{"pageNumber":"523","pageRowStart":"13050","pageSize":"25","recordCount":16501,"records":[{"id":29320,"text":"wri834210 - 1985 - Effects of sanitary sewers on ground-water levels and streams in Nassau and Suffolk Counties, New York; part 3: Development and application of southern Nassau County model","interactions":[],"lastModifiedDate":"2022-01-04T21:31:14.384008","indexId":"wri834210","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"83-4210","title":"Effects of sanitary sewers on ground-water levels and streams in Nassau and Suffolk Counties, New York; part 3: Development and application of southern Nassau County model","docAbstract":"

By 1990, sanitary sewers in Nassau County Sewage Disposal Districts 2 and 3 and Suffolk County Southwest Sewer District will discharge to the ocean 140 cu ft of water per second that would otherwise be returned to the groundwater system through septic tanks and similar systems. To evaluate the effects of this loss on groundwater levels and streamflow, the U.S. Geological Survey developed a groundwater flow model that couples a fine-scale subregional model to a regional model of a larger scale. The regional model generates flux boundary conditions for the subregional model, and the subregional model provides detail in the area of concern. Results indicate that the water table will decline by as much as 90% from conditions in the early 1970's. This report is one of a three-part series describing the predicted hydrologic effects of sewers in southern Nassau and southwestern Suffolk Counties. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834210","usgsCitation":"Reilly, T.E., and Buxton, H., 1985, Effects of sanitary sewers on ground-water levels and streams in Nassau and Suffolk Counties, New York; part 3: Development and application of southern Nassau County model: U.S. Geological Survey Water-Resources Investigations Report 83-4210, vi, 41 p., https://doi.org/10.3133/wri834210.","productDescription":"vi, 41 p.","costCenters":[],"links":[{"id":393885,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35853.htm"},{"id":58161,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4210/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123395,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4210/report-thumb.jpg"}],"country":"United States","state":"New York","county":"Nassau County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -73.74435424804688,\n 40.58997103470645\n ],\n [\n -73.42300415039062,\n 40.58997103470645\n ],\n [\n -73.42300415039062,\n 40.77950154452172\n ],\n [\n -73.74435424804688,\n 40.77950154452172\n ],\n [\n -73.74435424804688,\n 40.58997103470645\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db610f06","contributors":{"authors":[{"text":"Reilly, T. E.","contributorId":79460,"corporation":false,"usgs":true,"family":"Reilly","given":"T.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":201343,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buxton, H. T.","contributorId":67873,"corporation":false,"usgs":true,"family":"Buxton","given":"H. T.","affiliations":[],"preferred":false,"id":201342,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":25868,"text":"wri854092 - 1985 - Description of water-systems operations in the Arkansas River basin, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:31","indexId":"wri854092","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4092","title":"Description of water-systems operations in the Arkansas River basin, Colorado","docAbstract":"To facilitate a current project modeling the hydrology of the Arkansas River basin in Colorado, a description of the regulation of water in the basin is necessary. The geographic and climatic setting of the Arkansas River basin that necessitates the use, reuse, importation, and storage of water are discussed. The history of water-resource development in the basin, leading to the present complex of water systems, also is discussed. Municipal, irrigation, industrial, and multipurpose water systems are described. System descriptions are illustrated with schematic line drawings, and supplemented with physical data tables for the lakes, tunnels, conduits, and canals in the various systems. Copies of criteria under which certain of the water systems operate, are included. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854092","usgsCitation":"Abbott, P., 1985, Description of water-systems operations in the Arkansas River basin, Colorado: U.S. Geological Survey Water-Resources Investigations Report 85-4092, xii, 67 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854092.","productDescription":"xii, 67 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123984,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4092/report-thumb.jpg"},{"id":54617,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4092/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54618,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4092/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54619,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4092/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54620,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4092/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54621,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4092/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668ffd","contributors":{"authors":[{"text":"Abbott, P.O.","contributorId":21154,"corporation":false,"usgs":true,"family":"Abbott","given":"P.O.","email":"","affiliations":[],"preferred":false,"id":195397,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28285,"text":"wri854277 - 1985 - Management of ground water and evolving hydrogeologic studies in New Jersey : a heavily urbanized and industrialized state in the northeastern United States","interactions":[],"lastModifiedDate":"2018-11-14T10:13:28","indexId":"wri854277","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4277","title":"Management of ground water and evolving hydrogeologic studies in New Jersey : a heavily urbanized and industrialized state in the northeastern United States","docAbstract":"

New Jersey is the most densely populated and one of the most industrialized states in the United States. An abundance of freshwater and proximity to major northeastern metropolitan centers has facilitated this development. Pumpage of freshwater from all aquifers in the State in 1980 was 730 million gallons per day (2.76 million cubic meters per day).

Management and efficient development of the ground-water resources of the State are the responsibility of the New Jersey Department of Environmental Protection. Laws have been enacted and updated by the State legislature to manage water allocation and to control the disposal of hazardous wastes. Present resource management is guided by the New Jersey Water-Supply Master Plan of 1981. Funding for management activities is partially derived from the sale of state-approved bonds.

Effective planning and regional management require accurate and up-to-date hydrologic information and analyses. The U.S. Geological Survey, in cooperation with the New Jersey Geological Survey, is conducting three intensive ground-water studies involving the collection and interpretation of hydrologic data to meet the urgent water-management needs of New Jersey. These studies are part of a long-term cooperative program and are funded through the Water-Supply Bond Act of 1981. They began in 1983 and are scheduled to be completed in 1988.

The project areas are situated in the New Jersey part of the Atlantic Coastal Plain in and near Atlantic City, Camden, and South River. They range in size from 400 to 1,200 mil (1,040 to 3,120 km2). The studies are designed to define the geology, hydrology, and geochemistry of the local ground-water systems. The results of these studies will enable the State to address more effectively major problems in these areas such as declining water levels, overpumping, saltwater intrusion, and ground-water contamination resulting from the improper disposal of hazardous wastes.

Specific objectives of these studies by the U.S. Geological Survey are to (1) develop an accurate and up-to-date hydrogeologic data base, (2) design and implement a data-collection program and establish a computerized information management system, (3) refine the conceptualization of the ground-water flow system, and (4) define the geochemistry of the aquifer system by conducting a water-quality appraisal. The objectives are accomplished by standard hydrogeologic methods. Information concerning hydrogeologic framework, ground-water levels, water use, hydraulic characteristics, and water quality in the study areas is compiled from all available sources. Additional data needed are collected through well inventories, surface geophysical surveys, water-quality samplings, water-level measurements, and a well-drilling program.

Interpretation of the flow system is based on the use of standard analytical techniques and digital flow modeling. Calibrated flow models will provide ground-water managers with a mechanism to develop and test regional water-supply strategies.

Definition of the geochemistry of the aquifer system is accomplished through a variety of methods which depend on the problems and available data in the particular study area. The approach includes statistical analysis of water-quality data, reaction-path modeling, and determination of the movement of chemical constituents using analytical and numerical modeling techniques.

A combined staff of 25 to 30 professionals and technicians from the New Jersey District office of the U.S. Geological Survey is committed to the three studies. The staff has specialists in geohydrology, numerical modeling, geochemistry, geophysics, and computer science. The findings of these studies will be published in data reports, interpretive reports, instructional manuals and journal articles.

