{"pageNumber":"1698","pageRowStart":"42425","pageSize":"25","recordCount":68937,"records":[{"id":28339,"text":"wri934002 - 1993 - Hydrology and water quality of unmined and reclaimed basins in phosphate-mining areas, west-central Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:38","indexId":"wri934002","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"93-4002","title":"Hydrology and water quality of unmined and reclaimed basins in phosphate-mining areas, west-central Florida","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri934002","usgsCitation":"Lewelling, B., and Wylie, R., 1993, Hydrology and water quality of unmined and reclaimed basins in phosphate-mining areas, west-central Florida: U.S. Geological Survey Water-Resources Investigations Report 93-4002, viii, 93 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri934002.","productDescription":"viii, 93 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":120164,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4002/report-thumb.jpg"},{"id":57149,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4002/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604bcc","contributors":{"authors":[{"text":"Lewelling, B. R.","contributorId":17969,"corporation":false,"usgs":true,"family":"Lewelling","given":"B. R.","affiliations":[],"preferred":false,"id":199620,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wylie, R.W.","contributorId":53426,"corporation":false,"usgs":true,"family":"Wylie","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":199621,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26809,"text":"wri924119 - 1993 - Hydrogeology, water quality, and ground-water-development alternatives in the upper Wood River ground-water reservoir, Rhode Island","interactions":[],"lastModifiedDate":"2012-02-02T00:08:33","indexId":"wri924119","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"92-4119","title":"Hydrogeology, water quality, and ground-water-development alternatives in the upper Wood River ground-water reservoir, Rhode Island","docAbstract":"The 72.4-square-mile Upper Wood River study area is in the Pawcatuck River basin in southern Rhode Island. Stratified drift is the only principal geologic unit capable of producing yields greater than 0.5 Mgal/d. Transmissivity of the aquifer ranges from 7,600 to 49,200 sq ft/d. Water-table conditions prevail and the aquifer is in good hydraulic connection with perennial streams and ponds. Groundwater and surface water in the study area are generally suitable for most uses. Water is soft, slightly acidic, and contains less than 150 mg/L dissolved solids. Locally, however, groundwater has been contaminated with nitrate, chloride, and volatile organic compounds. A model of the groundwater-flow system was used to evaluate the effect of alternative schemes of groundwater development on water levels, pond levels, and streamflow. Till contacts were simulated as specified-flux boundaries, drainage divides as no-flow boundaries, and streams as leaky boundaries. The areas most favorable for development of 1 Mgal/d are along the Flat and Wood Rivers. From 50 to 65 percent of the water withdrawn from wells would be derived from induced recharge. Results of simulation of development alternatives indicate that the groundwater reservoir could sustain withdrawals of 6 to 12 Mgal/d from 11 wells under long-term average annual (1942-89) and simulated drought (1963-66) conditions without causing water-level declines of greater than 25 percent of the unstressed saturated thickness of the aquifer. Pumping 12 Mgal/d, however, would reduce flow of the Wood River at the basin outlet by an amount almost equal to the 7-day, 10-yr low flow of 20.4 cu ft/s.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri924119","usgsCitation":"Dickerman, D., and Bell, R., 1993, Hydrogeology, water quality, and ground-water-development alternatives in the upper Wood River ground-water reservoir, Rhode Island: U.S. Geological Survey Water-Resources Investigations Report 92-4119, vii, 87 p. :ill., maps ;28 cm. [PGS - 86 p.], https://doi.org/10.3133/wri924119.","productDescription":"vii, 87 p. :ill., maps ;28 cm. [PGS - 86 p.]","costCenters":[],"links":[{"id":123604,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4119/report-thumb.jpg"},{"id":55697,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4119/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db69612a","contributors":{"authors":[{"text":"Dickerman, D.C.","contributorId":48601,"corporation":false,"usgs":true,"family":"Dickerman","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":197043,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bell, R.W.","contributorId":77563,"corporation":false,"usgs":true,"family":"Bell","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":197044,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28362,"text":"wri914136 - 1993 - Hydrology and water quality of the Forest County Potawatomi Indian Reservation, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-26T13:58:58","indexId":"wri914136","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"91-4136","title":"Hydrology and water quality of the Forest County Potawatomi Indian Reservation, Wisconsin","docAbstract":"

This report presents data from a study by the U.S. Geological Survey, in cooperation with the Forest County Potawatomi Community of Wisconsin, to document the hydrology and water quality of the Potawatomi Indian Reservation in southern Forest County. Data were collected from October 1981 through September 1987.  

\n

Glacial sand and gravel forms the primary aquifer on the reservation. This aquifer is unconfined, and its saturated thickness ranges from approximately 200 feet to zero feet in areas where the bedrock crops out. Horizontal hydraulic conductivity of the glacial deposits is estimated to range from 0.4 to 48 feet per day.

\n

Three watersheds encompass the Reservation: The Wolf, the North Branch Oconto, and the Peshtigo. Estimates of base-flow discharge that will occur on the average once every 2 years for a 7- day period for Reservation streams range from 7.5 ft3/s (cubic feet per second) for North Branch Oconto at Wabeno to 32 ft3/s for the Rat River near Wabeno.

\n

Ground water in the study area is a calcium magnesium bicarbonate type and is suitable for most uses. The ground water sampled during the study was slightly alkaline and moderately hard to very hard; median hardness was 135 mg/L (milligrams per liter) as calcium carbonate. Alkalinity of ground water ranged from 79 to 318 mg/L; median alkalinity was 123 mg/L as calcium carbonate.

\n

With the exception of nitrate in water from one well sampled, constituent concentrations were less than the U.S. Environmental Protection Agency's Maximum Contaminant Levels (MCL's) for drinking water. Nitrate plus nitrite concentration was 15 mg/L as N, or 50 percent greater than the MCL, in one well located one-half mile northeast of Lake Lucerne.

\n

Secondary Maximum Contaminant Levels (SMCL's) for iron were exceeded in water from two wells. In one of these two well waters, the manganese concentration equaled the SMCL.

\n

Streams on the Reservation also contain a calcium magnesium bicarbonate type water. The stream waters are slightly alkaline and are considered soft to moderately hard; median hardness in stream samples was 56 mg/L as calcium carbonate. The alkalinity in stream samples ranged from 46 to 59 mg/L as calcium carbonate; the median value was 51 mg/L. Stream water is intermediate between hard, alkaline ground water and soft, acidic precipitation and surface runoff. Low but detectable concentrations of chromium, copper, iron, magnesium, mercury, and zinc were detected in most bottom-material samples.

