{"pageNumber":"814","pageRowStart":"20325","pageSize":"25","recordCount":68927,"records":[{"id":70004255,"text":"70004255 - 2009 - Evaluation of methods and uncertainties in the chemical budgets","interactions":[],"lastModifiedDate":"2021-03-29T18:07:35.705039","indexId":"70004255","displayToPublicDate":"2015-05-04T09:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"5","title":"Evaluation of methods and uncertainties in the chemical budgets","docAbstract":"<p><span>This chapter examines the uncertainties inherent in the water and chemical budgets of the lake in relation to the differences between chemical mass change in storage and to the balance between solute inputs and solute outputs associated with water fluxes. It begins by discussing uncertainty in the water budgets used to determine chemical budgets. It then examines uncertainties in chemical analyses of precipitation samples, surface water samples, and groundwater samples. It also discusses alternative approaches to determining chemical budgets. It describes the methods used to calculate chemical mass input from the tributaries, chemical mass loss by surface outflow, chemical mass input from groundwater, and chemical mass loss by flow through groundwater.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Mirror Lake: Interactions among air, land, and water","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"University of California Press","doi":"10.1525/california/9780520261198.003.0005","usgsCitation":"LaBaugh, J.W., Buso, D.C., and Likens, G.E., 2009, Evaluation of methods and uncertainties in the chemical budgets, chap. 5 <i>of</i> Mirror Lake: Interactions among air, land, and water, p. 225-295, https://doi.org/10.1525/california/9780520261198.003.0005.","productDescription":"71 p.","startPage":"225","endPage":"295","numberOfPages":"71","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-004925","costCenters":[{"id":493,"text":"Office of Ground 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,{"id":70120865,"text":"70120865 - 2009 - Online interactive U.S. Reservoir Sedimentation Survey Database","interactions":[],"lastModifiedDate":"2014-08-18T10:27:35","indexId":"70120865","displayToPublicDate":"2013-08-18T10:22:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Online interactive U.S. Reservoir Sedimentation Survey Database","docAbstract":"<p>In April 2009, the U.S. Geological Survey and the Natural Resources Conservation Service (prior to 1994, the Soil Conservation Service) created the Reservoir Sedimentation Survey Database (RESSED) and Web site, the most comprehensive compilation of data from reservoir bathymetric and dry basin surveys in the United States. RESSED data can be useful for a number of purposes, including calculating changes in reservoir storage characteristics, quantifying rates of sediment delivery to reservoirs, and estimating erosion rates in a reservoir's watershed.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Eos, Transactions American Geophysical Union","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wiley","doi":"10.1029/2009EO230003","usgsCitation":"Gray, J., Bernard, J., Schwarz, G., Stewart, D.W., and Ray, K., 2009, Online interactive U.S. Reservoir Sedimentation Survey Database: Eos, Transactions, American Geophysical Union, v. 90, no. 23, https://doi.org/10.1029/2009EO230003.","productDescription":"1 p.","startPage":"199","costCenters":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"links":[{"id":475967,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2009eo230003","text":"Publisher Index Page"},{"id":292389,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":292387,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2009EO230003"}],"country":"Puerto Rico;United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 144.616667,12.233333 ], [ 144.616667,71.833333 ], [ -64.566667,71.833333 ], [ -64.566667,12.233333 ], [ 144.616667,12.233333 ] ] ] } } ] }","volume":"90","issue":"23","noUsgsAuthors":false,"publicationDate":"2011-06-03","publicationStatus":"PW","scienceBaseUri":"53f25fe9e4b033341871893b","contributors":{"authors":[{"text":"Gray, J.B.","contributorId":73119,"corporation":false,"usgs":true,"family":"Gray","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":498503,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bernard, J.M.","contributorId":43999,"corporation":false,"usgs":true,"family":"Bernard","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":498502,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schwarz, G. E. 0000-0002-9239-4566","orcid":"https://orcid.org/0000-0002-9239-4566","contributorId":14852,"corporation":false,"usgs":true,"family":"Schwarz","given":"G. E.","affiliations":[],"preferred":false,"id":498501,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stewart, D. W.","contributorId":86194,"corporation":false,"usgs":true,"family":"Stewart","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":498505,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ray, K.T.","contributorId":77758,"corporation":false,"usgs":true,"family":"Ray","given":"K.T.","email":"","affiliations":[],"preferred":false,"id":498504,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70047115,"text":"70047115 - 2009 - Remote sensing of global croplands for food security: Way forward","interactions":[],"lastModifiedDate":"2021-04-09T13:30:46.266619","indexId":"70047115","displayToPublicDate":"2013-01-01T15:58:39","publicationYear":"2009","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"20","title":"Remote sensing of global croplands for food security: Way forward","docAbstract":"<p><span>This book opens a new pathway for global mapping that is focused on a specific land use theme, such as irrigated or rain-fed croplands and classes within these themes. Since croplands use most of the water consumed by humans, specific knowledge of irrigated and rain-fed croplands will be critical for precise estimates of water use. At present and in the coming decades, irrigated and rain-fed cropland area mapping is crucial for food security studies. Throughout this book, various subjects pertaining to global croplands are discussed comprehensively.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Remote sensing of global croplands for food security","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"CRC Press","publisherLocation":"Boca Raton, FL","doi":"10.1201/9781420090109","usgsCitation":"Thenkabail, P.S., and Lyon, J., 2009, Remote sensing of global croplands for food security: Way forward, chap. 20 <i>of</i> Remote sensing of global croplands for food security, p. 461-466, https://doi.org/10.1201/9781420090109.","productDescription":"6 p.","startPage":"461","endPage":"466","costCenters":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"links":[{"id":275163,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationDate":"2009-06-24","publicationStatus":"PW","scienceBaseUri":"51e90e61e4b0e157e9e86f19","contributors":{"editors":[{"text":"Thenkabail, Prasad S. 0000-0002-2182-8822 pthenkabail@usgs.gov","orcid":"https://orcid.org/0000-0002-2182-8822","contributorId":570,"corporation":false,"usgs":true,"family":"Thenkabail","given":"Prasad","email":"pthenkabail@usgs.gov","middleInitial":"S.","affiliations":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":509381,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Biradar, Chandrashekhar M.","contributorId":16300,"corporation":false,"usgs":true,"family":"Biradar","given":"Chandrashekhar","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":509378,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Turral, Hugh","contributorId":56537,"corporation":false,"usgs":true,"family":"Turral","given":"Hugh","email":"","affiliations":[],"preferred":false,"id":509380,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"Lyon, John G.","contributorId":38044,"corporation":false,"usgs":true,"family":"Lyon","given":"John G.","affiliations":[],"preferred":false,"id":509379,"contributorType":{"id":2,"text":"Editors"},"rank":4}],"authors":[{"text":"Thenkabail, Prasad S. 0000-0002-2182-8822 pthenkabail@usgs.gov","orcid":"https://orcid.org/0000-0002-2182-8822","contributorId":570,"corporation":false,"usgs":true,"family":"Thenkabail","given":"Prasad","email":"pthenkabail@usgs.gov","middleInitial":"S.","affiliations":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":481096,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lyon, John G.","contributorId":38044,"corporation":false,"usgs":true,"family":"Lyon","given":"John G.","affiliations":[],"preferred":false,"id":481097,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70047068,"text":"70047068 - 2009 - Remote sensing of global croplands for food security","interactions":[],"lastModifiedDate":"2021-04-09T13:37:03.224925","indexId":"70047068","displayToPublicDate":"2013-01-01T12:57:00","publicationYear":"2009","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":15,"text":"Monograph"},"title":"Remote sensing of global croplands for food security","docAbstract":"Increases in populations have created an increasing demand for food crops while increases in demand for biofuels have created an increase in demand for fuel crops. What has not increased is the amount of croplands and their productivity. These and many other factors such as decreasing water resources in a changing climate have created a crisis like situation in global food security. Decision makers in these situations need accurate information based on science. Remote Sensing of Global Croplands for Food Security provides a comprehensive knowledge base in use of satellite sensor-based maps and statistics that can be used to develop strategies for croplands (irrigated and rainfed) and their water use for food security.","language":"English","publisher":"CRC Press","publisherLocation":"Boca Raton, FL","doi":"10.1201/9781420090109","isbn":"978-1-4200-9009-3","usgsCitation":"Thenkabail, P.S., Biradar, C.M., Turral, H., and Lyon, J., 2009, Remote sensing of global croplands for food security, xxxi, 476 p., https://doi.org/10.1201/9781420090109.","productDescription":"xxxi, 476 