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Three sites on two cold-water trout streams Black Earth Creek at Cross Plains, Black Earth Creek near Cross Plains, and Garfoot Creek near Cross Plains were continuously monitored for streamflow and water-quality data. One site in a warm-water stream, Brewery Creek at Cross Plains, also was monitored. Aquatic macrophyte biomass was determined for three sites on Black Earth Creek.</p>\n<p>Streamflow at Black Earth Creek at Black Earth during the 1985 and 1986 water years (WY) were 44 and 60 percent greater than the long-term mean discharge of 33.3 ft3/s (cubic feet per second) for the period 1955-86. Water year 1986 had the highest annual mean discharge, 53.4 ft3/s, since records began in 1954 at the most downstream site Black Earth Creek at Black Earth. Although there have been considerable fluctuations in streamflow, it has tended to increase since WY 1965 as a result of above-average precipitation and consequent rising ground-water levels.</p>\n<p>Trout population densities may be related to annual mean streamflow. A regression analysis of adult trout populations and the 3-year moving annual mean discharge had a correlation coefficient of 0.75 with a standard error of 83 percent.</p>\n<p>Aquatic macrophyte biomass in Black Earth Creek was substantially less in 1986 than in 1985 as a result of substrate scouring from the flood of July 25, 1985. The frequency of occurrence of species during 1985 and 1986 was similar to that of 1981, and seasonal succession of species also was similar; Potamogeton crispus dominated early in the year and senesced in July. P. crispus and P. pectinatus, both indicative of eutrophic conditions, dominated upstream and downstream, respectively; neither species is native to the area. In 1985, the greatest biomass was found upstream from Cross Plains. This large biomass caused diurnal fluctuations in dissolved-oxygen concentration of 5 to 6 mg/L (milligrams per liter) as a result of photosynthesis and respiration. Many of the dissolved-oxygen minimums, recorded at night, were less than the State 6.0-mg/L water-quality standard for trout waters. Discharge from point sources may adversely affect Black Earth Creek's water quality. Warm water discharged to Black Earth Creek from a gravel pit operation upstream from Cross Plains increased water temperatures 2 to 4 degrees Celsius and decreased the dissolved oxygen about 1 mg/L at a site 1.8 miles downstream. Runoff from a settling pond from a landfill operation in the headwaters of the Black Earth Creek basin drains through a wetland that drains to Black Earth Creek and contained as much as 60 mg/L ammonia nitrogen, 980 mg/L biochemical oxygen demand, and 1,300 mg/L chemical oxygen demand, which may be detrimental to trout.</p>\n<p>Garfoot Creek had the highest suspended-sediment and phosphorus yields per unit area of the three upstream basins during low to moderate runoff. Detention ponds in the Brewery Creek basin appear to be less effective in controlling suspended-sediment and phosphorus loads during periods of high runoff than during moderate runoff. Brewery Creek had the highest concentrations of suspended sediment and total phosphorus during low and high flows. The water quality at the Black Earth Creek gaging station at Black Earth was affected by Garfoot Creek and unnamed tributaries. As a result, yields of suspended sediment, phosphorus, and nitrogen increased between Cross Plains and Black Earth. High streamflows during WY 1985 resulted in suspendedsediment yields at Black Earth Creek at Black Earth that were 29 percent greater than the 12-year (1955-65, 85-86) mean; yields ranged from 69.5 ton/mi2 (tons per square mile) in Black Earth Creek at Cross Plains to 116 ton/mi2 in the Brewery Creek basin. Phosphorus yields ranged from 312 lb/mi2 (pounds per square mile) in Black Earth Creek at Cross Plains to 628 lb/mi2 in the Brewery Creek basin. Total nitrogen yields ranged from 3,280 lb/mi2 in the Brewery Creek basin to 6,920 lb/mi2 in the Garfoot Creek basin.</p>\n<p>An increase in oxygen demand, caused by agricultural runoff, has resulted in reduced dissolved-oxygen content of the water in both Black Earth and Garfoot Creeks. The most substantial reduction occurred at Black Earth Creek at Cross Plains on July 25, 1985, as a result of the largest storm runoff event during the study. A rainfall of 5.54 inches caused streamflow discharges to increase from 9 to 122 ft3/s and dissolved-oxygen concentrations to decline to 3.0 mg/L; the dissolved-oxygen concentration was less than 6.0 mg/L for 30 hours.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri894089","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Field, S.J., and Graczyk, D., 1990, Hydrology, aquatic macrophytes, and water quality of Black Earth Creek and its tributaries, Dane County, Wisconsin, 1985-86: U.S. Geological Survey Water-Resources Investigations Report 89-4089, vi, 38 p., https://doi.org/10.3133/wri894089.","productDescription":"vi, 38 p.","numberOfPages":"44","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":55953,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4089/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122886,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4089/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","county":"Dane County","otherGeospatial":"Black Earth Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.72911834716797,\n              43.18440150752066\n            ],\n            [\n              -89.791259765625,\n              43.09170711357466\n            ],\n            [\n              -89.66697692871094,\n              43.06838615478111\n            ],\n            [\n              -89.54132080078125,\n              43.04555812998933\n            ],\n            [\n              -89.53239440917969,\n              43.11401670811261\n            ],\n            [\n              -89.51934814453125,\n              43.13130731581085\n            ],\n            [\n              -89.52587127685547,\n              43.14082759275761\n            ],\n            [\n              -89.72911834716797,\n              43.18440150752066\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc71d","contributors":{"authors":[{"text":"Field, S. J.","contributorId":50540,"corporation":false,"usgs":true,"family":"Field","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":197532,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Graczyk, D.J.","contributorId":108119,"corporation":false,"usgs":true,"family":"Graczyk","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":197533,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27128,"text":"wri864195 - 1990 - Technique for estimating depths of 100-year floods in Pennsylvania","interactions":[],"lastModifiedDate":"2017-07-05T11:24:39","indexId":"wri864195","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"86-4195","title":"Technique for estimating depths of 100-year floods in Pennsylvania","docAbstract":"<p>Techniques are developed for estimating 100-year flood depths in natural channels of unregulated Pennsylvania streams that drain less than 2,200 square miles. Equations and graphs are presented relating the depth of the 100-year flood above median stage and drainage area in five defined hydrologic areas in the State. Another graph defines the relation between drainage area and median depth of flow over the low point of riffles. Thus 100-year depths on riffles can be estimated by summing depth values derived from two simple relations.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864195","usgsCitation":"Flippo, H.N., 1990, Technique for estimating depths of 100-year floods in Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 86-4195, Report: iv, 16 p.; 1 Plate: 21.38 x 16.49 inches, https://doi.org/10.3133/wri864195.","productDescription":"Report: iv, 16 p.; 1 Plate: 21.38 x 16.49 inches","numberOfPages":"21","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":310317,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4195/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":158728,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri864195.jpg"},{"id":310318,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4195/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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Jr.","contributorId":36597,"corporation":false,"usgs":true,"family":"Flippo","given":"Herbert","suffix":"Jr.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":197600,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27249,"text":"wri904096 - 1990 - Water quality characteristics of inflow to and outflow from B. Everett Jordan Lake, North Carolina, 1982-86","interactions":[],"lastModifiedDate":"2025-01-10T19:27:32.634281","indexId":"wri904096","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-4096","title":"Water quality characteristics of inflow to and outflow from B. Everett Jordan Lake, North Carolina, 1982-86","docAbstract":"B. Everett Jordan Lake, a 13,900-acre reservoir in the north-central Piedmont of North Carolina, was completed in February 1982. Hydrologic data were collected at four inflow sites and one outflow site to define water-quality characteristics. Data include streamflow data and 56 physical and chemical characteristics of streamwater. Concentrations of some constituents at inflow sites were as much as 83-times greater than background concentrations in streams relatively unaffected by man. At the outflow site, however, some of these constituents were only as much as 6-times greater. The minimum dissolved-oxygen concentration measured at an inflow site was 1.0 mg/L, whereas the minimum concentration measured at the outflow site was 4.9 mg/L. Significant differences in other physical characteristics between inflow and outflow sites include a reduction in maximum concentration of suspended sediment from 2,360 mg/L in an inflow sample to 130 mg/L at the outflow site and a reduction of maximum specific conductance values from more than 1,100 microsiemens/centimeter in an inflow sample to 301 microsiemens/centimeter in outflow. The maximum concentration of total nitrogen at inflow sites was 27.0 mg/L compared with 3.2 mg/L at the outflow site. The maximum total phosphorus concentration at inflow sites was 13.0 mg/L compared with 0.6 mg/L at the outflow site. Average annual loads of total nitrogen and total phosphorus in the outflow were as much as 67% and 40% of inflow loads, respectively. Maximum yields at an inflow site were 5.8 t/sq mi (tons per square mile) for nitrogen and 1.4 t/sq mi for phosphorus. Yields of these constituents at the outflow site were 1.5 and 0.2 t/mi, respectively.