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,{"id":70198588,"text":"70198588 - 2006 - Attention of arsenic in Bangladesh sediments: Implications for ground-water development","interactions":[],"lastModifiedDate":"2018-08-13T10:16:42","indexId":"70198588","displayToPublicDate":"2006-01-01T07:31:45","publicationYear":"2006","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Attention of arsenic in Bangladesh sediments: Implications for ground-water development","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Managing arsenic in the environment: From soil to human health","language":"English","publisher":"CSIRO","publisherLocation":"Australia","isbn":"0643068686","usgsCitation":"Welch, A., Stollenwerk, K.G., Breit, G.N., Foster, A., Yount, J.C., Whitney, J., Uddin, M., and Alam, A., 2006, Attention of arsenic in Bangladesh sediments: Implications for ground-water development, chap. <i>of</i> Managing arsenic in the environment: From soil to human health, p. 363-377.","productDescription":"15 p.","startPage":"363","endPage":"377","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":356362,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Bangladesh ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              87.6708984375,\n              21.08450008351735\n            ],\n            [\n              92.4169921875,\n              21.08450008351735\n            ],\n            [\n              92.4169921875,\n              26.745610382199022\n            ],\n            [\n              87.6708984375,\n              26.745610382199022\n            ],\n            [\n              87.6708984375,\n              21.08450008351735\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5b98c454e4b0702d0e846159","contributors":{"authors":[{"text":"Welch, A. H.","contributorId":14836,"corporation":false,"usgs":true,"family":"Welch","given":"A. H.","affiliations":[],"preferred":false,"id":742065,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stollenwerk, Kenneth G. kgstolle@usgs.gov","contributorId":578,"corporation":false,"usgs":true,"family":"Stollenwerk","given":"Kenneth","email":"kgstolle@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":742066,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Breit, George N. 0000-0003-2188-6798 gbreit@usgs.gov","orcid":"https://orcid.org/0000-0003-2188-6798","contributorId":1480,"corporation":false,"usgs":true,"family":"Breit","given":"George","email":"gbreit@usgs.gov","middleInitial":"N.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":742067,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Foster, A. L. 0000-0003-1362-0068","orcid":"https://orcid.org/0000-0003-1362-0068","contributorId":17190,"corporation":false,"usgs":true,"family":"Foster","given":"A. L.","affiliations":[],"preferred":false,"id":742068,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Yount, J. C.","contributorId":69553,"corporation":false,"usgs":true,"family":"Yount","given":"J.","middleInitial":"C.","affiliations":[],"preferred":false,"id":742069,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Whitney, J.W.","contributorId":27437,"corporation":false,"usgs":true,"family":"Whitney","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":742070,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Uddin, M.N.","contributorId":105979,"corporation":false,"usgs":true,"family":"Uddin","given":"M.N.","email":"","affiliations":[],"preferred":false,"id":742071,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Alam, A.M.","contributorId":46975,"corporation":false,"usgs":true,"family":"Alam","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":742072,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70188286,"text":"70188286 - 2006 - Tracermodel1- Excel workbook for calculation and presentation of environmental tracer data for simple groundwater mixtures: Use of chlorofluorocarbons in hydrology - a guidebook; Section III.10.3","interactions":[],"lastModifiedDate":"2017-06-05T13:56:15","indexId":"70188286","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Tracermodel1- Excel workbook for calculation and presentation of environmental tracer data for simple groundwater mixtures: Use of chlorofluorocarbons in hydrology - a guidebook; Section III.10.3","docAbstract":"<p>Atmospheric environmental tracers commonly used to date groundwater on timescales of years to decades include CFC-11, CFC-12, CFC-113, SF6, 85Kr, 3 H and 3 H/3 H0 , where 3 H0 refers to initial tritium (3 H + tritiogenic 3 He) (Cook and Herczeg, 2000). Interpretation of age from environmental tracer data may be relatively simple for a water sample with a single age, but the interpretation is more complex for a sample that is a mixture of waters of varying ages. A mixture can be a natural result of convergence of flow lines to a discharge area such as a spring or stream, or it can be an artefact of sampling a long-screen well. TRACERMODEL1 contains a worksheet that can be used to determine hypothetical concentrations of atmospheric environmental tracers in water samples with several different age distributions. It is designed to permit plotting of ages and tracer concentrations in a variety of different combinations to facilitate interpretation of measurements. TRACERMODEL1 includes several different types of graphs that are linked to the calculations. The spreadsheet and accompanying graphs can be modified for specific applications. For example, the selection of atmospheric environmental tracers can be changed to reflect analytes of interest, the input tracer data can be modified to reflect local conditions or different timescales, and the analytes of interest can include other types of non-point-source contaminants, such as nitrate (Böhlke, 2002). Previous versions of this workbook have been used to evaluate field data in studies of groundwater residence time and agricultural contamination (Böhlke and Denver, 1995; Focazio et al., 1998; Katz et al., 1999; Katz et al., 2001; Plummer et al., 2001; Böhlke and Krantz, 2003; Lindsey et al., 2003). </p>","language":"English","publisher":"International Atomic Energy Agency","usgsCitation":"Bohlke, J., 2006, Tracermodel1- Excel workbook for calculation and presentation of environmental tracer data for simple groundwater mixtures: Use of chlorofluorocarbons in hydrology - a guidebook; Section III.10.3, 5 p.","productDescription":"5 p.","startPage":"239","endPage":"243","costCenters":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"links":[{"id":342110,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":342109,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www-pub.iaea.org/MTCD/publications/PDF/Pub1238_web.