{"pageNumber":"856","pageRowStart":"21375","pageSize":"25","recordCount":68934,"records":[{"id":70032309,"text":"70032309 - 2009 - Copper isotope fractionation in acid mine drainage","interactions":[],"lastModifiedDate":"2018-11-02T08:53:19","indexId":"70032309","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Copper isotope fractionation in acid mine drainage","docAbstract":"<p><span>We measured the Cu isotopic composition of primary minerals and stream water affected by acid mine drainage in a mineralized watershed (Colorado, USA). The δ</span><sup>65</sup><span>Cu values (based on&nbsp;</span><sup>65</sup><span>Cu/</span><sup>63</sup><span>Cu) of enargite (δ</span><sup>65</sup><span>Cu</span><span>&nbsp;</span><span>=</span><span>&nbsp;</span><span>−0.01</span><span>&nbsp;</span><span>±</span><span>&nbsp;</span><span>0.10‰; 2</span><i>σ</i><span>) and chalcopyrite (δ</span><sup>65</sup><span>Cu</span><span>&nbsp;</span><span>=</span><span>&nbsp;</span><span>0.16</span><span>&nbsp;</span><span>±</span><span>&nbsp;</span><span>0.10‰) are within the range of reported values for terrestrial primary Cu sulfides (−1‰</span><span>&nbsp;</span><span>&lt;</span><span>&nbsp;</span><span>δ</span><sup>65</sup><span>Cu</span><span>&nbsp;</span><span>&lt;</span><span>&nbsp;</span><span>1‰). These mineral samples show lower δ</span><sup>65</sup><span>Cu values than stream waters (1.38‰</span><span>&nbsp;</span><span>⩽</span><span>&nbsp;</span><span>δ</span><sup>65</sup><span>Cu</span><span>&nbsp;</span><span>⩽</span><span>&nbsp;</span><span>1.69‰). The average isotopic fractionation (Δ</span><sub>aq-min</sub><span>&nbsp;</span><span>=</span><span>&nbsp;</span><span>δ</span><sup>65</sup><span>Cu</span><sub>aq</sub><span>&nbsp;</span><span>−</span><span>&nbsp;</span><span>δ</span><sup>65</sup><span>Cu</span><sub>min</sub><span>, where the latter is measured on mineral samples from the field system), equals 1.43</span><span>&nbsp;</span><span>±</span><span>&nbsp;</span><span>0.14‰ and 1.60</span><span>&nbsp;</span><span>±</span><span>&nbsp;</span><span>0.14‰ for chalcopyrite and enargite, respectively. To interpret this field survey, we leached chalcopyrite and enargite in batch experiments and found that, as in the field, the leachate is enriched in&nbsp;</span><sup>65</sup><span>Cu relative to chalcopyrite (1.37</span><span>&nbsp;</span><span>±</span><span>&nbsp;</span><span>0.14‰) and enargite (0.98</span><span>&nbsp;</span><span>±</span><span>&nbsp;</span><span>0.14‰) when microorganisms are absent. Leaching of minerals in the presence of&nbsp;</span><i>Acidithiobacillus ferrooxidans</i><span>&nbsp;results in smaller average fractionation in the opposite direction for chalcopyrite (</span><span class=\"math\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mrow is=&quot;true&quot;><msub is=&quot;true&quot;><mrow is=&quot;true&quot;><mi mathvariant=&quot;normal&quot; is=&quot;true&quot;>&amp;#x394;</mi></mrow><mrow is=&quot;true&quot;><msup is=&quot;true&quot;><mrow is=&quot;true&quot;><mtext is=&quot;true&quot;>aq-min</mtext></mrow><mrow is=&quot;true&quot;><mtext is=&quot;true&quot;>o</mtext></mrow></msup></mrow></msub><mo is=&quot;true&quot;>=</mo><mo is=&quot;true&quot;>-</mo><mn is=&quot;true&quot;>0.57</mn><mo is=&quot;true&quot;>&amp;#xB1;</mo><mn is=&quot;true&quot;>0.14</mn><mi is=&quot;true&quot;>&amp;#x2030;</mi></mrow></math>\">‰<span class=\"MJX_Assistive_MathML\">Δaq-mino=-0.57±0.14‰</span></span></span><span>, where min</span><sup>o</sup><span>&nbsp;refers to the starting mineral) and no apparent fractionation for enargite (</span><span class=\"math\"><span id=\"MathJax-Element-2-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mrow is=&quot;true&quot;><msub is=&quot;true&quot;><mrow is=&quot;true&quot;><mi mathvariant=&quot;normal&quot; is=&quot;true&quot;>&amp;#x394;</mi></mrow><mrow is=&quot;true&quot;><msup is=&quot;true&quot;><mrow is=&quot;true&quot;><mtext is=&quot;true&quot;>aq-min</mtext></mrow><mrow is=&quot;true&quot;><mtext is=&quot;true&quot;>o</mtext></mrow></msup></mrow></msub><mo is=&quot;true&quot;>=</mo><mn is=&quot;true&quot;>0.14</mn><mo is=&quot;true&quot;>&amp;#xB1;</mo><mn is=&quot;true&quot;>0.14</mn><mi is=&quot;true&quot;>&amp;#x2030;</mi></mrow></math>\">‰<span class=\"MJX_Assistive_MathML\">Δaq-mino=0.14±0.14‰</span></span></span><span>). Abiotic fractionation is attributed to preferential oxidation of&nbsp;</span><sup>65</sup><span>Cu</span><sup>+</sup><span>at the interface of the isotopically homogeneous mineral and the surface oxidized layer, followed by solubilization. When microorganisms are present, the abiotic fractionation is most likely not seen due to preferential association of&nbsp;</span><sup>65</sup><span>Cu</span><sub>aq</sub><span>&nbsp;with&nbsp;</span><i>A. ferrooxidans</i><span>&nbsp;cells and related precipitates. In the biotic experiments, Cu was observed under TEM to occur in precipitates around bacteria and in intracellular polyphosphate granules. Thus, the values of δ</span><sup>65</sup><span>Cu in the field and laboratory systems are presumably determined by the balance of Cu released abiotically and Cu that interacts with cells and related precipitates. Such isotopic signatures resulting from Cu sulfide dissolution should be useful for acid mine drainage remediation and ore prospecting purposes.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.gca.2008.11.035","issn":"00167","usgsCitation":"Kimball, B., Mathur, R., Dohnalkova, A., Wall, A., Runkel, R., and Brantley, S., 2009, Copper isotope fractionation in acid mine drainage: Geochimica et Cosmochimica Acta, v. 73, no. 5, p. 1247-1263, https://doi.org/10.1016/j.gca.2008.11.035.","productDescription":"17 p.","startPage":"1247","endPage":"1263","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":242377,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":214635,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.gca.2008.11.035"}],"volume":"73","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fbfde4b0c8380cd4e07a","contributors":{"authors":[{"text":"Kimball, B.E.","contributorId":9479,"corporation":false,"usgs":true,"family":"Kimball","given":"B.E.","email":"","affiliations":[],"preferred":false,"id":435532,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mathur, R.","contributorId":75740,"corporation":false,"usgs":true,"family":"Mathur","given":"R.","email":"","affiliations":[],"preferred":false,"id":435534,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dohnalkova, A.C.","contributorId":77754,"corporation":false,"usgs":true,"family":"Dohnalkova","given":"A.C.","affiliations":[],"preferred":false,"id":435535,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wall, A.J.","contributorId":8686,"corporation":false,"usgs":true,"family":"Wall","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":435531,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Runkel, R.L.","contributorId":97529,"corporation":false,"usgs":true,"family":"Runkel","given":"R.L.","affiliations":[],"preferred":false,"id":435536,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Brantley, S.L.","contributorId":71676,"corporation":false,"usgs":true,"family":"Brantley","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":435533,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70032337,"text":"70032337 - 2009 - Relating groundwater to seasonal wetlands in southeastern Wisconsin, USA","interactions":[],"lastModifiedDate":"2012-03-12T17:21:25","indexId":"70032337","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1923,"text":"Hydrogeology Journal","active":true,"publicationSubtype":{"id":10}},"title":"Relating groundwater to seasonal wetlands in southeastern Wisconsin, USA","docAbstract":"Historically, drier types of wetlands have been difficult to characterize and are not well researched. Nonetheless, they are considered to reflect the precipitation history with little, if any, regard for possible relation to groundwater. Two seasonal coastal wetland types (wet prairie, sedge meadow) were investigated during three growing seasons at three sites in the Lake Michigan Basin, Wisconsin, USA. The six seasonal wetlands were characterized using standard soil and vegetation techniques and groundwater measurements from the shallow and deep systems. They all met wetland hydrology criteria (e.g., water within 30 cm of land surface for 5% of the growing season) during the early portion of the growing season despite the lack of appreciable regional groundwater discharge into the wetland root zones. Although root-zone duration analyses did not fit a lognormal distribution previously noted in groundwater-dominated wetlands, they were able to discriminate between the plant communities and showed that wet prairie communities had shorter durations of continuous soil saturation than sedge meadow communities. These results demonstrate that the relative rates of groundwater outflows can be important for wetland hydrology and resulting wetland type. Thus, regional stresses to the shallow groundwater system such as pumping or low Great Lake levels can be expected to affect even drier wetland types. ?? Springer-Verlag 2008.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hydrogeology Journal","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10040-008-0345-7","issn":"14312","usgsCitation":"Skalbeck, J., Reed, D., Hunt, R.J., and Lambert, J., 2009, Relating groundwater to seasonal wetlands in southeastern Wisconsin, USA: Hydrogeology Journal, v. 17, no. 1, p. 215-228, https://doi.org/10.1007/s10040-008-0345-7.","startPage":"215","endPage":"228","numberOfPages":"14","costCenters":[],"links":[{"id":215043,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10040-008-0345-7"},{"id":242812,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"1","noUsgsAuthors":false,"publicationDate":"2008-08-09","publicationStatus":"PW","scienceBaseUri":"50e4a624e4b0e8fec6cdc0dc","contributors":{"authors":[{"text":"Skalbeck, J.D.","contributorId":14657,"corporation":false,"usgs":true,"family":"Skalbeck","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":435664,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reed, D.M.","contributorId":55659,"corporation":false,"usgs":true,"family":"Reed","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":435666,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hunt, R. J.","contributorId":40164,"corporation":false,"usgs":true,"family":"Hunt","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":435665,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lambert, J.D.","contributorId":98557,"corporation":false,"usgs":true,"family":"Lambert","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":435667,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70032398,"text":"70032398 - 2009 - Post-breeding season distribution of black-footed and Laysan albatrosses satellite-tagged in Alaska: Inter-specific differences in spatial overlap with North Pacific fisheries","interactions":[],"lastModifiedDate":"2012-03-12T17:21:20","indexId":"70032398","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1015,"text":"Biological Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Post-breeding season distribution of black-footed and Laysan albatrosses satellite-tagged in Alaska: Inter-specific differences in spatial overlap with North Pacific fisheries","docAbstract":"We integrated satellite-tracking data from black-footed albatrosses (Phoebastria nigripes; n = 7) and Laysan albatrosses captured in Alaska (Phoebastria immutabilis; n = 18) with data on fishing effort and distribution from commercial fisheries in the North Pacific in order to assess potential risk from bycatch. Albatrosses were satellite-tagged at-sea in the Central Aleutian Islands, Alaska, and tracked during the post-breeding season, July-October 2005 and 2006. In Alaskan waters, fishing effort occurred almost exclusively within continental shelf and slope waters. Potential fishery interaction for black-footed albatrosses, which most often frequented shelf-slope waters, was greatest with sablefish (Anoplopoma fimbria) longline and pot fisheries and with the Pacific halibut (Hippoglossus stenolepsis) longline fishery. In contrast, Laysan albatrosses spent as much time over oceanic waters beyond the continental shelf and slope, thereby overlapping less with fisheries in Alaska than black-footed albatrosses. Regionally, Laysan albatrosses had the greatest potential fishery interaction with the Atka mackerel (Pleurogrammus monopterygius) trawl fishery in the Western Aleutian Islands and the sablefish pot fishery in the Central Aleutian Islands. Black-footed albatrosses ranged further beyond Alaskan waters than Laysan albatrosses, overlapping west coast Canada fisheries and pelagic longline fisheries in the subarctic transition domain; Laysan albatrosses remained north of these pelagic fisheries. Due to inter-specific differences in oceanic distribution and habitat use, the overlap of fisheries with the post-breeding distribution of black-footed albatrosses is greater than that for Laysan albatrosses, highlighting inter-specific differences in potential vulnerability to bycatch and risk of population-level impacts from fisheries. ?? 