{"pageNumber":"1748","pageRowStart":"43675","pageSize":"25","recordCount":68937,"records":[{"id":70197294,"text":"70197294 - 1992 - Modelling the bathymetry of the Antarctic continental shelf","interactions":[],"lastModifiedDate":"2018-05-25T15:02:56","indexId":"70197294","displayToPublicDate":"1993-12-31T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Modelling the bathymetry of the Antarctic continental shelf","docAbstract":"<p>Continental shelves are typically covered by relatively shallow waters (&lt;200 m) which deepen gradually from the coast to the shelf edge. The continental shelf around Antarctica is deeper than normal (400-700m) and is characterized in many areas by a nearshore trough (up to 1 km deep) that gradually shallows toward the shelf edge. We examine the cause for the unusual shelf bathymetry of Antarctica by 2-D numerical models that simulate the bathymetry along seismic line ODP-119 in Prydz Bay. Line ODP-119 was chosen because it is tied to to 5 ODP boreholes, and because the margin underwent little recent tectonic activity or changes in the glacial drainage pattern. The numerical models incorporate several factors that are likely to influence the bathymetry, such as the load of the ice cap, the isostatic response of the lithosphere, thermal and tectnoic subsidence of the margin, sea level changes, and the patterns of erosion and sedimentation across the margin. The models show that the observed bathymetry can be produced almost entirely by the sum of the outer-shelf sediment loading and inner-shelf unloading and by the load of the slope sediments. A simple statistical mdoel demonstrates that this distribution pattern of erosion and deposition can be generated by multiple cycles of ice sheet advances across the shelf, whereby in each cycle a thin (a few tens of meters) uniform layer of sediments is eroded from under the ice sheet and is redeposited seaward of the grounding line.</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Recent progress in Antarctic Earth Science","conferenceTitle":"Sixth International Symposium on Antarctic Earth Sciences","conferenceDate":"September 9-13, 1991","conferenceLocation":"Ranzan, JP","language":"English","publisher":"Terra Scientific Publishing Company","usgsCitation":"ten Brink, U., Rogers, W.P., and Kirkham, R., 1992, Modelling the bathymetry of the Antarctic continental shelf, <i>in</i> Recent progress in Antarctic Earth Science, Ranzan, JP, September 9-13, 1991, p. 763-771.","productDescription":"9 p.","startPage":"763","endPage":"771","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":354509,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":354508,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.terrapub.co.jp/e-library/aes/"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5b15a54de4b092d9651e22c3","contributors":{"authors":[{"text":"ten Brink, Uri S. 0000-0001-6858-3001 utenbrink@usgs.gov","orcid":"https://orcid.org/0000-0001-6858-3001","contributorId":127560,"corporation":false,"usgs":true,"family":"ten Brink","given":"Uri S.","email":"utenbrink@usgs.gov","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":736564,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rogers, William P.","contributorId":24220,"corporation":false,"usgs":true,"family":"Rogers","given":"William","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":736565,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kirkham, R. M.","contributorId":16915,"corporation":false,"usgs":false,"family":"Kirkham","given":"R. M.","affiliations":[],"preferred":false,"id":736566,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70007465,"text":"70007465 - 1992 - Management of habitat for breeding and migrating shorebirds in the Midwest","interactions":[],"lastModifiedDate":"2016-09-16T15:12:09","indexId":"70007465","displayToPublicDate":"1993-01-01T16:53:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":24,"text":"Fish and Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"13.2.14","title":"Management of habitat for breeding and migrating shorebirds in the Midwest","docAbstract":"<p>Shorebirds have always relied on the extensive network of natural wetlands from Texas to North Dakota. This network has now been fractured by wetland drainage and agriculture to the point where suitable wetlands are absent in much of the Midwest. Habitat loss and the resulting risk of population decline highlight the importance of management of shorebirds on refuges, hunting clubs, and preserves for both breeding and migrating species.</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":"Eldridge, J., 1992, Management of habitat for breeding and migrating shorebirds in the Midwest: Fish and Wildlife Leaflet 13.2.14, 6 p.","productDescription":"6 p.","costCenters":[],"links":[{"id":204597,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":115816,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://archive.usgs.gov/archive/sites/www.nwrc.usgs.gov/wdb/pub/wmh/13_2_14.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4c69e4b0c8380cd69c3c","contributors":{"authors":[{"text":"Eldridge, Jan","contributorId":101148,"corporation":false,"usgs":true,"family":"Eldridge","given":"Jan","email":"","affiliations":[],"preferred":false,"id":356433,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70156915,"text":"70156915 - 1992 - Semi-implicit finite difference methods for three-dimensional shallow water flow","interactions":[],"lastModifiedDate":"2018-09-19T13:12:00","indexId":"70156915","displayToPublicDate":"1993-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2023,"text":"International Journal for Numerical Methods in Fluids","active":true,"publicationSubtype":{"id":10}},"title":"Semi-implicit finite difference methods for three-dimensional shallow water flow","docAbstract":"<p><span>A semi-implicit finite difference method for the numerical solution of three-dimensional shallow water flows is presented and discussed. The governing equations are the primitive three-dimensional turbulent mean flow equations where the pressure distribution in the vertical has been assumed to be hydrostatic. In the method of solution a minimal degree of implicitness has been adopted in such a fashion that the resulting algorithm is stable and gives a maximal computational efficiency at a minimal computational cost. At each time step the numerical method requires the solution of one large linear system which can be formally decomposed into a set of small three-diagonal systems coupled with one five-diagonal system. All these linear systems are symmetric and positive definite. Thus the existence and uniquencess of the numerical solution are assured. When only one vertical layer is specified, this method reduces as a special case to a semi-implicit scheme for solving the corresponding two-dimensional shallow water equations. The resulting two- and three-dimensional algorithm has been shown to be fast, accurate and mass-conservative and can also be applied to simulate flooding and drying of tidal mud-flats in conjunction with three-dimensional flows. Furthermore, the resulting algorithm is fully vectorizable for an efficient implementation on modern vector computers.</span></p>","language":"English","publisher":"Wiley","doi":"10.1002/fld.1650150602","usgsCitation":"Casulli, V., and Cheng, R.T., 1992, Semi-implicit finite difference methods for three-dimensional shallow water flow: International Journal for Numerical Methods in Fluids, v. 15, no. 6, p. 629-648, https://doi.org/10.1002/fld.1650150602.","productDescription":"20 p.","startPage":"629","endPage":"648","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":307807,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"6","noUsgsAuthors":false,"publicationDate":"2005-07-05","publicationStatus":"PW","scienceBaseUri":"560bb6fae4b058f706e53e83","contributors":{"authors":[{"text":"Casulli, Vincenzo","contributorId":42302,"corporation":false,"usgs":true,"family":"Casulli","given":"Vincenzo","email":"","affiliations":[],"preferred":false,"id":571136,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cheng, Ralph T.","contributorId":69134,"corporation":false,"usgs":true,"family":"Cheng","given":"Ralph","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":571137,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70171564,"text":"70171564 - 1992 - Recovery of benthic-invertebrate communities in the White River near Indianapolis, Indiana, USA, following implementation of advanced treatment of municipal wastewater","interactions":[],"lastModifiedDate":"2016-06-03T16:49:08","indexId":"70171564","displayToPublicDate":"1993-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":883,"text":"Archiv fur Hydrobiologie","active":true,"publicationSubtype":{"id":10}},"title":"Recovery of benthic-invertebrate communities in the White River near Indianapolis, Indiana, USA, following implementation of advanced treatment of municipal wastewater","docAbstract":"<p><span>The City of Indianapolis, Indiana, USA, completed construction of advanced-wastewater-treatment systems to enlarge and upgrade existing secondary-treatment processes