p.","costCenters":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"links":[{"id":275073,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationDate":"2009-06-24","publicationStatus":"PW","scienceBaseUri":"51e66b6be4b017be1ba347b8","contributors":{"authors":[{"text":"Thenkabail, Prasad S. 0000-0002-2182-8822 pthenkabail@usgs.gov","orcid":"https://orcid.org/0000-0002-2182-8822","contributorId":570,"corporation":false,"usgs":true,"family":"Thenkabail","given":"Prasad","email":"pthenkabail@usgs.gov","middleInitial":"S.","affiliations":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":480966,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Biradar, Chandrashekhar M.","contributorId":16300,"corporation":false,"usgs":true,"family":"Biradar","given":"Chandrashekhar","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":480967,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Turral, Hugh","contributorId":56537,"corporation":false,"usgs":true,"family":"Turral","given":"Hugh","email":"","affiliations":[],"preferred":false,"id":480969,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lyon, John G.","contributorId":38044,"corporation":false,"usgs":true,"family":"Lyon","given":"John G.","affiliations":[],"preferred":false,"id":480968,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70046837,"text":"70046837 - 2009 - Climate and hydrological changes in the northeastern United States: recent trends and implications for forested and aquatic ecosystems","interactions":[],"lastModifiedDate":"2022-11-22T23:03:45.826356","indexId":"70046837","displayToPublicDate":"2013-01-01T11:25:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1170,"text":"Canadian Journal of Forest Research","active":true,"publicationSubtype":{"id":10}},"title":"Climate and hydrological changes in the northeastern United States: recent trends and implications for forested and aquatic ecosystems","docAbstract":"<p><span>We review twentieth century and projected twenty-first century changes in climatic and hydrologic conditions in the northeastern United States and the implications of these changes for forest ecosystems. Climate warming and increases in precipitation and associated changes in snow and hydrologic regimes have been observed over the last century, with the most pronounced changes occurring since 1970. Trends in specific climatic and hydrologic variables differ in their responses spatially (e.g., coastal vs. inland) and temporally (e.g., spring vs. summer). Trends can differ depending on the period of record analyzed, hinting at the role of decadal-scale climatic variation that is superimposed over the longer-term trend. Model predictions indicate that continued increases in temperature and precipitation across the northeastern United States can be expected over the next century. Ongoing increases in growing season length (earlier spring and later autumn) will most likely increase evapotranspiration and frequency of drought. In turn, an increase in the frequency of drought will likely increase the risk of fire and negatively impact forest productivity, maple syrup production, and the intensity of autumn foliage coloration. Climate and hydrologic changes could have profound effects on forest structure, composition, and ecological functioning in response to the changes discussed here and as described in related articles in this issue of the Journal.</span></p>","language":"English","publisher":"Canadian Science Press","doi":"10.1139/X08-116","usgsCitation":"Huntington, T.G., Richardson, A., McGuire, K.J., and Hayhoe, K., 2009, Climate and hydrological changes in the northeastern United States: recent trends and implications for forested and aquatic ecosystems: Canadian Journal of Forest Research, v. 39, no. 2, p. 199-212, https://doi.org/10.1139/X08-116.","productDescription":"14 p.","startPage":"199","endPage":"212","ipdsId":"IP-007939","costCenters":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"links":[{"id":274868,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Connecticut, Maine, 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,{"id":70045908,"text":"70045908 - 2009 - Mineral resource of the month: ferrous slag","interactions":[],"lastModifiedDate":"2013-05-08T17:36:58","indexId":"70045908","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1419,"text":"Earth","active":true,"publicationSubtype":{"id":10}},"title":"Mineral resource of the month: ferrous slag","docAbstract":"The article offers information on mineral resource ferrous slag. Ferrous slag is produced through the addition of materials such as limestone and dolomite to blast and steel furnaces to remove impurities from iron ore and to lower the heat requirements for processes in iron and steel making. It is stated that the method of cooling is important for the market uses and value of ferrous slag. Some types of slag can be used in construction, glass manufacturing and thermal insulation.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"AGI","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2009, Mineral resource of the month: ferrous slag: Earth, v. 54, no. 8, p. 39-39.","productDescription":"1 p.","startPage":"39","endPage":"39","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":272090,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"54","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"518b73ebe4b0037667dbc842","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535503,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70044585,"text":"wdr2009 - 2009 - Water-resources data for the United States: water year 2009","interactions":[],"lastModifiedDate":"2016-08-22T12:49:11","indexId":"wdr2009","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2009","title":"Water-resources data for the United States: water year 2009","docAbstract":"<p>Water resources data are published annually for use by engineers, scientists, managers, educators, and the general public. These archival products supplement direct access to current and historical water data provided by NWISWeb. Beginning with Water Year 2006, annual water data reports are available as individual electronic Site Data Sheets for the entire Nation for retrieval, download, and localized printing on demand. National distribution includes tabular and map interfaces for search, query, display and download of data. From 1962 until 2005, reports were published by State as paper documents, although most reports since the mid-1990s are also available in electronic form through this web page. Reports prior to 1962 were published in occasional USGS Water-Supply Papers and other reports.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdr2009","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2009, Water-resources data for the United States: water year 2009: U.S. Geological Survey Water Data Report 2009, HTML Document, https://doi.org/10.3133/wdr2009.","productDescription":"HTML Document","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":269338,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr2009.jpg"},{"id":269336,"type":{"id":15,"text":"Index Page"},"url":"https://wdr.water.usgs.gov/wy2009/search.jsp"},{"id":269337,"type":{"id":15,"text":"Index Page"},"url":"https://wdr.water.usgs.gov/"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 172.5,18.9 ], [ 172.5,71.4 ], [ -66.9,71.4 ], [ -66.9,18.9 ], [ 172.5,18.9 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5142f18be4b073a963ff6621","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535453,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70045923,"text":"70045923 - 2009 - Mineral resource of the month: bromine","interactions":[],"lastModifiedDate":"2013-05-08T20:30:00","indexId":"70045923","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1419,"text":"Earth","active":true,"publicationSubtype":{"id":10}},"title":"Mineral resource of the month: bromine","docAbstract":"The article offers information on bromine, a natural element considered as a dissolved species in seawater, saltwater lakes and underground brines linked with petroleum deposits. Bromine belongs to the halogen group of elements and is characterized with brownish-red color and beach-like odor. It is commonly used in flame retardants, agriculture and drilling.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"AGI","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2009, Mineral resource of the month: bromine: Earth, v. 54, no. 4, p. 29-29.","productDescription":"1 p.","startPage":"29","endPage":"29","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":272108,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"54","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"518b73e8e4b0037667dbc819","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535513,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043797,"text":"70043797 - 2009 - Channel water balance and exchange with subsurface flow along a mountain headwater stream in Montana, United States","interactions":[],"lastModifiedDate":"2018-10-12T09:39:08","indexId":"70043797","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Channel water balance and exchange with subsurface flow along a mountain headwater stream in Montana, United States","docAbstract":"Channel water balances of contiguous reaches along streams represent a poorly understood scale of stream-subsurface interaction. We measured reach water balances along a headwater stream in Montana, United States, during summer base flow recessions. Reach water balances were estimated from series of tracer tests in 13 consecutive reaches delineated evenly along a 2.6 km valley segment. For each reach, we estimated net change in discharge, gross hydrologic loss, and gross hydrologic gain from tracer dilution and mass recovery. Four series of tracer tests were performed during relatively high, intermediate, and low base flow conditions. The relative distribution of channel water along the stream was strongly related to a transition in valley structure, with a general increase in gross losses through the recession. During tracer tests at intermediate and low flows, there were frequent substantial losses of tracer mass (>10%) that could not be explained by net loss in flow over the reach, indicating that many of the study reaches