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Jersey\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a2ac","contributors":{"authors":[{"text":"Leahy, P. Patrick","contributorId":80648,"corporation":false,"usgs":true,"family":"Leahy","given":"P.","email":"","middleInitial":"Patrick","affiliations":[],"preferred":false,"id":199529,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30629,"text":"wri854172 - 1985 - Geochemistry and hydrology of thermal springs in the Idaho Batholith and adjacent areas, central Idaho","interactions":[],"lastModifiedDate":"2013-11-21T14:01:02","indexId":"wri854172","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4172","title":"Geochemistry and hydrology of thermal springs in the Idaho Batholith and adjacent areas, central Idaho","docAbstract":"The occurrence of nature of thermal springs in the Idaho batholith and adjacent areas suggest a relation between structural controls and deeply circulating hot-water systems. Springs issuing from granitic rocks are associated mostly with major regional fault structures. Springs issuing from other rocks probably are related to local faulting. Individual spring flows and water temperatures are variable and range from less than 1 gallon per minute to 2,710 gallons per minute and from 20.5 degrees to 94.0 degrees Celsius. Annual spring discharge is at least 27,000 acre-feet; heat discharges convectively is estimated to be 5.0 x 107 calories per second. Thermal springs discharge relatively dilute water; dissolved solids range from 103 to 839 milligrams per liter. The chemical quality of the water suggests deep circulation of meteoric water. Estimated reservoir temperatures are generally less than 100 degrees Celsius, but temperatures for several springs exceed 150 degrees Celsius. Stable-isotope data suggest that most of the thermal water is not derived from current precipitation. Carbon-14 values indicate that thermal waters are old; apparent residence times range from 9,000 to more than 40,000 years.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854172","usgsCitation":"Young, H., 1985, Geochemistry and hydrology of thermal springs in the Idaho Batholith and adjacent areas, central Idaho: U.S. Geological Survey Water-Resources Investigations Report 85-4172, Report: iii, 44 p.; 2 Plates: 33.92 x 35.78 inches and 34.62 x 36.35 inches, https://doi.org/10.3133/wri854172.","productDescription":"Report: iii, 44 p.; 2 Plates: 33.92 x 35.78 inches and 34.62 x 36.35 inches","numberOfPages":"49","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":119347,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4172/report-thumb.jpg"},{"id":59389,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4172/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59390,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4172/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59391,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4172/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","otherGeospatial":"Idaho Batholith","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.24,41.99 ], [ -117.24,49.0 ], [ -111.04,49.0 ], [ -111.04,41.99 ], [ -117.24,41.99 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab73f","contributors":{"authors":[{"text":"Young, H.W.","contributorId":68278,"corporation":false,"usgs":true,"family":"Young","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":203567,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26394,"text":"wri844318 - 1985 - The hydrologic bench-mark program; a standard to evaluate time-series trends in selected water-quality constituents for streams in Georgia","interactions":[],"lastModifiedDate":"2017-01-24T10:13:42","indexId":"wri844318","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4318","title":"The hydrologic bench-mark program; a standard to evaluate time-series trends in selected water-quality constituents for streams in Georgia","docAbstract":"Significant temporal trends in monthly pH, specific conductance, total alkalinity, hardness, total nitrite-plus-nitrite nitrogen, and total phosphorus measurements at five stream sites in Georgia were identified using a rank correlation technique, the seasonal Kendall test and slope estimator. These sites include a U.S. Geological Survey Hydrologic Bench-Mark site, Falling Creek near Juliette, and four periodic water-quality monitoring sites. Comparison of raw data trends with streamflow-residual trends and, where applicable, with chemical-discharge trends (instantaneous fluxes) shws that some of these trends are responses to factors other than changing streamflow. Percentages of forested, agricultural, and urban cover with each basin did not change much during the periods of water-quality record, and therefore these non-flow-related trends are not obviously related to changes in land cover or land use. Flow-residual water-quality trends at the Hydrologic Bench-Mark site and at the Chattooga River site probably indicate basin reponses to changes in the chemical quality of atmospheric deposition. These two basins are predominantly forested and have received little recent human use. Observed trends at the other three sites probably indicate basin responses to various land uses and water uses associated with agricultural and urban land or to changes in specific uses. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844318","usgsCitation":"Buell, G.R., and Grams, S., 1985, The hydrologic bench-mark program; a standard to evaluate time-series trends in selected water-quality constituents for streams in Georgia: U.S. Geological Survey Water-Resources Investigations Report 84-4318, v, 36 p. :ill., map ;28 cm., https://doi.org/10.3133/wri844318.","productDescription":"v, 36 p. :ill., map ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":157852,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4318/report-thumb.jpg"},{"id":55187,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4318/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a85e4b07f02db64d7c6","contributors":{"authors":[{"text":"Buell, G. R.","contributorId":57103,"corporation":false,"usgs":true,"family":"Buell","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":196314,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grams, S.C.","contributorId":31432,"corporation":false,"usgs":true,"family":"Grams","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":196313,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26378,"text":"wri854176 - 1985 - Hydrologic factors affecting lake-level fluctuations in Big Marine Lake, Washington County, Minnesota","interactions":[],"lastModifiedDate":"2022-02-22T19:17:08.589151","indexId":"wri854176","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4176","title":"Hydrologic factors affecting lake-level fluctuations in Big Marine Lake, Washington County, Minnesota","docAbstract":"

A study by the U.S. Geological Survey from 1981 through 1984, in cooperation with the Carnelian-Marine Watershed District and the Minnesota Department of Natural Resources, investigated the causes of large lake-level fluctuations at Big Marine Lake. Historic records document that Big Marine Lake has changed substantially in surface area during the period 1847 through 1983; the maximum lake-surface area was 2,300 acres in 1847, and the minimum lake-surface area was 890 acres in 1938. A change in lake level of about 11 feet caused these changes in surface area. Serious flooding of lake-shore properties has occurred in recent years because residential development commonly took place during periods of relatively low-lake level during the 1950's and 1960's.

\n

Evaporation from the lake was estimated to be approximately equal to incident precipitation on the lake surface on an annual basis. Big Marine Lake does not have a surface-water inlet, and the outlet from the lake is at an elevation well above the stage at which lake-shore property is flooded. Hydrogeologic and geochemical data collected during the study show that (1) fluctuation of water levels at Big Marine Lake is controlled primarily by ground-water discharge to and seepage from the lake, (2) water in the drift aquifer and water in the lake are chemically similar, and (3) changes in the potentiometric surface of the bedrock aquifer have minor effects on changes in lake level.

\n

Long-term trends in cumulative departure from mean annual precipitation suggest that recharge to the drift aquifer in the area has been increasing since the 1940's. The increase in precipitation and recharge corresponds to the observed rise in lake level since 1965 when regular lake-level measurements began. Fluctuations in lake level in the future will depend on changes in recharge to the drift and bedrock aquifers, which is directly related to changes in long-term precipitation patterns.

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Effects of adherent bacteria and bacterial extracellular polymer (exopolymer) upon uptake of particle-bound Cd, Zn and Ag by the deposit-feeding clam Macoma balthica were studied in the laboratory. Amorphous iron oxyhydroxide and unaltered and alkaline-extracted sediments were used as model particulates in separate, controlled deposit-feeding experiments. In general, amounts of metal taken up from ingested particles varied dramatically with the nature of the particle surface. Ingestion of contaminated iron oxide particles did not contribute to overall uptake of Cd and Ag in feeding clams, but accounted for 89 to 99% of total Zn uptake. Exopolymer adsorbed on iron oxide particles caused an increase in the biological availability of particle-bound metals in the order Ag>Cd>Zn, whereas adherent bacteria up to 3.2 X 1011 g-1 had no effect upon amounts of metal taken up from ingested particulates. At the higher Cd and Ag concentrations employed (3.6 X 10-7M), feeding rates declined with increasing amounts of iron oxide-bound exopolymer, suggesting behavioral avoidance due to increased metal availability. Much of the Cd (57 %) taken up by clams feeding on unaltered estuarine sediments originated from particulates, even though particle/solute distribution of Cd (86%) was similar to that in experiments with iron oxide particles. Uptake of Cd from alkalineextracted sediments was insignificant, as it was from unamended iron oxide. However, addition of exopolymer (10 mgg-1 sediment) caused a restoration nn bioavailability of sediment-bound Cd.

