{"pageNumber":"1040","pageRowStart":"25975","pageSize":"25","recordCount":68937,"records":[{"id":70175936,"text":"70175936 - 2006 - The conservation and population status of the world's waders at the turn of the millennium","interactions":[],"lastModifiedDate":"2018-05-20T11:19:34","indexId":"70175936","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"chapter":"5.2.1","title":"The conservation and population status of the world's waders at the turn of the millennium","docAbstract":"<p><span>Using information from many sources, but especially data collated for the third edition of Wetlands International’s Waterbird Population Estimates, we review the status of the world’s waders in the late 1990s. There are widespread declines in most regions and biotopes caused principally by loss and degradation of wetland (and other) habitats. On different flyways, between 33%and 68% of populations are in decline, compared with only 0% to 29% increasing. Non-migratory, island species have especially poor status, with about half of all island waders being globally threatened with extinction. Of particular conservation concern is the declining environmental status of several key staging areas,which provide energetic ‘spring-boards’ for long-distance migrants. The degradation of these areas compromises the status of many migrant waders. The rapid collapse of populations, forced below threshold levels, has been predicted theoretically, and now appears to be occurring in a number of rapidly declining populations. Conservation responses must urgently address causes of wetland loss and degradation, as well as enhancing monitoring and research so as better to inform appropriate conservation policies. National and international strategies and conservation instruments have scope to help, but need to be much more strategic in their implementation so as to address root causes.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Waterbirds around the world: A global overview of the conservation, management, and research of the world's waterbird flyways","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"The Waterbirds Around the World Conference","conferenceDate":"April 2004","conferenceLocation":"Edinburgh, Scotland","language":"English","publisher":"TSO Scotland Ltd","publisherLocation":"Edinburgh, UK","isbn":"9780114973339","usgsCitation":"Stroud, D.A., Baker, A., Blanco, D., Davidson, N.C., Ganter, B., Gill, R., Gonzalez, P., Haanstra, L., Morrison, R.I., Piersma, T., Scott, D., Thorup, O., West, R., Wilson, J., and Zockler, C., 2006, The conservation and population status of the world's waders at the turn of the millennium, <i>in</i> Waterbirds around the world: A global overview of the conservation, management, and research of the world's waterbird flyways, Edinburgh, Scotland, April 2004, p. 643-648.","productDescription":"6 p.","startPage":"643","endPage":"648","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":327257,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":339373,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://jncc.defra.gov.uk/worldwaterbirds"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bc224fe4b03fd6b7de1782","contributors":{"editors":[{"text":"Boere, Gerard C.","contributorId":111405,"corporation":false,"usgs":false,"family":"Boere","given":"Gerard","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":690230,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Galbraith, Colin A.","contributorId":113310,"corporation":false,"usgs":false,"family":"Galbraith","given":"Colin","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":690231,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Stroud, David A.","contributorId":113852,"corporation":false,"usgs":true,"family":"Stroud","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":690232,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Stroud, David A.","contributorId":113852,"corporation":false,"usgs":true,"family":"Stroud","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":646590,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baker, Andy","contributorId":73053,"corporation":false,"usgs":true,"family":"Baker","given":"Andy","email":"","affiliations":[],"preferred":false,"id":646591,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blanco, D.E.","contributorId":173932,"corporation":false,"usgs":false,"family":"Blanco","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":646592,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Davidson, Nick C.","contributorId":80553,"corporation":false,"usgs":true,"family":"Davidson","given":"Nick","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":646593,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ganter, B.","contributorId":173933,"corporation":false,"usgs":false,"family":"Ganter","given":"B.","email":"","affiliations":[],"preferred":false,"id":646594,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gill, Robert E. Jr. 0000-0002-6385-4500 rgill@usgs.gov","orcid":"https://orcid.org/0000-0002-6385-4500","contributorId":171747,"corporation":false,"usgs":true,"family":"Gill","given":"Robert E.","suffix":"Jr.","email":"rgill@usgs.gov","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":646595,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Gonzalez, P.M.","contributorId":76965,"corporation":false,"usgs":true,"family":"Gonzalez","given":"P.M.","email":"","affiliations":[],"preferred":false,"id":646596,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Haanstra, L.","contributorId":173934,"corporation":false,"usgs":false,"family":"Haanstra","given":"L.","email":"","affiliations":[],"preferred":false,"id":646597,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Morrison, R. I. G.","contributorId":66640,"corporation":false,"usgs":false,"family":"Morrison","given":"R.","email":"","middleInitial":"I. G.","affiliations":[],"preferred":false,"id":646598,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Piersma, Theunis","contributorId":95369,"corporation":false,"usgs":true,"family":"Piersma","given":"Theunis","affiliations":[],"preferred":false,"id":646599,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Scott, D.","contributorId":94107,"corporation":false,"usgs":true,"family":"Scott","given":"D.","affiliations":[],"preferred":false,"id":646600,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Thorup, O.","contributorId":173935,"corporation":false,"usgs":false,"family":"Thorup","given":"O.","email":"","affiliations":[],"preferred":false,"id":646601,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"West, R.","contributorId":26996,"corporation":false,"usgs":true,"family":"West","given":"R.","email":"","affiliations":[],"preferred":false,"id":646602,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Wilson, J.L.","contributorId":37345,"corporation":false,"usgs":true,"family":"Wilson","given":"J.L.","affiliations":[],"preferred":false,"id":646603,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Zockler, Christoph","contributorId":173936,"corporation":false,"usgs":false,"family":"Zockler","given":"Christoph","email":"","affiliations":[],"preferred":false,"id":646604,"contributorType":{"id":1,"text":"Authors"},"rank":15}]}}
,{"id":70030381,"text":"70030381 - 2006 - Evaluation of gridded snow water equivalent and satellite snow cover products for mountain basins in a hydrologic model","interactions":[],"lastModifiedDate":"2012-03-12T17:21:03","indexId":"70030381","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Evaluation of gridded snow water equivalent and satellite snow cover products for mountain basins in a hydrologic model","docAbstract":"The USGS precipitation-runoff modelling system (PRMS) hydrologic model was used to evaluate experimental, gridded, 1 km2 snow-covered area (SCA) and snow water equivalent (SWE) products for two headwater basins within the Rio Grande (i.e. upper Rio Grande River basin) and Salt River (i.e. Black River basin) drainages in the southwestern USA. The SCA product was the fraction of each 1 km2 pixel covered by snow and was derived from NOAA advanced very high-resolution radiometer imagery. The SWE product was developed by multiplying the SCA product by SWE estimates interpolated from National Resources Conservation Service snow telemetry point measurements for a 6 year period (1995-2000). Measured SCA and SWE estimates were consistently lower than values estimated from temperature and precipitation within PRMS. The greatest differences occurred in the relatively complex terrain of the Rio Grande basin, as opposed to the relatively homogeneous terrain of the Black River basin, where differences were small. Differences between modelled and measured snow were different for the accumulation period versus the ablation period and had an elevational trend. Assimilating the measured snowfields into a version of PRMS calibrated to achieve water balance without assimilation led to reduced performance in estimating streamflow for the Rio Grande and increased performance in estimating streamflow for the Black River basin. Correcting the measured SCA and SWE for canopy effects improved simulations by adding snow mostly in the mid-to-high elevations, where satellite estimates of SCA are lower than model estimates. Copyright ?? 2006 John Wiley & Sons, Ltd.","largerWorkTitle":"Hydrological Processes","language":"English","doi":"10.1002/hyp.6130","issn":"08856087","usgsCitation":"Dressler, K., Leavesley, G., Bales, R., and Fassnacht, S., 2006, Evaluation of gridded snow water equivalent and satellite snow cover products for mountain basins in a hydrologic model, <i>in</i> Hydrological Processes, v. 20, no. 4, p. 673-688, https://doi.org/10.1002/hyp.6130.","startPage":"673","endPage":"688","numberOfPages":"16","costCenters":[],"links":[{"id":211860,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/hyp.6130"},{"id":239232,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-02-27","publicationStatus":"PW","scienceBaseUri":"505a0c7ee4b0c8380cd52b8e","contributors":{"authors":[{"text":"Dressler, K.A.","contributorId":9455,"corporation":false,"usgs":true,"family":"Dressler","given":"K.A.","email":"","affiliations":[],"preferred":false,"id":426926,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leavesley, G.H.","contributorId":93895,"corporation":false,"usgs":true,"family":"Leavesley","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":426929,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bales, R.C.","contributorId":10379,"corporation":false,"usgs":true,"family":"Bales","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":426927,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fassnacht, S.R.","contributorId":58842,"corporation":false,"usgs":true,"family":"Fassnacht","given":"S.R.","affiliations":[],"preferred":false,"id":426928,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70030340,"text":"70030340 - 2006 - The contingent behavior of charter fishing participants on the Chesapeake Bay: Welfare estimates associated with water quality improvements","interactions":[],"lastModifiedDate":"2012-03-12T17:21:02","indexId":"70030340","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2261,"text":"Journal of Environmental Planning and Management","active":true,"publicationSubtype":{"id":10}},"title":"The contingent behavior of charter fishing participants on the Chesapeake Bay: Welfare estimates associated with water quality improvements","docAbstract":"Water quality in the Chesapeake Bay has deteriorated over recent years. Historically, fishing has contributed to the region's local economy in terms of commercial and recreational harvests. A contingent behavior model is used to estimate welfare measures for charter fishing participants with regard to a hypothetical improvement in water quality. Using a truncated Poisson count model corrected for endogenous stratification, it was found that charter fishers not only contribute to the local market economy, but they also place positive non-market value on preserving the Bay's water quality. Using two estimates for travels costs it is estimated that the individual consumer surplus is $200 and $117 per trip, and the average individual consumer surplus values for an improvement in water quality is $75 and $44 for two models estimated. ?? 2006 University of Newcastle upon Tyne.