{"pageNumber":"329","pageRowStart":"8200","pageSize":"25","recordCount":16440,"records":[{"id":70024819,"text":"70024819 - 2002 - Influence of eastern hemlock (Tsuga canadensis) forests on aquatic invertebrate assemblages in headwater streams","interactions":[],"lastModifiedDate":"2012-03-12T17:20:15","indexId":"70024819","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","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":"Influence of eastern hemlock (Tsuga canadensis) forests on aquatic invertebrate assemblages in headwater streams","docAbstract":"We conducted a comparative study in the Delaware Water Gap National Recreation Area to determine the potential long-term impacts of hemlock forest decline on stream benthic macroinvertebrate assemblages. Hemlock forests throughout eastern North America have been declining because of the hemlock woolly adelgid, an exotic insect pest. We found aquatic invertebrate community structure to be strongly correlated with forest composition. Streams draining hemlock forests supported significantly more total taxa than streams draining mixed hardwood forests, and over 8% of the taxa were strongly associated with hemlock. In addition, invertebrate taxa were more evenly distributed (i.e., higher Simpson's evenness values) in hemlock-drained streams. In contrast, the number of rare species and total densities were significantly lower in streams draining hemlock, suggesting that diversity differences observed between forest types were not related to stochastic factors associated with sampling and that streams draining mixed hardwood forests may be more productive. Analysis of stream habitat data indicated that streams draining hemlock forests had more stable thermal and hydrologic regimes. Our findings suggest that hemlock decline may result in long-term changes in headwater ecosystems leading to reductions in both within-stream (i.e., alpha) and park-wide (i.e., gamma) benthic community diversity.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Canadian Journal of Fisheries and Aquatic Sciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1139/f02-003","issn":"0706652X","usgsCitation":"Snyder, C., Young, J., Lemarie, D.P., and Smith, D., 2002, Influence of eastern hemlock (Tsuga canadensis) forests on aquatic invertebrate assemblages in headwater streams: Canadian Journal of Fisheries and Aquatic Sciences, v. 59, no. 2, p. 262-275, https://doi.org/10.1139/f02-003.","startPage":"262","endPage":"275","numberOfPages":"14","costCenters":[],"links":[{"id":232963,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":207766,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1139/f02-003"}],"volume":"59","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3b2ce4b0c8380cd622bf","contributors":{"authors":[{"text":"Snyder, C.D.","contributorId":73540,"corporation":false,"usgs":true,"family":"Snyder","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":402732,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Young, J.A. 0000-0002-4500-3673","orcid":"https://orcid.org/0000-0002-4500-3673","contributorId":37674,"corporation":false,"usgs":true,"family":"Young","given":"J.A.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":false,"id":402730,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lemarie, D. P.","contributorId":23100,"corporation":false,"usgs":true,"family":"Lemarie","given":"D.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":402729,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, D. R. 0000-0001-6074-9257","orcid":"https://orcid.org/0000-0001-6074-9257","contributorId":44108,"corporation":false,"usgs":true,"family":"Smith","given":"D. R.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":false,"id":402731,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70024814,"text":"70024814 - 2002 - 234U/238U evidence for local recharge and patterns of groundwater flow in the vicinity of Yucca Mountain, Nevada, USA","interactions":[],"lastModifiedDate":"2012-03-12T17:20:10","indexId":"70024814","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":835,"text":"Applied Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"234U/238U evidence for local recharge and patterns of groundwater flow in the vicinity of Yucca Mountain, Nevada, USA","docAbstract":"Uranium concentrations and 234U/238U ratios in saturated-zone and perched ground water were used to investigate hydrologic flow and downgradient dilution and dispersion in the vicinity of Yucca Mountain, a potential high-level radioactive waste disposal site. The U data were obtained by thermal ionization mass spectrometry on more than 280 samples from the Death Valley regional flow system. Large variations in both U concentrations (commonly 0.6-10 ??g 1-1) and 234U/238U activity ratios (commonly 1.5-6) are present on both local and regional scales; however, ground water with 234U/238U activity ratios from 7 up to 8.06 is restricted largely to samples from Yucca Mountain. Data from ground water in the Tertiary volcanic and Quaternary alluvial aquifers at and adjacent to Yucca Mountain plot in 3 distinct fields of reciprocal U concentration versus 234U/238U activity ratio correlated to different geographic areas. Ground water to the west of Yucca Mountain has large U concentrations and moderate 234U/238U whereas ground water to the east in the Fortymile flow system has similar 234U/238U, but distinctly smaller U concentrations. Ground water beneath the central part of Yucca Mountain has intermediate U concentrations but distinctive 234U/238U activity ratios of about 7-8. Perched water from the lower part of the unsaturated zone at Yucca Mountain has similarly large values of 234U/238U. These U data imply that the Tertiary volcanic aquifer beneath the central part of Yucca Mountain is isolated from north-south regional flow. The similarity of 234U/238U in both saturated- and unsaturated-zone ground water at Yucca Mountain further indicates that saturated-zone ground water beneath Yucca Mountain is dominated by local recharge rather than regional flow. The distinctive 234U/238U signatures also provide a natural tracer of downgradient flow. Elevated 234U/238U in ground water from two water-supply wells east of Yucca Mountain are interpreted as the result of induced flow from 40 a of ground-water withdrawal. Elevated 234U/238U in a borehole south of Yucca Mountain is interpreted as evidence that natural downgradient flow is more likely to follow southerly paths in the structurally anisotropic Tertiary volcanic aquifer where it becomes diluted by regional flow in the Fortymile system.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Applied Geochemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/S0883-2927(02)00037-9","issn":"08832927","usgsCitation":"Paces, J., Ludwig, K., Peterman, Z.E., and Neymark, L., 2002, 234U/238U evidence for local recharge and patterns of groundwater flow in the vicinity of Yucca Mountain, Nevada, USA: Applied Geochemistry, v. 17, no. 6, p. 751-779, https://doi.org/10.1016/S0883-2927(02)00037-9.","startPage":"751","endPage":"779","numberOfPages":"29","costCenters":[],"links":[{"id":207721,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0883-2927(02)00037-9"},{"id":232894,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e254e4b0c8380cd45ac6","contributors":{"authors":[{"text":"Paces, J.B. 0000-0002-9809-8493","orcid":"https://orcid.org/0000-0002-9809-8493","contributorId":27482,"corporation":false,"usgs":true,"family":"Paces","given":"J.B.","affiliations":[],"preferred":false,"id":402710,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ludwig, K.R.","contributorId":97112,"corporation":false,"usgs":true,"family":"Ludwig","given":"K.R.","email":"","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":402713,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peterman, Z. E.","contributorId":63781,"corporation":false,"usgs":true,"family":"Peterman","given":"Z.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":402712,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Neymark, L.A. 0000-0003-4190-0278","orcid":"https://orcid.org/0000-0003-4190-0278","contributorId":56673,"corporation":false,"usgs":true,"family":"Neymark","given":"L.A.","affiliations":[],"preferred":false,"id":402711,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70024802,"text":"70024802 - 2002 - Source water partitioning as a means of characterizing hydrologic function in mangroves","interactions":[],"lastModifiedDate":"2012-03-12T17:20:07","indexId":"70024802","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3751,"text":"Wetlands Ecology and Management","active":true,"publicationSubtype":{"id":10}},"title":"Source water partitioning as a means of characterizing hydrologic function in mangroves","docAbstract":"Mangrove ecosystems rely on seawater, rain-derived flow, and groundwater for hydrologic sustenance, flushing, and inflow of nutrients and sediments. The relative contribution of these source waters and their variability through time and space can provide key information concerning the hydrologic function of ecosystems. We used hydrologic tracers to partition source waters and trace their movements in the Enipoas stream, a river-dominated mangrove ecosystem on the island of Pohnpei, Federated States of Micronesia (FSM) and in the Yela watershed, an interior mangrove ecosystem on the island of Kosrae, FSM. The Enipoas site was characterized as a salt wedge estuary whose source water contributions alternated between predominantly seawater and rain-derived flow, depending on the tide. The source waters in the interior Yela site were also predominantly seawater and rain-derived flow, however the relative contribution of each was much more stable. The mean groundwater contribution was 5% (SD = 5.5) for the Enipoas site and 20% (SD = 11.0) for the Yela site. Although a small contributor to flow, groundwater was a steady source of freshwater for both systems. Hydrologic linkages between mangroves and adjacent ecosystems were demonstrated by the temporal and spatial distribution of source waters. The 0.8 km Enipoas estuary, with its highly dynamic bi-directional flows, transported source waters along a hydrologic continuum comprised of coral reef, mangroves, and palm forest. In the interior mangroves of the Yela watershed, the presence of rain-derived flow and groundwater demonstrated a hydraulic connection between the mangroves and an upstream freshwater swamp. Interior mangroves with such linkages avoid stresses such as desiccation and heightened salinity, and thus are more productive than those with little or no freshwater flows.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wetlands Ecology and Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1023/A:1016547103966","issn":"09234861","usgsCitation":"Drexler, J., and De Carlo, E.W., 2002, Source water partitioning as a means of characterizing hydrologic function in mangroves: Wetlands Ecology and Management, v. 10, no. 2, p. 103-113, https://doi.org/10.1023/A:1016547103966.","startPage":"103","endPage":"113","numberOfPages":"11","costCenters":[],"links":[{"id":207984,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1023/A:1016547103966"},{"id":233320,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b933ee4b08c986b31a3bd","contributors":{"authors":[{"text":"Drexler, J.Z. 0000-0002-0127-3866","orcid":"https://orcid.org/0000-0002-0127-3866","contributorId":54766,"corporation":false,"usgs":true,"family":"Drexler","given":"J.Z.","affiliations":[],"preferred":false,"id":402672,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"De Carlo, E. W.","contributorId":10201,"corporation":false,"usgs":true,"family":"De Carlo","given":"E.