Crossbred coho salmon Oncorhynchus kisutch were produced from all possible crosses among three stocks. The relative susceptibility of the progeny to infection by the myxosporean parasite Ceratomyxa shasta was determined by exposure of juvenile fish to Willamette River water that contained the infective stage of the parasite. Susceptibility of coho salmon native to the Columbia River basin to the disease ceratomyxosis was relatively low whereas that of coho salmon from remote locations was relatively high. Susceptibility of crossbred progeny nearly always was intermediate between the susceptibilities of fish from the parental stocks.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1986)115<492:SOPFCA>2.0.CO;2","usgsCitation":"Hemmingsen, A., McIntyre, J., and Fryer, J.L., 1986, Susceptibility of progeny from crosses among three stocks of coho salmon to infection by Ceratomyxa shasta: Transactions of the American Fisheries Society, v. 115, no. 3, p. 492-495, https://doi.org/10.1577/1548-8659(1986)115<492:SOPFCA>2.0.CO;2.","productDescription":"4 p.","startPage":"492","endPage":"495","numberOfPages":"4","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314306,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"115","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5698d4d2e4b0fbd3f7fa4c65","contributors":{"authors":[{"text":"Hemmingsen, A.R.","contributorId":84313,"corporation":false,"usgs":true,"family":"Hemmingsen","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":588664,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McIntyre, J.D.","contributorId":27006,"corporation":false,"usgs":true,"family":"McIntyre","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":588665,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fryer, J. L.","contributorId":21900,"corporation":false,"usgs":true,"family":"Fryer","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":588666,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70162144,"text":"70162144 - 1986 - Family size and effective population size in a hatchery stock of coho salmon (Oncorhynchus kisutch)","interactions":[],"lastModifiedDate":"2016-01-14T09:47:05","indexId":"70162144","displayToPublicDate":"2015-09-16T00:00:00","publicationYear":"1986","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":"Family size and effective population size in a hatchery stock of coho salmon (Oncorhynchus kisutch)","docAbstract":"Means and variances of family size measured in five year-classes of wire-tagged coho salmon (Oncorhynchus kisutch) were linearly related. Population effective size was calculated by using estimated means and variances of family size in a 25-yr data set. Although numbers of age 3 adults returning to the hatchery appeared to be large enough to avoid inbreeding problems (the 25-yr mean exceeded 4500), the numbers actually contributing to the hatchery production may be too low. Several strategies are proposed to correct the problem perceived. Argument is given to support the contention that the problem of effective size is fairly general and is not confined to the present study population.
","language":"English","publisher":"Canadian Science Publishing ","doi":"10.1139/f86-302","usgsCitation":"Simon, R., McIntyre, J., and Hemmingsen, A., 1986, Family size and effective population size in a hatchery stock of coho salmon (Oncorhynchus kisutch): Canadian Journal of Fisheries and Aquatic Sciences, v. 43, no. 12, p. 2434-2442, https://doi.org/10.1139/f86-302.","productDescription":"9 p.","startPage":"2434","endPage":"2442","numberOfPages":"9","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314317,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"43","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5698d4c9e4b0fbd3f7fa4c36","contributors":{"authors":[{"text":"Simon, R.C.","contributorId":34454,"corporation":false,"usgs":true,"family":"Simon","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":588677,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McIntyre, J.D.","contributorId":27006,"corporation":false,"usgs":true,"family":"McIntyre","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":588678,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hemmingsen, A.R.","contributorId":84313,"corporation":false,"usgs":true,"family":"Hemmingsen","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":588679,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70162142,"text":"70162142 - 1986 - Sequential tests for infectious hematopoietic necrosis virus in individuals and populations of sockeye salmon","interactions":[],"lastModifiedDate":"2017-02-12T15:34:32","indexId":"70162142","displayToPublicDate":"2015-09-15T00:00:00","publicationYear":"1986","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":"Sequential tests for infectious hematopoietic necrosis virus in individuals and populations of sockeye salmon","docAbstract":"The incidence and titer distribution of infectious hematopoietic necrosis virus in cavity fluid from spent female sockeye salmon (Oncorhynchus nerka) varied little when fish from a naturally spawning population were sampled three times on alternate days. However, when prespawning female sockeye salmon from a second population were individually tagged, penned, and sampled daily, the incidence and proportion of fish with high virus titer rose over a 6-d period. In 10 instances, consecutive cavity fluid samples from the same fish reverted from virus-positive to virus-negative. We suggest that spent fish should be sampled when accurate and quantitative data on the incidence and level of the virus are required.
","language":"English","publisher":"NRC Research Press","doi":"10.1139/f86-310","usgsCitation":"Mulcahy, D.M., and Pascho, R., 1986, Sequential tests for infectious hematopoietic necrosis virus in individuals and populations of sockeye salmon: Canadian Journal of Fisheries and Aquatic Sciences, v. 43, no. 12, p. 2515-2519, https://doi.org/10.1139/f86-310.","productDescription":"5 p.","startPage":"2515","endPage":"2519","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true},{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314309,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"43","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5698d4d1e4b0fbd3f7fa4c61","contributors":{"authors":[{"text":"Mulcahy, Daniel M. dmulcahy@usgs.gov","contributorId":3102,"corporation":false,"usgs":true,"family":"Mulcahy","given":"Daniel","email":"dmulcahy@usgs.gov","middleInitial":"M.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":588669,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pascho, Ron","contributorId":168941,"corporation":false,"usgs":true,"family":"Pascho","given":"Ron","email":"","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":588670,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70162145,"text":"70162145 - 1986 - Parasite burdens in experimental families of coho salmon.","interactions":[],"lastModifiedDate":"2016-01-14T09:50:35","indexId":"70162145","displayToPublicDate":"2015-09-15T00:00:00","publicationYear":"1986","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":" Parasite burdens in experimental families of coho salmon.","docAbstract":"We examined the possibility that parasites affect survival rates of anadromous hatchery coho salmon Oncorhynchus kisutch during their period in the wild. Survival was estimated from the rates at which adults returned to the hatchery. The frequency of infection of heart tissue by metacercariae of Nanophyetus sp. was higher in individuals from families with relatively high survival. Various degrees of parasitic and bacterial infection were observed in all groups. We frequently saw extensive infection and tissue reaction to trophozoites of Ceratomyxa sp. (probably C. shasta) in the apparent absence of spores, suggesting that the clinical method now used to determine the presence of Ceratomyxa infection needs to be reassessed.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1986)115<636:PBIEFO>2.0.CO;2","usgsCitation":"Yasutake, W.T., McIntyre, J., and Hemmingsen, A., 1986, Parasite burdens in experimental families of coho salmon.: Transactions of the American Fisheries Society, v. 115, no. 4, p. 636-640, https://doi.org/10.1577/1548-8659(1986)115<636:PBIEFO>2.0.CO;2.","productDescription":"5 p.","startPage":"636","endPage":"640","numberOfPages":"5","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314318,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"115","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5698d4b9e4b0fbd3f7fa4bf6","contributors":{"authors":[{"text":"Yasutake, W. T.","contributorId":103222,"corporation":false,"usgs":true,"family":"Yasutake","given":"W.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":588680,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McIntyre, J.D.","contributorId":27006,"corporation":false,"usgs":true,"family":"McIntyre","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":588681,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hemmingsen, A.R.","contributorId":84313,"corporation":false,"usgs":true,"family":"Hemmingsen","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":588682,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70162139,"text":"70162139 - 1986 - A hermaphroditic Arctic flounder, Liopsetta glacialis (Pleuronectidae), from Alaska","interactions":[],"lastModifiedDate":"2016-08-15T20:49:36","indexId":"70162139","displayToPublicDate":"2015-09-13T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1337,"text":"Copeia","active":true,"publicationSubtype":{"id":10}},"title":"A hermaphroditic Arctic flounder, Liopsetta glacialis (Pleuronectidae), from Alaska","docAbstract":"We discovered a hermaphrodite Liopsetta glacialis while examining tissues from a sample of 30 representatives of this species for a histopathological survey of fishes from the Beaufort Sea, Alaska. L. glacialis occurs in the Arctic Ocean from Queen Maude Gulf in arctic Canada, along the North American and Siberian coasts to the White Sea and Barents Sea (Morrow, 1980). The specimen was collected from Beaufort Lagoon on July 29, 1984, weighed 15, measured 100 mm (total length) and was between 3 and 4 years old.
