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,{"id":27457,"text":"wri8244 - 1982 - Preliminary evaluation of the ground-water-flow system in the Twin Cities Metropolitan area, Minnesota","interactions":[],"lastModifiedDate":"2018-03-12T11:43:11","indexId":"wri8244","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-44","title":"Preliminary evaluation of the ground-water-flow system in the Twin Cities Metropolitan area, Minnesota","docAbstract":"<p>A preliminary quasi-three-dimensional finite-difference ground-water-flow model of the seven-county Twin Cities Metropolitan area was constructed and used to evaluate parameter sensitivity and adequacy of available data. Fourteen geologic units that underlie the study area were grouped into nine hydr,bgeologic units and were incorporated into a five-layer model. The layers in the simulation model include the Mount SimonHinckley, Ironton-Galesville, Prairie du Chien-Jordan, and St. Peter aquifers, and the drift.</p>\n<p>Sensitivity analyses were made for 19 parameter and boundary-condition specifications. Model results are -most sensitive to recharge and withdrawal rates and to hydrogeologic variations related to drift-filled bedrock valleys. Analyses of available data and results of steady-state simulations indicate that critical data needs for improving the simulation model include spatial and temporal variations in ground-water withdrawals and potentiometric levels, and hydraulic properties of drift filling or partly filling bedrock valleys.</p>\n<p>Areal distribution of calcium, sodium, sulfate, and chloride concentrations were analyzed to provide information on the hydrologic and geochemical relationships between aquifers. Ground water is generally of the calcium magnesium bicarbonate type. Concentration of dissolved solids in water from the Jordan Sandstone and Mount Simon-Hinckley aquifer generally decreases from southwest to northeast across the study area. This decrease probably reflects differences in the quality of recharge water and geochemical processes within the aquifers, such as ion exchange.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri8244","collaboration":"Prepared in cooperation with the Metropolitan Council of the Twin Cities, Minnesota Department of Natural Resources, Minnesota Geological Survey","usgsCitation":"Guswa, J.H., Siegel, D., and Gillies, D.C., 1982, Preliminary evaluation of the ground-water-flow system in the Twin Cities Metropolitan area, Minnesota: U.S. Geological Survey Water-Resources Investigations Report 82-44, v, 65 p., https://doi.org/10.3133/wri8244.","productDescription":"v, 65 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":157946,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0044/report-thumb.jpg"},{"id":95634,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0044/report.pdf","size":"7263","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Twin Cites Metropolitan area","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-93.5093,45.4163],[-93.1289,45.4153],[-93.0186,45.4131],[-93.0188,45.2984],[-92.7894,45.297],[-92.7439,45.2963],[-92.7516,45.2935],[-92.7551,45.2927],[-92.7583,45.2904],[-92.7597,45.2872],[-92.7604,45.2845],[-92.7591,45.2794],[-92.7559,45.2739],[-92.7527,45.2694],[-92.7515,45.2657],[-92.7526,45.2626],[-92.7535,45.2584],[-92.7561,45.2541],[-92.7575,45.2502],[-92.7569,45.2443],[-92.7557,45.2397],[-92.7553,45.2356],[-92.7538,45.2305],[-92.7536,45.2276],[-92.7521,45.2236],[-92.752,45.2196],[-92.7527,45.2168],[-92.7546,45.2136],[-92.7573,45.2107],[-92.7603,45.2065],[-92.7619,45.2041],[-92.7632,45.2009],[-92.7637,45.1972],[-92.764,45.1895],[-92.7629,45.1853],[-92.7557,45.178],[-92.7522,45.1759],[-92.7493,45.173],[-92.748,45.1698],[-92.7472,45.1634],[-92.7483,45.1597],[-92.7475,45.1551],[-92.7473,45.1515],[-92.7484,45.1483],[-92.749,45.1419],[-92.7484,45.1373],[-92.7441,45.1264],[-92.7415,45.1172],[-92.7422,45.1135],[-92.7446,45.11],[-92.7467,45.1076],[-92.7513,45.1045],[-92.7591,45.0999],[-92.7624,45.0972],[-92.7803,45.0849],[-92.7847,45.083],[-92.7885,45.0806],[-92.7917,45.0791],[-92.795,45.0772],[-92.7982,45.0746],[-92.8001,45.0723],[-92.8019,45.0647],[-92.8016,45.0597],[-92.8005,45.0567],[-92.7984,45.0531],[-92.7952,45.0499],[-92.7926,45.0481],[-92.7881,45.0453],[-92.7837,45.0421],[-92.7745,45.0373],[-92.7707,45.0344],[-92.7683,45.0325],[-92.7645,45.0265],[-92.7639,45.0237],[-92.7639,45.0196],[-92.7682,45.0005],[-92.7694,44.9909],[-92.7686,44.9796],[-92.7646,44.9711],[-92.7547,44.9571],[-92.7527,44.9527],[-92.7523,44.9481],[-92.753,44.9369],[-92.7534,44.9237],[-92.7547,44.9159],[-92.7569,44.9105],[-92.7606,44.9068],[-92.7645,44.9046],[-92.767,44.9039],[-92.7707,44.9023],[-92.7729,44.901],[-92.775,44.8982],[-92.7738,44.8933],[-92.7689,44.8848],[-92.7632,44.8759],[-92.7628,44.8716],[-92.763,44.8671],[-92.7644,44.8622],[-92.7682,44.8554],[-92.7683,44.853],[-92.7671,44.8494],[-92.7652,44.8462],[-92.7646,44.8423],[-92.7644,44.8382],[-92.766,44.8308],[-92.7679,44.8265],[-92.7719,44.8211],[-92.7751,44.8161],[-92.7784,44.8125],[-92.7801,44.8095],[-92.781,44.8056],[-92.7823,44.8029],[-92.783,44.7966],[-92.7858,44.7893],[-92.7909,44.7842],[-92.7993,44.7765],[-92.802,44.7729],[-92.8046,44.7683],[-92.8059,44.7624],[-92.8073,44.7524],[-92.8061,44.7483],[-92.8054,44.7473],[-92.8022,44.7446],[-92.7901,44.7381],[-92.7805,44.7344],[-92.7722,44.7317],[-92.7658,44.7289],[-92.7569,44.7234],[-92.7536,44.7226],[-92.7471,44.7204],[-92.7415,44.7192],[-92.7339,44.7157],[-92.737,44.658],[-92.7386,44.6329],[-92.7957,44.6305],[-92.7915,44.5452],[-92.9165,44.5449],[-92.9179,44.5221],[-92.9218,44.518],[-92.9282,44.5158],[-92.9321,44.513],[-92.941,44.5149],[-92.9449,44.5131],[-92.9494,44.5104],[-92.9584,44.514],[-92.9634,44.5177],[-92.975,44.5159],[-92.9827,44.5173],[-92.991,44.5215],[-93.0057,44.5197],[-93.0121,44.5175],[-93.0166,44.5166],[-93.0275,44.5198],[-93.0301,44.5148],[-93.0346,44.5148],[-93.039,44.5171],[-93.0406,44.4729],[-93.2826,44.473],[-93.2798,44.546],[-93.5259,44.5466],[-93.9091,44.5446],[-93.9117,44.5492],[-93.9078,44.5528],[-93.9027,44.5524],[-93.9008,44.5492],[-93.8956,44.5483],[-93.8937,44.5515],[-93.8963,44.5561],[-93.9008,44.5606],[-93.8996,44.5647],[-93.8957,44.5675],[-93.8958,44.5711],[-93.8996,44.5743],[-93.8958,44.5775],[-93.8939,44.5807],[-93.8959,44.5871],[-93.8991,44.5903],[-93.8908,44.5962],[-93.8857,44.5967],[-93.8838,44.6012],[-93.878,44.6013],[-93.878,44.6077],[-93.8716,44.6063],[-93.8658,44.6063],[-93.8569,44.6168],[-93.8563,44.6218],[-93.8505,44.6219],[-93.8447,44.6201],[-93.8422,44.6233],[-93.8358,44.6242],[-93.8319,44.6251],[-93.8217,44.6297],[-93.8031,44.6366],[-93.7999,44.6361],[-93.7967,44.6343],[-93.7935,44.6311],[-93.7883,44.632],[-93.78,44.6362],[-93.7768,44.6385],[-93.7729,44.6366],[-93.7723,44.6325],[-93.7691,44.6312],[-93.7665,44.6362],[-93.7685,44.6417],[-93.7686,44.675],[-93.8887,44.6756],[-93.8902,44.7185],[-94.0104,44.719],[-94.0085,44.8947],[-94.0136,44.8951],[-94.0117,44.9796],[-93.7692,44.9789],[-93.7702,45.0734],[-93.7663,45.077],[-93.7631,45.0839],[-93.7534,45.0853],[-93.7399,45.0894],[-93.7341,45.0922],[-93.7322,45.0963],[-93.7257,45.1022],[-93.7225,45.11],[-93.72,45.1205],[-93.7155,45.1269],[-93.7019,45.1374],[-93.6852,45.1489],[-93.6793,45.1525],[-93.6716,45.1562],[-93.6574,45.1585],[-93.6554,45.1599],[-93.6529,45.1631],[-93.6503,45.169],[-93.6516,45.1841],[-93.6549,45.1905],[-93.6555,45.1969],[-93.6562,45.201],[-93.6471,45.2079],[-93.6387,45.2074],[-93.6361,45.206],[-93.6329,45.2056],[-93.6258,45.2092],[-93.6167,45.2115],[-93.6096,45.2111],[-93.6031,45.2111],[-93.5967,45.2134],[-93.5857,45.2189],[-93.5792,45.2189],[-93.5734,45.2202],[-93.5676,45.2225],[-93.5617,45.2289],[-93.554,45.2298],[-93.5462,45.2289],[-93.5371,45.2294],[-93.5332,45.2317],[-93.5197,45.2417],[-93.5158,45.2458],[-93.5138,45.2454],[-93.5093,45.4163]]]},\"properties\"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John