2008 Elsevier Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Biological Conservation","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.biocon.2008.12.007","issn":"00063","usgsCitation":"Fischer, K., Suryan, R., Roby, D., and Balogh, G., 2009, Post-breeding season distribution of black-footed and Laysan albatrosses satellite-tagged in Alaska: Inter-specific differences in spatial overlap with North Pacific fisheries: Biological Conservation, v. 142, no. 4, p. 751-760, https://doi.org/10.1016/j.biocon.2008.12.007.","startPage":"751","endPage":"760","numberOfPages":"10","costCenters":[],"links":[{"id":241614,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":213939,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.biocon.2008.12.007"}],"volume":"142","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7e59e4b0c8380cd7a4ae","contributors":{"authors":[{"text":"Fischer, K.N.","contributorId":32360,"corporation":false,"usgs":true,"family":"Fischer","given":"K.N.","email":"","affiliations":[],"preferred":false,"id":435960,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Suryan, R.M.","contributorId":52919,"corporation":false,"usgs":true,"family":"Suryan","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":435961,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Roby, D.D. 0000-0001-9844-0992","orcid":"https://orcid.org/0000-0001-9844-0992","contributorId":70944,"corporation":false,"usgs":true,"family":"Roby","given":"D.D.","affiliations":[],"preferred":false,"id":435962,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Balogh, G.R.","contributorId":74349,"corporation":false,"usgs":true,"family":"Balogh","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":435963,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70032423,"text":"70032423 - 2009 - An integrated approach to assess broad-scale condition of coastal wetlands - The Gulf of Mexico Coastal Wetlands pilot survey","interactions":[],"lastModifiedDate":"2012-03-12T17:21:21","indexId":"70032423","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"An integrated approach to assess broad-scale condition of coastal wetlands - The Gulf of Mexico Coastal Wetlands pilot survey","docAbstract":"The Environmental Protection Agency (EPA) and U.S. Geological Survey (USGS) initiated a two-year regional pilot survey in 2007 to develop, test, and validate tools and approaches to assess the condition of northern Gulf of Mexico (GOM) coastal wetlands. Sampling sites were selected from estuarine and palustrine wetland areas with herbaceous, forested, and shrub/scrub habitats delineated by the US Fish and Wildlife Service National Wetlands Inventory Status and Trends (NWI S&T) program and contained within northern GOM coastal watersheds. A multi-level, stepwise, iterative survey approach is being applied to multiple wetland classes at 100 probabilistically-selected coastal wetlands sites. Tier 1 provides information at the landscape scale about habitat inventory, land use, and environmental stressors associated with the watershed in which each wetland site is located. Tier 2, a rapid assessment conducted through a combination of office and field work, is based on best professional judgment and on-site evidence. Tier 3, an intensive site assessment, involves on-site collection of vegetation, water, and sediment samples to establish an integrated understanding of current wetland condition and validate methods and findings from Tiers 1 and 2. The results from this survey, along with other similar regional pilots from the Mid-Atlantic, West Coast, and Great Lakes Regions will contribute to a design and implementation approach for the National Wetlands Condition Assessment to be conducted by EPA's Office of Water in 2011. ?? Springer Science+Business Media B.V. 2008.","largerWorkTitle":"Environmental Monitoring and Assessment","language":"English","doi":"10.1007/s10661-008-0668-9","issn":"01676","usgsCitation":"Nestlerode, J., Engle, V., Bourgeois, P., Heitmuller, P., Macauley, J., and Allen, Y., 2009, An integrated approach to assess broad-scale condition of coastal wetlands - The Gulf of Mexico Coastal Wetlands pilot survey, <i>in</i> Environmental Monitoring and Assessment, v. 150, no. 1-4, p. 21-29, https://doi.org/10.1007/s10661-008-0668-9.","startPage":"21","endPage":"29","numberOfPages":"9","costCenters":[],"links":[{"id":241510,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":213847,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10661-008-0668-9"}],"volume":"150","issue":"1-4","noUsgsAuthors":false,"publicationDate":"2008-11-27","publicationStatus":"PW","scienceBaseUri":"5059ea7ee4b0c8380cd488d2","contributors":{"authors":[{"text":"Nestlerode, J.A.","contributorId":67738,"corporation":false,"usgs":true,"family":"Nestlerode","given":"J.A.","affiliations":[],"preferred":false,"id":436094,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Engle, V.D.","contributorId":15562,"corporation":false,"usgs":true,"family":"Engle","given":"V.D.","email":"","affiliations":[],"preferred":false,"id":436092,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bourgeois, P.","contributorId":94498,"corporation":false,"usgs":true,"family":"Bourgeois","given":"P.","affiliations":[],"preferred":false,"id":436097,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Heitmuller, P.T.","contributorId":70142,"corporation":false,"usgs":true,"family":"Heitmuller","given":"P.T.","email":"","affiliations":[],"preferred":false,"id":436095,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Macauley, J.M.","contributorId":90491,"corporation":false,"usgs":true,"family":"Macauley","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":436096,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Allen, Y.C.","contributorId":63761,"corporation":false,"usgs":true,"family":"Allen","given":"Y.C.","email":"","affiliations":[],"preferred":false,"id":436093,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70032425,"text":"70032425 - 2009 - Groundwater's significance to changing hydrology, water chemistry, and biological communities of a floodplain ecosystem, Everglades, South Florida, USA","interactions":[],"lastModifiedDate":"2012-03-12T17:21:21","indexId":"70032425","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1923,"text":"Hydrogeology Journal","active":true,"publicationSubtype":{"id":10}},"title":"Groundwater's significance to changing hydrology, water chemistry, and biological communities of a floodplain ecosystem, Everglades, South Florida, USA","docAbstract":"The Everglades (Florida, USA) is one of the world's larger subtropical peatlands with biological communities adapted to waters low in total dissolved solids and nutrients. Detecting how the pre-drainage hydrological system has been altered is crucial to preserving its functional attributes. However, reliable tools for hindcasting historic conditions in the Everglades are limited. A recent synthesis demonstrates that the proportion of surface-water inflows has increased relative to precipitation, accounting for 33% of total inputs compared with 18% historically. The largest new source of water is canal drainage from areas of former wetlands converted to agriculture. Interactions between groundwater and surface water have also increased, due to increasing vertical hydraulic gradients resulting from topographic and water-level alterations on the otherwise extremely flat landscape. Environmental solute tracer data were used to determine groundwater's changing role, from a freshwater storage reservoir that sustained the Everglades ecosystem during dry periods to a reservoir of increasingly degraded water quality. Although some of this degradation is attributable to increased discharge of deep saline groundwater, other mineral sources such as fertilizer additives and peat oxidation have made a greater contribution to water-quality changes that are altering mineral-sensitive biological communities. ?? Springer-Verlag 2008.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hydrogeology Journal","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10040-008-0379-x","issn":"14312","usgsCitation":"Harvey, J., and McCormick, P., 2009, Groundwater's significance to changing hydrology, water chemistry, and biological communities of a floodplain ecosystem, Everglades, South Florida, USA: Hydrogeology Journal, v. 17, no. 1, p. 185-201, https://doi.org/10.1007/s10040-008-0379-x.","startPage":"185","endPage":"201","numberOfPages":"17","costCenters":[],"links":[{"id":476265,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1007/s10040-008-0379-x","text":"Publisher Index Page"},{"id":213879,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10040-008-0379-x"},{"id":241545,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"1","noUsgsAuthors":false,"publicationDate":"2008-10-29","publicationStatus":"PW","scienceBaseUri":"505a2dc4e4b0c8380cd5c004","contributors":{"authors":[{"text":"Harvey, J. W. 0000-0002-2654-9873","orcid":"https://orcid.org/0000-0002-2654-9873","contributorId":39725,"corporation":false,"usgs":true,"family":"Harvey","given":"J. W.","affiliations":[],"preferred":false,"id":436102,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCormick, P.V.","contributorId":93272,"corporation":false,"usgs":true,"family":"McCormick","given":"P.V.","email":"","affiliations":[],"preferred":false,"id":436103,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70032455,"text":"70032455 - 2009 - Possible sources of archaeological maize found in Chaco Canyon and Aztec Ruin, New Mexico","interactions":[],"lastModifiedDate":"2018-02-15T12:56:53","indexId":"70032455","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2182,"text":"Journal of Archaeological Science","active":true,"publicationSubtype":{"id":10}},"title":"Possible sources of archaeological maize found in Chaco Canyon and Aztec Ruin, New Mexico","docAbstract":"Maize played a major role in Chaco's interaction with outlying communities in the southern Colorado Plateau. This paper seeks to determine where archaeological corn cobs brought to Chaco Canyon were grown. Strontium-isotope and trace-metal ratios of 180 soil-water and 18 surface-water sites in the Southern Colorado Plateau have revealed possible source areas for some of 37 archaeological corn cobs from Chaco Canyon and 10 archaeological corn cobs from Aztec Ruin, New Mexico. The most probable source areas for cobs that predate the middle-12th-century drought include several Upper Rio Chaco sites (not including Chaco Canyon). There are many potential source areas for cobs that date to the late A.D. 1100s and early 1200s, all of which lie in the eastern part of the study area. Some Athapascan-age cobs have potential source areas in the Totah, Lobo Mesa, and Dinetah regions. One Gallo Cliff Dwelling cob has a strontium-isotope ratio that exceeds all measured soil-water values. Field sites for this cob may exist in association with Paleozoic and Precambrian rocks found 80-90 km from Chaco Canyon. Potential source areas for most Aztec Ruin cobs (many of which were found in rooms dating to the first half of the 13th-century) appear to be associated with a loess deposit that blankets the Mesa Verde and McElmo Dome regions.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Archaeological Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.jas.2008.09.023","issn":"03054","usgsCitation":"Benson, L.V., Stein, J., and Taylor, H.E., 2009, Possible sources of archaeological maize found in Chaco Canyon and Aztec Ruin, New Mexico: Journal of Archaeological Science, v. 36, no. 2, p. 387-407, https://doi.org/10.1016/j.jas.2008.09.023.","startPage":"387","endPage":"407","numberOfPages":"21","costCenters":[],"links":[{"id":241477,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":213817,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jas.2008.09.023"}],"volume":"36","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7e3de4b0c8380cd7a409","contributors":{"authors":[{"text":"Benson, L. V.","contributorId":50159,"corporation":false,"usgs":true,"family":"Benson","given":"L.