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,{"id":70028688,"text":"70028688 - 2006 - Automatic alignment of vector data and orthoimagery for the national map","interactions":[],"lastModifiedDate":"2012-03-12T17:20:44","indexId":"70028688","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Automatic alignment of vector data and orthoimagery for the national map","docAbstract":"A general problem in combining road vector data with orthoimagery from different sources is that they rarely align. There are a variety of causes to this problem, but the most common one is that the latest products are collected with higher accuracy and improved processing techniques. In previous work, we developed techniques to automatically correct the alignment of vector data with orthoimagery using a technique called conflation. However, in applying our technique to real-world datasets provided by USGS, we discovered that these techniques failed in some areas. In this paper, we describe some refinements to our original approach that provide consistently better results in aligning the vector data with the orthoimagery.","largerWorkTitle":"ACM International Conference Proceeding Series","conferenceTitle":"7th Annual International Conference on Digital Government Research, Dg.o 2006","conferenceDate":"21 May 2006 through 24 May 2006","conferenceLocation":"San Diego, CA","language":"English","doi":"10.1145/1146598.1146680","usgsCitation":"Knoblock, C., Shahabi, C., Chen, C., and Usery, E., 2006, Automatic alignment of vector data and orthoimagery for the national map, <i>in</i> ACM International Conference Proceeding Series, v. 151, San Diego, CA, 21 May 2006 through 24 May 2006, p. 303-304, https://doi.org/10.1145/1146598.1146680.","startPage":"303","endPage":"304","numberOfPages":"2","costCenters":[],"links":[{"id":236783,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":209997,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1145/1146598.1146680"}],"volume":"151","noUsgsAuthors":false,"publicationDate":"2006-05-21","publicationStatus":"PW","scienceBaseUri":"5059eef8e4b0c8380cd4a094","contributors":{"authors":[{"text":"Knoblock, C.A.","contributorId":105107,"corporation":false,"usgs":true,"family":"Knoblock","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":419281,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shahabi, C.","contributorId":51521,"corporation":false,"usgs":true,"family":"Shahabi","given":"C.","email":"","affiliations":[],"preferred":false,"id":419280,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chen, C.-C.","contributorId":22559,"corporation":false,"usgs":true,"family":"Chen","given":"C.-C.","email":"","affiliations":[],"preferred":false,"id":419278,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Usery, E.L.","contributorId":45355,"corporation":false,"usgs":true,"family":"Usery","given":"E.L.","email":"","affiliations":[],"preferred":false,"id":419279,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70028685,"text":"70028685 - 2006 - Striping artifact reduction in lunar orbiter mosaic images","interactions":[],"lastModifiedDate":"2012-03-12T17:20:44","indexId":"70028685","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Striping artifact reduction in lunar orbiter mosaic images","docAbstract":"Photographic images of the moon from the 1960s Lunar Orbiter missions are being processed into maps for visual use. The analog nature of the images has produced numerous artifacts, the chief of which causes a vertical striping pattern in mosaic images formed from a series of filmstrips. Previous methods of stripe removal tended to introduce ringing and aliasing problems in the image data. This paper describes a recently developed alternative approach that succeeds at greatly reducing the striping artifacts while avoiding the creation of ringing and aliasing artifacts. The algorithm uses a one dimensional frequency domain step to deal with the periodic component of the striping artifact and a spatial domain step to handle the aperiodic residue. Several variations of the algorithm have been explored. Results, strengths, and remaining challenges are presented. ?? 2006 IEEE.","largerWorkTitle":"Proceedings of the IEEE Southwest Symposium on Image Analysis and Interpretation","conferenceTitle":"7th IEEE Southwest Symposium on Image Analysis and Interpretation","conferenceDate":"26 March 2006 through 28 March 2006","conferenceLocation":"Denver, CO","language":"English","isbn":"1424400694; 9781424400690","usgsCitation":"Mlsna, P., and Becker, T., 2006, Striping artifact reduction in lunar orbiter mosaic images, <i>in</i> Proceedings of the IEEE Southwest Symposium on Image Analysis and Interpretation, v. 2006, Denver, CO, 26 March 2006 through 28 March 2006, p. 95-99.","startPage":"95","endPage":"99","numberOfPages":"5","costCenters":[],"links":[{"id":236752,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2006","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9b77e4b08c986b31cee8","contributors":{"authors":[{"text":"Mlsna, P.A.","contributorId":53147,"corporation":false,"usgs":true,"family":"Mlsna","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":419267,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Becker, T.","contributorId":78125,"corporation":false,"usgs":true,"family":"Becker","given":"T.","affiliations":[],"preferred":false,"id":419268,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028684,"text":"70028684 - 2006 - Description of the L1C signal","interactions":[],"lastModifiedDate":"2012-03-12T17:20:44","indexId":"70028684","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Description of the L1C signal","docAbstract":"Detailed design of the modernized LI civil signal (L1C) signal has been completed, and the resulting draft Interface Specification IS-GPS-800 was released in Spring 2006. The novel characteristics of the optimized L1C signal design provide advanced capabilities while offering to receiver designers considerable flexibility in how to use these capabilities. L1C provides a number of advanced features, including: 75% of power in a pilot component for enhanced signal tracking, advanced Weilbased spreading codes, an overlay code on the pilot that provides data message synchronization, support for improved reading of clock and ephemeris by combining message symbols across messages, advanced forward error control coding, and data symbol interleaving to combat fading. The resulting design offers receiver designers the opportunity to obtain unmatched performance in many ways. This paper describes the design of L1C. A summary of LIC's background and history is provided. The signal description then proceeds with the overall signal structure consisting of a pilot component and a carrier component. The new L1C spreading code family is described, along with the logic used for generating these spreading codes. Overlay codes on the pilot channel are also described, as is the logic used for generating the overlay codes. Spreading modulation characteristics are summarized. The data message structure is also presented, showing the format for providing time, ephemeris, and system data to users, along with features that enable receivers to perform code combining. Encoding of rapidly changing time bits is described, as are the Low Density Parity Check codes used for forward error control of slowly changing time bits, clock, ephemeris, and system data. The structure of the interleaver is also presented. A summary of L 1C's unique features and their benefits is provided, along with a discussion of the plan for L1C implementation.","largerWorkTitle":"Proceedings of the Institute of Navigation - 19th International Technical Meeting of the Satellite Division, ION GNSS 2006","conferenceTitle":"Institute of Navigation - 19th International Technical Meeting of the Satellite Division, ION GNSS 2006","conferenceDate":"26 September 2006 through 29 September 2006","conferenceLocation":"Fort Worth, TX","language":"English","usgsCitation":"Betz, J., Blanco, M., Cahn, C., Dafesh, P., Hegarty, C., Hudnut, K., Kasemsri, V., Keegan, R., Kovach, K., Lenahan, L., Ma, H., Rushanan, J., Sklar, D., Stansell, T., Wang, C., and Yi, S., 2006, Description of the L1C signal, <i>in</i> Proceedings of the Institute of Navigation - 19th International Technical Meeting of the Satellite Division, ION GNSS 2006, v. 4, Fort Worth, TX, 26 September 2006 through 29 September 2006, p. 2080-2091.","startPage":"2080","endPage":"2091","numberOfPages":"12","costCenters":[],"links":[{"id":236751,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ff03e4b0c8380cd4f005","contributors":{"authors":[{"text":"Betz, J.W.","contributorId":7484,"corporation":false,"usgs":true,"family":"Betz","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":419251,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blanco, M.A.","contributorId":62396,"corporation":false,"usgs":true,"family":"Blanco","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":419260,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cahn, C.R.","contributorId":86556,"corporation":false,"usgs":true,"family":"Cahn","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":419263,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dafesh, P.A.","contributorId":98937,"corporation":false,"usgs":true,"family":"Dafesh","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":419265,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hegarty, C.J.","contributorId":26501,"corporation":false,"usgs":true,"family":"Hegarty","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":419255,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hudnut, K.W.","contributorId":25179,"corporation":false,"usgs":true,"family":"Hudnut","given":"K.W.","email":"","affiliations":[],"preferred":false,"id":419253,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kasemsri, V.","contributorId":92479,"corporation":false,"usgs":true,"family":"Kasemsri","given":"V.","email":"","affiliations":[],"preferred":false,"id":419264,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Keegan, R.","contributorId":49170,"corporation":false,"usgs":true,"family":"Keegan","given":"R.","email":"","affiliations":[],"preferred":false,"id":419259,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Kovach, K.","contributorId":69348,"corporation":false,"usgs":true,"family":"Kovach","given":"K.","email":"","affiliations":[],"preferred":false,"id":419261,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Lenahan, L.S.","contributorId":107916,"corporation":false,"usgs":true,"family":"Lenahan","given":"L.S.","email":"","affiliations":[],"preferred":false,"id":419266,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Ma, H.H.","contributorId":47959,"corporation":false,"usgs":true,"family":"Ma","given":"H.H.","email":"","affiliations":[],"preferred":false,"id":419258,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Rushanan, J.J.","contributorId":26129,"corporation":false,"usgs":true,"family":"Rushanan","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":419254,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Sklar, D.","contributorId":73804,"corporation":false,"usgs":true,"family":"Sklar","given":"D.","email":"","affiliations":[],"preferred":false,"id":419262,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Stansell, T.A.","contributorId":38761,"corporation":false,"usgs":true,"family":"Stansell","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":419257,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Wang, C.C.","contributorId":22956,"corporation":false,"usgs":true,"family":"Wang","given":"C.C.","email":"","affiliations":[],"preferred":false,"id":419252,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Yi, S.K.","contributorId":35108,"corporation":false,"usgs":true,"family":"Yi","given":"S.K.","email":"","affiliations":[],"preferred":false,"id":419256,"contributorType":{"id":1,"text":"Authors"},"rank":16}]}}
