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,{"id":40669,"text":"ofr80811H - 1983 - Distribution and abundance of gold and silver in non-magnetic and moderately magnetic heavy-mineral-concentrate and minus-80-mesh stream-sediment samples and silver in ash of aquatic-bryophyte samples, Medfra quadrangle, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:05:06","indexId":"ofr80811H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"80-811","chapter":"H","title":"Distribution and abundance of gold and silver in non-magnetic and moderately magnetic heavy-mineral-concentrate and minus-80-mesh stream-sediment samples and silver in ash of aquatic-bryophyte samples, Medfra quadrangle, Alaska","language":"ENGLISH","doi":"10.3133/ofr80811H","usgsCitation":"King, H.D., Cooley, E., Gruzensky, A., and Spiesman, D., 1983, Distribution and abundance of gold and silver in non-magnetic and moderately magnetic heavy-mineral-concentrate and minus-80-mesh stream-sediment samples and silver in ash of aquatic-bryophyte samples, Medfra quadrangle, Alaska: U.S. Geological Survey Open-File Report 80-811, 3 maps :photocopy ;45 x 61 cm., on sheet 84 x 91 cm. and smaller., https://doi.org/10.3133/ofr80811H.","productDescription":"3 maps :photocopy ;45 x 61 cm., on sheet 84 x 91 cm. and smaller.","costCenters":[],"links":[{"id":136671,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":77943,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0811h/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":77944,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0811h/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":77945,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0811h/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a103","contributors":{"authors":[{"text":"King, H. D.","contributorId":89113,"corporation":false,"usgs":true,"family":"King","given":"H.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":223679,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooley, E.F.","contributorId":83072,"corporation":false,"usgs":true,"family":"Cooley","given":"E.F.","email":"","affiliations":[],"preferred":false,"id":223678,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gruzensky, A.L.","contributorId":98303,"corporation":false,"usgs":true,"family":"Gruzensky","given":"A.L.","email":"","affiliations":[],"preferred":false,"id":223680,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Spiesman, D. L. Jr.","contributorId":41022,"corporation":false,"usgs":true,"family":"Spiesman","given":"D. L.","suffix":"Jr.","affiliations":[],"preferred":false,"id":223677,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":10742,"text":"ofr83491 - 1983 - A microcomputer-based data acquisition and control system for the direct shear, ring shear, triaxial shear, and consolidation tests","interactions":[],"lastModifiedDate":"2012-02-02T00:06:24","indexId":"ofr83491","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-491","title":"A microcomputer-based data acquisition and control system for the direct shear, ring shear, triaxial shear, and consolidation tests","docAbstract":"This report is intended to provide internal documentation for the U.S. Geological Survey laboratory's automatic data acquisition system. The operating procedures for each type of test are designed to independently lead a first-time user through the various stages of using the computer to control the test. \r\n\r\nContinuing advances in computer technology and the availability of desktop microcomputers with a wide variety of peripheral equipment at a reasonable cost can create an efficient automated geotechnical testing environment. A geotechnical testing environment is shown in figure 1. Using an automatic data acquisition system, laboratory test data from a variety of sensors can be collected, and manually or automatically recorded on a magnetic device at the same apparent time. The responses of a test can be displayed graphically on a CRT in a matter of seconds, giving the investigator an opportunity to evaluate the test data, and to make timely, informed decisions on such matters as whether to continue testing, abandon a test, or modify procedures. Data can be retrieved and results reported in tabular form, or graphic plots, suitable for publication. \r\n\r\nThermistors, thermocouples, load cells, pressure transducers, and linear variable differential transformers are typical sensors which are incorporated in automated systems. The geotechnical tests which are most practical to automate are the long-term tests which often require readings to be recorded outside normal work hours and on weekends. Automation applications include incremental load consolidation tests, constant-rate-of-strain consolidation tests, direct shear tests, ring shear tests, and triaxial shear tests.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83491","usgsCitation":"Powers, P.S., 1983, A microcomputer-based data acquisition and control system for the direct shear, ring shear, triaxial shear, and consolidation tests: U.S. Geological Survey Open-File Report 83-491, vi, 88 p. ill. ;28 cm., https://doi.org/10.3133/ofr83491.","productDescription":"vi, 88 p. ill. ;28 cm.","costCenters":[],"links":[{"id":143347,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0491/report-thumb.jpg"},{"id":38548,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0491/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adff4","contributors":{"authors":[{"text":"Powers, Philip S.","contributorId":102078,"corporation":false,"usgs":true,"family":"Powers","given":"Philip","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":161888,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27762,"text":"wri834033 - 1983 - Ground-water-use trends in the Twin Cities metropolitan area, Minnesota, 1880-1980","interactions":[],"lastModifiedDate":"2018-03-12T12:01:11","indexId":"wri834033","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4033","title":"Ground-water-use trends in the Twin Cities metropolitan area, Minnesota, 1880-1980","docAbstract":"<p>Detailed ground-water-use information from 1880 to 1980 has been collected and analyzed for the Twin Cities metropolitan area. Interpretation of historic water-use data was required to help water-resource planners and managers assess future trends in water use. Data were also needed for three computer-simulation models of ground-water flow being developed in the Twin Cities area. Methods were developed to collect, evaluate, store, and retrieve information from all local, State, and Federal agencies1 records and publications. A computerized water-use data base was constructed to facilitate generation of statistics on water-use trends and to store and retrieve data for the flow models.</p>\n<p>Ground-water use was analyzed by use category and aquifer and several trends were observed. Eighty percent of ground water currently withdrawn is from wells in the Prairie du Chien-Jordan aquifer. Ground-water use increased from 1880 until the early 1970's, and then declined slightly in the late 1970's. Industrial use in particular declined during the 1970's as a result of conservation that was prompted by increased sewagetreatment and energy costs. The intensity of pumping has decreased within the St. Paul and Minneapolis city limits and increased outside the city limits. The seasonal variability of ground-water use became more pronounced as the percentage of water used for irrigation and air conditioning increased.