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,{"id":54552,"text":"wdrGA901 - 1991 - Water resources data, Georgia, water year 1990","interactions":[],"lastModifiedDate":"2025-08-26T18:30:03.022336","indexId":"wdrGA901","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"GA-90-1","title":"Water resources data, Georgia, water year 1990","docAbstract":"<p>Water resources data for the 1990 water year for Georgia consists of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs; ground-water levels; and precipitation quality. This report contains discharge records of 117 gaging stations; stage for 28 gaging stations; stage and contents for 18 lakes and reservoirs; water quality for 128 continuing-record stations; peak stage and discharge only for 93 crest-stage partial-record stations and 8 miscellaneous sites; water levels of 25 observation wells; and water quality for 1 precipitation quality site. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Georgia. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrGA901","collaboration":"Prepared in cooperation with the State of Georgia and with other agencies","usgsCitation":"Stokes, W., McFarlane, R., and Buell, G.R., 1991, Water resources data, Georgia, water year 1990: U.S. Geological Survey Water Data Report GA-90-1, x, 557 p., https://doi.org/10.3133/wdrGA901.","productDescription":"x, 557 p.","costCenters":[],"links":[{"id":185166,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1990/ga-90-1/report-thumb.jpg"},{"id":494920,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1990/ga-90-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":54644,"text":"wdrMARI891 - 1991 - Water resources data, Massachusetts and Rhode Island, water year 1989","interactions":[],"lastModifiedDate":"2025-09-30T16:42:16.177225","indexId":"wdrMARI891","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MA-RI-89-1","title":"Water resources data, Massachusetts and Rhode Island, water year 1989","docAbstract":"<p>Water resources data for the 1991 water year for Maryland and Delaware consist of records of water levels and water quality of ground-water wells. This report (Volume 2. Ground-Water Data) contains water levels at 366 observation wells, discharge records for 4 springs and water quality at 276 wells. Locations of ground-water level wells are shown on figures 3 and 4. The data in this report represents that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State, local, and Federal agencies in Maryland and Delaware.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMARI891","collaboration":"Prepared in cooperation with the States of Massachusetts and Rhode Island and with other agencies","usgsCitation":"Socolow, R., Gadoury, R.A., Ramsbey, L., and Bell, R., 1991, Water resources data, Massachusetts and Rhode Island, water year 1989: U.S. Geological Survey Water Data Report MA-RI-89-1, xi, 227 p., https://doi.org/10.3133/wdrMARI891.","productDescription":"xi, 227 p.","costCenters":[],"links":[{"id":178199,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1989/mari-89-1/report-thumb.jpg"},{"id":496116,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1989/mari-89-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Massachusetts, Rhode Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -73.50297488831188,\n              42.97016577848564\n            ],\n            [\n              -73.50297488831188,\n              41.11994266161375\n            ],\n            [\n              -69.8918541821574,\n              41.11994266161375\n            ],\n            [\n              -69.8918541821574,\n              42.97016577848564\n            ],\n            [\n              -73.50297488831188,\n              42.97016577848564\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb6ae","contributors":{"authors":[{"text":"Socolow, R.S.","contributorId":17639,"corporation":false,"usgs":true,"family":"Socolow","given":"R.S.","affiliations":[],"preferred":false,"id":251011,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gadoury, R. A.","contributorId":26334,"corporation":false,"usgs":true,"family":"Gadoury","given":"R.","middleInitial":"A.","affiliations":[],"preferred":false,"id":251012,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ramsbey, L.R.","contributorId":78393,"corporation":false,"usgs":true,"family":"Ramsbey","given":"L.R.","email":"","affiliations":[],"preferred":false,"id":251014,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bell, R.W.","contributorId":77563,"corporation":false,"usgs":true,"family":"Bell","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":251013,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":30514,"text":"wri904052 - 1991 - Tributary-stream infiltration in Marsh Creek Valley, north-central Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-07T11:26:28","indexId":"wri904052","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"90-4052","title":"Tributary-stream infiltration in Marsh Creek Valley, north-central Pennsylvania","docAbstract":"The geohydrology of infiltration from five tributary streams along a 3.6-mile reach of Marsh Creek valley in north-central Pennsylvania was investigated during 1983-85. Marsh Creek valley is underlain by up to 100 feet of stratified drift that overlies Devonian bedrock. The stratified drift is overlain by up to 30 feet of alluvial-fan deposits near the tributary streams.\n\n      Four of the five tributary streams lose large amounts of water to the stratified-drift aquifer in Marsh Creek valley. Along reaches away from the valley wall, infiltration losses from the streams averaged about 2 cubic feet per second per 1,000 feet of wetted channel length. Estimated hydraulic conductivity of the deposits near these streams ranges from 31 to 100 feet per day and averages 61 feet per day. Silty beds of lower permeability near the streams may significantly affect infiltration. The low permeability of the sediments near the fifth stream, which probably consist largely of fine-grained alluvium and swamp deposits, may account for the lack of infiltration losses along this stream.\n\n      Tributary-stream infiltration accounted for more than 70 percent of the estimated recharge to the stratified-drift aquifer along the reach investigated during water year 1985, in which annual precipitation was below average. The sources of recharge and their estimated rates were: (1) direct infiltration of precipitation on the valley, 1.7 cubic feet per second; (2) unchanneled runoff and ground-water inflow from the uplands, 2.7 cubic feet per second; and (3) tributary-stream infiltration from Asaph Run, 3.7 cubic feet per second, Straight Run, 3.7 cubic feet per second, Dantz Run, 1.2 cubic feet per second, and Canada Run, 1.9 cubic feet per second. The temporal variation in recharge from tributary-stream infiltration greatly affects drawdowns caused by pumping from the wellfield at the National Fisheries Research and Development Laboratory near Straight Run.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri904052","usgsCitation":"Williams, J., 1991, Tributary-stream infiltration in Marsh Creek Valley, north-central Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 90-4052, vi, 39 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri904052.","productDescription":"vi, 39 p. :ill., maps ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":259319,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4052/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":260348,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4052/report-thumb.jpg"},{"id":259320,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1990/4052/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennsylvania","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -78.0908203125,\n              40.68063802521456\n            ],\n            [\n              -75.56396484375,\n              40.68063802521456\n            ],\n            [\n              -75.56396484375,\n              41.983994270935625\n            ],\n            [\n              -78.0908203125,\n              41.983994270935625\n            ],\n            [\n              -78.0908203125,\n              40.68063802521456\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dde4b07f02db5e260c","contributors":{"authors":[{"text":"Williams, John H. 0000-0002-6054-6908 jhwillia@usgs.gov","orcid":"https://orcid.org/0000-0002-6054-6908","contributorId":1553,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"jhwillia@usgs.gov","middleInitial":"H.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":203382,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18521,"text":"ofr90571 - 1991 - Surface water quality assessment of the Upper Illinois River basin in Illinois, Indiana, and Wisconsin: Geochemical data for fine-fraction streambed sediment from high- and low-order streams, 1987","interactions":[],"lastModifiedDate":"2022-08-31T18:56:10.139037","indexId":"ofr90571","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"90-571","title":"Surface water quality assessment of the Upper Illinois River basin in Illinois, Indiana, and Wisconsin: Geochemical data for fine-fraction streambed sediment from high- and low-order streams, 1987","docAbstract":"Geochemical data are presented from a synoptic survey of 46 elements in fine-fraction streambed sediments of the Upper Illinois River Basin during the fall of 1987. The survey was a component study of the Illinois pilot project of the U.S. Geological Survey's National Water-Quality Assessment program. Most of the sampling sites were randomly chosen--135 on main stems of rivers and 238 on first- and second-order streams. In addition, 196 samples were collected for quality-assurance and special-study purposes. The report includes element concentration data and summary-statistics tables of percentiles, nested analysis of variance, and correlation coefficients. All concentration data are included in tabular form and can be selected by map reference number, latitude and longitude, or remark code indicating purpose for collecting sample.