No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055290","usgsCitation":"Brush, C.F., Belitz, K., Phillips, S.P., Burow, K.R., and Knifong, D.L., 2006, MODGRASS: Update of a ground-water flow model for the central part of the western San Joaquin Valley, California: U.S. Geological Survey Scientific Investigations Report 2005-5290, *Report has been removed by the request of the authors*, https://doi.org/10.3133/sir20055290.","productDescription":"*Report has been removed by the request of the authors*","numberOfPages":"92","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":190702,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":115733,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5290/","linkFileType":{"id":5,"text":"html"}},{"id":400906,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_77419.htm"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648d47","contributors":{"authors":[{"text":"Brush, Charles F.","contributorId":93140,"corporation":false,"usgs":true,"family":"Brush","given":"Charles","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":288948,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Belitz, Kenneth 0000-0003-4481-2345 kbelitz@usgs.gov","orcid":"https://orcid.org/0000-0003-4481-2345","contributorId":442,"corporation":false,"usgs":true,"family":"Belitz","given":"Kenneth","email":"kbelitz@usgs.gov","affiliations":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true}],"preferred":true,"id":288944,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Phillips, Steven P. 0000-0002-5107-868X sphillip@usgs.gov","orcid":"https://orcid.org/0000-0002-5107-868X","contributorId":1506,"corporation":false,"usgs":true,"family":"Phillips","given":"Steven","email":"sphillip@usgs.gov","middleInitial":"P.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":288946,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Burow, Karen R. 0000-0001-6006-6667 krburow@usgs.gov","orcid":"https://orcid.org/0000-0001-6006-6667","contributorId":1504,"corporation":false,"usgs":true,"family":"Burow","given":"Karen","email":"krburow@usgs.gov","middleInitial":"R.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":288945,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Knifong, Donna L. dknifong@usgs.gov","contributorId":1517,"corporation":false,"usgs":true,"family":"Knifong","given":"Donna","email":"dknifong@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":288947,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":78568,"text":"sir20065135 - 2006 - Hydrogeologic framework refinement, ground-water flow and storage, water-chemistry analyses, and water-budget components of the Yuma area, southwestern Arizona and southeastern California","interactions":[],"lastModifiedDate":"2023-01-06T19:30:06.793867","indexId":"sir20065135","displayToPublicDate":"2006-08-18T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5135","title":"Hydrogeologic framework refinement, ground-water flow and storage, water-chemistry analyses, and water-budget components of the Yuma area, southwestern Arizona and southeastern California","docAbstract":"The ground-water and surface-water system in the Yuma area in southwestern Arizona and southeastern California is managed intensely to meet water-delivery requirements of customers in the United States, to manage high ground-water levels in the valleys, and to maintain treaty-mandated water-quality and quantity requirements of Mexico. The following components in this report, which were identified to be useful in the development of a ground-water management model, are: (1) refinement of the hydrogeologic framework; (2) updated water-level maps, general ground-water flow patterns, and an estimate of the amount of ground water stored in the mound under Yuma Mesa; (3) review and documentation of the ground-water budget calculated by the Bureau of Reclamation, U.S. Department of the Interior (Reclamation); and (4) water-chemistry characterization to identify the spatial distribution of water quality, information on sources and ages of ground water, and information about the productive-interval depths of the aquifer.
A refined three-dimensional digital hydrogeologic framework model includes the following hydrogeologic units from bottom to top: (1) the effective hydrologic basement of the basin aquifer, which includes the Pliocene Bouse Formation, Tertiary volcanic and sedimentary rocks, and pre-Tertiary metamorphic and plutonic rocks; (2) undifferentiated lower units to represent the Pliocene transition zone and wedge zone; (3) coarse-gravel unit; (4) lower, middle, and upper basin fill to represent the upper, fine-grained zone between the top of the coarse-gravel unit and the land surface; and (5) clay A and clay B. Data for the refined model includes digital elevation models, borehole lithology data, geophysical data, and structural data to represent the geometry of the hydrogeologic units. The top surface of the coarse-gravel unit, defined by using borehole and geophysical data, varies similarly to terraces resulting from the down cutting of the Colorado River. Clay A is nearly the same as the previous conceptual hydrogeologic model definition (Olmsted and others, 1973), except for a minor westward extension from the city of Yuma. Clay B is extended to the southerly international boundary and increased in areal extent by about two-thirds of the original extent (Olmsted and others, 1973). The other hydrogeologic units generally are the same as in the previous conceptual hydrogeologic model.
Before development, the Colorado and Gila Rivers were the sources of nearly all the ground water in the Yuma area through direct infiltration of water from river channels and annual overbank flooding. After construction of upstream reservoirs and clearing and irrigation of the floodplains, the rivers now act as drains for the ground water. Ground-water levels in most of the Yuma area are higher now than they were in predevelopment time. A general gradient of ground-water flow toward the natural discharge area south of the Yuma area still exists, but many other changes in flow are evident. Ground water in Yuma Valley once flowed away from the Colorado River, but now has a component of flow towards the river and Mexicali Valley. A ground-water mound has formed under Yuma Mesa from long-term surface-water irrigation; about 600,000 to 800,000 acre-ft of water are stored in the mound. Ground-water withdrawals adjacent to the southerly international boundary have resulted in water-level declines in that area.
The reviewed and documented water budget includes the following components: (1) recharge in irrigated areas, (2) evapotranspiration by irrigated crops and phreatophytes, (3) ground-water return flow to the Colorado River, and (4) ground-water withdrawals (including those in Mexicali Valley). Recharge components were calculated by subtracting the amount of water used by crops from the amount of water delivered. Evapotranspiration rates were calculated on the basis of established methods, thus were appropriate for input to the ground-water flow model developed by the Bureau of Reclamation (William Greer, hydrologist, Bureau of Reclamation, written commun., 2005). Evapotranspiration by crops and phreatophytes were calculated by using crop coefficient methods and meteorological data. Other methods of calculating evapotranspiration rates by using combinations of satellite imagery and ground-based data could be used for higher spatial and temporal resolution. Ground-water return flow during years of low flow on the Colorado River (1972–82, 1987–92, and 1994–96) averaged 79,000 acre-ft per year. Ground-water withdrawal data for 1970–99 were similar to other estimates made by the U.S. Geological Survey for the Yuma area.