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59366daee4b0f6c2d0d7d64e","contributors":{"authors":[{"text":"Bohlke, J.K. 0000-0001-5693-6455 jkbohlke@usgs.gov","orcid":"https://orcid.org/0000-0001-5693-6455","contributorId":191103,"corporation":false,"usgs":true,"family":"Bohlke","given":"J.K.","email":"jkbohlke@usgs.gov","affiliations":[{"id":36183,"text":"Hydro-Ecological Interactions Branch","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":697131,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175732,"text":"70175732 - 2006 - Hydroecological modeling of the Lower Missouri River","interactions":[],"lastModifiedDate":"2017-05-24T14:37:30","indexId":"70175732","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Hydroecological modeling of the Lower Missouri River","docAbstract":"<p>No abstract avaikable&nbsp;</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the third federal interagency hydrologic modeling conference","conferenceTitle":"Third federal interagency hydrologic modeling conference","conferenceLocation":"Reno, NV","language":"English","usgsCitation":"Johnson, H., Jacobson, R., and DeLonay, A., 2006, Hydroecological modeling of the Lower Missouri River, <i>in</i> Proceedings of the third federal interagency hydrologic modeling conference, Reno, NV, p. 1-8.","productDescription":"8 p.","startPage":"1","endPage":"8","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":326848,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b6dc66e4b03fd6b7d94c50","contributors":{"authors":[{"text":"Johnson, H.E.","contributorId":56757,"corporation":false,"usgs":true,"family":"Johnson","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":646220,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jacobson, R. B. 0000-0002-8368-2064","orcid":"https://orcid.org/0000-0002-8368-2064","contributorId":92614,"corporation":false,"usgs":true,"family":"Jacobson","given":"R. B.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":646221,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"DeLonay, A. J. 0000-0002-3752-2799","orcid":"https://orcid.org/0000-0002-3752-2799","contributorId":34246,"corporation":false,"usgs":true,"family":"DeLonay","given":"A. J.","affiliations":[],"preferred":false,"id":646222,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1001059,"text":"1001059 - 2006 - Forecasting effects of climate change on Great Lakes fisheries: models that link habitat supply to population dynamics can help","interactions":[],"lastModifiedDate":"2016-05-09T09:13:01","indexId":"1001059","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1169,"text":"Canadian Journal of Fisheries and Aquatic Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Forecasting effects of climate change on Great Lakes fisheries: models that link habitat supply to population dynamics can help","docAbstract":"<p><span>Future changes to climate in the Great Lakes may have important consequences for fisheries. Evidence suggests that Great Lakes air and water temperatures have risen and the duration of ice cover has lessened during the past century. Global circulation models (GCMs) suggest future warming and increases in precipitation in the region. We present new evidence that water temperatures have risen in Lake Erie, particularly during summer and winter in the period 19652000. GCM forecasts coupled with physical models suggest lower annual runoff, less ice cover, and lower lake levels in the future, but the certainty of these forecasts is low. Assessment of the likely effects of climate change on fish stocks will require an integrative approach that considers several components of habitat rather than water temperature alone. We recommend using mechanistic models that couple habitat conditions to population demographics to explore integrated effects of climate-caused habitat change and illustrate this approach with a model for Lake Erie walleye (</span><i>Sander vitreum</i><span>). We show that the combined effect on walleye populations of plausible changes in temperature, river hydrology, lake levels, and light penetration can be quite different from that which would be expected based on consideration of only a single factor.</span></p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/f05-239","usgsCitation":"Jones, M., Shuter, B.J., Zhao, Y., and Stockwell, J.D., 2006, Forecasting effects of climate change on Great Lakes fisheries: models that link habitat supply to population dynamics can help: Canadian Journal of Fisheries and Aquatic Sciences, v. 63, no. 2, p. 457-468, https://doi.org/10.1139/f05-239.","productDescription":"12 p.","startPage":"457","endPage":"468","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133279,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"63","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae519","contributors":{"authors":[{"text":"Jones, Michael L.","contributorId":7219,"corporation":false,"usgs":false,"family":"Jones","given":"Michael L.","affiliations":[{"id":6590,"text":"Department of Fisheries and Wildlife, Michigan State University","active":true,"usgs":false}],"preferred":false,"id":310364,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shuter, Brian J.","contributorId":29372,"corporation":false,"usgs":true,"family":"Shuter","given":"Brian","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":310365,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zhao, Yingming","contributorId":49752,"corporation":false,"usgs":true,"family":"Zhao","given":"Yingming","affiliations":[],"preferred":false,"id":310366,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stockwell, Jason D. 0000-0003-3393-6799","orcid":"https://orcid.org/0000-0003-3393-6799","contributorId":61004,"corporation":false,"usgs":false,"family":"Stockwell","given":"Jason","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":310367,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70028440,"text":"70028440 - 2006 - Increasing streamflow and baseflow in Mississippi River since the 1940 s: Effect of land use change","interactions":[],"lastModifiedDate":"2012-03-12T17:20:54","indexId":"70028440","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Increasing streamflow and baseflow in Mississippi River since the 1940 s: Effect of land use change","docAbstract":"A trend of increasing streamflow has been observed in the Mississippi River (MR) basin since the 1940 s as a result of increased precipitation. Herein we show that increasing MR flow is mainly in its baseflow as a result of land use change and accompanying agricultural activities that occurred in the MR basin during the last 60 years. Agricultural land use change in the MR basin has affected the basin-scale hydrology: more precipitation is being routed into streams as baseflow than stormflow since 1940 s. We explain that the conversion of perennial vegetation to seasonal row crops, especially soybeans, in the basin since 1940 s may have reduced evapotranspiration, increased groundwater recharge, and thus increased baseflow and streamflow. This explanation is supported with a data analysis of the annually and monthly flow rates at various river stations in the MR basin. Results from this study will help to direct our effort in managing land use and in reducing nutrient levels in MR and other major rivers since nutrient concentrations and loads carried by storm water and baseflow are different. ?? 