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri904096","usgsCitation":"Garrett, R.G., 1990, Water quality characteristics of inflow to and outflow from B. Everett Jordan Lake, North Carolina, 1982-86: U.S. Geological Survey Water-Resources Investigations Report 90-4096, v, 49 p., https://doi.org/10.3133/wri904096.","productDescription":"v, 49 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":158755,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4096/report-thumb.jpg"},{"id":393481,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47361.htm"},{"id":56115,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4096/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Carolina","otherGeospatial":"B. Everett Jordan Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.13177490234375,\n              35.51434313431818\n            ],\n            [\n              -78.90380859375,\n              35.51434313431818\n            ],\n            [\n              -78.90380859375,\n              35.93798832265393\n            ],\n            [\n              -79.13177490234375,\n              35.93798832265393\n            ],\n            [\n              -79.13177490234375,\n              35.51434313431818\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697d3f","contributors":{"authors":[{"text":"Garrett, R. G.","contributorId":93929,"corporation":false,"usgs":true,"family":"Garrett","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":197796,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27250,"text":"wri904097 - 1990 - Water-quality characteristics of inflow to and outflow from Falls Lake, North Carolina, 1982-87","interactions":[],"lastModifiedDate":"2025-01-10T19:36:38.908915","indexId":"wri904097","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-4097","title":"Water-quality characteristics of inflow to and outflow from Falls Lake, North Carolina, 1982-87","docAbstract":"Falls Lake, an 11,300-acre reservoir in the north-central Piedmont of North Carolina, was completed in December 1983. Hydrologic data were collected at seven inflow sites and one outflow site between 1982 and 1987 to define water-quality characteristics. Data include streamflow data and 56 physical and chemical characteristics of streamwater. Concentrations of some constituents at inflow sites were as much as 10-to 110-times greater than background concentrations in streams relatively unaffected by man. At the outflow site, these constituents generally were 2-to 3-times greater than background values. The minimum dissolved-oxygen concentration measured at an inflow site was 0.6 mg/L, whereas the minimum concentration measured at the outflow site was 6.7 milligrams per liter. Significant differences in other physical characteristics between inflow and outflow sites include a reduction in maximum concentration of suspended sediment from 1,850 milligrams per liter in an inflow sample to 100 milligrams per liter in an outflow sample, and a reduction of maximum specific-conductance values from more than 1,200 microsiemens/centimeter in an inflow sample to 140 microsiemens per centimeter in the outflow. The maximum concentration of total nitrogen at inflow sites was 33 milligrams per liter compared with 4.5 milligrams per liter at the outflow site. Similarly, the maximum total phosphorus concentration at inflow sites was 20 milligrams per liter, but 0.22 milligrams per liter at the outflow site. Average annual loads of nitrogen and phosphorus in the outflow were as much as 66 percent and 21 percent of inflow loads, respectively. Although maximum inflow yields were 13 tons per square mile for nitrogen and 2.8 tons per square mile for phosphorus, yields of these constituents at the outflow site were about 1.1 and 0.05 tons per square mile, respectively.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri904097","usgsCitation":"Garrett, R.G., 1990, Water-quality characteristics of inflow to and outflow from Falls Lake, North Carolina, 1982-87: U.S. Geological Survey Water-Resources Investigations Report 90-4097, v, 56 p., https://doi.org/10.3133/wri904097.","productDescription":"v, 56 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":126707,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4097/report-thumb.jpg"},{"id":56116,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4097/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":466031,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47362.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"North Carolina","otherGeospatial":"Falls Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -78.87095876391315,\n              36.24178484124681\n            ],\n            [\n              -78.87095876391315,\n              35.8769278093385\n            ],\n            [\n              -78.51633998817118,\n              35.8769278093385\n            ],\n            [\n              -78.51633998817118,\n              36.24178484124681\n            ],\n            [\n              -78.87095876391315,\n              36.24178484124681\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e715f","contributors":{"authors":[{"text":"Garrett, R. G.","contributorId":93929,"corporation":false,"usgs":true,"family":"Garrett","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":197797,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30601,"text":"wri904134 - 1990 - Ground-water hydrology and quality in the Valley and Ridge and Blue Ridge physiographic provinces of Clarke County, Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:09:12","indexId":"wri904134","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-4134","title":"Ground-water hydrology and quality in the Valley and Ridge and Blue Ridge physiographic provinces of Clarke County, Virginia","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri904134","usgsCitation":"Wright, W.G., 1990, Ground-water hydrology and quality in the Valley and Ridge and Blue Ridge physiographic provinces of Clarke County, Virginia: U.S. Geological Survey Water-Resources Investigations Report 90-4134, vi, 61 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri904134.","productDescription":"vi, 61 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123106,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4134/report-thumb.jpg"},{"id":59359,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4134/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668d30","contributors":{"authors":[{"text":"Wright, W. G.","contributorId":19582,"corporation":false,"usgs":true,"family":"Wright","given":"W.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":203519,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27955,"text":"wri904021 - 1990 - Methods for selection and hydrologic description of potential landfill sites in southeastern San Diego County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:36","indexId":"wri904021","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-4021","title":"Methods for selection and hydrologic description of potential landfill sites in southeastern San Diego County, California","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri904021","usgsCitation":"Kaehler, C., 1990, Methods for selection and hydrologic description of potential landfill sites in southeastern San Diego County, California: U.S. Geological Survey Water-Resources Investigations Report 90-4021, v, 73 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri904021.","productDescription":"v, 73 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":126461,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4021/report-thumb.jpg"},{"id":56763,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4021/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8e0c","contributors":{"authors":[{"text":"Kaehler, C. A.","contributorId":59469,"corporation":false,"usgs":true,"family":"Kaehler","given":"C. A.","affiliations":[],"preferred":false,"id":198963,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27448,"text":"wri904167 - 1990 - Gaged and estimated monthly streamflow during 1931-84 for selected sites in the Red River of the North basin in North Dakota and Minnesota","interactions":[],"lastModifiedDate":"2023-01-05T19:19:04.827574","indexId":"wri904167","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-4167","title":"Gaged and estimated monthly streamflow during 1931-84 for selected sites in the Red River of the North basin in North Dakota and Minnesota","docAbstract":"<p>Operation of the Garrison Diversion Unit in North Dakota may have various effects on the quantity and quality of streamflow in the Sheyenne River and the Red River of the North. To model the effects that the Garrison Diverson Unit could have on water quantity, monthly gaged and estimated streamflow data and estimated unregulated streamflow data were compiled to develop a complete monthly streamflow record for January 1931 through December 1984 (data-development period) for 29 sites in the Red River of the North basin.