{"pageNumber":"552","pageRowStart":"13775","pageSize":"25","recordCount":16449,"records":[{"id":8759,"text":"ofr811125 - 1981 - Hydrologic and morphologic changes in channels of the Platte River basin: A historical perspective","interactions":[],"lastModifiedDate":"2022-08-31T19:15:57.552529","indexId":"ofr811125","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-1125","title":"Hydrologic and morphologic changes in channels of the Platte River basin: A historical perspective","docAbstract":"<p>The channels of the Platte River and its major tributaries, the South Platte and North Platte Rivers in Colorado, Wyoming, and Nebraska, have undergone major changes in hydrologic regime and morphology since 1860. These changes are attributed here to agricultural, municipal, and industrial water use.</p><p>Although water-resource development varied temporally throughout the basin, the history of development along the Platte River and tributaries followed four stages: (1) Construction of small, crude ditches to irrigate flood plains; (2) construction of larger canals to irrigate bench lands; (3) construction of reservoirs to store snowmelt runoff; and (4) accelerated development of ground-water resources. Despite differences in rates of development, diversion and storage of water for irrigation, municipal, and industrial use have changed streamflow patterns throughout the basin. At some stations, significant changes in flood peaks, annual mean discharges, and shapes of flow-duration curves have been recorded.</p><p>Changes in streamflow patterns are manifested by changes in appearance of channels of the Platte River. Prior to water development in the 19th century, the Platte was a wide (-2 kilometers), shallow (1.8 to 2.4 meters) river characterized by bankfull spring flows and low summer flows. Although timber generally was scarce in the valley, the Platte channels contained hundreds of small, timbered islands. Since development, the channels have changed radically. Comparing surveyor's maps (General Land Office), drawn during the 1860's, with six sets of aerial photographs, taken between 1938 and 1979, for six 5-kilometer reaches of the river shows that the channels have narrowed considerably above the confluence with the Loup River. The width of the channels in 1979 ranged from 8 to 50 percent of the channel width in 1860. Below the confluence with the Loup River, the width of the river in 1979 was about 92 percent of the channel width in 1860. Above the confluence with the Loup River, width reduction has occurred by progressive encroachment of vegetation and consequent vertical and horizontal accretion on sand bars in the channel. Vegetative encroachment on sand bars has occurred because (1) the present hydrologic regime provides more favorable conditions for germination and growth on sand bars, and (2) since development of the basin, flood peaks are no longer capable of scouring vegetation from the sand bars. Overbank flows evidently have become more common, probably because channel narrowing and vegetative encroachment have increased the hydraulic roughness of the channels. Moreover, the magnitude of low flows has increased and the days of no flows has decreased giving the channels a more perennial character.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811125","usgsCitation":"Eschner, T., Hadley, R.F., and Crowley, K., 1981, Hydrologic and morphologic changes in channels of the Platte River basin: A historical perspective: U.S. Geological Survey Open-File Report 81-1125, v, 57 p., https://doi.org/10.3133/ofr811125.","productDescription":"v, 57 p.","costCenters":[],"links":[{"id":406027,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1125/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141947,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1125/report-thumb.jpg"}],"country":"United States","state":"Colorado, Nebraska, Wyoming","otherGeospatial":"Platte River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.67675781249999,\n              39.57182223734374\n            ],\n            [\n              -95.9326171875,\n              39.57182223734374\n            ],\n            [\n              -95.9326171875,\n              43.99281450048989\n            ],\n            [\n              -108.67675781249999,\n              43.99281450048989\n            ],\n            [\n              -108.67675781249999,\n              39.57182223734374\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6117ba","contributors":{"authors":[{"text":"Eschner, T.R.","contributorId":45700,"corporation":false,"usgs":true,"family":"Eschner","given":"T.R.","email":"","affiliations":[],"preferred":false,"id":158281,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hadley, R. F.","contributorId":27028,"corporation":false,"usgs":true,"family":"Hadley","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":158280,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crowley, K.D.","contributorId":86769,"corporation":false,"usgs":true,"family":"Crowley","given":"K.D.","email":"","affiliations":[],"preferred":false,"id":158282,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":8740,"text":"ofr81678 - 1981 - Progress report on the effects of surface mining on the surface-water hydrology of selected basins in the Fort Union coal region, North Dakota and Montana","interactions":[],"lastModifiedDate":"2018-02-16T16:22:55","indexId":"ofr81678","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-678","title":"Progress report on the effects of surface mining on the surface-water hydrology of selected basins in the Fort Union coal region, North Dakota and Montana","docAbstract":"The purpose of the investigation is to provide a means to assess the impacts on surface-water hydrology due to changes in land use resulting from surface mining of coal in the Fort Union Coal Region, North Dakota and Montana. The objectives of the study are to: (1) Determine premining hydrologic conditions in small representative drainage basins and provide historical data with which to compare the magnitude of changes resulting from mining, and (2) develop the capability of making reasonably accurate projections of hydrologic effects resulting from the various land-use changes caused by surface mining. Data collection has been underway since October 1976 for the West Branch Antelope Creek study area in western North Dakota and since March 1978 for the Hay Creek study area in eastern Montana. Data collected during the premining period are being analyzed using statistical methods for the evaluation of the premining conditions. A digitial model with the capability of making hydrologic projections is being developed. Most of the model components have been tested during 1979 and 1980. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81678","usgsCitation":"Emerson, D.G., 1981, Progress report on the effects of surface mining on the surface-water hydrology of selected basins in the Fort Union coal region, North Dakota and Montana: U.S. Geological Survey Open-File Report 81-678, v, 33 p., https://doi.org/10.3133/ofr81678.","productDescription":"v, 33 p.","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":142709,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0678/report-thumb.jpg"},{"id":36317,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0678/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64af90","contributors":{"authors":[{"text":"Emerson, Douglas G.","contributorId":40579,"corporation":false,"usgs":true,"family":"Emerson","given":"Douglas","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":158244,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3127,"text":"wsp2068 - 1981 - Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah","interactions":[{"subject":{"id":7233,"text":"ofr79988 - 1979 - Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah","indexId":"ofr79988","publicationYear":"1979","noYear":false,"title":"Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":3127,"text":"wsp2068 - 1981 - Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah","indexId":"wsp2068","publicationYear":"1981","noYear":false,"title":"Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah"},"id":1}],"lastModifiedDate":"2023-03-14T20:06:08.759442","indexId":"wsp2068","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"2068","title":"Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah","docAbstract":"<p>Data obtained during a hydrologic reconnaissance in 1975-77 in the Wasatch Plateau-Book Cliffs coal-fields area of Utah were correlated with existing long-term data. Maps were prepared showing average precipitation, average streamflow, stream temperature, ground- and surface-water quality, sediment yield, and geology. Recommendations were made for additional study and suggested approaches for continued monitoring in the coalfields areas.</p><p>moDuring the 1931-75 water years, the minimum discharges for the five major streams that head in the area ranged from about 12,000 to 26,000 acre-feet per year, and the maximum discharges ranged from about 59,000 to 315,000 acre-feet per year. Correlations indicate that 3 years of low-flow records at stream sites in the Wasatch Plateau would allow the development of relationships with long-term sites that can be used to estimate future low-flow records within a standard error of about 20 percent.</p><p>Most water-quality degradation in streams occurs along the flanks of the Wasatch Plateau and Book Cliffs. In the uplands, dissolved-solids concentrations generally ranged from less than 100 to about 250 milligrams per liter, and in the lowlands, the concentrations ranged from about 250 to more than 6,000 milligrams per liter.</p><p>Most springs in the Wasatch Plateau and Book Cliffs discharge from the Star Point Sandstone or younger formations, and the water generally contains less than about 1,000 milligrams per liter of dissolved solids. The discharges of 65 springs ranged from about 0.2 to 200 gallons per minute. The Blackhawk Formation, which is the principal coal-bearing formation, produces water in many of the mines. The dissolved-solids concentration in water discharging from springs and mines in the Blackhawk ranged from about 60 to 800 milligrams per liter.