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D.B.","contributorId":87971,"corporation":false,"usgs":true,"family":"Wood","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":254516,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":28953,"text":"wri824092 - 1983 - Mean annual runoff and peak flow estimates based on channel geometry of streams in southeastern Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:08:37","indexId":"wri824092","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4092","title":"Mean annual runoff and peak flow estimates based on channel geometry of streams in southeastern Montana","docAbstract":"Equations using channel-geometry measurements were developed for estimating mean runoff and peak flows of ungaged streams in southeastern Montana. Two separate sets of esitmating equations were developed for determining mean annual runoff: one for perennial streams and one for ephemeral and intermittent streams. Data from 29 gaged sites on perennial streams and 21 gaged sites on ephemeral and intermittent streams were used in these analyses. Data from 78 gaged sites were used in the peak-flow analyses. Southeastern Montana was divided into three regions and separate multiple-regression equations for each region were developed that relate channel dimensions to peak discharge having recurrence intervals of 2, 5, 10, 25, 50, and 100 years. Channel-geometery relations were developed using measurements of the active-channel width and bankfull width. Active-channel width and bankfull width were the most significant channel features for estimating mean annual runoff for al types of streams. Use of this method requires that onsite measurements be made of channel width. The standard error of estimate for predicting mean annual runoff ranged from about 38 to 79 percent. The standard error of estimate relating active-channel width or bankfull width to peak flow ranged from about 37 to 115 percent. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824092","usgsCitation":"Omang, R.J., Parrett, C., and Hull, J.A., 1983, Mean annual runoff and peak flow estimates based on channel geometry of streams in southeastern Montana: U.S. Geological Survey Water-Resources Investigations Report 82-4092, v, 38 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824092.","productDescription":"v, 38 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":120150,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4092/report-thumb.jpg"},{"id":57829,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4092/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db61047f","contributors":{"authors":[{"text":"Omang, R. J.","contributorId":31365,"corporation":false,"usgs":true,"family":"Omang","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":200675,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parrett, Charles","contributorId":9635,"corporation":false,"usgs":true,"family":"Parrett","given":"Charles","email":"","affiliations":[],"preferred":false,"id":200674,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hull, J. A.","contributorId":39345,"corporation":false,"usgs":true,"family":"Hull","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200676,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":28866,"text":"wri834083 - 1983 - Flood elevations for the Soleduck River at Sol Duc Hot Springs, Clallam County, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri834083","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4083","title":"Flood elevations for the Soleduck River at Sol Duc Hot Springs, Clallam County, Washington","docAbstract":"Elevations and inundation areas of a 100-year flood of the Soleduck River, Washington, were determined by the U.S. Geological Survey for the area in the vicinity of the Sol Duc Hot Springs resort, a public facility in the Olympic National Park that under Federal law must be located beyond or protected from damage by a 100-year flood. Results show that most flooding could be eliminated by raising parts of an existing dike. In general, little flood damage is expected, except at the southern end of an undeveloped airstrip that could become inundated and hazardous due to flow from a tributary. The airstrip is above the 100-year flood of the Soleduck River.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834083","usgsCitation":"Nelson, L.M., 1983, Flood elevations for the Soleduck River at Sol Duc Hot Springs, Clallam County, Washington: U.S. Geological Survey Water-Resources Investigations Report 83-4083, iii, 20 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834083.","productDescription":"iii, 20 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118932,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4083/report-thumb.jpg"},{"id":57746,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4083/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef25f","contributors":{"authors":[{"text":"Nelson, L. M.","contributorId":39773,"corporation":false,"usgs":true,"family":"Nelson","given":"L.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":200527,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27527,"text":"wri834108 - 1983 - Water resources of Hanson and Davison Counties, South Dakota","interactions":[],"lastModifiedDate":"2022-10-05T18:37:12.067961","indexId":"wri834108","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4108","title":"Water resources of Hanson and Davison Counties, South Dakota","docAbstract":"<p>Five glacial and four bedrock aquifers were delineated in Hanson and Davison Counties. The glacial aquifers, outwash deposits confined by as much as 275 feet of glacial till, are the Floyd, Plum Creek, Ethan, Warren, and Alexandria. The bedrock aquifers are the Niobrara, Codell, Dakota, and Sioux Quartzite Wash, and may be as much as 80, 350, 700, and 500 feet below land surface, respectively. The glacial aquifers averaged 13 to 40 feet in thickness and contain about 670,000 acre-feet of water in storage. Recharge to the Floyd and Plum Creek aquifers is from the Sioux Quartzite Wash aquifer and from fractures in the Sioux Quartzite. Recharge to the Ethan and Warren aquifers is from the Niobrara aquifer. Reported yield to wells from the Floyd and Plum Creek aquifers was as much as 1,000 gallons per minute. Predominant chemical constituents in water from the glacial aquifers are sulfate, calcium, and sodium. The bedrock aquifers averaged 40 to 110 feet in the thickness and contain about 11.3 million acre-feet of water in storage. The direction of water movement in the aquifers is to the northeast. The average reported yield from wells in the bedrock aquifers ranged from 1 to 75 gallons per minute. Reported yield from wells in the Niobrara aquifer was as much as 1,000 gallons per minute. Predominant chemical constituents in water from the Niobrara and Codell aquifers were sulfate, sodium, and calcium. Predominant chemical constituents in water from the Dakota and Sioux Quartzite wash were sulfate and calcium.