{"pageNumber":"5274","pageRowStart":"131825","pageSize":"25","recordCount":184660,"records":[{"id":70162197,"text":"70162197 - 1982 - Feeding activity and spawning time of striped bass in the Colorado River Inlet, Lake Powell, Utah","interactions":[],"lastModifiedDate":"2016-01-15T11:06:06","indexId":"70162197","displayToPublicDate":"2015-09-14T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Feeding activity and spawning time of striped bass in the Colorado River Inlet, Lake Powell, Utah","docAbstract":"

Striped bass, Morone saxatilis, from Lake Powell, Utah spawned in or near the mixing zone of the reservoir and the Colorado River in 1980 and 1981. The fish did not move through Cataract Canyon rapids just above the reservoir in either year. Of 321 adult striped bass stomachs examined, 30% contained food and 28% contained threadfin shad, Dorosoma petenense. No stomachs contained native threatened or endangered Colorado River fishes.

","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1982)2<403:FAASTO>2.0.CO;2","usgsCitation":"Persons, W.R., and Bulkly, R., 1982, Feeding activity and spawning time of striped bass in the Colorado River Inlet, Lake Powell, Utah: North American Journal of Fisheries Management, v. 2, no. 4, p. 403-408, https://doi.org/10.1577/1548-8659(1982)2<403:FAASTO>2.0.CO;2.","productDescription":"6 p.","startPage":"403","endPage":"408","numberOfPages":"6","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314414,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Colorado River, Lake Powell","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.86553955078124,\n 37.004746084814784\n ],\n [\n -111.86553955078124,\n 37.96368875328558\n ],\n [\n -110.159912109375,\n 37.96368875328558\n ],\n [\n -110.159912109375,\n 37.004746084814784\n ],\n [\n -111.86553955078124,\n 37.004746084814784\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"2","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569a2649e4b0ec051295efc8","contributors":{"authors":[{"text":"Persons, William R. wpersons@usgs.gov","contributorId":4028,"corporation":false,"usgs":true,"family":"Persons","given":"William","email":"wpersons@usgs.gov","middleInitial":"R.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":588812,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bulkly, R.V.","contributorId":152281,"corporation":false,"usgs":false,"family":"Bulkly","given":"R.V.","email":"","affiliations":[],"preferred":false,"id":588813,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70162190,"text":"70162190 - 1982 - Gasometer: An inexpensive device for continuous monitoring of dissolved gases and supersaturation","interactions":[],"lastModifiedDate":"2016-01-14T16:12:12","indexId":"70162190","displayToPublicDate":"2015-09-08T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":" Gasometer: An inexpensive device for continuous monitoring of dissolved gases and supersaturation","docAbstract":"

The “gasometer” is a device that measures differential dissolved-gas pressures (δP) in water relative to barometric pressure (as does the “Weiss saturometer”), but operates continuously without human attention. The gasometer can be plumbed into a water-supply system and requires 8 liters/minute of water or more at 60 kilopascals. The gasometer's surfaces are nontoxic, and flow-through water can be used for fish culture. The gasometer may be connected to a small submersible pump and operated as a portable unit. The gasometer can activate an alarm system and thus protect fish from hyperbaric (supersaturation) or hypobaric gas pressures (usually due to low dissolved oxygen). Instructions are included for calculating and reporting data including the pressure and saturation of individual gases. Construction and performance standards are given for the gasometer. Occasional cleaning is required to remove biofouling from the gas-permeable tubing.

","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1982)111<505:G>2.0.CO;2","usgsCitation":"Bouck, G., 1982, Gasometer: An inexpensive device for continuous monitoring of dissolved gases and supersaturation: Transactions of the American Fisheries Society, v. 111, no. 4, p. 505-516, https://doi.org/10.1577/1548-8659(1982)111<505:G>2.0.CO;2.","productDescription":"12 p.","startPage":"505","endPage":"516","numberOfPages":"12","costCenters":[],"links":[{"id":314400,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"111","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5698d4b8e4b0fbd3f7fa4bf4","contributors":{"authors":[{"text":"Bouck, G.R.","contributorId":152274,"corporation":false,"usgs":false,"family":"Bouck","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":588799,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70162192,"text":"70162192 - 1982 - Effects of temperature on biochemical reactions and drug resistance of virulent and avirulent Aeromonas salmonicida","interactions":[],"lastModifiedDate":"2016-01-15T09:18:43","indexId":"70162192","displayToPublicDate":"2015-09-07T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2286,"text":"Journal of Fish Diseases","active":true,"publicationSubtype":{"id":10}},"title":" Effects of temperature on biochemical reactions and drug resistance of virulent and avirulent Aeromonas salmonicida","docAbstract":"

Incubation temperatures of 11°, 18° and 28° did not substantially affect biochemical reactions of either virulent or avirulent forms of Aeromonas salmonicida subspecies salmonicida. The only change observed, amygdalin fermentation, was positive at 11° and 18° but negative at 28°C. Several isolates utilized sucrose, a characteristic not normally recognized for A. salmonicida subspecies salmonicida.Antimicrobial susceptibility screening indicated resistance to novobiocin increased at the higher incubation temperatures. Standardized drug sensitivity testing procedures and precise zone diameter interpretive standards for bacterial fish pathogens are needed.