at the City&rsquo;s two municipal wastewater-treatment plants in 1983. These plants discharge their effluent to the White River. A study was begun in 1981 to evaluate the effects of municipal wastewater on the quality of the White River near Indianapolis. As part of this study, benthic-invertebrate samples were collected from one riffle upstream and two riffles downstream from the treatment plants annually from 1981 through 1987 (2 times before and 5 times after the plant improvements became operational). Samples were collected during periods of late-summer or early-fall low streamflow with a Surber sampler. Upstream from the wastewater-treatment plants, mayflies and caddisflies were the predominant organisms in the benthic-invertebrate community (from 32 to 93 percent of all organisms; median value is 67 percent) with other insects and mollusks also present. Before implementation of advanced wastewater-treatment, the benthic-invertebrate community downstream from the wastewater treatment plants was predominantly chironomids and oligochaetes (more than 98 percent of all organisms)-organisms that generally are tolerant of organic wastes. Few intolerant species, such as mayflies or caddisflies were found. Following implementation of advanced wastewater treatment, mayflies and caddisflies became numerically dominant in samples collected downstream from the plants. By 1986, these organisms accounted for more than 90 percent of all organisms found at the two downstream sites. The diversity of benthic invertebrates found in these samples resembled that at the upstream site. The improvement in the quality of municipal wastewater effluent resulted in significant improvements in the water quality of the White River downstream from Indianapolis. These changes in river quality, in turn, have resulted in a shift from mostly pollution-tolerant to mostly pollution-intolerant organisms in the benthic-invertebrate community of the White River downstream from Indianapolis. The recovery was not immediate, however, with one of the downstream sites requiring 3 years before pollution-intolerant organisms became numerically dominant.</span></p>","publisher":"Schweizerbart","usgsCitation":"Crawford, C.G., and Wangsness, D.J., 1992, Recovery of benthic-invertebrate communities in the White River near Indianapolis, Indiana, USA, following implementation of advanced treatment of municipal wastewater: Archiv fur Hydrobiologie, v. 126, no. 1, p. 67-84.","productDescription":"18 p.","startPage":"67","endPage":"84","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":322157,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Indiana","city":"Indianapolis","otherGeospatial":"Upper White River Basin","volume":"126","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5752aa35e4b053f0edd13e98","contributors":{"authors":[{"text":"Crawford, Charles G. 0000-0003-1653-7841 cgcrawfo@usgs.gov","orcid":"https://orcid.org/0000-0003-1653-7841","contributorId":1064,"corporation":false,"usgs":true,"family":"Crawford","given":"Charles","email":"cgcrawfo@usgs.gov","middleInitial":"G.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":631829,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wangsness, David J.","contributorId":81475,"corporation":false,"usgs":true,"family":"Wangsness","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":631830,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70007462,"text":"70007462 - 1992 - Ecology of playa lakes","interactions":[],"lastModifiedDate":"2016-09-16T15:15:33","indexId":"70007462","displayToPublicDate":"1992-12-31T16:44:00","publicationYear":"1992","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":"13.3.7","title":"Ecology of playa lakes","docAbstract":"<p>Between 25,000 and 30,000 playa lakes are in the playa lakes region of the southern high plains (Fig. 1). Most playas are in west Texas (about 20,000), and fewer, in New Mexico, Oklahoma, Kansas, and Colorado. The playa lakes region is one of the most intensively cultivated areas of North America. Dominant crops range from cotton in southern areas to cereal grains in the north. Therefore, most of the native short-grass prairie is gone, replaced by crops and, recently, grasses of the Conservation Reserve Program. Playas are the predominant wetlands and major wildlife habitat of the region.</p><p>More than 115 bird species, including 20 species of waterfowl, and 10 mammal species have been documented in playas. Waterfowl nest in the area, producing up to 250,000 ducklings in wetter years. Dominant breeding and nesting species are mallards and blue-winged teals. During the very protracted breeding season, birds hatch from April through August. Several million shorebirds and waterfowl migrate through the area each spring and fall. More than 400,000 sandhill cranes migrate through and winter in the region, concentrating primarily on the larger saline lakes in the southern portion of the playa lakes region.</p><p>The primary importance of the playa lakes region to waterfowl is as a wintering area. Wintering waterfowl populations in the playa lakes region range from 1 to 3 million birds, depending on fall precipitation patterns that determine the number of flooded playas. The most common wintering ducks are mallards, northern pintails, green-winged teals, and American wigeons. About 500,000 Canada geese and 100,000 lesser snow geese winter in the playa lakes region, and numbers of geese have increased annually since the early 1980’s. This chapter describes the physiography and ecology of playa lakes and their attributes that benefit waterfowl.</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":"Haukos, D.A., and Smith, L., 1992, Ecology of playa lakes: Fish and Wildlife Leaflet 13.3.7, 7 p.","productDescription":"7 p.","costCenters":[],"links":[{"id":115813,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://archive.usgs.gov/archive/sites/www.nwrc.usgs.gov/wdb/pub/wmh/13_3_7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":204595,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a056fe4b0c8380cd50dd1","contributors":{"authors":[{"text":"Haukos, David A. 0000-0001-5372-9960 dhaukos@usgs.gov","orcid":"https://orcid.org/0000-0001-5372-9960","contributorId":3664,"corporation":false,"usgs":true,"family":"Haukos","given":"David","email":"dhaukos@usgs.gov","middleInitial":"A.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":356427,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Loren M.","contributorId":88876,"corporation":false,"usgs":true,"family":"Smith","given":"Loren M.","affiliations":[],"preferred":false,"id":356428,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70206251,"text":"70206251 - 1992 - Use of ground-penetrating radar and continuous seismic-reflection profiling on surface-water bodies in environmental and engineering studies","interactions":[],"lastModifiedDate":"2019-10-28T06:37:20","indexId":"70206251","displayToPublicDate":"1992-12-31T14:34:08","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Use of ground-penetrating radar and continuous seismic-reflection profiling on surface-water bodies in environmental and engineering studies","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the symposium on the application of geophysics to engineering and environmental problems","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Symposium on the Application of Geophysics to Engineering and Environmental Problems ","conferenceDate":"April 26-29, 1992","conferenceLocation":"Oakbrook, IL","language":"English","publisher":"Edgemont Branch Golden Society of Engineering and Mineral Exploration Geophysicists","usgsCitation":"Haeni, F., 1992, Use of ground-penetrating radar and continuous seismic-reflection profiling on surface-water bodies in environmental and engineering studies, <i>in</i> Proceedings of the symposium on the application of geophysics to engineering and environmental problems, Oakbrook, IL, April 26-29, 1992.","productDescription":"18 p.","endPage":"145","numberOfPages":"162","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"links":[{"id":368625,"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":773933,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70206250,"text":"70206250 - 1992 - Use of ground-penetrating radar to investigate refilled scour holes at bridge foundations","interactions":[],"lastModifiedDate":"2019-10-28T06:39:52","indexId":"70206250","displayToPublicDate":"1992-12-31T14:29:26","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Use of ground-penetrating radar to investigate refilled scour holes at bridge foundations","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Fourth international conference on ground penetrating radar","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Fourth International Conference on Ground Penetrating Radar ","conferenceDate":"June 8-13, 1992","conferenceLocation":"Rovaniemi, Finland","language":"English","publisher":"Geologian tutkimuskeskus","usgsCitation":"Haeni, F., Placzek, G., and Trent, R., 1992, Use of ground-penetrating radar to investigate refilled scour holes at bridge foundations, <i>in</i> Fourth