\n

Water quality of three lakes on the Reservation is variable and depends on the degree of connection with the ground-water system. In general, Bug Lake and Devils Lake are in poor hydraulic connection with the ground-water system, and their waters contain low concentrations of dissolved solids and alkalinity and low pH. King Lake is in good hydraulic connection with the ground-water system, and its waters contain higher concentrations of dissolved solids and alkalinity and higher pH than Bug and Devils Lakes.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri914136","collaboration":"Prepared in cooperation with the Forest County Potawatomi Community of Wisconsin","usgsCitation":"Lidwin, R., and Krohelski, J.T., 1993, Hydrology and water quality of the Forest County Potawatomi Indian Reservation, Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 91-4136, Report: v, 24 p.; 4 Plates: 25.06 x 21.81 inches or smaller, https://doi.org/10.3133/wri914136.","productDescription":"Report: v, 24 p.; 4 Plates: 25.06 x 21.81 inches or smaller","numberOfPages":"29","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":57167,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4136/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57168,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4136/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57169,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4136/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57165,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4136/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57166,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4136/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120153,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4136/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","county":"Forest County","otherGeospatial":"Potowatomi Indian Reservation","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-88.6833,46.0144],[-88.6844,45.9823],[-88.6746,45.9823],[-88.6757,45.8958],[-88.6761,45.8093],[-88.6758,45.7247],[-88.5519,45.723],[-88.4665,45.7224],[-88.4254,45.7225],[-88.4255,45.6356],[-88.4262,45.5492],[-88.4263,45.5071],[-88.4258,45.4925],[-88.4261,45.4774],[-88.4257,45.4633],[-88.4259,45.4505],[-88.4261,45.4358],[-88.4263,45.4212],[-88.4272,45.4066],[-88.4283,45.3769],[-88.5542,45.3778],[-88.6418,45.3784],[-88.6587,45.3785],[-88.6781,45.3787],[-88.7196,45.3784],[-88.754,45.3782],[-88.802,45.3775],[-88.9259,45.3799],[-88.9265,45.3909],[-88.9251,45.4014],[-88.9233,45.4659],[-89.0467,45.4668],[-89.0468,45.5518],[-89.0475,45.6391],[-89.0469,45.7265],[-89.047,45.8097],[-89.0477,45.8953],[-89.0478,45.9822],[-88.9332,45.9822],[-88.9329,46.0746],[-88.8507,46.0409],[-88.8473,46.0368],[-88.8431,46.0336],[-88.8426,46.0333],[-88.8371,46.0312],[-88.8325,46.0294],[-88.828,46.0294],[-88.8248,46.0294],[-88.8207,46.0289],[-88.819,46.0284],[-88.8169,46.0278],[-88.8143,46.026],[-88.8123,46.0247],[-88.8103,46.0238],[-88.8083,46.0238],[-88.8077,46.0238],[-88.8051,46.0238],[-88.8031,46.0252],[-88.803,46.0275],[-88.8024,46.0302],[-88.8017,46.032],[-88.7991,46.0338],[-88.7974,46.0344],[-88.7968,46.0346],[-88.7948,46.0341],[-88.7928,46.0332],[-88.7914,46.0318],[-88.7895,46.0324],[-88.7873,46.0334],[-88.786,46.0336],[-88.7843,46.0329],[-88.7828,46.0311],[-88.7828,46.0292],[-88.7841,46.0274],[-88.7847,46.026],[-88.7866,46.0232],[-88.7865,46.0209],[-88.7856,46.0196],[-88.7848,46.0186],[-88.7824,46.0178],[-88.7798,46.0178],[-88.7777,46.0179],[-88.7758,46.0181],[-88.7753,46.0197],[-88.7747,46.0203],[-88.7734,46.0216],[-88.7715,46.024],[-88.7691,46.0239],[-88.7669,46.0226],[-88.7662,46.0208],[-88.7637,46.02],[-88.7632,46.02],[-88.7615,46.02],[-88.7565,46.0212],[-88.754,46.0226],[-88.7507,46.0248],[-88.7458,46.0267],[-88.7408,46.028],[-88.7363,46.028],[-88.7334,46.0277],[-88.7317,46.0273],[-88.7284,46.0256],[-88.7251,46.0239],[-88.7232,46.0219],[-88.7221,46.0209],[-88.7216,46.0202],[-88.7241,46.0183],[-88.7254,46.0165],[-88.7253,46.0146],[-88.724,46.0133],[-88.7214,46.0133],[-88.7168,46.0139],[-88.7144,46.015],[-88.7129,46.0157],[-88.7084,46.0167],[-88.7023,46.0177],[-88.6977,46.0177],[-88.6953,46.0173],[-88.6913,46.0166],[-88.6846,46.0149],[-88.6833,46.0144]]]},\"properties\":{\"name\":\"Forest\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604cb6","contributors":{"authors":[{"text":"Lidwin, R.A.","contributorId":33349,"corporation":false,"usgs":true,"family":"Lidwin","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":199667,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krohelski, J. T.","contributorId":59046,"corporation":false,"usgs":true,"family":"Krohelski","given":"J.","email":"","middleInitial":"T.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":199668,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28405,"text":"wri924030 - 1993 - Analysis of residential use of water in the Denver metropolitan area, Colorado, 1980-87","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri924030","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"92-4030","title":"Analysis of residential use of water in the Denver metropolitan area, Colorado, 1980-87","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri924030","usgsCitation":"Litke, D.W., and Kauffman, L., 1993, Analysis of residential use of water in the Denver metropolitan area, Colorado, 1980-87: U.S. Geological Survey Water-Resources Investigations Report 92-4030, v, 69 p. :ill. ;28 cm., https://doi.org/10.3133/wri924030.","productDescription":"v, 69 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":119621,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4030/report-thumb.jpg"},{"id":57210,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4030/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db6801ff","contributors":{"authors":[{"text":"Litke, D. W.","contributorId":94346,"corporation":false,"usgs":true,"family":"Litke","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":199743,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kauffman, L.F.","contributorId":61866,"corporation":false,"usgs":true,"family":"Kauffman","given":"L.F.","email":"","affiliations":[],"preferred":false,"id":199742,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28414,"text":"wri934111 - 1993 - Results of ground-water, surface-water, and water-quality monitoring, Black Mesa area, northeastern Arizona– 1991-92","interactions":[],"lastModifiedDate":"2021-12-09T21:07:18.83874","indexId":"wri934111","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"93-4111","title":"Results of ground-water, surface-water, and water-quality monitoring, Black Mesa area, northeastern Arizona– 1991-92","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri934111","usgsCitation":"Littin, G.R., 1993, Results of ground-water, surface-water, and water-quality monitoring, Black Mesa area, northeastern Arizona– 1991-92: U.S. Geological Survey Water-Resources Investigations Report 93-4111, iv, 23 p., https://doi.org/10.3133/wri934111.","productDescription":"iv, 23 p.","costCenters":[],"links":[{"id":392695,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47825.htm"},{"id":57218,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4111/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159281,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4111/report-thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Black Mesa area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.5,\n 35.5\n ],\n [\n -109.5,\n 35.5\n ],\n [\n -109.5,\n 37\n ],\n [\n -111.5,\n 37\n ],\n [\n -111.5,\n 35.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db614923","contributors":{"authors":[{"text":"Littin, G. R.","contributorId":95924,"corporation":false,"usgs":true,"family":"Littin","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":199755,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28646,"text":"wri934044 - 1993 - Hydrogeology, water quality, and water-resources development potential of the upper Floridan Aquifer in the Valdosta area, south-central Georgia","interactions":[],"lastModifiedDate":"2017-01-25T13:50:56","indexId":"wri934044","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"93-4044","title":"Hydrogeology, water quality, and water-resources development potential of the upper Floridan Aquifer in the Valdosta area, south-central Georgia","docAbstract":"Water quality in the Upper Floridan aquifer in the Valdosta, Georgia area is adversely affected by direct recharge from the Withlacoochee River. Water enters the aquifer along a short reach of the river where sinkholes have formed in the stream bed. The water receives little filtration as it recharges the Upper Floridan aquifer through these sinkholes. Naturally occurring organic material in the river provides a readily available source of energy for the growth of microbiota in the aquifer. Microbiological processes and chemical reactions in the aquifer produce methane and hydrogen sulfide as the water from the river mixes with ground water and moves downgradient in the aquifer. Humic substances associated with the organic material in the ground water in this area can form trihalomethanes when the water is chlorinated for public supply. To assess areas most suitable for ground-water supply development, areal distributions of total organic carbon, total sulfide, and methane in the Upper Floridan aquifer were mapped and used to evaluate areas affected by recharge from the Withlacoochee River. Areas where concentrations of total organic carbon, total sulfide, and methane were less than or equal to 2.0 milligrams per liter, 0.5 milligrams per liter, and 100 micrograms per liter, respectively, were considered to be relatively unaffected by recharge from the river and to have the greatest potential for water- resources development.