{"pageNumber":"1876","pageRowStart":"46875","pageSize":"25","recordCount":184569,"records":[{"id":9000494,"text":"sir20105170 - 2010 - Estimation of selected streamflow statistics for a network of low-flow partial-record stations in areas affected by Base Realignment and Closure (BRAC) in Maryland","interactions":[],"lastModifiedDate":"2012-03-08T17:16:13","indexId":"sir20105170","displayToPublicDate":"2010-12-06T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-5170","title":"Estimation of selected streamflow statistics for a network of low-flow partial-record stations in areas affected by Base Realignment and Closure (BRAC) in Maryland","docAbstract":"The U.S. Geological Survey, in cooperation with the Maryland Department of the Environment, operated a network of 20 low-flow partial-record stations during 2008 in a region that extends from southwest of Baltimore to the northeastern corner of Maryland to obtain estimates of selected streamflow statistics at the station locations. The study area is expected to face a substantial influx of new residents and businesses as a result of military and civilian personnel transfers associated with the Federal Base Realignment and Closure Act of 2005. The estimated streamflow statistics, which include monthly 85-percent duration flows, the 10-year recurrence-interval minimum base flow, and the 7-day, 10-year low flow, are needed to provide a better understanding of the availability of water resources in the area to be affected by base-realignment activities. Streamflow measurements collected for this study at the low-flow partial-record stations and measurements collected previously for 8 of the 20 stations were related to concurrent daily flows at nearby index streamgages to estimate the streamflow statistics. Three methods were used to estimate the streamflow statistics and two methods were used to select the index streamgages. Of the three methods used to estimate the streamflow statistics, two of them--the Moments and MOVE1 methods--rely on correlating the streamflow measurements at the low-flow partial-record stations with concurrent streamflows at nearby, hydrologically similar index streamgages to determine the estimates. These methods, recommended for use by the U.S. Geological Survey, generally require about 10 streamflow measurements at the low-flow partial-record station. The third method transfers the streamflow statistics from the index streamgage to the partial-record station based on the average of the ratios of the measured streamflows at the partial-record station to the concurrent streamflows at the index streamgage. This method can be used with as few as one pair of streamflow measurements made on a single streamflow recession at the low-flow partial-record station, although additional pairs of measurements will increase the accuracy of the estimates. Errors associated with the two correlation methods generally were lower than the errors associated with the flow-ratio method, but the advantages of the flow-ratio method are that it can produce reasonably accurate estimates from streamflow measurements much faster and at lower cost than estimates obtained using the correlation methods. The two index-streamgage selection methods were (1) selection based on the highest correlation coefficient between the low-flow partial-record station and the index streamgages, and (2) selection based on Euclidean distance, where the Euclidean distance was computed as a function of geographic proximity and the basin characteristics: drainage area, percentage of forested area, percentage of impervious area, and the base-flow recession time constant, t. Method 1 generally selected index streamgages that were significantly closer to the low-flow partial-record stations than method 2. The errors associated with the estimated streamflow statistics generally were lower for method 1 than for method 2, but the differences were not statistically significant. The flow-ratio method for estimating streamflow statistics at low-flow partial-record stations was shown to be independent from the two correlation-based estimation methods. As a result, final estimates were determined for eight low-flow partial-record stations by weighting estimates from the flow-ratio method with estimates from one of the two correlation methods according to the respective variances of the estimates. Average standard errors of estimate for the final estimates ranged from 90.0 to 7.0 percent, with an average value of 26.5 percent. Average standard errors of estimate for the weighted estimates were, on average, 4.3 percent less than the best average standard errors of estima","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20105170","collaboration":"Prepared in cooperation with the\r\nMaryland Department of the Environment","usgsCitation":"Ries, K., and Eng, K., 2010, Estimation of selected streamflow statistics for a network of low-flow partial-record stations in areas affected by Base Realignment and Closure (BRAC) in Maryland: U.S. Geological Survey Scientific Investigations Report 2010-5170, v, 40 p.; 8 1/2 by 11 printed book; online, https://doi.org/10.3133/sir20105170.","productDescription":"v, 40 p.; 8 1/2 by 11 printed book; online","numberOfPages":"40","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"2008-01-01","temporalEnd":"2009-06-30","costCenters":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"links":[{"id":126110,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2010_5170.gif"},{"id":19168,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2010/5170/","linkFileType":{"id":5,"text":"html"}}],"scale":"1000000","projection":"Transverse Mercator Projection","country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.5,38.666666666666664 ], [ -77.5,39.833333333333336 ], [ -75.41666666666667,39.833333333333336 ], [ -75.41666666666667,38.666666666666664 ], [ -77.5,38.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb1f3","contributors":{"authors":[{"text":"Ries, Kernell G. III kries@usgs.gov","contributorId":1913,"corporation":false,"usgs":true,"family":"Ries","given":"Kernell G.","suffix":"III","email":"kries@usgs.gov","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":false,"id":344120,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eng, Ken","contributorId":89480,"corporation":false,"usgs":true,"family":"Eng","given":"Ken","affiliations":[],"preferred":false,"id":344121,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70207041,"text":"70207041 - 2010 - Calculation of aftershock accumulation from observed postseismic deformation: M6 2004 Parkfield, California, earthquake","interactions":[],"lastModifiedDate":"2020-05-26T15:35:04.030775","indexId":"70207041","displayToPublicDate":"2010-12-04T11:14:10","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Calculation of aftershock accumulation from observed postseismic deformation: M6 2004 Parkfield, California, earthquake","docAbstract":"<p><span class=\"paraNumber\">[1]<span>&nbsp;</span></span><span>The postseismic stress accumulation&nbsp;</span><i>τ</i><span>(</span><i>t</i><span>) over the interval 0.004 to 880 days following the 2004 Parkfield earthquake (M6) can be inferred from GPS measurements of postseismic deformation. The stress relaxation&nbsp;</span><i>τ</i><span>(</span><i>t</i><span>) −&nbsp;</span><i>τ</i><span>′</span><sub><i>l</i></sub><i>t</i><span>, where&nbsp;</span><i>τ</i><span>′</span><sub><i>l</i></sub><span>&nbsp;is the interseismic loading rate and&nbsp;</span><i>t</i><span>&nbsp;is the time after the earthquake, plotted as a function of the number of M &gt; 1.5 aftershocks&nbsp;</span><i>N</i><sub><i>a</i></sub><span>(</span><i>t</i><span>) that have occurred by time&nbsp;</span><i>t</i><span>&nbsp;is bilinear with the slope of the fit to the first half of the aftershock sequence less than the slope of the fit to the second half. Thus, the aftershock seismicity rate is not proportional to the stress relaxation rate&nbsp;</span><i>τ</i><span>′(</span><i>t</i><span>) −&nbsp;</span><i>τ</i><span>′</span><sub><i>l</i></sub><span>&nbsp;over the entire sequence, but rather exhibits two distinct proportionalities. The observed postearthquake accumulation of M &gt; 1.5 earthquakes in the aftershock zone as a function of time can be explained with the rate‐and‐state friction relation proposed by Dieterich (1994) between the cumulative number of earthquakes and&nbsp;</span><i>τ</i><span>(</span><i>t</i><span>).</span></p>","language":"English","publisher":"Wiley","doi":"10.1029/2010GL042872","usgsCitation":"Savage, J.C., 2010, Calculation of aftershock accumulation from observed postseismic deformation: M6 2004 Parkfield, California, earthquake: Geophysical Research Letters, v. 37, no. 13, p. 1-4, https://doi.org/10.1029/2010GL042872.","productDescription":"L13302, 4p.","startPage":"1","endPage":"4","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":369898,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","county":"Monterey 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,{"id":98914,"text":"fs20103068 - 2010 - Occurrence of Escherichia coli in the Cuyahoga River in the Cuyahoga Valley National Park, Ohio","interactions":[],"lastModifiedDate":"2012-03-08T17:16:13","indexId":"fs20103068","displayToPublicDate":"2010-12-04T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-3068","title":"Occurrence of Escherichia coli in the Cuyahoga River in the Cuyahoga Valley National Park, Ohio","docAbstract":"There are several measures of the 'cleanliness' of a natural body of water, including concentrations of indicator bacteria, anthropogenic chemicals (chemicals derived from human activities), and nutrients, such as nitrogen and phosphorous. Escherichia coli (E. coli) is a bacterium that lives in the intestinal tract of warm-blooded animals, such as humans, deer, cows, and dogs. Most strains of E. coli are not harmful and are in fact beneficial to humans by aiding in the digestive process. A few strains, such as the O157 strain, produce toxins that can cause gastrointestinal illness, but occurrence of toxic strains in the environment is not common. E. coli is considered a good indicator bacterium because its occurrence in the environment indicates the presence of fecal contamination and therefore the possible presence of pathogenic organisms associated with feces.  The U.S. Environmental Protection Agency (USEPA) recommends using measurements of E. coli to monitor freshwaters and set criteria for the concentration of bacteria that can be present in the water with minimal adverse human-health effects. Typically, a State's waters are assigned a recreational-use designation, such as bathing, primary-contact, or secondary contact waters, which is used to set the State's water-quality standards based on the USEPA criteria. The Cuyahoga River in the Cuyahoga Valley National Park is designated for primary-contact recreation; therefore, when concentrations of E. coli exceed 298 CFU/100mL, the river would be considered potentially unsafe for recreation.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/fs20103068","usgsCitation":"Brady, A., and Plona, M.B., 2010, Occurrence of Escherichia coli in the Cuyahoga River in the Cuyahoga Valley National Park, Ohio: U.S. Geological Survey Fact Sheet 2010-3068, 4 p., https://doi.org/10.3133/fs20103068.","productDescription":"4 p.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"links":[{"id":126026,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2010_3068.bmp"},{"id":14335,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2010/3068/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -81.66666666666667,41.083333333333336 ], [ -81.66666666666667,41.416666666666664 ], [ -81.5,41.416666666666664 ], [ -81.5,41.083333333333336 ], [ -81.66666666666667,41.083333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696080","contributors":{"authors":[{"text":"Brady, Amie M. G.","contributorId":29774,"corporation":false,"usgs":true,"family":"Brady","given":"Amie M. G.","affiliations":[],"preferred":false,"id":306927,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plona, Meg B.","contributorId":46470,"corporation":false,"usgs":true,"family":"Plona","given":"Meg","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":306928,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70157540,"text":"70157540 - 2010 - Report of the IAU Working Group on cartographic coordinates and rotational elements: 2009","interactions":[],"lastModifiedDate":"2021-04-01T20:56:50.587001","indexId":"70157540","displayToPublicDate":"2010-12-04T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1201,"text":"Celestial Mechanics and Dynamical Astronomy","active":true,"publicationSubtype":{"id":10}},"title":"Report of the IAU Working Group on cartographic coordinates and rotational elements: 2009","docAbstract":"<p><span>Every three years the IAU Working Group on Cartographic Coordinates and Rotational Elements revises tables giving the directions of the poles of rotation and the prime meridians of the planets, satellites, minor planets, and comets. This report takes into account the IAU Working Group for Planetary System Nomenclature (WGPSN) and the IAU Committee on Small Body Nomenclature (CSBN) definition of dwarf planets, introduces improved values for the pole and rotation rate of Mercury, returns the rotation rate of Jupiter to a previous value, introduces improved values for the rotation of five satellites of Saturn, and adds the equatorial radius of the Sun for comparison. It also adds or updates size and shape information for the Earth, Mars’ satellites Deimos and Phobos, the four Galilean satellites of Jupiter, and 22 satellites of Saturn. Pole, rotation, and size information has been added for the asteroids (21) Lutetia, (511) Davida, and (2867) Šteins. Pole and rotation information has been added for (2) Pallas and (21) Lutetia. Pole and rotation and mean radius information has been added for (1) Ceres. Pole information has been updated for (4) Vesta. The high precision realization for the pole and rotation rate of the Moon is updated. Alternative orientation models for Mars, Jupiter, and Saturn are noted. The Working Group also reaffirms that once an observable feature at a defined longitude is chosen, a longitude definition origin should not change except under unusual circumstances. It is also noted that alternative coordinate systems may exist for various (e.g. dynamical) purposes, but&nbsp;</span><i>specific cartographic</i><span>&nbsp;coordinate system information continues to be recommended for each body. The Working Group elaborates on its purpose, and also announces its plans to occasionally provide limited updates to its recommendations via its website, in order to address community needs for some updates more often than every 3&nbsp;years. Brief recommendations are also made to the general planetary community regarding the need for controlled products, and improved or consensus rotation models for Mars, Jupiter, and Saturn.