","language":"English","publisher":"Inter-Res","usgsCitation":"Harvey, R.W., and Luoma, S.N., 1985, Effect of adherent bacteria and bacterial extracellular polymers upon assimilation by Macoma balthica of sediment-bound Cd, Zn and Ag: Marine Ecology Progress Series, v. 22, p. 281-289.","productDescription":"9 p.","startPage":"281","endPage":"289","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":316654,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":316653,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.int-res.com/abstracts/meps/v22/"}],"volume":"22","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56b9ca52e4b08d617f63a807","contributors":{"authors":[{"text":"Harvey, Ronald W. 0000-0002-2791-8503 rwharvey@usgs.gov","orcid":"https://orcid.org/0000-0002-2791-8503","contributorId":564,"corporation":false,"usgs":true,"family":"Harvey","given":"Ronald","email":"rwharvey@usgs.gov","middleInitial":"W.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":597564,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Luoma, Samuel N. 0000-0001-5443-5091 snluoma@usgs.gov","orcid":"https://orcid.org/0000-0001-5443-5091","contributorId":2287,"corporation":false,"usgs":true,"family":"Luoma","given":"Samuel","email":"snluoma@usgs.gov","middleInitial":"N.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":597565,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70170445,"text":"70170445 - 1985 - Ground-water and surface-water interactions in Minnesota and Wisconsin wetlands","interactions":[],"lastModifiedDate":"2018-03-05T12:13:55","indexId":"70170445","displayToPublicDate":"1989-12-01T15:30:00","publicationYear":"1985","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Ground-water and surface-water interactions in Minnesota and Wisconsin wetlands","docAbstract":"

The interaction between ground water and surface water in wetlands is complex and depends on the hydrologic setting of the particular wetland. Hydrologic characteristics have been used in Wisconsin to classify wetlands into four categories; surface-waterdepression wetlands, surface-water-slope wetlands, ground-waterdepression wetlands, and ground-water-slope wetlands, as described by Novitzki (1978). The degree of ground- and surface-water interactions differs between the four categories.

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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5718a843e4b0ef3b7caba58e","contributors":{"authors":[{"text":"Brown, R. G.","contributorId":106118,"corporation":false,"usgs":true,"family":"Brown","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":627226,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stark, J. R.","contributorId":100406,"corporation":false,"usgs":true,"family":"Stark","given":"J. R.","affiliations":[],"preferred":false,"id":627227,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Patterson, G. L.","contributorId":35356,"corporation":false,"usgs":true,"family":"Patterson","given":"G.","email":"","middleInitial":"L.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":627228,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70156916,"text":"70156916 - 1985 - Remote sensing of tidal chlorophyll-a variations in estuaries","interactions":[],"lastModifiedDate":"2020-01-20T06:45:49","indexId":"70156916","displayToPublicDate":"1986-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2068,"text":"International Journal of Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Remote sensing of tidal chlorophyll-a variations in estuaries","docAbstract":"

Simultaneous acquisition of surface chlorophyll-a concentrations for 39 samples from boats and Daedalus 1260 Multispectral Scanner data from a U-2 aircraft was conducted in the northern reaches of San Francisco Bay on 28 August 1980. These data were used to develop regression models for predicting surface chlorophyll-a concentrations over the study area for ebb-tide (8.40 a.m. P.D.T. (Pacific Daylight Time)) and flood-tide (3.10 p.m. P.D.T.) conditions. After selection of a single ‘best fitting’ model for both morning and afternoon data sets, the chlorophyll-a concentration was predicted for ebb and flood tide for the entire study area at approximately 40m × 40m resolution. The predicted spatial display of chlorophyll-a revealed a localized area of high phytoplankton biomass that has been inferred from field surveys and appears to be a common summer phenomenon.

\n

Knowledge of the distribution of phytoplankton and the location of this zone of high biomass is valuable in establishing management policies for this ecologically important estuary. Furthermore, the techniques used here may provide an alternative cost-effective method for assessing water-quality conditions and they may prove useful for studying spatial variations (patchiness) and seasonal variations in phytoplankton biomass in other estuaries and coastal waters.

","language":"English","publisher":"Taylor & Francis","doi":"10.1080/01431168508948318","usgsCitation":"Catts, G.P., Khorram, S., Cloern, J.E., Knight, A.W., and Degloria, S.D., 1985, Remote sensing of tidal chlorophyll-a variations in estuaries: International Journal of Remote Sensing, v. 6, no. 11, p. 1685-1706, https://doi.org/10.1080/01431168508948318.","productDescription":"22 p.","startPage":"1685","endPage":"1706","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1980-08-28","temporalEnd":"1980-08-28","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":307808,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","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 -123.00292968749999,\n 37.339591851359174\n ],\n [\n -121.83837890625,\n 37.339591851359174\n ],\n [\n -121.83837890625,\n 38.156156969924915\n ],\n [\n -123.00292968749999,\n 38.156156969924915\n ],\n [\n -123.00292968749999,\n 37.339591851359174\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"6","issue":"11","noUsgsAuthors":false,"publicationDate":"2007-04-27","publicationStatus":"PW","scienceBaseUri":"560bb6f4e4b058f706e53e4c","contributors":{"authors":[{"text":"Catts, Glenn P.","contributorId":147307,"corporation":false,"usgs":false,"family":"Catts","given":"Glenn","email":"","middleInitial":"P.","affiliations":[{"id":7091,"text":"North Carolina State University","active":true,"usgs":false}],"preferred":false,"id":571138,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Khorram, Siamak","contributorId":147308,"corporation":false,"usgs":false,"family":"Khorram","given":"Siamak","email":"","affiliations":[{"id":7091,"text":"North Carolina State University","active":true,"usgs":false}],"preferred":false,"id":571139,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cloern, James E. 0000-0002-5880-6862 jecloern@usgs.gov","orcid":"https://orcid.org/0000-0002-5880-6862","contributorId":1488,"corporation":false,"usgs":true,"family":"Cloern","given":"James","email":"jecloern@usgs.gov","middleInitial":"E.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":571140,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Knight, Allen W.","contributorId":147309,"corporation":false,"usgs":false,"family":"Knight","given":"Allen","email":"","middleInitial":"W.","affiliations":[{"id":7082,"text":"University of California - Davis","active":true,"usgs":false}],"preferred":false,"id":571141,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Degloria, Stephen D.","contributorId":147310,"corporation":false,"usgs":false,"family":"Degloria","given":"Stephen","email":"","middleInitial":"D.","affiliations":[{"id":13243,"text":"University of California Berkeley","active":true,"usgs":false}],"preferred":false,"id":571142,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70236860,"text":"70236860 - 1985 - Automated derivation of hydrologic basin characteristics from digital elevation model data","interactions":[],"lastModifiedDate":"2022-09-20T15:05:54.578789","indexId":"70236860","displayToPublicDate":"1985-12-31T09:49:07","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Automated derivation of hydrologic basin characteristics from digital elevation model data","docAbstract":"

Digital elevation model (DEM) data in a raster format can be used to automatically derive the drainage characteristics of an area. A procedure has been designed that is capable of operating on matrices of elevation data having no algorithmically imposed size limit, while performing within the resolution and accuracy tolerances of the DEM data.

Each cell is processed as the center of a 3- by 3-cell spatial window in the raster elevation data. If a cell is a local minimum in comparison with two of its non-adjacent neighbors, it is labeled as a drainage cell. The linkages of the drainage cells within user-specified distance and elevation thresholds are established in a separate process. The products of these processing steps are digital masks of the drainage cells and the watershed basins, both in raster format.

A drainage cell mask derived using this procedure is useful in computing slope values for a raster data base. Slope has traditionally been calculated for each cell by fitting a plane through the eight nearest cells. However, if the terrain represented by these cells is V-shaped, such as a gully, a plane does not fit well; in fact, the desired slope value is the slope along the bottom of the gully, regardless of the steepness of the gully sides. The automated drainage process will label such a cell as a drainage cell, and its slope can then be computed from the elevation values of neighboring drainage cells.

