No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83663","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Aeromagnetic map of the Kingman-Trona area, California: U.S. Geological Survey Open-File Report 83-663, 2 Plates: 34.21 x 18.83 inches and 27.32 x 14.54 inches, https://doi.org/10.3133/ofr83663.","productDescription":"2 Plates: 34.21 x 18.83 inches and 27.32 x 14.54 inches","costCenters":[],"links":[{"id":167935,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":413552,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14163.htm","linkFileType":{"id":5,"text":"html"}},{"id":79536,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0663/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79535,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0663/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Kingman-Trona area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -117.5,\n 36.25\n ],\n [\n -117.5,\n 35\n ],\n [\n -114.583,\n 35\n ],\n [\n -114.583,\n 36.25\n ],\n [\n -117.5,\n 36.25\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691fd9","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530640,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44504,"text":"wri834045 - 1983 - Hydrogeologic and water-quality characteristics of the Prairie du Chien-Jordan aquifer, Southeast Minnesota","interactions":[],"lastModifiedDate":"2023-03-13T21:29:01.182397","indexId":"wri834045","displayToPublicDate":"1983-01-01T00:00:00","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":"83-4045","title":"Hydrogeologic and water-quality characteristics of the Prairie du Chien-Jordan aquifer, Southeast Minnesota","docAbstract":"Quality of water in the Prairie du Chien-Jordan aquifer is generally good, except for some localized contamination, Coal-tar derivatives that contaminate the aquifer in St. Louis Park, a western suburb in the Twin Cities Metropolitan Area, pose the most serious threat to water quality. High hardness and iron concentration limit suitability for municipal and industrial use in parts of extreme southeast Minnesota. Confining beds of bedrock and drift, however, protect most of the aquifer from surface pollutants.
The Prairie du Chien-Jordan aquifer is part of a sequence of sedimentary bedrock units in southeast Minnesota. The Jordan Sandstone is a white to yellow, fine- to coarse-grained sandstone. The Prairie du Chien Group comprises two dolomitic formations that are vuggy and fractured and interbedded with thin layers of shale. The aquifer formations were deposited in Paleozoic seas that occupied the Hollandale embayment. The aquifer dips toward the interior of the embayment where it is as deep as 750 feet below land surface and as thick as 500 feet.
Permeability is secondary in the Prairie du Chien Group because of solution cavities and fractures, and intergranular in the Jordan Sandstone. Water in the aquifer is confined except in the eastern part. Water generally flows to the north and east into the Minnesota and Mississippi Rivers. A ground-water divide separates part of the flow southward into Iowa. This aquifer supplies more water than any other bedrock one in the State.
Calcium magnesium bicarbonate type water is most common in the aquifer. Calcium and sulfate and, to a lesser degree sodium and magnesium, increase in concentration toward the southwestern part of the study area. Bicarbonate concentration, on the other hand, decreases toward the southwestern corner of the study area. Leakage from overlying Cretaceous deposits is the source of much of the sulfate and other minerals in the southwest.
This report is one of a series on the hydrogeology and water quality of the 14 principal aquifers in Minnesota prepared by the U. S. Geological Survey. The U. S. Environmental Protection Agency requested these studies because of the need for information to develop its Underground Injection Control Program.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri834045","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency","usgsCitation":"Ruhl, J.F., Wolf, R.J., and Adolphson, D.G., 1983, Hydrogeologic and water-quality characteristics of the Prairie du Chien-Jordan aquifer, Southeast Minnesota: U.S. Geological Survey Water-Resources Investigations Report 83-4045, 2 Plates: 39.28 x 33.33 inches and 39.08 x 33.41 inches, https://doi.org/10.3133/wri834045.","productDescription":"2 Plates: 39.28 x 33.33 inches and 39.08 x 33.41 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":170272,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414057,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35685.htm","linkFileType":{"id":5,"text":"html"}},{"id":81880,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4045/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81879,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4045/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Prairie du Chien-Jordan aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -92.8619384765625,\n 45.71385093029221\n ],\n [\n -93.3837890625,\n 45.706179285330855\n ],\n [\n -93.8507080078125,\n 45.65628792636447\n ],\n [\n -94.207763671875,\n 45.583289756006316\n ],\n [\n -94.3011474609375,\n 45.46783598133375\n ],\n [\n -94.39453125,\n 45.232349197513116\n ],\n [\n -94.537353515625,\n 45.058001435398296\n ],\n [\n -94.7186279296875,\n 44.85197466334987\n ],\n [\n -94.89990234375,\n 44.629573191951046\n ],\n [\n -94.976806640625,\n 44.53959000445632\n ],\n [\n -95.3118896484375,\n 44.465151013519616\n ],\n [\n -95.4052734375,\n 44.296332880058706\n ],\n [\n -95.3118896484375,\n 