","language":"English","publisher":"American Society of Ichthyologists and Herpetologists ","doi":"10.2307/1445306","usgsCitation":"Goldberg, S., Yasutake, W.T., and West, R., 1986, A hermaphroditic Arctic flounder, Liopsetta glacialis (Pleuronectidae), from Alaska: Copeia, v. 1986, no. 4, https://doi.org/10.2307/1445306.","productDescription":"1 p.","startPage":"1024","numberOfPages":"1","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314305,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Beaufort Lagoon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -142.2,\n 69.83\n ],\n [\n -142.2,\n 69.9\n ],\n [\n -142.3,\n 69.9\n ],\n [\n -142.3,\n 69.83\n ],\n [\n -142.2,\n 69.83\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"1986","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5698d4bae4b0fbd3f7fa4c02","contributors":{"authors":[{"text":"Goldberg, S.R.","contributorId":47975,"corporation":false,"usgs":true,"family":"Goldberg","given":"S.R.","email":"","affiliations":[],"preferred":false,"id":588661,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yasutake, W. T.","contributorId":103222,"corporation":false,"usgs":true,"family":"Yasutake","given":"W.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":588662,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"West, R.L.","contributorId":40696,"corporation":false,"usgs":true,"family":"West","given":"R.L.","affiliations":[],"preferred":false,"id":588663,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70162322,"text":"70162322 - 1986 - Requirements for integrating natural and artificial production of anadromous salmonids in the Pacific Northwest","interactions":[],"lastModifiedDate":"2016-01-21T12:51:14","indexId":"70162322","displayToPublicDate":"2015-09-07T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Requirements for integrating natural and artificial production of anadromous salmonids in the Pacific Northwest","docAbstract":"No abstract available
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Fish Culture in Fisheries Management: Proceedings of a Symposium on the Role of Fish Culture in Fisheries Management ","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Symposium on the Role of Fish Culture in Fisheries Management at Lake Ozark","conferenceDate":"March 31-April 3, 1985 ","conferenceLocation":"Lake Ozark, MO","language":"English","publisher":"American Fisheries Society","isbn":"978-0913235393","usgsCitation":"Reisenbichler, R., and McIntyre, J., 1986, Requirements for integrating natural and artificial production of anadromous salmonids in the Pacific Northwest, in Fish Culture in Fisheries Management: Proceedings of a Symposium on the Role of Fish Culture in Fisheries Management , Lake Ozark, MO, March 31-April 3, 1985 , p. 365-374.","productDescription":"10 p.","startPage":"365","endPage":"374","numberOfPages":"10","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314591,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Pacific Northwest","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -126.73828125,\n 41.3108238809182\n ],\n [\n -126.73828125,\n 49.83798245308484\n ],\n [\n -114.08203125,\n 49.83798245308484\n ],\n [\n -114.08203125,\n 41.3108238809182\n ],\n [\n -126.73828125,\n 41.3108238809182\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56a20f4ee4b0961cf2811c22","contributors":{"editors":[{"text":"Stroud, Richard H.","contributorId":152410,"corporation":false,"usgs":false,"family":"Stroud","given":"Richard","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":589225,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Reisenbichler, R.R.","contributorId":77356,"corporation":false,"usgs":true,"family":"Reisenbichler","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":589223,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McIntyre, J.D.","contributorId":27006,"corporation":false,"usgs":true,"family":"McIntyre","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":589224,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70157450,"text":"70157450 - 1986 - Hydrogeology and ground-water use and quality, Brown County, Wisconsin","interactions":[],"lastModifiedDate":"2018-01-08T19:27:03","indexId":"70157450","displayToPublicDate":"2015-04-06T04:30:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5596,"text":"Wisconsin Geological & Natural History Survey Information Circular","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"57","title":"Hydrogeology and ground-water use and quality, Brown County, Wisconsin","docAbstract":"The Paleozoic rock of Brown County includes formations of Cambrian, Ordovician, and Silurian age. These formations are eastward-dipping sedimentary rock that rest on Precambrian crystalline rock and are overlain by Pleistocene deposits. The units that are the principal sources of ground water were grouped into three aquifers (upper, St. Peter, and Elk Mound), and the less permeable units are grouped into three confining units (Maquoketa-Sinnipee, St. Lawrence, and Precambrian). The geologic and hydraulic characteristics of the aquifers and confining units are estimated from logs of more than 1,000 Brown County wells, from results of a packer test, and from published values.
\nRecharge to the water table, which was estimated at five monitored sites, ranges from 1 to 6 inches a year; most recharge is contributed by spring snowmelt and rainfall. A cone of depression caused by pumping the deeper aquifers in the Green Bay metropolitan area induces flow from the upper aquifer to the underlying st. Peter aquifer throughout most of the county. Several reaches of Duck Creek and the Suamico River also contribute water to the aquifers. A
\nbout 13 million gallons per day of ground water was pumped in Brown County during 1979, 63 percent of which was from wells open to both the St. Peter and Elk Mound aquifers. Municipal and industrial water users pumped 9.44 million gallons per day or 72 percent of the ground water withdrawn in 1979.
\nMost ground :water in the county is a calcium magnesium bicarbonate type. However, water from wells sampled in an area between the Fox River and Silurian escarpment have elevated levels of sodium (44 milligrams per liter) and sulfate (226 milligrams per liter). Water from wells that tap rocks older than Silurian dolomite contains high concentrations of strontium (more than 2.4 milligrams per liter) and fluoride (more than 0.85 milligrams per liter).
\nA three-dimensional digital model was used to simulate flow in the ground-water system. Model results indicate that sources of ground water pumped from wells tapping the St. Peter and Elk Mound aquifers in Brown County, 1979, include 4.8 million gallons per day of underflow, most of which enters the county across the west border; 1.9 million gallons per day of flow from vertical leakage within the county; and 1.5 million gallons per day from storage. The model is most sensitive to the horizontal hydraulic conductivity of the upper aquifer. Vertical hydraulic conductivity of the confining units and recharge rates to the water-table aquifer are the least well-defined model parameters.