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri934044","usgsCitation":"McConnell, J.B., and Hacke, C., 1993, Hydrogeology, water quality, and water-resources development potential of the upper Floridan Aquifer in the Valdosta area, south-central Georgia: U.S. Geological Survey Water-Resources Investigations Report 93-4044, vi, 44 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri934044.","productDescription":"vi, 44 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":120073,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4044/report-thumb.jpg"},{"id":57487,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4044/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57488,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4044/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57489,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4044/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57490,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4044/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Georgia","city":"Valdosta","otherGeospatial":"Upper Floridan Aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -83.73367309570312,\n 30.6071859028226\n ],\n [\n -83.73367309570312,\n 31.141129518743234\n ],\n [\n -82.80670166015625,\n 31.141129518743234\n ],\n [\n -82.80670166015625,\n 30.6071859028226\n ],\n [\n -83.73367309570312,\n 30.6071859028226\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db6147c0","contributors":{"authors":[{"text":"McConnell, J. B.","contributorId":25577,"corporation":false,"usgs":true,"family":"McConnell","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":200166,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hacke, C.M.","contributorId":74037,"corporation":false,"usgs":true,"family":"Hacke","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":200167,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27499,"text":"wri934006 - 1993 - Hydrology and water quality of Reedy Creek in the Reedy Creek Improvement District, central Florida, 1986-89","interactions":[],"lastModifiedDate":"2012-02-02T00:08:44","indexId":"wri934006","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"93-4006","title":"Hydrology and water quality of Reedy Creek in the Reedy Creek Improvement District, central Florida, 1986-89","docAbstract":"The Reedy Creek Improvement District encompasses an area of about 43 sq mi in southwestern Orange and northwestern Osceola Counties in central Florida. The District operates a wastewater-treatment plant that discharges through two forested wetland areas and a percolation-pond system into Reedy Creek. Discharges from these wetland systems provide a relatively steady base flow which maintains streamflow in Reedy Creek during periods of low rainfall. Streamflows during the study were characterized by relatively long periods of below-average discharge interspersed with periods of high discharges. The highest mean discharges were recorded in 1988 and the lowest mean discharges were recorded in 1989. Water-quality data collection included the operation of four continuous water-quality monitors recording hourly water temperature, specific conductance, and dissolved oxygen concentration, and the collection of water-quality samples. Dissolved oxygen concentrations were similar for all stations on Reedy Creek and frequently were less than the minimum Florida standard of 5.0 mg/L. These low dissolved oxygen concentrations probably are the result of natural conditions. Nutrient analyses of water-quality samples were used to compute loadings into and out of a wetland conservation area in the southern part of the District and in the reach of Reedy Creek downstream from the wastewater discharges. Overall retention percentages for 1986-89, not including atmospheric and precipitation inputs, were 59.1 percent for total ammonia nitrogen: 3.4 percent for total organic nitrogen, which was the predominant nitrogen species: 33.2 percent for total nitrate nitrogen; 27.0 percent for total phosphorus; and 26.0 percent for total organic carbon. Highest loading inputs to the wetland conservation area were from the reach of Reedy Creek receiving wastewater discharge. Discharges from the wetlands receiving wastewater and entering the wetland conservation area during 1988 carried 16.3 percent of the total nitrogen load, and 25.0 percent of the total phosphorus load: during 1989 the discharges carried 22.0 percent of the total N and 21.0 percent of the total P.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri934006","usgsCitation":"Hampson, P.S., 1993, Hydrology and water quality of Reedy Creek in the Reedy Creek Improvement District, central Florida, 1986-89: U.S. Geological Survey Water-Resources Investigations Report 93-4006, vi, 57 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri934006.","productDescription":"vi, 57 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123532,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4006/report-thumb.jpg"},{"id":56349,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4006/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604da7","contributors":{"authors":[{"text":"Hampson, P. S.","contributorId":58677,"corporation":false,"usgs":true,"family":"Hampson","given":"P.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":198219,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27492,"text":"wri924153 - 1993 - Summary of ground-water data and evaluation of ground-water monitoring networks for eastern Merced County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:35","indexId":"wri924153","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"92-4153","title":"Summary of ground-water data and evaluation of ground-water monitoring networks for eastern Merced County, California","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri924153","usgsCitation":"Hamlin, S.N., 1993, Summary of ground-water data and evaluation of ground-water monitoring networks for eastern Merced County, California: U.S. Geological Survey Water-Resources Investigations Report 92-4153, v, 14 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri924153.","productDescription":"v, 14 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158589,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4153/report-thumb.jpg"},{"id":56342,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4153/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6991de","contributors":{"authors":[{"text":"Hamlin, S. N.","contributorId":46560,"corporation":false,"usgs":true,"family":"Hamlin","given":"S.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":198209,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26594,"text":"wri924145 - 1993 - Method for predicting water demand for crop uses in New Jersey in 1990, 2000, 2010, and 2020, and for estimating water use for livestock and selected sectors of the food-processing industry in New Jersey in 1987","interactions":[],"lastModifiedDate":"2012-02-02T00:08:22","indexId":"wri924145","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"92-4145","title":"Method for predicting water demand for crop uses in New Jersey in 1990, 2000, 2010, and 2020, and for estimating water use for livestock and selected sectors of the food-processing industry in New Jersey in 1987","docAbstract":"A method was developed to predict water demand for crop uses in New Jersey. A separate method was developed to estimate water use for livestock and selected sectors of the food-processing industry in 1987. Predictions of water demand for field- grown crops in New Jersey were made for 1990, 2000, 2010, and 2020 under three climatological scenarios: (1) wet year, (2) average year, and (3) drought year. These estimates ranged from 4.10 times 10 to the 9th power to 16.82 times 10 to the 9th power gal (gallons). Irrigation amounts calculated for the three climatological scenarios by using a daily water-balance model were multiplied by predicted numbers of irrigated acreage. Irrigated acreage was predicted from historical crop-irrigation data and from predictions of harvested acreage produced by using a statistical model relating population to harvested acreage. Predictions of water demand for cranberries and container-grown nursery crops also were made for 1990, 2000, 2010, and 2020. Predictions of water demand under the three climatological scenarios were made for container- grown nursery crops, but not for cranberries, because water demand for cranberries varies little in response to climatological factors. Water demand for cranberries was predicted to remain constant at 4.43 times 10 to the 9th power gal through the year 2020. Predictions of water demand for container-grown nursery crops ranged from 1.89 times 10 to the 9th power to 3.63 times 10 to the 9th power gal. Water-use for livestock in 1987 was estimated to be 0.78 times 10 to the 9th power gal, and water use for selected sectors of the food-processing industry was estimated to be 3.75 times 10 to the 9th power gal.