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr90571","usgsCitation":"Colman, J.A., and Sanzolone, R.F., 1991, Surface water quality assessment of the Upper Illinois River basin in Illinois, Indiana, and Wisconsin: Geochemical data for fine-fraction streambed sediment from high- and low-order streams, 1987: U.S. Geological Survey Open-File Report 90-571, iv, 108 p., https://doi.org/10.3133/ofr90571.","productDescription":"iv, 108 p.","numberOfPages":"108","costCenters":[],"links":[{"id":47870,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0571/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":406015,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17976.htm","linkFileType":{"id":5,"text":"html"}},{"id":152027,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0571/report-thumb.jpg"}],"country":"United States","state":"Illinois, Indiana","otherGeospatial":"Upper Illinois River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.095,\n              40.3961\n            ],\n            [\n              -85.8931,\n              40.3961\n            ],\n            [\n              -85.8931,\n              43.2167\n            ],\n            [\n              -89.095,\n              43.2167\n            ],\n            [\n              -89.095,\n              40.3961\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696391","contributors":{"authors":[{"text":"Colman, John A. 0000-0001-9327-0779 jacolman@usgs.gov","orcid":"https://orcid.org/0000-0001-9327-0779","contributorId":2098,"corporation":false,"usgs":true,"family":"Colman","given":"John","email":"jacolman@usgs.gov","middleInitial":"A.","affiliations":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":179276,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sanzolone, R. F.","contributorId":64199,"corporation":false,"usgs":true,"family":"Sanzolone","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":179277,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70007464,"text":"70007464 - 1991 - Chufa biology and management","interactions":[],"lastModifiedDate":"2016-09-16T15:16:26","indexId":"70007464","displayToPublicDate":"1992-01-01T16:50:00","publicationYear":"1991","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":"13.4.18","title":"Chufa biology and management","docAbstract":"<p>Chufa (Cyperus esculentus) is an emergent perennial sedge that is common in seasonally flooded wetlands. Although chufa is common in many States, it is most abundant in the Southeast, including the Mississippi alluvial valley (Fig. 1). Belowground biomass of chufa, especially the tubers, serves as a valuable food source for waterfowl and cranes. Chufa tubers rank tenth among the most important waterfowl foods in the United States.</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","usgsCitation":"Fredrickson, L.H., and Kelley, J.R., 1991, Chufa biology and management: Fish and Wildlife Leaflet 13.4.18, 6 p.","productDescription":"6 p.","costCenters":[],"links":[{"id":204594,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":115815,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://archive.usgs.gov/archive/sites/www.nwrc.usgs.gov/wdb/pub/wmh/13_4_18.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f5fbe4b0c8380cd4c52b","contributors":{"authors":[{"text":"Fredrickson, Leigh H.","contributorId":55874,"corporation":false,"usgs":true,"family":"Fredrickson","given":"Leigh","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":356432,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kelley, James R. Jr.","contributorId":37062,"corporation":false,"usgs":true,"family":"Kelley","given":"James","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":356431,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70006479,"text":"70006479 - 1991 - Long-term decline in freshwater mussels (Bivalvia: Unionidae) of the western basin of Lake Erie","interactions":[],"lastModifiedDate":"2014-06-16T16:12:17","indexId":"70006479","displayToPublicDate":"1992-01-01T16:06:43","publicationYear":"1991","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2330,"text":"Journal of Great Lakes Research","active":true,"publicationSubtype":{"id":10}},"title":"Long-term decline in freshwater mussels (Bivalvia: Unionidae) of the western basin of Lake Erie","docAbstract":"Long-term trends in the abundance of unionids in the western basin of Lake Erie were examined from data collected at 17 stations in 1961, 1972, and 1982. The mean number of unionids at these stations declined over this time period, decreasing from 10 m<sup>−2</sup> in 1961, to 6 m<sup>−2</sup> in 1972, down to 4 m<sup>−2</sup> in 1982. This decline in abundance was reflected in the decrease in the number of stations where mussels were found; unionids were found at 16 of the 17 stations in 1961, but at only 6 stations in 1982. Reasons for the decrease in the unionid population are not generally apparent, but are probably related to the decline in water quality and periods of low oxygen levels over the time period of the surveys.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Great Lakes Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/S0380-1330(91)71358-0","usgsCitation":"Nalepa, T., Manny, B.A., Roth, J.C., Mozley, S.C., and Schloesser, D.W., 1991, Long-term decline in freshwater mussels (Bivalvia: Unionidae) of the western basin of Lake Erie: Journal of Great Lakes Research, v. 17, no. 2, p. 214-219, https://doi.org/10.1016/S0380-1330(91)71358-0.","productDescription":"5 p.","startPage":"214","endPage":"219","numberOfPages":"5","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":288667,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":288666,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0380-1330(91)71358-0"}],"country":"United States","otherGeospatial":"Lake Erie","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.73642,41.54045 ], [ -83.73642,42.10026 ], [ -82.898712,42.10026 ], [ -82.898712,41.54045 ], [ -83.73642,41.54045 ] ] ] } } ] }","volume":"17","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae775ce4b0abf75cf2c11c","contributors":{"authors":[{"text":"Nalepa, Thomas F.","contributorId":28212,"corporation":false,"usgs":true,"family":"Nalepa","given":"Thomas F.","affiliations":[],"preferred":false,"id":354594,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Manny, Bruce A. 0000-0002-4074-9329 bmanny@usgs.gov","orcid":"https://orcid.org/0000-0002-4074-9329","contributorId":3699,"corporation":false,"usgs":true,"family":"Manny","given":"Bruce","email":"bmanny@usgs.gov","middleInitial":"A.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":354592,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Roth, James C.","contributorId":56156,"corporation":false,"usgs":true,"family":"Roth","given":"James","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":354595,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mozley, Samuel C.","contributorId":22687,"corporation":false,"usgs":true,"family":"Mozley","given":"Samuel","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":354593,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schloesser, Donald W. dschloesser@usgs.gov","contributorId":3579,"corporation":false,"usgs":true,"family":"Schloesser","given":"Donald","email":"dschloesser@usgs.gov","middleInitial":"W.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":354591,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70206249,"text":"70206249 - 1991 - Use of processed geophysical data to improve the delineation of infilled scour holes at bridge piers","interactions":[],"lastModifiedDate":"2019-10-28T06:41:21","indexId":"70206249","displayToPublicDate":"1991-12-31T14:25:06","publicationYear":"1991","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Use of processed geophysical data to improve the delineation of infilled scour holes at bridge piers","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Expanded abstracts with biographies: 1991 technical program: 61st Annual International SEG Meeting","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"61st Annual International SEG Meeting","conferenceDate":"November 10-14, 1991","conferenceLocation":"Houston,TX","language":"English","publisher":"Society of Exploration Geophysicists","usgsCitation":"Haeni, F., and Placzek, G., 1991, Use of processed geophysical data to improve the delineation of infilled scour holes at bridge piers, <i>in</i> Expanded abstracts with biographies: 1991 technical program: 61st Annual International SEG Meeting, Houston,TX, November 10-14, 1991, p. 549-552.","productDescription":"4 p.","startPage":"549","endPage":"552","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"links":[{"id":368623,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Haeni, F.P.","contributorId":87105,"corporation":false,"usgs":true,"family":"Haeni","given":"F.P.","affiliations":[],"preferred":false,"id":773928,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Placzek, Gary","contributorId":58295,"corporation":false,"usgs":true,"family":"Placzek","given":"Gary","email":"","affiliations":[],"preferred":false,"id":773929,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70206248,"text":"70206248 - 1991 - Results of integrated surface-geophysical studies for shallow subsurface fracture detection at three New Hampshire sites","interactions":[],"lastModifiedDate":"2019-10-28T06:42:15","indexId":"70206248","displayToPublicDate":"1991-12-31T14:18:50","publicationYear":"1991","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Results of integrated surface-geophysical studies for shallow subsurface fracture detection at three New Hampshire sites","docAbstract":"<p>No abstract available.&nbsp;</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Expanded abstracts with biographies: 1991 technical program: 61st Annual International SEG Meeting","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"61st Annual International SEG Meeting","conferenceDate":"November 10-14, 1991","conferenceLocation":"Houston, 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,{"id":70208262,"text":"70208262 - 1991 - Ecosystem modeling of Barataria Basin, Louisiana utilizing desktop parallel technology","interactions":[],"lastModifiedDate":"2020-01-31T14:15:53","indexId":"70208262","displayToPublicDate":"1991-12-31T14:05:47","publicationYear":"1991","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Ecosystem modeling of Barataria Basin, Louisiana utilizing desktop parallel technology","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"27th Annual Conference : Water management of river systems, and symposium: Resource development of the lower Mississippi River","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"27th Annual Conference : Water Management of River Systems, and Symposium: Resource Development of the Lower Mississippi River","conferenceDate":"Sep 8-13, 1991","conferenceLocation":"New Orleans, LA","language":"English","publisher":"American Water Resources Association","usgsCitation":"White, M.L., Maxwell, T., Costanza, R., and Doyle, T.W., 1991, Ecosystem modeling of Barataria Basin, Louisiana utilizing desktop parallel technology, <i>in</i> 27th Annual Conference : Water management of river systems, and symposium: Resource development of the lower Mississippi River, New Orleans, LA, Sep 8-13, 1991, p. 225-234.","productDescription":"10 p.","startPage":"225","endPage":"234","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":371834,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Louisiana","otherGeospatial":"Barataria Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.05242919921875,\n              