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The report is a summary of data collected under the Utah Water Use program, a cooperative program between the Utah Division of Water Rights and the United States Geological Survey (USGS)</span></p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, Utah","collaboration":"Prepared in cooperation with the Utah Division of Water Rights","usgsCitation":"Utah Department of Natural Resources, Division of Water Rights, 1989, Water use data for public water suppliers and self supplied industry in Utah: 1986, 1987: Utah Division of Water Rights Water-Use Report 7, viii, 120 p.","productDescription":"viii, 120 p.","numberOfPages":"132","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333293,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333292,"rank":1,"type":{"id":15,"text":"Index 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,{"id":70179031,"text":"70179031 - 1989 - Seepage study of the South Bend, Richfield, and Vermillion Canals, Sevier County, Utah","interactions":[],"lastModifiedDate":"2016-12-28T12:33:46","indexId":"70179031","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1989","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":"97","title":"Seepage study of the South Bend, Richfield, and Vermillion Canals, Sevier County, Utah","docAbstract":"<p>A seepage investigation was made in 1987 on selected reaches of the South Bend, Richfield, and Vermillion Canals in Sevier County, Utah, to determine gains or losses in discharge. &nbsp;Fluctuations in discharge were adjusted using information from stage recorders operated at selected locations during each set of discharge measurements. The investigation showed a net gain of 0.2 cubic foot per second in the South Bend canal: the upper reach gained 1.5 cubic feet per second, the two middle reaches together lost 2.5 cubic feet per second, and the lower reach gained 1.2 cubic feet per second. &nbsp;The Richfield Canal showed a net loss of 2.4 cubic feet per second: the two upper reaches together lost 4.4 cubic feet per second and the two lower reaches together gained 2.0 cubic feet per second. &nbsp;The Vermillion canal showed a net loss of 0.2 cubic foot per second: the upper reach gained 2.3 cubic feet per second and the lower reach lost 2.5 cubic feet per second.</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United State Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Herbert, L.R., and Smith, G.J., 1989, Seepage study of the South Bend, Richfield, and Vermillion Canals, Sevier County, Utah: Technical Publication 97, iv, 50 p.","productDescription":"iv, 50 p.","numberOfPages":"54","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":332071,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":332070,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/y920/y9200005.pdf"},{"id":332069,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-6-420"}],"country":"United States","state":"Utah","county":"Sevier County","otherGeospatial":"Richfield Canal, South Bend Canal, Vermillion Canal","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.25,\n              38\n            ],\n            [\n              -112.25,\n              39\n            ],\n            [\n              -111.9,\n              39\n            ],\n            [\n              -111.9,\n              38\n            ],\n            [\n              -112.25,\n              38\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"585116bee4b08138bf1abd6e","contributors":{"authors":[{"text":"Herbert, L. R.","contributorId":39865,"corporation":false,"usgs":true,"family":"Herbert","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":655825,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, G. J.","contributorId":80767,"corporation":false,"usgs":true,"family":"Smith","given":"G.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":655826,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70176576,"text":"70176576 - 1989 - Glacier outburst floods at Mount Rainier, Washington State, U.S.A.","interactions":[],"lastModifiedDate":"2023-01-31T02:26:35.978155","indexId":"70176576","displayToPublicDate":"2016-09-21T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":794,"text":"Annals of Glaciology","active":true,"publicationSubtype":{"id":10}},"title":"Glacier outburst floods at Mount Rainier, Washington State, U.S.A.","docAbstract":"<p>During the twentieth century, glacial outburst floods have been the most destructive natural events on Mount Rainier, a stratovolcano in the Cascade Range in Washington State, U.S.A. In the period between 1930 and 1980 numerous floods were reported from five glaciers on the mountain, most of which flowed from Nisqually, Kautz, or South Tahoma Glaciers on its southern flank. Such floods threaten lives and property because they occur without warning and quickly mobilize the loose volcanic debris into debris flows.</p><p>A monitoring program was begun in 1987 which was designed to measure the dimensions and timing of outburst floods, but this has been unsuccessful because no floods have yet occurred on the monitored streams. Four floods did burst from South Tahoma Glacier that was unmonitored, but in spite of this they have been useful in providing evidence of flood storage and release mechanisms. All flood volumes were found to be of approximately similar orders of magnitude, of 1 × 10<span class=\"sup\">5</span><span>&nbsp;</span>m<span class=\"sup\">3</span><span>&nbsp;</span>of water, indicating that all floods probably had similar mechanisms for storage and release of water. Hydraulic pressure considerations indicate that such a large volume of flood water would be stored at the bed of the glacier rather than in isolated englacial cavities. The stepped bedrock terrain provides an ideal setting for the formation of subglacial cavities capable of storing the volumes of flood water noted.</p>","language":"English","publisher":"Cambridge University Press","publisherLocation":"Cambridge, UK","doi":"10.3189/S0260305500007631","usgsCitation":"Driedger, C.L., and Fountain, A.G., 1989, Glacier outburst floods at Mount Rainier, Washington State, U.S.A.: Annals of Glaciology, v. 13, p. 51-55, https://doi.org/10.3189/S0260305500007631.","productDescription":"5 p.","startPage":"51","endPage":"55","costCenters":[],"links":[{"id":479860,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3189/s0260305500007631","text":"Publisher Index Page"},{"id":328829,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Cascade Range, Mount Rainier","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.95373535156249,\n              46.73091909829101\n            ],\n            [\n              -121.95373535156249,\n              46.945105998259315\n            ],\n            [\n              -121.56852722167967,\n              46.945105998259315\n            ],\n            [\n              -121.56852722167967,\n              46.73091909829101\n            ],\n            [\n              -121.95373535156249,\n              46.73091909829101\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"13","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"57febcefe4b0824b2d156f08","contributors":{"authors":[{"text":"Driedger, Carolyn L. 0000-0002-4011-4112 driedger@usgs.gov","orcid":"https://orcid.org/0000-0002-4011-4112","contributorId":537,"corporation":false,"usgs":true,"family":"Driedger","given":"Carolyn","email":"driedger@usgs.gov","middleInitial":"L.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":649245,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fountain, A. G.","contributorId":29815,"corporation":false,"usgs":true,"family":"Fountain","given":"A.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":649246,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70178058,"text":"70178058 - 1989 - Dynamic pore-pressure fluctuations in rapidly shearing granular materials","interactions":[],"lastModifiedDate":"2021-12-20T22:26:48.2075","indexId":"70178058","displayToPublicDate":"2015-10-29T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Dynamic pore-pressure fluctuations in rapidly shearing granular materials","docAbstract":"<div id=\"abstracts\"><div class=\"core-container\"><div>Results from two types of experiments show that intergranular pore pressures fluctuated dynamically during rapid, steady shear deformation of water-saturated granular materials. During some fluctuations, the pore water locally supported all normal and shear stresses, while grain-contact stresses transiently fell to zero. Fluctuations also propagated outward from the shear zone; this process modifies grain-contact stresses in adjacent areas and potentially instigates shear-zone growth.</div></div></div>","language":"English","publisher":"American Association for the Advancement of Science","publisherLocation":"Washington, D.C.","doi":"10.1126/science.246.4931.796","usgsCitation":"Iverson, R.M., and Lahusen, R.G., 1989, Dynamic pore-pressure fluctuations in rapidly shearing granular materials: Science, v. 246, no. 4831, p. 796-799, https://doi.org/10.1126/science.246.4931.796.","productDescription":"4 p.","startPage":"796","endPage":"799","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":330633,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"246","issue":"4831","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5819a9c5e4b0bb36a4c91039","contributors":{"authors":[{"text":"Iverson, Richard M. 0000-0002-7369-3819 riverson@usgs.gov","orcid":"https://orcid.org/0000-0002-7369-3819","contributorId":536,"corporation":false,"usgs":true,"family":"Iverson","given":"Richard","email":"riverson@usgs.gov","middleInitial":"M.