{"pageNumber":"2123","pageRowStart":"53050","pageSize":"25","recordCount":68919,"records":[{"id":46848,"text":"ofr82633 - 1982 - Drainage divides, Massachusetts; Connecticut River lowlands and Chicopee River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:11:00","indexId":"ofr82633","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-633","title":"Drainage divides, Massachusetts; Connecticut River lowlands and Chicopee River basin","docAbstract":"Drainage boundaries for selected subbasins of the Connecticut River lowlands and Chicopee River basin in southern Franklin, eastern Hampshire, and western Worcester Counties, Massachusetts , are delineated on 18 topographic quadrangle maps at a scale of 1:24,000. Drainage basins are shown for all U.S. Geological Survey data-collection sites and for mouths of major rivers. Drainage basins are shown for the outlets of lakes or ponds and for streams where the drainage area is greater than 3 square miles. Successive sites along watercourses are indicated where the intervening area is at least 6 square miles on tributary streams or 10 square miles along the Chicopee River, or 20 square miles along the Connecticut River. (USGS)","language":"ENGLISH","doi":"10.3133/ofr82633","usgsCitation":"Krejmas, B.E., and Wandle, S.W., 1982, Drainage divides, Massachusetts; Connecticut River lowlands and Chicopee River basin: U.S. Geological Survey Open-File Report 82-633, 18 maps ;57 x 44 cm., https://doi.org/10.3133/ofr82633.","productDescription":"18 maps ;57 x 44 cm.","costCenters":[],"links":[{"id":168313,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635cbd","contributors":{"authors":[{"text":"Krejmas, Bruce E.","contributorId":102501,"corporation":false,"usgs":true,"family":"Krejmas","given":"Bruce","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":234190,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wandle, S. William Jr.","contributorId":99562,"corporation":false,"usgs":true,"family":"Wandle","given":"S.","suffix":"Jr.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":234189,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38604,"text":"pp1219 - 1982 - Digital classification of Landsat data for vegetation and land-cover mapping in the Blackfoot River watershed, southeastern Idaho","interactions":[],"lastModifiedDate":"2017-03-29T10:57:43","indexId":"pp1219","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1219","title":"Digital classification of Landsat data for vegetation and land-cover mapping in the Blackfoot River watershed, southeastern Idaho","docAbstract":"This paper documents the procedures, results, and final products of a digital analysis of Landsat data used to produce a vegetation and landcover map of the Blackfoot River watershed in southeastern Idaho. Resource classes were identified at two levels of detail: generalized Level I classes (for example, forest land and wetland) and detailed Levels II and III classes (for example, conifer forest, aspen, wet meadow, and riparian hardwoods). Training set statistics were derived using a modified clustering approach. Environmental stratification that separated uplands from lowlands improved discrimination between resource classes having similar spectral signatures. Digital classification was performed using a maximum likelihood algorithm. \r\n\r\nClassification accuracy was determined on a single-pixel basis from a random sample of 25-pixel blocks. These blocks were transferred to small-scale color-infrared aerial photographs, and the image area corresponding to each pixel was interpreted. Classification accuracy, expressed as percent agreement of digital classification and photo-interpretation results, was 83.0:t 2.1 percent (0.95 probability level) for generalized (Level I) classes and 52.2:t 2.8 percent (0.95 probability level) for detailed (Levels II and III) classes. \r\n\r\nAfter the classified images were geometrically corrected, two types of maps were produced of Level I and Levels II and III resource classes: color-coded maps at a 1:250,000 scale, and flatbed-plotter overlays at a 1:24,000 scale. The overlays are more useful because of their larger scale, familiar format to users, and compatibility with other types of topographic and thematic maps of the same scale.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1219","usgsCitation":"Pettinger, L.R., 1982, Digital classification of Landsat data for vegetation and land-cover mapping in the Blackfoot River watershed, southeastern Idaho: U.S. Geological Survey Professional Paper 1219, 33 p., https://doi.org/10.3133/pp1219.","productDescription":"33 p.","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":125044,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1219/report-thumb.jpg"},{"id":65423,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1219/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b463f","contributors":{"authors":[{"text":"Pettinger, L. R.","contributorId":85949,"corporation":false,"usgs":true,"family":"Pettinger","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":220152,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18183,"text":"ofr82575 - 1982 - Water quality of the tidal Potomac River and Estuary; hydrologic data report, 1981 water year, with a section on collection and analysis of chlorophyll-a","interactions":[],"lastModifiedDate":"2012-02-02T00:07:19","indexId":"ofr82575","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-575","title":"Water quality of the tidal Potomac River and Estuary; hydrologic data report, 1981 water year, with a section on collection and analysis of chlorophyll-a","docAbstract":"This report contains data on the physical and chemical properties measured in the Tidal Potomac River and Estuary during the 1981 water year. Data were collected at least weekly at five stations, and periodically at 15 stations and at two other stations near the mouth of the Potomac River in Chesapeake Bay. Each of the five stations represent a cross section at which the transport of selected dissolved and suspended materials can be computed. The remaining 17 stations are locations at which data were collected for special studies of selected phenomena, such as salt water migration and dissolved oxygen dynamics. Samples were routinely analyzed for chlorophyll-a, nitrogen, pheophytin, phosphorus, silica and suspended sediment. Additional samples were analyzed for adenosine triphosphate, algal growth potential, alkalinity, calcium, chloride, dissolved-solids residue, fluoride, iron, manganese, magnesium, nitrifying bacteria, organic carbon, potassium, seston, sodium, and sulfate. In addition, in-situ measurements of dissolved oxygen, specific conductance, pH, temperature, solar radiation, and secchi disk transparency were made. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82575","usgsCitation":"Blanchard, S.F., Coupe, R.H., and Woodward, J.C., 1982, Water quality of the tidal Potomac River and Estuary; hydrologic data report, 1981 water year, with a section on collection and analysis of chlorophyll-a: U.S. Geological Survey Open-File Report 82-575, ii, 304 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82575.","productDescription":"ii, 304 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":150310,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0575/report-thumb.jpg"},{"id":47547,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0575/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65db31","contributors":{"authors":[{"text":"Blanchard, Stephen F.","contributorId":54966,"corporation":false,"usgs":true,"family":"Blanchard","given":"Stephen","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":178669,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coupe, Richard H. 0000-0001-8679-1015 rhcoupe@usgs.gov","orcid":"https://orcid.org/0000-0001-8679-1015","contributorId":551,"corporation":false,"usgs":true,"family":"Coupe","given":"Richard","email":"rhcoupe@usgs.gov","middleInitial":"H.","affiliations":[{"id":394,"text":"Mississippi Water Science Center","active":true,"usgs":true}],"preferred":true,"id":178668,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Woodward, Joan C.","contributorId":91127,"corporation":false,"usgs":true,"family":"Woodward","given":"Joan","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":178670,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2588,"text":"wsp2077 - 1982 - Ground water in the Piedmont upland of central Maryland","interactions":[],"lastModifiedDate":"2012-02-02T00:05:20","indexId":"wsp2077","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"2077","title":"Ground