29.10897615145302\n            ],\n            [\n              -89.41497802734375,\n              29.379781767454972\n            ],\n            [\n              -89.89837646484375,\n              29.80966763726961\n            ],\n            [\n              -89.9176025390625,\n              30.06909396443887\n            ],\n            [\n              -89.8736572265625,\n              30.121373087823045\n            ],\n            [\n              -90.10162353515625,\n              30.0286775329042\n            ],\n            [\n              -90.32135009765625,\n              30.050076521698735\n            ],\n            [\n              -90.604248046875,\n              30.121373087823045\n            ],\n            [\n              -90.9228515625,\n              30.261439550638762\n            ],\n            [\n              -90.999755859375,\n              30.330212685432734\n            ],\n            [\n              -91.34857177734375,\n              30.247204606534158\n            ],\n            [\n              -90.10986328125,\n              29.248063243796576\n            ],\n            [\n              -90.0604248046875,\n              29.19053283229458\n            ],\n            [\n              -89.76654052734375,\n              29.379781767454972\n            ],\n            [\n              -89.45343017578125,\n              29.180941290001776\n            ],\n            [\n              -89.10186767578125,\n              29.068173545070536\n            ],\n            [\n              -89.05242919921875,\n              29.10897615145302\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"White, M. L.","contributorId":222097,"corporation":false,"usgs":false,"family":"White","given":"M.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":781183,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maxwell, T.","contributorId":222098,"corporation":false,"usgs":false,"family":"Maxwell","given":"T.","email":"","affiliations":[],"preferred":false,"id":781184,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Costanza, R.","contributorId":86497,"corporation":false,"usgs":true,"family":"Costanza","given":"R.","email":"","affiliations":[],"preferred":false,"id":781185,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Doyle, Thomas W. 0000-0001-5754-0671 doylet@usgs.gov","orcid":"https://orcid.org/0000-0001-5754-0671","contributorId":703,"corporation":false,"usgs":true,"family":"Doyle","given":"Thomas","email":"doylet@usgs.gov","middleInitial":"W.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":781186,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70208080,"text":"70208080 - 1991 - Global climate change: USFWS coastal research","interactions":[],"lastModifiedDate":"2020-01-27T12:49:30","indexId":"70208080","displayToPublicDate":"1991-12-31T12:42:15","publicationYear":"1991","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Global climate change: USFWS coastal research","docAbstract":"<p><span>Scenarios of global climate change are still ambiguous; however, increasing sea level and atmospheric carbon dioxide (CO</span><sub>2</sub><span>) concentrations seem certain, although rates of change are still being debated. Predictions for other aspects of climate change, such as temperature, tropical storm frequency and intensity, and precipitation, are still in debate, and all predictions for local (e.g., watershed) or regional effects are far from being useful for site-specific planning. While recognizing the weakness of current climate models, especially at regional and local scales, the U.S. Fish and Wildlife Service, in fulfilling its mandate for wildlife habitat protection and maintenance, advocates understanding the processes involved and forecasting potential changes. Because coastal wetlands constitute critical habitat for a significant portion of fish and wildlife under the Service's conservation charge, the Service's National Wetlands Research Center will study some of the most vulnerable coastal habitats of the Southern United States, namely coastal emergent marshes, submerged aquatic vegetation, forested wetlands, and communities of benthic invertebrates. Studies will include developing landscape-level data bases on National Wildlife Refuge wetland complexes along the coasts of the south Atlantic and Gulf of Mexico. Comparisons will be made between accreting and subsiding coastal marshes. Greenhouse and mesocosm experiments will be conducted on key species from each habitat type to determine their responses to elevated inorganic carbon, salinity, temperature, and ultraviolet radiation.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Coastal zone '91 : Proceedings of the seventh symposium on coastal and ocean management","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Coastal zone '91 :  Seventh Symposium on Coastal and Ocean Management","conferenceDate":"July 8-12, 1991","conferenceLocation":"Long Beach, CA","language":"English","publisher":"American Society of Civil Engineers","isbn":"9780872628090 ","usgsCitation":"Keough, J.R., Doyle, T.W., and Stewart, R.E., 1991, Global climate change: USFWS coastal research, <i>in</i> Coastal zone '91 : Proceedings of the seventh symposium on coastal and ocean management, v. 4, Long Beach, CA, July 8-12, 1991, p. 3163-3177.","productDescription":"15 p.","startPage":"3163","endPage":"3177","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":371579,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":371578,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://cedb.asce.org/CEDBsearch/record.jsp?dockey=0073040"}],"volume":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Keough, Janet R.","contributorId":49300,"corporation":false,"usgs":true,"family":"Keough","given":"Janet","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":780381,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Doyle, Thomas W. 0000-0001-5754-0671 doylet@usgs.gov","orcid":"https://orcid.org/0000-0001-5754-0671","contributorId":703,"corporation":false,"usgs":true,"family":"Doyle","given":"Thomas","email":"doylet@usgs.gov","middleInitial":"W.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":780382,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stewart, Robert E. Jr.","contributorId":72861,"corporation":false,"usgs":true,"family":"Stewart","given":"Robert","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":780383,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70204129,"text":"70204129 - 1991 - Remote sensing of water quality","interactions":[],"lastModifiedDate":"2019-07-08T12:46:09","indexId":"70204129","displayToPublicDate":"1991-12-31T12:21:36","publicationYear":"1991","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"title":"Remote sensing of water quality","docAbstract":"<p>Water property data were collected within 3 cooling water reservoirs (active to inactive, large [1,068 ha] to small [68.6 ha]. oligotrophic to eutrophic) at 31 locations. A description of the water characteristics was obtained including algal pigments, total suspended particles, dissolved and particulate organic matter, and total particle absorption spectra. Field data included generated water volume reflectance spectra and secchi depth. Specialized regression techniques were used to derive specific absorption coefficients from measured water property concentrations and total particle absorption spectra. Subsequently, using first order approximations relating water volume reflectance to water intrinsic properties, generated absorption coefficients were combined with an optimization procedure that minimized the difference between the observed and predicted water volume reflectances resulting in specific backscatter coefficient estimates.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"1991 ACSM-ASPRS Annual Convention, Baltimore, MD, Mar. 25-29, 1991, Technical Papers. Vol. 3 - Remote Sensing","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"ACSM-ASPRS Annual Convention","conferenceDate":"Mar 25-29, 1991","conferenceLocation":"Baltimore, MD","language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","usgsCitation":"Ramsey III, E., and Jensen, J.R., 1991, Remote sensing of water quality, <i>in</i> 1991 ACSM-ASPRS Annual Convention, Baltimore, MD, Mar. 25-29, 1991, Technical Papers. Vol. 3 - Remote Sensing, Baltimore, MD, Mar 25-29, 1991, p. 363-372.","productDescription":"10 p.","startPage":"363","endPage":"372","costCenters":[],"links":[{"id":365341,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Carolina","otherGeospatial":"Savannah River","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ramsey III, Elijah 0000-0002-4518-5796","orcid":"https://orcid.org/0000-0002-4518-5796","contributorId":204796,"corporation":false,"usgs":true,"family":"Ramsey III","given":"Elijah","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":765648,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jensen, John R.","contributorId":216821,"corporation":false,"usgs":false,"family":"Jensen","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":765649,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70219223,"text":"70219223 - 1991 - Seasonal changes in microhabitat selection by rainbow trout in a small stream","interactions":[],"lastModifiedDate":"2021-03-31T14:18:08.384384","indexId":"70219223","displayToPublicDate":"1991-12-31T09:13:00","publicationYear":"1991","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":"Seasonal changes in microhabitat selection by rainbow trout in a small stream","docAbstract":"<p><span>Shifts in microhabitat selection by rainbow trout&nbsp;</span><i>Oncorhynchus mykiss</i><span>&nbsp;were related to seasonal and ontogenetic factors in a small stream characterized by short riffles, small pools, and boulder substrate. Resource availability did not differ significantly between summer and November sampling dates for most variables related to water velocity, substrate, and cover, although depths were greater and temperatures were significantly lower in November. Ontogenetic shifts were found for total depth, focal elevation, mean water column velocity, focal velocity, surface velocity, and substrate, but not for relative depth or temperature. When microhabitat selection was adjusted for fish size, selection was significantly different between seasons, most notably for velocity. Ontogenetic shifts in microhabitat use by young-of-year rainbow trout were interrupted by cooling winter temperatures. These changes resulted in substantially different microhabitat requirements for all rainbow trout size-classes in different seasons.