2005 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Hydrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.jhydrol.2005.09.033","issn":"00221694","usgsCitation":"Zhang, Y., and Schilling, K.E., 2006, Increasing streamflow and baseflow in Mississippi River since the 1940 s: Effect of land use change: Journal of Hydrology, v. 324, no. 1-4, p. 412-422, https://doi.org/10.1016/j.jhydrol.2005.09.033.","startPage":"412","endPage":"422","numberOfPages":"11","costCenters":[],"links":[{"id":210300,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jhydrol.2005.09.033"},{"id":237178,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"324","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3a07e4b0c8380cd61b12","contributors":{"authors":[{"text":"Zhang, Y.-K.","contributorId":44309,"corporation":false,"usgs":true,"family":"Zhang","given":"Y.-K.","email":"","affiliations":[],"preferred":false,"id":418056,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schilling, K. E.","contributorId":61982,"corporation":false,"usgs":true,"family":"Schilling","given":"K.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":418057,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028429,"text":"70028429 - 2006 - Measuring permanence of CO<sub>2</sub> storage in saline formations: The Frio experiment","interactions":[],"lastModifiedDate":"2018-10-29T09:50:53","indexId":"70028429","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1541,"text":"Environmental Geosciences","active":true,"publicationSubtype":{"id":10}},"title":"Measuring permanence of CO<sub>2</sub> storage in saline formations: The Frio experiment","docAbstract":"<p class=\"abstractnoin\">If CO<sub>2</sub> released from fossil fuel during energy production is returned to the subsurface, will it be retained for periods of time significant enough to benefit the atmosphere? Can trapping be assured in saline formations where there is no history of hydrocarbon accumulation? The Frio experiment in Texas was undertaken to provide answers to these questions.</p><p>One thousand six hundred metric tons of CO<sub>2</sub> were injected into the Frio Formation, which underlies large areas of the United States Gulf Coast. Reservoir characterization and numerical modeling were used to design the experiment, as well as to interpret the results through history matching. Closely spaced measurements in space and time were collected to observe the evolution of immiscible and dissolved CO<sub>2</sub> during and after injection. The high-permeability, steeply dipping sandstone allowed updip flow of supercritical CO<sub>2</sub> as a result of the density contrast with formation brine and absence of a local structural trap.</p><p>The front of the CO<sub>2</sub> plume moved more quickly than had been modeled. By the end of the 10-day injection, however, the plume geometry in the plane of the observation and injection wells had thickened to a distribution similar to the modeled distribution. As expected, CO<sub>2</sub> dissolved rapidly into brine, causing pH to fall and calcite and metals to be dissolved.</p><p>Postinjection measurements, including time-lapse vertical seismic profiling transects along selected azimuths, cross-well seismic topography, and saturation logs, show that CO<sub>2</sub> migration under gravity slowed greatly 2 months after injection, matching model predictions that significant CO<sub>2</sub> is trapped as relative permeability decreases.</p>","language":"English","publisher":"Blackwell Science","doi":"10.1306/eg.11210505011","issn":"10759565","usgsCitation":"Hovorka, S.D., Benson, S.M., Doughty, C., Freifeild, B.M., Sakurai, S., Daley, T.M., Kharaka, Y.K., Holtz, M.H., Trautz, R.C., Nance, H.S., Myer, L.R., and Knauss, K.G., 2006, Measuring permanence of CO<sub>2</sub> storage in saline formations: The Frio experiment: Environmental Geosciences, v. 13, no. 2, p. 105-121, https://doi.org/10.1306/eg.11210505011.","productDescription":"17 p.","startPage":"105","endPage":"121","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":237036,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a534de4b0c8380cd6c9af","contributors":{"authors":[{"text":"Hovorka, Susan D.","contributorId":175572,"corporation":false,"usgs":false,"family":"Hovorka","given":"Susan","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":418020,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Benson, Sally M.","contributorId":177233,"corporation":false,"usgs":false,"family":"Benson","given":"Sally","email":"","middleInitial":"M.","affiliations":[{"id":6670,"text":"Lawrence Berkeley National Laboratory, Berkeley, CA","active":true,"usgs":false}],"preferred":false,"id":418022,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Doughty, Christine","contributorId":175587,"corporation":false,"usgs":false,"family":"Doughty","given":"Christine","email":"","affiliations":[],"preferred":false,"id":418017,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Freifeild, Barry M.","contributorId":42444,"corporation":false,"usgs":false,"family":"Freifeild","given":"Barry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":418012,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sakurai, Shinichi","contributorId":30025,"corporation":false,"usgs":false,"family":"Sakurai","given":"Shinichi","email":"","affiliations":[{"id":12933,"text":"Bureau of Economic Geology, The University of Texas at Austin","active":true,"usgs":false}],"preferred":false,"id":418014,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Daley, Thomas M.","contributorId":175586,"corporation":false,"usgs":false,"family":"Daley","given":"Thomas","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":418016,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kharaka, Yousif K. 0000-0001-9861-8260 ykharaka@usgs.gov","orcid":"https://orcid.org/0000-0001-9861-8260","contributorId":1928,"corporation":false,"usgs":true,"family":"Kharaka","given":"Yousif","email":"ykharaka@usgs.gov","middleInitial":"K.