were concurrently losing and gaining water. For example, one reach with little net change in discharge exchanged nearly 20% of upstream flow with gains and losses along the reach. These substantial bidirectional exchanges suggest that some channel interactions with subsurface flow paths were not measurable by net change in flow or transient storage of recovered tracer. Understanding bidirectional channel water balances in stream reaches along valleys is critical to an accurate assessment of stream solute fate and transport and to a full assessment of exchanges between the stream channel and surrounding subsurface.","language":"English","publisher":"AGU","doi":"10.1029/2008WR007644","usgsCitation":"Payn, R., Gooseff, M., McGlynn, B., Bencala, K., and Wondzell, S., 2009, Channel water balance and exchange with subsurface flow along a mountain headwater stream in Montana, United States: Water Resources Research, v. 45, no. 11, W11427, https://doi.org/10.1029/2008WR007644.","productDescription":"W11427","ipdsId":"IP-010244","costCenters":[{"id":148,"text":"Branch of Regional Research-Western Region","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":475970,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2008wr007644","text":"Publisher Index Page"},{"id":273512,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":273509,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2008WR007644"}],"country":"United States","state":"Montana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.05,44.36 ], [ -116.05,49.0 ], [ -104.04,49.0 ], [ -104.04,44.36 ], [ -116.05,44.36 ] ] ] } } ] }","volume":"45","issue":"11","noUsgsAuthors":false,"publicationDate":"2009-11-25","publicationStatus":"PW","scienceBaseUri":"51b6f565e4b0097a7158e594","contributors":{"authors":[{"text":"Payn, R.A.","contributorId":18208,"corporation":false,"usgs":true,"family":"Payn","given":"R.A.","affiliations":[],"preferred":false,"id":474239,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gooseff, M.N.","contributorId":21668,"corporation":false,"usgs":true,"family":"Gooseff","given":"M.N.","email":"","affiliations":[],"preferred":false,"id":474241,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McGlynn, B.L.","contributorId":106664,"corporation":false,"usgs":true,"family":"McGlynn","given":"B.L.","email":"","affiliations":[],"preferred":false,"id":474243,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bencala, K.E.","contributorId":105312,"corporation":false,"usgs":true,"family":"Bencala","given":"K.E.","email":"","affiliations":[],"preferred":false,"id":474242,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wondzell, S.M.","contributorId":18599,"corporation":false,"usgs":true,"family":"Wondzell","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":474240,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70045916,"text":"70045916 - 2009 - Mineral resource of the month: thorium","interactions":[],"lastModifiedDate":"2013-05-08T19:50:46","indexId":"70045916","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1419,"text":"Earth","active":true,"publicationSubtype":{"id":10}},"title":"Mineral resource of the month: thorium","docAbstract":"This article provides information on thorium. Thorium is a natural radioactive element that can be found with other minerals. It can be used to generate power, produce light and transmit energy. Thorium has a potential to be used as a nuclear fuel. This element was discovered by Swedish chemist and mineralogist Jóns Jakob Berzelius in 1828.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"AGI","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2009, Mineral resource of the month: thorium: Earth, v. 54, no. 5, p. 27-27.","productDescription":"1 p.","startPage":"27","endPage":"27","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":272098,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"54","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"518b73f4e4b0037667dbc8b2","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535507,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70045920,"text":"70045920 - 2009 - Mineral resource of the month: lime","interactions":[],"lastModifiedDate":"2013-05-08T20:11:19","indexId":"70045920","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1419,"text":"Earth","active":true,"publicationSubtype":{"id":10}},"title":"Mineral resource of the month: lime","docAbstract":"The article presents facts about lime, which is said to be a caustic chemical manufactured from limestone or other calcium carbonates in a kiln at temperatures ranging from 935 to 1,350 degrees Celsius. It states that lime is widely used in industries such as steelmaking, paper production and chemical manufacturing. It also mentions that global lime production amounts up to 280 million metric tons annually. However, it notes that international trade in lime is limited.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"AGI","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2009, Mineral resource of the month: lime: Earth, v. 54, no. 2, p. 29-29.","productDescription":"1 p.","startPage":"29","endPage":"29","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":272103,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"54","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"518b73efe4b0037667dbc875","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535510,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70044164,"text":"70044164 - 2009 - Changes in reproductive biomarkers in an endangered fish species (bonytail chub, Gila elegans) exposed to low levels of organic wastewater compounds in a controlled experiment","interactions":[],"lastModifiedDate":"2018-10-03T10:47:56","indexId":"70044164","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":874,"text":"Aquatic Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Changes in reproductive biomarkers in an endangered fish species (bonytail chub, Gila elegans) exposed to low levels of organic wastewater compounds in a controlled experiment","docAbstract":"In arid regions of the southwestern United States, municipal wastewater treatment plants commonly discharge treated effluent directly into streams that would otherwise be dry most of the year. A better understanding is needed of how effluent-dependent waters (EDWs) differ from more natural aquatic ecosystems and the ecological effect of low levels of environmentally persistent organic wastewater compounds (OWCs) with distance from the pollutant source. In a controlled experiment, we found 26 compounds common to municipal effluent in treatment raceways all at concentrations <1.0 μg/L. Male bonytail chub (Gila elegans) in tanks containing municipal effluent had significantly lower levels of 11-ketotestosterone (p = 0.021) yet higher levels of 17β-estradiol (p = 0.002) and vitellogenin (p = 0.036) compared to control male fish. Female bonytail chub in treatment tanks had significantly lower concentrations of 17β-estradiol than control females (p = 0.001). The normally inverse relationship between primary male and female sex hormones, expected in un-impaired fish, was greatly decreased in treatment (r = 0.00) versus control (r = −0.66) female fish. We found a similar, but not as significant, trend between treatment (r = −0.45) and control (r = −0.82) male fish. Measures of fish condition showed no significant differences between male or female fish housed in effluent or clean water. Inter-sex condition did not occur and testicular and ovarian cells appeared normal for the respective developmental stage and we observed no morphological alteration in fish. The population-level impacts of these findings are uncertain. Studies examining the long-term, generational and behavioral effects to aquatic organisms chronically exposed to low levels of OWC mixtures are needed.","language":"English","publisher":"Elsevier","doi":"10.1016/j.aquatox.2009.08.008","usgsCitation":"Walker, D.B., Paretti, N., Cordy, G., Gross, T.S., Zaugg, S.D., Furlong, E.T., Kolpin, D.W., Matter, W.J., Gwinn, J., and McIntosh, D., 2009, Changes in reproductive biomarkers in an endangered fish species (bonytail chub, Gila elegans) exposed to low levels of organic wastewater compounds in a controlled experiment: Aquatic Toxicology, v. 95, no. 2, p. 133-143, https://doi.org/10.1016/j.aquatox.2009.08.008.","productDescription":"11 p.","startPage":"133","endPage":"143","ipdsId":"IP-003596","costCenters":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":274048,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.aquatox.2009.08.008"},{"id":274049,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.8,24.5 ], [ -124.8,49.383333 ], [ -66.95,49.383333 ], [ -66.95,24.5 ], [ -124.8,24.5 ] ] ] } } ] }","volume":"95","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51c59e32e4b0c89b8f120e1a","contributors":{"authors":[{"text":"Walker, David B.","contributorId":7167,"corporation":false,"usgs":true,"family":"Walker","given":"David","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":474953,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Paretti, Nicholas V. nparetti@usgs.gov","contributorId":802,"corporation":false,"usgs":true,"family":"Paretti","given":"Nicholas V.","email":"nparetti@usgs.gov","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":false,"id":474951,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cordy, Gail","contributorId":32067,"corporation":false,"usgs":true,"family":"Cordy","given":"Gail","email":"","affiliations":[],"preferred":false,"id":474956,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gross, Timothy S.","contributorId":45381,"corporation":false,"usgs":true,"family":"Gross","given":"Timothy","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":474957,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Zaugg, Steven D. sdzaugg@usgs.gov","contributorId":768,"corporation":false,"usgs":true,"family":"Zaugg","given":"Steven","email":"sdzaugg@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":474950,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Furlong, Edward T. 0000-0002-7305-4603 efurlong@usgs.gov","orcid":"https://orcid.org/0000-0002-7305-4603","contributorId":740,"corporation":false,"usgs":true,"family":"Furlong","given":"Edward","email":"efurlong@usgs.gov","middleInitial":"T.