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"preferred":true,"id":652676,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lahusen, Richard G. rlahusen@usgs.gov","contributorId":535,"corporation":false,"usgs":true,"family":"Lahusen","given":"Richard","email":"rlahusen@usgs.gov","middleInitial":"G.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":652677,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70162026,"text":"70162026 - 1989 - Comparison of infectious hematopoietic necrosis in natural and experimental infections of spawning salmonids by infectivity and immunohistochemistry","interactions":[],"lastModifiedDate":"2016-01-12T09:56:23","indexId":"70162026","displayToPublicDate":"2015-10-13T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Comparison of infectious hematopoietic necrosis in natural and experimental infections of spawning salmonids by infectivity and immunohistochemistry","docAbstract":"<p><span>Infectious hematopoietic necrosis (IHN) continues to be a serious virus disease of salmonids with epizootics recorded in both wild and hatchery populations (Williams and Amend 1976; Carlisle et al 1979; Groberg and Fryer 1983; Saft and Pratt 1986; Traxler 1987; Follett et al 1987; Meyers et al 1988). While originally enzootic in western North America, the virus appears to be spreading further (Sano et al 1977; de Kinkelin et al 1987; Bovo et al 1987). In hatchery outbreaks occurring in regions where the virus is not enzootic, it is often possible to trace the virus to the importation of infected fingerlings or contaminated eggs. In regions where the virus is widespread among stocks of fish, the source of virus infection is more difficult to establish particularly in watersheds where there are anadromous salmonids. Although salmonid fish surviving infection as fry and returning from the ocean to spawn are considered to be parental carriers of IHNV, there is very little data to support this hypothesis. Amend (1975) in the study of rainbow trout reported that in a population surviving infection and assayed a few years later found that a few trout were carrying virus. This is the study often cited as evidence for the carrier status of returning salmonids. LaPatra et al (1987) presented data that indicated IHNV has been transmitted horizontally through water from adult chinook salmon (Oncorhynchus tshawytscha) to adult coho salmon (O. kisutch) at a hatchery in northern California. They suggested that horizontal transmission may be an important means for perpetuating IHN. However, the actual mechanisms for persistence and transmission of IHN among fish in a watershed is likely to be complex and involve multiple species and age groups as well as intermediate vectors and/or reservoirs.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Viruses of Lower Vertebrates","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Springer","isbn":"978-3-642-83727-2","usgsCitation":"Yamamoto, T., Arakawa, C., Batts, W., and Winton, J., 1989, Comparison of infectious hematopoietic necrosis in natural and experimental infections of spawning salmonids by infectivity and immunohistochemistry, chap. <i>of</i> Viruses of Lower Vertebrates, p. 411-429.","productDescription":"19 p.","startPage":"411","endPage":"429","numberOfPages":"19","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314206,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":314205,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.springer.com/us/book/9783642837296"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569631bbe4b039675d00a3c6","contributors":{"authors":[{"text":"Yamamoto, T.","contributorId":152174,"corporation":false,"usgs":false,"family":"Yamamoto","given":"T.","email":"","affiliations":[],"preferred":false,"id":588364,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Arakawa, C.K.","contributorId":152140,"corporation":false,"usgs":false,"family":"Arakawa","given":"C.K.","email":"","affiliations":[],"preferred":false,"id":588365,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Batts, W.N. 0000-0002-6469-9004","orcid":"https://orcid.org/0000-0002-6469-9004","contributorId":51043,"corporation":false,"usgs":true,"family":"Batts","given":"W.N.","affiliations":[],"preferred":false,"id":588366,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Winton, J. R. 0000-0002-3505-5509","orcid":"https://orcid.org/0000-0002-3505-5509","contributorId":82441,"corporation":false,"usgs":true,"family":"Winton","given":"J. R.","affiliations":[],"preferred":false,"id":588367,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70161954,"text":"70161954 - 1989 - Enhanced detection of infectious hematopoietic necrosis virus by pretreatment of cell monolayers with polyethylene glycol","interactions":[],"lastModifiedDate":"2016-01-11T10:52:21","indexId":"70161954","displayToPublicDate":"2015-09-21T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2177,"text":"Journal of Aquatic Animal Health","active":true,"publicationSubtype":{"id":10}},"title":"Enhanced detection of infectious hematopoietic necrosis virus by pretreatment of cell monolayers with polyethylene glycol","docAbstract":"<p class=\"last\">To improve quantification of very low levels of infectious hematopoietic necrosis virus (IHNV) in samples of tissue, ovarian fluid, or natural water supplies, we tested the ability of polyethylene glycol (PEG) to enhance the sensitivity and speed of the plaque assay system. We compared 4, 7, and 10% solutions of PEG of molecular weight 6,000, 8,000, or 20,000 applied at selected volumes and for various durations. When cell monolayers of epithelioma papulosum cyprini (EPC), fathead minnow (FHM), chinook salmon embryo (CHSE-214), and bluegill fry (BF2) were pretreated with 7% PEG-20,000, they produced 4-17-fold increases in plaque assay titers of IHNV. The plaque assay titers of viral hemorrhagic septicemia virus, chum salmon reovirus, and chinook salmon paramyxovirus were also enhanced by exposure of CHSE-214 cells to PEG, but the titers of infectious pancreatic necrosis virus and <i>Oncorhynchus masou</i> virus were not substantially changed. Plaques formed by IHNV on PEG-treated EPC cells incubated at 15°C had a larger mean diameter at 6 d than those on control cells at 8 d; this suggests the assay could be shortened by use of PEG. Pretreatment of EPC cell monolayers with PEG enabled detection of IHNV in some samples that appeared negative with untreated cells. For example, when ovarian fluid samples from chinook salmon <i>Oncorhynchus tshawytscha</i> were inoculated onto untreated monolayers of EPC cells, IHNV was detected in only 11 of 51 samples; 17 of the samples were positive when PEG-treated EPC cells were used.</p><div class=\"access\"><ul class=\"clear top_article_links\"><li><div class=\"showDownloadPopup-detailbtns_bold_face\"><a class=\"showDownloadPopup pdf\" href=\"http://www.tandfonline.com/doi/abs/10.1577/1548-8667%281989%29001%3C0284%3AEDOIHN%3E2.3.CO%3B2#aHR0cDovL3d3dy50YW5kZm9ubGluZS5jb20vZG9pL3BkZi8xMC4xNTc3LzE1NDgtODY2NyUyODE5ODklMjkwMDElM0MwMjg0JTNBRURPSUhOJTNFMi4zLkNPJTNCMkBAQDA=\" data-mce-href=\"http://www.tandfonline.com/doi/abs/10.1577/1548-8667%281989%29001%3C0284%3AEDOIHN%3E2.3.CO%3B2#aHR0cDovL3d3dy50YW5kZm9ubGluZS5jb20vZG9pL3BkZi8xMC4xNTc3LzE1NDgtODY2NyUyODE5ODklMjkwMDElM0MwMjg0JTNBRURPSUhOJTNFMi4zLkNPJTNCMkBAQDA=\">PDF</a></div></li></ul></div>","language":"English","publisher":"Taylor and Francis","doi":"10.1577/1548-8667(1989)001<0284:EDOIHN>2.3.CO;2","usgsCitation":"Batts, W., and Winton, J., 1989, Enhanced detection of infectious hematopoietic necrosis virus by pretreatment of cell monolayers with polyethylene glycol: Journal of Aquatic Animal Health, v. 1, no. 4, p. 261-267, https://doi.org/10.1577/1548-8667(1989)001<0284:EDOIHN>2.3.CO;2.","productDescription":"7 p.","startPage":"261","endPage":"267","numberOfPages":"7","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314107,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5694e043e4b039675d005e1b","contributors":{"authors":[{"text":"Batts, W.N. 0000-0002-6469-9004","orcid":"https://orcid.org/0000-0002-6469-9004","contributorId":51043,"corporation":false,"usgs":true,"family":"Batts","given":"W.N.","affiliations":[],"preferred":false,"id":588186,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Winton, J. R. 0000-0002-3505-5509","orcid":"https://orcid.org/0000-0002-3505-5509","contributorId":82441,"corporation":false,"usgs":true,"family":"Winton","given":"J. R.","affiliations":[],"preferred":false,"id":588187,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70162020,"text":"70162020 - 1989 - Variation in capture efficiency of a beach seine for small fishes","interactions":[],"lastModifiedDate":"2016-01-12T09:11:17","indexId":"70162020","displayToPublicDate":"2015-09-21T00:00:00","publicationYear":"1989","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":"Variation in capture efficiency of a beach seine for small fishes","docAbstract":"<p><span>We determined the capture efficiency of a beach seine as a means of improving abundance estimates of small fishes in littoral areas. Capture efficiency for 14 taxa (individual species or species groups) was determined by seining within an enclosure at night over fine and coarse substrates in the John Day Reservoir, Oregon–Washington. Mean efficiency ranged from 12% for prickly sculpin </span><i>Cottus asper</i><span> captured over coarse substrates to 96% for peamouth </span><i>Mylocheilus caurinus</i><span> captured over fine substrates. Mean capture efficiency for a taxon (genus or species) was generally higher over fine substrates than over coarse substrates, although mean capture efficiencies over fine substrates were significantly greater for only 3 of 10 taxa. Capture efficiency generally was not influenced by fish density or by water temperature (range, 8–26°C). Conclusions about the relative abundance of taxa captured by seining can change substantially after capture efficiencies are taken into account.