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":418013,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Holtz, Mark H.","contributorId":85384,"corporation":false,"usgs":false,"family":"Holtz","given":"Mark","email":"","middleInitial":"H.","affiliations":[{"id":12933,"text":"Bureau of Economic Geology, The University of Texas at Austin","active":true,"usgs":false}],"preferred":false,"id":418021,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Trautz, Robert C.","contributorId":171754,"corporation":false,"usgs":false,"family":"Trautz","given":"Robert","email":"","middleInitial":"C.","affiliations":[{"id":26941,"text":"Electric Power Research Institute, Palo Alto, CA","active":true,"usgs":false}],"preferred":false,"id":418018,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Nance, H. Seay","contributorId":59310,"corporation":false,"usgs":false,"family":"Nance","given":"H.","email":"","middleInitial":"Seay","affiliations":[{"id":12933,"text":"Bureau of Economic Geology, The University of Texas at Austin","active":true,"usgs":false}],"preferred":false,"id":418015,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Myer, Larry R.","contributorId":177239,"corporation":false,"usgs":false,"family":"Myer","given":"Larry","email":"","middleInitial":"R.","affiliations":[{"id":6670,"text":"Lawrence Berkeley National Laboratory, Berkeley, CA","active":true,"usgs":false}],"preferred":false,"id":418011,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Knauss, Kevin G.","contributorId":177240,"corporation":false,"usgs":false,"family":"Knauss","given":"Kevin","email":"","middleInitial":"G.","affiliations":[{"id":13621,"text":"Lawrence Livermore National Laboratory","active":true,"usgs":false}],"preferred":false,"id":418019,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}}
,{"id":70190595,"text":"70190595 - 2006 - Control of invasive weeds with prescribed burning","interactions":[],"lastModifiedDate":"2017-09-08T14:45:51","indexId":"70190595","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3739,"text":"Weed Technology","onlineIssn":"1550-2740","printIssn":"0890-037X","active":true,"publicationSubtype":{"id":10}},"title":"Control of invasive weeds with prescribed burning","docAbstract":"<p><span>Prescribed burning has primarily been used as a tool for the control of invasive late-season annual broadleaf and grass species, particularly yellow starthistle, medusahead, barb goatgrass, and several bromes. However, timely burning of a few invasive biennial broadleaves (e.g., sweetclover and garlic mustard), perennial grasses (e.g., bluegrasses and smooth brome), and woody species (e.g., brooms and Chinese tallow tree) also has been successful. In many cases, the effectiveness of prescribed burning can be enhanced when incorporated into an integrated vegetation management program. Although there are some excellent examples of successful use of prescribed burning for the control of invasive species, a limited number of species have been evaluated. In addition, few studies have measured the impact of prescribed burning on the long-term changes in plant communities, impacts to endangered plant species, effects on wildlife and insect populations, and alterations in soil biology, including nutrition, mycorrhizae, and hydrology. In this review, we evaluate the current state of knowledge on prescribed burning as a tool for invasive weed management.</span></p>","language":"English","publisher":"Weed Science Society of America","doi":"10.1614/WT-05-086R1.1","usgsCitation":"DiTomaso, J.M., Brooks, M.L., Allen, E.B., Minnich, R., Rice, P.M., and Kyser, G.B., 2006, Control of invasive weeds with prescribed burning: Weed Technology, v. 20, no. 2, p. 535-548, https://doi.org/10.1614/WT-05-086R1.1.","productDescription":"14 p.","startPage":"535","endPage":"548","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":345592,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"2","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"59b3ac34e4b08b1644d8f1c6","contributors":{"authors":[{"text":"DiTomaso, Joseph M.","contributorId":72925,"corporation":false,"usgs":true,"family":"DiTomaso","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":709937,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brooks, Matthew L. 0000-0002-3518-6787 mlbrooks@usgs.gov","orcid":"https://orcid.org/0000-0002-3518-6787","contributorId":393,"corporation":false,"usgs":true,"family":"Brooks","given":"Matthew","email":"mlbrooks@usgs.gov","middleInitial":"L.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":709938,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Allen, Edith B.","contributorId":139341,"corporation":false,"usgs":false,"family":"Allen","given":"Edith","email":"","middleInitial":"B.","affiliations":[{"id":12741,"text":"U of CA Dept of Botany and Plant Sciences","active":true,"usgs":false}],"preferred":false,"id":709939,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Minnich, Ralph","contributorId":196292,"corporation":false,"usgs":false,"family":"Minnich","given":"Ralph","affiliations":[],"preferred":false,"id":709940,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rice, Peter M.","contributorId":196293,"corporation":false,"usgs":false,"family":"Rice","given":"Peter","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":709941,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kyser, Guy B.","contributorId":196294,"corporation":false,"usgs":false,"family":"Kyser","given":"Guy","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":709942,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70035443,"text":"70035443 - 2006 - Geology of the Yucca Mountain region","interactions":[],"lastModifiedDate":"2012-03-12T17:21:54","indexId":"70035443","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2711,"text":"Memoir of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Geology of the Yucca Mountain region","docAbstract":"Yucca Mountain has been proposed as the site for the nation's first geologic repository for high-level radioactive waste. This chapter provides the geologic framework for the Yucca Mountain region. The regional geologic units range in age from late Precambrian through Holocene, and these are described briefly. Yucca Mountain is composed dominantly of pyroclastic units that range in age from 11.4 to 15.2 Ma. The proposed repository would be constructed within the Topopah Spring Tuff, which is the lower of two major zoned and welded ash-flow tuffs within the Paintbrush Group. The two welded tuffs are separated by the partly to nonwelded Pah Canyon Tuff and Yucca Mountain Tuff, which together figure prominently in the hydrology of the unsaturated zone. The Quaternary deposits are primarily alluvial sediments with minor basaltic cinder cones and flows. Both have been studied extensively because of their importance in predicting the long-term performance of the proposed repository. Basaltic volcanism began ca. 10 Ma and continued as recently as ca. 80 ka with the eruption of cones and flows at Lathrop Wells, ???10 km south-southwest of Yucca Mountain. Geologic structure in the Yucca Mountain region is complex. During the latest Paleozoic and Mesozoic, strong compressional forces caused tight folding and thrust faulting. The present regional setting is one of extension, and normal faulting has been active from the Miocene through to the present. There are three major local tectonic domains: (1) Basin and Range, (2) Walker Lane, and (3) Inyo-Mono. Each domain has an effect on the stability of Yucca Mountain. ?? 