44.12702800650004\n ],\n [\n -94.97131347656249,\n 43.91768033000405\n ],\n [\n -94.8944091796875,\n 43.504736854976954\n ],\n [\n -91.23046875,\n 43.504736854976954\n ],\n [\n -91.219482421875,\n 43.57243174740972\n ],\n [\n -91.2799072265625,\n 43.628123412124616\n ],\n [\n -91.241455078125,\n 43.75522505306928\n ],\n [\n -91.263427734375,\n 43.83452678223684\n ],\n [\n -91.3897705078125,\n 43.96909818325174\n ],\n [\n -91.461181640625,\n 44.008620115415354\n ],\n [\n -91.5655517578125,\n 44.03232064275084\n ],\n [\n -91.636962890625,\n 44.06390660801779\n ],\n [\n -91.73583984374999,\n 44.11125397357153\n ],\n [\n -91.8402099609375,\n 44.18614312298759\n ],\n [\n -91.8896484375,\n 44.24913396886894\n ],\n [\n -91.9500732421875,\n 44.32384807250689\n ],\n [\n -91.9720458984375,\n 44.35527821160296\n ],\n [\n -92.1148681640625,\n 44.41416430998939\n ],\n [\n -92.21923828124999,\n 44.44554600843547\n ],\n [\n -92.31262207031249,\n 44.49650533109348\n ],\n [\n -92.31262207031249,\n 44.53959000445632\n ],\n [\n -92.5048828125,\n 44.574817404670306\n ],\n [\n -92.57080078125,\n 44.59829048984011\n ],\n [\n -92.6641845703125,\n 44.65693173288727\n ],\n [\n -92.8070068359375,\n 44.750634493861064\n ],\n [\n -92.74658203125,\n 44.85586880735725\n ],\n [\n -92.7630615234375,\n 44.90646871709883\n ],\n [\n -92.74658203125,\n 44.94536144236941\n ],\n [\n -92.7850341796875,\n 45.03859654645257\n ],\n [\n -92.79602050781249,\n 45.06964120886863\n ],\n [\n -92.74108886718749,\n 45.11230010229608\n ],\n [\n -92.7630615234375,\n 45.178164812206376\n ],\n [\n -92.757568359375,\n 45.27488643704894\n ],\n [\n -92.691650390625,\n 45.36372498305678\n ],\n [\n -92.6641845703125,\n 45.398449976304086\n ],\n [\n -92.6531982421875,\n 45.463983441272745\n ],\n [\n -92.6751708984375,\n 45.48324350868221\n ],\n [\n -92.7191162109375,\n 45.533288879467456\n ],\n [\n -92.7630615234375,\n 45.56021795715051\n ],\n [\n -92.8179931640625,\n 45.56021795715051\n ],\n [\n -92.88940429687499,\n 45.57175504130605\n ],\n [\n -92.8729248046875,\n 45.6178796835697\n ],\n [\n -92.8619384765625,\n 45.71385093029221\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628d15","contributors":{"authors":[{"text":"Ruhl, J. F.","contributorId":81866,"corporation":false,"usgs":true,"family":"Ruhl","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":229896,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolf, R. J.","contributorId":21518,"corporation":false,"usgs":true,"family":"Wolf","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":229895,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Adolphson, D. G.","contributorId":106081,"corporation":false,"usgs":true,"family":"Adolphson","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":229897,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":47673,"text":"wri811182 - 1983 - Historical changes to Lake Washington and route of the Lake Washington Ship Canal, King County, Washington","interactions":[],"lastModifiedDate":"2022-08-29T13:55:24.290547","indexId":"wri811182","displayToPublicDate":"1983-01-01T00:00:00","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":"81-1182","title":"Historical changes to Lake Washington and route of the Lake Washington Ship Canal, King County, Washington","docAbstract":"Lake Washington, in the midst of the greater Seattle metropolitan area of the Puget Sound region (fig. 1), is an exceptional commercial, recreational, and esthetic resource for the region . In the past 130 years, Lake Washington has been changed from a \" wild \" lake in a wilderness setting to a regulated lake surrounded by a growing metropolis--a transformation that provides an unusual opportunity to study changes to a lake's shoreline and hydrologic characteristics -resulting from urbanization.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri811182","usgsCitation":"Chrzastowski, M.J., 1983, Historical changes to Lake Washington and route of the Lake Washington Ship Canal, King County, Washington: U.S. Geological Survey Water-Resources Investigations Report 81-1182, Report: 9 p.; Plate: 33.53 x 57.12 inches, https://doi.org/10.3133/wri811182.","productDescription":"Report: 9 p.; Plate: 33.53 x 57.12 inches","numberOfPages":"9","costCenters":[],"links":[{"id":162048,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr811182.jpg"},{"id":405790,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1182/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405789,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1182/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","county":"King County","otherGeospatial":"Lake Washington","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.46871948242186,\n 47.30903424774781\n ],\n [\n -122.46871948242186,\n 47.96510025611191\n ],\n [\n -121.40991210937499,\n 47.96510025611191\n ],\n [\n -121.40991210937499,\n 47.30903424774781\n ],\n [\n -122.46871948242186,\n 47.30903424774781\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6885d4","contributors":{"authors":[{"text":"Chrzastowski, Michael J.","contributorId":28643,"corporation":false,"usgs":true,"family":"Chrzastowski","given":"Michael","email":"","middleInitial":"J.