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834108","usgsCitation":"Hansen, D.S., 1983, Water resources of Hanson and Davison Counties, South Dakota: U.S. Geological Survey Water-Resources Investigations Report 83-4108, vi, 55 p., https://doi.org/10.3133/wri834108.","productDescription":"vi, 55 p.","costCenters":[],"links":[{"id":407983,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35729.htm","linkFileType":{"id":5,"text":"html"}},{"id":56387,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4108/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158856,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4108/report-thumb.jpg"}],"country":"United States","state":"South Dakota","county":"Davison County, Hanson County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-97.9621,43.4984],[-98.0871,43.4984],[-98.1136,43.4994],[-98.202,43.4982],[-98.3219,43.4998],[-98.3255,43.585],[-98.3266,43.851],[-97.9662,43.851],[-97.8494,43.8505],[-97.6083,43.85],[-97.6048,43.4987],[-97.7254,43.4995],[-97.8429,43.4978],[-97.9621,43.4984]]]},\"properties\":{\"name\":\"Davison\",\"state\":\"SD\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0878","contributors":{"authors":[{"text":"Hansen, D. S.","contributorId":70003,"corporation":false,"usgs":true,"family":"Hansen","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":198262,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10564,"text":"ofr821013 - 1983 - Water resources of the Zuni Tribal Lands, McKinley and Cibola counties, New Mexico","interactions":[{"subject":{"id":10564,"text":"ofr821013 - 1983 - Water resources of the Zuni Tribal Lands, McKinley and Cibola counties, New Mexico","indexId":"ofr821013","publicationYear":"1983","noYear":false,"title":"Water resources of the Zuni Tribal Lands, McKinley and Cibola counties, New Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":2420,"text":"wsp2227 - 1987 - Water resources of the Zuni tribal lands, McKinley and Cibola Counties, New Mexico","indexId":"wsp2227","publicationYear":"1987","noYear":false,"title":"Water resources of the Zuni tribal lands, McKinley and Cibola Counties, New Mexico"},"id":1}],"supersededBy":{"id":2420,"text":"wsp2227 - 1987 - Water resources of the Zuni tribal lands, McKinley and Cibola Counties, New Mexico","indexId":"wsp2227","publicationYear":"1987","noYear":false,"title":"Water resources of the Zuni tribal lands, McKinley and Cibola Counties, New Mexico"},"lastModifiedDate":"2022-09-07T15:44:24.905824","indexId":"ofr821013","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-1013","title":"Water resources of the Zuni Tribal Lands, McKinley and Cibola counties, New Mexico","docAbstract":"<p>An evaluation of the water resources of the Zuni Tribal lands in west-central New Mexico was made to determine the yield, variability, and quality of water available to the Pueblo of Zuni. This study is needed to aid in orderly development of these resources.</p><p>Rocks of Permian to Quaternary age supply stock, irrigation, and domestic water to the Zuni Indians. The Glorieta Sandstone and San Andres Limestone (Glorieta-San Andres aquifer) of Permian age and sandstones in the Chinle Formation of Triassic age provide most of this water supply.</p><p>Water in the Glorieta-San Andres aquifer is confined by minimal-permeability shales and is transmitted through the aquifer along interconnected solution channels and fractures. Water-level and water-quality information indicate greater hydraulic conductivities along the southern boundaries of Zuni Tribal lands.</p><p>Well yields from the Glorieta-San Andres aquifer are as much as 150 gallons per minute and aquifer transmissivity ranges from 30 to 1,400 feet squared per day. Long-term, water-level declines of as much as 29 feet have been measured near pumping centers at Black Rock. Multiple-well aquifer tests are needed to further define aquifer properties (storage, transmissivity, and leakage from confining units) and the effects of well design on well yields. Dissolved-solids concentrations in water from the aquifer ranged from 331 to 1,068 milligrams per liter. Calcium and sulfate are the predominant ions.</p><p>Water in sandstones of the Chinle Formation is confined by adjacent shales and is transmitted along interconnected fractures. Well yields range from 5 to 125 gallons per minute and aquifer transmissivity ranges from 40 to 1,400 feet squared per day. Water-level declines of as much as 27 feet have been measured near Zuni Village. Dissolved-solids concentrations in water from the aquifer ranged from 215 to 1,980 milligrams per liter. Sodium and bicarbonate are the predominant ions.</p><p>Other sources of ground water are used primarily for livestock watering by means of windmills, with the exception of buried alluvial channel deposits along the Rio Pescado. These deposits provide domestic and irrigation water through springs and wells to Pescado and Black Rock.</p><p>The Bidahochi Formation of Miocene and Pliocene age could potentially provide an additional supply of water chemically suitable for most uses. Seismic-reflection techniques are being used to locate buried channels eroded in the rocks underlying the Bidahochi Formation. These buried channels may contain thicker sections of saturated sands and gravels that could be developed for stock and domestic use.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr821013","collaboration":"Prepared in cooperation with the Pueblo of Zuni","usgsCitation":"Orr, B.R., 1983, Water resources of the Zuni Tribal Lands, McKinley and Cibola counties, New Mexico: U.S. Geological Survey Open-File Report 82-1013, Report: 179 p.; 2 Plates: 23.21 x 19.52 inches and 20.83 x 30.61 inches, https://doi.org/10.3133/ofr821013.","productDescription":"Report: 179 p.; 2 Plates: 23.21 x 19.52 inches and 20.83 x 30.61 inches","costCenters":[],"links":[{"id":406315,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1013/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":406314,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1013/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":406313,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1013/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144134,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1013/report-thumb.jpg"}],"country":"United States","state":"New Mexico","county":"Cibola County, McKinley County","otherGeospatial":"Zuni Tribal Lands","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.061279296875,\n              34.134541681937364\n            ],\n            [\n              -107.0068359375,\n              34.134541681937364\n            ],\n            [\n              -107.0068359375,\n              35.96022296929667\n            ],\n            [\n              -109.061279296875,\n              35.96022296929667\n            ],\n            [\n              -109.061279296875,\n              34.134541681937364\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f03be","contributors":{"authors":[{"text":"Orr, Brennon R.","contributorId":18747,"corporation":false,"usgs":true,"family":"Orr","given":"Brennon","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161599,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10461,"text":"ofr8336 - 1983 - Gain-loss study along two streams in the upper Sabine River basin, Texas; August-September 1981","interactions":[],"lastModifiedDate":"2016-08-11T15:30:58","indexId":"ofr8336","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-36","title":"Gain-loss study along two streams in the upper Sabine River basin, Texas; August-September 1981","docAbstract":"<p>A gain-loss study was made August-September 1981 along the upper Sabine River from Lake Tawakoni to Farm Road 2517 near Carthage and along Lake Fork Creek from Lake Fork Reservoir to its junction (mouth) with the Sabine River. The hydrologic data collected during the gain-loss study indicated that during periods of low flow on the Sabine River, at least as much water as is released from Lake Tawakoni and from Lake Fork Reservoir will be available downstream at Farm Road 14 near Big Sandy and at Farm Road 2517 near Carthage. Gains from bank seepage and small tributary inflows compensate for losses due to evaporation, evapotranspiration, and loss of water into the alluvial aquifer.