water in the Piedmont upland of central Maryland","docAbstract":"This report, describing ground-water occurrence in a 130-square-mile area of the central Maryland Piedmont, was originally designed for use by the U.S. Environmental Protection Agency in replying to a request for designation of the aquifers to be the sole or principal source of ground water. However, the information contained in the report is pertinent to other crystalline-rock areas as well. \r\n\r\nThe study area is underlain chiefly by crystalline rocks and partly by unaltered sandstones and siltstones. \r\n\r\nThe ground water is derived from local precipitation and generally occurs under water-table conditions. Its movement is restricted by the lack of interconnected openings, and most ground water occurs within 300 feet of the land surface. Hydrographs indicate no long-term change in ground-water storage. \r\n\r\nA few wells yield more than 100 gallons per minute, but about 70 percent of 286 inventoried wells yield 10 gallons per minute or less; most specific capacities are less than 1.0 gallon per minute per foot. \r\n\r\nThe ground-water quality is generally satisfactory without treatment, and there are no known widespread pollution problems. \r\n\r\nEstimated daily figures on ground-water use are as follows: 780,000 gallons for domestic purposes; 55,000, for commercial purposes; and 160,000, for public supply. \r\n\r\nAlthough part of the area is served by an existing surface-water supply and could be served by possible extension of it and of other public-supply water mains, much of the rural population is dependent on the ground water available from private wells tapping the single aquifer that underlies any given location. Neither the ground-water conditions nor this dependence on individual wells is unique to the study area, but, rather, applies to the entire Piedmont province.","language":"ENGLISH","publisher":"U.S. G.P.O. :\r\nfor sale by the Supt. of Docs., U.S. G.P.O.,","doi":"10.3133/wsp2077","usgsCitation":"Richardson, C.A., 1982, Ground water in the Piedmont upland of central Maryland: U.S. Geological Survey Water Supply Paper 2077, iv, 42 p. :ill., maps ;23 cm., https://doi.org/10.3133/wsp2077.","productDescription":"iv, 42 p. :ill., maps ;23 cm.","costCenters":[],"links":[{"id":94721,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2077/report.pdf","size":"3372","linkFileType":{"id":1,"text":"pdf"}},{"id":137574,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2077/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d908","contributors":{"authors":[{"text":"Richardson, Claire A.","contributorId":33299,"corporation":false,"usgs":true,"family":"Richardson","given":"Claire","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":145449,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46276,"text":"ofr811357 - 1982 - Leasable mineral and waterpower land classification map of the Soda Springs 30' x 1° quadrangle, Idaho and Wyoming","interactions":[],"lastModifiedDate":"2021-09-21T18:21:19.199465","indexId":"ofr811357","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-1357","title":"Leasable mineral and waterpower land classification map of the Soda Springs 30' x 1° quadrangle, Idaho and Wyoming","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811357","usgsCitation":"DeCicco, D., 1982, Leasable mineral and waterpower land classification map of the Soda Springs 30' x 1° quadrangle, Idaho and Wyoming: U.S. Geological Survey Open-File Report 81-1357, 1 Plate: 39.01 × 28.21 inches, https://doi.org/10.3133/ofr811357.","productDescription":"1 Plate: 39.01 × 28.21 inches","costCenters":[],"links":[{"id":389556,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11941.htm"},{"id":83256,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1357/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":170651,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Idaho, Wyoming","otherGeospatial":"Soda Springs 30' x 1° quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.0,\n              42.5\n            ],\n            [\n              -111,\n              42.5\n            ],\n            [\n              -111,\n              43\n            ],\n            [\n              -112.0,\n              43\n            ],\n            [\n              -112.0,\n              42.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8653","contributors":{"authors":[{"text":"DeCicco, Donald A.","contributorId":84416,"corporation":false,"usgs":true,"family":"DeCicco","given":"Donald A.","affiliations":[],"preferred":false,"id":232997,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28353,"text":"wri824006 - 1982 - Thermal springs in the Boise River basin, south-central Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:08:35","indexId":"wri824006","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4006","title":"Thermal springs in the Boise River basin, south-central Idaho","docAbstract":"The Boise River Basin, characterized by steep, rugged mountains and narrow river valleys, drains an area of about 2,680 square miles in south-central Idaho. Granitic rocks of the Idaho batholith predominate in the basin. Temperature of waters from thermal springs in the basin range from 33 degrees to 87 degrees Celsius, are sodium carbonate type and are slightly alkaline. Dissolved-solids concentrations are less than 280 milligrams per liter. Estimated reservoir temperatures determined by the silica and sodium-potassium-calcium geothermometers range from 50 degrees to 98 degrees Celsius. Tritium concentrations in sampled thermal springs are near zero and indicate these waters were recharged prior to 1954. Stable-isotope data are not conclusive insofar as indicating a source area of recharge for the thermal springs in the basin. Thermal springs discharged at least 4,900 acre-feet of water in 1981, and the associated convective heat flux is 11,000,000 calories per second. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri824006","usgsCitation":"Lewis, R., and Young, H., 1982, Thermal springs in the Boise River basin, south-central Idaho: U.S. Geological Survey Water-Resources Investigations Report 82-4006, iii, 28 p. :ill., map ;28 cm., https://doi.org/10.3133/wri824006.","productDescription":"iii, 28 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":158330,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4006/report-thumb.jpg"},{"id":57158,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4006/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a55e4b07f02db62c686","contributors":{"authors":[{"text":"Lewis, R.E.","contributorId":31735,"corporation":false,"usgs":true,"family":"Lewis","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":199649,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Young, H.W.","contributorId":68278,"corporation":false,"usgs":true,"family":"Young","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":199650,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7614,"text":"ofr82267 - 1982 - Water-resources investigations of the U.S. Geological Survey in New Mexico, fiscal year 1980","interactions":[],"lastModifiedDate":"2012-02-02T00:05:58","indexId":"ofr82267","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-267","title":"Water-resources investigations of the U.S. Geological Survey in New Mexico, fiscal year 1980","docAbstract":"This is the third in a series of annual reports in which the program of the New Mexico District, U.S. Geological Survey, Water Resources Division, is summarized. This report, which is for fiscal year 1980, may be of use to cooperating agencies and to the users of water data in that it summarizes and gives the status of the basic data-collection program and all current studies of the Water Resources Division in New Mexico. The New Mexico District, along with other Federal and State agencies, shares in the responsibility for the appraisal of the quantity, quality, and distribution of surface- and ground-water resources of the State of New Mexico. During fiscal year 1980, the District had 28 active projects, had released 24 reports, and had answered hundreds of requests for water-related information. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82267","usgsCitation":"White, R., 1982, Water-resources investigations of the U.S. Geological Survey in New Mexico, fiscal year 1980: U.S. Geological Survey Open-File Report 82-267, v, 41 p. :maps ;28 cm., https://doi.org/10.3133/ofr82267.","productDescription":"v, 41 p. :maps ;28 cm.","costCenters":[],"links":[{"id":140090,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0267/report-thumb.jpg"},{"id":35103,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0267/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9c5f","contributors":{"authors":[{"text":"White, R.R.","contributorId":52568,"corporation":false,"usgs":true,"family":"White","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":156304,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7709,"text":"ofr821051 - 1982 - Effects of processed oil shale on the element content of Atriplex cancescens","interactions":[],"lastModifiedDate":"2012-02-02T00:06:08","indexId":"ofr821051","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-1051","title":"Effects of processed oil shale on the element content of Atriplex cancescens","docAbstract":"Samples of four-wing saltbush were collected from the Colorado State University Intensive Oil Shale Revegetation Study Site test plots in the Piceance basin, Colorado. The test plots were constructed to evaluate the effects of processed oil shale geochemistry on plant growth using various thicknesses of soil cover over the processed shale and/or over a gravel barrier between the shale and soil. Generally, the thicker the soil cover, the less the influence of the shale geochemistry on the element concentrations in the plants. Concentrations of 20 elements were larger in the ash of four-wing saltbush growing on the plot with the gravel barrier (between the soil and processed shale) when compared to the sample from the control plot. A greater water content in the soil in this plot has been reported, and the interaction between the increased, percolating water and shale may have increased the availability of these elements for plant uptake. Concentrations of boron, copper, fluorine, lithium, molybdenum, selenium, silicon, and zinc were larger in the samples grown over processed shale, compared to those from the control plot, and concentrations for barium, calcium, lanthanum, niobium, phosphorus, and strontium were smaller. \r\n\r\nConcentrations for arsenic, boron, fluorine, molybdenum, and selenium-- considered to be potential toxic contaminants--were similar to results reported in the literature for vegetation from the test plots. The copper-to-molybdenum ratios in three of the four samples of four-wing saltbush growing over the processed shale were below the ratio of 2:1, which is judged detrimental to ruminants, particularly cattle. Boron concentrations averaged 140 ppm, well above the phytotoxicity level for most plant species. Arsenic, fluorine, and selenium concentrations were below toxic levels, and thus should not present any problem for revegetation or forage use at this time.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821051","usgsCitation":"Anderson, B., 1982, Effects of processed oil shale on the element content of Atriplex cancescens: U.S. Geological Survey Open-File Report 82-1051, 18 p., ill., map ;28 cm., https://doi.org/10.3133/ofr821051.","productDescription":"18 p., ill., map ;28 cm.","costCenters":[],"links":[{"id":141578,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1051/report-thumb.jpg"},{"id":35173,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1051/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cfe4b07f02db5460a4","contributors":{"authors":[{"text":"Anderson, B.M.","contributorId":69552,"corporation":false,"usgs":true,"family":"Anderson","given":"B.M.","email":"","affiliations":[],"preferred":false,"id":156479,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41692,"text":"ofr82661 - 1982 - Aeromagnetic map of parts of the Okanogan and Ritzville 1° x 2° quadrangles, Washington","interactions":[],"lastModifiedDate":"2021-12-06T20:04:11.328164","indexId":"ofr82661","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-661","title":"Aeromagnetic map of parts of the Okanogan and Ritzville 1° x 2° quadrangles, Washington","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82661","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Aeromagnetic map of parts of the Okanogan and Ritzville 1° x 2° quadrangles, Washington: U.S. Geological Survey Open-File Report 82-661, 1 Plate: 25.65 × 23.78 inches, https://doi.org/10.3133/ofr82661.","productDescription":"1 Plate: 25.65 × 23.78 inches","costCenters":[],"links":[{"id":173678,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79412,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0661/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392512,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13795.htm"}],"country":"United States","state":"Washington","otherGeospatial":"Okanogan and Ritzville 1° x 2° quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120,\n              47.75\n            ],\n            [\n              -119,\n              47.75\n            ],\n            [\n              -119,\n              48.25\n            ],\n            [\n              -120,\n              48.25\n            ],\n            [\n              -120,\n              47.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697535","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":530571,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10785,"text":"ofr8289 - 1982 - Specification for procurement of water-level sensing instrumentation, specification number HIF-I-1","interactions":[],"lastModifiedDate":"2012-02-02T00:06:34","indexId":"ofr8289","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-89","title":"Specification for procurement of water-level sensing instrumentation, specification number HIF-I-1","docAbstract":"This specification is to communicate to instrument manufacturers the U.S. Geological Survey 's requirements. It covers systems for sensing the elevation of the water surface on open channels, rivers, lakes, reservoirs, storm-sewer pipes, and observation wells at Survey data-collection sites. The signal output (mechanical or electrical) must meet the signal input requirements of analog to digital and digital input recorders in use by the Survey. A classification of stage-sensing systems by common characteristics is used to aid Survey people making system selections. These characteristics are (1) system type (contact or noncontact), (2) sensor type and sensing distance, (3) accuracy, (4) range, (5) power requirements, (6) system size and weight, and (7) data output signal. Acceptable system requirements cover system configurations, signal outputs, materials, operation manuals, detailed environmental conditions, calibration procedures, system accuracy, power requirements, installation limitations, maintainability, safety, and workmanship. An outline of the qualification test procedures and failure criteria are also given. The Hydrologic Instrumentation Facility at NSTL Station, Mississippi will test available systems to determine if they meet the specification in this report for inclusion in the Survey 's 'Qualified Products List'. This list will be used for future procurement of water-level sensing systems by the Survey. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8289","usgsCitation":"Rapp, D., 1982, Specification for procurement of water-level sensing instrumentation, specification number HIF-I-1: U.S. Geological Survey Open-File Report 82-89, iii, 27 p. ;28 cm., https://doi.org/10.3133/ofr8289.","productDescription":"iii, 27 p. ;28 cm.","costCenters":[],"links":[{"id":144845,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0089/report-thumb.jpg"},{"id":38583,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0089/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d61","contributors":{"authors":[{"text":"Rapp, D.H.","contributorId":99150,"corporation":false,"usgs":true,"family":"Rapp","given":"D.H.","email":"","affiliations":[],"preferred":false,"id":161957,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29922,"text":"wri8155 - 1982 - Flow model of the Hudson River estuary from Albany to New Hamburg, New York","interactions":[],"lastModifiedDate":"2020-11-04T18:15:57.450538","indexId":"wri8155","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-55","title":"Flow model of the Hudson River estuary from Albany to New Hamburg, New York","docAbstract":"<p><span>A one-dimensional transient-flow-simulation model was developed </span><span>to represent a 76-mile reach of the tidal Hudson River between Albany </span><span>and New Hamburg. In this reach, the direction of flow reverses four </span><span>times daily as a