{"pageNumber":"1048","pageRowStart":"26175","pageSize":"25","recordCount":40837,"records":[{"id":70029533,"text":"70029533 - 2005 - Authigenesis of trace metals in energetic tropical shelf environments","interactions":[],"lastModifiedDate":"2019-05-01T09:44:05","indexId":"70029533","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1333,"text":"Continental Shelf Research","active":true,"publicationSubtype":{"id":10}},"title":"Authigenesis of trace metals in energetic tropical shelf environments","docAbstract":"We evaluated authigenic changes of Fe, Mn, V, U, Mo, Cd and Re in suboxic, periodically remobilized, tropical shelf sediments from the Amazon continental shelf and the Gulf of Papua. The Cd/Al, Mo/Al, and U/Al ratios in Amazon shelf sediments were 82%, 37%, and 16% less than those in Amazon River suspended sediments, respectively. Very large depletions of U previously reported in this environment were not observed. The Cd/Al ratios in Gulf of Papua sediments were 76% lower than measurements made on several Papua New Guinea rivers, whereas U/Al ratios in the shelf sediments were enriched by approximately 20%. Other metal/Al ratios in the Papua New Guinea river suspended sediments and continental shelf sediments were not distinguishably different. Comparison of metal/Al ratios to grain size distributions in Gulf of Papua samples indicates that our observations cannot be attributed to differences in grain size between the river suspended sediments and continental shelf sediments. These two shelves constitute a source of dissolved Cd to the world ocean equal to 29–100% of the dissolved Cd input from rivers, but only 3% of the dissolved Mo input and 4% of the dissolved U input. Release of Cd, Mo, and U in tropical shelf sediments is likely a result of intense Fe and Mn oxide reduction in pore waters and resuspension of the sediments. Since we do not observe depletions of particulate Fe and Mn in the shelf sediments most of these dissolved metals must reoxidize in the overlying waters and reprecipitate. As Cd exhibits the largest losses on these tropical shelves, we examined the ability of newly formed Fe and Mn oxides to adsorb dissolved Cd using a geochemical diffuse double-layer surface complexation model and found the oxide surfaces are relatively ineffective at readsorbing Cd in seawater due to surface-site competition by Mg and Ca. If the remobilization and reoxidation of Fe and Mn occurs frequently enough before sediment is buried significant amounts of Cd may be removed from the oxide surfaces. Because a much greater percentage of Mn than Fe becomes remobilized in these shelf sediments, metals closely associated with Mn oxides (like Cd) are more likely to show losses during deposition.
We present an updated global earthquake catalogue for stable continental regions (SCRs; i.e. intraplate earthquakes) that is available on the Internet. Our database contains information on location, magnitude, seismic moment and focal mechanisms for over 1300 M (moment magnitude) ≥ 4.5 historic and instrumentally recorded crustal events. Using this updated earthquake database in combination with a recently published global catalogue of rifts, we assess the correlation of intraplate seismicity with ancient rifts on a global scale. Each tectonic event is put into one of five categories based on location: (i) interior rifts/taphrogens, (ii) rifted continental margins, (iii) non-rifted crust, (iv) possible interior rifts and (v) possible rifted margins. We find that approximately 27 per cent of all events are classified as interior rifts (i), 25 per cent are rifted continental margins (ii), 36 per cent are within non-rifted crust (iii) and 12 per cent (iv and v) remain uncertain. Thus, over half (52 per cent) of all events are associated with rifted crust, although within the continental interiors (i.e. away from continental margins), non-rifted crust has experienced more earthquakes than interior rifts. No major change in distribution is found if only large (M ≥ 6.0) earthquakes are considered. The largest events (M ≥ 7.0) however, have occurred predominantly within rifts (50 per cent) and continental margins (43 per cent). Intraplate seismicity is not distributed evenly. Instead several zones of concentrated seismicity seem to exist. This is especially true for interior rifts/taphrogens, where a total of only 12 regions are responsible for 74 per cent of all events and as much as 98 per cent of all seismic moment released in that category. Of the four rifts/taphrogens that have experienced the largest earthquakes, seismicity within the Kutch rift, India, and the East China rift system, may be controlled by diffuse plate boundary deformation more than by the presence of the ancient rifts themselves. The St. Lawrence depression, Canada, besides being an ancient rift, is also the site of a major collisional suture. Thus only at the Reelfoot rift (New Madrid seismic zone, NMSZ, USA), is the presence of features associated with rifting itself the sole candidate for causing seismicity. Our results suggest that on a global scale, the correlation of seismicity within SCRs and ancient rifts has been overestimated in the past. Because the majority of models used to explain intraplate seismicity have focused on seismicity within rifts, we conclude that a shift in attention more towards non-rifted as well as rifted crust is in order.
","largerWorkTitle":"","language":"English","publisher":"Oxford Academic","doi":"10.1111/j.1365-246X.2005.02554.x","issn":"0956540X","usgsCitation":"Schulte, S., and Mooney, W.D., 2005, An updated global earthquake catalogue for stable continental regions: Reassessing the correlation with ancient rifts: Geophysical Journal International, v. 161, no. 3, p. 707-721, https://doi.org/10.1111/j.1365-246X.2005.02554.x.","productDescription":"15 p.","startPage":"707","endPage":"721","numberOfPages":"15","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":477691,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1365-246x.2005.02554.x","text":"Publisher Index Page"},{"id":237749,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"161","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059eab5e4b0c8380cd48a1c","contributors":{"authors":[{"text":"Schulte, S.M.","contributorId":22568,"corporation":false,"usgs":true,"family":"Schulte","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":423155,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mooney, Walter D. 0000-0002-5310-3631 mooney@usgs.gov","orcid":"https://orcid.org/0000-0002-5310-3631","contributorId":3194,"corporation":false,"usgs":true,"family":"Mooney","given":"Walter","email":"mooney@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":423156,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029539,"text":"70029539 - 2005 - The role of topography on catchment‐scale water residence time","interactions":[],"lastModifiedDate":"2018-04-02T15:55:05","indexId":"70029539","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"The role of topography on catchment‐scale water residence time","docAbstract":"The age, or residence time, of water is a fundamental descriptor of catchment hydrology, revealing information about the storage, flow pathways, and source of water in a single integrated measure. While there has been tremendous recent interest in residence time estimation to characterize watersheds, there are relatively few studies that have quantified residence time at the watershed scale, and fewer still that have extended those results beyond single catchments to larger landscape scales. We examined topographic controls on residence time for seven catchments (0.085–62.4 km2) that represent diverse geologic and geomorphic conditions in the western Cascade Mountains of Oregon. Our primary objective was to determine the dominant physical controls on catchment‐scale water residence time and specifically test the hypothesis that residence time is related to the size of the basin. Residence times were estimated by simple convolution models that described the transfer of precipitation isotopic composition to the stream network. We found that base flow mean residence times for exponential distributions ranged from 0.8 to 3.3 years. Mean residence time showed no correlation to basin area (r2 < 0.01) but instead was correlated (r2 = 0.91) to catchment terrain indices representing the flow path distance and flow path gradient to the stream network. These results illustrate that landscape organization (i.e., topography) rather than basin area controls catchment‐scale transport. Results from this study may provide a framework for describing scale‐invariant transport across climatic and geologic conditions, whereby the internal form and structure of the basin defines the first‐order control on base flow residence time.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2004WR003657","usgsCitation":"McGuire, K., McDonnell, J.J., Weiler, M., Kendall, C., McGlynn, B., Welker, J., and Seibert, J., 2005, The role of topography on catchment‐scale water residence time: Water Resources Research, v. 41, no. 5, Article W05002; 14 p., https://doi.org/10.1029/2004WR003657.","productDescription":"Article W05002; 14 p.","costCenters":[],"links":[{"id":237782,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"41","issue":"5","noUsgsAuthors":false,"publicationDate":"2005-05-03","publicationStatus":"PW","scienceBaseUri":"505baf9fe4b08c986b324929","contributors":{"authors":[{"text":"McGuire, K.J.","contributorId":88943,"corporation":false,"usgs":true,"family":"McGuire","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":423189,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McDonnell, Jeffery J. 0000-0002-3880-3162","orcid":"https://orcid.org/0000-0002-3880-3162","contributorId":62723,"corporation":false,"usgs":false,"family":"McDonnell","given":"Jeffery","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":423187,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weiler, M.","contributorId":15003,"corporation":false,"usgs":false,"family":"Weiler","given":"M.","email":"","affiliations":[],"preferred":false,"id":423184,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kendall, C. 0000-0002-0247-3405","orcid":"https://orcid.org/0000-0002-0247-3405","contributorId":35050,"corporation":false,"usgs":true,"family":"Kendall","given":"C.","affiliations":[],"preferred":false,"id":423185,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"McGlynn, B.L.","contributorId":106664,"corporation":false,"usgs":true,"family":"McGlynn","given":"B.L.","email":"","affiliations":[],"preferred":false,"id":423190,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Welker, J.M.","contributorId":82868,"corporation":false,"usgs":true,"family":"Welker","given":"J.M.","affiliations":[],"preferred":false,"id":423188,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Seibert, J.","contributorId":37513,"corporation":false,"usgs":true,"family":"Seibert","given":"J.","email":"","affiliations":[],"preferred":false,"id":423186,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70029543,"text":"70029543 - 2005 - Arsenic-bearing pyrite and marcasite in the Fire Clay coal bed, Middle Pennsylvanian Breathitt Formation, eastern Kentucky","interactions":[],"lastModifiedDate":"2012-03-12T17:20:46","indexId":"70029543","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2033,"text":"International Journal of Coal Geology","active":true,"publicationSubtype":{"id":10}},"title":"Arsenic-bearing pyrite and marcasite in the Fire Clay coal bed, Middle Pennsylvanian Breathitt Formation, eastern Kentucky","docAbstract":"Arsenic concentrations determined on 11 lithotype samples from the Middle Pennsylvanian Breathitt Group Fire Clay coal bed, Leslie County, KY, range from 1 to 418 ppm (whole coal basis). The 11 lithotype samples, which vary in thickness from 4 to 18 cm, were sampled from a continuous 1.38 m channel sample, and were selected based on megascopic appearance (vitrain-rich versus attrital-rich). A lithotype that contains 418 ppm As is located near the top of the coal bed and is composed of 10.5 cm of bright clarain bands containing fusain that, within short distances, grade laterally into Fe sulfide bands. To determine the mode of occurrence of As in this lithotype, the coal was examined with scanning electron microscopy and analyzed by energy dispersive X-ray fluorescence. Massive, framboidal, cell filling, cell-wall replacement, and radiating forms of Fe sulfide were observed in the high As lithotype; many of the radiating Fe sulfide forms, and one of the cell-wall replacements contained As. Examination of the grains with optical light microscopy shows that the majority of radiating morphologies are pyrite, the remainder are marcasite. Selected Fe sulfide grains were also analyzed by electron microprobe microscopy. Arsenic concentrations within individual grains range from 0.0 wt.