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":402671,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70024798,"text":"70024798 - 2002 - Behavioural and physiological response of trout to winter habitat in tailwaters in Wyoming, USA","interactions":[],"lastModifiedDate":"2012-03-12T17:20:07","indexId":"70024798","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1924,"text":"Hydrological Processes","active":true,"publicationSubtype":{"id":10}},"title":"Behavioural and physiological response of trout to winter habitat in tailwaters in Wyoming, USA","docAbstract":"Fisheries managers have often suggested that survival of trout during the winter is a major factor affecting population densities in many stream ecosystems in the Rocky Mountains. In Wyoming, trout population reductions from fall to spring in excess of 90% have been documented in some reservoir tailwaters. Though biologists have surmised that these reductions were the result of either mortality or emigration from some river sections, the specific mechanisms have not been defined and the factors leading to the trout loss are unknown. This is a review of four studies that were conducted or funded between 1991 and 1998 by the Wyoming Game and Fish Department to understand the extent of overwinter losses, identify some of the mechanisms leading to those conditions and develop management strategies to help avoid those impacts. Winter studies were conducted on tailwater fisheries in the Green, North Platte, Bighorn and Shoshone rivers to document trout population dynamics, assess physical habitat availability, evaluate trout movement and habitat selection, and understand the relationships between food availability and bioenergetic relationships. Results indicate that winter trout losses are extreme in some years, that trout movement and habitat selection are affected by supercooled flows, and that mortality is probably not directly due to starvation. The combination of physiological impairment with frequently altered habitat availability probably leads to indirect mortality from predators and other factors. Copyright ?? 2002 John Wiley & Sons, Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hydrological Processes","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1002/hyp.376","issn":"08856087","usgsCitation":"Annear, T., Hubert, W., Simpkins, D., and Hebdon, L., 2002, Behavioural and physiological response of trout to winter habitat in tailwaters in Wyoming, USA: Hydrological Processes, v. 16, no. 4, p. 915-925, https://doi.org/10.1002/hyp.376.","startPage":"915","endPage":"925","numberOfPages":"11","costCenters":[],"links":[{"id":207937,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/hyp.376"},{"id":233249,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"4","noUsgsAuthors":false,"publicationDate":"2002-02-21","publicationStatus":"PW","scienceBaseUri":"5059f0ace4b0c8380cd4a854","contributors":{"authors":[{"text":"Annear, T.C.","contributorId":65640,"corporation":false,"usgs":true,"family":"Annear","given":"T.C.","email":"","affiliations":[],"preferred":false,"id":402655,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hubert, W.","contributorId":77707,"corporation":false,"usgs":true,"family":"Hubert","given":"W.","email":"","affiliations":[],"preferred":false,"id":402656,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Simpkins, D.","contributorId":101851,"corporation":false,"usgs":true,"family":"Simpkins","given":"D.","email":"","affiliations":[],"preferred":false,"id":402658,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hebdon, L.","contributorId":95656,"corporation":false,"usgs":true,"family":"Hebdon","given":"L.","email":"","affiliations":[],"preferred":false,"id":402657,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70024787,"text":"70024787 - 2002 - Removal of antibiotics from surface and distilled water in conventional water treatment processes","interactions":[],"lastModifiedDate":"2018-11-26T07:42:26","indexId":"70024787","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2255,"text":"Journal of Environmental Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Removal of antibiotics from surface and distilled water in conventional water treatment processes","docAbstract":"Conventional drinking water treatment processes were evaluated under typical water treatment plant conditions to determine their effectiveness in the removal of seven common antibiotics: carbadox, sulfachlorpyridazine, sulfadimethoxine, sulfamerazine, sulfamethazine, sulfathiazole, and trimethoprim. Experiments were conducted using synthetic solutions prepared by spiking both distilled/ deionized water and Missouri River water with the studied compounds. Sorption on Calgon WPH powdered activated carbon, reverse osmosis, and oxidation with chlorine and ozone under typical plant conditions were all shown to be effective in removing the studied antibiotics. Conversely, coagulation/flocculation/sedimentation with alum and iron salts, excess lime/soda ash softening, ultraviolet irradiation at disinfection dosages, and ion exchange were all relatively ineffective methods of antibiotic removal. This study shows that the studied antibiotics could be effectively removed using processes already in use many water treatment plants. Additional work is needed on by-product formation and the removal of other classes of antibiotics.","language":"English","publisher":"ASCE","doi":"10.1061/(ASCE)0733-9372(2002)128:3(253)","issn":"07339372","usgsCitation":"Adams, C., Wang, Y., Loftin, K., and Meyer, M., 2002, Removal of antibiotics from surface and distilled water in conventional water treatment processes: Journal of Environmental Engineering, v. 128, no. 3, p. 253-260, https://doi.org/10.1061/(ASCE)0733-9372(2002)128:3(253).","productDescription":"8 p.","startPage":"253","endPage":"260","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":233103,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":207856,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1061/(ASCE)0733-9372(2002)128:3(253)"}],"volume":"128","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aa725e4b0c8380cd85251","contributors":{"authors":[{"text":"Adams, C.","contributorId":88531,"corporation":false,"usgs":true,"family":"Adams","given":"C.","affiliations":[],"preferred":false,"id":402623,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wang, Y.","contributorId":64213,"corporation":false,"usgs":true,"family":"Wang","given":"Y.","affiliations":[],"preferred":false,"id":402622,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Loftin, K.","contributorId":36326,"corporation":false,"usgs":true,"family":"Loftin","given":"K.","email":"","affiliations":[],"preferred":false,"id":402621,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Meyer, M.","contributorId":92835,"corporation":false,"usgs":true,"family":"Meyer","given":"M.","affiliations":[],"preferred":false,"id":402624,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70024786,"text":"70024786 - 2002 - Diffusion model validation and interpretation of stable isotopes in river and lake ice","interactions":[],"lastModifiedDate":"2012-03-12T17:20:08","indexId":"70024786","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1924,"text":"Hydrological Processes","active":true,"publicationSubtype":{"id":10}},"title":"Diffusion model validation and interpretation of stable isotopes in river and lake ice","docAbstract":"The stable isotope stratigraphy of river- and lake-ice archives winter hydroclimatic conditions, and can potentially be used to identify changing water sources or to provide important insights into ice formation processes and growth rates. However, accurate interpretations rely on known isotopic fractionation during ice growth. A one-dimensional diffusion model of the liquid boundary layer adjacent to an advancing solid interface, originally developed to simulate solute rejection by growing crystals, has been used without verification to describe non-equilibrium fractionation during congelation ice growth. Results are not in agreement, suggesting the presence of important uncertainties. In this paper we seek validation of the diffusion model for this application using large-scale laboratory experiments with controlled freezing rates and frequent sampling. We obtained consistent, almost constant, isotopic boundary layer thicknesses over a representative range of ice growth rates on both quiescent and well-mixed water. With the 18O boundary layer thickness from the laboratory, the model successfully quantified reduced river-ice growth rates relative to those of a nearby lake. These results were more representative and easier to obtain than those of a conventional thermal ice-growth model. This diffusion model validation and boundary layer thickness determination provide a powerful tool for interpreting the stable isotope stratigraphy of floating ice. The laboratory experiment also replicated successive fractionation events in response to a freeze-thaw-refreeze cycle, providing a mechanism for apparent ice fractionation that exceeds equilibrium. Analysis of the composition of snow ice and frazil ice in river and lake cores indicated surprising similarities between these ice forms. Published in 2002 by John Wiley & Sons, Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hydrological Processes","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1002/hyp.374","issn":"08856087","usgsCitation":"Ferrick, M., Calkins, D., Perron, N., Cragin, J., and Kendall, C., 2002, Diffusion model validation and interpretation of stable isotopes in river and lake ice: Hydrological Processes, v. 16, no. 4, p. 851-872, https://doi.org/10.1002/hyp.374.","startPage":"851","endPage":"872","numberOfPages":"22","costCenters":[],"links":[{"id":207855,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/hyp.374"},{"id":233102,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"4","noUsgsAuthors":false,"publicationDate":"2002-02-21","publicationStatus":"PW","scienceBaseUri":"505a0110e4b0c8380cd4faa4","contributors":{"authors":[{"text":"Ferrick, M.G.","contributorId":46731,"corporation":false,"usgs":true,"family":"Ferrick","given":"M.G.","email":"","affiliations":[],"preferred":false,"id":402617,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Calkins, D.J.","contributorId":82896,"corporation":false,"usgs":true,"family":"Calkins","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":402620,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Perron, N.M.","contributorId":78122,"corporation":false,"usgs":true,"family":"Perron","given":"N.M.","email":"","affiliations":[],"preferred":false,"id":402619,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cragin, J.H.","contributorId":60819,"corporation":false,"usgs":true,"family":"Cragin","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":402618,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kendall, C. 0000-0002-0247-3405","orcid":"https://orcid.org/0000-0002-0247-3405","contributorId":35050,"corporation":false,"usgs":true,"family":"Kendall","given":"C.","affiliations":[],"preferred":false,"id":402616,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70024765,"text":"70024765 - 2002 - Bedform movement recorded by sequential single-beam surveys in tidal rivers","interactions":[],"lastModifiedDate":"2018-09-13T16:27:59","indexId":"70024765","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","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":"Bedform movement recorded by sequential single-beam surveys in tidal rivers","docAbstract":"A portable system for bedform-mapping was evaluated in the delta of the lower Sacramento and San Joaquin Rivers, California, from 1998 to 2000. Bedform profiles were surveyed with a two-person crew using an array of four single-beam transducers on boats about 6 m in length. Methods for processing the bedform profiles into maps with geographic coordinates were developed for spreadsheet programs and surface-contouring software. Straight reaches were surveyed every few days or weeks to determine locations of sand deposition, net transport directions, flow thresholds for bedform regimes, and bedform-transport rates. In one channel of unidirectional flow, the portable system was used to record changes in bedform regime through minor fluctuations of low discharge, and through high discharges near channel capacity. In another channel with reversing flows from tides, the portable system recorded directions of net bedload-transport that would be undetectable by standard bedload sampling alone.