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":436250,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stein, J.R.","contributorId":60029,"corporation":false,"usgs":true,"family":"Stein","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":436251,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Taylor, Howard E. hetaylor@usgs.gov","contributorId":1551,"corporation":false,"usgs":true,"family":"Taylor","given":"Howard","email":"hetaylor@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":436249,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70032456,"text":"70032456 - 2009 - The effects of aquaculture production noise on the growth, condition factor, feed conversion, and survival of rainbow trout, Oncorhynchus mykiss","interactions":[],"lastModifiedDate":"2012-03-12T17:21:21","indexId":"70032456","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":853,"text":"Aquaculture","active":true,"publicationSubtype":{"id":10}},"title":"The effects of aquaculture production noise on the growth, condition factor, feed conversion, and survival of rainbow trout, Oncorhynchus mykiss","docAbstract":"Intensive aquaculture systems, particularly recirculating systems, utilize equipment such as aerators, air and water pumps, blowers, and filtration systems that inadvertently increase noise levels in fish culture tanks. Sound levels and frequencies measured within intensive aquaculture systems are within the range of fish hearing, but species-specific effects of aquaculture production noise are not well defined. Field and laboratory studies have shown that fish behavior and physiology can be negatively impacted by intense sound. Therefore, chronic exposure to aquaculture production noise could cause increased stress, reduced growth rates and feed conversion efficiency, and decreased survival. The objective of this study was to provide an in-depth evaluation of the long term effects of aquaculture production noise on the growth, condition factor, feed conversion efficiency, and survival of cultured rainbow trout, Oncorhynchus mykiss. Rainbow trout were cultured in replicated tanks using two sound treatments: 117??dB re 1????Pa RMS which represented sound levels lower than those recorded in an intensive recycle system and 149??dB re 1????Pa RMS, representing sound levels near the upper limits known to occur in recycle systems. To begin the study mean fish weights in the 117 and 149??dB tanks were 40 and 39??g, respectively. After five months of exposure no significant differences were identified between treatments for mean weight, length, specific growth rates, condition factor, feed conversion, or survival (n = 4). Mean final weights for the 117 and 149??dB treatments were 641 ?? 3 and 631 ?? 10??g, respectively. Overall specific growth rates were equal, i.e. 1.84 ?? 0.00 and 1.84 ?? 0.01%/day. Analysis of growth rates of individually tagged rainbow trout indicated that fish from the 149??dB tanks grew slower during the first month of noise exposure (p < 0.05); however, fish acclimated to the noise thereafter. This study further suggests that rainbow trout growth and survival are unlikely to be affected over the long term by noise levels common to intensive aquaculture systems. ?? 2008 Elsevier B.V.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Aquaculture","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.aquaculture.2008.11.037","issn":"00448","usgsCitation":"Davidson, J., Bebak, J., and Mazik, P., 2009, The effects of aquaculture production noise on the growth, condition factor, feed conversion, and survival of rainbow trout, Oncorhynchus mykiss: Aquaculture, v. 288, no. 3-4, p. 337-343, https://doi.org/10.1016/j.aquaculture.2008.11.037.","startPage":"337","endPage":"343","numberOfPages":"7","costCenters":[],"links":[{"id":476374,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.aquaculture.2008.11.037","text":"Publisher Index Page"},{"id":241511,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":213848,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.aquaculture.2008.11.037"}],"volume":"288","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bab6ce4b08c986b322e22","contributors":{"authors":[{"text":"Davidson, J.","contributorId":107100,"corporation":false,"usgs":true,"family":"Davidson","given":"J.","affiliations":[],"preferred":false,"id":436254,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bebak, J.","contributorId":31704,"corporation":false,"usgs":true,"family":"Bebak","given":"J.","affiliations":[],"preferred":false,"id":436253,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mazik, P.","contributorId":22145,"corporation":false,"usgs":true,"family":"Mazik","given":"P.","affiliations":[],"preferred":false,"id":436252,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70032457,"text":"70032457 - 2009 - Case study of a full-scale evapotranspiration cover","interactions":[],"lastModifiedDate":"2018-10-12T09:47:52","indexId":"70032457","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2327,"text":"Journal of Geotechnical and Geoenvironmental Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Case study of a full-scale evapotranspiration cover","docAbstract":"<div class=\"NLM_sec NLM_sec_level_1 hlFld-Abstract\"><p>The design, construction, and performance analyses of a 6.1ha evapotranspiration (ET) landfill cover at the semiarid U.S. Army Fort Carson site, near Colorado Springs, Colo. are presented. Initial water-balance model simulations, using literature reported soil hydraulic data, aided selection of borrow-source soil type(s) that resulted in predictions of negligible annual drainage (⩽1mm∕year). Final construction design was based on refined water-balance simulations using laboratory determined soil hydraulic values from borrow area natural soil horizons that were described with USDA soil classification methods. Cover design components included a 122cm thick clay loam (USDA), compaction ⩽80% of the standard Proctor maximum dry density (dry bulk density ∼1.3Mg/m3), erosion control measures, top soil amended with biosolids, and seeding with native grasses. Favorable hydrologic performance for a 5year period was documented by lysimeter-measured and Richards’-based calculations of annual drainage that were all &lt;0.4mm∕year. Water potential data suggest that ET removed water that infiltrated the cover and contributed to a persistent driving force for upward flow and removal of water from below the base of the cover.</p></div>","language":"English","publisher":"ASCE","doi":"10.1061/(ASCE)1090-0241(2009)135:3(316)","usgsCitation":"McGuire, P.E., Andraski, B.J., and Archibald, R.E., 2009, Case study of a full-scale evapotranspiration cover: Journal of Geotechnical and Geoenvironmental Engineering, v. 135, no. 3, p. 316-332, https://doi.org/10.1061/(ASCE)1090-0241(2009)135:3(316).","productDescription":"17 p.","startPage":"316","endPage":"332","costCenters":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":241512,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"135","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f38ce4b0c8380cd4b88a","contributors":{"authors":[{"text":"McGuire, Patrick E.","contributorId":71008,"corporation":false,"usgs":false,"family":"McGuire","given":"Patrick","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":436257,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andraski, Brian J. 0000-0002-2086-0417 andraski@usgs.gov","orcid":"https://orcid.org/0000-0002-2086-0417","contributorId":168800,"corporation":false,"usgs":true,"family":"Andraski","given":"Brian","email":"andraski@usgs.gov","middleInitial":"J.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true},{"id":38175,"text":"Toxics Substances Hydrology Program","active":true,"usgs":true}],"preferred":false,"id":436256,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Archibald, Ryan E.","contributorId":27277,"corporation":false,"usgs":false,"family":"Archibald","given":"Ryan","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":436255,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70032458,"text":"70032458 - 2009 - Turbulent stresses and secondary currents in a tidal-forced channel with significant curvature and asymmetric bed forms","interactions":[],"lastModifiedDate":"2020-09-10T17:29:25.087434","indexId":"70032458","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2338,"text":"Journal of Hydraulic Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Turbulent stresses and secondary currents in a tidal-forced channel with significant curvature and asymmetric bed forms","docAbstract":"<div class=\"NLM_sec NLM_sec_level_1 hlFld-Abstract\"><p>Acoustic Doppler current profilers are deployed to measure both the mean flow and turbulent properties in a channel with significant curvature. Direct measurements of the Reynolds stress show a significant asymmetry over the tidal cycle where stresses are enhanced during the flood tide and less prominent over the ebb tide. This asymmetry is corroborated by logarithmic fits using<span>&nbsp;</span><span class=\"equationTd\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot; display=&quot;inline&quot; overflow=&quot;scroll&quot;><mrow><mn>10</mn><mspace width=&quot;0.3em&quot; /><mi>min</mi></mrow></math>\"><span id=\"MathJax-Span-1\" class=\"math\"><span><span id=\"MathJax-Span-2\" class=\"mrow\"><span id=\"MathJax-Span-3\" class=\"mrow\"><span id=\"MathJax-Span-4\" class=\"mn\">10</span><span id=\"MathJax-Span-5\" class=\"mspace\"></span><span id=\"MathJax-Span-6\" class=\"mi\">min</span></span></span></span></span><span class=\"MJX_Assistive_MathML\">10min</span></span></span><span>&nbsp;</span>averaged velocity data. A smaller yet similar tendency asymmetry in drag coefficient is inferred by fitting the velocity and estimated large-scale pressure gradient to a one-dimensional along-channel momentum balance. This smaller asymmetry is consistent with recent modeling work simulating regional flows in the vicinity of the study site. The asymmetry in drag suggests the importance of previously reported bed forms for this channel and demonstrates spatial and temporarily variations in bed stress. Secondary circulation patterns observed in a relatively straight section of channel appear driven by local curvature rather than being remotely forced by the regions of significant curvature only a few hundred meters from the measurement site.</p></div>","language":"English","publisher":"ASCE","doi":"10.1061/(ASCE)0733-9429(2009)135:3(198)","usgsCitation":"Fong, D., Monismith, S., Stacey, M., and Burau, J., 2009, Turbulent stresses and secondary currents in a tidal-forced channel with significant curvature and asymmetric bed forms: Journal of Hydraulic Engineering, v. 135, no. 3, p. 198-208, https://doi.org/10.1061/(ASCE)0733-9429(2009)135:3(198).","productDescription":"11 p.","startPage":"198","endPage":"208","numberOfPages":"11","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":241547,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"135","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb8f4e4b08c986b327b3b","contributors":{"authors":[{"text":"Fong, D.A.","contributorId":27624,"corporation":false,"usgs":true,"family":"Fong","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":436259,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Monismith, Stephen G.","contributorId":57228,"corporation":false,"usgs":true,"family":"Monismith","given":"Stephen G.","affiliations":[],"preferred":false,"id":436260,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stacey, M.T.","contributorId":82874,"corporation":false,"usgs":true,"family":"Stacey","given":"M.T.","email":"","affiliations":[],"preferred":false,"id":436261,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Burau, J.R. 0000-0002-5196-5035","orcid":"https://orcid.org/0000-0002-5196-5035","contributorId":7307,"corporation":false,"usgs":true,"family":"Burau","given":"J.R.","affiliations":[],"preferred":false,"id":436258,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70032461,"text":"70032461 - 2009 - Scenario liquefaction hazard maps of Santa Clara Valley, Northern California","interactions":[],"lastModifiedDate":"2012-03-12T17:21:21","indexId":"70032461","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"Scenario liquefaction hazard maps of Santa Clara Valley, Northern California","docAbstract":"Maps showing the probability of surface manifestations of liquefaction in the northern Santa Clara Valley were prepared with liquefaction probability curves. These curves were based on complementary cumulative frequency distributions of the liquefaction potential index (LPI) for surficial geologic units in the study area. LPI values were computed with extensive cone penetration test soundings. Maps were developed for three earthquake scenarios, an M 7.8 event on the San Andreas fault comparable to the 1906 event, an M 6.7 event on the Hayward fault comparable to the 1868 event, and an M 6.9 event on the Calaveras fault. Ground motions were estimated with the Boore and Atkinson (2008) attenuation relation. Liquefaction is predicted for all three events in young Holocene levee deposits along the major creeks. Liquefaction probabilities are highest for the M 7.8 earthquake, ranging from 0.33 to 0.37 if a 1.5 m deep water table is assumed, and from 0.10 to 0.14, if a 5 m deep water table is assumed. Liquefaction probabilities of the other surficial geologic units are less than 0.05. Probabilities for the scenario earthquakes are generally consistent with observations during historical earthquakes.