% to approximately 3.5 wt.%. On the basis of morphology, these Fe sulfides are presumed to be of syngenetic origin and would probably be removed from the coal during physical coal cleaning, thus eliminating a potential source of As from the coal combustion process. However, because the grains are radiating and have high surface area, dissolution and release of As could occur if the pyrite is oxidized in refuse ponds.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"International Journal of Coal Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.coal.2005.02.003","issn":"01665162","usgsCitation":"Ruppert, L., Hower, J., and Eble, C., 2005, Arsenic-bearing pyrite and marcasite in the Fire Clay coal bed, Middle Pennsylvanian Breathitt Formation, eastern Kentucky: International Journal of Coal Geology, v. 63, no. 1-2 SPEC. ISS., p. 27-35, https://doi.org/10.1016/j.coal.2005.02.003.","startPage":"27","endPage":"35","numberOfPages":"9","costCenters":[],"links":[{"id":210822,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.coal.2005.02.003"},{"id":237856,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"63","issue":"1-2 SPEC. ISS.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059eda2e4b0c8380cd498fe","contributors":{"authors":[{"text":"Ruppert, L.F. 0000-0003-4990-0539","orcid":"https://orcid.org/0000-0003-4990-0539","contributorId":59043,"corporation":false,"usgs":true,"family":"Ruppert","given":"L.F.","affiliations":[],"preferred":false,"id":423206,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hower, J.C.","contributorId":100541,"corporation":false,"usgs":true,"family":"Hower","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":423207,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eble, C.F.","contributorId":35346,"corporation":false,"usgs":true,"family":"Eble","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":423205,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029548,"text":"70029548 - 2005 - Time-dependent earthquake probabilities","interactions":[],"lastModifiedDate":"2012-03-12T17:20:53","indexId":"70029548","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Time-dependent earthquake probabilities","docAbstract":"We have attempted to provide a careful examination of a class of approaches for estimating the conditional probability of failure of a single large earthquake, particularly approaches that account for static stress perturbations to tectonic loading as in the approaches of Stein et al. (1997) and Hardebeck (2004). We have loading as in the framework based on a simple, generalized rate change formulation and applied it to these two approaches to show how they relate to one another. We also have attempted to show the connection between models of seismicity rate changes applied to (1) populations of independent faults as in background and aftershock seismicity and (2) changes in estimates of the conditional probability of failures of different members of a the notion of failure rate corresponds to successive failures of different members of a population of faults. The latter application requires specification of some probability distribution (density function of PDF) that describes some population of potential recurrence times. This PDF may reflect our imperfect knowledge of when past earthquakes have occurred on a fault (epistemic uncertainty), the true natural variability in failure times, or some combination of both. We suggest two end-member conceptual single-fault models that may explain natural variability in recurrence times and suggest how they might be distinguished observationally. When viewed deterministically, these single-fault patch models differ significantly in their physical attributes, and when faults are immature, they differ in their responses to stress perturbations. Estimates of conditional failure probabilities effectively integrate over a range of possible deterministic fault models, usually with ranges that correspond to mature faults. Thus conditional failure probability estimates usually should not differ significantly for these models. Copyright 2005 by the American Geophysical Union.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research B: Solid Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2004JB003405","issn":"01480227","usgsCitation":"Gomberg, J., Belardinelli, M., Cocco, M., and Reasenberg, P., 2005, Time-dependent earthquake probabilities: Journal of Geophysical Research B: Solid Earth, v. 110, no. 5, p. 1-12, https://doi.org/10.1029/2004JB003405.","startPage":"1","endPage":"12","numberOfPages":"12","costCenters":[],"links":[{"id":210461,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2004JB003405"},{"id":237385,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"110","issue":"5","noUsgsAuthors":false,"publicationDate":"2005-05-07","publicationStatus":"PW","scienceBaseUri":"505bb3b9e4b08c986b325f84","contributors":{"authors":[{"text":"Gomberg, J.","contributorId":95994,"corporation":false,"usgs":true,"family":"Gomberg","given":"J.","email":"","affiliations":[],"preferred":false,"id":423235,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Belardinelli, M.E.","contributorId":107464,"corporation":false,"usgs":true,"family":"Belardinelli","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":423236,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cocco, M.","contributorId":70128,"corporation":false,"usgs":true,"family":"Cocco","given":"M.","email":"","affiliations":[],"preferred":false,"id":423234,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Reasenberg, P.","contributorId":22913,"corporation":false,"usgs":true,"family":"Reasenberg","given":"P.","email":"","affiliations":[],"preferred":false,"id":423233,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70029550,"text":"70029550 - 2005 - Groundwater recharge and sustainability in the High Plains aquifer in Kansas, USA","interactions":[],"lastModifiedDate":"2012-03-12T17:20:53","indexId":"70029550","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1923,"text":"Hydrogeology Journal","active":true,"publicationSubtype":{"id":10}},"title":"Groundwater recharge and sustainability in the High Plains aquifer in Kansas, USA","docAbstract":"Sustainable use of groundwater must ensure not only that the future resource is not threatened by overuse, but also that natural environments that depend on the resource, such as stream baseflows, riparian vegetation, aquatic ecosystems, and wetlands are protected. To properly manage groundwater resources, accurate information about the inputs (recharge) and outputs (pumpage and natural discharge) within each groundwater basin is needed so that the long-term behavior of the aquifer and its sustainable yield can be estimated or reassessed. As a first step towards this effort, this work highlights some key groundwater recharge studies in the Kansas High Plains at different scales, such as regional soil-water budget and groundwater modeling studies, county-scale groundwater recharge studies, as well as field-experimental local studies, including some original new findings, with an emphasis on assumptions and limitations as well as on environmental factors affecting recharge processes. The general impact of irrigation and cultivation on recharge is to appreciably increase the amount of recharge, and in many cases to exceed precipitation as the predominant source of recharge. The imbalance between the water input (recharge) to the High Plains aquifer and the output (pumpage and stream baseflows primarily) is shown to be severe, and responses to stabilize the system by reducing water use, increasing irrigation efficiency, adopting water-saving land-use practices, and other measures are outlined. Finally, the basic steps necessary to move towards sustainable use of groundwater in the High Plains are delineated, such as improving the knowledge base, reporting and providing access to information, furthering public education, as well as promoting better understanding of the public's attitudinal motivations; adopting the ecosystem and adaptive management approaches to managing groundwater; further improving water efficiency; exploiting the full potential of dryland and biosaline agriculture; and adopting a goal of long-term sustainable use. ?? Springer-Verlag 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hydrogeology Journal","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10040-004-0385-6","issn":"14312174","usgsCitation":"Sophocleous, M., 2005, Groundwater recharge and sustainability in the High Plains aquifer in Kansas, USA: Hydrogeology Journal, v. 13, no. 2, p. 351-365, https://doi.org/10.1007/s10040-004-0385-6.","startPage":"351","endPage":"365","numberOfPages":"15","costCenters":[],"links":[{"id":210488,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10040-004-0385-6"},{"id":237422,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"2","noUsgsAuthors":false,"publicationDate":"2005-01-14","publicationStatus":"PW","scienceBaseUri":"505a2dbee4b0c8380cd5bfea","contributors":{"authors":[{"text":"Sophocleous, M.","contributorId":13373,"corporation":false,"usgs":true,"family":"Sophocleous","given":"M.","email":"","affiliations":[],"preferred":false,"id":423242,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70029551,"text":"70029551 - 2005 - Waveform tomography of crustal structure in the south San Francisco Bay region","interactions":[],"lastModifiedDate":"2012-03-12T17:20:53","indexId":"70029551","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Waveform tomography of crustal structure in the south San Francisco Bay region","docAbstract":"We utilize a scattering-based seismic tomography technique to constrain crustal tructure around the southern San Francisco Bay region (SFBR). This technique is based on coupled traveling wave scattering theory, which has usually been applied to the interpretation of surface waves in large regional-scale studies. Using fully three-dimensional kernels, this technique is here applied to observed P, S, and surface waves of intermediate period (3-4 s dominant period) observed following eight selected regional events. We use a total of 73 seismograms recorded by a U.S. Geological Survey short-period seismic array in the western Santa Clara Valley, the Berkeley Digital Seismic Network, and the Northern California Seismic Network. Modifications of observed waveforms due to scattering from crustal structure include (positive or negative) amplification, delay, and generation of coda waves. The derived crustal structure explains many of the observed signals which cannot be explained with a simple layered structure. There is sufficient sensitivity to both deep and shallow crustal structure that even with the few sources employed in the present study, we obtain shallow velocity structure which is reasonably consistent with previous P wave tomography results. We find a depth-dependent lateral velocity contrast across the San Andreas fault (SAF), with higher velocities southwest of the SAF in the shallow crust and higher velocities northeast of the SAF in the midcrust. The method does not have the resolution to identify very slow sediment velocities in the upper approximately 3 km since the tomographic models are smooth at a vertical scale of about 5 km. Copyright 2005 by the American Geophysical Union.