</p>\n<p>Dissolved solids concentrations in the Sabine River, estimated from specific conductance, increased from about 120 milligrams per liter near the upstream end of the reach to about 400 milligrams per liter near the downstream end of the reach. Water with these concentrations of dissolved solids generally is suitable for most uses.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8336","usgsCitation":"Myers, D.R., 1983, Gain-loss study along two streams in the upper Sabine River basin, Texas; August-September 1981: U.S. Geological Survey Open-File Report 83-36, iv, 11 p., https://doi.org/10.3133/ofr8336.","productDescription":"iv, 11 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":38331,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0036/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145033,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0036/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1451","contributors":{"authors":[{"text":"Myers, Dennis R.","contributorId":57860,"corporation":false,"usgs":true,"family":"Myers","given":"Dennis","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161443,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28741,"text":"wri824071 - 1983 - Selected hydrologic characteristics of the South Platte River in the vicinity of the proposed Narrows Reservoir near Fort Morgan, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:48","indexId":"wri824071","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4071","title":"Selected hydrologic characteristics of the South Platte River in the vicinity of the proposed Narrows Reservoir near Fort Morgan, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824071","usgsCitation":"Minges, D., 1983, Selected hydrologic characteristics of the South Platte River in the vicinity of the proposed Narrows Reservoir near Fort Morgan, Colorado: U.S. Geological Survey Water-Resources Investigations Report 82-4071, iv, 25 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824071.","productDescription":"iv, 25 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159402,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4071/report-thumb.jpg"},{"id":57593,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4071/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8c07","contributors":{"authors":[{"text":"Minges, D.R.","contributorId":31387,"corporation":false,"usgs":true,"family":"Minges","given":"D.R.","affiliations":[],"preferred":false,"id":200321,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26599,"text":"wri834110 - 1983 - Improvement of flood-frequency estimates for selected small watersheds in eastern Kansas using a rainfall-runoff model","interactions":[],"lastModifiedDate":"2012-02-02T00:08:22","indexId":"wri834110","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4110","title":"Improvement of flood-frequency estimates for selected small watersheds in eastern Kansas using a rainfall-runoff model","docAbstract":"The U.S. Geological Survey rainfall-runoff model was used to estimate model parameters for 13 small watersheds in eastern Kansas with drainage areas of less than 11 square miles. Model parameters and rainfall data from three long-term rainfall stations were used in the model to synthesize long-term records of simulated annual peak discharge, which were fitted to a log-Pearson Type III distribution. Final estimates of T-year floods, which were computed by combining weighted estimates of the synthesized and observed T-floods, represent the most reliable estimates based on observed and long-term synthesized records of peak discharges. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834110","usgsCitation":"Clement, R., 1983, Improvement of flood-frequency estimates for selected small watersheds in eastern Kansas using a rainfall-runoff model: U.S. Geological Survey Water-Resources Investigations Report 83-4110, iv, 26 p. :ill., map ;28 cm., https://doi.org/10.3133/wri834110.","productDescription":"iv, 26 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":123363,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4110/report-thumb.jpg"},{"id":55465,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4110/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fde4b07f02db5f5cdc","contributors":{"authors":[{"text":"Clement, R.W.","contributorId":11247,"corporation":false,"usgs":true,"family":"Clement","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":196685,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28692,"text":"wri834016 - 1983 - Geohydrology of the proposed Waste Isolation Pilot Plant site, Los Medanos area, southeastern New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:46","indexId":"wri834016","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4016","title":"Geohydrology of the proposed Waste Isolation Pilot Plant site, Los Medanos area, southeastern New Mexico","docAbstract":"Geohydrologic data have been collected in the Los Medanos area at the U.S. Department of Energy 's proposed Waste Isolation Pilot Plant (WIPP) site in southeastern New Mexico since 1975 as part of an intensive study evaluating the feasibility of storing defense-associated nuclear wastes within the bedded salt of the Salado Formation of Permian age. Drilling and hydrologic testing have identified three principal water-producing zones above the salt, including the Rustler-Salado Formational contact and the Culebra and Magenta Dolomite Members of the Permian Rustler Formation. Below the bedded salt there is another water-bearing zone, the channel sandstones of the Bell Canyon formation of the Permian Delaware Mountain Group. Most data collected from 33 hydrologic test holes indicate that the water-bearing zones are characterized by low transmissivities and contain slightly saline to briny water. Data collected from drill-stem tests in the Bell Canyon Formation indicate the channel sandstones have hydraulic conductivities ranging from 0.02 to 0.36 feet per day grade vertically and laterally into siltstones and shales of very low permeability. The Rustler Formation contains the principal water-producing zones identified at the WIPP site. The Rustler-Salado formational contact has the least transmissivity, ranging from 0.00003 to 0.003 feet squared per day. The Culebra Dolomite is the most productive unit at the WIPP site with transmissivities ranging from 0.001 to 73 feet squared per day; the greater values result from fracturing in the dolomite created by dissolution of underlying halite. Minute vertical permeabilities prevent movement of water between hydrologic units. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834016","usgsCitation":"Mercer, J.W., 1983, Geohydrology of the proposed Waste Isolation Pilot Plant site, Los Medanos area, southeastern New Mexico: U.S. Geological Survey Water-Resources Investigations Report 83-4016, viii, 121 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834016.","productDescription":"viii, 121 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119035,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4016/report-thumb.jpg"},{"id":57535,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4016/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8824","contributors":{"authors":[{"text":"Mercer, Jerry W.","contributorId":32534,"corporation":false,"usgs":true,"family":"Mercer","given":"Jerry","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":200242,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43846,"text":"ofr83107 - 1983 - Land use and land cover and associated maps for Williams, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:11:04","indexId":"ofr83107","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-107","title":"Land use and land cover and associated maps for Williams, Arizona","language":"ENGLISH","doi":"10.3133/ofr83107","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Land use and land cover and associated maps for Williams, Arizona: U.S. Geological Survey Open-File Report 83-107, maps :photocopy ;45 x 67 cm., https://doi.org/10.3133/ofr83107.","productDescription":"maps :photocopy ;45 x 67 cm.","costCenters":[],"links":[{"id":168053,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae676","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531396,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13206,"text":"ofr83221 - 1983 - Hydrology of area 47, Northern Great Plains and Rocky Mountain Coal Provinces, North Dakota, South Dakota, and Montana","interactions":[],"lastModifiedDate":"2018-02-16T14:27:38","indexId":"ofr83221","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-221","title":"Hydrology of area 47, Northern Great Plains and Rocky Mountain Coal Provinces, North Dakota, South Dakota, and Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83221","usgsCitation":"Crosby, O., and Klausing, R., 1983, Hydrology of area 47, Northern Great Plains and Rocky Mountain Coal Provinces, North Dakota, South Dakota, and Montana: U.S. Geological Survey Open-File Report 83-221, 150 p., https://doi.org/10.3133/ofr83221.","productDescription":"150 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":95115,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0221/report.pdf","size":"34188","linkFileType":{"id":1,"text":"pdf"}},{"id":146750,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0221/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601ff8","contributors":{"authors":[{"text":"Crosby, O.A.","contributorId":61047,"corporation":false,"usgs":true,"family":"Crosby","given":"O.A.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":167403,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klausing, R.L.","contributorId":73205,"corporation":false,"usgs":true,"family":"Klausing","given":"R.L.","affiliations":[],"preferred":false,"id":167404,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10321,"text":"ofr82771 - 1983 - Filling of Spirit Lake, Washington, May 18, 1980 to July 31, 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:06:22","indexId":"ofr82771","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-771","title":"Filling of Spirit Lake, Washington, May 18, 1980 to July 31, 1982","docAbstract":"The rockslide/debris avalanche from the north face of Mount St. Helens that precipitated the volcano 's eruption on May 18, 1980 , blocked outflow from Spirit Lake, Washington. There has been no surface outflow since that time. From May 21, 1980, when the first measurement of lake level was made, to August 1, 1982, Spirit Lake has increased its volume from 122,800 acre-ft to 264 ,000 acre-ft, an increase of 115%. Lake level has risen approximately 54 ft during this period. Hydrologic and geologic properties of the debris dam are unknown, but the materials obviously are easily erodible. Steep walled channels up to 60 ft deep have been eroded into the dam and are extending headward toward the lowest points on the crest. In addition, it appears that the lower areas on the crest of the dam are underlain by ash cloud deposits of low density. Indications are that the debris dam could fail by headward erosion, by overtopping with rapid downcutting, or by ' piping ' and rapid erosion. Each type of failure can produce rapid release of stored lake water with very high discharge rates. On the basis of observed filling rates of the lake over the last two yr and precipitation records at four long-term, low altitude National Weather Service stations, it is expected that normal precipitation will fill the lake to the dam crest in December 1985. This estimate is also based on the assumption that loss of water from the lake by seepage continues at the present rate until December 1985. With normal precipitation during the coming yr (August 1982 through July 1983 the lake will fill to a level 50 ft below the lowest existing point on the crest of the debris dam, which is at 3,532 ft altitude. If precipitation exceeds normal by 1.5 times during this coming year, the lake level will be 40 ft below the 3 ,532-ft crest of the debris dam by the end of July 1983. This same lake level can be reached by the end of March 1983 if precipitation from October through March is twice the winter mean. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82771","usgsCitation":"Meyer, W., and Carpenter, P.J., 1983, Filling of Spirit Lake, Washington, May 18, 1980 to July 31, 1982: U.S. Geological Survey Open-File Report 82-771, iv, 23 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82771.","productDescription":"iv, 23 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":143633,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0771/report-thumb.jpg"},{"id":38172,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0771/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f481e","contributors":{"authors":[{"text":"Meyer, William","contributorId":87538,"corporation":false,"usgs":true,"family":"Meyer","given":"William","affiliations":[],"preferred":false,"id":161195,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carpenter, Philip J.","contributorId":85034,"corporation":false,"usgs":true,"family":"Carpenter","given":"Philip","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":161194,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10272,"text":"ofr83286 - 1983 - A hydrogeochemical survey in east-central Nevada","interactions":[],"lastModifiedDate":"2022-07-22T21:20:44.950179","indexId":"ofr83286","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-286","title":"A hydrogeochemical survey in east-central Nevada","docAbstract":"A hydrogeochemical survey utilizing waters from springs and wells was conducted in east-central Nevada. None of the trace elements commonly associated with mineralization were found to be highly anomalous in the study area. Slightly anomalous values for some elements were found in the southern valleys of the study area and in a few scattered areas that contained old mines. Data from this study revealed no new areas of significant mineralization.