New water-chemistry data were collected in 12 wells and 8 canals/drains to characterize spatial patterns in chemical constituents, determine isotopic ages of water, infer possible sources of ground water, and locate the vertical intervals of the aquifer that contribute most water to wells. Depth-dependent samples were collected at one of the wells (YM-10). A large quantity of water-quality data were compiled from Bureau of Reclamation and U.S. Geological Survey records and merged into the U.S. Geological Survey National Water Information System database. New samples were analyzed for major ions, nutrients, stable isotopes of oxygen and hydrogen, tritium (3H), and carbon-14 (14C) (along with C13/C12 ratios). Light values of oxygen-18 (18O) and deuterium (2H, D) in well 242-2 indicate recharge from the Colorado River. Heavy water samples from wells 242-22, CADC, and Mesa del Sol indicate local recharge sources. Tritium data indicate there is young water in wells in the valleys and near the edge of Yuma Mesa, while older water is found far from the Colorado River. 14C data indicate that water from wells near the southerly international boundary is at least several thousand years old.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20065135","usgsCitation":"Dickinson, J.E., Land, M., Faunt, C., Leake, S.A., Reichard, E.G., Fleming, J.B., and Pool, D.R., 2006, Hydrogeologic framework refinement, ground-water flow and storage, water-chemistry analyses, and water-budget components of the Yuma area, southwestern Arizona and southeastern California: U.S. Geological Survey Scientific Investigations Report 2006-5135, ix, 88 p., https://doi.org/10.3133/sir20065135.","productDescription":"ix, 88 p.","numberOfPages":"97","onlineOnly":"Y","costCenters":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"links":[{"id":192267,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":411509,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_77428.htm","linkFileType":{"id":5,"text":"html"}},{"id":8483,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2006-5135/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Arizona, California","city":"Yuma","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -115,\n 32.8653\n ],\n [\n -115,\n 32.4833 \n ],\n [\n -114.25,\n 32.4833\n ],\n [\n -114.25,\n 32.8653\n ],\n [\n -115,\n 32.8653\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627994","contributors":{"authors":[{"text":"Dickinson, Jesse E. 0000-0002-0048-0839 jdickins@usgs.gov","orcid":"https://orcid.org/0000-0002-0048-0839","contributorId":152545,"corporation":false,"usgs":true,"family":"Dickinson","given":"Jesse","email":"jdickins@usgs.gov","middleInitial":"E.","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":true,"id":288931,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Land, Michael 0000-0001-5141-0307","orcid":"https://orcid.org/0000-0001-5141-0307","contributorId":56613,"corporation":false,"usgs":true,"family":"Land","given":"Michael","affiliations":[],"preferred":false,"id":288936,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Faunt, Claudia C. 0000-0001-5659-7529 ccfaunt@usgs.gov","orcid":"https://orcid.org/0000-0001-5659-7529","contributorId":1491,"corporation":false,"usgs":true,"family":"Faunt","given":"Claudia C.","email":"ccfaunt@usgs.gov","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":288933,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Leake, S. A.","contributorId":52164,"corporation":false,"usgs":true,"family":"Leake","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":288935,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Reichard, Eric G. 0000-0002-7310-3866 egreich@usgs.gov","orcid":"https://orcid.org/0000-0002-7310-3866","contributorId":1207,"corporation":false,"usgs":true,"family":"Reichard","given":"Eric","email":"egreich@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":288932,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Fleming, John B.","contributorId":33788,"corporation":false,"usgs":true,"family":"Fleming","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":288934,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Pool, D. R.","contributorId":75581,"corporation":false,"usgs":true,"family":"Pool","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":288937,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":78569,"text":"ofr20061189 - 2006 - Well construction information, lithologic logs, water level data, and overview of research in Handcart Gulch, Colorado: An alpine watershed affected by metalliferous hydrothermal alteration","interactions":[],"lastModifiedDate":"2023-04-05T21:40:08.60873","indexId":"ofr20061189","displayToPublicDate":"2006-08-18T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-1189","title":"Well construction information, lithologic logs, water level data, and overview of research in Handcart Gulch, Colorado: An alpine watershed affected by metalliferous hydrothermal alteration","docAbstract":"Integrated, multidisciplinary studies of the Handcart Gulch alpine watershed provide a unique opportunity to study and characterize the geology and hydrology of an alpine watershed along the Continental Divide. The study area arose out of the donation of four abandoned, deep mineral exploration boreholes to the U.S. Geological Survey for research purposes by Mineral Systems Inc. These holes were supplemented with nine additional shallow holes drilled by the U.S. Geological Survey along the Handcart Gulch trunk stream. All of the holes were converted into observation wells, and a variety of data and samples were measured and collected from each.\r\n\r\nThis open-file report contains: (1) An overview of the research conducted to date in Handcart Gulch; (2) well location, construction, lithologic log, and water level data from the research boreholes; and (3) a brief synopsis of preliminary results. The primary purpose of this report is to provide a research overview as well as raw data from the boreholes. Interpretation of the data will be reported in future publications. The drill hole data were tabulated into a spreadsheet included with this digital open-file report.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061189","usgsCitation":"Caine, J.S., Manning, A.H., Verplanck, P.L., Bove, D.J., Kahn, K.G., and Ge, S., 2006, Well construction information, lithologic logs, water level data, and overview of research in Handcart Gulch, Colorado: An alpine watershed affected by metalliferous hydrothermal alteration (Version 1.0): U.S. Geological Survey Open-File Report 2006-1189, Report: iv, 13 p.; Database, https://doi.org/10.3133/ofr20061189.","productDescription":"Report: iv, 13 p.; Database","numberOfPages":"17","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":192268,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8484,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1189/","linkFileType":{"id":5,"text":"html"}},{"id":8485,"rank":3,"type":{"id":9,"text":"Database"},"url":"https://pubs.usgs.gov/of/2006/1189/downloads/xls/HandcartWellData.xls"},{"id":415306,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_77422.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado","otherGeospatial":"Handcart Gulch","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -105.8453,\n 39.5319\n ],\n [\n -105.8453,\n 39.5\n ],\n [\n -105.8089,\n 39.5\n ],\n [\n -105.8089,\n 39.5319\n ],\n [\n -105.8453,\n 39.5319\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698219","contributors":{"authors":[{"text":"Caine, Jonathan S. 0000-0002-7269-6989 jscaine@usgs.gov","orcid":"https://orcid.org/0000-0002-7269-6989","contributorId":1272,"corporation":false,"usgs":true,"family":"Caine","given":"Jonathan","email":"jscaine@usgs.gov","middleInitial":"S.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":false,"id":288942,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Manning, Andrew H. 0000-0002-6404-1237 amanning@usgs.gov","orcid":"https://orcid.org/0000-0002-6404-1237","contributorId":1305,"corporation":false,"usgs":true,"family":"Manning","given":"Andrew","email":"amanning@usgs.gov","middleInitial":"H.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":288939,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Verplanck, Philip L. 0000-0002-3653-6419 plv@usgs.gov","orcid":"https://orcid.org/0000-0002-3653-6419","contributorId":728,"corporation":false,"usgs":true,"family":"Verplanck","given":"Philip","email":"plv@usgs.gov","middleInitial":"L.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":288938,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bove, Dana J. dbove@usgs.gov","contributorId":4855,"corporation":false,"usgs":true,"family":"Bove","given":"Dana","email":"dbove@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":288940,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kahn, Katherine Gurley","contributorId":91944,"corporation":false,"usgs":true,"family":"Kahn","given":"Katherine","email":"","middleInitial":"Gurley","affiliations":[],"preferred":false,"id":288943,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ge, Shemin","contributorId":37366,"corporation":false,"usgs":true,"family":"Ge","given":"Shemin","affiliations":[],"preferred":false,"id":288941,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":78571,"text":"ofr20061236 - 2006 - Scoping of flood hazard mapping needs for Carroll County, New Hampshire","interactions":[],"lastModifiedDate":"2012-03-08T17:16:18","indexId":"ofr20061236","displayToPublicDate":"2006-08-18T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-1236","title":"Scoping of flood hazard mapping needs for Carroll County, New Hampshire","docAbstract":"This report was prepared by the U.S. Geological Survey (USGS) New Hampshire/Vermont Water Science Center for scoping of flood-hazard mapping needs for Carroll County, New Hampshire, under Federal Emergency Management Agency (FEMA) Inter-Agency agreement Number HSFE01-05X-0018. FEMA is embarking on a map modernization program nationwide to:\r\n1. \tGather and develop updated data for all flood prone areas in support of flood plain management.\r\n2. \tProvide maps and data in a digital format for the improvement in the efficiency and precision of the mapping program.\r\n3. \tIntegrate FEMA's community and state partners into the mapping process\r\n\r\nOne of the priorities for FEMA, Region 1, is to develop updated Digital Flood Insurance Rate Maps (DFIRMs) and Flood Insurance Studies (FIS) for Carroll County, New Hampshire. The information provided in this report will be used to develop the scope for the first phase of a multiyear project that will ultimately result in the production of new DFIRMs and FIS for the communities and flooding sources in Carroll County.