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":235985,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30050,"text":"wri824100 - 1983 - Land application of wastewater and its effect on ground-water quality in the Livermore-Amador Valley, Alameda County, California","interactions":[],"lastModifiedDate":"2023-03-14T21:05:28.776892","indexId":"wri824100","displayToPublicDate":"1983-01-01T00:00:00","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":"82-4100","title":"Land application of wastewater and its effect on ground-water quality in the Livermore-Amador Valley, Alameda County, California","docAbstract":"Ground-water quality, ground-water level, and rainfall data collected during the 1975 water year through the 1980 water year were analyzed to determine the effects of land application of effluent from wastewater treatment plants on ground-water quality in the Livermore-Amador Valley. Annual rainfall varied markedly during the study: 1976 and 1977 water years had less than one half the normal rainfall; 1978 and 1980 water years had greater than normal rainfall; and 1975 and 1979 water years had nearly normal rainfall. The direction ground-water movement in the valley was found to be generally that of surface water. Dissolved nitrate concentrations were generally much less in areas not receiving wastewater applications than in areas that do. Specific conductance, dissolved solids, dissolved chloride, and dissolved nitrate were substantially less in the lower aquifers than in the upper aquifer in the Livermore wastewater application areas. In the Castlewood, Pleasanton, Veterans Administration Hospital, and Livermore wastewater applications areas ground-water quality was similar to the quality of effluent from wastewater treatment plants in the valley. Rainfall, soil, and geology appeared to be the main determinants of ground-water quality in the Castlewood and Dublin-San Ramon and Camp Parks Military Reservation areas. Wastewater application appeared to be the main determinant of ground-water quality in Pleasanton, Veterans Administration Hospital, and Livermore Municipal Airport areas. Comparison of ground-water quality in wastewater application areas with proposed State water-quality objectives for ground water in the Livermore-Amador Valley showed impaired water quality in all areas.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824100","usgsCitation":"Sylvester, M.A., 1983, Land application of wastewater and its effect on ground-water quality in the Livermore-Amador Valley, Alameda County, California: U.S. Geological Survey Water-Resources Investigations Report 82-4100, Report: vi, 53 p.; 2 Plates: 41.37 x 40.76 inches and 42.24 x 40.61 inches, https://doi.org/10.3133/wri824100.","productDescription":"Report: vi, 53 p.; 2 Plates: 41.37 x 40.76 inches and 42.24 x 40.61 inches","costCenters":[],"links":[{"id":110155,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35608.htm","linkFileType":{"id":5,"text":"html"},"description":"35608"},{"id":58861,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4100/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58860,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4100/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58859,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4100/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124278,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4100/report-thumb.jpg"}],"country":"United States","state":"California","county":"Alameda County","otherGeospatial":"Livermore-Amador Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -122,\n 37.5\n ],\n [\n -121.625,\n 37.5\n ],\n [\n -121.625,\n 37.8333\n ],\n [\n -122,\n 37.8333\n ],\n [\n -122,\n 37.5\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aeeaa","contributors":{"authors":[{"text":"Sylvester, M. A.","contributorId":10838,"corporation":false,"usgs":true,"family":"Sylvester","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":202595,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26859,"text":"wri834094 - 1983 - Impact of changes in land use on the ground-water system in the Sequim-Dungeness Peninsula, Clallam County, Washington","interactions":[],"lastModifiedDate":"2023-03-14T20:43:18.101534","indexId":"wri834094","displayToPublicDate":"1983-01-01T00:00:00","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":"83-4094","title":"Impact of changes in land use on the ground-water system in the Sequim-Dungeness Peninsula, Clallam County, Washington","docAbstract":"A digital-computer model was developed to simulate three-dimensional ground-water flow in aquifers underlying the Sequim-Dungeness peninsula, Clallam County, Washington. Analysis using the model shows that leakage from irrigation ditches is the area 's most important source of ground-water recharge. Termination of the irrigation system would lead to lower heads throughout the ground-water system. After 10-20 years of no irrigation, the water-table aquifer would have average drawdowns of about 20 feet and some areas would become completely unsaturated. Several hundred wells could be in danger of going dry. If irrigation were terminated, leakage from the Dungeness River would become the major source of ground-water recharge. As of June 1980, ground-water quality has apparently not been affected in the study area by the use of on-site domestic sewage-disposal systems. The median nitrate-plus-nitrite (as N) concentration in the water-table aquifer was 0.25 milligrams per liter, and the maximum concentration was 2.5 milligrams per liter.