","language":"English","publisher":"Wisconsin Geological & Natural History Survey","collaboration":"In cooperation with the University of Wisconsin-Extension, Geological and Natural History Survey","usgsCitation":"Krohelski, J.T., and Brown, B., 1986, Hydrogeology and ground-water use and quality, Brown County, Wisconsin: Wisconsin Geological & Natural History Survey Information Circular 57, v, 42 p.","productDescription":"v, 42 p.","numberOfPages":"49","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308459,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":350385,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://wgnhs.uwex.edu/pubs/download_ic57/"}],"country":"United States","state":"Wisconsin","county":"Brown County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-87.9887,44.6778],[-87.9888,44.6728],[-87.9901,44.6719],[-87.9907,44.6719],[-87.9914,44.6719],[-87.9932,44.6751],[-87.9939,44.6751],[-87.9952,44.6751],[-87.9958,44.6747],[-87.9971,44.6719],[-87.9991,44.672],[-88.0029,44.6738],[-88.0061,44.6743],[-88.0067,44.6739],[-88.0074,44.6734],[-88.008,44.673],[-88.0074,44.6716],[-88.0062,44.6702],[-88.0005,44.6679],[-87.9998,44.6674],[-87.9998,44.6665],[-88.0005,44.6651],[-88.0012,44.6647],[-88.0018,44.6647],[-88.0075,44.6679],[-88.0082,44.6679],[-88.0088,44.6675],[-88.0082,44.6638],[-88.009,44.6575],[-88.0099,44.6461],[-88.0106,44.6456],[-88.0112,44.6456],[-88.0144,44.6466],[-88.0151,44.6466],[-88.0151,44.6457],[-88.0145,44.6429],[-88.0145,44.642],[-88.0191,44.6352],[-88.0185,44.6343],[-88.0153,44.6338],[-88.0147,44.6334],[-88.0117,44.6251],[-88.0074,44.6141],[-88.0068,44.6132],[-88.0004,44.6118],[-87.9941,44.6067],[-87.9816,44.5947],[-87.9797,44.5933],[-87.979,44.5924],[-87.9798,44.5878],[-87.9805,44.5828],[-87.9818,44.5824],[-87.983,44.5892],[-87.9848,44.591],[-87.9861,44.5943],[-87.9898,44.6002],[-88.0012,44.6077],[-88.0082,44.61],[-88.0088,44.61],[-88.0101,44.61],[-88.0107,44.6105],[-88.0107,44.6119],[-88.0136,44.6228],[-88.0149,44.6238],[-88.0155,44.6247],[-88.0162,44.6247],[-88.0168,44.6247],[-88.0175,44.6234],[-88.0182,44.6188],[-88.0178,44.6092],[-88.0187,44.5974],[-88.0188,44.5946],[-88.0207,44.5937],[-88.0214,44.5924],[-88.0214,44.5901],[-88.019,44.585],[-88.0204,44.5782],[-88.0191,44.5782],[-88.0185,44.5759],[-88.0173,44.5745],[-88.0179,44.5732],[-88.0192,44.5723],[-88.0211,44.5737],[-88.0217,44.5755],[-88.0237,44.5755],[-88.0269,44.5746],[-88.0365,44.577],[-88.039,44.5766],[-88.0462,44.5726],[-88.0468,44.5717],[-88.0475,44.5694],[-88.0476,44.5658],[-88.0451,44.5644],[-88.0425,44.5639],[-88.0406,44.5648],[-88.0399,44.5675],[-88.0386,44.5684],[-88.0335,44.5665],[-88.0284,44.5637],[-88.0259,44.5614],[-88.0234,44.56],[-88.0234,44.5591],[-88.0247,44.5582],[-88.0266,44.5573],[-88.0286,44.5569],[-88.0337,44.5583],[-88.0349,44.5583],[-88.0356,44.5574],[-88.0356,44.5565],[-88.0287,44.5514],[-88.0255,44.5495],[-88.0249,44.5486],[-88.0249,44.5477],[-88.0249,44.5463],[-88.0218,44.5445],[-88.0212,44.5436],[-88.0212,44.5427],[-88.0218,44.5422],[-88.027,44.5391],[-88.0264,44.5386],[-88.0245,44.5386],[-88.0226,44.5386],[-88.02,44.5399],[-88.018,44.5435],[-88.0167,44.544],[-88.0154,44.5435],[-88.0142,44.5417],[-88.0116,44.5407],[-88.0046,44.5393],[-87.9925,44.5337],[-87.9811,44.5303],[-87.9664,44.5284],[-87.9504,44.5277],[-87.9401,44.529],[-87.9343,44.5316],[-87.931,44.5348],[-87.927,44.5416],[-87.9244,44.5429],[-87.9171,44.5529],[-87.9105,44.5605],[-87.9079,44.5628],[-87.9053,44.5664],[-87.9052,44.5682],[-87.9045,44.571],[-87.9031,44.575],[-87.905,44.5755],[-87.9095,44.576],[-87.914,44.5743],[-87.916,44.5743],[-87.9172,44.5752],[-87.9172,44.5761],[-87.9094,44.5797],[-87.9036,44.5819],[-87.8964,44.5864],[-87.8918,44.5918],[-87.886,44.5963],[-87.8839,44.6026],[-87.8813,44.6049],[-87.8741,44.6085],[-87.8695,44.6139],[-87.861,44.6188],[-87.8585,44.6192],[-87.8565,44.6187],[-87.8527,44.6178],[-87.8495,44.6173],[-87.8463,44.6177],[-87.8262,44.6284],[-87.8177,44.6338],[-87.8131,44.636],[-87.806,44.6373],[-87.7919,44.638],[-87.7823,44.6374],[-87.7732,44.6396],[-87.7706,44.6414],[-87.7654,44.645],[-87.7628,44.6477],[-87.7643,44.5888],[-87.7646,44.5017],[-87.7655,44.4146],[-87.7665,44.3271],[-87.8879,44.3277],[-87.888,44.2402],[-87.9238,44.2402],[-88.0099,44.2407],[-88.0431,44.2411],[-88.1317,44.2411],[-88.163,44.2414],[-88.193,44.2421],[-88.1919,44.3288],[-88.1921,44.3871],[-88.1921,44.4167],[-88.1918,44.5016],[-88.1908,44.5864],[-88.2203,44.5858],[-88.2453,44.5846],[-88.2446,44.6239],[-88.2432,44.664],[-88.2528,44.6641],[-88.2525,44.6846],[-88.2435,44.6845],[-88.2287,44.6844],[-88.2289,44.6725],[-88.1833,44.6734],[-88.1312,44.677],[-88.0092,44.6775],[-87.9887,44.6778]]]},\"properties\":{\"name\":\"Brown\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5603cd44e4b03bc34f544b0e","contributors":{"authors":[{"text":"Krohelski, J. T.","contributorId":59046,"corporation":false,"usgs":true,"family":"Krohelski","given":"J.","email":"","middleInitial":"T.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":573205,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, B.A.","contributorId":147913,"corporation":false,"usgs":false,"family":"Brown","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":573206,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70014857,"text":"70014857 - 1986 - Powder X-ray diffraction of florencite-(Nd)","interactions":[],"lastModifiedDate":"2025-06-24T16:54:24.729674","indexId":"70014857","displayToPublicDate":"2013-01-10T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3106,"text":"Powder Diffraction","active":true,"publicationSubtype":{"id":10}},"title":"Powder X-ray diffraction of florencite-(Nd)","docAbstract":"Florencite-(Nd) [(Nd,Ce)Al3(PO4)2(OH)6], was first described by Milton and Bastron (1971) from fracture surfaces in weathered cherts of the Franciscan Complex, south of Sausalito in Marin County, California. Florencite-(Nd) occurred there as a moderate-brown pulverulent earthy material; individual crystals were not discernible under microscopic examination. A semi-quantitative spectrographic analysis showed the presence of Nd (3 wt. %) and Ce (0.5 wt. %). No powder data for florencite-(Nd) exists in the current powder diffraction file.