\r\n\r\nThe average age of the FEMA flood plain maps in Carroll County, New Hampshire is 18 years. Most of these studies were computed in the late 1970s to the mid 1980s. However, in the ensuing 20-30 years, development has occurred in many of the watersheds, and the rivers and streams and their flood plains have changed as a result. In addition, as development has occurred, peak flooding has increased downstream of the development from increased flows across impervious surfaces. Therefore, many of the older studies may not depict current conditions nor accurately estimate risk in terms of flood heights.\r\n\r\nCarroll County gained 3,773 residents between 2000 and 2005. This represents a growth of 8.6 percent compared to 6.0 percent for the state as a whole. Carroll County ranks second (from highest to lowest) out of New Hampshire's 10 counties in terms of rate of population increase. Since 1990, Carroll County has gained 12,029 residents (University of New Hampshire, 2006).","language":"ENGLISH","doi":"10.3133/ofr20061236","usgsCitation":"Flynn, R.H., 2006, Scoping of flood hazard mapping needs for Carroll County, New Hampshire: U.S. Geological Survey Open-File Report 2006-1236, 73 p., https://doi.org/10.3133/ofr20061236.","productDescription":"73 p.","numberOfPages":"73","onlineOnly":"Y","costCenters":[{"id":468,"text":"New Hampshire-Vermont Water Science Center","active":false,"usgs":true}],"links":[{"id":191676,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8487,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1236/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcda4","contributors":{"authors":[{"text":"Flynn, Robert H. rflynn@usgs.gov","contributorId":2137,"corporation":false,"usgs":true,"family":"Flynn","given":"Robert","email":"rflynn@usgs.gov","middleInitial":"H.","affiliations":[{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":288949,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":78573,"text":"ofr20061224 - 2006 - Summary of the stakeholders workshop to develop a National Volcano Early Warning System (NVEWS)","interactions":[],"lastModifiedDate":"2012-02-02T00:14:09","indexId":"ofr20061224","displayToPublicDate":"2006-08-18T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-1224","title":"Summary of the stakeholders workshop to develop a National Volcano Early Warning System (NVEWS)","docAbstract":"The importance of investing in monitoring, mitigation, and preparedness before natural hazards occur has been amply demonstrated by recent disasters such as the Indian Ocean Tsunami in December 2004 and Hurricane Katrina in August 2005. Playing catch-up with hazardous natural phenomena such as these limits our ability to work with public officials and the public to lessen adverse impacts. With respect to volcanic activity, the starting point of effective pre-event mitigation is monitoring capability sufficient to detect and diagnose precursory unrest so that communities at risk have reliable information and sufficient time to respond to hazards with which they may be confronted. \r\n\r\nRecognizing that many potentially dangerous U.S. volcanoes have inadequate or no ground-based monitoring, the U.S Geological Survey (USGS) Volcano Hazards Program (VHP) and partners recently evaluated U.S. volcano-monitoring capabilities and published 'An Assessment of Volcanic Threat and Monitoring Capabilities in the United States: Framework for a National Volcano Early Warning System (NVEWS).' Results of the NVEWS volcanic threat and monitoring assessment are being used to guide long-term improvements to the national volcano-monitoring infrastructure operated by the USGS and affiliated groups. \r\nThe NVEWS report identified the need to convene a workshop of a broad group of stakeholders--such as representatives of emergency- and land-management agencies at the Federal, State, and local levels and the aviation sector--to solicit input about implementation of NVEWS and their specific information requirements. Accordingly, an NVEWS Stakeholders Workshop was held in Portland, Oregon, on 22-23 February 2006. A summary of the workshop is presented in this document.","language":"ENGLISH","doi":"10.3133/ofr20061224","usgsCitation":"Guffanti, M., Scott, W.E., Driedger, C.L., and Ewert, J.W., 2006, Summary of the stakeholders workshop to develop a National Volcano Early Warning System (NVEWS) (Version 1.0): U.S. Geological Survey Open-File Report 2006-1224, 17 p., https://doi.org/10.3133/ofr20061224.","productDescription":"17 p.","numberOfPages":"17","onlineOnly":"Y","costCenters":[],"links":[{"id":192269,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20061224.PNG"},{"id":8491,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1224/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698016","contributors":{"authors":[{"text":"Guffanti, Marianne","contributorId":68257,"corporation":false,"usgs":true,"family":"Guffanti","given":"Marianne","affiliations":[],"preferred":false,"id":288957,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, William E. 0000-0001-8156-979X wescott@usgs.gov","orcid":"https://orcid.org/0000-0001-8156-979X","contributorId":1725,"corporation":false,"usgs":true,"family":"Scott","given":"William","email":"wescott@usgs.gov","middleInitial":"E.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":288956,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Driedger, Carolyn L. 0000-0002-4011-4112 driedger@usgs.gov","orcid":"https://orcid.org/0000-0002-4011-4112","contributorId":537,"corporation":false,"usgs":true,"family":"Driedger","given":"Carolyn","email":"driedger@usgs.gov","middleInitial":"L.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":288954,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ewert, John W. 0000-0003-2819-4057 jwewert@usgs.gov","orcid":"https://orcid.org/0000-0003-2819-4057","contributorId":642,"corporation":false,"usgs":true,"family":"Ewert","given":"John","email":"jwewert@usgs.gov","middleInitial":"W.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":288955,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":78572,"text":"sir20065173 - 2006 - Water-level decline in the Apalachicola River, Florida, from 1954 to 2004, and effects on floodplain habitats","interactions":[],"lastModifiedDate":"2012-02-10T00:11:37","indexId":"sir20065173","displayToPublicDate":"2006-08-18T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5173","title":"Water-level decline in the Apalachicola River, Florida, from 1954 to 2004, and effects on floodplain habitats","docAbstract":"From 1954 to 2004, water levels declined in the nontidal reach of the Apalachicola River, Florida, as a result of long-term changes in stage-discharge relations. Channel widening and deepening, which occurred throughout much of the river, apparently caused the declines. The period of most rapid channel enlargement began in 1954 and occurred primarily as a gradual erosional process over two to three decades, probably in response to the combined effect of a dam located at the head of the study reach (106 miles upstream from the mouth of the river), river straightening, dredging, and other activities along the river. Widespread recovery has not occurred, but channel conditions in the last decade (1995-2004) have been relatively stable. Future channel changes, if they occur, are expected to be minor.\r\n\r\nThe magnitude and extent of water-level decline attributable to channel changes was determined by comparing pre-dam stage (prior to 1954) and recent stage (1995-2004) in relation to discharge. Long-term stage data for the pre-dam period and recent period from five streamflow gaging stations were related to discharge data from a single gage just downstream from the dam, by using a procedure involving streamflow lag times. The resulting pre-dam and recent stage-discharge relations at the gaging stations were used in combination with low-flow water-surface profile data from the U.S. Army Corps of Engineers to estimate magnitude of water-level decline at closely spaced locations (every 0.1 mile) along the river. The largest water-level declines occurred at the lowest discharges and varied with location along the river. The largest water-level decline, 4.8 feet, which occurred when sediments were scoured from the streambed just downstream from the dam, has been generally known and described previously. This large decline progressively decreased downstream to a magnitude of 1 foot about 40 river miles downstream from the dam, which is the location that probably marks the downstream limit of the influence of the dam on bed scour. Downstream from that location, previously unreported water-level declines progressively increased to 3 feet at a location 68 miles downstream from the dam, probably as a result of various channel modifications conducted in that part of the river.\r\n\r\nWater-level declines in the river have substantially changed long-term hydrologic conditions in more than 200 miles of off-channel floodplain sloughs, streams, and lakes and in most of the 82,200 acres of floodplain forests in the nontidal reach of the Apalachicola River. Decreases in duration of floodplain inundation at low discharges were large in the upstream-most 10 miles of the river (20-45 percent) and throughout most of the remaining 75 miles of the nontidal reach (10-25 percent). As a consequence of this decreased inundation, the quantity and quality of floodplain habitats for fish, mussels, and other aquatic organisms have declined, and wetland forests of the floodplain are changing in response to drier conditions. Water-level decline caused by channel change is probably the most serious anthropogenic impact that has occurred so far in the Apalachicola River and floodplain. This decline has been exacerbated by long-term reductions in spring and summer flow, especially during drought periods. Although no trends in total annual flow volumes were detected, long-term decreases in discharge for April, May, July, and August were apparent, and water-level declines during drought conditions resulting from decreased discharge in those 4 months were similar in magnitude to the water-level declines caused by channel changes. The observed changes in seasonal discharge are probably caused by a combination of natural climatic changes and anthropogenic activities in the Apalachicola-Chattahoochee-Flint River Basin. Continued research is needed for geomorphic studies to assist in the design of future floodplain restoration efforts and for hydrologic studies to monitor change","language":"ENGLISH","doi":"10.3133/sir20065173","usgsCitation":"Light, H.M., Vincent, K.R., Darst, M.R., and Price, F.D., 2006, Water-level decline in the Apalachicola River, Florida, from 1954 to 2004, and effects on floodplain habitats: U.S. Geological Survey Scientific Investigations Report 2006-5173, ix, 52 p.; CD-ROM, https://doi.org/10.3133/sir20065173.","productDescription":"ix, 52 p.; CD-ROM","numberOfPages":"61","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"1954-01-01","temporalEnd":"2004-12-31","costCenters":[{"id":275,"text":"Florida Integrated Science Center","active":false,"usgs":true}],"links":[{"id":193154,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8488,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5173/","linkFileType":{"id":5,"text":"html"}},{"id":8489,"rank":9999,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/sir/2006/5173/pdf/appendixesI-X.