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Environmental Planning and Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1080/09640560500508064","issn":"09640568","usgsCitation":"Poor, P., and Breece, M., 2006, The contingent behavior of charter fishing participants on the Chesapeake Bay: Welfare estimates associated with water quality improvements: Journal of Environmental Planning and Management, v. 49, no. 2, p. 265-278, https://doi.org/10.1080/09640560500508064.","startPage":"265","endPage":"278","numberOfPages":"14","costCenters":[],"links":[{"id":211745,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1080/09640560500508064"},{"id":239094,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"49","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baa5be4b08c986b3227e9","contributors":{"authors":[{"text":"Poor, P.J.","contributorId":21348,"corporation":false,"usgs":true,"family":"Poor","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":426752,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Breece, M.","contributorId":16652,"corporation":false,"usgs":true,"family":"Breece","given":"M.","email":"","affiliations":[],"preferred":false,"id":426751,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70030564,"text":"70030564 - 2006 - MODFLOW/MT3DMS-based simulation of variable-density ground water flow and transport","interactions":[],"lastModifiedDate":"2012-03-12T17:21:05","indexId":"70030564","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","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":"MODFLOW/MT3DMS-based simulation of variable-density ground water flow and transport","docAbstract":"This paper presents an approach for coupling MODFLOW and MT3DMS for the simulation of variable-density ground water flow. MODFLOW routines were modified to solve a variable-density form of the ground water flow equation in which the density terms are calculated using an equation of state and the simulated MT3DMS solute concentrations. Changes to the MODFLOW and MT3DMS input files were kept to a minimum, and thus existing data files and data files created with most pre- and postprocessors can be used directly with the SEAWAT code. The approach was tested by simulating the Henry problem and two of the saltpool laboratory experiments (low- and high-density cases). For the Henry problem, the simulated results compared well with the steady-state semianalytic solution and also the transient isochlor movement as simulated by a finite-element model. For the saltpool problem, the simulated breakthrough curves compared better with the laboratory measurements for the low-density case than for the high-density case but showed good agreement with the measured salinity isosurfaces for both cases. Results from the test cases presented here indicate that the MODFLOW/MT3DMS approach provides accurate solutions for problems involving variable-density ground water flow and solute transport. ?? 2006 National Ground Water Association.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ground Water","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1745-6584.2005.00156.x","issn":"0017467X","usgsCitation":"Langevin, C., and Guo, W., 2006, MODFLOW/MT3DMS-based simulation of variable-density ground water flow and transport: Ground Water, v. 44, no. 3, p. 339-351, https://doi.org/10.1111/j.1745-6584.2005.00156.x.","startPage":"339","endPage":"351","numberOfPages":"13","costCenters":[],"links":[{"id":477602,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.1049","text":"External Repository"},{"id":211960,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1745-6584.2005.00156.x"},{"id":239350,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"3","noUsgsAuthors":false,"publicationDate":"2005-12-06","publicationStatus":"PW","scienceBaseUri":"505a4ae4e4b0c8380cd69117","contributors":{"authors":[{"text":"Langevin, C.D.","contributorId":25976,"corporation":false,"usgs":true,"family":"Langevin","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":427663,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Guo, W.","contributorId":43230,"corporation":false,"usgs":true,"family":"Guo","given":"W.","email":"","affiliations":[],"preferred":false,"id":427664,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70030250,"text":"70030250 - 2006 - Carbon dioxide emissions from vegetation-kill zones around the resurgent dome of Long Valley caldera, eastern California, USA","interactions":[],"lastModifiedDate":"2019-03-25T10:27:06","indexId":"70030250","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Carbon dioxide emissions from vegetation-kill zones around the resurgent dome of Long Valley caldera, eastern California, USA","docAbstract":"<div class=\"abstract svAbstract \" data-etype=\"ab\"><p id=\"\">A survey of diffuse CO<sub>2</sub> efflux, soil temperature and soil-gas chemistry over areas of localized vegetation-kill on and around the resurgent dome of Long Valley caldera California was performed to evaluate the premise that gaseous and thermal anomalies are related to renewed intrusion of magma. Some kill sites are long-lived features and others have developed in the past few years. Total anomalous CO<sub>2</sub> emissions from the thirteen areas average around 8.7 t per day; but the majority of the emissions come from four sites west of the Casa Diablo geothermal power plant. Geochemical analyses of the soil-gases from locations west and east of the plant revealed the presence of isobutane related to plant operations. The <i>δ</i><sup>13</sup>C values of diffuse CO<sub>2</sub> range from −&nbsp;5.7‰ to −&nbsp;3.4‰, similar to values previously reported for CO<sub>2</sub> from hot springs and thermal wells around Long Valley.</p><p id=\"\">At many of the vegetation-kill sites soil temperatures reach boiling at depths ≤&nbsp;20 cm. Soil temperature/depth profiles at two of the high-emissions areas indicate that the conductive thermal gradient in the center of the areas is around 320 °C m<sup>−&nbsp;1</sup>. We estimate total heat loss from the two areas to be about 6.1 and 2.3 MW. Given current thinking on the rate of hydrothermal fluid flow across the caldera and using the CO<sub>2</sub> concentration in the thermal fluids, the heat and CO<sub>2</sub> loss from the kill areas is easily provided by the shallow hydrothermal system, which is sourced to the west of the resurgent dome. We find no evidence that the development of new areas of vegetation kill across the resurgent dome are related to new input of magma or magmatic fluids from beneath the resurgent dome. Our findings indicate that the areas have developed as a response to changes in the shallow hydrologic system. Some of the changes are likely related to fluid production at the power plant, but at distal sites the changes are more likely related to seismicity and uplift of the dome.</p></div>","language":"English","publisher":"Elsevier Science","doi":"10.1016/j.jvolgeores.2005.11.003","issn":"03770273","usgsCitation":"Bergfeld, D., Evans, W.C., Howle, J.F., and Farrar, C.D., 2006, Carbon dioxide emissions from vegetation-kill zones around the resurgent dome of Long Valley caldera, eastern California, USA: Journal of Volcanology and Geothermal Research, v. 152, no. 1-2, p. 140-156, https://doi.org/10.1016/j.jvolgeores.2005.11.003.","productDescription":"17 p.","startPage":"140","endPage":"156","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":239260,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Long Valley caldera","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.0421142578125,\n              37.448696585910376\n            ],\n            [\n              -120.0421142578125,\n              38.74551518488265\n            ],\n            [\n              -118.4600830078125,\n              38.74551518488265\n            ],\n            [\n              -118.4600830078125,\n              37.448696585910376\n            ],\n            [\n              -120.0421142578125,\n              37.448696585910376\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"152","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f35fe4b0c8380cd4b767","contributors":{"authors":[{"text":"Bergfeld, Deborah 0000-0003-4570-7627 dbergfel@usgs.gov","orcid":"https://orcid.org/0000-0003-4570-7627","contributorId":152531,"corporation":false,"usgs":true,"family":"Bergfeld","given":"Deborah","email":"dbergfel@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":426305,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Evans, William C.","contributorId":104903,"corporation":false,"usgs":true,"family":"Evans","given":"William","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":426308,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Howle, James F. 0000-0003-0491-6203 jfhowle@usgs.gov","orcid":"https://orcid.org/0000-0003-0491-6203","contributorId":2225,"corporation":false,"usgs":true,"family":"Howle","given":"James","email":"jfhowle@usgs.gov","middleInitial":"F.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":426306,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Farrar, Christopher D. cdfarrar@usgs.gov","contributorId":1501,"corporation":false,"usgs":true,"family":"Farrar","given":"Christopher","email":"cdfarrar@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":426307,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70031138,"text":"70031138 - 2006 - Sources of variation in survival of breeding female wood ducks","interactions":[],"lastModifiedDate":"2012-03-12T17:21:17","indexId":"70031138","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1318,"text":"Condor","active":true,"publicationSubtype":{"id":10}},"title":"Sources of variation in survival of breeding female wood ducks","docAbstract":"In waterfowl, reproduction is physiologically demanding and females are exposed to varying risks of mortality at different periods of the breeding cycle. Moreover, differences among females may influence survival within breeding periods. We captured and fitted female Wood Ducks (Aix sponsa) with radio-transmitters before nest initiation during two breeding seasons to estimate survival and investigate sources of variation in survival. We partitioned the breeding season into three periods (preincubation, incubation, postnesting) according to breeding status of individual females, and used information-theoretic methods to compare models in which daily survival varied among periods, between successful and failed nesting females, and with parameters describing individual heterogeneity. Our analysis suggested that daily survival was best modeled as a function of breeding period, differences between successful and failed nesting females during postnesting, and early incubation body condition of successful females during post-nesting. Model-averaged daily survival was 0.9988 (95% CL: 0.9963-0.9996) during preincubation and 1.0 during incubation. Postnesting daily survival was 1.0 for failed nesting females and 0.9948 (0.9773-0.9988) for successful females, suggesting a trade-off between current reproduction and survival. Female age, body condition at capture, nest initiation date, and brood size generally were not useful for explaining variation in survival. Only early incubation body condition was important for modeling survival of successful females during postnesting; however, weight of evidence was limited and the effect on survival was weak. Mortality was greatest for females during preincubation and for females that nested successfully. Results support the hypothesis that brood care is costly for females. ?? The Cooper Ornithological Society 2006.