","language":"English","publisher":"Cambridge University Press","doi":"10.1017/S0885715600012021","issn":"08857156","usgsCitation":"Fitzpatrick, J., 1986, Powder X-ray diffraction of florencite-(Nd): Powder Diffraction, v. 1, no. 4, p. 330-330, https://doi.org/10.1017/S0885715600012021.","productDescription":"1 p.","startPage":"330","endPage":"330","costCenters":[],"links":[{"id":225733,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","county":"Marin County","city":"Sausalito","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -122.5001410473408,\n 37.86029833407258\n ],\n [\n -122.5001410473408,\n 37.82493787595668\n ],\n [\n -122.46950199914482,\n 37.82493787595668\n ],\n [\n -122.46950199914482,\n 37.86029833407258\n ],\n [\n -122.5001410473408,\n 37.86029833407258\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"1","issue":"4","noUsgsAuthors":false,"publicationDate":"2013-01-10","publicationStatus":"PW","scienceBaseUri":"505a809ce4b0c8380cd7b0d1","contributors":{"authors":[{"text":"Fitzpatrick, J.","contributorId":28744,"corporation":false,"usgs":true,"family":"Fitzpatrick","given":"J.","affiliations":[],"preferred":false,"id":369459,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70046142,"text":"70046142 - 1986 - Geohydrology of the Vamoosa-Ada aquifer east-central Oklahoma with a section on chemical quality of water","interactions":[{"subject":{"id":8675,"text":"ofr77487 - 1977 - Hydrologic data for the Vamoosa Aquifer, east-central Oklahoma","indexId":"ofr77487","publicationYear":"1977","noYear":false,"title":"Hydrologic data for the Vamoosa Aquifer, east-central Oklahoma"},"predicate":"SUPERSEDED_BY","object":{"id":70046142,"text":"70046142 - 1986 - Geohydrology of the Vamoosa-Ada aquifer east-central Oklahoma with a section on chemical quality of water","indexId":"70046142","publicationYear":"1986","noYear":false,"title":"Geohydrology of the Vamoosa-Ada aquifer east-central Oklahoma with a section on chemical quality of water"},"id":1}],"lastModifiedDate":"2023-09-20T00:19:18.616106","indexId":"70046142","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":244,"text":"Circular","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"87","title":"Geohydrology of the Vamoosa-Ada aquifer east-central Oklahoma with a section on chemical quality of water","docAbstract":"The Vamoosa-Ada aquifer, which underlies an area of about 2,320 mi2, consists principally of the Vamoosa Formation and the overlying Ada Group of Pennsylvanian age. Rocks comprising the aquifer were deposited in a nearshore environment ranging from marine on the west to nonmarine on the east. Because of changes in depositional environments with time and from place to place, the aquifer is a complex sequence of fine- to very fine-grained sandstone, siltstone, shale, and conglomerate, with interbedded very thin limestone. The aggregate thickness of water-bearing sandstones is greatest south of the Cimarron River, where it reaches a maximum of 550 ft in the vicinity of Seminole. North of the Cimarron River, the average aggregate thickness of the sandstones is about 100 ft, but locally it may be as much as 200 ft. Transmissivity values derived from seven aquifer tests made for this study range from 70 to 490 ft2 per day; values decrease from south to north with decreasing sandstone thickness. Hydraulic-conductivity values range from 2 to 4 ft per day. Storage coefficients for the confined part of the aquifer, as determined from four aquifer tests made during 1944, have an average value of 0.0002. The average storage coefficient for the unconfined part of the aquifer is estimated at 0.12, based on an analysis of geophysical logs and grain-size data. The specific capacity of wells tested is generally less than 1 gallon per minute per foot of drawdown. An approximate hydrologic budget for the aquifer for 1975 gives values, in acre-feet per year, of 93,000 for recharge, 233,000 for runoff, and 2,003,000 for evapotranspiration. The total of these values is almost equal to the average annual precipitation of 2,330,000 acre-ft per year. The estimated amount of water containing a maximum of 1,500 milligrams per liter of dissolved solids stored in the aquifer is estimated at 60 million acre-ft. Of this amount, an estimated 36 million acre-ft is available for use. The quality of water in the Vamoosa-Ada aquifer generally is suitable for municipal, domestic, and stock use. Of 55 water samples analyzed in the laboratory, about 75 percent were of the sodium bicarbonate or sodium calcium bicarbonate type; the remainder were of the sodium sulfate, calcium sulfate, sodium chloride, or indeterminate types. Laboratory and on-site chemical-quality data indicate that mineralization of both ground and surface waters is greater than normal in some areas. Water samples from 7 wells and 12 stream sites had concentrations of bromide exceeding 1 milligram per liter; the only known source of bromide in the area is brine associated with petroleum production.","language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Reston, VA","collaboration":"Prepared by the United States Geological Survey in cooperation with the Oklahoma Geological Survey","usgsCitation":"D’Lugosz, J.J., McClaflin, R.G., and Marcher, M.V., 1986, Geohydrology of the Vamoosa-Ada aquifer east-central Oklahoma with a section on chemical quality of water: Circular 87, vi, 42 p.; Maps: 3 Sheets: 40 x 44 inches.","productDescription":"vi, 42 p.; Maps: 3 Sheets: 40 x 44 inches","numberOfPages":"48","costCenters":[{"id":634,"text":"Water Resources Program","active":false,"usgs":true}],"links":[{"id":272929,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.ou.edu/ogs/publications/circulars/circularssearch"},{"id":272933,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70046142.png"}],"country":"United States","state":"Oklahoma","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.62 ], [ -103.0,37.0 ], [ -94.43,37.0 ], [ -94.43,33.62 ], [ -103.0,33.62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51a5d1e9e4b0605bc571efbc","contributors":{"authors":[{"text":"D’Lugosz, Joseph J.","contributorId":71172,"corporation":false,"usgs":true,"family":"D’Lugosz","given":"Joseph","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":479029,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McClaflin, Roger G.","contributorId":50157,"corporation":false,"usgs":true,"family":"McClaflin","given":"Roger","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":479028,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Marcher, Melvin V.","contributorId":11590,"corporation":false,"usgs":true,"family":"Marcher","given":"Melvin","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":479027,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70043186,"text":"70043186 - 1986 - Bedrock aquifers of eastern San Juan County, Utah","interactions":[{"subject":{"id":12494,"text":"ofr85568 - 1985 - Bedrock aquifers of eastern San Juan County, Utah","indexId":"ofr85568","publicationYear":"1985","noYear":false,"title":"Bedrock aquifers of eastern San Juan County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043186,"text":"70043186 - 1986 - Bedrock aquifers of eastern San Juan County, Utah","indexId":"70043186","publicationYear":"1986","noYear":false,"title":"Bedrock aquifers of eastern San Juan County, Utah"},"id":1}],"lastModifiedDate":"2016-12-13T09:44:27","indexId":"70043186","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1986","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":"86","title":"Bedrock aquifers of eastern San Juan County, Utah","docAbstract":"This study is one of a series of studies appraising the waterbearing properties of the Navajo Sandstone and associated formations in southern Utah. The stu<¥ area is al:x>dy area is about 4,600 square miles, extending from the Utah-Arizona State line northward to the San Juan-Grand County line and westward from the Utah-Colorado State line to the longitude of about 109°50'.