,{"id":70028683,"text":"70028683 - 2006 - A new 1649-1884 catalog of destructive earthquakes near Tokyo and implications for the long-term seismic process","interactions":[],"lastModifiedDate":"2012-03-12T17:20:44","indexId":"70028683","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","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":"A new 1649-1884 catalog of destructive earthquakes near Tokyo and implications for the long-term seismic process","docAbstract":"In order to assess the long-term character of seismicity near Tokyo, we construct an intensity-based catalog of damaging earthquakes that struck the greater Tokyo area between 1649 and 1884. Models for 15 historical earthquakes are developed using calibrated intensity attenuation relations that quantitatively convey uncertainties in event location and magnitude, as well as their covariance. The historical catalog is most likely complete for earthquakes M ??? 6.7; the largest earthquake in the catalog is the 1703 M ??? 8.2 Genroku event. Seismicity rates from 80 years of instrumental records, which include the 1923 M = 7.9 Kanto shock, as well as interevent times estimated from the past ???7000 years of paleoseismic data, are combined with the historical catalog to define a frequency-magnitude distribution for 4.5 ??? M ??? 8.2, which is well described by a truncated Gutenberg-Richter relation with a b value of 0.96 and a maximum magnitude of 8.4. Large uncertainties associated with the intensity-based catalog are propagated by a Monte Carlo simulation to estimations of the scalar moment rate. The resulting best estimate of moment rate during 1649-2003 is 1.35 ?? 1026 dyn cm yr-1 with considerable uncertainty at the 1??, level: (-0.11, + 0.20) ?? 1026 dyn cm yr-1. Comparison with geodetic models of the interseismic deformation indicates that the geodetic moment accumulation and likely moment release rate are roughly balanced over the catalog period. This balance suggests that the extended catalog is representative of long-term seismic processes near Tokyo and so can be used to assess earthquake probabilities. The resulting Poisson (or time-averaged) 30-year probability for M ??? 7.9 earthquakes is 7-11%.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research B: Solid Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2005JB004059","issn":"01480227","usgsCitation":"Grunewald, E., and Stein, R., 2006, A new 1649-1884 catalog of destructive earthquakes near Tokyo and implications for the long-term seismic process: Journal of Geophysical Research B: Solid Earth, v. 111, no. 12, https://doi.org/10.1029/2005JB004059.","costCenters":[],"links":[{"id":477484,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2005jb004059","text":"Publisher Index Page"},{"id":209950,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2005JB004059"},{"id":236716,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"111","issue":"12","noUsgsAuthors":false,"publicationDate":"2006-12-20","publicationStatus":"PW","scienceBaseUri":"5059e497e4b0c8380cd4674c","contributors":{"authors":[{"text":"Grunewald, E.D.","contributorId":66465,"corporation":false,"usgs":true,"family":"Grunewald","given":"E.D.","email":"","affiliations":[],"preferred":false,"id":419250,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stein, R.S.","contributorId":8875,"corporation":false,"usgs":true,"family":"Stein","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":419249,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028682,"text":"70028682 - 2006 - Spatio-temporal availability of soft mast in clearcuts in the Southern Appalachians","interactions":[],"lastModifiedDate":"2012-03-12T17:20:44","indexId":"70028682","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1687,"text":"Forest Ecology and Management","active":true,"publicationSubtype":{"id":10}},"title":"Spatio-temporal availability of soft mast in clearcuts in the Southern Appalachians","docAbstract":"Soft mast is an important resource for many wild populations in the Southern Appalachians, yet the way clear-cutting affects availability of soft mast though time is not fully understood. We tested a theoretical model of temporal availability of soft mast in clearcuts using empirical data on percent cover and berry production of Gaylussacia, Vaccinium, and Rubus spp. plants in 100 stands that were clearcut (0-122 years old) in the Southern Appalachian Mountains. We modeled the relationship between soft mast availability and stand age, evaluated the effects of topography and forest type on soft mast, developed statistical models for predicting the spatio-temporal distribution of soft mast, and tested the hypothesis that percent cover of berry plants and berry production provided similar information about soft mast availability. We found temporal dynamics explained berry production better than it predicted percent plant cover, whereas topographic variables influenced percent plant cover more than they influenced berry production. Berry production and percent plant cover were highest in ???2-9-year-old stands. Percent plant cover was lowest in 10-69-year-old stands and intermediate in 70+-year-old stands. Three of our spatio-temporal models performed well during model testing and they were not biased by the training data, indicating the inferences about spatio-temporal availability of soft mast extended beyond our sample data. The methods we used to estimate the distribution of soft mast may be useful for modeling distributions of other resources. ?? 2006 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Forest Ecology and Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.foreco.2006.09.035","issn":"03781127","usgsCitation":"Reynolds-Hogland, M.J., Mitchell, M., and Powell, R.A., 2006, Spatio-temporal availability of soft mast in clearcuts in the Southern Appalachians: Forest Ecology and Management, v. 237, no. 1-3, p. 103-114, https://doi.org/10.1016/j.foreco.2006.09.035.","startPage":"103","endPage":"114","numberOfPages":"12","costCenters":[],"links":[{"id":209949,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.foreco.2006.09.035"},{"id":236715,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"237","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b94c7e4b08c986b31ac43","contributors":{"authors":[{"text":"Reynolds-Hogland, M. J.","contributorId":57647,"corporation":false,"usgs":true,"family":"Reynolds-Hogland","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":419248,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mitchell, M.S.","contributorId":26724,"corporation":false,"usgs":true,"family":"Mitchell","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":419246,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Powell, R. A.","contributorId":41789,"corporation":false,"usgs":true,"family":"Powell","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":419247,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70028679,"text":"70028679 - 2006 - Wetland and microhabitat use by nesting four-toed salamanders in Maine","interactions":[],"lastModifiedDate":"2012-03-12T17:20:44","indexId":"70028679","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2334,"text":"Journal of Herpetology","active":true,"publicationSubtype":{"id":10}},"title":"Wetland and microhabitat use by nesting four-toed salamanders in Maine","docAbstract":"Little is known of Four-Toed Salamander (Hemidactylium scutatum) habitat use, despite the species' extensive range and elevated conservation status. We investigated species-habitat relationships that predict H. scutatum nesting presence in Maine at wetland and microhabitat scales by comparing microhabitats with and without nests. We created logistic regression models, selected models with AIC, and evaluated models with reserve data. Wetlands with nests were best predicted by shoreline microhabitat of Sphagnum spp., wood substrate, water flow, blue-joint reed grass (Calamagrostis canadensis), meadowsweet (Spiraea alba), steeplebush (Spiraea tomentosa), sensitive fern (Onoclea sensibilis), and absence of sheep laurel (Kalmia angustifolia) or deciduous forest canopy. Within occupied wetlands, shoreline microhabitat where nests occurred was best distinguished from available, unoccupied shoreline microhabitat by steeper shore, greater near-shore and basin water depth, deeper nesting vegetation, presence of moss spp. and winterberry (Ilex verticillata), and a negative association with S. alba, leatherleaf (Chamaedaphne calyculata), and K. angustifolia. These models of wetland and microhabitat use by H. scutatum may assist ecologists and managers in detecting and conserving this species. Copyright 2006 Society for the Study of Amphibians and Reptiles.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Herpetology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1670/0022-1511(2006)40[478:WAMUBN]2.0.CO;2","issn":"00221511","usgsCitation":"Chalmers, R., and Loftin, C., 2006, Wetland and microhabitat use by nesting four-toed salamanders in Maine: Journal of Herpetology, v. 40, no. 4, p. 478-485, https://doi.org/10.1670/0022-1511(2006)40[478:WAMUBN]2.0.CO;2.","startPage":"478","endPage":"485","numberOfPages":"8","costCenters":[],"links":[{"id":209897,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1670/0022-1511(2006)40[478:WAMUBN]2.0.CO;2"},{"id":236642,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"40","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bd013e4b08c986b32ec74","contributors":{"authors":[{"text":"Chalmers, R.J.","contributorId":10894,"corporation":false,"usgs":true,"family":"Chalmers","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":419224,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Loftin, C.S.","contributorId":92771,"corporation":false,"usgs":true,"family":"Loftin","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":419225,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028676,"text":"70028676 - 2006 - Mineral mapping and applications of imaging spectroscopy","interactions":[],"lastModifiedDate":"2012-03-12T17:20:44","indexId":"70028676","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Mineral mapping and applications of imaging spectroscopy","docAbstract":"Spectroscopy is a tool that has been used for decades to identify, understand, and quantify solid, liquid, or gaseous materials, especially in the laboratory. In disciplines ranging from astronomy to chemistry, spectroscopic measurements are used to detect absorption and emission features due to specific chemical bonds, and detailed analyses are used to determine the abundance and physical state of the detected absorbing/emitting species. Spectroscopic measurements have a long history in the study of the Earth and planets. Up to the 1990s remote spectroscopic measurements of Earth and planets were dominated by multispectral imaging experiments that collect high-quality images in a few, usually broad, spectral bands or with point spectrometers that obtained good spectral resolution but at only a few spatial positions. However, a new generation of sensors is now available that combines imaging with spectroscopy to create the new discipline of imaging spectroscopy. Imaging spectrometers acquire data with enough spectral range, resolution, and sampling at every pixel in a raster image so that individual absorption features can be identified and spatially mapped (Goetz et al., 1985).","largerWorkTitle":"International Geoscience and Remote Sensing Symposium (IGARSS)","conferenceTitle":"2006 IEEE International Geoscience and Remote Sensing Symposium, IGARSS","conferenceDate":"31 July 2006 through 4 August 2006","conferenceLocation":"Denver, CO","language":"English","doi":"10.1109/IGARSS.2006.514","isbn":"0780395107; 9780780395107","usgsCitation":"Clark, R.N., Boardman, J., Mustard, J., Kruse, F., Ong, C., Pieters, C., and Swayze, G., 2006, Mineral mapping and applications of imaging spectroscopy, <i>in</i> International Geoscience and Remote Sensing Symposium (IGARSS), Denver, CO, 31 July 2006 through 4 August 2006, p. 1986-1989, https://doi.org/10.1109/IGARSS.2006.514.","startPage":"1986","endPage":"1989","numberOfPages":"4","costCenters":[],"links":[{"id":209866,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1109/IGARSS.2006.514"},{"id":236607,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5797e4b0c8380cd6dd89","contributors":{"authors":[{"text":"Clark, R. N.","contributorId":6568,"corporation":false,"usgs":true,"family":"Clark","given":"R.