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri834033","collaboration":"Prepared in cooperation with the Metropolitan Council of the Twin Cities and the Minnesota Department of Natural Resources","usgsCitation":"Horn, M., 1983, Ground-water-use trends in the Twin Cities metropolitan area, Minnesota, 1880-1980: U.S. Geological Survey Water-Resources Investigations Report 83-4033, iv, 37 p., https://doi.org/10.3133/wri834033.","productDescription":"iv, 37 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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M.A.","contributorId":92223,"corporation":false,"usgs":true,"family":"Horn","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":198655,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26693,"text":"wri834137 - 1983 - Computer program and data listing for two-dimensional ground-water model for Laramie County, Wyoming","interactions":[],"lastModifiedDate":"2017-09-20T16:33:22","indexId":"wri834137","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4137","title":"Computer program and data listing for two-dimensional ground-water model for Laramie County, Wyoming","docAbstract":"This is a supplement to the report, ' Effect of pumpage on ground-water levels as modeled in Laramie County, Wyoming, ' published as U.S. Geological Survey Water-Resources Investigations Open-File Report 80-1104. The computer program and data used to model ground-water conditions in post-Cretaceous rocks in Laramie County are listed. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834137","usgsCitation":"Crist, M.A., 1983, Computer program and data listing for two-dimensional ground-water model for Laramie County, Wyoming: U.S. Geological Survey Water-Resources Investigations Report 83-4137, iv, 137 p. ;28 cm., https://doi.org/10.3133/wri834137.","productDescription":"iv, 137 p. ;28 cm.","costCenters":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":121923,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4137/report-thumb.jpg"},{"id":55554,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4137/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d20","contributors":{"authors":[{"text":"Crist, M. A.","contributorId":84799,"corporation":false,"usgs":true,"family":"Crist","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":196842,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26696,"text":"wri834047 - 1983 - Hydrologic conditions in the Wheatland Flats area, Platte County, Wyoming","interactions":[],"lastModifiedDate":"2017-09-20T16:32:01","indexId":"wri834047","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4047","title":"Hydrologic conditions in the Wheatland Flats area, Platte County, Wyoming","docAbstract":"The area includes about 260 square miles in central Platte County that consists of Wheatland Flats and a border region. Wheatland Flats is an area of about 100 square miles that is bounded by Chugwater Creek on the east, the Laramie River on the north, and Sybille Creek on the west. The southern boundary is approximately the southernmost limit of alluvial terrace deposits. Surface water diverted from the Laramie River along with ground water from wells is used to irrigate about 57,000 acres most of which are on and adjacent to Wheatland Flats. More than 200 wells are used for irrigation, industrial, and municipal supplies. The wells are completed in an upper aquifer consisting primarily of shallow alluvial deposits of Quaternary age and a lower aquifer, the Arikaree Formation of early Miocene age. Net water-level decline after approximately 20 years (1958-60 to 1979) generally is less than 10 feet in each aquifer , although declines of as much as 13 feet have occurred in the Airkaree Formation at specific locations. A digital model was used to simulate hydrologic conditions in the Wheatland Flats area. The model indicated that ground-water discharge to streams decreased by 10 percent from 1971 to 1978. Stream-discharge measurements are not available to verify the loss. However, it is reasonable to assume, on the basis of hydraulic-head decline in the aquifers, that there has been some ground-water contribution to the stream. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834047","usgsCitation":"Crist, M.A., 1983, Hydrologic conditions in the Wheatland Flats area, Platte County, Wyoming: U.S. Geological Survey Water-Resources Investigations Report 83-4047, v, 41 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834047.","productDescription":"v, 41 p. :ill., maps ;28 cm.","costCenters":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":123554,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4047/report-thumb.jpg"},{"id":55562,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4047/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55563,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4047/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55564,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4047/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55565,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4047/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db6113ae","contributors":{"authors":[{"text":"Crist, M. A.","contributorId":84799,"corporation":false,"usgs":true,"family":"Crist","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":196845,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30562,"text":"wri824089 - 1983 - Hydrogeology of the Sarasota-Port Charlotte area, Florida","interactions":[],"lastModifiedDate":"2023-01-04T20:59:48.947233","indexId":"wri824089","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-4089","title":"Hydrogeology of the Sarasota-Port Charlotte area, Florida","docAbstract":"<p>The surficial and intermediate aquifers are the major source of public water supplies in the Sarasota-Port Charlotte, Florida, area because of the relatively poor quality of Floridan aquifer water. The hydrogeologic framework consists of the surficial aquifer, intermediate aquifers (Tamiami-upper Hawthorn and lower Hawthorn-upper Tampa aquifers) and confining beds, Floridan aquifer, and lower confining bed (or base of the Floridan aquifer). The quality of ground water in the surficial and intermediate aquifers is generally good, except in the western (coastal) and southern parts where saltwater intrusion or incomplete flushing of connate water has occurred. The mineral content of ground water generally increases with depth and areally from the northeast towards the west and south. A water budget for the study area shows that an average annual rainfall of 51.0 inches minus an evapotranspiration of 38.0 inches per year and streamflow of 12.5 inches per year leaves 0.5 inch per year of recharge to the surficial aquifer. Combined pumpage from the aquifers is 1.06 inches per year. A preliminary quasi-time dimensional model has been applied to the study area to check the reasonableness of the hydrogeologic framework defined and of aquifer parameters. The model was considered calibrated when the final head matrix was within plus or minus 5 feet of the starting head.