result of tidal influence; this produces complex </span><span>current patterns and retards the rate at which the river can flush </span><span>out pollutants. In the model, the reach studied is treated as two </span><span>subreaches to incorporate differences in channel conditions and to </span><span>simplify model calibration. </span></p><p><span>This report includes all stage (water-level) and discharge data that were used to calibrate and verify the model and compares the model results with measured data. The model accurately simulated observed flows, but further calibration based upon additional flow measurements would improve simulation of the flow magnitude and phasing of the tide reversal under low-flow conditions. The model can be used to calculate instantaneous stage, velocity, and discharge for any location in the reach and can also be used to calculate net volume flux between tide reversals. </span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8155","collaboration":"Prepared in cooperation with New York State Department of Environmental Conservation, New York City Department of Environmental Protection","usgsCitation":"Stedfast, D.A., 1982, Flow model of the Hudson River estuary from Albany to New Hamburg, New York: U.S. Geological Survey Water-Resources Investigations Report 81-55, vi, 69 p., https://doi.org/10.3133/wri8155.","productDescription":"vi, 69 p.","costCenters":[],"links":[{"id":160275,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0055/report-thumb.jpg"},{"id":380162,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0055/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New York","otherGeospatial":"Hudson River estuary","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.15771484375,\n              40.53050177574321\n            ],\n            [\n              -73.465576171875,\n              40.53050177574321\n            ],\n            [\n              -73.465576171875,\n              42.73894375124377\n            ],\n            [\n              -74.15771484375,\n              42.73894375124377\n            ],\n            [\n              -74.15771484375,\n              40.53050177574321\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df30c","contributors":{"authors":[{"text":"Stedfast, David A.","contributorId":53429,"corporation":false,"usgs":true,"family":"Stedfast","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":202363,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28039,"text":"wri824046 - 1982 - Evaluation of sediment yield and sediment data-collection network in the Piceance basin, northwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:25","indexId":"wri824046","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4046","title":"Evaluation of sediment yield and sediment data-collection network in the Piceance basin, northwestern Colorado","docAbstract":"Statistical relationships were developed between suspended-sediment discharge and several regional factors of climate, physiography, and land use in the Piceance basin, northwestern Colorado. The purpose of the study was to evaluate the existing sediment collection network, especially in regard to detecting changes in suspended-sediment discharge due to the development in the basin. Spatial- and time variability were examined using multiple linear regression techniques. Because of the short period of record, monthly mean sediment loads were used to determine shifts or changes in trends due to mining and related activities in the basin. Dummy variable analysis was used to detect these premining and postmining differences in the regression lines and also to detect seasonal differences in the sediment discharge. Differences did exist in the sediment discharge from season to season and before and after mining; however, due to the variability and short period of record the cause of these differences could not be adequately determined. Part of the high variability in sediment discharge was due to variability in the water discharge. Therefore, if the network is to be improved, the emphasis needs to be on improvement of the water-discharge. The results of the monthly mean regression analysis were used in the mean monthly and mean annual analysis for determination of initial network design equations. These were only preliminary in nature and could be improved with additional data. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824046","usgsCitation":"Kircher, J.E., and Von Guerard, P., 1982, Evaluation of sediment yield and sediment data-collection network in the Piceance basin, northwestern Colorado: U.S. Geological Survey Water-Resources Investigations Report 82-4046, vi, 25 p. :ill., map ;28 cm., https://doi.org/10.3133/wri824046.","productDescription":"vi, 25 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":123891,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4046/report-thumb.jpg"},{"id":56877,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4046/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db673e0e","contributors":{"authors":[{"text":"Kircher, J. E.","contributorId":11207,"corporation":false,"usgs":true,"family":"Kircher","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":199110,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Von Guerard, Paul","contributorId":40620,"corporation":false,"usgs":true,"family":"Von Guerard","given":"Paul","affiliations":[],"preferred":false,"id":199111,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":41831,"text":"ofr82663 - 1982 - Aeromagnetic map of part of the Cascade Range, southwestern Washington and northern Oregon","interactions":[],"lastModifiedDate":"2021-11-24T22:44:50.044448","indexId":"ofr82663","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-663","title":"Aeromagnetic map of part of the Cascade Range, southwestern Washington and northern Oregon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82663","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Aeromagnetic map of part of the Cascade Range, southwestern Washington and northern Oregon: U.S. Geological Survey Open-File Report 82-663, 1 Plate: 22.68 × 23.85 inches, https://doi.org/10.3133/ofr82663.","productDescription":"1 Plate: 22.68 × 23.85 inches","costCenters":[],"links":[{"id":169028,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79555,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0663/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392123,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13797.htm"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Cascade Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.5383,\n              45.4944\n            ],\n            [\n              -120.9777,\n              45.4944\n            ],\n            [\n              -120.9777,\n              46.5\n            ],\n            [\n              -122.5383,\n              46.5\n            ],\n            [\n              -122.5383,\n              45.4944\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69768a","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":530650,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28341,"text":"wri8225 - 1982 - Evaluation of a predictive ground-water solute-transport model at the Idaho National Engineering Laboratory, Idaho","interactions":[],"lastModifiedDate":"2019-11-27T09:32:01","indexId":"wri8225","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-25","title":"Evaluation of a predictive ground-water solute-transport model at the Idaho National Engineering Laboratory, Idaho","docAbstract":"<p>Aqueous chemical and radioactive wastes discharged to shallow ponds and to shallow or deep wells on the Idaho National Engineering Laboratory (INEL) since 1952 have affected the quality of the ground water in the underlying Snake River Plain aquifer. The aqueous wastes have created large and laterally dispersed concentration plumes within the aquifer. The waste plumes with the largest areal distribution are those of chloride, tritium, and with high specific conductance values. The data from eight wells drilled near the southern INEL boundary during the summer of 1980 were used to evaluate the accuracy of a predictive modeling study completed in 1973, and to simulate 1980 positions of chloride and tritium plumes. Data interpretation from the drilling program indicates that the hydrogeologic characteristics of the subsurface rocks have marked effects on the regional ground-water flow regimen and, therefore, the movement of aqueous wastes. As expected, the waste plumes projected