{"pageNumber":"2614","pageRowStart":"65325","pageSize":"25","recordCount":184605,"records":[{"id":70027648,"text":"70027648 - 2005 - Manganese concentration in lobster (Homarus americanus) gills as an index of exposure to reducing conditions in western Long Island Sound","interactions":[],"lastModifiedDate":"2022-05-24T16:49:22.912409","indexId":"70027648","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2455,"text":"Journal of Shellfish Research","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Manganese concentration in lobster (<i>Homarus americanus</i>) gills as an index of exposure to reducing conditions in western Long Island Sound","title":"Manganese concentration in lobster (Homarus americanus) gills as an index of exposure to reducing conditions in western Long Island Sound","docAbstract":"<p><span>We examined the accumulation of manganese (Mn) in gill tissues of chemically naïve lobsters held&nbsp;</span><i>in situ</i><span>&nbsp;at six sites in Long Island Sound (LIS) for up to six weeks to evaluate the possible contribution of eutrophication-driven habitat quality factors to the 1999 mass mortality of American lobsters (</span><i><span class=\"genus-species\">Homarus americanus</span></i><span>). These western LIS lobster habitats experience seasonal hypoxia, which results in redox-mobilized Mn being transferred to and deposited on the tissues of the lobsters. Manganese accumulated in gill tissue of lobsters throughout the study, but rates were highest at western and southern LIS sites, ranging from 3.4–0.8 μ g/g/d (~16 μg/g initial). The Baden-Eriksson observation that Mn accumulation in Norway lobsters (</span><i><span class=\"genus-species\">Nephrops norvegicus</span></i><span>) is associated with ecosystem hypoxia is confirmed and extended to&nbsp;</span><i><span class=\"genus-species\">H. americanus</span></i><span>. It seems likely that, after accounting for molting frequency, certain critical values may be applied to other lobster habitats of the NE US shelf. If a high proportion of lobsters in autumn have gill Mn concentrations exceeding 30 μg/g, then the habitats are likely experiencing some reduced oxygen levels. Manganese concentrations above 100 μg/g suggest exposure to conditions with the potential for lobster mortality should the temperatures of bottom waters become elevated, and gill concentrations above some higher level (perhaps 300 μg/g) indicate the most severe habitat conditions with a strong potential for hypoxia stress.</span></p>","language":"English","publisher":"National Shellfisheries Association","doi":"10.2983/0730-8000(2005)24[815:MCILHA]2.0.CO;2","usgsCitation":"Draxler, A.F., Sherrell, R.M., Wieczorek, D., Lavigne, M.G., and Paulson, A.J., 2005, Manganese concentration in lobster (Homarus americanus) gills as an index of exposure to reducing conditions in western Long Island Sound: Journal of Shellfish Research, v. 24, no. 3, p. 815-819, https://doi.org/10.2983/0730-8000(2005)24[815:MCILHA]2.0.CO;2.","productDescription":"5 p.","startPage":"815","endPage":"819","numberOfPages":"5","costCenters":[],"links":[{"id":238064,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Connecticut, New York","otherGeospatial":"western Long Island Sound","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.795166015625,\n              40.805493843894155\n            ],\n            [\n              -72.784423828125,\n              40.97160353279909\n            ],\n            [\n              -72.7569580078125,\n              41.27367811566259\n            ],\n            [\n              -72.99316406249999,\n              41.236511201246216\n            ],\n            [\n              -73.4326171875,\n              41.104190944576466\n            ],\n            [\n              -73.707275390625,\n              40.97160353279909\n            ],\n            [\n              -73.81164550781249,\n              40.85537053192494\n            ],\n            [\n              -73.795166015625,\n              40.805493843894155\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"24","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4caae4b0c8380cd69df8","contributors":{"authors":[{"text":"Draxler, Andrew F. J.","contributorId":29202,"corporation":false,"usgs":false,"family":"Draxler","given":"Andrew","email":"","middleInitial":"F. J.","affiliations":[],"preferred":false,"id":414559,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sherrell, Robert M.","contributorId":84101,"corporation":false,"usgs":false,"family":"Sherrell","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":414562,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wieczorek, Dan","contributorId":42022,"corporation":false,"usgs":false,"family":"Wieczorek","given":"Dan","email":"","affiliations":[],"preferred":false,"id":414560,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lavigne, Michele G.","contributorId":52783,"corporation":false,"usgs":false,"family":"Lavigne","given":"Michele","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":414561,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Paulson, Anthony J. 0000-0002-2358-8834 apaulson@usgs.gov","orcid":"https://orcid.org/0000-0002-2358-8834","contributorId":5236,"corporation":false,"usgs":true,"family":"Paulson","given":"Anthony","email":"apaulson@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":414563,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":1015318,"text":"1015318 - 2005 - Aggregate measures of ecosystem services: Can we take the pulse of nature?","interactions":[],"lastModifiedDate":"2018-02-21T15:58:32","indexId":"1015318","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1701,"text":"Frontiers in Ecology and the Environment","active":true,"publicationSubtype":{"id":10}},"title":"Aggregate measures of ecosystem services: Can we take the pulse of nature?","docAbstract":"<p><span>National scale aggregate indicators of ecosystem services are useful for stimulating and supporting a broad public discussion about trends in the provision of these services. There are important considerations involved in producing an aggregate indicator, including whether the scientific and technological capacity exists, how to address varying perceptions of the societal importance of different services, and how to communicate information about these services to both decision makers and the general public. Although the challenges are formidable, they are not insurmountable. Quantification of ecosystem services and dissemination of information to decision makers and the public is critical for the responsible and sustainable management of natural resources.</span></p>","language":"English","publisher":"Ecological Society of America","doi":"10.1890/1540-9295(2005)003[0056:AMOESC]2.0.CO;2","usgsCitation":"Meyerson, L., Baron, J., Melillo, J.M., Naiman, R., O’Malley, R., Orians, G., Palmer, M., Pfaff, A.S., Running, S.W., and Sala, O., 2005, Aggregate measures of ecosystem services: Can we take the pulse of nature?: Frontiers in Ecology and the Environment, v. 3, no. 1, p. 56-59, https://doi.org/10.1890/1540-9295(2005)003[0056:AMOESC]2.0.CO;2.","productDescription":"4 p.","startPage":"56","endPage":"59","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":477868,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1890/1540-9295(2005)003[0056:amoesc]2.0.co;2","text":"Publisher Index Page"},{"id":133126,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db689177","contributors":{"authors":[{"text":"Meyerson, L.A.","contributorId":47745,"corporation":false,"usgs":true,"family":"Meyerson","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":322870,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baron, Jill 0000-0002-5902-6251 jill_baron@usgs.gov","orcid":"https://orcid.org/0000-0002-5902-6251","contributorId":194124,"corporation":false,"usgs":true,"family":"Baron","given":"Jill","email":"jill_baron@usgs.gov","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":322868,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Melillo, J. M.","contributorId":73139,"corporation":false,"usgs":false,"family":"Melillo","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":322873,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Naiman, R.J.","contributorId":14354,"corporation":false,"usgs":true,"family":"Naiman","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":322867,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"O’Malley, R.I.","contributorId":34472,"corporation":false,"usgs":true,"family":"O’Malley","given":"R.I.","email":"","affiliations":[],"preferred":false,"id":322869,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Orians, G.","contributorId":67468,"corporation":false,"usgs":true,"family":"Orians","given":"G.","affiliations":[],"preferred":false,"id":322872,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Palmer, Margaret A.","contributorId":102429,"corporation":false,"usgs":false,"family":"Palmer","given":"Margaret A.","affiliations":[{"id":13383,"text":"University of Maryland Center for Environmental Science, Chesapeake Biological Laboratory, 6 Solomons, Maryland 20688","active":true,"usgs":false}],"preferred":false,"id":322876,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Pfaff, Alexander S.P.","contributorId":77492,"corporation":false,"usgs":true,"family":"Pfaff","given":"Alexander","email":"","middleInitial":"S.P.","affiliations":[],"preferred":false,"id":322874,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Running, S. W.","contributorId":51257,"corporation":false,"usgs":false,"family":"Running","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":322871,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Sala, O.E.","contributorId":96638,"corporation":false,"usgs":true,"family":"Sala","given":"O.E.","email":"","affiliations":[],"preferred":false,"id":322875,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70027570,"text":"70027570 - 2005 - Maximum known floodflows in Mississippi","interactions":[],"lastModifiedDate":"2012-03-12T17:20:48","indexId":"70027570","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Maximum known floodflows in Mississippi","docAbstract":"Maximum floodflows (stream discharges) that are known to have occurred on Mississippi streams were compiled. Most data were collected and archived by the