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":8490,"rank":9999,"type":{"id":9,"text":"Database"},"url":"https://pubs.usgs.gov/sir/2006/5173/executable_files/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -86,29 ], [ -86,35 ], [ -83,35 ], [ -83,29 ], [ -86,29 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7811","contributors":{"authors":[{"text":"Light, Helen M.","contributorId":18355,"corporation":false,"usgs":true,"family":"Light","given":"Helen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":288950,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vincent, Kirk R.","contributorId":64735,"corporation":false,"usgs":true,"family":"Vincent","given":"Kirk","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":288952,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Darst, Melanie R.","contributorId":93042,"corporation":false,"usgs":true,"family":"Darst","given":"Melanie","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":288953,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Price, Franklin D.","contributorId":34597,"corporation":false,"usgs":true,"family":"Price","given":"Franklin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":288951,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":78567,"text":"sir20055288 - 2006 - Rates of evapotranspiration, recharge from precipitation beneath selected areas of native vegetation, and streamflow gain and loss in Carson Valley, Douglas County, Nevada, and Alpine County, California","interactions":[],"lastModifiedDate":"2012-03-08T17:16:19","indexId":"sir20055288","displayToPublicDate":"2006-08-17T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5288","title":"Rates of evapotranspiration, recharge from precipitation beneath selected areas of native vegetation, and streamflow gain and loss in Carson Valley, Douglas County, Nevada, and Alpine County, California","docAbstract":"Rapid growth and development in Carson Valley is causing concern over the continued availability of water resources to sustain such growth into the future. A study to address concerns over water resources and to update estimates of water-budget components in Carson Valley was begun in 2003 by the U.S. Geological Survey, in cooperation with Douglas County, Nevada. This report summarizes micrometeorologic, soil-chloride, and streambed-temperature data collected in Carson Valley from April 2003 through November 2004. Using these data, estimates of rates of discharge by evapotranspiration (ET), rates of recharge from precipitation in areas of native vegetation on the eastern and northern sides of the valley, and rates of recharge and discharge from streamflow infiltration and seepage on the valley floor were calculated. These rates can be used to develop updated water budgets for Carson Valley and to evaluate potential effects of land- and water-use changes on the valley's water budget.\r\n\r\nData from eight ET stations provided estimates of annual ET during water year 2004, the sixth consecutive year of a drought with average or below average precipitation since 1999. Estimated annual ET from flood-irrigated alfalfa where the water table was from 3 to 6 feet below land surface was 3.1 feet. A similar amount of ET, 3.0 feet, was estimated from flood-irrigated alfalfa where the water table was about 40 feet below land surface. Estimated annual ET from flood-irrigated pasture ranged from 2.8 to 3.2 feet where the water table ranged from 2 to 5 feet below land surface, and was 4.4 feet where the water table was within 2 feet from land surface. Annual ET estimated from nonirrigated pasture was 1.7 feet. Annual ET estimated from native vegetation was 1.9 feet from stands of rabbitbrush and greasewood near the northern end of the valley, and 1.5 feet from stands of native bitterbrush and sagebrush covering alluvial fans along the western side of the valley. Uncertainty in most ET estimates is about 12 percent, but ranged from +30 and +50 percent to -20 and -40 percent for nonirrigated pasture and native bitterbrush and sagebrush. Estimated rates for water year 2004 likely are less than those during years of average, or above average precipitation when the water table would be closer to land surface.\r\n\r\nTest holes drilled in areas of native vegetation on the northern and eastern sides of Carson Valley had high concentrations of soil chloride at depths ranging from 4 to 18 feet below land surface at six locations on the eastern side of the valley. The high chloride concentrations indicate that modern-day precipitation at the six locations does not percolate deeper than the root zone of native vegetation. Estimates of the time required to accumulate the measured amount of chloride to depths of about 30 feet below land surface at the six test holes ranged from about 3,000 to 12,000 years.\r\n\r\nLow concentrations of soil chloride in two test holes on the northern end of Carson Valley and in a test hole on the eastern side of Fish Spring Flat indicate that a small amount of recharge from modern-day precipitation is taking place. Estimated annual recharge from precipitation at the two locations was 0.03 and 0.04 foot on the northern end of the valley and 0.02 foot on the eastern side of Fish Spring Flat. Uncertainty in the estimated recharge rates was about ?0.01 foot. Estimates of the time required to accumulate the measured amount of chloride to depths of about 30 feet below land surface at the three test holes ranged from about 100 to 700 years. The two test holes near the northern end of the valley are in gravel and eolian sand deposits and recharge from precipitation may be taking place at similar rates in other areas with gravel and eolian sand deposits. Based on results from other test holes, recharge at the rate estimated for the test hole on the eastern side of Fish Spring Flat is not likely applicable to a large area.\r\n\r\nData from 37 site","language":"ENGLISH","doi":"10.3133/sir20055288","usgsCitation":"Maurer, D.K., Berger, D.L., Tumbusch, M.L., and Johnson, M.J., 2006, Rates of evapotranspiration, recharge from precipitation beneath selected areas of native vegetation, and streamflow gain and loss in Carson Valley, Douglas County, Nevada, and Alpine County, California: U.S. Geological Survey Scientific Investigations Report 2005-5288, vi, 70 p., https://doi.org/10.3133/sir20055288.","productDescription":"vi, 70 p.","numberOfPages":"76","costCenters":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"links":[{"id":8482,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5288/","linkFileType":{"id":5,"text":"html"}},{"id":192330,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120,38 ], [ -120,42 ], [ -118,42 ], [ -118,38 ], [ -120,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648829","contributors":{"authors":[{"text":"Maurer, Douglas K. dkmaurer@usgs.gov","contributorId":2308,"corporation":false,"usgs":true,"family":"Maurer","given":"Douglas","email":"dkmaurer@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":288929,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berger, David L. dlberger@usgs.gov","contributorId":1861,"corporation":false,"usgs":true,"family":"Berger","given":"David","email":"dlberger@usgs.gov","middleInitial":"L.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":288927,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tumbusch, Mary L.","contributorId":37377,"corporation":false,"usgs":true,"family":"Tumbusch","given":"Mary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":288930,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Johnson, Michael J. johnsonm@usgs.gov","contributorId":2282,"corporation":false,"usgs":true,"family":"Johnson","given":"Michael","email":"johnsonm@usgs.gov","middleInitial":"J.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":288928,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":78566,"text":"gip32 - 2006 - Pikes Peak, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:14:12","indexId":"gip32","displayToPublicDate":"2006-08-17T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":315,"text":"General Information Product","code":"GIP","onlineIssn":"2332-354X","printIssn":"2332-3531","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"32","title":"Pikes Peak, Colorado","docAbstract":"For 200 years, Pikes Peak has been a symbol of America's Western Frontier--a beacon that drew prospectors during the great 1859-60 Gold Rush to the 'Pikes Peak country,' the scenic destination for hundreds of thousands of visitors each year, and an enduring source of pride for cities in the region, the State of Colorado, and the Nation.\r\n\r\nNovember 2006 marks the 200th anniversary of the Zebulon M. Pike expedition's first sighting of what has become one of the world's most famous mountains--Pikes Peak. In the decades following that sighting, Pikes Peak became symbolic of America's Western Frontier, embodying the spirit of Native Americans, early explorers, trappers, and traders who traversed the vast uncharted wilderness of the Western Great Plains and the Southern Rocky Mountains.