","largerWorkTitle":"Auto-Carto VII: Proceedings of the digital representations of spatial knowledge","conferenceTitle":"Auto-Carto VII: Digital Representations of Spatial Knowledge","conferenceDate":"Mar 11-14, 1985","conferenceLocation":"Washington D.C.","language":"English","publisher":"Cartography and Geographic Information Society","usgsCitation":"Jenson, S.K., 1985, Automated derivation of hydrologic basin characteristics from digital elevation model data, in Auto-Carto VII: Proceedings of the digital representations of spatial knowledge, Washington D.C., Mar 11-14, 1985, p. 301-310.","productDescription":"10 p.","startPage":"301","endPage":"310","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":407057,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://cartogis.org/docs/proceedings/archive/auto-carto-7/index.html"},{"id":407058,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Jenson, Susan K.","contributorId":66859,"corporation":false,"usgs":true,"family":"Jenson","given":"Susan","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":852389,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70121039,"text":"70121039 - 1985 - Disturbance in a cypress-tupelo wetland: an interaction between thermal loading and hydrology","interactions":[],"lastModifiedDate":"2014-08-19T11:02:41","indexId":"70121039","displayToPublicDate":"1985-12-01T11:00:31","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3750,"text":"Wetlands","onlineIssn":"1943-6246","printIssn":"0277-5212","active":true,"publicationSubtype":{"id":10}},"title":"Disturbance in a cypress-tupelo wetland: an interaction between thermal loading and hydrology","docAbstract":"The interaction between thermal loading and hydrology was examined in a forested wetland. As a result of flooding, portions of the wetland are periodically exposed to elevated water temperatures, resulting in progressive deterioration of the canopy. We chose three study sites along a gradient of canopy disturbance: most disturbed, intermediate disturbance and a least disturbed site. The timing of flooding has important effects on this wetland: floods which occur late in the growing season have greater impact on the timing of litterfall and the extent of tree mortality. Following a flood in May, there was no observed increase in litterfall, and woody detrital production (tree mortality) eliminated only o.4% and 1.1% of the aboveground woody biomass at the intermediate and least disturbed sites, respectively. In contrast. premature leaf senescence and literfall were observed at the intermediate site following an August flood, and tree mortality at the intermediate and least disturbed sites eliminated 10% and 8%, respectively, of the aboveground woody biomass. At the most disturbed site, where the majority of trees were already dead, no additional mortality was recorded during the study. Long-term effects of this disturbance regime are the loss of small stems and increased stem production of trees which remain. While stem production at the intermediate site (413 g.m−2.yr−1) exceeded that at the least disturbed site (373 g.m−2.y−1), total aboveground net primary production was highest at the least disturbed site (788 g·m−2· yr−1), primarily because of the greater stem density. Portions of this wetland continue to deteriorate after more than 30 years of thermal loading.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wetlands","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Wetland Scientists","publisherLocation":"McClean, VA","doi":"10.1007/BF03160787","usgsCitation":"Scott, M.L., Sharitz, R.R., and Lee, L.C., 1985, Disturbance in a cypress-tupelo wetland: an interaction between thermal loading and hydrology: Wetlands, v. 5, no. 1, p. 53-68, https://doi.org/10.1007/BF03160787.","productDescription":"16 p.","startPage":"53","endPage":"68","numberOfPages":"16","costCenters":[],"links":[{"id":292532,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":292531,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF03160787"}],"volume":"5","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f464c9e4b073ff773a7cf5","contributors":{"authors":[{"text":"Scott, Michael L. scottm@usgs.gov","contributorId":1169,"corporation":false,"usgs":true,"family":"Scott","given":"Michael","email":"scottm@usgs.gov","middleInitial":"L.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":498714,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sharitz, Rebecca R.","contributorId":44598,"corporation":false,"usgs":true,"family":"Sharitz","given":"Rebecca","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":498716,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lee, Lyndon C.","contributorId":36064,"corporation":false,"usgs":true,"family":"Lee","given":"Lyndon","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":498715,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70185596,"text":"70185596 - 1985 - Concentration of trace elements in water samples by reductive precipitation","interactions":[],"lastModifiedDate":"2020-01-19T11:17:26","indexId":"70185596","displayToPublicDate":"1985-12-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Concentration of trace elements in water samples by reductive precipitation","docAbstract":"

No abstract available.

","language":"English","publisher":"American Chemical Society","doi":"10.1021/ac00291a016","usgsCitation":"Skogerboe, R.K., Hanagan, W., and Taylor, H.E., 1985, Concentration of trace elements in water samples by reductive precipitation: Analytical Chemistry, v. 57, no. 14, p. 2815-2818, https://doi.org/10.1021/ac00291a016.","productDescription":"4 p. ","startPage":"2815","endPage":"2818","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338282,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"57","issue":"14","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"58d6303ae4b05ec7991310fd","contributors":{"authors":[{"text":"Skogerboe, R. K","contributorId":189803,"corporation":false,"usgs":false,"family":"Skogerboe","given":"R.","email":"","middleInitial":"K","affiliations":[],"preferred":false,"id":686068,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanagan, W.A.","contributorId":189804,"corporation":false,"usgs":false,"family":"Hanagan","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":686069,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Taylor, Howard E. hetaylor@usgs.gov","contributorId":1551,"corporation":false,"usgs":true,"family":"Taylor","given":"Howard","email":"hetaylor@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":686070,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70185590,"text":"70185590 - 1985 - Assessment of the instantaneous unit hydrograph derived from the theory of topologically random networks","interactions":[],"lastModifiedDate":"2020-01-19T11:09:50","indexId":"70185590","displayToPublicDate":"1985-11-01T00:00:00","publicationYear":"1985","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":"Assessment of the instantaneous unit hydrograph derived from the theory of topologically random networks","docAbstract":"

An instantaneous unit hydrograph (iuh) based on the theory of topologically random networks (topological iuh) is evaluated in terms of sets of basin characteristics and hydraulic parameters. Hydrographs were computed using two linear routing methods for each of two drainage basins in the southeastern United States and are the basis of comparison for the topological iuh's. Elements in the sets of basin characteristics for the topological iuh's are the number of first-order streams only, (N), or the nuber of sources together with the number of channel links in the topological diameter (N, D); the hydraulic parameters are values of the celerity and diffusivity constant. Sensitivity analyses indicate that the mean celerity of the internal links in the network is the critical hydraulic parameter for determining the shape of the topological iuh, while the diffusivity constant has minimal effect on the topological iuh. Asymptotic results (source-only) indicate the number of sources need not be large to approximate the topological iuh with the Weibull probability density function.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR021i011p01693","usgsCitation":"Karlinger, M., and Troutman, B., 1985, Assessment of the instantaneous unit hydrograph derived from the theory of topologically random networks: Water Resources Research, v. 21, no. 11, p. 1693-1702, https://doi.org/10.1029/WR021i011p01693.","productDescription":"10 p. ","startPage":"1693","endPage":"1702","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338263,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"11","noUsgsAuthors":false,"publicationDate":"2008-01-08","publicationStatus":"PW","scienceBaseUri":"58d6303be4b05ec7991310ff","contributors":{"authors":[{"text":"Karlinger, M.R.","contributorId":95039,"corporation":false,"usgs":true,"family":"Karlinger","given":"M.R.","affiliations":[],"preferred":false,"id":686050,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Troutman, B.M.","contributorId":73638,"corporation":false,"usgs":true,"family":"Troutman","given":"B.M.","email":"","affiliations":[],"preferred":false,"id":686051,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70185588,"text":"70185588 - 1985 - Field determination of the three-dimensional hydraulic conductivity tensor of anisotropic media: 1. Theory","interactions":[],"lastModifiedDate":"2020-01-19T11:11:34","indexId":"70185588","displayToPublicDate":"1985-11-01T00:00:00","publicationYear":"1985","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":"Field determination of the three-dimensional hydraulic conductivity tensor of anisotropic media: 1. Theory","docAbstract":"

