{"pageNumber":"4252","pageRowStart":"106275","pageSize":"25","recordCount":184904,"records":[{"id":70174357,"text":"70174357 - 1992 - Dispersion in tidally averaged transport equation","interactions":[],"lastModifiedDate":"2016-07-26T16:38:09","indexId":"70174357","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Dispersion in tidally averaged transport equation","docAbstract":"<div id=\"breadcrumb\">A general governing inter-tidal transport equation for conservative solutes has been derived without invoking the weakly nonlinear approximation. The governing inter-tidal transport equation is a convection-dispersion equation in which the convective velocity is a mean Lagrangian residual current, and the inter-tidal dispersion coefficient is defined by a dispersion patch. When the weakly nonlinear condition is violated, the physical significance of the Stokes' drift, as used in tidal dynamics, becomes questionable. For nonlinear problems, analytical solutions for the mean Lagrangian residual current and for the inter-tidal dispersion coefficient do not exist, they must be determined numerically. A rectangular tidal inlet with a constriction is used in the first example. The solutions of the residual currents and the computed properties of the inter-tidal dispersion coefficient are used to illuminate the mechanisms of the inter-tidal transport processes. Then, the present formulation is tested in a geometrically complex tidal estuary &ndash; San Francisco Bay, California. The computed inter-tidal dispersion coefficients are in the range between 5&times;10<sup>4</sup>&nbsp;and 5&times;10<sup>6</sup>&nbsp;cm<sup>2</sup>/sec., which are consistent with the values reported in the literature</div>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Dynamics and exchanges in estuaries and the coastal zone","language":"English","publisher":"Wiley","doi":"10.1029/CE040p0409","usgsCitation":"Cheng, R.T., and Casulli, V., 1992, Dispersion in tidally averaged transport equation, chap. <i>of</i> Dynamics and exchanges in estuaries and the coastal zone, p. 409-428, https://doi.org/10.1029/CE040p0409.","productDescription":"20 p.","startPage":"409","endPage":"428","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"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":324975,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5780ceb4e4b0811616822302","contributors":{"authors":[{"text":"Cheng, R. T.","contributorId":23138,"corporation":false,"usgs":false,"family":"Cheng","given":"R.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":642012,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Casulli, V.","contributorId":65994,"corporation":false,"usgs":true,"family":"Casulli","given":"V.","affiliations":[],"preferred":false,"id":642013,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70195910,"text":"70195910 - 1992 -  Access to spatial environmental data for development of an oil spill response geographic","interactions":[],"lastModifiedDate":"2018-03-07T15:50:05","indexId":"70195910","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":" Access to spatial environmental data for development of an oil spill response geographic","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Needs and solutions for pollution monitoring, control, and abatement: Proceedings of the First Thematic Conference on Remote Sensing for Marine and Coastal Environments","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"First Thematic Conference on Remote Sensing for Marine and Coastal Environments","conferenceDate":"June 15-17, 1992","conferenceLocation":"New Orleans, LA","language":"English","publisher":"Environmental Research Institute of Michigan","publisherLocation":"Ann Arbor, MI","usgsCitation":"Hiland, M., Byrnes, M., McBride, R., Penland, S., Ramsey, K., Debusschere, K., and Williams, S., 1992,  Access to spatial environmental data for development of an oil spill response geographic, <i>in</i> Needs and solutions for pollution monitoring, control, and abatement: Proceedings of the First Thematic Conference on Remote Sensing for Marine and Coastal Environments, New Orleans, LA, June 15-17, 1992, p. 21-21.","productDescription":"1 p.","startPage":"21","endPage":"21","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":352306,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff2827e4b0da30c1bfd774","contributors":{"authors":[{"text":"Hiland, M.W.","contributorId":34528,"corporation":false,"usgs":true,"family":"Hiland","given":"M.W.","affiliations":[],"preferred":false,"id":730466,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Byrnes, M.R.","contributorId":190677,"corporation":false,"usgs":false,"family":"Byrnes","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":730467,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McBride, R.A.","contributorId":13257,"corporation":false,"usgs":true,"family":"McBride","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":730468,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Penland, S.","contributorId":58778,"corporation":false,"usgs":true,"family":"Penland","given":"S.","email":"","affiliations":[],"preferred":false,"id":730469,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ramsey, K.","contributorId":52805,"corporation":false,"usgs":false,"family":"Ramsey","given":"K.","email":"","affiliations":[],"preferred":false,"id":730470,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Debusschere, K.","contributorId":120024,"corporation":false,"usgs":false,"family":"Debusschere","given":"K.","affiliations":[],"preferred":false,"id":730471,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Williams, S.J.","contributorId":85203,"corporation":false,"usgs":true,"family":"Williams","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":730472,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70017148,"text":"70017148 - 1992 - Discordant 14C ages from buried tidal-marsh soils in the Cascadia subduction zone, southern Oregon coast","interactions":[],"lastModifiedDate":"2013-01-25T14:00:01","indexId":"70017148","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3218,"text":"Quaternary Research","active":true,"publicationSubtype":{"id":10}},"title":"Discordant 14C ages from buried tidal-marsh soils in the Cascadia subduction zone, southern Oregon coast","docAbstract":"Peaty, tidal-marsh soils interbedded with estuarine mud in late Holocene stratigraphic sequences near Coos Bay, Oregon, may have been submerged and buried during great (M > 8) subduction earthquakes, smaller localized earthquakes, or by nontectonic processes. Radiocarbon dating might help distinguish among these alternatives by showing that soils at different sites were submerged at different times along this part of the Cascadia subduction zone. But comparison of conventional 14C ages for different materials from the same buried soils shows that they contain materials that differ in age by many hundreds of years. Errors in calibrated soil ages represent about the same length of time as recurrence times for submergence events (150-500 yr)-this similarity precludes using conventional 14C ages to distinguish buried soils along the southern Oregon coast. Accelerator mass spectrometer 14C ages of carefully selected macrofossils from the tops of peaty soils should provide more precise estimates of the times of submergence events. ?? 1992.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Quaternary Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0033-5894(92)90031-D","issn":"00335894","usgsCitation":"Nelson, A., 1992, Discordant 14C ages from buried tidal-marsh soils in the Cascadia subduction zone, southern Oregon coast: Quaternary Research, v. 38, no. 1, p. 74-90, https://doi.org/10.1016/0033-5894(92)90031-D.","startPage":"74","endPage":"90","numberOfPages":"17","costCenters":[],"links":[{"id":266482,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0033-5894(92)90031-D"},{"id":224778,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"38","issue":"1","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"505a01ece4b0c8380cd4fdbd","contributors":{"authors":[{"text":"Nelson, A.R. 0000-0001-7117-7098","orcid":"https://orcid.org/0000-0001-7117-7098","contributorId":55078,"corporation":false,"usgs":true,"family":"Nelson","given":"A.R.","affiliations":[],"preferred":false,"id":375558,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70195911,"text":"70195911 - 1992 - An aeromagnetic survey over the northwestern Ross Ice Shelf and the McMurdo Sound area","interactions":[],"lastModifiedDate":"2019-12-21T08:52:14","indexId":"70195911","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3097,"text":"Polarforschung","active":true,"publicationSubtype":{"id":10}},"title":"An aeromagnetic survey over the northwestern Ross Ice Shelf and the McMurdo Sound area","docAbstract":"<p><span>As part of the expedition GANOVEX VI 1990/91, the Bundesanstalt für Geowissenschaften und Rohstoffe (BGR), the Alfred Wegener Institute for Polar and Marine Research (AWI), and the United States Geological Survey (USGS) carried out an airborne magnetic survey over the northwestern Ross Ice Shelf and McMurdo Sound between Ross Island, the Transantarctic Mountains, and Minna Bluff.</span></p><p><span>The area planned for the aeromagnetic survey connects directly with the GANOVEX IV survey area (BGR &amp; USGS 1987, BACHEM et al. 1989a) which terminated along an approximately cast-west line at about the latitude of Cape Bird. The GANOVEX IV survey covered the Victoria Land Basin - which is the westernmost of the three north/south striking basins in the Ross Sea - from its northern end in the Terra Nova Bay region to its known southern end at Ross Island. A possible southem extension of the Victoria Land Basin and its central graben structure (the Terror Rift as found from seismic surveys (COOPER et al. 1987) and what has been referred to as Victoria Graben in the aeromagnetic interpretation of the GANOVEX IV data (BOSUM et al. 1989) was one of the major targets for this survey.