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1991)120%3C0166:SCIMSB%3E2.3.CO;2","usgsCitation":"Baltz, D.M., Vondracek, B.C., Brown, L.R., and Moyle, P.B., 1991, Seasonal changes in microhabitat selection by rainbow trout in a small stream: Transactions of the American Fisheries Society, v. 120, no. 2, p. 166-176, https://doi.org/10.1577/1548-8659(1991)120%3C0166:SCIMSB%3E2.3.CO;2.","productDescription":"11 p.","startPage":"166","endPage":"176","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":384779,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"120","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Baltz, Donald M.","contributorId":208263,"corporation":false,"usgs":false,"family":"Baltz","given":"Donald","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":813269,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vondracek, Bruce C. bcv@usgs.gov","contributorId":904,"corporation":false,"usgs":true,"family":"Vondracek","given":"Bruce","email":"bcv@usgs.gov","middleInitial":"C.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":813270,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, Larry R. 0000-0001-6702-4531 lrbrown@usgs.gov","orcid":"https://orcid.org/0000-0001-6702-4531","contributorId":1717,"corporation":false,"usgs":true,"family":"Brown","given":"Larry","email":"lrbrown@usgs.gov","middleInitial":"R.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":813271,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Moyle, Peter B.","contributorId":117099,"corporation":false,"usgs":false,"family":"Moyle","given":"Peter","email":"","middleInitial":"B.","affiliations":[{"id":7214,"text":"University of California, Davis","active":true,"usgs":false}],"preferred":false,"id":813272,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70209168,"text":"70209168 - 1991 - Evaluation of wetland development and waterbird response at Elk Creek Wildlife management area, Lake Mills, Iowa, 1961 to 1990","interactions":[],"lastModifiedDate":"2020-03-20T08:32:40","indexId":"70209168","displayToPublicDate":"1991-12-31T08:21:55","publicationYear":"1991","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3750,"text":"Wetlands","onlineIssn":"1943-6246","printIssn":"0277-5212","active":true,"publicationSubtype":{"id":10}},"title":"Evaluation of wetland development and waterbird response at Elk Creek Wildlife management area, Lake Mills, Iowa, 1961 to 1990","docAbstract":"<p><span>A waterfowl habitat&nbsp;</span><span class=\"ScopusTermHighlight\">development</span><span>&nbsp;project along 7.5 miles (12.07 km) of stream was evaluated after 27 years. There was a modest 12% net increase in wetlands in impounded areas, but much of the&nbsp;</span><span class=\"ScopusTermHighlight\">wetland</span><span>&nbsp;vegetation changed from seasonally flooded, nonpersistent and persistent emergents to shallow, open-water areas. An unimpounded, downstream reference area had drier plant communities, probably resulting from reduced flooding. The loss of shallow vegetated wetlands could have significant impacts on both water quality functions and&nbsp;</span><span class=\"ScopusTermHighlight\">waterbird</span><span>&nbsp;populations. The overall project goal of increasing numbers and diversity of waterfowl was met, but waterfowl numbers and species composition changed more because of transplanting and nest-box programs than habitat modifications. Although impacts on birds of shallow wetlands such as rails and songbirds were not quantitatively assessed, it is likely that the numbers of such birds were reduced because their preferred habitats were reduced markedly. Use of smaller lateral impoundments and increased management for emergents would diversity&nbsp;</span><span class=\"ScopusTermHighlight\">waterbird</span><span>&nbsp;populations and increase dabbling duck production. © 1991 Society of&nbsp;</span><span class=\"ScopusTermHighlight\">Wetland</span><span>&nbsp;Scientists.</span></p>","language":"English","doi":"10.1007/BF03160852","issn":"02775212","usgsCitation":"Weller, M., Kaufmann, G., and Vohs, P., 1991, Evaluation of wetland development and waterbird response at Elk Creek Wildlife management area, Lake Mills, Iowa, 1961 to 1990: Wetlands, v. 11, no. 2, p. 245-262, https://doi.org/10.1007/BF03160852.","productDescription":"18 p. ","startPage":"245","endPage":"262","numberOfPages":"18","costCenters":[],"links":[{"id":373406,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Iowa","city":"Lake Mills ","otherGeospatial":"Elk Creek Wildlife ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.55682373046875,\n              43.40679346455295\n            ],\n            [\n              -93.5053253173828,\n              43.40679346455295\n            ],\n            [\n              -93.5053253173828,\n              43.42674390969713\n            ],\n            [\n              -93.55682373046875,\n              43.42674390969713\n            ],\n            [\n              -93.55682373046875,\n              43.40679346455295\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"11","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Weller, M.W.","contributorId":54562,"corporation":false,"usgs":true,"family":"Weller","given":"M.W.","email":"","affiliations":[],"preferred":false,"id":785216,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kaufmann, G.W.","contributorId":223493,"corporation":false,"usgs":false,"family":"Kaufmann","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":785217,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vohs, P.A.","contributorId":64621,"corporation":false,"usgs":true,"family":"Vohs","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":785218,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70187757,"text":"70187757 - 1991 - The distribution of seabirds and fish in relation to ocean currents in the southeastern Chukchi Sea","interactions":[],"lastModifiedDate":"2022-08-16T15:11:24.121734","indexId":"70187757","displayToPublicDate":"1991-12-31T00:00:00","publicationYear":"1991","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The distribution of seabirds and fish in relation to ocean currents in the southeastern Chukchi Sea","docAbstract":"<p>In late August 1988, we studied the distribution of seabirds in the southeastern Chukchi Sea, particularly in waters near a major seabird colony at Cape Thompson. Foraging areas were characterized using hydrographic data obtained from hydroacoustic surveys for fish. Murres (<i>Uria spp.</i>) and Black-legged Kitttiwakes&nbsp;<i>Rissa tridactyla</i> breeding at Cape Thompson fed mostly on Arctic cod, which are known from previous studies to be the most abundant pelagic fish in the region. Our hydroacoustic surveys revealed that pelagic fish were distributed widely, but densities were estimated to be low (e.g., 0.1-10 g∙m<sup>-3</sup>) throughout the study area and a few schools were recorded. Large feeding flocks of murres and kittiwakes were observed over fish schools with densities estimated to exceed 15 g∙m<span>﻿<sup>-3</sup>. Fish densities were higher in shallow Alaska Coastal Current waters than offshore in Bering Sea waters, and most piscivorous seabirds foraged in coastal waters. Poor kittiwake breeding success and a low frequency of fish in murre and kittiwake stomachs in late August suggested that fish densities were marginal for sustaining breeding seabirds at that time. Planktivorous Least Auklets&nbsp;<i>Aethia pusilla&nbsp;</i>and Parakeet Auklets&nbsp;<i>Cyclorrhynchus psittacula</i> foraged almost exclusively in Bering Sea waters. Short-tailed Shearwaters&nbsp;<i>Puffinus tenuirostris</i> and Tufted Puffins&nbsp;<i>Fratercula cirrhata&nbsp;</i>foraged in transitional waters at the front between Coastal and Bering Sea currents.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Studies of high-latitude seabirds. 1. Behavioural, energetic, and oceanographic aspects of seabird feeding ecology (Occasional Paper 68 of the Canadian Wildlife Service)","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Population Biology and Conservation of Marine Birds Symposium","conferenceDate":"April, 1989","conferenceLocation":"St. John's, NL","language":"English","publisher":"Canadian Wildlife Service","publisherLocation":"Ottawa, CA","usgsCitation":"Piatt, J.F., Wells, J.L., MacCharles, A., and Fadely, B.S., 1991, The distribution of seabirds and fish in relation to ocean currents in the southeastern Chukchi Sea, <i>in</i> Studies of high-latitude seabirds. 1. Behavioural, energetic, and oceanographic aspects of seabird feeding ecology (Occasional Paper 68 of the Canadian Wildlife Service), St. John's, NL, April, 1989, p. 21-31.","productDescription":"11 p.","startPage":"21","endPage":"31","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":341427,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":405185,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://publications.gc.ca/site/eng/9.855957/publication.html"}],"country":"United States","state":"Alaska","otherGeospatial":"Chukchi Sea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -171.826171875,\n              64.12019460255497\n            ],\n            [\n              -163.23486328125,\n              64.12019460255497\n            ],\n            [\n              -163.23486328125,\n              67.83412789868609\n            ],\n            [\n              -171.826171875,\n              67.83412789868609\n            ],\n            [\n              -171.826171875,\n              64.12019460255497\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59269bd2e4b0b7ff9fb489de","contributors":{"editors":[{"text":"Montevecchi, W.A.","contributorId":62052,"corporation":false,"usgs":true,"family":"Montevecchi","given":"W.A.","affiliations":[],"preferred":false,"id":696017,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Gaston, A.J.","contributorId":21545,"corporation":false,"usgs":false,"family":"Gaston","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":696018,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Piatt, John F. 0000-0002-4417-5748 jpiatt@usgs.gov","orcid":"https://orcid.org/0000-0002-4417-5748","contributorId":3025,"corporation":false,"usgs":true,"family":"Piatt","given":"John","email":"jpiatt@usgs.gov","middleInitial":"F.