Some of the water-yielding formations are grouped into aquifer systems. The C aquifer is comprised of the DeChelly Sandstone Member of the Cutler Formation. The P aquifer is comprised of the Cedar Mesa Member of the Cutler Formation and the undifferentiated Cutler Formation. The N aquifer is comprised of the sedimentary section that includes the Wingate Sandstone, Kayenta Formation, Navajo Sandstone, Carmel Formation, and Entrada sandstone. The M aquifer is comprised of the Bluff Sandstone Member and other sandstone units of the Morrison Formation. The D aquifer is comprised of the Burro Canyon Formation and Dakota Sandstone. Discharge from the ground-water reservoir to the San Juan River between gaging stations at Four Corners and Mexican Hat is about 66 cubic feet per second.
The N aquifer is the main aquifer in the study area. Recharge by infiltration of precipitation is estimated to be 25,000 acre-feet per year. A major ground-water divide exists under the broad area east of Monticello. The thickness of the N aquifer, where the sedimentary section is fully preserved and saturated, generally is 750 to 1,250 feet. Hydraulic conductivity values obtained from aquifer tests range from 0.02 to 0.34 foot per day. The total volume of water in transient storage is about 11 million acre-feet. Well discharge somewhat exceeded 2,340 acre-feet during 1981. Discharge to the San Juan River from the N aquifer is estimated to be 6.9 cubic feet per second. Water quality ranges from a calcium bicarbonate to sodium chloride type water
","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the Unites States Geological Survey in cooperation with the Utah Department of Natural Resources and Energy Division of Water Rights","usgsCitation":"Avery, C., 1986, Bedrock aquifers of eastern San Juan County, Utah: Technical Publication 86, viii, 114 p.","productDescription":"viii, 114 p.","numberOfPages":"125","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267104,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":332013,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-6-200"},{"id":332014,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w92000ab.pdf"}],"country":"United States","state":"Utah","county":"San Juan County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.918212890625,\n 37.00255267215955\n ],\n [\n -109.918212890625,\n 38.74123075381228\n ],\n [\n -109.0447998046875,\n 38.74123075381228\n ],\n [\n -109.0447998046875,\n 37.00255267215955\n ],\n [\n -109.918212890625,\n 37.00255267215955\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5114dafce4b0ca7af0743b0c","contributors":{"authors":[{"text":"Avery, Charles","contributorId":70739,"corporation":false,"usgs":true,"family":"Avery","given":"Charles","affiliations":[],"preferred":false,"id":473124,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70044030,"text":"70044030 - 1986 - Water resources of the Park City area, Utah, with emphasis on ground water","interactions":[{"subject":{"id":14181,"text":"ofr85638 - 1985 - Water resources of the Park City area, Utah, with emphasis on ground water","indexId":"ofr85638","publicationYear":"1985","noYear":false,"title":"Water resources of the Park City area, Utah, with emphasis on ground water"},"predicate":"SUPERSEDED_BY","object":{"id":70044030,"text":"70044030 - 1986 - Water resources of the Park City area, Utah, with emphasis on ground water","indexId":"70044030","publicationYear":"1986","noYear":false,"title":"Water resources of the Park City area, Utah, with emphasis on ground water"},"id":1}],"lastModifiedDate":"2016-12-13T09:32:51","indexId":"70044030","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1986","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":"85","title":"Water resources of the Park City area, Utah, with emphasis on ground water","docAbstract":"The Park City area is a rapidly growing residential and recreational area about 30 miles east of Sal t Lake City (fig. 1). The area of study is about 140 square miles in which the principle industries are agriculture, skiing, and other recreational activities. The area once was a major lead- and silver-mining district, but no mines were active in 1984. A resumption in mining activity, however, could take place with an increase in the price of metals.
The population of the Park City area is expected to increase rapidly in the near future; and the provision of an adequate water supply for the growing population, while avoiding harmful affects of development, is a major concern for local municipalities, developers, and the Utah Division of Water Rights. In addition, agricultural interests in and below the area are concerned about the effects of increased ground-water withdrawals on streamflow, which is fully appropriated by downstream users. The area also contains the proposed site for the Jordanelle dam, a part of the Bonneville unit of the central Utah Project. The damsite is near an historic mining area; and mining companies are concerned that if mining is resumed, the reservoir may create some additional dewatering problems in the mines.
","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, Division of Water Rights","usgsCitation":"Holmes, W.F., Thompson, K.R., and Enright, M., 1986, Water resources of the Park City area, Utah, with emphasis on ground water: Technical Publication 85, vi, 82 p.","productDescription":"vi, 82 p.","numberOfPages":"90","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":268267,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268266,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w92000aa.pdf"},{"id":332012,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-6-170"}],"country":"United States","state":"Utah","city":"Park City","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.8792724609375,\n 40.44694705960048\n ],\n [\n -111.8792724609375,\n 41.025499378313754\n ],\n [\n -111.1376953125,\n 41.025499378313754\n ],\n [\n -111.1376953125,\n 40.44694705960048\n ],\n [\n -111.8792724609375,\n 40.44694705960048\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"512c9623e4b0855fde669820","contributors":{"authors":[{"text":"Holmes, Walter F.","contributorId":31737,"corporation":false,"usgs":true,"family":"Holmes","given":"Walter","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":474673,"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":474675,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Enright, Michael","contributorId":99979,"corporation":false,"usgs":true,"family":"Enright","given":"Michael","email":"","affiliations":[],"preferred":false,"id":474674,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70044044,"text":"70044044 - 1986 - Ground-water conditions in the Lake Powell area, Utah","interactions":[{"subject":{"id":48910,"text":"ofr8593 - 1986 - Ground-water conditions in the Lake Powell area, Utah","indexId":"ofr8593","publicationYear":"1986","noYear":false,"title":"Ground-water conditions in the Lake Powell area, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70044044,"text":"70044044 - 1986 - Ground-water conditions in the Lake Powell area, Utah","indexId":"70044044","publicationYear":"1986","noYear":false,"title":"Ground-water conditions in the Lake Powell area, Utah"},"id":1}],"lastModifiedDate":"2016-12-17T10:58:15","indexId":"70044044","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1986","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":"84","title":"Ground-water conditions in the Lake Powell area, Utah","docAbstract":"The Lake Powell area comprises about 2,450 square miles in south-central Utah. It is subdivided into three geographical areas by the Colorado and San Juan Rivers. The Henry Mountains area is north of the Colorado River, the Navajo Mountain area is south of the San Juan River, and the third area is between the Colorado and San Juan Rivers.","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 Division of Water Rights","usgsCitation":"Blanchard, P.J., 1986, Ground-water conditions in the Lake Powell area, Utah: Technical Publication 84, vi, 64 p.","productDescription":"vi, 64 p.","numberOfPages":"70","costCenters":[{"id":610,"text":"Utah Water Science 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37.00035919622158\n ]\n ]\n ]\n }\n }\n ]\n}","publicComments":"This report supersedes open-file report 85-93.