</span></p><p><span>The survey was laid out in the form of blocks. A 135 km wide transect from the Transantarctic Mountains to about 175° W formed the focal block of the survey (Fig. 1) in which all major scientific objectives could be covered. Other survey blocks were planned to the south of this. During the course of the survey it turned out that in the time available no further area could be covered. Indeed, the unfavourable weather conditions made it impossible to complete even the above described main section fully.</span></p><p><span>In detail, the lay-out of the survey area was closely following that of the GANOVEX IV survey to assure compatibility and direct continuation between the two data sets.</span></p><p><span>The line spacing was chosen again to 4.4 km with a tic-line separation of 22 km. The survey altitude of 2,000 ft (610 m) corresponds to that of the Ross Sea section of the GANOVEX IV survey to which this survey area is directly adjacent. The profile lines were aligned approximately E-W, the tie-lines N-S.</span></p><p><span>As part of the survey area is covered by the maps of the USGS Antarctica Reconnaissance Series 1:250,000 the Lambert conformal conic projection used for these maps was also used for the preparation of a flight line grid.</span></p>","language":"English","publisher":"Alfred Wegener Institut für Polar- und Meeresforschung und Deutsche Gesellschaft für Polarforschung","publisherLocation":"Bremerhaven, Germany","doi":"10.2312/polarforschung.60.2.152","usgsCitation":"Damaske, D., Meyer, U., McCafferty, A.E., Behrendt, J., and Hoppe, H., 1992, An aeromagnetic survey over the northwestern Ross Ice Shelf and the McMurdo Sound area: Polarforschung, v. 60, no. 2, p. 152-156, https://doi.org/10.2312/polarforschung.60.2.152.","productDescription":"5 p.","startPage":"152","endPage":"156","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":352307,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Ross Ice Shelf, McMurdo Sound","volume":"60","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff2826e4b0da30c1bfd772","contributors":{"authors":[{"text":"Damaske, Detlef","contributorId":77384,"corporation":false,"usgs":true,"family":"Damaske","given":"Detlef","email":"","affiliations":[],"preferred":false,"id":730476,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, Uwe","contributorId":1648,"corporation":false,"usgs":false,"family":"Meyer","given":"Uwe","email":"","affiliations":[],"preferred":false,"id":730477,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McCafferty, Anne E. 0000-0001-5574-9201 anne@usgs.gov","orcid":"https://orcid.org/0000-0001-5574-9201","contributorId":1120,"corporation":false,"usgs":true,"family":"McCafferty","given":"Anne","email":"anne@usgs.gov","middleInitial":"E.","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true},{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":730478,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Behrendt, John","contributorId":146726,"corporation":false,"usgs":false,"family":"Behrendt","given":"John","affiliations":[{"id":590,"text":"U.S. Army Corps of Engineers","active":false,"usgs":false}],"preferred":false,"id":730479,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hoppe, Herbert","contributorId":14503,"corporation":false,"usgs":false,"family":"Hoppe","given":"Herbert","email":"","affiliations":[],"preferred":false,"id":730480,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70185793,"text":"70185793 - 1992 - Nitrate is a preferred electron acceptor for growth of freshwater selenate-respiring bacteria","interactions":[],"lastModifiedDate":"2023-01-20T16:43:50.037905","indexId":"70185793","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":850,"text":"Applied and Environmental Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Nitrate is a preferred electron acceptor for growth of freshwater selenate-respiring bacteria","docAbstract":"<p><span>An anaerobic, freshwater enrichment grew with either nitrate or selenate as an electron acceptor. With both ions present, nitrate reduction preceded selenate reduction. An isolate from the enrichment grew on either ion, but the presence of nitrate precluded the reduction of selenate. Stock cultures of denitrifiers grew anaerobically on nitrate but not on selenate.</span></p>","language":"English","publisher":"American Society for Microbiology","doi":"10.1128/aem.58.1.426-428.1992","usgsCitation":"Steinberg, N.A., Blum, J.S., Hochstein, L., and Oremland, R.S., 1992, Nitrate is a preferred electron acceptor for growth of freshwater selenate-respiring bacteria: Applied and Environmental Microbiology, v. 58, no. 1, p. 426-428, https://doi.org/10.1128/aem.58.1.426-428.1992.","productDescription":"3 p.","startPage":"426","endPage":"428","costCenters":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":479648,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1128/aem.58.1.426-428.1992","text":"Publisher Index Page"},{"id":338544,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"58","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58dcc81ee4b02ff32c685722","contributors":{"authors":[{"text":"Steinberg, Nisan A.","contributorId":189726,"corporation":false,"usgs":false,"family":"Steinberg","given":"Nisan","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":686753,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blum, Jodi Switzer","contributorId":96946,"corporation":false,"usgs":true,"family":"Blum","given":"Jodi","email":"","middleInitial":"Switzer","affiliations":[],"preferred":false,"id":686754,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hochstein, Lawrence","contributorId":190004,"corporation":false,"usgs":false,"family":"Hochstein","given":"Lawrence","email":"","affiliations":[],"preferred":false,"id":686755,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Oremland, Ronald S. 0000-0001-7382-0147 roremlan@usgs.gov","orcid":"https://orcid.org/0000-0001-7382-0147","contributorId":931,"corporation":false,"usgs":true,"family":"Oremland","given":"Ronald","email":"roremlan@usgs.gov","middleInitial":"S.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":686756,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":30083,"text":"wri914130 - 1992 - Techniques for estimating 7-day, 10-year low-flow characteristics for ungaged sites on streams in Mississippi","interactions":[],"lastModifiedDate":"2023-04-04T21:49:38.53325","indexId":"wri914130","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","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":"91-4130","title":"Techniques for estimating 7-day, 10-year low-flow characteristics for ungaged sites on streams in Mississippi","docAbstract":"<p>Mississippi State water laws require that the 7-day, 10-year low-flow characteristic (7Q10) of streams be used as a criterion for issuing wastedischarge permits to dischargers to streams and for limiting withdrawals of water from streams. This report presents techniques for estimating the 7Q10 for ungaged sites on streams in Mississippi based on the availability of baseflow discharge measurements at the site, location of nearby gaged sites on the same stream, and drainage area of the ungaged site. These techniques may be used to estimate the 7Q10 at sites on natural, unregulated or partially regulated, and non-tidal streams. Low-flow characteristics for streams in the Mississippi River alluvial plain were not estimated because the annual lowflow data exhibit decreasing trends with time. Also presented are estimates of the 7Q10 for 493 gaged sites on Mississippi streams.</p><p>Techniques for estimating the 7Q10 have been developed for ungaged sites with base-flow discharge measurements, for ungaged sites on gaged streams, and for ungaged sites on ungaged streams. For an ungaged site with one or more base-flow discharge measurements, base-flow discharge data at the ungaged site are related to concurrent discharge data at a nearby gaged site. For ungaged sites on gaged streams, several methods of transferring the 7Q10 from a gaged site to an ungaged site were developed; the resulting 7Q10 values are based on drainage area prorations for the sites. For ungaged sites on ungaged streams, the 7Q10 is estimated from a map developed for. this study that shows the unit 7Q10 (7Q10 per square mile of drainage area) for ungaged basins in the State. The mapped values were estimated from the unit 7Q10 determined for nearby gaged basins, adjusted on the basis of the geology and topography of the ungaged basins.