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":5046,"text":"Branch of Analytical Serv (NWQL)","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true}],"preferred":true,"id":474949,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kolpin, Dana W. 0000-0002-3529-6505 dwkolpin@usgs.gov","orcid":"https://orcid.org/0000-0002-3529-6505","contributorId":1239,"corporation":false,"usgs":true,"family":"Kolpin","given":"Dana","email":"dwkolpin@usgs.gov","middleInitial":"W.","affiliations":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"preferred":true,"id":474952,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Matter, William J.","contributorId":23424,"corporation":false,"usgs":true,"family":"Matter","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":474955,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Gwinn, Jessica","contributorId":17902,"corporation":false,"usgs":true,"family":"Gwinn","given":"Jessica","email":"","affiliations":[],"preferred":false,"id":474954,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"McIntosh, Dennis","contributorId":91391,"corporation":false,"usgs":true,"family":"McIntosh","given":"Dennis","email":"","affiliations":[],"preferred":false,"id":474958,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70045917,"text":"70045917 - 2009 - Mineral resource of the month: pumice and pumicite","interactions":[],"lastModifiedDate":"2015-09-03T15:39:38","indexId":"70045917","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1419,"text":"Earth","active":true,"publicationSubtype":{"id":10}},"title":"Mineral resource of the month: pumice and pumicite","docAbstract":"<p>The article offers information on pumice, an important commodity for the construction, horticulture and abrasives industries. The commodity is described as an extremely light, highly porous extrusive volcanic rock which was formed due to the rapid cooling of air-pocketed lava. It is noted that the characteristics of pumice make it as an ideal aggregate material in lightweight building blocks in the U.S. and abroad. The leading countries in terms of pumice production are Greece and the U.S.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"AGI","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2009, Mineral resource of the month: pumice and pumicite: Earth, v. 54, no. 6, p. 29-29.","productDescription":"1 p.","startPage":"29","endPage":"29","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":272099,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":307929,"type":{"id":15,"text":"Index Page"},"url":"https://www.earthmagazine.org/issues/june-2009"}],"volume":"54","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"518b73f2e4b0037667dbc893","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535508,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70004012,"text":"70004012 - 2009 - Past climate variability and change in the Arctic and at high latitudes","interactions":[],"lastModifiedDate":"2020-04-17T12:53:21.152226","indexId":"70004012","displayToPublicDate":"2012-07-02T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":290,"text":"Synthesis and Assessment Product","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"1.2","title":"Past climate variability and change in the Arctic and at high latitudes","docAbstract":"Paleoclimate records play a key role in our understanding of Earth's past and present climate system and in our confidence in predicting future climate changes. Paleoclimate data help to elucidate past and present active mechanisms of climate change by placing the short instrumental record into a longer term context and by permitting models to be tested beyond the limited time that instrumental measurements have been available.","language":"English","publisher":"U.S. Climate Change Science Program","publisherLocation":"Washington, D.C.","usgsCitation":"Alley, R.B., Brigham-Grette, J., Miller, G.H., Polyak, L., U.S. Climate Change Science Program, Subcommittee on Global Change Research, and Water Resources Division, U.S. Geological Survey, 2009, Past climate variability and change in the Arctic and at high latitudes: Synthesis and Assessment Product 1.2, 257 p.","productDescription":"257 p.","numberOfPages":"270","costCenters":[{"id":308,"text":"Geology and Environmental Change Science Center","active":false,"usgs":true},{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":258138,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":258137,"rank":300,"type":{"id":15,"text":"Index Page"},"url":"https://www.globalchange.gov/browse/reports/sap-12-past-climate-variability-and-change-arctic-and-high-latitudes","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7584e4b0c8380cd77bbf","contributors":{"authors":[{"text":"Alley, Richard B.","contributorId":34365,"corporation":false,"usgs":false,"family":"Alley","given":"Richard","email":"","middleInitial":"B.","affiliations":[{"id":13035,"text":"Department of Geosciences, Pennsylvania State University","active":true,"usgs":false}],"preferred":false,"id":350144,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brigham-Grette, Julie","contributorId":76176,"corporation":false,"usgs":true,"family":"Brigham-Grette","given":"Julie","email":"","affiliations":[],"preferred":false,"id":350149,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, Gifford H.","contributorId":69402,"corporation":false,"usgs":true,"family":"Miller","given":"Gifford","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":350148,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Polyak, Leonid","contributorId":48014,"corporation":false,"usgs":true,"family":"Polyak","given":"Leonid","email":"","affiliations":[],"preferred":false,"id":350146,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"U.S. Climate Change Science Program","contributorId":128212,"corporation":true,"usgs":false,"organization":"U.S. Climate Change Science Program","id":535125,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Subcommittee on Global Change Research","contributorId":128024,"corporation":true,"usgs":false,"organization":"Subcommittee on Global Change Research","id":535123,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535124,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70003850,"text":"70003850 - 2009 - <i>Introduction to</i> paleoenvironments of Bear Lake, Utah and Idaho, and its catchment","interactions":[],"lastModifiedDate":"2014-05-30T13:38:46","indexId":"70003850","displayToPublicDate":"2012-06-22T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3459,"text":"Special Paper of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"<i>Introduction to</i> paleoenvironments of Bear Lake, Utah and Idaho, and its catchment","docAbstract":"<p>In 1996 a group led by the late Kerry Kelts (University of Minnesota) and Robert Thompson (U.S. Geological Survey) acquired three piston cores (BL96-1, -2, and -3) from Bear Lake. The coring arose from their recognition of Bear Lake as a potential repository of long records of paleoenvironmental change. They recognized that the lake is located in an area that is sensitive to changes in regional climate patterns (Dean et al., this volume), that the lake basin is long lived (see Colman, 2006; Kaufman et al., this volume), and that, unlike many lakes in the Great Basin, Bear Lake was never dry during warm dry periods.</p>\n<br>\n<p>Bear Lake lies in the northeastern Great Basin to the northeast of Great Salt Lake, just south of the Snake River drainage, and a short distance west of the Green River drainage that makes up part of the Upper Colorado River Basin (Fig. 1). Similarity among the historic Bear Lake and Great Salt Lake hydrographs and flows on the Green River indicates that the hydrology of Bear Lake reflects regional precipitation (Fig. 2). Therefore, paleorecords from Bear Lake are important to understanding past climate for a large region, including the Upper Colorado River Basin, the source of much of the water for the southwestern United States.</p>\n<br>\n<p>Initially, paleoenvironmental studies of Bear Lake sediments focused on cores BL96-1, -2, and -3. Additional coring was conducted to elucidate the spatial distribution of sedimentary units and to extend the record back in time. The study was also expanded to include extensive study of the catchment, including the properties of catchment materials and the processes that could potentially affect the delivery of catchment materials to the lake.</p>\n<br>\n<p>Cores BL96-1, -2, and -3 were taken with a Kullenburg piston corer along an east–west profile in roughly 50, 40, and 30 m of water, respectively (Table 1, Fig. 3). These three cores, each taken as a single 4- to 5-m-long segment, provide a nearly complete composite section from ca. 26 cal ka to the late Holocene. In 1998 a number of short gravity cores were taken from the uppermost water-rich sediments that were not sampled by the 1996 cores. During 2000, cores were taken with a percussion piston corer (manufactured by UWITEC) at three locations in and around Mud Lake and at two locations in the northern end of Bear Lake (Fig. 3). Cores acquired with the percussion corer comprise as many as three overlapping segments up to 2 m in length. In 2002, additional percussion piston cores and associated gravity cores of the uppermost sediments were acquired from five sites in the northern half of the lake. In conjunction with two of the cores collected in 2000, these cores form a north–south profile along a seismic line and span water depths from less than 10 m to ~40 m. Data from this profile provide much of the evidence for lake-level variations (Smoot and Rosenbaum, this volume). Finally, during 2000, two long cores, BL00-1D and -1E (collectively referred to here simply as BL00-1), were taken at a site near the depocenter during testing of the GLAD800 coring platform (Fig. 4; Dean et al., 2002). These cores provide a record back to ca. 220 ka.