U.S. Geological Survey in cooperation with Federal, State, and local agencies; however, some data were collected and provided by the U.S. Army Corps of Engineers. Maximum known discharges are plotted with drainage area and compared to an envelope curve derived from maximum known discharges at sites throughout the conterminous United States. This paper presents the maximum flood known to have occurred at a given gaged site, where stage and discharge measurements were obtained to determine the peak discharge, or at an ungaged site, where a flood was thought to be significant enough that an indirect measurement was computed to estimate the peak discharge.","largerWorkTitle":"Proceedings of the 2005 Watershed Management Conference - Managing Watersheds for Human and Natural Impacts: Engineering, Ecological, and Economic Challenges","conferenceTitle":"2005 Watershed Management Conference - Managing Watersheds for Human and Natural Impacts: Engineering, Ecological, and Economic Challenges","conferenceDate":"19 July 2005 through 22 July 2005","conferenceLocation":"Williamsburg, VA","language":"English","isbn":"0784407630","usgsCitation":"Van Wilson, K., 2005, Maximum known floodflows in Mississippi, <i>in</i> Proceedings of the 2005 Watershed Management Conference - Managing Watersheds for Human and Natural Impacts: Engineering, Ecological, and Economic Challenges, Williamsburg, VA, 19 July 2005 through 22 July 2005.","startPage":"1279","costCenters":[],"links":[{"id":237948,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a529ce4b0c8380cd6c54c","contributors":{"editors":[{"text":"Moglen G.E.","contributorId":128404,"corporation":true,"usgs":false,"organization":"Moglen G.E.","id":536620,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Van Wilson, K. Jr.","contributorId":62403,"corporation":false,"usgs":true,"family":"Van Wilson","given":"K.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":414191,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70027415,"text":"70027415 - 2005 - Drill hole logging with infrared spectroscopy","interactions":[],"lastModifiedDate":"2012-03-12T17:21:20","indexId":"70027415","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Drill hole logging with infrared spectroscopy","docAbstract":"Infrared spectroscopy has been used to identify rocks and minerals for over 40 years. The technique is sensitive to primary silicates as well as alteration products. Minerals can be uniquely identified based on multiple absorption features at wavelengths from the visible to the thermal infrared. We are currently establishing methods and protocols in order to use the technique for rapid assessment of downhole lithology on samples obtained during drilling operations. Initial work performed includes spectral analysis of chip cuttings and core sections from drill sites around Desert Peak, NV. In this paper, we report on a survey of 10,000 feet of drill cuttings, at 100 foot intervals, from the San Andreas Fault Observatory at Depth (SAFOD). Data from Blue Mountain geothermal wells will also be acquired. We will describe the utility of the technique for rapid assessment of lithologic and mineralogic discrimination.","largerWorkTitle":"Transactions - Geothermal Resources Council","conferenceTitle":"Geothermal Resources Council 2005 Annual Meeting","conferenceDate":"25 September 2005 through 28 September 2005","conferenceLocation":"Reno, NV","language":"English","issn":"01935933","usgsCitation":"Calvin, W.M., and Solum, J., 2005, Drill hole logging with infrared spectroscopy, <i>in</i> Transactions - Geothermal Resources Council, v. 29, Reno, NV, 25 September 2005 through 28 September 2005, p. 565-568.","startPage":"565","endPage":"568","numberOfPages":"4","costCenters":[],"links":[{"id":238443,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a03dde4b0c8380cd506ac","contributors":{"authors":[{"text":"Calvin, W. M.","contributorId":17379,"corporation":false,"usgs":false,"family":"Calvin","given":"W.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":413548,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Solum, J.G.","contributorId":79280,"corporation":false,"usgs":true,"family":"Solum","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":413549,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70027663,"text":"70027663 - 2005 - Linking demographic effects of habitat fragmentation across landscapes to continental source-sink dynamics","interactions":[],"lastModifiedDate":"2022-03-29T14:25:49.445946","indexId":"70027663","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1450,"text":"Ecological Applications","active":true,"publicationSubtype":{"id":10}},"title":"Linking demographic effects of habitat fragmentation across landscapes to continental source-sink dynamics","docAbstract":"<p><span>Forest fragmentation may cause increased brood parasitism and nest predation of breeding birds. In North America, nest parasitism and predation are expected to increase closer to forest edges because the brood-parasitic Brown-headed Cowbird (Molothrus ater) and generalist nest predators often enter the forest from adjoining developed (largely agricultural) habitats. Yet the abundance of brood parasites and nest predators at the patch scale may be strongly constrained by the total area of developed habitat at landscape scales. The scale and extent of landscape effects are unclear, however, because past studies were mostly conducted within local landscapes rather than across independent landscapes. We report replicated studies from 30 independent landscapes across 17 states of the United States that show that nest parasitism is strongly affected by fragmentation at a 20 km radius scale, equivalent to the maximum foraging range of cowbirds. Nest predation is influenced by both edge and landscape effects, and increases with fragmentation at a 10 km radius scale. Predation is additive to parasitism mortality, and the two together yield decreased population growth potential with increasing forest fragmentation at a 10 km radius scale for 20 of 22 bird species. Mapping of population growth potential across continental landscapes displays broad impacts of fragmentation on population viability and allows geographic prioritization for conservation.</span></p>","language":"English","publisher":"Ecological Society of America","doi":"10.1890/04-1243","usgsCitation":"Lloyd, P., Martin, T.E., Redmond, R.L., Langner, U., and Hart, M.M., 2005, Linking demographic effects of habitat fragmentation across landscapes to continental source-sink dynamics: Ecological Applications, v. 15, no. 5, p. 1504-1514, https://doi.org/10.1890/04-1243.","productDescription":"11 p.","startPage":"1504","endPage":"1514","numberOfPages":"11","costCenters":[],"links":[{"id":238309,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a47d1e4b0c8380cd679d4","contributors":{"authors":[{"text":"Lloyd, P.","contributorId":62405,"corporation":false,"usgs":true,"family":"Lloyd","given":"P.","email":"","affiliations":[],"preferred":false,"id":414633,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, T. E.","contributorId":10911,"corporation":false,"usgs":true,"family":"Martin","given":"T.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":414629,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Redmond, R. L.","contributorId":59922,"corporation":false,"usgs":true,"family":"Redmond","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":414632,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Langner, U.","contributorId":31959,"corporation":false,"usgs":true,"family":"Langner","given":"U.","email":"","affiliations":[],"preferred":false,"id":414630,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hart, M. M.","contributorId":58089,"corporation":false,"usgs":true,"family":"Hart","given":"M.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":414631,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70027413,"text":"70027413 - 2005 - Generation and verification of theoretical rating curves in the Whitewater River basin, Kansas","interactions":[],"lastModifiedDate":"2012-03-12T17:21:15","indexId":"70027413","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2318,"text":"Journal of Geophysical Research F: Earth Surface","active":true,"publicationSubtype":{"id":10}},"title":"Generation and verification of theoretical rating curves in the Whitewater River basin, Kansas","docAbstract":"[1] A new method for generating stage-discharge relations (rating curves) for geomorphically stable channels is presented and applied to two streams in the Whitewater River basin, Kansas. The approach converts measurements of stage into discharge using a fluid mechanically based model. The model does not use empirical roughness coefficients, such as Manning coefficients, but rather determines channel roughness from field measurements of the (1) channel geometry, (2) the physical roughness of the bed, banks, and floodplain, and (3) the vegetation density on the banks and floodplain. These measurements are used to calculate explicitly the drag on the small-scale topographic features on the boundary, the drag on the stems and branches of woody vegetation, and the friction on the bed, banks, and floodplain. The theoretical rating curves produced by the model for two study reaches, which are near U.S. Geological Survey (USGS) streamflow-gauging stations, are in good agreement with direct measurements of discharge made by the USGS. Our method has the potential of providing accurate estimates of stream flows less expensively than conventional gauging methods. In addition, the method can be used to obtain more accurate discharge estimates than conventional indirect methods for determining discharge, which are based on estimates of Manning's coefficient.