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":419212,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boardman, J.","contributorId":74184,"corporation":false,"usgs":true,"family":"Boardman","given":"J.","affiliations":[],"preferred":false,"id":419214,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mustard, J.","contributorId":103458,"corporation":false,"usgs":true,"family":"Mustard","given":"J.","email":"","affiliations":[],"preferred":false,"id":419217,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kruse, F.","contributorId":84142,"corporation":false,"usgs":true,"family":"Kruse","given":"F.","email":"","affiliations":[],"preferred":false,"id":419215,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ong, C.","contributorId":96071,"corporation":false,"usgs":true,"family":"Ong","given":"C.","email":"","affiliations":[],"preferred":false,"id":419216,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Pieters, C.","contributorId":104636,"corporation":false,"usgs":true,"family":"Pieters","given":"C.","email":"","affiliations":[],"preferred":false,"id":419218,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Swayze, G.A. 0000-0002-1814-7823","orcid":"https://orcid.org/0000-0002-1814-7823","contributorId":21570,"corporation":false,"usgs":true,"family":"Swayze","given":"G.A.","affiliations":[],"preferred":false,"id":419213,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70028672,"text":"70028672 - 2006 - Prediction and discovery of new geothermal resources in the Great Basin: Multiple evidence of a large undiscovered resource base","interactions":[],"lastModifiedDate":"2012-03-12T17:20:59","indexId":"70028672","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Prediction and discovery of new geothermal resources in the Great Basin: Multiple evidence of a large undiscovered resource base","docAbstract":"Geothermal potential maps by themselves cannot directly be used to estimate undiscovered resources. To address the undiscovered resource base in the Great Basin, a new and relatively quantitative methodology is presented. The methodology involves three steps, the first being the construction of a data-driven probabilistic model of the location of known geothermal systems using weights of evidence. The second step is the construction of a degree-of-exploration model. This degree-of-exploration model uses expert judgment in a fuzzy logic context to estimate how well each spot in the state has been explored, using as constraints digital maps of the depth to the water table, presence of the carbonate aquifer, and the location, depth, and type of drill-holes. Finally, the exploration model and the data-driven occurrence model are combined together quantitatively using area-weighted modifications to the weights-of-evidence equations. Using this methodology in the state of Nevada, the number of undiscovered geothermal systems with reservoir temperatures ???100??C is estimated at 157, which is 3.2 times greater than the 69 known systems. Currently, nine of the 69 known systems are producing electricity. If it is conservatively assumed that an additional nine for a total of 18 of the known systems will eventually produce electricity, then the model predicts 59 known and undiscovered geothermal systems are capable of producing electricity under current economic conditions in the state, a figure that is more than six times higher than the current number. Many additional geothermal systems could potentially become economic under improved economic conditions or with improved methods of reservoir stimulation (Enhanced Geothermal Systems).This large predicted geothermal resource base appears corroborated by recent grass-roots geothermal discoveries in the state of Nevada. At least two and possibly three newly recognized geothermal systems with estimated reservoir temperatures ???150??C have been identified on the Pyramid Lake Paiute Reservation in west-central Nevada. Evidence of three blind geothermal systems has recently been uncovered near the borate-bearing playas at Rhodes, Teels, and Columbus Marshes in southwestern Nevada. Recent gold exploration drilling has resulted in at least four new geothermal discoveries, including the McGinness Hills geothermal system with an estimated reservoir temperature of roughly 200??C. All of this evidence suggests that the potential for expansion of geothermal power production in Nevada is significant.","largerWorkTitle":"Transactions - Geothermal Resources Council","conferenceTitle":"GRC 2006 Annual Meeting: Geothermal Resources-Securing Our Energy Future","conferenceDate":"10 September 2006 through 13 September 2006","conferenceLocation":"San Diego, CA","language":"English","issn":"01935933","isbn":"1604230010; 9781604230017","usgsCitation":"Coolbaugh, M., Raines, G.L., Zehner, R.E., Shevenell, L., and Williams, C., 2006, Prediction and discovery of new geothermal resources in the Great Basin: Multiple evidence of a large undiscovered resource base, <i>in</i> Transactions - Geothermal Resources Council, v. 30 II, San Diego, CA, 10 September 2006 through 13 September 2006, p. 867-873.","startPage":"867","endPage":"873","numberOfPages":"7","costCenters":[],"links":[{"id":236539,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30 II","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a81e6e4b0c8380cd7b7b3","contributors":{"authors":[{"text":"Coolbaugh, M.F.","contributorId":55034,"corporation":false,"usgs":true,"family":"Coolbaugh","given":"M.F.","affiliations":[],"preferred":false,"id":419170,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Raines, G. L.","contributorId":90720,"corporation":false,"usgs":true,"family":"Raines","given":"G.","middleInitial":"L.","affiliations":[],"preferred":false,"id":419173,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zehner, R. E.","contributorId":67933,"corporation":false,"usgs":true,"family":"Zehner","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":419172,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Shevenell, L.","contributorId":55971,"corporation":false,"usgs":true,"family":"Shevenell","given":"L.","affiliations":[],"preferred":false,"id":419171,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Williams, C.F. 0000-0003-2196-5496","orcid":"https://orcid.org/0000-0003-2196-5496","contributorId":20401,"corporation":false,"usgs":true,"family":"Williams","given":"C.F.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":419169,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70028671,"text":"70028671 - 2006 - Earthquake ground-motion prediction equations for eastern North America","interactions":[],"lastModifiedDate":"2012-03-12T17:21:00","indexId":"70028671","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"Earthquake ground-motion prediction equations for eastern North America","docAbstract":"New earthquake ground-motion relations for hard-rock and soil sites in eastern North America (ENA), including estimates of their aleatory uncertainty (variability) have been developed based on a stochastic finite-fault model. The model incorporates new information obtained from ENA seismographic data gathered over the past 10 years, including three-component broadband data that provide new information on ENA source and path effects. Our new prediction equations are similar to the previous ground-motion prediction equations of Atkinson and Boore (1995), which were based on a stochastic point-source model. The main difference is that high-frequency amplitudes (f ??? 5 Hz) are less than previously predicted (by about a factor of 1.6 within 100 km), because of a slightly lower average stress parameter (140 bars versus 180 bars) and a steeper near-source attenuation. At frequencies less than 5 Hz, the predicted ground motions from the new equations are generally within 25% of those predicted by Atkinson and Boore (1995). The prediction equations agree well with available ENA ground-motion data as evidenced by near-zero average residuals (within a factor of 1.2) for all frequencies, and the lack of any significant residual trends with distance. However, there is a tendency to positive residuals for moderate events at high frequencies in the distance range from 30 to 100 km (by as much as a factor of 2). This indicates epistemic uncertainty in the prediction model. The positive residuals for moderate events at < 100 km could be eliminated by an increased stress parameter, at the cost of producing negative residuals in other magnitude-distance ranges; adjustment factors to the equations are provided that may be used to model this effect.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of the Seismological Society of America","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1785/0120050245","issn":"00371106","usgsCitation":"Atkinson, G.M., and Boore, D., 2006, Earthquake ground-motion prediction equations for eastern North America: Bulletin of the Seismological Society of America, v. 96, no. 6, p. 2181-2205, https://doi.org/10.1785/0120050245.","startPage":"2181","endPage":"2205","numberOfPages":"25","costCenters":[],"links":[{"id":209793,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1785/0120050245"},{"id":236508,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"96","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a04eee4b0c8380cd50b99","contributors":{"authors":[{"text":"Atkinson, G. M.","contributorId":69283,"corporation":false,"usgs":true,"family":"Atkinson","given":"G.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":419168,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boore, D.M. 0000-0002-8605-9673","orcid":"https://orcid.org/0000-0002-8605-9673","contributorId":64226,"corporation":false,"usgs":true,"family":"Boore","given":"D.M.","affiliations":[],"preferred":false,"id":419167,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028666,"text":"70028666 - 2006 - Two models for evaluating landslide hazards","interactions":[],"lastModifiedDate":"2012-03-12T17:21:00","indexId":"70028666","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1315,"text":"Computers & Geosciences","printIssn":"0098-3004","active":true,"publicationSubtype":{"id":10}},"title":"Two models for evaluating landslide hazards","docAbstract":"Two alternative procedures for estimating landslide hazards were evaluated using data on topographic digital elevation models (DEMs) and bedrock lithologies in an area adjacent to the Missouri River in Atchison County, Kansas, USA. The two procedures are based on the likelihood ratio model but utilize different assumptions. The empirical likelihood ratio model is based on non-parametric empirical univariate frequency distribution functions under an assumption of conditional independence while the multivariate logistic discriminant model assumes that likelihood ratios can be expressed in terms of logistic functions. The relative hazards of occurrence of landslides were estimated by an empirical likelihood ratio model and by multivariate logistic discriminant analysis. Predictor variables consisted of grids containing topographic elevations, slope angles, and slope aspects calculated from a 30-m DEM. An integer grid of coded bedrock lithologies taken from digitized geologic maps was also used as a predictor variable. Both statistical models yield relative estimates in the form of the proportion of total map area predicted to already contain or to be the site of future landslides. The stabilities of estimates were checked by cross-validation of results from random subsamples, using each of the two procedures. Cell-by-cell comparisons of hazard maps made by the two models show that the two sets of estimates are virtually identical. This suggests that the empirical likelihood ratio and the logistic discriminant analysis models are robust with respect to the conditional independent assumption and the logistic function assumption, respectively, and that either model can be used successfully to evaluate landslide hazards. ?? 2006.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Computers and Geosciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.cageo.2006.02.006","issn":"00983004","usgsCitation":"Davis, J., Chung, C., and Ohlmacher, G., 2006, Two models for evaluating landslide hazards: Computers & Geosciences, v. 32, no. 8, p. 1120-1127, https://doi.org/10.1016/j.cageo.2006.02.006.","startPage":"1120","endPage":"1127","numberOfPages":"8","costCenters":[],"links":[{"id":209737,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.cageo.2006.02.006"},{"id":236434,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb95be4b08c986b327be0","contributors":{"authors":[{"text":"Davis, J.C.","contributorId":72121,"corporation":false,"usgs":true,"family":"Davis","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":419123,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chung, C.-J.","contributorId":101861,"corporation":false,"usgs":true,"family":"Chung","given":"C.