</p><p>Gaged streamflow records were available for January 1931 through December 1984 for only 4 sites; no records or records of various length were available for the remaining 25 sites. Drainage-area ratio and Maintenance of Variance Extension Type 1 methods were used to estimate the streamflow for those sites that had no streamflow record or had a streamflow record available for only part of the data-development period.</p><p>Unregulated streamflow for the 29 sites was estimated by removing the hydrologic effects of Lake Ashtabula, which is formed behind Baldhill Dam on the Sheyenne River, and surface-water withdrawals. VIater-balance procedures were used to remove the hydrologic effects of Lake Ashtabula from the streamflow record for sites downstream of Baldhill Dam. </p><p>Mean annual gaged streamflow for the Sheyenne River below Baldhill Dam was 9,175 acre-feet less than mean annual estimated unregulated streamflow for 1950-84, when Baldhill Dam was in operation. Net evaporation losses from Lake Ashtabula account for most of the difference between gaged streamflow and estimated unregulated streamflow. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri904167","usgsCitation":"Guenthner, R., Weigel, J.F., and Emerson, D.G., 1990, Gaged and estimated monthly streamflow during 1931-84 for selected sites in the Red River of the North basin in North Dakota and Minnesota: U.S. Geological Survey Water-Resources Investigations Report 90-4167, Report: vi, 230 p.; 1 Plate: 21.28 x 15.64 inches, https://doi.org/10.3133/wri904167.","productDescription":"Report: vi, 230 p.; 1 Plate: 21.28 x 15.64 inches","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":56307,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4167/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56306,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1990/4167/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":126801,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4167/report-thumb.jpg"},{"id":411441,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47416.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Minnesota, North Dakota","otherGeospatial":"Red River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -94.5,\n              49\n            ],\n            [\n              -100.6667,\n              49\n            ],\n            [\n              -100.6667,\n              45.75\n            ],\n            [\n              -94.5,\n              45.75\n            ],\n            [\n              -94.5,\n              49\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1460","contributors":{"authors":[{"text":"Guenthner, R. S.","contributorId":31433,"corporation":false,"usgs":true,"family":"Guenthner","given":"R. S.","affiliations":[],"preferred":false,"id":198134,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weigel, J. F.","contributorId":74394,"corporation":false,"usgs":true,"family":"Weigel","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":198136,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Emerson, D. G.","contributorId":39385,"corporation":false,"usgs":true,"family":"Emerson","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":198135,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":18606,"text":"ofr89595 - 1990 - Hydrologic, meteorological, and unsaturated-zone moisture-content data, Franklin Lake Playa, Inyo County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:07:25","indexId":"ofr89595","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"89-595","title":"Hydrologic, meteorological, and unsaturated-zone moisture-content data, Franklin Lake Playa, Inyo County, California","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey :\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr89595","usgsCitation":"Czarnecki, J., 1990, Hydrologic, meteorological, and unsaturated-zone moisture-content data, Franklin Lake Playa, Inyo County, California: U.S. Geological Survey Open-File Report 89-595, iv, 38 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89595.","productDescription":"iv, 38 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":150864,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0595/report-thumb.jpg"},{"id":47947,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0595/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e99a","contributors":{"authors":[{"text":"Czarnecki, J.B.","contributorId":51768,"corporation":false,"usgs":true,"family":"Czarnecki","given":"J.B.","affiliations":[],"preferred":false,"id":179422,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20949,"text":"ofr8884 - 1990 - Hydrologic and water-quality data for streams and impoundments in the Coteau des Prairies-Upper Minnesota River basin, 1979-84","interactions":[],"lastModifiedDate":"2018-04-02T11:02:53","indexId":"ofr8884","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"88-84","title":"Hydrologic and water-quality data for streams and impoundments in the Coteau des Prairies-Upper Minnesota River basin, 1979-84","docAbstract":"<p>Water-quality and streamflow data were collected in the Coteau des Prairies region of southwestern Minnesota and eastern South Dakota from 1979- 84. Data were collected to (1) document the water-quality characteristics of streams and impoundments in the Coteau area, (2) predict the impact of proposed impoundments, (3) define the amount of dissolved and suspended material transported, and (4) determine the differences in water quality between the impoundment inflows and outflows.</p>\n<p>Streamflow and water-quality data were collected at 12 stream and four impoundment sites. Continuous-record gages, set to collect data at 15-minute intervals, and readings taken by local observers were used to complete discharge records at 10 stream sites and stage records at three impoundment sites. Automatic samplers and local observers collected storm runoff, sediment, and nutrient samples at 10 stream sites. Water-quality samples were collected at various time and stage intervals during high flow and periodically during low flow. Primary emphasis in the stream-sampling program was on analysis of samples for nutrients in 1980-82, and on analysis of suspended sediment and nutrients in 1983-84. Field measurements were made of pH, water temperature, dissolved oxygen, specific conductance, alkalinity, and bacteria. Secondary emphasis was on analysis of major dissolved substances. Primary emphasis in the impoundments was on analysis of samples for phosphorus and chlorophyll and on the measurement of transparency. Temperature and dissolved-oxygen concentrations were measured to determine the degree of stratification.</p>\n<p>All data collected during the study are given in tables 4-13 of this report. The tables list mean-daily stream discharge, mean-daily suspendedsediment concentration, daily suspended-sediment discharge, results of waterquality analyses, and bed-material particle-size analyses at stream sites. The tables also list information on pool stage, water temperature, and transparency, on dissolved-oxygen, chlorophyll a, phytoplankton, and nutrient concentrations, and on chemical and partical-size analyses of bed material at impoundment sites.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr8884","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers, U.S. Soil Conservation Service","usgsCitation":"Smith, C., Payne, G.A., and Tornes, L., 1990, Hydrologic and water-quality data for streams and impoundments in the Coteau des Prairies-Upper Minnesota River basin, 1979-84: U.S. Geological Survey Open-File Report 88-84, vii, 46 p., https://doi.org/10.3133/ofr8884.","productDescription":"vii, 46 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":154108,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0084/report-thumb.jpg"},{"id":50535,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0084/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Coteau des Prairies-Upper Minnesota River basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611718","contributors":{"authors":[{"text":"Smith, C.J.","contributorId":69141,"corporation":false,"usgs":true,"family":"Smith","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":183560,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Payne, G. A.","contributorId":62190,"corporation":false,"usgs":true,"family":"Payne","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":183559,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tornes, L. H.","contributorId":103675,"corporation":false,"usgs":true,"family":"Tornes","given":"L. H.","affiliations":[],"preferred":false,"id":183561,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3163,"text":"wsp2368B - 1990 - Effects of surface coal mining and reclamation on the geohydrology of six small watersheds in West-Central Indiana","interactions":[],"lastModifiedDate":"2016-06-21T09:29:24","indexId":"wsp2368B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"2368","chapter":"B","title":"Effects of surface coal mining and reclamation on the geohydrology of six small watersheds in West-Central Indiana","docAbstract":"<p>Six small watersheds in west-central Indiana were selected for study of the hydrologic effects of surface coal mining and reclamation. The watersheds include mined and reclaimed, mined and unreclaimed, and unmined agricultural land uses and are each less than 3 square miles in area. Surface-water, ground-water, and meteorologic data for the 1981 and 1982 water years were used to describe and compare hydrologic systems of the six watersheds and to identify hydrologic effects of mining and reclamation.