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research F: Earth Surface","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2004JF000250","issn":"01480227","usgsCitation":"Kean, J., and Smith, J., 2005, Generation and verification of theoretical rating curves in the Whitewater River basin, Kansas: Journal of Geophysical Research F: Earth Surface, v. 110, no. 4, https://doi.org/10.1029/2004JF000250.","costCenters":[],"links":[{"id":477939,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2004jf000250","text":"Publisher Index Page"},{"id":211186,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2004JF000250"},{"id":238409,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"110","issue":"4","noUsgsAuthors":false,"publicationDate":"2005-11-18","publicationStatus":"PW","scienceBaseUri":"505a1550e4b0c8380cd54d57","contributors":{"authors":[{"text":"Kean, J. W. 0000-0003-3089-0369","orcid":"https://orcid.org/0000-0003-3089-0369","contributorId":71679,"corporation":false,"usgs":true,"family":"Kean","given":"J. W.","affiliations":[],"preferred":false,"id":413544,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, J.D.","contributorId":35796,"corporation":false,"usgs":true,"family":"Smith","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":413543,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70027734,"text":"70027734 - 2005 - Task committee on experimental uncertainty and measurement errors in hydraulic engineering: An update","interactions":[],"lastModifiedDate":"2012-03-12T17:20:49","indexId":"70027734","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Task committee on experimental uncertainty and measurement errors in hydraulic engineering: An update","docAbstract":"As part of their long range goals for disseminating information on measurement techniques, instrumentation, and experimentation in the field of hydraulics, the Technical Committee on Hydraulic Measurements and Experimentation formed the Task Committee on Experimental Uncertainty and Measurement Errors in Hydraulic Engineering in January 2003. The overall mission of this Task Committee is to provide information and guidance on the current practices used for describing and quantifying measurement errors and experimental uncertainty in hydraulic engineering and experimental hydraulics. The final goal of the Task Committee on Experimental Uncertainty and Measurement Errors in Hydraulic Engineering is to produce a report on the subject that will cover: (1) sources of error in hydraulic measurements, (2) types of experimental uncertainty, (3) procedures for quantifying error and uncertainty, and (4) special practical applications that range from uncertainty analysis for planning an experiment to estimating uncertainty in flow monitoring at gaging sites and hydraulic structures. Currently, the Task Committee has adopted the first order variance estimation method outlined by Coleman and Steele as the basic methodology to follow when assessing the uncertainty in hydraulic measurements. In addition, the Task Committee has begun to develop its report on uncertainty in hydraulic engineering. This paper is intended as an update on the Task Committee's overall progress. Copyright ASCE 2005.","largerWorkTitle":"World Water Congress 2005: Impacts of Global Climate Change - Proceedings of the 2005 World Water and Environmental Resources Congress","conferenceTitle":"2005 World Water and Environmental Resources Congress","conferenceDate":"15 May 2005 through 19 May 2005","conferenceLocation":"Anchorage, AK","language":"English","doi":"10.1061/40792(173)447","isbn":"0784407924; 9780784407929","usgsCitation":"Wahlin, B., Wahl, T., Gonzalez-Castro, J.A., Fulford, J., and Robeson, M., 2005, Task committee on experimental uncertainty and measurement errors in hydraulic engineering: An update, <i>in</i> World Water Congress 2005: Impacts of Global Climate Change - Proceedings of the 2005 World Water and Environmental Resources Congress, Anchorage, AK, 15 May 2005 through 19 May 2005, https://doi.org/10.1061/40792(173)447.","startPage":"447","costCenters":[],"links":[{"id":211072,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1061/40792(173)447"},{"id":238242,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationDate":"2012-04-26","publicationStatus":"PW","scienceBaseUri":"505ba3e6e4b08c986b31ff87","contributors":{"authors":[{"text":"Wahlin, B.","contributorId":86164,"corporation":false,"usgs":true,"family":"Wahlin","given":"B.","email":"","affiliations":[],"preferred":false,"id":414988,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wahl, T.","contributorId":54788,"corporation":false,"usgs":true,"family":"Wahl","given":"T.","affiliations":[],"preferred":false,"id":414987,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gonzalez-Castro, J. A.","contributorId":96885,"corporation":false,"usgs":true,"family":"Gonzalez-Castro","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":414989,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fulford, J.","contributorId":31970,"corporation":false,"usgs":true,"family":"Fulford","given":"J.","email":"","affiliations":[],"preferred":false,"id":414986,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Robeson, M.","contributorId":101869,"corporation":false,"usgs":true,"family":"Robeson","given":"M.","email":"","affiliations":[],"preferred":false,"id":414990,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70027568,"text":"70027568 - 2005 - NO news is no new news","interactions":[],"lastModifiedDate":"2012-03-12T17:21:16","indexId":"70027568","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3370,"text":"Seed Science Research","active":true,"publicationSubtype":{"id":10}},"title":"NO news is no new news","docAbstract":"In the paper 'NO News', Preston et al. (2004) make a number of erroneous assumptions regarding nitrogen oxide chemistry. These authors also present some very significant misinterpretations of previous research into the effects of various nitrogen oxides on germination of post-fire followers. Methodological differences between the study by Preston et al. (2004) and previous work are also problematic, such as using NO-donors in solution versus the use of direct application of various nitrogen oxides in the gaseous phase. A closer review of these studies, with the proper understanding of nitrogen oxide chemistry, and interpretations of the available literature, would lead to the conclusion that, contrary to the authors' assertions, the Preston et al. (2004) study supports, rather than refutes, earlier findings by Keeley and Fotheringham (1997, 1998a, b, 2000). ?? CAB International 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Seed Science Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1079/SSR2005227","issn":"09602585","usgsCitation":"Fotheringham, C.J., and Keeley, J., 2005, NO news is no new news: Seed Science Research, v. 15, no. 4, p. 367-371, https://doi.org/10.1079/SSR2005227.","startPage":"367","endPage":"371","numberOfPages":"5","costCenters":[],"links":[{"id":477763,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1079/ssr2005227","text":"Publisher Index Page"},{"id":211243,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1079/SSR2005227"},{"id":238495,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"4","noUsgsAuthors":false,"publicationDate":"2007-02-22","publicationStatus":"PW","scienceBaseUri":"505a614ae4b0c8380cd718cf","contributors":{"authors":[{"text":"Fotheringham, C. J.","contributorId":63334,"corporation":false,"usgs":true,"family":"Fotheringham","given":"C.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":414184,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keeley, Jon E. 0000-0002-4564-6521","orcid":"https://orcid.org/0000-0002-4564-6521","contributorId":69082,"corporation":false,"usgs":true,"family":"Keeley","given":"Jon E.","affiliations":[],"preferred":false,"id":414185,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70027566,"text":"70027566 - 2005 - Multivariate analysis of scale-dependent associations between bats and landscape structure","interactions":[],"lastModifiedDate":"2022-03-29T14:28:05.843555","indexId":"70027566","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1450,"text":"Ecological Applications","active":true,"publicationSubtype":{"id":10}},"title":"Multivariate analysis of scale-dependent associations between bats and landscape structure","docAbstract":"<p><span>The assessment of biotic responses to habitat disturbance and fragmentation generally has been limited to analyses at a single spatial scale. Furthermore, methods to compare responses between scales have lacked the ability to discriminate among patterns related to the identity, strength, or direction of associations of biotic variables with landscape attributes. We present an examination of the relationship of population- and community-level characteristics of phyllostomid bats with habitat features that were measured at multiple spatial scales in Atlantic rain forest of eastern Paraguay. We used a matrix of partial correlations between each biotic response variable (i.e., species abundance, species richness, and evenness) and a suite of landscape characteristics to represent the multifaceted associations of bats with spatial structure. Correlation matrices can correspond based on either the strength (i.e., magnitude) or direction (i.e., sign) of association. Therefore, a simulation model independently evaluated correspondence in the magnitude and sign of correlations among scales, and results were combined via a meta-analysis to provide an overall test of significance. Our approach detected both species-specific differences in response to landscape structure and scale dependence in those responses. This matrix–simulation approach has broad applicability to ecological situations in which multiple intercorrelated factors contribute to patterns in space or time.