-J.","email":"","affiliations":[],"preferred":false,"id":419124,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ohlmacher, G.C.","contributorId":63064,"corporation":false,"usgs":true,"family":"Ohlmacher","given":"G.C.","email":"","affiliations":[],"preferred":false,"id":419122,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70028665,"text":"70028665 - 2006 - Location and timing of river-aquifer exchanges in six tributaries to the Columbia River in the Pacific Northwest of the United States","interactions":[],"lastModifiedDate":"2016-05-27T15:16:22","indexId":"70028665","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Location and timing of river-aquifer exchanges in six tributaries to the Columbia River in the Pacific Northwest of the United States","docAbstract":"<p>The flow of water between rivers and contiguous aquifers influences the quantity and quality of water resources, particularly in regions where precipitation and runoff are unevenly distributed through the year, such as the Columbia Basin (CB) in northwestern United States. Investigations of basin hydrogeology and gains and losses of streamflow for six rivers in the CB were reviewed to characterize general patterns in the timing and location of river-aquifer exchanges at a reach-scale (0.5-150 km) and to identify geologic and geomorphic features associated with the largest exchanges. Ground-water discharge to each river, or the gain in streamflow, was concentrated spatially: more than one-half of the total gains along each river segment were contributed from reaches that represented no more than 30% of the total segment length with the largest and most concentrated gains in rivers in volcanic terrains. Fluvial recharge of aquifers, or losses of streamflow, was largest in rivers in sedimentary basins where unconsolidated sediments form shallow aquifers. Three types of geologic or geomorphic features were associated with the largest exchanges: (1) changes in the thickness of unconsolidated aquifers; (2) contacts between lithologic units that represent contrasts in permeability; and (3) channel forms that increase the hydraulic gradient or cross-sectional area of flow paths between a river and shallow ground-water. The down-valley component of ground-water flow and its vertical convergence on or divergence from a riverbed account for large streamflow gains in some reaches and contrast with the common assumption of lateral ground-water discharge to a river that penetrates completely through the aquifer. Increased ground-water discharge was observed during high-flow periods in reaches of four rivers indicating that changes in ground-water levels can be more important than stage fluctuations in regulating the direction and magnitude of river-aquifer exchanges and that assumptions about ground-water discharge during high flow periods used for base-flow separation must be verified. Given the variety of geologic terrains in the CB, the spatial and temporal patterns of river-aquifer exchanges provide a framework for investigations in other regions that includes a focus on reaches where the largest exchanges are likely to occur, integration of ground-water and surface-water data, and verification of assumptions regarding ground-water flow direction and temporal variation of exchanges. ?? 2006 Elsevier B.V. All rights reserved.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jhydrol.2006.02.028","issn":"00221694","usgsCitation":"Konrad, C., 2006, Location and timing of river-aquifer exchanges in six tributaries to the Columbia River in the Pacific Northwest of the United States: Journal of Hydrology, v. 329, no. 3-4, p. 444-470, https://doi.org/10.1016/j.jhydrol.2006.02.028.","productDescription":"27 p.","startPage":"444","endPage":"470","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":236433,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":209736,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jhydrol.2006.02.028"}],"volume":"329","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a490be4b0c8380cd68305","contributors":{"authors":[{"text":"Konrad, C.P.","contributorId":39027,"corporation":false,"usgs":true,"family":"Konrad","given":"C.P.","email":"","affiliations":[],"preferred":false,"id":419121,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70028662,"text":"70028662 - 2006 - Coulomb stress transfer and tectonic loading preceding the 2002 Denali fault earthquake","interactions":[],"lastModifiedDate":"2017-04-26T14:03:11","indexId":"70028662","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"Coulomb stress transfer and tectonic loading preceding the 2002 Denali fault earthquake","docAbstract":"<p><span>Pre-2002 tectonic loading and Coulomb stress transfer are modeled along the rupture zone of the </span><strong>M</strong><span> 7.9 Denali fault earthquake (</span><span class=\"sc\">DFE</span><span>) and on adjacent segments of the right-lateral Denali–Totschunda fault system in central Alaska, using a three-dimensional boundary-element program. The segments modeled closely follow, for about 95°, the arc of a circle of radius 375 km centered on an inferred asperity near the northeastern end of the intersection of the Patton Bay fault with the Alaskan megathrust under Prince William Sound. The loading model includes slip of 6 mm/yr below 12 km along the fault system, consistent with rotation of the Wrangell block about the asperity at a rate of about 1°/m.y. as well as slip of the Pacific plate at 5 cm/yr at depth along the Fairweather–Queen Charlotte transform fault system and on the Alaska megathrust. The model is consistent with most available pre-2002 Global Positioning System (</span><span class=\"sc\">GPS</span><span>) displacement rate data. Coulomb stresses induced on the Denali–Totschunda fault system (locked above 12 km) by slip at depth and by transfer from the </span><strong>M</strong><span> 9.2 Prince William Sound earthquake of 1964 dominated the changing Coulomb stress distribution along the fault. The combination of loading (∼70–85%) and coseismic stress transfer from the great 1964 earthquake (∼15–30%) were the principal post-1900 stress factors building toward strike-slip failure of the northern Denali and Totschunda segments in the </span><strong>M</strong><span> 7.9 earthquake of November 2002. Postseismic stresses transferred from the 1964 earthquake may also have been a significant factor. The </span><strong>M</strong><span> 7.2–7.4 Delta River earthquake of 1912 (</span><span id=\"xref-ref-6-1\" class=\"xref-bibr\">Carver <i>et al.</i>, 2004</span><span>) may have delayed or advanced the timing of the </span><span class=\"sc\">DFE</span><span>, depending on the details and location of its rupture. The initial subevent of the 2002 </span><span class=\"sc\">DFE</span><span> earthquake was on the 40-km Susitna Glacier thrust fault at the western end of the Denali fault rupture. The Coulomb stress transferred from the 1964 earthquake moved the Susitna Glacier thrust fault uniformly away from thrust failure by about 100 kPa. The initiation of the Denali fault earthquake was advanced by transfer of 30–50 kPa of positive Coulomb stress to the Susitna Glacier fault (</span><span id=\"xref-ref-1-1\" class=\"xref-bibr\">Anderson and Ji, 2003</span><span>) by the nearby </span><strong>M</strong><span> 6.7 Nenana Mountain foreshock of 23 October 2002. The regional tectonic loading model used here suggests that the Semidi (Alaska Peninsula) segment of the megathrust that ruptured in 1938 (</span><strong>M</strong><span> 8.2) may be reloaded and approaching failure.</span></p>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/0120050007","issn":"00371106","usgsCitation":"Bufe, C.G., 2006, Coulomb stress transfer and tectonic loading preceding the 2002 Denali fault earthquake: Bulletin of the Seismological Society of America, v. 96, no. 5, p. 1662-1674, https://doi.org/10.1785/0120050007.","productDescription":"13","startPage":"1662","endPage":"1674","costCenters":[],"links":[{"id":236368,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"96","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fc84e4b0c8380cd4e2c5","contributors":{"authors":[{"text":"Bufe, Charles G. cbufe@usgs.gov","contributorId":1621,"corporation":false,"usgs":true,"family":"Bufe","given":"Charles","email":"cbufe@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":419114,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70028661,"text":"70028661 - 2006 - Adsorption site analysis of impurity embedded single-walled carbon nanotube bundles","interactions":[],"lastModifiedDate":"2012-03-12T17:20:56","indexId":"70028661","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1182,"text":"Carbon","active":true,"publicationSubtype":{"id":10}},"title":"Adsorption site analysis of impurity embedded single-walled carbon nanotube bundles","docAbstract":"Bundle morphology and adsorptive contributions from nanotubes and impurities are studied both experimentally and by simulation using a computer-aided methodology, which employs a small physisorbed probe molecule to explore the porosity of nanotube samples. Grand canonical Monte Carlo simulation of nitrogen adsorption on localized sites of a bundle is carried out to predict adsorption in its accessible internal pore volume and on its external surface as a function of tube diameter. External adsorption is split into the contributions from the clean surface of the outermost nanotubes of the bundle and from the surface of the impurities. The site-specific isotherms are then combined into a global isotherm for a given sample using knowledge of its tube-diameter distribution obtained by Raman spectroscopy. The structural parameters of the sample, such as the fraction of open-ended nanotubes and the contributions from impurities and nanotube bundles to total external surface area, are determined by fitting the experimental nitrogen adsorption data to the simulated isotherm. The degree of closure between experimental and calculated adsorption isotherms for samples manufactured by two different methods, to provide different nanotube morphology and contamination level, further strengthens the validity and resulting interpretations based on the proposed approach. The average number of nanotubes per bundle and average bundle size, within a sample, are also quantified. The proposed method allows for extrapolation of adsorption properties to conditions where the purification process is 100% effective at removing all impurities and opening access to all intrabundle adsorption sites. ?? 2006 Elsevier Ltd. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Carbon","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.carbon.2006.05.038","issn":"00086223","usgsCitation":"Agnihotri, S., Mota, J., Rostam-Abadi, M., and Rood, M., 2006, Adsorption site analysis of impurity embedded single-walled carbon nanotube bundles: Carbon, v. 44, no. 12, p. 2376-2383, https://doi.org/10.1016/j.carbon.2006.05.038.","startPage":"2376","endPage":"2383","numberOfPages":"8","costCenters":[],"links":[{"id":209691,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.carbon.2006.05.038"},{"id":236367,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e6fee4b0c8380cd477a3","contributors":{"authors":[{"text":"Agnihotri, S.","contributorId":19344,"corporation":false,"usgs":true,"family":"Agnihotri","given":"S.","email":"","affiliations":[],"preferred":false,"id":419112,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mota, J.P.B.","contributorId":18937,"corporation":false,"usgs":true,"family":"Mota","given":"J.P.B.","email":"","affiliations":[],"preferred":false,"id":419111,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rostam-Abadi, M.","contributorId":37061,"corporation":false,"usgs":true,"family":"Rostam-Abadi","given":"M.","affiliations":[],"preferred":false,"id":419113,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rood, M.J.","contributorId":15354,"corporation":false,"usgs":true,"family":"Rood","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":419110,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70028660,"text":"70028660 - 2006 - Testing of stack-unit/aquifer sensitivity analysis using contaminant plume distribution in the subsurface of Savannah River Site, South Carolina, USA","interactions":[],"lastModifiedDate":"2017-01-18T12:52:28","indexId":"70028660","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","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":"Testing of stack-unit/aquifer sensitivity analysis using contaminant plume distribution in the subsurface of Savannah River Site, South Carolina, USA","docAbstract":"Published information on the correlation and field-testing of the technique of stack-unit/aquifer sensitivity mapping with documented subsurface contaminant plumes is rare. The inherent characteristic of stack-unit mapping, which makes it a superior technique to other analyses that amalgamate data, is the ability to deconstruct the sensitivity analysis on a unit-by-unit basis. An aquifer sensitivity map, delineating the relative sensitivity of the Crouch Branch aquifer of the Administrative/Manufacturing Area (A/M) at the Savannah River Site (SRS) in South Carolina, USA, incorporates six hydrostratigraphic units, surface soil units, and relevant hydrologic data. When this sensitivity map is compared with the distribution of the contaminant tetrachloroethylene (PCE), PCE is present within the Crouch Branch aquifer within an area classified as highly sensitive, even though the PCE was primarily released on the ground surface within areas classified with low aquifer sensitivity. This phenomenon is explained through analysis of the aquifer sensitivity map, the groundwater potentiometric surface maps, and the plume distributions within the area on a unit-by- unit basis. The results of this correlation show how the paths of the PCE plume are influenced by both the geology and the groundwater flow. ?? Springer-Verlag 2006.