\r\n\r\nHigh-quality printed paper copies of this poster are available at no cost from Information Services, U.S. Geological Survey (1-888-ASK-USGS).","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/gip32","isbn":"1411310004","collaboration":"Prepared in cooperation with the Pikes Peak Lithographing Company, Colorado Springs, Colorado","usgsCitation":"Brunstein, C., Quesenberry, C., Davis, J., Jackson, G., Scott, G., D’Erchia, T.D., Swibas, E., Carter, L., McKinney, K., and Cole, J., 2006, Pikes Peak, Colorado: U.S. Geological Survey General Information Product 32, 2 Sided Poster: 40 x 32.5 inches, https://doi.org/10.3133/gip32.","productDescription":"2 Sided Poster: 40 x 32.5 inches","numberOfPages":"2","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":125078,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/gip_32.jpg"},{"id":8481,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/gip/2006/32/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a92e4b07f02db657a84","contributors":{"authors":[{"text":"Brunstein, Craig (compiler)","contributorId":25248,"corporation":false,"usgs":true,"family":"Brunstein","given":"Craig","suffix":"(compiler)","email":"","affiliations":[],"preferred":false,"id":288921,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Quesenberry, Carol","contributorId":46633,"corporation":false,"usgs":true,"family":"Quesenberry","given":"Carol","affiliations":[],"preferred":false,"id":288926,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Davis, John","contributorId":9357,"corporation":false,"usgs":true,"family":"Davis","given":"John","affiliations":[],"preferred":false,"id":288918,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jackson, Gene","contributorId":18859,"corporation":false,"usgs":true,"family":"Jackson","given":"Gene","email":"","affiliations":[],"preferred":false,"id":288919,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Scott, Glenn R.","contributorId":33324,"corporation":false,"usgs":true,"family":"Scott","given":"Glenn R.","affiliations":[],"preferred":false,"id":288924,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"D’Erchia, Terry D. tderchia@usgs.gov","contributorId":4197,"corporation":false,"usgs":true,"family":"D’Erchia","given":"Terry","email":"tderchia@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":false,"id":288917,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Swibas, Ed","contributorId":20842,"corporation":false,"usgs":true,"family":"Swibas","given":"Ed","email":"","affiliations":[],"preferred":false,"id":288920,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Carter, Lorna","contributorId":39070,"corporation":false,"usgs":true,"family":"Carter","given":"Lorna","affiliations":[],"preferred":false,"id":288925,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"McKinney, Kevin","contributorId":26766,"corporation":false,"usgs":true,"family":"McKinney","given":"Kevin","affiliations":[],"preferred":false,"id":288922,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Cole, Jim","contributorId":32619,"corporation":false,"usgs":true,"family":"Cole","given":"Jim","email":"","affiliations":[],"preferred":false,"id":288923,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}} ,{"id":78564,"text":"ofr20061216 - 2006 - Helicopter electromagnetic and magnetic survey maps and data, East Poplar oil field area, Fort Peck Indian Reservation, northeastern Montana, August 2004","interactions":[],"lastModifiedDate":"2021-09-22T21:08:49.83055","indexId":"ofr20061216","displayToPublicDate":"2006-08-15T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-1216","title":"Helicopter electromagnetic and magnetic survey maps and data, East Poplar oil field area, Fort Peck Indian Reservation, northeastern Montana, August 2004","docAbstract":"This report is a data release for a helicopter electromagnetic and magnetic survey that was conducted during August 2004 in a 275-square-kilometer area that includes the East Poplar oil field on the Fort Peck Indian Reservation. The electromagnetic equipment consisted of six different coil-pair orientations that measured resistivity at separate frequencies from about 400 hertz to about 140,000 hertz. The electromagnetic resistivity data were converted to six electrical conductivity grids, each representing different approximate depths of investigation. The range of subsurface investigation is comparable to the depth of shallow aquifers. Areas of high conductivity in shallow aquifers in the East Poplar oil field area are being delineated by the U.S. Geological Survey, in cooperation with the Fort Peck Assiniboine and Sioux Tribes, in order to map areas of saline-water plumes. Ground electromagnetic methods were first used during the early 1990s to delineate more than 31 square kilometers of high conductivity saline-water plumes in a portion of the East Poplar oil field area. In the 10 years since the first delineation, the quality of water from some wells completed in the shallow aquifers in the East Poplar oil field changed markedly. The extent of saline-water plumes in 2004 likely differs from that delineated in the early 1990s. The geophysical and hydrologic information from U.S. Geological Survey studies is being used by resource managers to develop ground-water resource plans for the area.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061216","usgsCitation":"Smith, B.D., Thamke, J., Cain, M.J., Tyrrell, C., and Hill, P.L., 2006, Helicopter electromagnetic and magnetic survey maps and data, East Poplar oil field area, Fort Peck Indian Reservation, northeastern Montana, August 2004 (Version 1.0): U.S. Geological Survey Open-File Report 2006-1216, Report: iv, 19 p.; Appendix, Spatial Data, https://doi.org/10.3133/ofr20061216.","productDescription":"Report: iv, 19 p.; Appendix, Spatial Data","numberOfPages":"23","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"2004-08-01","temporalEnd":"2004-08-31","costCenters":[],"links":[{"id":191675,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8477,"rank":9999,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/2006/1216/downloads/REPORTS/OF06-1216-Appendix_508.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":389615,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_77423.htm"},{"id":8478,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1216/","linkFileType":{"id":5,"text":"html"}},{"id":8479,"rank":9999,"type":{"id":23,"text":"Spatial Data"},"url":"https://pubs.usgs.gov/of/2006/1216/downloads/GIS/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Montana","otherGeospatial":"East Poplar oil field area, Fort Peck Indian Reservation","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -105.2,\n 48.1219\n ],\n [\n -105.0125,\n 48.1219\n ],\n [\n -105.0125,\n 48.3025\n ],\n [\n -105.2,\n 48.3025\n ],\n [\n -105.2,\n 48.1219\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635dc8","contributors":{"authors":[{"text":"Smith, Bruce D. 0000-0002-1643-2997 bsmith@usgs.gov","orcid":"https://orcid.org/0000-0002-1643-2997","contributorId":845,"corporation":false,"usgs":true,"family":"Smith","given":"Bruce","email":"bsmith@usgs.gov","middleInitial":"D.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":288909,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thamke, Joanna N. 0000-0002-6917-1946 jothamke@usgs.gov","orcid":"https://orcid.org/0000-0002-6917-1946","contributorId":1012,"corporation":false,"usgs":true,"family":"Thamke","given":"Joanna N.","email":"jothamke@usgs.gov","affiliations":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true},{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":true,"id":288910,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cain, Michael J.","contributorId":66359,"corporation":false,"usgs":true,"family":"Cain","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":288913,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tyrrell, Christa","contributorId":13704,"corporation":false,"usgs":true,"family":"Tyrrell","given":"Christa","email":"","affiliations":[],"preferred":false,"id":288912,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hill, Patricia L. pathill@usgs.gov","contributorId":1327,"corporation":false,"usgs":true,"family":"Hill","given":"Patricia","email":"pathill@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":288911,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":78565,"text":"sir20065037 - 2006 - Environmental setting of Maple Creek watershed, Nebraska","interactions":[],"lastModifiedDate":"2012-03-08T17:16:19","indexId":"sir20065037","displayToPublicDate":"2006-08-15T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5037","title":"Environmental setting of Maple Creek watershed, Nebraska","docAbstract":"The Maple Creek watershed covers a 955-square-kilometer area in eastern Nebraska, which is a region dominated by agricultural land use. The Maple Creek watershed is one of seven areas currently included in a nationwide study of the sources, transport, and fate of water and chemicals in agricultural watersheds. This study, known as the topical study of 'Agricultural Chemicals: Sources, Transport, and Fate' is part of the National Water-Quality Assessment Program being conducted by the U.S. Geological Survey. The Program is designed to describe water-quality conditions and trends based on representative surface- and ground-water resources across the Nation. The objective of the Agricultural Chemicals topical study is to investigate the sources, transport, and fate of selected agricultural chemicals in a variety of agriculturally diverse environmental settings. The Maple Creek watershed was selected for the Agricultural Chemicals topical study because its watershed represents the agricultural setting that characterizes eastern Nebraska. This report describes the environmental setting of the Maple Creek watershed in the context of how agricultural practices, including agricultural chemical applications and irrigation methods, interface with natural settings and hydrologic processes. A description of the environmental setting of a subwatershed within the drainage area of Maple Creek is included to improve the understanding of the variability of hydrologic and chemical cycles at two different scales.","language":"ENGLISH","doi":"10.3133/sir20065037","usgsCitation":"Fredrick, B.S., Linard, J.I., and Carpenter, J.L., 2006, Environmental setting of Maple Creek watershed, Nebraska: U.S. Geological Survey Scientific Investigations Report 2006-5037, viii, 22 p., https://doi.org/10.3133/sir20065037.","productDescription":"viii, 22 p.","numberOfPages":"30","onlineOnly":"Y","costCenters":[{"id":464,"text":"Nebraska Water Science Center","active":true,"usgs":true}],"links":[{"id":192362,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8480,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5037/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -97.33333333333333,41.5 ], [ -97.33333333333333,41.916666666666664 ], [ -96.58333333333333,41.916666666666664 ], [ -96.58333333333333,41.5 ], [ -97.33333333333333,41.