133/fs13001.","productDescription":"4 p.","costCenters":[{"id":49157,"text":"Rocky Mountain Regional 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,{"id":39967,"text":"wri024022 - 2002 - Hydrogeology and simulation of ground-water flow and land-surface subsidence in the Chicot and Evangeline aquifers, Houston area, Texas","interactions":[],"lastModifiedDate":"2017-01-18T15:59:10","indexId":"wri024022","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2002-4022","title":"Hydrogeology and simulation of ground-water flow and land-surface subsidence in the Chicot and Evangeline aquifers, Houston area, Texas","docAbstract":"<p>In November 1997, the U.S. Geological Survey, in cooperation with the City of Houston Utilities Planning Section and the City of Houston Department of Public Works &amp; Engineering, began an investigation of the Chicot and Evangeline aquifers in the greater Houston area in Texas to better understand the hydrology, flow, and associated land-surface subsidence. The principal part of the investigation was a numerical finite-difference model (MODFLOW) developed to simulate ground-water flow and land-surface subsidence in an 18,100-square-mile area encompassing greater Houston.</p><p>The focus of the study was Harris and Galveston Counties, but other counties were included to achieve the appropriate boundary conditions. The model was vertically discretized into three 103-row by 109-column layers resulting in a total of 33,681 grid cells. Layer 1 represents the water table using a specified head, layer 2 represents the Chicot aquifer, and layer 3 represents the Evangeline aquifer.</p><p>Simulations were made under transient conditions for 31 ground-water-withdrawal (stress) periods spanning 1891–1996. The years 1977 and 1996 were chosen as potentiometric-surface calibration periods for the model. Simulated and measured potentiometric surfaces of the Chicot and Evangeline aquifers for 1977 match closely. Waterlevel measurements indicate that by 1977, large ground-water withdrawals in east-central and southeastern areas of Harris County had caused the potentiometric surfaces to decline as much as 250 feet below sea level in the Chicot aquifer and as much as 350 feet below sea level in the Evangeline aquifer. Simulated and measured potentiometric surfaces of the Chicot and Evangeline aquifers for 1996 also match closely. The large potentiometric-surface decline in 1977 in the southeastern Houston area showed significant recovery by 1996. The 1996 centers of potentiometric-surface decline are located much farther northwest. Potentiometric-surface declines of more than 200 feet below sea level in the Chicot aquifer and more than 350 feet below sea level in the Evangeline aquifer were measured in observation wells and simulated in the flow model.</p><p>Simulation of land-surface subsidence and water released from storage in the clay layers was accomplished using the Interbed-Storage Package of the MODFLOW model. Land-surface subsidence was calibrated by comparing simulated long-term (1891–1995) and short-term (1978–95) land-surface subsidence with published maps of land-surface subsidence for about the same period until acceptable matches were achieved.</p><p>Simulated 1996 Chicot aquifer flow rates indicate that a net flow of 562.5 cubic feet per second enters the Chicot aquifer in the outcrop area, and a net flow of 459.5 cubic feet per second passes through the Chicot aquifer into the Evangeline aquifer. The remaining 103.0 cubic feet per second of flow is withdrawn as pumpage, with a shortfall of about 84.9 cubic feet per second supplied to the wells from storage in sands and clays. Water simulated from storage in clays in the Chicot aquifer is about 19 percent of the total water withdrawn from the aquifer.</p><p>Simulated 1996 Evangeline aquifer flow rates indicate that a net flow of 14.8 cubic feet per second enters the Evangeline aquifer in the outcrop area, and a net flow of 459.5 cubic feet per second passes through the Chicot aquifer into the Evangeline aquifer for a total inflow of 474.3 cubic feet per second. A greater amount, 528.6 cubic feet per second, is withdrawn by wells; the shortfall of about 54.8 cubic feet per second is supplied from storage in sands and clays. Water simulated from storage in clays in the Evangeline aquifer is about 10 percent of the total water withdrawn from the aquifer.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri024022","collaboration":"In cooperation with the City of Houston","usgsCitation":"Kasmarek, M.C., and Strom, E.W., 2002, Hydrogeology and simulation of ground-water flow and land-surface subsidence in the Chicot and Evangeline aquifers, Houston area, Texas: U.S. Geological Survey Water-Resources Investigations Report 2002-4022, HTML Document; Report: v, 61 p. , https://doi.org/10.3133/wri024022.","productDescription":"HTML Document; Report: v, 61 p. ","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":170067,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri024022.JPG"},{"id":3657,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024022","linkFileType":{"id":5,"text":"html"}},{"id":333403,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/wri024022/pdf/wri02-4022.pdf","text":"Report","size":"2.56 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Texas","city":"Houston","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97,\n              30\n            ],\n            [\n              -95,\n              31\n            ],\n            [\n              -94,\n              29.5\n            ],\n            [\n              -96,\n              28.4\n            ],\n            [\n              -97,\n              30\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625394","contributors":{"authors":[{"text":"Kasmarek, Mark C. 0000-0003-2808-2506 mckasmar@usgs.gov","orcid":"https://orcid.org/0000-0003-2808-2506","contributorId":1968,"corporation":false,"usgs":true,"family":"Kasmarek","given":"Mark","email":"mckasmar@usgs.gov","middleInitial":"C.