","language":"English","publisher":"Blackwell Science","doi":"10.1111/j.1365-2761.1982.tb00488.x","usgsCitation":"Hahnel, G., and Gould, R.W., 1982, Effects of temperature on biochemical reactions and drug resistance of virulent and avirulent Aeromonas salmonicida: Journal of Fish Diseases, v. 5, no. 4, p. 329-337, https://doi.org/10.1111/j.1365-2761.1982.tb00488.x.","productDescription":"9 p.","startPage":"329","endPage":"337","numberOfPages":"9","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314403,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-04-07","publicationStatus":"PW","scienceBaseUri":"569a263de4b0ec051295efb2","contributors":{"authors":[{"text":"Hahnel, G.B.","contributorId":79431,"corporation":false,"usgs":true,"family":"Hahnel","given":"G.B.","email":"","affiliations":[],"preferred":false,"id":588802,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gould, R. W.","contributorId":67054,"corporation":false,"usgs":true,"family":"Gould","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":588803,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70162189,"text":"70162189 - 1982 - Reciprocal allopreening in the Brownheaded Nuthatch","interactions":[],"lastModifiedDate":"2017-05-13T14:07:26","indexId":"70162189","displayToPublicDate":"2015-09-07T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3544,"text":"The Auk","onlineIssn":"1938-4254","printIssn":"0004-8038","active":true,"publicationSubtype":{"id":10}},"title":" Reciprocal allopreening in the Brownheaded Nuthatch","docAbstract":"

In his extensive reviews of allopreening, Harrison (1965, 1969) did not record this behavior for the Sittidae, nor did Kilham (1968, 1972, 1973) mention observing this behavior in either White-breasted (Sitta carolinensis) or Red-breasted (S. canadensis) nuthatches. Norris (1958: 187), however, mentioned the occurrence of allopreening in Brown-headed Nuthatches (S. pusilia), in passing. Here we relate our observations of reciprocal allopreening between two Brown-headed Nuthatches.

","language":"English","publisher":"American Ornithological Society","doi":"10.2307/4086037","usgsCitation":"Barbour, D., and DeGange, A., 1982, Reciprocal allopreening in the Brownheaded Nuthatch: The Auk, v. 99, no. 1, p. 171-171, https://doi.org/10.2307/4086037.","productDescription":"1 p.","startPage":"171","endPage":"171","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314399,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":314398,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://sora.unm.edu/node/23652"}],"volume":"99","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5698d4b9e4b0fbd3f7fa4bf8","contributors":{"authors":[{"text":"Barbour, D.B.","contributorId":152279,"corporation":false,"usgs":false,"family":"Barbour","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":588797,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeGange, A.R.","contributorId":52105,"corporation":false,"usgs":true,"family":"DeGange","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":588798,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70162198,"text":"70162198 - 1982 - Predation on seabirds by red foxes at Shaiak Island, Alaska","interactions":[],"lastModifiedDate":"2023-11-15T01:17:39.273755","indexId":"70162198","displayToPublicDate":"2015-08-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1163,"text":"Canadian Field-Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Predation on seabirds by red foxes at Shaiak Island, Alaska","docAbstract":"

Two Red Foxes (Vulpes fulva) that invaded Shaiak Island before the 1976 nesting season had a marked impact on the nesting success of five of seven species of seabirds breeding on the island that year. Common Eiders (Somateria mollissima), Glaucous-winged Gulls (Larus glaucescens), and Common Murres (Uria aalge), that nest in areas accessible to foxes, did not raise any young to fledging. Double-crested Cormorants (Phalacrocorax auritus) were only slightly more successful; 13 (4.3%) of 300 pairs raised one or more young to fledging. Evidence suggested that 21 (35.6%) of 62 pairs of Tufted Puffins (Lunda cirrhata) lost eggs or chicks to foxes, and foxes killed at least 13 (8.3%) of 156 adult puffins on ten sample plots. Conversely, Black-Legged Kittiwakes (Rissa tridactyla) and Pelagic Cormorants (Phalacrocorax pelagicus), which nested primarily on cliffs inaccessible to foxes, lost very few nests. There was no apparent change in general nest site selections by seabirds the following year, when foxes were no longer present. Any avoidance by birds of areas vulnerable to fox predation would probably be discernible only after several years of continuous predation.

","language":"English","publisher":"Ottawa Field-Naturalists' Club","usgsCitation":"Petersen, M.R., 1982, Predation on seabirds by red foxes at Shaiak Island, Alaska: Canadian Field-Naturalist, v. 96, no. 1, p. 41-45.","productDescription":"5 p.","startPage":"41","endPage":"45","numberOfPages":"5","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314417,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://www.biodiversitylibrary.org/part/354761"},{"id":314418,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Shaiak Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -152.33917236328125,\n 58.67979324840281\n ],\n [\n -152.48886108398435,\n 58.642652516575964\n ],\n [\n -152.56576538085935,\n 58.62835708998085\n ],\n [\n -152.70034790039062,\n 58.564671455866225\n ],\n [\n -152.70858764648438,\n 58.54819451046483\n ],\n [\n -152.666015625,\n 58.496564389069675\n ],\n [\n -152.55203247070312,\n 58.474311344996266\n ],\n [\n -152.34329223632812,\n 58.48077335833394\n ],\n [\n -152.25402832031247,\n 58.513782873082604\n ],\n [\n -152.21969604492188,\n 58.6212071822161\n ],\n [\n -152.33917236328125,\n 58.67979324840281\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"96","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569a264ee4b0ec051295efd7","contributors":{"authors":[{"text":"Petersen, Margaret R. 0000-0001-6082-3189 mrpetersen@usgs.gov","orcid":"https://orcid.org/0000-0001-6082-3189","contributorId":167729,"corporation":false,"usgs":true,"family":"Petersen","given":"Margaret","email":"mrpetersen@usgs.gov","middleInitial":"R.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":588814,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70162196,"text":"70162196 - 1982 - Reproduction and early-life accommodations of landlocked alewives to a southern range extension","interactions":[],"lastModifiedDate":"2016-01-15T10:45:53","indexId":"70162196","displayToPublicDate":"2015-08-11T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":" Reproduction and early-life accommodations of landlocked alewives to a southern range extension","docAbstract":"