</p><p>In the lowland areas, the Ferron Sandstone Member of the Maneos Shale appears to have the most potential for subsurface development of water of suitable chemical quality for human consumption. Three wells in the Ferron yielded water with dissolved-solids concentrations ranging from about 650 to 1,230 milligrams per liter.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2068","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management and the U.S. Environmental Protection Agency","usgsCitation":"Waddell, K.M., Contratto, P., Sumsion, C.T., and Butler, J.R., 1981, Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah: U.S. Geological Survey Water Supply Paper 2068, Report: v, 45 p.; 9 Plates: 40.00 in x 30.19 inches or smaller; Table: 12.50 in. x 13.45 inches, https://doi.org/10.3133/wsp2068.","productDescription":"Report: v, 45 p.; 9 Plates: 40.00 in x 30.19 inches or smaller; Table: 12.50 in. x 13.45 inches","numberOfPages":"61","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":414125,"rank":13,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25489.htm","linkFileType":{"id":5,"text":"html"}},{"id":30038,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2068/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":247290,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Hydrgraphs for selected wells, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247284,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing average discharges of streams, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247283,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing average annual precipitation, 1931-75, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247282,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing general geology of the Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":139323,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2068/report-thumb.jpg"},{"id":247289,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-8.pdf","text":"Plate 8","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Fence diagram showing stratigraphic units and concentrations of dissolved solids, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247288,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-7.pdf","text":"Plate 7","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing concentrations of dissolved solids in ground water, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247287,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-6.pdf","text":"Plate 6","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing estimated sediment yields, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247286,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-5.pdf","text":"Plate 5","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing concentrations of dissolved solids in surface water, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247285,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-4.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing estimated range of stream temperature, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247291,"rank":12,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/wsp/2068/plate-table_2.pdf","text":"Table 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Published stream-gaging records and ranges of annual discharge, 1931-75 water years"}],"country":"United States","state":"Utah","otherGeospatial":"Wasatch Plateau-Book Cliffs coal-fields area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -111.54,\n              40.045\n            ],\n            [\n              -111.54,\n              38.687\n            ],\n            [\n              -109.059,\n              38.687\n            ],\n            [\n              -109.059,\n              40.045\n            ],\n            [\n              -111.54,\n              40.045\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db605450","contributors":{"authors":[{"text":"Waddell, Kidd M.","contributorId":20720,"corporation":false,"usgs":true,"family":"Waddell","given":"Kidd","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":146301,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Contratto, P. Kay","contributorId":15598,"corporation":false,"usgs":true,"family":"Contratto","given":"P. Kay","affiliations":[],"preferred":false,"id":146300,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sumsion, C. T.","contributorId":23129,"corporation":false,"usgs":true,"family":"Sumsion","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":146302,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Butler, John R.","contributorId":36540,"corporation":false,"usgs":true,"family":"Butler","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":146303,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":8619,"text":"ofr81542 - 1981 - The U.S. Geological Survey Coal Hydrology Program and the potential of hydrologic models for impact assessments","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr81542","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-542","title":"The U.S. Geological Survey Coal Hydrology Program and the potential of hydrologic models for impact assessments","docAbstract":"A requirement of Public Law 95-87, the Surface Mining Control and Reclamation Act of 1977, is the understanding of the hydrology in actual and proposed surface-mined areas. Surface-water data for small specific-sites and for larger areas such as adjacent and general areas are needed also to satisfy the hydrologic requirements of the Act. The Act specifies that surface-water modeling techniques may be used to generate the data and information. The purpose of this report is to describe how this can be achieved for smaller watersheds. This report also characterizes 12 ' state-of-the-art ' strip-mining assessment models that are to be tested with data from two data-intensive studies involving small watersheds in Tennessee and Indiana. Watershed models are best applied to small watersheds with specific-site data. Extending the use of modeling techniques to larger watersheds remains relatively untested, and to date the upper limits for application have not been established. The U.S. Geological Survey is currently collecting regional hydrologic data in the major coal provinces of the United States and this data will be used to help satisfy the ' general-area ' data requirements of the Act. This program is reviewed and described in this report. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81542","usgsCitation":"Doyle, W., 1981, The U.S. Geological Survey Coal Hydrology Program and the potential of hydrologic models for impact assessments: U.S. Geological Survey Open-File Report 81-542, v, 61 p. :maps ;28 cm., https://doi.org/10.3133/ofr81542.","productDescription":"v, 61 p. :maps ;28 cm.","costCenters":[],"links":[{"id":141105,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0542/report-thumb.jpg"},{"id":36209,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0542/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667575","contributors":{"authors":[{"text":"Doyle, W. Harry","contributorId":32900,"corporation":false,"usgs":true,"family":"Doyle","given":"W. Harry","affiliations":[],"preferred":false,"id":158038,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3021,"text":"wsp2177 - 1981 - Hydrologic effects of stress-relief fracturing in an Appalachian Valley","interactions":[],"lastModifiedDate":"2012-02-02T00:05:45","indexId":"wsp2177","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"2177","title":"Hydrologic effects of stress-relief fracturing in an Appalachian Valley","docAbstract":"A hydrologic study at Twin Falls State Park, Wyoming County, West Virginia, was made to determine how fracture systems affect the occurrence and movement of ground water in a typical valley of the Appalachian Plateaus Physiographic Province. Twin Falls was selected because it is generally unaffected by factors that would complicate an analysis of the data. The study area was the Black Fork Valley at Twin Falls. The valley is about 3 miles long and 400 to 600 feet wide and is cut into massive sandstone units interbedded with thin coal and shale beds. The study was made to determine how aquifer characteristics were related to fracture systems in this valley, so that the relation could be applied to studies of other valleys. \r\n\r\nTwo sites were selected for test drilling, pumping tests, and geophysical studies. One site is in the upper part of the valley, and the second is near the lower central part. At both sites, ground water occurs mainly in horizontal bedding-plane fractures under the valley floor and in nearly vertical and horizontal slump fractures along the valley wall. The aquifer is under confined conditions under the valley floor and unconfined conditions along the valley wall. The fractures pinch out under the valley walls, which form impermeable barriers. Tests of wells near the valley center indicated a change in storage coefficient as the cone of depression caused by pumping reached the confined-unconfined boundaries; the tests also indicated barrier-image effects when the cone reached the impermeable boundaries. Drawdown from pumping near the center of the valley affected water levels at both sites, indicating a hydraulic connection from the upper to the lower end of the valley. Stream gain-and-loss studies show that ground water discharges to the stream from horizontal fractures beneath Black Fork Falls, near the mouth of Black Fork. The fracture systems that constitute most of the transmissive part of the aquifer at Twin Falls are like those described as being formed from stress relief. As stress-relief fractures have been described in other valleys of the Appalachian Plateaus, the same aquifer conditions may exist in those valleys.","language":"ENGLISH","publisher":"G.P.O.,","doi":"10.3133/wsp2177","usgsCitation":"Wyrick, G.G., and Borchers, J.W., 1981, Hydrologic effects of stress-relief fracturing in an Appalachian Valley: U.S. Geological Survey Water Supply Paper 2177, vii, 51 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/wsp2177.","productDescription":"vii, 51 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":139462,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2177/report-thumb.jpg"},{"id":29851,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2177/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db606ff8","contributors":{"authors":[{"text":"Wyrick, Granville