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":222706,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Strom, Eric W. ewstrom@usgs.gov","contributorId":337,"corporation":false,"usgs":true,"family":"Strom","given":"Eric","email":"ewstrom@usgs.gov","middleInitial":"W.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true},{"id":559,"text":"South Carolina Water Science Center","active":true,"usgs":true}],"preferred":true,"id":222705,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39995,"text":"ofr02192 - 2002 - Environmental quality and preservation - tiny windows to environmental change: the fascinating world of microfossils","interactions":[],"lastModifiedDate":"2012-02-02T00:10:53","indexId":"ofr02192","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","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":"2002-192","title":"Environmental quality and preservation - tiny windows to environmental change: the fascinating world of microfossils","docAbstract":"Though small in size, calcareous (calcium\r\ncarbonate) microfossils reveal volumes\r\nabout geologic time, events, processes,\r\nand past climate. The U.S. Geological\r\nSurvey (USGS) has the capability to\r\nprovide signifi cant scientifi c information\r\nbased on microfossils that can be used\r\nto help resolve issues raised in many\r\nother disciplines. A source for pioneering\r\ninvestigations and new discoveries little\r\nrecognized outside the fi eld, microfossils\r\nand the stories they tell lie preserved in\r\nthe geologic record.","language":"ENGLISH","doi":"10.3133/ofr02192","usgsCitation":"Lidz, B.H., 2002, Environmental quality and preservation - tiny windows to environmental change: the fascinating world of microfossils: U.S. Geological Survey Open-File Report 2002-192, 6 p., https://doi.org/10.3133/ofr02192.","productDescription":"6 p.","costCenters":[],"links":[{"id":172096,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9157,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/of02-192/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db6021e9","contributors":{"authors":[{"text":"Lidz, Barbara H. blidz@usgs.gov","contributorId":2475,"corporation":false,"usgs":true,"family":"Lidz","given":"Barbara","email":"blidz@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":222783,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39989,"text":"ofr0213 - 2002 - Fracture-correlated lineaments at Great Bay, southeastern New Hampshire","interactions":[],"lastModifiedDate":"2012-02-02T00:10:53","indexId":"ofr0213","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","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":"2002-13","title":"Fracture-correlated lineaments at Great Bay, southeastern New Hampshire","docAbstract":"Analysis by remote-sensing techniques and observations of exposed bedrock structure were preliminary steps taken in a study to locate potential bedrock-fracture zones that may store and transmit ground water near Great Bay, N.H. To help correlate lineaments on the surface with fractures, structural measurements were made at exposed bedrock, largely along the shoreline of the bay, and analyzed to identify fracture trends and fracture characteristics. With these fracture data, lineament-filtering techniques, such as (1) buffer analysis around individual lineaments, (2) discrete-measurement analysis by domain, and (3) spacing-normalized analysis by domain, identified 'fracture-correlated lineaments.' Of the 927 lineaments identified in the study area (180 square kilometers), 406 (44 percent) were evaluated because they either were located within 305 meters of an outcrop with fracture data or intersected one of five 3,300-meter-square grid domain cells that encompassed the fracture data. Of the 406 lineaments, 190 (47 percent) are fracture correlated, although only 15 percent were correlated by more than one filtering technique. \r\n\r\nThe large number of lineaments found in areas of thin glacial overburden and high densities of fractured outcrops suggests that filtering techniques are useful in these areas to selectively identify fracture-correlated lineaments. Fractures parallel to bedding in the Kittery Formation are open locally and often associated with vugs, with up to 1-centimeter aperture, and may provide appreciable secondary porosity in this rock unit. Discrete-measurement analysis by domain identified fracture-correlated lineaments with orientations parallel to these open and vug-filled fractures. Fracture-correlated lineaments related to closely spaced fractures were identified by the spacing-normalized analysis by domain. Analysis results may be used to indicate the potential bedrock pathways for ground-water-discharge points along the shoreline of Great Bay.","language":"ENGLISH","doi":"10.3133/ofr0213","usgsCitation":"Degnan, J.R., and Clark, S.F., 2002, Fracture-correlated lineaments at Great Bay, southeastern New Hampshire: U.S. Geological Survey Open-File Report 2002-13, iv, 14 p. : ill., maps (1 col.) ; 28 cm., 1 over-size sheet, scale 1:24,000 (1 inch = 2,000 feet)., https://doi.org/10.3133/ofr0213.","productDescription":"iv, 14 p. : ill., maps (1 col.) ; 28 cm., 1 over-size sheet, scale 1:24,000 (1 inch = 2,000 feet).","costCenters":[],"links":[{"id":171887,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3673,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/ofr02-013/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a909f","contributors":{"authors":[{"text":"Degnan, James R. 0000-0002-5665-9010 jrdegnan@usgs.gov","orcid":"https://orcid.org/0000-0002-5665-9010","contributorId":498,"corporation":false,"usgs":true,"family":"Degnan","given":"James","email":"jrdegnan@usgs.gov","middleInitial":"R.