H.","contributorId":97881,"corporation":false,"usgs":true,"family":"Guswa","given":"John","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":198151,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Siegel, Donald I.","contributorId":97499,"corporation":false,"usgs":true,"family":"Siegel","given":"Donald I.","affiliations":[],"preferred":false,"id":198150,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gillies, Daniel C.","contributorId":39824,"corporation":false,"usgs":true,"family":"Gillies","given":"Daniel","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":198149,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26400,"text":"wri8245 - 1982 - Delineation and hydrologic effects of a gasoline leak at Stovepipe Wells Hotel, Death Valley National Monument, California","interactions":[],"lastModifiedDate":"2019-08-05T11:21:19","indexId":"wri8245","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-45","title":"Delineation and hydrologic effects of a gasoline leak at Stovepipe Wells Hotel, Death Valley National Monument, California","docAbstract":"Ground water is the only local source of water available to the Stovepipe Wells Hotel facilities of the Death Valley National Monument, California. A leak in a service station storage tank caused the formation of a gasoline layer overlying the water table, creating the potential for contamination of the water supply. The maximum horizontal extent of the gasoline layer was mathematically estimated to be 1,300 feet downgradient from the leaky gasoline tank. Exploratory drilling detected the gasoline layer between 900 and 1,400 feet downgradient and between 50 and 150 feet upgradient from the source. Traces of the soluble components of gasoline were also found in the aquifer 150 feet upgradient, and 250 feet distant from the source perpendicular to the direction of ground-water movement. The gasoline spill is not likely to have an effect on the supply wells located 0.4 mile south of the leak source, which is nearly perpendicular to the direction of ground-water movement and the primary direction of gasoline movement in the area. No effect on phreatophytes 2 miles downgradient from the layer is likely, but the potential effects of gasoline vapors within the unsaturated zone on local xerophytes are not known. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8245","usgsCitation":"Buono, A., and Packard, E.M., 1982, Delineation and hydrologic effects of a gasoline leak at Stovepipe Wells Hotel, Death Valley National Monument, California: U.S. Geological Survey Water-Resources Investigations Report 82-45, iv, 23 p. , https://doi.org/10.3133/wri8245.","productDescription":"iv, 23 p. ","costCenters":[],"links":[{"id":157879,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0045/report-thumb.jpg"},{"id":366241,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0045/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Death Valley National Monument","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.14996337890625,\n              36.605055259475584\n            ],\n            [\n              -117.14275360107422,\n              36.605055259475584\n            ],\n            [\n              -117.14275360107422,\n              36.60774238525424\n            ],\n            [\n              -117.14996337890625,\n              36.60774238525424\n            ],\n            [\n              -117.14996337890625,\n              36.605055259475584\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671cbe","contributors":{"authors":[{"text":"Buono, A.","contributorId":61034,"corporation":false,"usgs":true,"family":"Buono","given":"A.","email":"","affiliations":[],"preferred":false,"id":196323,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Packard, Elaine M.","contributorId":99593,"corporation":false,"usgs":true,"family":"Packard","given":"Elaine","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":196324,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10568,"text":"ofr81128 - 1982 - Sediment and channel-geometry investigations for the Kansas River bank stabilization study, Kansas, Nebraska, and Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:28","indexId":"ofr81128","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-128","title":"Sediment and channel-geometry investigations for the Kansas River bank stabilization study, Kansas, Nebraska, and Colorado","docAbstract":"Analysis of hydrologic data from the Kansas River basin suggests that the channels of the lower Solomon, Saline, and Smoky Hill Rivers have narrowed and stabilized as a result of construction of upstream reservoirs. The Kansas River channel, however, remains relatively unstable and locally active. Streamflow regulation and sediment trapping by reservoirs are possible causes of changes occurring at various Kansas River sites. An inferred deficiency of the suspended-sediment load, however, is likely to cause continuing instability. Suspended sediment in the Kansas River apparently is too sparse to form and maintain stable alluvial banks. The deficiency probably results in an increase of bed material movement, general channel widening, and local braiding. Significant channel degradation is lacking at most sites, but may occur in response to long-term (decades-to-centuries) regulation. Recent degradation near Bonner Springs, Kans., may be the result of sand and gravel removal. Any imposed changes that shorten the channel or reduce the suspended-sediment discharge of the Kansas River are expected to cause additional channel instability. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81128","usgsCitation":"Osterkamp, W.R., Curtis, R., and Crowther, H., 1982, Sediment and channel-geometry investigations for the Kansas River bank stabilization study, Kansas, Nebraska, and Colorado: U.S. Geological Survey Open-File Report 81-128, 71 p.  :ill., maps ;28 cm., https://doi.org/10.3133/ofr81128.","productDescription":"71 p.  :ill., maps ;28 cm.","costCenters":[],"links":[{"id":144152,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0128/report-thumb.jpg"},{"id":38401,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0128/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae003","contributors":{"authors":[{"text":"Osterkamp, W. R.","contributorId":46044,"corporation":false,"usgs":true,"family":"Osterkamp","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161607,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Curtis, R.E.","contributorId":80741,"corporation":false,"usgs":true,"family":"Curtis","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":161608,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crowther, H.G.","contributorId":86629,"corporation":false,"usgs":true,"family":"Crowther","given":"H.G.","email":"","affiliations":[],"preferred":false,"id":161609,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10555,"text":"ofr8278 - 1982 - Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois; Part II, geology and hydrology of the glacial drift as related to the migration of tritium","interactions":[{"subject":{"id":10555,"text":"ofr8278 - 1982 - Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois; Part II, geology and hydrology of the glacial drift as related to the migration of tritium","indexId":"ofr8278","publicationYear":"1982","noYear":false,"title":"Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois; Part II, geology and hydrology of the glacial drift as related to the migration of tritium"},"predicate":"SUPERSEDED_BY","object":{"id":2414,"text":"wsp2226 - 1984 - Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois: Geology and hydrology of the glacial drift, as related to the migration of