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824089","usgsCitation":"Wolansky, R., 1983, Hydrogeology of the Sarasota-Port Charlotte area, Florida: U.S. Geological Survey Water-Resources Investigations Report 82-4089, vi, 48 p., https://doi.org/10.3133/wri824089.","productDescription":"vi, 48 p.","costCenters":[],"links":[{"id":411383,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35600.htm","linkFileType":{"id":5,"text":"html"}},{"id":59327,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4089/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123470,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4089/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Sarasota-Port Charlotte area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.55,\n              27.383\n            ],\n            [\n              -82.55,\n              26.75\n            ],\n            [\n              -81.667,\n              26.75\n            ],\n            [\n              -81.667,\n              27.383\n            ],\n            [\n              -82.55,\n              27.383\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc39a","contributors":{"authors":[{"text":"Wolansky, R. M.","contributorId":89163,"corporation":false,"usgs":true,"family":"Wolansky","given":"R. M.","affiliations":[],"preferred":false,"id":203459,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28900,"text":"wri7881 - 1983 - Meteorological, water-temperature, and discharge data for the Mattole River basin, Humboldt County, California","interactions":[],"lastModifiedDate":"2020-05-26T22:05:42.300638","indexId":"wri7881","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"78-81","title":"Meteorological, water-temperature, and discharge data for the Mattole River basin, Humboldt County, California","docAbstract":"To overcome a major difficulty in the testing of the validity of river-temperature models - the lack of adequate precise synoptic data for an entire river basin - synoptic meteorologic, water-temperature, and discharge data were obtained in the Mattole River Basin in northern California during the period June 10 through August 31, 1975. The variables monitored were water temperature in the main channel and major tributaries, wind velocity, wet-bulb and dry-bulb air temperature, total hemispherical incoming radiation, total incoming shortwave radiation, discharge in the main channel and major tributaries, and average velocity and axial dispersion coefficients in the main channel. This report describes the experimental design and the instrumentation and procedures followed to insure the best possible information, and it presents a detailed set of data which can be used in testing river-temperature models. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7881","usgsCitation":"Noble, R., and Jackman, A.P., 1983, Meteorological, water-temperature, and discharge data for the Mattole River basin, Humboldt County, California: U.S. Geological Survey Water-Resources Investigations Report 78-81, vi, 32 p., https://doi.org/10.3133/wri7881.","productDescription":"vi, 32 p.","costCenters":[],"links":[{"id":159136,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0081/report-thumb.jpg"},{"id":375041,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0081/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Humboldt County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.65087890624999,\n              40.42813291388417\n            ],\n            [\n              -124.26910400390625,\n              39.79376521264885\n            ],\n            [\n              -123.43688964843749,\n              39.79376521264885\n            ],\n            [\n              -123.43688964843749,\n              41.126952506008436\n            ],\n            [\n              -124.26910400390625,\n              41.126952506008436\n            ],\n            [\n              -124.65087890624999,\n              40.42813291388417\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629845","contributors":{"authors":[{"text":"Noble, R.D.","contributorId":76363,"corporation":false,"usgs":true,"family":"Noble","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":200585,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jackman, Alan P.","contributorId":28239,"corporation":false,"usgs":true,"family":"Jackman","given":"Alan","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":200584,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29754,"text":"wri834202 - 1983 - Hydrology of an abandoned coal-mining area near McCurtain, Haskell County, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri834202","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4202","title":"Hydrology of an abandoned coal-mining area near McCurtain, Haskell County, Oklahoma","docAbstract":"Water quality was investigated from October 1980 to May 1983 in an area of abandoned coal mines in Haskell county, Oklahoma. Bedrock in the area is shale, siltstone, sandstone, and the McAlester (Stigler) and Hartshorne coals of the McAlester Formation and Hartshorne Sandstone of Pennsylvanian age. The two coal beds, upper and lower Hartshorne, associated with the Hartshorne Sandstone converge or are separated by a few feet or less of bony coal or shale in the McCurtain area. Many small faults cut the Hartshorne coal in all the McCurtain-area mines. The main avenues of water entry to and movement through the bedrock are the exposed bedding-plane openings between layers of sandstone, partings between laminae of shale, fractures and joints developed during folding and faulting laminae of shale, fractures and joints developed during folding and faulting of the brittle rocks, and openings caused by surface mining--the overburden being shattered and broken to form spoil. Water-table conditions exist in bedrock and spoil in the area. Mine pond water is in direct hydraulic connections with water in the spoil piles and the underlying Hartshorne Sandstone.\r\nSulfate is the best indicator of the presence of coal-mine drainage in both surface and ground water in the Oklahoma coal field. Median sulfate concentrations for four sites on Mule Creek ranged from 26 to 260 milligrams per liter. Median sulfate concentrations increased with increased drainage from unreclaimed mined areas. The median sulfate concentration in Mule Creek where it drains the reclaimed area is less than one-third of that at the next site downstream where the stream begins to drain abandoned (unreclaimed) mine lands.\r\n\r\nWater from Mule Creek predominantly is a sodium sulfate type. Maximum and median values for specific conductance and concentrations of calcium, magnesium, sodium, sulfate, chloride, dissolved solids, and alkalinity increase as Mule Creek flows downstream and drains increasing areas of abandoned (unreclaimed) mining lands. Constituent concentrations in Mule Creek, except those for dissolved solids, iron, manganese, and sulfate, generally do not exceed drinking-water limits. Reclamation likely would result in decreased concentrations of dissolved solids, calcium, magnesium, sodium, sulfate, and alkalinity in Mule Creek in the vicinity of the reclaimed area.\r\n\r\nGround water in the area is moderately hard to very hard alkaline water with a median pH of 7.2 to 7.6. It predominately is a sodium sulfate type and, except for dissolved solids, iron manganese, and sulfate, constituent concentrations generally do not exceed drinking-water limits. Ground-water quality would likely be unchanged by reclamation.