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri914130","collaboration":"Prepared in cooperation with the Pat Harrison Waterway District, Pearl River Basin Development District, Tombigbee River Valley Water Management District, Mississippi Department of Environmental Quality, Mississippi Office of Land and Water Resources, Mississippi Office of Pollution Control","usgsCitation":"Telis, P.A., 1992, Techniques for estimating 7-day, 10-year low-flow characteristics for ungaged sites on streams in Mississippi: U.S. Geological Survey Water-Resources Investigations Report 91-4130, Report: iv, 143 p.; Plate: 35.61 x 48.12 inches, https://doi.org/10.3133/wri914130.","productDescription":"Report: iv, 143 p.; Plate: 35.61 x 48.12 inches","costCenters":[{"id":269,"text":"FLWSC-Ft. Lauderdale","active":true,"usgs":true}],"links":[{"id":415198,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47531.htm","linkFileType":{"id":5,"text":"html"}},{"id":58894,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4130/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160689,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4130/report-thumb.jpg"},{"id":347202,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4130/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":70171430,"text":"70171430 - 1992 - Sensitivity of ground - water recharge estimates to climate variability and change, Columbia Plateau, Washington","interactions":[],"lastModifiedDate":"2016-05-31T12:40:07","indexId":"70171430","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2316,"text":"Journal of Geophysical Research D: Atmospheres","active":true,"publicationSubtype":{"id":10}},"title":"Sensitivity of ground - water recharge estimates to climate variability and change, Columbia Plateau, Washington","docAbstract":"<p><span>The sensitivity of groundwater recharge estimates was investigated for the semiarid Ellensburg basin, located on the Columbia Plateau, Washington, to historic and projected climatic regimes. Recharge was estimated for predevelopment and current (1980s) land use conditions using a daily energy-soil-water balance model. A synthetic daily weather generator was used to simulate lengthy sequences with parameters estimated from subsets of the historical record that were unusually wet and unusually dry. Comparison of recharge estimates corresponding to relatively wet and dry periods showed that recharge for predevelopment land use varies considerably within the range of climatic conditions observed in the 87-year historical observation period. Recharge variations for present land use conditions were less sensitive to the same range of historical climatic conditions because of irrigation. The estimated recharge based on the 87-year historical climatology was compared with adjustments to the historical precipitation and temperature records for the same record to reflect CO</span><span>2</span><span>-doubling climates as projected by general circulation models (GCMs). Two GCM scenarios were considered: an average of conditions for three different GCMs with CO</span><span>2</span><span>&nbsp;doubling, and a most severe &ldquo;maximum&rdquo; case. For the average GCM scenario, predevelopment recharge increased, and current recharge decreased. Also considered was the sensitivity of recharge to the variability of climate within the historical and adjusted historical records. Predevelopment and current recharge were less and more sensitive, respectively, to the climate variability for the average GCM scenario as compared to the variability within the historical record. For the maximum GCM scenario, recharge for both predevelopment and current land use decreased, and the sensitivity to the CO</span><span>2</span><span>-related climate change was larger than sensitivity to the variability in the historical and adjusted historical climate records.</span></p>","language":"English","publisher":"Wiley","doi":"10.1029/91JD01788","usgsCitation":"Vaccaro, J.J., 1992, Sensitivity of ground - water recharge estimates to climate variability and change, Columbia Plateau, Washington: Journal of Geophysical Research D: Atmospheres, v. 97, no. D3, p. 2821-2833, https://doi.org/10.1029/91JD01788.","productDescription":"13 p.","startPage":"2821","endPage":"2833","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":321917,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"97","issue":"D3","noUsgsAuthors":false,"publicationDate":"2012-09-21","publicationStatus":"PW","scienceBaseUri":"574eb5dce4b0ee97d51a8400","contributors":{"authors":[{"text":"Vaccaro, John J. jvaccaro@usgs.gov","contributorId":5848,"corporation":false,"usgs":true,"family":"Vaccaro","given":"John","email":"jvaccaro@usgs.gov","middleInitial":"J.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":630961,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043734,"text":"70043734 - 1992 - Publications of the U.S. Geological Survey, 1992","interactions":[],"lastModifiedDate":"2013-05-23T10:13:45","indexId":"70043734","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":378,"text":"Publications of the US Geological Survey","active":false,"publicationSubtype":{"id":6}},"title":"Publications of the U.S. Geological Survey, 1992","docAbstract":"This catalog is a list of (1) books and maps 1 that were published during 1992, and (2) articles by U.S. Geological Survey personnel in non-U.S. Geological Survey journals and books that came to our attention in 1992; it supplements the permanent catalogs \"Publications of the Geological Survey, 1879-1961\", \"Publications of the Geological Survey, 1962-1970\", and \"Publications of the U.S. Geological Survey, 1971 through 1981.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70043734","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1992, Publications of the U.S. Geological Survey, 1992: Publications of the US Geological Survey, v, 501 p., https://doi.org/10.3133/70043734.","productDescription":"v, 501 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":267718,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70043734/report-thumb.jpg"},{"id":272674,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70043734/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5124ad67e4b0b6328103b513","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":535420,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70016751,"text":"70016751 - 1992 - Bluff recession rates along the Lake Michigan shoreline in Illinois","interactions":[],"lastModifiedDate":"2023-11-03T00:33:20.152207","indexId":"70016751","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1115,"text":"Bulletin of the Association of Engineering Geologists","active":true,"publicationSubtype":{"id":10}},"title":"Bluff recession rates along the Lake Michigan shoreline in Illinois","docAbstract":"<p>For two time periods, 1872-1937 and 1937-1987, rates of retreat vary from 10 to 75 cm/yr between discrete segments of bluffs (defined by lithology) and between time periods for a given bluff segment. The average retreat rates for the entire area, however, do not vary significantly between the two time periods and are approximately 20-25 cm/yr. The temporally constant regional retreat rates and the regular shape of the local shoreline indicate that a long-term uniform rate of retreat prevails and that local variations in rates balance out through time to produce long-term parallel (in map view) bluff retreat in the area.&nbsp;</p>","language":"English","publisher":"Association of Engineering Geologists","doi":"10.2113/gseegeosci.xxix.2.103","usgsCitation":"Jibson, R., and Staude, J., 1992, Bluff recession rates along the Lake Michigan shoreline in Illinois: Bulletin of the Association of Engineering Geologists, v. 29, no. 2, p. 103-117, https://doi.org/10.2113/gseegeosci.xxix.2.103.","productDescription":"15 p.","startPage":"103","endPage":"117","numberOfPages":"15","costCenters":[],"links":[{"id":224655,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Illinois","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -88.38584704896901,\n              42.53173013124035\n            ],\n            [\n              -88.38584704896901,\n              41.47041149636533\n            ],\n            [\n              -87.10044665834381,\n              41.47041149636533\n            ],\n            [\n              -87.10044665834381,\n              42.53173013124035\n            ],\n            [\n              -88.38584704896901,\n              42.53173013124035\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"29","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f1efe4b0c8380cd4aee8","contributors":{"authors":[{"text":"Jibson, R.W.","contributorId":8467,"corporation":false,"usgs":true,"family":"Jibson","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":374398,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Staude, J.-M.","contributorId":19712,"corporation":false,"usgs":true,"family":"Staude","given":"J.-M.","email":"","affiliations":[],"preferred":false,"id":374399,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70016799,"text":"70016799 - 1992 - The southern Washington Cascades conductor: A previously unrecognized thick sedimentary sequence?","interactions":[],"lastModifiedDate":"2023-01-19T17:06:55.497097","indexId":"70016799","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"The southern Washington Cascades conductor: A previously unrecognized thick sedimentary sequence?","docAbstract":"Geophysical studies in the southern Washington Cascades have outlined a possible, previously unrecognized sequence of sedimentary rocks. These postulated sedimentary units are interpreted to correspond to at least the upper section of a low-resistivity (high-conductivity) assemblage of rocks at depths of 1-10 km and with thicknesses up to 15 km that called the southern Washington Cascades conductor. Structure on the upper surface of this conductive assemblage correlates in some places with anticlines that bring Tertiary marine rocks near the surface. The geometry of the conductive rocks consists of a east-dipping, low-angle wedge that thickens to the north and with an undulating upper surface corresponding to the anticlines. Geothermal fluids may be a contributing factor to low resistivities in the deeper parts of the conductive section. -from Authors","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/BDFF8A56-1718-11D7-8645000102C1865D","usgsCitation":"Stanley, W.D., Gwilliam, W.J., Latham, G., and Westhusing, K., 1992, The southern Washington Cascades conductor: A previously unrecognized thick sedimentary sequence?: American Association of Petroleum Geologists Bulletin, v. 76, no. 10, p. 1569-1585, https://doi.org/10.1306/BDFF8A56-1718-11D7-8645000102C1865D.","productDescription":"17 p.","startPage":"1569","endPage":"1585","numberOfPages":"17","costCenters":[],"links":[{"id":224558,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"southern Washington Cascades","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -123.0476092389447,\n              47.09217717972356\n            ],\n            [\n              -123.0476092389447,\n              46.10926604734689\n            ],\n            [\n              -120.81643027066724,\n              46.10926604734689\n            ],\n            [\n              -120.81643027066724,\n              47.09217717972356\n            ],\n            [\n              -123.0476092389447,\n              47.09217717972356\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"76","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb052e4b08c986b324da8","contributors":{"authors":[{"text":"Stanley, W. D.","contributorId":86756,"corporation":false,"usgs":true,"family":"Stanley","given":"W.