tritium","indexId":"wsp2226","publicationYear":"1984","noYear":false,"title":"Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois: Geology and hydrology of the glacial drift, as related to the migration of tritium"},"id":1}],"supersededBy":{"id":2414,"text":"wsp2226 - 1984 - Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois: Geology and hydrology of the glacial drift, as related to the migration of tritium","indexId":"wsp2226","publicationYear":"1984","noYear":false,"title":"Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois: Geology and hydrology of the glacial drift, as related to the migration of tritium"},"lastModifiedDate":"2019-11-07T11:35:12","indexId":"ofr8278","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-78","title":"Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois; Part II, geology and hydrology of the glacial drift as related to the migration of tritium","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr8278","usgsCitation":"Olimpio, J., 1982, Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois; Part II, geology and hydrology of the glacial drift as related to the migration of tritium: U.S. Geological Survey Open-File Report 82-78, v, 57 p., https://doi.org/10.3133/ofr8278.","productDescription":"v, 57 p.","costCenters":[],"links":[{"id":142501,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0078/report-thumb.jpg"},{"id":369038,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0078/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Illinois","otherGeospatial":"Palos Forest Preserve","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.9290771484375,\n              41.66162721430806\n            ],\n            [\n              -87.83294677734375,\n              41.66162721430806\n            ],\n            [\n              -87.83294677734375,\n              41.72213058512578\n            ],\n            [\n              -87.9290771484375,\n              41.72213058512578\n            ],\n            [\n              -87.9290771484375,\n              41.66162721430806\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db64880f","contributors":{"authors":[{"text":"Olimpio, J.C.","contributorId":36137,"corporation":false,"usgs":true,"family":"Olimpio","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":161585,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8664,"text":"ofr82442 - 1982 - Data management system for USGS/USEPA urban hydrology studies program","interactions":[],"lastModifiedDate":"2012-02-02T00:06:11","indexId":"ofr82442","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-442","title":"Data management system for USGS/USEPA urban hydrology studies program","docAbstract":"A data management system was developed to store, update, and retrieve data collected in urban stormwater studies jointly conducted by the U.S. Geological Survey and U.S. Environmental Protection Agency in 11 cities in the United States. The data management system is used to retrieve and combine data from USGS data files for use in rainfall, runoff, and water-quality models and for data computations such as storm loads. The system is based on the data management aspect of the Statistical Analysis System (SAS) and was used to create all the data files in the data base. SAS is used for storage and retrieval of basin physiography, land-use, and environmental practices inventory data. Also, storm-event water-quality characteristics are stored in the data base. The advantages of using SAS to create and manage a data base are many with a few being that it is simple, easy to use, contains a comprehensive statistical package, and can be used to modify files very easily. Data base system development has progressed rapidly during the last two decades and the data managment system concepts used in this study reflect the advancement made in computer technology during this era. Urban stormwater data is, however, just one application for which the system can be used. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82442","usgsCitation":"Doyle, W., and Lorens, J., 1982, Data management system for USGS/USEPA urban hydrology studies program: U.S. Geological Survey Open-File Report 82-442, vi, 278 p. ill. ;28 cm., https://doi.org/10.3133/ofr82442.","productDescription":"vi, 278 p. ill. ;28 cm.","costCenters":[],"links":[{"id":141155,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0442/report-thumb.jpg"},{"id":36263,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0442/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b3d1","contributors":{"authors":[{"text":"Doyle, W.H. Jr.","contributorId":59029,"corporation":false,"usgs":true,"family":"Doyle","given":"W.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":158114,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lorens, J.A.","contributorId":15201,"corporation":false,"usgs":true,"family":"Lorens","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":158113,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":20415,"text":"ofr82696 - 1982 - Hydrologic data from Naval Oil Shale Reserves, Parachute Creek basin, northwestern Colorado, 1975-79","interactions":[],"lastModifiedDate":"2012-02-02T00:07:39","indexId":"ofr82696","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-696","title":"Hydrologic data from Naval Oil Shale Reserves, Parachute Creek basin, northwestern Colorado, 1975-79","docAbstract":"This report summarizes data collected by the U.S. Geological Survey for the U.S. Department of Energy, Naval Petroleum, and Oil Shale Reserves in the Parachute Creek drainage basin of western Colorado. It includes data from five surface-water gages, two automatic sediment samplers and two water-quality monitors. Instantaneous streamflow measurements were made at 63 sites on Parachute Creek tributaries to determine gain or loss of flow. Thirteen springs and nine surface-water sites were sampled and chemical analyses of these sites are included. From 1975 to 1979, 88 spring sites were inventoried; conductivity, temperature, pH, and discharge were measured. Climate data include maximum, minimum, and total daily solar radiation. Daily total precipitation is reported for three stations and snow-course data is reported for one site.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82696","usgsCitation":"Patt, R.O., Adams, D.B., and Collins, D.L., 1982, Hydrologic data from Naval Oil Shale Reserves, Parachute Creek basin, northwestern Colorado, 1975-79: U.S. Geological Survey Open-File Report 82-696, v, 134 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82696.","productDescription":"v, 134 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":152090,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0696/report-thumb.jpg"},{"id":49957,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0696/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db6077cc","contributors":{"authors":[{"text":"Patt, Ralph O.","contributorId":61450,"corporation":false,"usgs":true,"family":"Patt","given":"Ralph","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":182611,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adams, D. Briane","contributorId":35707,"corporation":false,"usgs":true,"family":"Adams","given":"D.","email":"","middleInitial":"Briane","affiliations":[],"preferred":false,"id":182610,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Collins, Dannie L.","contributorId":77925,"corporation":false,"usgs":true,"family":"Collins","given":"Dannie","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":182612,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":49705,"text":"ofr82640 - 1982 - Hydrology of the Somerset area, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:11:13","indexId":"ofr82640","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-640","title":"Hydrology of the Somerset