A field method is proposed for determining the three-dimensional hydraulic conductivity tensor and specific storage of an anisotropic porous or fractured medium. The method, known as cross-hole testing (to distinguish it from conventional single-hole packer tests), consists of injecting fluid into (or withdrawing fluid from) packed-off intervals in a number of boreholes and monitoring the transient head response in similar intervals in neighboring boreholes. The directions of the principal hydraulic conductivities need not be known prior to the test, and the boreholes may have arbitrary orientations (e.g., they can all be vertical). An important aspect of the proposed method is that it provides direct field information on whether it is proper to regard the medium as being uniform and anisotropic on the scale of the test. The first paper presents theoretical expressions describing transient and steady state head response in monitoring intervals of arbitrary lengths and orientations, to constant-rate injection into (or withdrawal from) intervals having similar or different lengths and orientations. The conditions under which these intervals can be treated mathematically as points are investigated by an asymptotic analysis. The effect of planar no-flow and constant-head boundaries on the response is analyzed by the theory of images. The second paper describes the field methodology and shows how the proposed approach works in the case of fractured granitic rocks.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR021i011p01655","usgsCitation":"Hsieh, P.A., and Neuman, S.P., 1985, Field determination of the three-dimensional hydraulic conductivity tensor of anisotropic media: 1. Theory: Water Resources Research, v. 21, no. 1, p. 1655-1665, https://doi.org/10.1029/WR021i011p01655.","productDescription":"11 p. ","startPage":"1655","endPage":"1665","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338261,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"1","noUsgsAuthors":false,"publicationDate":"2008-01-08","publicationStatus":"PW","scienceBaseUri":"58d6303be4b05ec799131101","contributors":{"authors":[{"text":"Hsieh, Paul A. 0000-0003-4873-4874 pahsieh@usgs.gov","orcid":"https://orcid.org/0000-0003-4873-4874","contributorId":1634,"corporation":false,"usgs":true,"family":"Hsieh","given":"Paul","email":"pahsieh@usgs.gov","middleInitial":"A.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":39113,"text":"WMA - Office of Quality Assurance","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":686040,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neuman, Shlomo P.","contributorId":189795,"corporation":false,"usgs":false,"family":"Neuman","given":"Shlomo","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":686041,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70185594,"text":"70185594 - 1985 - Comment on “Evaluation of slug tests in wells containing a finite-thickness skin” by C. R. Faust and J. W. Mercer","interactions":[],"lastModifiedDate":"2020-01-19T10:36:06","indexId":"70185594","displayToPublicDate":"1985-09-01T00:00:00","publicationYear":"1985","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":"Comment on “Evaluation of slug tests in wells containing a finite-thickness skin” by C. R. Faust and J. W. Mercer","docAbstract":"

No abstract available.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR021i009p01459","usgsCitation":"Moench, A.F., and Hsieh, P.A., 1985, Comment on “Evaluation of slug tests in wells containing a finite-thickness skin” by C. R. Faust and J. W. Mercer: Water Resources Research, v. 21, no. 9, p. 1459-1461, https://doi.org/10.1029/WR021i009p01459.","productDescription":"3 p. ","startPage":"1459","endPage":"1461","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":480160,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/wr021i009p01459","text":"Publisher Index Page"},{"id":338276,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"9","noUsgsAuthors":false,"publicationDate":"2008-01-08","publicationStatus":"PW","scienceBaseUri":"58d6303be4b05ec799131103","contributors":{"authors":[{"text":"Moench, Allen F. afmoench@usgs.gov","contributorId":3903,"corporation":false,"usgs":true,"family":"Moench","given":"Allen","email":"afmoench@usgs.gov","middleInitial":"F.","affiliations":[],"preferred":true,"id":686063,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hsieh, Paul A. 0000-0003-4873-4874 pahsieh@usgs.gov","orcid":"https://orcid.org/0000-0003-4873-4874","contributorId":1634,"corporation":false,"usgs":true,"family":"Hsieh","given":"Paul","email":"pahsieh@usgs.gov","middleInitial":"A.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":39113,"text":"WMA - Office of Quality Assurance","active":true,"usgs":true}],"preferred":true,"id":686064,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70186162,"text":"70186162 - 1985 - Biogeochemistry of aquatic humic substances in Thoreau's Bog, Concord, Massachusetts","interactions":[],"lastModifiedDate":"2020-01-19T11:44:48","indexId":"70186162","displayToPublicDate":"1985-08-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1465,"text":"Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Biogeochemistry of aquatic humic substances in Thoreau's Bog, Concord, Massachusetts","docAbstract":"

Thoreau's Bog is an ombrotrophic floating—mat Sphagnum bog developed in a glacial kettlehole and surrounded by a red maple swamp. Concentrations of dissolved organic carbon in the porewater of the bog average 36 mg/L and are greatest near the surface, especially during late summer. This distribution suggest that the upper layer of living and dead Sphagnum and moderately humified peat is the major site of dissolved organic material production in the bog. The dissolved organic material consists mainly of aquatic fulvic acid (67%) and hydrophilic acids (20%); these organic acids control the pH (typically 4 or somewhat lower) of the bogwater. The elemental, amino acid, carbohydrate, and carboxylic acid contents of fulvic acid from the bog are similar to those of aquatic fulvic acid from the nearby Shawsheen River, although the phenolic hydroxyl content of fulvic acid from Thoreau's Bog is higher. The hydrophilic acids have greater amino acid, carbohydrate, and carboxylic acid contents than the fulvic acid, consistent with the hypothesis that hydrophilic acids are more labile intermediate compounds in the formation of fulvic acid.

","language":"English","publisher":"Wiley","doi":"10.2307/1939187","usgsCitation":"McKnight, D.M., Thurman, E.M., Wershaw, R.L., and Hemond, H., 1985, Biogeochemistry of aquatic humic substances in Thoreau's Bog, Concord, Massachusetts: Ecology, v. 66, no. 4, https://doi.org/10.2307/1939187.","productDescription":"14 p. ","endPage":"1339","numberOfPages":"1352","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338823,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachusetts","city":"Concord ","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.37353897094727,\n 42.44537470235299\n ],\n [\n -71.31912231445312,\n 42.44537470235299\n ],\n [\n -71.31912231445312,\n 42.47475584135045\n ],\n [\n -71.37353897094727,\n 42.47475584135045\n ],\n [\n -71.37353897094727,\n 42.44537470235299\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"66","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58de1954e4b02ff32c699cd7","contributors":{"authors":[{"text":"McKnight, Diane M.","contributorId":59773,"corporation":false,"usgs":false,"family":"McKnight","given":"Diane","email":"","middleInitial":"M.","affiliations":[{"id":16833,"text":"INSTAAR, University of Colorado","active":true,"usgs":false}],"preferred":false,"id":687717,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thurman, E. Michael","contributorId":9636,"corporation":false,"usgs":true,"family":"Thurman","given":"E.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":687718,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wershaw, Robert L. rwershaw@usgs.gov","contributorId":4856,"corporation":false,"usgs":true,"family":"Wershaw","given":"Robert","email":"rwershaw@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":687719,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hemond, Herold","contributorId":190186,"corporation":false,"usgs":false,"family":"Hemond","given":"Herold","email":"","affiliations":[],"preferred":false,"id":687720,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70231501,"text":"70231501 - 1985 - Assessment and monitoring of sedimentation in the Aswan High Dam Reservoir using Landsat imagery","interactions":[],"lastModifiedDate":"2022-05-11T17:03:42.23185","indexId":"70231501","displayToPublicDate":"1985-07-11T11:31:40","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Assessment and monitoring of sedimentation in the Aswan High Dam Reservoir using Landsat imagery","docAbstract":"

No abstract available.