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Condor","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1650/0010-5422(2006)108[0201:SOVISO]2.0.CO;2","issn":"00105422","usgsCitation":"Hartke, K.M., Grand, J., Hepp, G.R., and Folk, T., 2006, Sources of variation in survival of breeding female wood ducks: Condor, v. 108, no. 1, p. 201-210, https://doi.org/10.1650/0010-5422(2006)108[0201:SOVISO]2.0.CO;2.","startPage":"201","endPage":"210","numberOfPages":"10","costCenters":[],"links":[{"id":477421,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1650/0010-5422(2006)108[0201:soviso]2.0.co;2","text":"Publisher Index Page"},{"id":211488,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1650/0010-5422(2006)108[0201:SOVISO]2.0.CO;2"},{"id":238784,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"108","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b93a0e4b08c986b31a5d2","contributors":{"authors":[{"text":"Hartke, Kevin M.","contributorId":84048,"corporation":false,"usgs":true,"family":"Hartke","given":"Kevin","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":430213,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grand, J.B.","contributorId":11150,"corporation":false,"usgs":true,"family":"Grand","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":430211,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hepp, Gary R.","contributorId":8191,"corporation":false,"usgs":true,"family":"Hepp","given":"Gary","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":430210,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Folk, T.H.","contributorId":50688,"corporation":false,"usgs":true,"family":"Folk","given":"T.H.","email":"","affiliations":[],"preferred":false,"id":430212,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70030836,"text":"70030836 - 2006 - Mineralogy and arsenic mobility in arsenic-rich Brazilian soils and sediments","interactions":[],"lastModifiedDate":"2012-03-12T17:21:19","indexId":"70030836","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2457,"text":"Journal of Soils and Sediments","active":true,"publicationSubtype":{"id":10}},"title":"Mineralogy and arsenic mobility in arsenic-rich Brazilian soils and sediments","docAbstract":"Background. Soils and sediments in certain mining regions of Brazil contain an unusually large amount of arsenic (As), which raises concerns that mining could promote increased As mobility, and thereby increase the risks of contaminating water supplies. Objectives. The purpose of t his study was to identify the most important factors governing As mobility in sediments and soils near three gold-mining sites in the State of Minas Gerais, Brazil. Methods. Surface and sub-surface soil samples were collected at those sites and characterized by chemical and mineralogical analyses. Oxalate (Feo) and citrate-bicarbonate-dithionite (Fed) iron contents were determined by atomic absorption spectroscopy (AAS). Arsenic mobilization was measured after incubating the samples in a 2.5 mM CaCl2 solution under anaerobic conditions for 1, 28, 56, 84, or 112 days. The solution concentrations of As, Fe, and Mn were then measured by inductively coupled plasma-mass spectrometry (ICP-MS) and AAS, respectively. Results and Discussion. Results indicated that As mobilization is largely independent of both the total As and the Feo/Fed ratio of the solid phase. Soluble As is roughly controlled by the Fe (hydr)oxide content of the soil, but a closer examination of the data revealed the importance of other highly weathered clay minerals and organic matter. Large amounts of organic matter and a low iron oxide content should favor As leaching from soils and sediments. Under reducing conditions, As is mobilized by the reductive dissolution of Fe and/or Mn oxides. However, released As may be readsorbed depending on the sorptive properties of the soil. Gibbsite is particularly effective in adsorbing or readsorbing As, as is the remaining unreduced fraction of the iron (hydr)oxides. Conclusion and Outlook. In general, low soluble As is rel ated to the presence of gibbsite, a large amount of iron oxides, and a lack of organic matter in the solid phase. This has environmental significance because gibbsite is thermodynamically more stable than Fe oxides under anaerobic conditions, such as those found in waterlogged soils and lake sediments. ?? 2006 ecomed publishers (Verlagsgruppe Hu??thig Jehle Rehm GmbH), D-86899 Landsberg and Tokyo.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Soils and Sediments","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1065/jss2005.09.144","issn":"14390108","usgsCitation":"Mello, D., Roy, W.R., Talbott, J., and Stucki, J., 2006, Mineralogy and arsenic mobility in arsenic-rich Brazilian soils and sediments: Journal of Soils and Sediments, v. 6, no. 1, p. 9-19, https://doi.org/10.1065/jss2005.09.144.","startPage":"9","endPage":"19","numberOfPages":"11","costCenters":[],"links":[{"id":211471,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1065/jss2005.09.144"},{"id":238764,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"1","noUsgsAuthors":false,"publicationDate":"2005-09-16","publicationStatus":"PW","scienceBaseUri":"505a5aade4b0c8380cd6f04e","contributors":{"authors":[{"text":"Mello, de","contributorId":72587,"corporation":false,"usgs":true,"family":"Mello","given":"de","email":"","affiliations":[],"preferred":false,"id":428892,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roy, William R.","contributorId":45454,"corporation":false,"usgs":true,"family":"Roy","given":"William","middleInitial":"R.","affiliations":[],"preferred":false,"id":428890,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Talbott, J.L.","contributorId":24472,"corporation":false,"usgs":true,"family":"Talbott","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":428889,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stucki, J.W.","contributorId":61640,"corporation":false,"usgs":true,"family":"Stucki","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":428891,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70030999,"text":"70030999 - 2006 - Sulfate deposition in subsurface regolith in Gusev crater, Mars","interactions":[],"lastModifiedDate":"2018-11-28T09:04:37","indexId":"70030999","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2317,"text":"Journal of Geophysical Research E: Planets","active":true,"publicationSubtype":{"id":10}},"title":"Sulfate deposition in subsurface regolith in Gusev crater, Mars","docAbstract":"<p>Excavating into the shallow Martian subsurface has the potential to expose stratigraphic layers and mature regolith, which may hold a record of more ancient aqueous interactions than those expected under current Martian surface conditions. During the Spirit rover's exploration of Gusev crater, rover wheels were used to dig three trenches into the subsurface regolith down to 6-11 cm depth: Road Cut, the Big Hole, and The Boroughs. A high oxidation state of Fe and high concentrations of Mg, S, Cl, and Br were found in the subsurface regolith within the two trenches on the plains, between the Bonneville crater and the foot of Columbia Hills. Data analyses on the basis of geochemistry and mineralogy observations suggest the deposition of sulfate minerals within the subsurface regolith, mainly Mg-sulfates accompanied by minor Ca-sulfates and perhaps Fe-sulfates. An increase of Fe2O3, an excess of SiO2, and a minor decrease in the olivine proportion relative to surface materials are also inferred. Three hypotheses are proposed to explain the geochemical trends observed in trenches: (1) multiple episodes of acidic fluid infiltration, accompanied by in situ interaction with igneous minerals and salt deposition; (2) an open hydrologic system characterized by ion transportation in the fluid, subsequent evaporation of the fluid, and salt deposition; and (3) emplacement and mixing of impact ejecta of variable composition. While all three may have plausibly contributed to the current state of the subsurface regolith, the geochemical data are most consistent with ion transportation by fluids and salt deposition as a result of open-system hydrologic behavior. Although sulfates make up &gt;20 wt.% of the regolith in the wall of The Boroughs trench, a higher hydrated sulfate than kieserite within The Boroughs or a greater abundance of sulfates elsewhere than is seen in The Boroughs wall regolith would be needed to hold the structural water indicated by the water-equivalent hydrogen concentration observed by the Gamma-Ray Spectrometer on Odyssey in the Gusev region.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research E: Planets","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Geophysical Union","publisherLocation":"Washington, D.C.","doi":"10.1029/2005JE002513","issn":"01480227","usgsCitation":"Wang, A., Haskin, L., Squyres, S.W., Jolliff, B., Crumpler, L., Gellert, R., Schroder, C., Herkenhoff, K.E., Hurowitz, J., Tosca, N., Farrand, W.H., Anderson, R., and Knudson, A., 2006, Sulfate deposition in subsurface regolith in Gusev crater, Mars: Journal of Geophysical Research E: Planets, v. 111, no. E2, 19 p., https://doi.org/10.1029/2005JE002513.","productDescription":"19 p.","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":477418,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2005je002513","text":"Publisher Index Page"},{"id":238641,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Gusev crater; Mars","volume":"111","issue":"E2","noUsgsAuthors":false,"publicationDate":"2006-02-21","publicationStatus":"PW","scienceBaseUri":"505b9dc0e4b08c986b31da54","contributors":{"authors":[{"text":"Wang, A.","contributorId":46735,"corporation":false,"usgs":true,"family":"Wang","given":"A.","email":"","affiliations":[],"preferred":false,"id":429578,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haskin, L.A.","contributorId":74926,"corporation":false,"usgs":true,"family":"Haskin","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":429582,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Squyres, S. W.","contributorId":31836,"corporation":false,"usgs":true,"family":"Squyres","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":429576,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jolliff, B.L.","contributorId":21268,"corporation":false,"usgs":true,"family":"Jolliff","given":"B.L.","email":"","affiliations":[],"preferred":false,"id":429575,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Crumpler, L.","contributorId":59545,"corporation":false,"usgs":true,"family":"Crumpler","given":"L.","email":"","affiliations":[],"preferred":false,"id":429579,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gellert, Ralf","contributorId":35049,"corporation":false,"usgs":false,"family":"Gellert","given":"Ralf","email":"","affiliations":[{"id":12660,"text":"University of Guelph","active":true,"usgs":false}],"preferred":false,"id":429577,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Schroder, C.","contributorId":67201,"corporation":false,"usgs":true,"family":"Schroder","given":"C.","affiliations":[],"preferred":false,"id":429581,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Herkenhoff, Kenneth E. 0000-0002-3153-6663 kherkenhoff@usgs.gov","orcid":"https://orcid.org/0000-0002-3153-6663","contributorId":2275,"corporation":false,"usgs":true,"family":"Herkenhoff","given":"Kenneth","email":"kherkenhoff@usgs.gov","middleInitial":"E.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":429572,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Hurowitz, J.","contributorId":17742,"corporation":false,"usgs":true,"family":"Hurowitz","given":"J.","email":"","affiliations":[],"preferred":false,"id":429574,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Tosca, N.J.","contributorId":17354,"corporation":false,"usgs":true,"family":"Tosca","given":"N.J.","email":"","affiliations":[],"preferred":false,"id":429573,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Farrand, W. H.","contributorId":64372,"corporation":false,"usgs":true,"family":"Farrand","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":429580,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Anderson, R.","contributorId":104191,"corporation":false,"usgs":false,"family":"Anderson","given":"R.","affiliations":[],"preferred":false,"id":429583,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Knudson, A.T.","contributorId":15746,"corporation":false,"usgs":true,"family":"Knudson","given":"A.T.","email":"","affiliations":[],"preferred":false,"id":429571,"contributorType":{"id":1,"text":"Authors"},"rank":13}]}}