\r\n\r\nThe quality of water in the two mine ponds is quite similar to that of the shallow ground water in the area. Constituents in water from both ponds generally do not exceed drinking-water limits and the water quality is unlikely to be changed by reclamation in the area.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834202","usgsCitation":"Slack, L.J., 1983, Hydrology of an abandoned coal-mining area near McCurtain, Haskell County, Oklahoma: U.S. Geological Survey Water-Resources Investigations Report 83-4202, v, 117 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834202.","productDescription":"v, 117 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124782,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4202/report-thumb.jpg"},{"id":58548,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4202/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58549,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4202/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dee4b07f02db5e2ef3","contributors":{"authors":[{"text":"Slack, L. J.","contributorId":44157,"corporation":false,"usgs":true,"family":"Slack","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":202062,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27732,"text":"wri834179 - 1983 - Three-dimensional digital-computer model of the principal ground-water reservoir of the Sevier Desert, Utah","interactions":[],"lastModifiedDate":"2022-12-09T21:40:24.164154","indexId":"wri834179","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4179","title":"Three-dimensional digital-computer model of the principal ground-water reservoir of the Sevier Desert, Utah","docAbstract":"<p>The principal ground-water reservoir in part of the Sevier Desert, Utah was modeled using a three-dimensional finite-difference model. The model was calibrated by comparing computed and observed water-level measurements in 1952, simulating results of aquifer tests, and simulating ground-water withdrawals during 1952-81 and comparing computed water-level changes during 1952-82 to observed changes. The results indicate the model is capable of predicting future water-level changes. The report includes a complete listing of the model data for the 1952-82 simulation.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834179","usgsCitation":"Holmes, W., 1983, Three-dimensional digital-computer model of the principal ground-water reservoir of the Sevier Desert, Utah: U.S. Geological Survey Water-Resources Investigations Report 83-4179, Report: iv, 127 p.; 1 Plate: 21.06 × 22.53 inches, https://doi.org/10.3133/wri834179.","productDescription":"Report: iv, 127 p.; 1 Plate: 21.06 × 22.53 inches","costCenters":[],"links":[{"id":56573,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4179/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56572,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4179/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158795,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4179/report-thumb.jpg"},{"id":410238,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35828.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Utah","otherGeospatial":"Sevier Desert","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -112.047,\n              40\n            ],\n            [\n              -113.409,\n              40\n            ],\n            [\n              -113.409,\n              39\n            ],\n            [\n              -112.047,\n              39\n            ],\n            [\n              -112.047,\n              40\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63e081","contributors":{"authors":[{"text":"Holmes, W. F.","contributorId":7277,"corporation":false,"usgs":true,"family":"Holmes","given":"W. F.","affiliations":[],"preferred":false,"id":198609,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28597,"text":"wri834004 - 1983 - Conveyance characteristics of the Nueces River, Cotulla to Simmons, Texas","interactions":[],"lastModifiedDate":"2016-08-09T13:28:30","indexId":"wri834004","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4004","title":"Conveyance characteristics of the Nueces River, Cotulla to Simmons, Texas","docAbstract":"<p>Analysis of discharge hydrographs for streamflow-gaging stations on the Nueces River at Cotulla, Tilden, and Simmons indicate that significant water losses occur along the 108-mile reach from Cotulla to Simmon during storm-runoff periods. Computed losses along the 83-mile reach from Cotulla to Tilden for 15 storm periods range from 32 to 59 percent of the total runoff volume passing the Cotulla gage. For six storm periods that occurred while the gage at Simmons was in operation, computed losses from Cotulla to Simmons averaged 48 percent of the storm runoff passing the Cotulla gage. Estimates of total-annual losses were made with the aid of a regression model developed to relate monthly rainfall totals to monthly runoff. Total annual water losses, estimated with the aid of the regression model, ranged from 46,000 acre-feet during 1969 to 368,500 acre-feet during 1967, and averaged about 174,000 acre-feet for 1966-77. (USGS)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri834004","usgsCitation":"Massey, B.C., and Reeves, W.E., 1983, Conveyance characteristics of the Nueces River, Cotulla to Simmons, Texas: U.S. Geological Survey Water-Resources Investigations Report 83-4004, Report: vi, 39 p.; Plate: 17.82 x 12.07 inches, https://doi.org/10.3133/wri834004.","productDescription":"Report: vi, 39 p.; Plate: 17.82 x 12.07 inches","numberOfPages":"45","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":57428,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4004/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124184,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4004/report-thumb.jpg"},{"id":57427,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4004/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d46c","contributors":{"authors":[{"text":"Massey, Bernard C.","contributorId":173558,"corporation":false,"usgs":false,"family":"Massey","given":"Bernard","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":200090,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reeves, William E.","contributorId":99426,"corporation":false,"usgs":true,"family":"Reeves","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":200089,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30169,"text":"wri824116 - 1983 - Appraisal of water-quality conditions, lower Black River, Windsor County, Vermont","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri824116","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-4116","title":"Appraisal of water-quality conditions, lower Black River, Windsor County, Vermont","docAbstract":"Six hydroelectric power dams are planned along a 22-mile reach of the lower Black River in southeastern Windsor County, Vermont. Data were collected at 10 stations, during water years 1977-81, to appraise quality conditions before construction. Average specific conductance of Black River is 101 micromhos indicating low concentrations of dissolved solids. Concentrations of common constituents and minor elements were generally low and within safe levels for aquatic life. Near-saturated dissolved oxygen concentrations and relatively low mean total organic carbon concentrations indicate little oxygen-consuming substances in Black River. Mean total nitrogen concentrations ranged from 0.31 mg/L (milligrams per liter) to 0.61 mg/L. The highest concentrations were most likely due to secondary waste discharges entering the river. Nitrate was the primary form of inorganic nitrogen, mean concentrations ranged from 0.13 to 0.27 mg/L. Concentrations seem high enough to promote excessive algal growth in the proposed Hawks Mountain Reservoir. Mean concentrations of total phosphorus ranged from 0.014 to 0.112 mg/L as P. Maximum concentrations at all stations generally exceeded U.S. Environmental Protection Agency suggested levels for water entering lakes and reservoirs. Mean orthophosphorus concentrations ranged from 0.005 to 0.029 mg/L, suggesting a potential for nuisance algal conditions to develop in the proposed reservoir. Mean algal growth potential concentrations ranged from 1.3 to 8.8 mg/L, falling within the moderately high to high productivity range. No pesticides and polychlorinated biphenyls were detected. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824116","usgsCitation":"Toppin, K., 1983, Appraisal of water-quality conditions, lower Black River, Windsor County, Vermont: U.S. Geological Survey Water-Resources Investigations Report 82-4116, 61 p. :ill., map ;28 cm., https://doi.org/10.3133/wri824116.","productDescription":"61 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":123968,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4116/report-thumb.jpg"},{"id":58970,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4116/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a305","contributors":{"authors":[{"text":"Toppin, K. W.","contributorId":35776,"corporation":false,"usgs":true,"family":"Toppin","given":"K. W.","affiliations":[],"preferred":false,"id":202800,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26618,"text":"wri834255 - 1983 - Primary productivity by phytoplankton in the tidal, fresh Potomac River, Maryland, May 1980 to August 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:08:20","indexId":"wri834255","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4255","title":"Primary productivity by phytoplankton in the tidal, fresh Potomac River, Maryland, May 1980 to August 1981","docAbstract":"Primary productivity by phytoplankton was measured on samples collected from the Potomac Tidal River, Maryland. The studies were performed monthly from May 1980 to September 1981. Additional studies were done once a week in August 1980, twice a week from August 4 to 8, 1980 and twice in September 1980. Depth-integrated samples were collected at five stations and incubated in boxes that were exposed to natural sunlight. The boxes were covered with neutral density filters transmitting 100 , 65, 32, 16, and 6 percent surface light. River water was pumped continuously over the samples. The extinction of light in the water column by phytoplankton was measured when samples were collected. Experiments were performed to select a method for routine productivity analysis. No difference was found between productivity: (1) determined in situ and in boxes; (2) measured in 300 ml and (4) calculated from short term (4 hours) and long term (10-24 hours) incubations. There were higher productivity differences in samples that were rotated among different light intensities every 15 minutes (simulating mixing) than those remaining stationary. Respiration was significantly less in samples pumped through a hose from those collected using a depth-integrating sampler. Depth-integrated primary productivity was determined from the productivity data using an equation modified from one reported in the literature. Depth-integrated gross primary productivity was highest in August 1980 and 1981 and lowest in January 1980. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834255","usgsCitation":"Cohen, R., and Pollock, S., 1983, Primary productivity by phytoplankton in the tidal, fresh Potomac River, Maryland, May 1980 to August 1981: U.S. Geological Survey Water-Resources Investigations Report 83-4255, 76 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834255.","productDescription":"76 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157200,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4255/report-thumb.jpg"},{"id":55489,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4255/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668e07","contributors":{"authors":[{"text":"Cohen, R.R.","contributorId":100426,"corporation":false,"usgs":true,"family":"Cohen","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":196721,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pollock, S.O.","contributorId":102916,"corporation":false,"usgs":true,"family":"Pollock","given":"S.O.","email":"","affiliations":[],"preferred":false,"id":196722,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28336,"text":"wri834146 - 1983 - Hydrogeology and simulation of water flow in the Kootenai aquifer of the Judith basin, central Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:08:38","indexId":"wri834146","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4146","title":"Hydrogeology and simulation of water flow in the Kootenai aquifer of the Judith basin, central Montana","docAbstract":"Five Jurassic and Cretaceous formations in the Judith basin of central Montana were investigated with a three-dimensional model to improve the understanding of water flow in the Kootenai aquifer. To accomplish this objective, of water flow in the aquifers and two intervening confining layers was constructed from existing data. A steady-state model was calibrated and evaluated using a parameter-estimation procedure. The digital model simulates horizontal flow in the middle (Kootenai) aquifer and vertical leakage through the overlying and underlying confining layers. The top and bottom aquifers are used as constant-head boundaries to aid in simulating vertical leakage. Transmissivity for the aquifer obtained from the calibrated model ranges from 137 to 364 ft super 2/d. Recharge in the form of precipitation on the outcrop is about 2% of total precipitation (5.44 ft super 3/s). The other component of net recharge is 32.48 ft super 3/s of vertical leakage from the Swift aquifer. The cumulative rate of discharge from all known wells completed in the aquifer is about 0.84 ft super 3/s. Other components of net discharge are 1.83 ft super 3/s of underflow and 35.25 ft super 3/s of vertical leakage to the Colorado aquifers. Estimates of vertical hydraulic conductivity are 2.15 x 10- super 2 ft/d for the lower confining layer, and 3.16 x 10- super 3 and 1.33 x 10- super 4 ft/d for the upper confining layer. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nOpen-File Services Section [distributor],","doi":"10.3133/wri834146","usgsCitation":"Levings, J.F., 1983, Hydrogeology and simulation of water flow in the Kootenai aquifer of the Judith basin, central Montana: U.S. Geological Survey Water-Resources Investigations Report 83-4146, v, 39 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834146.","productDescription":"v, 39 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123465,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4146/report-thumb.jpg"},{"id":57147,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4146/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57148,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4146/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68550a","contributors":{"authors":[{"text":"Levings, Julianne F.","contributorId":29818,"corporation":false,"usgs":true,"family":"Levings","given":"Julianne","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":199615,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9158,"text":"ofr83345 - 1983 - MAGPOLY; a modification of a three-dimensional magnetic modelling program","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr83345","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-345","title":"MAGPOLY; a modification of a three-dimensional magnetic modelling program","docAbstract":"The three-dimensional magnetic modelling program of Donald Plouff (Plouff, 1975) has been made operational on a Honeywell Multics 68/80 computer. Modifications were made to input and output procedures to make the program compatible with U.S. Geological Survey (USGS) standard geophysical input and output formats.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83345","usgsCitation":"Godson, R.H., 1983, MAGPOLY; a modification of a three-dimensional magnetic modelling program: U.S. Geological Survey Open-File Report 83-345, 64 p. ill. ;28 cm., https://doi.org/10.3133/ofr83345.","productDescription":"64 p. ill. ;28 cm.","costCenters":[],"links":[{"id":142648,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0345/report-thumb.jpg"},{"id":36785,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0345/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648b51","contributors":{"authors":[{"text":"Godson, Richard H.","contributorId":11190,"corporation":false,"usgs":true,"family":"Godson","given":"Richard","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":159198,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":36583,"text":"fwsobs82_10_62 - 1983 - Habitat Suitability Index Models: Field sparrow","interactions":[],"lastModifiedDate":"2022-02-09T15:30:14.752726","indexId":"fwsobs82_10_62","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.62","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Field sparrow","docAbstract":"Habitat preferences of the field sparrow (Spizella pusilla) are described in this report, which is one of a series of Habitat Suitability Index (HSI) models. A review and synthesis of the literature is followed by the development of a habitat model for the field sparrow throughout its breeding range in the United States. HSI models are designed to be used in conjunction with Habitat Evaluation Procedures previously developed by the U.S. Fish and Wildlife Service.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Sousa, P.J., 1983, Habitat Suitability Index Models: Field sparrow: FWS/OBS 82/10.62, vi, 14 p.","productDescription":"vi, 14 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":165609,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649939","contributors":{"authors":[{"text":"Sousa, Patrick J.","contributorId":19206,"corporation":false,"usgs":true,"family":"Sousa","given":"Patrick","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":216585,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7782,"text":"ofr83677 - 1983 - Hydrology of the Jasper (Miocene) Aquifer in the Southeast Texas coastal plain","interactions":[],"lastModifiedDate":"2025-09-23T16:51:31.349837","indexId":"ofr83677","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-677","title":"Hydrology of the Jasper (Miocene) Aquifer in the Southeast Texas coastal plain","docAbstract":"<p>The Jasper (Miocene) aquifer is one of several important hydrologic units in the Gulf Coastal Plain. Because the Jasper aquifer underlies shallower aquifers in many areas, regional water withdrawals from the Jasper are not significant; however, it is capable of yielding 3,000 gallons per minute (200 liters per second) or more of water to wells in certain areas. The Jasper is underlain by the Catahoula confining system (restricted) and overlain by the Burkeville confining system. The Evangeline and Chicot aquifers, in turn, overlie the Burkeville and also are prolific water-yielding aquifers.</p><p>The ground-water hydrology of the Jasper aquifer in an area of about 20,000 square miles (52,000 square kilometers) was simulated by a two-dimensional digital model using a steady-state approach. The model represents hydrologic conditions prior to development by wells, when natural recharge equaled natural discharge. The model's grid pattern of 15 x 24 nodes varies from a dimension of 5 by 10 miles (8 by 16 kilometers) in the outcrop to 10 by 10 miles (16 by 16 kilometers) in the artesian section downdip from the outcrop.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83677","collaboration":"Prepared in cooperation with the Texas Department of Water Resources","usgsCitation":"Baker, E., 1983, Hydrology of the Jasper (Miocene) Aquifer in the Southeast Texas coastal plain: U.S. Geological Survey Open-File Report 83-677, Report: viii, 68 p.; 17 Plates: 20.28 x 10.58 inches or smaller, https://doi.org/10.3133/ofr83677.","productDescription":"Report: viii, 68 p.; 17 Plates: 20.28 x 10.58 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science 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,{"id":44520,"text":"wri8252 - 1983 - Analog model analysis of the north coast limestone aquifers, Puerto Rico","interactions":[],"lastModifiedDate":"2012-02-02T00:10:09","indexId":"wri8252","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-52","title":"Analog model analysis of the north coast limestone aquifers, Puerto Rico","language":"ENGLISH","doi":"10.3133/wri8252","usgsCitation":"Heisel, J.E., Gonzalez, J., and Cruz, C., 1983, Analog model analysis of the north coast limestone aquifers, Puerto Rico: U.S. Geological Survey Water-Resources Investigations Report 82-52, 49 p., https://doi.org/10.3133/wri8252.","productDescription":"49 p.","costCenters":[],"links":[{"id":113820,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0052/report.pdf","size":"3395","linkFileType":{"id":1,"text":"pdf"}},{"id":162321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0052/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db68403e","contributors":{"authors":[{"text":"Heisel, J. E.","contributorId":103252,"corporation":false,"usgs":true,"family":"Heisel","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":229924,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gonzalez, J.R.","contributorId":34179,"corporation":false,"usgs":true,"family":"Gonzalez","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":229923,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cruz, Carlos","contributorId":15671,"corporation":false,"usgs":true,"family":"Cruz","given":"Carlos","email":"","affiliations":[],"preferred":false,"id":229922,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":40694,"text":"ofr80811I - 1983 - Distribution and abundance of copper, lead, and zinc in nonmagnetic and moderately magnetic heavy-mineral-concentrate, minus-80-mesh stream-sediment, and ash of aquatic-bryophyte samples, Medfra quadrangle, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:53","indexId":"ofr80811I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"80-811","chapter":"I","title":"Distribution and abundance of copper, lead, and zinc in nonmagnetic and moderately magnetic heavy-mineral-concentrate, minus-80-mesh