","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Hydrological applications of remote sensing and remote data transmission","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"1983 Hamburg Symposium","conferenceDate":"1983","conferenceLocation":"Hamburg, Germany","language":"English","publisher":"International Association of Hydrological Sciences","usgsCitation":"Smith, S., Mancy, K.H., Latif, A.F., and Fosnight, E.A., 1985, Assessment and monitoring of sedimentation in the Aswan High Dam Reservoir using Landsat imagery, in Hydrological applications of remote sensing and remote data transmission, v. 145, Hamburg, Germany, 1983, p. 499-508.","productDescription":"10 p.","startPage":"499","endPage":"508","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) 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E.","contributorId":291582,"corporation":false,"usgs":false,"family":"Smith","given":"S. E.","affiliations":[],"preferred":false,"id":842793,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mancy, K. H.","contributorId":14344,"corporation":false,"usgs":true,"family":"Mancy","given":"K.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":842794,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Latif, A. F. A.","contributorId":291583,"corporation":false,"usgs":false,"family":"Latif","given":"A.","email":"","middleInitial":"F. A.","affiliations":[],"preferred":false,"id":842795,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fosnight, Eugene A. 0000-0002-8557-3697 fosnight@usgs.gov","orcid":"https://orcid.org/0000-0002-8557-3697","contributorId":2961,"corporation":false,"usgs":true,"family":"Fosnight","given":"Eugene","email":"fosnight@usgs.gov","middleInitial":"A.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":842796,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70185595,"text":"70185595 - 1985 - Comment on \"Possible effects of erosional changes of the topographic relief on pore pressure at depth\" by J. Tóth and R.F. Millar","interactions":[],"lastModifiedDate":"2018-02-12T17:54:58","indexId":"70185595","displayToPublicDate":"1985-06-01T00:00:00","publicationYear":"1985","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":"Comment on \"Possible effects of erosional changes of the topographic relief on pore pressure at depth\" by J. Tóth and R.F. Millar","docAbstract":"

No abstract available.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR021i006p00895","usgsCitation":"Neuzil, C., 1985, Comment on \"Possible effects of erosional changes of the topographic relief on pore pressure at depth\" by J. Tóth and R.F. Millar: Water Resources Research, v. 21, no. 6, p. 895-898, https://doi.org/10.1029/WR021i006p00895.","productDescription":"4 p. ","startPage":"895","endPage":"898","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":480163,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/wr021i006p00895","text":"Publisher Index Page"},{"id":338281,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"6","noUsgsAuthors":false,"publicationDate":"2008-01-08","publicationStatus":"PW","scienceBaseUri":"58d6303ce4b05ec799131105","contributors":{"authors":[{"text":"Neuzil, C. E. 0000-0003-2022-4055","orcid":"https://orcid.org/0000-0003-2022-4055","contributorId":81078,"corporation":false,"usgs":true,"family":"Neuzil","given":"C. E.","affiliations":[],"preferred":false,"id":686067,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70012377,"text":"70012377 - 1985 - Bottomland vegetation distribution along Passage Creek, Virginia, in relation to fluvial landforms","interactions":[],"lastModifiedDate":"2023-12-18T17:13:31.420301","indexId":"70012377","displayToPublicDate":"1985-06-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1465,"text":"Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Bottomland vegetation distribution along Passage Creek, Virginia, in relation to fluvial landforms","docAbstract":"

Persistent distribution patterns of woody vegetation within the bottomland forest of Passage Creek, Virginia, were related to fluvial landforms, channel geometry, streamflow characteristics, and sediment—size characteristics. Vegetation patterns were determined from species presence as observed in transects and traverses on landforms developed along the stream. Distinct species distributional patterns were found on four common fluvial geomorphic landforms: depositional bar, active—channel shelf, floodplain, and terrace. Independent hydrologic characteristics (flow duration and flood frequency) were determined for each of the landforms. Vegetation data were analyzed by binary discriminant analysis, principal components analysis, and detrended correspondence analysis. Results and related field observations suggest that certain species are significantly associated with specific fluvial landforms. Vegetation patterns appear to develop more as a result of hydrologic processes associated with each fluvial landform rather than from sediment—size characteristics. Flood disturbance may be an important factor in maintaining the vegetation patterns, which may therefore be used as indicators for particular hydrogeomorphic site conditions.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.2307/1940528","usgsCitation":"Hupp, C.R., and Osterkamp, W.R., 1985, Bottomland vegetation distribution along Passage Creek, Virginia, in relation to fluvial landforms: Ecology, v. 66, no. 3, p. 670-681, https://doi.org/10.2307/1940528.","productDescription":"12 p.","startPage":"670","endPage":"681","numberOfPages":"12","costCenters":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"links":[{"id":222303,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"66","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f22fe4b0c8380cd4b063","contributors":{"authors":[{"text":"Hupp, Cliff R. 0000-0003-1853-9197 crhupp@usgs.gov","orcid":"https://orcid.org/0000-0003-1853-9197","contributorId":2344,"corporation":false,"usgs":true,"family":"Hupp","given":"Cliff","email":"crhupp@usgs.gov","middleInitial":"R.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":363409,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Osterkamp, W. R.","contributorId":46044,"corporation":false,"usgs":true,"family":"Osterkamp","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":363408,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70121027,"text":"70121027 - 1985 - Evolution and application of instream flow methodologies to small hydropower developments: an overview of the issues","interactions":[],"lastModifiedDate":"2014-08-19T09:50:54","indexId":"70121027","displayToPublicDate":"1985-05-01T09:49:37","publicationYear":"1985","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":12,"text":"Conference publication"},"title":"Evolution and application of instream flow methodologies to small hydropower developments: an overview of the issues","docAbstract":"ethods for evaluating instream flow needs have evolved over the last 30 years resulting in two categories which are defined as “standard-setting” and “incremental”. Standard-setting methodologies refer to those measurement and interpretative techniques designed to generate a flow value(s) which is intended to maintain the fishery at some acceptable level. Incremental methodologies on the other hand are organized and repeatable processes by which: (1) a fishery habitat/streamflow relationship and the hydrology of the stream are transformed into a baseline habitat time series; (2) proposed water management alternatives are quantified and compared with the baseline; and (3) project operating rules are negotiated. A hierarchical approach to small-hydro instream flow analysis is suggested.","largerWorkTitle":"Symposium on Small Hydro/Fisheries Symposium","conferenceTitle":"Small Hydro/Fisheries Symposium","conferenceDate":"1985-05-01T00:00:00","conferenceLocation":"Denver, CO","language":"English","publisher":"American Fisheries Society","publisherLocation":"Bethesda, MD","usgsCitation":"Trihey, E.W., and Stalnaker, C., 1985, Evolution and application of instream flow methodologies to small hydropower developments: an overview of the issues, 8 p.","productDescription":"8 p.","numberOfPages":"8","costCenters":[],"links":[{"id":292511,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f464cae4b073ff773a7d08","contributors":{"authors":[{"text":"Trihey, E. Woody","contributorId":54121,"corporation":false,"usgs":true,"family":"Trihey","given":"E.","email":"","middleInitial":"Woody","affiliations":[],"preferred":false,"id":498688,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stalnaker, Clair B.","contributorId":30871,"corporation":false,"usgs":true,"family":"Stalnaker","given":"Clair B.","affiliations":[],"preferred":false,"id":498687,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70186160,"text":"70186160 - 1985 - The aqueous photolysis of ethylene glycol adsorbed on geothite","interactions":[],"lastModifiedDate":"2020-01-19T11:08:41","indexId":"70186160","displayToPublicDate":"1985-04-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3049,"text":"Photochemistry and Photobiology","active":true,"publicationSubtype":{"id":10}},"title":"The aqueous photolysis of ethylene glycol adsorbed on geothite","docAbstract":"

Suspensions of goethite (α-FeOOH) were photolyzed in aerated ethylene glycol-water solutions at pH 6.5, with ultraviolet light in the wavelength range300–400 nm. Under these conditions, formaldehyde and glycolaldehyde were detected as photoproducts. Quantum yields of formaldehyde production ranged from 1.9 7times; 10-5 to 2.9 × 10-4 over the ethylene glycol concentration range of 0.002-2.0 mol/ℓ, and gave evidence that the reaction occurred at the goethite surface. Quantum yields of glycolaldehyde were 20% less than those of formaldehyde, and displayed a concentration-dependent relationship with ethylene glycol similar to that of formaldehyde. Immediately after photolysis, Fe2+ was measured to be 4.6 × 10-7 mol/ℓ in an aerated suspension containing 1.3 mol/ℓ ethylene glycol, and 8.5 × 10-6 mol/ℓ in the corresponding deoxygenated suspension. Glycolaldehyde was not generated in the deoxygenated suspensions. These results are consistent with a mechanism involving the transfer of an electron from an adsorbed ethylene glycol molecule to an excited state of Fe3+ (Iron[III]) in the goethite lattice, to produce Fe2+ and an organic cation. In a series of reactions involving O2, FeOOH, and Fe2+, the organic cation decomposes to form formaldehyde and the intermediate radicals “OH and” CH2OH. OH reacts further with ethylene glycol in the presence of O2to yield glycolaldehyde. Aqueous photolysis of ethylene glycol sorbed onto goethite is typical of reactions that can occur in the aquatic environment.