,{"id":70031059,"text":"70031059 - 2006 - Trends in the nutrient enrichment of U.S. rivers during the late 20th century and their relation to changes in probable stream trophic conditions","interactions":[],"lastModifiedDate":"2012-03-12T17:21:17","indexId":"70031059","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Trends in the nutrient enrichment of U.S. rivers during the late 20th century and their relation to changes in probable stream trophic conditions","docAbstract":"We estimated trends in concentrations of total phosphorus (TP) and total nitrogen (TN) and the related change in the probabilities of trophic conditions from 1975 to 1994 at 250 nationally representative riverine monitoring locations in the U.S. with drainage areas larger than about 1,000 km2. Statistically significant (p < 0.05) declines were detected in TP and TN concentrations at 44% and 37% of the monitoring sites, and significant increases were detected at 3% and 9% of the sites, respectively. We used a statistical model to assess changes in the probable trophic-state classification of the sites after adjusting for climate-related variability in nutrient concentrations. The probabilistic assessment accounts for current knowledge of the trophic response of streams to nutrient enrichment, based on a recently proposed definition of \"eutrophic,\" \"mesotrophic,\" and \"oligotrophic\" conditions in relation to total nutrient concentrations. Based on these trophic definitions, we found that the trophic state improved at 25% of the monitoring sites and worsened at fewer than 5% of the sites; about 70% of the sites were unchanged. Improvements in trophic-state related to declines in TP were more common in predominantly forested and shrub-grassland watersheds, whereas the trophic state of predominantly agricultural sites was unchanged. Despite the declines in TP concentrations at many sites, about 50% of all monitoring sites, and more than 60% of the sites in predominantly agricultural and urban watersheds, were classified as eutrophic in 1994 based on TP concentrations. Contemporaneous reductions in major nutrient sources to streams, related to wastewater treatment upgrades, phosphate detergent bans, and declines in some agricultural sources, may have contributed to the declines in riverine nutrient concentrations and associated improvements in trophic conditions. ?? 2006, by the American Society of Limnology and Oceanography, Inc.","largerWorkTitle":"Limnology and Oceanography","language":"English","issn":"00243590","usgsCitation":"Alexander, R.B., and Smith, R.A., 2006, Trends in the nutrient enrichment of U.S. rivers during the late 20th century and their relation to changes in probable stream trophic conditions, <i>in</i> Limnology and Oceanography, v. 51, no. 1 II, p. 639-654.","startPage":"639","endPage":"654","numberOfPages":"16","costCenters":[],"links":[{"id":238611,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"51","issue":"1 II","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb812e4b08c986b327669","contributors":{"authors":[{"text":"Alexander, R. B.","contributorId":108103,"corporation":false,"usgs":true,"family":"Alexander","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":429867,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, R. A.","contributorId":60584,"corporation":false,"usgs":true,"family":"Smith","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":429866,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70273211,"text":"70273211 - 2006 - Coastal wetlands of the northern Gulf of California: Inventory and conservation status","interactions":[],"lastModifiedDate":"2025-12-19T15:32:10.082696","indexId":"70273211","displayToPublicDate":"2005-12-22T09:21:01","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":862,"text":"Aquatic Conservation: Marine and Freshwater Ecosystems","active":true,"publicationSubtype":{"id":10}},"title":"Coastal wetlands of the northern Gulf of California: Inventory and conservation status","docAbstract":"<ul class=\"rlist hanging\"><li><span class=\"number\">1.</span><p>Above 28°N, the coastline of the northern Gulf of California is indented at frequent intervals by negative or inverse estuaries that are saltier at their backs than at their mouths due to the lack of freshwater inflow. These ‘esteros’ total over 215 000 ha in area and encompass mangrove marshes below 29°N and saltgrass (<i>Distichlis palmeri</i>) marshes north of 29°N. An additional 6000 ha of freshwater and brackish wetlands are found in the Colorado River delta where fresh water enters the intertidal zone.</p></li><li><span class=\"number\">2.</span><p>The mangrove marshes in the Gulf of California have been afforded some degree of protected status in Mexico, but the northern saltgrass esteros do not have priority conservation status and are increasingly becoming development targets for resorts, vacation homes and aquaculture sites.</p></li><li><span class=\"number\">3.</span><p>We conducted an inventory of the marshes using aerial photography and satellite images, and evaluated the extent and type of development on each marsh. We reviewed the available literature on the marshes to document their vegetation types and ecological functions in the adjacent marine and terrestrial ecosystems.</p></li><li><span class=\"number\">4.</span><p>Over 95% of the mangrove marshes have been developed for shrimp farming. However, the farms are built adjacent to, rather than in, the marshes, and the mangrove stands are still mostly intact.</p></li><li><span class=\"number\">5.</span><p>The majority of saltgrass marshes above the mangrove line are still relatively unspoiled. However, resort and vacation home development is taking place on land surrounding them.</p></li><li><span class=\"number\">6.</span><p>We recommend a system of protected reserves incorporating the pristine wetlands, along with water quality management and buffer zones for the more developed esteros. The saltgrass marshes should be considered for conservation protection, similar to the protection given to the southern mangrove marshes whose value has already been recognized.</p></li></ul>","language":"English","publisher":"Wiley","doi":"10.1002/aqc.681","usgsCitation":"Glenn, E., Nagler, P.L., Brusca, R., and Hinojosa-Huera, O., 2006, Coastal wetlands of the northern Gulf of California: Inventory and conservation status: Aquatic Conservation: Marine and Freshwater Ecosystems, v. 16, no. 1, p. 5-28, https://doi.org/10.1002/aqc.681.","productDescription":"24 p.","startPage":"5","endPage":"28","costCenters":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"links":[{"id":497768,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico","otherGeospatial":"Gulf of California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -115.5196415598833,\n              31.99882167372111\n            ],\n            [\n              -115.5196415598833,\n              26.81863980081141\n            ],\n            [\n              -109.92227879136078,\n              26.81863980081141\n            ],\n            [\n              -109.92227879136078,\n              31.99882167372111\n            ],\n            [\n              -115.5196415598833,\n              31.99882167372111\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"16","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Glenn, Edward P.","contributorId":56542,"corporation":false,"usgs":false,"family":"Glenn","given":"Edward P.","affiliations":[{"id":13060,"text":"Department of Soil, Water and Environmental Science, University of Arizona","active":true,"usgs":false}],"preferred":false,"id":952712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nagler, Pamela L. 0000-0003-0674-103X pnagler@usgs.gov","orcid":"https://orcid.org/0000-0003-0674-103X","contributorId":1398,"corporation":false,"usgs":true,"family":"Nagler","given":"Pamela","email":"pnagler@usgs.gov","middleInitial":"L.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":952713,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brusca, Richard","contributorId":258136,"corporation":false,"usgs":false,"family":"Brusca","given":"Richard","email":"","affiliations":[{"id":52227,"text":"University of Arizona, Tucson, AZ, USA","active":true,"usgs":false}],"preferred":false,"id":952714,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hinojosa-Huera, Osvel","contributorId":339751,"corporation":false,"usgs":false,"family":"Hinojosa-Huera","given":"Osvel","email":"","affiliations":[{"id":24640,"text":"Pronatura Noroeste","active":true,"usgs":false}],"preferred":false,"id":952715,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70175210,"text":"wdrNY053 - 2006 - Water resources data New York water year 2005, volume 3: Western New York","interactions":[],"lastModifiedDate":"2017-04-06T11:03:56","indexId":"wdrNY053","displayToPublicDate":"2005-11-06T09:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NY-05-3","title":"Water resources data New York water year 2005, volume 3: Western New York","docAbstract":"<p>Water resources data for the 2005 water year for Western New York consist of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs; ground-water levels and water quality; and quantity and chemical quality of precipitation. This volume contains records for water discharge at 71 gaging stations; stage only at 15 gaging stations; stage and contents at 6 gaging stations; water quality at 12 gaging stations, 29 wells, and 22 partial-record stations; water levels at 29 observation wells; daily precipitation totals at 1 site, and chemical quality of precipitation at 1 site. Also included are data for 38 crest-stage partial-record stations. Locations of these sites are shown on figure 1. Additional water data were collected at various sites not involved in the systematic data-collection program and are published as measurements made at miscellaneous sites. Surface-water, ground-water, and water-quality data at all sites are listed in Eastern Standard Time (EST), unless otherwise noted. These data together with the data in Volumes 1 and 2 represent that part of the National Water Information System operated by the U.S. Geological Survey and cooperating State, local, and Federal agencies in New York.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNY053","collaboration":"Prepared in cooperation with the State of New York and other agencies","usgsCitation":"Szabo, C.O., Grover, J.S., and McInnes, S., 2006, Water resources data New York water year 2005, volume 3: Western New York: U.S. Geological Survey Water Data Report NY-05-3, Summary: 12 p.; Data: v, 454 p.; Discontinued Sites: 9 p., https://doi.org/10.3133/wdrNY053.","productDescription":"Summary: 12 p.; Data: v, 454 p.; Discontinued Sites: 9 p.","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":474,"text":"New York Water Science 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,{"id":70175130,"text":"wdrNY052 - 2006 - Water Resources Data New York Water Year 2005, Volume 2: Long Island","interactions":[],"lastModifiedDate":"2017-03-30T16:24:35","indexId":"wdrNY052","displayToPublicDate":"2005-11-06T08:45:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NY-05-2","title":"Water Resources Data New York Water Year 2005, Volume 2: Long Island","docAbstract":"<p>Water resources data for the 2005 water year for Long Island New York consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; stage and water quality of estuaries; and water levels and water quality of ground-water wells. This volume contains records for water discharge at 15 gaging stations; lake stage at 7 gaging stations; tide stage at 6 gaging stations; and water levels at 478 observation wells. Also included are data for 10 low-flow partial record stations. Additional water data were collected at various sites not involved in the systematic data-collection program, and are published as miscellaneous measurements and analyses. These data, together with the data in volumes 1 and 3 represent that part of the National Water Data System operated by the U.S. Geological Survey in cooperation with State, Federal, and other agencies in New York.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNY052","collaboration":"Prepared in cooperation with the State of New York and other agencies","usgsCitation":"U.S. Geological Survey, 2006, Water Resources Data New York Water Year 2005, Volume 2: Long Island: U.S. Geological Survey Water Data Report NY-05-2, Summary: 4 p.; Data: 1800 p.; Discontinued Sites: 3 p., https://doi.org/10.3133/wdrNY052.","productDescription":"Summary: 4 p.; Data: 1800 p.; Discontinued Sites: 3 p.","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":474,"text":"New York Water Science 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,{"id":72252,"text":"ofr20051010 - 2006 - Potentiometric surface of the Lower Patapsco Aquifer in southern Maryland, September 2003","interactions":[],"lastModifiedDate":"2023-07-11T21:30:24.21569","indexId":"ofr20051010","displayToPublicDate":"2005-09-19T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1010","title":"Potentiometric surface of the Lower Patapsco Aquifer in southern Maryland, September 2003","docAbstract":"This report presents a map showing the potentiometric surface of the Lower Patapsco aquifer in the Patapsco Formation of Lower Cretaceous age in Southern Maryland during September 2003. The map is based on water-level measurements in 66 wells. The highest measured water level was 112 feet above sea level near the northwestern boundary and outcrop area of the aquifer in northern Prince Georges County. From this area, the potentiometric surface declined towards well fields at Severndale, Arnold, and Annapolis. The measured ground-water levels were 86 feet below sea level at Severndale, 41 feet below sea level at Arnold, and 39 feet below sea level a few miles west of Annapolis. There was also a cone of depression covering a large area in Charles County that includes Waldorf, LaPlata, Indian Head, and the Morgantown powerplant. The ground-water levels measured were as low as 165 feet below sea level at Waldorf, 135 feet below sea level at LaPlata, 114 feet below sea level at Indian Head, and 92 feet below sea level at the Morgantown powerplant.