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":374528,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gwilliam, W. J.","contributorId":36127,"corporation":false,"usgs":true,"family":"Gwilliam","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":374526,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Latham, Gary","contributorId":105739,"corporation":false,"usgs":true,"family":"Latham","given":"Gary","email":"","affiliations":[],"preferred":false,"id":374525,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Westhusing, Keith","contributorId":104920,"corporation":false,"usgs":true,"family":"Westhusing","given":"Keith","email":"","affiliations":[],"preferred":false,"id":374527,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1008507,"text":"1008507 - 1992 - Effects of impoundments on freshwater mussels (Mollusca: Bivalvia: Unionidae) in the main channel of the Black Warrior and Tombigbee rivers in western Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:04:27","indexId":"1008507","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1111,"text":"Bulletin of the Alabama Museum of Natural History","active":true,"publicationSubtype":{"id":10}},"title":"Effects of impoundments on freshwater mussels (Mollusca: Bivalvia: Unionidae) in the main channel of the Black Warrior and Tombigbee rivers in western Alabama","docAbstract":"Abstract not supplied at this time","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of the Alabama Museum of Natural History","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Williams, J., Fuller, S., and Grace, R., 1992, Effects of impoundments on freshwater mussels (Mollusca: Bivalvia: Unionidae) in the main channel of the Black Warrior and Tombigbee rivers in western Alabama: Bulletin of the Alabama Museum of Natural History, v. 13, p. 1-10.","productDescription":"p. 1-10","startPage":"1","endPage":"10","numberOfPages":"10","costCenters":[{"id":275,"text":"Florida Integrated Science Center","active":false,"usgs":true}],"links":[{"id":131920,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611e63","contributors":{"authors":[{"text":"Williams, J.D.","contributorId":74701,"corporation":false,"usgs":true,"family":"Williams","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":317967,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fuller, S.L.H.","contributorId":13933,"corporation":false,"usgs":true,"family":"Fuller","given":"S.L.H.","email":"","affiliations":[],"preferred":false,"id":317966,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grace, R.","contributorId":89845,"corporation":false,"usgs":true,"family":"Grace","given":"R.","email":"","affiliations":[],"preferred":false,"id":317968,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70016693,"text":"70016693 - 1992 - Pesticide residues in ground water of the San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2025-03-06T16:55:34.713704","indexId":"70016693","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Pesticide residues in ground water of the San Joaquin Valley, California","docAbstract":"<div class=\"u-margin-s-bottom\">A regional assessment of non-point-source contamination of pesticide residues in ground water was made of the San Joaquin Valley, an intensively farmed and irrigated structural trough in central California. About 10% of the total pesticide use in the USA is in the San Joaquin Valley. Pesticides detected include atrazine, bromacil, 2.4-DP, diazinon, dibromochloropropane, 1,2-dibromoethane, dicamba, 1,2-dichloropropane, diuron, prometon, prometryn, propazine and simazine. All are soil applied except diazinon.</div><div class=\"u-margin-s-bottom\">Pesticide leaching is dependent on use patterns, soil texture, total organic carbon in soil, pesticide half-life and depth to water table. Leaching is enhanced by flood-irrigation methods except where the pesticide is foliar applied such as diazinon. Soils in the western San Joaquin Valley are fine grained and are derived primarily from marine shales of the Coast Ranges. Although shallow ground water is present, the fewest number of pesticides were detected in this region. The fine-grained soil inhibits pesticide leaching because of either low vertical permeability or high surface area; both enhance adsorption on to solid phases. Soils of the valley floor tend to be fine grained and have low vertical permeability. Soils in the eastern part of the valley are coarse grained with low total organic carbon and are derived from Sierra Nevada granites. Most pesticide leaching is in these alluvial soils, particularly in areas where depth to ground water is less than 30m. The areas currently most susceptible to pesticide leaching are eastern Fresno and Tulare Counties.</div><div class=\"u-margin-s-bottom\">Tritium in water molecules is an indicator of aquifer recharge with water of recent origin. Pesticide residues transported as dissolved species were not detected in non-tritiated water. Although pesticides were not detected in all samples containing high tritium, these samples are indicative of the presence of recharge water that interacted with agricultural soils.</div>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(92)90115-C","issn":"00221694","usgsCitation":"Domagalski, J.L., and Dubrovsky, N., 1992, Pesticide residues in ground water of the San Joaquin Valley, California: Journal of Hydrology, v. 130, no. 1-4, p. 299-338, https://doi.org/10.1016/0022-1694(92)90115-C.","productDescription":"40 p.","startPage":"299","endPage":"338","numberOfPages":"40","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":224503,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"130","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a771fe4b0c8380cd78420","contributors":{"authors":[{"text":"Domagalski, Joseph L. 0000-0002-6032-757X joed@usgs.gov","orcid":"https://orcid.org/0000-0002-6032-757X","contributorId":1330,"corporation":false,"usgs":true,"family":"Domagalski","given":"Joseph","email":"joed@usgs.gov","middleInitial":"L.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":374235,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dubrovsky, N. M.","contributorId":48199,"corporation":false,"usgs":true,"family":"Dubrovsky","given":"N. M.","affiliations":[],"preferred":false,"id":374236,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70016738,"text":"70016738 - 1992 - A systematic approach to modelling the dynamic linkage of climate, physical catchment descriptors and hydrologic response components","interactions":[],"lastModifiedDate":"2019-03-07T07:00:51","indexId":"70016738","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2704,"text":"Mathematics and Computers in Simulation","active":true,"publicationSubtype":{"id":10}},"title":"A systematic approach to modelling the dynamic linkage of climate, physical catchment descriptors and hydrologic response components","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0378-4754(92)90122-W","issn":"03784754","usgsCitation":"Jakeman, A., Hornberger, G., Littlewood, I., Whitehead, P., Harvey, J., and Bencala, K., 1992, A systematic approach to modelling the dynamic linkage of climate, physical catchment descriptors and hydrologic response components: Mathematics and Computers in Simulation, v. 33, no. 5-6, p. 359-366, https://doi.org/10.1016/0378-4754(92)90122-W.","productDescription":"8 p.","startPage":"359","endPage":"366","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":224460,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"5-6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e5e9e4b0c8380cd4701c","contributors":{"authors":[{"text":"Jakeman, A.J.","contributorId":12639,"corporation":false,"usgs":true,"family":"Jakeman","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":374361,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hornberger, G.M.","contributorId":68463,"corporation":false,"usgs":true,"family":"Hornberger","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":374363,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Littlewood, I.G.","contributorId":82585,"corporation":false,"usgs":true,"family":"Littlewood","given":"I.G.","email":"","affiliations":[],"preferred":false,"id":374364,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Whitehead, P.G.","contributorId":85838,"corporation":false,"usgs":true,"family":"Whitehead","given":"P.G.","email":"","affiliations":[],"preferred":false,"id":374365,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Harvey, J. W. 0000-0002-2654-9873","orcid":"https://orcid.org/0000-0002-2654-9873","contributorId":39725,"corporation":false,"usgs":true,"family":"Harvey","given":"J. W.","affiliations":[],"preferred":false,"id":374362,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bencala, K.E.","contributorId":105312,"corporation":false,"usgs":true,"family":"Bencala","given":"K.E.","email":"","affiliations":[],"preferred":false,"id":374366,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70016750,"text":"70016750 - 1992 - Tale of three prospects","interactions":[],"lastModifiedDate":"2012-03-12T17:18:51","indexId":"70016750","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Tale of three prospects","docAbstract":"Most high-temperature, hydrothermal-convection systems probably are heated by bodies of magma (and/or hot plutons), whose presence is suggested by geologically young, if not active volcanism. Study of a young volcanic area provides information about the general thermal status of the underlying heat source, and detailed information about the time-space-volume-composition (TSVC) characteristics for a volcanic area can help define temperature at least semi-quantitatively when interpreted within the framework of published magma-cooling models. Thus, TSVC study is a fairly powerful and cost effective tool in the pre-drilling phase of an exploration program in young volcanic terrane. Examples are described for Coso, California; Agua de Pau, Azores; and Tecuamburro, Guatemala.","largerWorkTitle":"Transactions - Geothermal Resources Council","conferenceTitle":"1992 Annual Meeting of the Geothermal Resources Council","conferenceDate":"4 October 1992 through 7 October 1992","conferenceLocation":"San Diego, CA, USA","language":"English","publisher":"Publ by Geothermal Resources Council","publisherLocation":"Davis, CA, United States","issn":"01935933","usgsCitation":"Duffield, W.A., 1992, Tale of three prospects, <i>in</i> Transactions - Geothermal Resources Council, v. 16, San Diego, CA, USA, 4 October 1992 through 7 October 1992, p. 145-152.","startPage":"145","endPage":"152","numberOfPages":"8","costCenters":[],"links":[{"id":224654,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba3c3e4b08c986b31fe9d","contributors":{"editors":[{"text":"Anon","contributorId":128316,"corporation":true,"usgs":false,"organization":"Anon","id":536348,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Duffield, Wendell A.","contributorId":14363,"corporation":false,"usgs":true,"family":"Duffield","given":"Wendell","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":374397,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70016829,"text":"70016829 - 1992 - Analysis of geomagnetic secular variation during 1980-1985 and 1985- 1990, and geomagnetic models proposed for the 1991 revision of the International Geomagnetic Reference Field","interactions":[],"lastModifiedDate":"2024-04-24T11:15:40.730401","indexId":"70016829","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2310,"text":"Journal of Geomagnetism & Geoelectricity","active":true,"publicationSubtype":{"id":10}},"title":"Analysis of geomagnetic secular variation during 1980-1985 and 1985- 1990, and geomagnetic models proposed for the 1991 revision of the International Geomagnetic Reference Field","docAbstract":"<div id=\"article-overiew-abstract-wrap\"><p class=\"global-para-14\">The secular variation of the main geomagnetic field during the periods 1980-1985 and 1985-1990 was analyzed in terms of spherical harmonics up to the eighth degree and order. Data from worldwide magnetic observatories and the Navy's Project MAGNET aerial surveys were used. The resulting pair of secular-variation models was used to update the Definitive Geomagnetic Reference Field (DGRF) model for 1980, resulting in new main-field models for 1985.0 and 1990.0. These, along with the secular-variation model for 1985-1990, were proposed for the 1991 revision of the International Geomagnetic Reference Field (IGRF).</p></div><div id=\"datarepo-wrap\"><br></div><div id=\"article-overiew-references-wrap\"><br></div>","language":"English","publisher":"J-STAGE","doi":"10.5636/jgg.44.735","usgsCitation":"Peddie, N., 1992, Analysis of geomagnetic secular variation during 1980-1985 and 1985- 1990, and geomagnetic models proposed for the 1991 revision of the International Geomagnetic Reference Field: Journal of Geomagnetism & Geoelectricity, v. 44, no. 9, p. 735-743, https://doi.org/10.5636/jgg.44.735.","productDescription":"9 p.","startPage":"735","endPage":"743","numberOfPages":"9","costCenters":[],"links":[{"id":479616,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"http://doi.org/10.5636/jgg.44.735","text":"Publisher Index Page"},{"id":224949,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059eb15e4b0c8380cd48bec","contributors":{"authors":[{"text":"Peddie, N.W.","contributorId":75911,"corporation":false,"usgs":true,"family":"Peddie","given":"N.W.","affiliations":[],"preferred":false,"id":374607,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1008504,"text":"1008504 - 1992 - Study links Big Cypress fox squirrel to golf courses","interactions":[],"lastModifiedDate":"2012-02-02T00:04:27","indexId":"1008504","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3014,"text":"Park Science","active":true,"publicationSubtype":{"id":10}},"title":"Study links Big Cypress fox squirrel to golf courses","docAbstract":"Abstract not supplied at this time","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Park Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Jodice, P., and Snyder, J., 1992, Study links Big Cypress fox squirrel to golf courses: Park Science, v. 12, no. 4, p. 20-21.","productDescription":"p. 20-21","startPage":"20","endPage":"21","numberOfPages":"2","costCenters":[{"id":275,"text":"Florida Integrated Science Center","active":false,"usgs":true}],"links":[{"id":131917,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699d26","contributors":{"authors":[{"text":"Jodice, P.G.R.","contributorId":79846,"corporation":false,"usgs":true,"family":"Jodice","given":"P.G.R.","email":"","affiliations":[],"preferred":false,"id":317958,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snyder, J.R.","contributorId":96622,"corporation":false,"usgs":true,"family":"Snyder","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":317959,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70016682,"text":"70016682 - 1992 - An improved method for field extraction and laboratory analysis of large, intact soil cores","interactions":[],"lastModifiedDate":"2019-03-14T06:02:06","indexId":"70016682","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2262,"text":"Journal of Environmental Quality","active":true,"publicationSubtype":{"id":10}},"title":"An improved method for field extraction and laboratory analysis of large, intact soil cores","docAbstract":"<p>Various methods have been proposed for the extraction of large, undisturbed soil cores and for subsequent analysis of fluid movement within the cores. The major problems associated with these methods are expense, cumbersome field extraction, and inadequate simulation of unsaturated flow conditions. A field and laboratory procedure is presented that is economical, convenient, and simulates unsaturated and saturated flow without interface flow problems and can be used on a variety of soil types. In the field, a stainless steel core barrel is hydraulically pressed into the soil (30-cm diam. and 38 cm high), the barrel and core are extracted from the soil, and after the barrel is removed from the core, the core is then wrapped securely with flexible sheet metal and a stainless mesh screen is attached to the bottom of the core for support. In the laboratory the soil core is set atop a porous ceramic plate over which a soil-diatomaceous earth slurry has been poured to assure good contact between plate and core. A cardboard cylinder (mold) is fastened around the core and the empty space filled with paraffin wax. Soil cores were tested under saturated and unsaturated conditions using a hanging water column for potentials ≤0. Breakthrough curves indicated that no interface flow occurred along the edge of the core. This procedure proved to be reliable for field extraction of large, intact soil cores and for laboratory analysis of solute transport.</p>","language":"English","publisher":"ACSESS","doi":"10.2134/jeq1992.00472425002100020017x","issn":"00472425","usgsCitation":"Tindall, J., Hemmen, K., and Dowd, J., 1992, An improved method for field extraction and laboratory analysis of large, intact soil cores: Journal of Environmental Quality, v. 21, no. 2, p. 259-263, https://doi.org/10.2134/jeq1992.00472425002100020017x.","productDescription":"5 p.","startPage":"259","endPage":"263","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":225123,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ea70e4b0c8380cd48870","contributors":{"authors":[{"text":"Tindall, J.A.","contributorId":25711,"corporation":false,"usgs":true,"family":"Tindall","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":374213,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hemmen, K.","contributorId":57322,"corporation":false,"usgs":true,"family":"Hemmen","given":"K.","email":"","affiliations":[],"preferred":false,"id":374215,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dowd, J.F.","contributorId":47926,"corporation":false,"usgs":true,"family":"Dowd","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":374214,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1007892,"text":"1007892 - 1992 - Foraging on prey that are modified by parasites","interactions":[],"lastModifiedDate":"2023-02-17T15:18:55.368355","indexId":"1007892","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":740,"text":"American Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Foraging on prey that are modified by parasites","docAbstract":"<p><span>A model that weighs the energetic cost of parasitism for a predator against the energetic value of prey items that transmit the parasite to the predator suggests that there is often no selective pressure to avoid parasitized prey This offers an explanation for why parasites so frequently exploit predators and prey as definitive and intermediate hosts, respectively Furthermore, predators may actually benefit from their parasites if energetic costs of parasitism are moderate and prey capture is facilitated by parasites. Parasite species that benefit predators through modification of prey are not mutualistic, however.