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83286","usgsCitation":"McHugh, J., Miller, W.R., and Ficklin, W.H., 1983, A hydrogeochemical survey in east-central Nevada: U.S. Geological Survey Open-File Report 83-286, i, 28 p., https://doi.org/10.3133/ofr83286.","productDescription":"i, 28 p.","costCenters":[],"links":[{"id":404396,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13966.htm","linkFileType":{"id":5,"text":"html"}},{"id":38129,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0286/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142595,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0286/report-thumb.jpg"}],"country":"United States","state":"Nevada","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.49,\n              37.874\n            ],\n            [\n              -114,\n              37.874\n            ],\n            [\n              -114,\n              38.5\n            ],\n            [\n              -114.49,\n              38.5\n            ],\n            [\n              -114.49,\n              37.874\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae468","contributors":{"authors":[{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":161115,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, W. Roger","contributorId":60191,"corporation":false,"usgs":true,"family":"Miller","given":"W.","email":"","middleInitial":"Roger","affiliations":[],"preferred":false,"id":161114,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ficklin, Walter H.","contributorId":52565,"corporation":false,"usgs":true,"family":"Ficklin","given":"Walter","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":161113,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":48844,"text":"ofr83941 - 1983 - Summary of surface-water-quality data, Interior Coal Province, eastern region, October 1978 to September 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:10:05","indexId":"ofr83941","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-941","title":"Summary of surface-water-quality data, Interior Coal Province, eastern region, October 1978 to September 1982","language":"ENGLISH","doi":"10.3133/ofr83941","usgsCitation":"Hoffman, S.A., and Wetzel, K.L., 1983, Summary of surface-water-quality data, Interior Coal Province, eastern region, October 1978 to September 1982: U.S. Geological Survey Open-File Report 83-941, 20 p., https://doi.org/10.3133/ofr83941.","productDescription":"20 p.","costCenters":[],"links":[{"id":162843,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698979","contributors":{"authors":[{"text":"Hoffman, S. A.","contributorId":19575,"corporation":false,"usgs":true,"family":"Hoffman","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":238409,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wetzel, K. L.","contributorId":14418,"corporation":false,"usgs":true,"family":"Wetzel","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":238408,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3220,"text":"wsp2185E - 1983 - Water quality of the Yadkin-Pee Dee River system, North Carolina— Variability, pollution loads, and long-term trends","interactions":[],"lastModifiedDate":"2021-11-16T22:48:29.397725","indexId":"wsp2185E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2185","chapter":"E","title":"Water quality of the Yadkin-Pee Dee River system, North Carolina— Variability, pollution loads, and long-term trends","docAbstract":"Interpretation of water quality data collected by the U.S. Geological Survey and the North Carolina Department of Natural Resources and Community Development, for the Yadkin-Pee Dee River system, has identified water quality variations, characterized the current condition of the river in reference to water quality standards, estimated the degree of pollution caused by man, and evaluated long-term trends in concentrations of major dissolved constituents. Three stations, Yadkin River at Yadkin College (02116500), Rocky River near Norwood (02126000), and Pee Dee River near Rockingham (02129000) have been sampled over different periods of time beginning in 1906. Overall, the ambient water quality of the Yadkin-Pee Dee River system is satisfactory for most water uses. Iron and manganese concentrations are often above desirable levels, but they are not unusually high in comparison to other North Carolina streams. Lead concentrations also periodically rise above the recommended criterion for domestic water use. Mercury concentrations frequently exceed, and pH levels fall below, the recommended criteria for protection of aquatic life. Dissolved oxygen levels, while generally good, are lowest at the Pee Dee near Rockingham, due to the station 's location not far downstream from a lake. Suspended sediment is the most significant water quality problem of the Yadkin-Pee Dee River. The major cation in the river is sodium and the major anions are bicarbonate and carbonate. Eutrophication is currently a problem in the Yadkin-Pee Dee, particularly in High Rock Lake. An estimated nutrient and sediment balance of the system indicates that lakes along the Yadkin-Pee Dee River serve as a sink for sediment, ammonia, and phosphorus. Pollution makes up approximately 59% of the total dissolved solids load of the Yadkin River at Yadkin College, 43% for the Rocky River near Norwood, and 29% for the Pee Dee River near Rockingham. Statistically significant trends show a pattern of increasing concentration of most dissolved constituents over time, with a leveling off and decline in the middle to late 1970's.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Water quality of North Carolina streams","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2185E","usgsCitation":"Harned, D., and Meyer, D., 1983, Water quality of the Yadkin-Pee Dee River system, North Carolina— Variability, pollution loads, and long-term trends: U.S. Geological Survey Water Supply Paper 2185, vii, 71 p., https://doi.org/10.3133/wsp2185E.","productDescription":"vii, 71 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":391783,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25473.htm"},{"id":30213,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2185e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138939,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2185e/report-thumb.jpg"}],"country":"United States","state":"North Carolina","otherGeospatial":"Yadkin - Pee Dee River system","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.655,\n              34.807\n            ],\n            [\n              -79.683,\n              34.807\n            ],\n            [\n              -79.683,\n              36.583\n            ],\n            [\n              -81.655,\n              36.583\n            ],\n            [\n              -81.655,\n              34.807\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f08ea","contributors":{"authors":[{"text":"Harned, Douglas","contributorId":11195,"corporation":false,"usgs":true,"family":"Harned","given":"Douglas","affiliations":[],"preferred":false,"id":146460,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, Dann","contributorId":80256,"corporation":false,"usgs":true,"family":"Meyer","given":"Dann","email":"","affiliations":[],"preferred":false,"id":146461,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30142,"text":"wri834171 - 1983 - Geohydrologic data and test results from well J-13, Nevada Test Site, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:09:03","indexId":"wri834171","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4171","title":"Geohydrologic data and test results from well J-13, Nevada Test Site, Nye County, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834171","usgsCitation":"Thordarson, W., 1983, Geohydrologic data and test results from well J-13, Nevada Test Site, Nye County, Nevada: U.S. Geological Survey Water-Resources Investigations Report 83-4171, vi, 63 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834171.","productDescription":"vi, 63 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123154,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4171/report-thumb.jpg"},{"id":58954,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4171/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8f36","contributors":{"authors":[{"text":"Thordarson, William","contributorId":23539,"corporation":false,"usgs":true,"family":"Thordarson","given":"William","email":"","affiliations":[],"preferred":false,"id":202754,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18437,"text":"ofr83696 - 1983 - Long-range plans for hydrologic