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s10569-010-9320-4","usgsCitation":"Archinal, B.A., A’Hearn, M.F., Bowell, E., Conrad, A., Consolmagno, G.J., Courtin, R., Fukushima, T., Hestroffer, D., Hilton, J.L., Krasinsky, G.A., Neumann, G., Oberst, J., Seidelmann, P.K., Stooke, P., Tholen, D.J., Thomas, P.C., and Williams, I.P., 2010, Report of the IAU Working Group on cartographic coordinates and rotational elements: 2009: Celestial Mechanics and Dynamical Astronomy, v. 109, no. 2, p. 101-135, https://doi.org/10.1007/s10569-010-9320-4.","productDescription":"35 p.","startPage":"101","endPage":"135","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":308605,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"109","issue":"2","noUsgsAuthors":false,"publicationDate":"2010-12-04","publicationStatus":"PW","scienceBaseUri":"5606703be4b058f706e51956","contributors":{"authors":[{"text":"Archinal, Brent A. 0000-0002-6654-0742 barchinal@usgs.gov","orcid":"https://orcid.org/0000-0002-6654-0742","contributorId":2816,"corporation":false,"usgs":true,"family":"Archinal","given":"Brent","email":"barchinal@usgs.gov","middleInitial":"A.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":573508,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"A’Hearn, Michael F.","contributorId":147973,"corporation":false,"usgs":false,"family":"A’Hearn","given":"Michael","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":573509,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bowell, Edward","contributorId":147974,"corporation":false,"usgs":false,"family":"Bowell","given":"Edward","email":"","affiliations":[],"preferred":false,"id":573510,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Conrad, Al","contributorId":147975,"corporation":false,"usgs":false,"family":"Conrad","given":"Al","email":"","affiliations":[],"preferred":false,"id":573511,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Consolmagno, Guy J.","contributorId":147976,"corporation":false,"usgs":false,"family":"Consolmagno","given":"Guy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":573512,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Courtin, Regis","contributorId":147977,"corporation":false,"usgs":false,"family":"Courtin","given":"Regis","email":"","affiliations":[],"preferred":false,"id":573513,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Fukushima, Toshio","contributorId":147978,"corporation":false,"usgs":false,"family":"Fukushima","given":"Toshio","email":"","affiliations":[],"preferred":false,"id":573514,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Hestroffer, Daniel","contributorId":147979,"corporation":false,"usgs":false,"family":"Hestroffer","given":"Daniel","email":"","affiliations":[],"preferred":false,"id":573515,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Hilton, James L.","contributorId":147980,"corporation":false,"usgs":false,"family":"Hilton","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":573516,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Krasinsky, Georgij A.","contributorId":147981,"corporation":false,"usgs":false,"family":"Krasinsky","given":"Georgij","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":573517,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Neumann, Gregory","contributorId":147982,"corporation":false,"usgs":false,"family":"Neumann","given":"Gregory","email":"","affiliations":[],"preferred":false,"id":573518,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Oberst, Jurgen","contributorId":147983,"corporation":false,"usgs":false,"family":"Oberst","given":"Jurgen","email":"","affiliations":[],"preferred":false,"id":573519,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Seidelmann, P. Kenneth","contributorId":147984,"corporation":false,"usgs":false,"family":"Seidelmann","given":"P.","email":"","middleInitial":"Kenneth","affiliations":[],"preferred":false,"id":573520,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Stooke, Philip","contributorId":147985,"corporation":false,"usgs":false,"family":"Stooke","given":"Philip","email":"","affiliations":[],"preferred":false,"id":573521,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Tholen, David J.","contributorId":147986,"corporation":false,"usgs":false,"family":"Tholen","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":573522,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Thomas, Peter C.","contributorId":26567,"corporation":false,"usgs":true,"family":"Thomas","given":"Peter","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":573523,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Williams, Iwan P.","contributorId":147987,"corporation":false,"usgs":false,"family":"Williams","given":"Iwan","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":573524,"contributorType":{"id":1,"text":"Authors"},"rank":17}]}}
,{"id":98913,"text":"fs20103104 - 2010 - Quantifying effects of climate change on the snowmelt-dominated groundwater resources of northern New England","interactions":[],"lastModifiedDate":"2012-03-08T17:16:13","indexId":"fs20103104","displayToPublicDate":"2010-12-04T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-3104","title":"Quantifying effects of climate change on the snowmelt-dominated groundwater resources of northern New England","docAbstract":"Recent U.S. Geological Survey (USGS) climate studies in New England have shown substantial evidence of hydrologic changes during the last 100 years, including trends toward earlier snowmelt runoff, decreasing occurrence of river ice, and decreasing winter snowpack. These studies are being expanded to include investigation of trends in groundwater levels and fluctuations. Groundwater is an important drinking-water source throughout northern New England (Maine, New Hampshire, and Vermont). The USGS is currently investigating whether or not groundwater recharge from snowmelt and precipitation exhibits historical trends. In addition to trend-testing, groundwater resources also will be analyzed by relating groundwater-level changes to the large year-to-year variability in weather conditions.\r\n\r\nIntroduction\r\n\r\nThe USGS has documented many seasonal climate-related changes in the northeastern United States that have occurred during the last 30 to 150 years. These changes include earlier snowmelt runoff in the late winter and early spring, decreasing duration of ice on rivers and lakes, decreasing ratio of snowfall to total precipitation, and denser and thinner late-winter snowpack. All of these changes are consistent with warming winter and spring air temperatures (Dudley and Hodgkins, 2002; Hodgkins and others, 2002; Huntington and others, 2004; Hodgkins and others, 2005; Hodgkins and Dudley, 2006a; Hodgkins and Dudley, 2006b). Climate-model projections for the Northeast indicate air-temperature warming, earlier snowmelt runoff, increases in annual evaporation, and decreased low streamflows (Hayhoe and others, 2007).\r\n\r\nThe contribution and timing of spring snowmelt to groundwater recharge is particularly important to groundwater resources in the northeastern United States where aquifers typically consist of thin sediments overlying crystalline bedrock with relatively little storage capacity (Mack, 2009). Following spring recharge, groundwater slowly flows into streams throughout the summer. This groundwater flow is a source of cool water during the summer and accounts for a large proportion of the streamflow during summer low-flow periods.\r\n\r\nGroundwater is an important drinking-water source in northern New England. Approximately 32 percent of public water suppliers draw water from groundwater sources in Vermont, New Hampshire, and Maine, and approximately 40 percent of the population derives its drinking water from private wells (Kenny and others, 2009). It is vital to understand changes that may be occurring to such an important resource for planning industrial and agricultural water uses and protecting drinking water. ","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/fs20103104","usgsCitation":"Dudley, R.W., Hodgkins, G.A., Shanley, J.B., and Mack, T.J., 2010, Quantifying effects of climate change on the snowmelt-dominated groundwater resources of northern New England: U.S. Geological Survey Fact Sheet 2010-3104, 4 p., https://doi.org/10.3133/fs20103104.","productDescription":"4 p.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"links":[{"id":126025,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2010_3104.bmp"},{"id":14334,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2010/3104/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a86e4b07f02db64dba5","contributors":{"authors":[{"text":"Dudley, Robert W. 0000-0002-0934-0568 rwdudley@usgs.gov","orcid":"https://orcid.org/0000-0002-0934-0568","contributorId":2223,"corporation":false,"usgs":true,"family":"Dudley","given":"Robert","email":"rwdudley@usgs.gov","middleInitial":"W.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"preferred":true,"id":306926,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hodgkins, Glenn A. 0000-0002-4916-5565 gahodgki@usgs.gov","orcid":"https://orcid.org/0000-0002-4916-5565","contributorId":2020,"corporation":false,"usgs":true,"family":"Hodgkins","given":"Glenn","email":"gahodgki@usgs.gov","middleInitial":"A.","affiliations":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":306925,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shanley, James B. 0000-0002-4234-3437 jshanley@usgs.gov","orcid":"https://orcid.org/0000-0002-4234-3437","contributorId":1953,"corporation":false,"usgs":true,"family":"Shanley","given":"James","email":"jshanley@usgs.gov","middleInitial":"B.","affiliations":[{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":306924,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mack, Thomas J. 0000-0002-0496-3918 tjmack@usgs.gov","orcid":"https://orcid.org/0000-0002-0496-3918","contributorId":1677,"corporation":false,"usgs":true,"family":"Mack","given":"Thomas","email":"tjmack@usgs.gov","middleInitial":"J.","affiliations":[{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":306923,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":98911,"text":"fs20103114 - 2010 - Drought Monitoring with VegDRI","interactions":[],"lastModifiedDate":"2012-02-02T00:04:07","indexId":"fs20103114","displayToPublicDate":"2010-12-03T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-3114","title":"Drought Monitoring with VegDRI","docAbstract":"Drought strikes somewhere in the United States every year, turning green landscapes brown as precipitation falls below normal levels and water supplies dwindle. Drought is typically a temporary climatic aberration, but it is also an insidious natural hazard. It might last for weeks, months, or years and may have many negative effects. Drought can threaten crops, livestock, and livelihoods, stress wildlife and habitats, and increase wildfire risks and threats to human health.\r\n\r\nDrought conditions can vary tremendously from place to place and week to week. Accurate drought monitoring is essential to understand a drought's progression and potential effects, and to provide information necessary to support drought mitigation decisions. It is also crucial in light of climate change where droughts could become more frequent, severe, and persistent.