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of the Seismological Society of America","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1785/0120080227","issn":"00371","usgsCitation":"Holzer, T., Noce, T., and Bennett, M., 2009, Scenario liquefaction hazard maps of Santa Clara Valley, Northern California: Bulletin of the Seismological Society of America, v. 99, no. 1, p. 367-381, https://doi.org/10.1785/0120080227.","startPage":"367","endPage":"381","numberOfPages":"15","costCenters":[],"links":[{"id":213909,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1785/0120080227"},{"id":241580,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"99","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8735e4b08c986b316389","contributors":{"authors":[{"text":"Holzer, T.L.","contributorId":35739,"corporation":false,"usgs":true,"family":"Holzer","given":"T.L.","email":"","affiliations":[],"preferred":false,"id":436282,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Noce, T.E.","contributorId":54285,"corporation":false,"usgs":true,"family":"Noce","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":436283,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bennett, M.J.","contributorId":67504,"corporation":false,"usgs":true,"family":"Bennett","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":436284,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70032486,"text":"70032486 - 2009 - Hydrograph separation for karst watersheds using a two-domain rainfall-discharge model","interactions":[],"lastModifiedDate":"2012-03-12T17:21:22","indexId":"70032486","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","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":"Hydrograph separation for karst watersheds using a two-domain rainfall-discharge model","docAbstract":"Highly parameterized, physically based models may be no more effective at simulating the relations between rainfall and outflow from karst watersheds than are simpler models. Here an antecedent rainfall and convolution model was used to separate a karst watershed hydrograph into two outflow components: one originating from focused recharge in conduits and one originating from slow flow in a porous annex system. In convolution, parameters of a complex system are lumped together in the impulse-response function (IRF), which describes the response of the system to an impulse of effective precipitation. Two parametric functions in superposition approximate the two-domain IRF. The outflow hydrograph can be separated into flow components by forward modeling with isolated IRF components, which provides an objective criterion for separation. As an example, the model was applied to a karst watershed in the Madison aquifer, South Dakota, USA. Simulation results indicate that this watershed is characterized by a flashy response to storms, with a peak response time of 1 day, but that 89% of the flow results from the slow-flow domain, with a peak response time of more than 1 year. This long response time may be the result of perched areas that store water above the main water table. Simulation results indicated that some aspects of the system are stationary but that nonlinearities also exist.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Hydrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.jhydrol.2008.11.001","issn":"00221","usgsCitation":"Long, A., 2009, Hydrograph separation for karst watersheds using a two-domain rainfall-discharge model: Journal of Hydrology, v. 364, no. 3-4, p. 249-256, https://doi.org/10.1016/j.jhydrol.2008.11.001.","startPage":"249","endPage":"256","numberOfPages":"8","costCenters":[],"links":[{"id":213819,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jhydrol.2008.11.001"},{"id":241479,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"364","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a34f6e4b0c8380cd5fb7b","contributors":{"authors":[{"text":"Long, Andrew J.","contributorId":80023,"corporation":false,"usgs":false,"family":"Long","given":"Andrew J.","affiliations":[],"preferred":false,"id":436424,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70032487,"text":"70032487 - 2009 - Phenologically-tuned MODIS NDVI-based production anomaly estimates for Zimbabwe","interactions":[],"lastModifiedDate":"2017-04-03T15:06:34","indexId":"70032487","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3254,"text":"Remote Sensing of Environment","printIssn":"0034-4257","active":true,"publicationSubtype":{"id":10}},"title":"Phenologically-tuned MODIS NDVI-based production anomaly estimates for Zimbabwe","docAbstract":"For thirty years, simple crop water balance models have been used by the early warning community to monitor agricultural drought. These models estimate and accumulate actual crop evapotranspiration, evaluating environmental conditions based on crop water requirements. Unlike seasonal rainfall totals, these models take into account the phenology of the crop, emphasizing conditions during the peak grain filling phase of crop growth. In this paper we describe an analogous metric of crop performance based on time series of Moderate Resolution Imaging Spectroradiometer (MODIS) Normalized Difference Vegetation Index (NDVI) imagery. A special temporal filter is used to screen for cloud contamination. Regional NDVI time series are then composited for cultivated areas, and adjusted temporally according to the timing of the rainy season. This adjustment standardizes the NDVI response vis-??-vis the expected phenological response of maize. A national time series index is then created by taking the cropped-area weighted average of the regional series. This national time series provides an effective summary of vegetation response in agricultural areas, and allows for the identification of NDVI green-up during grain filling. Onset-adjusted NDVI values following the grain filling period are well correlated with U.S. Department of Agriculture production figures, possess desirable linear characteristics, and perform better than more common indices such as maximum seasonal NDVI or seasonally averaged NDVI. Thus, just as appropriately calibrated crop water balance models can provide more information than seasonal rainfall totals, the appropriate agro-phenological filtering of NDVI can improve the utility and accuracy of space-based agricultural monitoring.","language":"English","publisher":"Elsevier","doi":"10.1016/j.rse.2008.08.015","issn":"00344","usgsCitation":"Funk, C., and Budde, M.E., 2009, Phenologically-tuned MODIS NDVI-based production anomaly estimates for Zimbabwe: Remote Sensing of Environment, v. 113, no. 1, p. 115-125, https://doi.org/10.1016/j.rse.2008.08.015.","productDescription":"11 p.","startPage":"115","endPage":"125","numberOfPages":"11","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":241513,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":213850,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.rse.2008.08.015"}],"volume":"113","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7889e4b0c8380cd7870d","contributors":{"authors":[{"text":"Funk, Chris 0000-0002-9254-6718 cfunk@usgs.gov","orcid":"https://orcid.org/0000-0002-9254-6718","contributorId":167070,"corporation":false,"usgs":true,"family":"Funk","given":"Chris","email":"cfunk@usgs.gov","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true},{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"preferred":true,"id":436426,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Budde, Michael E. 0000-0002-9098-2751 mbudde@usgs.gov","orcid":"https://orcid.org/0000-0002-9098-2751","contributorId":3007,"corporation":false,"usgs":true,"family":"Budde","given":"Michael","email":"mbudde@usgs.gov","middleInitial":"E.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":436425,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70032524,"text":"70032524 - 2009 - Shallow water processes govern system-wide phytoplankton bloom dynamics: A modeling study","interactions":[],"lastModifiedDate":"2018-10-08T09:05:19","indexId":"70032524","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2381,"text":"Journal of Marine Systems","active":true,"publicationSubtype":{"id":10}},"title":"Shallow water processes govern system-wide phytoplankton bloom dynamics: A modeling study","docAbstract":"<p><span>A pseudo-two-dimensional numerical model of estuarine phytoplankton growth and consumption, vertical turbulent mixing, and idealized cross-estuary transport was developed and applied to South San Francisco Bay. This estuary has two bathymetrically distinct habitat types (deep channel, shallow shoal) and associated differences in local net rates of phytoplankton growth and consumption, as well as differences in the water column's tendency to stratify. Because many physical and biological time scales relevant to algal population dynamics decrease with decreasing depth, process rates can be especially fast in the shallow water. We used the model to explore the potential significance of hydrodynamic connectivity between a channel and shoal and whether lateral transport can allow physical or biological processes (e.g. stratification, benthic grazing, light attenuation) in one sub-region to control phytoplankton biomass and bloom development in the adjacent sub-region. Model results for South San Francisco Bay suggest that lateral transport from a productive shoal can result in phytoplankton biomass accumulation in an adjacent deep, unproductive channel. The model further suggests that turbidity and benthic grazing in the shoal can control the occurrence of a bloom system-wide; whereas, turbidity, benthic grazing, and vertical density stratification in the channel are likely to only control local bloom occurrence or modify system-wide bloom magnitude. Measurements from a related field program are generally consistent with model-derived conclusions.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jmarsys.2008.07.011","issn":"09247","usgsCitation":"Lucas, L., Koseff, J.R., Monismith, S., and Thompson, J., 2009, Shallow water processes govern system-wide phytoplankton bloom dynamics: A modeling study: Journal of Marine Systems, v. 75, no. 1-2, p. 70-86, https://doi.org/10.1016/j.jmarsys.2008.07.011.","productDescription":"17 p.","startPage":"70","endPage":"86","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":241516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":213853,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jmarsys.2008.07.011"}],"volume":"75","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8e46e4b08c986b318834","contributors":{"authors":[{"text":"Lucas, L.V.","contributorId":62777,"corporation":false,"usgs":true,"family":"Lucas","given":"L.V.","email":"","affiliations":[],"preferred":false,"id":436634,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Koseff, Jeffrey R.","contributorId":37915,"corporation":false,"usgs":false,"family":"Koseff","given":"Jeffrey","email":"","middleInitial":"R.","affiliations":[{"id":6986,"text":"Stanford University","active":true,"usgs":false}],"preferred":false,"id":436632,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Monismith, Stephen G.","contributorId":57228,"corporation":false,"usgs":true,"family":"Monismith","given":"Stephen G.","affiliations":[],"preferred":false,"id":436633,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thompson, J.K.","contributorId":103300,"corporation":false,"usgs":true,"family":"Thompson","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":436635,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70032529,"text":"70032529 - 2009 - Impact of AMD on water quality in critical watershed in the Hudson River drainage basin: Phillips Mine, Hudson Highlands, New York","interactions":[],"lastModifiedDate":"2016-08-25T17:03:40","indexId":"70032529","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1539,"text":"Environmental Geology","active":true,"publicationSubtype":{"id":10}},"title":"Impact of AMD on water quality in critical watershed in the Hudson River drainage basin: Phillips Mine, Hudson Highlands, New York","docAbstract":"<p>A sulfur and trace element enriched U-Th-laced tailings pile at the abandoned Phillips Mine in Garrison, New York, releases acid mine drainage (AMD, generally pH &lt; 3, minimum pH 1.78) into the first-order Copper Mine Brook (CMB) that drains into the Hudson River. The pyrrhotite-rich Phillips Mine is located in the Highlands region, a critical water source for the New York metro area. A conceptual model for derivation/dissolution, sequestration, transport and dilution of contaminants is proposed. The acidic water interacts with the tailings, leaching and dissolving the trace metals. AMD evaporation during dry periods concentrates solid phase trace metals and sulfate, forming melanterite (FeSO<sub>4</sub>.7H<sub>2</sub>O) on sulfide-rich tailings surfaces. Wet periods dissolve these concentrates/precipitates, releasing stored acidity and trace metals into the CMB. Sediments along CMB are enriched in iron hydroxides which act as sinks for metals, indicating progressive sequestration that correlates with dilution and sharp rise in pH when mine water mixes with tributaries. Seasonal variations in metal concentrations were partly attributable to dissolution of the efflorescent salts with their sorbed metals and additional metals from surging acidic seepage induced by precipitation.