</p>\n<p>Discharge at the unreclaimed watersheds was continuous during the study period, whereas discharge at the other watersheds was intermittent and more variable. Peak discharges were greater at the agricultural watersheds than at the unreclaimed watersheds, primarily because of large final-cut lakes in the unreclaimed watersheds. Annual runoff was greatest at the unreclaimed watersheds, intermediate at the agricultural watersheds, and least at the reclaimed watersheds.</p>\n<p>Hydrologic effects of mining were identified by comparing the hydrologic systems at mined and unreclaimed watersheds with those at unmined agricultural watersheds. These comparisons indicate that surface coal mining without reclamation can increase base flow, annual runoff, and ground-water recharge to the bedrock; reduce peak flow rates and variation in flow; lower the water table in upland areas; change the relation between surface- and ground-water divides; and create numerous, local flow systems in the shallow ground water. Hydrologic effects of reclamation were identified by comparing the hydrologic systems at mined and reclaimed watersheds with those at mined and unreclaimed watersheds. Reclamation can decrease base flow, annual runoff, and recharge to the bedrock; increase peak flow rates, variation in flow, and the response to thunderstorms; reestablish the premining relation between surface- and ground-water divides; and create fewer local flow systems in the shallow ground water.</p>\n<p>Hydrologic effects of mining and reclamation were identified by comparing the hydrologic systems at mined and reclaimed watersheds with those at unmined agricultural watersheds. The presence or absence of a large final-cut lake in the reclaimed watershed greatly influences the hydrologic systems and the effects of mining and reclamation. Surface coal mining and reclamation can decrease base flow, annual runoff, and peak flow rates; increase the variability of flow and recharge to the bedrock; reestablish the premining relation between surface- and ground-water divides; and lower the water table in upland areas.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2368B","usgsCitation":"Martin, J.D., Duwelius, R.F., and Crawford, C.G., 1990, Effects of surface coal mining and reclamation on the geohydrology of six small watersheds in West-Central Indiana: U.S. Geological Survey Water Supply Paper 2368, viii, 71 p. ;2 v. :ill. ;28 cm., https://doi.org/10.3133/wsp2368B.","productDescription":"viii, 71 p. ;2 v. :ill. ;28 cm.","startPage":"B1","endPage":"B71","numberOfPages":"81","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science 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,{"id":3162,"text":"wsp2368A - 1990 - Description of the physical environment and coal-mining history of west-central Indiana, with emphasis on six small watersheds","interactions":[{"subject":{"id":12010,"text":"ofr87212 - 1987 - Description of the physical environment and coal-mining history of west-central Indiana, with emphasis on six small watersheds","indexId":"ofr87212","publicationYear":"1987","noYear":false,"title":"Description of the physical environment and coal-mining history of west-central Indiana, with emphasis on six small watersheds"},"predicate":"SUPERSEDED_BY","object":{"id":3162,"text":"wsp2368A - 1990 - Description of the physical environment and coal-mining history of west-central Indiana, with emphasis on six small watersheds","indexId":"wsp2368A","publicationYear":"1990","noYear":false,"chapter":"A","title":"Description of the physical environment and coal-mining history of west-central Indiana, with emphasis on six small watersheds"},"id":1}],"lastModifiedDate":"2022-01-18T21:27:22.046793","indexId":"wsp2368A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"2368","chapter":"A","title":"Description of the physical environment and coal-mining history of west-central Indiana, with emphasis on six small watersheds","docAbstract":"<p>This report describes the physical and human environment and coal-mining history of west-central Indiana, with emphasis on six small watersheds selected for study of the hydrologic effects of surface coal mining. The report summarizes information on the geology, geomorphology, soils, climate, hydrology, water use, land use, population, and coal-mining history of Clay, Owen, Sullivan, and Vigo Counties in Indiana. Site-specific information is given on the morphology, geology, soils, land use, coal-mining history, and hydrologic instrumentation of the six watersheds, which are each less than 3 square miles in area.</p>\n<p>West-central Indiana is underlain by coal-bearing Pennsylvanian rocks. Nearly all of the area has been glaciated at least once and is characterized by wide flood plains and broad, flat uplands. Most of the soils have formed in loess or in loess overlying Illinoian till. The Wabash, White, and Eel Rivers are the major drainages in west-central Indiana. Average annual precipitation is about 39.5 inches per year, and average annual runoff is about 13 inches per year. The most productive aquifers are confined or unconfined outwash aquifers located along the major rivers. Bedrock aquifers are regionally insignificant but are the sole source of ground water for areas that lack outwash, alluvium, or sand and gravel lenses in till.</p>\n<p>Indiana has more than 17 billion short tons of recoverable coal reserves; about 11 percent can be mined by surface methods. Almost half of Indiana's surface reserves are in Clay, Owen, Sullivan, and Vigo Counties. More than 50,000 acres in west-central Indiana were disturbed by surface coal mining from 1941 through 1980.</p>\n<p>Big Slough and Hooker Creek are streams that drain unmined, agricultural watersheds. Row-crop corn and soybeans are the principal crops. Soils are moderately well-drained silt loams, and the watersheds have well-developed dendritic drainage systems.</p>\n<p>The unnamed tributary to Honey Creek and the unnamed tributary to Sulphur Creek are streams that drain mined and reclaimed watersheds. Ridges of mine spoil have been graded to a gently rolling topography. Soils are well drained and consist of 6 to 12 inches of silt-loam topsoil that was stockpiled and then replaced over shale and sandstone fragments of the graded mine spoil. Grasses and legumes form the vegetative cover in each watershed.</p>\n<p>Pond Creek and the unnamed tributary to Big Branch are streams that drain mined and unreclaimed watersheds. Approximately one-half of the Pond Creek watershed is unmined, agricultural land. Soils are very well-drained shaly silty loams that have formed or' steeply sloping spoil banks. Both watersheds contain numerous impoundments of water and have enclosed areas that do not contribute surface runoff to streamflow. The ridges of mine spoil are covered with pine trees, but much of the soil surface is devoid of vegetation.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Physical environment and geohydrologic effects of surface coal mining in west-central Indiana","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2368A","usgsCitation":"Martin, J.D., Crawford, C.G., Duwelius, R.F., and Renn, D.E., 1990, Description of the physical environment and coal-mining history of west-central Indiana, with emphasis on six small watersheds: U.S. Geological Survey Water Supply Paper 2368, vii, 38 p., https://doi.org/10.3133/wsp2368A.","productDescription":"vii, 38 p.","numberOfPages":"48","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":139164,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2368a/report-thumb.jpg"},{"id":30119,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2368a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":394474,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25298.htm"}],"country":"United States","state":"Indiana","county":"Clay County, Owen County, Sullivan County, Vigo County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.617,\n              38.9\n            ],\n            [\n              -86.633,\n              38.9\n            ],\n            [\n              -86.633,\n              39.606\n            ],\n            [\n              -87.617,\n              39.606\n            ],\n            [\n              -87.617,\n              38.9\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db6690ea","contributors":{"authors":[{"text":"Martin, Jeffrey D. 0000-0003-1994-5285 jdmartin@usgs.gov","orcid":"https://orcid.org/0000-0003-1994-5285","contributorId":1066,"corporation":false,"usgs":true,"family":"Martin","given":"Jeffrey","email":"jdmartin@usgs.gov","middleInitial":"D.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":27231,"text":"Indiana-Kentucky Water Science Center","active":true,"usgs":true},{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":146354,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crawford, Charles G. 0000-0003-1653-7841 cgcrawfo@usgs.gov","orcid":"https://orcid.org/0000-0003-1653-7841","contributorId":1064,"corporation":false,"usgs":true,"family":"Crawford","given":"Charles","email":"cgcrawfo@usgs.gov","middleInitial":"G.