Reproduction and first-year growth and food habits of landlocked alewives Alosa pseudoharengus in Claytor Lake, Virginia were examined and compared to descriptions for populations in the species' established New England-Great Lakes range. Alewives in mesothermal (2–27 C) Claytor Lake are shorter-lived (3 years) but grow faster, mature earlier (age 1), and have higher relative and absolute fecundities than have been reported for populations in colder northern waters. The 1979 spawning period extended from early May to early August, beginning at least 1 month earlier and lasting 4–9 weeks longer than in northern lakes. Changes in ovary condition during the spawning period suggest that alewives may be fractional spawners. Evidence of spawning was found in littoral areas throughout the lower 15 km of the reservoir. Growth in length of age-0 Claytor Lake alewives was linear through September and terminated in late autumn. Total first-year growth was reduced in 1979 (maximum of 130 mm total length, TL) from previous years (average of 160 mm TL), although it was substantially greater than recorded in the Great Lakes and the northeastern United States. The longer growing season, rather than accelerated in-season growth, appears to account for larger size achieved in Claytor Lake. High annual growth limits predation by Claytor Lake game fish on early spawned age-0 alewives by late summer. As elsewhere, larval and juvenile alewives (6–70 mm TL) fed primarily on copepods and cladocerans. Age-0 alewives longer than 35 mm TL demonstrated positive size-selection for cyclopoid copepods comparable to that shown by adults. Our findings suggest that self-sustaining alewife populations can be established in many inland waters but raise concerns regarding their forage value and community impacts.

","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1982)111<559:RAEAOL>2.0.CO;2","usgsCitation":"Nigro, A., and Ney, J.J., 1982, Reproduction and early-life accommodations of landlocked alewives to a southern range extension: Transactions of the American Fisheries Society, v. 111, no. 5, p. 559-569, https://doi.org/10.1577/1548-8659(1982)111<559:RAEAOL>2.0.CO;2.","productDescription":"11 p.","startPage":"559","endPage":"569","numberOfPages":"11","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314413,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Virginia","otherGeospatial":"Claytor Lake, Great Lakes, New England","volume":"111","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569a263ee4b0ec051295efb6","contributors":{"authors":[{"text":"Nigro, A.A.","contributorId":73963,"corporation":false,"usgs":true,"family":"Nigro","given":"A.A.","email":"","affiliations":[],"preferred":false,"id":588810,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ney, John J.","contributorId":91067,"corporation":false,"usgs":true,"family":"Ney","given":"John","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":588811,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70043525,"text":"70043525 - 1982 - Seepage study of the Sevier River and the Central Utah, McIntyre, and Leamington Canals, Juab and Millard Counties, Utah","interactions":[{"subject":{"id":9445,"text":"ofr81820 - 1981 - Seepage study of the Sevier River and the Central Utah, McIntyre, and Leamington Canals, Juab and Millard Counties, Utah","indexId":"ofr81820","publicationYear":"1981","noYear":false,"title":"Seepage study of the Sevier River and the Central Utah, McIntyre, and Leamington Canals, Juab and Millard Counties, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043525,"text":"70043525 - 1982 - Seepage study of the Sevier River and the Central Utah, McIntyre, and Leamington Canals, Juab and Millard Counties, Utah","indexId":"70043525","publicationYear":"1982","noYear":false,"title":"Seepage study of the Sevier River and the Central Utah, McIntyre, and Leamington Canals, Juab and Millard Counties, Utah"},"id":1}],"lastModifiedDate":"2016-12-17T12:41:26","indexId":"70043525","displayToPublicDate":"2013-02-14T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"74","title":"Seepage study of the Sevier River and the Central Utah, McIntyre, and Leamington Canals, Juab and Millard Counties, Utah","docAbstract":"

A study of the gains or losses of the Sevier River and the Central Utah, McIntyre, and Leamington Canals in the Leamington area, in Juab and Millard Counties, Utah, was made to determine changes in those reaches. Three to seven sets of seepage measurements made during 1980 were used in the analysis. Adjustments for fluctuations in flow were made from information obtained from water-stage recorders operated at selected locations during the time of each seepage run.

The study showed an overall net gain of about 9 cubic feet per second (0.25 cubic meter per second) in the Sevier River and about 1.3 cubic feet per second (0.04 cubic meter per second) in the Leamington Canal. It also showed a net loss of about 1 cubic feet per second (0.20 cubic meter per second) in the Central Utah Canal and about 0.8 cubic foot per second (0.02 cubic meter per second) in the McIntyre Canal. The gains in the Sevier River and Leamington Canal probably come chiefly as return seepage of water lost from the Central Utah and McIntyre Canals.

","language":"English","publisher":"Utah Department of Natural Resources and Energy, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources and Energy, Division of Water Rights","usgsCitation":"Herbert, L.R., Cruff, R., and Holmes, W., 1982, Seepage study of the Sevier River and the Central Utah, McIntyre, and Leamington Canals, Juab and Millard Counties, Utah: Technical Publication 74, iv, 43 p.","productDescription":"iv, 43 p.","numberOfPages":"48","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267420,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331999,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-750"},{"id":332000,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009z.pdf"}],"country":"United States","state":"Utah","county":"Juab County, Millard County","otherGeospatial":"Central Utah Canal, Leamington Canal, McIntyre Canal, Sevier River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.50102996826172,\n 39.445738080447484\n ],\n [\n -112.50102996826172,\n 39.63345647307571\n ],\n [\n -112.22911834716797,\n 39.63345647307571\n ],\n [\n -112.22911834716797,\n 39.445738080447484\n ],\n [\n -112.50102996826172,\n 39.445738080447484\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"511e078ce4b071e86a19a40f","contributors":{"authors":[{"text":"Herbert, L. R.","contributorId":39865,"corporation":false,"usgs":true,"family":"Herbert","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":473768,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cruff, R.W.","contributorId":77510,"corporation":false,"usgs":true,"family":"Cruff","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":473769,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Holmes, W. F.","contributorId":7277,"corporation":false,"usgs":true,"family":"Holmes","given":"W. F.","affiliations":[],"preferred":false,"id":473767,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70047700,"text":"70047700 - 1982 - Developing a state water plan: Ground-water conditions in Utah, spring of 1982","interactions":[{"subject":{"id":51038,"text":"ofr51139 - 1951 - Discharge of wells in East Shore area, Utah","indexId":"ofr51139","publicationYear":"1951","noYear":false,"title":"Discharge of wells in East Shore area, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70047700,"text":"70047700 - 1982 - Developing a state water plan: Ground-water conditions in Utah, spring of 1982","indexId":"70047700","publicationYear":"1982","noYear":false,"title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1982"},"id":1},{"subject":{"id":51791,"text":"ofr54325 - 1954 - Inventory of ground-water pumpage in three irrigation districts in southern Utah","indexId":"ofr54325","publicationYear":"1954","noYear":false,"title":"Inventory of ground-water pumpage in three irrigation districts in southern Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70047700,"text":"70047700 - 1982 - Developing a state water plan: Ground-water conditions in Utah, spring of 1982","indexId":"70047700","publicationYear":"1982","noYear":false,"title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1982"},"id":2}],"lastModifiedDate":"2017-01-20T17:57:36","indexId":"70047700","displayToPublicDate":"2013-01-01T15:15:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":110,"text":"Cooperative Investigations Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"22","title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1982","docAbstract":"