</span></p>","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8675(1989)009<0239:VICEOA>2.3.CO;2","usgsCitation":"Parsley, M., Palmer, D., and Burkhardt, R., 1989, Variation in capture efficiency of a beach seine for small fishes: North American Journal of Fisheries Management, v. 9, no. 2, p. 239-244, https://doi.org/10.1577/1548-8675(1989)009<0239:VICEOA>2.3.CO;2.","productDescription":"6 p.","startPage":"239","endPage":"244","numberOfPages":"6","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314197,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569631cee4b039675d00a3fe","contributors":{"authors":[{"text":"Parsley, M.J.","contributorId":59542,"corporation":false,"usgs":true,"family":"Parsley","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":588344,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Palmer, D.E.","contributorId":152169,"corporation":false,"usgs":false,"family":"Palmer","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":588345,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Burkhardt, R.W.","contributorId":152170,"corporation":false,"usgs":false,"family":"Burkhardt","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":588346,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70162016,"text":"70162016 - 1989 - Methods for developing new stocks of Atlantic salmon","interactions":[],"lastModifiedDate":"2016-01-11T15:25:30","indexId":"70162016","displayToPublicDate":"2015-09-15T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":8,"text":"Biological Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"89(12)","title":"Methods for developing new stocks of Atlantic salmon","docAbstract":"<p>The productivity of many streams in NewEngland for Atlantic salmon is being restored through abatement of water pollution and removal of barriers to migrating fish. As a result, interest is increasing in reestablishment of natural spawning runs of Atlantic salmon in some of these streams. I describe methods intended to help develop and maintain \"new\" stocks of these fish.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Atlantic Salmon Brood Stock Management and Breeding Handbook","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"U.S. Fish and Wildlife Service, 1989, Methods for developing new stocks of Atlantic salmon: Biological Report 89(12), 3 p.","productDescription":"3 p.","startPage":"19","endPage":"21","numberOfPages":"3","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314190,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5694e049e4b039675d005e37"}
,{"id":70161953,"text":"70161953 - 1989 - Concentration of infectious hematopoietic necrosis virus from water samples by tangential flow filtration and polyethylene glycol precipitation","interactions":[],"lastModifiedDate":"2016-01-11T10:44:32","indexId":"70161953","displayToPublicDate":"2015-09-08T00:00:00","publicationYear":"1989","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":"Concentration of infectious hematopoietic necrosis virus from water samples by tangential flow filtration and polyethylene glycol precipitation","docAbstract":"<p><span>Infectious hematopoietic necrosis virus (IHNV) was concentrated from water samples by polyethylene glycol (PEG) precipitation, tangential flow filtration (TFF), and by a combination of TFF followed by PEG precipitation of the retentate. Used alone, PEG increased virus titers more than 200-fold, and the efficiency of recovery was as great as 100%. Used alone, TFF concentrated IHNV more than 20-fold, and average recovery was 70%. When the two techniques were combined, 10-L water samples were reduced to about 300 mL by TFF and the virus was precipitated with PEG into a 1 to 2 g pellet; total recovery was as great as 100%. The combined techniques were used to isolate IHNV from water samples taken from a river containing adult sockeye salmon (</span><i>Oncorhynchus nerka</i><span>) and from a hatchery pond containing adult spring chinook salmon (</span><i>O</i><span>. </span><i>tshawytscha</i><span>). The combination of these methods was effective in concentrating and detecting IHNV from water containing only three infectious particles per 10-L sample.</span></p>","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/f89-125","usgsCitation":"Batts, W., and Winton, J., 1989, Concentration of infectious hematopoietic necrosis virus from water samples by tangential flow filtration and polyethylene glycol precipitation: Canadian Journal of Fisheries and Aquatic Sciences, v. 46 , no. 6, p. 964-968, https://doi.org/10.1139/f89-125.","productDescription":"5 p.","startPage":"964","endPage":"968","numberOfPages":"5","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314106,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46 ","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5694e03fe4b039675d005e02","contributors":{"authors":[{"text":"Batts, W.N. 0000-0002-6469-9004","orcid":"https://orcid.org/0000-0002-6469-9004","contributorId":51043,"corporation":false,"usgs":true,"family":"Batts","given":"W.N.","affiliations":[],"preferred":false,"id":588184,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Winton, J. R. 0000-0002-3505-5509","orcid":"https://orcid.org/0000-0002-3505-5509","contributorId":82441,"corporation":false,"usgs":true,"family":"Winton","given":"J. R.","affiliations":[],"preferred":false,"id":588185,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70161969,"text":"70161969 - 1989 -  A method to directly measure maximum volume of fish stomachs or digestive tracts","interactions":[],"lastModifiedDate":"2016-01-11T12:16:28","indexId":"70161969","displayToPublicDate":"2015-08-04T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2285,"text":"Journal of Fish Biology","active":true,"publicationSubtype":{"id":10}},"title":" A method to directly measure maximum volume of fish stomachs or digestive tracts","docAbstract":"<p><span>A new method for measuring maximum stomach or digestive tract volume of fish incorporates air injection at constant pressure with water displacement to measure directly the internal volume of a stomach or analogous structure. The method was tested with coho salmon, </span><i>Oncorhynchus kisutch</i><span> (Walbaum), which has a true stomach, and northern squawfish, </span><i>Ptychocheilus oregonensis</i><span>(Richardson), which has a modified foregut as a functional analogue. Both species were collected during July-October 1987 from the Columbia River, U.S.A. Relationships between fish weight (= volume) and maximum volume of the digestive organ were best fitted for coho salmon by an allometric model and for northern squawfish by an exponential model. Least squares regression analysis of individual measurements showed less variability in the volume of coho salmon stomachs (</span><i>R<sup>2</sup></i><span>= 0.85) than in the total digestive tracts (</span><i>R<sup>2</sup></i><span>= 0.55) and foreguts (</span><i>R<sup>2</sup></i><span>= 0.61) of northern squawfish, relative to fish size. Compared to previous methods, the new technique has the advantage of accurately measuring the internal volume of a wide range of digestive organ shapes and sizes.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1095-8649.1989.tb03351.x","usgsCitation":"Burley, C., and Vigg, S., 1989,  A method to directly measure maximum volume of fish stomachs or digestive tracts: Journal of Fish Biology, v. 34, no. 5, p. 707-714, https://doi.org/10.1111/j.1095-8649.1989.tb03351.x.","productDescription":"8 p.","startPage":"707","endPage":"714","numberOfPages":"8","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314126,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","issue":"5","noUsgsAuthors":false,"publicationDate":"2006-01-24","publicationStatus":"PW","scienceBaseUri":"5694e038e4b039675d005dce","contributors":{"authors":[{"text":"Burley, C.C.","contributorId":152149,"corporation":false,"usgs":false,"family":"Burley","given":"C.C.","email":"","affiliations":[],"preferred":false,"id":588223,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vigg, S.","contributorId":152150,"corporation":false,"usgs":false,"family":"Vigg","given":"S.","affiliations":[],"preferred":false,"id":588224,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70159101,"text":"70159101 - 1989 - Water-quality data for the Potomac-Raritan-Magothy aquifer system in the northern coast plain of New Jersey, 1923-86","interactions":[],"lastModifiedDate":"2015-10-22T09:24:42","indexId":"70159101","displayToPublicDate":"2015-06-02T05:15:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesNumber":"19","title":"Water-quality data for the Potomac-Raritan-Magothy aquifer system in the northern coast plain of New Jersey, 1923-86","docAbstract":"<p>Ground-water-quality data for the upper and middle aquifers of the Potomac-Raritan-Magothy aquifer system in Middlesex and Monmouth Counties are compiled for the period 1923-86. A total of 330 wells were sampled: 192 wells in the upper aquifer and 138 wells in the middle aquifer. Most of the complete water-quality analyses were collected after September 1984, as part of a regional ground-water assessment. Well-construction data for the sampled wells also are presented. Public-supply, domestic-supply, industrial, commercial, irrigation, and observation wells were sampled for the study. Field measurements made at the time of sample collection include water temperature, specific conductance , dissolved oxygen, pH, alkalinity, and bicarbonate concentration. Laboratory determinations include common ions, silica, dissolved solids, trace metals, volatile organic compounds, and pesticides. A quality-assurance program was followed to evaluate and assure the quality of the data.