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s00254-008-1310-4","issn":"09430","usgsCitation":"Gilchrist, S., Gates, A., Szabo, Z., and Lamothe, P.J., 2009, Impact of AMD on water quality in critical watershed in the Hudson River drainage basin: Phillips Mine, Hudson Highlands, New York: Environmental Geology, v. 57, no. 2, p. 397-409, https://doi.org/10.1007/s00254-008-1310-4.","productDescription":"13 p.","startPage":"397","endPage":"409","costCenters":[],"links":[{"id":241585,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":213913,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s00254-008-1310-4"}],"country":"United States","state":"New York","city":"Garrison","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.9683723449707,\n              41.286513853008614\n            ],\n            [\n              -73.9683723449707,\n              41.31133964539859\n            ],\n            [\n              -73.90726089477539,\n              41.31133964539859\n            ],\n            [\n              -73.90726089477539,\n              41.286513853008614\n            ],\n            [\n              -73.9683723449707,\n              41.286513853008614\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"57","issue":"2","noUsgsAuthors":false,"publicationDate":"2008-04-16","publicationStatus":"PW","scienceBaseUri":"505a38afe4b0c8380cd6165d","contributors":{"authors":[{"text":"Gilchrist, S.","contributorId":34332,"corporation":false,"usgs":true,"family":"Gilchrist","given":"S.","email":"","affiliations":[],"preferred":false,"id":436645,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gates, A.","contributorId":100203,"corporation":false,"usgs":true,"family":"Gates","given":"A.","email":"","affiliations":[],"preferred":false,"id":436648,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Szabo, Z. 0000-0002-0760-9607","orcid":"https://orcid.org/0000-0002-0760-9607","contributorId":44302,"corporation":false,"usgs":true,"family":"Szabo","given":"Z.","affiliations":[],"preferred":false,"id":436646,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lamothe, P. J.","contributorId":45672,"corporation":false,"usgs":true,"family":"Lamothe","given":"P.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":436647,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70032530,"text":"70032530 - 2009 - Mapping of accumulated nitrogen in the sediment pore water of a eutrophic lake in Iowa, USA","interactions":[],"lastModifiedDate":"2012-03-12T17:21:21","indexId":"70032530","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1539,"text":"Environmental Geology","active":true,"publicationSubtype":{"id":10}},"title":"Mapping of accumulated nitrogen in the sediment pore water of a eutrophic lake in Iowa, USA","docAbstract":"A large pool of nitrogen in the sediment pore fluid of a eutrophic lake in Iowa, USA, was mapped in this study. Previously, the lake had supported fishing and boating, but today it no longer supports its designated uses as a recreational water body. In the top 5 cm of the lake bottom, the pore water nitrogen ranges between 3.1 and 1,250 ??g/cm3 of sediments, with an average of 160.3 ??g/cm3. Vertically, nitrate concentrations were measured as 153 ??g/cm3 at 0-10 cm, 162 ??g/cm3 at 10-20 cm, and 32 ??g/cm3 at 20-30 cm. Nitrate mass distribution was quantified as 3.67 ?? 103 kg (65%) in the bottom sediments, 172 kg (3%) in suspended particulates, and 1.83 ?? 103 kg (32%) in the dissolved phase. Soil runoff nutrients arrive at the lake from the heavily fertilized lands in the watershed. Upon sedimentation, a large mass of nitrogen desorbs from mineral particles to the relatively immobile pore fluid. Under favorable conditions, this nitrogen diffuses back into the water column, thereby dramatically limiting the lake's capability to process incoming nutrients from farmlands. Consequently, a condition of oxygen deficiency disrupts the post-season biological activities in the lake. ?? 2008 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s00254-008-1317-x","issn":"09430","usgsCitation":"Iqbal, M., and Fields, C., 2009, Mapping of accumulated nitrogen in the sediment pore water of a eutrophic lake in Iowa, USA: Environmental Geology, v. 57, no. 2, p. 465-475, https://doi.org/10.1007/s00254-008-1317-x.","startPage":"465","endPage":"475","numberOfPages":"11","costCenters":[],"links":[{"id":213914,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s00254-008-1317-x"},{"id":241586,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"57","issue":"2","noUsgsAuthors":false,"publicationDate":"2008-04-18","publicationStatus":"PW","scienceBaseUri":"505a5065e4b0c8380cd6b680","contributors":{"authors":[{"text":"Iqbal, M.Z.","contributorId":45911,"corporation":false,"usgs":true,"family":"Iqbal","given":"M.Z.","email":"","affiliations":[],"preferred":false,"id":436649,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fields, C.L.","contributorId":83343,"corporation":false,"usgs":true,"family":"Fields","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":436650,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70032557,"text":"70032557 - 2009 - Evaluating the validity of using unverified indices of body condition","interactions":[],"lastModifiedDate":"2018-05-14T13:38:29","indexId":"70032557","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2190,"text":"Journal of Avian Biology","active":true,"publicationSubtype":{"id":10}},"title":"Evaluating the validity of using unverified indices of body condition","docAbstract":"<p><span>Condition indices are commonly used in an attempt to link body condition of birds to ecological variables of interest, including demographic attributes such as survival and reproduction. Most indices are based on body mass adjusted for structural body size, calculated as simple ratios or residuals from regressions. However, condition indices are often applied without confirming their predictive value (i.e., without being validated against measured values of fat and protein), which we term ‘unverified’ use. We evaluated the ability of a number of unverified indices frequently found in the literature to predict absolute and proportional levels of fat and protein across five species of waterfowl. Among indices we considered, those accounting for body size never predicted absolute protein more precisely than body mass, however, some indices improved predictability of fat, although the form of the best index varied by species. Further, the gain in precision by using a condition index to predict either absolute or percent fat was minimal (rise in r</span><sup>2</sup><span>≤0.13), and in many cases model fit was actually reduced. Our data agrees with previous assertions that the assumption that indices provide more precise indicators of body condition than body mass alone is often invalid. We strongly discourage the use of unverified indices, because subjectively selecting indices likely does little to improve precision and might in fact decrease predictability relative to using body mass alone.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1600-048X.2008.04462.x","issn":"09088","usgsCitation":"Schamber, J., Esler, D., and Flint, P.L., 2009, Evaluating the validity of using unverified indices of body condition: Journal of Avian Biology, v. 40, no. 1, p. 49-56, https://doi.org/10.1111/j.1600-048X.2008.04462.x.","productDescription":"8 p.","startPage":"49","endPage":"56","numberOfPages":"8","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":241484,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":213823,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1600-048X.2008.04462.x"}],"volume":"40","issue":"1","noUsgsAuthors":false,"publicationDate":"2009-01-13","publicationStatus":"PW","scienceBaseUri":"505a0c01e4b0c8380cd529c5","contributors":{"authors":[{"text":"Schamber, J.L.","contributorId":92012,"corporation":false,"usgs":true,"family":"Schamber","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":436806,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Esler, Daniel 0000-0001-5501-4555 desler@usgs.gov","orcid":"https://orcid.org/0000-0001-5501-4555","contributorId":5465,"corporation":false,"usgs":true,"family":"Esler","given":"Daniel","email":"desler@usgs.gov","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":12437,"text":"Simon Fraser University, Centre for Wildlife Ecology","active":true,"usgs":false}],"preferred":true,"id":436804,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Flint, Paul L. 0000-0002-8758-6993 pflint@usgs.gov","orcid":"https://orcid.org/0000-0002-8758-6993","contributorId":3284,"corporation":false,"usgs":true,"family":"Flint","given":"Paul","email":"pflint@usgs.gov","middleInitial":"L.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":436805,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70032564,"text":"70032564 - 2009 - Zooplankton assemblages in montane lakes and ponds of Mount Rainier National Park, Washington State, USA","interactions":[],"lastModifiedDate":"2017-11-17T15:37:35","indexId":"70032564","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2430,"text":"Journal of Plankton Research","active":true,"publicationSubtype":{"id":10}},"title":"Zooplankton assemblages in montane lakes and ponds of Mount Rainier National Park, Washington State, USA","docAbstract":"Water quality and zooplankton samples were collected during the ice-free periods between 1988 and 2005 from 103 oligotrophic montane lakes and ponds located in low forest to alpine vegetation zones in Mount Rainier National Park, Washington State, USA. Collectively, 45 rotifer and 44 crustacean taxa were identified. Most of the numerically dominant taxa appeared to have wide niche breadths. The average number of taxa per lake decreased with elevation and generally increased as maximum lake depths increased (especially for rotifers). With one exception, fish presence/absence did not explain the taxonomic compositions of crustacean zooplankton assemblages. Many rotifer species were common members of zooplankton assemblages in montane lakes and ponds in western North America, whereas the crustacean taxa were common to some areas of the west, but not others. Constraints of the environmental variables did not appear to provide strong gradients to separate the distributions of most zooplankton species. This suggests that interspecific competitive interactions and stochastic processes regulate the taxonomic structures of the zooplankton assemblages at the landscape level. Crustacean species that had broad niche breadths were associated with different rotifer taxa across the environmental gradients. Studies of zooplankton assemblages need to address both crustacean and rotifer taxa, not one or the other.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Plankton Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1093/plankt/fbn125","issn":"01427","usgsCitation":"Larson, G., Hoffman, R., McIntire, C.D., Lienkaemper, G., and Samora, B., 2009, Zooplankton assemblages in montane lakes and ponds of Mount Rainier National Park, Washington State, USA: Journal of Plankton Research, v. 31, no. 3, p. 273-285, https://doi.org/10.1093/plankt/fbn125.","startPage":"273","endPage":"285","numberOfPages":"13","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":213916,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1093/plankt/fbn125"},{"id":241588,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"3","noUsgsAuthors":false,"publicationDate":"2008-12-16","publicationStatus":"PW","scienceBaseUri":"505bd29de4b08c986b32f909","contributors":{"authors":[{"text":"Larson, G.L.","contributorId":103021,"corporation":false,"usgs":true,"family":"Larson","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":436835,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoffman, R.","contributorId":10205,"corporation":false,"usgs":true,"family":"Hoffman","given":"R.","affiliations":[],"preferred":false,"id":436832,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McIntire, C. D.","contributorId":35274,"corporation":false,"usgs":false,"family":"McIntire","given":"C.