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834094","usgsCitation":"Drost, B., 1983, Impact of changes in land use on the ground-water system in the Sequim-Dungeness Peninsula, Clallam County, Washington: U.S. Geological Survey Water-Resources Investigations Report 83-4094, viii, 69 p., https://doi.org/10.3133/wri834094.","productDescription":"viii, 69 p.","costCenters":[],"links":[{"id":414134,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35720.htm","linkFileType":{"id":5,"text":"html"}},{"id":55747,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4094/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123302,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4094/report-thumb.jpg"}],"country":"United States","state":"Washington","county":"Clallam County","otherGeospatial":"Sequim-Dungeness Peninsula","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -123.267,\n 48.167\n ],\n [\n -123.267,\n 48.043\n ],\n [\n -123.033,\n 48.043\n ],\n [\n -123.033,\n 48.167\n ],\n [\n -123.267,\n 48.167\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c4ac","contributors":{"authors":[{"text":"Drost, B. W.","contributorId":38526,"corporation":false,"usgs":true,"family":"Drost","given":"B. W.","affiliations":[],"preferred":false,"id":197136,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28427,"text":"wri834220 - 1983 - A method for estimating ground-water return flow to the lower Colorado River in the Yuma area, Arizona and California","interactions":[],"lastModifiedDate":"2023-04-06T18:31:52.318608","indexId":"wri834220","displayToPublicDate":"1983-01-01T00:00:00","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":"83-4220","title":"A method for estimating ground-water return flow to the lower Colorado River in the Yuma area, Arizona and California","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834220","usgsCitation":"Loeltz, O.J., and Leake, S.A., 1983, A method for estimating ground-water return flow to the lower Colorado River in the Yuma area, Arizona and California: U.S. Geological Survey Water-Resources Investigations Report 83-4220, ix, 86 p., https://doi.org/10.3133/wri834220.","productDescription":"ix, 86 p.","costCenters":[],"links":[{"id":57230,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4220/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119024,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4220/report-thumb.jpg"},{"id":415364,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35861.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Arizona, California","city":"Yuma","otherGeospatial":"lower Colorado River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -114.731,\n 32.886\n ],\n [\n -114.731,\n 32.699\n ],\n [\n -114.429,\n 32.699\n ],\n [\n -114.429,\n 32.886\n ],\n [\n -114.731,\n 32.886\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae136","contributors":{"authors":[{"text":"Loeltz, Omar J.","contributorId":86312,"corporation":false,"usgs":true,"family":"Loeltz","given":"Omar","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":199777,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leake, S. A.","contributorId":52164,"corporation":false,"usgs":true,"family":"Leake","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":199776,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27782,"text":"wri834192 - 1983 - Measurement of the reaeration coefficients of the North Fork Licking River at Utica, Ohio by radioactive tracers","interactions":[],"lastModifiedDate":"2023-03-29T21:16:33.711699","indexId":"wri834192","displayToPublicDate":"1983-01-01T00:00:00","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":"83-4192","title":"Measurement of the reaeration coefficients of the North Fork Licking River at Utica, Ohio by radioactive tracers","docAbstract":"Reaeration coefficients of the North Fork Licking River at Utica, Ohio were measured by the radioactive-tracer method. The tests were conducted on a 2.1-mile reach on September 23 and October 7, 1981, during low-flow conditions. Krypton-85 gas and tritium were the radioopactive tracers, which were used in conjunction with rhodamine-WT dye.
The reaertion coefficients determined on September 23 were 3.09 days-1 (subreach 1-2) and 3.32 days-1 (subreach 2-3). On October 7, the values were 2.04 days-1 and 2.23 days-1 respectively.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834192","usgsCitation":"Hren, J., 1983, Measurement of the reaeration coefficients of the North Fork Licking River at Utica, Ohio by radioactive tracers: U.S. Geological Survey Water-Resources Investigations Report 83-4192, iv, 19 p., https://doi.org/10.3133/wri834192.","productDescription":"iv, 19 p.","costCenters":[],"links":[{"id":56625,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4192/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414929,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35841.htm","linkFileType":{"id":5,"text":"html"}},{"id":118726,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4192/report-thumb.jpg"}],"country":"United States","state":"Ohio","city":"Utica","otherGeospatial":"North Fork Licking River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -82.458,\n 40.242\n ],\n [\n -82.458,\n 40.208\n ],\n [\n -82.435,\n 40.208\n ],\n [\n -82.435,\n 40.242\n ],\n [\n -82.458,\n 40.242\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db611210","contributors":{"authors":[{"text":"Hren, Janet","contributorId":69554,"corporation":false,"usgs":true,"family":"Hren","given":"Janet","email":"","affiliations":[],"preferred":false,"id":198678,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28089,"text":"wri834053 - 1983 - Ground water in the northeast part of Twentynine Palms Marine Corps Base, Bagdad area, California","interactions":[],"lastModifiedDate":"2023-04-11T19:27:17.935961","indexId":"wri834053","displayToPublicDate":"1983-01-01T00:00:00","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":"83-4053","title":"Ground water in the northeast part