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hydrogeology Journal","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10040-006-0083-7","issn":"14312174","usgsCitation":"Rine, J., Shafer, J., Covington, E., and Berg, R.C., 2006, Testing of stack-unit/aquifer sensitivity analysis using contaminant plume distribution in the subsurface of Savannah River Site, South Carolina, USA: Hydrogeology Journal, v. 14, no. 8, p. 1620-1634, https://doi.org/10.1007/s10040-006-0083-7.","startPage":"1620","endPage":"1634","numberOfPages":"15","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":236331,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":209662,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10040-006-0083-7"}],"country":"United 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Carolina\",\"nation\":\"USA  \"}}]}","volume":"14","issue":"8","noUsgsAuthors":false,"publicationDate":"2006-08-18","publicationStatus":"PW","scienceBaseUri":"505ba5cbe4b08c986b320ca8","contributors":{"authors":[{"text":"Rine, J.M.","contributorId":53145,"corporation":false,"usgs":true,"family":"Rine","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":419107,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shafer, J.M.","contributorId":72995,"corporation":false,"usgs":true,"family":"Shafer","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":419108,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Covington, E.","contributorId":92031,"corporation":false,"usgs":true,"family":"Covington","given":"E.","email":"","affiliations":[],"preferred":false,"id":419109,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Berg, R. C.","contributorId":11673,"corporation":false,"usgs":true,"family":"Berg","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":419106,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70028656,"text":"70028656 - 2006 - Slip on the San Andreas fault at Parkfield, California, over two earthquake cycles, and the implications for seismic hazard","interactions":[],"lastModifiedDate":"2012-03-12T17:20:57","indexId":"70028656","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"Slip on the San Andreas fault at Parkfield, California, over two earthquake cycles, and the implications for seismic hazard","docAbstract":"Parkfield, California, which experienced M 6.0 earthquakes in 1934, 1966, and 2004, is one of the few locales for which geodetic observations span multiple earthquake cycles. We undertake a comprehensive study of deformation over the most recent earthquake cycle and explore the results in the context of geodetic data collected prior to the 1966 event. Through joint inversion of the variety of Parkfield geodetic measurements (trilateration, two-color laser, and Global Positioning System), including previously unpublished two-color data, we estimate the spatial distribution of slip and slip rate along the San Andreas using a fault geometry based on precisely relocated seismicity. Although the three most recent Parkfield earthquakes appear complementary in their along-strike distributions of slip, they do not produce uniform strain release along strike over multiple seismic cycles. Since the 1934 earthquake, more than 1 m of slip deficit has accumulated on portions of the fault that slipped in the 1966 and 2004 earthquakes, and an average of 2 m of slip deficit exists on the 33 km of the fault southeast of Gold Hill to be released in a future, perhaps larger, earthquake. It appears that the fault is capable of partially releasing stored strain in moderate earthquakes, maintaining a disequilibrium through multiple earthquake cycles. This complicates the application of simple earthquake recurrence models that assume only the strain accumulated since the most recent event is relevant to the size or timing of an upcoming earthquake. Our findings further emphasize that accumulated slip deficit is not sufficient for earthquake nucleation.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of the Seismological Society of America","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1785/0120050820","issn":"00371106","usgsCitation":"Murray, J., and Langbein, J., 2006, Slip on the San Andreas fault at Parkfield, California, over two earthquake cycles, and the implications for seismic hazard: Bulletin of the Seismological Society of America, v. 96, no. 4 B, https://doi.org/10.1785/0120050820.","costCenters":[],"links":[{"id":209603,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1785/0120050820"},{"id":236256,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"96","issue":"4 B","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b914be4b08c986b319811","contributors":{"authors":[{"text":"Murray, J.","contributorId":94837,"corporation":false,"usgs":true,"family":"Murray","given":"J.","affiliations":[],"preferred":false,"id":419093,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Langbein, J.","contributorId":16990,"corporation":false,"usgs":true,"family":"Langbein","given":"J.","affiliations":[],"preferred":false,"id":419092,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028653,"text":"70028653 - 2006 - Research approach to teaching groundwater biodegradation in karst aquifers","interactions":[],"lastModifiedDate":"2012-03-12T17:20:43","indexId":"70028653","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Research approach to teaching groundwater biodegradation in karst aquifers","docAbstract":"TSU in partnership with the USGS has conducted extensive research regarding biode??gradation of contaminants in karst aquifers. This research resulted in the development of a numerical approach to modeling biodegradation of contaminants in karst aquifers that is taught to environmental engineering students in several steps. First, environmental engineering students are taught chemical-reaction engineering principles relating to a wide variety of environmental fate and transport issues. Second, as part of TSU's engineering course curriculum, students use a non-ideal flow laboratory reactor system and run a tracer study to establish residence time distribution (RTD). Next, the students couple that formula to a first-order biodegradation rate and predict the removal of a biodegradable contaminant as a function of residence time. Following this, students are shown data collected from karst bedrock wells that suggest that karst aquifers are analogous to non-ideal flow reactors. The students are challenged to develop rates of biodegradation through lab studies and use their results to predict biodegradaton at an actual contaminated karst site. Field studies are also conducted to determine the accuracy of the students' predictions. This academic approach teaches biodegradation processes, rate-kinetic processes, hydraulic processes and numerical principles. The students are able to experience how chemical engineering principles can be applied to other situations, such as, modeling biodegradation of contaminants in karst aquifers. This paper provides background on the chemical engineering principles and karst issues used in the research-enhanced curriculum. ?? American Society for Engineering Education, 2006.","largerWorkTitle":"ASEE Annual Conference and Exposition, Conference Proceedings","conferenceTitle":"113th Annual ASEE Conference and Exposition, 2006","conferenceDate":"18 June 2006 through 21 June 2006","conferenceLocation":"Chicago, IL","language":"English","usgsCitation":"King, L., Byl, T., and Painter, R., 2006, Research approach to teaching groundwater biodegradation in karst aquifers, <i>in</i> ASEE Annual Conference and Exposition, Conference Proceedings, Chicago, IL, 18 June 2006 through 21 June 2006.","numberOfPages":"12","costCenters":[],"links":[{"id":236779,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aa91be4b0c8380cd85c0e","contributors":{"authors":[{"text":"King, L.","contributorId":23744,"corporation":false,"usgs":true,"family":"King","given":"L.","email":"","affiliations":[],"preferred":false,"id":419072,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Byl, T.","contributorId":31967,"corporation":false,"usgs":true,"family":"Byl","given":"T.","email":"","affiliations":[],"preferred":false,"id":419073,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Painter, R.","contributorId":54393,"corporation":false,"usgs":true,"family":"Painter","given":"R.","email":"","affiliations":[],"preferred":false,"id":419074,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70028648,"text":"70028648 - 2006 - Influence of particle and surface quality on the vitrinite reflectance of dispersed organic matter: Comparative exercise using data from the qualifying system for reflectance analysis working group of ICCP","interactions":[],"lastModifiedDate":"2012-03-12T17:20:44","indexId":"70028648","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","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":"Influence of particle and surface quality on the vitrinite reflectance of dispersed organic matter: Comparative exercise using data from the qualifying system for reflectance analysis working group of ICCP","docAbstract":"The development of a qualifying system for reflectance analysis has been the scope of a working group within the International Committee for Coal and Organic Petrology (ICCP) since 1999, when J. Koch presented a system to qualify vitrinite particles according to their size, proximity to bright components and homogeneity of the surface. After some years of work aimed at improving the classification system using photomicrographs, it was decided to run a round robin exercise on microscopy samples. The classification system tested consists of three qualifiers ranging from excellent to low quality vitrinites with an additional option for unsuitable vitrinites. This paper reports on the results obtained by 22 analysts who were asked to measure random reflectance readings on vitrinite particles assigning to each reading a qualifier. Four samples containing different organic matter types and a variety of vitrinite occurrences have been analysed. Results indicated that the reflectance of particles classified as excellent, good or poor compared to the total average reflectance did not show trends to be systematically lower or higher for the four samples analysed. The differences in reflectance between the qualifiers for any given sample were lower than the scatter of vitrinite reflectance among participants. Overall, satisfactory results were obtained in determining the reflectance of vitrinite in the four samples analysed. This was so for samples having abundant and easy to identify vitrinites (higher plant-derived organic matter) as well as for samples with scarce and difficult to identify particles (samples with dominant marine-derived organic matter). The highest discrepancies were found for the organic-rich oil shales where the selection of the vitrinite population to measure proved to be particularly difficult. Special instructions should be provided for the analysis of this sort of samples. The certainty of identification of the vitrinite associated with the vitrinite reflectance values reported has been assessed through a reliability index which takes into account the number of readings and the coefficient of variation. The same statistical approach as that followed in the ICCP vitrinite reflectance accreditation program for single seam coals has been used for data evaluation. The results indicated low to medium dispersion for 17 out of 22 participants. This, combined with data from other sets of comparative analyses over a long period, is considered an encouraging result for the establishment of an accreditation program on vitrinite reflectance measurements in dispersed organic matter. ?? 2006 ICCP.