This is the nineteenth in a series of annual reports that describe ground-water conditions in Utah. Reports in this series, published cooperatively by the U.S. Geological Survey and the Utah Division of Water Resources, provide data to enable interested parties to keep abreast of changing ground-water conditions.

This report, like the others in the series, contains information on well construction, ground-water withdrawals from wells, water-level changes, and related changes in precipitation and streamflow. Supplementary data such as graphs showing chemical quality of water and maps showing ground-water level contours are included in reports of this series only for those years or areas for which applicable data are available and are important to a discussion of changing ground-water conditions.

This report includes individual discussions of selected major areas of ground-water development in the State for the calendar year 1981. Water-level fluctuations, however, are described for the periiod spring 1981 to spring 1982. Much of the data used in this report were collected by the U.S. Geological Survey in cooperation with the Division of Water Rights, Utah Department of Natural Resources.

","language":"English","publisher":"Utah Department of Natural Resources and Energy, Division of Water Resources","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the State of Utah","usgsCitation":"Holmes, W.F., Herbert, L.R., Bischoff, D., Smith, M.E., Seiler, R.L., Steiger, J.I., Appel, C.L., Jensen, V., Enright, M., Emett, D.C., Burden, C.B., Beard, R., Sultz, L., Eckenwiler, M., and Sandberg, G.W., 1982, Developing a state water plan: Ground-water conditions in Utah, spring of 1982: Cooperative Investigations Report 22, viii, 85 p.","productDescription":"viii, 85 p.","numberOfPages":"96","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":276778,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333661,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-183"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52136e34e4b0b08f446198e2","contributors":{"authors":[{"text":"Holmes, Walter F.","contributorId":31737,"corporation":false,"usgs":true,"family":"Holmes","given":"Walter","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":482760,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Herbert, L. R.","contributorId":39865,"corporation":false,"usgs":true,"family":"Herbert","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":482762,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bischoff, D.A.","contributorId":58548,"corporation":false,"usgs":true,"family":"Bischoff","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":482764,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, Melanie E.","contributorId":101977,"corporation":false,"usgs":true,"family":"Smith","given":"Melanie","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":482769,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Seiler, R. L.","contributorId":87546,"corporation":false,"usgs":true,"family":"Seiler","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":482766,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Steiger, Judy I. jsteiger@usgs.gov","contributorId":3689,"corporation":false,"usgs":true,"family":"Steiger","given":"Judy","email":"jsteiger@usgs.gov","middleInitial":"I.","affiliations":[],"preferred":true,"id":482756,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Appel, Cynthia L.","contributorId":34509,"corporation":false,"usgs":true,"family":"Appel","given":"Cynthia","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":482761,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Jensen, V.L.","contributorId":99034,"corporation":false,"usgs":true,"family":"Jensen","given":"V.L.","email":"","affiliations":[],"preferred":false,"id":482767,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Enright, Michael","contributorId":99979,"corporation":false,"usgs":true,"family":"Enright","given":"Michael","email":"","affiliations":[],"preferred":false,"id":482768,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Emett, D. C.","contributorId":21213,"corporation":false,"usgs":true,"family":"Emett","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":482759,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Burden, Carole B. cburden@usgs.gov","contributorId":852,"corporation":false,"usgs":true,"family":"Burden","given":"Carole","email":"cburden@usgs.gov","middleInitial":"B.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":482755,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Beard, R.C.","contributorId":16310,"corporation":false,"usgs":true,"family":"Beard","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":482758,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Sultz, L.G.","contributorId":61736,"corporation":false,"usgs":true,"family":"Sultz","given":"L.G.","email":"","affiliations":[],"preferred":false,"id":482765,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Eckenwiler, M.R.","contributorId":9674,"corporation":false,"usgs":true,"family":"Eckenwiler","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":482757,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Sandberg, G. W.","contributorId":55426,"corporation":false,"usgs":true,"family":"Sandberg","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":482763,"contributorType":{"id":1,"text":"Authors"},"rank":15}]}} ,{"id":70043399,"text":"70043399 - 1982 - Hydrology of the Beryl-Enterprise area, Escalante Desert, Utah, with emphasis on ground water; With a section on surface water","interactions":[{"subject":{"id":10426,"text":"ofr81533 - 1981 - Hydrology of the Beryl-Enterprise area, Escalante Desert, Utah, with emphasis on ground water","indexId":"ofr81533","publicationYear":"1981","noYear":false,"title":"Hydrology of the Beryl-Enterprise area, Escalante Desert, Utah, with emphasis on ground water"},"predicate":"SUPERSEDED_BY","object":{"id":70043399,"text":"70043399 - 1982 - Hydrology of the Beryl-Enterprise area, Escalante Desert, Utah, with emphasis on ground water; With a section on surface water","indexId":"70043399","publicationYear":"1982","noYear":false,"title":"Hydrology of the Beryl-Enterprise area, Escalante Desert, Utah, with emphasis on ground water; With a section on surface water"},"id":1}],"lastModifiedDate":"2016-12-17T12:48:26","indexId":"70043399","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"73","title":"Hydrology of the Beryl-Enterprise area, Escalante Desert, Utah, with emphasis on ground water; With a section on surface water","docAbstract":"