of Twentynine Palms Marine Corps Base, Bagdad area, California","docAbstract":"The hydrologic characteristics of the Bagdad area, in the northeast part of Twentynine Palms Marine Corps Base, were investigated to determine the feasibility of obtaining a supply of ground water. Five test holes were drilled and three of these were completed with 6-inch casings. Ground water in the eastern part of the study area is high in dissolved solids; water from well 5N/11E-36H1 contains 252,000 milligrams per liter of dissolved solids, and well 4N/12E-7R1 contains 21,800 milligrams per liter of dissolved solids. The dissolved-solids concentration in water from the test wells on the west side of Ludlow fault is much lower; the dissolved solids in water from the three test wells ranges from 669 to 961 milligrams per liter. The recommended limits for chloride and fluoride were exceeded in water from test well 4N/10E-21K1, arsenic and fluoride in water from well 5N/9E-3B1, and chloride in water from test well 6N/9E-34F1. An estimated 640,000 acre-feet of water is stored in the alluvium west of the Ludlow fault, sufficient to provide for several small diameter wells for many years.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834053","usgsCitation":"Koehler, J.H., 1983, Ground water in the northeast part of Twentynine Palms Marine Corps Base, Bagdad area, California: U.S. Geological Survey Water-Resources Investigations Report 83-4053, iv, 15 p., https://doi.org/10.3133/wri834053.","productDescription":"iv, 15 p.","costCenters":[],"links":[{"id":415591,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35692.htm","linkFileType":{"id":5,"text":"html"}},{"id":56908,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4053/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123623,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4053/report-thumb.jpg"}],"country":"United States","state":"Calilfornia","otherGeospatial":"Twentynine Palms Marine Corps Base","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -116.74714785522053,\n 34.772980861725955\n ],\n [\n -116.74714785522053,\n 34.196058657436936\n ],\n [\n -115.70337642189573,\n 34.196058657436936\n ],\n [\n -115.70337642189573,\n 34.772980861725955\n ],\n [\n -116.74714785522053,\n 34.772980861725955\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d7b2","contributors":{"authors":[{"text":"Koehler, J. H.","contributorId":108108,"corporation":false,"usgs":true,"family":"Koehler","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":199198,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70164354,"text":"70164354 - 1983 - Active submarine volcano sampled","interactions":[],"lastModifiedDate":"2019-11-13T15:52:48","indexId":"70164354","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Active submarine volcano sampled","docAbstract":"On June 4, 1982, two full dredge hauls of fresh lava were recovered from the upper flanks of Kavachi submarine volcano, Solomon Islands, in the western Pacific Ocean, from the water depths of 1,200 and 2,700 feet. the shallower dredge site was within 0.5 mile of the active submarine vent shown at the surface by an area of slick water, probably caused by gas emissions. Kavachi is a composite stratovolcano that has been observed to erupt every year or two for at least the last 30 years (see photographs). An island formed in 1952, 1961, 1965, and 1978; but, in each case, it rapidly eroded below sea level. The latest eruption was observed by Solair pilots during the several weeks up to and including May 18, 1982.
","language":"English","publisher":"U.S Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Taylor, B., 1983, Active submarine volcano sampled: Earthquake Information Bulletin (USGS), v. 15, no. 4, p. 148-149.","productDescription":"2 p.","startPage":"148","endPage":"149","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":316431,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Soloman Islands","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 154.62158203125,\n -4.806364708499984\n ],\n [\n 154.31396484375,\n -5.025282908609298\n ],\n [\n 156.81884765625,\n -9.037002898469408\n ],\n [\n 159.76318359375,\n -10.055402736564224\n ],\n [\n 162.79541015624997,\n -10.984335146101955\n ],\n [\n 162.66357421875,\n -10.206813072484595\n ],\n [\n 154.62158203125,\n -4.806364708499984\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"15","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56b08fbbe4b010e2af2a5d2b","contributors":{"authors":[{"text":"Taylor, B.","contributorId":36683,"corporation":false,"usgs":true,"family":"Taylor","given":"B.","email":"","affiliations":[],"preferred":false,"id":597097,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70182080,"text":"70182080 - 1983 - Seabirds between Alaska and Hawaii","interactions":[],"lastModifiedDate":"2022-10-31T16:02:54.665624","indexId":"70182080","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3551,"text":"The Condor","active":true,"publicationSubtype":{"id":10}},"title":"Seabirds between Alaska and Hawaii","docAbstract":"Seabirds were observed between Alaska and Hawaii along 158°W longitude from 24 October to 6 November 1976. Their distributions and abundances corresponded remarkably well to oceanographic regions. Indices of seabird density dropped in a series of plateaus from 44 birds/km2 in the Alaska Current System to less than 1 bird/km2 in subtropic waters. Northern distribution records were found for six species. The Subarctic Boundary marked the center of the separation between subarctic and subtropic pelagic avifaunas.