area, Kentucky","language":"ENGLISH","doi":"10.3133/ofr82640","usgsCitation":"Davis, R.W., 1982, Hydrology of the Somerset area, Kentucky: U.S. Geological Survey Open-File Report 82-640, p. 47, https://doi.org/10.3133/ofr82640.","productDescription":"p. 47","costCenters":[],"links":[{"id":175579,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdb19","contributors":{"authors":[{"text":"Davis, R. W.","contributorId":93459,"corporation":false,"usgs":true,"family":"Davis","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":240129,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43692,"text":"ofr82258 - 1982 - Hydrologic maps of Ogallala Aquifer, west-central Kansas, 1979-81","interactions":[],"lastModifiedDate":"2012-02-02T00:10:10","indexId":"ofr82258","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-258","title":"Hydrologic maps of Ogallala Aquifer, west-central Kansas, 1979-81","docAbstract":"A mathematical technique, called kriging, was programmed for a computer to interpolate hydrologic data based on a network of measured values in west-central Kansas. The computer program generated estimated values at the center of each 1-mile section in the Western Kansas Groundwater Management District No. 1 and facilitated contouring of selected hydrologic data that are needed in the effective management of ground water for irrigation. The kriging technique produced various maps that illustrated hydrologic conditions in the Ogallala aquifer, the principal source of water in west-central Kansas. Maps of the aquifer, which use a 3-year average, included the 1979-81 water-table altitudes, which ranged from about 2,580 to 3,720 feet; the 1979-81 saturated thicknesses, which ranged from about 0 to 250 feet; and the percentage changes in saturated thickness from 1950 to 1979-81, which ranged from about a 40-percent increase to a 100-percent decrease. A map showing errors of estimate also was provided as a measure of reliability for the 1979-81 water-table altitudes. Errors of estimate ranged from 2 to 24 feet. (USGS)","language":"ENGLISH","doi":"10.3133/ofr82258","usgsCitation":"Spinazola, J.M., 1982, Hydrologic maps of Ogallala Aquifer, west-central Kansas, 1979-81: U.S. Geological Survey Open-File Report 82-258, 4 maps on 4 sheets :photocopy ;62 x 126 cm., https://doi.org/10.3133/ofr82258.","productDescription":"4 maps on 4 sheets :photocopy ;62 x 126 cm.","costCenters":[],"links":[{"id":162526,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20547,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0258/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20548,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0258/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20549,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0258/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20550,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0258/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db6067a2","contributors":{"authors":[{"text":"Spinazola, Joseph M.","contributorId":102044,"corporation":false,"usgs":true,"family":"Spinazola","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":228566,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28725,"text":"wri8184 - 1982 - Water-quality and hydrogeologic data for three phosphate industry waste-disposal sites in central Florida, 1979-80","interactions":[],"lastModifiedDate":"2019-12-05T08:35:31","indexId":"wri8184","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-84","title":"Water-quality and hydrogeologic data for three phosphate industry waste-disposal sites in central Florida, 1979-80","docAbstract":"This report is a complilation of geologic, hydrologic, and water-quality data and information on test holes collected in the vicinity of gypsum stack complexes at two phosphate chemical plants and one phosphatic clayey waste disposal pond at a phosphate mine and beneficiation plant in central Florida. The data were collected from September 1979 to October 1980 at thee AMAX Phosphate, Inc., chemical plant, Piney Point; the USS AgriChemicals chemical plant, Bartow; and the International Minerals and Chemical Corporation Clear Springs mine, Bartow. Approximmmtely 5,400 field and laboratory water-quality determinations on water samples were collected from about 78 test holes and 31 surface-water, rainfall, and other sampling sites at phosphate industry beneficiation and chemical plant waste-disposal operations. Maps show locations of sampling sites. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8184","usgsCitation":"Miller, R.L., and Sutcliffe, H., 1982, Water-quality and hydrogeologic data for three phosphate industry waste-disposal sites in central Florida, 1979-80: U.S. Geological Survey Water-Resources Investigations Report 81-84, vii, 77 p. , https://doi.org/10.3133/wri8184.","productDescription":"vii, 77 p. 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,{"id":10554,"text":"ofr82692 - 1982 - Data for wells at the low-level radioactive-waste burial site in the Palos Forest Preserve, Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr82692","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-692","title":"Data for wells at the low-level radioactive-waste burial site in the Palos Forest Preserve, Illinois","docAbstract":"The U.S. Geological Survey is studying the geologic, hydrologic, and geochemical properties of the glacial drift and underlying bedrock at a low-level radioactive-waste burial site in the Palos Forest Preserve, 22 kilometers southwest of Chicago. Data collected from the 33 test wells drilled into the drift plus data from 4 wells drilled into the underlying dolomite bedrock are presented. Data include maps showing the location of the test wells, a general description of the drift, well-construction information, and lithologic descriptions of cores from the wells finished in the drift.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82692","usgsCitation":"Olimpio, J., 1982, Data for wells at the low-level radioactive-waste burial site in the Palos Forest Preserve, Illinois: U.S. Geological Survey Open-File Report 82-692, iii, 101 p., ill., map ;28 cm., https://doi.org/10.3133/ofr82692.","productDescription":"iii, 101 p., ill., map ;28 cm.","costCenters":[],"links":[{"id":142500,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0692/report-thumb.jpg"},{"id":38392,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0692/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c902","contributors":{"authors":[{"text":"Olimpio, J.C.","contributorId":36137,"corporation":false,"usgs":true,"family":"Olimpio","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":161584,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10536,"text":"ofr802046 - 1982 - Ground-water levels and water quality in an area near Topaz Lake, Douglas County, Nevada","interactions":[],"lastModifiedDate":"2022-04-18T16:03:53.25151","indexId":"ofr802046","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"80-2046","title":"Ground-water levels and water quality in an area near Topaz Lake, Douglas County, Nevada","docAbstract":"<p>Intensive residential development of land along the northwest shore of Topaz Lake has raised concern regarding the adequacy of the water supply and possible effects of septic-tank effluents on the quality of local ground water and the lake. Existing data on water levels, well construction, and water quality were compiled, and a limited program of water-level measurement and water-quality sampling was conducted during 1976-77 to provide documentation of current hydrologic conditions against which effects of future development may be measured.<br></p><p>Water-level measurements show the presence of small independent aquifers near the periphery of the alluvial fan covering the study area and a main alluvial aquifer in which water levels fluctuate in direct response to annual changes in lake stage.