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/fs20103114","collaboration":"Prepared in cooperation with the National Drought Mitigation Center, University of Nebraska, Lincoln","usgsCitation":"Brown, J., 2010, Drought Monitoring with VegDRI: U.S. Geological Survey Fact Sheet 2010-3114, 2 p., https://doi.org/10.3133/fs20103114.","productDescription":"2 p.","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":126738,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2010_3114.bmp"},{"id":14331,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2010/3114/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62ae12","contributors":{"authors":[{"text":"Brown, Jesslyn F. 0000-0002-9976-1998","orcid":"https://orcid.org/0000-0002-9976-1998","contributorId":85123,"corporation":false,"usgs":true,"family":"Brown","given":"Jesslyn F.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":306921,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":98912,"text":"sir20105210 - 2010 - Groundwater-flow assessment of the Mississippi River Valley alluvial aquifer of northeastern Arkansas","interactions":[],"lastModifiedDate":"2012-02-10T00:10:04","indexId":"sir20105210","displayToPublicDate":"2010-12-03T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-5210","title":"Groundwater-flow assessment of the Mississippi River Valley alluvial aquifer of northeastern Arkansas","docAbstract":"The Mississippi River Valley alluvial aquifer is a water-bearing assemblage of gravels and sands that underlies about 32,000 square miles of Arkansas, Kentucky, Louisiana, Mississippi, Missouri, and Tennessee. Pumping of groundwater from the alluvial aquifer for agriculture started in the early 1900s in the Grand Prairie area for the irrigation of rice and soybeans. From 1965 to 2005, water use in the alluvial aquifer increased 655 percent. In 2005, 6,242 million gallons per day of water were pumped from the aquifer, primarily for irrigation and fish farming. Water-level declines in the alluvial aquifer were documented as early as 1927. Long-term water-level measurements in the alluvial aquifer show an average annual decline of 1 foot per year in some areas.\r\n\r\nIn this report, the utility of the updated 2009 MODFLOW groundwater-flow model of the alluvial aquifer in northeastern Arkansas was extended by performing groundwater-flow assessments of the alluvial aquifer at specific areas of interest using a variety of methods. One such area is along the western side of Crowleys Ridge, which includes western parts of Clay, Greene, Craighead, Poinsett, Cross, St. Francis, and Lee Counties. This area was designated as the Cache Critical Groundwater Area by the Arkansas Natural Resources Commission in 2009 for the alluvial and Sparta/Memphis aquifers, because of the rate of change in groundwater levels and groundwater levels have dropped below half the original saturated thickness of the alluvial aquifer.\r\n\r\n","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/sir20105210","collaboration":"Prepared in cooperation with the Arkansas Natural Resources Commission","usgsCitation":"Czarnecki, J.B., 2010, Groundwater-flow assessment of the Mississippi River Valley alluvial aquifer of northeastern Arkansas: U.S. Geological Survey Scientific Investigations Report 2010-5210, v, 33 p.; Downloads: Scenario Information; Scenario 1; Scenario 2; Scenario 3, https://doi.org/10.3133/sir20105210.","productDescription":"v, 33 p.; Downloads: Scenario Information; Scenario 1; Scenario 2; Scenario 3","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":129,"text":"Arkansas Water Science Center","active":true,"usgs":true}],"links":[{"id":126022,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2010_5210.bmp"},{"id":14333,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2010/5210/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -92.25,33.75 ], [ -92.25,37 ], [ -89.75,37 ], [ -89.75,33.75 ], [ -92.25,33.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a91e4b07f02db656cbe","contributors":{"authors":[{"text":"Czarnecki, John B. jczarnec@usgs.gov","contributorId":2555,"corporation":false,"usgs":true,"family":"Czarnecki","given":"John","email":"jczarnec@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":306922,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9000493,"text":"fs20103111 - 2010 - Southeast Ecological Science Center","interactions":[],"lastModifiedDate":"2012-02-02T00:04:46","indexId":"fs20103111","displayToPublicDate":"2010-12-03T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-3111","title":"Southeast Ecological Science Center","docAbstract":"Aquatic ecosystems, from deep sea reefs and coastal marshes to freshwater springs and wetlands, are home to diverse assemblages of life. These commercially and ecologically important systems are part of our national heritage, and are often treasured places or refuges that protect rare or threatened species. In the water-rich Southeastern United States, managers face the challenge of understanding how water and land use affect the region's aquatic life. The Southeast Ecological Science Center (SESC) helps address that challenge by providing objective science that can be used to evaluate proposed actions and develop management strategies.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20103111","usgsCitation":"Pawlitz, R.J., 2010, Southeast Ecological Science Center: U.S. Geological Survey Fact Sheet 2010-3111, 2 p., https://doi.org/10.3133/fs20103111.","productDescription":"2 p.","numberOfPages":"2","additionalOnlineFiles":"N","costCenters":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"links":[{"id":126081,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2010_3111.jpg"},{"id":19167,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2010/3111/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e73d4","contributors":{"authors":[{"text":"Pawlitz, Rachel J. rpawlitz@usgs.gov","contributorId":4251,"corporation":false,"usgs":true,"family":"Pawlitz","given":"Rachel","email":"rpawlitz@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":344119,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":98910,"text":"sir20105192 - 2010 - Water quality (2000-08) and historical phosphorus concentrations from paleolimnological studies of Swamp and Speckled Trout Lakes, Grand Portage Reservation, northeastern Minnesota","interactions":[],"lastModifiedDate":"2012-03-08T17:16:12","indexId":"sir20105192","displayToPublicDate":"2010-12-03T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-5192","title":"Water quality (2000-08) and historical phosphorus concentrations from paleolimnological studies of Swamp and Speckled Trout Lakes, Grand Portage Reservation, northeastern Minnesota","docAbstract":"A paleolimnological approach was taken to aid the Grand Portage Reservation, in northeastern Minnesota, in determining reference conditions for lakes on the reservation. The U.S. Geological Survey, in cooperation with the Grand Portage Band of Chippewa Indians and the Science Museum of Minnesota, conducted a study to describe water quality (2000-08) and historical total phosphorus concentrations (approximately 1781-2006) for Swamp and Speckled Trout Lakes. Results from this study may be used as a guide in establishing nutrient criteria in these and other lakes on the Grand Portage Reservation.\r\n\r\nHistorical phosphorus concentrations were inferred through paleolimnological reconstruction methods involving diatom analysis and lead-210 dating of lake-sediment cores. Historical diatom-inferred total phosphorus concentrations in Swamp Lake ranged from 0.017 to 0.025 milligrams per liter (mg/L) based on diatom assemblages in sediment samples dated 1781-2005. Historical diatom-inferred total phosphorus concentrations in Speckled Trout Lake ranged from 0.008 to 0.014 mg/L based on diatom assemblages in sediment samples dated 1825-2006. In both lakes, historical changes in diatom-inferred total phosphorus concentrations did not exceed model error estimates, indicating that there has been minimal change in total phosphorus concentrations in the two lakes over about two centuries.\r\n\r\nNutrient concentrations in monthly water samples collected May through October during 2000, 2002, 2004, 2006, and 2008 were compared to the diatom-inferred total phosphorus concentrations. Total phosphorus concentrations from water samples collected from Swamp Lake during 2000-08 ranged from less than 0.002 to 0.160 mg/L (median= 0.023 mg/L) compared to diatom-inferred total phosphorus concentrations of 0.018 to 0.020 mg/L for 2002 to 2005. Total phosphorus concentrations in water samples collected from Speckled Trout Lake during 2000-08 were similar to those of Swamp Lake, ranging from less than 0.002 to 0.147 mg/L (median=0.012 mg/L), whereas the diatom-inferred total phosphorus concentrations were smaller, ranging from 0.009 to 0.010 mg/L for 2003 to 2006. Differences in total phosphorus concentrations between the two lakes may be because of differences in watershed characteristics, particularly the number of wetlands in the two watersheds. Similarities between recent total phosphorus concentrations in water-quality samples and diatom-inferred total phosphorus indicate that diatom-inferred phosphorus reconstructions might be used to help establish reference conditions. Nutrient criteria for Grand Portage Reservation lakes may be established when a sampling program is designed to ensure representative phosphorus concentrations in water samples are comparable to diatom-inferred concentrations.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/sir20105192","collaboration":"Prepared in cooperation with the Grand Portage Band of Chippewa Indians and the Science Museum of Minnesota","usgsCitation":"Christensen, V.G., Jones, P.M., Edlund, M.B., and Ramstack, J.M., 2010, Water quality (2000-08) and historical phosphorus concentrations from paleolimnological studies of Swamp and Speckled Trout Lakes, Grand Portage Reservation, northeastern Minnesota: U.S. Geological Survey Scientific Investigations Report 2010-5192, viii, 17 p.; Appendices, https://doi.org/10.3133/sir20105192.","productDescription":"viii, 17 p.; Appendices","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":126023,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2010_5192.bmp"},{"id":14330,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2010/5192/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89.86749999999999,47.86666666666667 ], [ -89.86749999999999,48.03333333333333 ], [ 89.5,48.03333333333333 ], [ 89.5,47.86666666666667 ], [ -89.86749999999999,47.86666666666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9cc6","contributors":{"authors":[{"text":"Christensen, Victoria G. 0000-0003-4166-7461 vglenn@usgs.gov","orcid":"https://orcid.org/0000-0003-4166-7461","contributorId":2354,"corporation":false,"usgs":true,"family":"Christensen","given":"Victoria","email":"vglenn@usgs.gov","middleInitial":"G.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":306918,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, Perry M. 0000-0002-6569-5144 pmjones@usgs.gov","orcid":"https://orcid.org/0000-0002-6569-5144","contributorId":2231,"corporation":false,"usgs":true,"family":"Jones","given":"Perry","email":"pmjones@usgs.gov","middleInitial":"M.","affiliations":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":306917,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Edlund, Mark B.","contributorId":104335,"corporation":false,"usgs":true,"family":"Edlund","given":"Mark","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":306920,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ramstack, Joy M.","contributorId":74238,"corporation":false,"usgs":true,"family":"Ramstack","given":"Joy","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":306919,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":98908,"text":"fs20103082 - 2010 - Assessment of goods and valuation of ecosystem services (AGAVES) San Pedro River Basin, United States and Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:04:34","indexId":"fs20103082","displayToPublicDate":"2010-12-02T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-3082","title":"Assessment of goods and valuation of ecosystem services (AGAVES) San Pedro River Basin, United States and Mexico","docAbstract":"A consortium of federal, academic, and nongovernment organization (NGO) partners have established a collaborative research enterprise in the San Pedro River Basin to develop methods, standards, and tools to assess and value ecosystem goods and services. The central premise of ecosystem services research is that human condition is intrinsically linked to the environment. Human health and well-being (including economic prosperity) depend on important supporting, regulating, provisioning, and cultural services that we derive from our surrounding ecosystems. The AGAVES project is intended as a demonstration study for incorporating ecosystem services information into resource management policy and decisionmaking. Accordingly, a nested, multiscale project design has been adopted to address a range of stakeholder information requirements. This design will further facilitate an evaluation of how well methods developed in this project can be transferred to other areas.