</p>\n<p>The report also contains a table of lithologic and hydrologic characteristics of the geologic units in the study area, a table of chloride concentrations and field measurements from 1923-86, and statistical summaries of selected water-quality data for the upper and middle aquifers. Many constituents were found in a wide range of concentrations.</p>\n<p>Water from more than 25 percent of the wells sampled contained lead concentrations above the detection limit of 10 ug/L (micrograms per liter). Included in this number are some wells that had lead concentrations greater than the U.S. Environmental Protection Agency (USEPA) primary drinking-water regulation of 50 ug/L. Cadmium concentrations, although lower than lead concentrations, followed a similar pattern. Water from approximately 25 percent of the wells in the upper aquifer, contain cadmium concentrations equal to or greater than the detection limit of 1 ug/L.</p>\n<p>Dissolved iron concentrations ranged from 5 ug/L to 480,000 ug/L. Water from more than 50 percent of the wells sampled contained iron concentrations in excess of the USEPA secondary drinking-water recommended limit of 300 ug/L.</p>\n<p>Chloride concentrations greater than the USEPA secondary drinking-water recommended limit of 250 milligrams per liter were found in samples from wells located in the cities of Perth Amboy and South Amboy; in the boroughs of Keansburg, Sayreville, Keyport, and Union Beach; and in the townships of Old Bridge and Woodbridge.</p>\n<p>Of 21 samples collected from wells screened in the upper aquifer and analyzed for 30 volatile organic compounds (VOCs), 5 samples contained at least 1 VOC at or above the detection limit. In the middle aquifer, 12 of the 21 samples collected and analyzed for VOCs contained at least 1 VOC greater than the detection limit.</p>\n<p>Concentrations of pesticides generally were low. Of the 43 samples collected from wells screened in the upper aquifer and analyzed for pesticides, 4 samples contained concentrations of pesticides at or greater than the detection limit. In the middle aquifer, 6 of 38 samples collected and analyzed for 32 pesticides had at least 1 pesticide with a concentration greater than the detection limit.</p>\n<p>&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","collaboration":"Prepared by the United States Geological Survey in cooperation with the New Jersey Department of Environmental Protection Division of Water Resources","usgsCitation":"Harriman, D.A., Pope, D.A., and Gordon, A.D., 1989, Water-quality data for the Potomac-Raritan-Magothy aquifer system in the northern coast plain of New Jersey, 1923-86, Report: iv, 94 p.; 2 Plates: 23.97 x 22.00 inches, 23.70 x 21.93 inches.","productDescription":"Report: iv, 94 p.; 2 Plates: 23.97 x 22.00 inches, 23.70 x 21.93 inches","numberOfPages":"100","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":309926,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70159101.jpg"},{"id":310333,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70159101/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":310334,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70159101/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":310335,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70159101/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Jersey","county":"Middlesex County, Monmouth County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.6630859375,\n              40.1452892956766\n            ],\n            [\n              -74.6630859375,\n              40.66813955408042\n            ],\n            [\n              -73.94210815429688,\n              40.66813955408042\n            ],\n            [\n              -73.94210815429688,\n              40.1452892956766\n            ],\n            [\n              -74.6630859375,\n              40.1452892956766\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5620cedde4b06217fc478b48","contributors":{"authors":[{"text":"Harriman, Douglas A.","contributorId":70544,"corporation":false,"usgs":true,"family":"Harriman","given":"Douglas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":577598,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pope, Daryll A. dpope@usgs.gov","contributorId":3796,"corporation":false,"usgs":true,"family":"Pope","given":"Daryll","email":"dpope@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":577599,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gordon, Alison D. 0000-0002-9502-8633 agordon@usgs.gov","orcid":"https://orcid.org/0000-0002-9502-8633","contributorId":890,"corporation":false,"usgs":true,"family":"Gordon","given":"Alison","email":"agordon@usgs.gov","middleInitial":"D.","affiliations":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"preferred":true,"id":577600,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70157488,"text":"70157488 - 1989 - A positive relationship between groundwater velocity and submersed macrophyte biomass in Sparkling Lake, Wisconsin","interactions":[],"lastModifiedDate":"2017-12-15T14:43:49","indexId":"70157488","displayToPublicDate":"2015-04-05T04:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2620,"text":"Limnology and Oceanography","active":true,"publicationSubtype":{"id":10}},"title":"A positive relationship between groundwater velocity and submersed macrophyte biomass in Sparkling Lake, Wisconsin","docAbstract":"<p>We measured groundwater velocity and submersed macrophyte biomass at 52 shal- low (0.4-6.6 m) sites in mesotrophic Sparkling Lake, Vilas County, Wisconsin, during May-Au- gust 1985. Seventeen percent of variation in macrophyte biomass was explained by a signifi- cant (P &lt; 0.005) relation with depth [log(biomass + 1) = 0.49 depth - 0.08 (depth)2 + 0.121. Some of the remaining variation in macrophyte bio- mass was explained by a significant rank corre- lation of biomass-on-depth residuals with groundwater velocity (rs = 0.46, P &lt; 0.0 1). These results suggest that water movement through the sediment-water interface may be a determinant of macrophyte abundance and distribution.&nbsp;</p>","language":"English","publisher":"American Society of Limnology and Oceanography, Inc.","doi":"10.4319/lo.1989.34.1.0235","usgsCitation":"Lodge, D.M., Krabbenhoft, D.P., and Striegl, R.G., 1989, A positive relationship between groundwater velocity and submersed macrophyte biomass in Sparkling Lake, Wisconsin: Limnology and Oceanography, v. 34, no. 1, p. 235-239, https://doi.org/10.4319/lo.1989.34.1.0235.","productDescription":"5 p.","startPage":"235","endPage":"239","numberOfPages":"5","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308537,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","county":"Vilas","otherGeospatial":"Sparkling Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.71040725708008,\n              45.99857150435143\n            ],\n            [\n              -89.71040725708008,\n              46.01723083989765\n            ],\n            [\n              -89.69023704528809,\n              46.01723083989765\n            ],\n            [\n              -89.69023704528809,\n              45.99857150435143\n            ],\n            [\n              -89.71040725708008,\n              45.99857150435143\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"34","issue":"1","noUsgsAuthors":false,"publicationDate":"2003-12-22","publicationStatus":"PW","scienceBaseUri":"56051eace4b058f706e512a4","contributors":{"authors":[{"text":"Lodge, David M.","contributorId":76622,"corporation":false,"usgs":false,"family":"Lodge","given":"David","email":"","middleInitial":"M.","affiliations":[{"id":16905,"text":"University of Notre Dame, Dept. of Biological Sciences, Notre Dame, IN, 46556, USA","active":true,"usgs":false}],"preferred":false,"id":573302,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krabbenhoft, David P. 0000-0003-1964-5020 dpkrabbe@usgs.gov","orcid":"https://orcid.org/0000-0003-1964-5020","contributorId":1658,"corporation":false,"usgs":true,"family":"Krabbenhoft","given":"David","email":"dpkrabbe@usgs.gov","middleInitial":"P.