international conference on ground penetrating radar, Rovaniemi, Finland, June 8-13, 1992, p. 285-292.","productDescription":"8 p.","startPage":"285","endPage":"292","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"links":[{"id":368624,"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":773930,"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":773931,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Trent, R.E.","contributorId":190884,"corporation":false,"usgs":false,"family":"Trent","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":773932,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70216679,"text":"70216679 - 1992 - Coupling of a lake model with a high resolution climate model for climate change studies","interactions":[],"lastModifiedDate":"2020-11-27T20:19:05.18195","indexId":"70216679","displayToPublicDate":"1992-12-31T14:14:16","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Coupling of a lake model with a high resolution climate model for climate change studies","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the workshop on the effects of global climate change on hydrology and water resources at the catchment scale","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Workshop on the Effects of Global Climate Change on Hydrology, and Water Resources at the Catchment Scale","conferenceDate":"Feb 3-6, 1992","conferenceLocation":"Tsukuba, Japan","language":"English","publisher":"The Committee","usgsCitation":"Hostetler, S.W., Bates, G.T., and Giorgi, F., 1992, Coupling of a lake model with a high resolution climate model for climate change studies, <i>in</i> Proceedings of the workshop on the effects of global climate change on hydrology and water resources at the catchment scale, Tsukuba, Japan, Feb 3-6, 1992, 17 p.","productDescription":"17 p.","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":380863,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hostetler, Steven W. 0000-0003-2272-8302 swhostet@usgs.gov","orcid":"https://orcid.org/0000-0003-2272-8302","contributorId":3249,"corporation":false,"usgs":true,"family":"Hostetler","given":"Steven","email":"swhostet@usgs.gov","middleInitial":"W.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":805867,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bates, G. T.","contributorId":29147,"corporation":false,"usgs":false,"family":"Bates","given":"G.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":805868,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Giorgi, F.","contributorId":28186,"corporation":false,"usgs":true,"family":"Giorgi","given":"F.","email":"","affiliations":[],"preferred":false,"id":805869,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70209982,"text":"70209982 - 1992 - Strontium isotope characterization of the Ash Meadows ground-water system, southern Nevada, USA","interactions":[],"lastModifiedDate":"2020-05-07T18:43:03.472527","indexId":"70209982","displayToPublicDate":"1992-12-31T13:30:25","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Strontium isotope characterization of the Ash Meadows ground-water system, southern Nevada, USA","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Water-rock interaction: Proceedings of the 7th international symposium on water-rock interaction","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"7th International Symposium on Water-Rock Interaction","conferenceDate":"Jul 13-18, 1992","conferenceLocation":"Park City, UT","language":"English","publisher":"Balkema","usgsCitation":"Peterman, Z.E., Stuckless, J.S., Mahan, S.A., Marshall, B.D., Gutentag, E., and Downey, J.S., 1992, Strontium isotope characterization of the Ash Meadows ground-water system, southern Nevada, USA, <i>in</i> Water-rock interaction: Proceedings of the 7th international symposium on water-rock interaction, v. 1, Park City, UT, Jul 13-18, 1992, p. 825-829.","productDescription":"5 p.","startPage":"825","endPage":"829","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":374549,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Ash Meadows","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.55670166015625,\n              36.26420679934512\n            ],\n            [\n              -115.99365234375,\n              36.26420679934512\n            ],\n            [\n              -115.99365234375,\n              36.66621584042748\n            ],\n            [\n              -116.55670166015625,\n              36.66621584042748\n            ],\n            [\n              -116.55670166015625,\n              36.26420679934512\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Peterman, Zell E. 0000-0002-5694-8082 peterman@usgs.gov","orcid":"https://orcid.org/0000-0002-5694-8082","contributorId":167699,"corporation":false,"usgs":true,"family":"Peterman","given":"Zell","email":"peterman@usgs.gov","middleInitial":"E.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":788689,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stuckless, John S. 0000-0002-7536-0444 jstuckless@usgs.gov","orcid":"https://orcid.org/0000-0002-7536-0444","contributorId":4974,"corporation":false,"usgs":true,"family":"Stuckless","given":"John","email":"jstuckless@usgs.gov","middleInitial":"S.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":788690,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mahan, Shannon A. 0000-0001-5214-7774 smahan@usgs.gov","orcid":"https://orcid.org/0000-0001-5214-7774","contributorId":147159,"corporation":false,"usgs":true,"family":"Mahan","given":"Shannon","email":"smahan@usgs.gov","middleInitial":"A.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":788691,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Marshall, Brian D. 0000-0002-8093-0093 bdmarsha@usgs.gov","orcid":"https://orcid.org/0000-0002-8093-0093","contributorId":520,"corporation":false,"usgs":true,"family":"Marshall","given":"Brian","email":"bdmarsha@usgs.gov","middleInitial":"D.","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":788692,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gutentag, E. D.","contributorId":70015,"corporation":false,"usgs":true,"family":"Gutentag","given":"E. D.","affiliations":[],"preferred":false,"id":788693,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Downey, J. S.","contributorId":100013,"corporation":false,"usgs":true,"family":"Downey","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":788694,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70209981,"text":"70209981 - 1992 - Isotopic studies of fracture coatings at Yucca Mountain, Nevada, USA","interactions":[],"lastModifiedDate":"2020-05-07T18:25:01.150599","indexId":"70209981","displayToPublicDate":"1992-12-31T13:21:02","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Isotopic studies of fracture coatings at Yucca Mountain, Nevada, USA","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Water-rock interaction: Proceedings of the 7th international symposium on water-rock interaction-WRI-7","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"7th International Symposium on Water-Rock Interaction","conferenceDate":"Jul 13-18, 1992","conferenceLocation":"Park City, UT","language":"English","publisher":"Balkema","usgsCitation":"Marshall, B.D., Whelan, J.F., Peterman, Z.E., Futa, K., Mahan, S.A., and Stuckless, J.S., 1992, Isotopic studies of fracture coatings at Yucca Mountain, Nevada, USA, <i>in</i> Water-rock interaction: Proceedings of the 7th international symposium on water-rock interaction-WRI-7, v. 1, Park City, UT, Jul 13-18, 1992, p. 737-740.","productDescription":"4 p.","startPage":"737","endPage":"740","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":374548,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Yucca Mountain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.48254394531249,\n              36.91352904330221\n            ],\n            [\n              -116.43602371215822,\n              36.91352904330221\n            ],\n            [\n              -116.43602371215822,\n              36.95757376878687\n            ],\n            [\n              -116.48254394531249,\n              36.95757376878687\n            ],\n            [\n              -116.48254394531249,\n              36.91352904330221\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Marshall, Brian D. 0000-0002-8093-0093 bdmarsha@usgs.gov","orcid":"https://orcid.org/0000-0002-8093-0093","contributorId":520,"corporation":false,"usgs":true,"family":"Marshall","given":"Brian","email":"bdmarsha@usgs.gov","middleInitial":"D.","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":788683,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Whelan, J. F.","contributorId":45328,"corporation":false,"usgs":true,"family":"Whelan","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":788684,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peterman, Zell E. 0000-0002-5694-8082 peterman@usgs.gov","orcid":"https://orcid.org/0000-0002-5694-8082","contributorId":167699,"corporation":false,"usgs":true,"family":"Peterman","given":"Zell","email":"peterman@usgs.gov","middleInitial":"E.