</p><p>The sampled ground water can be grouped into four chemical types--three based on the relative proportions of sulfate and bicarbonate and one based on an increased proportion of chloride plus nitrate.</p><p>Frequency distributions of the observed occurrences of nitrate (as NO3), phosphate (as PO4), and chloride in ground water indicate thresholds for background concentrations of these constituents at 0 to 3, 0 to 0.35, and 0 to 6 milligrams per liter, respectively. Above-background concentrations of nitrate and phosphate in ground water may be attributable, in part, to natural sources of these constituents; however, septic-tank effluents have increased the concentrations of nitrate, chloride, and perhaps phosphate in at least two areas of the current development. Sampling for dissolved organic carbon and coliform bacteria in ground water detected no contamination by these potential indicators of pollution.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr802046","collaboration":"Prepared in cooperation with the Nevada Division of Environmental Protection","usgsCitation":"Nowlin, J.O., 1982, Ground-water levels and water quality in an area near Topaz Lake, Douglas County, Nevada: U.S. Geological Survey Open-File Report 80-2046, vii, 76 p., https://doi.org/10.3133/ofr802046.","productDescription":"vii, 76 p.","costCenters":[],"links":[{"id":398930,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/2046/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142983,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/2046/report-thumb.jpg"}],"country":"United States","state":"Nevada","county":"Douglas County","otherGeospatial":"Topaz Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.55596923828124,\n              38.67371706140244\n            ],\n            [\n              -119.49279785156249,\n              38.67371706140244\n            ],\n            [\n              -119.49279785156249,\n              38.717126039425644\n            ],\n            [\n              -119.55596923828124,\n              38.717126039425644\n            ],\n            [\n              -119.55596923828124,\n              38.67371706140244\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db66889b","contributors":{"authors":[{"text":"Nowlin, Jon O.","contributorId":34937,"corporation":false,"usgs":true,"family":"Nowlin","given":"Jon","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":161561,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9909,"text":"ofr82868 - 1982 - Geohydrologic data from sandstone aquifers in southwestern Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:06:19","indexId":"ofr82868","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-868","title":"Geohydrologic data from sandstone aquifers in southwestern Kansas","docAbstract":"Data collected during a reconnaissance investigation of the geology and hydrology of sandstone aquifers provide useful information in the study of, and planning for, water-resources development in a 17,400 square-mile area in 26 counties of southwestern Kansas. The aquifers consist chiefly of saturated sandstones that occur in Upper Permian, Upper Jurassic, and Lower and Upper Cretaceous rocks. In parts of southwestern Kansas, the sandstone aquifers already serve as the principal or secondary source of ground water for irrigation and other uses. Data indicate that water may be available for development in sandstone aquifers in other parts of the study area. In still other areas, water from wells in sandstone aquifers may not be of a suitable quality for some purposes. The data provided include records of selected wells, lithologic logs of test holes and wells, selected formation surfaces and sandstone thicknesses , chemical analyses of water from selected wells, and water levels in observation wells. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82868","usgsCitation":"Kume, J., and Spinazola, J.M., 1982, Geohydrologic data from sandstone aquifers in southwestern Kansas: U.S. Geological Survey Open-File Report 82-868, iii, 116 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82868.","productDescription":"iii, 116 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":142698,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0868/report-thumb.jpg"},{"id":37701,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0868/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688814","contributors":{"authors":[{"text":"Kume, Jack","contributorId":100843,"corporation":false,"usgs":true,"family":"Kume","given":"Jack","email":"","affiliations":[],"preferred":false,"id":160494,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spinazola, Joseph M.","contributorId":102044,"corporation":false,"usgs":true,"family":"Spinazola","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":160495,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":43567,"text":"ofr81536 - 1982 - Hydrology of Lake Tohopekaliga, Osceola County, Florida","interactions":[],"lastModifiedDate":"2022-04-18T16:23:05.159371","indexId":"ofr81536","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-536","title":"Hydrology of Lake Tohopekaliga, Osceola County, Florida","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81536","collaboration":"Prepared in cooperation with the South Florida Water Management District","usgsCitation":"Phelps, G.G., 1982, Hydrology of Lake Tohopekaliga, Osceola County, Florida: U.S. Geological Survey Open-File Report 81-536, 2 Plates: 38.54 x 28.43 inches and 38.46 x 27.83 inches, https://doi.org/10.3133/ofr81536.","productDescription":"2 Plates: 38.54 x 28.43 inches and 38.46 x 27.83 inches","costCenters":[],"links":[{"id":398942,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0536/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":398941,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0536/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":167847,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0536/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Osceola County","otherGeospatial":"Lake Tohopekaliga","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.43890380859375,\n              28.132549863716783\n            ],\n            [\n              -81.31118774414062,\n              28.132549863716783\n            ],\n            [\n              -81.31118774414062,\n              28.311635046750613\n            ],\n            [\n              -81.43890380859375,\n              28.311635046750613\n            ],\n            [\n              -81.43890380859375,\n              28.132549863716783\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604893","contributors":{"authors":[{"text":"Phelps, G. G.","contributorId":82346,"corporation":false,"usgs":true,"family":"Phelps","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":228397,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8719,"text":"ofr81803 - 1982 - Hydrology of area 9, Eastern Coal Province, West Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:11","indexId":"ofr81803","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-803","title":"Hydrology of area 9, Eastern Coal Province, West Virginia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81803","usgsCitation":"Ehlke, T.A., Runner, G.S., and Downs, S.C., 1982, Hydrology of area 9, Eastern Coal Province, West Virginia: U.S. Geological Survey Open-File Report 81-803, v, 63 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/ofr81803.","productDescription":"v, 63 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":94874,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0803/report.pdf","size":"23135","linkFileType":{"id":1,"text":"pdf"}},{"id":142015,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0803/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601fe5","contributors":{"authors":[{"text":"Ehlke, Theodore