","language":"English","publisher":"Wiley","doi":"10.1111/j.1751-1097.1985.tb03505.x","usgsCitation":"Cunningham, K.M., Goldberg, M.C., and Weiner, E., 1985, The aqueous photolysis of ethylene glycol adsorbed on geothite: Photochemistry and Photobiology, v. 41, no. 4, p. 409-416, https://doi.org/10.1111/j.1751-1097.1985.tb03505.x.","productDescription":"8 p. ","startPage":"409","endPage":"416","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338811,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"41","issue":"4","noUsgsAuthors":false,"publicationDate":"2008-01-02","publicationStatus":"PW","scienceBaseUri":"58de1954e4b02ff32c699cd9","contributors":{"authors":[{"text":"Cunningham, Kirkwood M.","contributorId":85325,"corporation":false,"usgs":true,"family":"Cunningham","given":"Kirkwood","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":687705,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goldberg, Marvin C.","contributorId":26066,"corporation":false,"usgs":true,"family":"Goldberg","given":"Marvin","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":687706,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weiner, E.R.","contributorId":190183,"corporation":false,"usgs":false,"family":"Weiner","given":"E.R.","email":"","affiliations":[],"preferred":false,"id":687707,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70185591,"text":"70185591 - 1985 - Effects of copper on production of periphyton, nitrogen fixation and processing of leaf litter in a Sierra Nevada, California, stream","interactions":[],"lastModifiedDate":"2020-01-19T10:58:07","indexId":"70185591","displayToPublicDate":"1985-04-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1696,"text":"Freshwater Biology","active":true,"publicationSubtype":{"id":10}},"title":"Effects of copper on production of periphyton, nitrogen fixation and processing of leaf litter in a Sierra Nevada, California, stream","docAbstract":"","language":"English","publisher":"Wiley","doi":"10.1111/j.1365-2427.1985.tb00189.x","usgsCitation":"Leland, H.V., and Carter, J.L., 1985, Effects of copper on production of periphyton, nitrogen fixation and processing of leaf litter in a Sierra Nevada, California, stream: Freshwater Biology, v. 15, no. 2, p. 155-173, https://doi.org/10.1111/j.1365-2427.1985.tb00189.x.","productDescription":"19 p. ","startPage":"155","endPage":"173","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338270,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Convict Creek ","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -118.84855270385742,\n 37.59444376462195\n ],\n [\n -118.8416004180908,\n 37.60750012497884\n ],\n [\n -118.81662368774413,\n 37.61776679867661\n ],\n [\n -118.80246162414551,\n 37.61701894316063\n ],\n [\n -118.79164695739745,\n 37.6081800809684\n ],\n [\n -118.78546714782715,\n 37.61586315165877\n ],\n [\n -118.79593849182129,\n 37.62286561307131\n ],\n [\n -118.81430625915527,\n 37.62483706088789\n ],\n [\n -118.83130073547365,\n 37.61994233558931\n ],\n [\n -118.84855270385742,\n 37.615659186587635\n ],\n [\n -118.85378837585449,\n 37.60716014465307\n ],\n [\n -118.8523292541504,\n 37.596143941292326\n ],\n [\n -118.84855270385742,\n 37.59444376462195\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"15","issue":"2","noUsgsAuthors":false,"publicationDate":"2006-05-29","publicationStatus":"PW","scienceBaseUri":"58d6303ce4b05ec799131107","contributors":{"authors":[{"text":"Leland, Harry V.","contributorId":51158,"corporation":false,"usgs":true,"family":"Leland","given":"Harry","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":686052,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carter, James L. 0000-0002-0104-9776 jlcarter@usgs.gov","orcid":"https://orcid.org/0000-0002-0104-9776","contributorId":3278,"corporation":false,"usgs":true,"family":"Carter","given":"James","email":"jlcarter@usgs.gov","middleInitial":"L.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":686053,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70012178,"text":"70012178 - 1985 - Uranium-series dating of sediments from Searles Lake: Differences between continental and marine climate records","interactions":[],"lastModifiedDate":"2025-09-29T16:37:09.211605","indexId":"70012178","displayToPublicDate":"1985-03-08T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Uranium-series dating of sediments from Searles Lake: Differences between continental and marine climate records","docAbstract":"

One of the major unresolved questions in Pleistocene paleoclimatology has been whether continental climatic transitions are consistent with the glacial δ18O marine record. Searles Lake in California, now a dry salt pan, is underlain by sediment layers deposited in a succession of lakes whose levels and salinities have fluctuated in response to changes in climate over the last 3 × 106 years. Uranium-series dates on the salt beds range from 35 × 103 to 231 × 103 years. This range of dates allows identification of lake-sediment horizons that are time correlatives of the boundaries of marine isotope stages from the recent 3/4 boundary back to the 8/9 boundary. The 5/6 boundary coincided with a deepening of the lake, but the analogous 1/2 boundary coincided with desiccation. The 3/4, 4/5, 6/7, 7/8, and 8/9 boundaries correspond in age to horizons that record little or no change in sedimentation or climate. These hydrologic results demonstrate that the continental paleoclimate record at this mid-latitude site does not mimic the marine record.

","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.227.4691.1222","issn":"00368075","usgsCitation":"Bischoff, J.L., Rosenbauer, R.J., and Smith, G.I., 1985, Uranium-series dating of sediments from Searles Lake: Differences between continental and marine climate records: Science, v. 227, no. 4691, p. 1222-1224, https://doi.org/10.1126/science.227.4691.1222.","productDescription":"3 p.","startPage":"1222","endPage":"1224","costCenters":[],"links":[{"id":221933,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Searles Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -117.40087461036393,\n 35.79349271401435\n ],\n [\n -117.40087461036393,\n 35.6452953903202\n ],\n [\n -117.23120813918258,\n 35.6452953903202\n ],\n [\n -117.23120813918258,\n 35.79349271401435\n ],\n [\n -117.40087461036393,\n 35.79349271401435\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"227","issue":"4691","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbdfee4b08c986b329350","contributors":{"authors":[{"text":"Bischoff, James L. jbischoff@usgs.gov","contributorId":1389,"corporation":false,"usgs":true,"family":"Bischoff","given":"James","email":"jbischoff@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":362931,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosenbauer, Robert J. brosenbauer@usgs.gov","contributorId":204,"corporation":false,"usgs":true,"family":"Rosenbauer","given":"Robert","email":"brosenbauer@usgs.gov","middleInitial":"J.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":362932,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, George I.","contributorId":92637,"corporation":false,"usgs":true,"family":"Smith","given":"George","email":"","middleInitial":"I.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":362933,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70120936,"text":"70120936 - 1985 - Effects of flood control alternatives on fish and wildlife resources of the Malheur-Harney lakes basin","interactions":[],"lastModifiedDate":"2014-08-18T14:26:41","indexId":"70120936","displayToPublicDate":"1985-03-01T14:15:31","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesNumber":"WELUT-85/W06","title":"Effects of flood control alternatives on fish and wildlife resources of the Malheur-Harney lakes basin","docAbstract":"

Malheur Lake is the largest freshwater marsh in the western contiguous United States and is one of the main management units of the Malheur National Wildlife Refuge in southeastern Oregon. The marsh provides excellent waterfowl production habitat as well as vital migration habitats for birds in the Pacific flyway. Water shortages have typically been a problem in this semiarid area; however, record snowfalls and cool summers have recently caused Malheur Lake to rise to its highest level in recorded history. This has resulted in the loss of approximately 57,000 acres of important wildlife habitat as well as extensive flooding of local ranches, roads, and railroad lines. Because of the importance of the Refuge, any water management plan for the Malheur-Harney Lakes Basin needs to consider the impact of management alternatives on the hydrology of Malheur Lake.