investigations in New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:07:25","indexId":"ofr83696","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-696","title":"Long-range plans for hydrologic investigations in New Mexico","docAbstract":"Objectives of the hydrologic-data-collection projects presented in this report include continuing to identify future data needs; conducting an analysis of the water-quality, ground-water, and surface-water observation networks; and entering all available current and historical hydrologic data into the U.S. Geological Survey Water Data Storage and Retrieval System (WATSTORE). Objectives of areal-appraisal studies include evaluating the water resources in the Gallup-Grants-Zuni-Acoma Sag area and on the eastern flank of the Sandi and Manzano Mountains in Bernalillo County. Potential projects for basin assessments include quantifying the ground-water/surface-water relationships on rivers with flows governed by compacts and an investigation of the water resources of the Estancia Basin. Projects that will assist in the evaluation of energy-related activities include describing the effects of resaturation of coal mines and of milling operations on the quality and quantity of ground and surface water. Activities that need to be undertaken to assist in addressing waste-disposal problems include the evaluation of the hydrologic factors influencing the feasibility of cleanup at the Albuquerque South Valley ' superfund ' site and the establishment of a monitoring network at the Waste Isolation Pilot Plant project near Carlsbad. Scientific methods that need to be developed include (1) the testing of analytical techniques for estimating site-specific conditions with the results of digital hydrologic models, and (2) the determination of the influence of recharge from ephemeral streams on alluvial aquifers. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83696","usgsCitation":"Case, H.L., and Welder, G.E., 1983, Long-range plans for hydrologic investigations in New Mexico: U.S. Geological Survey Open-File Report 83-696, iv, 29 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr83696.","productDescription":"iv, 29 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":151222,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0696/report-thumb.jpg"},{"id":47788,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0696/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db6352fb","contributors":{"authors":[{"text":"Case, H. L. III","contributorId":70435,"corporation":false,"usgs":true,"family":"Case","given":"H.","suffix":"III","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":179117,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Welder, G. E.","contributorId":100814,"corporation":false,"usgs":true,"family":"Welder","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":179118,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":47671,"text":"wri834058 - 1983 - Shallow ground water in the Boulder-Fort Collins-Greeley area, Front Range urban corridor, Colorado, 1975-77","interactions":[],"lastModifiedDate":"2022-12-05T21:04:03.995944","indexId":"wri834058","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4058","title":"Shallow ground water in the Boulder-Fort Collins-Greeley area, Front Range urban corridor, Colorado, 1975-77","docAbstract":"<p>Shallow ground water may limit the location of construction and excavation projects in parts of the Front Range Urban Corridor. A shallow water table occurs from 0 to 50 feet below the land surface principally in the alluvial deposits along the streams and rivers in the Boulder-Fort Collins-Greeley area. This shallow water table underlies approximately 400 square miles and is maintained by natural recharge within the South Platte River basin and by the infiltration of irrigation water that is diverted into the basin from streams and reservoirs in the Colorado and the Laramie River basins. Return flow from irrigation, which is mostly ground water, helps maintain the flow of the South Platte River and its tributaries. The report includes a map from which depth to water table and the direction of ground-water movement can be determined. The map, compiled on a topographic base, shows the areal extent of the saturated materials and the altitude and configuration of the ground-water surface. The water-table contour map was prepared using data from approximately 400 wells. Monitoring of shallow ground-water within the study area shows depths to water have changed only slightly over the last 20 years, except for some seasonal and drought-related fluctuations. Gradients, computed from ground-water measurements, range from 27.7 feet per mile in Lone Tree-Spring Creek valley to 10.3 feet per mile in the South Platte River valley. The shallow ground-water underflow from the major tributaries in the basin is about 29,000 acre-feet per year, and underflow calculated at a cross section near Kersey is about 12,000 acre-feet per year.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834058","usgsCitation":"Schneider, P.A., 1983, Shallow ground water in the Boulder-Fort Collins-Greeley area, Front Range urban corridor, Colorado, 1975-77: U.S. Geological Survey Water-Resources Investigations Report 83-4058, 1 Plate: 41.96 × 31.86 inches, https://doi.org/10.3133/wri834058.","productDescription":"1 Plate: 41.96 × 31.86 inches","costCenters":[],"links":[{"id":161788,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":410064,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35694.htm","linkFileType":{"id":5,"text":"html"}},{"id":84582,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4058/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","city":"Boulder, Fort Collins, Greeley","otherGeospatial":"Front Range urban corridor","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -105.46470339334677,\n              40.68848809489273\n            ],\n            [\n              -105.46470339334677,\n              39.92665986663209\n            ],\n            [\n              -104.58735150676397,\n              39.92665986663209\n            ],\n            [\n              -104.58735150676397,\n              40.68848809489273\n            ],\n            [\n              -105.46470339334677,\n              40.68848809489273\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f420a","contributors":{"authors":[{"text":"Schneider, Paul A. Jr.","contributorId":50183,"corporation":false,"usgs":true,"family":"Schneider","given":"Paul","suffix":"Jr.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":235982,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70110354,"text":"wdrIN821 - 1983 - Water resources data, Indiana, water year 1982","interactions":[],"lastModifiedDate":"2014-06-11T13:06:00","indexId":"wdrIN821","displayToPublicDate":"1984-01-01T10:18:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"IN-82-1","title":"Water resources data, Indiana, water year 1982","docAbstract":"Water resources data for the 1982 water year for Indiana consists of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs; and water levels in wells. This report contains discharge records for 176 gaging stations, stage and contents for 9 lakes and reservoirs, releases from 8 flood control reservoirs, water quality for 26 gaging stations, and water levels for 87 observation wells. Also included are 71 crest-stage partial-record stations. Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Indiana.