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Hydrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/S0022-1694(01)00558-3","issn":"00221694","usgsCitation":"Dinehart, R., 2002, Bedform movement recorded by sequential single-beam surveys in tidal rivers: Journal of Hydrology, v. 258, no. 1-4, p. 25-39, https://doi.org/10.1016/S0022-1694(01)00558-3.","startPage":"25","endPage":"39","numberOfPages":"15","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":232780,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":207647,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0022-1694(01)00558-3"}],"volume":"258","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f040e4b0c8380cd4a69c","contributors":{"authors":[{"text":"Dinehart, R.L.","contributorId":54610,"corporation":false,"usgs":true,"family":"Dinehart","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":402552,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70024760,"text":"70024760 - 2002 - Controls on old and new water contributions to stream flow at some nested catchments in Vermont, USA","interactions":[],"lastModifiedDate":"2012-03-12T17:20:07","indexId":"70024760","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1924,"text":"Hydrological Processes","active":true,"publicationSubtype":{"id":10}},"title":"Controls on old and new water contributions to stream flow at some nested catchments in Vermont, USA","docAbstract":"Factors controlling the partitioning of old and new water contributions to stream flow were investigated for three events in four catchments (three of which were nested) at Sleepers River Research Watershed in Danville, Vermont. In the 1993 snowmelt period, two-component isotopic hydrograph separations showed that new water (meltwater) inputs to the stream ranged widely from 41 to 74%, and increased with catchment size (41 to 11 125 ha) (with one exception) and with open land cover (0-73%). Peak dissolved organic carbon concentrations and relative alkalinity dilution in stream water ranked in the same order among catchments as the new water fractions, suggesting that new water followed shallow flow paths. During the 1994 snowmelt, despite similar timing and magnitude of melt inputs, the new-water contribution to stream flow ranged only from 30 to 36% in the four catchments. We conclude that the uncommonly high and variable new water fractions in streamwater during the 1993 melt were caused by direct runoff of meltwater over frozen ground, which was prevalent in open land areas during the 1993 winter. In a high-intensity summer rainstorm in 1993, new water fractions were smaller relative to the 1993 snowmelt, ranging from 28 to 46%, but they ranked in the identical catchment order. Reconciliation of the contrasting patterns of new-old water partitioning in the three events appears to require an explanation that invokes multiple processes and effects, including: 1 topographically controlled increase in surface-saturated area with increasing catchment size; 2 direct runoff over frozen ground; 3 low infiltration in agriculturally compacted soils; 4 differences in soil transmissivity, which may be more relevant under dry antecedent conditions. These data highlight some of the difficulties faced by catchment hydrologists in formulating a theory of runoff generation at varying basin scales. Copyright ?? 2002 John Wiley and Sons, Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hydrological Processes","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1002/hyp.312","issn":"08856087","usgsCitation":"Shanley, J.B., Kendall, C., Smith, T.E., Wolock, D., and McDonnell, J.J., 2002, Controls on old and new water contributions to stream flow at some nested catchments in Vermont, USA: Hydrological Processes, v. 16, no. 3, p. 589-609, https://doi.org/10.1002/hyp.312.","startPage":"589","endPage":"609","numberOfPages":"21","costCenters":[],"links":[{"id":207956,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/hyp.312"},{"id":233279,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"3","noUsgsAuthors":false,"publicationDate":"2002-01-31","publicationStatus":"PW","scienceBaseUri":"5059fbd2e4b0c8380cd4dfa8","contributors":{"authors":[{"text":"Shanley, J. B.","contributorId":52226,"corporation":false,"usgs":true,"family":"Shanley","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":402535,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kendall, C. 0000-0002-0247-3405","orcid":"https://orcid.org/0000-0002-0247-3405","contributorId":35050,"corporation":false,"usgs":true,"family":"Kendall","given":"C.","affiliations":[],"preferred":false,"id":402533,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, T. E.","contributorId":23530,"corporation":false,"usgs":true,"family":"Smith","given":"T.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":402532,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wolock, D.M. 0000-0002-6209-938X","orcid":"https://orcid.org/0000-0002-6209-938X","contributorId":36601,"corporation":false,"usgs":true,"family":"Wolock","given":"D.M.","affiliations":[],"preferred":false,"id":402534,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"McDonnell, Jeffery J. 0000-0002-3880-3162","orcid":"https://orcid.org/0000-0002-3880-3162","contributorId":62723,"corporation":false,"usgs":false,"family":"McDonnell","given":"Jeffery","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":402536,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70024754,"text":"70024754 - 2002 - Increased selenium threat as a result of invasion of the exotic bivalve Potamocorbula amurensis into the San Francisco Bay-Delta","interactions":[],"lastModifiedDate":"2018-11-28T08:54:37","indexId":"70024754","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","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":"Increased selenium threat as a result of invasion of the exotic bivalve Potamocorbula amurensis into the San Francisco Bay-Delta","docAbstract":"<div id=\"abstracts\" class=\"Abstracts\"><div id=\"aep-abstract-id12\" class=\"abstract author\"><div id=\"aep-abstract-sec-id13\"><p>Following the aggressive invasion of the bivalve,<span>&nbsp;</span><i>Potamocorbula amurensis</i>, in the San Francisco Bay-Delta in 1986, selenium contamination in the benthic food web increased. Concentrations in this dominant (exotic) bivalve in North Bay were three times higher in 1995–1997 than in earlier studies, and 1990 concentrations in benthic predators (sturgeon and diving ducks) were also higher than in 1986. The contamination was widespread, varied seasonally and was greater in<span>&nbsp;</span><i>P. amurensis</i><span>&nbsp;</span>than in co-occurring and transplanted species. Selenium concentrations in the water column of the Bay were enriched relative to the Sacramento River but were not as high as observed in many contaminated aquatic environments. Total Se concentrations in the dissolved phase never exceeded 0.3 μg Se per l in 1995 and 1996; Se concentrations on particulate material ranged from 0.5 to 2.0 μg Se per g dry weight (dw) in the Bay. Nevertheless, concentrations in<span>&nbsp;</span><i>P. amurensis</i><span>&nbsp;</span>reached as high as 20 μg Se per g dw in October 1996. The enriched concentrations in bivalves (6–20 μg Se per g dw) were widespread throughout North San Francisco Bay in October 1995 and October 1996. Concentrations varied seasonally from 5 to 20 μg Se per g dw, and were highest during the periods of lowest river inflows and lowest after extended high river inflows. Transplanted bivalves (oysters, mussels or clams) were not effective indicators of either the degree of Se contamination in<span>&nbsp;</span><i>P. amurensis</i><span>&nbsp;</span>or the seasonal increases in contamination in the resident benthos. Se is a potent environmental toxin that threatens higher trophic level species because of its reproductive toxicity and efficient food web transfer. Bivalves concentrate selenium effectively because they bioaccumulate the element strongly and lose it slowly; and they are a direct link in the exposure of predaceous benthivore species. Biological invasions of estuaries are increasing worldwide. Changes in ecological structure and function are well known in response to invasions. This study shows that changes in processes such as cycling and effects of contaminants can accompany such invasions.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/S0166-445X(01)00265-X","issn":"0166445X","usgsCitation":"Linville, R., Luoma, S., Cutter, L., and Cutter, G., 2002, Increased selenium threat as a result of invasion of the exotic bivalve Potamocorbula amurensis into the San Francisco Bay-Delta: Aquatic Toxicology, v. 57, no. 1-2, p. 51-64, https://doi.org/10.1016/S0166-445X(01)00265-X.","productDescription":"14 p.","startPage":"51","endPage":"64","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":233173,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":207894,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0166-445X(01)00265-X"}],"volume":"57","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a39fde4b0c8380cd61af3","contributors":{"authors":[{"text":"Linville, R.G.","contributorId":39554,"corporation":false,"usgs":true,"family":"Linville","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":402510,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Luoma, S. N.","contributorId":86353,"corporation":false,"usgs":true,"family":"Luoma","given":"S. N.","affiliations":[],"preferred":false,"id":402512,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cutter, L.","contributorId":83310,"corporation":false,"usgs":true,"family":"Cutter","given":"L.","email":"","affiliations":[],"preferred":false,"id":402511,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cutter, G.A.","contributorId":29166,"corporation":false,"usgs":true,"family":"Cutter","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":402509,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70024745,"text":"70024745 - 2002 - Effect of growth conditions and staining procedure upon the subsurface transport and attachment behaviors of a groundwater protist","interactions":[],"lastModifiedDate":"2018-11-28T09:38:51","indexId":"70024745","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":850,"text":"Applied and Environmental Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Effect of growth conditions and staining procedure upon the subsurface transport and attachment behaviors of a groundwater protist","docAbstract":"<div id=\"abstract-1\" class=\"section abstract\"><p id=\"p-2\">The transport and attachment behaviors of<span>&nbsp;</span><i>Spumella guttula</i><span>&nbsp;</span>(Kent), a nanoflagellate (protist) found in contaminated and uncontaminated aquifer sediments in Cape Cod, Mass., were assessed in flowthrough and static columns and in a field injection-and-recovery transport experiment involving an array of multilevel samplers. Transport of<span>&nbsp;</span><i>S. guttula</i><span>&nbsp;</span>harvested from low-nutrient (10 mg of dissolved organic carbon per liter), slightly acidic, granular (porous) growth media was compared to earlier observations involving nanoflagellates grown in a traditional high-nutrient liquid broth. In contrast to the highly retarded (retardation factor of ∼3) subsurface transport previously reported for<span>&nbsp;</span><i>S. guttula</i>, the peak concentration of porous-medium-grown<span>&nbsp;</span><i>S. guttula</i>traveled concomitantly with that of a conservative (bromide) tracer. About one-third of the porous-medium-grown nanoflagellates added to the aquifer were transported at least 2.8 m downgradient, compared to only ∼2% of the broth-grown nanoflagellates. Flowthrough column studies revealed that a vital (hydroethidine [HE]) staining procedure resulted in considerably less attachment (more transport) of<span>&nbsp;</span><i>S. guttula</i><span>&nbsp;</span>in aquifer sediments than did a staining-and-fixation procedure involving 4′,6′-diamidino-2-phenylindole (DAPI) and glutaraldehyde. The calculated collision efficiency (∼10<sup>−2</sup><span>&nbsp;</span>for porous-medium-grown, DAPI-stained nanoflagellates) was comparable to that observed earlier for the indigenous community of unattached groundwater bacteria that serve as prey. The attachment of HE-labeled<span>&nbsp;</span><i>S. guttula</i><span>&nbsp;</span>onto aquifer sediment grains was independent of pH (over the range from pH 3 to 9) suggesting a primary attachment mechanism that may be fundamentally different from that of their prey bacteria, which exhibit sharp decreases in fractional attachment with increasing pH. The high degree of mobility of<span>&nbsp;</span><i>S. guttula</i><span>&nbsp;</span>in the aquifer sediments has important ecological implications for the protistan community within the temporally changing plume of organic contaminants in the Cape Cod aquifer.