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research B: Solid Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2004JB003509","issn":"01480227","usgsCitation":"Pollitz, F., and Fletcher, J., 2005, Waveform tomography of crustal structure in the south San Francisco Bay region: Journal of Geophysical Research B: Solid Earth, v. 110, no. 8, p. 1-37, https://doi.org/10.1029/2004JB003509.","startPage":"1","endPage":"37","numberOfPages":"37","costCenters":[],"links":[{"id":478018,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2004jb003509","text":"Publisher Index Page"},{"id":210489,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2004JB003509"},{"id":237423,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"110","issue":"8","noUsgsAuthors":false,"publicationDate":"2005-08-16","publicationStatus":"PW","scienceBaseUri":"505bcfa2e4b08c986b32ea00","contributors":{"authors":[{"text":"Pollitz, F. F.","contributorId":108280,"corporation":false,"usgs":true,"family":"Pollitz","given":"F. F.","affiliations":[],"preferred":false,"id":423244,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fletcher, J.P.","contributorId":44540,"corporation":false,"usgs":true,"family":"Fletcher","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":423243,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029553,"text":"70029553 - 2005 - Survival and selection of migrating salmon from capture-recapture models with individual traits","interactions":[],"lastModifiedDate":"2021-07-02T16:35:04.572632","indexId":"70029553","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1450,"text":"Ecological Applications","active":true,"publicationSubtype":{"id":10}},"title":"Survival and selection of migrating salmon from capture-recapture models with individual traits","docAbstract":"Capture–recapture studies are powerful tools for studying animal population dynamics, providing information on population abundance, survival rates, population growth rates, and selection for phenotypic traits. In these studies, the probability of observing a tagged individual reflects both the probability of the individual surviving to the time of recapture and the probability of recapturing an animal, given that it is alive. If both of these probabilities are related to the same phenotypic trait, it can be difficult to distinguish effects on survival probabilities from effects on recapture probabilities. However, when animals are individually tagged and have multiple opportunities for recapture, we can properly partition observed trait-related variability into survival and recapture components. We present an overview of capture–recapture models that incorporate individual variability and develop methods to incorporate results from these models into estimates of population survival and selection for phenotypic traits. We conducted a series of simulations to understand the performance of these estimators and to assess the consequences of ignoring individual variability when it exists. In addition, we analyzed a large data set of >153 000 juvenile chinook salmon (Oncorhynchus tshawytscha) and steelhead (O. mykiss) of known length that were PIT-tagged during their seaward migration. Both our simulations and the case study indicated that the ability to precisely estimate selection for phenotypic traits was greatly compromised when differential recapture probabilities were ignored. Estimates of population survival, however, were far more robust. In the chinook salmon and steelhead study, we consistently found that smaller fish had a greater probability of recapture. We also uncovered length-related survival relationships in over half of the release group/river segment combinations that we observed, but we found both positive and negative relationships between length and survival probability. These results have important implications for the management of salmonid populations.
","language":"English","publisher":"Ecological Society of America","doi":"10.1890/04-0940","usgsCitation":"Zabel, R., Wagner, T., Congleton, J., Smith, S.G., and Williams, J.G., 2005, Survival and selection of migrating salmon from capture-recapture models with individual traits: Ecological Applications, v. 15, no. 4, p. 1427-1439, https://doi.org/10.1890/04-0940.","productDescription":"13 p.","startPage":"1427","endPage":"1439","numberOfPages":"13","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":237457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba2b9e4b08c986b31f8f5","contributors":{"authors":[{"text":"Zabel, Richard","contributorId":219280,"corporation":false,"usgs":false,"family":"Zabel","given":"Richard","affiliations":[{"id":39987,"text":"Western Forestry and Conservation Association, Portland, OR","active":true,"usgs":false}],"preferred":false,"id":423256,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wagner, Tyler 0000-0003-1726-016X twagner@usgs.gov","orcid":"https://orcid.org/0000-0003-1726-016X","contributorId":1050,"corporation":false,"usgs":true,"family":"Wagner","given":"Tyler","email":"twagner@usgs.gov","affiliations":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"preferred":true,"id":423252,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Congleton, James","contributorId":100239,"corporation":false,"usgs":true,"family":"Congleton","given":"James","email":"","affiliations":[],"preferred":false,"id":423254,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, Steven G. sgsmith@usgs.gov","contributorId":1560,"corporation":false,"usgs":true,"family":"Smith","given":"Steven","email":"sgsmith@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":423255,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Williams, John G.","contributorId":10270,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":423253,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029555,"text":"70029555 - 2005 - The World Coal Quality Inventory: A status report","interactions":[],"lastModifiedDate":"2012-03-12T17:20:53","indexId":"70029555","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2033,"text":"International Journal of Coal Geology","active":true,"publicationSubtype":{"id":10}},"title":"The World Coal Quality Inventory: A status report","docAbstract":"National and international policy makers and industry require accurate information on coal, including coal quality data, to make informed decisions regarding international import needs and export opportunities, foreign policy, technology transfer policies, foreign investment prospects, environmental and health assessments, and byproduct use and disposal issues. Unfortunately, the information needed is generally proprietary and does not exist in the public domain. The U.S. Geological Survey (USGS), in conjunction with partners in about 60 countries, is developing a digital compilation of worldwide coal quality. The World Coal Quality Inventory (WoCQI) will contain coal quality information for samples obtained from major coal beds in countries having significant coal production, as well as from many countries producing smaller volumes of coal, with an emphasis on coals currently being burned. The information that will be incorporated includes, but is not limited to, proximate and ultimate analyses; sulfur-form data; major, minor, and trace element analysis; and semi-quantitative analyses of minerals, modes of occurrence, and petrography. The coal quality information will eventually be linked to a Geographic Information System (GIS) that shows the coal basins and sample locations along with geologic, land use, transportation, industrial, and cultural information. The WoCQI will be accessible on the USGS web page and new data added periodically. This multi-national collaboration is developing global coal quality data that contain a broad array of technologic, economic, and environmental parameters, which should help to ensure the efficient and environmentally compatible use of global coal resources in the 21st century.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"International Journal of Coal Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.coal.2005.02.013","issn":"01665162","usgsCitation":"Tewalt, S., Willett, J., and Finkelman, R.B., 2005, The World Coal Quality Inventory: A status report: International Journal of Coal Geology, v. 63, no. 1-2 SPEC. ISS., p. 190-194, https://doi.org/10.1016/j.coal.2005.02.013.","startPage":"190","endPage":"194","numberOfPages":"5","costCenters":[],"links":[{"id":210542,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.coal.2005.02.013"},{"id":237496,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"63","issue":"1-2 SPEC. ISS.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba98ae4b08c986b322328","contributors":{"authors":[{"text":"Tewalt, S.J.","contributorId":55838,"corporation":false,"usgs":true,"family":"Tewalt","given":"S.J.","affiliations":[],"preferred":false,"id":423261,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Willett, J.C.","contributorId":41858,"corporation":false,"usgs":true,"family":"Willett","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":423260,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Finkelman, R. B.","contributorId":20341,"corporation":false,"usgs":true,"family":"Finkelman","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":423259,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029560,"text":"70029560 - 2005 - Characterizing the spatial structure of endangered species habitat using geostatistical analysis of IKONOS imagery","interactions":[],"lastModifiedDate":"2020-08-27T19:45:55.250915","indexId":"70029560","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2068,"text":"International Journal of Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Characterizing the spatial structure of endangered species habitat using geostatistical analysis of IKONOS imagery","docAbstract":"Our study used geostatistics to extract measures that characterize the spatial structure of vegetated landscapes from satellite imagery for mapping endangered Sonoran pronghorn habitat. Fine spatial resolution IKONOS data provided information at the scale of individual trees or shrubs that permitted analysis of vegetation structure and pattern. We derived images of landscape structure by calculating local estimates of the nugget, sill, and range variogram parameters within 25 ?? 