{"pageNumber":"1296","pageRowStart":"32375","pageSize":"25","recordCount":46734,"records":[{"id":3618,"text":"cir1136 - 1996 - Nutrients in the Nation's Waters--Too Much of a Good Thing?","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"cir1136","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1136","title":"Nutrients in the Nation's Waters--Too Much of a Good Thing?","docAbstract":"Historical data on nutrients (nitrogen and phosphorus) from about 12,000 ground-water and more than 22,000 stream samples have been compiled and related to possible sources. This existing information was collected by many agencies for a variety of purposes. Therefore, though it can be used to determine where concentrations differ, the exact percentages should not be taken as those for the Nation as a whole. Major findings include: (1) nutrient concentrations in water generally are related to land use in the area overlying ground-water aquifers or upstream from surface-water locations, (2) regional differences are related to differences in soil-drainage properties and agricultural practices, (3) nitrate concentrations in about 12 percent of domestic-supply wells in agricultural areas exceeded the U.S. Environmental Protection Agency's drinking-water standard (10 mg/L), and (4) nitrate concentrations in surface water rarely exceed the drinking-water standard. This information has helped identify locations across the Nation where ground water and streams are most likely to be vulnerable to nutrient contamination. Programs to manage and protect water resources can therefore be targeted to the most critical areas, providing the greatest protection for the least cost.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/cir1136","usgsCitation":"Mueller, D.K., and Helsel, D., 1996, Nutrients in the Nation's Waters--Too Much of a Good Thing?: U.S. Geological Survey Circular 1136, 24 p., https://doi.org/10.3133/cir1136.","productDescription":"24 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":123714,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1996/1136/report-thumb.jpg"},{"id":11745,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/circ/circ1136/","linkFileType":{"id":5,"text":"html"}},{"id":30655,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1996/1136/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696743","contributors":{"authors":[{"text":"Mueller, David K. mueller@usgs.gov","contributorId":1585,"corporation":false,"usgs":true,"family":"Mueller","given":"David","email":"mueller@usgs.gov","middleInitial":"K.","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true}],"preferred":true,"id":147265,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Helsel, Dennis R.","contributorId":85569,"corporation":false,"usgs":true,"family":"Helsel","given":"Dennis R.","affiliations":[],"preferred":false,"id":147266,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4942,"text":"fs09996 - 1996 - Relation of land use to nitrate in the surficial aquifer along the Straight River, north-central Minnesota, 1992-93","interactions":[],"lastModifiedDate":"2018-03-19T11:22:45","indexId":"fs09996","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1996","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":"099-96","title":"Relation of land use to nitrate in the surficial aquifer along the Straight River, north-central Minnesota, 1992-93","docAbstract":"<p>The U.S. Geological Survey studied the relation of land use to nitrate concentrations in the surficial aquifer along the Straight River near Park Rapids in north-central Minnesota (see adjacent map) during 1992 to 1993. Concern about health hazards to humans and livestock from use of ground water contaminated by nitrate prompted the study.</p>\n<p>Data collected for this study included: (1) water levels from 38 monitoring wells; (2) nitrate-nitrogen concentrations in ground-water samples from 34 monitoring wells; and (3) land use determined for 2.5-acre parcels throughout the study area. Eighteen of the monitoring wells were installed as nested pairs; the other 20 wells were installed singly. The wells were screened near the water table except the deep wells of each nested pair, which were screened near the bottom of the aquifer.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View, MN","doi":"10.3133/fs09996","usgsCitation":"Ruhl, J.F., 1996, Relation of land use to nitrate in the surficial aquifer along the Straight River, north-central Minnesota, 1992-93: U.S. Geological Survey Fact Sheet 099-96, 2 p., https://doi.org/10.3133/fs09996.","productDescription":"2 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":31804,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1996/0099/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":125236,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1996/0099/report-thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"Straight River","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db634c44","contributors":{"authors":[{"text":"Ruhl, J. F.","contributorId":81866,"corporation":false,"usgs":true,"family":"Ruhl","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":150179,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70202463,"text":"70202463 - 1996 - Techniques for visualizing urban growth using a temporal GIS database","interactions":[],"lastModifiedDate":"2019-05-28T15:08:40","indexId":"70202463","displayToPublicDate":"1996-05-01T12:11:08","publicationYear":"1996","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Techniques for visualizing urban growth using a temporal GIS database","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"ASPRS/ACSM Annual Convention and Exhibition, Baltimore, Md., 22–25 April 1996, Proceedings","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"ASPRS/ACSM Annual Convention and Exhibition","conferenceDate":"April 22-25, 1996","conferenceLocation":"Baltimore, Maryland","language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","publisherLocation":"Bethesda, Maryland","usgsCitation":"Masuoka, P., Acevedo, W., Fifer, S., Foresman, T.W., and Tuttle, M., 1996, Techniques for visualizing urban growth using a temporal GIS database, <i>in</i> ASPRS/ACSM Annual Convention and Exhibition, Baltimore, Md., 22–25 April 1996, Proceedings, Baltimore, Maryland, April 22-25, 1996, p. 89-100.","productDescription":"12 p.","startPage":"89","endPage":"100","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":361684,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Masuoka, Penny","contributorId":213913,"corporation":false,"usgs":false,"family":"Masuoka","given":"Penny","email":"","affiliations":[],"preferred":false,"id":758686,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Acevedo, William wacevedo@usgs.gov","contributorId":2689,"corporation":false,"usgs":true,"family":"Acevedo","given":"William","email":"wacevedo@usgs.gov","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true},{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":758687,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fifer, S.","contributorId":213916,"corporation":false,"usgs":false,"family":"Fifer","given":"S.","email":"","affiliations":[],"preferred":false,"id":758688,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Foresman, Timothy W.","contributorId":213897,"corporation":false,"usgs":false,"family":"Foresman","given":"Timothy","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":758689,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Tuttle, M.","contributorId":26397,"corporation":false,"usgs":true,"family":"Tuttle","given":"M.","affiliations":[],"preferred":false,"id":758690,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70202452,"text":"70202452 - 1996 - Development of the temporal transportation database for the analysis of urban development in the Baltimore-Washington region","interactions":[],"lastModifiedDate":"2019-05-28T15:09:30","indexId":"70202452","displayToPublicDate":"1996-05-01T09:42:35","publicationYear":"1996","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Development of the temporal transportation database for the analysis of urban development in the Baltimore-Washington region","docAbstract":"<p><span>The U.S. Geological Survey is participating in a joint effort with the University of Maryland Baltimore County and other government agencies to construct a dynamic database of urban development for the Baltimore-Washington region from the late-1700's to the 1990's. The multi-theme temporal database includes a principal transportation data layer that documents the primary roads, railroads, and other transportation features that provided the infrastructure for urban development. A geographic information system was used to collect from various maps at various scales. Compilation criteria, such as connectivity, mobility, lineage, and alignment, were developed to accommodate limitations in the source materials. Visualization techniques such as animation and flight simulation are used to portray the changing transportation infrastructure and its effect on urbanization. The database will be used to study the evolution of the Baltimore-Washington metropolitan area. The principal transportation data layer is essential to illustrate and analyze the regional and temporal aspects of human-induced land transformations. Modeling applications will explore the urban growth process and its correlation to key transportation development.