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":146353,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Duwelius, Richard F.","contributorId":31378,"corporation":false,"usgs":true,"family":"Duwelius","given":"Richard","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":146356,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Renn, Danny E.","contributorId":14808,"corporation":false,"usgs":true,"family":"Renn","given":"Danny","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":146355,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":17103,"text":"ofr89576 - 1990 - Evaluation of three electronic report processing systems for preparing hydrologic reports of the U.S Geological Survey, Water Resources Division","interactions":[],"lastModifiedDate":"2012-02-02T00:07:18","indexId":"ofr89576","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"89-576","title":"Evaluation of three electronic report processing systems for preparing hydrologic reports of the U.S Geological Survey, Water Resources Division","docAbstract":"In 1987, the Water Resources Division of the U.S. Geological Survey undertook three pilot projects to evaluate electronic report processing systems as a means to improve the quality and timeliness of reports pertaining to water resources investigations. The three projects selected for study included the use of the following configuration of software and hardware: Ventura Publisher software on an IBM model AT personal computer, PageMaker software on a Macintosh computer, and FrameMaker software on a Sun Microsystems workstation. The following assessment criteria were to be addressed in the pilot studies: The combined use of text, tables, and graphics; analysis of time; ease of learning; compatibility with the existing minicomputer system; and technical limitations. It was considered essential that the camera-ready copy produced be in a format suitable for publication. Visual improvement alone was not a consideration. This report consolidates and summarizes the findings of the electronic report processing pilot projects. Text and table files originating on the existing minicomputer system were successfully transformed to the electronic report processing systems in American Standard Code for Information Interchange (ASCII) format. Graphics prepared using a proprietary graphics software package were transferred to all the electronic report processing software through the use of Computer Graphic Metafiles. Graphics from other sources were entered into the systems by scanning paper images. Comparative analysis of time needed to process text and tables by the electronic report processing systems and by conventional methods indicated that, although more time is invested in creating the original page composition for an electronically processed report , substantial time is saved in producing subsequent reports because the format can be stored and re-used by electronic means as a template. Because of the more compact page layouts, costs of printing the reports were 15% to 25% less than costs of printing the reports prepared by conventional methods. Because the largest report workload in the offices conducting water resources investigations is preparation of Water-Resources Investigations Reports, Open-File Reports, and annual State Data Reports, the pilot studies only involved these projects. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr89576","usgsCitation":"Stiltner, G., 1990, Evaluation of three electronic report processing systems for preparing hydrologic reports of the U.S Geological Survey, Water Resources Division: U.S. Geological Survey Open-File Report 89-576, 66 p.  :ill. ;28 cm., https://doi.org/10.3133/ofr89576.","productDescription":"66 p.  :ill. ;28 cm.","costCenters":[],"links":[{"id":150457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0576/report-thumb.jpg"},{"id":46232,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0576/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa051","contributors":{"authors":[{"text":"Stiltner, G.J.","contributorId":56668,"corporation":false,"usgs":true,"family":"Stiltner","given":"G.J.","affiliations":[],"preferred":false,"id":174940,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":17916,"text":"ofr90176 - 1990 - Hydrologic data for the Jemez Mountains, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:07:22","indexId":"ofr90176","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-176","title":"Hydrologic data for the Jemez Mountains, New Mexico","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr90176","usgsCitation":"Abeyta, C.G., and Delaney, B.M., 1990, Hydrologic data for the Jemez Mountains, New Mexico: U.S. Geological Survey Open-File Report 90-176, iv, 51 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr90176.","productDescription":"iv, 51 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":150093,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0176/report-thumb.jpg"},{"id":47157,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0176/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":47158,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0176/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":47159,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0176/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60eb90","contributors":{"authors":[{"text":"Abeyta, Cynthia G.","contributorId":52187,"corporation":false,"usgs":true,"family":"Abeyta","given":"Cynthia","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":178196,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Delaney, B. M.","contributorId":42217,"corporation":false,"usgs":true,"family":"Delaney","given":"B.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":178195,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":17789,"text":"ofr89580 - 1990 - U.S. Geological Survey applied research studies of the Cheyenne River System, South Dakota; description and collation of data, water years 1987-88","interactions":[],"lastModifiedDate":"2018-09-19T18:26:18","indexId":"ofr89580","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"89-580","title":"U.S. Geological Survey applied research studies of the Cheyenne River System, South Dakota; description and collation of data, water years 1987-88","docAbstract":"The Cheyenne River System in western South Dakota has been impacted by the discharge of about 100 million metric tons of gold-mill tailings to Whitewood Creek near Lead, South Dakota. In April 1985, the U.S. Geological Survey initiated an extensive series of research studies to investigate the magnitude of the impact and to define important processes acting on the contaminated sediments present in the system. The report presents all data collected during the 1987 and 1988 water years for these research studies. Some of the data included have been published previously. Data collected in the 1985 and 1986 water years have been published in a companion report (U.S. Geological Survey Open-File Report 88-484). Hydrologic, geochemical, and biologic data are available for sites on Whitewood Creek, and the Belle Fourche and Cheyenne Rivers. Data complexity varies from routine discharge and water-quality to very complex energy-dispersive x-ray analysis. Methods for sample collection, handling and preservation, and laboratory analysis are also presented. No interpretations or complex statistical summaries are included. (See also W89-08390) (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports,","doi":"10.3133/ofr89580","usgsCitation":"1990, U.S. Geological Survey applied research studies of the Cheyenne River System, South Dakota; description and collation of data, water years 1987-88: U.S. Geological Survey Open-File Report 89-580, vii, 145 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89580.","productDescription":"vii, 145 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":47029,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0580/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149081,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0580/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2be4b07f02db612e6b","contributors":{"editors":[{"text":"Goddard, K.E.","contributorId":82319,"corporation":false,"usgs":true,"family":"Goddard","given":"K.E.","email":"","affiliations":[],"preferred":false,"id":745681,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":20268,"text":"ofr90391 - 1990 - Records of wells and chemical analyses of ground water in Deuel and Hamlin counties, South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:07:40","indexId":"ofr90391","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-391","title":"Records of wells and chemical analyses of ground water in Deuel and Hamlin counties, South Dakota","docAbstract":"Well and chemical groundwater data contained in three tables were collected during a 5-year study started in 1971 to determine the geology and water resources of Deuel and Hamlin Counties, South Dakota. Physical, hydrologic, and geologic data for 3,228 wells and test holes have been entered into computer storage in the Ground-Water Site Inventory File of the U.S. Geological Survey 's National Water Data Storage and Retrieval System (WATSTORE). The well tables in the report are computer printouts from WATSTORE. Water quality data from 564 chemical analyses have been stored in the Water-Quality File of WATSTORE and is computer printed in the chemical analyses table by aquifer. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr90391","usgsCitation":"Neitzert, K., and Hansen, D.S., 1990, Records of wells and chemical analyses of ground water in Deuel and Hamlin counties, South Dakota: U.S. Geological Survey Open-File Report 90-391, iv, 113 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr90391.","productDescription":"iv, 113 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":152284,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0391/report-thumb.jpg"},{"id":49803,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0391/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635736","contributors":{"authors":[{"text":"Neitzert, K.M.","contributorId":62613,"corporation":false,"usgs":true,"family":"Neitzert","given":"K.M.","affiliations":[],"preferred":false,"id":182356,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hansen, D. S.","contributorId":70003,"corporation":false,"usgs":true,"family":"Hansen","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":182357,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":17856,"text":"ofr90150 - 1990 - Water-resources activities of the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-02-02T00:07:21","indexId":"ofr90150","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-150","title":"Water-resources activities of the U.S. Geological Survey","docAbstract":"The U.S. Geological Survey (USGS) has been active in West Virginia since the early 1900's. During recent years, the District completed several investigations as well as initiated others. An intense effort has been made to publish interpretive reports and data on a near-current basis. As a result of this effort, a significant number of water resources reports were completed and/or published during the 1989 fiscal year. This report contains a complete list of USGS reports addressing West Virginia hydrology as of December 1989. The mission of the Water Resources Division is to provide the hydrologic information and understanding needed for the optimum utilization and management of the Nation 's water resources for the overall benefit of the people in the United States. This is accomplished, in large part , through cooperation with other Federal and non-Federal agencies, by: (1) Collecting, on a systematic basis, data needed for the continuing determination and evaluation of the quantity, quality, and use of the Nation 's water resources; (2) Conducting analytical and interpretive water resource appraisals describing the occurrence, availability, and the physical, chemical, and biological characteristics of surface and groundwater; (3) conducting supportive basic and problem-oriented research in hydraulics, hydrology, and related fields of science to improve the scientific basis for investigations and measurement techniques and to understand hydrologic systems sufficiently well to quantitatively predict their response to stress, either natural or manmade; (4) disseminating the water data and the results of these investigations and research through reports, maps, computerized information services, and other forms of public releases; (5) Coordinating the activities of Federal agencies in the acquisition of water data for streams, lakes, reservoirs, estuaries, and groundwaters; and (6) Providing scientific and technical assistance in hydrologic fields to other Federal, State and local agencies, to licensees of the Federal Power Commission, and to international agencies on behalf of the Department of State. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr90150","usgsCitation":"Appel, D.H., 1990, Water-resources activities of the U.S. Geological Survey: U.S. Geological Survey Open-File Report 90-150, iv, 46 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr90150.","productDescription":"iv, 46 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":149933,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0150/report-thumb.jpg"},{"id":47094,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0150/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697d97","contributors":{"authors":[{"text":"Appel, D. H. (compiler)","contributorId":72397,"corporation":false,"usgs":true,"family":"Appel","given":"D.","suffix":"(compiler)","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":178080,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20259,"text":"ofr90161 - 1990 - U.S. Geological Survey National Computer Technology Meeting; Program and abstracts, May 7-11, 1990","interactions":[],"lastModifiedDate":"2012-02-02T00:07:43","indexId":"ofr90161","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-161","title":"U.S. Geological Survey National Computer Technology Meeting; Program and abstracts, May 7-11, 1990","docAbstract":"Computer-related information from all Divisions of the U.S. Geological Survey are discussed in this compilation of abstracts. Some of the topics addressed are system administration; distributed information systems and data bases, both current (1990) and proposed; hydrologic applications; national water information systems; geographic information systems applications and techniques. The report contains some of the abstracts that were presented at the National Computer Technology Meeting that was held in May 1990. The meeting was sponsored by the Water Resources Division and was attended by more than 200 technical and managerial personnel representing all the Divisions of the U.S. Geological Survey. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr90161","usgsCitation":"Balthrop, B.H., and Baker, E., 1990, U.S. Geological Survey National Computer Technology Meeting; Program and abstracts, May 7-11, 1990: U.S. Geological Survey Open-File Report 90-161, xviii, 56 p. ;28 cm., https://doi.org/10.3133/ofr90161.","productDescription":"xviii, 56 p. ;28 cm.","costCenters":[],"links":[{"id":1126,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr_90-161","linkFileType":{"id":5,"text":"html"}},{"id":153421,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2be4b07f02db6130cb","contributors":{"authors":[{"text":"Balthrop, B. H. (compiler)","contributorId":92286,"corporation":false,"usgs":true,"family":"Balthrop","given":"B.","suffix":"(compiler)","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":182342,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baker, E.G.","contributorId":84382,"corporation":false,"usgs":true,"family":"Baker","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":182341,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":18669,"text":"ofr90136 - 1990 - Ground-water flow and solute movement to drain laterals, western San Joaquin Valley, California; I, Geochemical assessment","interactions":[{"subject":{"id":18669,"text":"ofr90136 - 1990 - Ground-water flow and solute movement to drain laterals, western San Joaquin Valley, California; I, Geochemical assessment","indexId":"ofr90136","publicationYear":"1990","noYear":false,"title":"Ground-water flow and solute movement to drain laterals, western San Joaquin Valley, California; I, Geochemical assessment"},"predicate":"SUPERSEDED_BY","object":{"id":70042508,"text":"70042508 - 1991 - Groundwater flow and solute movement to drain laterals, western San Joaquin Valley, California: 1. Geochemical assessment","indexId":"70042508","publicationYear":"1991","noYear":false,"title":"Groundwater flow and solute movement to drain laterals, western San Joaquin Valley, California: 1. Geochemical assessment"},"id":1}],"supersededBy":{"id":70042508,"text":"70042508 - 1991 - Groundwater flow and solute movement to drain laterals, western San Joaquin Valley, California: 1. Geochemical assessment","indexId":"70042508","publicationYear":"1991","noYear":false,"title":"Groundwater flow and solute movement to drain laterals, western San Joaquin Valley, California: 1. Geochemical assessment"},"lastModifiedDate":"2018-11-19T12:24:36","indexId":"ofr90136","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-136","title":"Ground-water flow and solute movement to drain laterals, western San Joaquin Valley, California; I, Geochemical assessment","docAbstract":"<p>A study was undertaken to quantitatively evaluate the hydrologic processes affecting the chemical and isotopic composition of drain-lateral water in a drained agricultural field in the western San Joaquin Valley, California. The results of chemical and isotopic analysis of the samples and analysis of hydraulic-head data and drain-lateral flow data elucidate the process of mixing of deep and shallow ground water entering the drain laterals. The deep ground water was subject to partial evaporation prior to drainage-system installation and has been displaced downward (at depths greater than 6 meters) in the ground-water system. This ground water is flowing toward the drain laterals. The percentage of the deep, isotopically enriched ground water entering the drain laterals varies with time and between drain laterals. The percentage of the total drain-lateral flow, which is deep ground-water flow, is about 30 percent for the shallow drain lateral (1.8 meters below land surface) and 60 percent for the deep drain lateral (2.7 meters below land surface). During irrigation, the percentages decrease to 0 and 30 percent for the shallow and deep drain laterals, respectively.</p><p>Selenium loads in the drain laterals vary with time and between drain laterals. The selenium load for the shallow drain lateral (68 kilograms) during 1 year is 21 percent of the load for the deep drain lateral (332 kilograms) because it collects less deep, high-selenium ground water and does not flow continuously. Although selenium concentrations in the drain-lateral water decreased during irrigation, selenium loads increased substantially during a preplant irrigation because of increased flow into the drain laterals. The selenium loads during 8 days of irrigation represented a substantial percentage (25 percent for the shallow drain lateral and 11 percent for the deep drain lateral) of the total selenium load for 1 year.