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Special Paper of the Geological Society of America","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Geological Society of America","publisherLocation":"Boulder, CO","doi":"10.1130/2009.2450(00)","usgsCitation":"Rosenbaum, J.G., and Kaufman, D.S., 2009, <i>Introduction to</i> paleoenvironments of Bear Lake, Utah and Idaho, and its catchment: Special Paper of the Geological Society of America, v. 450, p. v-xiii, https://doi.org/10.1130/2009.2450(00).","productDescription":"9 p.","startPage":"v","endPage":"xiii","numberOfPages":"9","costCenters":[{"id":271,"text":"Federal Center","active":false,"usgs":true}],"links":[{"id":257819,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":287883,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1130/2009.2450(00)"}],"country":"United States","state":"Idaho;Utah;Wyoming","otherGeospatial":"Bear Lake;Great Basin;Great Salt Lake;Green River;Snake River;Upper Colorado River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.25,40.0 ], [ -114.25,44.75 ], [ -109.5,44.75 ], [ -109.5,40.0 ], [ -114.25,40.0 ] ] ] } } ] }","volume":"450","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e271e4b0c8380cd45bb4","contributors":{"authors":[{"text":"Rosenbaum, Joseph G. jrosenbaum@usgs.gov","contributorId":1524,"corporation":false,"usgs":true,"family":"Rosenbaum","given":"Joseph","email":"jrosenbaum@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":349147,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kaufman, Darrell S. 0000-0002-7572-1414","orcid":"https://orcid.org/0000-0002-7572-1414","contributorId":28308,"corporation":false,"usgs":true,"family":"Kaufman","given":"Darrell","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":349148,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70038123,"text":"70038123 - 2009 - Technological advances in suspended‐sediment surrogate monitoring","interactions":[],"lastModifiedDate":"2018-04-02T17:15:18","indexId":"70038123","displayToPublicDate":"2012-06-18T12:08:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Technological advances in suspended‐sediment surrogate monitoring","docAbstract":"<p><span>Surrogate technologies to continuously monitor suspended sediment show promise toward supplanting traditional data collection methods requiring routine collection and analysis of water samples. Commercially available instruments operating on bulk optic (turbidity), laser optic, pressure difference, and acoustic backscatter principles are evaluated based on cost, reliability, robustness, accuracy, sample volume, susceptibility to biological fouling, and suitable range of mass concentration and particle size distribution. In situ turbidimeters are widely used. They provide reliable data where the point measurements can be reliably correlated to the river's mean cross section concentration value, effects of biological fouling can be minimized, and concentrations remain below the sensor's upper measurement limit. In situ laser diffraction instruments have similar limitations and can cost 6 times the approximate $5000 purchase price of a turbidimeter. However, laser diffraction instruments provide volumetric‐concentration data in 32 size classes. Pressure differential instruments measure mass density in a water column, thus integrating substantially more streamflow than a point measurement. They are designed for monitoring medium‐to‐large concentrations, are generally unaffected by biological fouling, and cost about the same as a turbidimeter. However, their performance has been marginal in field applications. Acoustic Doppler profilers use acoustic backscatter to measure suspended sediment concentrations in orders of magnitude more streamflow than do instruments that rely on point measurements. The technology is relatively robust and generally immune to effects of biological fouling. Cost of a single‐frequency device is about double that of a turbidimeter. Multifrequency arrays also provide the potential to resolve concentrations by clay silt versus sand size fractions. Multifrequency hydroacoustics shows the most promise for revolutionizing collection of continuous suspended sediment data by instruments that require only periodic calibration for correlation to mean concentrations in river cross sections. Broad application of proven suspended sediment surrogate technologies has the potential to revolutionize fluvial sediment monitoring. Once applied, benefits could be enormous, providing for safer, more frequent and consistent, arguably more accurate, and ultimately less expensive sediment data for managing the world's sedimentary resources.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2008WR007063","usgsCitation":"Gray, J.R., and Gartner, J.W., 2009, Technological advances in suspended‐sediment surrogate monitoring: Water Resources Research, v. 45, no. 4, Article W00D29; 20 p., https://doi.org/10.1029/2008WR007063.","productDescription":"Article W00D29; 20 p.","costCenters":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"links":[{"id":475975,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2008wr007063","text":"Publisher Index Page"},{"id":257928,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"4","noUsgsAuthors":false,"publicationDate":"2009-03-06","publicationStatus":"PW","scienceBaseUri":"505ba43de4b08c986b3201d2","contributors":{"authors":[{"text":"Gray, John R. 0000-0002-8817-3701 jrgray@usgs.gov","orcid":"https://orcid.org/0000-0002-8817-3701","contributorId":1158,"corporation":false,"usgs":true,"family":"Gray","given":"John","email":"jrgray@usgs.gov","middleInitial":"R.","affiliations":[{"id":5058,"text":"Office of the Chief Scientist for Water","active":true,"usgs":true}],"preferred":true,"id":463463,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gartner, Jeffrey W.","contributorId":77524,"corporation":false,"usgs":true,"family":"Gartner","given":"Jeffrey","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":463464,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70038730,"text":"70038730 - 2009 - Sustainable wetland management and support of ecosystem services","interactions":[],"lastModifiedDate":"2018-01-05T11:35:39","indexId":"70038730","displayToPublicDate":"2012-06-18T11:54:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2819,"text":"National Wetlands Newsletter","active":true,"publicationSubtype":{"id":10}},"title":"Sustainable wetland management and support of ecosystem services","docAbstract":"This article is a follow-up on a previous piece in the <i>National Wetlands Newsletter</i> in which we outlined problems associated with a static, local approach to wetland management versus an alternative that proposes a temporal and geomorphic approach (Euliss et al. 2009). We extend that concept by drawing on companion papers recently published in the journal <i>Wetlands</i> (Euliss et al. 2008, Smith et al. 2008). Here we highlight reasons for the failure of many managed wetlands to provide a suite of ecosystem services (e.g., carbon storage, diodiversity, ground-water recharge, contaminant filtering, floodwater storage). Our principal theme is that wetland management is best approached by giving consideration to the hydrogeomorphic processes that maintain productive ecosystems and by removing physical and social impediments to those processes. Traditional management actions are often oriented toward maintaining static conditions in wetlands without considering the temporal cycles that wetlands need to undergo or achieve productivity for specific groups of wildlife, such as waterfowl. Possibly more often, a manager's ability to influence hydrogeomorphic processes is restricted by activities in surrounding watersheds. These could be dams, for example, which do not allow management of flood-pulse processes essential to productivity of riparian systems. In most cases, sediments and nutrients associated with land use in contributing watersheds complicate management of wetlands for a suite of services, including wildlife. Economic or policy forces far-removed from a wetland often interact to prevent occurrence of basic ecosystem processes. Our message is consistent with recommendation of supply-side sustainability of Allen et al. (2002) in which ecosystems are managed \"for the system that produces outputs rather than the outputs themselves.\"","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"National Wetlands Newsletter","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Environmental Law Institute","publisherLocation":"Washington, D.C.","usgsCitation":"Smith, L., Euliss, N.H., Wilcox, D.A., and Brinson, M., 2009, Sustainable wetland management and support of ecosystem services: National Wetlands Newsletter, v. 31, no. 3, p. 4-7, 21.","productDescription":"5 p.","startPage":"4","endPage":"7, 21","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":257927,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba320e4b08c986b31fbaf","contributors":{"authors":[{"text":"Smith, Loren M.","contributorId":88876,"corporation":false,"usgs":true,"family":"Smith","given":"Loren M.","affiliations":[],"preferred":false,"id":464803,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Euliss, Ned H. Jr. ceuliss@usgs.gov","contributorId":2916,"corporation":false,"usgs":true,"family":"Euliss","given":"Ned","suffix":"Jr.","email":"ceuliss@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":false,"id":464800,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilcox, Douglas A.","contributorId":36880,"corporation":false,"usgs":true,"family":"Wilcox","given":"Douglas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":464801,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brinson, Mark M.","contributorId":45761,"corporation":false,"usgs":true,"family":"Brinson","given":"Mark M.","affiliations":[],"preferred":false,"id":464802,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70003362,"text":"70003362 - 2009 - Investigating hydraulic connections and the origin of water in a mine tunnel using stable isotopes and hydrographs","interactions":[],"lastModifiedDate":"2021-03-25T18:36:07.567184","indexId":"70003362","displayToPublicDate":"2012-05-27T11:42:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":835,"text":"Applied Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Investigating hydraulic connections and the origin of water in a mine tunnel using stable