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"ASPRS/ACSM Annual Convention and Exhibition, Baltimore, Md., 20–26 April 1996, Proceedings","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"ASPRS/ACSM Annual Convention and Exhibition","conferenceDate":"April 20-26, 1996","conferenceLocation":"Baltimore, Maryland","language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","publisherLocation":"Falls Church, Virginia","usgsCitation":"Clark, S.C., Starr, J., Foresman, T.W., Acevedo, W., and Solomon, C., 1996, Development of the temporal transportation database for the analysis of urban development in the Baltimore-Washington region, <i>in</i> ASPRS/ACSM Annual Convention and Exhibition, Baltimore, Md., 20–26 April 1996, Proceedings, Baltimore, Maryland, April 20-26, 1996.","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":361665,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":361664,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://archive.usgs.gov/archive/sites/landcover.usgs.gov/urban/umap/pubs/asprs_sc.php.html"}],"country":"United States","state":"Maryland","otherGeospatial":"Baltimore-Washington Region","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Clark, Susan C.","contributorId":213899,"corporation":false,"usgs":false,"family":"Clark","given":"Susan","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":758643,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Starr, John","contributorId":213900,"corporation":false,"usgs":false,"family":"Starr","given":"John","email":"","affiliations":[],"preferred":false,"id":758644,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Foresman, Timothy W.","contributorId":213897,"corporation":false,"usgs":false,"family":"Foresman","given":"Timothy","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":758645,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Acevedo, William wacevedo@usgs.gov","contributorId":2689,"corporation":false,"usgs":true,"family":"Acevedo","given":"William","email":"wacevedo@usgs.gov","affiliations":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true},{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":758646,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Solomon, Carol","contributorId":213901,"corporation":false,"usgs":true,"family":"Solomon","given":"Carol","email":"","affiliations":[],"preferred":true,"id":758647,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70202451,"text":"70202451 - 1996 - Origins and philosophy of building a temporal database to examine human transformation processes","interactions":[],"lastModifiedDate":"2019-05-28T15:10:11","indexId":"70202451","displayToPublicDate":"1996-05-01T09:27:13","publicationYear":"1996","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Origins and philosophy of building a temporal database to examine human transformation processes","docAbstract":"<p><span>The U.S. Geological Survey (USGS), in partnership with the University of Maryland Baltimore County, is using historical maps and satellite images to map human-induced land transformations for the Baltimore-Washington metropolitan area. This work builds on an earlier effort that documented the historical urban development for the San Francisco Bay area. That effort used a geographic information system to compile a database that provided a visual and historical perspective of the urban growth experienced in the Bay area between 1850 and 1990. Historical overviews of urban development can be used to provide insights into the future. The Bay area work was inspired by the desire to draw upon the USGS's rich 100-year topographic map, and 20-year Landsat satellite data archives. A methodology was developed to combine the information from a variety of sources into an integrated, multi-scale, and multi-resolution dataset. Temporal urban mapping is used to examine past landscapes by incorporating historic maps, census statistics, and commerce records to generate a progressive geo-referenced representation of the past changes in the region. Contemporary analysis focuses on the use of remotely sensed data, existing digital land use data, digital census information, and a variety of Earth science infrastructure data, such as Digital Line Graphs, Digital Elevation Models, and key ancillary demographic information. The resulting database of temporal urban demographic changes provides an ideal source of test data and information for both urban geographers and global change research scientists.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Annual Convention and Exhibition, Baltimore, Md., 22–25 April 1996, Proceedings","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Annual Convention and Exhibition","conferenceDate":"April 22-25, 1996","conferenceLocation":"Baltimore, Maryland","language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","publisherLocation":"Bethesda, Maryland","usgsCitation":"Acevedo, W., Foresman, T.W., and Buchanan, J., 1996, Origins and philosophy of building a temporal database to examine human transformation processes, <i>in</i> Annual Convention and Exhibition, Baltimore, Md., 22–25 April 1996, Proceedings, Baltimore, Maryland, April 22-25, 1996.","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":361662,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://archive.usgs.gov/archive/sites/landcover.usgs.gov/urban/umap/pubs/asprs_wma.php.html"},{"id":361663,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"San Francisco Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.64862060546875,\n              37.391981943533544\n            ],\n            [\n              -121.74362182617188,\n              37.391981943533544\n            ],\n            [\n              -121.74362182617188,\n              38.238180119798635\n            ],\n            [\n              -122.64862060546875,\n              38.238180119798635\n            ],\n            [\n              -122.64862060546875,\n              37.391981943533544\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Acevedo, William wacevedo@usgs.gov","contributorId":2689,"corporation":false,"usgs":true,"family":"Acevedo","given":"William","email":"wacevedo@usgs.gov","affiliations":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true},{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":758640,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foresman, Timothy W.","contributorId":213897,"corporation":false,"usgs":false,"family":"Foresman","given":"Timothy","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":758641,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Buchanan, Janis T.","contributorId":213898,"corporation":false,"usgs":false,"family":"Buchanan","given":"Janis T.","affiliations":[],"preferred":false,"id":758642,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70246980,"text":"70246980 - 1996 - Uncertainty of groundwater vulnerability assessments for agricultural regions in Hawaii: Review","interactions":[],"lastModifiedDate":"2023-07-20T14:23:00.157461","indexId":"70246980","displayToPublicDate":"1996-05-01T09:15:11","publicationYear":"1996","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2262,"text":"Journal of Environmental Quality","active":true,"publicationSubtype":{"id":10}},"title":"Uncertainty of groundwater vulnerability assessments for agricultural regions in Hawaii: Review","docAbstract":"<p><span>There are important challenges associated with assessing potential groundwater vulnerability hazards that may result from regional scale applications of agrochemicals. The increasing availability of Geographic Information System (GIS) software to those involved in assisting with landuse decisions has resulted in the widespread production of multicolored risk management maps for many environmentally sensitive issues. Soil-based GIS's have recently been coupled to various solute-leaching models to make near-surface groundwater vulnerability assessments for guidance in pesticide regulation in several states. In general, these assessments rest on soil, climatic, and chemical data that are extremely sparse and contain considerable uncertainty. It is also important to acknowledge the uncertainty associated with the transport/fate processes that are not accounted for by the modeling approach used to make the assessment. In this paper, we review the results from a series of papers that have focused on characterization of uncertainty in pesticide mobility estimates, using the attenuation and retardation indices (AF and RF), for the Pearl Harbor Basin on the Hawaiian island of Oahu. Relative to data error uncertainties, we discuss the impacts of: (i) soil, climatic, and chemical data base uncertainties, (ii) reductions in data base uncertainties, (iii) extrapolation of soil data base information based on soil taxonomy and soil survey, and (iv) importing information from outside the region of interest. Relative to model error uncertainties, we compare pesticide leaching estimates from the simple AF and RF mobility indices with simulations from the EPA's Pesticide Root Zone Model (PRZM) and field observations. Finally, we outline a Regional Integrated Risk Assessment approach for characterizing regional scale groundwater vulnerability for near-surface nonpoint sources.</span></p>","language":"English","publisher":"American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America","doi":"10.2134/jeq1996.00472425002500030013x","usgsCitation":"Loague, K., Bernknopf, R., Green, R.E., and Giambelluca, T., 1996, Uncertainty of groundwater vulnerability assessments for agricultural regions in Hawaii: Review: Journal of Environmental Quality, v. 25, p. 475-490, https://doi.org/10.2134/jeq1996.00472425002500030013x.","productDescription":"16 p.","startPage":"475","endPage":"490","costCenters":[],"links":[{"id":419185,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Oahu","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -158.17001943695823,\n              21.455619564327932\n            ],\n            [\n              -158.17001943695823,\n              21.299771904317055\n            ],\n            [\n              -157.87349649295143,\n              21.299771904317055\n            ],\n            [\n              -157.87349649295143,\n              21.455619564327932\n            ],\n            [\n              -158.17001943695823,\n              21.455619564327932\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"25","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Loague, Keith","contributorId":178119,"corporation":false,"usgs":false,"family":"Loague","given":"Keith","email":"","affiliations":[],"preferred":false,"id":878461,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bernknopf, R. L.","contributorId":46082,"corporation":false,"usgs":true,"family":"Bernknopf","given":"R. L.","affiliations":[],"preferred":false,"id":878462,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Green, R. E.","contributorId":316828,"corporation":false,"usgs":false,"family":"Green","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":878463,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Giambelluca, T. W.","contributorId":90115,"corporation":false,"usgs":false,"family":"Giambelluca","given":"T. W.","affiliations":[],"preferred":false,"id":878464,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70185706,"text":"70185706 - 1996 - Identification of hydraulic conductivity structure in sand and gravel aquifers: Cape Cod data set ","interactions":[],"lastModifiedDate":"2018-03-29T10:25:38","indexId":"70185706","displayToPublicDate":"1996-05-01T00:00:00","publicationYear":"1996","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":"Identification of hydraulic conductivity structure in sand and gravel aquifers: Cape Cod data set ","docAbstract":"<p>This study evaluates commonly used geostatistical methods to assess reproduction of hydraulic conductivity (K) structure and sensitivity under limiting amounts of data. Extensive conductivity measurements from the Cape Cod sand and gravel aquifer are used to evaluate two geostatistical estimation methods, conditional mean as an estimate and ordinary kriging, and two stochastic simulation methods, simulated annealing and sequential Gaussian simulation. Our results indicate that for relatively homogeneous sand and gravel aquifers such as the Cape Cod aquifer, neither estimation methods nor stochastic simulation methods give highly accurate point predictions of hydraulic conductivity despite the high density of collected data. Although the stochastic simulation methods yielded higher errors than the estimation methods, the stochastic simulation methods yielded better reproduction of the measured In (K) distribution and better reproduction of local contrasts in In (K). The inability of kriging to reproduce high In (K) values, as reaffirmed by this study, provides a strong instigation for choosing stochastic simulation methods to generate conductivity fields when performing fine-scale contaminant transport modeling. Results also indicate that estimation error is relatively insensitive to the number of hydraulic conductivity measurements so long as more than a threshold number of data are used to condition the realizations. This threshold occurs for the Cape Cod site when there are approximately three conductivity measurements per integral volume. The lack of improvement with additional data suggests that although fine-scale hydraulic conductivity structure is evident in the variogram, it is not accurately reproduced by geostatistical estimation methods. If the Cape Cod aquifer spatial conductivity characteristics are indicative of other sand and gravel deposits, then the results on predictive error versus data collection obtained here have significant practical consequences for site characterization. Heavily sampled sand and gravel aquifers, such as Cape Cod and Borden, may have large amounts of redundant data, while in more common real world settings, our results suggest that denser data collection will likely improve understanding of permeability structure.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/96WR00272","usgsCitation":"Eggleston, J., Rojstaczer, S., and Peirce, J., 1996, Identification of hydraulic conductivity structure in sand and gravel aquifers: Cape Cod data set : Water Resources Research, v. 32, no. 5, p. 1209-1222, https://doi.org/10.1029/96WR00272.","productDescription":"14 p. ","startPage":"1209","endPage":"1222","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338436,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58db7632e4b0ee37af29e4b2","contributors":{"authors":[{"text":"Eggleston, J.R.","contributorId":58296,"corporation":false,"usgs":true,"family":"Eggleston","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":686477,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rojstaczer, S.A.","contributorId":54620,"corporation":false,"usgs":true,"family":"Rojstaczer","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":686478,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peirce, J.J.","contributorId":189921,"corporation":false,"usgs":false,"family":"Peirce","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":686479,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70018579,"text":"70018579 - 1996 - Chemical evaluation of soil-solution in acid forest soils","interactions":[],"lastModifiedDate":"2025-08-15T16:31:20.052455","indexId":"70018579","displayToPublicDate":"1996-05-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3419,"text":"Soil Science","active":true,"publicationSubtype":{"id":10}},"title":"Chemical evaluation of soil-solution in acid forest soils","docAbstract":"Soil-solution chemistry is commonly studied in forests through the use of soil lysimeters.This approach is impractical for regional survey studies, however, because lysimeter installation and operation is expensive and time consuming. To address these problems, a new technique was developed to compare soil-solution chemistry among red spruce stands in New York, Vermont, New Hampshire, Maine. Soil solutions were expelled by positive air pressure from soil that had been placed in a sealed cylinder. Before the air pressure was applied, a solution chemically similar to throughfall was added to the soil to bring it to approximate field capacity. After the solution sample was expelled, the soil was removed from the cylinder and chemically analyzed. The method was tested with homogenized Oa and Bs horizon soils collected from a red spruce stand in the Adirondack Mountains of New York, a red spruce stand in east-central Vermont, and a mixed hardwood stand in the Catskill Mountains of New York. Reproducibility, effects of varying the reaction time between adding throughfall and expelling soil solution (5-65 minutes) and effects of varying the chemical composition of added throughfall, were evaluated. In general, results showed that (i) the method was reproducible (coefficients of variation were generally < 15%), (ii) variations in the length of reaction-time did not affect expelled solution concentrations, and (iii) adding and expelling solution did not cause detectable changes in soil exchange chemistry. Concentrations of expelled solutions varied with the concentrations of added throughfall; the lower the CEC, the more sensitive expelled solution concentrations were to the chemical concentrations of added throughfall. Addition of a tracer (NaBr) showed that the expelled solution was a mixture of added solution and solution that preexisted in the soil. Comparisons of expelled solution concentrations with concentrations of soil solutions collected by zero-tension and tension lysimetry indicated that expelled solution concentrations were higher than those obtained with either type of lysimeter, although there was less difference with tension lysimeters than zero-tension lysimeters. The method used for collection of soil solution should be taken into consideration whenever soil solution data are being interpreted.","language":"English","publisher":"Wolters Kluwer","doi":"10.1097/00010694-199605000-00005","issn":"0038075X","usgsCitation":"Lawrence, G., and David, M.B., 1996, Chemical evaluation of soil-solution in acid forest soils: Soil Science, v. 161, no. 5, p. 298-313, https://doi.org/10.1097/00010694-199605000-00005.","productDescription":"16 p.","startPage":"298","endPage":"313","costCenters":[],"links":[{"id":227080,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York, Vermont","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -75.07854938310682,\n              45.0375693793855\n            ],\n            [\n              -76.84879221247608,\n              43.645207343131446\n            ],\n            [\n              -78.71545121677863,\n              43.65390388320041\n            ],\n            [\n              -79.15472998074212,\n              43.46427693178023\n            ],\n            [\n              -79.80390956890837,\n              42.01496762411051\n            ],\n            [\n              -76.10118224340155,\n              42.06809908544358\n            ],\n            [\n              -75.37117922518975,\n              42.00656159213099\n            ],\n            [\n              -74.92059668437619,\n              41.41942050156172\n            ],\n            [\n              -73.63653860327466,\n              40.94701324452626\n            ],\n            [\n              -73.24938035081587,\n              42.72783107480066\n            ],\n            [\n              -72.44760520406116,\n              42.713014923774494\n            ],\n            [\n              -72.23101112234596,\n              43.7957620531397\n            ],\n            [\n              -71.44624914128815,\n              45.00137034379799\n            ],\n            [\n              -75.07854938310682,\n              45.0375693793855\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"161","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f57be4b0c8380cd4c24d","contributors":{"authors":[{"text":"Lawrence, G.B. 0000-0002-8035-2350","orcid":"https://orcid.org/0000-0002-8035-2350","contributorId":76347,"corporation":false,"usgs":true,"family":"Lawrence","given":"G.B.","affiliations":[],"preferred":false,"id":380104,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"David, Mark B.","contributorId":43255,"corporation":false,"usgs":false,"family":"David","given":"Mark","email":"","middleInitial":"B.","affiliations":[{"id":35161,"text":"University of Illinois, Urbana-Champaign","active":true,"usgs":false}],"preferred":false,"id":380103,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24414,"text":"ofr964 - 1996 - Active-, inactive-, and abandoned-mine information and selected geochemical data for the State of California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:14","indexId":"ofr964","displayToPublicDate":"1996-05-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"96-4","title":"Active-, inactive-, and abandoned-mine information and selected geochemical data for the State of California","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr964","issn":"0094-9140","usgsCitation":"Ryder, J.L., 1996, Active-, inactive-, and abandoned-mine information and selected geochemical data for the State of California (Diskette version.): U.S. Geological Survey Open-File Report 96-4, 2 computer disks ;3 1/2 in., https://doi.org/10.3133/ofr964.","productDescription":"2 computer disks ;3 1/2 in.","costCenters":[],"links":[{"id":157091,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1758,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1996/ofr-96-0004/","linkFileType":{"id":5,"text":"html"}}],"edition":"Diskette version.