25-m image windows. These variogram parameters, which describe the spatial autocorrelation of the 1-m image pixels, are shown in previous studies to discriminate between different species-specific vegetation associations. We constructed two independent models of pronghorn landscape preference by coupling the derived measures with Sonoran pronghorn sighting data: a distribution-based model and a cluster-based model. The distribution-based model used the descriptive statistics for variogram measures at pronghorn sightings, whereas the cluster-based model used the distribution of pronghorn sightings within clusters of an unsupervised classification of derived images. Both models define similar landscapes, and validation results confirm they effectively predict the locations of an independent set of pronghorn sightings. Such information, although not a substitute for field-based knowledge of the landscape and associated ecological processes, can provide valuable reconnaissance information to guide natural resource management efforts.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/01430060500099394","usgsCitation":"Wallace, C., and Marsh, S., 2005, Characterizing the spatial structure of endangered species habitat using geostatistical analysis of IKONOS imagery: International Journal of Remote Sensing, v. 26, no. 12, p. 2607-2629, https://doi.org/10.1080/01430060500099394.","productDescription":"23 p.","startPage":"2607","endPage":"2629","numberOfPages":"23","costCenters":[{"id":570,"text":"Southwest Geographic Science Center","active":false,"usgs":true},{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"links":[{"id":237571,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Barry M. Goldwater Range","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.79089355468749,\n 32.35676318267808\n ],\n [\n -112.3626708984375,\n 32.35676318267808\n ],\n [\n -112.3626708984375,\n 33.073130945006625\n ],\n [\n -113.79089355468749,\n 33.073130945006625\n ],\n [\n -113.79089355468749,\n 32.35676318267808\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"26","issue":"12","noUsgsAuthors":false,"publicationDate":"2007-02-22","publicationStatus":"PW","scienceBaseUri":"5059f503e4b0c8380cd4c041","contributors":{"authors":[{"text":"Wallace, C.S.A.","contributorId":89712,"corporation":false,"usgs":true,"family":"Wallace","given":"C.S.A.","email":"","affiliations":[],"preferred":false,"id":423275,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marsh, S.E.","contributorId":70922,"corporation":false,"usgs":true,"family":"Marsh","given":"S.E.","email":"","affiliations":[],"preferred":false,"id":423274,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029561,"text":"70029561 - 2005 - Modeling duckweed growth in wastewater treatment systems","interactions":[],"lastModifiedDate":"2012-03-12T17:20:52","indexId":"70029561","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2627,"text":"Livestock Research for Rural Development","active":true,"publicationSubtype":{"id":10}},"title":"Modeling duckweed growth in wastewater treatment systems","docAbstract":"Species of the genera Lemnaceae, or duckweeds, are floating aquatic plants that show great promise for both wastewater treatment and livestock feed production. Research conducted in the Southern High Plains of Texas has shown that Lemna obscura grew well in cattle feedlot runoff water and produced leaf tissue with a high protein content. A model or mathematical expression derived from duckweed growth data was used to fit data from experiments conducted in a greenhouse in Lubbock, Texas. The relationship between duckweed growth and the total nitrogen concentration in the mediium follows the Mitscherlich Function and is similar to that of other plants. Empirically derived model equations have successfully predicted the growth response of Lemna obscura.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Livestock Research for Rural Development","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"01213784","usgsCitation":"Landesman, L., Parker, N., Fedler, C., and Konikoff, M., 2005, Modeling duckweed growth in wastewater treatment systems: Livestock Research for Rural Development, v. 17, no. 6.","costCenters":[],"links":[{"id":237572,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5bf1e4b0c8380cd6f903","contributors":{"authors":[{"text":"Landesman, L.","contributorId":13804,"corporation":false,"usgs":true,"family":"Landesman","given":"L.","email":"","affiliations":[],"preferred":false,"id":423276,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parker, N. C.","contributorId":101209,"corporation":false,"usgs":true,"family":"Parker","given":"N. C.","affiliations":[],"preferred":false,"id":423279,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fedler, C.B.","contributorId":49147,"corporation":false,"usgs":true,"family":"Fedler","given":"C.B.","email":"","affiliations":[],"preferred":false,"id":423278,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Konikoff, M.","contributorId":35111,"corporation":false,"usgs":true,"family":"Konikoff","given":"M.","email":"","affiliations":[],"preferred":false,"id":423277,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70029564,"text":"70029564 - 2005 - The spectral irradiance of the moon","interactions":[],"lastModifiedDate":"2012-03-12T17:20:52","indexId":"70029564","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":914,"text":"Astronomical Journal","active":true,"publicationSubtype":{"id":10}},"title":"The spectral irradiance of the moon","docAbstract":"Images of the Moon at 32 wavelengths from 350 to 2450 nm have been obtained from a dedicated observatory during the bright half of each month over a period of several years. The ultimate goal is to develop a spectral radiance model of the Moon with an angular resolution and radiometric accuracy appropriate for calibration of Earth-orbiting spacecraft. An empirical model of irradiance has been developed that treats phase and libration explicitly, with absolute scale founded on the spectra of the star Vega and returned Apollo samples. A selected set of 190 standard stars are observed regularly to provide nightly extinction correction and long-term calibration of the observations. The extinction model is wavelength-coupled and based on the absorption coefficients of a number of gases and aerosols. The empirical irradiance model has the same form at each wavelength, with 18 coefficients, eight of which are constant across wavelength, for a total of 328 coefficients. Over 1000 lunar observations are fitted at each wavelength; the average residual is less than 1%. The irradiance model is actively being used in lunar calibration of several spacecraft instruments and can track sensor response changes at the 0.1% level. ?? 2005. The American Astronomical Society. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Astronomical Journal","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1086/430185","issn":"00046256","usgsCitation":"Kieffer, H.H., and Stone, T., 2005, The spectral irradiance of the moon: Astronomical Journal, v. 129, no. 6, p. 2887-2901, https://doi.org/10.1086/430185.","startPage":"2887","endPage":"2901","numberOfPages":"15","costCenters":[],"links":[{"id":210631,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1086/430185"},{"id":237608,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"129","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb05be4b08c986b324df1","contributors":{"authors":[{"text":"Kieffer, H. H.","contributorId":40725,"corporation":false,"usgs":false,"family":"Kieffer","given":"H.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":423289,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stone, T.C.","contributorId":74874,"corporation":false,"usgs":true,"family":"Stone","given":"T.C.","email":"","affiliations":[],"preferred":false,"id":423290,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029568,"text":"70029568 - 2005 - Applying petrophysical models to radar travel time and electrical resistivity tomograms: Resolution-dependent limitations","interactions":[],"lastModifiedDate":"2019-10-16T17:06:14","indexId":"70029568","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Applying petrophysical models to radar travel time and electrical resistivity tomograms: Resolution-dependent limitations","docAbstract":"[1] Geophysical imaging has traditionally provided qualitative information about geologic structure; however, there is increasing interest in using petrophysical models to convert tomograms to quantitative estimates of hydrogeologic, mechanical, or geochemical parameters of interest (e.g., permeability, porosity, water content, and salinity). Unfortunately, petrophysical estimation based on tomograms is complicated by limited and variable image resolution, which depends on (1) measurement physics (e.g., electrical conduction or electromagnetic wave propagation), (2) parameterization and regularization, (3) measurement error, and (4) spatial variability. We present a framework to predict how core‐scale relations between geophysical properties and hydrologic parameters are altered by the inversion, which produces smoothly varying pixel‐scale estimates. We refer to this loss of information as “correlation loss.” Our approach upscales the core‐scale relation to the pixel scale using the model resolution matrix from the inversion, random field averaging, and spatial statistics of the geophysical property. Synthetic examples evaluate the utility of radar travel time tomography (RTT) and electrical‐resistivity tomography (ERT) for estimating water content. This work provides (1) a framework to assess tomograms for geologic parameter estimation and (2) insights into the different patterns of correlation loss for ERT and RTT. Whereas ERT generally performs better near boreholes, RTT performs better in the interwell region. Application of petrophysical models to the tomograms in our examples would yield misleading estimates of water content. Although the examples presented illustrate the problem of correlation loss in the context of near‐surface geophysical imaging, our results have clear implications for quantitative analysis of tomograms for diverse geoscience applications.
Tar yields from low-temperature carbonization correlate with the amount of crypto-eugelinite in samples selected to represent petrographically distinct coal facies of the Wyodak-Anderson coal zone. Tar yields from Fischer Assay range from <1 to 11 wt.% on a dry basis and correspond (r = 0.72) to crypto-eugelinite contents of the coal that range from 15 to 60 vol.%. Core and highwall samples were obtained from active surface mines in the Gillette field, Powder River Basin, Wyoming. Because the rank of the samples is essentially the same, differences in low-temperature carbonization yields are interpreted from compositional differences, particularly the crypto-eugelinite content. In the Wyodak-Anderson coal zone, crypto-eugelinite probably was derived from degraded humic matter which absorbed decomposition products from algae, fungi, bacteria, and liptinitic plant parts (materials possibly high in hydrogen). Previous modeling of the distribution of crypto-eugelinite in the discontinuous Wyodak-Anderson coal zone indicated that tar yields should be greater from coal composing the upper part and interior areas than from coal composing the lower parts and margins of the individual coal bodies. It is possible that hydrocarbon yields from natural coalification processes would be similar to yields obtained from laboratory pyrolysis. If so, the amount of crypto-eugelinite may also be an important characteristic when evaluating coal as source rock for migrated hydrocarbons.