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\n

The facilitated modeling workshop described in this report was conducted January 14-18, 1985, under the joint sponsorship of the Portland Ecological Services Field Office and the Malheur National Wildlife Refuge, Region 1, U.S. Fish and Wildlife Service (FWS). The Portland Field Office is responsible for FWS reporting requirements on Federal water resource projects while the Refuge staff has management responsibility for much of the land affected by high water levels in the Malheur-Harney Lakes Basin. The primary objective of the workshop was to begin gathering and analyzing information concerning potential fish and wildlife impacts, needs, and opportunities associated with proposed U.S. Army Corps of Engineers (COE) flood control alternatives for Malheur Lake. The workshop was structured around the formulation of a computer model that would simulate the hydrologic effects of the various alternatives and any concommitant changes in vegetation communities and wildlife use patterns.

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\n

The simulation model is composed of three connected submodels. The Hydrology submodel calculates changes in lake volume, elevation, and surface area, as well as changes in water quality, that result from the proposed water management projects (upstream storage, upstream diversions, drainage canals) and the no action alternative. The Vegetation submodel determines associated changes in the areal extent of wetland and upland vegetation communities. Finally, the Wildlife submodel calculates indices of abundance or habitat suitability for colonial nesting birds (great egret, double-crested cormorant, white-faced ibis), greater sandhill crane, diving ducks, tundra swan, dabbling ducks, and Canada goose based on hydrologic and vegetation conditions. The model represents the Malheur-Harney Lakes Basin, but provides water quantity and quality indicators associated with additional flows that might occur in the Malheur River Basin. Several management scenarios, representing various flood control alternatives and assumptions concerning future runoff, were run to analyze model behavior. Scenario results are not intended as an analysis of all potential management actions or assumptions concerning future runoff. Rather, they demonstrate the type of analysis that could be conducted if the model was sufficiently refined and tested.

\n
\n

Early in a model development project, the process of building the model is usually of greater benefit than the model itself. The model building process stimulates interaction among agencies, assists in integrating existing information, and helps identify research needs. These benefits usually accrue even in the absence of real predictive power in the resulting model. This workshop initiated interaction among the primary State and Federal resource and development agencies in a nonadversarial forum. The exchange of information and expertise among agencies provided the FWS with the best information currently available for use in the Planning Aid Letter it will develop at the Reconnaissance state of the COE study. If the COE subsequently initiates a Feasability Study, this information will be refined further and will aid the FWS in preparing its Coordination Act Report on any flood control alternative proposed by the COE.

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\n

The model building and testing process also helped identify model limitations and more general information needs that should be evaluated for further study prior to preparation of an FWS Coordination Act Report. Major needs associated with the Hydrology submodel include a more detailed representation of hydrologic units (separately consider Harney Lake, Mud Lake, and Malheur Lake or the three hydrological units within Malheur Lake, rather than a combined lake system) and explicitly representation of groundwater storage and discharge in water budget calculations. A better representation of the hydrological units will require more detailed topographic data for the basin, capacity-elevation and elevation-surface area curves for each unit, and better water flow data between the units. Additional water quality parameters and constraints on proposed canal operation due to conditions in the Malheur River might also be added. Key Vegetation submodel needs include fine-tuning existing vegetation relationships in the model and adding relationships to address the influence of historical conditions on vegetation development, effects of very rapid changes in lake level, effects of wildlife populations (e.g., carp, muskrat), responses of vegetation to habitat management actions (e.g, haying, grazing, burning), and better representation of sago pondweed dynamics. A complementary geographic information system might also be developed for spatial analyses. Major needs that should be evaluated for the Wildlife submodel include addition of other wildlife species that have important effects on habitat on the Refuge (e.g., carp, muskrat) and consideration of additional life-cycle requisites and controlling variable for species presently in the model. Some of these limitations could perhaps be overcome if historical data on habitat conditions were developed to use with historical data on wildlife populations.

","language":"English","publisher":"U.S. Fish and Wildlife Service, Western Energy and Land Use Team","publisherLocation":"Fort Collins, CO","usgsCitation":"Hamilton, D.B., Auble, G.T., Ellison, R.A., and Roelle, J.E., 1985, Effects of flood control alternatives on fish and wildlife resources of the Malheur-Harney lakes basin, 51 p.","productDescription":"51 p.","numberOfPages":"51","costCenters":[],"links":[{"id":292467,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"Malheur Lake","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.974578,43.253095 ], [ -118.974578,43.415232 ], [ -118.629841,43.415232 ], [ -118.629841,43.253095 ], [ -118.974578,43.253095 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f25fe1e4b033341871890d","contributors":{"authors":[{"text":"Hamilton, David B. hamiltond@usgs.gov","contributorId":193,"corporation":false,"usgs":true,"family":"Hamilton","given":"David","email":"hamiltond@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":498647,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Auble, Gregor T. 0000-0002-0843-2751 aubleg@usgs.gov","orcid":"https://orcid.org/0000-0002-0843-2751","contributorId":2187,"corporation":false,"usgs":true,"family":"Auble","given":"Gregor","email":"aubleg@usgs.gov","middleInitial":"T.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":498648,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ellison, Richard A.","contributorId":19087,"corporation":false,"usgs":true,"family":"Ellison","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":498650,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Roelle, James E. roelleb@usgs.gov","contributorId":2330,"corporation":false,"usgs":true,"family":"Roelle","given":"James","email":"roelleb@usgs.gov","middleInitial":"E.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":498649,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70185587,"text":"70185587 - 1985 - Sorption of lead onto two gram-negative marine bacteria in seawater","interactions":[],"lastModifiedDate":"2020-01-19T11:19:37","indexId":"70185587","displayToPublicDate":"1985-03-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2662,"text":"Marine Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Sorption of lead onto two gram-negative marine bacteria in seawater","docAbstract":"

Laboratory adsorption experiments performed at environmentally significant lead (Pb) and cell concentrations indicate that the marine bacteria examined have significant binding capacities for Pb. However, the behavior governing Pb sorption onto gram-negative bacteria in seawater may be quite complex. The sorption kinetics appear to involve two distinct phases, i.e., a rapid removal of Pb from solution within the first few minutes, followed by a slow but nearly constant removal over many hours. Also, the average binding coefficient, calculated for Pb sorption onto bacteria and a measure of binding intensity, increases with decreasing sorption density (amounts of bacteria-associated Pb per unit bacterial surface) at low cell concentrations (105 cells ml−1), but decreases with decreasing sorption density at higher cell concentrations (107 cells ml−1). The latter effect is apparently due to the production of significant amounts of extra-cellular organics at high cell concentrations that compete directly with bacterial surfaces for available lead. Lead toxicity and active uptake by marine bacteria did not appear significant at the Pb concentrations used.

","language":"English","publisher":"Elsevier","doi":"10.1016/0304-4203(85)90044-1","usgsCitation":"Harvey, R.W., and Leckie, J.O., 1985, Sorption of lead onto two gram-negative marine bacteria in seawater: Marine Chemistry, v. 15, no. 4, p. 333-344, https://doi.org/10.1016/0304-4203(85)90044-1.","productDescription":"12 p. ","startPage":"333","endPage":"344","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338257,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d6303ce4b05ec799131109","contributors":{"authors":[{"text":"Harvey, Ronald W. 0000-0002-2791-8503 rwharvey@usgs.gov","orcid":"https://orcid.org/0000-0002-2791-8503","contributorId":564,"corporation":false,"usgs":true,"family":"Harvey","given":"Ronald","email":"rwharvey@usgs.gov","middleInitial":"W.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":686038,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leckie, James O.","contributorId":77297,"corporation":false,"usgs":true,"family":"Leckie","given":"James","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":686039,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}