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a3496","contributors":{"authors":[{"text":"Ryder, Jean L.","contributorId":80709,"corporation":false,"usgs":true,"family":"Ryder","given":"Jean","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":191882,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4896,"text":"ds19 - 1996 - Geology and resource assessment of Costa Rica at 1:500,000 scale; a digital representation of maps of the U.S. Geological Survey's 1987 Folio I-1865","interactions":[],"lastModifiedDate":"2012-02-02T00:05:48","indexId":"ds19","displayToPublicDate":"1996-05-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"19","title":"Geology and resource assessment of Costa Rica at 1:500,000 scale; a digital representation of maps of the U.S. Geological Survey's 1987 Folio I-1865","docAbstract":"This CD-ROM contains digital versions of the geology and resource assessment maps of Costa Rica originally published by the U.S. Geological Survey (USGS), the Direccion General de Geologia, Minas e Hidrocarburos, and the Universidad de Costa Rica in 1987 at a scale of 1:500,000 in USGS Folio I-1865. The following layers of the map are available on the CD-ROM: geology, favorable domains for selected deposit types, Bouguer gravity, isostatic gravity, mineral deposits, and rock geochemistry sample points. Some of the layers are provided in the following formats: ArcView 1 for Windows and UNIX, ARC/INFO 6.1.2 Export, Digital Line Graph (DLG) Optional, and Drawing Exchange File (DXF). This CD-ROM was produced in accordance with the ISO 9660 and Apple Computer's HFS standards.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ds19","issn":"1088-1018","isbn":"060762177X","usgsCitation":"Schruben, P.G., 1996, Geology and resource assessment of Costa Rica at 1:500,000 scale; a digital representation of maps of the U.S. Geological Survey's 1987 Folio I-1865 (Release 1): U.S. Geological Survey Data Series 19, 1 computer laser optical disc :col. ;4 3/4 in., https://doi.org/10.3133/ds19.","productDescription":"1 computer laser optical disc :col. ;4 3/4 in.","costCenters":[],"links":[{"id":139863,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Release 1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ce4b07f02db69efb9","contributors":{"authors":[{"text":"Schruben, Paul G.","contributorId":38974,"corporation":false,"usgs":true,"family":"Schruben","given":"Paul","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":150063,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4851,"text":"ds35 - 1996 - Digital map data, text, and graphical images in support of the 1995 National assessment of United States oil and gas resources","interactions":[],"lastModifiedDate":"2024-05-24T14:03:01.592519","indexId":"ds35","displayToPublicDate":"1996-05-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"35","title":"Digital map data, text, and graphical images in support of the 1995 National assessment of United States oil and gas resources","docAbstract":"This CD-ROM contains files in support of the 1995 USGS National assessment of United States oil and gas resources (DDS-30), which was published separately and summarizes the results of a 3-year study of the oil and gas resources of the onshore and state waters of the United States. The study describes about 560 oil and gas plays in the United States--confirmed and hypothetical, conventional and unconventional. A parallel study of the Federal offshore is being conducted by the U.S. Minerals Management Service. This CD-ROM contains files in multiple formats, so that almost any computer user can import them into word processors and mapping software packages. No proprietary data are released on this CD-ROM. The complete text of DDS-30 is also available, as well as many figures. A companion CD-ROM (DDS-36) includes the tabular data, the programs, and the same text data, but none of the map data.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds35","usgsCitation":"Beeman, W.R., Obuch, R.C., and Brewton, J.D., 1996, Digital map data, text, and graphical images in support of the 1995 National assessment of United States oil and gas resources: U.S. Geological Survey Data Series 35, HTML Document: 1 CD-ROM, https://doi.org/10.3133/ds35.","productDescription":"HTML Document: 1 CD-ROM","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":429254,"rank":3,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P13YZJZG","text":"1995 National Oil and Gas Assessment Data Collection Archive"},{"id":570,"rank":2,"type":{"id":15,"text":"Index 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R.","contributorId":69539,"corporation":false,"usgs":true,"family":"Beeman","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":149936,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Obuch, Raymond C. 0000-0003-4032-7086 obuch@usgs.gov","orcid":"https://orcid.org/0000-0003-4032-7086","contributorId":3092,"corporation":false,"usgs":true,"family":"Obuch","given":"Raymond","email":"obuch@usgs.gov","middleInitial":"C.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":149934,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brewton, James D.","contributorId":9244,"corporation":false,"usgs":true,"family":"Brewton","given":"James","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":149935,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1003092,"text":"1003092 - 1996 - Effects of implanted transmitters on adult bluegills at two temperatures","interactions":[],"lastModifiedDate":"2026-03-25T16:16:08.548689","indexId":"1003092","displayToPublicDate":"1996-05-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Effects of implanted transmitters on adult bluegills at two temperatures","docAbstract":"<p><span id=\"_mce_caret\" data-mce-bogus=\"1\" data-mce-type=\"format-caret\"><span>Laterally compressed panfishes are small and have limited intraperitoneal space; thus, they may suffer adversely from surgically implanted transmitters even if the transmitter meets the generally recommended ratio of transmitter weight to fish weight of 2%. We studied the effects of intraperitoneal transmitters (2.81 g) on survival, growth, healing, and health of bluegills&nbsp;</span><i>Lepomis macrochirus</i><span>&nbsp;(mean weight 133 g) held for 8 weeks at 6°C and 20°C. Radio‐tagged bluegills at 20°C had a mortality rate of 10% and tag loss rate of 15%. At 6°C, bluegills had no mortality or tag loss. Radio‐tagged and reference fish fed in both 20°C raceways; however, a few reference fish appeared dominant at feeding time. This dominance by a few reference fish was also indicated by a large weight gain for three reference fish in each 20°C raceway. At 6°C, neither reference fish nor radio‐tagged fish fed activity. Radio‐tagged fish held at 20°C exhibited pelvic fin erosion, erythema and necrosis at the antenna exit and at suture insertions, and lost or loose sutures, effects not observed in other test fishes. Examination of fish held at 20°C also showed enclosure of the transmitters in a fibrous capsule and adhesion of visceral organs. Epithelialization over the incision occurred in radio‐tagged bluegills at both temperatures, but there was little further healing at 6°C. At 20°C, tissue responses included chronic inflammation and dermal granulation. Radio‐tagged fish did not appear to be more susceptible than reference fish to bacterial infection. Mortality, adverse morphological effects, altered behavior, and limited healing in blue‐gills suggest that implanted transmitters impaired their health. Thus, movement and habitat use data collected by telemetry for this species and perhaps for other panfishes should be interpreted with caution.</span></span></p>","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1996)125<0440:EOITOA>2.3.CO;2","usgsCitation":"Knights, B.C., and Lasee, B.A., 1996, Effects of implanted transmitters on adult bluegills at two temperatures: Transactions of the American Fisheries Society, v. 125, no. 3, p. 440-449, https://doi.org/10.1577/1548-8659(1996)125<0440:EOITOA>2.3.CO;2.","productDescription":"10 p.","startPage":"440","endPage":"449","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":134004,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"125","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611e37","contributors":{"authors":[{"text":"Knights, Brent C. 0000-0001-8526-8468 bknights@usgs.gov","orcid":"https://orcid.org/0000-0001-8526-8468","contributorId":2906,"corporation":false,"usgs":true,"family":"Knights","given":"Brent","email":"bknights@usgs.gov","middleInitial":"C.","affiliations":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"preferred":true,"id":312743,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lasee, Becky A.","contributorId":30586,"corporation":false,"usgs":true,"family":"Lasee","given":"Becky","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":312744,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":32925,"text":"ds36 - 1996 - Tabular data, text, and graphical images in support of the 1995 National assessment of United States oil and gas resources","interactions":[],"lastModifiedDate":"2024-05-24T14:08:48.156532","indexId":"ds36","displayToPublicDate":"1996-05-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"36","title":"Tabular data, text, and graphical images in support of the 1995 National assessment of United States oil and gas resources","docAbstract":"This CD-ROM contains files in support of the 1995 USGS National assessment of United States oil and gas resources (DDS-30), which was published separately and summarizes the results of a 3-year study of the oil and gas resources of the onshore and state waters of the United States. The study describes about 560 oil and gas plays in the United States; confirmed and hypothetical, conventional and unconventional. A parallel study of the Federal offshore is being conducted by the U.S. Minerals Management Service. This CD-ROM contains files in multiple formats, so that almost any computer user can import them into word processors and spreadsheets. The tabular data include some tables not released in DDS-30. No proprietary data are released on this CD-ROM, but some tables of summary statistics from the proprietary files are provided. The complete text of DDS-30 is also available, as well as many figures. Also included are some of the programs used in the assessment, in source code and with supporting documentation. A companion CD-ROM (DDS-35) includes the map data and the same text data, but none of the tabular data or assessment programs.