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":695514,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wells, John L.","contributorId":189278,"corporation":false,"usgs":false,"family":"Wells","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":695515,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"MacCharles, Andrea","contributorId":192114,"corporation":false,"usgs":false,"family":"MacCharles","given":"Andrea","email":"","affiliations":[],"preferred":false,"id":695516,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fadely, Brian S.","contributorId":184042,"corporation":false,"usgs":false,"family":"Fadely","given":"Brian","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":695517,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":81059,"text":"gap1 - 1991 - GAP Analysis Bulletin Number 1","interactions":[],"lastModifiedDate":"2018-12-21T13:14:48","indexId":"gap1","displayToPublicDate":"1991-12-31T00:00:00","publicationYear":"1991","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":30,"text":"GAP Bulletin","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"1","title":"GAP Analysis Bulletin Number 1","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1991, GAP Analysis Bulletin Number 1: GAP Bulletin 1, 25 p.","productDescription":"25 p.","costCenters":[{"id":37226,"text":"Core Science Analytics, Synthesis, and Libraries","active":true,"usgs":true},{"id":38315,"text":"GAP Analysis Project","active":true,"usgs":true}],"links":[{"id":195344,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b30e4b07f02db6b40d6","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":534943,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70193872,"text":"70193872 - 1991 - Sensitivity of greenback cutthroat trout to acidic pH and elevated aluminum","interactions":[],"lastModifiedDate":"2017-11-07T10:05:03","indexId":"70193872","displayToPublicDate":"1991-12-31T00:00:00","publicationYear":"1991","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":"Sensitivity of greenback cutthroat trout to acidic pH and elevated aluminum","docAbstract":"<p><span>The greenback cutthroat trout&nbsp;</span><i>Oncorhynchus clarki stomias</i><span><span>&nbsp;</span>is a threatened subspecies native to the upper South Platte and Arkansas rivers between Denver and Fort Collins, Colorado, an area also susceptible to acid deposition. In laboratory studies, we exposed this subspecies to nominal pHs of 4.5–6.5 and to nominal aluminum concentrations of 0, 50, 100, and 300 μg/L; the control was pH 6.5 treatment without Al. We used soft water that contained 1.3 mg Ca/L. Exposures of 7 d each were made for four early life stages: fertilized egg, eyed embryo, alevin, and swim-up larva. Effects were measured at the end of exposure and again after a recovery period lasting until 40 d posthatch. The alevin stage was the most sensitive: at pH 5.0 with no Al, survival was reduced by 68% and swimming duration by 76%; at pH 6.0 and 50 μg Al/L, swimming duration was reduced by 62%, but survival was not affected. Reductions in whole-body concentrations of Na, K, and Ca indicated organism stress. Sodium was reduced most—about 50% in alevins exposed to pH 5.0 without Al and to pH 6.0 with 50 μg Al/L. Growth and the ratio of RNA to DNA were not affected by any exposure. All responses that were affected during exposure returned to normal by 40 d posthatch. Overall, it appeared that pH 6.0 and 50 μg Al/L might be detrimental to greenback cutthroat trout populations.</span></p>","language":"English","publisher":"Wiley","doi":"10.1577/1548-8659(1991)120<0034:SOGCTT>2.3.CO;2","usgsCitation":"Woodward, D.F., Farag, A.M., Little, E.E., Steadman, B.L., and Yancik, R., 1991, Sensitivity of greenback cutthroat trout to acidic pH and elevated aluminum: Transactions of the American Fisheries Society, v. 120, no. 1, p. 34-42, https://doi.org/10.1577/1548-8659(1991)120<0034:SOGCTT>2.3.CO;2.","productDescription":"9 p.","startPage":"34","endPage":"42","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":348339,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","city":"Denver, Fort Collins","otherGeospatial":"Arkansas River, South Platte River ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.116943359375,\n              39.07251146922361\n            ],\n            [\n              -103.87847900390625,\n              39.07251146922361\n            ],\n            [\n              -103.87847900390625,\n              40.97575093157534\n            ],\n            [\n              -106.116943359375,\n              40.97575093157534\n            ],\n            [\n              -106.116943359375,\n              39.07251146922361\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"120","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a081f67e4b09af898c8cef4","contributors":{"authors":[{"text":"Woodward, D. F.","contributorId":85645,"corporation":false,"usgs":true,"family":"Woodward","given":"D.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":720834,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Farag, Aida M. 0000-0003-4247-6763 aida_farag@usgs.gov","orcid":"https://orcid.org/0000-0003-4247-6763","contributorId":1139,"corporation":false,"usgs":true,"family":"Farag","given":"Aida","email":"aida_farag@usgs.gov","middleInitial":"M.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":false,"id":720835,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Little, E. E.","contributorId":13187,"corporation":false,"usgs":true,"family":"Little","given":"E.","email":"","middleInitial":"E.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":false,"id":720836,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Steadman, B. L.","contributorId":176635,"corporation":false,"usgs":false,"family":"Steadman","given":"B.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":720837,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Yancik, R.","contributorId":200061,"corporation":false,"usgs":false,"family":"Yancik","given":"R.","email":"","affiliations":[],"preferred":false,"id":720838,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70195483,"text":"70195483 - 1991 - Numerical simulations of hydrothermal circulation resulting from basalt intrusions in a buried spreading center","interactions":[],"lastModifiedDate":"2018-02-16T13:11:45","indexId":"70195483","displayToPublicDate":"1991-12-31T00:00:00","publicationYear":"1991","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Numerical simulations of hydrothermal circulation resulting from basalt intrusions in a buried spreading center","docAbstract":"<p>A two-dimensional, one by two-kilometer section through the seafloor was simulated with a numerical model to investigate coupled fluid and heat flow resulting from basalt intrusions in a buried spreading center. Boundary and initial conditions and physical properties of both sediments and basalt were constrained by field surveys and drilling in the Guaymas Basin, central Gulf of California. Parametric variations in these studies included sediment and basalt permeability, anisotropy in sediment permeability, and the size of heat sources. Faults were introduced through new intrusions both before and after cooling.</p><p>Background heat input caused fluid convection at velocities ≤ 3 cm a<sup>−1</sup><span>&nbsp;</span>through shallow sediments. Eighty to ninety percent of the heat introduced at the base of the simulations exited through the upper, horizontal surface, even when the vertical boundaries were made permeable to fluid flow. The simulated injection of a 25–50 m thick basalt intrusion at a depth of 250 m resulted in about 10 yr of pore-fluid expulsion through the sea-floor in all cases, leaving the sediments above the intrusions strongly underpressured. A longer period of fluid recharge followed, sometimes accompanied by reductions in total seafloor heat output of 10% in comparison to pre-intrusion values. Additional discharge-recharge events were dispersed chaotically through the duration of the cooling period. These cycles in heat and fluid flow resulted from the response of the simulated system to a thermodynamic shock, the sudden emplacement of a large heat source, and not from mechanical displacement of sediments and pore fluids, which was not simulated.</p><p>Water/rock mass ratios calculated from numerical simulations are in good agreement with geochemical estimates from materials recovered from the Guaymas Basin, assuming a bulk basalt permeability value of at least 10<sup>−17</sup><span>&nbsp;</span>m<sup>2</sup>/(10<sup>−2</sup><span>&nbsp;</span>mD). The addition of faults through intrusions and sediments in these simulations did not facilitate continuous, rapid venting. Increased heat input at the base of the faults resulted in temporarily greater fluid discharge, but the flow could not be sustained because the modeled system could not recharge cold fluid quickly enough to remove sufficient heat through the vents.</p>","language":"English","publisher":"Elsevier B.V.","doi":"10.1016/0012-821X(91)90153-9","usgsCitation":"Fisher, A., and Narasimhan, T., 1991, Numerical simulations of hydrothermal circulation resulting from basalt intrusions in a buried spreading center: Earth and Planetary Science Letters, v. 103, no. 1-4, p. 100-115, https://doi.org/10.1016/0012-821X(91)90153-9.","productDescription":"16 p.","startPage":"100","endPage":"115","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":351732,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"103","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff2a4ae4b0da30c1bfd7d0","contributors":{"authors":[{"text":"Fisher, A.T.","contributorId":51528,"corporation":false,"usgs":true,"family":"Fisher","given":"A.T.","email":"","affiliations":[],"preferred":false,"id":728823,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Narasimhan, T.N.","contributorId":202548,"corporation":false,"usgs":false,"family":"Narasimhan","given":"T.N.","email":"","affiliations":[],"preferred":false,"id":728824,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70194854,"text":"70194854 - 1991 -  Transient eddy formation around headlands","interactions":[],"lastModifiedDate":"2018-01-23T16:10:04","indexId":"70194854","displayToPublicDate":"1991-12-31T00:00:00","publicationYear":"1991","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2312,"text":"Journal of Geophysical Research","active":true,"publicationSubtype":{"id":10}},"title":" Transient eddy formation around headlands","docAbstract":"<div class=\"t m0 x4 h5 y4 ff1 fs4 fc0 sc0 ls0 ws0\"><span class=\"current-selection\">Eddies </span><span class=\"current-selection\">with </span><span class=\"current-selection\">length </span><span class=\"current-selection\">scales </span><span class=\"current-selection\">of </span><span class=\"current-selection\">1-10 </span><span class=\"current-selection\">km </span><span class=\"current-selection\">are </span><span class=\"current-selection\">commonly </span><span class=\"current-selection\">observed </span><span class=\"current-selection\">in </span><span class=\"current-selection\">coastal </span><span class=\"current-selection\">waters </span><span class=\"current-selection\">and </span><span class=\"current-selection\">play </span><span class=\"current-selection\">an&nbsp;</span><span class=\"current-selection\">important </span><span class=\"current-selection\">role </span><span class=\"current-selection\">in </span><span class=\"current-selection\">the </span><span class=\"current-selection\">dispersion </span><span class=\"current-selection\">of </span><span class=\"current-selection\">water-borne </span><span class=\"current-selection\">materials. </span><span class=\"current-selection\">The </span><span class=\"current-selection\">generation </span><span class=\"current-selection\">and </span><span class=\"current-selection\">evolution </span><span class=\"current-selection\">of </span><span class=\"current-selection\">these&nbsp;</span><span class=\"current-selection\">eddies </span><span class=\"current-selection\">by </span><span class=\"current-selection\">oscillatory </span><span class=\"current-selection\">tidal </span><span class=\"current-selection\">flow </span><span class=\"current-selection\">around </span><span class=\"current-selection\">coastal </span><span class=\"current-selection\">headlands </span><span class=\"current-selection\">is </span><span class=\"current-selection\">investigated </span><span class=\"current-selection\">with </span><span class=\"current-selection\">analytical </span><span class=\"current-selection\">and </span><span class=\"current-selection\">nu</span><span class=\"current-selection\">merical </span><span class=\"current-selection\">models. </span><span class=\"current-selection\">Using </span><span class=\"current-selection\">shallow </span><span class=\"current-selection\">water </span><span class=\"current-selection\">depth-averaged </span><span class=\"current-selection\">vorticity </span><span class=\"current-selection\">dynamics, </span><span class=\"current-selection\">eddies </span><span class=\"current-selection\">are </span><span class=\"current-selection\">shown </span><span class=\"current-selection\">to </span><span class=\"current-selection\">form&nbsp;</span><span class=\"current-selection\">when </span><span class=\"current-selection\">flow </span><span class=\"current-selection\">separation </span><span class=\"current-selection\">occurs </span><span class=\"current-selection\">near </span><span class=\"current-selection\">the </span><span class=\"current-selection\">tip </span><span class=\"current-selection\">of </span><span class=\"current-selection\">the </span><span class=\"current-selection\">headland, </span><span class=\"current-selection\">causing </span><span class=\"current-selection\">intense </span><span class=\"current-selection\">vorticity </span><span class=\"current-selection\">generated </span><span class=\"current-selection\">along&nbsp;</span><span class=\"current-selection\">the </span><span class=\"current-selection\">headland </span><span class=\"current-selection\">to </span><span class=\"current-selection\">be </span><span class=\"current-selection\">injected </span><span class=\"current-selection\">into </span><span class=\"current-selection\">the </span><span class=\"current-selection\">interior. </span><span class=\"current-selection\">An </span><span class=\"current-selection\">analytic </span><span class=\"current-selection\">boundary </span><span class=\"current-selection\">layer </span><span class=\"current-selection\">model </span><span class=\"current-selection\">demonstrates </span><span class=\"current-selection\">that </span><span class=\"current-selection\">flow </span><span class=\"current-selection\">separation </span><span class=\"current-selection\">occurs </span><span class=\"current-selection\">when </span><span class=\"current-selection\">the </span><span class=\"current-selection\">pressure </span><span class=\"current-selection\">gradient </span><span class=\"current-selection\">along </span><span class=\"current-selection\">the </span><span class=\"current-selection\">boundary </span><span class=\"current-selection\">switches </span><span class=\"current-selection\">from </span><span class=\"current-selection\">favoring </span><span class=\"current-selection\">(ac</span><span class=\"current-selection\">celerating) </span><span class=\"current-selection\">to </span><span class=\"current-selection\">adverse </span><span class=\"current-selection\">(decelerating), </span><span class=\"current-selection\">and </span><span class=\"current-selection\">its </span><span class=\"current-selection\">occurrence </span><span class=\"current-selection\">depends </span><span class=\"current-selection\">principally </span><span class=\"current-selection\">on </span><span class=\"current-selection\">three </span><span class=\"current-selection\">parameters:&nbsp;</span><span class=\"current-selection\">the </span><span class=\"current-selection\">aspect </span><span class=\"current-selection\">ratio </span><span class=\"current-selection\">[b/a], </span><span class=\"current-selection\">where </span><span class=\"current-selection\">b </span><span class=\"current-selection\">and </span><span class=\"current-selection\">a </span><span class=\"current-selection\">are </span><span class=\"current-selection\">characteristic </span><span class=\"current-selection\">width </span><span class=\"current-selection\">and </span><span class=\"current-selection\">length </span><span class=\"current-selection\">scales </span><span class=\"current-selection\">of </span><span class=\"current-selection\">the </span><span class=\"current-selection\">headland;&nbsp;</span><span class=\"current-selection\">[H/CDa], </span><span class=\"current-selection\">where </span><span class=\"current-selection\">H is </span><span class=\"current-selection\">the </span><span class=\"current-selection\">water </span><span class=\"current-selection\">depth, </span><span class=\"current-selection\">CD </span><span class=\"current-selection\">is </span><span class=\"current-selection\">the </span><span class=\"current-selection\">depth-averaged </span><span class=\"current-selection\">drag </span><span class=\"current-selection\">coefficient; </span><span class=\"current-selection\">and </span><span class=\"current-selection\">[Uo/aa],&nbsp;</span><span class=\"current-selection\">where </span><span class=\"current-selection\">Uo </span><span class=\"current-selection\">and </span><span class=\"current-selection\">a </span><span class=\"current-selection\">are </span><span class=\"current-selection\">the </span><span class=\"current-selection\">magnitude </span><span class=\"current-selection\">and </span><span class=\"current-selection\">frequency </span><span class=\"current-selection\">of </span><span class=\"current-selection\">the </span><span class=\"current-selection\">far-field </span><span class=\"current-selection\">tidal </span><span class=\"current-selection\">flow. </span><span class=\"current-selection\">Simulations </span><span class=\"current-selection\">with </span><span class=\"current-selection\">a&nbsp;</span><span class=\"current-selection\">depth-averaged </span><span class=\"current-selection\">numerical </span><span class=\"current-selection\">model </span><span class=\"current-selection\">show </span><span class=\"current-selection\">a </span><span class=\"current-selection\">wide </span><span class=\"current-selection\">range </span><span class=\"current-selection\">of </span><span class=\"current-selection\">responses </span><span class=\"current-selection\">to </span><span class=\"current-selection\">changes </span><span class=\"current-selection\">in </span><span class=\"current-selection\">these </span><span class=\"current-selection\">parameters, </span><span class=\"current-selection\">including </span><span class=\"current-selection\">cases </span><span class=\"current-selection\">where </span><span class=\"current-selection\">no </span><span class=\"current-selection\">separation </span><span class=\"current-selection\">occurs, </span><span class=\"current-selection\">cases </span><span class=\"current-selection\">where </span><span class=\"current-selection\">only </span><span class=\"current-selection\">one </span><span class=\"current-selection\">eddy </span><span class=\"current-selection\">exists </span><span class=\"current-selection\">at </span><span class=\"current-selection\">a </span><span class=\"current-selection\">given </span><span class=\"current-selection\">time, </span><span class=\"current-selection\">and&nbsp;</span><span class=\"current-selection\">cases </span><span class=\"current-selection\">where </span><span class=\"current-selection\">bottom </span><span class=\"current-selection\">friction </span><span class=\"current-selection\">is </span><span class=\"current-selection\">weak </span><span class=\"current-selection\">enough </span><span class=\"current-selection\">that </span><span class=\"current-selection\">eddies </span><span class=\"current-selection\">produced </span><span class=\"current-selection\">during </span><span class=\"current-selection\">successive </span><span class=\"current-selection\">tidal cycles&nbsp;</span><span class=\"current-selection\">coexist, </span><span class=\"current-selection\">interacting </span><span class=\"current-selection\">strongly </span><span class=\"current-selection\">with </span><span class=\"current-selection\">each </span><span class=\"current-selection\">other. </span><span class=\"current-selection\">These </span><span class=\"current-selection\">simulations </span><span class=\"current-selection\">also </span><span class=\"current-selection\">demonstrate </span><span class=\"current-selection\">that </span><span class=\"current-selection\">in </span><span class=\"current-selection\">unsteady&nbsp;</span><span class=\"current-selection\">flow, </span><span class=\"current-selection\">a </span><span class=\"current-selection\">strong </span><span class=\"current-selection\">start-up </span><span class=\"current-selection\">vortex </span><span class=\"current-selection\">forms </span><span class=\"current-selection\">after </span><span class=\"current-selection\">the </span><span class=\"current-selection\">flow </span><span class=\"current-selection\">separates, </span><span class=\"current-selection\">leading </span><span class=\"current-selection\">to </span><span class=\"current-selection\">a </span><span class=\"current-selection\">much </span><span class=\"current-selection\">more </span><span class=\"current-selection\">intense </span><span class=\"current-selection\">patch&nbsp;</span><span class=\"current-selection\">of </span><span class=\"current-selection\">vorticity </span><span class=\"current-selection\">and </span><span class=\"current-selection\">stronger </span><span class=\"current-selection\">recirculation </span><span class=\"current-selection\">than </span><span class=\"current-selection\">found </span><span class=\"current-selection\">in </span><span class=\"current-selection\">steady </span><span class=\"current-selection\">flow.