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri924145","usgsCitation":"Clawges, R., and Titus, E., 1993, Method for predicting water demand for crop uses in New Jersey in 1990, 2000, 2010, and 2020, and for estimating water use for livestock and selected sectors of the food-processing industry in New Jersey in 1987: U.S. Geological Survey Water-Resources Investigations Report 92-4145, ix, 211 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri924145.","productDescription":"ix, 211 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123613,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4145/report-thumb.jpg"},{"id":55461,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4145/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55462,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4145/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629f09","contributors":{"authors":[{"text":"Clawges, R.M.","contributorId":24779,"corporation":false,"usgs":true,"family":"Clawges","given":"R.M.","affiliations":[],"preferred":false,"id":196675,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Titus, E.O.","contributorId":85984,"corporation":false,"usgs":true,"family":"Titus","given":"E.O.","email":"","affiliations":[],"preferred":false,"id":196676,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28453,"text":"wri914153 - 1993 - Characteristics of fluvial systems in the plains and deserts of Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:52","indexId":"wri914153","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"91-4153","title":"Characteristics of fluvial systems in the plains and deserts of Wyoming","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri914153","usgsCitation":"Lowham, H., and Smith, M., 1993, Characteristics of fluvial systems in the plains and deserts of Wyoming: U.S. Geological Survey Water-Resources Investigations Report 91-4153, v, 57 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri914153.","productDescription":"v, 57 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118936,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4153/report-thumb.jpg"},{"id":57254,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4153/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e5020","contributors":{"authors":[{"text":"Lowham, H. W.","contributorId":8111,"corporation":false,"usgs":true,"family":"Lowham","given":"H. W.","affiliations":[],"preferred":false,"id":199825,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, M.E.","contributorId":104525,"corporation":false,"usgs":true,"family":"Smith","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":199826,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28458,"text":"wri904154 - 1993 - Assessment of the hydrologic system and hydrologic effects of uranium exploration and mining in the southern Powder River Basin Uranium District and adjacent areas, Wyoming, 1983","interactions":[],"lastModifiedDate":"2012-02-02T00:08:52","indexId":"wri904154","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"90-4154","title":"Assessment of the hydrologic system and hydrologic effects of uranium exploration and mining in the southern Powder River Basin Uranium District and adjacent areas, Wyoming, 1983","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri904154","usgsCitation":"Lowry, M., Daddow, P., and Rucker, S.J., 1993, Assessment of the hydrologic system and hydrologic effects of uranium exploration and mining in the southern Powder River Basin Uranium District and adjacent areas, Wyoming, 1983: U.S. Geological Survey Water-Resources Investigations Report 90-4154, iv, 42 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri904154.","productDescription":"iv, 42 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":121574,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4154/report-thumb.jpg"},{"id":57260,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1990/4154/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57261,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1990/4154/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57262,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4154/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671d47","contributors":{"authors":[{"text":"Lowry, M.E.","contributorId":55807,"corporation":false,"usgs":true,"family":"Lowry","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":199834,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Daddow, P. B.","contributorId":26700,"corporation":false,"usgs":true,"family":"Daddow","given":"P. B.","affiliations":[],"preferred":false,"id":199832,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rucker, Samuel J. IV","contributorId":37717,"corporation":false,"usgs":true,"family":"Rucker","given":"Samuel","suffix":"IV","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":199833,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":28482,"text":"wri934013 - 1993 - Regionalization of low-flow characteristics of Arkansas streams","interactions":[],"lastModifiedDate":"2012-02-02T00:08:46","indexId":"wri934013","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"93-4013","title":"Regionalization of low-flow characteristics of Arkansas streams","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri934013","usgsCitation":"Ludwig, A.H., and Tasker, G.D., 1993, Regionalization of low-flow characteristics of Arkansas streams: U.S. Geological Survey Water-Resources Investigations Report 93-4013, iv, 19, 1-7 p. :maps ;28 cm. +1 computer disk (3 1/2 in.) [PGS - 26 p.], https://doi.org/10.3133/wri934013.","productDescription":"iv, 19, 1-7 p. :maps ;28 cm. +1 computer disk (3 1/2 in.) [PGS - 26 p.]","costCenters":[],"links":[{"id":159195,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4013/report-thumb.jpg"},{"id":57280,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4013/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57281,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4013/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db634da4","contributors":{"authors":[{"text":"Ludwig, A. H.","contributorId":63007,"corporation":false,"usgs":true,"family":"Ludwig","given":"A.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":199883,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tasker, Gary D.","contributorId":83097,"corporation":false,"usgs":true,"family":"Tasker","given":"Gary","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":199884,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27361,"text":"wri914087 - 1993 - Summary appraisal of water resources of the Umatilla Indian Reservation","interactions":[],"lastModifiedDate":"2017-02-07T07:55:14","indexId":"wri914087","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"91-4087","title":"Summary appraisal of water resources of the Umatilla Indian Reservation","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri914087","usgsCitation":"Gonthier, J.B., and Bolke, E., 1993, Summary appraisal of water resources of the Umatilla Indian Reservation: U.S. Geological Survey Water-Resources Investigations Report 91-4087, vi, 54 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri914087.","productDescription":"vi, 54 p. :ill., maps ;28 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":56224,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4087/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56225,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4087/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158281,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4087/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6995fb","contributors":{"authors":[{"text":"Gonthier, J. B.","contributorId":63805,"corporation":false,"usgs":true,"family":"Gonthier","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":197981,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bolke, E.L.","contributorId":52151,"corporation":false,"usgs":true,"family":"Bolke","given":"E.L.","affiliations":[],"preferred":false,"id":197980,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28492,"text":"wri924042 - 1993 - Maximum known stages and discharges of New York streams, 1865-1989, with descriptions of five selected floods, 1913-85","interactions":[],"lastModifiedDate":"2012-02-02T00:08:46","indexId":"wri924042","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"92-4042","title":"Maximum known stages and discharges of New York streams, 1865-1989, with descriptions of five selected floods, 1913-85","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri924042","usgsCitation":"Lumia, R., and Murray, P., 1993, Maximum known stages and discharges of New York streams, 1865-1989, with descriptions of five selected floods, 1913-85: U.S. Geological Survey Water-Resources Investigations Report 92-4042, iv, 123 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri924042.","productDescription":"iv, 123 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119043,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4042/report-thumb.jpg"},{"id":57290,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4042/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57291,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4042/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57292,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4042/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db61012d","contributors":{"authors":[{"text":"Lumia, Richard rlumia@usgs.gov","contributorId":4579,"corporation":false,"usgs":true,"family":"Lumia","given":"Richard","email":"rlumia@usgs.gov","affiliations":[],"preferred":true,"id":199903,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Murray, P.M.","contributorId":33358,"corporation":false,"usgs":true,"family":"Murray","given":"P.M.","email":"","affiliations":[],"preferred":false,"id":199904,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27468,"text":"wri904011 - 1993 - Water quality of the Upper West Branch Susquehanna River and tributary streams between Curwensville and Renovo, Pennsylvania, May and July 1984","interactions":[],"lastModifiedDate":"2017-07-05T10:07:49","indexId":"wri904011","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"90-4011","title":"Water quality of the Upper West Branch Susquehanna River and tributary streams between Curwensville and Renovo, Pennsylvania, May and July 1984","docAbstract":"The soils and rocks of the Upper West Branch Susquehanna River basin, from its headwaters downstream for 150 miles, are laden with pyritic materials that have the potential to produce acid mine drainage. The effects of mine drainage are severe, particularly in the reach between Curwensville and Renovo where present water quality cannot support viable populations of benthic macroinvertebrates or fish.\r\n\r\n During base-flow periods in May and July 1984, streamflow and water quality were measured at four sites on the West Branch Susquehanna River and near the mouths of 94 tributaries. Water-quality constituents determined were temperature, specific conductance, pH, acidity, alkalinity, and concentrations of dissolved sulfate and total and dissolved forms of iron, manganese, aluminum, and zinc.\r\n\r\n The data collected for the study indicate that the predominant influence on water quality of the tributaries is land use. An area where few or no coal deposits or disturbed area were present was found to have relatively good surface-water quality (median pH was nearly 5.5 units), whereas areas where coal mining was active in the basin, or where large areas of unreclaimed mines were present, were found to have poorest water quality (median pH was generally less than 4.0 units).\r\n\r\n In general, Moshannon, Sinnemahoning, Clearfield, and Kettle Creeks were found to be the largest tributary sources of acidity and total-recoverable iron to the river. During the May sampling, Moshannon, Sinnemahoning, and Clearfield Creeks contributed 63 percent of the 365 tons/day of acidity, and Moshannon and Clearfield Creeks contributed 76 percent of the 44.8 tons/day of total-recoverable iron that were discharged to the river. During the July sampling, Moshannon, Kettle, and Clearfield Creeks contributed 60 percent of the 131 tons/day of acidity, and Moshannon and Kettle Creeks contributed 51 percent of the 6.5 tons/day of total-recoverable iron discharged to the river .\r\n\r\n The West Branch Susquehanna River was found to have pH ranging from 5.4 to 6.5 units and specific conductance ranging from 267 to 310 microsiemens per centimeter at the most upstream site at Curwensville. The water quality was most degraded at the site at Karthaus (pH 3.9 to 4.1 units, specific conductance 330 to 610 microsiemens per centimeter). Quality gradually improved downstream to the site at Renovo (pH 3.8 to 4.6 units, specific conductance 200 to 392 microsiemens per centimeter), although the quality did not recover to that found at Curwensville.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri904011","usgsCitation":"Hainly, R., and Barker, J.L., 1993, Water quality of the Upper West Branch Susquehanna River and tributary streams between Curwensville and Renovo, Pennsylvania, May and July 1984: U.S. Geological Survey Water-Resources Investigations Report 90-4011, v, 61 p. :ill. ;28 cm., https://doi.org/10.3133/wri904011.","productDescription":"v, 61 p. :ill. ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":157970,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4011/report-thumb.jpg"},{"id":56324,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4011/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f991f","contributors":{"authors":[{"text":"Hainly, R.A.","contributorId":45732,"corporation":false,"usgs":true,"family":"Hainly","given":"R.A.","affiliations":[],"preferred":false,"id":198171,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barker, J. L.","contributorId":83518,"corporation":false,"usgs":true,"family":"Barker","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":198172,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28538,"text":"wri924106 - 1993 - Development, calibration, and testing of ground-water flow models for the Mississippi River Valley alluvial aquifer in eastern Arkansas using one-square-mile cells","interactions":[],"lastModifiedDate":"2012-02-02T00:08:46","indexId":"wri924106","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"92-4106","title":"Development, calibration, and testing of ground-water flow models for the Mississippi River Valley alluvial aquifer in eastern Arkansas using one-square-mile cells","docAbstract":"Significant water-level declines in the Mississippi River Valley alluvial aquifer prompted the need to better understand the flow system in the aquifer which, in turn, led to the development of digital groundwater flow models of the alluvial aquifer. Two models were developed in the eastern Arkansas study area with the Arkansas River dividing the study area and functioning as a hydrologic boundary to the models. Both models simulate groundwater flow in one layer with recharge entering the aquifer from head-dependent surface infiltration through the overlying confining unit and from seepage through river beds. Digital models were used to simulate flow in the aquifer during seven stress periods between 1918 and 1987. Pumpage used in the simulations ranged from 83,400,000 to 412,000,000 cu ft/d in the north model and from 12,800,000 to 58,500,000 cu ft/d in the south model. Three different spatial and temporal pumpage scenarios were tested to simulate pumpage stress in the models. The pumpage distribution used in the calibrated model was based on a combination of all three scenarios. Several criteria were used during model development to determine how well the model simulated conditions in the aquifer. Potentiometric maps of model-computed water levels were compared to measured data to check the computed water levels and direction of flow. Hydrographs of observation wells were compared to computed water levels at corresponding model cells to assess the temporal distribution of pumpage. A root-mean-square error analysis was performed during calibration by comparing observation-well and model-computed water levels for 1972. Sensitivity analyses were performed to determine the effects of changes in input parameters on computed heads (water levels). Both models were sensitive to changes in recharge and pumpage but the south model generally was less sensitive than the north model.