","language":"English","publisher":"Elsevier","doi":"10.1016/j.coal.2005.02.002","usgsCitation":"Stanton, R.W., Warwick, P.D., and Swanson, S.M., 2005, Tar yields from low-temperature carbonization of coal facies from the Powder River Basin, Wyoming, USA: International Journal of Coal Geology, v. 63, no. 1-2, p. 13-26, https://doi.org/10.1016/j.coal.2005.02.002.","productDescription":"14 p.","startPage":"13","endPage":"26","costCenters":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":237715,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Powder River Basin","volume":"63","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba3e1e4b08c986b31ff59","contributors":{"authors":[{"text":"Stanton, Ronald W.","contributorId":37386,"corporation":false,"usgs":true,"family":"Stanton","given":"Ronald","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":423308,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Warwick, Peter D. 0000-0002-3152-7783 pwarwick@usgs.gov","orcid":"https://orcid.org/0000-0002-3152-7783","contributorId":762,"corporation":false,"usgs":true,"family":"Warwick","given":"Peter","email":"pwarwick@usgs.gov","middleInitial":"D.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":423310,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Swanson, Sharon M. 0000-0002-4235-1736 smswanson@usgs.gov","orcid":"https://orcid.org/0000-0002-4235-1736","contributorId":590,"corporation":false,"usgs":true,"family":"Swanson","given":"Sharon","email":"smswanson@usgs.gov","middleInitial":"M.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":423309,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029578,"text":"70029578 - 2005 - Real-time forecasts of tomorrow's earthquakes in California","interactions":[],"lastModifiedDate":"2012-03-12T17:20:47","indexId":"70029578","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Real-time forecasts of tomorrow's earthquakes in California","docAbstract":"Despite a lack of reliable deterministic earthquake precursors, seismologists have significant predictive information about earthquake activity from an increasingly accurate understanding of the clustering properties of earthquakes. In the past 15 years, time-dependent earthquake probabilities based on a generic short-term clustering model have been made publicly available in near-real time during major earthquake sequences. These forecasts describe the probability and number of events that are, on average, likely to occur following a mainshock of a given magnitude, but are not tailored to the particular sequence at hand and contain no information about the likely locations of the aftershocks. Our model builds upon the basic principles of this generic forecast model in two ways: it recasts the forecast in terms of the probability of strong ground shaking, and it combines an existing time-independent earthquake occurrence model based on fault data and historical earthquakes with increasingly complex models describing the local time-dependent earthquake clustering. The result is a time-dependent map showing the probability of strong shaking anywhere in California within the next 24 hours. The seismic hazard modelling approach we describe provides a better understanding of time-dependent earthquake hazard, and increases its usefulness for the public, emergency planners and the media.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Nature","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1038/nature03622","issn":"00280836","usgsCitation":"Gerstenberger, M., Wiemer, S., Jones, L., and Reasenberg, P., 2005, Real-time forecasts of tomorrow's earthquakes in California: Nature, v. 435, no. 7040, p. 328-331, https://doi.org/10.1038/nature03622.","startPage":"328","endPage":"331","numberOfPages":"4","costCenters":[],"links":[{"id":210797,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1038/nature03622"},{"id":237823,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"435","issue":"7040","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a95a1e4b0c8380cd81b36","contributors":{"authors":[{"text":"Gerstenberger, M.C.","contributorId":51977,"corporation":false,"usgs":true,"family":"Gerstenberger","given":"M.C.","email":"","affiliations":[],"preferred":false,"id":423328,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wiemer, S.","contributorId":22115,"corporation":false,"usgs":true,"family":"Wiemer","given":"S.","affiliations":[],"preferred":false,"id":423327,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jones, L.M.","contributorId":61433,"corporation":false,"usgs":true,"family":"Jones","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":423329,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Reasenberg, P.A.","contributorId":19959,"corporation":false,"usgs":true,"family":"Reasenberg","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":423326,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70029581,"text":"70029581 - 2005 - Near-infrared (0.8-4.0 m) spectroscopy of mimas, enceladus, tethys, and rhea","interactions":[],"lastModifiedDate":"2015-05-04T13:35:11","indexId":"70029581","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":915,"text":"Astronomy and Astrophysics","active":true,"publicationSubtype":{"id":10}},"title":"Near-infrared (0.8-4.0 m) spectroscopy of mimas, enceladus, tethys, and rhea","docAbstract":"Spectral measurements from the ground in the time leading up to the Cassini mission at Saturn provide important context for the interpretation of the forthcoming spacecraft data. Whereas ground-based observations cannot begin to approach the spatial scales Cassini will achieve, they do possess the benefits of better spectral resolution, a broader possible time baseline, and unique veiewing geometries not obtained by spacecraft (i.e., opposition). In this spirit, we present recent NIR reflectance spectra of four icy satellites of Saturn measured with the SpeX instrument at the IRTF. These measurements cover the range 0.8-4.0 ![\"$\\mu$\"](\"http://www.aanda.org/articles/aa/abs/2005/19/aa2482-04/img2.gif\")
m of both the leading and trailing sides of Tethys and the leading side of Rhea. The L-band region (2.8-4.0 m) offers new opportunities for searches of minor components on these objects. Additionally, these data include 0.8-2.5 m spectra of both the leading and trailing sides of Mimas and of the (mostly) trailing side of Enceladus. The spectrum of Enceladus shows activity near 2.25 m that we interpret as a possible signature of NH3 ice. The presence of ammonia in the Saturn system is not unexpected, and may help explain the apparent recent geologic activity of Enceladus. Analysis of leading/trailing differences inH2O band depths, spectral slopes, and albedo imply a separate regime of surface modification for Mimas and Enceladus than for the more distant icy satellites (Tethys, Dione, Rhea). Aside from the potential NH3 on Enceladus, no other minor constituents are detected in these icy surfaces.
","language":"English","publisher":"EDP Sciences","doi":"10.1051/0004-6361:20042482","issn":"00046361","usgsCitation":"Emery, J., Burr, D., Cruikshank, D.P., Brown, R.H., and Dalton, J., 2005, Near-infrared (0.8-4.0 m) spectroscopy of mimas, enceladus, tethys, and rhea: Astronomy and Astrophysics, v. 435, no. 1, p. 353-362, https://doi.org/10.1051/0004-6361:20042482.","productDescription":"10 p.","startPage":"353","endPage":"362","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":477905,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1051/0004-6361:20042482","text":"Publisher Index Page"},{"id":237858,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210824,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1051/0004-6361:20042482"}],"volume":"435","issue":"1","noUsgsAuthors":false,"publicationDate":"2005-04-25","publicationStatus":"PW","scienceBaseUri":"505a63f9e4b0c8380cd727cf","contributors":{"authors":[{"text":"Emery, J.P.","contributorId":8669,"corporation":false,"usgs":true,"family":"Emery","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":423335,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burr, D.M.","contributorId":60420,"corporation":false,"usgs":true,"family":"Burr","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":423338,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cruikshank, D. P.","contributorId":51434,"corporation":false,"usgs":false,"family":"Cruikshank","given":"D.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":423337,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brown, R. H.","contributorId":19931,"corporation":false,"usgs":false,"family":"Brown","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":423336,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dalton, J.B.","contributorId":77251,"corporation":false,"usgs":true,"family":"Dalton","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":423339,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029582,"text":"70029582 - 2005 - Transient rheology of the upper mantle beneath central Alaska inferred from the crustal velocity field following the 2002 Denali earthquake","interactions":[],"lastModifiedDate":"2012-03-12T17:20:47","indexId":"70029582","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Transient rheology of the upper mantle beneath central Alaska inferred from the crustal velocity field following the 2002 Denali earthquake","docAbstract":"The M7.9 2002 Denali earthquake, Alaska, is one of the largest strike-slip earthquakes ever recorded. The postseismic GPS velocity field around the 300-km-long rupture is characterized by very rapid horizontal velocity up to ???300 mm/yr for the first 0.1 years and slower but still elevated horizontal velocity up to ???100 mm/yr for the succeeding 1.5 years. I find that the spatial and temporal pattern of the displacement field may be explained by a transient mantle rheology. Representing the regional upper mantle as a Burghers body, I infer steady state and transient viscosities of ??1 = 2.8 ?? 1018 Pa s and ??2 = 1.0 ?? 1017 Pa s, respectively, corresponding to material relaxation times of 1.3 and 0.05 years. The lower crustal viscosity is poorly constrained by the considered horizontal velocity field, and the quoted mantle viscosities assume a steady state lower crust viscosity that is 7??1. Systematic bias in predicted versus observed velocity vectors with respect to a fixed North America during the first 3-6 months following the earthquake is reduced when all velocity vectors are referred to a fixed site. This suggests that the post-Denali GPS time series for the first 1.63 years are shaped by a combination of a common mode noise source during the first 3-6 months plus viscoelastic relaxation controlled by a transient mantle rheology.