An investigation of the water resources of the Beryl-Enterprise area, Escalante Desert, Utah (pl. 1), was made during 1976-78 as part of a cooperative program with the Utah Department of Natural Resources, Division of Water Rights. Wells were the most important source of water for all purposes in the Beryl-Enterprise area during 1978, but it has not always been so. For nearly a century after the first settlers arrived in about 1860, streams supplied most of the irrigation water and springs supplied much of the water for domestic and stock use. A few shallow wells were dug by the early settlers for domestic and stock water, but the widespread use of ground water did not start until the 1920's when shallow wells were first dug to supply irrigation water. Ground-water withdrawals from wells, principally for irrigation, have increased nearly every year since the 1920's. The quantity withdrawn from wells surpassed that diverted from surface sources during the mid-1940's and was about eight times that amount during the 1970's. As a result, water levels have declined measurably throughout the area resulting in administrative water-rights problems.

The primary purpose of this report is to describe the water resources with emphasis on ground water. The surface-water resources are evaluated only as they pertain to the understanding of the ground-water resources. A secondary purpose is to discuss the extent and effects of the development of ground water in order to provide the hydrologic information needed for the orderly and optimum development of the resource and for the effective administration and adjudication of water rights in the area. The hydrologic data on which this report is based are given in a companion report by Mower (1981).