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true},{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":573303,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Striegl, Robert G. 0000-0002-8251-4659 rstriegl@usgs.gov","orcid":"https://orcid.org/0000-0002-8251-4659","contributorId":1630,"corporation":false,"usgs":true,"family":"Striegl","given":"Robert","email":"rstriegl@usgs.gov","middleInitial":"G.","affiliations":[{"id":36183,"text":"Hydro-Ecological Interactions Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":false,"id":573304,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70157480,"text":"70157480 - 1989 - Water resources of Vilas County, WI","interactions":[],"lastModifiedDate":"2015-09-24T11:56:31","indexId":"70157480","displayToPublicDate":"2015-02-16T13:15:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesTitle":{"id":406,"text":"Miscellaneous Public","active":false,"publicationSubtype":{"id":9}},"seriesNumber":"89-1","title":"Water resources of Vilas County, WI","language":"English","publisher":"Geological and Natural History Survey","publisherLocation":"Madison, WI","collaboration":"Prepared by the United States Department of Interior Geological Survey in cooperation with the University of Wisconsin-Extension Wisconsin, Geological and Natural History Survey","usgsCitation":"Patterson, G.L., 1989, Water resources of Vilas County, WI: Miscellaneous Public 89-1, v, 46.","productDescription":"v, 46","numberOfPages":"54","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308508,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","county":"Vilas","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-88.9879,46.0971],[-88.9329,46.0746],[-88.9332,45.9822],[-89.0478,45.9822],[-89.0477,45.8953],[-89.1091,45.8973],[-89.1752,45.8993],[-89.1754,45.859],[-89.3008,45.8606],[-89.3007,45.9014],[-89.3628,45.8987],[-89.4256,45.8987],[-89.5498,45.8988],[-89.6741,45.8987],[-89.7571,45.8985],[-89.797,45.898],[-89.8199,45.8984],[-89.9212,45.8981],[-89.9846,45.8974],[-90.0428,45.8972],[-90.0442,45.9823],[-90.0134,45.9824],[-89.9853,45.9821],[-89.9289,45.9818],[-89.9282,46.0693],[-89.9288,46.1558],[-89.9287,46.2428],[-89.929,46.3],[-89.7599,46.268],[-89.7368,46.2636],[-89.5829,46.2347],[-89.5331,46.2252],[-89.5133,46.2215],[-89.4272,46.2048],[-89.3759,46.1949],[-89.2666,46.1737],[-89.2302,46.1662],[-89.0854,46.1365],[-88.9879,46.0971]]]},\"properties\":{\"name\":\"Vilas\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56051eece4b058f706e5132c","contributors":{"authors":[{"text":"Patterson, G. L.","contributorId":35356,"corporation":false,"usgs":true,"family":"Patterson","given":"G.","email":"","middleInitial":"L.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":573274,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70157443,"text":"70157443 - 1989 - Hydrogeology of Wood County, Wisconsin","interactions":[],"lastModifiedDate":"2018-01-08T19:23:20","indexId":"70157443","displayToPublicDate":"2014-11-03T04:00:00","publicationYear":"1989","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":"60","title":"Hydrogeology of Wood County, Wisconsin","docAbstract":"<p>The presence of low-permeability Precambrian rocks near land surface limits ground-water availability in the northern two-thirds of Wood County. Sand and gravel deposits provide large amounts of water (more than 500 gallons per minute) to some wells in the southeastern part of the county. Fine-grained unconsolidated deposits generally are less than 20 feet thick in the northern two-thirds of the county, but sand and gravel deposits 40- to 100-feet thick underlie the extreme southeastern part of the county. Horizontal hydraulic conductivity of the sand and gravel deposits ranges from about 155 to about 280 feet per day. The horizontal hydraulic conductivity of fine-grained unconsolidated deposits in the northern part of the county ranges from about 0.02 to 2 feet per day. Where unconsolidated deposits do not yield dependable water supplies, wells are finished in Precambrian rocks. Fractures occurring at shallow depths are the primary source of water for wells finished in Precambrian rocks. Because the number of fractures tends to decrease with depth, the horizontal hydraulic conductivity of these rocks generally decreases from about 11 feet per day in wells less than 50-feet deep to about 0.02 foot per day in wells greater than 160 feet deep.</p>\n<p>Estimates of ground-water recharge to sand and gravel deposits in the southeastern part of the county range from about 7 to 12 inches per year. Recharge estimates for the central and northern parts of the county range from about 1 to 4 inches per year.</p>\n<p>The total dissolved-solids concentration in ground water in Wood County is relatively low. Concentrations in water samples from 124 wells ranged from 21 to 578 milligrams per liter, with a median concentration of about 190 milligrams per liter. Major dissolved constituents are calcium, magnesium, and bicarbonate; sodium, potassium, chloride, and sulfate are present in low concentrations. The most common water-quality problem in Wood County is elevated iron concentrations. Iron concentrations greater than 300 micrograms per liter were found in 54 of 124 samples, and 15 samples contained iron concentrations greater than 5,000 micrograms per liter.</p>\n<p>Nitrate as nitrogen concentrations exceeded Wisconsin's drinking-water standard (10 milligrams per liter) in water from just 4 of 124 wells. The pesticide aldicarb was detected in 7 of 36 samples, and various volatile organic compounds were detected in 24 of 102 ground-water samples collected by the Wisconsin Department of Natural Resources since 1980. Wells in which these chemicals were detected are near irrigated agricultural fields and in commercially developed areas where buried gasoline-storage tanks and chemical spills are more likely to occur.</p>\n<p>A reconnaissance approach combining electromagnetic surveys and sampling for water-quality indicators was used to assess effects of leachate on ground water near seven landfills. Results of the electromagnetic surveys were used to site water-quality observation wells. Total dissolved-solids concentrations and concentrations of volatile organic compounds, chloride, sulfate, iron, chemical oxygen demand, and organic carbon are some of the chemical constituents analyzed in samples collected from these wells.</p>\n<p>The average rate of ground&middot;water pumpage in Wood County in 1985 was 9.7 million gallons per day. Of this rate, about 6 million gallons per day is pumped from municipal-supply wells in seven communities.An additional 1.08 million gallons per day is pumped for agricultural irrigation.</p>","language":"English","publisher":"Wisconsin Geological & Natural History Survey","collaboration":"Prepared in cooperation with the University of Wisconsin-Extension, Geological and Natural History Survey, and Wood County","usgsCitation":"Batten, W.G., 1989, Hydrogeology of Wood County, Wisconsin: Wisconsin Geological & Natural History Survey Information Circular 60, vi, 27 p.","productDescription":"vi, 27 p.","numberOfPages":"33","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308446,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":350382,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://wgnhs.uwex.edu/pubs/download_ic60/"}],"country":"United States","state":"Wisconsin","county":"Wood County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-89.8449,44.6849],[-89.8451,44.5983],[-89.8447,44.5116],[-89.7268,44.5114],[-89.7259,44.4239],[-89.7243,44.3372],[-89.7247,44.2479],[-89.8376,44.249],[-89.8982,44.2493],[-89.9557,44.2491],[-89.9908,44.249],[-90.073,44.2491],[-90.0807,44.2491],[-90.1675,44.2491],[-90.1924,44.249],[-90.1975,44.249],[-90.1994,44.249],[-90.3123,44.2497],[-90.3161,44.2497],[-90.3172,44.3377],[-90.3163,44.4247],[-90.3161,44.5127],[-90.3165,44.5989],[-90.3163,44.6852],[-90.1981,44.6854],[-90.0793,44.685],[-89.9644,44.685],[-89.8449,44.6849]]]},\"properties\":{\"name\":\"Wood\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5603cd44e4b03bc34f544b10","contributors":{"authors":[{"text":"Batten, W. G.","contributorId":89504,"corporation":false,"usgs":true,"family":"Batten","given":"W.","email":"","middleInitial":"G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":573196,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043190,"text":"70043190 - 1989 - Relation of salinity and selenium in shallow groundwater to hydrologic and geochemical processes, Western San Joaquin Valley, California","interactions":[{"subject":{"id":13332,"text":"ofr88336 - 1988 - Relation of salinity and selenium in shallow ground water to hydrologic and geochemical processes, western San Joaquin Valley, California","indexId":"ofr88336","publicationYear":"1988","noYear":false,"title":"Relation of salinity and selenium in shallow ground water to hydrologic and geochemical processes, western San Joaquin Valley, California"},"predicate":"SUPERSEDED_BY","object":{"id":70043190,"text":"70043190 - 1989 - Relation of salinity and selenium in shallow groundwater to hydrologic and geochemical processes, Western San Joaquin Valley, California","indexId":"70043190","publicationYear":"1989","noYear":false,"title":"Relation of salinity and selenium in shallow groundwater to hydrologic and geochemical processes, Western San Joaquin Valley, California"},"id":1}],"lastModifiedDate":"2013-02-07T11:22:36","indexId":"70043190","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Relation of salinity and selenium in shallow groundwater to hydrologic and geochemical processes, Western San Joaquin Valley, California","docAbstract":"Salinity and selenium concentrations in shallow groundwater of the western San Joaquin Valley, California, are related to the geomorphology and hydrology of the alluvial fans. The highest salinity and selenium concentrations in shallow groundwater occur in alluvium deposited by ephemeral streams and at the margins of the major alluvial fans, where there were naturally saline, fine-grained soils. Low-to-moderate salinity and selenium concentrations in shallow groundwater are associated with upper and middle areas of the major alluvial fans deposited by intermittent streams. Areas with the most naturally saline soils have been irrigated in the last 40 years. These are now the areas of highest salinity and selenium concentrations in the shallow groundwater. Present-day (1986) groundwater salinity is spatially correlated with natural soil salinity in these areas. Isotopic data indicate that the highest salinity and selenium concentrations in groundwater present at low altitudes resulted from evaporative concentration when the water table was shallow.