</span></p>","language":"English","publisher":"Ecological Society of America","doi":"10.1890/04-0532","usgsCitation":"Gorresen, P.M., Willig, M.R., and Strauss, R.E., 2005, Multivariate analysis of scale-dependent associations between bats and landscape structure: Ecological Applications, v. 15, no. 6, p. 2126-2136, https://doi.org/10.1890/04-0532.","productDescription":"11 p.","startPage":"2126","endPage":"2136","numberOfPages":"11","costCenters":[],"links":[{"id":238493,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a60b5e4b0c8380cd71637","contributors":{"authors":[{"text":"Gorresen, P. M. mgorresen@usgs.gov","contributorId":18552,"corporation":false,"usgs":true,"family":"Gorresen","given":"P.","email":"mgorresen@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":false,"id":414179,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Willig, M. R.","contributorId":68517,"corporation":false,"usgs":true,"family":"Willig","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":414181,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Strauss, R. E.","contributorId":50722,"corporation":false,"usgs":true,"family":"Strauss","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":414180,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70027732,"text":"70027732 - 2005 - Use of XML and Java for collaborative petroleum reservoir modeling on the Internet","interactions":[],"lastModifiedDate":"2012-03-12T17:20:49","indexId":"70027732","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1315,"text":"Computers & Geosciences","printIssn":"0098-3004","active":true,"publicationSubtype":{"id":10}},"title":"Use of XML and Java for collaborative petroleum reservoir modeling on the Internet","docAbstract":"The GEMINI (Geo-Engineering Modeling through INternet Informatics) is a public-domain, web-based freeware that is made up of an integrated suite of 14 Java-based software tools to accomplish on-line, real-time geologic and engineering reservoir modeling. GEMINI facilitates distant collaborations for small company and academic clients, negotiating analyses of both single and multiple wells. The system operates on a single server and an enterprise database. External data sets must be uploaded into this database. Feedback from GEMINI users provided the impetus to develop Stand Alone Web Start Applications of GEMINI modules that reside in and operate from the user's PC. In this version, the GEMINI modules run as applets, which may reside in local user PCs, on the server, or Java Web Start. In this enhanced version, XML-based data handling procedures are used to access data from remote and local databases and save results for later access and analyses. The XML data handling process also integrates different stand-alone GEMINI modules enabling the user(s) to access multiple databases. It provides flexibility to the user to customize analytical approach, database location, and level of collaboration. An example integrated field-study using GEMINI modules and Stand Alone Web Start Applications is provided to demonstrate the versatile applicability of this freeware for cost-effective reservoir modeling. ?? 2005 Elsevier Ltd. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Computers and Geosciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.cageo.2004.12.007","issn":"00983004","usgsCitation":"Victorine, J., Watney, W., and Bhattacharya, S., 2005, Use of XML and Java for collaborative petroleum reservoir modeling on the Internet: Computers & Geosciences, v. 31, no. 9, p. 1151-1164, https://doi.org/10.1016/j.cageo.2004.12.007.","startPage":"1151","endPage":"1164","numberOfPages":"14","costCenters":[],"links":[{"id":211050,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.cageo.2004.12.007"},{"id":238208,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbe8de4b08c986b329655","contributors":{"authors":[{"text":"Victorine, J.","contributorId":59239,"corporation":false,"usgs":true,"family":"Victorine","given":"J.","email":"","affiliations":[],"preferred":false,"id":414983,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Watney, W.L.","contributorId":43087,"corporation":false,"usgs":true,"family":"Watney","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":414982,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bhattacharya, S.","contributorId":97226,"corporation":false,"usgs":true,"family":"Bhattacharya","given":"S.","email":"","affiliations":[],"preferred":false,"id":414984,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2002773,"text":"2002773 - 2005 - Coastal iron fluxes to surface waters of the NE Pacific: A driver of the marine ecosystem and carbon cycle","interactions":[],"lastModifiedDate":"2018-05-02T21:26:50","indexId":"2002773","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesTitle":{"id":419,"text":"White Paper","active":false,"publicationSubtype":{"id":9}},"title":"Coastal iron fluxes to surface waters of the NE Pacific: A driver of the marine ecosystem and carbon cycle","language":"English","usgsCitation":"Crusius, J., and Nielsen, J., 2005, Coastal iron fluxes to surface waters of the NE Pacific: A driver of the marine ecosystem and carbon cycle: White Paper.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":198393,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aeac2","contributors":{"authors":[{"text":"Crusius, John 0000-0003-2554-0831 jcrusius@usgs.gov","orcid":"https://orcid.org/0000-0003-2554-0831","contributorId":2155,"corporation":false,"usgs":true,"family":"Crusius","given":"John","email":"jcrusius@usgs.gov","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":326635,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nielsen, J.L.","contributorId":105665,"corporation":false,"usgs":true,"family":"Nielsen","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":326636,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70027693,"text":"70027693 - 2005 - Tracing water and suspended matter in Raritan and Lower New York Bays using dissolved and particulate elemental concentrations","interactions":[],"lastModifiedDate":"2016-05-30T13:15:21","indexId":"70027693","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2662,"text":"Marine Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Tracing water and suspended matter in Raritan and Lower New York Bays using dissolved and particulate elemental concentrations","docAbstract":"<p id=\"\">Geochemical tracers were used to examine the mixing of water and particles in Lower New York and Raritan Bays in August 1999 during low-flow conditions. Four brackish water masses (20&nbsp;&le;&nbsp;<i>S</i>&nbsp;&le;&nbsp;28) originating in the Raritan and Shrewsbury Rivers, Arthur Kill, and Upper New York Bay were characterized by their dissolved metals concentrations. The mixing lines of dissolved Cu, Ni, and Pb in Lower New York Bay were similar to those in Upper New York Bay, the source of most of the freshwater to the system. Dissolved Cd and Mn seemed to have been removed by particles in several regions of the study. Dissolved Cu, Ni and Pb in the Raritan River fell below the mixing lines of the Lower New York Bay. In contrast, the concentrations of dissolved Co and Mn in the Raritan River were distinctly higher than those in the Lower New York Bay, while dissolved Cu and Ni were elevated in the Arthur Kill. A plot of dissolved Co versus dissolved Ni clearly differentiated among three water masses: (1) Upper and Lower New York Bays and Sandy Hood Bay, (2) the Raritan River, and (3) Arthur Kill&ndash;Raritan Bay&ndash;Shrewsbury River.</p>\n<p id=\"\">The concentrations of 22 elements also were measured in the suspended matter of Raritan and Lower New York Bays and brackish water sources. The elemental composition of the suspended matter in surface and bottom waters was correlated with Fe concentrations, which ranged between 50 and 900 &mu;mol g<sup>&minus;&nbsp;1</sup>. Statistical differences among the geographical regions were detected in the relationships of Ti, Ni, Co, As, and U with Fe, with particulate As being an especially strong geochemical indicator of Raritan River particles. The geochemical signatures of Lower New York Bay particles were similar to those of Upper New York Bay. The geochemical signatures of Raritan River particles were distinctly different than those of the Upper New York Bay, but the influence of Raritan River particles appeared to be limited to only inner Raritan Bay. This study illustrates the utility of trace elements for characterization of physical processes in complex estuaries.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.marchem.2005.01.007","issn":"03044203","usgsCitation":"Paulson, A., 2005, Tracing water and suspended matter in Raritan and Lower New York Bays using dissolved and particulate elemental concentrations: Marine Chemistry, v. 97, no. 1-2, p. 60-77, https://doi.org/10.1016/j.marchem.2005.01.007.","productDescription":"18 p.","startPage":"60","endPage":"77","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":238137,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211003,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.marchem.2005.01.007"}],"volume":"97","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb69be4b08c986b326d8d","contributors":{"authors":[{"text":"Paulson, A.J. apaulson@usgs.gov","contributorId":89617,"corporation":false,"usgs":true,"family":"Paulson","given":"A.J.","email":"apaulson@usgs.gov","affiliations":[],"preferred":false,"id":414756,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70027730,"text":"70027730 - 2005 - Postseismic deformation following the June 2000 earthquake sequence in the south Iceland seismic zone","interactions":[],"lastModifiedDate":"2012-03-12T17:20:49","indexId":"70027730","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Postseismic deformation following the June 2000 earthquake sequence in the south Iceland seismic zone","docAbstract":"We observe postseismic deformation on two spatiotemporal scales following Mw = 6.5 earthquakes in the south Iceland seismic zone on 17 and 21 June 2000. We see a rapidly decaying deformation transient lasting no more than 2 months and extending about 5 km away from the two main shock ruptures. This local, month-scale transient is captured by several radar interferograms and is also observed at a few campaign GPS sites located near the faults. A slower transient with a characteristic timescale of about a year is detected only by GPS measurements. The month-scale deformation pattern has been explained by poroelastic rebound due to postearthquake pore pressure changes. In contrast, the year-scale deformation can be explained by either afterslip at 8-14 km depth or viscoelastic relaxation of the lower crust and upper mantle in response to the coseismic stress changes. The optimal viscoelastic models have lower crustal viscosities of 0.5-1 ?? 1019 Pa s and upper mantle viscosity of ???3 ?? 1018 Pa s. Because of the limitations of our GPS campaign data, we consider both afterslip and viscoelastic relaxation as plausible mechanisms explaining the deformation field. Both types of postseismic deformation models suggest that the areas of large coseismic stress increase east of the 17 June and west of the 21 June ruptures continue to be loaded by the postseismic deformation. Copyright 2005 by the American Geophysical Union.