","language":"English","publisher":"Cooper Ornithological Society","doi":"10.2307/1367061","usgsCitation":"Gould, P.J., 1983, Seabirds between Alaska and Hawaii: The Condor, v. 85, no. 3, p. 286-291, https://doi.org/10.2307/1367061.","productDescription":"6 p.","startPage":"286","endPage":"291","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":503097,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digitalcommons.usf.edu/condor/vol85/iss3/4","text":"External Repository"},{"id":335662,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska, Hawaii","otherGeospatial":"North Pacific 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\"}}]}","volume":"85","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a5770ce4b057081a24eec0","contributors":{"authors":[{"text":"Gould, Patrick J.","contributorId":11667,"corporation":false,"usgs":true,"family":"Gould","given":"Patrick","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":669485,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70180857,"text":"70180857 - 1983 - Use of nearshore and estuarine areas by gray whales (Eschrichtius robustus) in the eastern Bering Sea","interactions":[],"lastModifiedDate":"2018-05-20T11:33:37","indexId":"70180857","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":894,"text":"Arctic","active":true,"publicationSubtype":{"id":10}},"title":"Use of nearshore and estuarine areas by gray whales (Eschrichtius robustus) in the eastern Bering Sea","docAbstract":"During spring aerial surveys of the coast of the southeastern Bering Sea significant numbers of gray whales were seen in nearshore waters along the north side of the Alaska Peninsula. Many (50-80%) of these animals were observed surfacing with mud trails or lying on their sides, characteristics both associated with feeding. A migration route close to shore (within 1-2 km) was used until whales neared Egegik Bay, where they began to head west 5-8 km offshore, across northern Bristol Bay. Smaller numbers of gray whales were present throughout summer in nearshore waters and estuaries along the north side of the Alaska Peninsula. At Nelson Lagoon gray whales normally used the lagoon in spring, were absent during early summer, returned in mid-summer, and then were present until late November when they departed for the wintering grounds. Gray whales were present in the lagoon most often during periods of peak tidal flow; those that appeared to be feeding were oriented into the current. Three behaviors that appeared to be associated with feeding were observed: side-feeding from a stationary position within shallow waters of lagoon channels, diving within the lagoon and in nearshore waters, and elliptical side-feeding in the surf zone along the outer coast. Large crustaceans of the genus Crangon were available to and probably eaten by gray whales at Nelson Lagoon.
","language":"English","publisher":"Arctic Institute of North America","publisherLocation":"Calgary, AB","doi":"10.14430/arctic2276","usgsCitation":"Gill, R., and Hall, J.D., 1983, Use of nearshore and estuarine areas by gray whales (Eschrichtius robustus) in the eastern Bering Sea: Arctic, v. 36, no. 3, p. 275-281, https://doi.org/10.14430/arctic2276.","productDescription":"7 p.","startPage":"275","endPage":"281","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"links":[{"id":480225,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.14430/arctic2276","text":"Publisher Index Page"},{"id":334784,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Bering Sea","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -167.03613281249997,\n 54.08517342088679\n ],\n [\n -167.03613281249997,\n 59.80063426102869\n ],\n [\n -154.3359375,\n 59.80063426102869\n ],\n [\n -154.3359375,\n 54.08517342088679\n ],\n [\n -167.03613281249997,\n 54.08517342088679\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"36","issue":"3","noUsgsAuthors":false,"publicationDate":"1983-01-01","publicationStatus":"PW","scienceBaseUri":"589847abe4b0efcedb7072e5","contributors":{"authors":[{"text":"Gill, Robert E. Jr. 0000-0002-6385-4500 rgill@usgs.gov","orcid":"https://orcid.org/0000-0002-6385-4500","contributorId":171747,"corporation":false,"usgs":true,"family":"Gill","given":"Robert E.","suffix":"Jr.","email":"rgill@usgs.gov","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":662612,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hall, John D. 0000-0002-7670-5459","orcid":"https://orcid.org/0000-0002-7670-5459","contributorId":179094,"corporation":false,"usgs":false,"family":"Hall","given":"John","email":"","middleInitial":"D.","affiliations":[{"id":28155,"text":"Century Engineering, Anchorage, AK","active":true,"usgs":false}],"preferred":false,"id":662613,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70185619,"text":"70185619 - 1983 - Complexation of copper by aquatic humic substances from different environments","interactions":[],"lastModifiedDate":"2020-01-20T19:52:46","indexId":"70185619","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3352,"text":"Science of the Total Environment","active":true,"publicationSubtype":{"id":10}},"title":"Complexation of copper by aquatic humic substances from different environments","docAbstract":"The copper-complexing properties of aquatic humic substances isolated from eighteen different environments were characterized by potentiometric titration, using a cupric ion selective electrode. Potentiometric data were analyzed using FITEQL, a computer program for the determination of chemical equilibrium constants from experimental data. All the aquatic humic substances could be modelled as having two types of Cu(II)-binding sites: one with K equal to about 106 and a concentration of 1.0 ± 0.4 × 10−6 M(mg C)−1 and another with K equal to about 108 and a concentration of 2.6 ± 1.6 × 10−7 M(mg C)−1.
A method is described for estimating the Cu(II)-binding sites associated with dissolved humic substances in natural water based on a measurement of dissolved organic carbon, which may be helpful in evaluating chemical processes controlling speciation of Cu and bioavailability of Cu to aquatic organisms.