","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, Utah","collaboration":"Prepared by the United State Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Mower, R.W., and Sandberg, G.W., 1982, Hydrology of the Beryl-Enterprise area, Escalante Desert, Utah, with emphasis on ground water; With a section on surface water: Technical Publication 73, vi, 66 p.","productDescription":"vi, 66 p.","numberOfPages":"86","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267297,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331998,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009y.pdf"},{"id":331997,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-730"}],"country":"United States","state":"Utah","otherGeospatial":"Escalante Desert","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.1,\n 37.6\n ],\n [\n -114.1,\n 38.3\n ],\n [\n -113,\n 38.3\n ],\n [\n -113,\n 37.6\n ],\n [\n -114.1,\n 37.6\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"511b7282e4b0e3ef7b6f1e3c","contributors":{"authors":[{"text":"Mower, Reed W.","contributorId":32503,"corporation":false,"usgs":true,"family":"Mower","given":"Reed","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":473505,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sandberg, George Woodard","contributorId":87434,"corporation":false,"usgs":true,"family":"Sandberg","given":"George","email":"","middleInitial":"Woodard","affiliations":[],"preferred":false,"id":473506,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70044322,"text":"70044322 - 1982 - Ground-water resources in the central part of the Flathead Indian Reservation, northwestern Montana","interactions":[{"subject":{"id":22514,"text":"ofr80731 - 1980 - Ground-water resources in the central part of the Flathead Indian Reservation, northwestern Montana","indexId":"ofr80731","publicationYear":"1980","noYear":false,"title":"Ground-water resources in the central part of the Flathead Indian Reservation, northwestern Montana"},"predicate":"SUPERSEDED_BY","object":{"id":70044322,"text":"70044322 - 1982 - Ground-water resources in the central part of the Flathead Indian Reservation, northwestern Montana","indexId":"70044322","publicationYear":"1982","noYear":false,"title":"Ground-water resources in the central part of the Flathead Indian Reservation, northwestern Montana"},"id":1}],"lastModifiedDate":"2013-03-02T13:52:17","indexId":"70044322","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":266,"text":"Memoir","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"48","title":"Ground-water resources in the central part of the Flathead Indian Reservation, northwestern Montana","language":"English","publisher":"Montana Bureau of Mines and Geology","publisherLocation":"Butte, MT","collaboration":"Prepared in cooperation with the U.S. Geological Survey","usgsCitation":"Boettcher, A.J., 1982, Ground-water resources in the central part of the Flathead Indian Reservation, northwestern Montana: Memoir 48, iii, 28 p.; Maps: 3 Sheets.","productDescription":"iii, 28 p.; Maps: 3 Sheets","costCenters":[],"links":[{"id":268659,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Montana","otherGeospatial":"Flathead Indian Reservation","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.85,47.0 ], [ -114.85,47.89 ], [ -113.67,47.89 ], [ -113.67,47.0 ], [ -114.85,47.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51332d83e4b0c316aaf06824","contributors":{"authors":[{"text":"Boettcher, Arnold J.","contributorId":93025,"corporation":false,"usgs":true,"family":"Boettcher","given":"Arnold","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":475290,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70043184,"text":"70043184 - 1982 - A topology of mineralization and its meaning for prospecting","interactions":[{"subject":{"id":10514,"text":"ofr80298 - 1980 - A topology of mineralization and its meaning for prospecting","indexId":"ofr80298","publicationYear":"1980","noYear":false,"title":"A topology of mineralization and its meaning for prospecting"},"predicate":"SUPERSEDED_BY","object":{"id":70043184,"text":"70043184 - 1982 - A topology of mineralization and its meaning for prospecting","indexId":"70043184","publicationYear":"1982","noYear":false,"title":"A topology of mineralization and its meaning for prospecting"},"id":1}],"lastModifiedDate":"2013-02-20T08:55:41","indexId":"70043184","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"A topology of mineralization and its meaning for prospecting","docAbstract":"Epigenetic mineral deposits are universal members of an orderly spatial and temporal arrangement of igneous rocks, endomorphic rocks, and hydrothermally altered rocks. The association and sequence of these rocks is invariant whereas the metric relations and configurations of the properties of these rocks are unlimited in variety. This characterization satisfies the doctrines of topology. Metric relations are statistical, and their modes are among the better guides to optimal areas for exploration. Metric configurations are graphically irregular and unpredictable mathematical surfaces like mountain topography. Each mineral edifice must be mapped to locate its mineral deposits. All measurements and observations are only positive or neutral for the occurrence of a mineral deposit. Effective prospecting is based on an increasing density of positive data with proximity to the mineral deposit. This means sampling for maximal numbers of positive data, pragmatically the highest ore-element assays at each site, by selecting rock showing maximal development of lode attributes.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Ore Genesis: Special Publication of the Society for Geology Applied to Mineral Deposits","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Springer","publisherLocation":"Amsterdam, Netherlands","doi":"10.1007/978-3-642-68344-2_62","usgsCitation":"Neuerburg, G.J., 1982, A topology of mineralization and its meaning for prospecting, chap. of Ore Genesis: Special Publication of the Society for Geology Applied to Mineral Deposits, v. 2, p. 657-666, https://doi.org/10.1007/978-3-642-68344-2_62.","productDescription":"10 p.","startPage":"657","endPage":"666","costCenters":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"links":[{"id":267099,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267098,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/978-3-642-68344-2_62"}],"volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5114daf2e4b0ca7af0743aef","contributors":{"authors":[{"text":"Neuerburg, G. J.","contributorId":29395,"corporation":false,"usgs":true,"family":"Neuerburg","given":"G.","middleInitial":"J.","affiliations":[],"preferred":false,"id":473122,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70043690,"text":"70043690 - 1982 - Reconnaissance of the quality of surface water in the San Rafael River basin, Utah","interactions":[{"subject":{"id":24003,"text":"ofr80574 - 1980 - Reconnaissance of the quality of surface water in the San Rafael River basin, Utah","indexId":"ofr80574","publicationYear":"1980","noYear":false,"title":"Reconnaissance of the quality of surface water in the San Rafael River basin, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043690,"text":"70043690 - 1982 - Reconnaissance of the quality of surface water in the San Rafael River basin, Utah","indexId":"70043690","publicationYear":"1982","noYear":false,"title":"Reconnaissance of the quality of surface water in the San Rafael River basin, Utah"},"id":1}],"lastModifiedDate":"2016-12-12T16:11:37","indexId":"70043690","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"72","title":"Reconnaissance of the quality of surface water in the San Rafael River basin, Utah","docAbstract":"The water-quality reconnaissance of the San Rafael River basin, Utah, encompassed an area of about 2,300 square miles (5,960 square kilometers). Data were obtained by the U.S. Geological Survey one or more times at 116 sites from June 1977 to September 1978. At 19 other sites visited during the same period, the streams were dry. Precipitation and stream discharge were significantly less than normal during 1977 and ranged from less than to more than normal during 1978. Exposed rocks in the San Rafael River basin range in age from Permian to Holocene. The Carmel Formation of Jurassic age and various members of the Mancos Shale of Cretaceous age are major contributors of dissolved solids to streams in the basin. There are eight major reservoirs having a total usable capacity of 115, 000 acre-feet (142 cubic hectometers); seven are mainly for irrigation supply; one, having a usable capacity of 30,530 acre-feet (38 cubic hectometers), is for power plant water supply. From about April to November, major diversions from Huntington, Cottonwood, and Ferron Creeks nearly deplete the flow downstream; during such periods, downstream flow in these streams and in the San Rafael River is mainly irrigation-return flow and some ground-water seepage. The water at the points of major diversion on Huntington, Cottonwood, and Ferron Creeks is of excellent quality for irrigation; salinity hazard is low to medium, and sodium hazard is low. Dissolved-solids concentrations are less than 500 milligrams per liter. The water at the mouths of Huntington, Cottonwood, and Ferron Creeks has markedly larger dissolved-solids concentrations than does the water upstream from major diversions. The changes in the chemical quality occur in stream reaches that cross a belt of land 10 to 15 miles (16 to 24 kilometers) wide where the Mancos Shale is widely exposed. This also is the area where nearly all the intensive irrigation in the San Rafael River basin is practiced. There are no perennial tributaries to the San Rafael River downstream from Ferron Creek. Except during infrequent short periods of runoff from cloudbursts or snowmelt, the flow in the San Rafael River is composed of the flow that reaches the mouths of Huntington, Cottonwood, and Ferron Creeks. The quality of water in the mainstem of the San Rafael River is largely determined by the major consumptive use of water for irrigation in upstream areas and by the poor quality of irrigation-return flow. During the data-collection periods for this study, dissolved-solids concentrations in the San Rafael River were more than 2,000 milligrams per liter except during snowmelt runoff in June 1978 and during a major flood in August 1977. The concentrations of trace elements, with the exception of strontium, were relatively small; strontium concentrations exceeded 1,500 micrograms per liter at seven sites. Most of the suspended-sediment discharge of the San Rafael River probably occurs during a few days each year and results mainly from cloudburst runoff.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with The Utah Department of Natural Resources and Energy Division of Water Rights","usgsCitation":"Mundorff, J.C., and Thompson, K.R., 1982, Reconnaissance of the quality of surface water in the San Rafael River basin, Utah: Technical Publication 72, vi, 53 p.","productDescription":"vi, 53 p.","numberOfPages":"64","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267618,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331994,"rank":0,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-720"},{"id":267617,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009x.pdf"}],"country":"United States","state":"Utah","otherGeospatial":"San Rafael River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.5,\n 38.4\n ],\n [\n -111.5,\n 39.75\n ],\n [\n -110,\n 39.75\n ],\n [\n -110,\n 38.4\n ],\n [\n -111.5,\n 38.4\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51235b85e4b0c9f2bfcf8d47","contributors":{"authors":[{"text":"Mundorff, J. C.","contributorId":63374,"corporation":false,"usgs":true,"family":"Mundorff","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":474085,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, Kendall R.","contributorId":100854,"corporation":false,"usgs":true,"family":"Thompson","given":"Kendall","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":474086,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70006817,"text":"70006817 - 1982 - You asked for it! Using a catfish hatching trough for other eggs","interactions":[],"lastModifiedDate":"2012-08-23T01:02:05","indexId":"70006817","displayToPublicDate":"2012-08-08T16:17:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":855,"text":"Aquaculture Magazine","active":true,"publicationSubtype":{"id":10}},"title":"You asked for it! Using a catfish hatching trough for other eggs","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Aquaculture Magazine","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Richard V. Gallagher","publisherLocation":"Arden, NC","collaboration":"None","usgsCitation":"Martin, M., 1982, You asked for it! Using a catfish hatching trough for other eggs: Aquaculture Magazine, v. 8, no. 5, p. 37-37.","productDescription":"1 p.","startPage":"37","endPage":"37","numberOfPages":"1","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":259779,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bd246e4b08c986b32f705","contributors":{"authors":[{"text":"Martin, M.","contributorId":103217,"corporation":false,"usgs":true,"family":"Martin","given":"M.","affiliations":[],"preferred":false,"id":355288,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70038344,"text":"70038344 - 1982 - Water resources inventory of Connecticut Part 10: Lower Connecticut River basin","interactions":[],"lastModifiedDate":"2014-06-27T11:19:00","indexId":"70038344","displayToPublicDate":"2012-05-01T11:47:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":108,"text":"Connecticut Water Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"31","title":"Water resources inventory of Connecticut Part 10: Lower Connecticut River basin","docAbstract":"