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds36","usgsCitation":"Charpentier, R., Klett, T., Obuch, R., and Brewton, J., 1996, Tabular data, text, and graphical images in support of the 1995 National assessment of United States oil and gas resources: U.S. Geological Survey Data Series 36, HTML Document: 1 CD-ROM, https://doi.org/10.3133/ds36.","productDescription":"HTML Document: 1 CD-ROM","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":429255,"rank":3,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P13YZJZG","text":"1995 National Oil and Gas Assessment Data Collection Archive"},{"id":3092,"rank":2,"type":{"id":15,"text":"Index 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R. 0000-0001-9779-1168","orcid":"https://orcid.org/0000-0001-9779-1168","contributorId":83067,"corporation":false,"usgs":true,"family":"Klett","given":"T. R.","affiliations":[],"preferred":false,"id":209441,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Obuch, R. C.","contributorId":85976,"corporation":false,"usgs":true,"family":"Obuch","given":"R. C.","affiliations":[],"preferred":false,"id":209442,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brewton, J. D.","contributorId":46579,"corporation":false,"usgs":true,"family":"Brewton","given":"J. D.","affiliations":[],"preferred":false,"id":209440,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1209,"text":"wsp2404 - 1996 - Suspended-sediment characteristics of Indiana streams, 1952-84","interactions":[{"subject":{"id":13197,"text":"ofr87527 - 1988 - Suspended-sediment characteristics of Indiana streams, 1952-84","indexId":"ofr87527","publicationYear":"1988","noYear":false,"title":"Suspended-sediment characteristics of Indiana streams, 1952-84"},"predicate":"SUPERSEDED_BY","object":{"id":1209,"text":"wsp2404 - 1996 - Suspended-sediment characteristics of Indiana streams, 1952-84","indexId":"wsp2404","publicationYear":"1996","noYear":false,"title":"Suspended-sediment characteristics of Indiana streams, 1952-84"},"id":1}],"lastModifiedDate":"2016-05-13T09:49:57","indexId":"wsp2404","displayToPublicDate":"1996-05-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2404","title":"Suspended-sediment characteristics of Indiana streams, 1952-84","docAbstract":"<p>Suspended-sediment concentration and discharge data were collected at 7 daily record stations and 70 partial-record stations during 1952- 84. Median suspended-sediment concentrations ranged from 24 to 61 milligrams per liter at daily record stations; concentrations ranged from 6 to 539 milligrams per liter at partial-record stations. Most suspended sediment transported in Indiana streams is silt and clay size (particles between 0.062 and 0.004 millimeter in diameter and particles less than 0.004 millimeter in diameter).</p>\n<p>Large suspended-sediment concentrations were associated with storm runoff but not always with peak streamflow. Some peak concentrations of suspended sediment preceded peak streamflow by as much as 18 to 30 hours during storms. Suspended-sediment concentrations frequently were largest during a storm that occurred after a period of low streamflow, when large amounts of sediment were eroded and transported into the stream and little base flow was available for dilution. For most of the streams studied, reliable predictive equations could not be developed to quantify the relation between suspended-sediment concentration and streamflow because of the extreme variability in the data. Annual suspended-sediment yields at four daily record stations ranged from 186 to 1,914 tons per square mile.</p>\n<p>Annual suspended-sediment yields for 70 partial-record stations, estimated by use of the suspended-sediment transport, flowduration-curve method, ranged from 11 to 2,310 tons per square mile. However, because of the poor correlation between suspended-sediment discharge and streamflow, these estimates are imprecise.</p>\n<p>Periods of record at 4 daily record and 32 partial-record stations were sufficient to test for trends. The trend in suspended-sediment concentration, adjusted for streamflow, was significant for only 9 of the 36 stations. At six of the nine stations, flow-adjusted suspended-sediment concentrations decreased with time.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wsp2404","collaboration":"Indiana Department of Natural Resources","usgsCitation":"Crawford, C.G., and Mansue, L.J., 1996, Suspended-sediment characteristics of Indiana streams, 1952-84: U.S. Geological Survey Water Supply Paper 2404, v, 55 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2404.","productDescription":"v, 55 p. :ill., maps ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":137960,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2404/report-thumb.jpg"},{"id":26095,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2404/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":253,"text":"wsp2451 - 1996 - Surface-water-quality assessment of the lower Kansas River basin, Kansas and Nebraska: Results of investigations, 1987-90","interactions":[{"subject":{"id":17760,"text":"ofr94365 - 1995 - Surface-water-quality assessment of the lower Kansas River basin, Kansas and Nebraska; results of investigations, 1987-90","indexId":"ofr94365","publicationYear":"1995","noYear":false,"title":"Surface-water-quality assessment of the lower Kansas River basin, Kansas and Nebraska; results of investigations, 1987-90"},"predicate":"SUPERSEDED_BY","object":{"id":253,"text":"wsp2451 - 1996 - Surface-water-quality assessment of the lower Kansas River basin, Kansas and Nebraska: Results of investigations, 1987-90","indexId":"wsp2451","publicationYear":"1996","noYear":false,"title":"Surface-water-quality assessment of the lower Kansas River basin, Kansas and Nebraska: Results of investigations, 1987-90"},"id":1}],"lastModifiedDate":"2022-12-13T20:26:22.096889","indexId":"wsp2451","displayToPublicDate":"1996-05-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2451","title":"Surface-water-quality assessment of the lower Kansas River basin, Kansas and Nebraska: Results of investigations, 1987-90","docAbstract":"Analysis of surface-water-quality data has enabled an assessment of water-quality conditions and trends and their relation to human and natural factors in the lower Kansas River basin, Kansas and Nebraska. This basin drains 15,300 square miles of predominantly agricultural land and is one of seven pilot studies completed as part of the National Water-Quality Assessment Program.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2451","usgsCitation":"Helgesen, J.O., 1996, Surface-water-quality assessment of the lower Kansas River basin, Kansas and Nebraska: Results of investigations, 1987-90: U.S. Geological Survey Water Supply Paper 2451, vii, 129 p., https://doi.org/10.3133/wsp2451.","productDescription":"vii, 129 p.","costCenters":[],"links":[{"id":136619,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2451/report-thumb.jpg"},{"id":94693,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2451/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":410396,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25445.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Kansas, Nebraska","otherGeospatial":"lower Kansas River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -99,\n              41.256\n            ],\n            [\n              -99,\n              38.658\n            ],\n            [\n              -94.561,\n              38.658\n            ],\n            [\n              -94.561,\n              41.256\n            ],\n            [\n              -99,\n              41.256\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604335","contributors":{"authors":[{"text":"Helgesen, John O.","contributorId":101630,"corporation":false,"usgs":true,"family":"Helgesen","given":"John","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":142152,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2423,"text":"wsp2407 - 1996 - An accounting system for water and consumptive use along the Colorado River, Hoover Dam to Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"wsp2407","displayToPublicDate":"1996-05-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2407","title":"An accounting system for water and consumptive use along the Colorado River, Hoover Dam to Mexico","docAbstract":"An accounting system for estimating and distributing consumptive use of water by vegetation to water users was developed for the Colorado River to meet the requirements of a U.S. Supreme Court decree and used with data from calendar year 1984. The system is based on a water-budget method to estimate total consumptive use by vegetation which is apportioned to agricultural users by using percentages of total evapotranspiration by vegetation estimated from digital-image analysis of satellite data.","language":"ENGLISH","publisher":"U.S. G.P.O. ;\r\nFor sale by the U.S. Geological Survey, Information Services,","doi":"10.3133/wsp2407","usgsCitation":"Owen-Joyce, S.J., and Raymond, L.H., 1996, An accounting system for water and consumptive use along the Colorado River, Hoover Dam to Mexico: U.S. Geological Survey Water Supply Paper 2407, viii, 94 p. :ill., maps (some col.) ;28 cm.; 3 plates in pocket, https://doi.org/10.3133/wsp2407.","productDescription":"viii, 94 p. :ill., maps (some col.) ;28 cm.; 3 plates in pocket","costCenters":[],"links":[{"id":138943,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2407/report-thumb.jpg"},{"id":247210,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2407/plate-1.pdf","size":"2885","linkFileType":{"id":1,"text":"pdf"}},{"id":247211,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2407/plate-2.pdf","size":"6958","linkFileType":{"id":1,"text":"pdf"}},{"id":247212,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2407/plate-3.pdf","size":"4618","linkFileType":{"id":1,"text":"pdf"}},{"id":28436,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2407/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685ce5","contributors":{"authors":[{"text":"Owen-Joyce, Sandra