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrIN821","collaboration":"Prepared in cooperation with the State of Indiana and with other agencies","usgsCitation":"Miller, R.L., Hoggatt, R., and Nell, G., 1983, Water resources data, Indiana, water year 1982: U.S. Geological Survey Water Data Report IN-82-1, xiv, 340 p., https://doi.org/10.3133/wdrIN821.","productDescription":"xiv, 340 p.","numberOfPages":"357","temporalStart":"1981-10-01","temporalEnd":"1982-09-30","costCenters":[],"links":[{"id":288332,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288331,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1982/in-82-1/report.pdf"}],"country":"United States","state":"Indiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.0979,37.7717 ], [ -88.0979,41.7607 ], [ -84.7847,41.7607 ], [ -84.7847,37.7717 ], [ -88.0979,37.7717 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"538052f2e4b0826cd5016aaa","contributors":{"authors":[{"text":"Miller, R. L.","contributorId":54178,"corporation":false,"usgs":true,"family":"Miller","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":494039,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoggatt, R.E.","contributorId":96751,"corporation":false,"usgs":true,"family":"Hoggatt","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":494040,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nell, G.E.","contributorId":45960,"corporation":false,"usgs":true,"family":"Nell","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":494038,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70006370,"text":"70006370 - 1983 - Chemical characteristics of waters in northern prairie wetlands","interactions":[],"lastModifiedDate":"2017-08-31T09:45:31","indexId":"70006370","displayToPublicDate":"1984-01-01T10:05:18","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3168,"text":"Proceedings of the North Dakota Academy of Science","active":true,"publicationSubtype":{"id":10}},"title":"Chemical characteristics of waters in northern prairie wetlands","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Proceedings of the North Dakota Academy of Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"conferenceTitle":"North Dakota Academy of Science","language":"English","publisher":"North Dakota Academy of Science","publisherLocation":"Grand Forks, ND","collaboration":"None","usgsCitation":"Adomaitis, V.A., Swanson, G., and Shoesmith, J., 1983, Chemical characteristics of waters in northern prairie wetlands: Proceedings of the North Dakota Academy of Science, v. 37.","productDescription":"1 p.","startPage":"61","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":286413,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Dakota","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.05,45.9351 ], [ -104.05,49.0007 ], [ -96.5545,49.0007 ], [ -96.5545,45.9351 ], [ -104.05,45.9351 ] ] ] } } ] }","volume":"37","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53558ffae4b0120853e8be80","contributors":{"editors":[{"text":"Johnson, A. William","contributorId":113124,"corporation":false,"usgs":true,"family":"Johnson","given":"A.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":508309,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Adomaitis, V. A.","contributorId":66198,"corporation":false,"usgs":true,"family":"Adomaitis","given":"V.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":354403,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swanson, G.A.","contributorId":49299,"corporation":false,"usgs":true,"family":"Swanson","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":354401,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shoesmith, J.A.","contributorId":58599,"corporation":false,"usgs":true,"family":"Shoesmith","given":"J.A.","affiliations":[],"preferred":false,"id":354402,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70170918,"text":"70170918 - 1983 - Status of water-resources projects in Minnesota, fiscal year 1983","interactions":[],"lastModifiedDate":"2018-03-12T12:14:07","indexId":"70170918","displayToPublicDate":"1983-12-31T14:30:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Status of water-resources projects in Minnesota, fiscal year 1983","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/70170918","usgsCitation":"Jannis, J.A., 1983, Status of water-resources projects in Minnesota, fiscal year 1983, 74 p., https://doi.org/10.3133/70170918.","productDescription":"74 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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,{"id":70231500,"text":"70231500 - 1983 - Uptake and transport of heavy metals by heated seawater: A summary of the experimental results","interactions":[],"lastModifiedDate":"2022-05-11T16:34:54.340017","indexId":"70231500","displayToPublicDate":"1983-12-31T11:30:50","publicationYear":"1983","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Uptake and transport of heavy metals by heated seawater: A summary of the experimental results","docAbstract":"<p><span>In general, the chemistry of seawater experimentally reacted with basalt is in accord with the observed chemistry of the 350°C vent waters from 21°N on the East Pacific Rise. Experiments at 350°C, 500 bar, and a water/rock ratio of ≤10 reproduce most of the major components in the vent waters, in particular the low Mg and SO</span><sub>4</sub><span>&nbsp;and high Si0</span><sub>2</sub><span>, Ca, and K. In comparison with the vent waters however the experimental fluids are deficient in H</span><sup>+</sup><span>&nbsp;and heavy metals. Experiments with natural and evolved seawater (Mg and SO</span><sub>4</sub><span>&nbsp;depleted) at ≥400 C and 500 bars or 375°C and ~375 bars under rock-dominated conditions more closely reproduce the vent-water chemistry.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Hydrothermal processes at seafloor spreading centers","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Springer Link","doi":"10.1007/978-1-4899-0402-7_9","usgsCitation":"Rosenbauer, R.J., and Bischoff, J.L., 1983, Uptake and transport of heavy metals by heated seawater: A summary of the experimental results, chap. <i>of</i> Hydrothermal processes at seafloor spreading centers, p. 177-197, https://doi.org/10.1007/978-1-4899-0402-7_9.","productDescription":"21 p.","startPage":"177","endPage":"197","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":400516,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Rosenbauer, Robert J. brosenbauer@usgs.gov","contributorId":204,"corporation":false,"usgs":true,"family":"Rosenbauer","given":"Robert","email":"brosenbauer@usgs.gov","middleInitial":"J.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":842791,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bischoff, James L. jbischoff@usgs.gov","contributorId":1389,"corporation":false,"usgs":true,"family":"Bischoff","given":"James","email":"jbischoff@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":842792,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011350,"text":"70011350 - 1983 - Plutonium speciation in water from Mono Lake, California","interactions":[],"lastModifiedDate":"2025-11-25T15:22:04.609349","indexId":"70011350","displayToPublicDate":"1983-12-23T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Plutonium speciation in water from Mono Lake, California","docAbstract":"The solubility of plutonium in Mono Lake water is enhanced by the presence of large concentrations of indigenous carbonate ions and moderate concentrations of fluoride ions. In spite of the complex chemical composition of this water, only a few ions govern the behavior of plutonium, as demonstrated by the fact that it was possible to duplicate plutonium speciation in a synthetic water containing only the principal components of Mono Lake water.