","language":"English","publisher":"Elsevier","doi":"10.1016/S0048-9697(83)80008-4","usgsCitation":"McKnight, D.M., Feder, G., Thurman, E.M., and Wershaw, R.L., 1983, Complexation of copper by aquatic humic substances from different environments: Science of the Total Environment, v. 28, no. 1-3, p. 65-76, https://doi.org/10.1016/S0048-9697(83)80008-4.","productDescription":"12 p. ","startPage":"65","endPage":"76","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338320,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d63040e4b05ec799131119","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":686132,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Feder, Gerald L.","contributorId":60192,"corporation":false,"usgs":true,"family":"Feder","given":"Gerald L.","affiliations":[],"preferred":false,"id":686133,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thurman, E. Michael","contributorId":9636,"corporation":false,"usgs":true,"family":"Thurman","given":"E.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":686134,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"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":686135,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70184465,"text":"70184465 - 1983 - Yellow birds stand out in a crowd","interactions":[],"lastModifiedDate":"2018-05-20T11:33:23","indexId":"70184465","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2881,"text":"North American Bird Bander","active":true,"publicationSubtype":{"id":10}},"title":"Yellow birds stand out in a crowd","docAbstract":"Highly visible auxiliary markers, such as neck collars, nasal saddles, patagial tags, and leg streamers, are used regularly and effectively with banding in studying migration and distribution of large birds (e.g. waterfowl, birds of prey, wading birds). Simply stated, a large bird can accommodate a marker that is large enough to be seen readily by an observer but still small enough not to alter behavior or impair flight (see Marion and Shamis 1977 for review). Such is not true with smaller birds, and consequently information on their migration routes and distribution is usually poorer than for larger birds. The use of colored leg bands increases the frequency of detection of small birds that have been banded; however, a large percentage of such marked birds is usually still overlooked. Only by using highly visible techniques, such as plumage dyes and bleaches in conjunction with leg bands, can one obtain significant numbers of sightings of small birds. Here we present information from sightings of large numbers of marked Dunlins (Calidris alpina) and Western Sandpipers (C. mauri) that dramatically demonstrates this.
","language":"English","publisher":"Western, Inland, and Eastern Bird Banding Associations","usgsCitation":"Handel, C.M., and Gill, R., 1983, Yellow birds stand out in a crowd: North American Bird Bander, v. 8, no. 1, p. 6-9.","productDescription":"4 p.","startPage":"6","endPage":"9","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":337249,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":337243,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.westernbirdbanding.org/publications_NABB.html","text":"Journal's Website"}],"volume":"8","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58c277fae4b014cc3a3e770c","contributors":{"authors":[{"text":"Handel, Colleen M. 0000-0002-0267-7408 cmhandel@usgs.gov","orcid":"https://orcid.org/0000-0002-0267-7408","contributorId":3067,"corporation":false,"usgs":true,"family":"Handel","given":"Colleen","email":"cmhandel@usgs.gov","middleInitial":"M.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":681624,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gill, Robert E. Jr. 0000-0002-6385-4500 rgill@usgs.gov","orcid":"https://orcid.org/0000-0002-6385-4500","contributorId":171747,"corporation":false,"usgs":true,"family":"Gill","given":"Robert E.","suffix":"Jr.","email":"rgill@usgs.gov","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":681625,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70184255,"text":"70184255 - 1983 - Detection of infectious hematopoietic necrosis virus in river water and demonstration of waterborne transmission","interactions":[],"lastModifiedDate":"2017-03-06T09:59:58","indexId":"70184255","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2286,"text":"Journal of Fish Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Detection of infectious hematopoietic necrosis virus in river water and demonstration of waterborne transmission","docAbstract":"In a study of the possible role of waterborne infectious haematopoietic necrosis virus in transmission of the disease among spawning sockeye salmon, Oncorhynchus nerka (Walbaum), both infection rates and virus titres were higher in fish held at high density in a side channel than in fish in the adjacent river. Virus was never isolated from river water, but was found in water from the side channel at levels ranging from 32.5 to 1600 plaque-forming units (p.f.u.)/ml. Uninfected yearling sockeye salmon held in a box in the side channel developed localized gill infections with IHN virus. The disease did not progress to the viscera until a threshold titre of about 105 p.f.u./g was reached in the gill. The effectiveness of the gill as a barrier limiting development of systemic infections means that waterborne IHN virus probably does not greatly increase the infection rate in a sockeye salmon population during spawning.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1365-2761.1983.tb00083.x","usgsCitation":"Mulcahy, D.M., Pascho, R.J., and Jenes, C., 1983, Detection of infectious hematopoietic necrosis virus in river water and demonstration of waterborne transmission: Journal of Fish Diseases, v. 6, no. 4, p. 321-330, https://doi.org/10.1111/j.1365-2761.1983.tb00083.x.","productDescription":"10","startPage":"321","endPage":"330","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":336847,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Cedar River","volume":"6","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-04-07","publicationStatus":"PW","scienceBaseUri":"58be8350e4b014cc3a3a9a53","contributors":{"authors":[{"text":"Mulcahy, Daniel M. dmulcahy@usgs.gov","contributorId":3102,"corporation":false,"usgs":true,"family":"Mulcahy","given":"Daniel","email":"dmulcahy@usgs.gov","middleInitial":"M.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":680752,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pascho, Ronald J.","contributorId":177070,"corporation":false,"usgs":false,"family":"Pascho","given":"Ronald","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":680753,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jenes, C.K.","contributorId":152262,"corporation":false,"usgs":false,"family":"Jenes","given":"C.K.","email":"","affiliations":[],"preferred":false,"id":680754,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70185617,"text":"70185617 - 1983 - Partition equilibriums of nonionic organic compounds between soil organic matter and water","interactions":[],"lastModifiedDate":"2020-01-20T19:51:56","indexId":"70185617","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Partition equilibriums of nonionic organic compounds between soil organic matter and water","docAbstract":"No abstract available.