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"International Journal of Coal Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.coal.2006.02.002","issn":"01665162","usgsCitation":"Borrego, A., Araujo, C., Balke, A., Cardott, B., Cook, A., David, P., Flores, D., Hamor-Vido, M., Hiltmann, W., Kalkreuth, W., Koch, J., Kommeren, C., Kus, J., Ligouis, B., Marques, M., Mendonca Filho, J., Misz, M., Oliveira, L., Pickel, W., Reimer, K., Ranasinghe, P., Suarez-Ruiz, I., and Vieth, A., 2006, Influence of particle and surface quality on the vitrinite reflectance of dispersed organic matter: Comparative exercise using data from the qualifying system for reflectance analysis working group of ICCP: International Journal of Coal Geology, v. 68, no. 3-4, p. 151-170, https://doi.org/10.1016/j.coal.2006.02.002.","startPage":"151","endPage":"170","numberOfPages":"20","costCenters":[],"links":[{"id":209922,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.coal.2006.02.002"},{"id":236678,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"68","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3b63e4b0c8380cd624b0","contributors":{"authors":[{"text":"Borrego, A.G.","contributorId":53583,"corporation":false,"usgs":true,"family":"Borrego","given":"A.G.","email":"","affiliations":[],"preferred":false,"id":419020,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Araujo, C.V.","contributorId":36738,"corporation":false,"usgs":true,"family":"Araujo","given":"C.V.","email":"","affiliations":[],"preferred":false,"id":419018,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Balke, A.","contributorId":78524,"corporation":false,"usgs":true,"family":"Balke","given":"A.","email":"","affiliations":[],"preferred":false,"id":419025,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cardott, B.","contributorId":25342,"corporation":false,"usgs":true,"family":"Cardott","given":"B.","email":"","affiliations":[],"preferred":false,"id":419015,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cook, A.C.","contributorId":43133,"corporation":false,"usgs":true,"family":"Cook","given":"A.C.","email":"","affiliations":[],"preferred":false,"id":419019,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"David, P.","contributorId":14180,"corporation":false,"usgs":true,"family":"David","given":"P.","email":"","affiliations":[],"preferred":false,"id":419013,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Flores, D.","contributorId":107915,"corporation":false,"usgs":true,"family":"Flores","given":"D.","email":"","affiliations":[],"preferred":false,"id":419032,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Hamor-Vido, M.","contributorId":25343,"corporation":false,"usgs":true,"family":"Hamor-Vido","given":"M.","affiliations":[],"preferred":false,"id":419016,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Hiltmann, W.","contributorId":71371,"corporation":false,"usgs":true,"family":"Hiltmann","given":"W.","email":"","affiliations":[],"preferred":false,"id":419024,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Kalkreuth, W.","contributorId":12255,"corporation":false,"usgs":true,"family":"Kalkreuth","given":"W.","email":"","affiliations":[],"preferred":false,"id":419012,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Koch, J.","contributorId":7065,"corporation":false,"usgs":false,"family":"Koch","given":"J.","affiliations":[],"preferred":false,"id":419010,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Kommeren, C.J.","contributorId":103852,"corporation":false,"usgs":true,"family":"Kommeren","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":419031,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Kus, J.","contributorId":98523,"corporation":false,"usgs":true,"family":"Kus","given":"J.","email":"","affiliations":[],"preferred":false,"id":419029,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Ligouis, B.","contributorId":59228,"corporation":false,"usgs":true,"family":"Ligouis","given":"B.","email":"","affiliations":[],"preferred":false,"id":419021,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Marques, M.","contributorId":102260,"corporation":false,"usgs":true,"family":"Marques","given":"M.","email":"","affiliations":[],"preferred":false,"id":419030,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Mendonca Filho, J.G.","contributorId":26128,"corporation":false,"usgs":true,"family":"Mendonca Filho","given":"J.G.","affiliations":[],"preferred":false,"id":419017,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Misz, M.","contributorId":68524,"corporation":false,"usgs":true,"family":"Misz","given":"M.","email":"","affiliations":[],"preferred":false,"id":419023,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Oliveira, L.","contributorId":98099,"corporation":false,"usgs":true,"family":"Oliveira","given":"L.","email":"","affiliations":[],"preferred":false,"id":419028,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Pickel, W.","contributorId":64014,"corporation":false,"usgs":true,"family":"Pickel","given":"W.","affiliations":[],"preferred":false,"id":419022,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"Reimer, K.","contributorId":14998,"corporation":false,"usgs":true,"family":"Reimer","given":"K.","email":"","affiliations":[],"preferred":false,"id":419014,"contributorType":{"id":1,"text":"Authors"},"rank":20},{"text":"Ranasinghe, P.","contributorId":92477,"corporation":false,"usgs":true,"family":"Ranasinghe","given":"P.","affiliations":[],"preferred":false,"id":419027,"contributorType":{"id":1,"text":"Authors"},"rank":21},{"text":"Suarez-Ruiz, I.","contributorId":10598,"corporation":false,"usgs":true,"family":"Suarez-Ruiz","given":"I.","affiliations":[],"preferred":false,"id":419011,"contributorType":{"id":1,"text":"Authors"},"rank":22},{"text":"Vieth, A.","contributorId":92036,"corporation":false,"usgs":true,"family":"Vieth","given":"A.","email":"","affiliations":[],"preferred":false,"id":419026,"contributorType":{"id":1,"text":"Authors"},"rank":23}]}}
,{"id":70028645,"text":"70028645 - 2006 - The ionospheric impact on GPS performance in southern polar region","interactions":[],"lastModifiedDate":"2012-03-12T17:20:44","indexId":"70028645","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The ionospheric impact on GPS performance in southern polar region","docAbstract":"The primary objective of this paper is to present the results of the study of the effects of varying ionospheric conditions on the GPS signal tracking in the southern polar region. In the first stage of this study, the data collected by the OSU/USGS team in October-November 2003 within the TAMDEF (Transantarctic Mountains Deformation) network were used together with some IGS Antarctic stations to study the effect of severe ionospheric storms on GPS hardware. Note that TAMDEF is a joint USGS/OSU project with the primary objective of measuring crustal motion in the Transantarctic Mountains of Southern Victoria Land using GPS techniques. This study included ten Antarctic stations equipped with different dual-frequency GPS hardware, and the data were evaluated for two 24-hour periods of severe ionospheric storm (2003/10/29) and moderate ionospheric conditions (minor storm of 2003/11/11). The results of this study were presented at the LAG Assembly in Cairns, Australia (Grejner-Brzezinska et al., 2005). Additional tests, in a more controlled environment, were carried out at the US Antarctic station, McMurdo, between January 10 and February 6, 2006, under varying ionospheric conditions, where several different types of receivers were connected to the same antenna located on the rooftop of the Crary Laboratory (the primary test site). In this scenario, each antenna was subject to identical ionospheric effects during each day of the test, and no spatial decorrelation effects were present, as seen in the previous study, due to the spatial separation of the receivers tested. It should be noted, however, that no moderate or severe ionospheric storms occurred during the experiment, so, unfortunately, this type of conditions was not tested here. The test was repeated with different receivers connected to different antenna types; a total of four 5-day sessions were carried out. The following receiver types were used at the primary site: Trimble 5700, Ashtech Z-Surveyor, JNS Euro-80 and Novatel DL-4, with the following antennas: Trimble Zephyr Geodetic, Ashtech D/M and Ashtech E/M chokering. In addition, data collected by the MCM4 IGS station, MCMD UNAVCO station, and CRAR USGS station, all located within 300 m from the primary test site, were used in the analyses. These stations were equipped with the following receiver/antenna combinations: ADA SNR-12/AOAD/MJT chokering (MCM4), Trimble NETRS/AOAD/MJT chokering (MCMD), and TPS ODYSEY_E/JPSREGANT_DD_E (CRAR). The UNAVCO TEQC software was used to carry out the analyses. Depending on the data sampling rate and the mask angle, the expected numbers of observations per receiver/satellite were compared to the actual number of measurements collected during the ionospheric events, with a special emphasis on L2 data. A total number of cycle slips and losses of lock were computed and compared among the hardware types. The results presented here indicate that there is no significant effects on the GPS receivers during minor ionospheric storms (Kp<5). However, the results reported in ibid, indicate significant differences in the hardware performance under severe ionospheric storms. Thus, careful hardware selection is needed to assure data quality/continuity when observations may be affected by severe ionospheric disturbances, while under calm to minor ionospheric activity level there is no significant difference in performance among the hardware tested here.","largerWorkTitle":"Proceedings of the Institute of Navigation - 19th International Technical Meeting of the Satellite Division, ION GNSS 2006","conferenceTitle":"Institute of Navigation - 19th International Technical Meeting of the Satellite Division, ION GNSS 2006","conferenceDate":"26 September 2006 through 29 September 2006","conferenceLocation":"Fort Worth, TX","language":"English","usgsCitation":"Hong, C., Grejner-Brzezinska, D.A., Arslan, N., Willis, M., and Hothem, L., 2006, The ionospheric impact on GPS performance in southern polar region, <i>in</i> Proceedings of the Institute of Navigation - 19th International Technical Meeting of the Satellite Division, ION GNSS 2006, v. 3, Fort Worth, TX, 26 September 2006 through 29 September 2006, p. 1418-1426.","startPage":"1418","endPage":"1426","numberOfPages":"9","costCenters":[],"links":[{"id":236605,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bad64e4b08c986b323bab","contributors":{"authors":[{"text":"Hong, C.-K.","contributorId":90526,"corporation":false,"usgs":true,"family":"Hong","given":"C.-K.","email":"","affiliations":[],"preferred":false,"id":419004,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grejner-Brzezinska, D. A.","contributorId":42772,"corporation":false,"usgs":true,"family":"Grejner-Brzezinska","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":419001,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Arslan, N.","contributorId":86557,"corporation":false,"usgs":true,"family":"Arslan","given":"N.","email":"","affiliations":[],"preferred":false,"id":419003,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Willis, M.","contributorId":82910,"corporation":false,"usgs":true,"family":"Willis","given":"M.","email":"","affiliations":[],"preferred":false,"id":419002,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hothem, L.","contributorId":13801,"corporation":false,"usgs":true,"family":"Hothem","given":"L.","email":"","affiliations":[],"preferred":false,"id":419000,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70028644,"text":"70028644 - 2006 - Inhibition of coral recruitment by macroalgae and cyanobacteria","interactions":[],"lastModifiedDate":"2012-03-12T17:20:59","indexId":"70028644","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2663,"text":"Marine Ecology Progress Series","active":true,"publicationSubtype":{"id":10}},"title":"Inhibition of coral recruitment by macroalgae and cyanobacteria","docAbstract":"Coral recruitment is a key process in the maintenance and recovery of coral reef ecosystems. While intense competition between coral and algae is often assumed on reefs that have undergone phase shifts from coral to algal dominance, data examining the competitive interactions involved, particularly during the larval and immediate post-settlement stage, are scarce. Using a series of field and outdoor seawater table experiments, we tested the hypothesis that common species of macroalgae and cyanobacteria inhibit coral recruitment. We examined the effects of Lyngbya spp., Dictyota spp., Lobophora variegata (J. V. Lamouroux) Womersley, and Chondrophycus poiteaui (J. V. Lamouroux) Nam (formerly Laurencia poiteaui) on the recruitment success of Porites astreoides larvae. All species but C. poiteaui caused either recruitment inhibition or avoidance behavior in P. astreoides larvae, while L. confervoides and D. menstrualis significantly increased mortality rates of P. astreoides recruits. We also tested the effect of some of these macrophytes on larvae of the gorgonian octocoral Briareum asbestinum. Exposure to Lyngbya majuscula reduced survival and recruitment in the octocoral larvae. Our results provide evidence that algae and cyanobacteria use tactics beyond space occupation to inhibit coral recruitment. On reefs experiencing phase shifts or temporary algal blooms, the restocking of adult coral populations may be slowed due to recruitment inhibition, thereby perpetuating reduced coral cover and limiting coral community recovery. ?? Inter-Research 2006.