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/fs20103082","usgsCitation":"Semmens, D., Kepner, W., and Goodrich, D., 2010, Assessment of goods and valuation of ecosystem services (AGAVES) San Pedro River Basin, United States and Mexico: U.S. Geological Survey Fact Sheet 2010-3082, 4 p., https://doi.org/10.3133/fs20103082.","productDescription":"4 p.","additionalOnlineFiles":"N","costCenters":[{"id":547,"text":"Rocky Mountain Geographic Science Center","active":true,"usgs":true}],"links":[{"id":126145,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2010_3082.bmp"},{"id":14327,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2010/3082/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671f9c","contributors":{"authors":[{"text":"Semmens, Darius J. 0000-0001-7924-6529","orcid":"https://orcid.org/0000-0001-7924-6529","contributorId":64201,"corporation":false,"usgs":true,"family":"Semmens","given":"Darius J.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":306911,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kepner, William","contributorId":9214,"corporation":false,"usgs":true,"family":"Kepner","given":"William","affiliations":[],"preferred":false,"id":306910,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goodrich, David","contributorId":74723,"corporation":false,"usgs":true,"family":"Goodrich","given":"David","affiliations":[],"preferred":false,"id":306912,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":98907,"text":"sir20105129 - 2010 - Geochemical evolution processes and water-quality observations based on results of the National Water-Quality Assessment Program in the San Antonio segment of the Edwards aquifer, Texas, 1996-2006","interactions":[],"lastModifiedDate":"2022-01-07T20:17:48.457498","indexId":"sir20105129","displayToPublicDate":"2010-12-02T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-5129","title":"Geochemical evolution processes and water-quality observations based on results of the National Water-Quality Assessment Program in the San Antonio segment of the Edwards aquifer, Texas, 1996-2006","docAbstract":"<p>As part of the National Water-Quality Assessment Program, the U.S. Geological Survey collected and analyzed groundwater samples during 1996-2006 from the San Antonio segment of the Edwards aquifer of central Texas, a productive karst aquifer developed in Cretaceous-age carbonate rocks. These National Water-Quality Assessment Program studies provide an extensive dataset of groundwater geochemistry and water quality, consisting of 249 groundwater samples collected from 136 sites (wells and springs), including (1) wells completed in the shallow, unconfined, and urbanized part of the aquifer in the vicinity of San Antonio (shallow/urban unconfined category), (2) wells completed in the unconfined (outcrop area) part of the regional aquifer (unconfined category), and (3) wells completed in and springs discharging from the confined part of the regional aquifer (confined category). This report evaluates these data to assess geochemical evolution processes, including local- and regional-scale processes controlling groundwater geochemistry, and to make water-quality observations pertaining to sources and distribution of natural constituents and anthropogenic contaminants, the relation between geochemistry and hydrologic conditions, and groundwater age tracers and travel time. Implications for monitoring water-quality trends in karst are also discussed. Geochemical and isotopic data are useful tracers of recharge, groundwater flow, fluid mixing, and water-rock interaction processes that affect water quality. Sources of dissolved constituents to Edwards aquifer groundwater include dissolution of and geochemical interaction with overlying soils and calcite and dolomite minerals that compose the aquifer. Geochemical tracers such as magnesium to calcium and strontium to calcium ratios and strontium isotope compositions are used to evaluate and constrain progressive fluid-evolution processes. Molar ratios of magnesium to calcium and strontium to calcium in groundwater typically increase along flow paths; results for samples of Edwards aquifer groundwater show an increase from shallow/urban unconfined, to unconfined, to confined groundwater categories. These differences are consistent with longer residence times and greater extents of water-rock interaction controlling fluid compositions as groundwater evolves from shallow unconfined groundwater to deeper confined groundwater. Results for stable isotopes of hydrogen and oxygen indicate specific geochemical processes affect some groundwater samples, including mixing with downdip saline water, mixing with recent recharge associated with tropical cyclonic storms, or mixing with recharge water than has undergone evaporation. The composition of surface water recharging the aquifer, as well as mixing with downdip water from the Trinity aquifer or the saline zone, also might affect water quality. A time-series record (1938-2006) of discharge at Comal Springs, one of the major aquifer discharge points, indicates an upward trend for nitrate and chloride concentrations, which likely reflects anthropogenic activities. A small number of organic contaminants were routinely or frequently detected in Edwards aquifer groundwater samples. These were the pesticides atrazine, its degradate deethylatrazine, and simazine; the drinking-water disinfection byproduct chloroform; and the solvent tetrachloroethene. Detection of these contaminants was most frequent in samples of the shallow/urban unconfined groundwater category and least frequent in samples of the unconfined groundwater category. Results indicate that the shallow/urban unconfined part of the aquifer is most affected by anthropogenic contaminants and the unconfined part of the aquifer is the least affected. The high frequency of detection for these anthropogenic contaminants aquifer-wide and in samples of deep, confined groundwater indicates that the entire aquifer is susceptible to water-quality changes as a result of anthropogenic activities. L</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, Virginia","doi":"10.3133/sir20105129","usgsCitation":"Musgrove, M., Fahlquist, L., Houston, N.A., Lindgren, R.J., and Ging, P.B., 2010, Geochemical evolution processes and water-quality observations based on results of the National Water-Quality Assessment Program in the San Antonio segment of the Edwards aquifer, Texas, 1996-2006: U.S. Geological Survey Scientific Investigations Report 2010-5129, xi, 93 p., https://doi.org/10.3133/sir20105129.","productDescription":"xi, 93 p.","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"1996-01-01","temporalEnd":"2006-12-31","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":126144,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2010_5129.png"},{"id":14326,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2010/5129/","linkFileType":{"id":5,"text":"html"}},{"id":394053,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_94624.htm"}],"country":"United States","state":"Texas","otherGeospatial":"San Antonio segment of Edwards aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -100.4375,\n              29\n            ],\n            [\n              -97.66667,\n              29\n            ],\n            [\n              -97.6667,\n              30.3\n            ],\n            [\n              -100.4375,\n              30.3\n            ],\n            [\n              -100.4375,\n              29\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db697f08","contributors":{"authors":[{"text":"Musgrove, MaryLynn","contributorId":34878,"corporation":false,"usgs":true,"family":"Musgrove","given":"MaryLynn","affiliations":[],"preferred":false,"id":306909,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fahlquist, Lynne","contributorId":8810,"corporation":false,"usgs":true,"family":"Fahlquist","given":"Lynne","affiliations":[],"preferred":false,"id":306908,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Houston, Natalie A. 0000-0002-6071-4545 nhouston@usgs.gov","orcid":"https://orcid.org/0000-0002-6071-4545","contributorId":1682,"corporation":false,"usgs":true,"family":"Houston","given":"Natalie","email":"nhouston@usgs.gov","middleInitial":"A.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":306906,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lindgren, Richard J. lindgren@usgs.gov","contributorId":1667,"corporation":false,"usgs":true,"family":"Lindgren","given":"Richard","email":"lindgren@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":306905,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ging, Patricia B. 0000-0001-5491-8448 pbging@usgs.gov","orcid":"https://orcid.org/0000-0001-5491-8448","contributorId":1788,"corporation":false,"usgs":true,"family":"Ging","given":"Patricia","email":"pbging@usgs.gov","middleInitial":"B.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":306907,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":98906,"text":"fs20103108 - 2010 - Possible effects of groundwater pumping on surface water in the Verde Valley, Arizona","interactions":[],"lastModifiedDate":"2012-02-10T00:10:05","indexId":"fs20103108","displayToPublicDate":"2010-12-02T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-3108","title":"Possible effects of groundwater pumping on surface water in the Verde Valley, Arizona","docAbstract":"The U.S. Geological Survey (USGS), in cooperation with The Nature Conservancy, has applied a groundwater model to simulate effects of groundwater pumping and artificial recharge on surface water in the Verde Valley sub-basin of Arizona. Results are in two sets of maps that show effects of locations of pumping or recharge on streamflow. These maps will help managers make decisions that will meet water needs and minimize environmental impacts. ","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/fs20103108","collaboration":"In cooperation with The Nature Conservancy","usgsCitation":"Leake, S.A., and Haney, J., 2010, Possible effects of groundwater pumping on surface water in the Verde Valley, Arizona: U.S. Geological Survey Fact Sheet 2010-3108, 4 p., https://doi.org/10.3133/fs20103108.","productDescription":"4 p.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"links":[{"id":126143,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2010_3108.gif"},{"id":14325,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2010/3108/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,34 ], [ -114,35.5 ], [ -110,35.5 ], [ -110,34 ], [ -114,34 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683b7b","contributors":{"authors":[{"text":"Leake, Stanley A. 0000-0003-3568-2542 saleake@usgs.gov","orcid":"https://orcid.org/0000-0003-3568-2542","contributorId":1846,"corporation":false,"usgs":true,"family":"Leake","given":"Stanley","email":"saleake@usgs.gov","middleInitial":"A.","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":true,"id":306903,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haney, Jeanmarie","contributorId":13192,"corporation":false,"usgs":true,"family":"Haney","given":"Jeanmarie","email":"","affiliations":[],"preferred":false,"id":306904,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":98909,"text":"sir20105240 - 2010 - Channel-conveyance capacity, channel change, and sediment transport in the lower Puyallup, White, and Carbon Rivers, western Washington","interactions":[],"lastModifiedDate":"2012-03-08T17:16:13","indexId":"sir20105240","displayToPublicDate":"2010-12-02T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-5240","title":"Channel-conveyance capacity, channel change, and sediment transport in the lower Puyallup, White, and Carbon Rivers, western Washington","docAbstract":"Draining the volcanic, glaciated terrain of Mount Rainier, Washington, the Puyallup, White, and Carbon Rivers convey copious volumes of water and sediment down to Commencement Bay in Puget Sound. Recent flooding in the lowland river system has renewed interest in understanding sediment transport and its effects on flow conveyance throughout the lower drainage basin. Bathymetric and topographic data for 156 cross sections were surveyed in the lower Puyallup River system by the U.S. Geological Survey (USGS) and were compared with similar datasets collected in 1984. Regions of significant aggradation were measured along the Puyallup and White Rivers. Between 1984 and 2009, aggradation totals as measured by changes in average channel elevation were as much as 7.5, 6.5, and 2 feet on the Puyallup, White, and Carbon Rivers, respectively. These aggrading river sections correlated with decreasing slopes in riverbeds where the rivers exit relatively confined sections in the upper drainage and enter the relatively unconstricted valleys of the low-gradient Puget Lowland. Measured grain-size distributions from each riverbed showed a progressive fining downstream.\r\n\r\nAnalysis of stage-discharge relations at streamflow-gaging stations along rivers draining Mount Rainier demonstrated the dynamic nature of channel morphology on river courses influenced by glaciated, volcanic terrain. The greatest rates of aggradation since the 1980s were in the Nisqually River near National (5.0 inches per year) and the White River near Auburn (1.8 inches per year). Less pronounced aggradation was measured on the Puyallup River and the White River just downstream of Mud Mountain Dam. The largest measured rate of incision was measured in the Cowlitz River at Packwood (5.0 inches per year).