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051010","usgsCitation":"Curtin, S.E., Andreasen, D., and Wheeler, J.C., 2006, Potentiometric surface of the Lower Patapsco Aquifer in southern Maryland, September 2003: U.S. Geological Survey Open-File Report 2005-1010, 1 p., https://doi.org/10.3133/ofr20051010.","productDescription":"1 p.","temporalStart":"2003-09-01","temporalEnd":"2003-09-30","costCenters":[],"links":[{"id":191578,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8914,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1010/","linkFileType":{"id":5,"text":"html"}},{"id":389093,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_78443.htm"}],"country":"United States","state":"Maryland","otherGeospatial":"lower Patapsco aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.2833,\n              38.32657512192453\n            ],\n            [\n              -76.3604736328125,\n              38.32657512192453\n            ],\n            [\n              -76.3604736328125,\n              39.34916646551957\n            ],\n            [\n              -77.2833,\n              39.34916646551957\n            ],\n            [\n              -77.2833,\n              38.32657512192453\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae3cf","contributors":{"authors":[{"text":"Curtin, Stephen E. securtin@usgs.gov","contributorId":3703,"corporation":false,"usgs":true,"family":"Curtin","given":"Stephen","email":"securtin@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285265,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreasen, David C.","contributorId":59003,"corporation":false,"usgs":true,"family":"Andreasen","given":"David C.","affiliations":[],"preferred":false,"id":285267,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wheeler, Judith C.","contributorId":13620,"corporation":false,"usgs":true,"family":"Wheeler","given":"Judith","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":285266,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":71066,"text":"sir20055059 - 2006 - Methods Used to Assess the Susceptibility to Contamination of Transient, Non-Community Public Ground-Water Supplies in Indiana","interactions":[],"lastModifiedDate":"2016-05-09T11:09:16","indexId":"sir20055059","displayToPublicDate":"2005-08-23T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5059","title":"Methods Used to Assess the Susceptibility to Contamination of Transient, Non-Community Public Ground-Water Supplies in Indiana","docAbstract":"<p>The Safe Water Drinking Act of 1974 as amended in 1996 gave each State the responsibility of developing a Source-Water Assessment Plan (SWAP) that is designed to protect public-water supplies from contamination. Each SWAP must include three elements: (1) a delineation of the source-water protection area, (2) an inventory of potential sources of contaminants within the area, and (3) a determination of the susceptibility of the public-water supply to contamination from the inventoried sources. The Indiana Department of Environmental Management (IDEM) was responsible for preparing a SWAP for all public-water supplies in Indiana, including about 2,400 small public ground-water supplies that are designated transient, non-community (TNC) supplies. In cooperation with IDEM, the U.S. Geological Survey compiled information on conditions near the TNC supplies and helped IDEM complete source-water assessments for each TNC supply. The delineation of a source-water protection area (called the assessment area) for each TNC ground-water supply was defined by IDEM as a circular area enclosed by a 300-foot radius centered at the TNC supply well. Contaminants of concern (COCs) were defined by IDEM as any of the 90 contaminants for which the U.S. Environmental Protection Agency has established primary drinking-water standards. Two of these, nitrate as nitrogen and total coliform bacteria, are Indiana State-regulated contaminants for TNC water supplies. IDEM representatives identified potential point and nonpoint sources of COCs within the assessment area, and computer database retrievals were used to identify potential point sources of COCs in the area outside the assessment area. Two types of methods-subjective and subjective hybrid-were used in the SWAP to determine susceptibility to contamination. Subjective methods involve decisions based upon professional judgment, prior experience, and (or) the application of a fundamental understanding of processes without the collection and analysis of data for a specific condition. Subjective hybrid methods combine subjective methods with quantitative hydrologic analyses. The subjective methods included an inventory of potential sources and associated contaminants, and a qualitative description of the inherent susceptibility of the area around the TNC supply. The description relies on a classification of the hydrogeologic and geomorphic characteristics of the general area around the TNC supply in terms of its surficial geology, regional aquifer system, the occurrence of fine- and coarse-grained geologic materials above the screen of the TNC well, and the potential for infiltration of contaminants. The subjective hybrid method combined the results of a logistic regression analysis with a subjective analysis of susceptibility and a subjective set of definitions that classify the thickness of fine-grained geologic materials above the screen of a TNC well in terms of impedance to vertical flow. The logistic regression determined the probability of elevated concentrations of nitrate as nitrogen (greater than or equal to 3 milligrams per liter) in ground water associated with specific thicknesses of fine-grained geologic materials above the screen of a TNC well. In this report, fine-grained geologic materials are referred to as a geologic barrier that generally impedes vertical flow through an aquifer. A geologic barrier was defined to be thin for fine-grained materials between 0 and 45 feet thick, moderate for materials between 45 and 75 feet thick, and thick if the fine-grained materials were greater than 75 feet thick. A flow chart was used to determine the susceptibility rating for each TNC supply. The flow chart indicated a susceptibility rating using (1) concentrations of nitrate as nitrogen and total coliform bacteria reported from routine compliance monitoring of the TNC supply, (2) the presence or absence of potential sources of regulated contaminants (nitrate as nitrogen and coliform bac</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055059","collaboration":"Prepared in cooperation with the Indiana Department of Environmental Management","usgsCitation":"Arihood, L.D., and Cohen, D.A., 2006, Methods Used to Assess the Susceptibility to Contamination of Transient, Non-Community Public Ground-Water Supplies in Indiana: U.S. Geological Survey Scientific Investigations Report 2005-5059, vi, 40 p., https://doi.org/10.3133/sir20055059.","productDescription":"vi, 40 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,{"id":70205401,"text":"70205401 - 2006 - Evidence for intensification of the global water cycle: Review and synthesis","interactions":[],"lastModifiedDate":"2019-09-17T11:30:55","indexId":"70205401","displayToPublicDate":"2005-08-22T11:27:32","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Evidence for intensification of the global water cycle: Review and synthesis","docAbstract":"<p><span>One of the more important questions in&nbsp;hydrology&nbsp;is: if the climate warms in the future, will there be an&nbsp;intensification&nbsp;of the water cycle and, if so, the nature of that intensification? There is considerable interest in this question because an intensification of the water cycle may lead to changes in water-resource availability, an increase in the frequency and intensity of&nbsp;tropical storms, floods, and&nbsp;droughts, and an amplification of warming through the&nbsp;water vapor&nbsp;feedback. Empirical evidence for ongoing intensification of the water cycle would provide additional support for the theoretical framework that links intensification with warming. This paper briefly reviews the current state of science regarding historical trends in hydrologic variables, including precipitation,&nbsp;runoff, tropospheric water vapor, soil moisture,&nbsp;</span>glacier<span>&nbsp;mass balance, evaporation,&nbsp;evapotranspiration, and growing season length. Data are often incomplete in spatial and temporal domains and regional analyses are variable and sometimes contradictory; however, the&nbsp;weight of evidence&nbsp;indicates an ongoing intensification of the water cycle. In contrast to these trends, the empirical evidence to date does not consistently support an increase in the frequency or intensity of tropical storms and floods.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jhydrol.2005.07.003","usgsCitation":"Huntington, T.G., 2006, Evidence for intensification of the global water cycle: Review and synthesis: Journal of Hydrology, v. 319, no. 1-4, p. 83-95, https://doi.org/10.1016/j.jhydrol.2005.07.003.","productDescription":"13 p.","startPage":"83","endPage":"95","costCenters":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"links":[{"id":367479,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"319","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Huntington, Thomas G. 0000-0002-9427-3530 thunting@usgs.gov","orcid":"https://orcid.org/0000-0002-9427-3530","contributorId":1884,"corporation":false,"usgs":true,"family":"Huntington","given":"Thomas","email":"thunting@usgs.gov","middleInitial":"G.","affiliations":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":771056,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70440,"text":"sir20045143 - 2006 - Evaluation of metal loading to streams near Creede, Colorado, August and September 2000","interactions":[],"lastModifiedDate":"2020-01-26T11:13:33","indexId":"sir20045143","displayToPublicDate":"2005-04-22T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-5143","title":"Evaluation of metal loading to streams near Creede, Colorado, August and September 2000","docAbstract":"Decisions about remediation of mine drainage on the watershed scale require an understanding of metal contributions from all sources to be able to choose the best sites for remediation. A hydrologic framework to study metal loading in the Willow Creek watershed, a tributary to the Rio Grande River, was established by conducting a series of tracer-injection studies. Each study used the tracer-dilution method in conjunction with synoptic sampling to determine the spatial distribution of discharge and concentration. Discharge and concentration data were then used to develop mass-loading curves for the metals of interest. The discharge and load profiles (1) identify the principal sources of load to the streams; (2) demonstrate the scale of unsampled, dispersed subsurface inflows; and (3) estimate the amount of natural attenuation. The greatest source of metal loads was from the Nelson Tunnel on West Willow Creek, which contributed 158 kilograms per day of zinc to the stream. Additional loading from other dispersed, subsurface inflows along West Willow Creek added substantial loads, but these were small in comparison to the loads from the Nelson Tunnel. No significant contributions of metal load from potential sources occurred along East Willow Creek. The lack of measurable loading may be a result of previous remedial actions along that stream. The lower Willow Creek section had relatively small contributions of load compared to what had been contributed upstream. This watershed approach provides a detailed snapshot of metal load for the watershed to support remediation decisions and quantifies processes that affect metal transport.