isotopes and hydrographs","docAbstract":"Turquoise Lake is a water-supply reservoir located north of the historic Sugarloaf Mining district near Leadville, Colorado, USA. Elevated water levels in the reservoir may increase flow of low-quality water from abandoned mine tunnels in the Sugarloaf District and degrade water quality downstream. The objective of this study was to understand the sources of water to Dinero mine drainage tunnel and evaluate whether or not there was a direct hydrologic connection between Dinero mine tunnel and Turquoise Lake from late 2002 to early 2008. This study utilized hydrograph data from nearby draining mine tunnels and the lake, and stable isotope (&delta;<sup>18</sup>O and &delta;<sup>2</sup>H) data from the lake, nearby draining mine tunnels, imported water, and springs to characterize water sources in the study area. Hydrograph results indicate that flow from the Dinero mine tunnel decreased 26% (2006) and 10% (2007) when lake elevation (above mean sea level) decreased below approximately 3004 m (approximately 9855 feet). Results of isotope analysis delineated two meteoric water lines in the study area. One line characterizes surface water and water imported to the study area from the western side of the Continental Divide. The other line characterizes groundwater including draining mine tunnels, springs, and seeps. Isotope mixing calculations indicate that water from Turquoise Lake or seasonal groundwater recharge from snowmelt represents approximately 10% or less of the water in Dinero mine tunnel. However, most of the water in Dinero mine tunnel is from deep groundwater having minimal isotopic variation. The asymmetric shape of the Dinero mine tunnel hydrograph may indicate that a limited mine pool exists behind a collapse in the tunnel and attenutates seasonal recharge. Alternatively, a conceptual model is presented (and supported with MODFLOW simulations) that is consistent with current and previous data collected in the study area, and illustrates how fluctuating lake levels change the local water-table elevation which can affect discharge from the Dinero mine tunnel without physical transfer of water between the two locations.","language":"English","publisher":"Elsevier","doi":"10.1016/j.apgeochem.2009.09.015","usgsCitation":"Walton-Day, K., and Poeter, E., 2009, Investigating hydraulic connections and the origin of water in a mine tunnel using stable isotopes and hydrographs: Applied Geochemistry, v. 24, no. 12, p. 2266-2282, https://doi.org/10.1016/j.apgeochem.2009.09.015.","productDescription":"17 p.","startPage":"2266","endPage":"2282","temporalStart":"2002-01-01","temporalEnd":"2008-12-31","costCenters":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":257154,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","city":"Leadville","otherGeospatial":"Turquoise Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.4688491821289,\n              39.19581074223468\n            ],\n            [\n              -106.28929138183594,\n              39.19581074223468\n            ],\n            [\n              -106.28929138183594,\n              39.313581716526485\n            ],\n            [\n              -106.4688491821289,\n              39.313581716526485\n            ],\n            [\n              -106.4688491821289,\n              39.19581074223468\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"24","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3e68e4b0c8380cd63d63","contributors":{"authors":[{"text":"Walton-Day, Katherine 0000-0002-9146-6193","orcid":"https://orcid.org/0000-0002-9146-6193","contributorId":68339,"corporation":false,"usgs":true,"family":"Walton-Day","given":"Katherine","affiliations":[],"preferred":false,"id":347022,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poeter, Eileen","contributorId":24616,"corporation":false,"usgs":true,"family":"Poeter","given":"Eileen","affiliations":[],"preferred":false,"id":347021,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70038409,"text":"fs20093003 - 2009 - Streamflow of 2008--Water year summary","interactions":[],"lastModifiedDate":"2012-05-26T01:01:37","indexId":"fs20093003","displayToPublicDate":"2012-05-22T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2009-3003","title":"Streamflow of 2008--Water year summary","docAbstract":"The maps and graphs appearing in this summary describe streamflow conditions for water-year 2008 (October 1, 2007 to September 30, 2008) in the context of the 79-year period 1930-2008, unless otherwise noted. The illustrations are based on observed data from the U.S. Geological Survey's (USGS) National Streamflow Information Program. The period 1930-2008 was used because prior to 1930, the number of streamgages was too small to provide representative data for computing statistics for most regions of the country.\r\nIn the summary, reference is made to the term \"runoff,\" which is the depth to which a river basin, State, or other geographic area would be covered with water if all the streamflow within the area during a single year was uniformly distributed upon it. Runoff quantifies the magnitude of water flowing through the Nation's rivers and streams in measurement units that can be compared from one area to another. The runoff value for a geographic area is computed as the median runoff value for all streamgages in that geographic area. For example, the runoff value for a State is the median for all streamgages in that State, and the median for the Nation is the median value for all streamgages in the Nation.\r\nEach of the maps and graphs below can be expanded to a larger view by clicking on the image. In all the graphics, a rank of 1 indicates the highest flow of all years analyzed.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20093003","usgsCitation":"Xiaodong, J., Wolock, D.M., Lins, H.F., and Brady, S., 2009, Streamflow of 2008--Water year summary: U.S. Geological Survey Fact Sheet 2009-3003, 8 p., https://doi.org/10.3133/fs20093003.","productDescription":"8 p.","onlineOnly":"Y","costCenters":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"links":[{"id":256942,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2009_3003.gif"},{"id":256937,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2009/3003/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9b11e4b08c986b31cc6c","contributors":{"authors":[{"text":"Xiaodong, Jian","contributorId":10260,"corporation":false,"usgs":true,"family":"Xiaodong","given":"Jian","email":"","affiliations":[],"preferred":false,"id":464054,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolock, David M. 0000-0002-6209-938X dwolock@usgs.gov","orcid":"https://orcid.org/0000-0002-6209-938X","contributorId":540,"corporation":false,"usgs":true,"family":"Wolock","given":"David","email":"dwolock@usgs.gov","middleInitial":"M.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true}],"preferred":true,"id":464052,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lins, Harry F. 0000-0001-5385-9247 hlins@usgs.gov","orcid":"https://orcid.org/0000-0001-5385-9247","contributorId":1505,"corporation":false,"usgs":true,"family":"Lins","given":"Harry","email":"hlins@usgs.gov","middleInitial":"F.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":464053,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brady, Steve","contributorId":108351,"corporation":false,"usgs":true,"family":"Brady","given":"Steve","email":"","affiliations":[],"preferred":false,"id":464055,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70003417,"text":"70003417 - 2009 - Estuarine water quality in parks of the Northeast Coastal and Barrier Network: Development and early implementation of vital signs estuarine nutrient-enrichment monitoring, 2003-06","interactions":[],"lastModifiedDate":"2012-05-29T01:01:35","indexId":"70003417","displayToPublicDate":"2012-05-20T09:40:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2828,"text":"Natural Resource Technical Report","active":true,"publicationSubtype":{"id":10}},"title":"Estuarine water quality in parks of the Northeast Coastal and Barrier Network: Development and early implementation of vital signs estuarine nutrient-enrichment monitoring, 2003-06","docAbstract":"This report documents results of pilot tests of a protocol for monitoring estuarine nutrient enrichment for the Vital Signs Monitoring Program of the National Park Service Northeast Coastal and Barrier Network. Data collected from four parks during protocol development in 2003-06 are presented: Gateway National Recreation Area, Colonial National Historic Park, Fire Island National Seashore, and Assateague Island National Seashore. The monitoring approach incorporates several spatial and temporal designs to address questions at a hierarchy of scales. Indicators of estuarine response to nutrient enrichment were sampled using a probability design within park estuaries during a late-summer index period. Monitoring variables consisted of dissolved-oxygen concentration, chlorophyll a concentration, water temperature, salinity, attenuation of downwelling photosynthetically available radiation (PAR), and turbidity. The statistical sampling design allowed the condition of unsampled locations to be inferred from the distribution of data from a set of randomly positioned \"probability\" stations. A subset of sampling stations was sampled repeatedly during the index period, and stations were not rerandomized in subsequent years. These \"trend stations\" allowed us to examine temporal variability within the index period, and to improve the sensitivity of the monitoring protocol to detecting change through time. Additionally, one index site in each park was equipped for continuous monitoring throughout the index period. Thus, the protocol includes elements of probabilistic and targeted spatial sampling, and the temporal intensity ranges from snapshot assessments to continuous monitoring.