&nbsp;</span></div>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/90JC02029","usgsCitation":"Signell, R.P., and Geyer, W.R., 1991,  Transient eddy formation around headlands: Journal of Geophysical Research, v. 96, no. C2, p. 2561-2575, https://doi.org/10.1029/90JC02029.","productDescription":"15 p.","startPage":"2561","endPage":"2575","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":350551,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"96","issue":"C2","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"5a6857f4e4b06e28e9c65f43","contributors":{"authors":[{"text":"Signell, Richard P. rsignell@usgs.gov","contributorId":1435,"corporation":false,"usgs":true,"family":"Signell","given":"Richard","email":"rsignell@usgs.gov","middleInitial":"P.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":725673,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Geyer, W. Rockwell","contributorId":195908,"corporation":false,"usgs":false,"family":"Geyer","given":"W.","email":"","middleInitial":"Rockwell","affiliations":[],"preferred":false,"id":725674,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70194848,"text":"70194848 - 1991 - Wave processes and geologic responses on the floor of the Yellow Sea","interactions":[],"lastModifiedDate":"2018-01-23T15:15:20","indexId":"70194848","displayToPublicDate":"1991-12-31T00:00:00","publicationYear":"1991","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Wave processes and geologic responses on the floor of the Yellow Sea","docAbstract":"<p>The floor of the Yellow Sea is a geologically mundane surface: it is nearly horizontal, lacks relief, and, with few exceptions, is devoid of conspicuous geomorphologic features. However, it is the principal repository for the prodigious sediment load of the Huanghe (Yellow River); and, due to its inherent shallowness (average depth is 40 m), it is frequently stressed by waves generated by winter storms and typhoons. Analyses of mass physical properties of cores representing the upper few meters of sediment in the central and north-central Yellow Sea (near the Shandong Peninsula), in conjunction with analyses of slope stability, failure modes, and erodibility, permit an assessment of the likelihood and effect of dynamic, transient geologic events on the seabed.</p><p>Vane shear-strength profiles along with consolidation test data indicate that the present surface of the seabed is in a depositional mode and is compacting normally. in addition, liquid-limit profiles imply that in the study area these neritic sediments have been accumulating in an environment that probably has not been modified significantly since sea level reached its current level. There is no geotechnical evidence in the nine cores recovered that slope failures have occurred, and clasts, sand lenses or other manifestations of mass movements, including flows, also are absent. These observations support previous interpretations of seismic records. Moreover, slope stability analysis for static conditions shows that the sea floor is quite stable.</p><p>Regardless, shear-stress levels generated by cyclic loading during major storms may approach the sediment shear strengths, and, when coupled with concomitant excess pore pressures, could cause slope failure. Unless the failed beds collapsed or flowed, however, there probably would be little conspicuous evidence of such a failure. in fact, evaluation of the potential of these sediments for disintegrative behavior suggests that they are not prone to either collapse or flow.</p><p>Storm waves also generate oscillatory bottom currents that may erode the seabed. Whether the sediment is considered as cohesionless or cohesive, typhoons could have the potential to erode at all water depths within the Yellow Sea (i.e., to 90 m), and winter storms to water depths of 60 m or more. However, in the case of cohesive behavior, it could be that the effect of winter storms and most typhoons is generally less extreme. If the sea floor is repeatedly scoured, it is likely limited to the top few centimeters.</p><p>Despite the fact that storm waves may cause slope failure and are certainly responsible for frequent scouring, they probably leave only a subtle sedimentologic imprint on the seabed.</p><p><i>﻿</i>﻿</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"From shoreline to abyss: Contributions in marine geology in honor of Francis Parker Shepard","publisher":"SEPM Society for Sedimentary Geology","doi":"10.2110/pec.91.09","usgsCitation":"Booth, J.S., and Winters, W.J., 1991, Wave processes and geologic responses on the floor of the Yellow Sea, chap. <i>of</i> From shoreline to abyss: Contributions in marine geology in honor of Francis Parker Shepard, v. 46, https://doi.org/10.2110/pec.91.09.","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":350543,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"China, North Korea, South Korea","otherGeospatial":"Yellow Sea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              115.75195312499999,\n              30.486550842588485\n            ],\n            [\n              128.49609375,\n              30.486550842588485\n            ],\n            [\n              128.49609375,\n              41.705728515237524\n            ],\n            [\n              115.75195312499999,\n              41.705728515237524\n            ],\n            [\n              115.75195312499999,\n              30.486550842588485\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"46","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a6857f5e4b06e28e9c65f4a","contributors":{"authors":[{"text":"Booth, James S.","contributorId":93477,"corporation":false,"usgs":true,"family":"Booth","given":"James","email":"","middleInitial":"S.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":725643,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Winters, William J. bwinters@usgs.gov","contributorId":522,"corporation":false,"usgs":true,"family":"Winters","given":"William","email":"bwinters@usgs.gov","middleInitial":"J.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":725644,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70195959,"text":"70195959 - 1991 - Impact of exploratory wells, offshore Florida: A biological assessment","interactions":[],"lastModifiedDate":"2018-03-09T13:41:49","indexId":"70195959","displayToPublicDate":"1991-12-31T00:00:00","publicationYear":"1991","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1106,"text":"Bulletin of Marine Science","active":true,"publicationSubtype":{"id":10}},"title":"Impact of exploratory wells, offshore Florida: A biological assessment","docAbstract":"<p><span>Seven offshore exploratory oil well sites were examined in an effort to determine the ecological impact of exploratory drilling on the subtropical marine ecosystems of southern Florida, including seagrass beds and coral reefs. The time since drilling ranged from 2 to 29 years; water depths varied between 5 and 70 m. The major long-term ecological impact observed at these sites ranged from the creation of \"artificial-reef\" conditions to the physical destruction of hardbottom habitat that had not recovered in 29 years. Long-term ecological perturbation appeared to be limited to physical destruction and the deposition of drilling debris, which provided substratum for settling organisms. Significant deposits of drill muds or cuttings were not encountered at any of the sites, and there was no evidence of ecological damage from cuttings or drill muds. The results of this study pertain only to exploratory drilling that, unlike production wells that remain in place for tens of years, is a one-time perturbation to the habitat.</span></p>","language":"English","publisher":"University of Miami, Rosenstiel School of Marine and Atmospheric Science","usgsCitation":"Dustan, P.A., Lidz, B.H., and Shinn, E., 1991, Impact of exploratory wells, offshore Florida: A biological assessment: Bulletin of Marine Science, v. 48, no. 1, p. 94-124.","productDescription":"31 p.","startPage":"94","endPage":"124","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":352375,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Florida Keys","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.99072265625,\n              25.661333498952683\n            ],\n            [\n              -81.45263671875,\n              25.661333498952683\n            ],\n            [\n              -81.45263671875,\n              27.039556602163195\n            ],\n            [\n              -82.99072265625,\n              27.039556602163195\n            ],\n            [\n              -82.99072265625,\n              25.661333498952683\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -85.1220703125,\n              23.926013033021192\n            ],\n            [\n              -80.13427734374999,\n              23.926013033021192\n            ],\n            [\n              -80.13427734374999,\n              25.58208527870072\n            ],\n            [\n              -85.1220703125,\n              25.58208527870072\n            ],\n            [\n              -85.1220703125,\n              23.926013033021192\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"48","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff2a4ae4b0da30c1bfd7cc","contributors":{"authors":[{"text":"Dustan, Phillip A.","contributorId":138646,"corporation":false,"usgs":false,"family":"Dustan","given":"Phillip","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":730698,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lidz, Barbara H. blidz@usgs.gov","contributorId":2475,"corporation":false,"usgs":true,"family":"Lidz","given":"Barbara","email":"blidz@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":730699,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shinn, Eugene A.","contributorId":86708,"corporation":false,"usgs":true,"family":"Shinn","given":"Eugene A.","affiliations":[],"preferred":false,"id":730700,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70195474,"text":"70195474 - 1991 - Oxygen-isotope exchange and mineral alteration in gabbros of the Lower Layered Series, Kap Edvard Holm Complex, East Greenland","interactions":[],"lastModifiedDate":"2018-02-16T12:37:54","indexId":"70195474","displayToPublicDate":"1991-12-31T00:00:00","publicationYear":"1991","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Oxygen-isotope exchange and mineral alteration in gabbros of the Lower Layered Series, Kap Edvard Holm Complex, East Greenland","docAbstract":"<p><span>Multiple intrusions of gabbros, mafic dikes, and syenites in the Kap Edvard Holm Complex gave rise to prolonged circulation of meteoric hydrothermal solutions and extreme isotope exchange and mineral alteration in the 3600-m-thick Lower Layered Series gabbros. In the Lower Layered Series, δ</span><sup>18</sup><span>O of plagioclase varies from +0.3‰ to -5.8‰, and it decreases with an increase in the volume of secondary talc, chlorite, and actinolite. In the same gabbros, pyroxenes have a more restricted range in δ</span><sup>18</sup><span>O, from 5.0‰ to 3.8‰ and values of δ</span><sup>18</sup><span>O</span><sub>pyroxene&nbsp;</sub><span>are independent of the abundance of secondary minerals, which ranges from 14% to 30%. These relations indicate that large amounts of water continued to flow through the rocks at temperatures of &lt;500-600°C, altering the gabbros to assemblages of talc + chlorite + actinolite ± epidote ±albite and causing significant oxygen-isotope exchange in plagioclase, but not in pyroxene. The extensive low-temperature secondary mineralization and<span>&nbsp;</span></span><sup>18</sup><span>O depletion of plagioclase in the Lower Layered Series are associated with the later emplacement of dikes and gabbros and syenites, which created new fracture systems and provided heat sources for hydrothermal fluid circulation. This produced subsolidus mineral alteration and isotope exchange in the Lower Layered Series that are distinct from those in the Skaergaard and Cuillin gabbros of the North Atlantic Tertiary province, but are similar to those observed in some oceanic gabbros.