by the computer model for 1980, extended somewhat further downgradient than indicated by well data due to conservative worst-case assumptions in the model input and inaccurate approximations of subsequent waste discharge and aquifer recharge conditions. (USGS)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8225","usgsCitation":"Lewis, B.D., and Goldstein, F.J., 1982, Evaluation of a predictive ground-water solute-transport model at the Idaho National Engineering Laboratory, Idaho: U.S. Geological Survey Water-Resources Investigations Report 82-25, vi, 71 p. , https://doi.org/10.3133/wri8225.","productDescription":"vi, 71 p. ","costCenters":[],"links":[{"id":369705,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0025/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158474,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0025/report-thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Idaho National Engineering Laboratory","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.04681396484375,\n              43.51916261057404\n            ],\n            [\n              -112.04477548599242,\n              43.51916261057404\n            ],\n            [\n              -112.04477548599242,\n              43.51984724248989\n            ],\n            [\n              -112.04681396484375,\n              43.51984724248989\n            ],\n            [\n              -112.04681396484375,\n              43.51916261057404\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faf18","contributors":{"authors":[{"text":"Lewis, Barney D.","contributorId":93873,"corporation":false,"usgs":true,"family":"Lewis","given":"Barney","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":199625,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goldstein, Flora J.","contributorId":89573,"corporation":false,"usgs":true,"family":"Goldstein","given":"Flora","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":199624,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11260,"text":"ofr82450 - 1982 - Water-quality assessment of the Merced River, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:38","indexId":"ofr82450","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-450","title":"Water-quality assessment of the Merced River, California","docAbstract":"The Merced River and its major tributaries have been subject of water-quality and water-quantity studies by local, State, and Federal agencies since before 1900. Data have been compiled and analyzed, and even though water-quality problems exist in the basin, the water generally is of good quality for most of the beneficial uses defined by the California State Water Resources Control Board. Water-quality objectives for dissolved oxygen, pesticides, and pH were violated in some parts of the basin. The most likely cause of the dissolved-oxygen and pesticide violations is the return of agricultural irrigation water to the river in the lower 30 miles of the river. Violations of pH objectives occurred only in the upper drainage and were likely due to naturally occurring, poorly buffered water. Water quality is currently being monitored at three stations in the basin by California Department of Water Resources, at one station by the U.S. Geological Survey, and at several sites by the National Park Service. Modifications to the current water-quality monitoring program are proposed to gain further information on dissolved-oxygen fluctuations and pesticide concentrations in the lower river and to investigate nutrient input to Lake McClue. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82450","usgsCitation":"Sorenson, S.K., 1982, Water-quality assessment of the Merced River, California: U.S. Geological Survey Open-File Report 82-450, v, 51 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82450.","productDescription":"v, 51 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":144561,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0450/report-thumb.jpg"},{"id":39060,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0450/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39061,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0450/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47c8e4b07f02db4ab9a1","contributors":{"authors":[{"text":"Sorenson, Stephen K.","contributorId":90314,"corporation":false,"usgs":true,"family":"Sorenson","given":"Stephen","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":162825,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7693,"text":"ofr82687 - 1982 - Floods of October 1977 in southern Arizona and March 1978 in central Arizona","interactions":[{"subject":{"id":7693,"text":"ofr82687 - 1982 - Floods of October 1977 in southern Arizona and March 1978 in central Arizona","indexId":"ofr82687","publicationYear":"1982","noYear":false,"title":"Floods of October 1977 in southern Arizona and March 1978 in central Arizona"},"predicate":"SUPERSEDED_BY","object":{"id":3211,"text":"wsp2223 - 1984 - Floods of October 1977 in southern Arizona and March 1978 in central Arizona","indexId":"wsp2223","publicationYear":"1984","noYear":false,"title":"Floods of October 1977 in southern Arizona and March 1978 in central Arizona"},"id":1}],"supersededBy":{"id":3211,"text":"wsp2223 - 1984 - Floods of October 1977 in southern Arizona and March 1978 in central Arizona","indexId":"wsp2223","publicationYear":"1984","noYear":false,"title":"Floods of October 1977 in southern Arizona and March 1978 in central Arizona"},"lastModifiedDate":"2024-03-25T18:24:07.028716","indexId":"ofr82687","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-687","title":"Floods of October 1977 in southern Arizona and March 1978 in central Arizona","docAbstract":"<p>Major floods occurred in October 1977 and March 1978 in Arizona. As much as 14 inches of rain fell during October 6-9, 1977, over the mountains of southern Arizona and northern Mexico and caused the highest discharge since at least 1892 on the Santa Cruz River upstream from Tucson. The flood inundated areas as much as 4 miles wide, covered at least 16,000 acres of farmland, and caused $15.2 million in damage. Residential losses occurred at Nogales, Amado, Green Valley, and Sahuarita. Severe erosional damage occurred along the Santa Cruz River, Agua Fria Canyon, Potrero Creek, and many small drainages in the Sonoita Creek basin. The peak discharge in Agua Fria Canyon was the highest since before 1900. Less severe flooding occurred along the San Pedro River and the Gila River downstream from the San Pedro.</p><p>Widespread rainfall of 3 to 6 inches and 9 to 14 inches in some areas in the central mountains during February 28 to March 3, 1978, caused the highest discharge since 1920 on the Salt River in Phoenix and resulted in three deaths. Flooding along the Salt and Gila Rivers and several lesser streams caused statewide damage totaling $65.9 million, of which about $37 million occurred in Maricopa County. Nine counties were declared disaster areas.</p><p>During the flood of March 1978, moderate peak discharges and unusually high volumes of runoff occurred on tributaries to the Salt and Verde Rivers upstream from a system of reservoirs. Flood magnitudes were greater at the main-stem gaging stations than on the tributaries. The peak discharge into Theodore Roosevelt Lake, which was 21 percent full at the start of the flood, was about 155,000 cubic feet per second and is the largest known from 1890 to 1978. The reservoirs stored large quantities of water and greatly reduced the magnitude of the flood. The peak discharge of the Salt River was 125,000 cubic feet per second below Granite Reef Dam and 122,000 cubic feet per second at Phoenix. Discharges in excess of 100,000 cubic feet per second occurred for 8 hours. Without the storage provided by the reservoirs, the peak discharge would have been 260,000 cubic feet per second and the discharge would have exceeded 100,000 cubic feet per second for 66 hours. The Verde River was the principal flood source, but flows at the upstream gaging stations did not indicate the magnitude of the impending flood at Horseshoe Reservoir because large inflow from tributaries immediately upstream from the reservoir caused the river to rise at downstream stations before it rose at upstream stations.</p><p>About 17 percent of the water entering the reach from Granite Reef Dam to Gillespie Dam went to recharge, temporary ground-water storage, or evapotranspiration losses. All water was stored at Painted Rock Reservoir and released at a low rate that prevented water from reaching the Gila River near Mohawk gaging station.