\r\n\r\nChannel-conveyance capacity estimated using a one-dimensional hydraulic model decreased in some river reaches since 1984. The reach exhibiting the largest decrease (about 20-50 percent) in channel-conveyance capacity was the White River between R Street Bridge and the Lake Tapps return, a reach affected by recent flooding. Conveyance capacity also decreased in sections of the Puyallup River. Conveyance capacity was mostly unchanged along other study reaches. Bedload transport was simulated throughout the entire river network and consistent with other observations and analyses, the hydraulic model showed that the upper Puyallup and White Rivers tended to accumulate sediment. Accuracy of the bedload-transport modeling, however, was limited due to a scarcity of sediment-transport data sets from the Puyallup system, mantling of sand over cobbles in the lower Puyallup and White Rivers, and overall uncertainty in modeling sediment transport in gravel-bedded rivers. Consequently, the output results from the model were treated as more qualitative in value, useful in comparing geomorphic trends within different river reaches, but not accurate in producing precise predictions of mass of sediment moved or deposited.\r\n\r\nThe hydraulic model and the bedload-transport component were useful for analyzing proposed river-management options, if surveyed cross sections adequately represented the river-management site and proposed management options. The hydraulic model showed that setback levees would provide greater flood protection than gravel-bar scalping after the initial project construction and for some time thereafter, although the model was not accurate enough to quantify the length of time of the flood protection.  The greatest hydraulic benefit from setback levees would be a substantial increase in the effective channel-conveyance area. By widening the distance between levees, the new floodplain would accommodate larger increases in discharge with relatively small incremental increases in stage. Model simulation results indicate that the hydraulic benefit from a setback levee also would be long-lived and would effectively compensate for increased deposition within the setback reach","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/sir20105240","collaboration":"Prepared in cooperation with Pierce County Public Works and Utilities, Surface Water Managment","usgsCitation":"Czuba, J., Czuba, C.R., Magirl, C.S., and Voss, F.D., 2010, Channel-conveyance capacity, channel change, and sediment transport in the lower Puyallup, White, and Carbon Rivers, western Washington: U.S. Geological Survey Scientific Investigations Report 2010-5240, xii, 85 p.; Appendices; Data Files: 2009 Bed Material Grain Size Distributions; 2009 USGS Cross Sections; 2010 USGS Additional Sumner Cross Sections, https://doi.org/10.3133/sir20105240.","productDescription":"xii, 85 p.; Appendices; Data Files: 2009 Bed Material Grain Size Distributions; 2009 USGS Cross Sections; 2010 USGS Additional Sumner Cross Sections","additionalOnlineFiles":"Y","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":126142,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2010_5240.bmp"},{"id":14328,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2010/5240/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.5,46.666666666666664 ], [ -122.5,47.333333333333336 ], [ -121.33333333333333,47.333333333333336 ], [ -121.33333333333333,46.666666666666664 ], [ -122.5,46.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e629a","contributors":{"authors":[{"text":"Czuba, Jonathan A.","contributorId":19917,"corporation":false,"usgs":true,"family":"Czuba","given":"Jonathan A.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":false,"id":306915,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Czuba, Christiana R. cczuba@usgs.gov","contributorId":4555,"corporation":false,"usgs":true,"family":"Czuba","given":"Christiana","email":"cczuba@usgs.gov","middleInitial":"R.","affiliations":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"preferred":false,"id":306914,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Magirl, Chistopher S.","contributorId":92213,"corporation":false,"usgs":true,"family":"Magirl","given":"Chistopher","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":306916,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Voss, Frank D. fdvoss@usgs.gov","contributorId":1651,"corporation":false,"usgs":true,"family":"Voss","given":"Frank","email":"fdvoss@usgs.gov","middleInitial":"D.","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":306913,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":9000489,"text":"sir20105187 - 2010 - Thunderstorms and flooding of August 17, 2007, with a context provided by a history of other large storm and flood events in the Black Hills area of South Dakota","interactions":[],"lastModifiedDate":"2017-10-14T11:54:34","indexId":"sir20105187","displayToPublicDate":"2010-12-02T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-5187","title":"Thunderstorms and flooding of August 17, 2007, with a context provided by a history of other large storm and flood events in the Black Hills area of South Dakota","docAbstract":"The Black Hills area of western South Dakota has a history of damaging flash floods that have resulted primarily from exceptionally strong rain-producing thunderstorms. The best known example is the catastrophic storm system of June 9-10, 1972, which caused severe flooding in several major drainages near Rapid City and resulted in 238 deaths. More recently, severe thunderstorms caused flash flooding near Piedmont and Hermosa on August 17, 2007. Obtaining a thorough understanding of peak-flow characteristics for low-probability floods will require a comprehensive long-term approach involving (1) documentation of scientific information for extreme events such as these; (2) long-term collection of systematic peak-flow records; and (3) regional assessments of a wide variety of peak-flow information. To that end, the U.S. Geological Survey cooperated with the South Dakota Department of Transportation and National Weather Service to produce this report, which provides documentation regarding the August 17, 2007, storm and associated flooding and provides a context through examination of other large storm and flood events in the Black Hills area. The area affected by the August 17, 2007, storms and associated flooding generally was within the area affected by the larger storm of June 9-10, 1972. The maximum observed 2007 precipitation totals of between 10.00 and 10.50 inches occurred within about 2-3 hours in a small area about 5 miles west of Hermosa. The maximum documented precipitation amount in 1972 was 15.0 inches, and precipitation totals of 10.0 inches or more were documented for 34 locations within an area of about 76 square miles. A peak flow of less than 1 cubic foot per second occurred upstream from the 2007 storm extent for streamflow-gaging station 06404000 (Battle Creek near Keystone); whereas, the 1972 peak flow of 26,200 cubic feet per second was large, relative to the drainage area of only 58.6 square miles. Farther downstream along Battle Creek, a 2007 flow of 26,000 cubic feet per second was generated entirely within an intervening drainage area of only 44.4 square miles. An especially large flow of 44,100 cubic feet per second was documented for this location in 1972. The 2007 peak flow of 18,600 cubic feet per second for Battle Creek at Hermosa (station 06406000) was only slightly smaller than the 1972 peak flow of 21,400 cubic feet per second. Peak-flow values from 2007 for three sites with small drainage areas (less than 1.0 square mile) plot close to a regional envelope curve, indicating exceptionally large flow values, relative to drainage area. Physiographic factors that affect flooding in the area were examined. The limestone headwater hydrogeologic setting (within and near the Limestone Plateau area on the western flank of the Black Hills) has distinctively suppressed peak-flow characteristics for small recurrence intervals. Uncertainty is large, however, regarding characteristics for large recurrence intervals (low-probability floods) because of a dearth of information regarding the potential for generation of exceptionally strong rain-producing thunderstorms. In contrast, the greatest potential for exceptionally damaging floods is around the flanks of the rest of the Black Hills area because of steep topography and limited potential for attenuation of flood peaks in narrow canyons. Climatological factors that affect area flooding also were examined. Area thunderstorms are largely terrain-driven, especially with respect to their requisite upward motion, which can be initiated by orographic lifting effects, thermally enhanced circulations, and obstacle effects. Several other meteorological processes are influential in the development of especially heavy precipitation for the area, including storm cell training, storm anchoring or regeneration, storm mergers, supercell development, and weak upper-level air flow. A composite of storm total precipitation amounts for 13 recent individual storm events indicates","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20105187","collaboration":"Prepared in cooperation with the South Dakota Department of Transportation and the National Weather Service","usgsCitation":"Driscoll, D.G., Bunkers, M.J., Carter, J.M., Stamm, J., and Williamson, J., 2010, Thunderstorms and flooding of August 17, 2007, with a context provided by a history of other large storm and flood events in the Black Hills area of South Dakota: U.S. Geological Survey Scientific Investigations Report 2010-5187, viii, 140 p., https://doi.org/10.3133/sir20105187.","productDescription":"viii, 140 p.","numberOfPages":"139","additionalOnlineFiles":"N","costCenters":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":126024,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2010_5187.bmp"},{"id":19166,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2010/5187/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"South Dakota","otherGeospatial":"Black Hills","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.5,43.25 ], [ -104.5,45 ], [ -102,45 ], [ -102,43.25 ], [ -104.5,43.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b88f","contributors":{"authors":[{"text":"Driscoll, Daniel G. dgdrisco@usgs.gov","contributorId":1558,"corporation":false,"usgs":true,"family":"Driscoll","given":"Daniel","email":"dgdrisco@usgs.gov","middleInitial":"G.","affiliations":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":344115,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bunkers, Matthew J.","contributorId":73149,"corporation":false,"usgs":true,"family":"Bunkers","given":"Matthew","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":344118,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carter, Janet M. 0000-0002-6376-3473 jmcarter@usgs.gov","orcid":"https://orcid.org/0000-0002-6376-3473","contributorId":339,"corporation":false,"usgs":true,"family":"Carter","given":"Janet","email":"jmcarter@usgs.gov","middleInitial":"M.","affiliations":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"preferred":false,"id":344114,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stamm, John F. 0000-0002-3404-2933 jstamm@usgs.gov","orcid":"https://orcid.org/0000-0002-3404-2933","contributorId":2859,"corporation":false,"usgs":true,"family":"Stamm","given":"John F.","email":"jstamm@usgs.gov","affiliations":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":false,"id":344117,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Williamson, Joyce E. jewillia@usgs.gov","contributorId":1964,"corporation":false,"usgs":true,"family":"Williamson","given":"Joyce E.","email":"jewillia@usgs.gov","affiliations":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":false,"id":344116,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70003731,"text":"70003731 - 2010 - The effects of raking on sugar pine mortality following prescribed fire in Sequoia and Kings Canyon National Parks, California, USA","interactions":[],"lastModifiedDate":"2021-01-15T15:04:25.880484","indexId":"70003731","displayToPublicDate":"2010-12-01T13:32:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1636,"text":"Fire Ecology","active":true,"publicationSubtype":{"id":10}},"title":"The effects of raking on sugar pine mortality following prescribed fire in Sequoia and Kings Canyon National Parks, California, USA","docAbstract":"<p><span>Prescribed fire is an important tool for fuel reduction, the control of competing vegetation, and forest restoration. The accumulated fuels associated with historical fire exclusion can cause undesirably high tree mortality rates following prescribed fires and wildfires. This is especially true for sugar pine (</span><i>Pinus lambertiana</i><span>&nbsp;Douglas), which is already negatively affected by the introduced pathogen white pine blister rust (</span><i>Cronartium ribicola</i><span>&nbsp;J.C. Fisch. ex Rabenh). We tested the efficacy of raking away fuels around the base of sugar pine to reduce mortality following prescribed fire in Sequoia and Kings Canyon national parks, California, USA. This study was conducted in three prescribed fires and included 457 trees, half of which had the fuels around their bases raked away to mineral soil to 0.5 m away from the stem. Fire effects were assessed and tree mortality was recorded for three years after prescribed fires. Overall, raking had no detectable effect on mortality: raked trees averaged 30% mortality compared to 36% for unraked trees. There was a significant effect, however, between the interaction of raking and average pre-treatment forest floor fuel depth: the predicted probability of survival of a 50 cm dbh tree was 0.94 vs. 0.96 when average pre-treatment fuel depth was 0 cm for a raked and unraked tree, respectively. When average pre-treatment forest floor fuel depth was 30 cm, the predicted probability of survival for a raked 50 cm dbh tree was 0.60 compared to only 0.07 for an unraked tree. Raking did not affect mortality when fire intensity, measured as percent crown volume scorched, was very low (0% scorch) or very high (&gt;80% scorch), but the raking treatment significantly increased the proportion of trees that survived by 9.6% for trees that burned under moderate fire intensity (1% to 80% scorch). Raking significantly reduced the likelihood of bole charring and bark beetle activity three years post fire. Fuel depth and anticipated fire intensity need to be accounted for to maximize the effectiveness of the treatments. Raking is an important management option to reduce tree mortality from prescribed fire, but is most effective under specific fuel and burning conditions.