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Natural Resource Technical Report","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"National Park Service","usgsCitation":"Kopp, B.S., Nielsen, M., Glisic, D., and Neckles, H.A., 2009, Estuarine water quality in parks of the Northeast Coastal and Barrier Network: Development and early implementation of vital signs estuarine nutrient-enrichment monitoring, 2003-06: Natural Resource Technical Report, v. 266.","numberOfPages":"135","temporalStart":"2003-01-01","temporalEnd":"2006-12-31","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":256980,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":21686,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.nps.gov/nero/science/FINAL/NCBN_water_quality.html","linkFileType":{"id":5,"text":"html"}}],"country":"United States","volume":"266","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0bc5e4b0c8380cd52881","contributors":{"authors":[{"text":"Kopp, Blaine S.","contributorId":99648,"corporation":false,"usgs":true,"family":"Kopp","given":"Blaine","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":347223,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nielsen, Martha","contributorId":19415,"corporation":false,"usgs":true,"family":"Nielsen","given":"Martha","affiliations":[],"preferred":false,"id":347221,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Glisic, Dejan","contributorId":93742,"corporation":false,"usgs":true,"family":"Glisic","given":"Dejan","email":"","affiliations":[],"preferred":false,"id":347222,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Neckles, Hilary A. 0000-0002-5662-2314 hneckles@usgs.gov","orcid":"https://orcid.org/0000-0002-5662-2314","contributorId":3821,"corporation":false,"usgs":true,"family":"Neckles","given":"Hilary","email":"hneckles@usgs.gov","middleInitial":"A.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":347220,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70037902,"text":"fs20093101 - 2009 - A brief geologic history of Volusia County, Florida","interactions":[],"lastModifiedDate":"2012-04-30T16:43:35","indexId":"fs20093101","displayToPublicDate":"2012-03-28T09:27:00","publicationYear":"2009","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2009-3101","title":"A brief geologic history of Volusia County, Florida","docAbstract":"Volusia County is in a unique and beautiful setting. This Florida landscape is characterized by low coastal plains bordered by upland areas of sandy ridges and many lakes. Beautiful streams and springs abound within the vicinity. Underneath the land surface is a deep layer of limestone rocks that stores fresh, clean water used to serve drinking and other needs. However, the landscape and the subsurface rocks have not always been as they appear today. These features are the result of environmental forces and processes that began millions of years ago and are still ongoing. This fact sheet provides a brief geologic history of the Earth, Florida, and Volusia County, with an emphasis on explaining why the Volusia County landscape and geologic structure exists as it does today.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20093101","collaboration":"Prepared in cooperation with Volusia County","usgsCitation":"German, E.R., 2009, A brief geologic history of Volusia County, Florida: U.S. Geological Survey Fact Sheet 2009-3101, 6 p., https://doi.org/10.3133/fs20093101.","productDescription":"6 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":246857,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2009_3101.jpg"},{"id":246853,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2009/3101/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Florida","county":"Volusia","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -81.61666666666666,28.5 ], [ -81.61666666666666,29.5 ], [ -80.66666666666667,29.5 ], [ -80.66666666666667,28.5 ], [ -81.61666666666666,28.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd497ae4b0b290850ef36b","contributors":{"authors":[{"text":"German, Edward R.","contributorId":85567,"corporation":false,"usgs":true,"family":"German","given":"Edward","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":462999,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70044320,"text":"70044320 - 2009 - Evaluation of methods and uncertainties in the water budget","interactions":[],"lastModifiedDate":"2022-12-27T16:32:13.105119","indexId":"70044320","displayToPublicDate":"2012-03-01T14:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"chapter":"4","title":"Evaluation of methods and uncertainties in the water budget","docAbstract":"<p><span>Water budget studies of Mirror Lake aim to measure hydrologic components interacting with the lake as accurately as possible. However, measurements of water budget components are subject to some degree of uncertainty. This chapter describes the methods used to quantify water budget components of Mirror Lake in detail. It examines uncertainties in precipitation values, monthly evaporation, water flows, and exchange with groundwater. It shows how those values were derived, including the assumptions that went into the calculations and the uncertainties inherent in the values.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Mirror Lake: Interactions among air, land, and water","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"University of California Press","doi":"10.1525/california/9780520261198.003.0004","usgsCitation":"Winter, T.C., and Rosenberry, D.O., 2009, Evaluation of methods and uncertainties in the water budget, chap. 4 <i>of</i> Mirror Lake: Interactions among air, land, and water, p. 205-224, https://doi.org/10.1525/california/9780520261198.003.0004.","productDescription":"20 p.","startPage":"205","endPage":"224","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-007758","costCenters":[],"links":[{"id":319927,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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C.","contributorId":84736,"corporation":false,"usgs":true,"family":"Winter","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":626287,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Likens, Gene E.","contributorId":56363,"corporation":false,"usgs":true,"family":"Likens","given":"Gene","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":626288,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Winter, Thomas C.","contributorId":84736,"corporation":false,"usgs":true,"family":"Winter","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":626285,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosenberry, Donald O. 0000-0003-0681-5641 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,{"id":70170158,"text":"70170158 - 2009 - Hydrologic processes and the water budget: Chapter 2","interactions":[],"lastModifiedDate":"2016-04-08T15:50:36","indexId":"70170158","displayToPublicDate":"2012-03-01T12:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"title":"Hydrologic processes and the water budget: Chapter 2","docAbstract":"<p><span>This chapter focuses on the hydrological setting of Mirror Lake and its water budget. It first describes the glacial deposits and bedrock topography in the Mirror Lake area. It then provides an overview of the hydrologic processes associated with Mirror Lake and examines the field and analytical methods used to determine its water budget. It presents results from the hydrologic studies, which are based on monthly and annual water budgets for the calendar years 1981 through 2000.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Mirror Lake: Interactions among air, land, and water","language":"English","publisher":"University of California Press","doi":"10.1525/california/9780520261198.003.0002","usgsCitation":"Rosenberry, D.O., and Winter, T.C., 2009, Hydrologic processes and the water budget: Chapter 2, chap. <i>of</i> Mirror Lake: Interactions among air, land, and water, p. 23-68, https://doi.org/10.1525/california/9780520261198.003.0002.","productDescription":"46 p.","startPage":"23","endPage":"68","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319931,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Hampshire","otherGeospatial":"Mirror Lake","geographicExtents":"{\n  \"type\": 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E.","contributorId":56363,"corporation":false,"usgs":true,"family":"Likens","given":"Gene","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":626297,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Rosenberry, Donald O. 0000-0003-0681-5641 rosenber@usgs.gov","orcid":"https://orcid.org/0000-0003-0681-5641","contributorId":1312,"corporation":false,"usgs":true,"family":"Rosenberry","given":"Donald","email":"rosenber@usgs.gov","middleInitial":"O.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":626294,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Winter, Thomas C.","contributorId":84736,"corporation":false,"usgs":true,"family":"Winter","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":626295,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70157395,"text":"70157395 - 2009 - Dynamics in phosphorus retention in wetlands upstream of Delavan Lake, Wisconsin","interactions":[],"lastModifiedDate":"2018-02-06T12:35:36","indexId":"70157395","displayToPublicDate":"2012-02-01T06:15:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2592,"text":"Lake and Reservoir Management","active":true,"publicationSubtype":{"id":10}},"title":"Dynamics in phosphorus retention in wetlands upstream of Delavan Lake, Wisconsin","docAbstract":"<p>A <span class=\"single_highlight_class\">phosphorus</span> budget was constructed for Delavan Lake Inlet, a perennial riverine <span class=\"single_highlight_class\">wetland</span> with submersed and floating aquatic vegetation in southeastern Wisconsin, to better understand the <span class=\"single_highlight_class\">phosphorus</span> <span class=\"single_highlight_class\">dynamics</span> in natural <span class=\"single_highlight_class\">wetlands</span> and the role of <span class=\"single_highlight_class\">wetlands</span> in lake-rehabilitation efforts. During the growing season, the inlet served as a net source of <span class=\"single_highlight_class\">phosphorus</span>, primarily due to the release of <span class=\"single_highlight_class\">phosphorus</span> from the sediments. More <span class=\"single_highlight_class\">phosphorus</span> was released from the sediments of the inlet (600 kg) than was input from the