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research B: Solid Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2005JB003672","issn":"01480227","usgsCitation":"Pollitz, F., 2005, Transient rheology of the upper mantle beneath central Alaska inferred from the crustal velocity field following the 2002 Denali earthquake: Journal of Geophysical Research B: Solid Earth, v. 110, no. 8, p. 1-16, https://doi.org/10.1029/2005JB003672.","startPage":"1","endPage":"16","numberOfPages":"16","costCenters":[],"links":[{"id":210850,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2005JB003672"},{"id":237894,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"110","issue":"8","noUsgsAuthors":false,"publicationDate":"2005-08-16","publicationStatus":"PW","scienceBaseUri":"505bb702e4b08c986b326fde","contributors":{"authors":[{"text":"Pollitz, F. F.","contributorId":108280,"corporation":false,"usgs":true,"family":"Pollitz","given":"F. F.","affiliations":[],"preferred":false,"id":423340,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70029584,"text":"70029584 - 2005 - Nutritional condition of elk in rocky mountain national park","interactions":[],"lastModifiedDate":"2012-03-12T17:20:46","indexId":"70029584","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3746,"text":"Western North American Naturalist","onlineIssn":"1944-8341","printIssn":"1527-0904","active":true,"publicationSubtype":{"id":10}},"title":"Nutritional condition of elk in rocky mountain national park","docAbstract":"We tested the hypothesis that elk in Rocky Mountain National Park (RMNP) were at ecological carrying capacity by determining herd-specific levels of nutritional condition and fecundity. Ingesta-free body fat levels in adult cows that were lactating were 10.6% (s = 1.7; range = 6.2-15.4) and 7.7% (s = 0.5; range = 5.9-10.1) in November 2001 for the Horseshoe and Moraine Park herds, respectively. Cows that were not lactating were able to accrue significantly more body fat: 14.0% (s = 1.1; range = 7.7-19.3) and 11.5% (s = 0.8; range = 8.6-15.1) for the Horseshoe and Moraine Park herds, respectively. Cow elk lost most of their body fat over winter (April 2002 levels were 3.9% [s = 0.4] and 2.9% [s = 0.4] for the Horseshoe and Moraine Park herds, respectively). Nutritional condition indicated that both Horseshoe Park and Moraine Park elk were well below condition levels elk can achieve on very good-excellent nutrition (i.e., >15% body fat; Cook et al. 2004) and were comparable to other free-ranging elk populations. However, condition levels were higher than those expected at a \"food-limited\" carrying capacity, and a proportion of elk in each herd were able to achieve condition levels indicative of very good-excellent nutrition. Elk in RMNP are likely regulated and/or limited by a complex combination of density-independent (including significant heterogeneity in forage conditions across RMNP's landscape) and density-dependent processes, as condition levels contradict a simple density-dependent model of a population at ecological carrying capacity.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Western North American Naturalist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"15270904","usgsCitation":"Bender, L.C., and Cook, J., 2005, Nutritional condition of elk in rocky mountain national park: Western North American Naturalist, v. 65, no. 3, p. 329-334.","startPage":"329","endPage":"334","numberOfPages":"6","costCenters":[],"links":[{"id":237930,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"65","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a69d5e4b0c8380cd73eff","contributors":{"authors":[{"text":"Bender, Louis C.","contributorId":72509,"corporation":false,"usgs":true,"family":"Bender","given":"Louis","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":423343,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cook, J.G.","contributorId":75885,"corporation":false,"usgs":true,"family":"Cook","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":423344,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029587,"text":"70029587 - 2005 - Species abundance in a forest community in South China: A case of poisson lognormal distribution","interactions":[],"lastModifiedDate":"2017-08-31T12:42:32","indexId":"70029587","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2358,"text":"Journal of Integrative Plant Biology","active":true,"publicationSubtype":{"id":10}},"title":"Species abundance in a forest community in South China: A case of poisson lognormal distribution","docAbstract":"Case studies on Poisson lognormal distribution of species abundance have been rare, especially in forest communities. We propose a numerical method to fit the Poisson lognormal to the species abundance data at an evergreen mixed forest in the Dinghushan Biosphere Reserve, South China. Plants in the tree, shrub and herb layers in 25 quadrats of 20 m??20 m, 5 m??5 m, and 1 m??1 m were surveyed. Results indicated that: (i) for each layer, the observed species abundance with a similarly small median, mode, and a variance larger than the mean was reverse J-shaped and followed well the zero-truncated Poisson lognormal; (ii) the coefficient of variation, skewness and kurtosis of abundance, and two Poisson lognormal parameters (?? and ??) for shrub layer were closer to those for the herb layer than those for the tree layer; and (iii) from the tree to the shrub to the herb layer, the ?? and the coefficient of variation decreased, whereas diversity increased. We suggest that: (i) the species abundance distributions in the three layers reflects the overall community characteristics; (ii) the Poisson lognormal can describe the species abundance distribution in diverse communities with a few abundant species but many rare species; and (iii) 1/?? should be an alternative measure of diversity.","language":"English","publisher":"Wiley","doi":"10.1111/j.1744-7909.2005.00095.x","issn":"16729072","usgsCitation":"Yin, Z., Ren, H., Zhang, Q., Peng, S., Guo, Q., and Zhou, G., 2005, Species abundance in a forest community in South China: A case of poisson lognormal distribution: Journal of Integrative Plant Biology, v. 47, no. 7, p. 801-810, https://doi.org/10.1111/j.1744-7909.2005.00095.x.","productDescription":"10 p.","startPage":"801","endPage":"810","numberOfPages":"10","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":477968,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.572.7351","text":"External Repository"},{"id":237387,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210462,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1744-7909.2005.00095.x"}],"volume":"47","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b94f0e4b08c986b31accc","contributors":{"authors":[{"text":"Yin, Z.-Y.","contributorId":8278,"corporation":false,"usgs":true,"family":"Yin","given":"Z.-Y.","email":"","affiliations":[],"preferred":false,"id":423351,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ren, H.","contributorId":45273,"corporation":false,"usgs":true,"family":"Ren","given":"H.","email":"","affiliations":[],"preferred":false,"id":423354,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zhang, Q.-M.","contributorId":31190,"corporation":false,"usgs":true,"family":"Zhang","given":"Q.-M.","email":"","affiliations":[],"preferred":false,"id":423352,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Peng, S.-L.","contributorId":85762,"corporation":false,"usgs":true,"family":"Peng","given":"S.-L.","email":"","affiliations":[],"preferred":false,"id":423356,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Guo, Q.-F.","contributorId":74180,"corporation":false,"usgs":true,"family":"Guo","given":"Q.-F.","email":"","affiliations":[],"preferred":false,"id":423355,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Zhou, G.-Y.","contributorId":37522,"corporation":false,"usgs":true,"family":"Zhou","given":"G.-Y.","affiliations":[],"preferred":false,"id":423353,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70029589,"text":"70029589 - 2005 - Environmental impacts of oil production on soil, bedrock, and vegetation at the U.S. Geological Survey Osage-Skiatook Petroleum Environmental Research site A, Osage County, Oklahoma","interactions":[],"lastModifiedDate":"2018-10-31T09:59:49","indexId":"70029589","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1541,"text":"Environmental Geosciences","active":true,"publicationSubtype":{"id":10}},"title":"Environmental impacts of oil production on soil, bedrock, and vegetation at the U.S. Geological Survey Osage-Skiatook Petroleum Environmental Research site A, Osage County, Oklahoma","docAbstract":"The U.S. Geological Survey is investigating the impacts of oil and gas production on soils, groundwater, surface water, and ecosystems in the United States. Two sites in northeastern Oklahoma (sites A and B) are presently being investigated under the Osage–Skiatook Petroleum Environmental Research project. Oil wells on the lease surrounding site A in Osage County, Oklahoma, produced about 100,000 bbl of oil between 1913 and 1981. Prominent production features on the 1.5-ha (3.7-ac) site A include a tank battery, an oil-filled trench, pipelines, storage pits for both produced water and oil, and an old power unit. Site activities and historic releases have left open areas in the local oak forest adjacent to these features and a deeply eroded salt scar downslope from the pits that extends to nearby Skiatook Lake. The site is underlain by surficial sediments comprised of very fine-grained eolian sand and colluvium as much as 1.4 m (4.6 ft) thick, which, in turn, overlie flat-lying, fractured bedrock comprised of sandstone, clayey sandstone, mudstone, and shale. A geophysical survey of ground conductance and concentration measurements of aqueous extracts (1:1 by weight) of core samples taken in the salt scar and adjacent areas indicate that unusual concentrations of NaCl-rich salt are present at depths to at least 8 m (26 ft) in the bedrock; however, little salt occurs in the eolian sand. Historic aerial photographs, anecdotal reports from oil-lease operators, and tree-ring records indicate that the surrounding oak forest was largely established after 1935 and thus postdates the majority of surface damage at the site. Blackjack oaks adjacent to the salt scar have anomalously elevated chloride (![\"gt\"](\"http://archives.datapages.com/data/deg/2005/EG04030/IMAGES/GT.JPG\")
400 ppm) in their leaves and record the presence of NaCl-rich salt or salty water in the shallow subsurface. The geophysical measurements also indicate moderately elevated conductance beneath the oak forest adjoining the salt scar.