</span></p>","language":"English","publisher":"University of Chicago Press","doi":"10.1086/285444","usgsCitation":"Lafferty, K.D., 1992, Foraging on prey that are modified by parasites: American Naturalist, v. 140, no. 5, p. 854-867, https://doi.org/10.1086/285444.","productDescription":"14 p.","startPage":"854","endPage":"867","numberOfPages":"14","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130137,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"140","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae5ad","contributors":{"authors":[{"text":"Lafferty, Kevin D. 0000-0001-7583-4593 klafferty@usgs.gov","orcid":"https://orcid.org/0000-0001-7583-4593","contributorId":1415,"corporation":false,"usgs":true,"family":"Lafferty","given":"Kevin","email":"klafferty@usgs.gov","middleInitial":"D.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":316228,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70016758,"text":"70016758 - 1992 - A reconnaissance study of herbicides and their metabolites in surface water of the midwestern united states using immunoassay and gas chromatography/mass spectrometry","interactions":[],"lastModifiedDate":"2019-03-14T05:20:24","indexId":"70016758","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"A reconnaissance study of herbicides and their metabolites in surface water of the midwestern united states using immunoassay and gas chromatography/mass spectrometry","docAbstract":"<p>Preemergent herbicides and their metabolites, particularly atrazine, deethylatrazine, and metolachlor, persisted from 1989 to 1990 in the majority of rivers and streams in the midwestern United States. In spring, after the application of herbicides, the concentrations of atrazine, alachlor, and simazine were frequently 3-10 times greater than the U.S. Environmental Protection Agency maximum contaminant level (MCL). The concentration of herbicides exceeded the MCLs both singly and in combination. Two major degradation products of atrazine (deisopropylatrazine and deethylatrazine) also were found in many of the streams. The order of persistence of the herbicides and their metabolites in surface water was atrazine &gt; deethylatrazine &gt; metolachlor &gt; alachlor &gt; deisopropylatrazine &gt; cyanazine. Storm runoff collected at several sites exceeded the MCL multiple times during the summer months as a function of stream discharge, with increased concentrations during times of increased streamflow. It is proposed that metabolites of atrazine may be used as indicators of surface-water movement into adjacent alluvial aquifers.</p>","language":"English","publisher":"American Chemical Society","doi":"10.1021/es00036a016","issn":"0013936X","usgsCitation":"Thurman, E.M., Goolsby, D.A., Meyer, M.T., Mills, M.S., Pomes, M., and Kolpin, D.W., 1992, A reconnaissance study of herbicides and their metabolites in surface water of the midwestern united states using immunoassay and gas chromatography/mass spectrometry: Environmental Science & Technology, v. 26, no. 12, p. 2440-2447, https://doi.org/10.1021/es00036a016.","productDescription":"8 p.","startPage":"2440","endPage":"2447","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":224800,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-87.800477,42.49192],[-87.812461,42.232278],[-87.511043,41.696535],[-87.187651,41.629653],[-86.616978,41.896625],[-86.321803,42.310743],[-86.208309,42.762789],[-86.540916,43.633158],[-86.25395,44.64808],[-86.066745,44.905685],[-85.780439,44.977932],[-85.540497,45.210169],[-85.641652,44.810816],[-85.520205,44.960347],[-85.477423,44.813781],[-85.355478,45.282774],[-84.91585,45.393115],[-85.110884,45.526285],[-84.94565,45.708621],[-85.011433,45.757962],[-84.204218,45.627116],[-84.095905,45.497298],[-83.488826,45.355872],[-83.291346,45.062597],[-83.435822,45.000012],[-83.277213,44.7167],[-83.335248,44.357995],[-83.890145,43.934672],[-83.909479,43.672622],[-83.618602,43.628891],[-83.227093,43.981003],[-82.833103,44.036851],[-82.643166,43.852468],[-82.423086,42.988728],[-82.509935,42.637294],[-82.648776,42.550401],[-82.630922,42.64211],[-82.780817,42.652232],[-83.431103,41.757457],[-82.481214,41.381342],[-81.69325,41.514161],[-80.533774,41.973475],[-80.518991,40.638801],[-80.667957,40.582496],[-80.619297,40.26517],[-80.88036,39.620706],[-81.656138,39.277355],[-81.874857,38.881174],[-82.068864,38.984878],[-82.318111,38.457876],[-82.569368,38.406258],[-82.923694,38.750076],[-83.301951,38.598178],[-83.512571,38.701716],[-83.762445,38.652103],[-84.212904,38.805707],[-84.445242,39.114461],[-84.744149,39.147458],[-84.888873,39.066376],[-84.816506,38.80532],[-85.448862,38.713368],[-85.415272,38.555416],[-85.816164,38.282969],[-86.042354,37.958018],[-86.33281,38.182938],[-86.634271,37.843845],[-86.810913,37.99715],[-87.065388,37.810481],[-87.402632,37.942267],[-87.666522,37.827455],[-87.921744,37.907885],[-88.158374,37.639948],[-88.063311,37.515755],[-88.450127,37.411717],[-88.490068,37.067874],[-89.058036,37.188767],[-89.171881,37.068184],[-89.202607,36.601576],[-89.343753,36.630991],[-89.429311,36.481875],[-89.55264,36.577178],[-89.527029,36.341679],[-89.703511,36.243412],[-89.615128,36.113816],[-89.733095,36.000608],[-90.368718,35.995812],[-90.075934,36.281485],[-90.157136,36.484317],[-94.617919,36.499414],[-94.699735,36.998805],[-102.000447,36.993249],[-102.051614,41.002377],[-104.039238,41.001502],[-104.048807,48.933636],[-95.153711,48.998903],[-95.153314,49.384358],[-94.974286,49.367738],[-94.555835,48.716207],[-93.741843,48.517347],[-92.984963,48.623731],[-92.634931,48.542873],[-92.698824,48.494892],[-92.341207,48.23248],[-92.066269,48.359602],[-91.542512,48.053268],[-90.88548,48.245784],[-90.703702,48.096009],[-89.489226,48.014528],[-90.86827,47.5569],[-92.058888,46.809938],[-91.942988,46.679939],[-90.880358,46.957661],[-90.78804,46.844886],[-90.920813,46.637432],[-90.398478,46.575832],[-88.982483,46.99883],[-88.400224,47.379551],[-87.816958,47.471998],[-87.730804,47.449112],[-88.349952,47.076377],[-88.462349,46.786711],[-88.167373,46.9588],[-87.915943,46.909508],[-87.619747,46.79821],[-87.366767,46.507303],[-86.850111,46.434114],[-86.188024,46.654008],[-84.964652,46.772845],[-84.969464,46.47629],[-84.177428,46.52692],[-84.097766,46.256512],[-84.247687,46.17989],[-83.931175,46.017871],[-83.63498,46.103953],[-83.49484,45.999541],[-84.345451,45.946569],[-84.656567,46.052654],[-84.820557,45.868293],[-85.047028,46.020603],[-85.528403,46.087121],[-85.663966,45.967013],[-86.278007,45.942057],[-86.687208,45.634253],[-86.532989,45.882665],[-86.92106,45.697868],[-87.018902,45.838886],[-88.027103,44.578992],[-87.943801,44.529693],[-87.428144,44.890738],[-87.021088,45.296541],[-87.73063,43.893862],[-87.910172,43.236634],[-87.800477,42.49192]]],[[[-88.684434,48.115785],[-88.447236,48.182916],[-89.022736,47.858532],[-89.255202,47.876102],[-88.684434,48.115785]]],[[[-86.880572,45.331467],[-86.956192,45.351179],[-86.82177,45.427602],[-86.880572,45.331467]]]]},\"properties\":{\"name\":\"Iowa\",\"nation\":\"USA  \"}}]}","volume":"26","issue":"12","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059e53ae4b0c8380cd46bfe","contributors":{"authors":[{"text":"Thurman, E. Michael","contributorId":9636,"corporation":false,"usgs":true,"family":"Thurman","given":"E.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":759258,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goolsby, D. A.","contributorId":50508,"corporation":false,"usgs":true,"family":"Goolsby","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":374416,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meyer, M. T.","contributorId":92279,"corporation":false,"usgs":true,"family":"Meyer","given":"M.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":374420,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mills, M. S.","contributorId":96279,"corporation":false,"usgs":true,"family":"Mills","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":374421,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pomes, M.L.","contributorId":84393,"corporation":false,"usgs":true,"family":"Pomes","given":"M.L.","affiliations":[],"preferred":false,"id":374417,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kolpin, Dana W. 0000-0002-3529-6505 dwkolpin@usgs.gov","orcid":"https://orcid.org/0000-0002-3529-6505","contributorId":1239,"corporation":false,"usgs":true,"family":"Kolpin","given":"Dana","email":"dwkolpin@usgs.gov","middleInitial":"W.","affiliations":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"preferred":true,"id":759259,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70016826,"text":"70016826 - 1992 - A new model for tabular-type uranium deposits","interactions":[],"lastModifiedDate":"2024-01-03T17:50:11.837352","indexId":"70016826","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"A new model for tabular-type uranium deposits","docAbstract":"<p><span>Tabular-type uranium deposits occur as tabular, originally subhorizontal bodies entirely within reduced fluvial sandstones of Late Silurian age or younger. This paper proposes that belts of tabular-type uranium deposits formed in areas of mixed local and regional ground-water discharge shortly after deposition of the host sediments. The general characteristics of tabular-type uranium deposits, especially the most studied deposits, those in the Uravan mineral belt, Henry basin, and Grants uranium region, indicate that their essential feature was the formation at a density-stratified ground-water interface in areas of local and regional ground-water discharge. Reconstruction of the paleohydrogeology is the key to understanding the formation of these deposits. Gravity-driven ground water recharged in major highlands and discharged in lowlands at major concave changes in paleotopographic slope. Shallow local and deep regional ground-water systems were characterized by dilute and saline water, respectively. Typically, underlying marine rocks, especially evaporites, provided the solutes to the deep regional ground water. A density-stabilized interface existed at the ground-water divide between local and regional flow systems. Tabular-type uranium deposits formed where these divides or interfaces intersected pockets of reduction where organic matter accumulated. The precipitation of humate and uranium at an interface accounts for the tabular shape and the tendency of deposits to rise stratigraphically into the basin. Geologic ground-water controls that favor discharge, such as the pinch-out of major aquifers, are also favorable for uranium ore. The combination of topographic and geologic features that both cause discharge is most favorable for ore deposition.