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82687","collaboration":"Prepared in cooperation with U.S. Bureau of Reclamation; U.S. Army Corps of Engineers, Los Angeles District; Arizona Department of Water Resources; Flood Control District of Maricopa County; and Salt River Valley Water Users' Association","usgsCitation":"Aldridge, B.N., and Eychaner, J., 1982, Floods of October 1977 in southern Arizona and March 1978 in central Arizona: U.S. Geological Survey Open-File Report 82-687, Report: v, 167 p.; 6 Plates: 39.37 x 22.21 inches or smaller, https://doi.org/10.3133/ofr82687.","productDescription":"Report: v, 167 p.; 6 Plates: 39.37 x 22.21 inches or smaller","costCenters":[],"links":[{"id":427015,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0687/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427014,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0687/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427013,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0687/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427012,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0687/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427011,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0687/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427010,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0687/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427009,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0687/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142041,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0687/report-thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"central Arizona, southern Arizona","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -114.51282734641853,\n              34.76108820121095\n            ],\n            [\n              -114.51282734641853,\n              31.355482940702416\n            ],\n            [\n              -108.9975564540747,\n              31.355482940702416\n            ],\n            [\n              -108.9975564540747,\n              34.76108820121095\n            ],\n            [\n              -114.51282734641853,\n              34.76108820121095\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48c4e4b07f02db53e8a0","contributors":{"authors":[{"text":"Aldridge, B. N.","contributorId":73179,"corporation":false,"usgs":true,"family":"Aldridge","given":"B.","middleInitial":"N.","affiliations":[],"preferred":false,"id":156450,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eychaner, J.H.","contributorId":34511,"corporation":false,"usgs":true,"family":"Eychaner","given":"J.H.","affiliations":[],"preferred":false,"id":156449,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28040,"text":"wri8172 - 1982 - Sediment transport and source areas of sediment and runoff, Big Sandy River basin, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:25","indexId":"wri8172","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-72","title":"Sediment transport and source areas of sediment and runoff, Big Sandy River basin, Wyoming","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri8172","usgsCitation":"Kircher, J.E., 1982, Sediment transport and source areas of sediment and runoff, Big Sandy River basin, Wyoming: U.S. Geological Survey Water-Resources Investigations Report 81-72, vi, 51 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri8172.","productDescription":"vi, 51 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157948,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0072/report-thumb.jpg"},{"id":56878,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0072/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbf33","contributors":{"authors":[{"text":"Kircher, J. E.","contributorId":11207,"corporation":false,"usgs":true,"family":"Kircher","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":199112,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7926,"text":"ofr82152 - 1982 - Water quality of the tidal Potomac River and estuary hydrologic data report, 1980 water year","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr82152","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-152","title":"Water quality of the tidal Potomac River and estuary hydrologic data report, 1980 water year","docAbstract":"This report contains data on the physical and chemical properties measured in the Tidal Potomac River and Estuary during the 1980 Water Year. Data were collected routinely at five stations, and periodically at 17 stations including three stations near the mouth of the Potomac River in Chesapeake Bay. Each of the five stations represent a cross section through which the transport of selected dissolved and suspended materials can be computed. The remaining stations represent locations at which data were collected for special synoptic studies such as salt water migration, and dissolved oxygen dynamics. Routinely, samples were analyzed for silica, nitrogen, phosphorus, chlorophyll-a, pheophytin, and suspended sediment. Additional samples were analyzed for organic carbon, calcium, manganese, magnesium, sodium, alkalinity, sulfate, iron, potassium, chloride, fluoride, seston, algal growth potential, adenosine triphosphate, nitrifying bacteria and dissolved-solids residue. In addition, solar radiation measurements and in-situ measurements of dissolved oxygen, specific conductance, pH, temperature, and Secchi disk transparency are reported. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82152","usgsCitation":"Blanchard, S., Coupe, R., and Woodward, J., 1982, Water quality of the tidal Potomac River and estuary hydrologic data report, 1980 water year: U.S. Geological Survey Open-File Report 82-152, i, 335 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82152.","productDescription":"i, 335 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":140722,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0152/report-thumb.jpg"},{"id":35490,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0152/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8882","contributors":{"authors":[{"text":"Blanchard, Stephen","contributorId":6852,"corporation":false,"usgs":true,"family":"Blanchard","given":"Stephen","affiliations":[],"preferred":false,"id":156845,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coupe, R.H. Jr.","contributorId":84755,"corporation":false,"usgs":true,"family":"Coupe","given":"R.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":156847,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Woodward, J.C.","contributorId":62590,"corporation":false,"usgs":true,"family":"Woodward","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":156846,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7087,"text":"ofr821039 - 1982 - Depth and temperature of permafrost on the Alaskan Arctic Slope; preliminary results","interactions":[],"lastModifiedDate":"2012-02-02T00:06:07","indexId":"ofr821039","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-1039","title":"Depth and temperature of permafrost on the Alaskan Arctic Slope; preliminary results","docAbstract":"As permafrost is defined by its temperature, the only way to determine its depth is to monitor the return to equilibrium of temperatures in boreholes that penetrate permafrost. Such measurements are under way in 25 wells on the Alaskan Arctic Slope; 21 are in Naval Petroleum Reserve Alaska (NPRA), and 4 are in the foothills to the east. Near-equilibrium results indicate that permafrost thickness in NPRA generally ranges between 200 and 400 m (compared to 600+ m at Prudhoe Bay); there are large local variations and no conspicuous regional trends. By contrast the long-term mean temperature of the ground surface (one factor determining permafrost depth) varies systematically from north to south in a pattern modified by the regional topography. The observed variation in permafrost temperature and depth cannot result primarily from effects of surface bodies of water or regional variations in heat flow; they are consistent, however, with expectable variations in the thermal conductivity of the sediments. It remains to be determined (with conductivity measurements) whether certain sites with anomalously high local gradients have anomalously high heat flow; if they do, they might indicate upwelling of interstitial fluids in the underlying basin sediments.