The lower Connecticut River basin study area in south-central Connecticut includes 639 square miles and is drained principally by the Connecticut River and by seven smaller streams that flow directly to Long Island Sound between the West River on the west and the Connecticut River on the east. The population in 1979 was estimated to be 210,380. Much of the industrial development and population centers are in the Mattabesset River basin in the northwestern part, and the largest water use is also in the Mattabesset River basin.

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\n

Precipitation averages 47 inches per year and provides an abundant supply of water. About 20 inches returns to the atmosphere as evapotranspiration, and the remainder either flows directly to streams or percolates to the water table, eventually discharging to Long Island Sound. Small quantities of water are exported from the basin by the New Haven and Meridan Water Departments, and small quantities are imported by the New Britain Water Department and Metropolitan Direct Commission. Precipitation during 1931-60 resulted in an average annual runoff of 302 billion gallons. In inflow from the Connecticut River is added to the average annual runoff, the 4,370 billion gallon s per year is potentially available for water ue.

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\n

The domestic, institutional, commercial, and industrial (other than cooling water) water use for 1970 was 7 billion gallons, which is only 3 percent of the total water used, whereas 97 percent of the total is cooling water for power plants. Approximately 60 percent of the 7 billion gallons is treated before being discharged back to the streams.

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\n

The total amount of fresh water used during 1970 was estimated to be 256,000 million gallons (Mgal), of which 247,000 Mgal was used for cooling water at stream electric-generating plants. The quantity for domestic, commercial, industrial, and agricultural used was 9,000 Mgal, which was approximately 120 gallons a day per person. Public water systems providing 70 percent of these requirement and all the systems supplying water met the drinking water standards of the Connecticut General Assembly (1975).

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\n

Till is widespread and generally provides only small amounts of water. Wells in till normally yield only a few hundred gallons of water daily and may be inadequate during dry periods. The thickness of of till ranges from 0 to 15 feet; a median thickness of 26 feet is estimated from information provided in drillers' logs of 467 wells penetrating underlying bedrock. The till is generally used only as an emergency or secondary source of water.

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\n

Bedrock aquifers underlie the entire area and include sedimentary and crystalline (igneous and metamorphic) rock types. These aquifers supply small and usually reliable quantities of water to wells and are the chief source of water for many rural homes and farms., About 90 percent of the wells tapping bedrock yield at least 2 gal/min. The median yields from wells tapping aquifers in sedimentary, igneous, and metamorphic rocks are 11, 8, and 6.5 gal/min, respectively.

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\n

The quantity of water potentially available from stratified drift was estimated on the basis of hydraulic characteristics of the aquifers, mathematical modeling of the aquifer system, and evaluation of natural and induced recharge. Long-term yields estimated or ten areas underlain by significant thickness of stratified drift range from 0.4 to 4.4 million gallons per day (Mgal/d). A change in well spacing or numbering could increase the long-term yields, but detailed modeling verification studies are needed to confirm optimal well locations.

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\n

The chemical and physical (turbidity, color, taste, and sediment load) quality of water is good. The water if generally low in dissolved solids and is classified as soft to hard. Surface water is less mineralized than ground water, especially during high flow, when it is primarily derived from surface runoff rather than groundwater runoff. A median dissolved-solids concentration of 42 milligrams per liter (mg/L) and median hardness of 18 mg/L were determined from water samples collected from 26 streams during the high-flow period. During the low-flow period, median dissolved-solids concentration of 61 mg/L and median hardness of 27 mg/L were determined from sample from the same streams.

\n
\n

The quality of water in stratified-drift and crystalline-rock aquifers is generally better than that in the sedimentary-rock aquifers. Water from 32 wells tapping stratified drift had median dissolved-solids concentrations of 116 mg/L; and 33 wells tapping stratified drift and 42 tapping crystalline rock had median hardness of 73 mg/L and 68 mg/L, respectively. Water from 32 wells tapping sedimentary rock had median dissolved concentrations of 231 and 156 mg/L, respectively. Sedimentary rock generally yields the hardest water.

\n
\n

Iron and manganese occur objectionable concentrations in places, particularly in water from streams draining swamps and in water from aquifers either rich in iron and manganese-nearing minerals or where the reducing environment for solution of these minerals is favorable. Concentrations of iron in excess of 0.3 mg/L were found in 35 percent of the high streamflow samples, and in 45 percent of the ground-water samples. Most of the high iron and manganese concentration in streams and aquifers are found east of the Connecticut River.

\n
\nHuman activities and tidal influence along the coast have modified the quality of water in much f the study area. The greatest influence from human activities has been in the northwestern part, in the Mattabesset River basin. There, the quality of water has been affected by domestic and animal wastes, which cause high dissolved-solids concentrations, high nitrate and phosphate loads and high bacterial counts. In the entire area, high nitrate in groundwater occur only locally, and its presence in an individual water supply is chiefly a function of its proximity to sources of contamination, of well construction, and of thickness of overburden. Thirty public-supply wells did have water that had high sodium concentrations or objectionable iron and manganese concentrations, but these are not considered health hazards in the concentrations found in the water samples. Streams, wetlands, and some aquifers along the sough boundary of the basin contain salty water because of tidal movement or extensive ground-water withdrawals. High sediment concentrations also occur as a result of tidal influence in this area.