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.87.8.2041","issn":"03610128","usgsCitation":"Sanford, R., 1992, A new model for tabular-type uranium deposits: Economic Geology, v. 87, no. 8, p. 2041-2055, https://doi.org/10.2113/gsecongeo.87.8.2041.","productDescription":"15 p.","startPage":"2041","endPage":"2055","numberOfPages":"15","costCenters":[],"links":[{"id":224946,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"87","issue":"8","noUsgsAuthors":false,"publicationDate":"1992-12-01","publicationStatus":"PW","scienceBaseUri":"5059e4abe4b0c8380cd46818","contributors":{"authors":[{"text":"Sanford, R.F.","contributorId":38562,"corporation":false,"usgs":true,"family":"Sanford","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":374602,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70016685,"text":"70016685 - 1992 - Late Cretaceous inoceramid bivalves of the Kuskokwim Basin, southwestern Alaska, and their implications for basin evolution","interactions":[],"lastModifiedDate":"2024-06-18T11:22:15.953259","indexId":"70016685","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2412,"text":"Journal of Paleontology","active":true,"publicationSubtype":{"id":10}},"title":"Late Cretaceous inoceramid bivalves of the Kuskokwim Basin, southwestern Alaska, and their implications for basin evolution","docAbstract":"<div class=\"abstract-content\"><div class=\"abstract\" data-abstract-type=\"normal\"><p>Upper Cretaceous rocks of the Kuskokwim Group are exposed in a large region of southwestern Alaska and are mainly composed of deformed turbidite deposits that contain few fossils other than inoceramid bivalves. This paper documents the taxonomy of the inoceramids in the Kuskokwim Group, develops an inoceramid biostratigraphy based on known ranges in other regions, and analyzes biogeographic patterns, paleoecology, and depositional history of the Kuskokwim Group.</p><p>Most of the inoceramid bivalves present in the Kuskokwim Group are of Cenomanian and Turonian age, and an assemblage of species typical of late Turonian age rocks is particularly well developed. Only two localities appear to be as young as Santonian age. The following 16 species or subspecies are discussed and illustrated in detail:<span>&nbsp;</span><span class=\"italic\">Birostrina tamurai</span><span>&nbsp;</span>Matsumoto and Noda,<span>&nbsp;</span><span class=\"italic\">Inoceramus virgatus</span><span>&nbsp;</span>Schlüter,<span>&nbsp;</span><span class=\"italic\">I. pennatulus</span><span>&nbsp;</span>Pergament,<span>&nbsp;</span><span class=\"italic\">I. pictus minus</span><span>&nbsp;</span>Matsumoto,<span>&nbsp;</span><span class=\"italic\">I.</span><span>&nbsp;</span>cf.<span>&nbsp;</span><span class=\"italic\">I. yabei</span><span>&nbsp;</span>Nagao and Matsumoto,<span>&nbsp;</span><span class=\"italic\">I.</span>? sp. aff.<span>&nbsp;</span><span class=\"italic\">I. costatus</span><span>&nbsp;</span>Nagao and Matsumoto,<span>&nbsp;</span><span class=\"italic\">I. hobetsensis</span><span>&nbsp;</span>Nagao and Matsumoto,<span>&nbsp;</span><span class=\"italic\">I. longealatus</span><span>&nbsp;</span>Tröger,<span>&nbsp;</span><span class=\"italic\">I. frechi</span><span>&nbsp;</span>Flegel,<span>&nbsp;</span><span class=\"italic\">I. waltersdorfensis waltersdorfensis</span><span>&nbsp;</span>Andert,<span>&nbsp;</span><span class=\"italic\">I.</span><span>&nbsp;</span>cf.<span>&nbsp;</span><span class=\"italic\">I. waltersdorfensis hannovrensis</span><span>&nbsp;</span>Heinz,<span>&nbsp;</span><span class=\"italic\">I. kuskokwimensis</span><span>&nbsp;</span>n. sp.,<span>&nbsp;</span><span class=\"italic\">Mytiloides</span><span>&nbsp;</span>cf.<span>&nbsp;</span><span class=\"italic\">M. opalensis</span><span>&nbsp;</span>(Böse),<span>&nbsp;</span><span class=\"italic\">M. teraokai</span><span>&nbsp;</span>(Matsumoto and Noda),<span>&nbsp;</span><span class=\"italic\">M.</span><span>&nbsp;</span>cf.<span>&nbsp;</span><span class=\"italic\">M. incertus</span><span>&nbsp;</span>(Jimbo), and<span>&nbsp;</span><span class=\"italic\">Sphenoceramus naumanni</span><span>&nbsp;</span>(Yokoyama). In addition, a specimen with affinities to<span>&nbsp;</span><span class=\"italic\">Mytiloides striatoconcentricus carpathicus</span><span>&nbsp;</span>(Simionescu) and a specimen that may belong to the<span>&nbsp;</span><span class=\"italic\">I. (Cremnoceramus?) rotundatus–I.</span><span>&nbsp;</span>(<span class=\"italic\">C</span>.)<span>&nbsp;</span><span class=\"italic\">erectus</span><span>&nbsp;</span>lineage are illustrated.</p><p>Most of the taxa present in the Kuskokwim region are found in other regions of the North Pacific, particularly Japan and eastern Siberia, or are found throughout the Northern Hemisphere. Only one species,<span>&nbsp;</span><span class=\"italic\">I. kuskokwimensis</span><span>&nbsp;</span>n. sp., is new and may be endemic. North Pacific taxa are predominant in the Kuskokwim region, but intervals near the Cenomanian–Turonian Stage boundary and in the upper Turonian contain taxa characteristic of Europe and the Western Interior basin of North America; some of these taxa have not been recorded previously in the North Pacific region. Turonian heteromorph ammonite assemblages associated with inoceramids in the finer grained facies of the Kuskokwim region are similar to those found in coeval rocks of Japan and Germany.</p><p>The depositional area of the Kuskokwim Group can be broken into two northeast-trending subbasins, the Kuskokwim River subbasin to the northwest and the Mulchatna River subbasin to the southeast, connected by the Nushagak Hills corridor. Within the Kuskokwim River subbasin, deposition apparently started earlier in the north (middle Cenomanian) than in the south (late Cenomanian to early Turonian), and prograding deltaic sedimentation along the western margin also appears to have started earlier in the north. No marine fossils younger than latest Turonian to earliest Coniacian are known from the Kuskokwim River subbasin. The youngest fossils identified are Santonian in age and are from deep-water deposits in the Nushagak Hills corridor. Few fossils are known from the Mulchatna River subbasin and age control is limited.</p></div></div>","language":"English","publisher":"Cambridge University","doi":"10.1017/S0022336000061400","issn":"00223360","usgsCitation":"Elder, W., and Box, S.E., 1992, Late Cretaceous inoceramid bivalves of the Kuskokwim Basin, southwestern Alaska, and their implications for basin evolution: Journal of Paleontology, v. 66, no. 2 Suppl., 39 p., https://doi.org/10.1017/S0022336000061400.","productDescription":"39 p.","numberOfPages":"39","costCenters":[],"links":[{"id":225177,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"66","issue":"2 Suppl.","noUsgsAuthors":false,"publicationDate":"2017-08-11","publicationStatus":"PW","scienceBaseUri":"505a44d5e4b0c8380cd66e16","contributors":{"authors":[{"text":"Elder, W.P.","contributorId":65467,"corporation":false,"usgs":true,"family":"Elder","given":"W.P.","email":"","affiliations":[],"preferred":false,"id":374219,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Box, S. E.","contributorId":38567,"corporation":false,"usgs":true,"family":"Box","given":"S.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":374218,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70016684,"text":"70016684 - 1992 - Remagnetization of the Coast Range ophiolite at Stanley Mountain, California, during accretion near 10°N paleolatitude","interactions":[],"lastModifiedDate":"2020-09-02T18:46:56.531342","indexId":"70016684","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Remagnetization of the Coast Range ophiolite at Stanley Mountain, California, during accretion near 10°N paleolatitude","docAbstract":"<p>Paleomagnetic data are presented for a 50-m-thick sequence of Oxfordian to Tithonian sedimentary rocks conformably overlying Upper Jurassic pillow basalt within the Coast Range ophiolite at Stanley Mountain, California. These new data are similar in direction and polarity to previously published paleomagnetic data for the pillow basalt. The Jurassic sedimentary rocks were deposited during a mixed-polarity interval of the geomagnetic field, and uniformity of the remanent magnetization within the entire section of pillow basalt and sedimentary rocks indicates later remagnetization. Remagnetization of the Coast Range ophiolite is interpreted to have occurred during accretion to the continental margin, possibly by burial and low-temperature alteration related to this event. Similar paleolatitudes calculated for the ophiolite (11&deg; &plusmn;3&deg;) and for mid-Cretaceous sedimentary rocks of the Stanley Mountain terrane at Figueroa Mountain (6&deg; &plusmn;5&deg;) are consistent with remagnetization of the ophiolite at low paleo-latitudes. Uniform-polarity directions for other remnants of ophiolite in southern California and elsewhere along the Pacific coast imply that these rocks were also overprinted, and their magnetic inclinations suggest remagnetization at low paleolatitudes as well. The Coast Range ophiolite at Stanley Mountain is thus inferred to have been remagnetized along the North American margin near 10&deg;N paleolatitude between earliest and mid-Cretaceous time and subsequently transported northward by strike-slip faulting related to relative motions between the Farallon, Kula, Pacific, and North American plates.