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821039","usgsCitation":"Lachenbruch, A.H., Sass, J., Lawver, L., Brewer, M., and Moses, T., 1982, Depth and temperature of permafrost on the Alaskan Arctic Slope; preliminary results: U.S. Geological Survey Open-File Report 82-1039, 30 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr821039.","productDescription":"30 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":141344,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1039/report-thumb.jpg"},{"id":34414,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1039/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667a77","contributors":{"authors":[{"text":"Lachenbruch, Arthur H.","contributorId":27850,"corporation":false,"usgs":true,"family":"Lachenbruch","given":"Arthur","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":154243,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sass, J.H.","contributorId":70749,"corporation":false,"usgs":true,"family":"Sass","given":"J.H.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":154245,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lawver, L.A.","contributorId":73599,"corporation":false,"usgs":true,"family":"Lawver","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":154246,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brewer, M.C.","contributorId":54994,"corporation":false,"usgs":true,"family":"Brewer","given":"M.C.","email":"","affiliations":[],"preferred":false,"id":154244,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Moses, T.H.","contributorId":24344,"corporation":false,"usgs":true,"family":"Moses","given":"T.H.","email":"","affiliations":[],"preferred":false,"id":154242,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":8541,"text":"ofr8215 - 1982 - South Atlantic summary report 2: A revision of Outer Continental Shelf oil and gas activities in the South Atlantic (U.S.) and their onshore impacts, a summary report, July 1980","interactions":[],"lastModifiedDate":"2022-09-19T22:20:37.299269","indexId":"ofr8215","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-15","title":"South Atlantic summary report 2: A revision of Outer Continental Shelf oil and gas activities in the South Atlantic (U.S.) and their onshore impacts, a summary report, July 1980","docAbstract":"<p>The search for oil and gas on the Outer Continental Shelf (OCS) in the South Atlantic Region began in 1960, when geophysical surveys of the area were initiated. In 1977, a Continental Offshore Stratigraphic Test (COST) well was drilled in the Southeast Georgia Embayment. In March 1978, the first lease sale, Sale 43, was held, resulting in the leasing of 43 tracts. Approximately a year later, in May 1979, the first exploratory drilling began, and by February 1980, six exploratory wells had been drilled by four companies. Hydrocarbons were not found in any of these wells.</p><p>Lease Sale 56, the second lease sale in the South Atlantic Region, was held in August 1981. The sale resulted in the leasing of 47 tracts. Most of the leased tracts are in deep water along the Continental Slope off North Carolina. To date, no drilling has occurred on these tracts, but it is likely that two wells will be drilled or will be in the process of being drilled by the end of 1982. Reoffering Sale RS-2 is scheduled for July 1982, and it will include tracts offered in Lease Sale 56 that were not awarded leases. Lease Sale 78 is scheduled to be held in July 1983.</p><p>The most recent (March 1982) estimates of risked resources for leased lands in the South Atlantic OCS are 27 million barrels of oil and 120 billion cubic feet of gas.</p><p>To date, onshore impacts resulting from OCS exploration have been minimal, and they were associated with Lease Sale 43 exploratory activities. Tenneco, using existing facilities, established a support base in Savannah, Georgia; Getty, Transco, and Exxon used a support base established for them by the city of Brunswick, Georgia. The port at Morehead City, North Carolina, is expected to provide the onshore facilities for exploration in the near future on Lease Sale 56 tracts. Arrangements for the use of these facilities are currently being negotiated.</p><p>In June 1981, the South Atlantic Regional Technical Working Group prepared a Regional Transportation Management Plan for the South Atlantic OCS. The plan is principally an integration of regulatory frameworks, policies, and plans that are applicable to pipeline siting from each of the South Atlantic coastal States and Federal agencies with jurisdiction in the area.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8215","collaboration":"Prepared for the U.S. Department of the Interior, Minerals Management Service, in cooperation with the U.S. Geological Survey","usgsCitation":"Deis, J.L., Kurz, F.N., and Porter, E.O., 1982, South Atlantic summary report 2: A revision of Outer Continental Shelf oil and gas activities in the South Atlantic (U.S.) and their onshore impacts, a summary report, July 1980: U.S. Geological Survey Open-File Report 82-15, viii, 50 p., https://doi.org/10.3133/ofr8215.","productDescription":"viii, 50 p.","costCenters":[],"links":[{"id":407021,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0015/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141696,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0015/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Outer Continental Shelf, South Atlantic","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.298828125,\n              25.48295117535531\n            ],\n            [\n              -76.46484375,\n              25.48295117535531\n            ],\n            [\n              -76.46484375,\n              36.66841891894786\n            ],\n            [\n              -81.298828125,\n              36.66841891894786\n            ],\n            [\n              -81.298828125,\n              25.48295117535531\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7510","contributors":{"authors":[{"text":"Deis, Jeffrey L.","contributorId":10423,"corporation":false,"usgs":true,"family":"Deis","given":"Jeffrey","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":157905,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kurz, Frederick N.","contributorId":47785,"corporation":false,"usgs":true,"family":"Kurz","given":"Frederick","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":157906,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Porter, Elizabeth O.","contributorId":104491,"corporation":false,"usgs":true,"family":"Porter","given":"Elizabeth","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":157907,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3869,"text":"cir863 - 1982 - Water-data program of the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-02-02T00:05:36","indexId":"cir863","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"863","title":"Water-data program of the U.S. Geological Survey","docAbstract":"The U.S. Geological Survey is the principal Federal agency responsible for the collection of hydrologic data needed for the planning, development, use, and management of the Nation 's water resources. These data are the foundation necessary for conducting analytical and interpretive appraisals describing the occurrence and availability of surface and ground waters, and their physical, chemical, and biological characteristics. The data are likewise required for basic and problem-oriented research in hydraulics, hydrology, and related fields. Hydrologic data collection by the Geological Survey began in 1894. Current operations include about 17,000 stations for collection of river, lake, and reservoir data; about 27,000 wells for collection of ground-water data; and almost 17,000 stations for collection of water-quality information. These activities are described as well as the means by which the data are made available, and how the program is coordinated with other agencies. (USGS)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir863","usgsCitation":"Gilbert, B.K., and Buchanan, T.J., 1982, Water-data program of the U.S. Geological Survey: U.S. Geological Survey Circular 863, iii, 16 p. :ill., maps ;27 cm., https://doi.org/10.3133/cir863.","productDescription":"iii, 16 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":126650,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1982/0863/report-thumb.jpg"},{"id":30961,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1982/0863/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee2c2","contributors":{"authors":[{"text":"Gilbert, Bruce