A.","contributorId":83523,"corporation":false,"usgs":true,"family":"Ehlke","given":"Theodore","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":158207,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Runner, Gerald S.","contributorId":90297,"corporation":false,"usgs":true,"family":"Runner","given":"Gerald","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":158208,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Downs, Sanford C.","contributorId":66233,"corporation":false,"usgs":true,"family":"Downs","given":"Sanford","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":158206,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30344,"text":"wri8234 - 1982 - Water-quality characteristics of Everglades National Park, 1959-77, with reference to the effects of water management","interactions":[],"lastModifiedDate":"2019-08-05T12:06:39","indexId":"wri8234","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-34","title":"Water-quality characteristics of Everglades National Park, 1959-77, with reference to the effects of water management","docAbstract":"The U.S. Geological Survey has collected water-quality data in the Everglades National Park since 1959. Major ions, macronutrients, trace elements, and pesticides are the primary chemical groups analyzed. The period of record and frequency of sampling vary for each chemical group, with the longest record for the major ions and the shortest for the macronutrients. Within the park there are three major drainageways: Big Cypress Swamp, Shark River Slough, and Taylor Slough. Each drainageway exhibits unique hydrologic conditions, yet there is a high degree of homogeneity in water-quality characteristics among these areas. Seasonal changes in major-ion, trace-element, and macronutrient concentrations are marked in the shallow marsh. Concentrations generally increase in the dry season due to evapotranspiration, changes in chemical equilibria, and precipitation. Water-management practices in south Florida have changed the water quality in the Shark River Slough. Most major-ion, dissolved-solid, and iron concentrations and color levels have steadily increased since 1963. The water quality in the other two drainageways has not changed since sampling began. Chlorinated-hydrocarbon insecticide residues in bottom material were found in low concentration at every sampling station in the park. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8234","usgsCitation":"Waller, B.G., 1982, Water-quality characteristics of Everglades National Park, 1959-77, with reference to the effects of water management: U.S. Geological Survey Water-Resources Investigations Report 82-34, vi, 51 p. , https://doi.org/10.3133/wri8234.","productDescription":"vi, 51 p. ","costCenters":[],"links":[{"id":366265,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0034/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159310,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0034/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Everglades National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.15600585937499,\n              25.13533901613099\n            ],\n            [\n              -80.48583984375,\n              25.13533901613099\n            ],\n            [\n              -80.48583984375,\n              25.517657429994035\n            ],\n            [\n              -81.15600585937499,\n              25.517657429994035\n            ],\n            [\n              -81.15600585937499,\n              25.13533901613099\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d9f0","contributors":{"authors":[{"text":"Waller, Bradley G.","contributorId":83492,"corporation":false,"usgs":true,"family":"Waller","given":"Bradley","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":203093,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8727,"text":"ofr82426 - 1982 - Annual snowmelt and rainfall peak-flow data on selected foothills region streams, South Platte River, Arkansas River, and Colorado River basins, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:11","indexId":"ofr82426","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-426","title":"Annual snowmelt and rainfall peak-flow data on selected foothills region streams, South Platte River, Arkansas River, and Colorado River basins, Colorado","docAbstract":"Peak flows in the foothills region of Colorado are attributable to two meteorological sources--snowmelt and rainfall. As part of a study of the hydrology of foothills streams in Colorado, charts from streamflow gages on unregulated streams were examined to determined the source of peak-flow events. Snowmelt-runoff peaks were distinguished from rainfall-runoff peaks on the basis of daily and seasonal occurrence, hydrograph shape, and local weather conditions. Peak-flow data for snowmelt runoff and rainfall runoff are presented for 69 streamflow-gaging stations in the South Platte River, the Arkansas River, and the Colorado River basins. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82426","usgsCitation":"Elliott, J.G., Jarrett, R., and Ebling, J., 1982, Annual snowmelt and rainfall peak-flow data on selected foothills region streams, South Platte River, Arkansas River, and Colorado River basins, Colorado: U.S. Geological Survey Open-File Report 82-426, iv, 90 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82426.","productDescription":"iv, 90 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":141062,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0426/report-thumb.jpg"},{"id":36298,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0426/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b8df","contributors":{"authors":[{"text":"Elliott, J. G.","contributorId":45341,"corporation":false,"usgs":true,"family":"Elliott","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":158218,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jarrett, R.D.","contributorId":36551,"corporation":false,"usgs":true,"family":"Jarrett","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":158217,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ebling, J.L.","contributorId":81978,"corporation":false,"usgs":true,"family":"Ebling","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":158219,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30351,"text":"wri8182 - 1982 - Streamflow characteristics of the upper Columbia River basin, Montana, through 1979","interactions":[],"lastModifiedDate":"2020-12-28T18:00:28.071514","indexId":"wri8182","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-82","title":"Streamflow characteristics of the upper Columbia River basin, Montana, through 1979","docAbstract":"Statistical summaries of streamflow data for selected stream-gaging sites presented in this report aid in appraising the hydrology of the upper Columbia River basin in Montana. Streamflow records are provided for 54 gaging stations for the period of record. Streamflow records for five gaging stations were compiled into separate periods related to changes in regulation after data collection commenced. The entire period of record, the period before regulation, and the period after regulation are presented for comparison. For each gaging station selected for this report, a brief description is given for station location, drainage area, period of record, revisions of previously published records, type and history of gages, regulation and diversions, and extremes of discharge. These data are followed by tables of monthly and annual flow statistics, flood-frequency data, low-flow and high-flow frequency data, and flow-duration information. 