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":222765,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, Stewart F. 0000-0001-8841-2728 sclark@usgs.gov","orcid":"https://orcid.org/0000-0001-8841-2728","contributorId":3658,"corporation":false,"usgs":true,"family":"Clark","given":"Stewart","email":"sclark@usgs.gov","middleInitial":"F.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":222766,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":32735,"text":"fs02702 - 2002 - Pharmaceuticals, hormones, and other organic wastewater contaminants in U.S. streams","interactions":[],"lastModifiedDate":"2023-08-07T13:37:31.14403","indexId":"fs02702","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","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":"027-02","title":"Pharmaceuticals, hormones, and other organic wastewater contaminants in U.S. streams","docAbstract":"<p>A recent study by the Toxic Substances Hydrology Program of the U.S. Geological Survey (USGS) shows that a broad range of chemicals found in residential, industrial, and agricultural wastewaters commonly occurs in mixtures at low concentrations downstream from areas of intense urbanization and animal production. The chemicals include human and veterinary drugs (including antibiotics), natural and synthetic hormones, detergent metabolites, plasticizers, insecticides, and fire retardants. One or more of these chemicals were found in 80 percent of the streams sampled. Half of the streams contained 7 or more of these chemicals, and about one-third of the streams contained 10 or more of these chemicals. This study is the first national-scale examination of these organic wastewater contaminants in streams and supports the USGS mission to assess the quantity and quality of the Nation's water resources. A more complete analysis of these and other emerging water-quality issues is ongoing.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs02702","usgsCitation":"Buxton, H.T., and Kolpin, D.W., 2002, Pharmaceuticals, hormones, and other organic wastewater contaminants in U.S. streams: U.S. Geological Survey Fact Sheet 027-02, 2 p., https://doi.org/10.3133/fs02702.","productDescription":"2 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":119244,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_027_02.jpg"},{"id":3314,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2002/0027/fs-027-02.pdf","text":"Report","size":"240 KB","linkFileType":{"id":1,"text":"pdf"},"description":"FS-027-02"}],"country":"United States","geographicExtents":"{\n  \"type\": 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,{"id":39932,"text":"wri024143 - 2002 - Simulated changes in the sources of ground water for public-supply wells, ponds, streams, and coastal areas on western Cape Cod, Massachusetts","interactions":[],"lastModifiedDate":"2020-02-18T19:36:31","indexId":"wri024143","displayToPublicDate":"2002-10-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2002-4143","title":"Simulated changes in the sources of ground water for public-supply wells, ponds, streams, and coastal areas on western Cape Cod, Massachusetts","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri024143","usgsCitation":"Masterson, J., Hess, K.M., Walter, D.A., and LeBlanc, D.R., 2002, Simulated changes in the sources of ground water for public-supply wells, ponds, streams, and coastal areas on western Cape Cod, Massachusetts: U.S. Geological Survey Water-Resources Investigations Report 2002-4143, 12 p., https://doi.org/10.3133/wri024143.","productDescription":"12 p.","costCenters":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":164640,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3632,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024143","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Massachusetts ","otherGeospatial":"Cape Cod","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -70.7025146484375,\n              41.49623534616764\n            ],\n            [\n              -69.7796630859375,\n              41.49623534616764\n            ],\n            [\n              -69.7796630859375,\n              42.12267315117256\n            ],\n            [\n              -70.7025146484375,\n              42.12267315117256\n            ],\n            [\n              -70.7025146484375,\n              41.49623534616764\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f38ae","contributors":{"authors":[{"text":"Masterson, John P. 0000-0003-3202-4413 jpmaster@usgs.gov","orcid":"https://orcid.org/0000-0003-3202-4413","contributorId":1865,"corporation":false,"usgs":true,"family":"Masterson","given":"John P.","email":"jpmaster@usgs.gov","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":false,"id":222638,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hess, Kathryn M.","contributorId":49012,"corporation":false,"usgs":true,"family":"Hess","given":"Kathryn","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":222639,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Walter, Donald A. 0000-0003-0879-4477 dawalter@usgs.gov","orcid":"https://orcid.org/0000-0003-0879-4477","contributorId":1101,"corporation":false,"usgs":true,"family":"Walter","given":"Donald","email":"dawalter@usgs.gov","middleInitial":"A.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":222636,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"LeBlanc, Denis R. 0000-0002-4646-2628 dleblanc@usgs.gov","orcid":"https://orcid.org/0000-0002-4646-2628","contributorId":1696,"corporation":false,"usgs":true,"family":"LeBlanc","given":"Denis","email":"dleblanc@usgs.gov","middleInitial":"R.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":222637,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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