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":436833,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lienkaemper, G.","contributorId":69113,"corporation":false,"usgs":true,"family":"Lienkaemper","given":"G.","email":"","affiliations":[],"preferred":false,"id":436834,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Samora, B.","contributorId":10012,"corporation":false,"usgs":true,"family":"Samora","given":"B.","affiliations":[],"preferred":false,"id":436831,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70032593,"text":"70032593 - 2009 - Mercury isotopic composition of hydrothermal systems in the Yellowstone Plateau volcanic field and Guaymas Basin sea-floor rift","interactions":[],"lastModifiedDate":"2019-04-29T10:43:04","indexId":"70032593","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Mercury isotopic composition of hydrothermal systems in the Yellowstone Plateau volcanic field and Guaymas Basin sea-floor rift","docAbstract":"To characterize mercury (Hg) isotopes and isotopic fractionation in hydrothermal systems we analyzed fluid and precipitate samples from hot springs in the Yellowstone Plateau volcanic field and vent chimney samples from the Guaymas Basin sea-floor rift. These samples provide an initial indication of the variability in Hg isotopic composition among marine and continental hydrothermal systems that are controlled predominantly by mantle-derived magmas. Fluid samples from Ojo Caliente hot spring in Yellowstone range in &delta;<sup>202</sup>Hg from - 1.02&permil; to 0.58&permil; (&plusmn; 0.11&permil;, 2SD) and solid precipitate samples from Guaymas Basin range in &delta;<sup>202</sup>Hg from - 0.37&permil; to - 0.01&permil; (&plusmn; 0.14&permil;, 2SD). Fluid samples from Ojo Caliente display mass-dependent fractionation (MDF) of Hg from the vent (&delta;<sup>202</sup>Hg = 0.10&permil; &plusmn; 0.11&permil;, 2SD) to the end of the outflow channel (&delta<sup>202</sup>Hg = 0.58&permil; &plusmn; 0.11&permil;, 2SD) in conjunction with a decrease in Hg concentration from 46.6pg/g to 20.0pg/g. Although a small amount of Hg is lost from the fluids due to co-precipitation with siliceous sinter, we infer that the majority of the observed MDF and Hg loss from waters in Ojo Caliente is due to volatilization of Hg<sup>0</sup><sub>(aq)</sub> to Hg<sup>0</sup><sub>(g)</sub> and the preferential loss of Hg with a lower &delta;<sup>202</sup>Hg value to the atmosphere. A small amount of mass-independent fractionation (MIF) was observed in all samples from Ojo Caliente (&Delta;<sup>199</sup>Hg = 0.13&permil; &plusmn;1 0.06&permil;, 2SD) but no significant MIF was measured in the sea-floor rift samples from Guaymas Basin. This study demonstrates that several different hydrothermal processes fractionate Hg isotopes and that Hg isotopes may be used to better understand these processes.","language":"English","publisher":"Elsevier","doi":"10.1016/j.epsl.2008.12.032","issn":"00128","usgsCitation":"Sherman, L., Blum, J., Nordstrom, D.K., McCleskey, R.B., Barkay, T., and Vetriani, C., 2009, Mercury isotopic composition of hydrothermal systems in the Yellowstone Plateau volcanic field and Guaymas Basin sea-floor rift: Earth and Planetary Science Letters, v. 279, no. 1-2, p. 86-96, https://doi.org/10.1016/j.epsl.2008.12.032.","productDescription":"11 p.","startPage":"86","endPage":"96","numberOfPages":"11","costCenters":[{"id":435,"text":"National Research Program - Central Region","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":241558,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Yellowstone Caldera","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.7337760925293,\n              44.40447671189411\n            ],\n            [\n              -110.71188926696777,\n              44.40447671189411\n            ],\n            [\n              -110.71188926696777,\n              44.42004966190147\n            ],\n            [\n              -110.7337760925293,\n              44.42004966190147\n            ],\n            [\n              -110.7337760925293,\n              44.40447671189411\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"279","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5420e4b0c8380cd6ceb4","contributors":{"authors":[{"text":"Sherman, L.S.","contributorId":36765,"corporation":false,"usgs":true,"family":"Sherman","given":"L.S.","email":"","affiliations":[],"preferred":false,"id":436973,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blum, J.D.","contributorId":30829,"corporation":false,"usgs":true,"family":"Blum","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":436972,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nordstrom, D. Kirk 0000-0003-3283-5136 dkn@usgs.gov","orcid":"https://orcid.org/0000-0003-3283-5136","contributorId":749,"corporation":false,"usgs":true,"family":"Nordstrom","given":"D.","email":"dkn@usgs.gov","middleInitial":"Kirk","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":false,"id":436975,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McCleskey, R. Blaine 0000-0002-2521-8052 rbmccles@usgs.gov","orcid":"https://orcid.org/0000-0002-2521-8052","contributorId":147399,"corporation":false,"usgs":true,"family":"McCleskey","given":"R.","email":"rbmccles@usgs.gov","middleInitial":"Blaine","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":436970,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Barkay, T.","contributorId":57617,"corporation":false,"usgs":true,"family":"Barkay","given":"T.","affiliations":[],"preferred":false,"id":436974,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Vetriani, C.","contributorId":20166,"corporation":false,"usgs":true,"family":"Vetriani","given":"C.","email":"","affiliations":[],"preferred":false,"id":436971,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70032653,"text":"70032653 - 2009 - Predator avoidance performance of larval fathead minnows (<i>Pimephales promelas</i>) following short-term exposure to estrogen mixtures","interactions":[],"lastModifiedDate":"2018-10-12T07:59:25","indexId":"70032653","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":874,"text":"Aquatic Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Predator avoidance performance of larval fathead minnows (<i>Pimephales promelas</i>) following short-term exposure to estrogen mixtures","docAbstract":"<p><span>Aquatic organisms exposed to endocrine disrupting compounds (EDCs) at early life-stages may have reduced reproductive fitness via disruption of reproductive and non-reproductive behavioral and physiological pathways. Survival to reproductive age relies upon optimal non-reproductive trait expression, such as adequate predator avoidance responses, which may be impacted through EDC exposure. During a predator&ndash;prey confrontation, larval fish use an innate C-start escape behavior to rapidly move away from an approaching threat. We tested the hypotheses that (1) larval fathead minnows exposed to estrogens, a primary class of EDCs, singularly or in mixture, suffer a reduced ability to perform an innate C-start behavior when faced with a threat stimulus; (2) additive effects will cause greater reductions in C-start behavior; and (3) effects will differ among developmental stages. In this study, embryos (post-fertilization until hatching) were exposed for 5 days to environmentally relevant concentrations of estrone (E1), 17&beta;-estradiol (E2), and 17&alpha;-ethinylestradiol (EE2) singularly and in mixture. Exposed embryos were allowed to hatch and grow in control well water until 12 days old. Similarly, post-hatch fathead minnows were exposed for 12 days to these compounds. High-speed (1000&nbsp;frames/s) video recordings of escape behavior were collected and transferred to National Institutes of Health Image for frame-by-frame analysis of latency period, escape velocity, and total escape response (combination of latency period and escape velocity). When tested 12 days post-hatch, only E1 adversely affected C-start performance of larvae exposed as embryos. Conversely, larvae exposed for 12 days post-hatch did not exhibit altered escape responses when exposed to E1, while adverse responses were seen in E2 and the estrogen mixture. Ethinylestradiol exposure did not elicit changes in escape behaviors at either developmental stage. The direct impact of reduced C-start performance on survival, and ultimately, reproductive fitness provides an avenue to assess the ecological relevance of exposure in an assay of relatively short duration.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.aquatox.2008.12.002","issn":"01664","usgsCitation":"McGee, M., Julius, M., Vajda, A., Norris, D., Barber, L.B., and Schoenfuss, H., 2009, Predator avoidance performance of larval fathead minnows (<i>Pimephales promelas</i>) following short-term exposure to estrogen mixtures: Aquatic Toxicology, v. 91, no. 4, p. 355-361, https://doi.org/10.1016/j.aquatox.2008.12.002.","productDescription":"7 p.","startPage":"355","endPage":"361","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":241421,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":213764,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.aquatox.2008.12.002"}],"volume":"91","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a816ce4b0c8380cd7b514","contributors":{"authors":[{"text":"McGee, M.R.","contributorId":82930,"corporation":false,"usgs":true,"family":"McGee","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":437291,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Julius, M.L.","contributorId":11775,"corporation":false,"usgs":true,"family":"Julius","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":437287,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vajda, A.M.","contributorId":35961,"corporation":false,"usgs":true,"family":"Vajda","given":"A.M.","affiliations":[],"preferred":false,"id":437288,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Norris, D.O.","contributorId":58475,"corporation":false,"usgs":true,"family":"Norris","given":"D.O.","email":"","affiliations":[],"preferred":false,"id":437289,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Barber, L. B.","contributorId":64602,"corporation":false,"usgs":true,"family":"Barber","given":"L.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":437290,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Schoenfuss, H.L.","contributorId":103877,"corporation":false,"usgs":true,"family":"Schoenfuss","given":"H.L.","affiliations":[],"preferred":false,"id":437292,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70032654,"text":"70032654 - 2009 - Identification of methyl triclosan and halogenated analogues in male common carp (Cyprinus carpio) from Las Vegas Bay and semipermeable membrane devices from Las Vegas Wash, Nevada","interactions":[],"lastModifiedDate":"2021-05-27T17:40:03.248634","indexId":"70032654","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3352,"text":"Science of the Total Environment","active":true,"publicationSubtype":{"id":10}},"title":"Identification of methyl triclosan and halogenated analogues in male common carp (Cyprinus carpio) from Las Vegas Bay and semipermeable membrane devices from Las Vegas Wash, Nevada","docAbstract":"Methyl triclosan and four halogenated analogues have been identified in extracts of individual whole-body male carp (Cyprinus carpio) tissue that were collected from Las Vegas Bay, Nevada, and Semipermeable Membrane Devices (SPMD) that were deployed in Las Vegas Wash, Nevada. Methyl triclosan is believed to be the microbially methylated product of the antibacterial agent triclosan (2, 4, 4'-trichloro-4-hydroxydiphenyl ether, Chemical Abstract Service Registry Number 3380-34-5, Irgasan DP300). The presence of methyl triclosan and four halogenated analogues was confirmed in SPMD extracts by comparing low- and high-resolution mass spectral data and Kovats retention indices of methyl triclosan with commercially obtained triclosan that was derivatized to the methyl ether with ethereal diazomethane. The four halogenated analogues of methyl triclosan detected in both whole-body tissue and SPMD extracts were tentatively identified by high resolution mass spectrometry. Methyl triclosan was detected in all 29 male common carp from Las Vegas Bay with a mean concentration of 596????g kg- 1 wet weight (ww) which is more than an order of magnitude higher than previously reported concentrations in the literature. The halogenated analogs were detected less frequently (21%-76%) and at much lower concentrations (< 51????g kg- 1 ww). None of these compounds were detected in common carp from a Lake Mead reference site in Overton Arm, Nevada.