</p></div>","language":"English","publisher":"ASM","doi":"10.1128/AEM.68.4.1872-1881.2002","issn":"00992240","usgsCitation":"Harvey, R., Mayberry, N., Kinner, N., Metge, D., and Novarino, F., 2002, Effect of growth conditions and staining procedure upon the subsurface transport and attachment behaviors of a groundwater protist: Applied and Environmental Microbiology, v. 68, no. 4, p. 1872-1881, https://doi.org/10.1128/AEM.68.4.1872-1881.2002.","productDescription":"10 p.","startPage":"1872","endPage":"1881","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":478638,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://www.ncbi.nlm.nih.gov/pmc/articles/123859","text":"External Repository"},{"id":233031,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":207807,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1128/AEM.68.4.1872-1881.2002"}],"volume":"68","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a05e6e4b0c8380cd50ffb","contributors":{"authors":[{"text":"Harvey, R.W. 0000-0002-2791-8503","orcid":"https://orcid.org/0000-0002-2791-8503","contributorId":11757,"corporation":false,"usgs":true,"family":"Harvey","given":"R.W.","affiliations":[],"preferred":false,"id":402477,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mayberry, N.","contributorId":56410,"corporation":false,"usgs":true,"family":"Mayberry","given":"N.","email":"","affiliations":[],"preferred":false,"id":402480,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kinner, N.E.","contributorId":29583,"corporation":false,"usgs":true,"family":"Kinner","given":"N.E.","email":"","affiliations":[],"preferred":false,"id":402478,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Metge, D.W.","contributorId":51477,"corporation":false,"usgs":true,"family":"Metge","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":402479,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Novarino, F.","contributorId":75723,"corporation":false,"usgs":true,"family":"Novarino","given":"F.","email":"","affiliations":[],"preferred":false,"id":402481,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70024724,"text":"70024724 - 2002 - Source of solutes to the coastal sabkha of Abu Dhabi","interactions":[],"lastModifiedDate":"2022-01-14T17:15:29.997277","indexId":"70024724","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Source of solutes to the coastal sabkha of Abu Dhabi","docAbstract":"An ascending-brine model is proposed to address the observed isotope geochemistry, solute composition, and solute and water fluxes in the coastal sabkha of the Emirate of Abu Dhabi. Mass-balance measurements document that >95% of the solutes are derived from ascending continental brines; minor amounts are derived from rainfall and from groundwater entering from upgradient areas. Nearly 100% of the annual water loss is from evaporation and not lateral discharge. Direct rainfall on the sabkha and subsequent recharge to the underlying aquifer account for ~ 90% of the annual water input to the system; the remaining 10% comes from both lateral and ascending groundwater flow. Thus, the water and solutes in this system are from different sources. Solute concentrations of conservative (i.e., nonreactive) elements in the coastal, sabkha-covered aquifer are consistent with the fluid pore volumes of ascending brine calculated from hydrologic properties. Calcium to sulfate ratios and sulfur isotopes are consistent with this source of solute from the underlying Tertiary formations. Recharging rainwater dissolves halite and other soluble minerals on the surface, causing the solution to become more dense and sink to the bottom of the aquifer where it vertically mixes with less dense ascending brines. Solutes are returned to the surface by capillary forces and recycled or lost from the system by eolian or fluvial processes. Thus, the system becomes vertically mixed, consistent with the presence of tritium throughout the aquifer; but there is essentially no horizontal mixing of seawater with groundwater. The observed seawater solutes in the supratidal zone come from interstitial seawater trapped by the rapid progradation of the sediments into the Arabian Gulf and are not refluxed or laterally mixed. The ascending-brine model contrasts significantly with both the seawater-flooding and evaporative-pumping models previously proposed as a source of solutes to the coastal sabkha of the Emirate of Abu Dhabi. Use of these earlier models leads to incorrect conclusions and raises serious questions about their applicability in the evaluation of sabkhat in the geologic record.","language":"English","publisher":"GeoScienceWorld","doi":"10.1130/0016-7606(2002)114<0259:SOSTTC>2.0.CO;2","usgsCitation":"Wood, W., Sanford, W., and Al Habshi, A., 2002, Source of solutes to the coastal sabkha of Abu Dhabi: Geological Society of America Bulletin, v. 114, no. 3, p. 259-268, https://doi.org/10.1130/0016-7606(2002)114<0259:SOSTTC>2.0.CO;2.","productDescription":"10 p.","startPage":"259","endPage":"268","costCenters":[],"links":[{"id":233314,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United Arab Emirates","city":"Abu Dhabi","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              54.228515625,\n              24.37712083961039\n            ],\n            [\n              54.33837890624999,\n              24.367113562651262\n            ],\n            [\n              55.26123046875,\n              24.926294766395593\n            ],\n            [\n              55.843505859375,\n              25.72073513441208\n            ],\n            [\n              55.447998046875,\n              25.562265014427492\n            ],\n            [\n              54.964599609375,\n              25.16517336866393\n            ],\n            [\n              54.228515625,\n              24.37712083961039\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"114","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9333e4b08c986b31a362","contributors":{"authors":[{"text":"Wood, W.W.","contributorId":21974,"corporation":false,"usgs":true,"family":"Wood","given":"W.W.","email":"","affiliations":[],"preferred":false,"id":402420,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sanford, W. E. 0000-0002-6624-0280","orcid":"https://orcid.org/0000-0002-6624-0280","contributorId":102112,"corporation":false,"usgs":true,"family":"Sanford","given":"W. E.","affiliations":[],"preferred":false,"id":402422,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Al Habshi, A.R.S.","contributorId":60416,"corporation":false,"usgs":true,"family":"Al Habshi","given":"A.R.S.","email":"","affiliations":[],"preferred":false,"id":402421,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70024687,"text":"70024687 - 2002 - The geohydrologic setting of Yucca Mountain, Nevada","interactions":[],"lastModifiedDate":"2012-03-12T17:20:06","indexId":"70024687","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":835,"text":"Applied Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"The geohydrologic setting of Yucca Mountain, Nevada","docAbstract":"This paper provides a geologic and hydrologic framework of the Yucca Mountain region for the geochemical papers in this volume. The regional geologic units, which range in age from late Precambrian through Holocene, are briefly described. Yucca Mountain is composed of dominantly pyroclastic units that range in age from 11.4 to 15.2 Ma. The principal focus of study has been on the Paintbrush Group, which includes two major zoned and welded ash-flow tuffs separated by an important hydrogeologic unit referred to as the Paintbrush non-welded (PTn). The regional structural setting is currently one of extension, and the major local tectonic domains are presented together with a tectonic model that is consistent with the known structures at Yucca Mountain. Streamflow in this arid to semi-arid region occurs principally in intermittent or ephemeral channels. Near Yucca Mountain, the channels of Fortymile Wash and Amargosa River collect infrequent runoff from tributary basins, ultimately draining to Death Valley. Beneath the surface, large-scale interbasin flow of groundwater from one valley to another occurs commonly in the region. Regional groundwater flow beneath Yucca Mountain originates in the high mesas to the north and returns to the surface either in southern Amargosa Desert or in Death Valley, where it is consumed by evapotranspiration. The water table is very deep beneath the upland areas such as Yucca Mountain, where it is 500-750 m below the land surface, providing a large thickness of unsaturated rocks that are potentially suitable to host a nuclear-waste repository. The nature of unsaturated flow processes, which are important for assessing radionuclide migration, are inferred mainly from hydrochemical or isotopic evidence, from pneumatic tests of the fracture systems, and from the results of in situ experiments. Water seeping down through the unsaturated zone flows rapidly through fractures and more slowly through the pores of the rock matrix. Although capillary forces are expected to divert much of the flow around repository openings, some may drip onto waste packages, ultimately causing release of radionuclides, followed by transport down to the water table. ?? 2002 Elsevier Science Ltd. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Applied Geochemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/S0883-2927(02)00029-X","issn":"08832927","usgsCitation":"Stuckless, J., and Dudley, W.W., 2002, The geohydrologic setting of Yucca Mountain, Nevada: Applied Geochemistry, v. 17, no. 6, p. 659-682, https://doi.org/10.1016/S0883-2927(02)00029-X.","startPage":"659","endPage":"682","numberOfPages":"24","costCenters":[],"links":[{"id":207979,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0883-2927(02)00029-X"},{"id":233313,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bac53e4b08c986b323412","contributors":{"authors":[{"text":"Stuckless, J. S.","contributorId":6060,"corporation":false,"usgs":true,"family":"Stuckless","given":"J. S.","affiliations":[],"preferred":false,"id":402252,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dudley, W. W.","contributorId":101941,"corporation":false,"usgs":true,"family":"Dudley","given":"W.