</span></p>","language":"English","publisher":"The Association for Fire Ecology","doi":"10.4996/fireecology.0603097","usgsCitation":"Nesmith, J.C., O’Hara, K.L., van Mantgem, P.J., and de Valpine, P., 2010, The effects of raking on sugar pine mortality following prescribed fire in Sequoia and Kings Canyon National Parks, California, USA: Fire Ecology, v. 6, no. 3, p. 97-116, https://doi.org/10.4996/fireecology.0603097.","productDescription":"20 p.","startPage":"97","endPage":"116","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":475635,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.4996/fireecology.0603097","text":"Publisher Index Page"},{"id":382217,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Sequoia National Park;Kings Canyon National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.6083984375,\n              37.431250501793585\n            ],\n            [\n              -119.388427734375,\n              37.046408899699564\n            ],\n            [\n              -118.91601562499999,\n              36.53612263184686\n            ],\n            [\n              -118.970947265625,\n              36.26199220445664\n            ],\n            [\n              -118.487548828125,\n              35.8356283888737\n            ],\n            [\n              -117.7734375,\n              35.23664622093195\n            ],\n            [\n              -117.8173828125,\n              35.88014896488361\n            ],\n            [\n              -118.070068359375,\n              36.4566360115962\n            ],\n            [\n              -118.311767578125,\n              37.15156050223665\n            ],\n            [\n              -118.6083984375,\n              37.431250501793585\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"3","noUsgsAuthors":false,"publicationDate":"2010-12-01","publicationStatus":"PW","scienceBaseUri":"505bab96e4b08c986b322f3c","contributors":{"authors":[{"text":"Nesmith, Jonathan C. B.","contributorId":88618,"corporation":false,"usgs":true,"family":"Nesmith","given":"Jonathan","email":"","middleInitial":"C. B.","affiliations":[],"preferred":false,"id":348566,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Hara, Kevin L.","contributorId":9923,"corporation":false,"usgs":true,"family":"O’Hara","given":"Kevin","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":348564,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"van Mantgem, Phillip J. 0000-0002-3068-9422 pvanmantgem@usgs.gov","orcid":"https://orcid.org/0000-0002-3068-9422","contributorId":2838,"corporation":false,"usgs":true,"family":"van Mantgem","given":"Phillip","email":"pvanmantgem@usgs.gov","middleInitial":"J.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":348563,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"de Valpine, Perry","contributorId":58147,"corporation":false,"usgs":true,"family":"de Valpine","given":"Perry","affiliations":[],"preferred":false,"id":348565,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70154929,"text":"70154929 - 2010 - Summer microhabitat use by adult and young-of-year snail darters (Percina tanasi) in two rivers","interactions":[],"lastModifiedDate":"2021-03-16T18:08:55.860634","indexId":"70154929","displayToPublicDate":"2010-12-01T13:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1471,"text":"Ecology of Freshwater Fish","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Summer microhabitat use by adult and young-of-year snail darters (<i>Percina tanasi</i>) in two rivers","title":"Summer microhabitat use by adult and young-of-year snail darters (Percina tanasi) in two rivers","docAbstract":"<p><span>We characterised microhabitat availability and use by adult and young‐of‐year (YOY) snail darters (</span><i>Percina tanasi </i><span><a id=\"#b6R\" class=\"bibLink tab-link\" href=\"https://onlinelibrary.wiley.com/doi/full/10.1111/j.1600-0633.2010.00442.x#b6\" data-tab=\"pane-pcw-references\" data-mce-href=\"https://onlinelibrary.wiley.com/doi/full/10.1111/j.1600-0633.2010.00442.x#b6\">Etnier 1976</a></span><span>) while snorkelling in the French Broad and Hiwassee rivers, TN, USA. Both age groups of snail darters disproportionately used most microhabitat variables compared to their availability. Snail darters primarily occupied moderately deep, swift water over gravel substrates with little macrophyte coverage and no silt. Univariate comparisons indicated that adult and YOY darters occupied different habitat, but there was no marked differences between principal components analysis plots of multivariate microhabitat use within a river. Although the availability of microhabitat variables differed between the French Broad and Hiwassee rivers, univariate means and multivariate plots illustrated that the habitats used were generally similar by age groups of snail darters between rivers. Because our observations of habitat availability and use were constrained to low flow periods and depths &lt;1 m, the transferability of our results to higher flow periods may be limited. However, the similarity in habitat use between rivers suggests that our results can be applied to low‐normal flow conditions in other streams.</span></p>","language":"English","publisher":"Wiley","publisherLocation":"Copenhagen","doi":"10.1111/j.1600-0633.2010.00442.x","usgsCitation":"Ashton, M.J., and Layzer, J.B., 2010, Summer microhabitat use by adult and young-of-year snail darters (Percina tanasi) in two rivers: Ecology of Freshwater Fish, v. 19, no. 4, p. 609-617, https://doi.org/10.1111/j.1600-0633.2010.00442.x.","productDescription":"9 p.","startPage":"609","endPage":"617","numberOfPages":"9","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-019539","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":305808,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"4","publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationDate":"2010-11-11","publicationStatus":"PW","scienceBaseUri":"55aa2740e4b0183d66e47e9f","contributors":{"authors":[{"text":"Ashton, M. J.","contributorId":24206,"corporation":false,"usgs":false,"family":"Ashton","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":565012,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Layzer, James B. jim_layzer@usgs.gov","contributorId":1917,"corporation":false,"usgs":true,"family":"Layzer","given":"James","email":"jim_layzer@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":564375,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70235955,"text":"70235955 - 2010 - Invasion biology and parasitic infections","interactions":[],"lastModifiedDate":"2026-01-29T20:33:46.710316","indexId":"70235955","displayToPublicDate":"2010-12-01T12:47:24","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Invasion biology and parasitic infections","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Infectious disease ecology: Effects of ecosystems on disease and of disease on ecosystems","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Princeton University Press","usgsCitation":"Perkins, S., Altizer, S., Bjornstad, O., Burdon, J.J., Clay, K., Gomez-Aparicio, L., Jeschke, J., Johnson, P., Lafferty, K.D., Malmstrom, C.M., Martin, P., Power, A., Strayer, D., Thrall, P.H., and Uriarte, M., 2010, Invasion biology and parasitic infections, chap. <i>of</i> Infectious disease ecology: Effects of ecosystems on disease and of disease on ecosystems, p. 179-204.","productDescription":"26 p.","startPage":"179","endPage":"204","costCenters":[],"links":[{"id":405605,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":405604,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://press.princeton.edu/books/paperback/9780691124858/infectious-disease-ecology"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Ostfeld, Richard S.","contributorId":64800,"corporation":false,"usgs":true,"family":"Ostfeld","given":"Richard","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":849708,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Keesing, Felicia","contributorId":295595,"corporation":false,"usgs":false,"family":"Keesing","given":"Felicia","email":"","affiliations":[],"preferred":false,"id":849709,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Eviner, Valerie T.","contributorId":167553,"corporation":false,"usgs":false,"family":"Eviner","given":"Valerie","email":"","middleInitial":"T.","affiliations":[{"id":24746,"text":"Department of Plant Sciences, UC Davis, CA","active":true,"usgs":false}],"preferred":false,"id":849710,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Perkins, Sarah","contributorId":168336,"corporation":false,"usgs":false,"family":"Perkins","given":"Sarah","affiliations":[{"id":25257,"text":"Battelle Memorial Institute","active":true,"usgs":false}],"preferred":false,"id":849693,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Altizer, Sonia","contributorId":195669,"corporation":false,"usgs":false,"family":"Altizer","given":"Sonia","email":"","affiliations":[],"preferred":false,"id":849694,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bjornstad, Ottar","contributorId":193645,"corporation":false,"usgs":false,"family":"Bjornstad","given":"Ottar","affiliations":[],"preferred":false,"id":849695,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Burdon, Jeremy J.","contributorId":295602,"corporation":false,"usgs":false,"family":"Burdon","given":"Jeremy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":849696,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Clay, Keith","contributorId":140472,"corporation":false,"usgs":false,"family":"Clay","given":"Keith","email":"","affiliations":[{"id":12645,"text":"Indiana University - Northwest","active":true,"usgs":false}],"preferred":false,"id":849697,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gomez-Aparicio, Lorena","contributorId":295603,"corporation":false,"usgs":false,"family":"Gomez-Aparicio","given":"Lorena","email":"","affiliations":[],"preferred":false,"id":849698,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Jeschke, Jonathan M.","contributorId":268106,"corporation":false,"usgs":false,"family":"Jeschke","given":"Jonathan M.","affiliations":[{"id":38332,"text":"Leibniz-Institute of Freshwater Ecology and Inland Fisheries","active":true,"usgs":false}],"preferred":false,"id":849699,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Johnson, Pieter T. J.","contributorId":245043,"corporation":false,"usgs":false,"family":"Johnson","given":"Pieter T. J.","affiliations":[{"id":36621,"text":"University of Colorado","active":true,"usgs":false}],"preferred":false,"id":849700,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Lafferty, Kevin D. 0000-0001-7583-4593 klafferty@usgs.gov","orcid":"https://orcid.org/0000-0001-7583-4593","contributorId":1415,"corporation":false,"usgs":true,"family":"Lafferty","given":"Kevin","email":"klafferty@usgs.gov","middleInitial":"D.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":849701,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Malmstrom, Carolyn M.","contributorId":295604,"corporation":false,"usgs":false,"family":"Malmstrom","given":"Carolyn","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":849702,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Martin, Patrick","contributorId":244109,"corporation":false,"usgs":false,"family":"Martin","given":"Patrick","email":"","affiliations":[],"preferred":false,"id":849703,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Power, Alison","contributorId":295605,"corporation":false,"usgs":false,"family":"Power","given":"Alison","email":"","affiliations":[],"preferred":false,"id":849704,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Strayer, David L.","contributorId":238531,"corporation":false,"usgs":false,"family":"Strayer","given":"David L.","affiliations":[{"id":47722,"text":"Cary Institute of Ecosystem Studies, Millbrook, NY","active":true,"usgs":false}],"preferred":false,"id":849705,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Thrall, Peter H.","contributorId":295606,"corporation":false,"usgs":false,"family":"Thrall","given":"Peter","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":849706,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Uriarte, Maria","contributorId":287019,"corporation":false,"usgs":false,"family":"Uriarte","given":"Maria","affiliations":[{"id":7171,"text":"Columbia University","active":true,"usgs":false}],"preferred":false,"id":849707,"contributorType":{"id":1,"text":"Authors"},"rank":15}]}}