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Science of the Total Environment","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.scitotenv.2008.11.009","issn":"00489","usgsCitation":"Leiker, T., Abney, S., Goodbred, S.L., and Rosen, M.R., 2009, Identification of methyl triclosan and halogenated analogues in male common carp (Cyprinus carpio) from Las Vegas Bay and semipermeable membrane devices from Las Vegas Wash, Nevada: Science of the Total Environment, v. 407, no. 6, p. 2102-2114, https://doi.org/10.1016/j.scitotenv.2008.11.009.","startPage":"2102","endPage":"2114","numberOfPages":"13","costCenters":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true}],"links":[{"id":241455,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":213796,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.scitotenv.2008.11.009"}],"volume":"407","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3832e4b0c8380cd614a1","contributors":{"authors":[{"text":"Leiker, T.J.","contributorId":96719,"corporation":false,"usgs":true,"family":"Leiker","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":437295,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Abney, S.R.","contributorId":103094,"corporation":false,"usgs":true,"family":"Abney","given":"S.R.","email":"","affiliations":[],"preferred":false,"id":437296,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goodbred, S. L.","contributorId":58232,"corporation":false,"usgs":true,"family":"Goodbred","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":437294,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rosen, Michael R.","contributorId":43096,"corporation":false,"usgs":true,"family":"Rosen","given":"Michael","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":437293,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70032655,"text":"70032655 - 2009 - Seasonal stability of Cladophora-associated Salmonella in Lake Michigan watersheds","interactions":[],"lastModifiedDate":"2012-03-12T17:21:23","indexId":"70032655","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3716,"text":"Water Research","onlineIssn":"1879-2448","printIssn":"0043-1354","active":true,"publicationSubtype":{"id":10}},"title":"Seasonal stability of Cladophora-associated Salmonella in Lake Michigan watersheds","docAbstract":"The bacterial pathogens Shigella, Salmonella, Campylobacter, and shiga toxin-producing E. coli (STEC) were recently found to be associated with Cladophora growing in southern Lake Michigan. Preliminary results indicated that the Salmonella strains associated with Cladophora were genetically identical to each other. However, because of the small sample size (n = 37 isolates) and a lack of information on spatial-temporal relationships, the nature of the association between Cladophora and Salmonella remained speculative. In this study, we investigated the population structure and genetic relatedness of a large number of Cladophora-borne Salmonella isolates from Lake Michigan (n = 133), as well as those isolated from stream and lake water (n = 31), aquatic plants (n = 8), and beach sands and sediments (n = 8) from adjacent watersheds. Salmonella isolates were collected during 2005-2007 between May and August from Lake Michigan beachsheds in Wisconsin, Illinois, and Indiana. The genetic relatedness of Salmonella isolates was examined by using the horizontal, fluorophore-enhanced rep-PCR (HFERP) DNA fingerprinting technique. While the Salmonella isolates associated with Cladophora exhibited a high degree of genetic relatedness (???92% similarity), the isolates were not all genetically identical. Spatial and temporal relationships were evident in the populations examined, with tight clustering of the isolates both by year and location. These findings suggest that the relationship between Salmonella and Cladophora is likely casual and is related to input sources (e.g. wastewater, runoff, birds) and the predominant Salmonella genotype surviving in the environment during a given season. Our studies indicate that Cladophora is likely an important reservoir for Salmonella and other enteric bacterial pathogens in Lake Michigan beachsheds, which in turn may influence nearshore water quality. ?? 2008 Elsevier Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Water Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.watres.2008.11.012","issn":"00431","usgsCitation":"Byappanahalli, M., Sawdey, R., Ishii, S., Shively, D., Ferguson, J., Whitman, R., and Sadowsky, M., 2009, Seasonal stability of Cladophora-associated Salmonella in Lake Michigan watersheds: Water Research, v. 43, no. 3, p. 806-814, https://doi.org/10.1016/j.watres.2008.11.012.","startPage":"806","endPage":"814","numberOfPages":"9","costCenters":[],"links":[{"id":241456,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":213797,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.watres.2008.11.012"}],"volume":"43","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b88d9e4b08c986b316bd6","contributors":{"authors":[{"text":"Byappanahalli, M.N.","contributorId":11384,"corporation":false,"usgs":true,"family":"Byappanahalli","given":"M.N.","email":"","affiliations":[],"preferred":false,"id":437297,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sawdey, R.","contributorId":35962,"corporation":false,"usgs":true,"family":"Sawdey","given":"R.","email":"","affiliations":[],"preferred":false,"id":437299,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ishii, S.","contributorId":59613,"corporation":false,"usgs":true,"family":"Ishii","given":"S.","email":"","affiliations":[],"preferred":false,"id":437300,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Shively, D.A.","contributorId":78123,"corporation":false,"usgs":true,"family":"Shively","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":437302,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ferguson, J.A.","contributorId":100621,"corporation":false,"usgs":true,"family":"Ferguson","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":437303,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Whitman, R.L.","contributorId":69750,"corporation":false,"usgs":true,"family":"Whitman","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":437301,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Sadowsky, M.J.","contributorId":19337,"corporation":false,"usgs":true,"family":"Sadowsky","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":437298,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70032721,"text":"70032721 - 2009 - Flow and geochemistry of groundwater beneath a back-barrier lagoon: The subterranean estuary at Chincoteague Bay, Maryland, USA","interactions":[],"lastModifiedDate":"2018-10-05T10:18:08","indexId":"70032721","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2662,"text":"Marine Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Flow and geochemistry of groundwater beneath a back-barrier lagoon: The subterranean estuary at Chincoteague Bay, Maryland, USA","docAbstract":"<p><span>To better understand large-scale interactions between fresh and saline groundwater beneath an Atlantic coastal estuary, an offshore drilling and sampling study was performed in a large barrier-bounded lagoon, Chincoteague Bay, Maryland, USA. Groundwater that was significantly fresher than overlying bay water was found in shallow plumes up to 8&nbsp;m thick extending more than 1700&nbsp;m offshore. Groundwater saltier than bay surface water was found locally beneath the lagoon and the barrier island, indicating recharge by saline water concentrated by evaporation prior to infiltration. Steep salinity and nutrient gradients occur within a few meters of the sediment surface in most locations studied, with buried peats and estuarine muds acting as confining units. Groundwater ages were generally more than 50&nbsp;years in both fresh and brackish waters as deep as 23&nbsp;m below the bay bottom. Water chemistry and isotopic data indicate that freshened plumes beneath the estuary are mixtures of water originally recharged on land and varying amounts of estuarine surface water that circulated through the bay floor, possibly at some distance from the sampling location. Ammonium is the dominant fixed nitrogen species in saline groundwater beneath the estuary at the locations sampled. Isotopic and dissolved-gas data from one location indicate that denitrification within the subsurface flow system removed terrestrial nitrate from fresh groundwater prior to discharge along the western side of the estuary. Similar situations, with one or more shallow semi-confined flow systems where groundwater geochemistry is strongly influenced by circulation of surface estuary water through organic-rich sediments, may be common on the Atlantic margin and elsewhere.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.marchem.2009.01.004","issn":"03044","usgsCitation":"Bratton, J., Böhlke, J., Krantz, D., and Tobias, C., 2009, Flow and geochemistry of groundwater beneath a back-barrier lagoon: The subterranean estuary at Chincoteague Bay, Maryland, USA: Marine Chemistry, v. 113, no. 1-2, p. 78-92, https://doi.org/10.1016/j.marchem.2009.01.004.","productDescription":"15 p.","startPage":"78","endPage":"92","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":476365,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://hdl.handle.net/1912/2963","text":"External Repository"},{"id":241424,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":213767,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.marchem.2009.01.004"}],"volume":"113","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1238e4b0c8380cd54210","contributors":{"authors":[{"text":"Bratton, J.F.","contributorId":94354,"corporation":false,"usgs":true,"family":"Bratton","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":437627,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Böhlke, J.K. 0000-0001-5693-6455","orcid":"https://orcid.org/0000-0001-5693-6455","contributorId":96696,"corporation":false,"usgs":true,"family":"Böhlke","given":"J.K.","affiliations":[],"preferred":false,"id":437628,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krantz, D.E.","contributorId":9838,"corporation":false,"usgs":true,"family":"Krantz","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":437626,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tobias, C.R.","contributorId":9442,"corporation":false,"usgs":true,"family":"Tobias","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":437625,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70032745,"text":"70032745 - 2009 - Effects of the herbicide diuron on cordgrass (Spartina foliosa) reflectance and photosynthetic parameters","interactions":[],"lastModifiedDate":"2018-10-15T06:54:11","indexId":"70032745","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1584,"text":"Estuaries and Coasts","active":true,"publicationSubtype":{"id":10}},"title":"Effects of the herbicide diuron on cordgrass (Spartina foliosa) reflectance and photosynthetic parameters","docAbstract":"<p><span>Early indicators of salt marsh plant stress are needed to detect stress before it is manifested as changes in biomass and coverage. We explored a variety of leaf-level spectral reflectance and fluorescence variables as indicators of stress in response to the herbicide diuron. Diuron, a Photosystem II inhibitor, is heavily used in areas adjacent to estuaries, but its ecological effects are just beginning to be recognized. In a greenhouse experiment, we exposed&nbsp;</span><i class=\"EmphasisTypeItalic \">Spartina foliosa</i><span>, the native cordgrass in California salt marshes, to two levels of diuron. After plant exposure to diuron for 28&nbsp;days, all spectral reflectance indices and virtually all fluorescence parameters indicated reduced pigment and photosynthetic function, verified as reduced CO</span><sub>2</sub><span>&nbsp;assimilation. Diuron exposure was not evident, however, in plant morphometry, indicating that reflectance and fluorescence were effective indicators of sub-lethal diuron exposure. Several indices (spectral reflectance index ARI and fluorescence parameters EQY, Fo, and maximum rETR) were sensitive to diuron concentration. In field trials, most of the indices as well as biomass, % cover, and canopy height varied predictably and significantly across a pesticide gradient. In the field, ARI and Fo regressed most significantly and strongly with pesticide levels. The responses of ARI and Fo in both the laboratory and the field make these indices promising as sensitive, rapid, non-destructive indicators of responses of&nbsp;</span><i class=\"EmphasisTypeItalic \">S. foliosa</i><span>&nbsp;to herbicides in the field. These techniques are employed in remote sensing and could potentially provide a link between landscapes of stressed vegetation and the causative stressor(s), which is crucial for effective regulation of pollution.