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Ecology Progress Series","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.3354/meps323107","issn":"01718630","usgsCitation":"Kuffner, I., Walters, L., Becerro, M., Paul, V., Ritson-Williams, R., and Beach, K., 2006, Inhibition of coral recruitment by macroalgae and cyanobacteria: Marine Ecology Progress Series, v. 323, p. 107-117, https://doi.org/10.3354/meps323107.","startPage":"107","endPage":"117","numberOfPages":"11","costCenters":[],"links":[{"id":477687,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.3354/meps323107","text":"External Repository"},{"id":209842,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.3354/meps323107"},{"id":236573,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"323","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3bd7e4b0c8380cd62878","contributors":{"authors":[{"text":"Kuffner, I. B.","contributorId":40328,"corporation":false,"usgs":true,"family":"Kuffner","given":"I. B.","affiliations":[],"preferred":false,"id":418996,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walters, L.J.","contributorId":107081,"corporation":false,"usgs":true,"family":"Walters","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":418999,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Becerro, M.A.","contributorId":18956,"corporation":false,"usgs":true,"family":"Becerro","given":"M.A.","affiliations":[],"preferred":false,"id":418994,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Paul, V.J.","contributorId":40782,"corporation":false,"usgs":true,"family":"Paul","given":"V.J.","email":"","affiliations":[],"preferred":false,"id":418997,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ritson-Williams, R.","contributorId":88546,"corporation":false,"usgs":true,"family":"Ritson-Williams","given":"R.","affiliations":[],"preferred":false,"id":418998,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Beach, K.S.","contributorId":37134,"corporation":false,"usgs":true,"family":"Beach","given":"K.S.","email":"","affiliations":[],"preferred":false,"id":418995,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70028642,"text":"70028642 - 2006 - Pelagic seabird surveys in the Tuamotu and Gambier Archipelagos, French Polynesia","interactions":[],"lastModifiedDate":"2018-08-21T13:08:10","indexId":"70028642","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2675,"text":"Marine Ornithology: Journal of Seabird Research and Conservation","onlineIssn":"2074-1235","printIssn":"1018-3337","active":true,"publicationSubtype":{"id":10}},"title":"Pelagic seabird surveys in the Tuamotu and Gambier Archipelagos, French Polynesia","docAbstract":"We conducted pelagic seabird surveys in the Gambier and Tuamotu Archipelagos in the southeastern Pacific Ocean totaling 40 hours during 7-27 March 2003 and 22.5 hours during 22-27 July 2001. We used a 300-m-wide strip transect to estimate seabird density, and we estimated relative abundance of birds at all distances. In 2001, we observed a total of 326 birds of 18 species. The mean relative abundance of all birds was 14.3 ?? 3.1/h. Red-footed Booby Sula sula was the most abundant species (5.6/h), followed by White Tern Gygis alba (3.4/h), and Great Crested or Swift Tern Sterna bergii (1.2/h). In 2003, we observed a total of 1463 birds of 25 species. The mean relative abundance of all birds was 36.6 ?? 11.4/h and the mean density of all birds was 4.14 ?? 0.72/km2. Brown Noddy Anous stolidus was the most abundant species (17.6/h, 1.5/km2), followed by White Tern (8.4/h, 1.3/km2), and Red-footed Booby (4.6/h, 0.8/km2). Several globally or locally rare species were observed infrequently, including Phoenix Petrel Pterodroma alba (0.1/h, 0.03/km2). Distribution of birds was uneven, with long periods of no birds punctuated by occasional feeding flocks. In 2003, species diversity was related to length of observation period, with more species observed on longer segments (r2 = 0.58, F1.5 = 6.03, P = 0.05). Although the duration and extent of our surveys were limited, these data are valuable because little published information is available on pelagic seabirds in southeastern Polynesia.","language":"English","publisher":"Pacific Seabird Group","issn":"10183337","usgsCitation":"Vanderwerf, E.A., Pierce, R.J., Gill, V., Wragg, G., Raust, P., and Tibbitts, T.L., 2006, Pelagic seabird surveys in the Tuamotu and Gambier Archipelagos, French Polynesia: Marine Ornithology: Journal of Seabird Research and Conservation, v. 34, no. 1, p. 65-70.","productDescription":"6 p.","startPage":"65","endPage":"70","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"links":[{"id":236538,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":337053,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.marineornithology.org/content/get.cgi?rn=684"}],"country":"France","state":"French Polynesia","otherGeospatial":"Gambier Archipelago, Tuamotu Archipelago","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -150,\n              -10\n            ],\n            [\n              -134,\n              -10\n            ],\n            [\n              -134,\n              -25\n            ],\n            [\n              -150,\n              -25\n            ],\n            [\n              -150,\n              -10\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"34","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a763ce4b0c8380cd77fd7","contributors":{"authors":[{"text":"Vanderwerf, Eric A.","contributorId":104689,"corporation":false,"usgs":false,"family":"Vanderwerf","given":"Eric","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":418988,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pierce, Ray J.","contributorId":16635,"corporation":false,"usgs":false,"family":"Pierce","given":"Ray","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":418984,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gill, Verena A.","contributorId":140658,"corporation":false,"usgs":false,"family":"Gill","given":"Verena A.","affiliations":[{"id":6678,"text":"U.S. Fish and Wildlife Service, Alaska Maritime National Wildlife Refuge","active":true,"usgs":false}],"preferred":false,"id":418986,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wragg, Graham","contributorId":8272,"corporation":false,"usgs":false,"family":"Wragg","given":"Graham","email":"","affiliations":[],"preferred":false,"id":418983,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Raust, Philippe","contributorId":46288,"corporation":false,"usgs":false,"family":"Raust","given":"Philippe","email":"","affiliations":[],"preferred":false,"id":418987,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Tibbitts, T. Lee 0000-0002-0290-7592 ltibbitts@usgs.gov","orcid":"https://orcid.org/0000-0002-0290-7592","contributorId":140455,"corporation":false,"usgs":true,"family":"Tibbitts","given":"T.","email":"ltibbitts@usgs.gov","middleInitial":"Lee","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":false,"id":418985,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70028635,"text":"70028635 - 2006 - Importance of spatial autocorrelation in modeling bird distributions at a continental scale","interactions":[],"lastModifiedDate":"2012-03-12T17:20:59","indexId":"70028635","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1445,"text":"Ecography","active":true,"publicationSubtype":{"id":10}},"title":"Importance of spatial autocorrelation in modeling bird distributions at a continental scale","docAbstract":"Spatial autocorrelation in species' distributions has been recognized as inflating the probability of a type I error in hypotheses tests, causing biases in variable selection, and violating the assumption of independence of error terms in models such as correlation or regression. However, it remains unclear whether these problems occur at all spatial resolutions and extents, and under which conditions spatially explicit modeling techniques are superior. Our goal was to determine whether spatial models were superior at large extents and across many different species. In addition, we investigated the importance of purely spatial effects in distribution patterns relative to the variation that could be explained through environmental conditions. We studied distribution patterns of 108 bird species in the conterminous United States using ten years of data from the Breeding Bird Survey. We compared the performance of spatially explicit regression models with non-spatial regression models using Akaike's information criterion. In addition, we partitioned the variance in species distributions into an environmental, a pure spatial and a shared component. The spatially-explicit conditional autoregressive regression models strongly outperformed the ordinary least squares regression models. In addition, partialling out the spatial component underlying the species' distributions showed that an average of 17% of the explained variation could be attributed to purely spatial effects independent of the spatial autocorrelation induced by the underlying environmental variables. We concluded that location in the range and neighborhood play an important role in the distribution of species. Spatially explicit models are expected to yield better predictions especially for mobile species such as birds, even in coarse-grained models with a large extent. ?? Ecography.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecography","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.2006.0906-7590.04621.x","issn":"09067590","usgsCitation":"Bahn, V., O’Connor, R., and Krohn, W., 2006, Importance of spatial autocorrelation in modeling bird distributions at a continental scale: Ecography, v. 29, no. 6, p. 835-844, https://doi.org/10.1111/j.2006.0906-7590.04621.x.","startPage":"835","endPage":"844","numberOfPages":"10","costCenters":[],"links":[{"id":209734,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.2006.0906-7590.04621.x"},{"id":236431,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"6","noUsgsAuthors":false,"publicationDate":"2006-12-13","publicationStatus":"PW","scienceBaseUri":"505a3943e4b0c8380cd61876","contributors":{"authors":[{"text":"Bahn, V.","contributorId":23741,"corporation":false,"usgs":true,"family":"Bahn","given":"V.","email":"","affiliations":[],"preferred":false,"id":418952,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Connor, R.J.","contributorId":37861,"corporation":false,"usgs":true,"family":"O’Connor","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":418953,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krohn, W.B.","contributorId":64355,"corporation":false,"usgs":true,"family":"Krohn","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":418954,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70028630,"text":"70028630 - 2006 - The importance of physiological ecology in conservation biology","interactions":[],"lastModifiedDate":"2012-03-12T17:20:56","indexId":"70028630","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The importance of physiological ecology in conservation biology","docAbstract":"Many of the threats to the persistence of populations of sensitive species have physiological or pathological mechanisms, and those mechanisms are best understood through the inherently integrative discipline of physiological ecology. The desert tortoise was listed under the Endangered Species Act largely due to a newly recognized upper respiratory disease thought to cause mortality in individuals and severe declines in populations. Numerous hypotheses about the threats to the persistence of desert tortoise populations involve acquisition of nutrients, and its connection to stress and disease. The nutritional wisdom hypothesis posits that animals should forage not for particular food items, but instead, for particular nutrients such as calcium and phosphorus used in building bones. The optimal foraging hypothesis suggests that, in circumstances of resource abundance, tortoises should forage as dietary specialists as a means of maximizing intake of resources. The optimal digestion hypothesis suggests that tortoises should process ingesta in ways that regulate assimilation rate. Finally, the cost-of-switching hypothesis suggests that herbivores, like the desert tortoise, should avoid switching food types to avoid negatively affecting the microbe community responsible for fermenting plants into energy and nutrients. Combining hypotheses into a resource acquisition theory leads to novel predictions that are generally supported by data presented here. Testing hypotheses, and synthesizing test results into a theory, provides a robust scientific alternative to the popular use of untested hypotheses and unanalyzed data to assert the needs of species. The scientific approach should focus on hypotheses concerning anthropogenic modifications of the environment that impact physiological processes ultimately important to population phenomena. We show how measurements of such impacts as nutrient starvation, can cause physiological stress, and that the endocrine mechanisms involved with stress can result in disease. Finally, our new syntheses evince a new hypothesis. Free molecules of the stress hormone corticosterone can inhibit immunity, and the abundance of \"free corticosterone\" in the blood (thought to be the active form of the hormone) is regulated when the corticosterone molecules combine with binding globulins. The sex hormone, testosterone, combines with the same binding globulin. High levels of testosterone, naturally occurring in the breeding season, may be further enhanced in populations at high densities, and the resulting excess testosterone may compete with binding globulins, thereby releasing corticosterone and reducing immunity to disease. This sequence could result in physiological and pathological phenomena leading to population cycles with a period that would be essentially impossible to observe in desert tortoise. Such cycles could obscure population fluctuations of anthropogenic origin. ?? 