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/sir20045143","collaboration":"Prepared in cooperation with the City of Creede, Colorado and the U.S. Forest Service","usgsCitation":"Kimball, B.A., Runkel, R., Walton-Day, K., and Stover, B., 2006, Evaluation of metal loading to streams near Creede, Colorado, August and September 2000 (Online only): U.S. Geological Survey Scientific Investigations Report 2004-5143, viii, 64 p., https://doi.org/10.3133/sir20045143.","productDescription":"viii, 64 p.","numberOfPages":"75","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"2000-08-01","temporalEnd":"2000-09-30","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":185498,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":334251,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2004/5143/PDF/SIR2004_5143.pdf"},{"id":6989,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2004/5143/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado","city":"Creede","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.95,37.81666666666667 ], [ -106.95,37.916666666666664 ], [ -106.9,37.916666666666664 ], [ -106.9,37.81666666666667 ], [ -106.95,37.81666666666667 ] ] ] } } ] }","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fafd5","contributors":{"authors":[{"text":"Kimball, B. A.","contributorId":87583,"corporation":false,"usgs":false,"family":"Kimball","given":"B.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":282437,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Runkel, R.L.","contributorId":97529,"corporation":false,"usgs":true,"family":"Runkel","given":"R.L.","affiliations":[],"preferred":false,"id":282438,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Walton-Day, K.","contributorId":14054,"corporation":false,"usgs":true,"family":"Walton-Day","given":"K.","affiliations":[],"preferred":false,"id":282435,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stover, B.K.","contributorId":67975,"corporation":false,"usgs":true,"family":"Stover","given":"B.K.","email":"","affiliations":[],"preferred":false,"id":282436,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70461,"text":"ds85 - 2006 - The Massachusetts Bay internal wave experiment, August 1998: Data report","interactions":[],"lastModifiedDate":"2023-04-05T18:40:08.869595","indexId":"ds85","displayToPublicDate":"2005-04-22T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85","title":"The Massachusetts Bay internal wave experiment, August 1998: Data report","docAbstract":"<p>This data report presents oceanographic observations made in Massachusetts Bay (fig. 1) in August 1998 as part of the Massachusetts Bay Internal Wave Experiment (MBIWE98). MBIWE98 was carried out to characterize large-amplitude internal waves in Massachusetts Bay and to investigate the possible resuspension and transport of bottom sediments caused by these waves. This data report presents a description of the field program and instrumentation, an overview of the data through summary plots and statistics, and the time-series data in NetCDF format. The objective of this report is to make the data available in digital form and to provide summary plots and statistics to facilitate browsing of the data set.</p>\n<br>\n<p>The existence of large-amplitude internal waves in Massachusetts Bay was first described by Halpern (1971). In summer when the water is stratified, packets of waves propagate westward into the bay on the flood (westward flowing) tide at about 0.5 m/s. The internal waves are observed in packets of 5-10 waves, have periods of 5-10 minutes and wavelengths of 200-400 m, and cause downward excursions of the thermocline of as much as 30 m. The waves are generated by interaction of the barotropic tide with Stellwagen Bank (Haury and others (1979).</p>\n<br>\n<p>Several papers present analyses and interpretations of the data collected during the MBIWE98. Grosenbaugh and others (2002) report on the results of the horizontal array, Scotti and others (2005) describe a strategy for processing observations made by Acoustic Doppler Current Profilers (ADCPs) in the presence of short-wavelength internal waves, Butman and others (in press) describe the effect of these waves on sediment transport, and Scotti and others (in press) describe the energetics of the internal waves.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds85","usgsCitation":"Butman, B., Alexander, P., Anderson, S.P., Lightsom, F.L., Scotti, A., and Beardsley, R.C., 2006, The Massachusetts Bay internal wave experiment, August 1998: Data report (Version 2.0): U.S. Geological Survey Data Series 85, HTML Document; Spatial Data; Meta Data, https://doi.org/10.3133/ds85.","productDescription":"HTML Document; Spatial Data; Meta Data","temporalStart":"1998-08-01","temporalEnd":"1998-08-31","costCenters":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true},{"id":680,"text":"Woods Hole Science Center","active":false,"usgs":true}],"links":[{"id":8592,"rank":5,"type":{"id":23,"text":"Spatial Data"},"url":"https://woodshole.er.usgs.gov/pubs/ds-85/WEBPAGES/dig_data_files.html","linkFileType":{"id":5,"text":"html"}},{"id":8591,"rank":4,"type":{"id":16,"text":"Metadata"},"url":"https://woodshole.er.usgs.gov/pubs/ds-85/WEBPAGES/metadata.html","linkFileType":{"id":5,"text":"html"}},{"id":295183,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://woodshole.er.usgs.gov/pubs/ds-85/WEBPAGES/title_page.html","linkFileType":{"id":5,"text":"html"}},{"id":188600,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds85.PNG"},{"id":8590,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/2006/85/","linkFileType":{"id":5,"text":"html"}},{"id":415269,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_77664.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Massachusetts","otherGeospatial":"Massachusetts Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -70.8333,\n              42.75\n            ],\n            [\n              -70.8333,\n              42.0833\n            ],\n            [\n              -70,\n              42.0833\n            ],\n            [\n              -70,\n              42.75\n            ],\n            [\n              -70.8333,\n              42.75\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","edition":"Version 2.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67aeca","contributors":{"authors":[{"text":"Butman, Bradford 0000-0002-4174-2073 bbutman@usgs.gov","orcid":"https://orcid.org/0000-0002-4174-2073","contributorId":943,"corporation":false,"usgs":true,"family":"Butman","given":"Bradford","email":"bbutman@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":282479,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alexander, P. Soupy sdalyander@usgs.gov","contributorId":82780,"corporation":false,"usgs":true,"family":"Alexander","given":"P. Soupy","email":"sdalyander@usgs.gov","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":282482,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Anderson, Steven P.","contributorId":95148,"corporation":false,"usgs":true,"family":"Anderson","given":"Steven","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":282484,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lightsom, Frances L. 0000-0003-4043-3639 flightsom@usgs.gov","orcid":"https://orcid.org/0000-0003-4043-3639","contributorId":1535,"corporation":false,"usgs":true,"family":"Lightsom","given":"Frances","email":"flightsom@usgs.gov","middleInitial":"L.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":282480,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Scotti, Alberto","contributorId":86852,"corporation":false,"usgs":true,"family":"Scotti","given":"Alberto","email":"","affiliations":[],"preferred":false,"id":282483,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Beardsley, Robert C.","contributorId":8560,"corporation":false,"usgs":false,"family":"Beardsley","given":"Robert","email":"","middleInitial":"C.","affiliations":[{"id":6706,"text":"Woods Hole Oceanographic Institution,","active":true,"usgs":false}],"preferred":false,"id":282481,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70206631,"text":"ofr20051066 - 2006 - Project PROBE Leg I - Report and archive of multibeam bathymetry and acoustic backscatter , CTD/XBT and GPS navigation data collected during USGS Cruise 02051 (NOAA Cruise RB0208) Puerto Rico Trench September 24, 2002 to September 30, 2002","interactions":[],"lastModifiedDate":"2024-05-09T20:13:39.083002","indexId":"ofr20051066","displayToPublicDate":"2005-01-01T09:28:39","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1066","title":"Project PROBE Leg I - Report and archive of multibeam bathymetry and acoustic backscatter , CTD/XBT and GPS navigation data collected during USGS Cruise 02051 (NOAA Cruise RB0208) Puerto Rico Trench September 24, 2002 to September 30, 2002","docAbstract":"<p>On September 24-30, 2002, six days of scientific surveying to map a section of the Puerto Rico Trench (PRT) took place aboard the National Oceanic and Atmospheric Administration (NOAA) ship Ron Brown. The cruise was funded by NOAA's Office of Ocean Exploration. Multibeam bathymetry and acoustic-backscatter data were collected over an area of about 25,000 sq. km of the Puerto Rico trench and its vicinity at water depths of 4000-8400 m. Weather conditions during the entire survey were good; there were light to moderate winds and 1-2 foot swells experiencing minor chop. The roll and pitch of the ship's interaction with the ocean were not conspicuous. Cruise participants included personnel from USGS, NOAA, and University of New Hampshire Center for Coastal and Ocean Mapping/Joint Hydrographic Center. The cruise resulted in the discovery of a major active strike-slip fault system close to the trench, submarine slides on the descending North American tectonic plate, and an extinct mud volcano, which was cut by the strike-slip fault system. Another strike-slip fault system closer to Puerto Rico that was previously considered to accommodate much of the relative plate motion appears to be inactive. The seaward continuation of the Mona Rift, a zone of extension between Puerto Rico and the Dominican Republic that generated a devastating tsunami in 1918, was mapped for the first time.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051066","usgsCitation":"ten Brink, U., Worley, C.R., Smith, S., Stepka, T., and Williams, G.F., 2006, Project PROBE Leg I - Report and archive of multibeam bathymetry and acoustic backscatter , CTD/XBT and GPS navigation data collected during USGS Cruise 02051 (NOAA Cruise RB0208) Puerto Rico Trench September 24, 2002 to September 30, 2002: U.S. Geological Survey Open-File Report 2005-1066, HTML document, https://doi.org/10.3133/ofr20051066.","productDescription":"HTML document","temporalStart":"2002-09-24","temporalEnd":"2002-09-30","costCenters":[{"id":680,"text":"Woods Hole Science Center","active":false,"usgs":true}],"links":[{"id":369195,"rank":4,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2005/1066/htmldocs/meta.htm","linkFileType":{"id":5,"text":"html"}},{"id":369194,"rank":3,"type":{"id":23,"text":"Spatial Data"},"url":"https://pubs.usgs.gov/of/2005/1066/htmldocs/cruisedata.htm","linkFileType":{"id":5,"text":"html"}},{"id":369192,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2005/1066/coverthb.jpg"},{"id":369193,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1066/index.htm","linkFileType":{"id":5,"text":"html"}}],"state":"Puerto Rico","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -67.75,\n              18.9\n            ],\n            [\n              -65.5,\n              18.9\n            ],\n            [\n              -65.5,\n              20.25\n            ],\n            [\n              -67.75,\n              20.25\n            ],\n            [\n              -67.75,\n              18.9\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://pubs.usgs.gov/contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"ten Brink, Uri S. 0000-0001-6858-3001 utenbrink@usgs.gov","orcid":"https://orcid.org/0000-0001-6858-3001","contributorId":127560,"corporation":false,"usgs":true,"family":"ten Brink","given":"Uri S.","email":"utenbrink@usgs.gov","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":775267,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Worley, Charles R. cworley@usgs.gov","contributorId":3063,"corporation":false,"usgs":true,"family":"Worley","given":"Charles","email":"cworley@usgs.gov","middleInitial":"R.