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Hydrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0022-1694(89)90011-5","usgsCitation":"Deverel, S.J., and Gallanthine, S., 1989, Relation of salinity and selenium in shallow groundwater to hydrologic and geochemical processes, Western San Joaquin Valley, California: Journal of Hydrology, v. 109, no. 1-2, p. 125-149, https://doi.org/10.1016/0022-1694(89)90011-5.","productDescription":"25 p.","startPage":"125","endPage":"149","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":267109,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267108,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0022-1694(89)90011-5"}],"country":"United States","state":"California","otherGeospatial":"San Joaquin Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.84,35.0 ], [ -121.84,38.17 ], [ -118.67,38.17 ], [ -118.67,35.0 ], [ -121.84,35.0 ] ] ] } } ] }","volume":"109","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5114db0ae4b0ca7af0743b44","contributors":{"authors":[{"text":"Deverel, S. J.","contributorId":65478,"corporation":false,"usgs":true,"family":"Deverel","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":473130,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gallanthine, S.K.","contributorId":90472,"corporation":false,"usgs":true,"family":"Gallanthine","given":"S.K.","affiliations":[],"preferred":false,"id":473131,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70046669,"text":"70046669 - 1989 - United States Geological Survey yearbook, fiscal year 1988","interactions":[],"lastModifiedDate":"2017-03-08T16:09:36","indexId":"70046669","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","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 1988","docAbstract":"<p><span>The fiscal year 1988 Yearbook summarizes the activities of the U.S. Geological Survey in response to its scientific and regulatory missions.</span></p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/70046669","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1989, United States Geological Survey yearbook, fiscal year 1988: Yearbook, iii, 134 p., https://doi.org/10.3133/70046669.","productDescription":"iii, 134 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":309899,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/yb/1988/report.pdf","text":"Report","size":"59.95 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":274018,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/yb/1988/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51c42462e4b03c77dce65a69","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":535555,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70044327,"text":"70044327 - 1989 - Geochemistry of oils and hydrocarbon source rocks, greater Anadarko Basin: evidence for multiple sources of oils and long-distance oil migration","interactions":[],"lastModifiedDate":"2013-03-03T09:30:32","indexId":"70044327","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Geochemistry of oils and hydrocarbon source rocks, greater Anadarko Basin: evidence for multiple sources of oils and long-distance oil migration","docAbstract":"Organic geochemical analyses of 104 crude oils and 190 core samples of dark-colored shales from the greater Anadarko basin show three major oil types which generally correlate with reservoir age and source-rock age. Analyses include C<sub>3</sub>-C<sub>30</sub> whole-oil gas chromatography, C<sub>10+</sub> saturated-hydrocarbon-fraction gas chromatography, and carbon stable isotopes (ppt relative to PDB) of saturated (sat) and aromatic (arom) hydrocarbon fractions. Three samples from Middle Ordovician Simpson Group reservoirs are \"typical\" Ordovician oils (type 1), having strong odd-carbon predominance in the C<sub>13</sub> to C<sub>19</sub> n-alkanes, containing little or no acyclic isoprenoids, an &delta;<sup>13</sup>C values of -33.9 ppt (sat) and -33.7 ppt (arom). Oils from Silurian to Devonian and Mississippian reservoirs (type 2) show little or no odd-carbon predominance in the n-alkanes, a regular decrease in abundance of n-alkanes with increasing carbon number, pristane/phytane ratios (pr/ph) of 1.1 to 1.5, and &delta;<sup>13</sup>C values of -30.6 ppt (sat) and -30.1 ppt (arom). Oils in Pennsylvanian reservoirs (type 3) have the greatest amounts of C<sub>15+</sub> hydrocarbons, are isotopically heavy (-27.5 ppt [sat] and -26.4 ppt [arom]), have methyl-cyclohexane as the most abundant hydrocarbon, and have pr/ph values from 2.0 to 0.9. Oils from the Kansas shelf area of the Anadarko basin are similar to the Anadarko oil types except that they have only traces of toluene and no detectable benzene. The relative abundance of toluene in the C<sub>7</sub> hydrocarbons systematically decreases with distance from the depocenter of the basin. The aromatic compounds are removed by water-washing, and hence could have been lost by contact with progressively greater amounts of formation water during long-distance migration. The lack of thermally mature source rocks in southern and central Kansas supports this hypothesis.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium, 1988 (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Burruss, R., and Hatch, J.R., 1989, Geochemistry of oils and hydrocarbon source rocks, greater Anadarko Basin: evidence for multiple sources of oils and long-distance oil migration, chap. <i>of</i> Anadarko Basin symposium, 1988 (Circular 90), p. 53-64.","productDescription":"12 p.","startPage":"53","endPage":"64","costCenters":[],"links":[{"id":268669,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268668,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Anadarko Basin","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":"51347f06e4b0e1603e4fec50","contributors":{"authors":[{"text":"Burruss, R.C. 0000-0001-6827-804X","orcid":"https://orcid.org/0000-0001-6827-804X","contributorId":99574,"corporation":false,"usgs":true,"family":"Burruss","given":"R.C.","affiliations":[],"preferred":false,"id":475298,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hatch, J. R.","contributorId":14775,"corporation":false,"usgs":true,"family":"Hatch","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":475297,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70044335,"text":"70044335 - 1989 - Paleohydrology of the Anadarko Basin, central United States","interactions":[],"lastModifiedDate":"2013-03-03T10:52:25","indexId":"70044335","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Paleohydrology of the Anadarko Basin, central United States","docAbstract":"Geohydrologic systems in the Anadarko basin in the central United States are controlled by topography, climate, geologic structures, and aquifer hydraulic properties, all of which are the result of past geologic and hydrologic processes, including tectonics and diagenesis. From Late Cambrian through Middle Ordovician time, a generally transgressive but cyclic sea covered the area. The first deposits were permPable sand, followed by calcareous mud. During periods of sea transgression, burial diagenesis decreased porosity and permeability. During periods of sea recession, uplift diagenesis increased porosity and permeability, especially in exposed rocks. During most of Silurian and Devonian time, the sea receded; increased porosity and permeability resulted from uplift diagenesis. However, at the end of the Devonian and during the Early Mississippian, very slightly permeable clay, which now is a regional confining unit, was deposited in a mostly euxinic sea. Later during Mississippian time, calcareous muds, which became limestone, were deposited in and adjacent to the Anadarko basin and underwent burial diagenesis. During Pennsylvanian time, rapid sedimentation accompanied rapid subsidence in the Anadarko basin. A geopressure zone probably resulted when sediments with little permeability trapped depositional water in Lower Pennsylvanian sands. Burial diagenesis included compaction and thermal alteration of deeply buried organic material, which released carbon dioxide, water, and hydrocarbons. By Middle Pennsylvanian time, the sea had submerged most of the central United States, including the Ozarks, as tectonic activity reached its maximum. During Late Pennsylvanian and Early Permian time, the Ouachita uplift had been formed and was higher than the Ozarks. Uplift was accompanied by a regional upward tilt toward the Ouachita-Ozarks area; the sea receded westward, depositing large quantities of calcareous mud and clay, and precipitating evaporitic material in the restricted-circulation environment. By the end of Permian time, > 20,000 ft of Pennsylvanian and Permian sediments had been deposited in the Anadarko basin. These thick sediments caused rapid and extreme burial diagenesis, including alteration of organic material. During Permian time in the Ozarks area, development of the Ozark Plateaus aquifer system commenced in the permeable Cambrian-Mississippian rocks near the St. Francois Mountains as the Pennsylvanian confining material was removed. Since Permian time, uplift diagenesis has been more active than burial diagenesis in the Anadarko basin. Synopsis of paleohydrologic interpretation indicates that Cambrian-Mississippian rocks in the Anadarko basin should be relatively impermeable, except for local secondary permeability, because rocks in the basin have undergone little uplift diagenesis.