2006 The Author(s).","largerWorkTitle":"Integrative and Comparative Biology","language":"English","doi":"10.1093/icb/icl054","issn":"15407063","usgsCitation":"Tracy, C., Nussear, K., Esque, T., Dean-Bradley, K., DeFalco, L., Castle, K., Zimmerman, L., Espinoza, R., and Barber, A., 2006, The importance of physiological ecology in conservation biology, <i>in</i> Integrative and Comparative Biology, v. 46, no. 6, p. 1191-1205, https://doi.org/10.1093/icb/icl054.","startPage":"1191","endPage":"1205","numberOfPages":"15","costCenters":[],"links":[{"id":477395,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1093/icb/icl054","text":"Publisher Index Page"},{"id":209690,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1093/icb/icl054"},{"id":236365,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"6","noUsgsAuthors":false,"publicationDate":"2006-10-11","publicationStatus":"PW","scienceBaseUri":"505bacfbe4b08c986b3238c3","contributors":{"authors":[{"text":"Tracy, C.R.","contributorId":73524,"corporation":false,"usgs":true,"family":"Tracy","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":418912,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nussear, K.E.","contributorId":80227,"corporation":false,"usgs":true,"family":"Nussear","given":"K.E.","affiliations":[],"preferred":false,"id":418914,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Esque, T. C. 0000-0002-4166-6234","orcid":"https://orcid.org/0000-0002-4166-6234","contributorId":76250,"corporation":false,"usgs":true,"family":"Esque","given":"T. C.","affiliations":[],"preferred":false,"id":418913,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dean-Bradley, K.","contributorId":35268,"corporation":false,"usgs":true,"family":"Dean-Bradley","given":"K.","affiliations":[],"preferred":false,"id":418908,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"DeFalco, L.A.","contributorId":46032,"corporation":false,"usgs":true,"family":"DeFalco","given":"L.A.","affiliations":[],"preferred":false,"id":418909,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Castle, K.T.","contributorId":60592,"corporation":false,"usgs":true,"family":"Castle","given":"K.T.","email":"","affiliations":[],"preferred":false,"id":418911,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Zimmerman, L.C.","contributorId":55784,"corporation":false,"usgs":true,"family":"Zimmerman","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":418910,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Espinoza, R.E.","contributorId":9048,"corporation":false,"usgs":true,"family":"Espinoza","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":418907,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Barber, A.M.","contributorId":6238,"corporation":false,"usgs":true,"family":"Barber","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":418906,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70028629,"text":"70028629 - 2006 - Denitrification in nitrate-rich streams: Application of N2:Ar and 15N-tracer methods in intact cores","interactions":[],"lastModifiedDate":"2018-10-26T10:47:56","indexId":"70028629","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1450,"text":"Ecological Applications","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Denitrification in nitrate-rich streams: Application of N<sub>2</sub>:Ar and <sup>15</sup>N-tracer methods in intact cores","title":"Denitrification in nitrate-rich streams: Application of N2:Ar and 15N-tracer methods in intact cores","docAbstract":"<div class=\"article-section__content en main\"><p>Rates of benthic denitrification were measured using two techniques, membrane inlet mass spectrometry (MIMS) and isotope ratio mass spectrometry (IRMS), applied to sediment cores from two NO<sub>3</sub><sup>−</sup>‐rich streams draining agricultural land in the upper Mississippi River Basin. Denitrification was estimated simultaneously from measurements of N<sub>2</sub>:Ar (MIMS) and<span>&nbsp;</span><sup>15</sup>N[N<sub>2</sub>] (IRMS) after the addition of low‐level<span>&nbsp;</span><sup>15</sup>NO<sub>3</sub><sup>−</sup><span>&nbsp;</span>tracer (<sup>15</sup>N:N = 0.03–0.08) in stream water overlying intact sediment cores. Denitrification rates ranged from about 0 to 4400 μmol N·m<sup>−2</sup>·h<sup>−1</sup><span>&nbsp;</span>in Sugar Creek and from 0 to 1300 μmol N·m<sup>−2</sup>·h<sup>−1</sup><span>&nbsp;</span>in Iroquois River, the latter of which possesses greater streamflow discharge and a more homogeneous streambed and water column. Within the uncertainties of the two techniques, there is good agreement between the MIMS and IRMS results, which indicates that the production of N<sub>2</sub><span>&nbsp;</span>by the coupled process of nitrification/denitrification was relatively unimportant and surface‐water NO<sub>3</sub><sup>−</sup><span>&nbsp;</span>was the dominant source of NO<sub>3</sub><sup>−</sup><span>&nbsp;</span>for benthic denitrification in these streams. Variation in stream NO<sub>3</sub><sup>−</sup><span>&nbsp;</span>concentration (from about 20 μmol/L during low discharge to 1000 μmol/L during high discharge) was a significant control of benthic denitrification rates, judging from the more abundant MIMS data. The interpretation that NO<sub>3</sub><sup>−</sup><span>&nbsp;</span>concentration directly affects denitrification rate was corroborated by increased rates of denitrification in cores amended with NO<sub>3</sub><sup>−</sup>. Denitrification in Sugar Creek removed ≤11% per day of the in‐stream NO<sub>3</sub><sup>−</sup><span>&nbsp;</span>in late spring and removed roughly 15–20% in late summer. The fraction of NO<sub>3</sub><sup>−</sup><span>&nbsp;</span>removed in Iroquois River was less than that of Sugar Creek. Although benthic denitrification rates were relatively high during periods of high stream flow, when NO<sub>3</sub>concentrations were also high, the increase in benthic denitrification could not compensate for the much larger increase in stream NO<sub>3</sub><sup>−</sup><span>&nbsp;</span>fluxes during high flow. Consequently, fractional NO<sub>3</sub><sup>−</sup><span>&nbsp;</span>losses were relatively low during high flow.</p></div>","language":"English","publisher":"Ecological Society of America","doi":"10.1890/1051-0761(2006)016[2191:DINSAO]2.0.CO;2","issn":"10510761","usgsCitation":"Smith, L.K., Voytek, M., Böhlke, J., and Harvey, J., 2006, Denitrification in nitrate-rich streams: Application of N2:Ar and 15N-tracer methods in intact cores: Ecological Applications, v. 16, no. 6, p. 2191-2207, https://doi.org/10.1890/1051-0761(2006)016[2191:DINSAO]2.0.CO;2.","productDescription":"17 p.","startPage":"2191","endPage":"2207","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":236329,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":209660,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1890/1051-0761(2006)016[2191:DINSAO]2.0.CO;2"}],"volume":"16","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fe99e4b0c8380cd4ee08","contributors":{"authors":[{"text":"Smith, Lesley K.","contributorId":82657,"corporation":false,"usgs":true,"family":"Smith","given":"Lesley","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":418904,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Voytek, M.A.","contributorId":44272,"corporation":false,"usgs":true,"family":"Voytek","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":418903,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Böhlke, J.K. 0000-0001-5693-6455","orcid":"https://orcid.org/0000-0001-5693-6455","contributorId":96696,"corporation":false,"usgs":true,"family":"Böhlke","given":"J.K.","affiliations":[],"preferred":false,"id":418905,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Harvey, J. W. 0000-0002-2654-9873","orcid":"https://orcid.org/0000-0002-2654-9873","contributorId":39725,"corporation":false,"usgs":true,"family":"Harvey","given":"J. W.","affiliations":[],"preferred":false,"id":418902,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70028626,"text":"70028626 - 2006 - Evaluating minerals of environmental concern using spectroscopy","interactions":[],"lastModifiedDate":"2012-03-12T17:20:56","indexId":"70028626","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Evaluating minerals of environmental concern using spectroscopy","docAbstract":"Imaging spectroscopy has been successfully used to aid researchers in characterizing potential environmental impacts posed by acid-rock drainage, ore-processing dust on mangroves, and asbestos in serpentine mineral deposits and urban dust. Many of these applications synergistically combine field spectroscopy with remote sensing data, thus allowing more-precise data calibration, spectral analysis of the data, and verification of mapping. The increased accuracy makes these environmental evaluation tools efficient because they can be used to focus field work on those areas most critical to the research effort. The use of spectroscopy to evaluate minerals of environmental concern pushes current imaging spectrometer technology to its limits; we present laboratory results that indicate the direction for future designs of imaging spectrometers.","largerWorkTitle":"International Geoscience and Remote Sensing Symposium (IGARSS)","conferenceTitle":"2006 IEEE International Geoscience and Remote Sensing Symposium, IGARSS","conferenceDate":"31 July 2006 through 4 August 2006","conferenceLocation":"Denver, CO","language":"English","doi":"10.1109/IGARSS.2006.515","isbn":"0780395107; 9780780395107","usgsCitation":"Swayze, G., Clark, R.N., Higgins, C., Kokaly, R., Livo, K., Hoefen, T., Ong, C., and Kruse, F., 2006, Evaluating minerals of environmental concern using spectroscopy, <i>in</i> International Geoscience and Remote Sensing Symposium (IGARSS), Denver, CO, 31 July 2006 through 4 August 2006, p. 1990-1991, https://doi.org/10.1109/IGARSS.2006.515.","startPage":"1990","endPage":"1991","numberOfPages":"2","costCenters":[],"links":[{"id":209631,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1109/IGARSS.2006.515"},{"id":236292,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0be9e4b0c8380cd52936","contributors":{"authors":[{"text":"Swayze, G.A. 0000-0002-1814-7823","orcid":"https://orcid.org/0000-0002-1814-7823","contributorId":21570,"corporation":false,"usgs":true,"family":"Swayze","given":"G.A.","affiliations":[],"preferred":false,"id":418880,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, R. N.","contributorId":6568,"corporation":false,"usgs":true,"family":"Clark","given":"R.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":418878,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Higgins, C.T.","contributorId":42814,"corporation":false,"usgs":true,"family":"Higgins","given":"C.T.","email":"","affiliations":[],"preferred":false,"id":418884,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kokaly, R.F. 0000-0003-0276-7101","orcid":"https://orcid.org/0000-0003-0276-7101","contributorId":42381,"corporation":false,"usgs":true,"family":"Kokaly","given":"R.F.","affiliations":[],"preferred":false,"id":418883,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Livo, K. Eric 0000-0001-7331-8130","orcid":"https://orcid.org/0000-0001-7331-8130","contributorId":27327,"corporation":false,"usgs":true,"family":"Livo","given":"K. Eric","affiliations":[],"preferred":false,"id":418881,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hoefen, T.M. 0000-0002-3083-5987","orcid":"https://orcid.org/0000-0002-3083-5987","contributorId":18143,"corporation":false,"usgs":true,"family":"Hoefen","given":"T.M.","affiliations":[],"preferred":false,"id":418879,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ong, C.","contributorId":96071,"corporation":false,"usgs":true,"family":"Ong","given":"C.","email":"","affiliations":[],"preferred":false,"id":418885,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Kruse, F.A.","contributorId":30676,"corporation":false,"usgs":true,"family":"Kruse","given":"F.A.","email":"","affiliations":[],"preferred":false,"id":418882,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
]}