G.","contributorId":67493,"corporation":false,"usgs":true,"family":"Wyrick","given":"Granville","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":146160,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Borchers, James W.","contributorId":25931,"corporation":false,"usgs":true,"family":"Borchers","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":146159,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8544,"text":"ofr811185 - 1981 - Hydrologic data of the lower Merrimack River basin, Massachusetts, from Concord River, Lowell, to Plum Island, Newburyport","interactions":[],"lastModifiedDate":"2022-09-02T17:15:45.287223","indexId":"ofr811185","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-1185","title":"Hydrologic data of the lower Merrimack River basin, Massachusetts, from Concord River, Lowell, to Plum Island, Newburyport","docAbstract":"<p>The lower Merrimack River basin study area drains approximately 180 square miles along the New Hampshire border in northeastern Massachusetts. This area includes parts of the Merrimack River basin within Massachusetts east of the Beaver Brook and Concord River basins, except for the Shawsheen River basin. Even though the Blackwater River basin within Massachusetts isn't part of the lower Merrimack River basin, it has been included in this report. Principal tributaries to the Merrimack River, which discharges to the Atlantic Ocean at Newburyport, Massachusetts, are: Bare Meadow, Bartlett, Cobbler Creek, Fish, Richardson, and Trull Brooks, Artichoke, East Meadow, Indian, Little, Powwow, and Spicket Rivers, and Johnson Creek.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811185","collaboration":"Prepared in cooperation with the Commonwealth of Massachusetts, Water Resources Commission","usgsCitation":"Delaney, D.F., and Gay, F.B., 1981, Hydrologic data of the lower Merrimack River basin, Massachusetts, from Concord River, Lowell, to Plum Island, Newburyport: U.S. Geological Survey Open-File Report 81-1185, Report: iii, 34 p.; 1 Plate: 44.98 x 34.31 inches, https://doi.org/10.3133/ofr811185.","productDescription":"Report: iii, 34 p.; 1 Plate: 44.98 x 34.31 inches","costCenters":[],"links":[{"id":406153,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1185/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":406152,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1185/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141699,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1185/report-thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Merrimack River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.30401611328125,\n              42.64204079304426\n            ],\n            [\n              -70.80001831054688,\n              42.64204079304426\n            ],\n            [\n              -70.80001831054688,\n              42.85180609584705\n            ],\n            [\n              -71.30401611328125,\n              42.85180609584705\n            ],\n            [\n              -71.30401611328125,\n              42.64204079304426\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db607348","contributors":{"authors":[{"text":"Delaney, David F.","contributorId":41797,"corporation":false,"usgs":false,"family":"Delaney","given":"David","email":"","middleInitial":"F.","affiliations":[{"id":27261,"text":"U.S. Army Construction Engineering Research Laboratory, Champaig","active":true,"usgs":false}],"preferred":false,"id":157911,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gay, Frederick B.","contributorId":102052,"corporation":false,"usgs":true,"family":"Gay","given":"Frederick","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":157912,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8526,"text":"ofr80159 - 1981 - Hydrologic data for the alluvium and terrace aquifer of the Beaver-North Canadian River from the Panhandle to Canton Reservoir, northwestern Oklahoma","interactions":[],"lastModifiedDate":"2018-03-30T16:12:06","indexId":"ofr80159","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-159","title":"Hydrologic data for the alluvium and terrace aquifer of the Beaver-North Canadian River from the Panhandle to Canton Reservoir, northwestern Oklahoma","docAbstract":"<p>The U.S. Geological Survey has collected data on Oklahoma's groundwater resources since 1934. The data in this report were collected as part of a study in cooperation with the Oklahoma Water Resources Board to evaluate the geohydrology of the alluvium and terrace aquifer of the Beaver-North Canadian River 4] in northwestern Oklahoma. The data include records of approximately 900 wells, test-holes, and springs, results of chemical analyses of water from 30 wells tapping the aquifer, monthly water-level measurements for selected wells, and low-flow discharge measurements of the Beaver-North Canadian River and its tributaries (plate 1). All of the data were collected in the field during the period 1977-79. Information prior to this period is not included in this report but is contained in reports by Wood and Stacy (1965) and Morton (in press).</p><p>The stratigraphic nomenclature is that of the Oklahoma Geological Survey and does.not necessarily agree with that of the U.S. Geological Survey.</p><p>Acknowledgement is extended to the residents of the study area for their cooperation in obtaining the data in this report.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80159","usgsCitation":"Davis, R.E., Christenson, S.C., and Blumer, S.P., 1981, Hydrologic data for the alluvium and terrace aquifer of the Beaver-North Canadian River from the Panhandle to Canton Reservoir, northwestern Oklahoma: U.S. Geological Survey Open-File Report 80-159, Report: iii, 77 p.; Plate: 28.92 x 21.39 inches, https://doi.org/10.3133/ofr80159.","productDescription":"Report: iii, 77 p.; Plate: 28.92 x 21.39 inches","costCenters":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"links":[{"id":142798,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Oklahoma","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -100,\n              36\n            ],\n            [\n              -98.5,\n              36\n            ],\n            [\n              -98.5,\n              37\n            ],\n            [\n              -100,\n              37\n            ],\n            [\n              -100,\n              36\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c62d","contributors":{"authors":[{"text":"Davis, Robert E.","contributorId":10403,"corporation":false,"usgs":true,"family":"Davis","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":157872,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Christenson, Scott C. schris@usgs.gov","contributorId":980,"corporation":false,"usgs":true,"family":"Christenson","given":"Scott","email":"schris@usgs.gov","middleInitial":"C.","affiliations":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"preferred":true,"id":157873,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blumer, Stephen P. spblumer@usgs.gov","contributorId":2419,"corporation":false,"usgs":true,"family":"Blumer","given":"Stephen","email":"spblumer@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":157871,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":8525,"text":"ofr81483 - 1981 - Geohydrology and numerical simulation of the alluvium and terrace aquifer along the Beaver-North Canadian River from the Panhandle to Canton Lake, northwestern Oklahoma","interactions":[],"lastModifiedDate":"2018-11-05T11:39:46","indexId":"ofr81483","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-483","title":"Geohydrology and numerical simulation of the alluvium and terrace aquifer along the Beaver-North Canadian River from the Panhandle to Canton Lake, northwestern Oklahoma","docAbstract":"<p>A quantitative description of the hydrologic system in alluvium and terrace deposits along the Beaver-North Canadian River in northwestern Oklahoma is needed as an aid for planning and management of the aquifer. A two-dimensional finite-difference model was used to describe the aquifer and to predict the effects of future ground-water withdrawals.</p><p>The aquifer principally consists of three geologic units: Alluvium with an average thickness of 30 feet, low terrace deposits with an average thickness of 50 feet, and high terrace deposits with an average thickness of 70 feet. A thin cover of dune sand overlies much of the area and provides an excellent catchment for recharge, but is generally unsaturated.</p><p>Hydraulic conductivity of the aquifer ranges from 0 to 160 feet per day and averages 59 feet per day. Specific yield is estimated to be 0.29. Recharge to the aquifer is approximately 1 inch annually. Under present conditions (1978), most discharge is the result of ground-water flow to the Beaver-North Canadian River at a rate of 36 cubic feet per second and to pumpage for public-supply, industrial, and irrigation use at a rate of 28 cubic feet per second. In 1978, the aquifer had an average saturated thickness of 31 feet and contained 4.07 million acre-feet of water.</p><p>The model was used to predict future head response in the aquifer to various pumping stresses. For any one area, the pumping stress was applied until the saturated thickness for that area was less than 5 feet, at which time the pumping ceased.</p><p>The results of the modeled projections show that if the aquifer is stressed from 1978 to 1993 at the 1977 pumpage rates and well distribution, the average saturated thickness will decrease 1.0 foot and the volume of water in storage will be 3.94 million acre-feet, or 97 percent of the 1978 volume. If the aquifer is stressed at this same rate until 2020, the average saturated thickness will decrease an additional 0.7 foot and the volume of water in storage will be 3.84 million acre-feet, or 94 percent of the 1978 volume.</p><p>If all areas of the aquifer having a 1978 saturated thickness of 5 feet or more are stressed from 1978 to 1993 at a rate of approximately<br>1.4 acre-feet per acre per year, the average saturated thickness will decrease by 20.9 feet and the volume of water in storage will be 1.28 million acre-feet, or 31 percent of the 1978 volume. If the aquifer is stressed at this same rate until 2020, the average saturated thickness will decrease an additional 2.2 feet and the volume of water in storage will be 980,000 acre-feet, or 24 percent of the 1978 volume.