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research B: Solid Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2005JB003701","issn":"01480227","usgsCitation":"Arnadottir, T., Jonsson, S., Pollitz, F., Jiang, W., and Feigl, K., 2005, Postseismic deformation following the June 2000 earthquake sequence in the south Iceland seismic zone: Journal of Geophysical Research B: Solid Earth, v. 110, no. 12, p. 1-13, https://doi.org/10.1029/2005JB003701.","startPage":"1","endPage":"13","numberOfPages":"13","costCenters":[],"links":[{"id":477933,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2005jb003701","text":"Publisher Index Page"},{"id":238174,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211029,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2005JB003701"}],"volume":"110","issue":"12","noUsgsAuthors":false,"publicationDate":"2005-12-30","publicationStatus":"PW","scienceBaseUri":"505a7e96e4b0c8380cd7a61e","contributors":{"authors":[{"text":"Arnadottir, T.","contributorId":80830,"corporation":false,"usgs":true,"family":"Arnadottir","given":"T.","affiliations":[],"preferred":false,"id":414976,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jonsson, Sigurjon","contributorId":72123,"corporation":false,"usgs":true,"family":"Jonsson","given":"Sigurjon","email":"","affiliations":[],"preferred":false,"id":414975,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pollitz, F. F.","contributorId":108280,"corporation":false,"usgs":true,"family":"Pollitz","given":"F. F.","affiliations":[],"preferred":false,"id":414977,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jiang, W.","contributorId":60010,"corporation":false,"usgs":true,"family":"Jiang","given":"W.","email":"","affiliations":[],"preferred":false,"id":414974,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Feigl, K.L.","contributorId":59238,"corporation":false,"usgs":true,"family":"Feigl","given":"K.L.","affiliations":[],"preferred":false,"id":414973,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70027412,"text":"70027412 - 2005 - New evidence for persistent or transient seed banks in three Sonoran Desert cacti","interactions":[],"lastModifiedDate":"2012-03-12T17:21:15","indexId":"70027412","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3451,"text":"Southwestern Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"New evidence for persistent or transient seed banks in three Sonoran Desert cacti","docAbstract":"Seedlings of Ferocactus wislizeni and Mammillaria grahamii, 2 common cactus species in the northern Sonoran Desert, emerged under protective cages that had been left in place for 6 years after an initial sowing of numerous Carnegiea gigantea and F. wislizeni seeds. Because no seeds were sown in the interim, Mammillaria and Ferocactus seedlings must have emerged from persistent seed banks. Mammillaria seeds evidently survived in or on the soil as long as 6 years, forming a long-term persistent seed bank, and Ferocactus seeds apparently survived up to 3 years, forming a short-term persistent seed bank. No Carnegiea seedlings emerged, confirming that this species has a transient seed bank This is the first evidence for a between-year seed bank in M. grahamii and the first confirmation of a between-year seed bank in F. wislizeni.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Southwestern Naturalist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1894/0038-4909(2005)050[0482:NEFPOT]2.0.CO;2","issn":"00384909","usgsCitation":"Bowers, J.E., 2005, New evidence for persistent or transient seed banks in three Sonoran Desert cacti: Southwestern Naturalist, v. 50, no. 4, p. 482-487, https://doi.org/10.1894/0038-4909(2005)050[0482:NEFPOT]2.0.CO;2.","startPage":"482","endPage":"487","numberOfPages":"6","costCenters":[],"links":[{"id":211160,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1894/0038-4909(2005)050[0482:NEFPOT]2.0.CO;2"},{"id":238370,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"50","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6579e4b0c8380cd72bdf","contributors":{"authors":[{"text":"Bowers, Janice E.","contributorId":18119,"corporation":false,"usgs":true,"family":"Bowers","given":"Janice","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":413542,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70027664,"text":"70027664 - 2005 - Assessing background ground water chemistry beneath a new unsewered subdivision","interactions":[],"lastModifiedDate":"2012-03-12T17:21:17","indexId":"70027664","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1861,"text":"Ground Water","active":true,"publicationSubtype":{"id":10}},"title":"Assessing background ground water chemistry beneath a new unsewered subdivision","docAbstract":"Previous site-specific studies designed to assess the impacts of unsewered subdivisions on ground water quality have relied on upgradient monitoring wells or very limited background data to characterize conditions prior to development. In this study, an extensive monitoring program was designed to document ground water conditions prior to construction of a rural subdivision in south-central Wisconsin. Previous agricultural land use has impacted ground water quality; concentrations of chloride, nitrate-nitrogen, and atrazine ranged from below the level of detection to 296 mg/L, 36 mg/L, and 0.8 ??g/L, respectively, and were highly variable from well to well and through time. Seasonal variations in recharge, surface topography, aquifer heterogeneities, surficial loading patterns, and well casing depth explain observed variations in ground water chemistry. This variability would not have been detected if background conditions were determined from only a few monitoring wells or inferred from wells located upgradient of the subdivision site. This project demonstrates the importance of characterizing both ground water quality and chemical variability prior to land-use change to detect any changes once homes are constructed. Copyright ?? 2005 National Ground Water Association.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ground Water","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1745-6584.2005.00044.x","issn":"0017467X","usgsCitation":"Wilcox, J., Bradbury, K.R., Thomas, C.L., and Bahr, J., 2005, Assessing background ground water chemistry beneath a new unsewered subdivision: Ground Water, v. 43, no. 6, p. 787-795, https://doi.org/10.1111/j.1745-6584.2005.00044.x.","startPage":"787","endPage":"795","numberOfPages":"9","costCenters":[],"links":[{"id":238346,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211141,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1745-6584.2005.00044.x"}],"volume":"43","issue":"6","noUsgsAuthors":false,"publicationDate":"2005-08-24","publicationStatus":"PW","scienceBaseUri":"5059edcce4b0c8380cd499f2","contributors":{"authors":[{"text":"Wilcox, J.D.","contributorId":107920,"corporation":false,"usgs":true,"family":"Wilcox","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":414637,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bradbury, K. R.","contributorId":86070,"corporation":false,"usgs":true,"family":"Bradbury","given":"K.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":414636,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, C. L.","contributorId":43802,"corporation":false,"usgs":true,"family":"Thomas","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":414634,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bahr, J.M.","contributorId":62346,"corporation":false,"usgs":true,"family":"Bahr","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":414635,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70027729,"text":"70027729 - 2005 - Earthquake fracture energy inferred from kinematic rupture models on extended faults","interactions":[],"lastModifiedDate":"2012-03-12T17:20:49","indexId":"70027729","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Earthquake fracture energy inferred from kinematic rupture models on extended faults","docAbstract":"We estimate fracture energy on extended faults for several recent earthquakes by retrieving dynamic traction evolution at each point on the fault plane from slip history imaged by inverting ground motion waveforms. We define the breakdown work (Wb) as the excess of work over some minimum traction level achieved during slip. Wb is equivalent to \"seismological\" fracture energy (G) in previous investigations. Our numerical approach uses slip velocity as a boundary condition on the fault. We employ a three-dimensional finite difference algorithm to compute the dynamic traction evolution in the time domain during the earthquake rupture. We estimate Wb by calculating the scalar product between dynamic traction and slip velocity vectors. This approach does not require specifying a constitutive law and assuming dynamic traction to be collinear with slip velocity. If these vectors are not collinear, the inferred breakdown work depends on the initial traction level. We show that breakdown work depends on the square of slip. The spatial distribution of breakdown work in a single earthquake is strongly correlated with the slip distribution. Breakdown work density and its integral over the fault, breakdown energy, scale with seismic moment according to a power law (with exponent 0.59 and 1.18, respectively). Our estimates of breakdown work range between 4 ?? 105 and 2 ?? 107 J/m2 for earthquakes having moment magnitudes between 5.6 and 7.2. We also compare our inferred values with geologic surface energies. This comparison might suggest that breakdown work for large earthquakes goes primarily into heat production. Copyright 2005 by the American Geophysical Union.