2007 Geological Society of America. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Memoir of the Geological Society of America","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1130/2007.1199(02)","issn":"00721069","usgsCitation":"Stuckless, J., and O’Leary, D.W., 2006, Geology of the Yucca Mountain region: Memoir of the Geological Society of America, v. 199, p. 9-50, https://doi.org/10.1130/2007.1199(02).","startPage":"9","endPage":"50","numberOfPages":"42","costCenters":[],"links":[{"id":215498,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1130/2007.1199(02)"},{"id":243308,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"199","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a26d4e4b0c8380cd593ad","contributors":{"authors":[{"text":"Stuckless, J. S.","contributorId":6060,"corporation":false,"usgs":true,"family":"Stuckless","given":"J. S.","affiliations":[],"preferred":false,"id":450712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Leary, Dennis W.","contributorId":91501,"corporation":false,"usgs":true,"family":"O’Leary","given":"Dennis","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":450713,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70035442,"text":"70035442 - 2006 - Water-quality characteristics and contaminants in the rural karst-dominated Spring Mill Lake watershed, southern Indiana","interactions":[],"lastModifiedDate":"2012-03-12T17:21:54","indexId":"70035442","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3459,"text":"Special Paper of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Water-quality characteristics and contaminants in the rural karst-dominated Spring Mill Lake watershed, southern Indiana","docAbstract":"The Spring Mill Lake watershed is located in the Mitchell Plateau, a karst area that developed on Mississippian carbonates in southern Indiana. Spring Mill Lake is a reservoir built in the late 1930s and is located in Spring Mill State Park. Within the park, groundwater from subsurface conduits issues as natural springs and then flows in surface streams to the lake. From 1998 to 2002, surface and subsurface hydrology and water quality were investigated to determine the types and sources of potential contaminants entering the lake. Water samples collected during base flow and a February 2000 storm event were analyzed for selected cations, anions, trace elements, selected U.S. Environmental Protection Agency (EPA) primary and secondary drinkingwater contaminants, nitrogen isotopes, suspended solids, Escherichia coli, and pesticides. All of the water samples met the EPA drinking-water standards for inorganic constituents, except those collected at five sites in August 1999 during a drought. Nitrate nitrogen (NO<sub>3</sub>-N) concentrations were highest during base-flow conditions and displayed a dilutional trend during peak-flow periods. The NO<sub>3</sub>-N concentrations in water samples collected during the 2001 spring fertilizer applications tended to increase from early to late spring. All of the ??<sup>15</sup>N values were low, which is indicative of either an inorganic source or soil organic matter. Storm discharge contained increased concentrations of total suspended solids; thus, storms are responsible for most of the sediment accumulation in the lake. E. coli levels in 24% of the samples analyzed contained a most probable number (MPN) greater than 235/100 mL, which is the maximum acceptable level set for recreational waters in Indiana. E. coli does appear to be a potential health risk, particularly at Rubble spring. The sources of E. coli found at this spring may include barnyard runoff from a horse barn or wastes from a wastewater treatment facility. The pesticides atrazine, metolachlor, acetochlor, and simazine were detected during the spring of 2001. Atrazine, metolachlor, acetochlor, and simazine are used to suppress weeds during corn and soybean production. Additional sources of atrazine and simazine may result from application to right-of-ways, orchards, and managed forest areas. ?? 2006 Geological Society of America.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Special Paper of the Geological Society of America","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1130/2006.2404(13)","issn":"00721077","usgsCitation":"Hasenmueller, N., Buehler, M., Krothe, N., Comer, J., Branam, T., Ennis, M., Smith, R., Zamani, D., Hahn, L., and Rybarczyk, J., 2006, Water-quality characteristics and contaminants in the rural karst-dominated Spring Mill Lake watershed, southern Indiana: Special Paper of the Geological Society of America, no. 404, p. 153-167, https://doi.org/10.1130/2006.2404(13).","startPage":"153","endPage":"167","numberOfPages":"15","costCenters":[],"links":[{"id":215469,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1130/2006.2404(13)"},{"id":243277,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"404","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bcdd5e4b08c986b32e0f9","contributors":{"authors":[{"text":"Hasenmueller, N.R.","contributorId":89950,"corporation":false,"usgs":true,"family":"Hasenmueller","given":"N.R.","email":"","affiliations":[],"preferred":false,"id":450710,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buehler, M.A.","contributorId":43588,"corporation":false,"usgs":true,"family":"Buehler","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":450705,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krothe, N.C.","contributorId":76378,"corporation":false,"usgs":true,"family":"Krothe","given":"N.C.","affiliations":[],"preferred":false,"id":450708,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Comer, J.B.","contributorId":34185,"corporation":false,"usgs":true,"family":"Comer","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":450703,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Branam, T.D.","contributorId":52332,"corporation":false,"usgs":true,"family":"Branam","given":"T.D.","email":"","affiliations":[],"preferred":false,"id":450707,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ennis, M.V.","contributorId":100125,"corporation":false,"usgs":true,"family":"Ennis","given":"M.V.","email":"","affiliations":[],"preferred":false,"id":450711,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Smith, R.T.","contributorId":37558,"corporation":false,"usgs":true,"family":"Smith","given":"R.T.","email":"","affiliations":[],"preferred":false,"id":450704,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Zamani, D.D.","contributorId":22127,"corporation":false,"usgs":true,"family":"Zamani","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":450702,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Hahn, L.","contributorId":81327,"corporation":false,"usgs":true,"family":"Hahn","given":"L.","email":"","affiliations":[],"preferred":false,"id":450709,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Rybarczyk, J.P.","contributorId":52006,"corporation":false,"usgs":true,"family":"Rybarczyk","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":450706,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70033636,"text":"70033636 - 2006 - Hydrologic-hydraulic analysis of the Toa Vaca Dam","interactions":[],"lastModifiedDate":"2012-03-12T17:21:30","indexId":"70033636","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Hydrologic-hydraulic analysis of the Toa Vaca Dam","docAbstract":"[No abstract available]","largerWorkTitle":"Association of State Dam Safety Officials - Dam Safety 2006, Proceedings from the 2006 Annual Conference","conferenceTitle":"2006 Annual Conference on Dam Safety","conferenceDate":"10 September 2008 through 14 September 2008","conferenceLocation":"Boston, MA","language":"English","usgsCitation":"Heriberto, T., and MillerArthur, A., 2006, Hydrologic-hydraulic analysis of the Toa Vaca Dam, <i>in</i> Association of State Dam Safety Officials - Dam Safety 2006, Proceedings from the 2006 Annual Conference, Boston, MA, 10 September 2008 through 14 September 2008.","numberOfPages":"1","costCenters":[],"links":[{"id":242026,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a36a5e4b0c8380cd608a2","contributors":{"authors":[{"text":"Heriberto, T.-S.","contributorId":7097,"corporation":false,"usgs":true,"family":"Heriberto","given":"T.-S.","email":"","affiliations":[],"preferred":false,"id":441786,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"MillerArthur, A.C.","contributorId":98130,"corporation":false,"usgs":true,"family":"MillerArthur","given":"A.C.","email":"","affiliations":[],"preferred":false,"id":441787,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70033346,"text":"70033346 - 2006 - Sediment and nutrient accumulation within lowland bottomland ecosystems: An example from the Atchafalaya River Basin, Louisiana","interactions":[],"lastModifiedDate":"2012-03-12T17:21:36","indexId":"70033346","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Sediment and nutrient accumulation within lowland bottomland ecosystems: An example from the Atchafalaya River Basin, Louisiana","docAbstract":"Sediment and nutrient deposition, storage, and transformations are important environmental functions of riverine forested wetland ecosystems, yet documentation and interpretation of sedimentation/nutrient processes remain incomplete. Our studies located in the Coastal Plain of southeastern USA, including the Atchafalaya Basin, La. (a distributary of the Mississippi River) serve as example for detailed discussion of sediment and nutrient accumulation in lowland systems. The Atchafalaya Basin is the largest contiguously forested riparian wetland in North America and is incurring high sediment loads and hypoxic zones in backswamp settings. We established several floodplain transects, located to reflect major depositional environments within the Basin, to monitor general and local sediment deposition patterns over a multi-year period. Deposition rate and loss on ignition (LOI) data were collected above artificial markers (clay pads) at multiple stations along each transect. Mean floodplain sedimentation rates ranged from about 2 to 42 mm/yr and mean percent organic material ranged from about 7 to 28 percent. The transects were categorized into statistically different deposition groups based on sedimentation rate; most of these groups could be coherently interpreted based on a suite of parameters that includes hydroperiod (elevation), source(s) of sediment-laden water, hydraulic connectivity, flow stagnation, and location in transect (levee versus backswamp). Low elevatic (long hydroperiod), high hydraulic connectivity to multiple sources of sediment-laden water, and hydraulic damming (flow stagnation) lead to the highest amounts of sediment trapping; the converse in any of these factors may diminish sediment trapping. Based on aerial extent of deposition groups, the study area (about 500 km 2) potentially traps 6.72+109 kg of sediment, annually, of which 12 percent or 8.20.108 kg are organic material. This accumulated sediment contains a coarsely estimated 5% and 27% of the annual nitrogen and phosphorus loads to the Atchafalaya Basin, respectively, and 3.7+108 kg C. Thus, the Atchafalaya Basin plays an important role in sediment storage, including the sequestration of carbon, nitrogen, and phosphorus.","largerWorkTitle":"Hydrology and Management of Forested Wetlands - Proceeding of the International Conference","conferenceTitle":"International Conference on Hydrology and Management of Forested Wetlands","conferenceDate":"8 April 2006 through 12 April 2006","conferenceLocation":"New Bern, NC","language":"English","isbn":"1892769530; 9781892769534","usgsCitation":"Hupp, C., and Noe, G., 2006, Sediment and nutrient accumulation within lowland bottomland ecosystems: An example from the Atchafalaya River Basin, Louisiana, <i>in</i> Hydrology and Management of Forested Wetlands - Proceeding of the International Conference, New Bern, NC, 8 April 2006 through 12 April 2006, p. 175-187.","startPage":"175","endPage":"187","numberOfPages":"13","costCenters":[],"links":[{"id":240967,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8954e4b08c986b316da1","contributors":{"authors":[{"text":"Hupp, C.R. 0000-0003-1853-9197","orcid":"https://orcid.org/0000-0003-1853-9197","contributorId":78775,"corporation":false,"usgs":true,"family":"Hupp","given":"C.R.","affiliations":[],"preferred":false,"id":440441,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Noe, G.B.","contributorId":66464,"corporation":false,"usgs":true,"family":"Noe","given":"G.B.","email":"","affiliations":[],"preferred":false,"id":440440,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70033345,"text":"70033345 - 2006 - Towards sustainable management of Louisiana's coastal wetland forests: Problems, constraints, and a new beginning","interactions":[],"lastModifiedDate":"2019-10-10T07:03:45","indexId":"70033345","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Towards sustainable management of Louisiana's coastal wetland forests: Problems, constraints, and a new beginning","docAbstract":"Over 345,000 ha of forested swamps occur throughout the Mississippi River Deltaic Plain. Natural and anthropogenic changes in hydrology and geomorphology at local and landscape levels have reduced the productivity in many of these coastal wetland forests areas and have caused the complete loss of forest cover in some places. A summary and interpretation of the available science, suggestions for policy change, and a multidisciplinary (multi-responsibility) approach were needed to address these issues [in the context of private land]. In response, the Louisiana Governor's office formed a Coastal Wetland Forest Conservation and Use Science Working Group (SWG) and an associated Advisory Panel to provide the Governor with information and suggestions of strategies for environmental and economic utilization, conservation, and protection of Louisiana's coastal wetland forest ecosystem in the long-term. The process of engaging scientists, resource managers, and other stakeholders in this effort is described, and the recommendations of the SWG are presented relative to forestry practices and the potential for sustainable management of coastal wetland forests.