K.","contributorId":60198,"corporation":false,"usgs":true,"family":"Gilbert","given":"Bruce","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":147761,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buchanan, Thomas J.","contributorId":6842,"corporation":false,"usgs":true,"family":"Buchanan","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":147760,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":36497,"text":"fwsobs82_22 - 1982 - Impact of water level changes on woody riparian and wetland communities. Vol. IX, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:09:35","indexId":"fwsobs82_22","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/22","title":"Impact of water level changes on woody riparian and wetland communities. Vol. IX, Alaska","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Teskey, R.O., Hinckley, T.M., and Walters, M.A., 1982, Impact of water level changes on woody riparian and wetland communities. Vol. IX, Alaska: FWS/OBS 82/22, v. : ill.; 27 cm.","productDescription":"v. : ill.; 27 cm.","costCenters":[],"links":[{"id":167160,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8890","contributors":{"authors":[{"text":"Teskey, Robert O.","contributorId":87596,"corporation":false,"usgs":true,"family":"Teskey","given":"Robert","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":216425,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hinckley, Thomas M.","contributorId":51351,"corporation":false,"usgs":true,"family":"Hinckley","given":"Thomas","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":216424,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Walters, M. Alice","contributorId":13293,"corporation":false,"usgs":true,"family":"Walters","given":"M.","email":"","middleInitial":"Alice","affiliations":[],"preferred":false,"id":216423,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":43101,"text":"ofr82867 - 1982 - Ground-water levels in selected well fields and in west-central Florida, May 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:05:03","indexId":"ofr82867","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-867","title":"Ground-water levels in selected well fields and in west-central Florida, May 1982","docAbstract":"The water table in the surficial aquifer and the potentiometric surface of the Floridan aquifer in a 1,700-square-mile area in west-central Florida are mapped semiannually by the U.S. Geological Survey. Maps are based on water levels measured in wells each May to coincide with the seasonal low levels and each September to coincide with seasonal high levels. The mapped area shows 14 well fields that supplied 181.1 million gallons to municipalities on May 10, 1982. The water is withdrawn from the Floridan aquifer, the major aquifer in Florida. The effect of localized withdrawal on ground water is shown on the maps as depressions in both the potentiometric and water-table surfaces. In May 1982, ground-water levels were lower than those of September 1981. Seasonal recharge from above-average rainfall and reduced pumpage aided in the water-level recovery from record to near record levels of May 1981. (USGS)","language":"ENGLISH","doi":"10.3133/ofr82867","usgsCitation":"Barr, G., 1982, Ground-water levels in selected well fields and in west-central Florida, May 1982: U.S. Geological Survey Open-File Report 82-867, 29 maps on 2 sheets ;36 x 27 cm., sheets 107 x 77 cm., https://doi.org/10.3133/ofr82867.","productDescription":"29 maps on 2 sheets ;36 x 27 cm., sheets 107 x 77 cm.","costCenters":[],"links":[{"id":135667,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20749,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0867/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20750,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0867/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667618","contributors":{"authors":[{"text":"Barr, G. L.","contributorId":22312,"corporation":false,"usgs":true,"family":"Barr","given":"G. L.","affiliations":[],"preferred":false,"id":227722,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29377,"text":"wri824096 - 1982 - Estimated natural streamflow in the Rio San Jose upstream from the pueblos of Acoma and Laguna, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:55","indexId":"wri824096","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4096","title":"Estimated natural streamflow in the Rio San Jose upstream from the pueblos of Acoma and Laguna, New Mexico","docAbstract":"The development of surface and ground water, which began about 1870 in the upper Rio San Jose drainage basin, has decreased the flow of the Rio San Jose on the Pueblo of Acoma and the Pueblo of Laguna. The purpose of this study was to estimate the natural streamflow in the Rio San Jose that would have entered the pueblos if no upstream water development had taken place. Estimates of natural flow were based upon streamflow and precipitation records, historical accounts of streamflow, records of irrigated acreage, and empirically-derived estimates of the effects on streamflow of Bluewater Lake, groundwater withdrawals, and irrigation diversions. Natural streamflow in the Rio San Jose at the western boundary of the Pueblo of Acoma is estimated to be between 13,000 and 15,000 acre-feet per year, based on 55 years of recorded and reconstructed streamflow data from water years 1913 to 1972. Natural streamflow at the western boundary of the Pueblo of Laguna is estimated to be between 17 ,000 and 19,000 acre-feet per year for the same period. The error in these estimates of natural streamflow is difficult to assess accurately, but it probably is less than 25 percent. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri824096","usgsCitation":"Risser, D.W., 1982, Estimated natural streamflow in the Rio San Jose upstream from the pueblos of Acoma and Laguna, New Mexico: U.S. Geological Survey Water-Resources Investigations Report 82-4096, v, 56 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824096.","productDescription":"v, 56 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":126896,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4096/report-thumb.jpg"},{"id":58222,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4096/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fceb5","contributors":{"authors":[{"text":"Risser, D. W.","contributorId":48211,"corporation":false,"usgs":true,"family":"Risser","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":201432,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8538,"text":"ofr82362 - 1982 - Hydrologic data from test wells and low-flow investigations in the middle reach of the Eagle River valley, Alaska; 1980-81","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr82362","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-362","title":"Hydrologic data from test wells and low-flow investigations in the middle reach of the Eagle River valley, Alaska; 1980-81","docAbstract":"Test wells and low-flow investigations in the Eagle River valley , Alaska, were used to evaluate the feasibility of developing ground water for a public supply. Aquifers capable of supplying large yield wells were not indicated in any of the drilling areas. The data include: results of low-flow seepage investigations at 22 river sites; geologic materials logs of eight test wells; water-quality data from two observation wells, two springs, and two river sites; and water level and temperature information for the observation wells and streams. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82362","usgsCitation":"Deeter, G., and George, R., 1982, Hydrologic data from test wells and low-flow investigations in the middle reach of the Eagle River valley, Alaska; 1980-81: U.S. Geological Survey Open-File Report 82-362, iii, 16 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82362.","productDescription":"iii, 16 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":141694,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0362/report-thumb.jpg"},{"id":36117,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0362/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db66712e","contributors":{"authors":[{"text":"Deeter, Gary","contributorId":60216,"corporation":false,"usgs":true,"family":"Deeter","given":"Gary","email":"","affiliations":[],"preferred":false,"id":157901,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"George, R.S.","contributorId":12854,"corporation":false,"usgs":true,"family":"George","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":157900,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}