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":788685,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Futa, Kiyoto 0000-0001-8649-7510 kfuta@usgs.gov","orcid":"https://orcid.org/0000-0001-8649-7510","contributorId":619,"corporation":false,"usgs":true,"family":"Futa","given":"Kiyoto","email":"kfuta@usgs.gov","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":788686,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mahan, Shannon A. 0000-0001-5214-7774 smahan@usgs.gov","orcid":"https://orcid.org/0000-0001-5214-7774","contributorId":147159,"corporation":false,"usgs":true,"family":"Mahan","given":"Shannon","email":"smahan@usgs.gov","middleInitial":"A.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":788687,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Stuckless, John S. 0000-0002-7536-0444 jstuckless@usgs.gov","orcid":"https://orcid.org/0000-0002-7536-0444","contributorId":4974,"corporation":false,"usgs":true,"family":"Stuckless","given":"John","email":"jstuckless@usgs.gov","middleInitial":"S.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":788688,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70207871,"text":"70207871 - 1992 - Ecology and management of postbreeding waterfowl","interactions":[],"lastModifiedDate":"2020-01-16T11:59:54","indexId":"70207871","displayToPublicDate":"1992-12-31T11:55:01","publicationYear":"1992","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"5","title":"Ecology and management of postbreeding waterfowl","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Ecology and management of breeding waterfowl","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"University of Minnesota Press","isbn":"9780816684083","usgsCitation":"Hohman, W.L., Ankney, C.D., and Gordon, D., 1992, Ecology and management of postbreeding waterfowl, chap. 5 <i>of</i> Ecology and management of breeding waterfowl, p. 128-189.","productDescription":"62 p.","startPage":"128","endPage":"189","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":371308,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hohman, William L.","contributorId":73141,"corporation":false,"usgs":false,"family":"Hohman","given":"William","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":779597,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ankney, C. Davison","contributorId":112215,"corporation":false,"usgs":true,"family":"Ankney","given":"C.","email":"","middleInitial":"Davison","affiliations":[],"preferred":false,"id":779598,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gordon, David H.","contributorId":221670,"corporation":false,"usgs":false,"family":"Gordon","given":"David H.","affiliations":[],"preferred":false,"id":779599,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70205391,"text":"70205391 - 1992 - Regional evaluations of acid deposition effects on forests: Eastern spruce-fir","interactions":[],"lastModifiedDate":"2019-09-19T10:44:24","indexId":"70205391","displayToPublicDate":"1992-12-31T09:40:11","publicationYear":"1992","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"title":"Regional evaluations of acid deposition effects on forests: Eastern spruce-fir","docAbstract":"<p><span>Having reviewed the results of the Integrated Forest Study (IFS) project, we now try to place the results in a larger perspective by very briefly summarizing acid deposition effects and their potential role in forest health in the several forest types represented in the IFS project. This chapter gives brief overviews of the situation in eastern spruce-fir, eastern hardwood, and southern pine forests in North America; and a very brief overview of air pollution in arid forest ecosystems in Europe (with special emphasis on the situation in Norway where the single European IFS site was located). What follows in this chapter is by no means intended to be a comprehensive review of forest health and atmospheric deposition; such an analysis would require a volume of this size for each forest type and is well beyond the scope of this chapter. A comprehensive analysis of forest health and the role of atmospheric deposition has been published for Norway spruce in Europe (Schulze et al. 1989), and one is in preparation for red spruce (Eagar and Adams, in press); the reader is referred to those volumes for a far more detailed discussion than is possible here. The intent of this chapter is merely to highlight those aspects of forest health and atmospheric deposition that have bearing on, or that can be illuminated by, the IFS results.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Atmospheric deposition and forest nutrient cycling: A synthesis of the integrated forest study","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Springer","isbn":"9781461228066","usgsCitation":"Johnson, A., Friedland, A.J., Miller, E.K., Battles, J., Huntington, T.G., Vann, D.R., and Strimbeck, G.R., 1992, Regional evaluations of acid deposition effects on forests: Eastern spruce-fir, chap. <i>of</i> Atmospheric deposition and forest nutrient cycling: A synthesis of the integrated forest study, p. 495-570.","startPage":"495","endPage":"570","costCenters":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"links":[{"id":367470,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":367469,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://link.springer.com/chapter/10.1007/978-1-4612-2806-6_13"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Johnson, A. H.","contributorId":49645,"corporation":false,"usgs":true,"family":"Johnson","given":"A. H.","affiliations":[],"preferred":false,"id":771028,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friedland, A. J.","contributorId":28430,"corporation":false,"usgs":true,"family":"Friedland","given":"A.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":771029,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, E. K.","contributorId":218777,"corporation":false,"usgs":false,"family":"Miller","given":"E.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":771030,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Battles, J. J.","contributorId":21770,"corporation":false,"usgs":true,"family":"Battles","given":"J. J.","affiliations":[],"preferred":false,"id":771031,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Huntington, Thomas G. 0000-0002-9427-3530 thunting@usgs.gov","orcid":"https://orcid.org/0000-0002-9427-3530","contributorId":117440,"corporation":false,"usgs":true,"family":"Huntington","given":"Thomas","email":"thunting@usgs.gov","middleInitial":"G.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":771032,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Vann, D. R.","contributorId":219018,"corporation":false,"usgs":false,"family":"Vann","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":771033,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Strimbeck, G. R.","contributorId":219019,"corporation":false,"usgs":false,"family":"Strimbeck","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":771034,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70196621,"text":"70196621 - 1992 - Physical oceanographic investigation of Massachusetts and Cape Cod Bays","interactions":[],"lastModifiedDate":"2018-04-20T12:11:36","indexId":"70196621","displayToPublicDate":"1992-12-31T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Physical oceanographic investigation of Massachusetts and Cape Cod Bays","docAbstract":"<p>This physical oceanographic study of the Massachusetts Bays (fig. 1) was designed to provide for the first time a bay-wide description of the circulation and mixing processes on a seasonal basis. Most of the measurements were conducted between April 1990 and June 1991 and consisted of moored observations to study the current flow patterns (fig. 2), hydrographic surveys to document the changes in water properties (fig. 3), high-resolution surveys of velocity and water properties to provide information on the spatial variability of the flow, drifter deployments to measure the currents, and acquisition of satellite images to provide a bay-wide picture of the surface temperature and its spatial variability. A longterm objective of the Massachusetts Bays program is to develop an understanding of the transport of water, dissolved substances and particles throughout the bays. Because horizontal and vertical transport is important to biological, chemical, and geological processes in Massachusetts and Cape Cod Bays, this physical oceanographic study will have broad application and will improve the ability to manage and monitor the water and sediment quality of the Bays. </p><p>Key results are:</p><ul><li>There is a marked seasonal variation in stratification in the bays, from well mixed conditions during the winter to strong stratification in the summertime. The stratification acts as a partial barrier to exchange between the surface waters and the deeper waters and causes the motion of the surface waters to be decoupled from the more sluggish flow of the deep waters. </li><li>During much of the year, there is weak but persistent counterclockwise flow around the bays, made up of southwesterly flow past Cape Ann, southward flow along the western shore, and outflow north of Race Point. The data suggest that this residual flow pattern reverses in fall. Fluctuations caused by wind and density variations are typically larger than the long-term mean. </li><li>With the exception of western Massachusetts Bay, flushing of the Bays is largely the result of the mean throughflow. Residence time estimates of the surface waters range from 20-45 days. The deeper water has a longer residence time, but its value is difficult to estimate. There is evidence that the deep waters in Stellwagen Basin are not renewed between the onset of stratification and the fall cooling period.