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri924106","usgsCitation":"Mahon, G., and Poynter, D., 1993, Development, calibration, and testing of ground-water flow models for the Mississippi River Valley alluvial aquifer in eastern Arkansas using one-square-mile cells: U.S. Geological Survey Water-Resources Investigations Report 92-4106, iv, 33 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri924106.","productDescription":"iv, 33 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123658,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4106/report-thumb.jpg"},{"id":57351,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4106/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65dd48","contributors":{"authors":[{"text":"Mahon, G.L. 0000-0002-7410-0261","orcid":"https://orcid.org/0000-0002-7410-0261","contributorId":28636,"corporation":false,"usgs":true,"family":"Mahon","given":"G.L.","affiliations":[],"preferred":false,"id":199986,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poynter, D.T.","contributorId":57902,"corporation":false,"usgs":true,"family":"Poynter","given":"D.T.","affiliations":[],"preferred":false,"id":199987,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28544,"text":"wri934082 - 1993 - Quality-assurance data for routine water analysis in the laboratories of the US Geological Survey for water year 1990","interactions":[],"lastModifiedDate":"2012-02-02T00:08:46","indexId":"wri934082","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"93-4082","title":"Quality-assurance data for routine water analysis in the laboratories of the US Geological Survey for water year 1990","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri934082","usgsCitation":"Maloney, T.J., Ludtke, A., and Krizman, T., 1993, Quality-assurance data for routine water analysis in the laboratories of the US Geological Survey for water year 1990: U.S. Geological Survey Water-Resources Investigations Report 93-4082, xiii, 145 p. :ill. ;28 cm., https://doi.org/10.3133/wri934082.","productDescription":"xiii, 145 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":159253,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4082/report-thumb.jpg"},{"id":57376,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4082/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ae4b07f02db6515b6","contributors":{"authors":[{"text":"Maloney, T. J.","contributorId":56660,"corporation":false,"usgs":true,"family":"Maloney","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":199996,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ludtke, A. S.","contributorId":6846,"corporation":false,"usgs":true,"family":"Ludtke","given":"A. S.","affiliations":[],"preferred":false,"id":199995,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krizman, T.L.","contributorId":57505,"corporation":false,"usgs":true,"family":"Krizman","given":"T.L.","email":"","affiliations":[],"preferred":false,"id":199997,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":26673,"text":"wri934056 - 1993 - Surface-water and streambed-sediment quality of streams draining surface-mined land reclaimed with sewage sludge, Fulton County, Illinois, 1972-89","interactions":[],"lastModifiedDate":"2012-02-02T00:08:32","indexId":"wri934056","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"93-4056","title":"Surface-water and streambed-sediment quality of streams draining surface-mined land reclaimed with sewage sludge, Fulton County, Illinois, 1972-89","docAbstract":"Sewage sludge has been used to reclaim surface- mined land in Fulton County, Ill. The sludge contains substantial concentrations of nutrients and significant concentrations of toxic organic compounds. Because of the concern of the fate of these toxins, the U.S. Geological Survey in cooperation with the Metropolitan Water Reclamation District of Greater Chicago began an analysis of historical data in 1989 to compare the quality of water and streambed sediments to determine whether the application of sludge is adversely affecting the quality of surface water. Trend analyses on surface-water-quality data suggest that sludge application is affecting the quality of water in Evelyn Branch in the form of increased concentrations of nitrite plus nitrate and kjeldahl nitrogen. However, the concentrations of these constituents in Evelyn Branch, the stream draining the sludge-application field, are small compared to the concentrations upstream from the project area. Analysis of the streambed-quality data indicates that, for the constituents measured, the application of sludge is not affecting the streambed quality in Evelyn Branch. Trend analyses of streambed constituents did not indicate any adverse effects that could be related to the application of sludge. However, the avail- able data are not adequate to determine if the quality of the streambed has been adversely affected by the sludge application. A refinement of the sampling scheme would be necessary to rule out the possibility of present and future adverse effects of sludge application on streambed quality.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri934056","usgsCitation":"Coupe, R., and Macy, J.A., 1993, Surface-water and streambed-sediment quality of streams draining surface-mined land reclaimed with sewage sludge, Fulton County, Illinois, 1972-89: U.S. Geological Survey Water-Resources Investigations Report 93-4056, v, 53 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri934056.","productDescription":"v, 53 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158105,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4056/report-thumb.jpg"},{"id":55538,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4056/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a7dd","contributors":{"authors":[{"text":"Coupe, R.H.","contributorId":84778,"corporation":false,"usgs":true,"family":"Coupe","given":"R.H.","affiliations":[],"preferred":false,"id":196808,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Macy, J. A.","contributorId":10047,"corporation":false,"usgs":true,"family":"Macy","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":196807,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28564,"text":"wri934084 - 1993 - Estimated use of water in the Apalachicola-Chattahoochee-Flint River basin during 1990, with state summaries from 1970 to 1990","interactions":[],"lastModifiedDate":"2023-01-11T19:29:26.165727","indexId":"wri934084","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"93-4084","title":"Estimated use of water in the Apalachicola-Chattahoochee-Flint River basin during 1990, with state summaries from 1970 to 1990","docAbstract":"The Apalachicola-Chattahoochee-Flint River basin covers approximately 19,800 square miles in parts of Alabama, Florida, and Georgia. Most of the basin lies within Georgia as does most of the population. Most of the water withdrawn in the basin in 1990 was withdrawn in Georgia (82 percent). Withdrawals in Florida and Alabama each accounted for 9 percent of the total withdrawal in the basin. Water with- drawn in the basin for 1990 totaled 2,098 million gallons per day, of which approximately 17 percent (351 million gallons per day) was consumed. Of the total water used, nearly 86 percent was withdrawn from surface-water sources, and the remaining 14 percent was withdrawn from ground-water sources. Nearly 63 percent of the surface water used in the basin during 1990 was for thermoelectric power generation; other surface water uses included public supply (24 percent), self-supplied commercial- industrial use (12 percent), and agricultural use (4 percent). Nearly 58 percent of the ground water used in the basin for 1990 was used for agricultural irrigation; other ground-water uses included public supply (21 percent), self-supplied domestic use (11 percent), self-supplied commercial-industrial use (9 percent), and thermoelectric power generation (less than 1 percent). The Chattahoochee River supplied most of the surface water used in the basin (64 percent) and the Floridan aquifer system supplied most of the ground water used (44 percent) in 1990. During 1990, 39,815 Mgal/d of water was used to produce 35,843 gigawatthours of electricity. Of that total, 1.076 Mgal/d was used to produced 33,460 gigawwatthours of electricity at 8 fossil fuel facilities and 38,740 Mgal/d was used to produce 2,384 gigawatthours of electricity at 14 hydroelectric facilities.