upstream watershed (460 kg). This release was caused by high pH associated with high photosynthetic activity. During the remainder of the year, the inlet served as a net sink for <span class=\"single_highlight_class\">phosphorus</span>, <span class=\"single_highlight_class\">retaining</span> 6% of die <span class=\"single_highlight_class\">phosphorus</span> input from the watershed. Over the entire year, this <span class=\"single_highlight_class\">wetland</span> was a net source of over 500 kg of <span class=\"single_highlight_class\">phosphorus</span> to downstream Delavan Lake. A constructed riverine <span class=\"single_highlight_class\">wetland</span> upstream of Delavan Lake Inlet demonstrated a similar periodic release of <span class=\"single_highlight_class\">phosphorus</span>. However, in this case, the summer release of <span class=\"single_highlight_class\">phosphorus</span> was less than that trapped during the remainder of the year. The constructed <span class=\"single_highlight_class\">wetland</span> served as a net sink for approximately 20% of the input <span class=\"single_highlight_class\">phosphorus</span> on an annual time scale. The role of existing and constructed <span class=\"single_highlight_class\">wetlands</span> as <span class=\"single_highlight_class\">phosphorus</span> traps is complex. <span class=\"single_highlight_class\">Wetlands</span> can act as a source or a sink for <span class=\"single_highlight_class\">phosphorus</span> depending on the ambient conditions in die <span class=\"single_highlight_class\">wetland</span>. Howa <span class=\"single_highlight_class\">wetland</span> fits into a rehabilitation plan depends upon its net <span class=\"single_highlight_class\">retention</span> efficiency and the importance of the periodic releases of <span class=\"single_highlight_class\">phosphorus</span> to downstream waters.</p>","language":"English","publisher":"The North American Lake Management Society","doi":"10.1080/07438149809354353","usgsCitation":"Robertson, D.M., Elder, J.F., Goddard, G.L., and James, W., 2009, Dynamics in phosphorus retention in wetlands upstream of Delavan Lake, Wisconsin: Lake and Reservoir Management, v. 14, no. 4, p. 466-477, https://doi.org/10.1080/07438149809354353.","productDescription":"12 p.","startPage":"466","endPage":"477","numberOfPages":"12","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":475978,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/07438149809354353","text":"Publisher Index Page"},{"id":308380,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","otherGeospatial":"Delevan Lake, Elkhorn, Jackson Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.69880676269531,\n              42.59454359788448\n            ],\n            [\n              -88.64593505859375,\n              42.55839115400449\n            ],\n            [\n              -88.61331939697266,\n              42.54195129663955\n            ],\n            [\n              -88.55512619018555,\n              42.5739418016264\n            ],\n            [\n              -88.5171890258789,\n              42.60023001112722\n            ],\n            [\n              -88.47513198852539,\n              42.61943361476022\n            ],\n            [\n              -88.4651756286621,\n              42.62423359056032\n            ],\n            [\n              -88.44732284545898,\n              42.633200974757294\n            ],\n            [\n              -88.4425163269043,\n              42.64002037386321\n            ],\n            [\n              -88.45865249633789,\n              42.679406713370305\n            ],\n            [\n              -88.49349975585938,\n              42.69543182848484\n            ],\n            [\n              -88.52182388305664,\n              42.69517949650704\n            ],\n            [\n              -88.56542587280273,\n              42.66640693046163\n            ],\n            [\n              -88.5856819152832,\n              42.66628070564928\n            ],\n            [\n              -88.60198974609375,\n              42.65883298807084\n            ],\n            [\n              -88.62653732299805,\n              42.63307468254104\n            ],\n            [\n              -88.65108489990234,\n              42.61059058539327\n            ],\n            [\n              -88.68558883666992,\n              42.606042252773435\n            ],\n            [\n              -88.69880676269531,\n              42.59454359788448\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"14","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56027bbce4b03bc34f544826","contributors":{"authors":[{"text":"Robertson, Dale M. 0000-0001-6799-0596 dzrobert@usgs.gov","orcid":"https://orcid.org/0000-0001-6799-0596","contributorId":150760,"corporation":false,"usgs":true,"family":"Robertson","given":"Dale","email":"dzrobert@usgs.gov","middleInitial":"M.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":572959,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elder, John F.","contributorId":23919,"corporation":false,"usgs":true,"family":"Elder","given":"John","email":"","middleInitial":"F.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":572960,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goddard, Gerald L.","contributorId":35721,"corporation":false,"usgs":true,"family":"Goddard","given":"Gerald","email":"","middleInitial":"L.","affiliations":[{"id":676,"text":"Wisconsin Water Resource Division","active":false,"usgs":true}],"preferred":false,"id":572961,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"James, William F.","contributorId":75472,"corporation":false,"usgs":true,"family":"James","given":"William F.","affiliations":[],"preferred":false,"id":572962,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70006008,"text":"70006008 - 2009 - The occurrence of antibiotics in an urban watershed: From wastewater to drinking water","interactions":[],"lastModifiedDate":"2018-10-03T11:11:10","indexId":"70006008","displayToPublicDate":"2012-01-08T10:25:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3352,"text":"Science of the Total Environment","active":true,"publicationSubtype":{"id":10}},"title":"The occurrence of antibiotics in an urban watershed: From wastewater to drinking water","docAbstract":"The presence of 28 antibiotics in three hospital effluents, five wastewater treatment plants (WWTPs), six rivers and a drinking water storage catchment were investigated within watersheds of South&ndash;East Queensland, Australia. All antibiotics were detected at least once, with the exception of the polypeptide bacitracin which was not detected at all. Antibiotics were found in hospital effluent ranging from 0.01&ndash;14.5 &mu;g L<sup>-1</sup>, dominated by the &beta;-lactam, quinolone and sulphonamide groups. Antibiotics were found in WWTP influent up to 64 &mu;g L<sup>-1</sup>, dominated by the &beta;-lactam, quinolone and sulphonamide groups. Investigated WWTPs were highly effective in removing antibiotics from the water phase, with an average removal rate of greater than 80% for all targeted antibiotics. However, antibiotics were still detected in WWTP effluents in the low ng L<sup>-1</sup> range up to a maximum of 3.4 &mu;g L<sup>-1</sup>, with the macrolide, quinolone and sulphonamide antibiotics most prevalent. Similarly, antibiotics were detected quite frequently in the low ng L<sup>-1</sup> range, up to 2 &mu;g L<sup>-1</sup> in the surface waters of six investigated rivers including freshwater, estuarine and marine samples. The total investigated antibiotic concentration (TIAC) within the Nerang River was significantly lower (<i>p</i> < 0.05) than all other rivers sampled. The absence of WWTP discharge to this river is a likely explanation for the significantly lower TIAC and suggests that WWTP discharges are a dominant source of antibiotics to investigated surface waters. A significant difference (<i>p</i> < 0.001) was identified between TIACs at surface water sites with WWTP discharge compared to sites with no WWTP discharge, providing further evidence that WWTPs are an important source of antibiotics to streams. Despite the presence of antibiotics in surface waters used for drinking water extraction, no targeted antibiotics were detected in any drinking water samples.","language":"English","publisher":"Elsevier","doi":"10.1016/j.scitotenv.2008.11.059","usgsCitation":"Watkinson, A., Murby, E., Kolpin, D.W., and Costanzo, S., 2009, The occurrence of antibiotics in an urban watershed: From wastewater to drinking water: Science of the Total Environment, v. 407, no. 8, p. 2711-2723, https://doi.org/10.1016/j.scitotenv.2008.11.059.","productDescription":"13 p.","startPage":"2711","endPage":"2723","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":475982,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.scitotenv.2008.11.059","text":"Publisher Index Page"},{"id":204554,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Australia","state":"Queensland","volume":"407","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bae3ce4b08c986b323f6a","contributors":{"authors":[{"text":"Watkinson, A.J.","contributorId":20887,"corporation":false,"usgs":true,"family":"Watkinson","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":353641,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Murby, E.J.","contributorId":39112,"corporation":false,"usgs":true,"family":"Murby","given":"E.J.","email":"","affiliations":[],"preferred":false,"id":353642,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kolpin, Dana W. 0000-0002-3529-6505 dwkolpin@usgs.gov","orcid":"https://orcid.org/0000-0002-3529-6505","contributorId":1239,"corporation":false,"usgs":true,"family":"Kolpin","given":"Dana","email":"dwkolpin@usgs.gov","middleInitial":"W.","affiliations":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"preferred":true,"id":353643,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Costanzo, S.D.","contributorId":8608,"corporation":false,"usgs":true,"family":"Costanzo","given":"S.D.","email":"","affiliations":[],"preferred":false,"id":353640,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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