</li><li>Current measurements made near the new outfall site in western Massachusetts Bay suggest that water and material discharged there are not swept away in a consistent direction by a well-defined steady current but are mixed and transported by a variety of processes, including the action of tides, winds, and river inflow. One-day particle excursions are typically less than 10 km. The outfall is apparently located in a region to the west of the basin-wide residual flow pattern.</li><li>Observations in western Massachusetts Bay, near the location of the future Boston sewage outfall, show that the surficial sediments are episodically resuspended from the seafloor during storms. The observations suggest onshore transport of suspended material during tranquil periods and episodic offshore and southerly alongshore transport of resuspended sediments during storms. </li><li>The spatial complexity of the flow in the Massachusetts Bays is typical of nearshore areas that have irregular coastal shorelines and topography and currents that are forced locally by wind and river runoff as well as by the flow in adjacent regions. Numerical models are providing a mechanism to interpret the complex spatial flow patterns that cannot be completely resolved by field observations and to investigate key physical processes that control the physics of water and particle transport.<br></li></ul>","language":"English","publisher":"The Massachusetts Environmental Trust","usgsCitation":"Geyer, W.R., Gardner, G.B., Brown, W.S., Irish, J.D., Butman, B., Loder, T., and Signell, R.P., 1992, Physical oceanographic investigation of Massachusetts and Cape Cod Bays, 23 p.","productDescription":"23 p.","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":353621,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachussetts","otherGeospatial":"Cape Cod Bay, Massachussetts Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.4935302734375,\n              41.09591205639546\n            ],\n            [\n              -69.3072509765625,\n              41.09591205639546\n            ],\n            [\n              -69.3072509765625,\n              42.819580715795915\n            ],\n            [\n              -71.4935302734375,\n              42.819580715795915\n            ],\n            [\n              -71.4935302734375,\n              41.09591205639546\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff2814e4b0da30c1bfd741","contributors":{"authors":[{"text":"Geyer, W. Rockwell","contributorId":195908,"corporation":false,"usgs":false,"family":"Geyer","given":"W.","email":"","middleInitial":"Rockwell","affiliations":[],"preferred":false,"id":733791,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gardner, George B.","contributorId":204370,"corporation":false,"usgs":false,"family":"Gardner","given":"George","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":733792,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, Wendell S.","contributorId":204371,"corporation":false,"usgs":false,"family":"Brown","given":"Wendell","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":733793,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Irish, James D.","contributorId":177134,"corporation":false,"usgs":false,"family":"Irish","given":"James","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":733794,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Butman, Bradford 0000-0002-4174-2073 bbutman@usgs.gov","orcid":"https://orcid.org/0000-0002-4174-2073","contributorId":943,"corporation":false,"usgs":true,"family":"Butman","given":"Bradford","email":"bbutman@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":733795,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Loder, T.C.","contributorId":62817,"corporation":false,"usgs":true,"family":"Loder","given":"T.C.","email":"","affiliations":[],"preferred":false,"id":733796,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"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":733797,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70195040,"text":"70195040 - 1992 - Rare earth, major and trace element composition of Leg 127 sediments","interactions":[],"lastModifiedDate":"2018-02-05T15:53:27","indexId":"70195040","displayToPublicDate":"1992-12-31T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Rare earth, major and trace element composition of Leg 127 sediments","docAbstract":"<p>The relative effects of paleoceanographic and paleogeographic variations, sediment lithology, and diagenetic processes on the final preserved chemistry of Japan Sea sediments are evaluated by investigating the rare earth element (REE), major element, and trace element concentrations in 59 squeeze-cake whole-round and 27 physical-property sample residues from Sites 794, 795, and 797, cored during ODP Leg 127. </p><p>The most important variation in sedimentary chemical composition is the increase in SiO2 concentration through the Pliocene diatomaceous sequences, which dilutes most other major and trace element components by various degrees. This biogenic input is largest at Site 794 (Yamato Basin), moderately developed at Site 797 (Yamato Basin), and of only minor importance at Site 795 (Japan Basin), potentially reflecting basinal contrasts in productivity with the Yamato Basin recording greater biogenic input than the Japan Basin and with the easternmost sequence of Site 794 lying beneath the most productive waters. There are few systematic changes in solid-phase chemistry resulting from the opal-A/opal-CT or opal-CT/quartz silica phase transformations. Most major and trace element concentrations are controlled by the aluminosilicate fraction of the sediment, although the effects of diagenetic silica phases and manganese carbonates are of localized importance. </p><p>REE total abundances (IREE) in the Japan Sea are strongly dependent upon the paleoceanographic position of a given site with respect to terrigenous and biogenic sources. REE concentrations at Site 794 overall correspond well to aluminosilicate chemical indices and are strongly diluted by SiO2 within the upper Miocene-Pliocene diatomaceous sequence. Eu/Eu* values at Site 794 reach a maximum through the diatomaceous interval as well, most likely suggesting an association of Eu/Eu* with the siliceous component, or reflecting slight incorporation of a detrital feldspar phase. XREE at Site 795 also is affiliated strongly with aluminosilicate phases and yet is diluted only slightly by siliceous input. At Site 797, ΣRE E is not as clearly associated with the aluminosilicate fraction, is correlated moderately to siliceous input, and may be sporadically influenced by detrital heavy minerals originating from the nearby rifted continental fragment composing the Yamato Rise. </p><p>Ce/Ce* profiles at all three sites increase essentially monotonically with depth and record progressive diagenetic LREE fractionation. The observed Ce/Ce* increases are not responding to changes in the paleoceanographic oxygenation state of the overlying water, as there is no independent evidence to suggest the proper Oceanographic conditions. Ce/Ce* correlates slightly better with depth than with age at the two Yamato Basin sites. </p><p>The downhole increase in Ce/Ce* at Sites 794 and 797 is a passive response to the diagenetic transfer of LREE (except Ce) from sediment to interstitial water. At Site 795, the overall lack of correlation between Ce/Ce* and La/Y^ suggests that other processes mask the diagenetic behavior of all LREEs. First-order calculations of the Ce budget in Japan Sea waters and sediment indicate that ~20% of the excess Ce adsorbed by settling particles is recycled within the water column and that an additional -38% is recycled at or near the seafloor. Thus, because the remaining excess Ce is only -10% of the total Ce, there is not a large source of Ce to the deeply buried sediment, further suggesting that the downhole increase in Ce/Ce* is a passive response to diagenetic behavior of the other LREEs. The REE chemistry of Japan Sea sediment therefore predicts successive downhole addition of LREEs to deeply buried interstitial waters.