","language":"English","publisher":"Connecticut Department of Environmental Protection","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Connecticut Department of Environmental Protection","usgsCitation":"Weiss, L.A., Bingham, J.W., and Thomas, M.P., 1982, Water resources inventory of Connecticut Part 10: Lower Connecticut River basin: Connecticut Water Resources Bulletin 31, Report: viii, 85 p.; 5 Plates: 42.00 x 30.34 inches and smaller.","productDescription":"Report: viii, 85 p.; 5 Plates: 42.00 x 30.34 inches and smaller","numberOfPages":"94","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":258824,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ctwrb/0031/report.pdf","size":"27252","linkFileType":{"id":1,"text":"pdf"}},{"id":258825,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ctwrb/0031/report-thumb.jpg"},{"id":286232,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038344/plate-c.pdf"},{"id":286233,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038344/plate-d.pdf"},{"id":286234,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038344/plate-e.pdf"},{"id":286230,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038344/plate-a.pdf"},{"id":286231,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038344/plate-b.pdf"}],"scale":"48000","country":"United States","state":"Connecticut","otherGeospatial":"Lower Connecticut River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.833333,41.233333 ], [ -72.833333,41.8 ], [ -72.2,41.8 ], [ -72.2,41.233333 ], [ -72.833333,41.233333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bcb76e4b08c986b32d675","contributors":{"authors":[{"text":"Weiss, Lawrence A.","contributorId":102528,"corporation":false,"usgs":true,"family":"Weiss","given":"Lawrence","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":463918,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bingham, James W.","contributorId":36939,"corporation":false,"usgs":true,"family":"Bingham","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":463917,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, Mendall P.","contributorId":104314,"corporation":false,"usgs":true,"family":"Thomas","given":"Mendall","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":463919,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70006939,"text":"70006939 - 1982 - Tubifex worms identified as essential host for salmonid whirling disease","interactions":[],"lastModifiedDate":"2017-07-18T08:42:50","indexId":"70006939","displayToPublicDate":"2012-01-01T21:45:14","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":284,"text":"Research Information Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"82-39","title":"Tubifex worms identified as essential host for salmonid whirling disease","docAbstract":"No abstract available at this time","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Arlington, VA","collaboration":"None","usgsCitation":"Wolf, K., 1982, Tubifex worms identified as essential host for salmonid whirling disease: Research Information Bulletin 82-39, 1 p.","productDescription":"1 p.","startPage":"1","endPage":"1","numberOfPages":"1","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":258263,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb8b3e4b08c986b327a0c","contributors":{"authors":[{"text":"Wolf, K.","contributorId":16344,"corporation":false,"usgs":true,"family":"Wolf","given":"K.","email":"","affiliations":[],"preferred":false,"id":355509,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70006938,"text":"70006938 - 1982 - Fish smoking process inactivates whirling disease parasite","interactions":[],"lastModifiedDate":"2012-07-09T01:01:40","indexId":"70006938","displayToPublicDate":"2012-01-01T21:40:49","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":284,"text":"Research Information Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"82-4","title":"Fish smoking process inactivates whirling disease parasite","docAbstract":"No abstract available at this time","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Arlington, VA","collaboration":"None","usgsCitation":"Wolf, K., 1982, Fish smoking process inactivates whirling disease parasite: Research Information Bulletin 82-4, 1 p.","productDescription":"1 p.","startPage":"1","endPage":"1","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":258262,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a10a6e4b0c8380cd53d5c","contributors":{"authors":[{"text":"Wolf, K.","contributorId":16344,"corporation":false,"usgs":true,"family":"Wolf","given":"K.","email":"","affiliations":[],"preferred":false,"id":355508,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70006788,"text":"70006788 - 1982 - A rapid high-performance liquid-chromatographic method for simultaneously determining the concentrations of TFM and Bayer 73 in water during lampricide treatments","interactions":[],"lastModifiedDate":"2012-07-12T01:01:45","indexId":"70006788","displayToPublicDate":"2012-01-01T19:55:17","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1169,"text":"Canadian Journal of Fisheries and Aquatic Sciences","active":true,"publicationSubtype":{"id":10}},"title":"A rapid high-performance liquid-chromatographic method for simultaneously determining the concentrations of TFM and Bayer 73 in water during lampricide treatments","docAbstract":"The high-performance liquid-chromatography (HPLC) procedure requires only minutes per sample, is specific, and is relatively sensitive (limit of detection < 0.005 mg/L for both chemicals). A combined buffer (pH 4) and internal standard (3-chlorodiphenylamine) reagent is added to the water sample, which is injected through a Sep Pak C18 disposable cartridge. The cartridge adsorbs and retains both the lampricides and the internal standard. The quantitative elution of the three chemicals from the cartridge with a small volume of methanol effectively concentrates the sample and provides sample cleanup. The methanol extract is then analyzed directly by HPLC on an MCH 10 reverse phase column by using a methanol:0.01 mol/L acetate buffer (87:13, v:v) as the mobile phase at 2 mL/min and detected by ultraviolet spectrophotometry at 330 (or 254) nm. 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High-performance liquid chromatographic (HPLC) conditions are presented for the separation and quantitative determination of a homologous antibiotic complex (antimycin A). Combined HPLC and chemical ionization mass spectrometry proved to be exceptionally useful for the structural identification of chromatographic components. Using electrochemical, fluorescence, and ultraviolet detectors, the minimum detectable amounts of the antibiotics were found to be in the ranges 0.10–1.12, 0.31–1.69, and 4.10–28.2 ng, respectively. Advantages of the preparation of Dns derivatives for use in fluorescence detection are discussed. Application of the HPLC technique to the analysis of the antibiotic mixture in organic tissues is demonstrated.

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