","language":"English","publisher":"AAPG","doi":"10.1306/eg.09280404030","issn":"10759565","usgsCitation":"Otton, J.K., Zielinski, R.A., Smith, B.D., Abbott, M., and Keeland, B.D., 2005, Environmental impacts of oil production on soil, bedrock, and vegetation at the U.S. Geological Survey Osage-Skiatook Petroleum Environmental Research site A, Osage County, Oklahoma: Environmental Geosciences, v. 12, no. 2, p. 73-87, https://doi.org/10.1306/eg.09280404030.","productDescription":"15 p.","startPage":"73","endPage":"87","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":210490,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1306/eg.09280404030"},{"id":237424,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oklahoma","county":"Osage County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-96.0004,37.0002],[-95.9999,36.7735],[-95.9996,36.7654],[-95.9999,36.6864],[-96.0002,36.6792],[-96,36.5122],[-96.0003,36.5059],[-96,36.4255],[-96.0003,36.4201],[-96.0001,36.2509],[-95.9996,36.1632],[-95.9997,36.1601],[-96.0755,36.161],[-96.0852,36.1608],[-96.1832,36.1618],[-96.2003,36.1627],[-96.2659,36.1628],[-96.2756,36.1631],[-96.2745,36.1757],[-96.2692,36.182],[-96.2621,36.1873],[-96.2563,36.1912],[-96.2504,36.197],[-96.2474,36.2014],[-96.2466,36.2055],[-96.2485,36.216],[-96.2545,36.2238],[-96.2601,36.2267],[-96.2652,36.2282],[-96.2715,36.2288],[-96.2777,36.2289],[-96.2828,36.2299],[-96.2913,36.2315],[-96.2976,36.2321],[-96.3073,36.2318],[-96.309,36.2319],[-96.3131,36.2306],[-96.3205,36.229],[-96.3257,36.2286],[-96.3365,36.2289],[-96.3444,36.2318],[-96.3589,36.2421],[-96.3671,36.2509],[-96.3753,36.261],[-96.3831,36.268],[-96.3926,36.2723],[-96.4051,36.2762],[-96.4232,36.2802],[-96.4317,36.2836],[-96.4383,36.2887],[-96.442,36.2974],[-96.4447,36.3043],[-96.4456,36.3106],[-96.4488,36.3171],[-96.4515,36.3217],[-96.4525,36.3253],[-96.4564,36.3281],[-96.4575,36.3299],[-96.4597,36.3314],[-96.4677,36.3329],[-96.4723,36.333],[-96.4809,36.33],[-96.4861,36.3287],[-96.4885,36.3265],[-96.4926,36.3234],[-96.4967,36.3181],[-96.5052,36.3055],[-96.5116,36.3016],[-96.5133,36.3007],[-96.5213,36.3],[-96.5242,36.2991],[-96.5271,36.2987],[-96.5488,36.2996],[-96.5573,36.3016],[-96.564,36.304],[-96.5697,36.3064],[-96.5735,36.311],[-96.5751,36.3161],[-96.5761,36.3197],[-96.5765,36.3247],[-96.5763,36.3315],[-96.5744,36.3364],[-96.5702,36.3436],[-96.5643,36.3485],[-96.5568,36.3511],[-96.5453,36.3535],[-96.5366,36.3566],[-96.5291,36.3596],[-96.5278,36.3623],[-96.5264,36.3713],[-96.5221,36.3803],[-96.5247,36.3881],[-96.528,36.3927],[-96.5392,36.4011],[-96.5478,36.3999],[-96.5594,36.3929],[-96.5659,36.388],[-96.5678,36.3812],[-96.5714,36.3759],[-96.5755,36.3741],[-96.5829,36.3738],[-96.5914,36.3772],[-96.5959,36.3791],[-96.6015,36.3833],[-96.6093,36.3898],[-96.6133,36.408],[-96.616,36.4112],[-96.6234,36.4137],[-96.6279,36.4156],[-96.635,36.4257],[-96.6441,36.4268],[-96.6493,36.4264],[-96.6534,36.4251],[-96.6585,36.4234],[-96.6637,36.4221],[-96.674,36.4237],[-96.6872,36.4235],[-96.718,36.4441],[-96.7236,36.4482],[-96.7205,36.4573],[-96.7196,36.4668],[-96.7143,36.4712],[-96.7142,36.493],[-96.7164,36.4971],[-96.7203,36.4995],[-96.7248,36.5014],[-96.7275,36.5064],[-96.728,36.5105],[-96.7284,36.515],[-96.7295,36.5187],[-96.7282,36.5241],[-96.7292,36.5291],[-96.7307,36.5337],[-96.7373,36.5456],[-96.7443,36.5571],[-96.7545,36.5631],[-96.7618,36.5669],[-96.7774,36.5645],[-96.7844,36.5605],[-96.7954,36.5566],[-96.8006,36.5545],[-96.81,36.5465],[-96.8146,36.5438],[-96.8223,36.5381],[-96.8281,36.5323],[-96.8317,36.5283],[-96.8371,36.5211],[-96.8425,36.5103],[-96.8469,36.4991],[-96.8599,36.4843],[-96.8669,36.4776],[-96.871,36.4741],[-96.8751,36.4719],[-96.8797,36.4711],[-96.8837,36.4711],[-96.89,36.4717],[-96.8928,36.4727],[-96.8986,36.4719],[-96.9044,36.4692],[-96.9084,36.4675],[-96.9142,36.4662],[-96.9199,36.4659],[-96.9234,36.465],[-96.9275,36.4606],[-96.9316,36.457],[-96.9385,36.4562],[-96.9561,36.4588],[-96.9663,36.4653],[-96.9748,36.4664],[-96.9822,36.4692],[-96.9906,36.4766],[-97.0012,36.4872],[-97.0057,36.4905],[-97.0112,36.4987],[-97.0116,36.506],[-97.0109,36.5105],[-97.0096,36.5155],[-97.0083,36.5204],[-97.0025,36.5249],[-96.9978,36.5275],[-96.9915,36.5292],[-96.988,36.531],[-96.9828,36.5327],[-96.977,36.5344],[-96.9667,36.5352],[-96.9564,36.535],[-96.9506,36.5367],[-96.946,36.538],[-96.939,36.5424],[-96.9355,36.5455],[-96.929,36.5513],[-96.9261,36.554],[-96.9243,36.554],[-96.9175,36.5529],[-96.906,36.5536],[-96.9003,36.554],[-96.8968,36.5553],[-96.8921,36.5597],[-96.8909,36.5634],[-96.8873,36.5683],[-96.8866,36.5732],[-96.8876,36.5792],[-96.8932,36.5824],[-96.9034,36.5867],[-96.9162,36.6001],[-96.9387,36.5959],[-96.9468,36.5911],[-96.9526,36.5889],[-96.9549,36.589],[-96.9612,36.5882],[-96.974,36.5843],[-96.982,36.583],[-96.986,36.5827],[-96.9952,36.5837],[-97.0032,36.5839],[-97.0153,36.5827],[-97.029,36.5847],[-97.0415,36.5858],[-97.0512,36.5883],[-97.0568,36.5929],[-97.055,36.5979],[-97.0532,36.601],[-97.0469,36.6018],[-97.0473,36.6054],[-97.049,36.6068],[-97.0547,36.6106],[-97.0551,36.6165],[-97.0528,36.6364],[-97.0617,36.651],[-97.0656,36.6547],[-97.067,36.6656],[-97.0666,36.6829],[-97.0606,36.6918],[-97.0548,36.6926],[-97.0491,36.6939],[-97.0253,36.7012],[-97.0238,36.6953],[-97.017,36.6907],[-97.0038,36.6909],[-96.994,36.6903],[-96.9878,36.6875],[-96.9682,36.6889],[-96.958,36.6865],[-96.9477,36.6836],[-96.9345,36.6852],[-96.9263,36.691],[-96.9262,36.6937],[-96.9267,36.6982],[-96.9254,36.7014],[-96.9206,36.7085],[-96.9204,36.7176],[-96.9151,36.7216],[-96.9061,36.7351],[-96.8907,36.7525],[-96.8786,36.7536],[-96.8689,36.7521],[-96.8604,36.7483],[-96.849,36.7445],[-96.8404,36.7434],[-96.8248,36.7472],[-96.8218,36.7531],[-96.821,36.7589],[-96.822,36.7662],[-96.8133,36.7665],[-96.8041,36.7663],[-96.7967,36.7662],[-96.7881,36.7661],[-96.7812,36.7664],[-96.7812,36.7832],[-96.7554,36.7831],[-96.7544,36.8344],[-96.7543,36.8389],[-96.7542,36.862],[-96.754,36.8675],[-96.7532,36.9998],[-96.5436,37.0008],[-96.5414,37.0008],[-96.5283,37.0008],[-96.3041,37.0006],[-96.2811,37.0006],[-96.2459,37.0005],[-96.2367,37.0007],[-96.1168,37.0007],[-96.0949,37.0003],[-96.0004,37.0002]]]},\"properties\":{\"name\":\"Osage\",\"state\":\"OK\"}}]}","volume":"12","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a09cfe4b0c8380cd52090","contributors":{"authors":[{"text":"Otton, J. K.","contributorId":52589,"corporation":false,"usgs":true,"family":"Otton","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":423365,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zielinski, R. A. 0000-0002-4047-5129","orcid":"https://orcid.org/0000-0002-4047-5129","contributorId":106930,"corporation":false,"usgs":true,"family":"Zielinski","given":"R.","email":"","middleInitial":"A.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":423368,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, B. D.","contributorId":71123,"corporation":false,"usgs":true,"family":"Smith","given":"B.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":423366,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Abbott, M.M.","contributorId":95431,"corporation":false,"usgs":true,"family":"Abbott","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":423367,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Keeland, B. D.","contributorId":45275,"corporation":false,"usgs":true,"family":"Keeland","given":"B.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":423364,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029591,"text":"70029591 - 2005 - Mineralogy and provenance of clays in miarolitic cavities of the Pikes Peak batholith, Colorado","interactions":[],"lastModifiedDate":"2021-06-11T13:40:11.791591","indexId":"70029591","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1177,"text":"Canadian Mineralogist","active":true,"publicationSubtype":{"id":10}},"title":"Mineralogy and provenance of clays in miarolitic cavities of the Pikes Peak batholith, Colorado","docAbstract":"Clay samples from 105 cavities within miarolitic granitic pegmatites throughout the Pikes Peak batholith, in Colorado, were analyzed by powder X-ray diffraction (XRD). Smectite (beidellite), illite, and kaolinite were found within the cavities. Calculation of crystallite-thickness distribution (CTD), mean thickness of the crystallites, and variance in crystallite thickness, as deduced from XRD patterns, allowed a determination of provenance and mode of formation for illite and smectite. Authigenic miarolitic-cavity illite and smectite show lognormal CTDs and larger mean thicknesses of crystallites than do their soil-derived counterparts; non-lognormal illite in a cavity results from mixing of cavity and soil illite. Analysis of mean thickness and thickness variance shows that crystal growth of illite is initiated by a nucleation event of short duration, followed by surface-controlled kinetics. Crystallization of the miarolitic cavity clays is presumed to occur by neoformation from hydrothermal fluids. The assessment of provenance allows a determination of regional and local distributions of clay minerals in miarolitic cavities within the Pikes Peak batholith.