</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the Ocean Drilling Program, Scientific Results","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"language":"English","publisher":"Ocean Drilling Program","usgsCitation":"Murray, R., Buchholtz ten Brink, M.R., Brumsack, H., Gerlach, D.C., and Russ, G.P., 1992, Rare earth, major and trace element composition of Leg 127 sediments, <i>in</i> Proceedings of the Ocean Drilling Program, Scientific Results, v. 127/128, no. 1, p. 677-695.","productDescription":"19 p.","startPage":"677","endPage":"695","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":351024,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              124.71679687499999,\n              29.916852233070173\n            ],\n            [\n              145.634765625,\n              29.916852233070173\n            ],\n            [\n              145.634765625,\n              46.98025235521883\n            ],\n            [\n              124.71679687499999,\n              46.98025235521883\n            ],\n            [\n              124.71679687499999,\n              29.916852233070173\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"127/128","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a797b95e4b00f54eb1f5e1e","contributors":{"authors":[{"text":"Murray, R.W.","contributorId":6196,"corporation":false,"usgs":true,"family":"Murray","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":726694,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buchholtz ten Brink, Marilyn R.","contributorId":88021,"corporation":false,"usgs":true,"family":"Buchholtz ten Brink","given":"Marilyn","email":"","middleInitial":"R.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":726695,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brumsack, Hans-Juergen","contributorId":61141,"corporation":false,"usgs":true,"family":"Brumsack","given":"Hans-Juergen","email":"","affiliations":[],"preferred":false,"id":726696,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gerlach, David C.","contributorId":138786,"corporation":false,"usgs":false,"family":"Gerlach","given":"David","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":726697,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Russ, G. Price","contributorId":138787,"corporation":false,"usgs":false,"family":"Russ","given":"G.","email":"","middleInitial":"Price","affiliations":[],"preferred":false,"id":726698,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70195421,"text":"70195421 - 1992 - On the age of the penultimate full glaciation of New England","interactions":[],"lastModifiedDate":"2018-04-23T09:43:08","indexId":"70195421","displayToPublicDate":"1992-12-31T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1727,"text":"GSA Special Papers","active":true,"publicationSubtype":{"id":10}},"title":"On the age of the penultimate full glaciation of New England","docAbstract":"<p>Tills that discontinuously underlie the late Wisconsinan till throughout New England represent the penultimate full glaciation of the region. In southern New England, the late Wisconsinan till and the tills that locally underlie it are informally referred to as upper and lower tills, respectively. For the most part, the ages of the lower tills are not firmly established, and regional correlations between occurrences of lower till, including those on Long Island, New York, are tenuous. Where a lower till underlies deposits having limiting middle Wisconsinan radiocarbon ages (e.g., the Montauk till member of the Manhassett Formation on Long Island at Port Washington, New York, and the lower till at New Sharon, Maine), many workers have assigned the till an early Wisconsinan age. However, lower tills throughout much of New England may be Illinoian or older in age and may correlate with a lower till exposed at Sankaty Head, Nantucket Island, Massachusetts, that is pre-Sangamonian in age. The till at Sankaty Head lies below marine beds containing marine faunas indicative of sea-water temperatures both warmer and slightly cooler than those off Nantucket today and that have uranium-thorium and amino-acid racemization (AAR) age estimates suggesting a Sangamonian age (marine oxygen-isotope stage 5).</p><p>The lower till at Sankaty Head and the Montauk till member on Long Island were deposited during a full glaciation of New England that was at least as extensive as the late Wisconsinan advance of the Laurentide ice. Global ice-volume data from the marine oxygen-isotope record and the late Pleistocene eustatic sea-level record inferred from raised coral terraces support an advance of this magnitude during marine oxygenisotope stage 6, but not during stage 4.</p><p>An early Wisconsinan age of the southern New England lower tills and, hence, of the penultimate glaciation there is problematic in terms of the pre-Sangamonian age of the lower till on Nantucket, and in terms of the late Pleistocene global ice-volume and sea-level records. An Illinoian age for the tills and for the penultimate full glaciation of New England is compatible with all the available evidence except some equivocal radiocarbon ages and AAR age estimates.</p>","largerWorkTitle":"The Last Interglacial-Glacial Transition in North America","language":"English","publisher":"Geological Society of America","doi":"10.1130/SPE270-p163","usgsCitation":"Oldale, R.N., and Colman, S., 1992, On the age of the penultimate full glaciation of New England: GSA Special Papers, v. 270, p. 163-170, https://doi.org/10.1130/SPE270-p163.","productDescription":"8 p.","startPage":"163","endPage":"170","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":351588,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","volume":"270","noUsgsAuthors":false,"publicationDate":"1992-01-01","publicationStatus":"PW","scienceBaseUri":"5aff2815e4b0da30c1bfd749","contributors":{"authors":[{"text":"Oldale, R. N.","contributorId":92680,"corporation":false,"usgs":true,"family":"Oldale","given":"R.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":728526,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Colman, S.M.","contributorId":32851,"corporation":false,"usgs":true,"family":"Colman","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":728527,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70189554,"text":"70189554 - 1992 - Acid base accounting--An improved method of interpreting overburden chemistry to predict the quality of coal-mine drainage","interactions":[],"lastModifiedDate":"2017-07-17T10:17:38","indexId":"70189554","displayToPublicDate":"1992-12-31T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Acid base accounting--An improved method of interpreting overburden chemistry to predict the quality of coal-mine drainage","docAbstract":"<p>Acidic mine drainage (AMD), which results from the accelerated oxidation of pyrite (FeS<sub>2</sub> ) in mined coal and overburden, has contaminated thousands of miles of streams in the Appalachian region of the United States. Acid‐base accounting (ABA), which simplifies the complex hydrogeochemical system through use of a limited number of variables, commonly is used to predict the post‐mining occurrence of AMD. ABA involves the measurement of sulfur (S) and carbonate (CO<sub>3</sub>) concentrations in coal‐bearing rocks and the computation of overburden net‐neutralization potential (NNP) in units of tons of calcium carbonate per thousand tons of rock (tons CaCO3/1,000 ton) (Sobek and others, 1978). ABA was developed on the assumption that the stoichiometry of the following overall reaction of FeS<sub>2</sub> and CaCO<sub>3</sub> can be used to convert acid (H<sup>+</sup>) into units of CaCO<sub>3</sub>:</p><p>FeS<sub>2</sub> + CaCO<sub>3</sub> + 3.75 O<sub>2</sub> + 1.5 H<sub>2</sub>O --&gt; Fe(OH)<sub>3</sub> + 2 SO<sub>4</sub><sup>-2</sup> + 2 Ca<sup>+2</sup> + 2 CO<sub>2</sub>(g), (1)<br></p><p> where the H + from 1 mol (mole) of FeS2 [64 g (gram) of S] is neutralized by 2 mol of CaCO3 (200 g). This method presumes that gaseous carbon dioxide (CO2 ) will exsolve. Thus 3.125 g CaCO3 will neutralize the acid from 1 g S; or 31.25 tons of CaCO<sub>3</sub> will neutralize the acid from 1,000 tons of rock that contains 1.0 percent pyritic S. The total S concentration, in percent, is multiplied by 31.25 and is assumed to be pyritic and acid‐producing in order to compute maximum potential acidity (MPA) for comparison with neutralization potential (NP), in units of tons CaCO<sub>3</sub> /1,000 ton (Sobek and others, 1978). NNP is computed by subtracting mass‐ weighted MPA from NP (Smith and Brady, 1990). if the value of NNP is less than zero, the acid‐producing potential of the rock exceeds its neutralization potential and if mined, therefore, would be expected to produce AMD.</p>","largerWorkTitle":"Proceedings Thirteenth Annual West Virginia Surface Mine Drainage Task Force Symposium","conferenceTitle":"Thirteenth Annual West Virginia Surface Mine Drainage Task Force Symposium","conferenceDate":"April 8-9, 1992","conferenceLocation":"Morgantown, WV","language":"English","publisher":"West Virginia Surface Mine Drainage Task Force","usgsCitation":"Brady, K., and Cravotta, C.A., 1992, Acid base accounting--An improved method of interpreting overburden chemistry to predict the quality of coal-mine drainage, <i>in</i> Proceedings Thirteenth Annual West Virginia Surface Mine Drainage Task Force Symposium, Morgantown, WV, April 8-9, 1992, 8 p.","productDescription":"8 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":343925,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":343924,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://wvmdtaskforce.com/past-symposium-papers/1992-symposium-papers/"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"596dcca8e4b0d1f9f06275a5","contributors":{"authors":[{"text":"Brady, Keith","contributorId":92764,"corporation":false,"usgs":true,"family":"Brady","given":"Keith","affiliations":[],"preferred":false,"id":705156,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cravotta, Charles A. III, 0000-0003-3116-4684 cravotta@usgs.gov","orcid":"https://orcid.org/0000-0003-3116-4684","contributorId":2193,"corporation":false,"usgs":true,"family":"Cravotta","given":"Charles","suffix":"III,","email":"cravotta@usgs.gov","middleInitial":"A.