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Hydrology and management of forested wetlands - Proceeding of the international conference","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"International Conference on Hydrology and Management of Forested Wetlands","conferenceDate":"April 8-12, 2006","conferenceLocation":"New Bern, NC","language":"English","publisher":"ASABE","doi":"10.13031/2013.20309","isbn":"1892769530; 9781892769534","usgsCitation":"Chambers, J.L., Conner, W., Keim, R., Faulkner, S., Day, J., Gardiner, E., Hughes, M., King, S., McLeod, K., Miller, C., Nyman, J., and Shaffer, G., 2006, Towards sustainable management of Louisiana's coastal wetland forests: Problems, constraints, and a new beginning, <i>in</i> Hydrology and management of forested wetlands - Proceeding of the international conference, New Bern, NC, April 8-12, 2006, p. 150-157, https://doi.org/10.13031/2013.20309.","productDescription":"8 p.","startPage":"150","endPage":"157","numberOfPages":"8","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":240995,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Louisiana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.835205078125,\n              30.732392734006083\n            ],\n            [\n              -93.790283203125,\n              30.372875188118016\n            ],\n            [\n              -93.834228515625,\n              29.726222319395504\n            ],\n            [\n              -93.31787109374999,\n              29.707139348134145\n            ],\n            [\n              -92.2412109375,\n              29.48742484748479\n            ],\n            [\n              -92.054443359375,\n              29.516110386062277\n            ],\n            [\n              -91.845703125,\n              29.420460341013133\n            ],\n            [\n              -91.56005859375,\n              29.554345125748267\n            ],\n            [\n              -91.285400390625,\n              29.180941290001776\n            ],\n            [\n              -90.977783203125,\n              29.123373210819224\n            ],\n            [\n              -90.648193359375,\n              28.969700808694157\n            ],\n            [\n              -89.80224609374999,\n              29.19053283229458\n            ],\n            [\n              -89.395751953125,\n              28.844673680771795\n            ],\n            [\n              -88.890380859375,\n              29.19053283229458\n            ],\n            [\n              -89.09912109375,\n              30.06909396443887\n            ],\n            [\n              -89.56054687499999,\n              30.20211367909724\n            ],\n            [\n              -89.835205078125,\n              30.732392734006083\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb5c2e4b08c986b3268a8","contributors":{"authors":[{"text":"Chambers, J. L.","contributorId":100787,"corporation":false,"usgs":true,"family":"Chambers","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":440437,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Conner, W.H.","contributorId":54165,"corporation":false,"usgs":true,"family":"Conner","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":440430,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Keim, R.F.","contributorId":62840,"corporation":false,"usgs":true,"family":"Keim","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":440434,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Faulkner, S.P.","contributorId":55190,"corporation":false,"usgs":true,"family":"Faulkner","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":440431,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Day, J.W.","contributorId":27417,"corporation":false,"usgs":true,"family":"Day","given":"J.W.","affiliations":[],"preferred":false,"id":440428,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gardiner, E.S.","contributorId":30808,"corporation":false,"usgs":true,"family":"Gardiner","given":"E.S.","email":"","affiliations":[],"preferred":false,"id":440429,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Hughes, M.S.","contributorId":106718,"corporation":false,"usgs":true,"family":"Hughes","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":440439,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"King, S.L.","contributorId":105663,"corporation":false,"usgs":true,"family":"King","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":440438,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"McLeod, K.W.","contributorId":77366,"corporation":false,"usgs":true,"family":"McLeod","given":"K.W.","email":"","affiliations":[],"preferred":false,"id":440436,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Miller, C.A.","contributorId":67253,"corporation":false,"usgs":true,"family":"Miller","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":440435,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Nyman, J.A.","contributorId":56835,"corporation":false,"usgs":true,"family":"Nyman","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":440432,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Shaffer, G.P.","contributorId":62415,"corporation":false,"usgs":true,"family":"Shaffer","given":"G.P.","email":"","affiliations":[],"preferred":false,"id":440433,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}}