</p><p>The water in the aquifer is generally of the calcium bicarbonate type and is suitable for most uses. Most of the 30 water samples analyzed contained less than 500 milligrams of dissolved solids per liter.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81483","usgsCitation":"Davis, R.E., and Christenson, S.C., 1981, Geohydrology and numerical simulation of the alluvium and terrace aquifer along the Beaver-North Canadian River from the Panhandle to Canton Lake, northwestern Oklahoma: U.S. Geological Survey Open-File Report 81-483, Report: vi, 42 p.; 15 Plates, https://doi.org/10.3133/ofr81483.","productDescription":"Report: vi, 42 p.; 15 Plates","numberOfPages":"51","costCenters":[],"links":[{"id":359181,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142797,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0483/report-thumb.jpg"},{"id":359182,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359183,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359184,"rank":15,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359185,"rank":16,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359186,"rank":17,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359176,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359177,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359178,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359179,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359180,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359171,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0483/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359172,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359173,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359174,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359175,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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Robert E.","contributorId":10403,"corporation":false,"usgs":true,"family":"Davis","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":157870,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Christenson, Scott C. schris@usgs.gov","contributorId":980,"corporation":false,"usgs":true,"family":"Christenson","given":"Scott","email":"schris@usgs.gov","middleInitial":"C.","affiliations":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"preferred":true,"id":157869,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8504,"text":"ofr81539 - 1981 - Hydrology of the coal-resource areas in the upper drainages of Huntington and Cottonwood creeks, central Utah","interactions":[],"lastModifiedDate":"2022-08-15T18:16:56.208692","indexId":"ofr81539","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-539","title":"Hydrology of the coal-resource areas in the upper drainages of Huntington and Cottonwood creeks, central Utah","docAbstract":"<p>The hydrology of coal-resource areas in the upper drainages of Huntington and Cottonwood Creeks in central Utah was studied in order to better define the hydrologic system, to identify the hydrologic effects of underground coal mining, and to devise methods to detect the effects.</p><p>Discharge records from gaging stations in this mountainous area indicated that there are large differences in the annual discharge of streams per unit area of drainage. These differences are attributed to differences in precipitation, differences in evaporation and sublimation of the snowpack, and to subsurface movement of water out of some basins. Surface waters sampled during 1977-79 were of good chemical quality; dissolved-solids concentrations rarely exceeded 500 milligrams per liter.</p><p>The Star Point Sandstone and the lower coal-bearing part of the Blackhawk Formation, both of Cretaceous age, are saturated in some areas, and the aquifer yields water to underground coal mines. Most of the larger discharging springs in the study area issue from the Star Point-Blackhawk aquifer where faulted. Ground water also occurs in several water-bearing zones above the Star Point-Blackhawk aquifer. It is not known whether the water in these overlying units is part of a continuous zone of saturation or whether unsaturated zones occur between units and some water is perched.</p><p>Dissolved-solids concentrations in water from about 140 springs ranged from 50 to 750 milligrams per liter. The chemical characteristics of water from the water-bearing zones of different formations usually were very similar.</p><p>Dewatering of underground coal mines was the largest manmade discharge from the Star Point-Blackhawk aquifer in the study area during 1979. The dewatering of mines has decreased the amount of water in storage in the aquifer, but water-level data were not available to define the extent of the depletion. Other possible impacts due to mine dewatering include the diminution of spring flows and increases in ground-water recharge, both of which are more likely to occur where rocks have been fractured due to subsidence above mines. Also, the flows of streams that receive water discharged from mines probably have increased accordingly. The discharge of mine water into streams causes some degradation in surface-water quality, but the quality of ground water is probably not adversely affected by mining.</p><p>Some environmental changes associated with underground mining are difficult to detect without data collected over a long period. With respect to the ground-water system, the year-to-year similarity of spring-discharge recession curves may provide a method to detect some of these changes. Changes in the benthic-invertebrate population may help detect pollution of surface waters.</p><p>Comprehensive studies of the ground-water system are needed in conjunction with hydrologic monitoring in order to fully assess the hydrologic impacts of the underground coal mining.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81539","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources and Energy, Division of Oil, Gas, and Mining","usgsCitation":"Danielson, T.W., ReMillard, M.D., and Fuller, R.H., 1981, Hydrology of the coal-resource areas in the upper drainages of Huntington and Cottonwood creeks, central Utah: U.S. Geological Survey Open-File Report 81-539, Report: vi, 85 p.; 2 Plates: 24.71 x 37.66 inches and 24.58 x 37.93 inches, https://doi.org/10.3133/ofr81539.","productDescription":"Report: vi, 85 p.; 2 Plates: 24.71 x 37.66 inches and 24.58 x 37.93 inches","costCenters":[],"links":[{"id":405144,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0539/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405143,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0539/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405142,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0539/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143564,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0539/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"central Utah","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.39175415039062,\n              39.13645165015621\n            ],\n            [\n              -111.13014221191406,\n              39.13645165015621\n            ],\n            [\n              -111.13014221191406,\n              39.35022841846271\n            ],\n            [\n              -111.39175415039062,\n              39.35022841846271\n            ],\n            [\n              -111.39175415039062,\n              39.13645165015621\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc78b","contributors":{"authors":[{"text":"Danielson, T. W.","contributorId":48590,"corporation":false,"usgs":true,"family":"Danielson","given":"T.","middleInitial":"W.","affiliations":[],"preferred":false,"id":157825,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"ReMillard, Michael D.","contributorId":95748,"corporation":false,"usgs":true,"family":"ReMillard","given":"Michael","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":157827,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fuller, Richard H.","contributorId":66236,"corporation":false,"usgs":true,"family":"Fuller","given":"Richard","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":157826,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":8262,"text":"ofr811005 - 1981 - Hydrologic reconnaissance of the Noatak River basin, Alaska, 1978","interactions":[],"lastModifiedDate":"2012-02-02T00:05:59","indexId":"ofr811005","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-1005","title":"Hydrologic reconnaissance of the Noatak River basin, Alaska, 1978","docAbstract":"Hydrologic data were collected in 1978 described water resources of the Noatak River basin, Alaska. Streamflow varies seasonally. No flow was observed from the upper part of the basin in late winter (April). In the lower part of the basin springs support perennial flow in the Kugururok River and downstream along the Noatak. The discharge of the Noatak was 150 cubic feet per second in April 1978. During the summer, rainstorms are common, and runoff produces high flow. During August 1978, flow was normal in the basin; unit runoff averaged about 1 cubic foot per second per square mile. The Noatak is a gravel-bed stream of moderate slope. It drops about 1,800 feet in elevation from a point near the head waters to the mouth, a distance of 400 miles. Streambed material in most places is gravel, cobbles, and boulders, maximum riffle depths and pool widths increase in a downstream direction. Stream velocity in August 1978 increased from about 1 foot per second in the upper basin to about 4 feet per second in the lower reaches. High-water marks of the maximum evident flood were found at elevations from bankfull to 5 feet above bankfull. Maximum evident flood unit runoff rates were estimated to be less than 50 cubic feet per second per square mile. Scars produced by ice jams were seldom seen above bankfull. Bank erosion appears to be most active in the lowlands. Water in the Noatak River basin is virtually unaffected by man 's activity. Water quality varies with location, weather, season, and source; the water is normally clear, cool, and hard. During late winter sea water intrudes into the Lower Noatak Canyon. Benthic invertebrate community composition and variability suggest the river 's undiminished natural quality. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811005","usgsCitation":"Childers, J.M., and Kernodle, D.R., 1981, Hydrologic reconnaissance of the Noatak River basin, Alaska, 1978: U.S. Geological Survey Open-File Report 81-1005, iv, 47 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr811005.","productDescription":"iv, 47 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":140075,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1005/report-thumb.jpg"},{"id":35876,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1005/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605614","contributors":{"authors":[{"text":"Childers, Joseph M.","contributorId":14379,"corporation":false,"usgs":true,"family":"Childers","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":157444,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kernodle, Donald R.","contributorId":63003,"corporation":false,"usgs":true,"family":"Kernodle","given":"Donald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":157445,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8234,"text":"ofr81412 - 1981 - Selected hydrologic and climatologic data from the Prairie Dog Creek Basin, southeastern Montana, water year 1979","interactions":[],"lastModifiedDate":"2022-11-04T17:28:11.083743","indexId":"ofr81412","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-412","title":"Selected hydrologic and climatologic data from the Prairie Dog Creek Basin, southeastern Montana, water year 1979","docAbstract":"<p>Hydrologic and climatologic data are being collected in a 19-square-mile (49-square-kilometer) basin in southeastern Montana to provide a base for development, calibration, and verification of a precipitation-runoff model. The study area and data-collection stations within the area are shown on a map. A summary of data collected at each station during the first year, beginning in October 1978, is provided in tables. The data include precipitation, snow depth and water content, air temperature, relative humidity, wind run, solar radiation, soil temperature and moisture, stream discharge, chemical analyses of water, and sediment content.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81412","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Cary, L.E., and Johnson, J.D., 1981, Selected hydrologic and climatologic data from the Prairie Dog Creek Basin, southeastern Montana, water year 1979: U.S. Geological Survey Open-File Report 81-412, iv, 73 p., https://doi.org/10.3133/ofr81412.","productDescription":"iv, 73 p.","costCenters":[],"links":[{"id":409169,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0412/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141308,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0412/report-thumb.jpg"}],"country":"United States","state":"Montana","otherGeospatial":"Prairie Dog Creek Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -107.86376953125,\n              44.99588261816546\n            ],\n            [\n              -106.512451171875,\n              44.99588261816546\n            ],\n            [\n              -106.512451171875,\n              45.99314540468519\n            ],\n            [\n              -107.86376953125,\n              45.99314540468519\n            ],\n            [\n              -107.86376953125,\n              44.99588261816546\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8ec7","contributors":{"authors":[{"text":"Cary, Lawrence E.","contributorId":43764,"corporation":false,"usgs":true,"family":"Cary","given":"Lawrence","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":157393,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Joel D.","contributorId":60212,"corporation":false,"usgs":true,"family":"Johnson","given":"Joel","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":157394,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8117,"text":"ofr811116 - 1981 - Simulated hydrologic effects of possible ground-water and surface-water management alternatives in and near the Platte River, south-central Nebraska","interactions":[{"subject":{"id":8117,"text":"ofr811116 - 1981 - Simulated hydrologic effects of possible ground-water and surface-water management alternatives in and near the Platte River, south-central Nebraska","indexId":"ofr811116","publicationYear":"1981","noYear":false,"title":"Simulated hydrologic effects of possible ground-water and surface-water management alternatives in and near the Platte River, south-central Nebraska"},"predicate":"SUPERSEDED_BY","object":{"id":38584,"text":"pp1277 - 1983 - Hydrologic and geomorphic studies of the Platte River basin","indexId":"pp1277","publicationYear":"1983","noYear":false,"title":"Hydrologic and geomorphic studies of the Platte River basin"},"id":1}],"supersededBy":{"id":38584,"text":"pp1277 - 1983 - Hydrologic and geomorphic studies of the Platte River basin","indexId":"pp1277","publicationYear":"1983","noYear":false,"title":"Hydrologic and geomorphic studies of the Platte River basin"},"lastModifiedDate":"2019-07-10T09:32:22","indexId":"ofr811116","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-1116","title":"Simulated hydrologic effects of possible ground-water and surface-water management alternatives in and near the Platte River, south-central Nebraska","docAbstract":"Digital computer models were developed and used to simulate the hydrologic effects of hypothetical water-management alternatives on the wetland habitat area near Grand Island, Nebr. Areally distributed recharge to and discharge from the aquifer system adjacent to the Platte River between Overton and Grand Island were computed for four hypothetical water-management alternatives. Using stream-aquifer response functions, the stream depletions resulting from the different alternatives ranged from 53,000 acre-feet per year for increased surface-water irrigation to 177,000 acre-feet per year for increased ground-water pumpage. Current conditions would result in stream depletions of 125,000 acre-feet per year. Using the relationship between discharge and river stage, frequency curves of the stage in the river near the wildlife habitat area were computed using a 50-year sequence of historical streamflow at Overton, minus the stream depletions resulting from various management practices. For the management alternatives previously discussed, differences in the stage-frequency curves were minimal. For comparative purposes, three additional water-management alternatives whose application would change the incoming streamflow at Overton were simulated. Although in these alternatives the amounts of water that were diverted or imported were similar to the amounts in the previous alternatives, their effects on the stage-frequency curves were much more dramatic. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr811116","usgsCitation":"Burns, A.W., 1981, Simulated hydrologic effects of possible ground-water and surface-water management alternatives in and near the Platte River, south-central Nebraska: U.S. Geological Survey Open-File Report 81-1116, iv, 41 p., https://doi.org/10.3133/ofr811116.","productDescription":"iv, 41 p.","costCenters":[],"links":[{"id":365415,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1116/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140650,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1116/report-thumb.jpg"}],"country":"United States","state":"Nebraska","otherGeospatial":"Platte River","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bddc","contributors":{"authors":[{"text":"Burns, Alan W.","contributorId":41419,"corporation":false,"usgs":true,"family":"Burns","given":"Alan","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":157178,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7925,"text":"ofr811074 - 1981 - Water quality in the tidal Potomac River and estuary, hydrologic data report, 1979 water year","interactions":[],"lastModifiedDate":"2022-04-12T17:34:45.557708","indexId":"ofr811074","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-1074","title":"Water quality in the tidal Potomac River and estuary, hydrologic data report, 1979 water year","docAbstract":"<p>This report contains data on the physical and chemical properties measured during the 1979 water year for the tidal Potomac River and estuary. Data were collected routinely at five major stations and periodically at 14 intervening stations. Each major station represents a cross section through which the transport of selected dissolved and suspended materials will be computed. The intervening stations represent locations at which data were collected for special studies such as: salt water migration, dissolved oxygen dynamics, and other synoptic studies. About 960 samples were analyzed for silicate, Kjeldhal nitrogen, nitrite, phosphorus, chlorophyll and suspended sediment, with additional samples analyzed for organic carbon, calcium, magnesium, sodium, bicarbonate, sulfate, potassium, chloride, fluoride, seston and dissolved solids residue. In addition, about 1400 in-situ measurements of dissolved oxygen, specific conductance, temperature, and Secchi disk transparency are reported.