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research B: Solid Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2005JB003644","issn":"01480227","usgsCitation":"Tinti, E., Spudich, P., and Cocco, M., 2005, Earthquake fracture energy inferred from kinematic rupture models on extended faults: Journal of Geophysical Research B: Solid Earth, v. 110, no. 12, p. 1-25, https://doi.org/10.1029/2005JB003644.","startPage":"1","endPage":"25","numberOfPages":"25","costCenters":[],"links":[{"id":477930,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2005jb003644","text":"Publisher Index Page"},{"id":238173,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211028,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2005JB003644"}],"volume":"110","issue":"12","noUsgsAuthors":false,"publicationDate":"2005-12-07","publicationStatus":"PW","scienceBaseUri":"505a04ece4b0c8380cd50b91","contributors":{"authors":[{"text":"Tinti, E.","contributorId":16644,"corporation":false,"usgs":true,"family":"Tinti","given":"E.","affiliations":[],"preferred":false,"id":414970,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spudich, P.","contributorId":85700,"corporation":false,"usgs":true,"family":"Spudich","given":"P.","affiliations":[],"preferred":false,"id":414972,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cocco, M.","contributorId":70128,"corporation":false,"usgs":true,"family":"Cocco","given":"M.","email":"","affiliations":[],"preferred":false,"id":414971,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1015257,"text":"1015257 - 2005 - Characterizing flow regimes for floodplain forest conservation: An assessment of factors affecting sapling growth and survivorship on three cold desert rivers","interactions":[],"lastModifiedDate":"2017-12-26T13:03:01","indexId":"1015257","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1170,"text":"Canadian Journal of Forest Research","active":true,"publicationSubtype":{"id":10}},"title":"Characterizing flow regimes for floodplain forest conservation: An assessment of factors affecting sapling growth and survivorship on three cold desert rivers","docAbstract":"<p>I analyzed annual height growth and survivorship of Fremont cottonwood (<i>Populus fremontii</i> S. Watson) saplings on three floodplains in Colorado and Utah to assess responses to interannual variation in flow regime and summer precipitation. Mammal exclosures, supplemented with an insecticide treatment at one site, were used to assess flow regime – herbivore interactions. Multiple regression analyses on data collected over 7–11 years indicated that growth of continuously injury-free saplings was positively related to either peak discharge or the maximum 30-day discharge but was not related to interannual decline in the late-summer river stage (Δ<i>W</i><sub>MIN</sub>) or precipitation. Growth was fastest where Δ<i>W</i><sub>MIN</sub> was smallest and depth to the late-summer water table moderate (≤1.5 m). Survivorship increased with Δ<i>W</i><sub>MIN</sub> where the water table was at shallow depths. Herbivory reduced long-term height growth and survivorship by up to 60% and 50%, respectively. The results support the concept that flow history and environmental context determine whether a particular flow will have a net positive or negative influence on growth and survivorship and suggest that the flow regime that best promotes sapling growth and survival along managed rivers features a short spring flood pulse and constant base flow, with no interannual variation in the hydrograph. Because environmental contexts vary, interannual variation may be necessary for best overall stand performance.</p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/x05-203","usgsCitation":"Andersen, D., 2005, Characterizing flow regimes for floodplain forest conservation: An assessment of factors affecting sapling growth and survivorship on three cold desert rivers: Canadian Journal of Forest Research, v. 35, no. 12, p. 2886-2899, https://doi.org/10.1139/x05-203.","productDescription":"14 p.","startPage":"2886","endPage":"2899","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":132378,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"35","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4cd5","contributors":{"authors":[{"text":"Andersen, D.C.","contributorId":19119,"corporation":false,"usgs":true,"family":"Andersen","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":322690,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70027542,"text":"70027542 - 2005 - Bulk sediment Qp and Qs in the Mississippi embayment, central United States","interactions":[],"lastModifiedDate":"2020-05-01T18:47:32.860638","indexId":"70027542","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Bulk sediment Q<sub>p</sub> and Q<sub>s</sub> in the Mississippi embayment, central United States","title":"Bulk sediment Qp and Qs in the Mississippi embayment, central United States","docAbstract":"<p><span>We have estimated&nbsp;</span><i>P</i><span>-wave and&nbsp;</span><i>S</i><span>-wave anelastic attenuation coefficients for the thick, unconsolidated sediments of the Mississippi embayment, central United States, using the spectral distance decay of explosion&nbsp;</span><i>P</i><span>&nbsp;and Rayleigh waves. The sediment-trapped&nbsp;</span><i>P</i><span>&nbsp;wave,&nbsp;</span><i>P</i><sub>sed</sub><span>, is observed to ranges of 80 km at 10 Hz, and 1-Hz Rayleigh waves are observed out to 130 km from a 5000-lb borehole explosion in the northern part of the embayment. Rayleigh waves of 4 Hz are seen to distances of 3 km from a smaller 50-lb explosion. Analysis of the group velocity and amplitude-distance decay of both waves yields an average&nbsp;</span><i>Q</i><sub>s</sub><span>&nbsp;of 100 and&nbsp;</span><i>Q</i><sub>p</sub><span>&nbsp;of 200 for embayment sediments that are independent of frequency. Scatter in the&nbsp;</span><i>Q</i><span>&nbsp;estimates comes from interference of multiple&nbsp;</span><i>P</i><span>-wave reverberations and Rayleigh-wave modes. The attenuation model is self-consistent in that it is the same as obtained by the analysis of synthetic seismograms using the inferred&nbsp;</span><i>Q</i><span>-values. Inferred&nbsp;</span><i>Q</i><sub>p</sub><span>&nbsp;and&nbsp;</span><i>Q</i><sub>s</sub><span>&nbsp;values are more than three times higher than previous estimates and imply that unconsolidated sediments of the embayment do not significantly attenuate small-strain earthquake ground motions. These estimates represent a lower bound to&nbsp;</span><i>Q</i><span>&nbsp;of the sediments since significant scattering is observed in the waveform data that contributes to the distance decay of wave amplitude. Higher&nbsp;</span><i>Q</i><span>&nbsp;values also imply that the unconsolidated sediments of the embayment will form an efficient wave guide for surface waves radiated from shallow earthquakes or large earthquakes that rupture into the sediments, producing high-amplitude, long-duration wave trains that should be considered in earthquake hazard assessments.</span></p>","largerWorkTitle":"","language":"English","publisher":"Geological Society of America","doi":"10.1785/0120050047","issn":"","usgsCitation":"Langston, C., Bodin, P., Powell, C., Withers, M., Horton, S., and Mooney, W.D., 2005, Bulk sediment Qp and Qs in the Mississippi embayment, central United States: Bulletin of the Seismological Society of America, v. 95, no. 6, p. 2162-2179, https://doi.org/10.1785/0120050047.","productDescription":"18 p.","startPage":"2162","endPage":"2179","numberOfPages":"18","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":238129,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arkansas, Kentucky, Missouri, Tennessee","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.98876953125,\n              34.75966612466248\n            ],\n            [\n              -88.74755859375,\n              34.75966612466248\n            ],\n            [\n              -88.74755859375,\n              36.756490329505176\n            ],\n            [\n              -90.98876953125,\n              36.756490329505176\n            ],\n            [\n              -90.98876953125,\n              34.75966612466248\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"95","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f2aee4b0c8380cd4b2c8","contributors":{"authors":[{"text":"Langston, C.A.","contributorId":84882,"corporation":false,"usgs":true,"family":"Langston","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":414090,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bodin, P.","contributorId":29554,"corporation":false,"usgs":true,"family":"Bodin","given":"P.","email":"","affiliations":[],"preferred":false,"id":414087,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Powell, C.","contributorId":56849,"corporation":false,"usgs":true,"family":"Powell","given":"C.","email":"","affiliations":[],"preferred":false,"id":414089,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Withers, M.","contributorId":27667,"corporation":false,"usgs":true,"family":"Withers","given":"M.","email":"","affiliations":[],"preferred":false,"id":414086,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Horton, S.","contributorId":20146,"corporation":false,"usgs":true,"family":"Horton","given":"S.","email":"","affiliations":[],"preferred":false,"id":414085,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mooney, Walter D. 0000-0002-5310-3631 mooney@usgs.gov","orcid":"https://orcid.org/0000-0002-5310-3631","contributorId":3194,"corporation":false,"usgs":true,"family":"Mooney","given":"Walter","email":"mooney@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":414088,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":1015282,"text":"1015282 - 2005 - Examining patterns of bat activity in Bandelier National Monument, New Mexico, using walking point transects","interactions":[],"lastModifiedDate":"2017-12-18T10:26:42","indexId":"1015282","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3451,"text":"Southwestern Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Examining patterns of bat activity in Bandelier National Monument, New Mexico, using walking point transects","docAbstract":"<p><span>We conducted a preliminary study using small field crews, a single Anabat II detector coupled with a laptop computer, and point transects to examine patterns of bat activity at a scale of interest to local resource managers. The study was conducted during summers of 1996–1998 in Bandelier National Monument in the Jemez Mountains of northern New Mexico, a landscape with distinct vegetation zones and high species richness of bats. We developed simple models that described general patterns of acoustic activity within 4 vegetation zones based primarily on nightly variation and a qualitative index of habitat complexity. Bat acoustic activity (number of bat passes&amp;sol point) did not vary dramatically among a limited sample of transects within a vegetation zone during 1996. In 1997 and 1998, single transects within each vegetation zone were established, and bat activity did not vary annually within these zones. Acoustic activity differed among the 4 vegetation zones of interest, with the greatest activity occurring in riparian canyon bottomland, intermediate activity in coniferous forest and a 1977 burned zone, and lowest activity in piñon-juniper woodlands. We identified 68.5% of 2,529 bat passes recorded during point-transect surveys to species using an echolocation call reference library we established for the area and qualitative characteristics of bat calls. Bat species richness and composition differed among vegetation zones. Results of these efforts were consistent with general knowledge of where different bat species typically forage and with the natural history of bats of New Mexico, suggesting such a method might have value for drawing inferences about bat activity in different vegetation zones.