,{"id":70235948,"text":"70235948 - 2010 - Effects of disease on community interactions and food web structure","interactions":[],"lastModifiedDate":"2022-08-25T17:29:27.220758","indexId":"70235948","displayToPublicDate":"2010-12-01T12:22:50","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Effects of disease on community interactions and food web structure","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Infectious disease ecology: Effects of ecosystems on disease and of disease on ecosystems","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Princeton University Press","usgsCitation":"Lafferty, K.D., 2010, Effects of disease on community interactions and food web structure, chap. <i>of</i> Infectious disease ecology: Effects of ecosystems on disease and of disease on ecosystems, p. 205-222.","productDescription":"18 p.","startPage":"205","endPage":"222","costCenters":[],"links":[{"id":405603,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":405602,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://press.princeton.edu/books/paperback/9780691124858/infectious-disease-ecology"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Ostfeld, Richard S.","contributorId":64800,"corporation":false,"usgs":true,"family":"Ostfeld","given":"Richard","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":849690,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Keesing, Felicia","contributorId":295595,"corporation":false,"usgs":false,"family":"Keesing","given":"Felicia","email":"","affiliations":[],"preferred":false,"id":849691,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Eviner, Valerie T.","contributorId":167553,"corporation":false,"usgs":false,"family":"Eviner","given":"Valerie","email":"","middleInitial":"T.","affiliations":[{"id":24746,"text":"Department of Plant Sciences, UC Davis, CA","active":true,"usgs":false}],"preferred":false,"id":849692,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Lafferty, Kevin D. 0000-0001-7583-4593 klafferty@usgs.gov","orcid":"https://orcid.org/0000-0001-7583-4593","contributorId":1415,"corporation":false,"usgs":true,"family":"Lafferty","given":"Kevin","email":"klafferty@usgs.gov","middleInitial":"D.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":849689,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70236320,"text":"70236320 - 2010 - Seasonal ice and hydrologic controls on dissolved organic carbon and nitrogen concentrations in a boreal-rich fen","interactions":[],"lastModifiedDate":"2022-09-01T16:42:32.726099","indexId":"70236320","displayToPublicDate":"2010-12-01T11:42:18","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2319,"text":"Journal of Geophysical Research G: Biogeosciences","active":true,"publicationSubtype":{"id":10}},"title":"Seasonal ice and hydrologic controls on dissolved organic carbon and nitrogen concentrations in a boreal-rich fen","docAbstract":"<p>[1] Boreal wetland carbon cycling is vulnerable to climate change in part because hydrology and the extent of frozen ground have strong influences on plant and microbial functions. We examined the response of dissolved organic carbon (DOC) and total dissolved nitrogen (TDN) across an experimental manipulation of water table position (both raised and lowered water table treatments) in a boreal-rich fen in interior Alaska. DOC and TDN responses to water table manipulation exhibited an interaction with seasonal ice dynamics. We observed consistently higher DOC and TDN concentrations in the lowered water table treatment (71.7 ± 6.5 and 3.0 ± 0.3 mg−L) than in both the control (55.6 ± 5.1 and 2.3 ± 0.2 mg−L) and raised (49.1 ± 4.3 and 1.9 ± 0.1 mg L−1, respectively) water table treatments. Across all plots, pore water DOC concentrations at 20 cm increased as the depth to water table increased (R2 = 0.43, p &lt; 0.001). DOC concentrations also increased as the seasonal thaw depth increased, with solutes increasing most rapidly in the drained plot (R2 = 0.62, p &lt; 0.001). About half of the TDN pool was composed of dissolved organic N (DON). Inorganic N and DON were both highly correlated with changes in DOC, and their respective constraints to mineralization are discussed. These results demonstrate that a declining water table position and dryer conditions affect thaw depth and peat temperatures, and interactions among these ecosystem properties will likely increase DOC and TDN loading and potential for export in these systems.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2010JG001366","usgsCitation":"Kane, E.S., Turetsky, M.R., Harden, J.W., McGuire, A.D., and Waddington, J.M., 2010, Seasonal ice and hydrologic controls on dissolved organic carbon and nitrogen concentrations in a boreal-rich fen: Journal of Geophysical Research G: Biogeosciences, v. 115, no. G4, G04012, 15 p., https://doi.org/10.1029/2010JG001366.","productDescription":"G04012, 15 p.","costCenters":[],"links":[{"id":475636,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2010jg001366","text":"Publisher Index Page"},{"id":406075,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Alaska Peatland Experiment, Bonanza Creek Experimental Forest, Tanana Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -147.3204803466797,\n              64.71831979769435\n            ],\n            [\n              -147.2995376586914,\n              64.69822506859181\n            ],\n            [\n              -147.23567962646484,\n              64.65960723743939\n            ],\n            [\n              -147.1127700805664,\n              64.6706255344161\n            ],\n            [\n              -147.1402359008789,\n              64.70218652380355\n            ],\n            [\n              -147.16976165771484,\n              64.71084102073965\n            ],\n            [\n              -147.20993041992188,\n              64.7181731748711\n            ],\n            [\n              -147.2380828857422,\n              64.7213986934753\n            ],\n            [\n              -147.26726531982422,\n              64.72975393054311\n            ],\n            [\n              -147.3204803466797,\n              64.71831979769435\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"115","issue":"G4","noUsgsAuthors":false,"publicationDate":"2010-10-14","publicationStatus":"PW","contributors":{"authors":[{"text":"Kane, Evan S.","contributorId":11903,"corporation":false,"usgs":true,"family":"Kane","given":"Evan","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":850600,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Turetsky, Merritt R.","contributorId":80980,"corporation":false,"usgs":true,"family":"Turetsky","given":"Merritt","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":850601,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harden, Jennifer W. 0000-0002-6570-8259 jharden@usgs.gov","orcid":"https://orcid.org/0000-0002-6570-8259","contributorId":1971,"corporation":false,"usgs":true,"family":"Harden","given":"Jennifer","email":"jharden@usgs.gov","middleInitial":"W.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"preferred":true,"id":850602,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McGuire, A. David 0000-0003-4646-0750 ffadm@usgs.gov","orcid":"https://orcid.org/0000-0003-4646-0750","contributorId":166708,"corporation":false,"usgs":true,"family":"McGuire","given":"A.","email":"ffadm@usgs.gov","middleInitial":"David","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":false,"id":850603,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Waddington, James Michael","contributorId":89774,"corporation":false,"usgs":true,"family":"Waddington","given":"James","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":850604,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70118927,"text":"70118927 - 2010 - Characterization of ten microsatellite loci in midget faded rattlesnake (Crotalus oreganus concolor)","interactions":[],"lastModifiedDate":"2017-11-27T15:48:02","indexId":"70118927","displayToPublicDate":"2010-12-01T11:21:13","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1325,"text":"Conservation Genetics Resources","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Characterization of ten microsatellite loci in midget faded rattlesnake (<i>Crotalus oreganus concolor</i>)","title":"Characterization of ten microsatellite loci in midget faded rattlesnake (Crotalus oreganus concolor)","docAbstract":"Primers for 10 microsatellite loci were developed for midget faded rattlesnake (<i>Crotalus oreganus concolor</i>), a small bodied subspecies of the Western Rattlesnake, which is found in the Colorado Plateau of eastern Utah, western Colorado and southwestern Wyoming. In a screen of 23 individuals from the most northern portion of the subspecies range in southwestern Wyoming, the 10 loci were found to have levels of variability ranging from 4 to 11 alleles. No loci were found to be linked, although one locus revealed significant departures from Hardy–Weinberg equilibrium. These microsatellite loci will be applicable for population genetic analyses, which will ultimately aid in management efforts for this rare subspecies of rattlesnake.","language":"English","publisher":"Springer","doi":"10.1007/s12686-010-9181-x","usgsCitation":"Oyler-McCance, S.J., and Parker, J.M., 2010, Characterization of ten microsatellite loci in midget faded rattlesnake (Crotalus oreganus concolor): Conservation Genetics Resources, v. 2, no. 1, p. 123-125, https://doi.org/10.1007/s12686-010-9181-x.","productDescription":"3 p.","startPage":"123","endPage":"125","numberOfPages":"3","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":291484,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":291483,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s12686-010-9181-x"}],"volume":"2","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-02-07","publicationStatus":"PW","scienceBaseUri":"53db5841e4b0fba533fa3569","contributors":{"authors":[{"text":"Oyler-McCance, Sara J. 0000-0003-1599-8769 sara_oyler-mccance@usgs.gov","orcid":"https://orcid.org/0000-0003-1599-8769","contributorId":1973,"corporation":false,"usgs":true,"family":"Oyler-McCance","given":"Sara","email":"sara_oyler-mccance@usgs.gov","middleInitial":"J.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":497509,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parker, Joshua M.","contributorId":91794,"corporation":false,"usgs":true,"family":"Parker","given":"Joshua","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":497510,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70256011,"text":"70256011 - 2010 - Great Plains regional roadmap","interactions":[],"lastModifiedDate":"2024-07-12T15:50:34.076013","indexId":"70256011","displayToPublicDate":"2010-12-01T10:40:45","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Great Plains regional roadmap","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Sustainable alternative fuel feedstock opportunities, challenges and roadmaps for six U.S. regions: Proceedings of the sustainable feedstocks for advance biofuels workshop","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Sustainable Feedstocks for Advance Biofuels Workshop","conferenceDate":"September 28-30, 2010","conferenceLocation":"Atlanta, GA","language":"English","publisher":"Soil and Water Conservation Society","usgsCitation":"Tieszen, L.L., Owens, V., Mitchell, R., Jenkins, R., Gerik, T., Franzluebbers, A.J., Ferrell, J., Doolittle, J., Bliss, N.B., and Archer, D., 2010, Great Plains regional roadmap, <i>in</i> Sustainable alternative fuel feedstock opportunities, challenges and roadmaps for six U.S. regions: Proceedings of the sustainable feedstocks for advance biofuels workshop, Atlanta, GA, September 28-30, 2010, p. 401-405.","productDescription":"5 p.","startPage":"401","endPage":"405","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":431019,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Tieszen, Larry L. tieszen@usgs.gov","contributorId":2831,"corporation":false,"usgs":true,"family":"Tieszen","given":"Larry","email":"tieszen@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":906371,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Owens, Vance","contributorId":340147,"corporation":false,"usgs":false,"family":"Owens","given":"Vance","email":"","affiliations":[],"preferred":false,"id":906372,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mitchell, Rob","contributorId":340149,"corporation":false,"usgs":false,"family":"Mitchell","given":"Rob","affiliations":[],"preferred":false,"id":906373,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jenkins, Robin","contributorId":340148,"corporation":false,"usgs":false,"family":"Jenkins","given":"Robin","email":"","affiliations":[],"preferred":false,"id":906374,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gerik, Tom","contributorId":340150,"corporation":false,"usgs":false,"family":"Gerik","given":"Tom","email":"","affiliations":[],"preferred":false,"id":906375,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Franzluebbers, Alan J.","contributorId":146789,"corporation":false,"usgs":false,"family":"Franzluebbers","given":"Alan","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":906376,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ferrell, John","contributorId":340151,"corporation":false,"usgs":false,"family":"Ferrell","given":"John","email":"","affiliations":[],"preferred":false,"id":906377,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Doolittle, Jim","contributorId":340152,"corporation":false,"usgs":false,"family":"Doolittle","given":"Jim","email":"","affiliations":[],"preferred":false,"id":906378,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Bliss, Norman B. 0000-0003-2409-5211 bliss@usgs.gov","orcid":"https://orcid.org/0000-0003-2409-5211","contributorId":1921,"corporation":false,"usgs":true,"family":"Bliss","given":"Norman","email":"bliss@usgs.gov","middleInitial":"B.