No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr82472","usgsCitation":"Shideler, G.L., and Stelting, C., 1982, Time-sequence measurements of estuarine hydrography and suspended sediments in Corpus Christi Bay, Texas: U.S. Geological Survey Open-File Report 82-472, i, 27 p. , https://doi.org/10.3133/ofr82472.","productDescription":"i, 27 p. ","costCenters":[],"links":[{"id":367098,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0472/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142446,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0472/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Corpus Christi Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -97.38830566406249,\n 27.68352808378776\n ],\n [\n -97.10540771484375,\n 27.68352808378776\n ],\n [\n -97.10540771484375,\n 27.894921808206057\n ],\n [\n -97.38830566406249,\n 27.894921808206057\n ],\n [\n -97.38830566406249,\n 27.68352808378776\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b4fc","contributors":{"authors":[{"text":"Shideler, G. L.","contributorId":63393,"corporation":false,"usgs":true,"family":"Shideler","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":162603,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stelting, C. E.","contributorId":53792,"corporation":false,"usgs":true,"family":"Stelting","given":"C. E.","affiliations":[],"preferred":false,"id":162602,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29035,"text":"wri824004 - 1982 - Reconnaissance of ground-water quality, eastern Snake River basin, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:08:44","indexId":"wri824004","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":"82-4004","title":"Reconnaissance of ground-water quality, eastern Snake River basin, Idaho","docAbstract":"Water-quality, geologic, and hydrologic data were collected for 165 wells in the eastern Snake River basin, Idaho. Water-quality characteristics analyzed include specific conductance, pH, water temperature, major dissolved cations and anions, and coliform bacteria. Ground water from aquifers in all rock units is generally composed of calcium, magnesium, and bicarbonate type and contains carbonate ions. Changes in area trends of ground-water composition probably are most directly related to variability in aquifer composition and proximity to varying sources of recharge, especially those related to man 's land- and water-use activities. In the uplands subareas, median values for selected ground-water characteristics from current analyses are 2000 mg/l hardness; 7.6, pH; 200 mg/l alkalinity; 13C; 0.2 mg/l fluoride; 15 mg/l silica; 0.51 mg/l nitrite (as nitrogen); less than 1 colony per 100 milliliters of water coliform bacteria; 0.02 mg/l phosphorus (total); and 25 mg/l hardness; 7.7, pH; 180 mg/l alkalinity; 11C; 0.4 mg/l fluoride; 26 mg/l silica; 1.2 mg/l nitrite plus nitrate; less than 1 colony per 100 milliliters of water coliform bacteria; 0.01 amg/l phosphorus; and 283 mg/l dissolved solids. Ground-water quality in most of the study area meets recommended standards or criteria for most uses. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824004","usgsCitation":"Parliman, D., 1982, Reconnaissance of ground-water quality, eastern Snake River basin, Idaho: U.S. Geological Survey Water-Resources Investigations Report 82-4004, vii, 100 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824004.","productDescription":"vii, 100 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158893,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4004/report-thumb.jpg"},{"id":57898,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4004/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57899,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4004/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57900,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4004/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57901,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4004/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57902,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4004/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a63e4b07f02db636fdf","contributors":{"authors":[{"text":"Parliman, D. J.","contributorId":64220,"corporation":false,"usgs":true,"family":"Parliman","given":"D. J.","affiliations":[],"preferred":false,"id":200831,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68419,"text":"ha645 - 1982 - Dissolved-solids concentrations of ground water in the Sacramento Valley, California","interactions":[],"lastModifiedDate":"2012-02-10T00:11:12","indexId":"ha645","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"645","title":"Dissolved-solids concentrations of ground water in the Sacramento Valley, California","docAbstract":"The general quality of the ground water in the Sacramento Valley , Calif., in terms of dissolved-solids concentration is considered good for irrigation, domestic, and most other uses. This map shows the distribution of dissolved-solids concentrations and is based on about 1,330 chemical analyses collected from about 900 wells between 1974 and 1978. On the west side of the valley some of the smaller streams contribute water of higher dissolved-solids concentrations to the ground water. The sources of these waters are thought to be the upper Cretaceous Chico Formation or marine deposits of Early Cretaceous age that are exposed in the Coast Ranges. (USGS)","language":"ENGLISH","doi":"10.3133/ha645","usgsCitation":"Fogelman, R.P., 1982, Dissolved-solids concentrations of ground water in the Sacramento Valley, California: U.S. Geological Survey Hydrologic Atlas 645, 1 map :col. ;70 x 99 cm., on sheet 76 x 112 cm., folded in envelope 32 x 24 cm., https://doi.org/10.3133/ha645.","productDescription":"1 map :col. ;70 x 99 cm., on sheet 76 x 112 cm., folded in envelope 32 x 24 cm.","costCenters":[],"links":[{"id":188901,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89942,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/645/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.75,38.083333333333336 ], [ -122.75,40.333333333333336 ], [ -120.75,40.333333333333336 ], [ -120.75,38.083333333333336 ], [ -122.75,38.083333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a1ed","contributors":{"authors":[{"text":"Fogelman, Ronald P.","contributorId":62597,"corporation":false,"usgs":true,"family":"Fogelman","given":"Ronald","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":278186,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9631,"text":"ofr821002 - 1982 - Plankton studies in San Francisco Bay; V, Zooplankton species composition and abundance in the South Bay, 1980-1981","interactions":[],"lastModifiedDate":"2016-07-27T11:35:38","indexId":"ofr821002","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":"82-1002","title":"Plankton studies in San Francisco Bay; V, Zooplankton species composition and abundance in the South Bay, 1980-1981","docAbstract":"Data are presented that summarize zooplankton species composition and abundance in South San Francisco Bay during 1980 and 1981. Sampling was conducted at least twice monthly at thirteen stations, from the southern extremity of the South Bay to the Golden Gate Bridge between January 1980 and May 1981. Samples were collected by pump at three depths in the shipping channel and one depth over the shoals. Subsamples were enumerated while alive. Total zooplankton biomass as carbon was calculated from estimated carbon quotas and abundances of each organism enumerated.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Menlo Park, CA","doi":"10.3133/ofr821002","usgsCitation":"Hutchinson, A., 1982, Plankton studies in San Francisco Bay; V, Zooplankton species composition and abundance in the South Bay, 1980-1981: U.S. Geological Survey Open-File Report 82-1002, 151 p., https://doi.org/10.3133/ofr821002.","productDescription":"151 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":37362,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1002/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142636,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1002/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685581","contributors":{"authors":[{"text":"Hutchinson, Anne","contributorId":45316,"corporation":false,"usgs":true,"family":"Hutchinson","given":"Anne","email":"","affiliations":[],"preferred":false,"id":160019,"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":10786,"text":"ofr82609 - 1982 - Aliphatic Hydrocarbons in Surface Sediments of Willapa Bay and Grays Harbor, Washington","interactions":[{"subject":{"id":10786,"text":"ofr82609 - 1982 - Aliphatic Hydrocarbons in Surface Sediments of Willapa Bay and Grays Harbor, Washington","indexId":"ofr82609","publicationYear":"1982","noYear":false,"title":"Aliphatic Hydrocarbons in Surface Sediments of Willapa Bay and Grays Harbor, Washington"},"predicate":"SUPERSEDED_BY","object":{"id":32588,"text":"pp1273B - 1984 - Correlation of paleostructure and sediment deposition in the Madison Limestone and associated rocks in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska","indexId":"pp1273B","publicationYear":"1984","noYear":false,"chapter":"B","title":"Correlation of paleostructure and sediment deposition in the Madison Limestone and associated rocks in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska"},"id":1}],"supersededBy":{"id":32588,"text":"pp1273B - 1984 - Correlation of paleostructure and sediment deposition in the Madison Limestone and associated rocks in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska","indexId":"pp1273B","publicationYear":"1984","noYear":false,"title":"Correlation of paleostructure and sediment deposition in the Madison Limestone and associated rocks in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska"},"lastModifiedDate":"2012-02-02T00:06:34","indexId":"ofr82609","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":"82-609","title":"Aliphatic Hydrocarbons in Surface Sediments of Willapa Bay and Grays Harbor, Washington","docAbstract":"Willapa Bay and Grays Harbor are two adjacent estuaries along the coast of Washington state. Willapa Bay is a recreational area minimally affected by industry; Grays Harbor, on the other hand, is moderately industrialized. Aliphatic hydrocarbons in surface sediments from these two estuaries reflect the differences in human activities. For example, the mean concentration of aliphatic hydrocarbons for seven stations in Willapa Bay is 1,000 ?g/g (relative to organic carbon) while in Grays Harbor this mean concentration for \r\nsix stations is 1,900 ?g/g. The difference is attributed mainly to the greater urban and industrial pollution in Grays Harbor. The gas chromatographic records of aliphatic hydrocarbons also reflect the extent of hydrocarbon pollution by the presence of a chromatographically unresolved mixture of hydrocarbons. This kind of mixture is more evident in sediments from Grays Harbor, and in both estuaries it is more concentrated in sediments collected nearest to urban centers.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr82609","usgsCitation":"Rapp, J.B., Kvenvolden, K., and Clifton, H., 1982, Aliphatic Hydrocarbons in Surface Sediments of Willapa Bay and Grays Harbor, Washington: U.S. Geological Survey Open-File Report 82-609, 14 p., ill., map ;28 cm., https://doi.org/10.3133/ofr82609.","productDescription":"14 p., ill., map ;28 cm.