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"512c960fe4b0855fde6697bd","contributors":{"authors":[{"text":"Blanchard, Paul J.","contributorId":24388,"corporation":false,"usgs":true,"family":"Blanchard","given":"Paul","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":474688,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70044324,"text":"70044324 - 1986 - Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole Counties, Oklahoma","interactions":[{"subject":{"id":20205,"text":"ofr84445 - 1984 - Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole counties, Oklahoma","indexId":"ofr84445","publicationYear":"1984","noYear":false,"title":"Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole counties, Oklahoma"},"predicate":"SUPERSEDED_BY","object":{"id":70044324,"text":"70044324 - 1986 - Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole Counties, Oklahoma","indexId":"70044324","publicationYear":"1986","noYear":false,"title":"Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole Counties, Oklahoma"},"id":1}],"lastModifiedDate":"2013-03-02T14:44:35","indexId":"70044324","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":244,"text":"Circular","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"89","title":"Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole Counties, Oklahoma","docAbstract":"A study of water-quality degradation due to brine contamination was made in an area of ~1,700 mi2 in east-central Oklahoma. The study area coincides in part with the outcrop of the Vamoosa-Ada aquifer of Pennsylvanian age.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","collaboration":"Prepared by the United States Geological Survey in cooperation with the Oklahoma Geological Survey","usgsCitation":"Morton, R.B., 1986, Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole Counties, Oklahoma: Circular 89, iii, 38 p.; Map: 1 Sheet.","productDescription":"iii, 38 p.; Map: 1 Sheet","startPage":"i","endPage":"38","numberOfPages":"42","costCenters":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"links":[{"id":268663,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268661,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/circular89mm.pdf"},{"id":268662,"type":{"id":17,"text":"Plate"},"url":"https://www.ogs.ou.edu/pubsscanned/CircularsPlates/C89P1.pdf"}],"country":"United States","state":"Oklahoma","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.62 ], [ -103.0,37.0 ], [ -94.43,37.0 ], [ -94.43,33.62 ], [ -103.0,33.62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51332d74e4b0c316aaf0681d","contributors":{"authors":[{"text":"Morton, Robert B.","contributorId":50899,"corporation":false,"usgs":true,"family":"Morton","given":"Robert","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":475292,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70038342,"text":"70038342 - 1986 - Water resources inventory of Connecticut Part 9: Farmington River basin","interactions":[],"lastModifiedDate":"2015-11-30T10:06:57","indexId":"70038342","displayToPublicDate":"2012-05-01T10:47:00","publicationYear":"1986","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":"29","title":"Water resources inventory of Connecticut Part 9: Farmington River basin","docAbstract":"The Farmington River basin covers 435 square miles in north-central Connecticut upstream from Tariffville and downstream of the Massachusetts state line. Most water in the basin is derived from precipitation, which averages 48 inches (366 billion gallons) per year. An additional 67 billion gallons of water per year enters the basin from Massachusetts in the West Branch of the Farmington River, Hubbard River, Valley Brook and some smaller streams. Of the total 433 billion gallons, 174 billion gallons returns to the atmosphere through evaporation and transpiration. 239 billion gallons flows out of the study area in the Farmington River at Tariffville, and 20 billion gallons is diverted for Hartford water supply. Variations in streamflow at 23 continuous-record gaging stations are summarized in standardized graphs and tables that can be used to estimate streamflow characteristics at other sites. For example, mean flow and low-flow characteristics such as the 7-day annual minimum flow for 2-year and 10-year recurrence intervals, have been determined for many partial-record stations from the data for the 23 continuous-record stations. Of the 31 principal lakes, ponds, and reservoirs in the basin, eight have usable storage capacities of more than 1 billion gallons. Two of the largest, Colebrook River Lake and Barkhamsted Reservoir, have more than 30 billion gallons usable storage. Floods have occurred in the area in every month of the year. The greatest known flood on the Farmington River was in August 1955, which had a peak flow of 140,000 cubic feet per second at Collinsville. Since then, three major floodcontrol reservoirs have been constructed to reduce the hazards of high streamflow. The major aquifers underlying the basin are composed of unconsolidated materials (stratified drift and till) and bedrock (sedimentary, igneous, and metamorphic). Stratified drift overlies till and bedrock in valleys and lowlands; it averages about 90 feet in thickness, and is capable of large sustained yields of water to individual wells. Based on hydrologic characteristics and available recharge, sixteen stratified-drift areas are selected as the most favorable for large-scale development. Potential yields can be estimated by several methods. Small water supplies can be obtained from all aquifers. Wells in bedrock yield at least one to two gallons per minute at most sites. The probability of adequate yields for domestic supply is greater from sedimentary than from crystalline bedrock and is also greater from stratified-drift overburden than from till. The quality of water from all sources in the basin is good except where adversely affected by swamp drainage, aquifer composition or human activities. The water is generally low in dissolved-solids concentration and is soft to moderately hard. Surface water is less mineralized than ground water, especially during high-flow conditions when it is primarily direct runoff. Samples of water collected from 20 streams during high flow had 34 mg/L median dissolved-solids concentration and 16 mg/L median hardness. Samples collected from the same sites at low flow had 52 mg/L median dissolved solids and 28 mg/L median hardness. In contrast, water from wells had 112 mg/L median dissolved-solids concentration and 60 mg/L median hardness. Iron and manganese occur in objectionable concentrations ~n a few parts of the basin where streams drain swamps and aquifers are rich in iron- and manganese-bearing minerals. Five percent of streams at high flow, 21 percent at low flow, and 7 percent of ground-water samples contained iron in sufficient concentration to cause stains on plumbing fixtures and laundry. Human activities have modified the quality of water in parts of the basin. The high bacterial content of the Pequabuck River. and the high nitrate and chloride concentrations in some ground-water samples, are evidence of man’s influence. The quantity and quality of water in the basin’s streams and aquifers are satisfactory for a wide variety of uses. and, with suitable treatment, may be used for most purposes. The total amount of water used by 21 principal public supplies within the basin was 29 billion gallons in 1970. About 70 percent of this was used for domestic and commercial purposes, and nearly 30 percent was used by industry. Analyses of water from these systems show good quality.