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true},{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"preferred":true,"id":906379,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Archer, D.","contributorId":33078,"corporation":false,"usgs":true,"family":"Archer","given":"D.","affiliations":[],"preferred":false,"id":906380,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70123980,"text":"70123980 - 2010 - A river system to watch: documenting the effects of saltcedar (<i>Tamarix</i> spp.) biocontrol in the Virgin River valley","interactions":[],"lastModifiedDate":"2014-09-11T10:53:31","indexId":"70123980","displayToPublicDate":"2010-12-01T10:36:06","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1462,"text":"Ecological Restoration","active":true,"publicationSubtype":{"id":10}},"title":"A river system to watch: documenting the effects of saltcedar (<i>Tamarix</i> spp.) biocontrol in the Virgin River valley","docAbstract":"<p>Throughout riparian areas of the southwestern United States, non-native saltcedar (also known as tamarisk; <i>Tamarix</i> spp.) can form dense, monotypic stands and is often reported to have detrimental effects on native plants and habitat quality (Everitt 1980; Shafroth et al. 2005). Natural resource managers of these riparian areas spend considerable time and resources controlling saltcedar using a variety of techniques, including chemical (Duncan and McDaniel 1998), mechanical, and burning methods (Shafroth et al. 2005). Approximately one billion dollars are spent each year on river restoration projects nationally (Bernhardt et al. 2005), and a majority of these projects focus on invasive species control in the Southwest (Follstad Shah et al. 2007).</p>\n<br/>\n<p>A technique that has drawn much attention is the use of the saltcedar leaf beetle (<i>Diorhabda</i> spp.), a specialist herbivore, as biological control of saltcedar (Lewis et al. 2003). Research testing was conducted with beetles housed in secure enclosures in six states in 1998 and 1999 (Dudley et al. 2001), followed by open release at some of those sites starting in 2001 (DeLoach et al. 2004). By 2005, full-scale saltcedar biocontrol was implemented in 13 states, led by the USDA Animal and Plant Health Inspection Service (APHIS), the agency that oversees biological control programs, and with the participation and support of the U.S. Fish and Wildlife Service (USFWS). Despite the widespread application of <i>Diorhabda</i>, however, only limited research has quantified the consequences (benefits and costs) on biotic communities and ecosystem services. Alterations to riparian areas caused by various non-native species control activities have the potential to affect a variety of habitat types used by wildlife (Bateman et al. 2008a); processes like water availability, fluvial deposition, and erosion; and the establishment of other non-native species (Carruthers and D'Antonio 2005, Shafroth et al. 2005, DeLoach et al. 2006). Similarly, biocontrol is expected to modify riparian ecosystems, and it is imperative to document and evaluate both the environmental benefits and the potential costs of this tamarisk management method.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecological Restoration","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"University of Wisconsin Press","publisherLocation":"Madison, WI","doi":"10.3368/er.28.4.405","usgsCitation":"Bateman, H.L., Dudley, T.L., Bean, D., Ostoja, S.M., Hultine, K.R., and Kuehn, M.J., 2010, A river system to watch: documenting the effects of saltcedar (<i>Tamarix</i> spp.) biocontrol in the Virgin River valley: Ecological Restoration, v. 28, no. 4, p. 405-410, https://doi.org/10.3368/er.28.4.405.","productDescription":"6 p.","startPage":"405","endPage":"410","numberOfPages":"6","ipdsId":"IP-022978","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":293670,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":293665,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.3368/er.28.4.405"}],"country":"United States","otherGeospatial":"Virgin River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.151,35.9865 ], [ -115.151,37.4919 ], [ -112.4484,37.4919 ], [ -112.4484,35.9865 ], [ -115.151,35.9865 ] ] ] } } ] }","volume":"28","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-11-15","publicationStatus":"PW","scienceBaseUri":"5412b99be4b0239f1986b9fd","contributors":{"authors":[{"text":"Bateman, Heather L.","contributorId":72294,"corporation":false,"usgs":true,"family":"Bateman","given":"Heather","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":500506,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dudley, Tom L.","contributorId":59730,"corporation":false,"usgs":true,"family":"Dudley","given":"Tom","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":500505,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bean, Dan W.","contributorId":58133,"corporation":false,"usgs":true,"family":"Bean","given":"Dan W.","affiliations":[],"preferred":false,"id":500504,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ostoja, Steven M. sostoja@usgs.gov","contributorId":3039,"corporation":false,"usgs":true,"family":"Ostoja","given":"Steven","email":"sostoja@usgs.gov","middleInitial":"M.","affiliations":[{"id":33665,"text":"USDA California Climate Hub, UC Davis","active":true,"usgs":false},{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":500501,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hultine, Kevin R. 0000-0001-9747-6037","orcid":"https://orcid.org/0000-0001-9747-6037","contributorId":23772,"corporation":false,"usgs":true,"family":"Hultine","given":"Kevin","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":500502,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kuehn, Michael J.","contributorId":32095,"corporation":false,"usgs":true,"family":"Kuehn","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":500503,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70256010,"text":"70256010 - 2010 - Coordination of space data acquisition in support of geo forest carbon tracking","interactions":[],"lastModifiedDate":"2024-07-12T15:26:01.153383","indexId":"70256010","displayToPublicDate":"2010-12-01T10:19:16","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Coordination of space data acquisition in support of geo forest carbon tracking","docAbstract":"<p>The Group on Earth Observation (GEO) required for their Forest Carbon Tracking (FCT) task the assistance of the Committee on Earth Observation Satellites (CEOS) space agencies to implement coordinated data acquisition strategies from Earth Observation (EO) over key areas of interest to demonstrate the value of linking coordinated acquisition of satellite data with standardised processing methods, forest inventory and ecosystem models. Both optical and radar of midresolution have been acquired within the coordinated acquisition campaigns developed in 2009 and 2010. Homogeneous and coherent EO databases have already started by means of full key areas coverage according with suitable sensor operating modes. CEOS effort seeks now continuing with an updated strategy over expanded area coverage. </p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of ESA living planet symposium","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"ESA Communications","usgsCitation":"Siefert, F.M., Costa, H., Rosenqvist, A., and Holm, T., 2010, Coordination of space data acquisition in support of geo forest carbon tracking, <i>in</i> Proceedings of ESA living planet symposium, 5 p.","productDescription":"5 p.","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":431018,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Siefert, Frank M.","contributorId":340143,"corporation":false,"usgs":false,"family":"Siefert","given":"Frank","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":906367,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Costa, Hugo","contributorId":340144,"corporation":false,"usgs":false,"family":"Costa","given":"Hugo","email":"","affiliations":[],"preferred":false,"id":906368,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rosenqvist, Ake","contributorId":340145,"corporation":false,"usgs":false,"family":"Rosenqvist","given":"Ake","email":"","affiliations":[],"preferred":false,"id":906369,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Holm, Tom","contributorId":340146,"corporation":false,"usgs":true,"family":"Holm","given":"Tom","email":"","affiliations":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"preferred":false,"id":906370,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70211029,"text":"70211029 - 2010 - Dr. Carl Marti 1944-2010","interactions":[],"lastModifiedDate":"2020-07-10T15:09:02.384732","indexId":"70211029","displayToPublicDate":"2010-12-01T10:02:43","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2442,"text":"Journal of Raptor Research","active":true,"publicationSubtype":{"id":10}},"title":"Dr. Carl Marti 1944-2010","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"BioOne","doi":"10.3356/0892-1016-44.4.335","usgsCitation":"Kochert, M.N., Steenhof, K., and Kennedy, P.L., 2010, Dr. Carl Marti 1944-2010: Journal of Raptor Research, v. 44, no. 4, p. 335-336, https://doi.org/10.3356/0892-1016-44.4.335.","productDescription":"2 p.","startPage":"335","endPage":"336","costCenters":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"links":[{"id":376262,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Kochert, Michael N. 0000-0002-4380-3298 mkochert@usgs.gov","orcid":"https://orcid.org/0000-0002-4380-3298","contributorId":3037,"corporation":false,"usgs":true,"family":"Kochert","given":"Michael","email":"mkochert@usgs.gov","middleInitial":"N.","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":true,"id":792483,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steenhof, Karen karen_steenhof@usgs.gov","contributorId":30585,"corporation":false,"usgs":true,"family":"Steenhof","given":"Karen","email":"karen_steenhof@usgs.gov","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":false,"id":792484,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kennedy, Patricia L.","contributorId":172826,"corporation":false,"usgs":false,"family":"Kennedy","given":"Patricia","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":792485,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70118906,"text":"70118906 - 2010 - Amphibian declines: promising directions in understanding the role of disease","interactions":[],"lastModifiedDate":"2014-07-31T09:34:57","indexId":"70118906","displayToPublicDate":"2010-12-01T09:33:24","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":774,"text":"Animal Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Amphibian declines: promising directions in understanding the role of disease","docAbstract":"No abstract available.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Animal Conservation","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Zoological Society of London","publisherLocation":"Cambridge, England","doi":"10.1111/j.1469-1795.2010.00410.x","usgsCitation":"Muths, E., and Hero, J., 2010, Amphibian declines: promising directions in understanding the role of disease: Animal Conservation, v. 13, no. s1, p. 33-35, https://doi.org/10.1111/j.1469-1795.2010.00410.x.","productDescription":"3 p.","startPage":"33","endPage":"35","numberOfPages":"3","costCenters":[],"links":[{"id":291453,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":291452,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1469-1795.2010.00410.x"}],"volume":"13","issue":"s1","noUsgsAuthors":false,"publicationDate":"2010-11-04","publicationStatus":"PW","scienceBaseUri":"53db5840e4b0fba533fa3563","contributors":{"authors":[{"text":"Muths, Erin 0000-0002-5498-3132","orcid":"https://orcid.org/0000-0002-5498-3132","contributorId":14012,"corporation":false,"usgs":true,"family":"Muths","given":"Erin","affiliations":[],"preferred":false,"id":497395,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hero, J.-M.","contributorId":100999,"corporation":false,"usgs":true,"family":"Hero","given":"J.-M.","affiliations":[],"preferred":false,"id":497396,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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