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811074","usgsCitation":"Blanchard, S.F., and Hahl, D.C., 1981, Water quality in the tidal Potomac River and estuary, hydrologic data report, 1979 water year: U.S. Geological Survey Open-File Report 81-1074, iii, 149 p., https://doi.org/10.3133/ofr811074.","productDescription":"iii, 149 p.","costCenters":[],"links":[{"id":398557,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1074/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140721,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1074/report-thumb.jpg"}],"country":"United States","state":"Maryland, Virgina","otherGeospatial":"Potomac River and estuary","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.31353759765625,\n              38.00698412839117\n            ],\n            [\n              -76.3714599609375,\n              38.00698412839117\n            ],\n            [\n              -76.3714599609375,\n              38.556757147352215\n            ],\n            [\n              -77.31353759765625,\n              38.556757147352215\n            ],\n            [\n              -77.31353759765625,\n              38.00698412839117\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c378","contributors":{"authors":[{"text":"Blanchard, Stephen F.","contributorId":54966,"corporation":false,"usgs":true,"family":"Blanchard","given":"Stephen","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":156843,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hahl, D. C.","contributorId":57436,"corporation":false,"usgs":true,"family":"Hahl","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":156844,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7810,"text":"ofr81634 - 1981 - Hydrogeologic data from test drilling near Verna, Florida, 1978","interactions":[],"lastModifiedDate":"2013-08-02T07:16:24","indexId":"ofr81634","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-634","title":"Hydrogeologic data from test drilling near Verna, Florida, 1978","docAbstract":"Four test wells were drilled in the vicinity of the city of Sarasota well field near Verna, Fla., to provide hydrologic and geologic information. An expedient and economical method of air lifting water samples from isolated water-producing zones while drilling was utilized. Lithologic logs of drill cuttings and geophysical logs, including point resistance and spontaneous potential electric logs, gamma-ray logs, and caliper logs, were made. Chemical quality of water was determined for principal producing zones at each well. Dissolved solids from composite water samples ranged from 313 milligrams per liter in test well 0-1 north of the well field to 728 milligrams per liter in test well 0-3 within the well field. Each test well was pumped to determine maximum discharge, water-level drawdown, and recovery time. A leaking pump column on test well 0-1 prevented accurate measurement of drawdown on the well. Test well 0-2, located east of the well field, had a pumping rate of 376 gallons per minute and 13.11 feet of drawdown after 3 hours and 50 minutes; test well 0-3 had a maximum yield of 320 gallons per minute, a drawdown of 31.91 feet after 2 hours and 35 minutes of pumping, had a recovery time of 20 minutes; and test well 0-4, south of the well field, had a pumping rate of 200 gallons per minute with 63.34 feet of drawdown after 2 hours and 35 minutes. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81634","usgsCitation":"Barker, M., Bowman, G., and Sutcliffe, H., 1981, Hydrogeologic data from test drilling near Verna, Florida, 1978: U.S. Geological Survey Open-File Report 81-634, iii, 29 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr81634.","productDescription":"iii, 29 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":140400,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0634/report-thumb.jpg"},{"id":275908,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0634/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628b35","contributors":{"authors":[{"text":"Barker, Michael","contributorId":34917,"corporation":false,"usgs":true,"family":"Barker","given":"Michael","email":"","affiliations":[],"preferred":false,"id":156647,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bowman, Geronia","contributorId":50890,"corporation":false,"usgs":true,"family":"Bowman","given":"Geronia","email":"","affiliations":[],"preferred":false,"id":156648,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sutcliffe, Horace","contributorId":28598,"corporation":false,"usgs":true,"family":"Sutcliffe","given":"Horace","affiliations":[],"preferred":false,"id":156646,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7757,"text":"ofr81421 - 1981 - Background hydrologic information in potential lignite mining areas in Mississippi, August 1980","interactions":[],"lastModifiedDate":"2022-11-04T17:29:59.898863","indexId":"ofr81421","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-421","title":"Background hydrologic information in potential lignite mining areas in Mississippi, August 1980","docAbstract":"<p>The U.S. Geological Survey in cooperation with Mississippi Bureau of Geology is conducting a hydrologic data-collection program in the potential lignite-producing areas in Mississippi. During the week of August 25-28, 1980, hydrologic data on channel characteristics were collected at 15 sites on small streams draining potential lignite mining areas in east-central Mississippi. Streamflow measurements were made and water-quality samples were collected at 11 of the 15 sites.</p><p>Main channel widths at the 15 sampling sites in east-central Mississippi ranged from 126 feet on Sucarnoochee Creek to 15 feet on Houston Creek. Maximum water depth ranged from 7 feet on Pawticfaw Creek and Tallahatta Creek to one-half foot on Okatibbee Creek. The maximum stream discharge measured was 56 cubic feet per second on Pawticfaw Creek. Four sites had no discharge. Specific conductance at sampling sites ranged from 115 micromhos on Ponta Creek to 26 micromhos on Sucarnoochee Creek. The dissolved-oxygen concentration was 5.7 milligrams per liter or higher at all sites. The concentration of suspended sediment was not greater than 38 milligrams per liter at any site. Concentrations of calcium, magnesium, sodium, potassium, chloride, and sulfate were less than 10 milligrams per liter in all samples, but were highest at site 10 on Ponta Creek. Bottom-material samples commonly contained iron, manganese, and zinc.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81421","collaboration":"Prepared in cooperation with the Mississippi Department of Natural Resources, Bureau of Geology","usgsCitation":"Arthur, J.K., 1981, Background hydrologic information in potential lignite mining areas in Mississippi, August 1980: U.S. Geological Survey Open-File Report 81-421, 19 p., https://doi.org/10.3133/ofr81421.","productDescription":"19 p.","costCenters":[],"links":[{"id":409171,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0421/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142244,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0421/report-thumb.jpg"}],"country":"United 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,{"id":7623,"text":"ofr81493 - 1981 - A wind powered, ground-water monitoring installation at a radioactive waste management site in Idaho","interactions":[],"lastModifiedDate":"2022-08-12T19:20:57.323917","indexId":"ofr81493","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-493","title":"A wind powered, ground-water monitoring installation at a radioactive waste management site in Idaho","docAbstract":"<p>In 1971, four wells were drilled just outside a radioactive solid waste storage and disposal facility located on the Idaho National Engineering Laboratory in southeastern Idaho. This facility, the Radioactive Waste Management Complex (RWMC), has been in use since 1952. These wells serve several purposes: to study the geology and hydrology at the RWMC, to determine the potential for radioactive waste migration, and to obtain water samples to determine if waste products are migrating downward into the Snake River Plain aquifer.</p><p>Special efforts are made to insure that surface contamination does not enter the wells by either water, wind, or contaminated equipment. A submersible pump and a continuous water-level measuring device were installed in each well. Permanent installation of this equipment allowed the well heads to be sealed while providing for collection of data from these wells.</p><p>The water-level measuring device is a small diameter, differential-pressure, transducer probe. The transducer produces a variable-reluctance signal which is converted to an analog signal and recorded as the depth to water on a strip chart recorder. Windmill-charged storage batteries provide power for the water-level measuring system. This system is reliable, sensitive, and relatively maintenance free.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81493","usgsCitation":"Bagby, J.C., Ghering, G., Jensen, R.G., and Barr, A.G., 1981, A wind powered, ground-water monitoring installation at a radioactive waste management site in Idaho: U.S. Geological Survey Open-File Report 81-493, ii, 28 p., https://doi.org/10.3133/ofr81493.","productDescription":"ii, 28 p.","costCenters":[],"links":[{"id":405121,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0493/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139729,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0493/report-thumb.jpg"}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d82","contributors":{"authors":[{"text":"Bagby, Jefferson C.","contributorId":9696,"corporation":false,"usgs":true,"family":"Bagby","given":"Jefferson","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":156325,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ghering, G.E.","contributorId":96273,"corporation":false,"usgs":true,"family":"Ghering","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":156328,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jensen, Rodger G.","contributorId":27420,"corporation":false,"usgs":true,"family":"Jensen","given":"Rodger","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":156327,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Barr, A. G.","contributorId":192096,"corporation":false,"usgs":false,"family":"Barr","given":"A.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":156326,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":7616,"text":"ofr81347 - 1981 - Water-resources investigations of the USGS in Texas, fiscal year 1981","interactions":[],"lastModifiedDate":"2017-07-12T10:45:50","indexId":"ofr81347","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-347","title":"Water-resources investigations of the USGS in Texas, fiscal year 1981","docAbstract":"<p>Water-resources investigations in Texas consist of the collection of basic records through the hydrologic-data network, interpretive studies, and research projects. The hydrologic records and the results of investigations are published by the Geological Survey or by cooperating agencies. This report describes the water-resources projects and activities of the Geological Survey in Texas for the 1981 fiscal year (October 1, 1980 to September 30, 1981).</p><p>The Geological Survey's investigations of the water resources of Texas are under the general direction of Jack Rawson, Acting District Chief. The Texas District office is in the Federal Building, 300 East Eighth Street, Austin, Texas 78701.