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr90136","usgsCitation":"Deverel, S.J., and Fio, J., 1990, Ground-water flow and solute movement to drain laterals, western San Joaquin Valley, California; I, Geochemical assessment: U.S. Geological Survey Open-File Report 90-136, iv, 23 p., https://doi.org/10.3133/ofr90136.","productDescription":"iv, 23 p.","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":151900,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0136/report-thumb.jpg"},{"id":359564,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0136/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"San Joaquin Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.84,35.06 ], [ -121.84,38.17 ], [ -118.67,38.17 ], [ -118.67,35.06 ], [ -121.84,35.06 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d5f9","contributors":{"authors":[{"text":"Deverel, S. J.","contributorId":65478,"corporation":false,"usgs":true,"family":"Deverel","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":179532,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fio, J.L.","contributorId":56662,"corporation":false,"usgs":true,"family":"Fio","given":"J.L.","affiliations":[],"preferred":false,"id":179531,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":19048,"text":"ofr90184 - 1990 - Feasibility of privatization of the hydrologic data collection and analysis functions of the U.S. Geological Survey.","interactions":[],"lastModifiedDate":"2012-02-02T00:07:31","indexId":"ofr90184","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-184","title":"Feasibility of privatization of the hydrologic data collection and analysis functions of the U.S. Geological Survey.","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/ofr90184","usgsCitation":"Wahl, K.L., Condes de la Torre, A., Kilpatrick, F.A., Martens, L.A., Mattraw, H., Pollock, D.W., Rosenshein, J.S., and Solley, W.B., 1990, Feasibility of privatization of the hydrologic data collection and analysis functions of the U.S. Geological Survey.: U.S. Geological Survey Open-File Report 90-184, 64 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr90184.","productDescription":"64 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":152005,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0184/report-thumb.jpg"},{"id":48483,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0184/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f71ad","contributors":{"authors":[{"text":"Wahl, Kenneth L.","contributorId":61024,"corporation":false,"usgs":true,"family":"Wahl","given":"Kenneth","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":180215,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Condes de la Torre, Alberto","contributorId":73570,"corporation":false,"usgs":true,"family":"Condes de la Torre","given":"Alberto","email":"","affiliations":[],"preferred":false,"id":180217,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kilpatrick, Frederick A.","contributorId":19306,"corporation":false,"usgs":true,"family":"Kilpatrick","given":"Frederick","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":180213,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Martens, Lawrence A.","contributorId":17973,"corporation":false,"usgs":true,"family":"Martens","given":"Lawrence","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":180212,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mattraw, Harold C.","contributorId":81878,"corporation":false,"usgs":true,"family":"Mattraw","given":"Harold C.","affiliations":[],"preferred":false,"id":180218,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Pollock, David W. dwpolloc@usgs.gov","contributorId":4248,"corporation":false,"usgs":true,"family":"Pollock","given":"David","email":"dwpolloc@usgs.gov","middleInitial":"W.","affiliations":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":180211,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Rosenshein, Joseph S.","contributorId":32904,"corporation":false,"usgs":true,"family":"Rosenshein","given":"Joseph","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":180214,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Solley, Wayne B.","contributorId":61409,"corporation":false,"usgs":true,"family":"Solley","given":"Wayne","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":180216,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":20210,"text":"ofr90389 - 1990 - Manual for comparing methods of designing hydrologic-data-collection networks","interactions":[],"lastModifiedDate":"2012-02-02T00:07:39","indexId":"ofr90389","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-389","title":"Manual for comparing methods of designing hydrologic-data-collection networks","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr90389","usgsCitation":"Moss, M.E., and Tasker, G.D., 1990, Manual for comparing methods of designing hydrologic-data-collection networks: U.S. Geological Survey Open-File Report 90-389, 104 p. :ill. ;28 cm., https://doi.org/10.3133/ofr90389.","productDescription":"104 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":152384,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0389/report-thumb.jpg"},{"id":49756,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0389/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64aebd","contributors":{"authors":[{"text":"Moss, M. E.","contributorId":50500,"corporation":false,"usgs":true,"family":"Moss","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":182254,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tasker, Gary D.","contributorId":83097,"corporation":false,"usgs":true,"family":"Tasker","given":"Gary","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":182255,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":20174,"text":"ofr90131 - 1990 - Annual yield and selected hydrologic data for the Arkansas River Basin Compact, Arkansas-Oklahoma: 1989 water year","interactions":[],"lastModifiedDate":"2022-05-12T21:46:39.780569","indexId":"ofr90131","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-131","title":"Annual yield and selected hydrologic data for the Arkansas River Basin Compact, Arkansas-Oklahoma: 1989 water year","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr90131","usgsCitation":"Moore, M.A., Lamb, T., and Hauth, L., 1990, Annual yield and selected hydrologic data for the Arkansas River Basin Compact, Arkansas-Oklahoma: 1989 water year: U.S. Geological Survey Open-File Report 90-131, iv, 35 p., https://doi.org/10.3133/ofr90131.","productDescription":"iv, 35 p.","costCenters":[],"links":[{"id":49714,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0131/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":400602,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17863.htm"},{"id":152782,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0131/report-thumb.jpg"}],"country":"United States","state":"Arkansas, Oklahoma","otherGeospatial":"Arkansas River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.6580,\n              34.674\n            ],\n            [\n              -93.921,\n              34.674\n            ],\n            [\n              -93.921,\n              36.456\n            ],\n            [\n              -95.6580,\n              36.456\n            ],\n            [\n              -95.6580,\n              34.674\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b7f0","contributors":{"authors":[{"text":"Moore, M. A.","contributorId":84767,"corporation":false,"usgs":true,"family":"Moore","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":182199,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lamb, T.E.","contributorId":58272,"corporation":false,"usgs":true,"family":"Lamb","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":182198,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hauth, L.D.","contributorId":48551,"corporation":false,"usgs":true,"family":"Hauth","given":"L.D.","affiliations":[],"preferred":false,"id":182197,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":17619,"text":"ofr89275 - 1990 - Report planning, preparation and review guide","interactions":[],"lastModifiedDate":"2012-02-02T00:07:22","indexId":"ofr89275","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"89-275","title":"Report planning, preparation and review guide","docAbstract":"The guide describes critical steps in the planning, preparation, and review of hydrologic projects and reports. Project and report planning and organization are discussed first. Report writing and guidelines for writing selected parts of the report are covered next. The last topics covered are editorial and technical review. The guide contains examples of good and poor writing, report checklists, and source references to assist authors in the various stages of report preparation.","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr89275","usgsCitation":"Moore, J., Aronson, D.A., Green, J.H., and Puente, C., 1990, Report planning, preparation and review guide: U.S. Geological Survey Open-File Report 89-275, iv, 81 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89275.","productDescription":"iv, 81 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":1034,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr89-275","linkFileType":{"id":5,"text":"html"}},{"id":149845,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b7b5","contributors":{"authors":[{"text":"Moore, J.E.","contributorId":34927,"corporation":false,"usgs":true,"family":"Moore","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":177134,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aronson, D. A.","contributorId":20308,"corporation":false,"usgs":true,"family":"Aronson","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":177133,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Green, J. H.","contributorId":43312,"corporation":false,"usgs":true,"family":"Green","given":"J.","email":"","middleInitial":"H.