","language":"English","publisher":"Mineralogical Association of Canada","doi":"10.2113/gscanmin.43.3.1093","usgsCitation":"Kile, D.E., 2005, Mineralogy and provenance of clays in miarolitic cavities of the Pikes Peak batholith, Colorado: Canadian Mineralogist, v. 43, no. 3, p. 1093-1105, https://doi.org/10.2113/gscanmin.43.3.1093.","productDescription":"13 p.","startPage":"1093","endPage":"1105","numberOfPages":"13","costCenters":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":237458,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Pikes Peak batholith","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.2652587890625,\n 38.47939467327645\n ],\n [\n -105.457763671875,\n 38.06971703320484\n ],\n [\n -104.8974609375,\n 38.39333888832238\n ],\n [\n -104.952392578125,\n 39.01491572891582\n ],\n [\n -105.18310546875,\n 39.740986355883564\n ],\n [\n -105.6610107421875,\n 39.871803651624425\n ],\n [\n -106.25976562499999,\n 39.92237576385941\n ],\n [\n -106.50146484374999,\n 39.787433886224406\n ],\n [\n -106.5618896484375,\n 39.41497702499074\n ],\n [\n -106.2652587890625,\n 38.47939467327645\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"43","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5ac6e4b0c8380cd6f109","contributors":{"authors":[{"text":"Kile, Daniel E. dekile@usgs.gov","contributorId":1286,"corporation":false,"usgs":true,"family":"Kile","given":"Daniel","email":"dekile@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":423373,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70029594,"text":"70029594 - 2005 - Stratigraphic and geochemical evolution of an oceanic arc upper crustal section: The Jurassic Talkeetna Volcanic Formation, south-central Alaska","interactions":[],"lastModifiedDate":"2012-03-12T17:20:53","indexId":"70029594","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Stratigraphic and geochemical evolution of an oceanic arc upper crustal section: The Jurassic Talkeetna Volcanic Formation, south-central Alaska","docAbstract":"The Early Jurassic Talkeetna Volcanic Formation forms the upper stratigraphic level of an oceanic volcanic arc complex within the Peninsular Terrane of south-central Alaska. The section comprises a series of lavas, tuffs, and volcaniclastic debris-How and flow turbidite deposits, showing significant lateral facies variability. There is a general trend toward more volcaniclastic sediment at the top of the section and more lavas and tuff breccias toward the base. Evidence for dominant submarine, mostly mid-bathyal or deeper (>500 m) emplacement is seen throughout the section, which totals ???7 km in thickness, similar to modern western Pacific arcs, and far more than any other known exposed section. Subaerial sedimentation was rare but occurred over short intervals in the middle of the section. The Talkeetna Volcanic Formation is dominantly calc-alkatine and shows no clear trend to increasing SiO2 up-section. An oceanic subduction petrogenesis is shown by trace element and Nd isotope data. Rocks at the base of the section show no relative enrichment of light rare earth elements (LREEs) versus heavy rare earth elements (REES) or in melt-incompatible versus compatible high field strength elements (HFSEs). Relative enrichment of LREEs and HFSEs increases slightly up-section. The Talkeetna Volcanic Formation is typically more REE depleted than average continental crust, although small volumes of light REE-enriched and heavy REE-depleted mafic lavas are recognized low in the stratigraphy. The Talkeetna Volcanic Formation was formed in an intraoceanic arc above a north-dipping subduction zone and contains no preserved record of its subsequent collisions with Wrangellia or North America. ?? 2005 Geological Society of America.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geological Society of America Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1130/B25638.1","issn":"00167606","usgsCitation":"Clift, P., Draut, A., Kelemen, P., Blusztajn, J., and Greene, A., 2005, Stratigraphic and geochemical evolution of an oceanic arc upper crustal section: The Jurassic Talkeetna Volcanic Formation, south-central Alaska: Geological Society of America Bulletin, v. 117, no. 7-8, p. 902-925, https://doi.org/10.1130/B25638.1.","startPage":"902","endPage":"925","numberOfPages":"24","costCenters":[],"links":[{"id":210543,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1130/B25638.1"},{"id":237498,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"117","issue":"7-8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b98c8e4b08c986b31c138","contributors":{"authors":[{"text":"Clift, P.D.","contributorId":100182,"corporation":false,"usgs":true,"family":"Clift","given":"P.D.","email":"","affiliations":[],"preferred":false,"id":423385,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Draut, A.E.","contributorId":50273,"corporation":false,"usgs":true,"family":"Draut","given":"A.E.","affiliations":[],"preferred":false,"id":423384,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kelemen, P.B.","contributorId":107034,"corporation":false,"usgs":true,"family":"Kelemen","given":"P.B.","email":"","affiliations":[],"preferred":false,"id":423386,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Blusztajn, J.","contributorId":16639,"corporation":false,"usgs":true,"family":"Blusztajn","given":"J.","email":"","affiliations":[],"preferred":false,"id":423382,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Greene, A.","contributorId":34711,"corporation":false,"usgs":true,"family":"Greene","given":"A.","email":"","affiliations":[],"preferred":false,"id":423383,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029595,"text":"70029595 - 2005 - Annual survival and site fidelity of northern pintails banded on the Yukon-Kuskokwim Delta, Alaska","interactions":[],"lastModifiedDate":"2016-06-29T16:20:05","indexId":"70029595","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Annual survival and site fidelity of northern pintails banded on the Yukon-Kuskokwim Delta, Alaska","docAbstract":"We banded northern pintails (Anas acuta; n = 13,645) at a single site on the Yukon-Kuskokwim Delta (YKD), Alaska, USA, from 1990 to 2001. We used recaptures from our site in combination with hunter recoveries to model annual survival, recovery rates, and fidelity to our capture location. Most recoveries (>90%) occurred in the Pacific Flyway with 64% reported from California's Central Valley. Our top candidate models allowed survival to vary by sex but not by age or year. Estimated annual survival was 77.6% (95% CI: 73.9-81.0%) for males and 60.2% (95% CI: 53.2-67.0%) for females. Reporting rates varied by age, sex, and year; estimates for adult males exceeded those for adult females by 3.5 times. Within sexes, reporting rates of hatch-year pintails exceeded those of adults. Estimated recovery rates were considerably lower than those estimated during the 1950s-1970s for winter banded pintails (Hestbeck 1993b), but there were no differences in survival rates. This suggests that changes in harvest regulations may not have influenced annual survival in this population. The propensity of banded pintails to return to our capture site (fidelity rate) varied between sexes and was positively correlated with water conditions in prairie Canada. Our estimates of fidelity rates varied from 77.4% to 87.2% for males and 89.8% to 94.3% for females. Our fidelity estimates suggest that some level of subpopulation structuring may exist for northern pintails. Additionally, our estimates of fidelity support previous observations of northern pintails overflying poor wetland habitat conditions on the Canadian prairies.
","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Wildlife Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Washington Wildlife Society","doi":"10.2193/0022-541X(2005)069[1202:ASASFO]2.0.CO;2","issn":"0022541X","usgsCitation":"Nicolai, C.A., Flint, P.L., and Wege, M.L., 2005, Annual survival and site fidelity of northern pintails banded on the Yukon-Kuskokwim Delta, Alaska: Journal of Wildlife Management, v. 69, no. 3, p. 1202-1210, https://doi.org/10.2193/0022-541X(2005)069[1202:ASASFO]2.0.CO;2.","productDescription":"9 p.","startPage":"1202","endPage":"1210","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":237535,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210571,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2193/0022-541X(2005)069[1202:ASASFO]2.0.CO;2"}],"volume":"69","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ec39e4b0c8380cd49132","contributors":{"authors":[{"text":"Nicolai, Christopher A.","contributorId":107140,"corporation":false,"usgs":true,"family":"Nicolai","given":"Christopher","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":423388,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flint, Paul L. 0000-0002-8758-6993 pflint@usgs.gov","orcid":"https://orcid.org/0000-0002-8758-6993","contributorId":3284,"corporation":false,"usgs":true,"family":"Flint","given":"Paul","email":"pflint@usgs.gov","middleInitial":"L.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":423389,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wege, Michael L.","contributorId":78629,"corporation":false,"usgs":true,"family":"Wege","given":"Michael","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":423387,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029598,"text":"70029598 - 2005 - The persistence of the water budget myth and its relationship to sustainability","interactions":[],"lastModifiedDate":"2012-03-12T17:20:53","indexId":"70029598","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1923,"text":"Hydrogeology Journal","active":true,"publicationSubtype":{"id":10}},"title":"The persistence of the water budget myth and its relationship to sustainability","docAbstract":"Sustainability and sustainable pumping are two different concepts that are often used interchangeably. The latter term refers to a pumping rate that can be maintained indefinitely without mining an aquifer, whereas the former term is broader and concerns such issues as ecology and water quality, among others, in addition to sustainable pumping. Another important difference between the two concepts is that recharge can be very important to consider when assessing sustainability, but is not necessary to estimate sustainable pumping rates. Confusion over this distinction is made worse by the Water Budget Myth, which comprises the mistaken yet persistent ideas that (1) sustainable pumping rates cannot exceed virgin recharge rates in aquifers, and (2) that virgin recharge rates must therefore be known to estimate sustainable pumping rates. Analysis of the water balance equation shows the special circumstances that must apply for the Water Budget Myth to be true. However, due to the effects recharge is likely to have on water quality, ecology, socioeconomic factors, and, under certain circumstances, its requirement for numerical modeling, it remains important in assessments of sustainability. ?? Springer-Verlag 2004.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hydrogeology Journal","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10040-004-0354-0","issn":"14312174","usgsCitation":"Devlin, J., and Sophocleous, M., 2005, The persistence of the water budget myth and its relationship to sustainability: Hydrogeology Journal, v. 13, no. 4, p. 549-554, https://doi.org/10.1007/s10040-004-0354-0.","startPage":"549","endPage":"554","numberOfPages":"6","costCenters":[],"links":[{"id":210600,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10040-004-0354-0"},{"id":237574,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"4","noUsgsAuthors":false,"publicationDate":"2004-05-28","publicationStatus":"PW","scienceBaseUri":"505bae8ae4b08c986b324180","contributors":{"authors":[{"text":"Devlin, J.F.","contributorId":12679,"corporation":false,"usgs":true,"family":"Devlin","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":423401,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sophocleous, M.","contributorId":13373,"corporation":false,"usgs":true,"family":"Sophocleous","given":"M.","email":"","affiliations":[],"preferred":false,"id":423402,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}