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri934084","usgsCitation":"Marella, R., Fanning, J.L., and Mooty, W., 1993, Estimated use of water in the Apalachicola-Chattahoochee-Flint River basin during 1990, with state summaries from 1970 to 1990: U.S. Geological Survey Water-Resources Investigations Report 93-4084, vi, 45 p., https://doi.org/10.3133/wri934084.","productDescription":"vi, 45 p.","costCenters":[],"links":[{"id":124114,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_93_4084.jpg"},{"id":411728,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47802.htm","linkFileType":{"id":5,"text":"html"}},{"id":2350,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri934084","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alabama, Florida, Georgia","otherGeospatial":"Apalachicola-Chattahoochee-Flint River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -85.5833,\n 34.8167\n ],\n [\n -85.5833,\n 29.5833\n ],\n [\n -83.4,\n 29.5833\n ],\n [\n -83.4,\n 34.8167\n ],\n [\n -85.5833,\n 34.8167\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fccc0","contributors":{"authors":[{"text":"Marella, R. L.","contributorId":34164,"corporation":false,"usgs":true,"family":"Marella","given":"R. L.","affiliations":[],"preferred":false,"id":200035,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fanning, J. L.","contributorId":43395,"corporation":false,"usgs":true,"family":"Fanning","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":200036,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mooty, W. S.","contributorId":55837,"corporation":false,"usgs":true,"family":"Mooty","given":"W. S.","affiliations":[],"preferred":false,"id":200037,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":26651,"text":"wri914111 - 1993 - Hydrology of the L.C. Holding coal-lease tract and adjacent areas, southwestern Utah, and potential effects of coal mining","interactions":[],"lastModifiedDate":"2022-01-12T22:06:33.129767","indexId":"wri914111","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"91-4111","title":"Hydrology of the L.C. Holding coal-lease tract and adjacent areas, southwestern Utah, and potential effects of coal mining","docAbstract":"The U.S. Bureau of Land Management recognized a need for baseline hydrologic data and an understanding of the hydrologic system in the L.C. Holding coal-lease tract in order to determine the potential effects of mining on the water resources of the area. The potential impacts of mining on the hydrology of the area are of concern because Zion National Park is less than 3 miles from the westernmost part of the lease tract. Much of the water that passes through the Park either originates in the lease tract or traverses it. Runoff from melting snowpacks and summer thundershowers contributes most of the flow to perennial streams in the area. Base flow is sustained by spring discharge and diffuse seepage. Regional groundwater movement is southward. Most of the geologic formations in the study area contain aquifers. The water table of the regional aquifer is about 870 ft deep in the Navajo Sandstone. Groundwater issuing from the Navajo Sandstone on the east side of Zion Canyon has specific conductance values several times larger than groundwater from the west side, indicating recharge to the Navajo from the overlying strata, which contain water of larger specific conductance. Potential effects of mining in the area include: (1) increased dissolved-solids concen- trations and decreased pH values in both surface and groundwater; (2) dewatering of aquifers, causing a decrease or cessation of flow to some springs; and (3) land subsidence and associated subsidence fractures.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri914111","usgsCitation":"Cordy, G., Seiler, R.L., and Stolp, B., 1993, Hydrology of the L.C. Holding coal-lease tract and adjacent areas, southwestern Utah, and potential effects of coal mining: U.S. Geological Survey Water-Resources Investigations Report 91-4111, Report: vii, 84 p.; 2 Plates: 24.88 × 27.67 inches and 25.92 × 29.21 inches, https://doi.org/10.3133/wri914111.","productDescription":"Report: vii, 84 p.; 2 Plates: 24.88 × 27.67 inches and 25.92 × 29.21 inches","costCenters":[],"links":[{"id":394286,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47518.htm"},{"id":55529,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4111/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55528,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4111/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55527,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4111/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123741,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4111/report-thumb.jpg"}],"country":"United States","state":"Utah","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.8667,\n 37.2639\n ],\n [\n -112.7192,\n 37.2639\n ],\n [\n -112.7192,\n 37.45\n ],\n [\n -112.8667,\n 37.45\n ],\n [\n -112.8667,\n 37.2639\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db66712f","contributors":{"authors":[{"text":"Cordy, G. E.","contributorId":59075,"corporation":false,"usgs":true,"family":"Cordy","given":"G. E.","affiliations":[],"preferred":false,"id":196774,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Seiler, R. L.","contributorId":87546,"corporation":false,"usgs":true,"family":"Seiler","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":196776,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stolp, Bernard J. 0000-0003-3803-1497","orcid":"https://orcid.org/0000-0003-3803-1497","contributorId":71942,"corporation":false,"usgs":true,"family":"Stolp","given":"Bernard J.","affiliations":[],"preferred":false,"id":196775,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":28585,"text":"wri924173 - 1993 - Regionalization of harmonic-mean streamflows in Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:08:47","indexId":"wri924173","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"92-4173","title":"Regionalization of harmonic-mean streamflows in Kentucky","docAbstract":"Harmonic-mean streamflow (Qh), defined as the reciprocal of the arithmetic mean of the reciprocal daily streamflow values, was determined for selected stream sites in Kentucky. Daily mean discharges for the available period of record through the 1989 water year at 230 continuous record streamflow-gaging stations located in and adjacent to Kentucky were used in the analysis. Periods of record affected by regulation were identified and analyzed separately from periods of record unaffected by regulation. Record-extension procedures were applied to short-term stations to reducetime-sampling error and, thus, improve estimates of the long-term Qh. \r\n\r\nTechniques to estimate the Qh at ungaged stream sites in Kentucky were developed. A regression model relating Qh to total drainage area and streamflow-variability index was presented with example applications. The regression model has a standard error of estimate of 76 percent and a standard error of prediction of 78 percent.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri924173","usgsCitation":"Martin, G.R., and Ruhl, K.J., 1993, Regionalization of harmonic-mean streamflows in Kentucky: U.S. Geological Survey Water-Resources Investigations Report 92-4173, v, 47 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri924173.","productDescription":"v, 47 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159152,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2361,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri924173/","linkFileType":{"id":5,"text":"html"}},{"id":57413,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4173/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db634e1c","contributors":{"authors":[{"text":"Martin, Gary R. 0000-0002-3274-5846 grmartin@usgs.gov","orcid":"https://orcid.org/0000-0002-3274-5846","contributorId":3413,"corporation":false,"usgs":true,"family":"Martin","given":"Gary","email":"grmartin@usgs.gov","middleInitial":"R.","affiliations":[{"id":354,"text":"Kentucky Water Science Center","active":true,"usgs":true}],"preferred":true,"id":200069,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ruhl, Kevin J.","contributorId":35769,"corporation":false,"usgs":true,"family":"Ruhl","given":"Kevin","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":200070,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26637,"text":"wri924178 - 1993 - Digital data acquisition and development of geographic information system coverages for use with the public water-supply wells and springs in Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:08:27","indexId":"wri924178","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"92-4178","title":"Digital data acquisition and development of geographic information system coverages for use with the public water-supply wells and springs in Tennessee","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nCopies of this report can be purchased from U.S. Geological Survey Books and Open-File Reports Section,","doi":"10.3133/wri924178","usgsCitation":"Connell, J.F., and Barron, W., 1993, Digital data acquisition and development of geographic information system coverages for use with the public water-supply wells and springs in Tennessee: U.S. Geological Survey Water-Resources Investigations