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688212","contributors":{"authors":[{"text":"Fredrick, Brian S.","contributorId":105392,"corporation":false,"usgs":true,"family":"Fredrick","given":"Brian","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":288916,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Linard, Joshua I. jilinard@usgs.gov","contributorId":1465,"corporation":false,"usgs":true,"family":"Linard","given":"Joshua","email":"jilinard@usgs.gov","middleInitial":"I.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":288914,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carpenter, Jennifer L.","contributorId":12940,"corporation":false,"usgs":true,"family":"Carpenter","given":"Jennifer","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":288915,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":78563,"text":"ofr20061222 - 2006 - Compositional data for Bengal delta sediment collected from boreholes at Srirampur, Kachua, Bangladesh","interactions":[],"lastModifiedDate":"2012-02-10T00:11:45","indexId":"ofr20061222","displayToPublicDate":"2006-08-15T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-1222","title":"Compositional data for Bengal delta sediment collected from boreholes at Srirampur, Kachua, Bangladesh","docAbstract":"Processes active within sediment of the Bengal delta have attracted world concern because of the locally high content of arsenic dissolved in ground water drawn from that sediment. Sediment samples were collected from two boreholes in Srirampur village, Kachua upazila, Chandphur district, Bangladesh, to investigate the processes contributing to arsenic contamination. The samples were mineralogically and chemically analyzed to determine compositional variations related to the arsenic content of the sediment. Mineralogy of the sediments was determined using powder X-ray diffraction. Bulk chemical composition was measured by Combustion, Inductively Coupled Plasma Atomic Emission Spectroscopy, Energy Dispersive X-ray Fluorescence, and Hydride Generation Atomic Absorption Spectrophotometry. Solutions produced by four chemical extractions-0.1 molar strontium chloride, 0.5 normal hydrochloric acid, titanium(III)-EDTA, and a solution of hydrogen peroxide and hydrochloric acid-were analyzed to evaluate the chemical reactivity of the sediment with an emphasis on arsenic residence. Acid-volatile sulfide, acid-soluble sulfate, and reducible sulfide were also measured.\r\n\r\nSediment sampled at Srirampur is typically unlithified, gray, micaceous, feldspathic, arenaceous silt and sand. Arsenic content of the sediment ranges from <1 to 210 ppm, with the highest contents measured in sediment collected at a depth of 320 meters. Samples with high arsenic contents typically contain high concentrations of sulfur. The greatest amount of arsenic was extracted using the oxidative hydrogen peroxide and hydrochloric acid extraction solution. The extraction results are consistent with the apparent association of arsenic in sulfur in the bulk chemical analyses. Pyrite is typically the most abundant form of sulfur in the sediment and is dissolved by the oxidative extraction.","language":"ENGLISH","doi":"10.3133/ofr20061222","usgsCitation":"Breit, G.N., Yount, J., Uddin, N., Muneem, A.A., Lowers, H., Driscoll, R.L., and Whitney, J.W., 2006, Compositional data for Bengal delta sediment collected from boreholes at Srirampur, Kachua, Bangladesh (Revised and reprinted 2006, Version 1.0): U.S. Geological Survey Open-File Report 2006-1222, vi, 51 p., https://doi.org/10.3133/ofr20061222.","productDescription":"vi, 51 p.","numberOfPages":"57","onlineOnly":"Y","costCenters":[],"links":[{"id":195802,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8476,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1222/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 91.53388888888888,23.552500000000002 ], [ 91.53388888888888,23.552500000000002 ], [ 91.535,23.552500000000002 ], [ 91.535,23.552500000000002 ], [ 91.53388888888888,23.552500000000002 ] ] ] } } ] }","edition":"Revised and reprinted 2006, Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7fb1","contributors":{"authors":[{"text":"Breit, George N. 0000-0003-2188-6798 gbreit@usgs.gov","orcid":"https://orcid.org/0000-0003-2188-6798","contributorId":1480,"corporation":false,"usgs":true,"family":"Breit","given":"George","email":"gbreit@usgs.gov","middleInitial":"N.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":288905,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yount, James C.","contributorId":39341,"corporation":false,"usgs":true,"family":"Yount","given":"James C.","affiliations":[],"preferred":false,"id":288906,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Uddin, Nehal","contributorId":60721,"corporation":false,"usgs":true,"family":"Uddin","given":"Nehal","email":"","affiliations":[],"preferred":false,"id":288908,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Muneem, Ad. Atual","contributorId":49873,"corporation":false,"usgs":true,"family":"Muneem","given":"Ad.","email":"","middleInitial":"Atual","affiliations":[],"preferred":false,"id":288907,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lowers, Heather 0000-0001-5360-9264 hlowers@usgs.gov","orcid":"https://orcid.org/0000-0001-5360-9264","contributorId":710,"corporation":false,"usgs":true,"family":"Lowers","given":"Heather","email":"hlowers@usgs.gov","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":false,"id":288902,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Driscoll, Rhonda L. 0000-0001-7725-8956 rdriscoll@usgs.gov","orcid":"https://orcid.org/0000-0001-7725-8956","contributorId":745,"corporation":false,"usgs":true,"family":"Driscoll","given":"Rhonda","email":"rdriscoll@usgs.gov","middleInitial":"L.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":288903,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Whitney, John W. 0000-0003-3824-3692 jwhitney@usgs.gov","orcid":"https://orcid.org/0000-0003-3824-3692","contributorId":804,"corporation":false,"usgs":true,"family":"Whitney","given":"John","email":"jwhitney@usgs.gov","middleInitial":"W.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":288904,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":78562,"text":"sir20065126 - 2006 - Use of dye tracing to determine ground-water movement to Mammoth Crystal Springs, Sylvan Pass area, Yellowstone National Park, Wyoming","interactions":[],"lastModifiedDate":"2017-01-27T10:29:59","indexId":"sir20065126","displayToPublicDate":"2006-08-14T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5126","title":"Use of dye tracing to determine ground-water movement to Mammoth Crystal Springs, Sylvan Pass area, Yellowstone National Park, Wyoming","docAbstract":"At the request of and in cooperation with the Geology Program at Yellowstone National Park, the U.S. Geological Survey conducted a hydrologic investigation of the Sylvan Pass area in June 2005 to determine the relation between surface water and ground-water flow to Mammoth Crystal Springs. Results of a dye-tracing investigation indicate that streamflow lost into talus deposits on Sylvan Pass enters the ground-water system and moves to the southeast to discharge at Mammoth Crystal Springs. Ground-water travel times to the springs from a distance of 1.45 miles and a vertical relief of 500 feet were less than 1 day, indicating apparent rates of movement of at least 8,000 feet per day, values that are similar to those in karst aquifers. Peak dye concentrations were reached about 2 days after dye injection, and transit time of most of the dye mass through the system was about 3 weeks. High permeability and rapid travel times within this aquifer also are indicated by the large variation in springflow in response to snowmelt runoff and precipitation, and by the high concentration of suspended sediment (turbidity) in the water discharging into the spring-fed lake.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20065126","collaboration":"Prepared in cooperation with the National Park Service, Yellowstone National Park","usgsCitation":"Spangler, L.E., and Susong, D.D., 2006, Use of dye tracing to determine ground-water movement to Mammoth Crystal Springs, Sylvan Pass area, Yellowstone National Park, Wyoming: U.S. Geological Survey Scientific Investigations Report 2006-5126, iv, 12 p., https://doi.org/10.3133/sir20065126.","productDescription":"iv, 12 p.","numberOfPages":"19","onlineOnly":"Y","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":125009,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2006_5126.jpg"},{"id":8475,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5126/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Wyoming","otherGeospatial":"Mammoth Crystal Springs, Sylvan Pass, Yellowstone National Park","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.16666666666667,44.450833333333335 ], [ -110.16666666666667,44.483333333333334 ], [ -110.11749999999999,44.483333333333334 ], [ -110.11749999999999,44.450833333333335 ], [ -110.16666666666667,44.450833333333335 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604901","contributors":{"authors":[{"text":"Spangler, Lawrence E. 0000-0003-3928-8809 spangler@usgs.gov","orcid":"https://orcid.org/0000-0003-3928-8809","contributorId":973,"corporation":false,"usgs":true,"family":"Spangler","given":"Lawrence","email":"spangler@usgs.gov","middleInitial":"E.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":288900,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Susong, David D. ddsusong@usgs.gov","contributorId":1040,"corporation":false,"usgs":true,"family":"Susong","given":"David","email":"ddsusong@usgs.gov","middleInitial":"D.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":288901,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70242047,"text":"70242047 - 2006 - Toward \"Supervolcano\" technology","interactions":[],"lastModifiedDate":"2023-04-05T14:27:24.124587","indexId":"70242047","displayToPublicDate":"2006-08-11T09:25:31","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Toward \"Supervolcano\" technology","docAbstract":"In addition to depicting the ultimate volcano-eruption horror story, the recent Discovery Channel/BBC coproduction “Supervolcano” speculates about what technology will be available to the geophysicist in 2025 to monitor active volcanoes. The result is a fictional Virtual Geophysical Laboratory that, when fed the right data, predicts eruption scenarios, thereby providing information to help guide civil emergency-response decisions. On page 821 of this issue, Patanè et al. (1) report a key step toward realizing such an advanced volcano-monitoring technology.