</span></p>","language":"English","publisher":"Southwestern Association of Naturalists","doi":"10.1894/0038-4909(2005)050[0197:EPOBAI]2.0.CO;2","usgsCitation":"Ellison, L., Everette, A., and Bogan, M., 2005, Examining patterns of bat activity in Bandelier National Monument, New Mexico, using walking point transects: Southwestern Naturalist, v. 50, no. 2, p. 197-208, https://doi.org/10.1894/0038-4909(2005)050[0197:EPOBAI]2.0.CO;2.","productDescription":"12 p.","startPage":"197","endPage":"208","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":132701,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"50","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f95a2","contributors":{"authors":[{"text":"Ellison, L.E.","contributorId":103610,"corporation":false,"usgs":true,"family":"Ellison","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":322753,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Everette, A. L. 0000-0003-2539-9129","orcid":"https://orcid.org/0000-0003-2539-9129","contributorId":31718,"corporation":false,"usgs":true,"family":"Everette","given":"A. L.","affiliations":[],"preferred":false,"id":322752,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bogan, M.A.","contributorId":17939,"corporation":false,"usgs":true,"family":"Bogan","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":322751,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1015283,"text":"1015283 - 2005 - Drought allocations using the Systems Impact Assessment Model: Klamath River","interactions":[],"lastModifiedDate":"2017-12-26T11:54:33","indexId":"1015283","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2501,"text":"Journal of Water Resources Planning and Management","active":true,"publicationSubtype":{"id":10}},"title":"Drought allocations using the Systems Impact Assessment Model: Klamath River","docAbstract":"<p>Water supply and allocation scenarios for the Klamath River, Ore. and Calif., were evaluated using the Systems Impact Assessment Model (SIAM), a decision support system developed by the U.S. Geological Survey. SIAM is a set of models with a graphical user interface that simulates water supply and delivery in a managed river system, water quality, and fish production. Simulation results are presented for drought conditions, one aspect of Klamath River water operations. The Klamath River Basin has experienced critically dry conditions in 1992, 1994, and 2001. Drought simulations are useful to estimate the impacts of specific legal or institutional flow constraints. In addition, simulations help to identify potential adverse water quality consequences including evaluating the potential for reducing adverse temperature impacts on anadromous fish. In all drought simulations, water supply was insufficient to fully meet upstream and downstream targets for endangered species.</p>","language":"English","publisher":"American Society of Civil Engineers","doi":"10.1061/(ASCE)0733-9496(2005)131:2(110)","usgsCitation":"Flug, M., and Campbell, S., 2005, Drought allocations using the Systems Impact Assessment Model: Klamath River: Journal of Water Resources Planning and Management, v. 131, no. 2, p. 110-115, https://doi.org/10.1061/(ASCE)0733-9496(2005)131:2(110).","productDescription":"6 p.","startPage":"110","endPage":"115","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":132702,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"131","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5ee4b07f02db633da4","contributors":{"authors":[{"text":"Flug, M.","contributorId":57419,"corporation":false,"usgs":true,"family":"Flug","given":"M.","affiliations":[],"preferred":false,"id":322755,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, S.G.","contributorId":37694,"corporation":false,"usgs":true,"family":"Campbell","given":"S.G.","email":"","affiliations":[],"preferred":false,"id":322754,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70027665,"text":"70027665 - 2005 - A simple method for calculating growth rates of petroleum hydrocarbon plumes","interactions":[],"lastModifiedDate":"2018-10-29T11:04:45","indexId":"70027665","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1861,"text":"Ground Water","active":true,"publicationSubtype":{"id":10}},"title":"A simple method for calculating growth rates of petroleum hydrocarbon plumes","docAbstract":"<div class=\"abstract-group\"><div class=\"article-section__content en main\"><p>Consumption of aquifer Fe(III) during biodegradation of ground water contaminants may result in expansion of a contaminant plume, changing the outlook for monitored natural attenuation. Data from two research sites contaminated with petroleum hydrocarbons show that toluene and xylenes degrade under methanogenic conditions, but the benzene and ethylbenzene plumes grow as aquifer Fe(III) supplies are depleted. By considering a one‐dimensional reaction front in a constant unidirectional flow field, it is possible to derive a simple expression for the growth rate of a benzene plume. The method balances the mass flux of benzene with the Fe(III) content of the aquifer, assuming that the biodegradation reaction is instantaneous. The resulting expression shows that the benzene front migration is retarded relative to the ground water velocity by a factor that depends on the concentrations of hydrocarbon and bioavailable Fe(III). The method provides good agreement with benzene plumes at a crude oil study site in Minnesota and a gasoline site in South Carolina. Compared to the South Carolina site, the Minnesota site has 25% higher benzene flux but eight times the Fe(III), leading to about one‐sixth the expansion rate. Although it was developed for benzene, toluene, ethylbenzene, and xylenes, the growth‐rate estimation method may have applications to contaminant plumes from other persistent contaminant sources.</p></div></div>","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.2005.00093.x","issn":"0017467X","usgsCitation":"Bekins, B., Cozzarelli, I., and Curtis, G., 2005, A simple method for calculating growth rates of petroleum hydrocarbon plumes: Ground Water, v. 43, no. 6, p. 817-826, https://doi.org/10.1111/j.1745-6584.2005.00093.x.","productDescription":"10 p.","startPage":"817","endPage":"826","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":238347,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211142,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1745-6584.2005.00093.x"}],"volume":"43","issue":"6","noUsgsAuthors":false,"publicationDate":"2005-08-24","publicationStatus":"PW","scienceBaseUri":"5059e58fe4b0c8380cd46e13","contributors":{"authors":[{"text":"Bekins, B.A.","contributorId":98309,"corporation":false,"usgs":true,"family":"Bekins","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":414640,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cozzarelli, I.M. 0000-0002-5123-1007","orcid":"https://orcid.org/0000-0002-5123-1007","contributorId":22343,"corporation":false,"usgs":true,"family":"Cozzarelli","given":"I.M.","affiliations":[],"preferred":false,"id":414638,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Curtis, G.P.","contributorId":65619,"corporation":false,"usgs":true,"family":"Curtis","given":"G.P.","email":"","affiliations":[],"preferred":false,"id":414639,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70027666,"text":"70027666 - 2005 - Radiated energy and the physics of earthquake faulting","interactions":[],"lastModifiedDate":"2012-03-12T17:21:17","indexId":"70027666","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Radiated energy and the physics of earthquake faulting","docAbstract":"[No abstract available]","largerWorkTitle":"Eos","language":"English","issn":"00963941","usgsCitation":"McGarr, A., Abercrombie, R., and Kanamori, H., 2005, Radiated energy and the physics of earthquake faulting, <i>in</i> Eos, v. 86, no. 45.","startPage":"447","costCenters":[],"links":[{"id":238348,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"86","issue":"45","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a9391e4b0c8380cd80edd","contributors":{"authors":[{"text":"McGarr, Art 0000-0001-9769-4093","orcid":"https://orcid.org/0000-0001-9769-4093","contributorId":43491,"corporation":false,"usgs":true,"family":"McGarr","given":"Art","affiliations":[],"preferred":false,"id":414641,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Abercrombie, R.E.","contributorId":57611,"corporation":false,"usgs":true,"family":"Abercrombie","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":414643,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kanamori, H.","contributorId":55438,"corporation":false,"usgs":true,"family":"Kanamori","given":"H.","affiliations":[],"preferred":false,"id":414642,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70027667,"text":"70027667 - 2005 - Delineating priority habitat areas for the conservation of Andean bears in northern Ecuador","interactions":[],"lastModifiedDate":"2012-03-12T17:21:17","indexId":"70027667","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3671,"text":"Ursus","active":true,"publicationSubtype":{"id":10}},"title":"Delineating priority habitat areas for the conservation of Andean bears in northern Ecuador","docAbstract":"We sought to identify priority areas for the conservation of Andean bear (Tremarctos ornatus) habitat in the northern portion of the eastern Andean cordillera in Ecuador. The study area included pa??ramo and montane forest habitats within the Antisana and Cayambe-Coca ecological reserves, and unprotected areas north of these reserves with elevations ranging from 1,800 to 4,300 m. We collected data on bear occurrence along 53 transects during 2000-01 in the Oyacachi River basin, an area of indigenous communities within the Cayambe-Coca Ecological Reserve. We used those data and a set of 7 environmental variables to predict suitability of Andean bear habitat using Mahalanobis distance, a multivariate measure of dissimilarity. The Mahalanobis distance values were classified into 5 classes of habitat suitability and generalized to a resolution of 1,650-m ?? 