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Jorgensen, D.G., 1989, Paleohydrology of the Anadarko Basin, central United States, chap. <i>of</i> Anadarko Basin symposium (Circular 90), p. 176-193.","productDescription":"18 p.","startPage":"176","endPage":"193","costCenters":[],"links":[{"id":268683,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268682,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -126.0,23.5 ], [ -126.0,50.0 ], [ -66.9,50.0 ], [ -66.9,23.5 ], [ -126.0,23.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51347f09e4b0e1603e4fec62","contributors":{"authors":[{"text":"Jorgensen, Donald G.","contributorId":19537,"corporation":false,"usgs":true,"family":"Jorgensen","given":"Donald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":475307,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70044342,"text":"70044342 - 1989 - Formation resistivity as an indicator of the onset of oil generation in the Woodford Shale, Anadarko Basin, Oklahoma","interactions":[],"lastModifiedDate":"2013-03-03T19:24:48","indexId":"70044342","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Formation resistivity as an indicator of the onset of oil generation in the Woodford Shale, Anadarko Basin, Oklahoma","docAbstract":"The Upper Devonian and Lower Mississippian Woodford Shale is a black, organic-rich shale that is a major hydrocarbon source rock in the Anadarko basin. With the onset of oil generation, nonconductive hydrocarbons begin to replace conductive pore water in the Woodford, and formation resistivity increases. Crossplots of formation resistivity versus either vitrinite reflectance (R<sub>O</sub>) or Lopatin's time-temperature index of thermal maturity (TTI) define two data populations that represent immature shales and shales that have generated oil. The midpoint of the resistivity zone marking the transition between immature and mature shales is -35 ohm-m. The onset of appreciable oil generation in the Woodford Shale of the study area occurs at maturity levels of R<sub>O</sub> near 0.57% and of TTI between 33 and 48.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium, 1988 (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Schmoker, J.W., and Hester, T.C., 1989, Formation resistivity as an indicator of the onset of oil generation in the Woodford Shale, Anadarko Basin, Oklahoma, chap. <i>of</i> Anadarko Basin symposium, 1988 (Circular 90), p. 262-266.","productDescription":"5 p.","startPage":"262","endPage":"266","costCenters":[],"links":[{"id":268697,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268696,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Anadarko Basin","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":"51347f05e4b0e1603e4fec4c","contributors":{"authors":[{"text":"Schmoker, James W.","contributorId":52171,"corporation":false,"usgs":true,"family":"Schmoker","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":475324,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hester, Timothy C.","contributorId":21995,"corporation":false,"usgs":true,"family":"Hester","given":"Timothy","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":475323,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70044325,"text":"70044325 - 1989 - Thermal maturity of the Anadarko Basin","interactions":[],"lastModifiedDate":"2013-03-03T09:35:17","indexId":"70044325","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Thermal maturity of the Anadarko Basin","docAbstract":"Levels of thermal maturity are estimated for Paleozoic strata in five areas of the central Anadarko basin for times between the Paleozoic and the present, and depths of the oil window are plotted as a function of geologic time. Mean surface temperature assumed here for calculating Lopatin's time-temperature index of thermal maturity (TTl) in the central Anadarko basin declines from 80°F (27°C) to 60°F (16°C) from early Paleozoic time to the present. Shallow-water carbonates and lower paleolatitudes suggest warmer climates in the Paleozoic for this area. The geothermal gradient is assumed to equal 4.0°F/100 ft (7.3°C/100 m) in the Late Cambrian and to decay over a 100-m.y. period to the present regional gradient of 1.3°F/100 ft (2.4°C/100 m). Initial\nbasin formation was caused by crustal thinning. Accumulation of thick Pennsylvanian sediments in a foreland-style basin dominated by vertical lithospheric flexure represents a second major period of subsidence. An elevated geothermal gradient during this time is not assumed for TTl calculations, because mathematical models suggest time-invariant heat flows in such basins. TTl computations based on these assumptions indicate that oil could have been generated in the ancestral Anadarko basin >350 m.y. ago. By the end of the Pennsylvanian, significant volumes of kerogen were in the oil window (and perhaps beyond), and significant volumes have remained in the oil window up to the present day. These circumstances may partially explain the unusual richness of the Anadarko basin as a Paleozoic hydrocarbon province.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium, 1988 (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Schmoker, J.W., 1989, Thermal maturity of the Anadarko Basin, chap. <i>of</i> Anadarko Basin symposium, 1988 (Circular 90), p. 25-31.","productDescription":"7 p.","startPage":"25","endPage":"31","costCenters":[],"links":[{"id":268665,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268664,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Anadarko Basin","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":"51347f0ee4b0e1603e4fec7a","contributors":{"authors":[{"text":"Schmoker, James W.","contributorId":52171,"corporation":false,"usgs":true,"family":"Schmoker","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":475293,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70006517,"text":"70006517 - 1989 - Behavior of fish predators and their prey: Habitat choice between open water and dense vegetation","interactions":[],"lastModifiedDate":"2020-09-01T22:56:17.578049","indexId":"70006517","displayToPublicDate":"2012-07-06T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1528,"text":"Environmental Biology of Fishes","active":true,"publicationSubtype":{"id":10}},"title":"Behavior of fish predators and their prey: Habitat choice between open water and dense vegetation","docAbstract":"<p><span>Behavior of largemouth bass,&nbsp;</span><i class=\"EmphasisTypeItalic \">Micropterus salmoides</i><span>, and northern pike,&nbsp;</span><i class=\"EmphasisTypeItalic \">Esox lucius</i><span>, foraging on fathead minnows,&nbsp;</span><i class=\"EmphasisTypeItalic \">Pimephales promelas</i><span>, or bluegills,&nbsp;</span><i class=\"EmphasisTypeItalic \">Lepomis macrochirus</i><span>, was quantified in pools with 50% cover (half the pool had artificial stems at a density of 1000 stems m</span><sup><span>&minus;2</span></sup><span>). Both predators spent most of their time in the vegetation. Largemouth bass searched for bluegills and ambushed minnows, whereas the relatively immobile northern pike ambushed all prey. Minnows were closer to predators and were captured more frequently than bluegills. Even when minnows dispersed, they moved continually and eventually wandered within striking distance of a predator. Bluegills dispersed in the cover with predators. Bass captured the few bluegills that strayed into the open and pike captured those that approached too closely in the cover. The ability of predators to capture prey while residing in habitats containing patches of dense cover may explain their residence in areas often considered to be poor ones for foraging.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/BF00001402","usgsCitation":"Savino, J.F., and Stein, R., 1989, Behavior of fish predators and their prey: Habitat choice between open water and dense vegetation: Environmental Biology of Fishes, v. 24, no. 4, p. 287-293, https://doi.org/10.1007/BF00001402.","productDescription":"7 p.","startPage":"287","endPage":"293","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":479862,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/1811/37301","text":"External Repository"},{"id":259084,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","volume":"24","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f09fe4b0c8380cd4a802","contributors":{"authors":[{"text":"Savino, Jacqueline F. jsavino@usgs.gov","contributorId":2213,"corporation":false,"usgs":true,"family":"Savino","given":"Jacqueline","email":"jsavino@usgs.gov","middleInitial":"F.