","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":"Handman, E.H., Haeni, F.P., and Thomas, M.P., 1986, Water resources inventory of Connecticut Part 9: Farmington River basin: Connecticut Water Resources Bulletin 29, Report: viii, 91 p.; 4 Plates: 38.67 x 42.36 inches and smaller.","productDescription":"Report: viii, 91 p.; 4 Plates: 38.67 x 42.36 inches and smaller","numberOfPages":"101","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":286022,"rank":6,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70038342.jpg"},{"id":311385,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70038342/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":286018,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038342/plate-a.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":286021,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038342/plate-d.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":286019,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038342/plate-b.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":286020,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038342/plate-c.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","country":"United States","state":"Connecticut","otherGeospatial":"Farmington River Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -73.30215454101562,\n 41.53839396783225\n ],\n [\n -73.30215454101562,\n 42.04317376494972\n ],\n [\n -72.68280029296875,\n 42.04317376494972\n ],\n [\n -72.68280029296875,\n 41.53839396783225\n ],\n [\n -73.30215454101562,\n 41.53839396783225\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bcb7fe4b08c986b32d69f","contributors":{"authors":[{"text":"Handman, Elinor H.","contributorId":31748,"corporation":false,"usgs":true,"family":"Handman","given":"Elinor","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":463911,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haeni, F. 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A distinguishing characteristic of a topographic map is the portrayal of the shape and elevation of the terrain by contour lines.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039570","usgsCitation":"Steger, T.D., 1986, Topographic maps: Monograph, 27 p.; col. ill.; maps (col.), https://doi.org/10.3133/70039570.","productDescription":"27 p.; col. ill.; maps (col.)","numberOfPages":"28","costCenters":[],"links":[{"id":261085,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039570/report.pdf"},{"id":261086,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039570/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb4d6e4b08c986b326594","contributors":{"authors":[{"text":"Steger, Theodore D.","contributorId":28473,"corporation":false,"usgs":true,"family":"Steger","given":"Theodore","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":466496,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70006875,"text":"70006875 - 1986 - Immersion treatments against the Asian tapeworm (Bothriocephalus opsarichthydis) in grass carp","interactions":[],"lastModifiedDate":"2012-07-17T01:01:41","indexId":"70006875","displayToPublicDate":"2012-01-01T15:19:36","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1649,"text":"Fish Health Section Newsletter","active":true,"publicationSubtype":{"id":10}},"title":"Immersion treatments against the Asian tapeworm (Bothriocephalus opsarichthydis) in grass carp","docAbstract":"No abstract available at this time.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fish Health Section Newsletter","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Fisheries Society","publisherLocation":"Bethesda, MD","collaboration":"None","usgsCitation":"Mitchell, A., 1986, Immersion treatments against the Asian tapeworm (Bothriocephalus opsarichthydis) in grass carp: Fish Health Section Newsletter, v. 14, no. 2, p. 5-5.","productDescription":"1 p.","startPage":"5","endPage":"5","numberOfPages":"1","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":258937,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a388fe4b0c8380cd615fc","contributors":{"authors":[{"text":"Mitchell, A.J.","contributorId":16345,"corporation":false,"usgs":true,"family":"Mitchell","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":355386,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70006386,"text":"70006386 - 1986 - Book Review: Diseases of marine animals: Introduction, Pisces; Volume IV, Part I","interactions":[],"lastModifiedDate":"2012-09-06T01:02:24","indexId":"70006386","displayToPublicDate":"2012-01-01T15:15:07","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1657,"text":"Fisheries","onlineIssn":"1548-8446","printIssn":"0363-2415","active":true,"publicationSubtype":{"id":10}},"title":"Book Review: Diseases of marine animals: Introduction, Pisces; Volume IV, Part I","docAbstract":"As stated in Volume 1, Diseases of Marine Animals was originally planned as a contribution to Marine Ecology, Volume III Cultivation.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fisheries","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor & Francis Online","publisherLocation":"Philadelphia, PA","doi":"10.1577/1548-8446-11-4","collaboration":"None","usgsCitation":"Bullock, G.L., and Herman, R.L., 1986, Book Review: Diseases of marine animals: Introduction, Pisces; Volume IV, Part I: Fisheries, v. 11, no. 4, p. 63-63, https://doi.org/10.1577/1548-8446-11-4.","productDescription":"1 p.","startPage":"63","endPage":"63","numberOfPages":"1","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":260239,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":260212,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/1548-8446-11-4","linkFileType":{"id":5,"text":"html"}}],"volume":"11","issue":"4","noUsgsAuthors":false,"publicationDate":"1986-07-01","publicationStatus":"PW","scienceBaseUri":"5059f1ffe4b0c8380cd4af5c","contributors":{"authors":[{"text":"Bullock, G. L.","contributorId":69498,"corporation":false,"usgs":true,"family":"Bullock","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":354421,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Herman, R. L.","contributorId":21101,"corporation":false,"usgs":true,"family":"Herman","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":354420,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70006772,"text":"70006772 - 1986 - Energy budget and prey requirements of breeding lapland longspurs Calcarius lapponicus near Barrow Alaska, U.S.A.","interactions":[],"lastModifiedDate":"2017-05-04T16:23:15","indexId":"70006772","displayToPublicDate":"2012-01-01T14:43:43","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":898,"text":"Arctic and Alpine Research","active":true,"publicationSubtype":{"id":10}},"title":"Energy budget and prey requirements of breeding lapland longspurs Calcarius lapponicus near Barrow Alaska, U.S.A.","docAbstract":"Breeding Lapland longspurs, Calcarius lapponicus, near Barrow, Alaska, have relatively constant energy demands throughout the summer; the average estimated daily energy budgets (DEBs) were 132 and 118 kJ for the male and female. Thermoregulation accounted consistently for one-quarter to one-third of the total DEB. Flight in the male and incubation in the female were major components of the DEB early in the season, whereas cost of molt was a major component for both sexes near the end of the season. Our estimates of longspur DEB based on a time-activity approach were similar to those based on a cage existence model. Minor differences are explained by increased male territorial activity, by energy savings of the female during incubation, and by contraction of the molt for both sexes within the short summer season. Male and female longspurs were estimated to capture 3000 to 10,000 seeds and insects d-1 (3-20 items min-1 foraging) for self maintenance while in summer residence near Barrow. Each adult was estimated to capture an additional 3000 insects d-1 ( 6-7 insects min-1 foraging) during the peak energy requirements to raise five young. While raising young, the maximum required capture rate of prey per time foraging for each adult occurred during the nestling stage; young are just achieving independence, however, when food supply is at a maximum.
","language":"English","publisher":"INSTAAR, University of Colorado","publisherLocation":"Boulder, CO","doi":"10.2307/1551091","usgsCitation":"Custer, T., Osborn, R.G., Pitelka, F., and Gessaman, J., 1986, Energy budget and prey requirements of breeding lapland longspurs Calcarius lapponicus near Barrow Alaska, U.S.A.: Arctic and Alpine Research, v. 18, no. 4, p. 415-428, https://doi.org/10.2307/1551091.","productDescription":"14 p.","startPage":"415","endPage":"428","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":258934,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","city":"Barrow","volume":"18","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0945e4b0c8380cd51e4f","contributors":{"authors":[{"text":"Custer, T. W. 0000-0003-3170-6519","orcid":"https://orcid.org/0000-0003-3170-6519","contributorId":91802,"corporation":false,"usgs":true,"family":"Custer","given":"T. W.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":355188,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Osborn, R. G.","contributorId":76700,"corporation":false,"usgs":false,"family":"Osborn","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":355187,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pitelka, F.A.","contributorId":7676,"corporation":false,"usgs":true,"family":"Pitelka","given":"F.A.","email":"","affiliations":[],"preferred":false,"id":355185,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gessaman, J.A.","contributorId":14910,"corporation":false,"usgs":true,"family":"Gessaman","given":"J.A.","affiliations":[],"preferred":false,"id":355186,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70006870,"text":"70006870 - 1986 - Effect of injected rotenone on the production and composition of urine from the rainbow trout (Salmo gairdneri)","interactions":[],"lastModifiedDate":"2012-07-14T01:01:39","indexId":"70006870","displayToPublicDate":"2012-01-01T14:40:38","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":874,"text":"Aquatic Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Effect of injected rotenone on the production and composition of urine from the rainbow trout (Salmo gairdneri)","docAbstract":"Renal function was evaluated in adult rainbow trout (Salmo gairdneri) dosed i.a. with rotenone at 225 and 275 μg/kg. The chemical composition of urine samples and urine flow rates collected over a 5-h pretreatment period were compared with hourly urine samples collected over a 5-h posttreatment period. Significant increases in osmolality and in concentrations of sodium, potassium, chloride, glucose, and total protein were observed in the urine of treated fish. Urine solute concentrations reached maximum values within 1 to 3 h after treatment and decreased thereafter, indicating that the effects were reversible. Concentrations of sodium and chloride were highly correlated in 2-h posttreatment urine samples at the low (r = 0.922) and high (r = 0.981) rotenone treatments. Urine flow rates were reduced in trout at each dose of rotenone but the decrease in volume of urine voided was not dose-dependent. In a separate study, [14C]polyethylene glycol was used as a filtration marker to determine the effect of rotenone treatment (225 &mu:g/kg) on urine flow rate, glomerular filtration rate, and renal water reabsorption. We showed that posttreatment urine flow rates were reduced partly by reduced glomerular filtration and partly by increased water reabsorption. Transient increases in plasma osmolality and hematocrit also were observed 0.5 h after rotenone treatment.