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":false,"id":705157,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70187780,"text":"70187780 - 1992 - Deep-water facies of the Lisburne Group, west-central Brooks Range, Alaska","interactions":[],"lastModifiedDate":"2018-05-07T21:23:56","indexId":"70187780","displayToPublicDate":"1992-12-31T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Deep-water facies of the Lisburne Group, west-central Brooks Range, Alaska","docAbstract":"<p>Deep-water lithofacies of the Lisburne Group (chiefly Carboniferous) occur in thurst sheets in the western part of the foreland fold-and-thrust belt of the Brooks Range and represent at least three discrete units. The Kuna Formation (Brooks Range allochthon) consists mostly of spiculitic mudstone and lesser shale; subordinate carbonate layers are chiefly diagenetic dolomite. The Akmalik Chert (Picnic Creek allochthon) is mostly radiolarian-spiculitic chert; rare limy beds are calcitized radiolarite. The Rim Butte unit (Ipnavik river allochthon) consists chiefly of calcareous turbidites, derived from shallow- and deep-water sources, interbedded with spiculitic mudstone. Much of the material in the turbidites came from a contemporaneous carbonate platform and margin, but some fossils and lithic clasts were eroded from older, already lithified carbonate-platform rocks. All three units appear to be roughly coeval in the Howard Pass area and are chiefly late Tournaisian and early Viséan (late Early Mississippian) in age.</p><p>Shallow-water lithofacies of the Lisburne Group exposed in the Howard Pass area (Brooks Range allochthon) are mostly of Viséan and younger (Late Mississippian) age. Thus, these carbonate-platform rocks were not the source of the calcareous turbidites in the Rim Butte unit. Rim Butte turbidites could have been derived from older carbonate-platform rocks such as the Utukok Formation of Tournaisian age (Kelly River allochthon) exposed mainly to the west of the Howard Pass quadrangle.</p>","largerWorkTitle":"Proceedings: 1992 international conference on Arctic margins (MMS 94-0040)","conferenceTitle":"1992 International Conference on Arctic Margins (ICAM)","conferenceDate":"September 2-3, 1992","conferenceLocation":"Anchorage, AK","language":"English","publisher":"Bureau of Ocean Energy Management","publisherLocation":"Anchorage, AK","usgsCitation":"Dumoulin, J.A., Harris, A.G., and Schmidt, J.M., 1992, Deep-water facies of the Lisburne Group, west-central Brooks Range, Alaska, <i>in</i> Proceedings: 1992 international conference on Arctic margins (MMS 94-0040), Anchorage, AK, September 2-3, 1992, p. 77-82.","productDescription":"6 p.","startPage":"77","endPage":"82","costCenters":[{"id":114,"text":"Alaska Science 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Kazuya","contributorId":15654,"corporation":false,"usgs":true,"family":"Fujita","given":"Kazuya","email":"","affiliations":[],"preferred":false,"id":696072,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Dumoulin, Julie A. 0000-0003-1754-1287 dumoulin@usgs.gov","orcid":"https://orcid.org/0000-0003-1754-1287","contributorId":203209,"corporation":false,"usgs":true,"family":"Dumoulin","given":"Julie","email":"dumoulin@usgs.gov","middleInitial":"A.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":695591,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harris, Anita G.","contributorId":50162,"corporation":false,"usgs":true,"family":"Harris","given":"Anita","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":695592,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schmidt, Jeanine M. jschmidt@usgs.gov","contributorId":3138,"corporation":false,"usgs":true,"family":"Schmidt","given":"Jeanine","email":"jschmidt@usgs.gov","middleInitial":"M.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":695593,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70016880,"text":"70016880 - 1992 - A tsunami about 1000 years ago in Puget Sound, Washington","interactions":[],"lastModifiedDate":"2025-09-16T16:22:38.910592","indexId":"70016880","displayToPublicDate":"1992-12-04T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"A tsunami about 1000 years ago in Puget Sound, Washington","docAbstract":"<p><span>Water surged from Puget Sound sometime between 1000 and 1100 years ago, overrunning tidal marshes and mantling them with centimeters of sand. One overrun site is 10 kilometers northwest of downtown Seattle; another is on Whidbey Island, some 30 kilometers farther north. Neither site has been widely mantled with sand at any other time in the past 2000 years. Deposition of the sand coincided—to the year or less—with abrupt, probably tectonic subsidence at the Seattle site and with landsliding into nearby Lake Washington. These findings show that a tsunami was generated in Puget Sound, and they tend to confirm that a large shallow earthquake occurred in the Seattle area about 1000 years ago.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.258.5088.1614","issn":"00368075","usgsCitation":"Atwater, B., and Moore, A., 1992, A tsunami about 1000 years ago in Puget Sound, Washington: Science, v. 258, no. 5088, p. 1614-1617, https://doi.org/10.1126/science.258.5088.1614.","productDescription":"4 p.","startPage":"1614","endPage":"1617","costCenters":[],"links":[{"id":495739,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://zenodo.org/record/1231020","text":"External Repository"},{"id":224901,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Puget Sound","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -123.65886846523934,\n              49.00731757648293\n            ],\n            [\n              -123.65886846523934,\n              47.1048310775121\n            ],\n            [\n              -122.15457987611427,\n              47.1048310775121\n            ],\n            [\n              -122.15457987611427,\n              49.00731757648293\n            ],\n            [\n              -123.65886846523934,\n              49.00731757648293\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"258","issue":"5088","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e607e4b0c8380cd470f0","contributors":{"authors":[{"text":"Atwater, Brian F. atwater@usgs.gov","contributorId":149872,"corporation":false,"usgs":true,"family":"Atwater","given":"Brian F.","email":"atwater@usgs.gov","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":374745,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, A.L.","contributorId":70931,"corporation":false,"usgs":true,"family":"Moore","given":"A.L.","email":"","affiliations":[],"preferred":false,"id":374746,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70169037,"text":"70169037 - 1992 - Herbicide and nitrate variation in alluvium underlying a cornfield at a site in Iowa County, Iowa","interactions":[],"lastModifiedDate":"2016-03-11T16:02:13","indexId":"70169037","displayToPublicDate":"1992-12-01T17:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2529,"text":"Journal of the American Water Resources Association","active":true,"publicationSubtype":{"id":10}},"title":"Herbicide and nitrate variation in alluvium underlying a cornfield at a site in Iowa County, Iowa","docAbstract":"<p><span>A hydrologic investigation to determine vertical and seasonal variation of atrazine, alachlor, cyanazine, and nitrate at one location and to relate the variation to ground-water movement in the Iowa River alluvium was conducted in Iowa County, Iowa, from March 1986 to December 1987. Water samples were collected at discrete intervals through the alluvial sequence from the soil zone to the base of the aquifer. Alachlor, atrazine, and cyanazine were detected most frequently in the soil zone but also were present in the upper part of the alluvial aquifer. Alachlor was detected sporadically, whereas, atrazine, cyanazine, and nitrate were present throughout the year. In the alluvial aquifer, the herbicides generally were not detected during 1986 and were present in detectable concentrations for only a short period of time in the upper 1.6 meters of the aquifer during 1987. Nitrate was present throughout the alluvium and was stratified in the alluvial aquifer. The largest nitrate concentrations were detected in the middle part of the aquifer. Nitrate concentrations were variable only in the upper 2 meters of the aquifer. Vertical movement of herbicides and nitrate in the soil correlated with precipitation and degree of saturation. A clay layer retarded vertical movement of atrazine but not nitrate from the soil layer to the aquifer. Vertical movement could not account for the chemical variation in the alluvial aquifer.