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":402253,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70024673,"text":"70024673 - 2002 - Influence of fracture anisotropy on ground water ages and chemistry, Valley and Ridge province, Pennsylvania","interactions":[],"lastModifiedDate":"2018-11-28T10:23:23","indexId":"70024673","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1861,"text":"Ground Water","active":true,"publicationSubtype":{"id":10}},"title":"Influence of fracture anisotropy on ground water ages and chemistry, Valley and Ridge province, Pennsylvania","docAbstract":"Model ground water ages based on chlorofluorocarbons (CFCs) and tritium/helium-3 (3H/3He) data were obtained from two arrays of nested piezometers located on the north limb of an anticline in fractured sedimentary rocks in the Valley and Ridge geologic province of Pennsylvania. The fracture geometry of the gently east plunging fold is very regular and consists predominately of south dipping to subhorizontal to north dipping bedding-plane parting and east striking, steeply dipping axial-plane spaced cleavage. In the area of the piezometer arrays, which trend north-south on the north limb of the fold, north dipping bedding-plane parting is a more dominant fracture set than is steeply south dipping axial-plane cleavage. The dating of ground water from the piezometer arrays reveals that ground water traveling along paths parallel to the dip direction of bedding-plane parting has younger 3H/3He and CFC model ages, or a greater component of young water, than does ground water traveling along paths opposite to the dip direction. In predominantly unmixed samples there is a strong positive correlation between age of the young fraction of water and dissolved sodium concentration. The travel times inferred from the model ages are significantly longer than those previously calculated by a ground water flow model, which assumed isotropically fractured layers parallel to topography. A revised model factors in the directional anisotropy to produce longer travel times. Ground water travel times in the watershed therefore appear to be more influenced by anisotropic fracture geometry than previously realized. This could have significant implications for ground water models in other areas underlain by similarly tilted or folded sedimentary rock, such as elsewhere in the Valley and Ridge or the early Mesozoic basins.","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.2002.tb02652.x","issn":"0017467X","usgsCitation":"Burton, W., Plummer, N., Busenberg, E., Lindsey, B., and Gburek, W., 2002, Influence of fracture anisotropy on ground water ages and chemistry, Valley and Ridge province, Pennsylvania: Ground Water, v. 40, no. 3, p. 242-257, https://doi.org/10.1111/j.1745-6584.2002.tb02652.x.","productDescription":"16 p.","startPage":"242","endPage":"257","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":233096,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Valley and Ridge Province","volume":"40","issue":"3","noUsgsAuthors":false,"publicationDate":"2005-12-13","publicationStatus":"PW","scienceBaseUri":"505a3b3ae4b0c8380cd6233c","contributors":{"authors":[{"text":"Burton, W.C.","contributorId":41439,"corporation":false,"usgs":true,"family":"Burton","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":402186,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":402189,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Busenberg, E.","contributorId":56796,"corporation":false,"usgs":true,"family":"Busenberg","given":"E.","affiliations":[],"preferred":false,"id":402187,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lindsey, B.D.","contributorId":89696,"corporation":false,"usgs":true,"family":"Lindsey","given":"B.D.","email":"","affiliations":[],"preferred":false,"id":402190,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gburek, W.J.","contributorId":76098,"corporation":false,"usgs":true,"family":"Gburek","given":"W.J.","affiliations":[],"preferred":false,"id":402188,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70024672,"text":"70024672 - 2002 - Regional controls on geomorphology, hydrology, and ecosystem integrity in the Orinoco Delta, Venezuela","interactions":[],"lastModifiedDate":"2012-03-12T17:20:07","indexId":"70024672","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1801,"text":"Geomorphology","active":true,"publicationSubtype":{"id":10}},"title":"Regional controls on geomorphology, hydrology, and ecosystem integrity in the Orinoco Delta, Venezuela","docAbstract":"Interacting river discharge, tidal oscillation, and tropical rainfall across the 22,000 km2 Orinoco delta plain support diverse fresh and brackish water ecosystems. To develop environmental baseline information for this largely unpopulated region, we evaluate major coastal plain, shallow marine, and river systems of northeastern South America, which serves to identify principal sources and controls of water and sediment flow into, through, and out of the Orinoco Delta. The regional analysis includes a summary of the geology, hydrodynamics, sediment dynamics, and geomorphic characteristics of the Orinoco drainage basin, river, and delta system. Because the Amazon River is a major source of sediment deposited along the Orinoco coast, we summarize Amazon water and sediment input to the northeastern South American littoral zone. We investigate sediment dynamics and geomorphology of the Guiana coast, where marine processes and Holocene history are similar to the Orinoco coast. Major factors controlling Orinoco Delta water and sediment dynamics include the pronounced annual flood discharge; the uneven distribution of water and sediment discharge across the delta plain; discharge of large volumes of water with low sediment concentrations through the Rio Grande and Araguao distributaries; water and sediment dynamics associated with the Guayana littoral current along the northeastern South American coast; inflow of large volumes of Amazon sediment to the Orinoco coast; development of a fresh water plume seaward of Boca Grande; disruption of the Guayana Current by Trinidad, Boca de Serpientes, and Gulf of Paria; and the constriction at Boca de Serpientes. ?? 2002 Elsevier Science B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geomorphology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/S0169-555X(01)00179-9","issn":"0169555X","usgsCitation":"Warne, A., Meade, R., White, W., Guevara, E., Gibeaut, J., Smyth, R., Aslan, A., and Tremblay, T., 2002, Regional controls on geomorphology, hydrology, and ecosystem integrity in the Orinoco Delta, Venezuela: Geomorphology, v. 44, no. 3-4, p. 273-307, https://doi.org/10.1016/S0169-555X(01)00179-9.","startPage":"273","endPage":"307","numberOfPages":"35","costCenters":[],"links":[{"id":478648,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.505.3083","text":"External Repository"},{"id":207850,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0169-555X(01)00179-9"},{"id":233095,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e4a4b6e4b0e8fec6cdbc1b","contributors":{"authors":[{"text":"Warne, A.G.","contributorId":97669,"corporation":false,"usgs":true,"family":"Warne","given":"A.G.","email":"","affiliations":[],"preferred":false,"id":402184,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meade, R.H.","contributorId":27449,"corporation":false,"usgs":true,"family":"Meade","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":402180,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"White, W.A.","contributorId":24489,"corporation":false,"usgs":true,"family":"White","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":402179,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Guevara, E.H.","contributorId":89693,"corporation":false,"usgs":true,"family":"Guevara","given":"E.H.","email":"","affiliations":[],"preferred":false,"id":402183,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gibeaut, J.","contributorId":51502,"corporation":false,"usgs":true,"family":"Gibeaut","given":"J.","email":"","affiliations":[],"preferred":false,"id":402182,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Smyth, R.C.","contributorId":41994,"corporation":false,"usgs":true,"family":"Smyth","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":402181,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Aslan, A.","contributorId":9802,"corporation":false,"usgs":true,"family":"Aslan","given":"A.","email":"","affiliations":[],"preferred":false,"id":402178,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Tremblay, T.","contributorId":106288,"corporation":false,"usgs":true,"family":"Tremblay","given":"T.","email":"","affiliations":[],"preferred":false,"id":402185,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70024670,"text":"70024670 - 2002 - U-Pb ages of secondary silica at Yucca Mountain, Nevada: Implications for the paleohydrology of the unsaturated zone","interactions":[],"lastModifiedDate":"2012-03-12T17:20:07","indexId":"70024670","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":835,"text":"Applied Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"U-Pb ages of secondary silica at Yucca Mountain, Nevada: Implications for the paleohydrology of the unsaturated zone","docAbstract":"Uranium, Th and Pb isotopes were analyzed in layers of opal and chalcedony from individual mm- to cm-thick calcite and silica coatings at Yucca Mountain, Nevada, USA, a site that is being evaluated for a potential high-level nuclear waste repository. These calcite and silica coatings on fractures and in lithophysal cavities in Miocene-age tuffs in the unsaturated zone (UZ) precipitated from descending water and record a long history of percolation through the UZ. Opal and chalcedony have high concentrations of U (10 to 780 ppm) and low concentrations of common Pb as indicated by large values of 206Pb/204Pb (up to 53,806), thus making them suitable for U-Pb age determinations. Interpretations of U-Pb isotope systems in opal samples at Yucca Mountain are complicated by the incorporation of excess 234U at the time of mineral formation, resulting in reverse discordance of U-Pb ages. However, the 207PB/235U ages are much less affected by deviation from initial secular equilibrium and provide reliable ages of most silica deposits between 0.6 and 9.8 Ma. For chalcedony subsamples showing normal age discordance, these ages may represent minimum times of deposition. Typically, 207Pb/235U ages are consistent with the microstratigraphy in the mineral coating samples, such that the youngest ages are for subsamples from outer layers, intermediate ages are from inner layers, and oldest ages are from innermost layers. 234U and 230Th in most silica layers deeper in the coatings are in secular equilibrium with 238U, which is consistent with their old age and closed system behavior during the past -0.5 Ma. The ages for subsamples of silica layers from different microstratigraphic positions in individual calcite and silica coating samples collected from lithophysal cavities in the welded part of the Topopah Spring Tuff yield slow long-term average growth rates of 1 to 5 mm/Ma. These data imply that the deeper parts of the UZ at Yucca Mountain maintained long-term hydrologic stability over the past 10 Ma. despite significant climate variations. U-Pb ages for subsamples of silica layers from different microstratigraphic positions in individual calcite and silica coating samples collected from fractures in the shallower part of the UZ (welded part of the overlying Tiva Canyon Tuff) indicate larger long-term average growth rates up to 23 mm/Ma and an absence of recently deposited materials (ages of outermost layers are 3-5 Ma.). These differences between the characteristics of the coatings for samples from the shallower and deeper parts of the UZ may indicate that the nonwelded tuffs (PTn), located between the welded parts of the Tiva Canyon and Topopah Spring Tuffs, play an important role in moderating UZ flow.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Applied Geochemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/S0883-2927(02)00032-X","issn":"08832927","usgsCitation":"Neymark, L., Amelin, Y., Paces, J., and Peterman, Z.E., 2002, U-Pb ages of secondary silica at Yucca Mountain, Nevada: Implications for the paleohydrology of the unsaturated zone: Applied Geochemistry, v. 17, no. 6, p. 709-734, https://doi.org/10.1016/S0883-2927(02)00032-X.","startPage":"709","endPage":"734","numberOfPages":"26","costCenters":[],"links":[{"id":478726,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digital.library.unt.edu/ark:/67531/metadc740548/","text":"External Repository"},{"id":207826,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0883-2927(02)00032-X"},{"id":233061,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb9c3e4b08c986b327dba","contributors":{"authors":[{"text":"Neymark, L.A. 0000-0003-4190-0278","orcid":"https://orcid.org/0000-0003-4190-0278","contributorId":56673,"corporation":false,"usgs":true,"family":"Neymark","given":"L.A.","affiliations":[],"preferred":false,"id":402174,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Amelin, Y.","contributorId":62800,"corporation":false,"usgs":true,"family":"Amelin","given":"Y.","affiliations":[],"preferred":false,"id":402175,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Paces, J.B. 0000-0002-9809-8493","orcid":"https://orcid.org/0000-0002-9809-8493","contributorId":27482,"corporation":false,"usgs":true,"family":"Paces","given":"J.B.","affiliations":[],"preferred":false,"id":402173,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Peterman, Z. E.","contributorId":63781,"corporation":false,"usgs":true,"family":"Peterman","given":"Z.