stream-sediment, and ash of aquatic-bryophyte samples, Medfra quadrangle, Alaska","language":"ENGLISH","doi":"10.3133/ofr80811I","usgsCitation":"King, H.D., 1983, Distribution and abundance of copper, lead, and zinc in nonmagnetic and moderately magnetic heavy-mineral-concentrate, minus-80-mesh stream-sediment, and ash of aquatic-bryophyte samples, Medfra quadrangle, Alaska: U.S. Geological Survey Open-File Report 80-811, 6 maps :photocopy ;47 x 63 cm., on sheets 78 x 88 cm. or smaller., https://doi.org/10.3133/ofr80811I.","productDescription":"6 maps :photocopy ;47 x 63 cm., on sheets 78 x 88 cm. or smaller.","costCenters":[],"links":[{"id":171133,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":77973,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0811i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":77974,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0811i/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":77975,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0811i/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":77976,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0811i/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":77977,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0811i/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":77978,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0811i/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a0ed","contributors":{"authors":[{"text":"King, H. D.","contributorId":89113,"corporation":false,"usgs":true,"family":"King","given":"H.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":223767,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40707,"text":"ofr80811L - 1983 - Distribution and abundance of antimony and mercury in minus-80-mesh stream-sediment and antimony in nonmagnetic and moderately magnetic heavy-mineral-concentrate samples, Medfra quadrangle, Alaska","interactions":[],"lastModifiedDate":"2024-07-31T19:01:33.576748","indexId":"ofr80811L","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"80-811","chapter":"L","title":"Distribution and abundance of antimony and mercury in minus-80-mesh stream-sediment and antimony in nonmagnetic and moderately magnetic heavy-mineral-concentrate samples, Medfra quadrangle, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80811L","usgsCitation":"King, H.D., O’Leary, R.M., Risoli, D., and Galland, D.W., 1983, Distribution and abundance of antimony and mercury in minus-80-mesh stream-sediment and antimony in nonmagnetic and moderately magnetic heavy-mineral-concentrate samples, Medfra quadrangle, Alaska: U.S. Geological Survey Open-File Report 80-811, 2 Plates: 35.52 x 28.10 inches and 35.48 x 23.80 inches, https://doi.org/10.3133/ofr80811L.","productDescription":"2 Plates: 35.52 x 28.10 inches and 35.48 x 23.80 inches","costCenters":[],"links":[{"id":431730,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11780.htm","linkFileType":{"id":5,"text":"html"}},{"id":77984,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0811l/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":77983,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0811l/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":172099,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Medfra quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -156,\n              64\n            ],\n            [\n              -156,\n              63\n            ],\n            [\n              -153,\n              63\n            ],\n            [\n              -153,\n              64\n            ],\n            [\n              -156,\n              64\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a14e","contributors":{"authors":[{"text":"King, H. D.","contributorId":89113,"corporation":false,"usgs":true,"family":"King","given":"H.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":223826,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Leary, R. M.","contributorId":44894,"corporation":false,"usgs":true,"family":"O’Leary","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":223823,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Risoli, D. A.","contributorId":48156,"corporation":false,"usgs":true,"family":"Risoli","given":"D. A.","affiliations":[],"preferred":false,"id":223824,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Galland, D. W.","contributorId":65108,"corporation":false,"usgs":true,"family":"Galland","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":223825,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":40709,"text":"ofr80811K - 1983 - Distribution and abundance of arsenic and bismuth in nonmagnetic and moderately magnetic heavy-mineral-concentrate samples and arsenic in minus-80-mesh stream-sediment and ash of aquatic-bryophyte samples, Medfra quadrangle, Alaska","interactions":[],"lastModifiedDate":"2024-06-14T20:30:51.258725","indexId":"ofr80811K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"80-811","chapter":"K","title":"Distribution and abundance of arsenic and bismuth in nonmagnetic and moderately magnetic heavy-mineral-concentrate samples and arsenic in minus-80-mesh stream-sediment and ash of aquatic-bryophyte samples, Medfra quadrangle, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80811K","usgsCitation":"King, H.D., Cooley, E., and Spiesman, D., 1983, Distribution and abundance of arsenic and bismuth in nonmagnetic and moderately magnetic heavy-mineral-concentrate samples and arsenic in minus-80-mesh stream-sediment and ash of aquatic-bryophyte samples, Medfra quadrangle, Alaska: U.S. Geological Survey Open-File Report 80-811, 3 Plates: 36.08 x 29.28 inches or smaller, https://doi.org/10.3133/ofr80811K.","productDescription":"3 Plates: 36.08 x 29.28 inches or smaller","costCenters":[],"links":[{"id":77988,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0811k/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":77987,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0811k/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":77986,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0811k/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":171970,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":430237,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11779.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","otherGeospatial":"Medfra quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -156,\n              64\n            ],\n            [\n              -156,\n              63\n            ],\n            [\n              -153,\n              63\n            ],\n            [\n              -153,\n              64\n            ],\n            [\n              -156,\n              64\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a137","contributors":{"authors":[{"text":"King, H. D.","contributorId":89113,"corporation":false,"usgs":true,"family":"King","given":"H.