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":354660,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stein, Roy A.","contributorId":21494,"corporation":false,"usgs":true,"family":"Stein","given":"Roy A.","affiliations":[],"preferred":false,"id":354661,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70006740,"text":"70006740 - 1989 - Avian botulism: geographic expansion of a historic disease","interactions":[],"lastModifiedDate":"2018-03-23T16:24:33","indexId":"70006740","displayToPublicDate":"2012-02-17T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":24,"text":"Fish and Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"13.2.4","title":"Avian botulism: geographic expansion of a historic disease","docAbstract":"<p>Avian botulism is a paralytic, often fatal disease of birds resulting from ingestion of toxin produced by the bacterium Clostridium botulinum. Waterfowl die-offs from the botulism are usually caused by type C toxin; sporadic die-offs among fish-eating birds, such as common loons (Gavia immer) and gulls, have been caused by type E toxin.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Waterfowl Management Handbook","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, DC","usgsCitation":"Locke, L.N., and Friend, M., 1989, Avian botulism: geographic expansion of a historic disease: Fish and Wildlife Leaflet 13.2.4, 6 p.","productDescription":"6 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":204598,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":115812,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://archive.usgs.gov/archive/sites/www.nwrc.usgs.gov/wdb/pub/wmh/13_2_4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ef5ce4b0c8380cd4a1f0","contributors":{"authors":[{"text":"Locke, Louis N.","contributorId":71233,"corporation":false,"usgs":true,"family":"Locke","given":"Louis","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":355114,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friend, Milton 0000-0002-2882-3629","orcid":"https://orcid.org/0000-0002-2882-3629","contributorId":31332,"corporation":false,"usgs":true,"family":"Friend","given":"Milton","email":"","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":355115,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70039577,"text":"70039577 - 1989 - Resident research associateships, postdoctoral research awards 1989: opportunities for research at the U.S. Geological Survey, U.S. Department of the Interior","interactions":[],"lastModifiedDate":"2012-08-14T01:01:44","indexId":"70039577","displayToPublicDate":"2012-01-01T21:10:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":371,"text":"Monograph","active":false,"publicationSubtype":{"id":6}},"title":"Resident research associateships, postdoctoral research awards 1989: opportunities for research at the U.S. Geological Survey, U.S. Department of the Interior","docAbstract":"The scientists of the U.S. Geological Survey are engaged in a wide range of geologic, geophysical, geochemical, hydrologic, and cartographic programs, including the application of computer science to them. These programs offer exciting possibilities for scientific achievement and professional growth to young scientists through participation as Research Associates.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039577","usgsCitation":"Water Resources Division, U.S. Geological Survey, and U.S. National Research Council, 1989, Resident research associateships, postdoctoral research awards 1989: opportunities for research at the U.S. Geological Survey, U.S. Department of the Interior: Monograph, v, 122 p., https://doi.org/10.3133/70039577.","productDescription":"v, 122 p.","numberOfPages":"130","costCenters":[],"links":[{"id":259585,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aa97be4b0c8380cd85e0e","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":535373,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"U.S. National Research Council","contributorId":128227,"corporation":true,"usgs":false,"organization":"U.S. National Research Council","id":535374,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70006866,"text":"70006866 - 1989 - Comparison of fish catches with buoyant pop nets and seines in vegetated and nonvegetated habitats","interactions":[],"lastModifiedDate":"2012-08-24T01:02:05","indexId":"70006866","displayToPublicDate":"2012-01-01T16:15:00","publicationYear":"1989","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":"Comparison of fish catches with buoyant pop nets and seines in vegetated and nonvegetated habitats","docAbstract":"Two models of pop nets were developed to sample fish in shallow riverine waters, one for use in vegetated areas and the other for nonvegetated areas. Both nets have a mechanical release mechanism that can be tripped from the water surface. Replicated field tests were conducted to compare pop-net catches with bag-seine collections every 2 weeks from May through mid-October. Overall, total catch per effort did not vary significantly (<i>P</i> < 0.05) between the two gears at either the vegetated or nonvegetated site. However, collections with the pop net were not as diverse as with the seine at either sampling site, perhaps because the area sampled by pop nets (5.6 m<sup>2</sup>) was smaller than the area swept by the average seine haul (70-140 m<sup>2</sup>). The pop net effectively sampled fish in shallow nonvegetated habitats and was useful in heavily vegetated areas where seining or electroshocking was difficult.","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":"10.1577/1548-8675(1989)009<0249:COFCWB>2.3.CO;2","collaboration":"Abstract has subscript/superscript to be fixed","usgsCitation":"Dewey, M.R., Holland-Bartels, L., and Zigler, S.J., 1989, Comparison of fish catches with buoyant pop nets and seines in vegetated and nonvegetated habitats: North American Journal of Fisheries Management, v. 9, no. 2, p. 249-253, https://doi.org/10.1577/1548-8675(1989)009<0249:COFCWB>2.3.CO;2.","productDescription":"5 p.","startPage":"249","endPage":"253","numberOfPages":"5","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":259816,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":259804,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/1548-8675(1989)009<0249:COFCWB>2.3.CO;2","linkFileType":{"id":5,"text":"html"}}],"volume":"9","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f863e4b0c8380cd4d081","contributors":{"authors":[{"text":"Dewey, M. R.","contributorId":48908,"corporation":false,"usgs":true,"family":"Dewey","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":355379,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holland-Bartels, L. E.","contributorId":53221,"corporation":false,"usgs":true,"family":"Holland-Bartels","given":"L. E.","affiliations":[],"preferred":false,"id":355380,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zigler, S. J.","contributorId":21513,"corporation":false,"usgs":true,"family":"Zigler","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":355378,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70039068,"text":"70039068 - 1989 - Earthquakes & Volcanoes, Volume 21, Number 1, 1989: Featuring the U.S. Geological Survey's National Earthquake Information Center in Golden, Colorado, USA","interactions":[],"lastModifiedDate":"2017-05-22T11:26:50","indexId":"70039068","displayToPublicDate":"2012-01-01T14:27:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Earthquakes & Volcanoes, Volume 21, Number 1, 1989: Featuring the U.S. Geological Survey's National Earthquake Information Center in Golden, Colorado, USA","docAbstract":"Earthquakes and Volcanoes is published bimonthly by the U.S. Geological Survey to provide current information on earthquakes and seismology, volcanoes, and related natural hazards of interest to both generalized and specialized readers. The Secretary of the Interior has determined that the publication of this periodical is necessary in the transaction of the public business required by law of this Department. Use of funds for printing this periodical has been approved by the Office of Management and Budget through June 30, 1989. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039068","usgsCitation":"Water Resources Division, U.S. Geological Survey, Spall, H., and Schnabel, D.C., 1989, Earthquakes & Volcanoes, Volume 21, Number 1, 1989: Featuring the U.S. Geological Survey's National Earthquake Information Center in Golden, Colorado, USA, 63 p., https://doi.org/10.3133/70039068.","productDescription":"63 p.","numberOfPages":"64","costCenters":[{"id":415,"text":"National Earthquake Information Center","active":false,"usgs":true}],"links":[{"id":261289,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039068/report.pdf"},{"id":261290,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039068/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a050de4b0c8380cd50c37","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":535212,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spall, Henry","contributorId":77933,"corporation":false,"usgs":true,"family":"Spall","given":"Henry","email":"","affiliations":[],"preferred":false,"id":465561,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schnabel, Diane C.","contributorId":94538,"corporation":false,"usgs":true,"family":"Schnabel","given":"Diane","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":465562,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}