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":775268,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, Shep","contributorId":77624,"corporation":false,"usgs":true,"family":"Smith","given":"Shep","email":"","affiliations":[],"preferred":false,"id":775269,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stepka, Thomas","contributorId":84862,"corporation":false,"usgs":true,"family":"Stepka","given":"Thomas","email":"","affiliations":[],"preferred":false,"id":775270,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Williams, Glynn F.","contributorId":83618,"corporation":false,"usgs":true,"family":"Williams","given":"Glynn","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":775271,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":50694,"text":"ofr02372 - 2006 - Physical properties of Long Island Sound sediment cores","interactions":[],"lastModifiedDate":"2023-05-03T19:37:45.368535","indexId":"ofr02372","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-372","title":"Physical properties of Long Island Sound sediment cores","docAbstract":"<p><span>This report presents data on x-radiography, water content, and sediment texture from sediment cores collected in 1996 in Long Island Sound, offshore of Connecticut and New York (Figure 1). Core locations and analytical data are presented in both graphical and numerical form. The physical properties data presented here are a subset of a larger dataset consisting of results from these cores and other sediment samples. (See&nbsp;</span>Poppe and others<span>&nbsp;(1998) and&nbsp;</span>Mecray and others<span>&nbsp;(2000) for samples collected in Long Island Sound from 1996-2001 by the USGS</span><span>.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02372","usgsCitation":"Moore, J., Galvin Gutierrez, E., Mecray, E.L., and Buchholtz ten Brink, M.R., 2006, Physical properties of Long Island Sound sediment cores: U.S. Geological Survey Open-File Report 2002-372, HTML Document, https://doi.org/10.3133/ofr02372.","productDescription":"HTML Document","onlineOnly":"Y","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":176451,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":416673,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_76217.htm","linkFileType":{"id":5,"text":"html"}},{"id":4168,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/of02-372/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","otherGeospatial":"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              -73.85009765625,\n              40.78054143186033\n            ],\n            [\n              -71.641845703125,\n              40.78054143186033\n            ],\n            [\n              -71.641845703125,\n              41.40153558289846\n            ],\n            [\n              -73.85009765625,\n              41.40153558289846\n            ],\n            [\n              -73.85009765625,\n              40.78054143186033\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685b05","contributors":{"authors":[{"text":"Moore, Joel","contributorId":49034,"corporation":false,"usgs":false,"family":"Moore","given":"Joel","affiliations":[],"preferred":false,"id":242093,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Galvin Gutierrez, Erin","contributorId":78007,"corporation":false,"usgs":true,"family":"Galvin Gutierrez","given":"Erin","email":"","affiliations":[],"preferred":false,"id":242095,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mecray, Ellen L.","contributorId":50887,"corporation":false,"usgs":true,"family":"Mecray","given":"Ellen","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":242094,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Buchholtz ten Brink, Marilyn R.","contributorId":88021,"corporation":false,"usgs":true,"family":"Buchholtz ten Brink","given":"Marilyn","email":"","middleInitial":"R.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":242096,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":4910,"text":"twri09A4 - 2006 - Chapter A4. Collection of water samples","interactions":[],"lastModifiedDate":"2019-05-28T11:18:13","indexId":"twri09A4","displayToPublicDate":"1999-12-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"09-A4","displayTitle":"Chapter A4. Collection of Water Samples","title":"Chapter A4. Collection of water samples","docAbstract":"<p>The National Field Manual for the Collection of Water-Quality Data (National Field Manual) describes protocols and provides guidelines for U.S. Geological Survey (USGS) personnel who collect data that are used to assess the quality of the Nation's surface-water and ground-water resources. This chapter addresses preparations and appropriate methods for the collection of surface-water, groundwater, and associated quality-control samples. Among the topics covered are considerations and procedures to prevent sample contamination; establishing site files; instructions for collecting depth-integrated isokinetic and nonisokinetic samples at flowing- and still-water sites; and guidelines for collecting formation water from wells having various types of construction and hydraulic and aquifer characteristics. Each chapter of the National Field Manual is published separately and revised periodically. Newly published and revised chapters will be announced on the USGS Home Page on the World Wide Web under 'New Publications of the U.S. Geological Survey.'</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"National Field Manual for the Collection of Water-Quality Data. U.S. Geological Survey Techniques of Water-Resources Investigations, Book 9","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/twri09A4","usgsCitation":"U.S. Geological Survey, 2006, Chapter A4. Collection of water samples (Version 2.0, Revised September 2006 (original version published September 1999)): U.S. Geological Survey Techniques of Water-Resources Investigations 09-A4, 166 p., https://doi.org/10.3133/twri09A4.","productDescription":"166 p.","numberOfPages":"231","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":139832,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/twri/twri9a4/coverthb.jpg"},{"id":363708,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/tm9A0","text":"Techniques and Methods 9-A0","linkHelpText":"- General introduction for the “National Field Manual for the Collection of Water-Quality Data”"},{"id":653,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/twri/twri9a4/twri9a4_Chap4_v2.pdf","text":"Report - September 2006","size":"5.27 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"- Version 2"},{"id":362110,"rank":3,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://pubs.usgs.gov/twri/twri9a4/twri9a4_chapter4.pdf","text":"Report - September 1999","size":"2.05 mB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"- Original"}],"edition":"Version 2.0, Revised September 2006 (original version published September 1999)","contact":"<p><a href=\"https://www.usgs.gov/mission-areas/water-resources?qt-mission_areas_l2_landing_page_ta=0#qt-mission_areas_l2_landing_page_ta\" data-mce-href=\"https://www.usgs.gov/mission-areas/water-resources?qt-mission_areas_l2_landing_page_ta=0#qt-mission_areas_l2_landing_page_ta\">Water Mission Area</a><br>U.S. Geological Survey<br>12201 Sunrise Valley Drive<br>Reston, VA 20192</p><p>Email: <a href=\"mailto:nfm@usgs.gov\" data-mce-href=\"mailto:nfm@usgs.gov\">nfm@usgs.gov</a></p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>A4. Collection of Water Samples</li><li>Conversion factors, selected terms, and abbreviations</li><li>Selected references and documents</li><li>Appendix A4-A. Transit rate and volume guidelines and filling times for isokinetic samplers</li><li>Appendix A4-B. Instructions related to measuring water levels at wells and a sample USGS ground-water-quality field form</li><li>A4B-1. Establishing a permanent measuring point on wells at which water level will be measured</li><li>A4-B-2. Well-depth measurement</li><li>A4-B-3. Water-level measurement by: Steel Tape and Electrical Tape</li><li>A4-B-4. Water-level measurement by the air-line method</li><li>A4-B-5. Water-level measurement at flowing wells using ow-pressure and high-pressure methods</li><li>A4-B-6. Sample of the U.S. Geological Survey Ground-Water Quality Notes field form</li><li>Appendix A4-C. Quality-control samples collected by field personnel for water-quality studies</li><li>Appendix A4-D. Examples from the National Water-Quality Assessment Program related to protocols for collecting</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691a2b","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":202815,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":759396,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":79771,"text":"mineral2006 - 2006 - Mineral Commodity Summaries 2006","interactions":[],"lastModifiedDate":"2013-02-04T10:58:10","indexId":"mineral2006","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":323,"text":"Mineral Commodity Summaries","code":"MCS","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006","title":"Mineral Commodity Summaries 2006","docAbstract":"Published on an annual basis, this report is the earliest Government publication to furnish estimates covering nonfuel mineral industry data. Data sheets contain information on the domestic industry structure, Government programs, tariffs, and 5-year salient statistics for over 90 individual minerals and materials.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/mineral2006","usgsCitation":"Mineral Commodity Summaries 2006; 2006; MINERAL; 2006; U.S. Geological Survey","productDescription":"202 p; 4 Appendixes (6 p.); Individual Commodity Data Sheets; Available Online, Printed, and on CD-ROM","additionalOnlineFiles":"Y","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":9455,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://minerals.usgs.gov/minerals/pubs/mcs/2006/mcs2006.pdf","size":"2550","linkFileType":{"id":1,"text":"pdf"}},{"id":194969,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mineral_2006.jpg"},{"id":9454,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://minerals.usgs.gov/minerals/pubs/mcs/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db63575a","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534854,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70121225,"text":"70121225 - No Year - Constraining rates and trends of historical wetland loss, Mississippi River Delta Plain, south-central Louisiana","interactions":[],"lastModifiedDate":"2019-06-03T15:01:17","indexId":"70121225","displayToPublicDate":"2006-01-01T10:11:00","publicationYear":"2006","noYear":true,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Constraining rates and trends of historical wetland loss, Mississippi River Delta Plain, south-central Louisiana","docAbstract":"<p>The timing, magnitude, and rate of wetland loss were described for five wetland-loss \nhotspots in the Terrebonne Basin of the Mississippi River delta plain. Land and water areas \nwere mapped for 34 dates between 1956 and 2004 from historical National Wetlands \nInventory (NWI) datasets, aerial photographs, and Landsat Thematic Mapper (TM) satellite \nimages. Since 1956, the emergent land area at the five study areas in south-central Louisiana \nhas decreased by about 50%. Comparison of the water-area curve derived from the 29 TM \nimages with water-level records from the nearby Grand Isle, Louisiana tide gauge (NOS \n#8761724) clearly shows that changes in land and water areas fluctuate in response to \nvariations in regional water levels. The magnitude of water-area fluctuations decreased from \nthe 1980s to the 1990s as former areas of wet marsh within and immediately adjacent to the \nwetland-loss hotspots became permanently submerged. The most rapid wetland loss \noccurred during the late 1960s and 1970s. Peak wetland-loss rates during this period were \ntwo to four times greater than both the pre-1970s background rates and the most recent \nwetland-loss rates. These results provide constraints on predicting future delta-plain wetland \nlosses and identify Landsat TM imagery as an important source for analyzing land- and \nwater-area changes across the entire delta plain. </p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Coastal environment and water quality: proceedings of the AIH 25th Anniversary Meeting & International Conference \"Challenges in Coastal Hyrology and Water Quality\"","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"Water Resource Publications","publisherLocation":"Highlands Ranch, CO","usgsCitation":"Bernier, J., Morton, R., and Barras, J., 2006, Constraining rates and trends of historical wetland loss, Mississippi River Delta Plain, south-central Louisiana, <i>in</i> Coastal environment and water quality: proceedings of the AIH 25th Anniversary Meeting & International Conference \"Challenges in Coastal Hyrology and Water Quality\", p. 371-382.","productDescription":"12 p.","startPage":"371","endPage":"382","numberOfPages":"12","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":292614,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":292613,"type":{"id":15,"text":"Index Page"},"url":"https://coastal.er.usgs.gov/gc-subsidence/historical-wetland-loss.html"}],"country":"United States","state":"Louisiana","otherGeospatial":"Mississippi River Delta Plain","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -91.25,29.0 ], [ -91.25,29.5 ], [ -89.75,29.5 ], [ -89.75,29.0 ], [ -91.25,29.