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":223832,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooley, E.F.","contributorId":83072,"corporation":false,"usgs":true,"family":"Cooley","given":"E.F.","email":"","affiliations":[],"preferred":false,"id":223831,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Spiesman, D. L. Jr.","contributorId":41022,"corporation":false,"usgs":true,"family":"Spiesman","given":"D. L.","suffix":"Jr.","affiliations":[],"preferred":false,"id":223830,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":56648,"text":"fwsobs82_10_36 - 1983 - Habitat Suitability Index Models: Smallmouth bass","interactions":[],"lastModifiedDate":"2022-02-09T15:27:17.4465","indexId":"fwsobs82_10_36","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.36","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Smallmouth bass","docAbstract":"A review and synthesis of existing information were used to develop riverine and lacustrine habitat models for Smallmouth bass (Micropterus dolomieui), a freshwater species. The models are scaled to produce an index of habitat suitability between 0 (unsuitable habitat) and 1 (optimally suitable habitat) for freshwater areas of the continental United States. Habitat suitability indexes (HSI's) are designed for use with the habitat evaluation procedures developed by the U.S. Fish and Wildlife Service. The instream flow suitability curves are intended for use with the Instream Flow Incremental Methodology.\r\n\r\nAlso included are discussions of Suitability Index (SI) curves as used by the Instream Flow Incremental Methodology (IFIM) and SI curves available for an IFIM analysis of Smallmouth bass habitat.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Edwards, E.A., Gebhart, G., and Maughan, O.E., 1983, Habitat Suitability Index Models: Smallmouth bass: FWS/OBS 82/10.36, viii, 47 p.","productDescription":"viii, 47 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":181661,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64975f","contributors":{"authors":[{"text":"Edwards, Elizabeth A.","contributorId":39421,"corporation":false,"usgs":true,"family":"Edwards","given":"Elizabeth","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":255594,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gebhart, Glen","contributorId":52237,"corporation":false,"usgs":true,"family":"Gebhart","given":"Glen","email":"","affiliations":[],"preferred":false,"id":255596,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Maughan, O. Eugene","contributorId":43006,"corporation":false,"usgs":true,"family":"Maughan","given":"O.","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":255595,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":56650,"text":"fwsobs82_10_50 - 1983 - Habitat Suitability Index Models: Roseate spoonbill","interactions":[],"lastModifiedDate":"2022-02-09T15:26:11.161465","indexId":"fwsobs82_10_50","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.50","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Roseate spoonbill","docAbstract":"<p>The roseate spoonbill is a long-legged wading bird with a height of approximately 80 cm (31.5 inches), a wingspan of 1.3 m (4.3 ft), and a weight of 1.6 kg (3.5 Ib }. The bill is narrower near the base (2-3 em, 0.8-1.2 inches) than at the flattened tip (5 cm, 2 inches) and is 15-18 cm (5.9-7.1 inches) in length.</p><p>Roseate spoonbills occur and nest in peninsular Florida, coastal Louisiana, and Texas, south through the West Indies, Mexico, Central and South America to Argentina and Chile. Marine, brackish, and freshwater habitats are utilized, but brackish areas are favored (Blacklock et al. 1978). In the late 1970·s there were 2,500 pairs nesting along the Texas coast (Texas Colonial Waterbird Society 1982), 1,300 pairs in southwestern Louisiana (Portnoy 1977), and 1,400 pairs in Florida (Robertson et al. 1983). These birds are resident year round in Florida, Louisiana, and Texas, but fewer bi rds are present duri ng the nonbreedi ng season than in the breeding season. Some individuals move northward after nesting and have been reported in Georgia, Nebraska, Pennsylvania, Utah, and Wisconsin, but most spoonbills move south when they leave the breeding area.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Lewis, J., 1983, Habitat Suitability Index Models: Roseate spoonbill: FWS/OBS 82/10.50, vi, 16 p.","productDescription":"vi, 16 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":181765,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64977c","contributors":{"authors":[{"text":"Lewis, James C.","contributorId":88799,"corporation":false,"usgs":true,"family":"Lewis","given":"James C.","affiliations":[],"preferred":false,"id":255599,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56651,"text":"fwsobs82_10_58 - 1983 - Habitat Suitability Index Models: Alewife and blueback herring","interactions":[],"lastModifiedDate":"2022-02-09T15:25:41.078632","indexId":"fwsobs82_10_58","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.58","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Alewife and blueback herring","docAbstract":"Alewives and blueback herring are anadromous clupeids found along the Atlantic coast in marine, estuarine, and riverine habitats, depending upon life stage. Both are important commercial species, used fresh or salted for human consumption, and used as crab bait, fish meal (particularly in animal food manufacturing), and fish oil. Alewife and blueback herring are marketed collectively as 'river herring,' a term that will be used for both species in this report. River herring play important ecological roles. In marine, estuarine, and riverine food webs, they occupy a level between zooplankton, their principal food, and piscivores.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Pardue, G.B., 1983, Habitat Suitability Index Models: Alewife and blueback herring: FWS/OBS 82/10.58, vi, 22 p.","productDescription":"vi, 22 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":181766,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649e1f","contributors":{"authors":[{"text":"Pardue, Garland B.","contributorId":53014,"corporation":false,"usgs":true,"family":"Pardue","given":"Garland","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":255600,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28683,"text":"wri834028 - 1983 - Computer simulation model of the Pleistocene valley-fill aquifer in southwestern Essex and southeastern Morris counties, New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:08:35","indexId":"wri834028","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4028","title":"Computer simulation model of the Pleistocene valley-fill aquifer in southwestern Essex and southeastern Morris counties, New Jersey","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834028","usgsCitation":"Meisler, H., 1983, Computer simulation model of the Pleistocene valley-fill aquifer in southwestern Essex and southeastern Morris counties, New Jersey: U.S. Geological Survey Water-Resources Investigations Report 83-4028, 76 p. :maps ;28 cm., https://doi.org/10.3133/wri834028.","productDescription":"76 p. :maps ;28 cm.","costCenters":[],"links":[{"id":121639,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4028/report-thumb.jpg"},{"id":57523,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4028/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57524,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4028/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7662","contributors":{"authors":[{"text":"Meisler, Harold","contributorId":34103,"corporation":false,"usgs":true,"family":"Meisler","given":"Harold","email":"","affiliations":[],"preferred":false,"id":200226,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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