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1991)019<0819:OIEAMA>2.3.CO;2","usgsCitation":"Fehlhaber, K.L., and Bird, D.K., 1991, Oxygen-isotope exchange and mineral alteration in gabbros of the Lower Layered Series, Kap Edvard Holm Complex, East Greenland: Geology, v. 19, no. 8, p. 819-822, https://doi.org/10.1130/0091-7613(1991)019<0819:OIEAMA>2.3.CO;2.","productDescription":"4 p.","startPage":"819","endPage":"822","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":351716,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Greenland","otherGeospatial":"Kap Edward Holm Complex","volume":"19","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff2a5de4b0da30c1bfd7e1","contributors":{"authors":[{"text":"Fehlhaber, Kristen L.","contributorId":42090,"corporation":false,"usgs":true,"family":"Fehlhaber","given":"Kristen","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":728771,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bird, Dennis K.","contributorId":9339,"corporation":false,"usgs":true,"family":"Bird","given":"Dennis","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":728772,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70189555,"text":"70189555 - 1991 - Geochemical evolution of acidic ground water at a reclaimed surface coal mine in western Pennsylvania","interactions":[],"lastModifiedDate":"2017-07-17T10:41:18","indexId":"70189555","displayToPublicDate":"1991-12-31T00:00:00","publicationYear":"1991","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Geochemical evolution of acidic ground water at a reclaimed surface coal mine in western Pennsylvania","docAbstract":"<p>Concentrations of dissolved sulfate and acidity in ground water increase downflow in mine spoil and underlying bedrock at a reclaimed surface coal mine in the bituminous field of western Pennsylvania. Elevated dissolved sulfate and negligible oxygen in ground water from bedrock about 100 feet below the water table suggest that pyritic sulfur is oxidized below the water table, in a system closed to oxygen. Geochemical models for the oxidation of pyrite (FeS<sub>2</sub>) and production of sulfate (SO<sub>4</sub><sup>2-</sup>) and acid (H<sup>+</sup>) are presented to explain the potential role of oxygen (O<sub>2</sub>) and ferric iron (Fe<sup>3+</sup>) as oxidants. Oxidation of pyrite by O<sub>2</sub> and Fe<sup>3+</sup> can occur under oxic conditions above the water table, whereas oxidation by Fe<sup>3+</sup> also can occur under anoxic conditions below the water table. The hydrated ferric-sulfate minerals roemerite [Fe<sup>2+</sup>Fe<sub>4</sub><sup>3+</sup>(SO<sub>4</sub>)<sub>4</sub>·14H<sub>2</sub>O], copiapite [Fe<sup>2+</sup>Fe<sub>4</sub><sup>3+</sup>(SO<sub>4</sub>)<sub>6</sub>(OH)<sub>2</sub>·20H<sub>2</sub>0], and coquimbite [Fe<sub>2</sub>(SO<sub>4</sub>)<sub>3</sub><span>·</span>9H<sub>2</sub>O] were identified with FeS<sub>2</sub> in coal samples, and form on the oxidizing surface of pyrite in an oxic system above the water table. These soluble ferric-sulfate 11 salts11 can dissolve with recharge waters or a rising water table releasing Fe<sup>3+</sup>, SO<sub>4</sub><sup>2-</sup>. and H<sup>+</sup>, which can be transported along closed-system ground-water flow paths to pyrite reaction sites where O<sub>2</sub> may be absent. The Fe<sup>3+</sup> transported to these sites can oxidize pyritic sulfur. The computer programs WATEQ4F and NEWBAL were used to compute chemical speciation and mass transfer, respectively, considering mineral dissolution and precipitation reactions plus mixing of waters from different upflow zones. Alternative mass-balance models indicate that (a) extremely large quantities of O<sub>2</sub>, over 100 times its aqueous solubility, can generate the observed concentrations of dissolved SO<sub>4</sub><sup>2-</sup> from FeS<sub>2</sub>, or (b) under anoxic conditions, Fe<sup>3+</sup> from dissolved ferric-sulfate minerals can oxidize FeS<sub>2</sub> along closed-system ground-water flow paths. In a system open to O<sub>2</sub>, such as in the unsaturated zone, the aqueous solubility of O<sub>2</sub> is not limiting, and oxidation of pyrite by O<sub>2</sub> and Fe<sup>3+</sup> accounts for most SO<sub>4</sub><sup>2-</sup> and Fe<sup>2+</sup> observed in acidic ground water. However, in a system closed to O<sub>2</sub>, such as in the saturated zone, O<sub>2</sub> solubility is limiting; hence, ferric oxidation of pyrite is a reasonable explanation for the observed elevated SO<sub>4</sub><sup>2-</sup> with increasing depth below the water table.</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings American Society of Mining and Reclamation, 1991","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"8th Annual Meeting of the ASSMR","conferenceDate":"May 14-17, 1991","conferenceLocation":"Durango, CO","language":"English","publisher":"American Society of Mining and Reclamation","usgsCitation":"Cravotta, C.A., 1991, Geochemical evolution of acidic ground water at a reclaimed surface coal mine in western Pennsylvania, <i>in</i> Proceedings American Society of Mining and Reclamation, 1991, Durango, CO, May 14-17, 1991, p. 43-68.","productDescription":"26 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,{"id":70014965,"text":"70014965 - 1991 - Organic matter and containment of uranium and fissiogenic isotopes at the Oklo natural reactors","interactions":[],"lastModifiedDate":"2025-05-28T16:26:53.233553","indexId":"70014965","displayToPublicDate":"1991-12-12T00:00:00","publicationYear":"1991","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Organic matter and containment of uranium and fissiogenic isotopes at the Oklo natural reactors","docAbstract":"<p><span>Some of the Precambrian natural fission reactors at Oklo in Gabon contain abundant organic matter</span><sup>1,2</sup><span>, part of which was liquefied at the time of criticality and subsequently converted to a graphitic solid</span><sup>3,4</sup><span>. The liquid organic matter helps to reduce U(VI) to U(IV) from aqueous solutions, resulting in the precipitation of uraninite</span><sup>5</sup><span>. It is known that in the prevailing reactor environments, precipitated uraninite grains incorporated fission products. We report here observations which show that these uraninite crystals were held immobile within the resolidified, graphitic bitumen. Unlike water-soluble (humic) organic matter, the graphitic bituminous organics at Oklo thus enhanced radionuclide containment. Uraninite encased in solid graphitic matter in the organic-rich reactor zones lost virtually no fissiogenic lanthanide isotopes. The first major episode of uranium and lead migration was caused by the intrusion of a swarm of adjacent dolerite dykes about 1,100 Myr after the reactors went critical. Our results from Oklo imply that the use of organic, hydrophobic solids such as graphitic bitumen as a means of immobilizing radionuclides in pretreated nuclear waste warrants further investigation.</span></p>","language":"English","publisher":"Springer Nature","doi":"10.1038/354472a0","issn":"00280836","usgsCitation":"Nagy, B., Gauthier-Lafaye, F., Holliger, P., Davis, D., Mossman, D., Leventhal, J., Rigali, M., and Parnell, J., 1991, Organic matter and containment of uranium and fissiogenic isotopes at the Oklo natural reactors: Nature, v. 354, no. 6353, p. 472-475, https://doi.org/10.1038/354472a0.","productDescription":"4 p.","startPage":"472","endPage":"475","costCenters":[],"links":[{"id":223739,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"354","issue":"6353","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6fc5e4b0c8380cd75c6b","contributors":{"authors":[{"text":"Nagy, B.","contributorId":47912,"corporation":false,"usgs":true,"family":"Nagy","given":"B.","email":"","affiliations":[],"preferred":false,"id":369727,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gauthier-Lafaye, F.","contributorId":98345,"corporation":false,"usgs":true,"family":"Gauthier-Lafaye","given":"F.","email":"","affiliations":[],"preferred":false,"id":369732,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Holliger, P.","contributorId":88884,"corporation":false,"usgs":true,"family":"Holliger","given":"P.","email":"","affiliations":[],"preferred":false,"id":369731,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Davis, D.W.","contributorId":67945,"corporation":false,"usgs":true,"family":"Davis","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":369729,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mossman, D.J.","contributorId":46225,"corporation":false,"usgs":true,"family":"Mossman","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":369726,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Leventhal, J.S.","contributorId":60640,"corporation":false,"usgs":true,"family":"Leventhal","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":369728,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Rigali, M.J.","contributorId":79243,"corporation":false,"usgs":true,"family":"Rigali","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":369730,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Parnell, J.","contributorId":24100,"corporation":false,"usgs":true,"family":"Parnell","given":"J.","affiliations":[],"preferred":false,"id":369725,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
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