Report 92-4178, 28 p. :maps ;28 cm., https://doi.org/10.3133/wri924178.","productDescription":"28 p. :maps ;28 cm.","costCenters":[],"links":[{"id":121862,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4178/report-thumb.jpg"},{"id":55510,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4178/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d52f","contributors":{"authors":[{"text":"Connell, J. F.","contributorId":88779,"corporation":false,"usgs":true,"family":"Connell","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":196748,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barron, W.R.","contributorId":104103,"corporation":false,"usgs":true,"family":"Barron","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":196749,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26623,"text":"wri914018 - 1993 - Estimated average annual ground-water pumpage in the Portland Basin, Oregon and Washington 1987-88","interactions":[],"lastModifiedDate":"2017-02-07T08:26:08","indexId":"wri914018","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"91-4018","title":"Estimated average annual ground-water pumpage in the Portland Basin, Oregon and Washington 1987-88","docAbstract":"Data for ground-water pumpage were collected during an inventory of wells in 1987-88 in the Portland Basin located in northwestern Oregon and southwestern Washington. Estimates of annual ground-water pumpage were made for the three major categories of use: public supply, industry, and irrigation. A large rapidly expanding metropolitan area is situated within the Portland Basin, along with several large industries that use significant quantities of ground water. The estimated total average annual ground-water pumpage for 1987 was about 127,800 acre-feet. Of this quantity, about 50 percent was pumped for industrial use, about 40 percent for public supply and about 10 percent for irrigation. Domestic use from individual wells is a small part of the total and is not included.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri914018","usgsCitation":"Collins, C.A., and Broad, T., 1993, Estimated average annual ground-water pumpage in the Portland Basin, Oregon and Washington 1987-88: U.S. Geological Survey Water-Resources Investigations Report 91-4018, v, 26 p. :maps (chiefly col.) ;28 cm., https://doi.org/10.3133/wri914018.","productDescription":"v, 26 p. :maps (chiefly col.) ;28 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":121508,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4018/report-thumb.jpg"},{"id":55491,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4018/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55492,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4018/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55493,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4018/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55494,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4018/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55495,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4018/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdc4b","contributors":{"authors":[{"text":"Collins, C. A.","contributorId":43731,"corporation":false,"usgs":true,"family":"Collins","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":196730,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Broad, T.M.","contributorId":6478,"corporation":false,"usgs":true,"family":"Broad","given":"T.M.","affiliations":[],"preferred":false,"id":196729,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28617,"text":"wri934043 - 1993 - Hydrogeologic setting and hydrologic data of the Smoke Creek Desert basin, Washoe County, Nevada, and Lassen County, California, water years 1988-90","interactions":[],"lastModifiedDate":"2012-02-02T00:08:47","indexId":"wri934043","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"93-4043","title":"Hydrogeologic setting and hydrologic data of the Smoke Creek Desert basin, Washoe County, Nevada, and Lassen County, California, water years 1988-90","docAbstract":"Smoke Creek Desert is a potential source of water for urban development in Washoe County, Nevada. Hydrogeologic data were collected from 1988 to 1990 to learn more about surface- and ground-water flow in the basin. Impermeable rocks form a boundary to ground-water flow on the east side of the basin and at unknown depths at the base of the flow system. Permeable volcanic rocks on the west and north sides of the basin represent a previously unrecognized aquifer and provide potential avenues for interbasin flow. Geophysical data indicate that basin-fill sediments are about 2,000 feet thick near the center of the basin. The geometry of the aquifers, however, remains largely unknown. Measurements of water levels, pressure head, flow rate, water temperature, and specific conductance at 19 wells show little change from 1988 to 1990. Chemically, ground water begins as a dilute sodium and calcium bicarbonate water in the mountain blocks, changes to a slightly saline sodium bicarbonate solution beneath the alluvial fans, and becomes a briny sodium chloride water near the playa. Concentrations of several inorganic constituents in the briny water near the playa commonly exceed Nevada drinking-water standards. Ground water in the Honey Lake basin and Smoke Creek Desert basin has similar stable-isotope composition, except near Sand Pass. If interbasin flow takes place, it likely occurs at depths greater than 400-600 feet beneath Sand Pass or through volcanic rocks to the north of Sand Pass. Measure- ments of streamflow indicate that about 2,800 acre-feet/year discharged from volcanic rocks to streamflow and a minimum of 7.300 acre-feet/year infiltrated and recharged unconsolidated sediments near Smoke, Buffalo, and Squaw Creeks during the period of study. Also about 1,500 acre-feet per year was lost to evapotranspiration along the channel of Smoke Creek, and about 1,680 acre-feet per year of runoff from Smoke, Buffalo, and Squaw Creeks was probably lost to evaporation from the playa.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri934043","usgsCitation":"Maurer, D.K., 1993, Hydrogeologic setting and hydrologic data of the Smoke Creek Desert basin, Washoe County, Nevada, and Lassen County, California, water years 1988-90: U.S. Geological Survey Water-Resources Investigations Report 93-4043, v, 45 p. :ill., maps (1 col.) ;28 cm., https://doi.org/10.3133/wri934043.","productDescription":"v, 45 p. :ill., maps (1 col.) ;28 cm.","costCenters":[],"links":[{"id":123516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4043/report-thumb.jpg"},{"id":57444,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4043/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57445,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4043/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57446,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4043/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db6278ed","contributors":{"authors":[{"text":"Maurer, D. K.","contributorId":37757,"corporation":false,"usgs":true,"family":"Maurer","given":"D.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":200122,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27744,"text":"wri934030 - 1993 - Application of a hydrochemical model and a multivariate soil-solution mixing model to alpine watersheds in the Sierra Nevada, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:26","indexId":"wri934030","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"93-4030","title":"Application of a hydrochemical model and a multivariate soil-solution mixing model to alpine watersheds in the Sierra Nevada, California","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri934030","usgsCitation":"Hooper, R.P., and Peters, N., 1993, Application of a hydrochemical model and a multivariate soil-solution mixing model to alpine watersheds in the Sierra Nevada, California: U.S. Geological Survey Water-Resources Investigations Report 93-4030, vi, 58 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri934030.","productDescription":"vi, 58 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123105,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4030/report-thumb.jpg"},{"id":56589,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4030/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67ab64","contributors":{"authors":[{"text":"Hooper, R. P.","contributorId":26321,"corporation":false,"usgs":true,"family":"Hooper","given":"R.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":198627,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peters, N.E.","contributorId":33332,"corporation":false,"usgs":true,"family":"Peters","given":"N.E.","email":"","affiliations":[],"preferred":false,"id":198628,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}