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.222.4630.1323","issn":"00368075","usgsCitation":"Cleveland, J., Rees, T., and Nash, K., 1983, Plutonium speciation in water from Mono Lake, California: Science, v. 222, no. 4630, p. 1323-1325, https://doi.org/10.1126/science.222.4630.1323.","productDescription":"3 p.","startPage":"1323","endPage":"1325","costCenters":[],"links":[{"id":220973,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Mono Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -119.23547883490315,\n              38.11956391803898\n            ],\n            [\n              -119.23547883490315,\n              37.894106221864334\n            ],\n            [\n              -118.82146949863339,\n              37.894106221864334\n            ],\n            [\n              -118.82146949863339,\n              38.11956391803898\n            ],\n            [\n              -119.23547883490315,\n              38.11956391803898\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"222","issue":"4630","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7c9de4b0c8380cd79aa4","contributors":{"authors":[{"text":"Cleveland, J.M.","contributorId":66734,"corporation":false,"usgs":true,"family":"Cleveland","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":360892,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rees, T.F.","contributorId":26068,"corporation":false,"usgs":true,"family":"Rees","given":"T.F.","email":"","affiliations":[],"preferred":false,"id":360890,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nash, K.L.","contributorId":27191,"corporation":false,"usgs":true,"family":"Nash","given":"K.L.","affiliations":[],"preferred":false,"id":360891,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5223721,"text":"5223721 - 1983 - The significance of diurnal terrestrial emergency of green turtles (Chelonia mydas) in the Gal?pagos Archipelago","interactions":[],"lastModifiedDate":"2023-08-29T15:52:09.35813","indexId":"5223721","displayToPublicDate":"1983-12-01T12:19:13","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1045,"text":"Biotropica","active":true,"publicationSubtype":{"id":10}},"title":"The significance of diurnal terrestrial emergency of green turtles (Chelonia mydas) in the Gal?pagos Archipelago","docAbstract":"<p><span>The diurnal, nonreproductive emergence of green turtles Chelonia mydas in Galapagos apparently occurs throughout the year on several islands. Turtles on beaches have cloacal temperatures that exceed temperatures of adjacent coastal waters. Basking turtles are predominately females. We hypothesize that females bask to accelerate digestion and fat build-up, necessary antecedents to egg production in reproductive periods. Basking turtles show a trend to clump among available beaches. Such behavior may be a response to microclimatic differences between beaches, although such differences were not apparent to us. The occurrence of thermoregulatory behavior in marine turtles in Galapagos may be a response to the cool waters of the Humboldt Current.</span></p>","language":"English","publisher":"Wiley","doi":"10.2307/2387653","usgsCitation":"Snell, H., and Fritts, T.H., 1983, The significance of diurnal terrestrial emergency of green turtles (Chelonia mydas) in the Gal?pagos Archipelago: Biotropica, v. 15, no. 4, p. 285-291, https://doi.org/10.2307/2387653.","productDescription":"7 p.","startPage":"285","endPage":"291","numberOfPages":"7","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":199957,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Ecuador","otherGeospatial":"Galapagos Archipelago","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -92.30646174996666,\n              0.8730502262746143\n            ],\n            [\n              -92.30646174996666,\n              -1.5980348549939265\n            ],\n            [\n              -88.94125174801036,\n              -1.5980348549939265\n            ],\n            [\n              -88.94125174801036,\n              0.8730502262746143\n            ],\n            [\n              -92.30646174996666,\n              0.8730502262746143\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"15","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db636405","contributors":{"authors":[{"text":"Snell, H.L.","contributorId":49314,"corporation":false,"usgs":false,"family":"Snell","given":"H.L.","email":"","affiliations":[],"preferred":false,"id":339343,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fritts, Thomas H.","contributorId":77204,"corporation":false,"usgs":true,"family":"Fritts","given":"Thomas","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":339342,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70185620,"text":"70185620 - 1983 - Effect of retorted-oil shale leachate on a blue-green alga (Anabaena flos-aquae)","interactions":[],"lastModifiedDate":"2020-03-09T19:46:04","indexId":"70185620","displayToPublicDate":"1983-12-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1103,"text":"Bulletin of Environmental Contamination and Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Effect of retorted-oil shale leachate on a blue-green alga (Anabaena flos-aquae)","docAbstract":"<p>In the event of the development of the large oil shale reserves of Colorado, Utah, and Wyoming, one of the main environmental concerns will be disposal of retorted-oil shale which will be generated in greater volume than the original volume oI the mined oil shale. Investigators have found that leachates of retorted-oil shale are alkaline and have large concentrations of dissolved solids, molybdenum, boron, and fluoride (STOLLENWERK &amp; RUNNELS 1981). STOLLENWERK &amp; RUNNELS (1981) concluded that drainage from waste shale piles could have deleterious effects on the water quality of streams in northwestern Colorado. </p>","language":"English","publisher":"Springer","doi":"10.1007/BF01610091","usgsCitation":"McKnight, D.M., Pereira, W.E., Rostad, C.E., and Stiles, E.A., 1983, Effect of retorted-oil shale leachate on a blue-green alga (Anabaena flos-aquae): Bulletin of Environmental Contamination and Toxicology, v. 30, no. 1, p. 6-16, https://doi.org/10.1007/BF01610091.","productDescription":"11 p. ","startPage":"6","endPage":"16","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338321,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d6303fe4b05ec799131115","contributors":{"authors":[{"text":"McKnight, Diane M.","contributorId":59773,"corporation":false,"usgs":false,"family":"McKnight","given":"Diane","email":"","middleInitial":"M.","affiliations":[{"id":16833,"text":"INSTAAR, University of Colorado","active":true,"usgs":false}],"preferred":false,"id":686136,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pereira, Wilfred E.","contributorId":95552,"corporation":false,"usgs":true,"family":"Pereira","given":"Wilfred","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":686137,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rostad, Colleen E. cerostad@usgs.gov","contributorId":833,"corporation":false,"usgs":true,"family":"Rostad","given":"Colleen","email":"cerostad@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":686138,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stiles, Eric A.","contributorId":8449,"corporation":false,"usgs":true,"family":"Stiles","given":"Eric","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":686139,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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