","language":"English","publisher":"AAAS","doi":"10.1126/science.1131790","usgsCitation":"Foulger, G.R., 2006, Toward \"Supervolcano\" technology: Science, v. 313, no. 5788, p. 768-769, https://doi.org/10.1126/science.1131790.","productDescription":"2 p.","startPage":"768","endPage":"769","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":415230,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"313","issue":"5788","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Foulger, Gillian R.","contributorId":34796,"corporation":false,"usgs":true,"family":"Foulger","given":"Gillian","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":868698,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":78043,"text":"tm6B3 - 2006 - Section 3. The SPARROW Surface Water-Quality Model—Theory, application and user documentation","interactions":[],"lastModifiedDate":"2019-03-20T10:59:08","indexId":"tm6B3","displayToPublicDate":"2006-08-10T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":335,"text":"Techniques and Methods","code":"TM","onlineIssn":"2328-7055","printIssn":"2328-7047","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"6-B3","title":"Section 3. The SPARROW Surface Water-Quality Model—Theory, application and user documentation","docAbstract":"SPARROW (SPAtially Referenced Regressions On Watershed attributes) is a watershed modeling technique for relating water-quality measurements made at a network of monitoring stations to attributes of the watersheds containing the stations. The core of the model consists of a nonlinear regression equation describing the non-conservative transport of contaminants from point and diffuse sources on land to rivers and through the stream and river network. The model predicts contaminant flux, concentration, and yield in streams and has been used to evaluate alternative hypotheses about the important contaminant sources and watershed properties that control transport over large spatial scales.
This report provides documentation for the SPARROW modeling technique and computer software to guide users in constructing and applying basic SPARROW models. The documentation gives details of the SPARROW software, including the input data and installation requirements, and guidance in the specification, calibration, and application of basic SPARROW models, as well as descriptions of the model output and its interpretation. The documentation is intended for both researchers and water-resource managers with interest in using the results of existing models and developing and applying new SPARROW models.
The documentation of the model is presented in two parts. Part 1 provides a theoretical and practical introduction to SPARROW modeling techniques, which includes a discussion of the objectives, conceptual attributes, and model infrastructure of SPARROW. Part 1 also includes background on the commonly used model specifications and the methods for estimating and evaluating parameters, evaluating model fit, and generating water-quality predictions and measures of uncertainty. Part 2 provides a user's guide to SPARROW, which includes a discussion of the software architecture and details of the model input requirements and output files, graphs, and maps. The text documentation and computer software are available on the Web at http://usgs.er.gov/sparrow/sparrow-mod.html.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Section B: Ground-water techniques in Book 3: Applications of hydraulics","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey ","publisherLocation":"Reston, VA","doi":"10.3133/tm6B3","usgsCitation":"Schwarz, G., Hoos, A.B., Alexander, R.B., and Smith, R.A., 2006, Section 3. The SPARROW Surface Water-Quality Model—Theory, application and user documentation: U.S. Geological Survey Techniques and Methods 6-B3, 248 p., https://doi.org/10.3133/tm6B3.","productDescription":"248 p.","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true}],"links":[{"id":359664,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tm/2006/tm6b3/PDF/tm6b3_contents.pdf","text":"Report ","size":"2 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"- Table of Contents"},{"id":359662,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tm/2006/tm6b3/PDF/tm6b3_titlepages.pdf","text":"Report ","size":"1 MB","linkFileType":{"id":1,"text":"pdf"},"description":"TM 6-B3 ","linkHelpText":"- Title Pages"},{"id":359665,"rank":6,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tm/2006/tm6b3/PDF/tm6b3_part1b.pdf","text":"Report","size":"1.4 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"- Part 1 (continued, p. 30-68)"},{"id":359663,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tm/2006/tm6b3/PDF/tm6b3_part1a.pdf","text":"Report ","size":"1 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"- Abstract and Part 1 (p. 1-29)"},{"id":359667,"rank":11,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tm/2006/tm6b3/PDF/tm6b3_part1d.pdf","text":"Report ","size":".7 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"- Part 1 (continued, p. 98-122)"},{"id":359668,"rank":12,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tm/2006/tm6b3/PDF/tm6b3_part2.pdf","text":"Report","size":"3.6 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"- Part 2 (p. 123-202)"},{"id":9892,"rank":9998,"type":{"id":12,"text":"Errata"},"url":"https://pubs.usgs.gov/tm/2006/tm6b3/errata.htm","linkFileType":{"id":5,"text":"html"}},{"id":359669,"rank":9,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/tm/2006/tm6b3/PDF/tm6b3_appendix.pdf","text":"Appendix A. ","size":".8 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"- Determination of the Bootstrap Confidence Interval Quantiles"},{"id":190713,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tm/2006/tm6b3/coverthb.jpg"},{"id":359666,"rank":10,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tm/2006/tm6b3/PDF/tm6b3_part1c.pdf","text":"Report","size":"1.1 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"- Part 1 (continued, p. 69-97)"},{"id":8461,"rank":9998,"type":{"id":4,"text":"Application Site"},"url":"https://water.usgs.gov/nawqa/sparrow/sparrow-mod.html","linkFileType":{"id":5,"text":"html"}}],"contact":"National Water-Quality Assessment Program
U.S. Geological Survey
413 National Center
12201 Sunrise Valley Drive
Reston, Virginia 20192
https://water.usgs.gov/nawqa/
Chemical analyses and K-Ar ages are presented for rocks sampled from drill holes at Medicine Lake volcano, northern California. A location map and a cross-section are included, as are separate tables for drill hole information, major and trace element data, and for K-Ar dates.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061041","collaboration":"See also OFR 2005-1416","usgsCitation":"Donnelly-Nolan, J.M., 2006, Chemical analyses and K-Ar ages of samples from 13 drill holes, Medicine Lake volcano, California (Version 1.0): U.S. Geological Survey Open-File Report 2006-1041, 20 p., https://doi.org/10.3133/ofr20061041.","productDescription":"20 p.","numberOfPages":"20","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":195515,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20061041.JPG"},{"id":8447,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1041/","linkFileType":{"id":5,"text":"html"}},{"id":8448,"rank":9999,"type":{"id":25,"text":"Version History"},"url":"https://pubs.usgs.gov/of/2006/1041/version_history.txt","linkFileType":{"id":2,"text":"txt"}}],"country":"United States","state":"California","otherGeospatial":"Medicine Lake volcano","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122,\n 41\n ],\n [\n -122,\n 42\n ],\n [\n -121,\n 42\n ],\n [\n -121,\n 41\n ],\n [\n -122,\n 41\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4bf1","contributors":{"authors":[{"text":"Donnelly-Nolan, Julie M. 0000-0001-8714-9606 jdnolan@usgs.gov","orcid":"https://orcid.org/0000-0001-8714-9606","contributorId":3271,"corporation":false,"usgs":true,"family":"Donnelly-Nolan","given":"Julie","email":"jdnolan@usgs.gov","middleInitial":"M.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":288869,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":78169,"text":"ofr20061168 - 2006 - Compilation of water-resources data and hydrogeologic setting for four research stations in the Piedmont and Blue Ridge Physiographic Provinces of North Carolina, 2000—2004","interactions":[],"lastModifiedDate":"2022-07-14T13:50:07.990594","indexId":"ofr20061168","displayToPublicDate":"2006-08-10T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-1168","title":"Compilation of water-resources data and hydrogeologic setting for four research stations in the Piedmont and Blue Ridge Physiographic Provinces of North Carolina, 2000—2004","docAbstract":"Water-resources data were collected to describe the hydrologic conditions at four research stations in the Piedmont and Blue Ridge Physiographic Provinces of North Carolina. Data collected by the U.S. Geological Survey and the North Carolina Department of Environment and Natural Resources, Division of Water Quality, from September 2000 through September 2004 are presented in this report. The locations and periods of data collection are as follows: the Lake Wheeler Road research station (Raleigh) from April 2001 to September 2004, the Langtree Peninsula research station (Mooresville) from September 2000 to September 2004, the Upper Piedmont research station (Reidsville) from March 2002 to September 2004, and the Bent Creek research station (Asheville) from July 2002 to September 2004.