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":402176,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70024640,"text":"70024640 - 2002 - Crosswell seismic investigation of hydraulically conductive, fracture bedrock near Mirror Lake, New Hampshire","interactions":[],"lastModifiedDate":"2018-11-26T09:53:27","indexId":"70024640","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2165,"text":"Journal of Applied Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Crosswell seismic investigation of hydraulically conductive, fracture bedrock near Mirror Lake, New Hampshire","docAbstract":"<div id=\"abstracts\" class=\"Abstracts\"><div id=\"aep-abstract-id14\" class=\"abstract author\"><div id=\"aep-abstract-sec-id15\"><p>Near Mirror Lake, New Hampshire (USA), hydraulically conductive, fractured bedrock was investigated with the crosswell seismic method to determine whether this method could provide any information about hydraulic conductivity between wells. To this end, crosswell seismic data, acoustic logs from boreholes, image logs from boreholes, and single borehole hydraulic tests were analyzed. The analysis showed that, first, the P-wave velocities from the acoustic logs tended to be higher in schist than they were in granite. (Schist and granite were the dominant rock types). Second, the P-wave velocities from the acoustic logs tended to be low near fractures. Third, the hydraulic conductivity was always low (always less than to 10<sup>−8</sup><span>&nbsp;</span>m/s) where no fractures intersected the borehole, but the hydraulic conductivity ranged from low to high (from less than to 10<sup>−10</sup><span>&nbsp;</span>m/s to 10<sup>−4</sup><span>&nbsp;</span>m/s) where one or more fractures intersected the borehole. Fourth, high hydraulic conductivities were slightly more frequent when the P-wave velocity was low (less than 5200 m/s) than when it was high (greater than or equal to 5200 m/s). The interpretation of this statistical relation was that the fractures tended to increase the hydraulic conductivity and to lower the P-wave velocity. This statistical relation was applied to a velocity tomogram to create a map showing the probability of high hydraulic conductivity; the map was consistent with results from independent hydraulic tests.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/S0926-9851(02)00149-0","issn":"09269851","usgsCitation":"Ellefsen, K., Hsieh, P.A., and Shapiro, A., 2002, Crosswell seismic investigation of hydraulically conductive, fracture bedrock near Mirror Lake, New Hampshire: Journal of Applied Geophysics, v. 50, no. 3, p. 299-317, https://doi.org/10.1016/S0926-9851(02)00149-0.","productDescription":"19 p.","startPage":"299","endPage":"317","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":233132,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":207874,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0926-9851(02)00149-0"}],"country":"United States","state":"New Hampshire","otherGeospatial":"Mirror Lake","volume":"50","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fcc8e4b0c8380cd4e429","contributors":{"authors":[{"text":"Ellefsen, K.J. 0000-0003-3075-4703","orcid":"https://orcid.org/0000-0003-3075-4703","contributorId":12061,"corporation":false,"usgs":true,"family":"Ellefsen","given":"K.J.","affiliations":[],"preferred":false,"id":402064,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hsieh, P. A.","contributorId":40596,"corporation":false,"usgs":true,"family":"Hsieh","given":"P.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":402065,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shapiro, A.M. 0000-0002-6425-9607","orcid":"https://orcid.org/0000-0002-6425-9607","contributorId":88384,"corporation":false,"usgs":true,"family":"Shapiro","given":"A.M.","affiliations":[],"preferred":true,"id":402066,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70024618,"text":"70024618 - 2002 - Parasite (Ribeiroia ondatrae) infection linked to amphibian malformations in the western United States","interactions":[],"lastModifiedDate":"2018-11-28T08:41:07","indexId":"70024618","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1459,"text":"Ecological Monographs","active":true,"publicationSubtype":{"id":10}},"title":"Parasite (Ribeiroia ondatrae) infection linked to amphibian malformations in the western United States","docAbstract":"<p>Parasites and pathogens can influence the survivorship, behavior, and very structure of their host species. For example, experimental studies have shown that trematode parasites can cause high frequencies of severe limb malformations in amphibians. In a broad-scale field survey covering parts of California, Oregon, Washington, Idaho, and Montana, we examined relationships between the frequency and types of morphological abnormalities in amphibians and the abundance of trematode parasite infection, pH, concentrations of 61 pesticides, and levels of orthophosphate and total nitrate. We recorded severe malformations at frequencies ranging from 1% to 90% in nine amphibian species from 53 aquatic systems. Infection of larvae by the trematode Ribeiroia ondatrae was associated with, and functionally related to, higher frequencies of amphibian limb malformations than found in uninfected populations (≤5%). Parasites were concentrated around the basal tissue of hind limbs in infected anurans, and malformations associated with infection included skin webbings, supernumerary limbs and digits, and missing or malformed hind limbs. In the absence of Ribeiroia, amphibian populations exhibited low (0-5%) frequencies of abnormalities involving missing digits or distal portions of a hind limb. Species were affected differentially by the parasite, and Ambystoma macrodactylum, Hyla regilla, Rand aurora, R. luteiventris, and Taricha torosa typically exhibited the highest frequencies of abnormalities. None of the water-quality variables measured was associated with malformed amphibians, but aquatic snail hosts (Planorbella spp.) were significant predictors of the presence and abundance of Ribeiroia infection. Morphological comparisons of adult specimens of Ribeiroia collected from different sites and raised in experimental definitive hosts suggested that all samples represented the same species - R. ondatrae. These field results, coupled with experimental research on the effects of Ribeiroia on amphibians, demonstrate that Ribeiroia infection is an important and widespread cause of amphibian limb malformations in the western United States. The relevance of trematode infection to declines of amphibian populations and the influence of habitat modification on the pathology and life cycle of Ribeiroia are emphasized as areas requiring further research.</p>","language":"English","publisher":"ESA","doi":"10.1890/0012-9615(2002)072[0151:PROILT]2.0.CO;2","issn":"00129615","usgsCitation":"Johnson, P., Lunde, K., Thurman, E., Ritchie, E., Wray, S., Sutherland, D., Kapfer, J., Frest, T., Bowerman, J., and Blaustein, A., 2002, Parasite (Ribeiroia ondatrae) infection linked to amphibian malformations in the western United States: Ecological Monographs, v. 72, no. 2, p. 151-168, https://doi.org/10.1890/0012-9615(2002)072[0151:PROILT]2.0.CO;2.","productDescription":"18 p.","startPage":"151","endPage":"168","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":233308,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","volume":"72","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a74d6e4b0c8380cd77867","contributors":{"authors":[{"text":"Johnson, P.T.J.","contributorId":104255,"corporation":false,"usgs":true,"family":"Johnson","given":"P.T.J.","email":"","affiliations":[],"preferred":false,"id":401934,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lunde, K.B.","contributorId":10200,"corporation":false,"usgs":true,"family":"Lunde","given":"K.B.","email":"","affiliations":[],"preferred":false,"id":401925,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thurman, E.M.","contributorId":102864,"corporation":false,"usgs":true,"family":"Thurman","given":"E.M.","affiliations":[],"preferred":false,"id":401933,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ritchie, E.G.","contributorId":97285,"corporation":false,"usgs":true,"family":"Ritchie","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":401932,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wray, S.N.","contributorId":90505,"corporation":false,"usgs":true,"family":"Wray","given":"S.N.","email":"","affiliations":[],"preferred":false,"id":401930,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Sutherland, D.R.","contributorId":15376,"corporation":false,"usgs":true,"family":"Sutherland","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":401926,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kapfer, J.M.","contributorId":68505,"corporation":false,"usgs":true,"family":"Kapfer","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":401928,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Frest, T.J.","contributorId":70964,"corporation":false,"usgs":true,"family":"Frest","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":401929,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Bowerman, J.","contributorId":94824,"corporation":false,"usgs":true,"family":"Bowerman","given":"J.","email":"","affiliations":[],"preferred":false,"id":401931,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Blaustein, A.R.","contributorId":40325,"corporation":false,"usgs":true,"family":"Blaustein","given":"A.R.","affiliations":[],"preferred":false,"id":401927,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70024589,"text":"70024589 - 2002 - Fluvial sediment transport and deposition following the 1991 eruption of Mount Pinatubo","interactions":[],"lastModifiedDate":"2012-03-12T17:20:14","indexId":"70024589","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1801,"text":"Geomorphology","active":true,"publicationSubtype":{"id":10}},"title":"Fluvial sediment transport and deposition following the 1991 eruption of Mount Pinatubo","docAbstract":"The 1991 eruption of Mount Pinatubo generated extreme sediment yields from watersheds heavily impacted by pyroclastic flows. Bedload sampling in the Pasig-Potrero River, one of the most heavily impacted rivers, revealed negligible critical shear stress and very high transport rates that reflected an essentially unlimited sediment supply and the enhanced mobility of particles moving over a smooth, fine-grained bed. Dimensionless bedload transport rates in the Pasig-Potrero River differed substantially from those previously reported for rivers in temperate regions for the same dimensionless shear stress, but were similar to rates identified in rivers on other volcanoes and ephemeral streams in arid environments. The similarity between volcanically disturbed and arid rivers appears to arise from the lack of an armored bed surface due to very high relative sediment supply; in arid rivers, this is attributed to a flashy hydrograph, whereas volcanically disturbed rivers lack armoring due to sustained high rates of sediment delivery. This work suggests that the increases in sediment supply accompanying massive disturbance induce morphologic and hydrologic changes that temporarily enhance transport efficiency until the watershed recovers and sediment supply is reduced. ?? 