J. 0000-0002-4400-5618 sjowen@usgs.gov","orcid":"https://orcid.org/0000-0002-4400-5618","contributorId":5215,"corporation":false,"usgs":true,"family":"Owen-Joyce","given":"Sandra","email":"sjowen@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":145175,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Raymond, Lee H.","contributorId":83501,"corporation":false,"usgs":true,"family":"Raymond","given":"Lee","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":145176,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":22848,"text":"ofr95654 - 1996 - Exploratory analysis of environmental interactions in central California","interactions":[],"lastModifiedDate":"2012-04-15T17:28:14","indexId":"ofr95654","displayToPublicDate":"1996-05-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-654","title":"Exploratory analysis of environmental interactions in central California","docAbstract":"As part of its global change research program, the United States Geological Survey (USGS) has produced raster data that describe the land cover of the United States using a consistent format. The data consist of elevations, satellite measurements, computed vegetation indices, land cover classes, and ancillary political, topographic and hydrographic information. This open-file report uses some of these data to explore the environment of a (256-km)? region of central California. We present various visualizations of the data, multiscale correlations between topography and vegetation, a path analysis of more complex statistical interactions, and a map that portrays the influence of agriculture on the region's vegetation. An appendix contains C and Mathematica code used to generate the graphics and some of the analysis.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr95654","issn":"0094-9140","usgsCitation":"De Cola, L., and Falcone, N.L., 1996, Exploratory analysis of environmental interactions in central California: U.S. Geological Survey Open-File Report 95-654, NA, https://doi.org/10.3133/ofr95654.","productDescription":"NA","costCenters":[],"links":[{"id":155313,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1309,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/0654/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f1204","contributors":{"authors":[{"text":"De Cola, Lee","contributorId":59821,"corporation":false,"usgs":true,"family":"De Cola","given":"Lee","email":"","affiliations":[],"preferred":false,"id":188992,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Falcone, Neil L.","contributorId":71204,"corporation":false,"usgs":true,"family":"Falcone","given":"Neil","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":188993,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70018625,"text":"70018625 - 1996 - Crustal and upper mantle velocity structure of the Salton Trough, southeast California","interactions":[],"lastModifiedDate":"2025-09-09T15:15:05.045292","indexId":"70018625","displayToPublicDate":"1996-04-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3524,"text":"Tectonics","active":true,"publicationSubtype":{"id":10}},"title":"Crustal and upper mantle velocity structure of the Salton Trough, southeast California","docAbstract":"<p><span>This paper presents data and modelling results from a crustal and upper mantle wide-angle seismic transect across the Salton Trough region in southeast California. The Salton Trough is a unique part of the Basin and Range province where mid-ocean ridge/transform spreading in the Gulf of California has evolved northward into the continent. In 1992, the U.S. Geological Survey (USGS) conducted the final leg of the Pacific to Arizona Crustal Experiment (PACE). Two perpendicular models of the crust and upper mantle were fit to wide-angle reflection and refraction travel times, seismic amplitudes, and Bouguer gravity anomalies. The first profile crossed the Salton Trough from the southwest to the northeast, and the second was a strike line that paralleled the Salton Sea along its western edge. We found thin crust (∼21–22 km thick) beneath the axis of the Salton Trough (Imperial Valley) and locally thicker crust (∼27 km) beneath the Chocolate Mountains to the northeast. We modelled a slight thinning of the crust further to the northeast beneath the Colorado River (∼24 km) and subsequent thickening beneath the metamorphic core complex belt northeast of the Colorado River. There is a deep, apparently young basin (∼5–6 km unmetamorphosed sediments) beneath the Imperial Valley and a shallower (∼2–3 km) basin beneath the Colorado River. A regional 6.9-km/s layer (between ∼15-km depth and the Moho) underlies the Salton Trough as well as the Chocolate Mountains where it pinches out at the Moho. This lower crustal layer is spatially associated with a low-velocity (7.6–7.7 km/s) upper mantle. We found that our crustal model is locally compatible with the previously suggested notion that the crust of the Salton Trough has formed almost entirely from magmatism in the lower crust and sedimentation in the upper crust. However, we observe an apparently magmatically emplaced lower crust to the northeast, outside of the Salton Trough, and propose that this layer in part predates Salton Trough rifting. It may also in part result from migration of magmatic spreading centers associated with the southern San Andreas fault system. These spreading centers may have existed east of their current locations in the past and may have influenced the lower crust and upper mantle to the east of the current Salton Trough.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/95TC02616","issn":"02787407","usgsCitation":"Parsons, T., and McCarthy, J., 1996, Crustal and upper mantle velocity structure of the Salton Trough, southeast California: Tectonics, v. 15, no. 2, p. 456-471, https://doi.org/10.1029/95TC02616.","productDescription":"16 p.","startPage":"456","endPage":"471","costCenters":[],"links":[{"id":227171,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"southeast California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -116.22055370171185,\n              33.6645044265011\n            ],\n            [\n              -116.22055370171185,\n              32.7266371497649\n            ],\n            [\n              -114.50255964296149,\n              32.7266371497649\n            ],\n            [\n              -114.50255964296149,\n              33.6645044265011\n            ],\n            [\n              -116.22055370171185,\n              33.6645044265011\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"15","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fcd9e4b0c8380cd4e475","contributors":{"authors":[{"text":"Parsons, T.","contributorId":48288,"corporation":false,"usgs":true,"family":"Parsons","given":"T.","email":"","affiliations":[],"preferred":false,"id":380254,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCarthy, J.","contributorId":50290,"corporation":false,"usgs":true,"family":"McCarthy","given":"J.","affiliations":[],"preferred":false,"id":380255,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70017774,"text":"70017774 - 1996 - Middle Pliocene vegetation: Reconstructions, paleoclimatic inferences, and boundary conditions for climate modeling","interactions":[],"lastModifiedDate":"2024-09-30T16:52:59.112118","indexId":"70017774","displayToPublicDate":"1996-04-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2673,"text":"Marine Micropaleontology","active":true,"publicationSubtype":{"id":10}},"title":"Middle Pliocene vegetation: Reconstructions, paleoclimatic inferences, and boundary conditions for climate modeling","docAbstract":"<p><span>The general characteristics of global vegetation during the middle Pliocene warm period can be reconstructed from fossil pollen and plant megafossil data. The largest differences between Pliocene vegetation and that of today occurred at high latitudes in both hemispheres, where warming was pronounced relative to today. In the Northern Hemisphere coniferous forests lived in the modern tundra and polar desert regions, whereas in the Southern Hemisphere southern beech apparently grew in coastal areas of Antarctica.</span></p><p><span>Pliocene middle latitude vegetation differed less, although moister-than-modern conditions supported forest and woodland growth in some regions now covered by steppe or grassland. Pliocene tropical vegetation reflects essentially modem conditions in some regions and slightly cooler-than-or warmer-than- modern climates in other areas. Changes in topography induced by tectonics may be responsible for many of the climatic changes since the Pliocene in both middle and lower latitudes. However, the overall latitudinal progression of climatic conditions on land parallels that seen in the reconstruction of middle Pliocene sea-surface temperatures.</span></p><p><span>Pliocene paleovegetational data was employed to construct a 2 ° × 2 ° global grid of estimated mid-Pliocene vegetational cover for use as boundary conditions for numerical General Circulation Model simulations of middle Pliocene climates. Continental outlines and topography were first modified to represent the Pliocene landscape on the 2 ° × 2 ° grid. A modern 1 ° × 1 ° vegetation grid was simplified and mapped on this Pliocene grid, and then modified following general geographic trends evident in the Pliocene paleovegetation data set.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0377-8398(95)00051-8","usgsCitation":"Thompson, R.S., and Fleming, R., 1996, Middle Pliocene vegetation: Reconstructions, paleoclimatic inferences, and boundary conditions for climate modeling: Marine Micropaleontology, v. 27, no. 1-4, p. 27-49, https://doi.org/10.1016/0377-8398(95)00051-8.","productDescription":"23 p.","startPage":"27","endPage":"49","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":228771,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a56dde4b0c8380cd6d8a2","contributors":{"authors":[{"text":"Thompson, Robert S. 0000-0001-9287-2954 rthompson@usgs.gov","orcid":"https://orcid.org/0000-0001-9287-2954","contributorId":891,"corporation":false,"usgs":true,"family":"Thompson","given":"Robert","email":"rthompson@usgs.gov","middleInitial":"S.