\r\n\r\nData presented in this report include well-construction characteristics for 110 wells, periodic ground-water-level measurements for 96 wells, borehole geophysical logs for 23 wells, hourly ground-water-level measurements for 12 wells, continuous-stage measurements for 2 streams, continuous water-quality measurements for 8 wells and 2 streams, periodic water-quality samples for 57 wells and 6 stream sites, slug-test results for 38 wells, and shallow ground-water-flow maps. In addition, the geology and hydrogeology at each site are summarized.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061168","usgsCitation":"Huffman, B.A., Pfeifle, C.A., Chapman, M.J., Bolich, R.E., Campbell, T.R., Geddes, D.J., and Pippin, C.G., 2006, Compilation of water-resources data and hydrogeologic setting for four research stations in the Piedmont and Blue Ridge Physiographic Provinces of North Carolina, 2000—2004 (Version 1.0): U.S. Geological Survey Open-File Report 2006-1168, x, 102 p., https://doi.org/10.3133/ofr20061168.","productDescription":"x, 102 p.","numberOfPages":"112","onlineOnly":"Y","temporalStart":"2000-01-01","temporalEnd":"2004-12-31","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":190950,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":403726,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_77415.htm","linkFileType":{"id":5,"text":"html"}},{"id":8462,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1168/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"North Carolina","otherGeospatial":"Piedmont and Blue Ridge Physiographic Provinces","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -78.6819,\n 35.725\n ],\n [\n -78.6778,\n 35.725\n ],\n [\n -78.6778,\n 35.7306\n ],\n [\n -78.6819,\n 35.7306\n ],\n [\n -78.6819,\n 35.725\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a84ec","contributors":{"authors":[{"text":"Huffman, Brad A. 0000-0003-4025-1325 bahuffma@usgs.gov","orcid":"https://orcid.org/0000-0003-4025-1325","contributorId":1596,"corporation":false,"usgs":true,"family":"Huffman","given":"Brad","email":"bahuffma@usgs.gov","middleInitial":"A.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":288888,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pfeifle, Cassandra A.","contributorId":91939,"corporation":false,"usgs":true,"family":"Pfeifle","given":"Cassandra","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":288893,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chapman, Melinda J. 0000-0003-4021-0320 mjchap@usgs.gov","orcid":"https://orcid.org/0000-0003-4021-0320","contributorId":1597,"corporation":false,"usgs":true,"family":"Chapman","given":"Melinda","email":"mjchap@usgs.gov","middleInitial":"J.","affiliations":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true},{"id":476,"text":"North Carolina Water Science Center","active":true,"usgs":true}],"preferred":true,"id":288889,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bolich, Richard E.","contributorId":89615,"corporation":false,"usgs":true,"family":"Bolich","given":"Richard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":288892,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Campbell, Ted R.","contributorId":41881,"corporation":false,"usgs":true,"family":"Campbell","given":"Ted","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":288890,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Geddes, Donald J. Jr.","contributorId":104991,"corporation":false,"usgs":true,"family":"Geddes","given":"Donald","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":288894,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Pippin, Charles G.","contributorId":64739,"corporation":false,"usgs":true,"family":"Pippin","given":"Charles","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":288891,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":78042,"text":"tm5B2 - 2006 - Determination of wastewater compounds in sediment and soil by pressurized solvent extraction, solid-phase extraction, and capillary-column gas chromatography/mass spectrometry","interactions":[],"lastModifiedDate":"2020-01-26T16:07:16","indexId":"tm5B2","displayToPublicDate":"2006-08-10T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":335,"text":"Techniques and Methods","code":"TM","onlineIssn":"2328-7055","printIssn":"2328-7047","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"5-B2","title":"Determination of wastewater compounds in sediment and soil by pressurized solvent extraction, solid-phase extraction, and capillary-column gas chromatography/mass spectrometry","docAbstract":"No abstract available.
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(Devon), participated in an exploratory drilling and coring program for coal-bed methane in north-central Louisiana. The USGS and LGS collected 25 coal core and cuttings samples from two coal-bed methane test wells that were drilled in west-central Caldwell Parish, Louisiana. The purpose of this report is to provide the results of the analytical program conducted on the USGS/LGS samples. The data generated from this project are summarized in various topical sections that include:\r\n\r\n 1. molecular and isotopic data from coal gas samples;\r\n 2. results of low-temperature ashing and X-ray analysis;\r\n 3. palynological data;\r\n 4. down-hole temperature data;\r\n 5. detailed core descriptions and selected core photographs;\r\n 6. coal physical and chemical analytical data;\r\n 7. coal gas desorption results;\r\n 8. methane and carbon dioxide coal sorption data;\r\n 9. coal petrographic results; and\r\n 10. geophysical logs.\r\n","language":"ENGLISH","doi":"10.3133/ofr20061213","usgsCitation":"Warwick, P.D., Breland, F.C., Hackley, P.C., Dulong, F.T., Nichols, D.J., Karlsen, A.W., Bustin, R., Barker, C., Willett, J.C., and Trippi, M.H., 2006, Analytical results from samples collected during coal-bed methane exploration drilling in Caldwell Parish, Louisiana (Revised and reprinted 2006, Version 1.0): U.S. Geological Survey Open-File Report 2006-1213, vi, 520 p., https://doi.org/10.3133/ofr20061213.","productDescription":"vi, 520 p.","numberOfPages":"526","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":190655,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8445,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1213/","linkFileType":{"id":5,"text":"html"}},{"id":8446,"rank":9999,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://pubs.usgs.gov/of/2006/1213/app7.zip"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -92.26805555555555,32.11666666666667 ], [ -92.26805555555555,32.134166666666665 ], [ -92.26666666666667,32.134166666666665 ], [ -92.26666666666667,32.11666666666667 ], [ -92.26805555555555,32.11666666666667 ] ] ] } } ] }","edition":"Revised and reprinted 2006, Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67ca5f","contributors":{"authors":[{"text":"Warwick, Peter D. 0000-0002-3152-7783 pwarwick@usgs.gov","orcid":"https://orcid.org/0000-0002-3152-7783","contributorId":762,"corporation":false,"usgs":true,"family":"Warwick","given":"Peter","email":"pwarwick@usgs.gov","middleInitial":"D.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":288861,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Breland, F. 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Where they were available we also included the isotopic ratios of strontium, neodymium, and carbon. The database is sub-divided both into material sampled (e.g., volcanic glass, different minerals, fumarole, spring), and into different tectonic settings (MOR, ocean islands, volcanic arcs). Included is also a reference list in MS-Word and pdf from which the data was derived. The database extends previous compilations by Ozima (1994), Farley and Neroda (1998), and Graham (2002). The extended database allows scientists to test competing hypotheses, and it provides a framework for analysis of noble gas data during periods of volcanic unrest.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds202","usgsCitation":"Abedini, A.A., Hurwitz, S., and Evans, W.C., 2006, USGS-NoGaDat - A global dataset of noble gas concentrations and their isotopic ratios in volcanic systems: U.S. Geological Survey Data Series 202, HTML Document; Database; Image, https://doi.org/10.3133/ds202.","productDescription":"HTML Document; Database; Image","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":194499,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8425,"rank":9999,"type":{"id":14,"text":"Image"},"url":"https://pubs.usgs.gov/ds/2006/202/htdocs/SampleMap.gif"},{"id":8426,"rank":9999,"type":{"id":9,"text":"Database"},"url":"https://pubs.usgs.gov/ds/2006/202/htdocs/NogaDat-V1.0%20-%200629006.xls"},{"id":8424,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/2006/202/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f848","contributors":{"authors":[{"text":"Abedini, Atosa A.","contributorId":69668,"corporation":false,"usgs":false,"family":"Abedini","given":"Atosa","email":"","middleInitial":"A.","affiliations":[{"id":6672,"text":"former: USGS Southwest Biological Science Center, Colorado Plateau Research Station, Flagstaff, AZ. 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