</span></p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the American Water Resources Association","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Water Resources Association","publisherLocation":"Herndon, VA","doi":"10.1111/j.1752-1688.1992.tb04012.x","usgsCitation":"Kalkhoff, S., Detroy, M., Cherryholmes, K., and Kuzniar, R., 1992, Herbicide and nitrate variation in alluvium underlying a cornfield at a site in Iowa County, Iowa: Journal of the American Water Resources Association, v. 28, no. 6, p. 1001-1011, https://doi.org/10.1111/j.1752-1688.1992.tb04012.x.","productDescription":"11 p.","startPage":"1001","endPage":"1011","numberOfPages":"11","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":318831,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Iowa","county":"Iowa County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-91.8318,41.8617],[-91.8327,41.775],[-91.8335,41.6865],[-91.8337,41.6006],[-91.827,41.6001],[-91.8291,41.5116],[-91.9463,41.5108],[-92.0659,41.5104],[-92.183,41.5098],[-92.2995,41.5096],[-92.2986,41.6008],[-92.3017,41.6008],[-92.3014,41.6889],[-92.2999,41.7765],[-92.299,41.8623],[-92.1832,41.8626],[-92.066,41.8627],[-91.949,41.8618],[-91.8318,41.8617]]]},\"properties\":{\"name\":\"Iowa\",\"state\":\"IA\"}}]}","volume":"28","issue":"6","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","scienceBaseUri":"56e3fa4fe4b0f59b85d49444","contributors":{"authors":[{"text":"Kalkhoff, S. J.","contributorId":28967,"corporation":false,"usgs":true,"family":"Kalkhoff","given":"S. J.","affiliations":[],"preferred":false,"id":622648,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Detroy, M.G.","contributorId":6066,"corporation":false,"usgs":true,"family":"Detroy","given":"M.G.","affiliations":[],"preferred":false,"id":622649,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cherryholmes, K.","contributorId":67672,"corporation":false,"usgs":true,"family":"Cherryholmes","given":"K.","email":"","affiliations":[],"preferred":false,"id":622650,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kuzniar, R.L.","contributorId":44558,"corporation":false,"usgs":true,"family":"Kuzniar","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":622651,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70127584,"text":"70127584 - 1992 - Descriptive risk assessment of the effects of acidic deposition on Rocky Mountain amphibians","interactions":[],"lastModifiedDate":"2014-09-30T12:43:16","indexId":"70127584","displayToPublicDate":"1992-12-01T12:41:36","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2334,"text":"Journal of Herpetology","active":true,"publicationSubtype":{"id":10}},"title":"Descriptive risk assessment of the effects of acidic deposition on Rocky Mountain amphibians","docAbstract":"We evaluated the risk of habitat acidification to the six species of amphibians that occur in the mountains of Colorado and Wyoming. Our evaluation included extrinsic environmental factors (habitat sensitivity and amount of acidic atmospheric deposition) and species-specific intrinsic factors (sensitivity to acid conditions, habitat preferences, and timing of breeding). Only one of 57 surveyed localities had both acid neutralizing capacity <200 <i>μ</i>eq/L and sulfate deposition >10 kg/ha/yr, extrinsic conditions with a possible risk of acidification. Amphibian breeding habitats in the Rocky Mountains do not appear to be sufficiently acidic to kill amphibian embryos. Some species breed in high-elevation vernal pools during snowmelt, and an acidic pulse during snowmelt may pose a risk to embryos of these species. However, the acidic pulse, if present, probably occurs before open water appears and before breeding begins. Although inherent variability of amphibian population size may make detection of declines from anthropogenic effects difficult, acidic deposition is unlikely to have caused the observed declines of <i>Bufo boreas</i> and <i>Rana pipiens</i> in Colorado and Wyoming. Amphibians in the Rocky Mountains are not likely to be at risk with acidification inputs at present levels.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Herpetology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society for the Study of Amphibians and Reptiles","publisherLocation":"Athens, OH","doi":"10.2307/1565112","usgsCitation":"Corn, P., and Vertucci, F.A., 1992, Descriptive risk assessment of the effects of acidic deposition on Rocky Mountain amphibians: Journal of Herpetology, v. 26, no. 4, p. 361-369, https://doi.org/10.2307/1565112.","productDescription":"9 p.","startPage":"361","endPage":"369","numberOfPages":"9","costCenters":[],"links":[{"id":294648,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":294647,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2307/1565112"}],"volume":"26","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"542bc62ae4b0abfb4c809781","contributors":{"authors":[{"text":"Corn, Paul Stephen 0000-0002-4106-6335","orcid":"https://orcid.org/0000-0002-4106-6335","contributorId":107379,"corporation":false,"usgs":true,"family":"Corn","given":"Paul Stephen","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":502459,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vertucci, Frank A.","contributorId":57388,"corporation":false,"usgs":true,"family":"Vertucci","given":"Frank","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":502458,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1001320,"text":"1001320 - 1992 - Effects of irrigation on seed production and vegetative characteristics of four moist-soil plants on impounded wetlands in California","interactions":[],"lastModifiedDate":"2026-04-27T17:39:38.60244","indexId":"1001320","displayToPublicDate":"1992-12-01T00:00:00","publicationYear":"1992","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":"Effects of irrigation on seed production and vegetative characteristics of four moist-soil plants on impounded wetlands in California","docAbstract":"<p><span id=\"_mce_caret\" data-mce-bogus=\"1\" data-mce-type=\"format-caret\"><span>We examined the effects of irrigation on 4 moist-soil plants commonly managed for waterfowl in the Sacramento Valley, California. Irrigation resulted in taller and heavier swamp timothy (</span><i>Heleochloa schoenoides</i><span>), pricklegrass (</span><i>Crypsis niliaca</i><span>), and sprangletop (</span><i>Leptochloa fasicularis</i><span>). Barnyardgrass (</span><i>Echinochloa crusgalli</i><span>) grew taller in irrigated wetlands, but no significant difference in weight was detected. Only sprangletop yielded larger seed masses in response to irrigation. Without irrigation, swamp timothy and pricklegrass assumed a typical prostrate growth form, but with irrigation, they assumed a vertical growth form. Irrigation did not significantly affect plant density. Because of rising water costs, wetland managers should consider wildlife management objectives and plant responses before implementing irrigation practices.</span></span></p>","language":"English","publisher":"Springer Nature","doi":"10.1007/BF03160610","usgsCitation":"Mushet, D., Euliss, N., and Harris, S., 1992, Effects of irrigation on seed production and vegetative characteristics of four moist-soil plants on impounded wetlands in California: Wetlands, v. 12, no. 3, p. 204-207, https://doi.org/10.1007/BF03160610.","productDescription":"4 p.","startPage":"204","endPage":"207","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":133758,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Sacramento Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.37910254578382,\n              39.822500523112154\n            ],\n            [\n              -122.37910254578382,\n              38.107108797177375\n            ],\n            [\n              -120.84482767834879,\n              38.107108797177375\n            ],\n            [\n              -120.84482767834879,\n              39.822500523112154\n            ],\n            [\n              -122.37910254578382,\n              39.822500523112154\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"12","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611de0","contributors":{"authors":[{"text":"Mushet, D.M. 0000-0002-5910-2744","orcid":"https://orcid.org/0000-0002-5910-2744","contributorId":59377,"corporation":false,"usgs":true,"family":"Mushet","given":"D.M.","affiliations":[],"preferred":false,"id":310876,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Euliss, N.H. Jr.","contributorId":54917,"corporation":false,"usgs":true,"family":"Euliss","given":"N.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":310875,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harris, S.W.","contributorId":66201,"corporation":false,"usgs":true,"family":"Harris","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":310877,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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