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":377532,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fleming, R.F.","contributorId":31918,"corporation":false,"usgs":true,"family":"Fleming","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":377531,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":33606,"text":"b2142 - 1996 - Thermal evolution of sedimentary basins in Alaska","interactions":[],"lastModifiedDate":"2025-03-06T19:51:53.04338","indexId":"b2142","displayToPublicDate":"1996-04-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2142","title":"Thermal evolution of sedimentary basins in Alaska","docAbstract":"The complex tectonic collage of Alaska is reflected in\r\nthe conjunction of rocks of widely varying thermal maturity.\r\nIndicators of the level of thermal maturity of rocks exposed\r\nat the surface, such as vitrinite reflectance and conodont color\r\nalteration index, can help constrain the tectonic evolution of\r\nsuch complex regions and, when combined with petrographic,\r\nmodern heat flow, thermogeochronologic, and isotopic data,\r\nallow for the detailed evaluation of a region?s burial and uplift\r\nhistory. We have collected and assembled nearly 10,000\r\nvitrinite-reflectance and conodont-color-alteration index values from the literature, previous U.S. Geological Survey investigations,\r\nand our own studies in Alaska. This database\r\nallows for the first synthesis of thermal maturity on a broadly\r\nregional scale.\r\nPost-accretionary sedimentary basins in Alaska show\r\nwide variability in terms of thermal maturity. The Tertiary\r\ninterior basins, as well as some of the forearc and backarc\r\nbasins associated with the Aleutian Arc, are presently at their\r\ngreatest depth of burial, with immature rocks exposed at the\r\nsurface. Other basins, such as some backarc basins on the\r\nAlaska Peninsula, show higher thermal maturities, indicating\r\nmodest uplift, perhaps in conjunction with higher geothermal\r\ngradients related to the arc itself. Cretaceous ?flysch?\r\nbasins, such as the Yukon-Koyukuk basin, are at much higher\r\nthermal maturity, reflecting great amounts of uplift perhaps\r\nassociated with compressional regimes generated through\r\nterrane accretion. Many sedimentary basins in Alaska, such\r\nas the Yukon-Koyukuk and Colville basins, show higher thermal\r\nmaturity at basin margins, perhaps reflecting greater uplift\r\nof the margins in response to isostatic unloading, owing\r\nto erosion of the hinterland adjacent to the basin or to compressional\r\nstresses adjacent to basin margins.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b2142","usgsCitation":"1996, Thermal evolution of sedimentary basins in Alaska: U.S. Geological Survey Bulletin 2142, v, 131 p., https://doi.org/10.3133/b2142.","productDescription":"v, 131 p.","costCenters":[],"links":[{"id":3381,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/dds/dds-54/Report/Bull2142.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61488,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/2142/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":165900,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":110059,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25586.htm","text":"Thermal evolution of sedimentary basins in Alaska","linkFileType":{"id":5,"text":"html"},"description":"25586"},{"id":483001,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25587.htm","text":"Thermal-maturity patterns and geothermal gradients on the Alaska Peninsula","linkFileType":{"id":5,"text":"html"}},{"id":483002,"rank":6,"type":{"id":36,"text":"NGMDB Index 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,{"id":30749,"text":"fs08596 - 1996 - The National Geochronological Database","interactions":[],"lastModifiedDate":"2012-02-02T00:09:13","indexId":"fs08596","displayToPublicDate":"1996-04-01T00:00:00","publicationYear":"1996","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":"085-96","title":"The National Geochronological Database","language":"ENGLISH","doi":"10.3133/fs08596","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1996, The National Geochronological Database: U.S. Geological Survey Fact Sheet 085-96, NA, https://doi.org/10.3133/fs08596.","productDescription":"NA","costCenters":[],"links":[{"id":119497,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1996/0085/report-thumb.jpg"},{"id":59477,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1996/0085/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b16f","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":529237,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1001151,"text":"1001151 - 1996 - Long-term declines in nest success of prairie ducks","interactions":[],"lastModifiedDate":"2024-12-27T16:49:22.745483","indexId":"1001151","displayToPublicDate":"1996-04-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Long-term declines in nest success of prairie ducks","docAbstract":"<p>Increased predation on nests of ducks in prairie uplands, as a result of habitat alteration, has been hypothesized to cause decreased nest success and population sizes. We tested whether, and by how much, nest success declined using data compiled from 37 studies conducted between 1935 and 1992 at 67 sites in the Prairie Pothole Region of Canada and the United States. Nest success declined (P = 0.0002) over time, but time explained only 10% of the variation; precipitation (<i>P</i> = 0.79) did not account for additional variation in nest success. Nest success declined at similar (<i>P</i> = 0.13) rates among 5 species, but late nesters (gadwall [Anas strepera], blue-winged teal [<i>A. discors</i>] and northern shoveler [<i>A. clypeata</i>]) had higher success (<i>P</i> = 0.004) than early nesters (mallard [<i>A.</i> <i>platyrhynchos</i>] and northern pintail [<i>A. acuta</i>]). Populations of gadwalls and northern shovelers, however, have not declined, indicating that declines in nest success may not be related causally to population change. Long-term population declines in blue-winged teal, northern pintails, and mallards coincide with large-scale temporal declines in nest success. Declines in nest success were parallel in parkland and grassland regions, suggesting a causal agent (or agents) that act(s) at a broad scale, despite inherent differences in the composition of the predator communities and habitats between regions.</p>","language":"English","publisher":"Wildlife Society","doi":"10.2307/3802222","usgsCitation":"Beauchamp, W., Koford, R.R., Nudds, T.D., Clark, R.G., and Johnson, D.H., 1996, Long-term declines in nest success of prairie ducks: Journal of Wildlife Management, v. 60, no. 2, p. 247-257, https://doi.org/10.2307/3802222.","productDescription":"11 p.","startPage":"247","endPage":"257","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":134026,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","otherGeospatial":"Prairie Pothole Region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -117.6621026378391,\n              54.22960374181571\n            ],\n            [\n              -115.1710009797501,\n              50.95601012821028\n            ],\n            [\n              -114.7031548073634,\n              48.53100061727011\n            ],\n            [\n              -104.08194910332246,\n              48.4450463601093\n            ],\n            [\n              -98.34665404574199,\n              42.8487699482325\n            ],\n            [\n              -96.96190905464837,\n              43.10358039599805\n            ],\n            [\n              -95.6089231851656,\n              44.322050477856095\n            ],\n            [\n              -96.17349364011999,\n              46.33095729323018\n            ],\n            [\n              -98.2749286963188,\n              47.68249972207552\n            ],\n            [\n              -99.4153286142953,\n              50.889542061873414\n            ],\n            [\n              -117.6621026378391,\n              54.22960374181571\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"60","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db63599a","contributors":{"authors":[{"text":"Beauchamp, W.D.","contributorId":89494,"corporation":false,"usgs":true,"family":"Beauchamp","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":310600,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Koford, Rolf R.","contributorId":16347,"corporation":false,"usgs":true,"family":"Koford","given":"Rolf","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":310597,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nudds, Thomas D.","contributorId":178164,"corporation":false,"usgs":false,"family":"Nudds","given":"Thomas","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":310598,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Clark, Robert G.","contributorId":33781,"corporation":false,"usgs":false,"family":"Clark","given":"Robert","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":310601,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Johnson, Douglas H. 0000-0002-7778-6641","orcid":"https://orcid.org/0000-0002-7778-6641","contributorId":70327,"corporation":false,"usgs":true,"family":"Johnson","given":"Douglas","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":310599,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":28049,"text":"wri944069 - 1996 - Statistical summaries of streamflow data for selected gaging stations in Idaho and adjacent states through September 1990 - Volume 1: Gaging stations with 10 or more years of record","interactions":[],"lastModifiedDate":"2021-12-14T20:15:05.822015","indexId":"wri944069","displayToPublicDate":"1996-04-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"94-4069","title":"Statistical summaries of streamflow data for selected gaging stations in Idaho and adjacent states through September 1990 - Volume 1: Gaging stations with 10 or more years of record","docAbstract":"<p>This volume presents statistical summaries of streamflow data for 257 gaging stations with 10 or more years of continuous record through September 1990. The gaging stations are located in Idaho and adjacent States. Volume 2 presents statistical summaries of streamflow data for 76 gaging stations with 5 to 9 years of continuous record, or with records of discharge measurements from springs, through September 1990. The gaging stations are located in Idaho and western Wyoming. </p><p>Streamflow statistics generated for gaging stations with 10 or more years of record were (1) magnitudes of monthly and annual flows; (2) magnitudes and frequencies of daily low, high, instantaneous peak (flood frequency), and annual mean flows; (3) duration of daily mean flows; and (4) maximum, median, and minimum daily mean flows. Streamflow statistics generated for gaging stations with 5 to 9 years of record or that measure discharge from springs (volume 2) were (1) magnitudes of monthly and annual flows; (2) duration of daily mean flows; and (3) maximum, median, and minimum daily mean flows. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944069","usgsCitation":"Kjelstrom, L., Stone, M.A., and Harenberg, W., 1996, Statistical summaries of streamflow data for selected gaging stations in Idaho and adjacent states through September 1990 - Volume 1: Gaging stations with 10 or more years of record: U.S. Geological Survey Water-Resources Investigations Report 94-4069, iii, 533 p., https://doi.org/10.3133/wri944069.","productDescription":"iii, 533 p.","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":392877,"rank":3,"type":{"id":36,"text":"NGMDB Index 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cfe4b07f02db545c0d","contributors":{"authors":[{"text":"Kjelstrom, L.C.","contributorId":89104,"corporation":false,"usgs":true,"family":"Kjelstrom","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":199128,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stone, M. A. J.","contributorId":27496,"corporation":false,"usgs":true,"family":"Stone","given":"M.","email":"","middleInitial":"A. J.","affiliations":[],"preferred":false,"id":199126,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harenberg, W. A.","contributorId":78743,"corporation":false,"usgs":true,"family":"Harenberg","given":"W. A.","affiliations":[],"preferred":false,"id":199127,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70211064,"text":"70211064 - 1996 - Controls on 222Rn variations in a fractured crystalline rock aquifer evaluated using aquifer tests and geophysical logging","interactions":[],"lastModifiedDate":"2021-02-01T14:56:28.157324","indexId":"70211064","displayToPublicDate":"1996-03-31T10:01:42","publicationYear":"1996","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Controls on <sup>222</sup>Rn variations in a fractured crystalline rock aquifer evaluated using aquifer tests and geophysical logging","title":"Controls on 222Rn variations in a fractured crystalline rock aquifer evaluated using aquifer tests and geophysical logging","docAbstract":"<p>Concentrations of<span>&nbsp;</span><sup>222</sup>Rn in ground water may vary considerably within megascopically homogeneous rocks over relatively short distances. Calculations indicate that different hydraulic apertures of water‐bearing fractures may account for variations in dissolved<span>&nbsp;</span><sup>222</sup>Rn concentration measured in domestic water wells completed in fractured Pikes Peak Granite, assuming that all other factors influencing dissolved<span>&nbsp;</span><sup>222</sup>Rn concentrations are constant. Concentrations of dissolved<span>&nbsp;</span><sup>222</sup>Rn range from 124 to 840 kBq m<sup>‐3</sup><span>&nbsp;</span>[3,360 to 22,700 picocuries per liter (pCi L<sup>‐1</sup>)] within a 2.5 km<sup>2</sup><span>&nbsp;</span>well field. Aquifer tests show that transmissivities range from 0.072 to 160 m<sup>2</sup><span>&nbsp;</span>day<sup>‐1</sup><span>&nbsp;</span>within the well field. Acoustic televiewer and heat‐pulse flow meter logging of four wells reveals that, despite tens to hundreds of fractures that intersect each well, a single fracture supplies all the flow to three wells, and one fracture provides 65% of the flow to the fourth well. Aquifer tests indicate that two pairs of the four wells are hydraulically connected. Type‐curve interpretation of early‐time data from aquifer tests reveals classic half‐slope behavior on log‐log plots of drawdown versus time for two wells, suggesting linear flow to a single fracture. Drawdown versus time for the other two wells indicates radial or pseudo‐radial flow, which suggests a higher degree of fracture interconnectivity near those boreholes.</p><p>Hydraulic apertures calculated using the cubic law are 0.024 and 0.038 cm for producing fractures in the first hydraulically connected well pair and 0.011 and 0.020 cm for flowing fractures in the second well pair. Assuming uniform distribution of<span>&nbsp;</span><sup>226</sup>Ra along fracture walls and long residence time of water relative to<span>&nbsp;</span><sup>222</sup>Rn decay, the ratio of fracture apertures should equal the inverse ratio of<span>&nbsp;</span><sup>222</sup>Rn concentration in each well. Assuming 50% error in hydraulic aperture estimation and 10% analytical uncertainty in<span>&nbsp;</span><sup>222</sup>Rn measurement, differences in<span>&nbsp;</span><sup>222</sup>Rn concentration between wells in the hydraulically connected pairs can be attributed solely to differences in hydraulic aperture. Different hydraulic apertures, however, do not explain different<span>&nbsp;</span><sup>222</sup>Rn concentrations<span>&nbsp;</span><i>between<span>&nbsp;</span></i>well pairs. Allowing for measurement error, a cubic meter of rock transfers from 1.3 to 20 times more<span>&nbsp;</span><sup>222</sup>Rn to ground water in the first pair of wells than in the second pair. Nonuniform distribution of<span>&nbsp;</span><sup>226</sup>Ra along fracture walls, heterogeneous emanating power in the rock‐water system, or short ground‐water residence time along the transmissive fracture network may account for the difference between well pairs.</p>","language":"English","publisher":"National Groundwater Association","doi":"10.1111/j.1745-6584.1996.tb01885.x","usgsCitation":"Folger, P.F., Poeter, E., Wanty, R.B., Frishman, D., and Day, W., 1996, Controls on 222Rn variations in a fractured crystalline rock aquifer evaluated using aquifer tests and geophysical logging: Groundwater, v. 34, no. 2, p. 250-261, https://doi.org/10.1111/j.1745-6584.1996.tb01885.x.","productDescription":"12 p.","startPage":"250","endPage":"261","costCenters":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":376324,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Conifer, Elk Creek drainage basin, Pine Junction","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.39527893066406,\n              39.44520783247914\n            ],\n            [\n              -105.28987884521484,\n              39.44520783247914\n            ],\n            [\n              -105.28987884521484,\n              39.5712929506796\n            ],\n            [\n              -105.39527893066406,\n              39.5712929506796\n            ],\n            [\n              -105.39527893066406,\n              39.44520783247914\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"34","issue":"2","noUsgsAuthors":false,"publicationDate":"2005-08-04","publicationStatus":"PW","contributors":{"authors":[{"text":"Folger, P. F.","contributorId":57862,"corporation":false,"usgs":true,"family":"Folger","given":"P.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":792648,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poeter, E.","contributorId":48708,"corporation":false,"usgs":true,"family":"Poeter","given":"E.","affiliations":[],"preferred":false,"id":792649,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wanty, Richard B. 0000-0002-2063-6423 rwanty@usgs.gov","orcid":"https://orcid.org/0000-0002-2063-6423","contributorId":443,"corporation":false,"usgs":true,"family":"Wanty","given":"Richard","email":"rwanty@usgs.gov","middleInitial":"B.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":792650,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Frishman, D.","contributorId":14959,"corporation":false,"usgs":true,"family":"Frishman","given":"D.","affiliations":[],"preferred":false,"id":792651,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Day, W. 0000-0002-9278-2120","orcid":"https://orcid.org/0000-0002-9278-2120","contributorId":72136,"corporation":false,"usgs":true,"family":"Day","given":"W.","affiliations":[],"preferred":false,"id":792652,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":4489,"text":"cir1120I - 1996 - Sediment transport in the lower Missouri and the central Mississippi rivers, June 26 through September 14, 1993","interactions":[],"lastModifiedDate":"2012-02-02T00:05:47","indexId":"cir1120I","displayToPublicDate":"1996-03-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1120","chapter":"I","title":"Sediment transport in the lower Missouri and the central Mississippi rivers, June 26 through September 14, 1993","docAbstract":"Sediment data were collected for five sediment stations on the lower Missouri and the central Mississippi rivers during the 1993 flood. During the period of June 26 to September 14, 1993, 55 million metric tons was transported past St. Louis, Missouri by the Mississippi River. Sediment was stored in the Missouri River floodplain above the Mississippi River as more than 22,000 hectares of floodplain had newly deposited sediments from the receding floodwater.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir1120I","usgsCitation":"Holmes, R.R., 1996, Sediment transport in the lower Missouri and the central Mississippi rivers, June 26 through September 14, 1993: U.S. Geological Survey Circular 1120, vi, 23 p. :ill. (some col.), map ;28 cm.28 cm., https://doi.org/10.3133/cir1120I.","productDescription":"vi, 23 p. :ill. (some col.), map ;28 cm.28 cm.","costCenters":[],"links":[{"id":121446,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/cir_1120_I.bmp"},{"id":534,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/circ1120-i","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbdee","contributors":{"authors":[{"text":"Holmes, Robert R. Jr. 0000-0002-5060-3999 bholmes@usgs.gov","orcid":"https://orcid.org/0000-0002-5060-3999","contributorId":1624,"corporation":false,"usgs":true,"family":"Holmes","given":"Robert","suffix":"Jr.","email":"bholmes@usgs.gov","middleInitial":"R.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":false,"id":149325,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}