,{"id":70031191,"text":"70031191 - 2006 - Urban contributions of glyphosate and its degradate AMPA to streams in the United States","interactions":[],"lastModifiedDate":"2018-10-22T10:44:06","indexId":"70031191","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","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":"Urban contributions of glyphosate and its degradate AMPA to streams in the United States","docAbstract":"<p>Glyphosate is the most widely used herbicide in the world, being routinely applied to control weeds in both agricultural and urban settings. Microbial degradation of glyphosate produces aminomethyl phosphonic acid (AMPA). The high polarity and water-solubility of glyphosate and AMPA has, until recently, made their analysis in water samples problematic. Thus, compared to other herbicides (e.g. atrazine) there are relatively few studies on the environmental occurrence of glyphosate and AMPA. In 2002, treated effluent samples were collected from 10 wastewater treatment plants (WWTPs) to study the occurrence of glyphosate and AMPA. Stream samples were collected upstream and downstream of the 10 WWTPs. Two reference streams were also sampled. The results document the apparent contribution of WWTP effluent to stream concentrations of glyphosate and AMPA, with roughly a two-fold increase in their frequencies of detection between stream samples collected upstream and those collected downstream of the WWTPs. Thus, urban use of glyphosate contributes to glyphosate and AMPA concentrations in streams in the United States. Overall, AMPA was detected much more frequently (67.5%) compared to glyphosate (17.5%).</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.scitotenv.2005.01.028","issn":"00489697","usgsCitation":"Kolpin, D., Thurman, E., Lee, E., Meyer, M.T., Furlong, E., and Glassmeyer, S., 2006, Urban contributions of glyphosate and its degradate AMPA to streams in the United States: Science of the Total Environment, v. 354, no. 2-3, p. 191-197, https://doi.org/10.1016/j.scitotenv.2005.01.028.","productDescription":"7 p.","startPage":"191","endPage":"197","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":238880,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  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E.M.","contributorId":102864,"corporation":false,"usgs":true,"family":"Thurman","given":"E.M.","affiliations":[],"preferred":false,"id":430445,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lee, E.A.","contributorId":48608,"corporation":false,"usgs":true,"family":"Lee","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":430440,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Meyer, M. T.","contributorId":92279,"corporation":false,"usgs":true,"family":"Meyer","given":"M.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":430442,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Furlong, E. T. 0000-0002-7305-4603","orcid":"https://orcid.org/0000-0002-7305-4603","contributorId":98346,"corporation":false,"usgs":true,"family":"Furlong","given":"E. T.","affiliations":[],"preferred":false,"id":430443,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Glassmeyer, S.T.","contributorId":100190,"corporation":false,"usgs":true,"family":"Glassmeyer","given":"S.T.","affiliations":[],"preferred":false,"id":430444,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70031178,"text":"70031178 - 2006 - Ge/Si and 87Sr/86Sr tracers of weathering reactions and hydrologic pathways in a tropical granitoid system","interactions":[],"lastModifiedDate":"2012-03-12T17:21:18","indexId":"70031178","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2302,"text":"Journal of Geochemical Exploration","active":true,"publicationSubtype":{"id":10}},"title":"Ge/Si and 87Sr/86Sr tracers of weathering reactions and hydrologic pathways in a tropical granitoid system","docAbstract":"Ge/Si and 87Sr/86Sr data from primary and secondary minerals, soil waters, and stream waters in a tropical granitoid catchment quantitatively reflect mineral alteration reactions that occur at different levels within the bedrock-saprolite-soil zone. Near the bedrock-saprolite interface, plagioclase to kaolinite reaction yields low Ge/Si and 87Sr/86Sr. Higher in the regolith column, biotite weathering and kaolinite dissolution drive Ge/Si and 87Sr/86Sr to high values. Data from streams at base flow sample the bedrock-saprolite interface zone, while at high discharge solutes are derived from upper saprolite-soil zone. Coupled Ge/Si and 87Sr/86Sr can be effective tools for quantifying the importance of specific weathering reactions, and for geochemical hydrograph separation. ?? 2005 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geochemical Exploration","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.gexplo.2005.08.054","issn":"03756742","usgsCitation":"Derry, L., Pett-Ridge, J.C., Kurtz, A., and Troester, J., 2006, Ge/Si and 87Sr/86Sr tracers of weathering reactions and hydrologic pathways in a tropical granitoid system: Journal of Geochemical Exploration, v. 88, no. 1-3 SPEC. ISS., p. 271-274, https://doi.org/10.1016/j.gexplo.2005.08.054.","startPage":"271","endPage":"274","numberOfPages":"4","costCenters":[],"links":[{"id":211463,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.gexplo.2005.08.054"},{"id":238756,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"88","issue":"1-3 SPEC. ISS.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a14f0e4b0c8380cd54c27","contributors":{"authors":[{"text":"Derry, L.A.","contributorId":47162,"corporation":false,"usgs":true,"family":"Derry","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":430379,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pett-Ridge, J. C.","contributorId":18574,"corporation":false,"usgs":true,"family":"Pett-Ridge","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":430378,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kurtz, A.C.","contributorId":89341,"corporation":false,"usgs":true,"family":"Kurtz","given":"A.C.","email":"","affiliations":[],"preferred":false,"id":430380,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Troester, J.W.","contributorId":90750,"corporation":false,"usgs":true,"family":"Troester","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":430381,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70031140,"text":"70031140 - 2006 - Oink if you love coal","interactions":[],"lastModifiedDate":"2018-10-22T10:55:45","indexId":"70031140","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1829,"text":"Geotimes","active":true,"publicationSubtype":{"id":10}},"title":"Oink if you love coal","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"AGI","issn":"00168556","usgsCitation":"Landa, E.R., 2006, Oink if you love coal: Geotimes, v. 51, no. 4.","productDescription":"1 p.","startPage":"60","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":238815,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"51","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6d1ee4b0c8380cd74f96","contributors":{"authors":[{"text":"Landa, E. R.","contributorId":100002,"corporation":false,"usgs":true,"family":"Landa","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":430218,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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