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1992)020<0503:ROTCRO>2.3.CO;2","issn":"00917613","usgsCitation":"Hagstrum, J.T., 1992, Remagnetization of the Coast Range ophiolite at Stanley Mountain, California, during accretion near 10°N paleolatitude: Geology, v. 20, no. 6, p. 503-506, https://doi.org/10.1130/0091-7613(1992)020<0503:ROTCRO>2.3.CO;2.","productDescription":"4 p.","startPage":"503","endPage":"506","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":225176,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aa6c1e4b0c8380cd8502d","contributors":{"authors":[{"text":"Hagstrum, Jonathan T. 0000-0002-0689-280X jhag@usgs.gov","orcid":"https://orcid.org/0000-0002-0689-280X","contributorId":3474,"corporation":false,"usgs":true,"family":"Hagstrum","given":"Jonathan","email":"jhag@usgs.gov","middleInitial":"T.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":374217,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70016672,"text":"70016672 - 1992 - Identification of persisten anionic surfactant-derived chemicals in sewage effluent and groundwater","interactions":[],"lastModifiedDate":"2012-03-12T17:18:48","indexId":"70016672","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Identification of persisten anionic surfactant-derived chemicals in sewage effluent and groundwater","docAbstract":"Preparative isolation and fractionation procedures coupled with spectrometric analyses were used to identify surfactant-derived contaminants in sewage effluent and sewage-contaminated groundwater from a site located on Cape Cod, Massachusetts. Anionic surfactants and their biodegradation intermediates were isolated from field samples by ion exchange and fractionated by solvent extraction and adsorption chromatography. Fractions were analyzed by 13C nuclear magnetic resonance spectrometry and gas chromatography-mass spectrometry. Carboxylated residues of alkylphenol polyethoxylate surfactants were detected in sewage effluent and contaminated groundwater. Linear alkylbenzenesulfonates (LAS) were identified in sewage effluent and groundwater. Groundwater LAS composition suggested preferential removal of select isomers and homologs due to processes of biodegradation and partitioning. Tetralin and indane sulfonates (DATS), alicyclic analogs of LAS, were also identified in field samples. Although DATS are a minor portion of LAS formulations, equivalent concentrations of LAS and DATS in groundwater suggested persistence of alicyclic contaminant structures over those of linear structure. Sulfophenyl-carboxylated (SPC) LAS biodegradation intermediates were determined in sewage effluent and groundwater. Homolog distributions suggested that SPC containing 3-10 alkyl-chain carbons persist during infiltration and groundwater transport. Surfactant-derived residues detected in well F300-50 groundwater have a minimum residence time in the range of 2.7-4.6 yr. LAS detected in groundwater at 500 m from infiltration has been stable over an estimated 50-500 half lives.","largerWorkTitle":"Journal of Contaminant Hydrology","language":"English","issn":"01697722","usgsCitation":"Field, J., Leenheer, J., Thorn, K.A., Barber, L., Rostad, C., Macalady, D., and Daniel, S., 1992, Identification of persisten anionic surfactant-derived chemicals in sewage effluent and groundwater, <i>in</i> Journal of Contaminant Hydrology, v. 9, no. 1-2, p. 55-78.","startPage":"55","endPage":"78","numberOfPages":"24","costCenters":[],"links":[{"id":224983,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3835e4b0c8380cd614ab","contributors":{"authors":[{"text":"Field, J.A.","contributorId":27616,"corporation":false,"usgs":true,"family":"Field","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":374188,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leenheer, J.A.","contributorId":75123,"corporation":false,"usgs":true,"family":"Leenheer","given":"J.A.","affiliations":[],"preferred":false,"id":374191,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thorn, K. A.","contributorId":33294,"corporation":false,"usgs":true,"family":"Thorn","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":374190,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Barber, L.B. II","contributorId":6097,"corporation":false,"usgs":true,"family":"Barber","given":"L.B.","suffix":"II","affiliations":[],"preferred":false,"id":374186,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rostad, C.","contributorId":8622,"corporation":false,"usgs":true,"family":"Rostad","given":"C.","affiliations":[],"preferred":false,"id":374187,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Macalady, D.L.","contributorId":76468,"corporation":false,"usgs":true,"family":"Macalady","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":374192,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Daniel, S.R.","contributorId":28379,"corporation":false,"usgs":true,"family":"Daniel","given":"S.R.","email":"","affiliations":[],"preferred":false,"id":374189,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70016828,"text":"70016828 - 1992 - Thermal springs in Lake Baikal","interactions":[],"lastModifiedDate":"2024-01-23T01:12:13.220777","indexId":"70016828","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Thermal springs in Lake Baikal","docAbstract":"<div id=\"15574758\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>Pore waters extracted from sediment cores were analyzed for their oxygen and hydrogen isotopic compositions and major ion chemistry to determine the source of water from a vent area for diffuse lake-bottom thermal springs or seeps in Frolikha Bay, northeastern Lake Baikal. The δ<sup>18</sup>O values of pore waters range from -15.2‰ to -16.7‰, and δD values range from -119‰ to -126‰ (both isotopes determined relative to standard mean ocean water [SMOW]). Bottom water in Lake Baikal has a δ<sup>18</sup>O value of -5.6‰ and a δD value of -120‰ Pore waters in the vent area are significantly enriched in Mg, B, Ca, and especially Na and have the lowest δD and δ<sup>18</sup>O values; these pore waters are isotopically and chemically distinct from pore waters in other, more typical parts of the lake. The pore-water isotopic data fall on a local meteoric water line, and covariations in water isotopes and chemistry are not consistent with evaporation or hydrothermal water-rock interaction. The thermal springs represent discharging meteoric waters that have been gently heated during subsurface circulation and are largely unaltered isotopically. Chemical variations are most likely due to dissolution of subsurface evaporites.</p></div>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1992)020<0495:TSILB>2.3.CO;2","issn":"00917613","usgsCitation":"Shanks, W.C., and Callender, E., 1992, Thermal springs in Lake Baikal: Geology, v. 20, no. 6, p. 495-497, https://doi.org/10.1130/0091-7613(1992)020<0495:TSILB>2.3.CO;2.","productDescription":"3 p.","startPage":"495","endPage":"497","numberOfPages":"3","costCenters":[],"links":[{"id":224948,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb257e4b08c986b325741","contributors":{"authors":[{"text":"Shanks, Wayne C. III","contributorId":100527,"corporation":false,"usgs":true,"family":"Shanks","given":"Wayne","suffix":"III","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":374606,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Callender, E.","contributorId":72528,"corporation":false,"usgs":true,"family":"Callender","given":"E.","email":"","affiliations":[],"preferred":false,"id":374605,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70187596,"text":"70187596 - 1992 - Mesozoic structure, metamorphism, and magmatism in the Pilot Range and the Toano Ranges","interactions":[],"lastModifiedDate":"2017-05-09T18:14:09","indexId":"70187596","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Mesozoic structure, metamorphism, and magmatism in the Pilot Range and the Toano Ranges","docAbstract":"<p>No abstract available&nbsp;</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Field guide to geologic excursions in Utah and adjacent areas of Nevada, Idaho, and Wyoming","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Utah Geological Survey","usgsCitation":"Miller, D., and Hoisch, T., 1992, Mesozoic structure, metamorphism, and magmatism in the Pilot Range and the Toano Ranges, chap. <i>of</i> Field guide to geologic excursions in Utah and adjacent areas of Nevada, Idaho, and Wyoming, p. 79-92.","productDescription":"14 p. ","startPage":"79","endPage":"92","costCenters":[],"links":[{"id":341028,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5912d53ee4b0e541a03d4553","contributors":{"authors":[{"text":"Miller, D. M. 0000-0003-3711-0441","orcid":"https://orcid.org/0000-0003-3711-0441","contributorId":104422,"corporation":false,"usgs":true,"family":"Miller","given":"D. M.","affiliations":[],"preferred":false,"id":694687,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoisch, T.D.","contributorId":105863,"corporation":false,"usgs":true,"family":"Hoisch","given":"T.D.","affiliations":[],"preferred":false,"id":694688,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}