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,{"id":8747,"text":"ofr82910 - 1982 - Selected ground-water data, Sevier Desert, Utah, 1935-82","interactions":[],"lastModifiedDate":"2020-06-16T21:17:15.316532","indexId":"ofr82910","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-910","title":"Selected ground-water data, Sevier Desert, Utah, 1935-82","docAbstract":"<p>No abstract available.<br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82910","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources, Division of Water Rights","usgsCitation":"Enright, M., and Holmes, W.F., 1982, Selected ground-water data, Sevier Desert, Utah, 1935-82: 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,{"id":27999,"text":"wri824074 - 1982 - Physical and hydrologic environments of the Mulberry coal reserves in eastern Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:08:40","indexId":"wri824074","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4074","title":"Physical and hydrologic environments of the Mulberry coal reserves in eastern Kansas","docAbstract":"Strippable reserves of Mulberry coal underlie an area of approximately 300 square miles of Miami, Linn, and Bourbon Counties of eastern Kansas. Although subject to State reclamation law, current and projected strip mining of this relatively thin coal seam could alter and hydrologic environment of the study area. Drained by the Marais des Cygnes and Little Osage Rivers and their tributaries, this area is characterized by low relief and moderately impermeable soils. Streamflows are poorly sustained by ground-water discharge and fluctuate widely due to climatic extremes and usage of surface-water supplies. Because ground-water supplies are generally unreliable in quantity and quality, surface water is used to meet most water requirements in the study area. Primary used of surface waters are for domestic supplies, maintenance of wildlife and recreational areas, and cooling needs at LaCygne Power Plant. The prevailing chemical type of the natural streamflow is calcium bicarbonate, with concentrations of dissolved solids generally less than 500 milligrams per liter and pH near neutral. Additional streamflow and water-quality data are needed to evaluate the premining characteristics of and the anticipated changes in the hydrologic environment as strip mining proceeds within the study area. A network of data-collection stations and a sampling scheme have been established to acquire this additional information. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, WRD,","doi":"10.3133/wri824074","usgsCitation":"Kenny, J.F., Bevans, H., and Diaz, A., 1982, Physical and hydrologic environments of the Mulberry coal reserves in eastern Kansas: U.S. Geological Survey Water-Resources Investigations Report 82-4074, 50 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824074.","productDescription":"50 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122828,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4074/report-thumb.jpg"},{"id":56826,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4074/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685c0f","contributors":{"authors":[{"text":"Kenny, J. F.","contributorId":100378,"corporation":false,"usgs":true,"family":"Kenny","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":199042,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bevans, H.E.","contributorId":102892,"corporation":false,"usgs":true,"family":"Bevans","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":199043,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Diaz, A.M.","contributorId":27084,"corporation":false,"usgs":true,"family":"Diaz","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":199041,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":42569,"text":"ofr82760 - 1982 - Saturated thickness of the High Plains regional aquifer in 1980, northwestern Oklahoma","interactions":[],"lastModifiedDate":"2017-09-29T08:09:44","indexId":"ofr82760","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-760","title":"Saturated thickness of the High Plains regional aquifer in 1980, northwestern Oklahoma","docAbstract":"During 1978, the U.S. Geological Survey began a 5-year study of the High Plains regional aquifer system to provide hydrologic information for evaluation of the effects of long-term development of the aquifer and to develop computer models for prediction of aquifer response to alternative changes in ground-water management (Weeks, 1978). This report is one of a series presenting hydrologic information of the High Plains aquifer in Oklahoma.\r\nThe 1980 saturated thickness of the High Plains regional aquifer in Oklahoma is shown for the eastern area (plate 1), consisting of Harper, Ellis, Woodward, Dewey, and Roger Mills Counties, and for the Panhandle area (plate 2), consisting of Cimarron, Texas, and Beaver Counties.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82760","usgsCitation":"Havens, J., 1982, Saturated thickness of the High Plains regional aquifer in 1980, northwestern Oklahoma: U.S. Geological Survey Open-File Report 82-760, 2 Plates: 24.15 x 35.67 inches and 46.57 x 17.35 inches, https://doi.org/10.3133/ofr82760.","productDescription":"2 Plates: 24.15 x 35.67 inches and 46.57 x 17.35 inches","costCenters":[],"links":[{"id":346202,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0760/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":346203,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0760/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":168758,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0760/report-thumb.jpg"}],"country":"United States","state":"Oklahoma","otherGeospatial":"High Plains Regional Aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -103.0023193359375,\n              36.99816565700228\n            ],\n            [\n              -103.0078125,\n              36.49638952000399\n            ],\n            [\n              -100.008544921875,\n              36.50963615733049\n            ],\n            [\n              -99.99755859375,\n              35.38457160381764\n            ],\n            [\n              -99.151611328125,\n              35.38457160381764\n            ],\n            [\n              -99.151611328125,\n              37.00255267215955\n            ],\n            [\n              -103.0023193359375,\n              36.99816565700228\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdbcc","contributors":{"authors":[{"text":"Havens, John S.","contributorId":13949,"corporation":false,"usgs":true,"family":"Havens","given":"John S.","affiliations":[],"preferred":false,"id":226729,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23607,"text":"ofr81330 - 1982 - Ground-water quality and data on wells and springs in Pennsylvania; Volume III, Delaware River basin","interactions":[],"lastModifiedDate":"2017-06-22T11:08:23","indexId":"ofr81330","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-330","title":"Ground-water quality and data on wells and springs in Pennsylvania; Volume III, Delaware River basin","docAbstract":"Volume III presents ground-water quality and physical data on about 1,250 wells and springs in the Delaware River Basin in Pennsylvania. Locations are shown on site-location maps derived from the hydrologic unit map. Codes showing the geologic age and aquifer are provided.