2002 Elsevier Science B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geomorphology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/S0169-555X(01)00155-6","issn":"0169555X","usgsCitation":"Hayes, S., Montgomery, D.R., and Newhall, C.G., 2002, Fluvial sediment transport and deposition following the 1991 eruption of Mount Pinatubo: Geomorphology, v. 45, no. 3-4, p. 211-224, https://doi.org/10.1016/S0169-555X(01)00155-6.","startPage":"211","endPage":"224","numberOfPages":"14","costCenters":[],"links":[{"id":207641,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0169-555X(01)00155-6"},{"id":232769,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a12a4e4b0c8380cd543a4","contributors":{"authors":[{"text":"Hayes, S.K.","contributorId":81667,"corporation":false,"usgs":true,"family":"Hayes","given":"S.K.","email":"","affiliations":[],"preferred":false,"id":401808,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Montgomery, D. R.","contributorId":41582,"corporation":false,"usgs":false,"family":"Montgomery","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":401807,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Newhall, C. G.","contributorId":93056,"corporation":false,"usgs":true,"family":"Newhall","given":"C.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":401809,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70024574,"text":"70024574 - 2002 - Effects of tidal shallowing and deepening on phytoplankton production dynamics: A modeling study","interactions":[],"lastModifiedDate":"2018-11-26T10:39:16","indexId":"70024574","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1583,"text":"Estuaries","active":true,"publicationSubtype":{"id":10}},"title":"Effects of tidal shallowing and deepening on phytoplankton production dynamics: A modeling study","docAbstract":"<p>Processes influencing estuarine phytoplankton growth occur over a range of time scales, but many conceptual and numerical models of estuarine phytoplankton production dynamics neglect mechanisms occurring on the shorter (e.g., intratidal) time scales. We used a numerical model to explore the influence of short time-scale variability in phytoplankton sources and sinks on long-term growth in an idealized water column that shallows and deepens with the semidiurnal tide. Model results show that tidal fluctuations in water surface elevation can determine whether long-term phytoplankton growth is positive or negative. Hourly-scale interactions influencing weekly-scale to monthly-scale phytoplankton dynamics include intensification of the depth-averaged benthic grazing effect by water column shallowing and enhancement of water column photosynthesis when solar noon coincides with low tide. Photosynthesis and benthic consumption may modulate over biweekly time scales due to spring-neap fluctuations in tidal range and the 15-d cycle of solar noon-low tide phasing. If tidal range is a large fraction of mean water depth, then tidal shallowing and deepening may significantly influence net phytoplankton growth. In such a case, models or estimates of long-term phytoplankton production dynamics that neglect water surface fluctuations may overestimate or underestimate net growth and could even predict the wrong sign associated with net growth rate.</p>","language":"English","publisher":"Springer","doi":"10.1007/BF02804885","issn":"01608347","usgsCitation":"Lucas, L., and Cloern, J., 2002, Effects of tidal shallowing and deepening on phytoplankton production dynamics: A modeling study: Estuaries, v. 25, no. 4 A, p. 497-507, https://doi.org/10.1007/BF02804885.","productDescription":"11 p.","startPage":"497","endPage":"507","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":233162,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"4 A","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a080de4b0c8380cd51955","contributors":{"authors":[{"text":"Lucas, L.V.","contributorId":62777,"corporation":false,"usgs":true,"family":"Lucas","given":"L.V.","email":"","affiliations":[],"preferred":false,"id":401754,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cloern, J. E.","contributorId":59453,"corporation":false,"usgs":true,"family":"Cloern","given":"J. E.","affiliations":[],"preferred":false,"id":401753,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70024552,"text":"70024552 - 2002 - Movement of water through the thick unsaturated zone underlying Oro Grande and Sheep Creek Washes in the western Mojave Desert, USA","interactions":[],"lastModifiedDate":"2018-09-19T08:36:41","indexId":"70024552","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","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":"Movement of water through the thick unsaturated zone underlying Oro Grande and Sheep Creek Washes in the western Mojave Desert, USA","docAbstract":"Previous studies indicate that a small quantity of recharge occurs from infiltration of streamflow in intermittent streams in the upper Mojave River basin, in the western Mojave Desert, near Victorville, California. Chloride, tritium, and stable isotope data collected in the unsaturated zone between 1994 and 1998 from boreholes drilled in Oro Grande and Sheep Creek Washes indicate that infiltration of streamflow occurs to depths below the root zone, and presumably to the water table, along much of Oro Grande Wash and near the mountain front along Sheep Creek Wash. Differences in infiltration at sites along each wash are the result of hydrologic variables such as proximity to the mountain front, quantity of streamflow, and texture of the subsurface deposits. Differences in infiltration between the washes are the result of large-scale geomorphic processes. For example, Oro Grande wash is incised into the Victorville fan and infiltration has occurred at approximately the same location over recent geologic time. In contrast, Sheep Creek Wash overlies an active alluvial fan and the stream channel can move across the fan surface through time. Infiltration does not occur to depths below the root zone at control sites outside of the washes.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hydrogeology Journal","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10040-002-0194-8","issn":"14312174","usgsCitation":"Izbicki, J., Radyk, J., and Michel, R.L., 2002, Movement of water through the thick unsaturated zone underlying Oro Grande and Sheep Creek Washes in the western Mojave Desert, USA: Hydrogeology Journal, v. 10, no. 3, p. 409-427, https://doi.org/10.1007/s10040-002-0194-8.","startPage":"409","endPage":"427","numberOfPages":"19","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":232843,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":207685,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10040-002-0194-8"}],"volume":"10","issue":"3","noUsgsAuthors":false,"publicationDate":"2002-04-24","publicationStatus":"PW","scienceBaseUri":"505a5f27e4b0c8380cd70dd5","contributors":{"authors":[{"text":"Izbicki, J. A. 0000-0003-0816-4408","orcid":"https://orcid.org/0000-0003-0816-4408","contributorId":28244,"corporation":false,"usgs":true,"family":"Izbicki","given":"J. A.","affiliations":[],"preferred":false,"id":401686,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Radyk, J.","contributorId":63984,"corporation":false,"usgs":true,"family":"Radyk","given":"J.","email":"","affiliations":[],"preferred":false,"id":401687,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Michel, R. L.","contributorId":86375,"corporation":false,"usgs":true,"family":"Michel","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":401688,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70024548,"text":"70024548 - 2002 - 15N NMR investigation of the reduction and binding of TNT in an aerobic bench scale reactor simulating windrow composting","interactions":[],"lastModifiedDate":"2020-01-04T14:00:13","indexId":"70024548","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"15N NMR investigation of the reduction and binding of TNT in an aerobic bench scale reactor simulating windrow composting","docAbstract":"T15NT was added to a soil of low organic carbon content and composted for 20 days in an aerobic bench scale reactor. The finished whole compost and fulvic acid, humic acid, humin, and lignocellulose fractions extracted from the compost were analyzed by solid-state CP/MAS and DP/MAS 15N NMR. 15N NMR spectra provided direct spectroscopic evidence for reduction of TNT followed by covalent binding of the reduced metabolites to organic matter of the composted soil, with the majority of metabolite found in the lignocellulose fraction, by mass also the major fraction of the compost. In general, the types of bonds formed between soil organic matter and reduced TNT amines in controlled laboratory reactions were observed in the spectra of the whole compost and fractions, confirming that during composting TNT is reduced to amines that form covalent bonds with organic matter through aminohydroquinone, aminoquinone, heterocyclic, and imine linkages, among others. Concentrations of imine nitrogens in the compost spectra suggestthat covalent binding bythe diamines 2,4DANT and 2,6DANT is a significant process in the transformation of TNT into bound residues. Liquid-phase 15N NMR spectra of the fulvic acid and humin fractions provided possible evidence for involvement of phenoloxidase enzymes in covalent bond formation.","language":"English","publisher":"ACS","doi":"10.1021/es011382r","issn":"0013936X","usgsCitation":"Thorn, K.A., Pennington, J., and Hayes, C., 2002, 15N NMR investigation of the reduction and binding of TNT in an aerobic bench scale reactor simulating windrow composting: Environmental Science & Technology, v. 36, no. 17, p. 3797-3805, https://doi.org/10.1021/es011382r.","productDescription":"9 p.","startPage":"3797","endPage":"3805","numberOfPages":"9","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":232764,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","issue":"17","noUsgsAuthors":false,"publicationDate":"2002-08-06","publicationStatus":"PW","scienceBaseUri":"5059e227e4b0c8380cd459d8","contributors":{"authors":[{"text":"Thorn, K. A.","contributorId":33294,"corporation":false,"usgs":true,"family":"Thorn","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":401670,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pennington, J.C.","contributorId":105085,"corporation":false,"usgs":true,"family":"Pennington","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":401672,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hayes, C.A.","contributorId":50691,"corporation":false,"usgs":true,"family":"Hayes","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":401671,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70024539,"text":"70024539 - 2002 - Nitrate in aquifers beneath agricultural systems","interactions":[],"lastModifiedDate":"2012-03-12T17:20:06","indexId":"70024539","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Nitrate in aquifers beneath agricultural systems","docAbstract":"Research from several regions of the world provides spatially anecdotal evidence to hypothesize which hydrologic and agricultural factors contribute to groundwater vulnerability to nitrate contamination. Analysis of nationally consistent measurements from the U.S. Geological Survey's NAWOA program confirms these hypotheses for a substantial range of agricultural systems. Shallow unconfined aquifers are most susceptible to nitrate contamination associated with agricultural systems. Alluvial and other unconsolidated aquifers are the most vulnerable and shallow carbonate aquifers provide a substantial but smaller contamination risk. Where any of these aquifers are overlain by permeable soils the risk of contamination is larger. Irrigated systems can compound this vulnerability by increasing leaching facilitated by additional recharge and additional nutrient applications. The agricultural system of corn, soybeans, and hogs produced significantly larger concentrations of groundwater nitrate than all other agricultural systems, although mean nitrate concentrations in counties