","language":"English","publisher":"American Chemical Society","doi":"10.1021/es00110a009","usgsCitation":"Chiou, C.T., Porter, P.E., and Schmedding, D.W., 1983, Partition equilibriums of nonionic organic compounds between soil organic matter and water: Environmental Science & Technology, v. 17, no. 4, p. 227-231, https://doi.org/10.1021/es00110a009.","productDescription":"5 p. ","startPage":"227","endPage":"231","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338318,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"4","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"58d63041e4b05ec79913111d","contributors":{"authors":[{"text":"Chiou, Cary T. 0000-0002-8743-0702","orcid":"https://orcid.org/0000-0002-8743-0702","contributorId":189558,"corporation":false,"usgs":true,"family":"Chiou","given":"Cary","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":686128,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Porter, Paul E.","contributorId":189805,"corporation":false,"usgs":false,"family":"Porter","given":"Paul","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":686129,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schmedding, David W.","contributorId":189818,"corporation":false,"usgs":false,"family":"Schmedding","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":686130,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":30341,"text":"wri824093 - 1982 - Effects of land use on ground-water quality in the East Everglades, Dade County, Florida","interactions":[],"lastModifiedDate":"2021-12-13T12:30:20.981613","indexId":"wri824093","displayToPublicDate":"2021-12-12T20:45:00","publicationYear":"1982","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":"82-4093","title":"Effects of land use on ground-water quality in the East Everglades, Dade County, Florida","docAbstract":"Groundwater quality characteristics of the Biscayne aquifer from September 1978 through June 1979 were determined for seven land use areas within the East Everglades in Dade County, Florida. Four agricultural areas, two low-density residential areas, and Chekika Hammock State Park were investigated. The effects of land use on the groundwater were minimal in all areas; only iron , which occurs naturally in high concentrations in the Everglades, exceeded potable groundwater standards. Potassium and nitrate concentrations in certain samples increased over background concentrations in the agricultural areas. Groundwater at Chekika Hammock State Park and at a citrus grove is contaminated by brackish water flowing from an artesian well. The soil at the agricultural areas had higher concentrations of chromium, copper, and manganese than at the two residential areas or at Chekika Hammock State Park. One residential area (Coopertown) had the highest concentrations of lead and zinc and detectable polychlorinated biphenyls. Chlorinated-hydrocarbon insecticide residues in soil at three agricultural areas were higher than background concentrations. (Author 's abstract)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri824093","collaboration":"Prepared in cooperation with the Metropolitan Dade County Planning Department","usgsCitation":"Waller, B., 1982, Effects of land use on ground-water quality in the East Everglades, Dade County, Florida: U.S. Geological Survey Water-Resources Investigations Report 82-4093, viii, 75 p., https://doi.org/10.3133/wri824093.","productDescription":"viii, 75 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":124279,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4093/coverthb.jpg"},{"id":59134,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4093/wri824093.pdf","text":"Report","size":"1.56 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 82-4093"}],"country":"United States","state":"Florida","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.66162109375,\n 25.18505888358067\n ],\n [\n -79.98046875,\n 25.18505888358067\n ],\n [\n -79.98046875,\n 25.997549919572112\n ],\n [\n -80.66162109375,\n 25.997549919572112\n ],\n [\n -80.66162109375,\n 25.18505888358067\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMDDE811","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data for Maryland and Delaware, water year 1981: U.S. Geological Survey Water Data Report MD-DE-81-1, 503 p., https://doi.org/10.3133/wdrMDDE811.","productDescription":"503 p.","costCenters":[{"id":41514,"text":"Maryland-Delaware-District of Columbia Water Science Center","active":true,"usgs":true}],"links":[{"id":184414,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1981/md-de-81-1/wdrMDDE811_coverthb.jpg"},{"id":381780,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1981/md-de-81-1/wdrMDDE811.pdf","text":"Report","size":"21.4 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Water Data Report MD-DE-81-1"}],"country":"United States","state":"Delaware, 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\"}}]}","contact":"","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f4636","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532960,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":126,"text":"wsp2175 - 1982 - Measurement and computation of streamflow","interactions":[],"lastModifiedDate":"2020-01-15T10:30:44","indexId":"wsp2175","displayToPublicDate":"2020-01-15T11:35:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2175","displayTitle":"Measurement and Computation of Streamflow","title":"Measurement and computation of streamflow","docAbstract":"The purpose of this manual is to provide a comprehensive description of state-of-the-art standardized stream-gaging procedures, within the scope described below. The manual is intended for use as a training guide and reference text, primarily for hydraulic engineers and technicians in the U.S. Geological Survey, but the manual is also appropriate for use by other stream-gaging practitioners, both in the United States and elsewhere.
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