1,650-m grid cells. Clusters of grid cells with high suitability values were delineated from the generalized model and denned as important habitat areas (IHAs) for conservation. The IHAs were ranked using a weighted index that included factors of elevation range, influence from disturbed areas, and current conservation status. We identified 12 IHAs, which were mainly associated with pa??ramo and cloud forest habitats; 2 of these areas have high conservation priorities because they are outside existing reserves and close to areas of human pressure. The distribution of the IHAs highlighted the role of human land use as the main source of fragmentation of Andean bear habitat in this region, emphasizing the importance of preserving habitat connectivity to allow the seasonal movements among habitat types that we documented for this species. Furthermore, the existence of areas with high habitat suitability close to areas of intense human use indicates the importance of bear-human conflict management as a critical Andean bear conservation strategy. We suggest that a promising conservation opportunity for this species is linked to its occurrence in highland habitats, which play a key role in the maintenance of long-term water supplies.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ursus","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2192/1537-6176(2005)016[0222:DPHAFT]2.0.CO;2","issn":"15376176","usgsCitation":"Peralvo, M., Cuesta, F., and Van Manen, F., 2005, Delineating priority habitat areas for the conservation of Andean bears in northern Ecuador: Ursus, v. 16, no. 2, p. 222-233, https://doi.org/10.2192/1537-6176(2005)016[0222:DPHAFT]2.0.CO;2.","startPage":"222","endPage":"233","numberOfPages":"12","costCenters":[],"links":[{"id":211172,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2192/1537-6176(2005)016[0222:DPHAFT]2.0.CO;2"},{"id":238386,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fe61e4b0c8380cd4ecee","contributors":{"authors":[{"text":"Peralvo, M.F.","contributorId":8672,"corporation":false,"usgs":true,"family":"Peralvo","given":"M.F.","affiliations":[],"preferred":false,"id":414644,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cuesta, F.","contributorId":79696,"corporation":false,"usgs":true,"family":"Cuesta","given":"F.","email":"","affiliations":[],"preferred":false,"id":414646,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Van Manen, F.","contributorId":25329,"corporation":false,"usgs":true,"family":"Van Manen","given":"F.","email":"","affiliations":[],"preferred":false,"id":414645,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70027723,"text":"70027723 - 2005 - Further evidence for the invasion and establishment of Pterois volitans (Teleostei: Scorpaenidae) along the Atlantic Coast of the United States","interactions":[],"lastModifiedDate":"2012-03-12T17:20:49","indexId":"70027723","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3444,"text":"Southeastern Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Further evidence for the invasion and establishment of Pterois volitans (Teleostei: Scorpaenidae) along the Atlantic Coast of the United States","docAbstract":"We document the continued population expansion of red lionfish, Pterois volitans, the first documented successful introduction of an invasive marine fish species from the western Pacific to Atlantic coastal waters of the United States. Red lionfish are indigenous to the Indo-Pacific and have apparently established one or more breeding populations on reefs off the southeastern United States. Fifty-nine specimens, most presumably adult red lionfish, were documented or collected on live-bottom reefs off North Carolina, South Carolina, and Florida, and on a manmade structure off Georgia. Observation/collection depths and bottom water temperatures for these fish ranged from 40-99 m and 13.8-24.4??C, respectively. Eleven juvenile lionfish, believed to be expatriated from southeastern waters, were collected in estuaries along the coast of Long Island, NY, at depths of 0-5 m and water temperatures ranging from 13.8-16.5??C. Twelve of the total 70 specimens collected or observed were positively identified as red lionfish. Based on histological assessment of gonad tissue, two reproductively-active males and one immature female were collected. The life history of red lionfish, especially their reproductive biology and food habits, should be investigated along the east coast of the US to determine the potential impacts of this species on ecosystems they have invaded.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Southeastern Naturalist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1656/1528-7092(2005)004[0193:FEFTIA]2.0.CO;2","issn":"15287092","usgsCitation":"Meister, H., Wyanski, D., Loefer, J., Ross, S.W., Quattrini, A., and Sulak, K., 2005, Further evidence for the invasion and establishment of Pterois volitans (Teleostei: Scorpaenidae) along the Atlantic Coast of the United States: Southeastern Naturalist, v. 4, no. 2, p. 193-206, https://doi.org/10.1656/1528-7092(2005)004[0193:FEFTIA]2.0.CO;2.","startPage":"193","endPage":"206","numberOfPages":"14","costCenters":[],"links":[{"id":210981,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1656/1528-7092(2005)004[0193:FEFTIA]2.0.CO;2"},{"id":238101,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1423e4b0c8380cd5491a","contributors":{"authors":[{"text":"Meister, H.S.","contributorId":30814,"corporation":false,"usgs":true,"family":"Meister","given":"H.S.","email":"","affiliations":[],"preferred":false,"id":414945,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wyanski, D.M.","contributorId":22962,"corporation":false,"usgs":true,"family":"Wyanski","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":414944,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Loefer, J.K.","contributorId":95673,"corporation":false,"usgs":true,"family":"Loefer","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":414949,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ross, Steve W.","contributorId":72543,"corporation":false,"usgs":false,"family":"Ross","given":"Steve","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":414947,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Quattrini, A.M.","contributorId":70985,"corporation":false,"usgs":true,"family":"Quattrini","given":"A.M.","affiliations":[],"preferred":false,"id":414946,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Sulak, K. J. 0000-0002-4795-9310","orcid":"https://orcid.org/0000-0002-4795-9310","contributorId":76690,"corporation":false,"usgs":true,"family":"Sulak","given":"K. J.","affiliations":[],"preferred":false,"id":414948,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70027724,"text":"70027724 - 2005 - An integrated environmental tracer approach to characterizing groundwater circulation in a mountain block","interactions":[],"lastModifiedDate":"2018-03-30T11:07:22","indexId":"70027724","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"An integrated environmental tracer approach to characterizing groundwater circulation in a mountain block","docAbstract":"<p><span>The subsurface transfer of water from a mountain block to an adjacent basin (mountain block recharge (MBR)) is a commonly invoked mechanism of recharge to intermountain basins. However, MBR estimates are highly uncertain. We present an approach to characterize bulk fluid circulation in a mountain block and thus MBR that utilizes environmental tracers from the basin aquifer. Noble gas recharge temperatures, groundwater ages, and temperature data combined with heat and fluid flow modeling are used to identify clearly improbable flow regimes in the southeastern Salt Lake Valley, Utah, and adjacent Wasatch Mountains. The range of possible MBR rates is reduced by 70%. Derived MBR rates (5.5–12.6 × 10</span><sup>4</sup><span><span>&nbsp;</span>m</span><sup>3</sup><span><span>&nbsp;</span>d</span><sup>−1</sup><span>) are on the same order of magnitude as previous large estimates, indicating that significant MBR to intermountain basins is plausible. However, derived rates are 50–100% of the lowest previous estimate, meaning total recharge is probably less than previously thought.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2005WR004178","usgsCitation":"Manning, A.H., and Solomon, D., 2005, An integrated environmental tracer approach to characterizing groundwater circulation in a mountain block: Water Resources Research, v. 41, no. 12, Article W12412; 19 p., https://doi.org/10.1029/2005WR004178.","productDescription":"Article W12412; 19 p.","costCenters":[],"links":[{"id":477723,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2005wr004178","text":"Publisher Index Page"},{"id":238102,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"41","issue":"12","noUsgsAuthors":false,"publicationDate":"2005-12-06","publicationStatus":"PW","scienceBaseUri":"5059ea80e4b0c8380cd488e1","contributors":{"authors":[{"text":"Manning, Andrew H. 0000-0002-6404-1237 amanning@usgs.gov","orcid":"https://orcid.org/0000-0002-6404-1237","contributorId":1305,"corporation":false,"usgs":true,"family":"Manning","given":"Andrew","email":"amanning@usgs.gov","middleInitial":"H.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":414950,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Solomon, D. Kip","contributorId":71441,"corporation":false,"usgs":true,"family":"Solomon","given":"D. Kip","affiliations":[],"preferred":false,"id":414951,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}