with dairy, poultry, cattle and grains, and horticulture systems were similar. If trends in the relation between increased fertilizer use and groundwater nitrate in the United States are repeated in other regions of the world, Asia may experience increasing problems because of recent increases in fertilizer use. Groundwater monitoring in Western and Eastern Europe as well as Russia over the next decade may provide data to determine if the trend in increased nitrate contamination can be reversed. If the concentrated livestock trend in the United States is global, it may be accompanied by increasing nitrogen contamination in groundwater. Concentrated livestock provide both point sources in the confinement area and intense non-point sources as fields close to facilities are used for manure disposal. Regions where irrigated cropland is expanding, such as in Asia, may experience the greatest impact of this practice.","largerWorkTitle":"Water Science and Technology","language":"English","issn":"02731223","usgsCitation":"Burkart, M.R., and Stoner, J., 2002, Nitrate in aquifers beneath agricultural systems, <i>in</i> Water Science and Technology, v. 45, no. 9, p. 19-28.","startPage":"19","endPage":"28","numberOfPages":"10","costCenters":[],"links":[{"id":233160,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a66a1e4b0c8380cd72eb9","contributors":{"authors":[{"text":"Burkart, M. R.","contributorId":42190,"corporation":false,"usgs":true,"family":"Burkart","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":401640,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stoner, J.D.","contributorId":58261,"corporation":false,"usgs":true,"family":"Stoner","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":401641,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70024538,"text":"70024538 - 2002 - Potential toxicity of pesticides measured in midwestern streams to aquatic organisms","interactions":[],"lastModifiedDate":"2018-11-28T09:55:48","indexId":"70024538","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3724,"text":"Water Science and Technology","active":true,"publicationSubtype":{"id":10}},"title":"Potential toxicity of pesticides measured in midwestern streams to aquatic organisms","docAbstract":"<p><span>Society is becoming increasingly aware of the value of healthy aquatic ecosystems as well as the effects that man’s activities have on those ecosystems. In recent years, many urban and industrial sources of contamination have been reduced or eliminated. The agricultural community also has worked towards reducing off-site movement of agricultural chemicals, but their use in farming is still growing. A small fraction, estimated at &lt;1 to 2% of the pesticides applied to crops are lost from fields and enter nearby streams during rainfall events. In many cases aquatic organisms are exposed to mixtures of chemicals, which may lead to greater non-target risk than that predicted based on traditional risk assessments for single chemicals. We evaluated the potential toxicity of environmental mixtures of 5 classes of pesticides using concentrations from water samples collected from ∼50 sites on midwestern streams during late spring or early summer runoff events in 1989 and 1998. Toxicity index values are calculated as the concentration of the compound in the sample divided by the EC50 or LC50 of an aquatic organism. These index values are summed within a pesticide class and for all classes to determine additive pesticide class and total pesticide toxicity indices. Toxicity index values greater than 1.0 indicate probable toxicity of a class of pesticides measured in a water sample to aquatic organisms. Results indicate that some samples had probable toxicity to duckweed and green algae, but few are suspected of having significant toxicity to bluegill sunfish or chorus frogs.</span></p>","language":"English","publisher":"IWA Publishing","usgsCitation":"Battaglin, W., and Fairchild, J., 2002, Potential toxicity of pesticides measured in midwestern streams to aquatic organisms: Water Science and Technology, v. 45, no. 9, p. 95-103.","productDescription":"9 p.","startPage":"95","endPage":"103","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":233126,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":351866,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://wst.iwaponline.com/content/45/9/95"}],"volume":"45","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7f65e4b0c8380cd7aae3","contributors":{"authors":[{"text":"Battaglin, W.","contributorId":80388,"corporation":false,"usgs":true,"family":"Battaglin","given":"W.","email":"","affiliations":[],"preferred":false,"id":401639,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fairchild, J.","contributorId":50321,"corporation":false,"usgs":true,"family":"Fairchild","given":"J.","email":"","affiliations":[],"preferred":false,"id":401638,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70024535,"text":"70024535 - 2002 - Historical patterns of river stage and fish communities as criteria for operations of dams on the Illinois river","interactions":[],"lastModifiedDate":"2018-02-23T15:38:59","indexId":"70024535","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3301,"text":"River Research and Applications","active":true,"publicationSubtype":{"id":10}},"title":"Historical patterns of river stage and fish communities as criteria for operations of dams on the Illinois river","docAbstract":"<p><span>The hydrologic regime of the Illinois River has been altered over the past 100 years. Locks and dams regulate water surface elevations and flow, enabling commercial navigation to continue year round. This study relates changes in water surface elevation to fish abundance in the river, and establishes target criteria for operating locks and dams. Using long-term records of daily river stage, we identified ecologically meaningful hydrological parameters for eight gage locations along the Illinois River. Inter-annual variability of a long-term fisheries dataset beginning in 1957 was related to variability in stage, flood and recession duration, frequency, timing, and rate of change of water levels. Reversals in water surface elevation, maximum stage levels, and length of the spring flood were the most important parameters influencing abundance of age-zero fishes in annual collections. Smallmouth buffalo (</span><i>Ictiobus bubalus</i><span>), black crappie (</span><i>Pomoxis nigromaculatus</i><span>), freshwater drum (</span><i>Aplodinotus grunneins</i><span>), and white bass (</span><i>Morone chrysops</i><span>) were most abundant in samples during years that approximated the natural water level regime. Of the 33 hydrologic parameters evaluated for the entire water year from an Illinois River gage site on La Grange Reach, all except average stage in January and Julian date (JD) of maximum stage had moderate or high hydrologic alteration based on the historical range of variation (RVA). The highest degree of hydrologic alteration was for minimum stage levels (1-day, 3-day, and 7-day), rate-of-rise, and rate-of-fall. Other parameters that have been severely altered were 30-day minimum stage, 90-day maximum stage, and the annual number of water level reversals. Operations of the La Grange and Peoria locks and dams could be modified so water level variability would approximate that of the late 1800s, when fish and wildlife resources were abundant. The water regime could be regulated to maintain navigation and improve conditions for native plants and animals without increasing flood damages.</span></p>","language":"English","publisher":"Wiley","doi":"10.1002/rra.630","usgsCitation":"Koel, T., and Sparks, R.E., 2002, Historical patterns of river stage and fish communities as criteria for operations of dams on the Illinois river: River Research and Applications, v. 18, no. 1, p. 3-19, https://doi.org/10.1002/rra.630.","productDescription":"17 p.","startPage":"3","endPage":"19","costCenters":[],"links":[{"id":233087,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Illinois River","volume":"18","issue":"1","noUsgsAuthors":false,"publicationDate":"2002-01-28","publicationStatus":"PW","scienceBaseUri":"505a3195e4b0c8380cd5e045","contributors":{"authors":[{"text":"Koel, Todd M.","contributorId":196920,"corporation":false,"usgs":false,"family":"Koel","given":"Todd M.","affiliations":[],"preferred":false,"id":401612,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sparks, Richard E.","contributorId":39091,"corporation":false,"usgs":false,"family":"Sparks","given":"Richard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":401613,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70024534,"text":"70024534 - 2002 - Classification of reaches in the Missouri and lower Yellowstone Rivers based on flow characteristics","interactions":[],"lastModifiedDate":"2018-02-23T15:40:07","indexId":"70024534","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3301,"text":"River Research and Applications","active":true,"publicationSubtype":{"id":10}},"title":"Classification of reaches in the Missouri and lower Yellowstone Rivers based on flow characteristics","docAbstract":"<p><span>Several aspects of flow have been shown to be important determinants of biological community structure and function in streams, yet direct application of this approach to large rivers has been limited. Using a multivariate approach, we grouped flow gauges into hydrologically similar units in the Missouri and lower Yellowstone Rivers and developed a model based on flow variability parameters that could be used to test hypotheses about the role of flow in determining aquatic community structure. This model could also be used for future comparisons as the hydrological regime changes. A suite of hydrological parameters for the recent, post-impoundment period (1 October 1966–30 September 1996) for each of 15 gauges along the Missouri and lower Yellowstone Rivers were initially used. Preliminary graphical exploration identified five variables for use in further multivariate analyses. Six hydrologically distinct units composed of gauges exhibiting similar flow characteristics were then identified using cluster analysis. Discriminant analyses identified the three most influential variables as flow per unit drainage area, coefficient of variation of mean annual flow, and flow constancy. One surprising result was the relative similarity of flow regimes between the two uppermost and three lowermost gauges, despite large differences in magnitude of flow and separation by roughly 3000 km. Our results synthesize, simplify and interpret the complex changes in flow occurring along the Missouri and lower Yellowstone Rivers, and provide an objective grouping for future tests of how these changes may affect biological communities.&nbsp;</span></p>","language":"English","publisher":"Wiley","doi":"10.1002/rra.635","usgsCitation":"Pegg, M.A., and Pierce, C.L., 2002, Classification of reaches in the Missouri and lower Yellowstone Rivers based on flow characteristics: River Research and Applications, v. 18, no. 1, p. 31-42, https://doi.org/10.1002/rra.635.","productDescription":"12 p.","startPage":"31","endPage":"42","costCenters":[],"links":[{"id":233054,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Missouri River, Yellowstone River","volume":"18","issue":"1","noUsgsAuthors":false,"publicationDate":"2002-01-28","publicationStatus":"PW","scienceBaseUri":"5059f61ce4b0c8380cd4c5cd","contributors":{"authors":[{"text":"Pegg, Mark A.","contributorId":198830,"corporation":false,"usgs":false,"family":"Pegg","given":"Mark","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":401610,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pierce, Clay L. cpierce@usgs.gov","contributorId":525,"corporation":false,"usgs":true,"family":"Pierce","given":"Clay","email":"cpierce@usgs.gov","middleInitial":"L.","affiliations":[{"id":350,"text":"Iowa Cooperative Fish and Wildlife Research Unit","active":false,"usgs":true}],"preferred":false,"id":401611,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}