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Aquatic Toxicology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0166-445X(86)90014-7","collaboration":"Abstract has subscript/superscript to be fixed","usgsCitation":"Erickson, D., and Gingerich, W., 1986, Effect of injected rotenone on the production and composition of urine from the rainbow trout (Salmo gairdneri): Aquatic Toxicology, v. 9, no. 4-5, p. 263-274, https://doi.org/10.1016/0166-445X(86)90014-7.","productDescription":"12 p.","startPage":"263","endPage":"274","numberOfPages":"12","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":258894,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":258873,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0166-445X(86)90014-7","linkFileType":{"id":5,"text":"html"}}],"volume":"9","issue":"4-5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a05eee4b0c8380cd51028","contributors":{"authors":[{"text":"Erickson, D.A.","contributorId":96942,"corporation":false,"usgs":true,"family":"Erickson","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":355383,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gingerich, W.H.","contributorId":83481,"corporation":false,"usgs":true,"family":"Gingerich","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":355382,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70006493,"text":"70006493 - 1986 - Liquid chromatography of hydrocarbonaeous quaternary amines on cyclodextrin bonded silica","interactions":[],"lastModifiedDate":"2024-04-16T23:08:30.505957","indexId":"70006493","displayToPublicDate":"2012-01-01T14:11:57","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2213,"text":"Journal of Chromatography","active":true,"publicationSubtype":{"id":10}},"title":"Liquid chromatography of hydrocarbonaeous quaternary amines on cyclodextrin bonded silica","docAbstract":"Mixtures of n-alkylbenzyldimethylammonium chloride (ABDAC) were resolved into homologous components by high-performance liquid chromatography (HPLC) with a cyclodextrin-bonded silica stationary phase. With a few exceptions, results from this study are similar to those obtained from traditional reversed-phase HPLC. It was found that the presence of electrolytes in aqueous mobile phases is not a critical factor in determining the success of HPLC separation. Under normal HPLC conditions, a mobile phase consisting of either methanol—water (50:50) or acetonitrile—water (30:70) was employed for obtaining adequate resolution of the quaternary ammonium mixtures. Although the percent organic modifier—water profiles were similar to those in previous studies with these compounds, resolution (R) and selectivity (α) parameters were found to be quite susceptible to changes in the mobile phase solvent composition. The retention behavior of the cationic analytes in the homologous series is consistent with the hydrophobic-interaction concept proposed for the retention mechanism via dominant inclusion complex formation. Several electolytes were chosen for a study of the counter ion effect on the chromatographic characteristics of ABDAC components. Among the electrolytes examined, the perchlorate ion was found most likely to act as an ion-pairing counter ion for ammonium cations in the HPLC system studied. A correlation study established linear relationships between the chain length of ABDAC and the logarithmic capacity factor (k′). The analytical utility of the HPLC method was demonstrated by the analysis of various unknown mixtures.
","language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/S0021-9673(01)86948-X","usgsCitation":"Abidi, S.L., 1986, Liquid chromatography of hydrocarbonaeous quaternary amines on cyclodextrin bonded silica: Journal of Chromatography, v. 362, no. 1, p. 33-46, https://doi.org/10.1016/S0021-9673(01)86948-X.","productDescription":"14 p.","startPage":"33","endPage":"46","numberOfPages":"14","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":259538,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"362","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a47fce4b0c8380cd67b30","contributors":{"authors":[{"text":"Abidi, S. 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1986 - Squash plate technique for identifying or detecting intestinal worms","interactions":[],"lastModifiedDate":"2012-08-16T01:02:05","indexId":"70006876","displayToPublicDate":"2012-01-01T13:07:03","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1649,"text":"Fish Health Section Newsletter","active":true,"publicationSubtype":{"id":10}},"title":"Squash plate technique for identifying or detecting intestinal worms","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fish Health Section Newsletter","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Fisheries Society","publisherLocation":"Bethesda, MD","collaboration":"None","usgsCitation":"Mitchell, A., 1986, Squash plate technique for identifying or detecting intestinal worms: Fish Health Section Newsletter, v. 14, no. 2, p. 7-7.","productDescription":"1 p.","startPage":"7","endPage":"7","numberOfPages":"1","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":259651,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9639e4b08c986b31b38e","contributors":{"authors":[{"text":"Mitchell, A.J.","contributorId":16345,"corporation":false,"usgs":true,"family":"Mitchell","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":355387,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70039038,"text":"70039038 - 1986 - United States Geological Survey Yearbook, fiscal year 1985","interactions":[],"lastModifiedDate":"2017-03-08T16:22:17","indexId":"70039038","displayToPublicDate":"2012-01-01T12:35:55","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":392,"text":"Yearbook","active":false,"publicationSubtype":{"id":6}},"title":"United States Geological Survey Yearbook, fiscal year 1985","docAbstract":"The fiscal year 1985 Yearbook summarizes the activities of the U.S. Geological Survey in response to its scientific and regulatory missions.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039038","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, United States Geological Survey Yearbook, fiscal year 1985: Yearbook, vi, 143 p., https://doi.org/10.3133/70039038.","productDescription":"vi, 143 p.","costCenters":[],"links":[{"id":261281,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039038/report.pdf","text":"Report","size":"51.64 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":261282,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039038/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbc94e4b08c986b328d07","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535207,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70006829,"text":"70006829 - 1986 - Persistence of rotenone in ponds at different temperatures","interactions":[],"lastModifiedDate":"2012-07-07T01:01:38","indexId":"70006829","displayToPublicDate":"2012-01-01T11:31:00","publicationYear":"1986","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":"Persistence of rotenone in ponds at different temperatures","docAbstract":"Two ponds were treated with liquid rotenone (5% rotenone), one with 3 mg/L at 24°C and the other with 2 mg/L at 0°C (concentrations of active rotenone were 0.15 and 0.10 mg/L, respectively). Water samples were collected and analyzed by high-performance liquid chromatography. The concentration of rotenone declined to 0.02 mg/L in 48 h in warm water and in 11 d in cold water. The half-life of rotenone was calculated at 13.9 h in warm water and 83.9 h in cold water.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"North American Journal of Fisheries Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor & Francis","publisherLocation":"Philadelphia, PA","doi":"10.1577/1548-8659(1986)6<129:PORIPA>2.0.CO;2","collaboration":"Abstract has subscript/superscript to be fixed","usgsCitation":"Gilderhus, P., Allen, J.L., and Dawson, V.K., 1986, Persistence of rotenone in ponds at different temperatures: North American Journal of Fisheries Management, v. 6, no. 1, p. 129-130, https://doi.org/10.1577/1548-8659(1986)6<129:PORIPA>2.0.CO;2.","productDescription":"2 p.","startPage":"129","endPage":"130","numberOfPages":"2","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":258238,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":258228,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/1548-8659(1986)6<129:PORIPA>2.0.CO;2","linkFileType":{"id":5,"text":"html"}}],"volume":"6","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a76f0e4b0c8380cd783a3","contributors":{"authors":[{"text":"Gilderhus, P.A.","contributorId":60156,"corporation":false,"usgs":true,"family":"Gilderhus","given":"P.A.","affiliations":[],"preferred":false,"id":355311,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allen, J. L.","contributorId":49295,"corporation":false,"usgs":true,"family":"Allen","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":355310,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dawson, V. K.","contributorId":48900,"corporation":false,"usgs":true,"family":"Dawson","given":"V.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":355309,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}