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":144866,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0609/report-thumb.jpg"},{"id":38584,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0609/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db68805c","contributors":{"authors":[{"text":"Rapp, J. B.","contributorId":28987,"corporation":false,"usgs":true,"family":"Rapp","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":161958,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kvenvolden, K.A.","contributorId":80674,"corporation":false,"usgs":true,"family":"Kvenvolden","given":"K.A.","email":"","affiliations":[],"preferred":false,"id":161960,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clifton, H.E.","contributorId":44151,"corporation":false,"usgs":true,"family":"Clifton","given":"H.E.","affiliations":[],"preferred":false,"id":161959,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10966,"text":"ofr8227 - 1982 - An oilspill risk analysis for the Mid-Atlantic (proposed sale 76) outer continental shelf lease area","interactions":[],"lastModifiedDate":"2012-02-02T00:06:26","indexId":"ofr8227","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":"82-27","title":"An oilspill risk analysis for the Mid-Atlantic (proposed sale 76) outer continental shelf lease area","docAbstract":"An oilspill risk analysis was conducted for the mid-Atlantic (proposed sale 76) Outer Continental Shelf (OCS) lease area. The analysis considered: the probability of spill occurrences based on historical trends; likely movement of oil slicks based on a climatological model; and locations of environmental resources which could be vulnerable to spilled oil. The times between spill occurrence and contact with resources were estimated to aid analysts in estimating slick characteristics. \r\n\r\nCritical assumptions made for this particular analysis were (1) that oil exists in the lease area, and (2) that 0.879 billion barrels of oil will be found and produced from tracts sold in sale 76. On the basis of this resource estimate, it was calculated that 3 to 4 oilspills of 1,000 barrels or greater will occur over the 30-year production life of the proposed sale 76 lease tracts. The results also depend upon the routes and methods chosen to transport oil from 0CS platforms to shore. \r\n\r\nGiven the above assumptions, the estimated probability that one or more oilspills of 1,000 barrels or larger will occur and contact land after being at sea less than 30 days is 0.36; for spills 10,000 barrels or larger, the probability is 0.22. These probabilities also reflect the following assumptions: oilspills remain intact for up to 30 days, do not weather, and are not cleaned up. It is noteworthy that over 90 percent of the risk from proposed sale 76 is due to transportation rather than production of oil. In addition, the risks from proposed sale 76 are about 1/10 to 1/15 those of existing tanker transportation of crude oil imports and refined products in the mid-Atlantic area.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8227","usgsCitation":"Samuels, W., and Hopkins, D., 1982, An oilspill risk analysis for the Mid-Atlantic (proposed sale 76) outer continental shelf lease area: U.S. Geological Survey Open-File Report 82-27, vi, 170 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr8227.","productDescription":"vi, 170 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":142967,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0027/report-thumb.jpg"},{"id":38736,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0027/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db6842be","contributors":{"authors":[{"text":"Samuels, W.B.","contributorId":85958,"corporation":false,"usgs":true,"family":"Samuels","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":162291,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hopkins, Dorothy","contributorId":11614,"corporation":false,"usgs":true,"family":"Hopkins","given":"Dorothy","email":"","affiliations":[],"preferred":false,"id":162290,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9483,"text":"ofr82321 - 1982 - Evaluation of Proterozoic quartzite and conglomerate in central Idaho for quartz-pebble conglomerate uranium deposits","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr82321","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":"82-321","title":"Evaluation of Proterozoic quartzite and conglomerate in central Idaho for quartz-pebble conglomerate uranium deposits","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82321","usgsCitation":"Hills, F., 1982, Evaluation of Proterozoic quartzite and conglomerate in central Idaho for quartz-pebble conglomerate uranium deposits: U.S. Geological Survey Open-File Report 82-321, 38 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82321.","productDescription":"38 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":141907,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0321/report-thumb.jpg"},{"id":37191,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0321/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fafbc","contributors":{"authors":[{"text":"Hills, F. A.","contributorId":22768,"corporation":false,"usgs":true,"family":"Hills","given":"F. A.","affiliations":[],"preferred":false,"id":159768,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11009,"text":"ofr82341 - 1982 - Report of the River Master of the Delaware River for the period of December 1, 1980 to November 30, 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:06:29","indexId":"ofr82341","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":"82-341","title":"Report of the River Master of the Delaware River for the period of December 1, 1980 to November 30, 1981","docAbstract":"Water supply conditions at the beginning of the year were marginal in marked contrast to those for the preceeding nine years. Discharge of the Delaware River at Montague, New Jersey, was only 72% of median as compared to 68% in excess of median the previous year. In December, with reservoir storage again declining, further reductions in both diversions and releases were imposed. With consent of all the parties, reductions were effected on December 20 limiting New York City diversions to 560 mgd, New Jersey to 65 mgd, and the required discharge at Montague was targeted at 1550 cfs. To conserve supplies, additional reductions were imposed in January when the Delaware River basin Commission formally declared a drought. New York City 's limitations was set at 520 mgd and that for New Jersey at 62 mgd. Montague flows were targeted between 1100 cfs, depending upon the location of the salt front in the estuary. Water quality of the Delaware River and Estuary was monitored on a continuous basis at eight sites for most of the year and on a monthly basis at ten sites to accurately locate the salt front. Highest concentrations observed at the Benjamin Franklin Bridge site was 133 mg/l (milligram per liter) on February 2. 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