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s12237-008-9114-z","issn":"15592","usgsCitation":"Williams, S., Carranza, A., Kunzelman, J., Datta, S., and Kuivila, K., 2009, Effects of the herbicide diuron on cordgrass (Spartina foliosa) reflectance and photosynthetic parameters: Estuaries and Coasts, v. 32, no. 1, p. 146-157, https://doi.org/10.1007/s12237-008-9114-z.","productDescription":"12 p.","startPage":"146","endPage":"157","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":241772,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":214084,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s12237-008-9114-z"}],"volume":"32","issue":"1","noUsgsAuthors":false,"publicationDate":"2008-11-14","publicationStatus":"PW","scienceBaseUri":"505a0805e4b0c8380cd51931","contributors":{"authors":[{"text":"Williams, S.L.","contributorId":71398,"corporation":false,"usgs":true,"family":"Williams","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":437714,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carranza, A.","contributorId":84076,"corporation":false,"usgs":true,"family":"Carranza","given":"A.","email":"","affiliations":[],"preferred":false,"id":437715,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kunzelman, J.","contributorId":39206,"corporation":false,"usgs":true,"family":"Kunzelman","given":"J.","email":"","affiliations":[],"preferred":false,"id":437713,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Datta, S.","contributorId":19754,"corporation":false,"usgs":true,"family":"Datta","given":"S.","email":"","affiliations":[],"preferred":false,"id":437711,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kuivila, Kathryn 0000-0001-7940-489X kkuivila@usgs.gov","orcid":"https://orcid.org/0000-0001-7940-489X","contributorId":190790,"corporation":false,"usgs":true,"family":"Kuivila","given":"Kathryn","email":"kkuivila@usgs.gov","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true},{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":437712,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70032748,"text":"70032748 - 2009 - Potential effects of mercury on threatened California black rails","interactions":[],"lastModifiedDate":"2017-08-26T13:53:48","indexId":"70032748","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":887,"text":"Archives of Environmental Contamination and Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Potential effects of mercury on threatened California black rails","docAbstract":"San Francisco Bay (SFB) estuary sediments contain high levels of mercury (Hg), and tidal marsh resident species may be vulnerable to Hg contamination. We examined Hg concentrations in California black rails, a threatened waterbird species that inhabits SFB tidal salt marshes. We captured 127 black rails during the prebreeding and postbreeding seasons and examined the influence of site, sex, and year on Hg, methylmercury (MeHg), and also selenium (Se) concentrations in feathers and blood. Feather Hg concentrations averaged 6.94 ??g/g dry weight (dw) and MeHg and Se concentrations in blood averaged 0.38 and 0.42 ??g/g wet weight (ww). We used Akaike's information criterion model selection process to evaluate the importance of year, site, sex, and age on patterns of MeHg concentrations; sex and year were the most important of these factors. Feather Hg concentrations (dw) were higher in males (8.22 ??g/g) than females (6.63 ??g/g) and higher in adult birds (7.36 ??g/g) than in hatch-year birds (4.61 ??g/g). A substantial portion of SFB black rail populations may be at risk of reproductive effects due to MeHg contamination, as 32-78% of feathers and <10% of blood samples exceeded no observed adverse effect levels. Sea level rise and other anthropogenic threats to endemic tidal marsh species such as black rails may be exacerbated by the presence of MeHg. Further study of population demographics and toxicological effects would further elucidate the effects of MeHg contamination on black rail populations in SFB. ?? 2008 Springer Science+Business Media, LLC.","language":"English","publisher":"Springer","doi":"10.1007/s00244-008-9188-4","issn":"00904","usgsCitation":"Tsao, D.C., Miles, A.K., Takekawa, J.Y., and Woo, I., 2009, Potential effects of mercury on threatened California black rails: Archives of Environmental Contamination and Toxicology, v. 56, no. 2, p. 292-301, https://doi.org/10.1007/s00244-008-9188-4.","productDescription":"10 p.","startPage":"292","endPage":"301","costCenters":[],"links":[{"id":241265,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"56","issue":"2","noUsgsAuthors":false,"publicationDate":"2008-07-22","publicationStatus":"PW","scienceBaseUri":"505a7ed9e4b0c8380cd7a7b5","contributors":{"authors":[{"text":"Tsao, Danika C.","contributorId":24079,"corporation":false,"usgs":true,"family":"Tsao","given":"Danika","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":437728,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miles, A. Keith 0000-0002-3108-808X keith_miles@usgs.gov","orcid":"https://orcid.org/0000-0002-3108-808X","contributorId":196,"corporation":false,"usgs":true,"family":"Miles","given":"A.","email":"keith_miles@usgs.gov","middleInitial":"Keith","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":437729,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Takekawa, John Y. 0000-0003-0217-5907 john_takekawa@usgs.gov","orcid":"https://orcid.org/0000-0003-0217-5907","contributorId":176168,"corporation":false,"usgs":true,"family":"Takekawa","given":"John","email":"john_takekawa@usgs.gov","middleInitial":"Y.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":437727,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Woo, Isa 0000-0002-8447-9236 iwoo@usgs.gov","orcid":"https://orcid.org/0000-0002-8447-9236","contributorId":2524,"corporation":false,"usgs":true,"family":"Woo","given":"Isa","email":"iwoo@usgs.gov","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":437726,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70032749,"text":"70032749 - 2009 - Forecasting the combined effects of urbanization and climate change on stream ecosystems: from impacts to management options","interactions":[],"lastModifiedDate":"2015-05-14T13:06:01","indexId":"70032749","displayToPublicDate":"2009-01-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2163,"text":"Journal of Applied Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Forecasting the combined effects of urbanization and climate change on stream ecosystems: from impacts to management options","docAbstract":"<p>&nbsp;</p>\n<ol>\n<li>Streams collect runoff, heat, and sediment from their watersheds, making them highly vulnerable to anthropogenic disturbances such as urbanization and climate change. Forecasting the effects of these disturbances using process-based models is critical to identifying the form and magnitude of likely impacts. Here, we integrate a new biotic model with four previously developed physical models (downscaled climate projections, stream hydrology, geomorphology, and water temperature) to predict how stream fish growth and reproduction will most probably respond to shifts in climate and urbanization over the next several decades.</li>\n<li>The biotic submodel couples dynamics in fish populations and habitat suitability to predict fish assemblage composition, based on readily available biotic information (preferences for habitat, temperature, and food, and characteristics of spawning) and day-to-day variability in stream conditions.</li>\n<li>We illustrate the model using Piedmont headwater streams in the Chesapeake Bay watershed of the USA, projecting ten scenarios: Baseline (low urbanization; no on-going construction; and present-day climate); one Urbanization scenario (higher impervious surface, lower forest cover, significant construction activity); four future climate change scenarios [Hadley CM3 and Parallel Climate Models under medium-high (A2) and medium-low (B2) emissions scenarios]; and the same four climate change scenarios plus Urbanization.</li>\n<li>Urbanization alone depressed growth or reproduction of 8 of 39 species, while climate change alone depressed 22 to 29 species. Almost every recreationally important species (i.e. trouts, basses, sunfishes) and six of the ten currently most common species were predicted to be significantly stressed. The combined effect of climate change and urbanization on adult growth was sometimes large compared to the effect of either stressor alone. Thus, the model predicts considerable change in fish assemblage composition, including loss of diversity.</li>\n<li><i>Synthesis and applications</i>. The interaction of climate change and urban growth may entail significant reconfiguring of headwater streams, including a loss of ecosystem structure and services, which will be more costly than climate change alone. On local scales, stakeholders cannot control climate drivers but they can mitigate stream impacts via careful land use. Therefore, to conserve stream ecosystems, we recommend that proactive measures be taken to insure against species loss or severe population declines. Delays will inevitably exacerbate the impacts of both climate change and urbanization on headwater systems.</li>\n</ol>","language":"English","publisher":"Wiley-Blackwell Publishing Ltd.","doi":"10.1111/j.1365-2664.2008.01599.x","issn":"00218","usgsCitation":"Nelson, K.C., Palmer, M., Pizzuto, J.E., Moglen, G.E., Angermeier, P.L., Hilderbrand, R.H., Dettinger, M., and Hayhoe, K., 2009, Forecasting the combined effects of urbanization and climate change on stream ecosystems: from impacts to management options: Journal of Applied Ecology, v. 46, no. 1, p. 154-163, https://doi.org/10.1111/j.1365-2664.2008.01599.x.","productDescription":"10 p.","startPage":"154","endPage":"163","numberOfPages":"10","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":476129,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1365-2664.2008.01599.x","text":"Publisher Index Page"},{"id":241294,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":213646,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1365-2664.2008.01599.x"}],"country":"United States","state":"Maryland","otherGeospatial":"Chesapeake Bay watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.03956604003905,\n              38.99517305687675\n            ],\n            [\n              -77.244873046875,\n              39.01384869832171\n            ],\n            [\n              -77.24555969238281,\n              39.027718840211605\n            ],\n            [\n              -77.34374999999999,\n              39.06291544026173\n            ],\n            [\n              -77.46322631835938,\n              39.07890809706475\n            ],\n            [\n              -77.45773315429688,\n              39.24501680713314\n            ],\n            [\n              -77.14874267578124,\n              39.358723461000494\n            ],\n            [\n              -76.98257446289062,\n              39.3130504637139\n            ],\n            [\n              -76.97433471679688,\n              39.11088253765176\n            ],\n            [\n              -77.03956604003905,\n              38.99517305687675\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"46","issue":"1","noUsgsAuthors":false,"publicationDate":"2009-01-14","publicationStatus":"PW","scienceBaseUri":"505a131ae4b0c8380cd5450e","contributors":{"authors":[{"text":"Nelson, Karen C.","contributorId":32864,"corporation":false,"usgs":false,"family":"Nelson","given":"Karen","email":"","middleInitial":"C.","affiliations":[{"id":7083,"text":"University of Maryland","active":true,"usgs":false}],"preferred":false,"id":437732,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Palmer, Margaret A.","contributorId":102429,"corporation":false,"usgs":false,"family":"Palmer","given":"Margaret A.","affiliations":[{"id":13383,"text":"University of Maryland Center for Environmental Science, Chesapeake Biological Laboratory, 6 Solomons, Maryland 20688","active":true,"usgs":false}],"preferred":false,"id":437736,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pizzuto, James E.","contributorId":49424,"corporation":false,"usgs":false,"family":"Pizzuto","given":"James","email":"","middleInitial":"E.","affiliations":[{"id":13220,"text":"The Charles E. 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