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Harrisburg,, PA","doi":"10.3133/ofr81330","issn":"0094-9140","collaboration":"Prepared in cooperation with the  Pennsylvania Department of Environmental Resources","usgsCitation":"Koester, H., and Miller, D., 1982, Ground-water quality and data on wells and springs in Pennsylvania; Volume III, Delaware River basin: U.S. Geological Survey Open-File Report 81-330, iii, 111 p., https://doi.org/10.3133/ofr81330.","productDescription":"iii, 111 p.","numberOfPages":"116","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":154891,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0330/report-thumb.jpg"},{"id":277909,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0330/report.pdf"}],"country":"United States","state":"Pennsylvania","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.8054,39.7241 ], [ -76.8054,41.9983 ], [ -74.707,41.9983 ], [ -74.707,39.7241 ], [ -76.8054,39.7241 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6673f1","contributors":{"authors":[{"text":"Koester, H.E.","contributorId":26323,"corporation":false,"usgs":true,"family":"Koester","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":190398,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, D.R.","contributorId":106147,"corporation":false,"usgs":true,"family":"Miller","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":190399,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23559,"text":"ofr82913 - 1982 - A summary of selected publications, project activities, and data sources related to hydrology in the Warrior and Plateau coal fields of Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:08:09","indexId":"ofr82913","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-913","title":"A summary of selected publications, project activities, and data sources related to hydrology in the Warrior and Plateau coal fields of Alabama","docAbstract":"The report is a reference source on hydrologic information related to coal-mining activities in the Warrior and Plateau coal fields of Alabama. It contains a bibliography of more than 200 references and selected annotations. Also included is information on maps, automated-data bases, water-monitoring programs, and data-source agencies and organizations.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr82913","issn":"0094-9140","usgsCitation":"Kidd, R.E., and Hill, T.J., 1982, A summary of selected publications, project activities, and data sources related to hydrology in the Warrior and Plateau coal fields of Alabama: U.S. Geological Survey Open-File Report 82-913, iv, 63 p. 1 map ;28 cm., https://doi.org/10.3133/ofr82913.","productDescription":"iv, 63 p. 1 map ;28 cm.","costCenters":[],"links":[{"id":156551,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0913/report-thumb.jpg"},{"id":52852,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0913/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a5fad","contributors":{"authors":[{"text":"Kidd, Robert E.","contributorId":21523,"corporation":false,"usgs":true,"family":"Kidd","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":190317,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hill, Thomas J.","contributorId":13270,"corporation":false,"usgs":true,"family":"Hill","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":190316,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":36476,"text":"fwsobs82_59 - 1982 - Proceedings of the conference on coastal erosion and wetland modification in Louisiana: causes, consequences, and options","interactions":[],"lastModifiedDate":"2018-01-30T12:45:31","indexId":"fwsobs82_59","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/59","title":"Proceedings of the conference on coastal erosion and wetland modification in Louisiana: causes, consequences, and options","docAbstract":"<p>This volume contains 16 papers and panel discussions from a conference held in Baton Rouge, La., 5-6 October 1981. The presentations consider the causes and consequences of coastal erosion and wetland modification in Louisiana and the mitigative options available to slow or reverse the rapid rate of coastal land loss. Detailed habitat mapping studies have allowed accurate estimates of coastal habitat change and land loss through 1978. Projections from these rates of change indicate an annual rate of land loss in coastal Louisiana in the early 1980's of approximately 130 km<sup>2</sup>/yr (50 m<sup>2</sup>/yr).</p><p>The projected effects of wetland modification on the bountiful living resources of coastal Louisiana (fisheries, fur and hide bearers and waterfowl) are major because of the close dependence of these resources on estuarine wetlands. These changes and others related to flood protection, transportation and ownership of mineral resources are projected to have extensive social and economic consequences.</p><p>Options proposed to slow coastal land loss include major and minor diversion of the Mississippi River, barrier island and shoreline restoration protection, hydrological management of wetlands and more restrictive permitting of dredging activities.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service, Biological Services Program","publisherLocation":"Washington, D.C.","usgsCitation":"1982, Proceedings of the conference on coastal erosion and wetland modification in Louisiana: causes, consequences, and options: FWS/OBS 82/59, viii, 256 p.","productDescription":"viii, 256 p.","numberOfPages":"265","costCenters":[],"links":[{"id":289595,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":289594,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fwsobs/1982/0059/report.pdf"}],"country":"United States","state":"Louisiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94.0434,28.9254 ], [ -94.0434,33.0195 ], [ -88.8162,33.0195 ], [ -88.8162,28.9254 ], [ -94.0434,28.9254 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db660489","contributors":{"editors":[{"text":"Boesch, Donald F.","contributorId":23599,"corporation":false,"usgs":true,"family":"Boesch","given":"Donald","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":504035,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":42457,"text":"ofr82515 - 1982 - Preliminary map showing availability of ground water from glacial-drift aquifers in Logan County, south-central North Dakota","interactions":[],"lastModifiedDate":"2018-03-08T13:44:53","indexId":"ofr82515","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-515","title":"Preliminary map showing availability of ground water from glacial-drift aquifers in Logan County, south-central North Dakota","docAbstract":"<p>This preliminary map is the first product of the ground-water resources study of Logan County, which has an area of 1,015 mi<span id=\"_mce_caret\" data-mce-bogus=\"true\"><sup>﻿2</sup><span id=\"_mce_caret\" data-mce-bogus=\"true\">﻿ (2,629 km<span id=\"_mce_caret\" data-mce-bogus=\"true\"><sup>﻿2</sup><span id=\"_mce_caret\" data-mce-bogus=\"true\">﻿) in south-central North Dakota (see location map).&nbsp; This study is part of a statewide program to determine the location, extent, chemical quality, and hydrologic characteristics of the ground-water reservoirs (aquifers) in North Dakota.&nbsp; The study was made by the U.S. Geological Survey in cooperation with the North Dakota State Water Commission, North Dakota Geological Survey, and Logan County Water Management District.</span></span></span></span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82515","usgsCitation":"Klausing, R.L., 1982, Preliminary map showing availability of ground water from glacial-drift aquifers in Logan County, south-central North Dakota: U.S. Geological Survey Open-File Report 82-515, 33.15 x 19.52 inches, https://doi.org/10.3133/ofr82515.","productDescription":"33.15 x 19.52 inches","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":136615,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80220,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0515/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d721","contributors":{"authors":[{"text":"Klausing, Robert L.","contributorId":55797,"corporation":false,"usgs":true,"family":"Klausing","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":226527,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}