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f5b64ce4b09d12e0e8e673","contributors":{"authors":[{"text":"Bernier, Julie 0000-0002-9918-5353 jbernier@usgs.gov","orcid":"https://orcid.org/0000-0002-9918-5353","contributorId":3549,"corporation":false,"usgs":true,"family":"Bernier","given":"Julie","email":"jbernier@usgs.gov","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":498825,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morton, Robert A.","contributorId":88333,"corporation":false,"usgs":true,"family":"Morton","given":"Robert A.","affiliations":[],"preferred":false,"id":498826,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barras, John A. jbarras@usgs.gov","contributorId":2425,"corporation":false,"usgs":true,"family":"Barras","given":"John A.","email":"jbarras@usgs.gov","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":false,"id":498824,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":74213,"text":"fs20053135 - 2005 - The U.S. Geological Survey Hydrologic Benchmark Network","interactions":[],"lastModifiedDate":"2021-04-28T12:18:57.548163","indexId":"fs20053135","displayToPublicDate":"2021-04-27T14:30:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-3135","title":"The U.S. Geological Survey Hydrologic Benchmark Network","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs20053135","usgsCitation":"Murdoch, P.S., McHale, M.R., Mast, M.A., and Clow, D.W., 2005, The U.S. Geological Survey Hydrologic Benchmark Network: U.S. Geological Survey Fact Sheet 2005-3135, 5 p., https://doi.org/10.3133/fs20053135.","productDescription":"5 p.","costCenters":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true},{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":120999,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2005/3135/report-thumb.jpg"},{"id":91188,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2005/3135/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db6732df","contributors":{"authors":[{"text":"Murdoch, Peter S. 0000-0001-9243-505X pmurdoch@usgs.gov","orcid":"https://orcid.org/0000-0001-9243-505X","contributorId":2453,"corporation":false,"usgs":true,"family":"Murdoch","given":"Peter","email":"pmurdoch@usgs.gov","middleInitial":"S.","affiliations":[{"id":5067,"text":"Northeast Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":286575,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McHale, Michael R. 0000-0003-3780-1816 mmchale@usgs.gov","orcid":"https://orcid.org/0000-0003-3780-1816","contributorId":1735,"corporation":false,"usgs":true,"family":"McHale","given":"Michael","email":"mmchale@usgs.gov","middleInitial":"R.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":286574,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mast, M. Alisa 0000-0001-6253-8162 mamast@usgs.gov","orcid":"https://orcid.org/0000-0001-6253-8162","contributorId":827,"corporation":false,"usgs":true,"family":"Mast","given":"M.","email":"mamast@usgs.gov","middleInitial":"Alisa","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":286572,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Clow, David W. 0000-0001-6183-4824 dwclow@usgs.gov","orcid":"https://orcid.org/0000-0001-6183-4824","contributorId":1671,"corporation":false,"usgs":true,"family":"Clow","given":"David","email":"dwclow@usgs.gov","middleInitial":"W.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":286573,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":74773,"text":"ofr20051384 - 2005 - Concentrations of Insecticides in Selected Surface Water Bodies in Suffolk County, New York, Before and After Mosquito Spraying, 2002-04","interactions":[],"lastModifiedDate":"2021-04-28T12:19:51.10342","indexId":"ofr20051384","displayToPublicDate":"2021-04-27T13:45:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1384","displayTitle":"Concentrations of Insecticides in Selected Surface Water Bodies in Suffolk County, New York, Before and After Mosquito Spraying, 2002-04","title":"Concentrations of Insecticides in Selected Surface Water Bodies in Suffolk County, New York, Before and After Mosquito Spraying, 2002-04","docAbstract":"<p>Concentrations of insecticides sprayed from truck or helicopter onto selected surface-water bodies in Suffolk County, N.Y., during the summers of 2002-04 decreased to below detection limits within 4 days after application. The U.S. Geological Survey (USGS), in cooperation with Suffolk County Department of Health Services (SCDHS), sampled surface waters from selected wetlands for insecticides that were sprayed seasonally from a truck or helicopter as part of the county’s West Nile Virus vector-control program. A total of 72 samples were collected from 27 sites and analyzed for 6 compunds—malathion, methoprene, methoprene acid, piperonyl butoxide (PBO), resmethrin, and sumithrin—that are typically used to help control mosquitoes. PBO was the most frequently detected analyte (33.3%), followed by resmethrin (11.1%), methoprene (9.7%), and methoprene acid (2.4%). Sumithrin and malathion were not applied and were not detected in any of the samples. Maximum recorded concentration of compounds in surface water were: PBO (59,800 ng/L), methoprene (9,030 ng/L), methoprene acid (1,710 ng/L), and resmethrin (293 ng/L). PBO and resmethrin were detected more often in samples when the compounds were applied by a helicopter rather than a truck. This report describes the 27 sampled locations, the sampling methods, and presents the initial results of the study. Detail is provided about concentrations of the applied compounds with respect to time as well as comparisons between the two application processes (truck versus helicopter). All data collected are presented in a table.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20051384","collaboration":"Prepared in cooperation with the Suffolk County Department of Health Services","usgsCitation":"Abbene, I.J., Fisher, S.C., and Terracciano, S.A., 2005, Concentrations of Insecticides in Selected Surface Water Bodies in Suffolk County, New York, Before and After Mosquito Spraying, 2002-04: U.S. Geological Survey Open-File Report 2005-1384, iv, 14 p., https://doi.org/10.3133/ofr20051384.","productDescription":"iv, 14 p.","numberOfPages":"14","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":193326,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2005/1384/coverthb.jpg"},{"id":7602,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2005/1384/ofr20051384.pdf","text":"Report","size":"2.03 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2005-1384"}],"country":"United States","state":"New York","county":"Suffolk County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.4490966796875,\n              40.68063802521456\n            ],\n            [\n              -71.6912841796875,\n              40.68063802521456\n            ],\n            [\n              -71.6912841796875,\n              41.12902134749507\n            ],\n            [\n              -73.4490966796875,\n              41.12902134749507\n            ],\n            [\n              -73.4490966796875,\n              40.68063802521456\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"mailto:dc_ny@usgs.gov\" data-mce-href=\"mailto:dc_ny@usgs.gov\">Director</a>, <a href=\"https://www.usgs.gov/centers/ny-water\" data-mce-href=\"https://www.usgs.gov/centers/ny-water\">New York Water Science Center</a><br>U.S. Geological Survey<br>425 Jordan Road<br>Troy, NY 12180–8349</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Approach and Methods</li><li>Pesticide Concentrations Before and After the Spray Applications</li><li>Summary</li><li>References Cited</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635fef","contributors":{"authors":[{"text":"Abbene, Irene J.","contributorId":63492,"corporation":false,"usgs":true,"family":"Abbene","given":"Irene","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":286717,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fisher, Shawn C. 0000-0001-6324-1061 scfisher@usgs.gov","orcid":"https://orcid.org/0000-0001-6324-1061","contributorId":4843,"corporation":false,"usgs":true,"family":"Fisher","given":"Shawn","email":"scfisher@usgs.gov","middleInitial":"C.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":286716,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Terracciano, Stephen A. saterrac@usgs.gov","contributorId":1076,"corporation":false,"usgs":true,"family":"Terracciano","given":"Stephen","email":"saterrac@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":286715,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":71045,"text":"sir20055083 - 2005 - Development of an approach for integrating components of the U.S. Geological Survey Biomonitoring of Environmental Status and Trends (BEST) and National Stream Quantity Accounting Network (NASQAN) programs for large U.S. rivers","interactions":[],"lastModifiedDate":"2020-07-03T15:57:43.122233","indexId":"sir20055083","displayToPublicDate":"2020-07-01T12:30:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5083","displayTitle":"Development of an Approach for Integrating Components of the U.S. Geological Survey Biomonitoring of Environmental Status and Trends (BEST) and National Stream Quantity Accounting Network (NASQAN) Programs for Large U.S. Rivers","title":"Development of an approach for integrating components of the U.S. Geological Survey Biomonitoring of Environmental Status and Trends (BEST) and National Stream Quantity Accounting Network (NASQAN) programs for large U.S. rivers","docAbstract":"<p>A national-scale framework for monitoring environmental contaminants in fish and effects of contaminant exposure on fish in large U.S. rivers has been proposed by the Biomonitoring of Environmental Status and Trends (BEST) Program of the U.S. Geological Survey (USGS). The framework shares many features and objectives with the USGS National Stream Quantity Accounting Network (NASQAN) Program, which monitors water quality in large U.S. river basins–those with drainage areas of 250,000 to 1,200,000 square miles at their most downstream stations. Because the two programs appear to be complementary, this study was initiated in 2001 to investigate alternative techniques for summarizing and integrating the water-quality data with the fish-contaminant and fish-health data, and to provide recommendations to the BEST program for future integrated studies.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055083","usgsCitation":"Bauch, N.J., Schmitt, C.J., and Crawford, C.G., 2005, Development of an approach for integrating components of the U.S. Geological Survey Biomonitoring of Environmental Status and Trends (BEST) and National Stream Quantity Accounting Network (NASQAN) programs for large U.S. rivers: U.S. Geological Survey, Columbia Environmental Research Center, Columbia, Mo., Scientific Investigations Report 2005&mdash;5083, 53 p., https://doi.org/10.3133/sir20055083.","productDescription":"vi, 53 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PSC"},"publishedDate":"2005-08-20","noUsgsAuthors":false,"publicationDate":"2005-08-20","publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65dfe2","contributors":{"authors":[{"text":"Bauch, Nancy J. 0000-0002-0302-2892 njbauch@usgs.gov","orcid":"https://orcid.org/0000-0002-0302-2892","contributorId":1297,"corporation":false,"usgs":true,"family":"Bauch","given":"Nancy","email":"njbauch@usgs.gov","middleInitial":"J.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":true,"id":283543,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schmitt, Christopher J. 0000-0001-6804-2360 cjschmitt@usgs.gov","orcid":"https://orcid.org/0000-0001-6804-2360","contributorId":491,"corporation":false,"usgs":true,"family":"Schmitt","given":"Christopher","email":"cjschmitt@usgs.gov","middleInitial":"J.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":283541,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crawford, Charles G. 0000-0003-1653-7841 cgcrawfo@usgs.gov","orcid":"https://orcid.org/0000-0003-1653-7841","contributorId":1064,"corporation":false,"usgs":true,"family":"Crawford","given":"Charles","email":"cgcrawfo@usgs.gov","middleInitial":"G.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":true,"id":283542,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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