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81347","usgsCitation":"Mitchell, A.A., and Buckner, H., 1981, Water-resources investigations of the USGS in Texas, fiscal year 1981: U.S. Geological Survey Open-File Report 81-347, 44 p., https://doi.org/10.3133/ofr81347.","productDescription":"44 p.","numberOfPages":"47","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":140092,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0347/report-thumb.jpg"},{"id":343678,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0347/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":7611,"text":"ofr81683 - 1981 - Water-resources investigations of the U.S. Geological Survey in Missouri, fiscal year 1981","interactions":[],"lastModifiedDate":"2022-08-16T17:40:29.394795","indexId":"ofr81683","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-683","title":"Water-resources investigations of the U.S. Geological Survey in Missouri, fiscal year 1981","docAbstract":"<p>Water-resources investigations of the U.S. Geological Survey in Missouri consist of collecting hydrologic data and making interpretative investigations. The data and the results of the investigations are published or released by either the U.S. Geological Survey or by cooperating agencies. This report describes the data-collection activities and investigations in Missouri for the 1981 fiscal year and provides an extensive list of water-resources references for the State of Missouri.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81683","usgsCitation":"Kratzer, W.M., 1981, Water-resources investigations of the U.S. Geological Survey in Missouri, fiscal year 1981: U.S. Geological Survey Open-File Report 81-683, i, 60 p., https://doi.org/10.3133/ofr81683.","productDescription":"i, 60 p.","costCenters":[],"links":[{"id":405197,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0683/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140080,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0683/report-thumb.jpg"}],"country":"United 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,{"id":7610,"text":"ofr81348 - 1981 - Water-resources investigations of the U.S. Geological Survey in Kansas; fiscal years 1979 and 1980","interactions":[],"lastModifiedDate":"2017-09-29T08:00:09","indexId":"ofr81348","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-348","title":"Water-resources investigations of the U.S. Geological Survey in Kansas; fiscal years 1979 and 1980","docAbstract":"<p>Activities of the U.S. Geological Survey in Kansas include the systematic collection and analysis of data to describe the framework of hydrologic systems, assess the water resources, define existing or potential problems in the quantity or quality of water, and provide information for optimum development and management of resources. Streamflow studies are made to determine availability of supplies and relations to rainfall runoff, urbanization, flood frequencies, and sediment-transport. Ground-water studies are made to determine the quantity of supplies available in aquifer systems, the effects of natural or artificial contamination, and the effects of withdrawals by irrigation, industrial, and municipal supplies. Water-quality studies are made to define physical, chemical, and biological characteristics in streams and principal aquifers, and to evaluate the chemical changes due to urbanization and surface mining.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81348","usgsCitation":"McGovern, H.E., and Combs, L., 1981, Water-resources investigations of the U.S. Geological Survey in Kansas; fiscal years 1979 and 1980: U.S. Geological Survey Open-File Report 81-348, 107 p., https://doi.org/10.3133/ofr81348.","productDescription":"107 p.","numberOfPages":"111","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":346196,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0348/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139976,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0348/report-thumb.jpg"}],"country":"United 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,{"id":7609,"text":"ofr81150 - 1981 - Water-resources investigations of the U.S. Geological Survey in Colorado: fiscal year 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:05:58","indexId":"ofr81150","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-150","title":"Water-resources investigations of the U.S. Geological Survey in Colorado: fiscal year 1981","docAbstract":"The report provides an overview of water-resources data collection and hydrologic investigations in Colorado from October 1, 1980, to September 30, 1981. Most of the work is carried out in cooperation with 51 Federal, State, and local agencies. Data are being collected at 503 surface-water gaging stations, 161 surface-water quality stations, and 1,151 observation wells. Sixty-seven hydrologic investigations are underway and are described in the report by a map showing the location of the study area and a statement of the purpose, objective, approach, progress, and plans. Twelve of the investigations are statewide, 6 are regional, 9 are in the Missouri River basin, 8 in the Arkansas River basin, 6 in the Rio Grande basin, and 5 are multistate. Listed in the report are references to 9 data reports and 27 interpretive reports released or published in fiscal year 1980 as a result of water-resources investigations in Colorado. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81150","usgsCitation":"Price, W., 1981, Water-resources investigations of the U.S. Geological Survey in Colorado: fiscal year 1981: U.S. Geological Survey Open-File Report 81-150, v, 136 p., 1 over-size sheet, scale 1:500,000 ;28 cm., https://doi.org/10.3133/ofr81150.","productDescription":"v, 136 p., 1 over-size sheet, scale 1:500,000 ;28 cm.","costCenters":[],"links":[{"id":139975,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0150/report-thumb.jpg"},{"id":35099,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0150/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35100,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0150/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4e5b","contributors":{"authors":[{"text":"Price, W.E.","contributorId":17989,"corporation":false,"usgs":true,"family":"Price","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":156298,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7505,"text":"ofr81401 - 1981 - Selective annotated bibliography of geology and ground-water resources for the Montana part of the Northern Great Plains regional aquifer-system analysis","interactions":[],"lastModifiedDate":"2012-02-02T00:06:11","indexId":"ofr81401","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-401","title":"Selective annotated bibliography of geology and ground-water resources for the Montana part of the Northern Great Plains regional aquifer-system analysis","docAbstract":"Increasing demand for water to meet needs for energy, industry, irrigation, domestic, and municipal uses has resulted in a study of the geology and hydrology of rocks of Mesozoic and Cenozoic age. This report presents the results of a literature search for the part of the study area in Montana. It consists of an annotated listing of pertinent published reports, a partial subject and area index of the reports, and a correlation chart of geologic and aquifer units listed in the annotations. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81401","usgsCitation":"Levings, J.F., Levings, G.W., Feltis, R., Hotchkiss, W.R., and Lee, R.W., 1981, Selective annotated bibliography of geology and ground-water resources for the Montana part of the Northern Great Plains regional aquifer-system analysis: U.S. Geological Survey Open-File Report 81-401, iii, 93 p., 1 over-size sheet ;26 cm., https://doi.org/10.3133/ofr81401.","productDescription":"iii, 93 p., 1 over-size sheet ;26 cm.","costCenters":[],"links":[{"id":142181,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0401/report-thumb.jpg"},{"id":34959,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0401/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34960,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0401/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a00e4b07f02db5f7d3b","contributors":{"authors":[{"text":"Levings, Julianne F.","contributorId":29818,"corporation":false,"usgs":true,"family":"Levings","given":"Julianne","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":155922,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Levings, G. W.","contributorId":12485,"corporation":false,"usgs":true,"family":"Levings","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":155921,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Feltis, R.D.","contributorId":93467,"corporation":false,"usgs":true,"family":"Feltis","given":"R.D.","affiliations":[],"preferred":false,"id":155925,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hotchkiss, W. R.","contributorId":61820,"corporation":false,"usgs":true,"family":"Hotchkiss","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":155923,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lee, R. W.","contributorId":86757,"corporation":false,"usgs":true,"family":"Lee","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":155924,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":7422,"text":"ofr811187 - 1981 - Preliminary appraisal of the hydrology of the Blocker area, Pittsburg County, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:06:04","indexId":"ofr811187","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-1187","title":"Preliminary appraisal of the hydrology of the Blocker area, Pittsburg County, Oklahoma","docAbstract":"Bedrock in the Blocker area of southeastern Oklahoma consists principally of shale, siltstone, and sandstone of the Boggy and Savanna Formations of Pennsylvanian age. These rocks have been folded to form the Panther Mountain syncline on the south and the Kinta anticline on the north. Alluvium along streams is less than 15 feet thick and consists mainly of sandy silt. Water in bedrock is under artesian conditions. Well depths range from 11 to 213 feet and average 75 feet. In 86% of the wells measured, the water level was less than 30 feet below the land surface. Because the rocks have minimal permeability, well yields probably are less than 5 gallons per minute. Ground water is commonly a mixed cation bicarbonate type with dissolved solids ranging from about 300 to 2,000 milligrams per liter. No relationship between water chemistry and well depth or geographic distribution is apparent. Streams in the area are ephemeral and there are extended periods of no flow. Blue Creek was dry 30% of the time during 1976-80 and had flows of less than 0.1 cubic foot per second for at least 80 consecutive days. Stream water is generally a mixed cation sulfate type. The maximum dissolved-solids concentration determined in stream water was 3670 milligrams per liter. Maximum suspended sediment discharge, in tons per day, was about 235 for Blue Creek, 40 for Blue Creek tributary, and 630 for Mathuldy Creek. Silt-clay particles (diameters less than 0.062 millimeter) are the dominant sediment size. Surface mining for coal undoubtedly will have some effect on the environment. The most likely deleterious effects are increased sediment loads in streams and increased mineralization of stream waters. However, these effects should be of only limited extent and duration if appropriate mining and reclamation practices are followed. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811187","usgsCitation":"Marcher, M.V., Bergman, D.L., Stoner, J., and Blumer, S.P., 1981, Preliminary appraisal of the hydrology of the Blocker area, Pittsburg County, Oklahoma: U.S. Geological Survey Open-File Report 81-1187, iv, 52 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr811187.","productDescription":"iv, 52 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":140449,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1187/report-thumb.jpg"},{"id":34831,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1187/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34832,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1187/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34833,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1187/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34834,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1187/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67ca5b","contributors":{"authors":[{"text":"Marcher, Melvin V.","contributorId":11590,"corporation":false,"usgs":true,"family":"Marcher","given":"Melvin","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":155545,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bergman, D. L.","contributorId":93038,"corporation":false,"usgs":true,"family":"Bergman","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":155548,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stoner, J.D.","contributorId":58261,"corporation":false,"usgs":true,"family":"Stoner","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":155547,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Blumer, S. P.","contributorId":23938,"corporation":false,"usgs":true,"family":"Blumer","given":"S.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":155546,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":7312,"text":"ofr8174 - 1981 - Methodology for hydrologic evaluation of a potential surface mine: The Tsosie Swale basin, San Juan County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:03","indexId":"ofr8174","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-74","title":"Methodology for hydrologic evaluation of a potential surface mine: The Tsosie Swale basin, San Juan County, New Mexico","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8174","usgsCitation":"Shown, L., Frickel, D., Hadley, R.F., and Miller, R., 1981, Methodology for hydrologic evaluation of a potential surface mine: The Tsosie Swale basin, San Juan County, New Mexico: U.S. Geological Survey Open-File Report 81-74, vi, 63 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr8174.","productDescription":"vi, 63 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":140619,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0074/report-thumb.jpg"},{"id":34702,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0074/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629fcb","contributors":{"authors":[{"text":"Shown, L. M.","contributorId":43757,"corporation":false,"usgs":true,"family":"Shown","given":"L. M.","affiliations":[],"preferred":false,"id":155176,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frickel, D. G.","contributorId":11213,"corporation":false,"usgs":true,"family":"Frickel","given":"D. G.","affiliations":[],"preferred":false,"id":155174,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hadley, R. F.","contributorId":27028,"corporation":false,"usgs":true,"family":"Hadley","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":155175,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, R.F.","contributorId":83882,"corporation":false,"usgs":true,"family":"Miller","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":155177,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":7311,"text":"ofr8175 - 1981 - Methodology for hydrologic evaluation of a potential surface mine, Red Rim Site, Carbon and Sweetwater counties, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:06:03","indexId":"ofr8175","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-75","title":"Methodology for hydrologic evaluation of a potential surface mine, Red Rim Site, Carbon and Sweetwater counties, Wyoming","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8175","usgsCitation":"Frickel, D.G., Shown, L., Hadley, R.F., and Miller, R., 1981, Methodology for hydrologic evaluation of a potential surface mine, Red Rim Site, Carbon and Sweetwater counties, Wyoming: U.S. Geological Survey Open-File Report 81-75, vi, 65 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr8175.","productDescription":"vi, 65 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":140618,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0075/report-thumb.jpg"},{"id":34701,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0075/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629fbe","contributors":{"authors":[{"text":"Frickel, Donald G.","contributorId":23524,"corporation":false,"usgs":true,"family":"Frickel","given":"Donald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":155170,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shown, L. M.","contributorId":43757,"corporation":false,"usgs":true,"family":"Shown","given":"L. M.","affiliations":[],"preferred":false,"id":155172,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hadley, R. F.","contributorId":27028,"corporation":false,"usgs":true,"family":"Hadley","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":155171,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, R.F.","contributorId":83882,"corporation":false,"usgs":true,"family":"Miller","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":155173,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":7249,"text":"ofr81815 - 1981 - Hydrology of Area 7, Eastern Coal Province, Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:05:49","indexId":"ofr81815","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-815","title":"Hydrology of Area 7, Eastern Coal Province, Ohio","docAbstract":"The U.S. Geological Survey established 24 study areas in Eastern Appalachian Coal Province to appraise the hydrology and water resources from Alabama to Pennsylvania. Chemical, physical, biological, and streamflow data were collected from 138 synoptic sites in Area 7, eastern Ohio. The data are evaluated and presented in this report. Area 7 lies within the drainage basins of Muskingum Rivers and Duck and Willis Creeks in eastern Ohio. Walhounding, Tuscarawas, and Little Muskingum, and Muskingum Rivers and Wills and Duck Creeks are the major streams draining the study area.\r\n\r\nIn Ohio, surface and subsurface coal mining has altered the environment. In areas where land has been reclaimed, the environmental stress expected to be temporary. Hydrologic problems related to coal mining are erosion and sedimentation which degrade water-quality. Based on available sediment data, suspended sediment concentration were highest in abandoned mine areas, followed by currently mined and reclaimed areas, and lowest in unmined areas.\r\n\r\nLow pH, high specific conductance, high concentrations of iron, sulfate and manganese, increased sediment yields, discoloration of streambeds, limited aquatic vegetation and animal life typify streams draining areas with abandoned mines. In abandoned mine areas, the specific conductance of water ranged from 800 to 2,300 micromhos; pH ranged from 2.8 to 5.8; dissolved-iron concentrations ranged from 1,000 to 85,000 micrograms per liter; dissolved-sulfate concentrations ranged from 14 to 1,200 milligrams per liter and dissolved-manganese concentration commonly exceeded 2,000 micrograms per liter. Red and yellow coloration on the streambeds were precipitates from the hydrolysis of iron, manganese, and sulfate minerals carried into the stream channel by increased sediment erosion from abandoned coal mines. Trace metal concentrations (arsenic, cadmium, chromium, cobalt, copper, lead, mercury, selenium, and zinc) were generally low. Degradation of fish habitat is illustrated by conceptual model of the aquatic biology related to water chemistry.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81815","usgsCitation":"Engelke, M.J., Roth, D., and and others, 1981, Hydrology of Area 7, Eastern Coal Province, Ohio: U.S. Geological Survey Open-File Report 81-815, v, 60 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/ofr81815.","productDescription":"v, 60 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":94764,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0815/report.pdf","size":"21723","linkFileType":{"id":1,"text":"pdf"}},{"id":139916,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0815/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e780","contributors":{"authors":[{"text":"Engelke, Morris J. Jr.","contributorId":100379,"corporation":false,"usgs":true,"family":"Engelke","given":"Morris","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":154898,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roth, D.K.","contributorId":60275,"corporation":false,"usgs":true,"family":"Roth","given":"D.K.","email":"","affiliations":[],"preferred":false,"id":154897,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"and others","contributorId":127886,"corporation":true,"usgs":false,"organization":"and others","id":528824,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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