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":177136,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Puente, Celso","contributorId":36140,"corporation":false,"usgs":true,"family":"Puente","given":"Celso","email":"","affiliations":[],"preferred":false,"id":177135,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":17229,"text":"ofr88500 - 1990 - Hydrogeochemical data from an acidic deposition study at McDonalds Branch basin in the New Jersey Pinelands, 1983-86","interactions":[],"lastModifiedDate":"2012-02-02T00:07:15","indexId":"ofr88500","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"88-500","title":"Hydrogeochemical data from an acidic deposition study at McDonalds Branch basin in the New Jersey Pinelands, 1983-86","docAbstract":"Data from a 1983-86 acidic-deposition study at McDonalds Branch basin, a small (2.35-sq-mi) forested watershed in Lebanon State Forest, New Jersey include mineralogy of soil and depositional clays; physical and chemical analyses of soils; hydrologic measurements (precipitation and throughfall amounts, stream stage and discharge, and water-table altitudes); and water quality data from precipitation, throughfall, soil water, surface water, and groundwater. Site locations, collector designs, and well- construction data also are presented. The pH of bulk precipitation to McDonalds Branch basin over the sampling period (January 1985 to March 1986) ranged from 4.0 to 4.7, with a mean of approximately 4.3. Stream pH ranged from 3.2 to 4.8 and generally increased in a downstream direction. In general sulfate was the dominant anion throughout the basin. Aluminum concentrations commonly were elevated in surface and groundwaters, and were as high as 10,000 micrograms/L at one upstream site on McDonalds Branch. Dissolved organic carbon was an important component of stream waters in some locations and ranged in concentration from 1/1 to 37 mg/L. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr88500","usgsCitation":"Lord, D.G., Barringer, J.L., Johnsson, P., Schuster, P., Walker, R., Fairchild, J., Sroka, B., and Jacobsen, E., 1990, Hydrogeochemical data from an acidic deposition study at McDonalds Branch basin in the New Jersey Pinelands, 1983-86: U.S. Geological Survey Open-File Report 88-500, vi, 132 p. :ill. ;28 cm., https://doi.org/10.3133/ofr88500.","productDescription":"vi, 132 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":149283,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0500/report-thumb.jpg"},{"id":46378,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0500/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628ee4","contributors":{"authors":[{"text":"Lord, D. G.","contributorId":9254,"corporation":false,"usgs":true,"family":"Lord","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":175509,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barringer, J. L.","contributorId":13994,"corporation":false,"usgs":true,"family":"Barringer","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":175510,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnsson, P.A.","contributorId":105735,"corporation":false,"usgs":true,"family":"Johnsson","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":175515,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schuster, P. F.","contributorId":30197,"corporation":false,"usgs":true,"family":"Schuster","given":"P. F.","affiliations":[],"preferred":false,"id":175512,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Walker, R.L.","contributorId":27009,"corporation":false,"usgs":true,"family":"Walker","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":175511,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Fairchild, J.E.","contributorId":49811,"corporation":false,"usgs":true,"family":"Fairchild","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":175513,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Sroka, B.N.","contributorId":72392,"corporation":false,"usgs":true,"family":"Sroka","given":"B.N.","affiliations":[],"preferred":false,"id":175514,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Jacobsen, Eric jacobsen@usgs.gov","contributorId":3864,"corporation":false,"usgs":true,"family":"Jacobsen","given":"Eric","email":"jacobsen@usgs.gov","affiliations":[],"preferred":true,"id":175508,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":21181,"text":"ofr90197 - 1990 - Importance of return flow as a component of water use","interactions":[],"lastModifiedDate":"2018-04-02T11:53:17","indexId":"ofr90197","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-197","title":"Importance of return flow as a component of water use","docAbstract":"<p>Understanding the relation between the hydrologjc cycle and water use is important for effective water-resources management. The hydrologic cycle is the natural pathway of water from evaporation to precipitation to infiltration or runoff and to storage from which evaporation can again occur. The science of water use is the study of human influences on the hydrologic cycle. Human activities affect the hydrologic cycle by changing the quantity, distribution, and quality of available water. Quantifying return flow is useful to water managers in evaluating such changes. Return flow is often thought of as what runs down the drain, or what is leftover after the water's purpose has been served. As innocuous as that may sound, return flow plays a significant part in the overall water-use picture.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr90197","usgsCitation":"Trotta, L.C., and Horn, M., 1990, Importance of return flow as a component of water use: U.S. Geological Survey Open-File Report 90-197, 2 p., https://doi.org/10.3133/ofr90197.","productDescription":"2 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":153049,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0197/report-thumb.jpg"},{"id":50773,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0197/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fde4b07f02db5f5f19","contributors":{"authors":[{"text":"Trotta, L. C.","contributorId":63410,"corporation":false,"usgs":true,"family":"Trotta","given":"L.","email":"","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":183983,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Horn, M.S.","contributorId":107720,"corporation":false,"usgs":true,"family":"Horn","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":183984,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":17634,"text":"ofr90597 - 1990 - Results of test drilling and hydrologic monitoring in the Indian Bathtub area, Owyhee County, southwestern Idaho, January 1989 through September 1990","interactions":[],"lastModifiedDate":"2013-11-26T15:37:59","indexId":"ofr90597","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-597","title":"Results of test drilling and hydrologic monitoring in the Indian Bathtub area, Owyhee County, southwestern Idaho, January 1989 through September 1990","docAbstract":"This report presents data collected during the period January 1989 through \nSeptember 1990 from eight test holes and selected thermal-water wells and \nsprings in the Indian Bathtub area, southwestern Idaho. The data include \ncompletion, lithologic, and gamma logs for eight test holes, hydrographs of water \nlevels in the test holes and ten other wells, hydrographs of discharges at four \nsprings, and chemical and isotopic analyses of water from six of the test holes. \nThese data were collected as part of a continuing study to determine the cause or \ncauses of decreased discharge at Indian Bathtub Spring and other thermal \nsprings along Hot Creek.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Boise, ID","doi":"10.3133/ofr90597","collaboration":"Prepared in cooperation with the U.S. Fish and Wildlife Service","usgsCitation":"Young, H., Jones, M., Parliman, D., and Tungate, A., 1990, Results of test drilling and hydrologic monitoring in the Indian Bathtub area, Owyhee County, southwestern Idaho, January 1989 through September 1990: U.S. Geological Survey Open-File Report 90-597, ii, 40 p., https://doi.org/10.3133/ofr90597.","productDescription":"ii, 40 p.","numberOfPages":"44","temporalStart":"1989-01-01","temporalEnd":"1990-09-30","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":149824,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0597/report-thumb.jpg"},{"id":46831,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0597/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","country":"United States","state":"Idaho","county":"Owyhee County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.006012,42.717759 ], [ -116.006012,42.890052 ], [ -115.669556,42.890052 ], [ -115.669556,42.717759 ], [ -116.006012,42.717759 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6055e6","contributors":{"authors":[{"text":"Young, H.W.","contributorId":68278,"corporation":false,"usgs":true,"family":"Young","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":177220,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, M.L.","contributorId":88731,"corporation":false,"usgs":true,"family":"Jones","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":177221,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Parliman, D. J.","contributorId":64220,"corporation":false,"usgs":true,"family":"Parliman","given":"D. J.","affiliations":[],"preferred":false,"id":177219,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tungate, A.M.","contributorId":38638,"corporation":false,"usgs":true,"family":"Tungate","given":"A.M.","affiliations":[],"preferred":false,"id":177218,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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