{"pageNumber":"1885","pageRowStart":"47100","pageSize":"25","recordCount":184563,"records":[{"id":70236312,"text":"70236312 - 2010 - Monitoring land-surface deformation on Bicycle Lake playa, Fort Irwin, California, USA","interactions":[],"lastModifiedDate":"2022-09-01T14:46:53.207125","indexId":"70236312","displayToPublicDate":"2010-10-01T09:34:03","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Monitoring land-surface deformation on Bicycle Lake playa, Fort Irwin, California, USA","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Eighth International Symposium on Land Subsidence","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"8th International Symposium on Land Subsidence","conferenceDate":"October 17-22, 2010","conferenceLocation":"Querétaro, Mexico","language":"English","publisher":"International Association of Hydrological Sciences Press","usgsCitation":"Densmore, J.N., Ellett, K., Howle, J.F., Carpenter, M.C., and Sneed, M., 2010, Monitoring land-surface deformation on Bicycle Lake playa, Fort Irwin, California, USA, <i>in</i> Eighth International Symposium on Land Subsidence, Querétaro, Mexico, October 17-22, 2010, p. 39-43.","productDescription":"5 p.","startPage":"39","endPage":"43","costCenters":[],"links":[{"id":406065,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","city":"Fort Irwin","otherGeospatial":"Bicycle Lake playa, Mojave Desert","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.63274765014648,\n              35.263842186385766\n            ],\n            [\n              -116.62141799926756,\n              35.266224903216894\n            ],\n            [\n              -116.61523818969727,\n              35.27288212294965\n            ],\n            [\n              -116.6113758087158,\n              35.28381279171024\n            ],\n            [\n              -116.60751342773436,\n              35.29544252406548\n            ],\n            [\n              -116.62442207336426,\n              35.29621310995517\n            ],\n            [\n              -116.64570808410643,\n              35.28276182997691\n            ],\n            [\n              -116.65145874023438,\n              35.27302226906422\n            ],\n            [\n              -116.64931297302246,\n              35.26965869539278\n            ],\n            [\n              -116.63678169250488,\n              35.266645375384165\n            ],\n            [\n              -116.63274765014648,\n              35.263842186385766\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Densmore, Jill N. 0000-0002-5345-6613 jidensmo@usgs.gov","orcid":"https://orcid.org/0000-0002-5345-6613","contributorId":197491,"corporation":false,"usgs":true,"family":"Densmore","given":"Jill","email":"jidensmo@usgs.gov","middleInitial":"N.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":850570,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ellett, Kevin","contributorId":66398,"corporation":false,"usgs":true,"family":"Ellett","given":"Kevin","affiliations":[],"preferred":false,"id":850571,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Howle, James F. 0000-0003-0491-6203 jfhowle@usgs.gov","orcid":"https://orcid.org/0000-0003-0491-6203","contributorId":2225,"corporation":false,"usgs":true,"family":"Howle","given":"James","email":"jfhowle@usgs.gov","middleInitial":"F.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":850572,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Carpenter, Michael C. mcarpent@usgs.gov","contributorId":3977,"corporation":false,"usgs":true,"family":"Carpenter","given":"Michael","email":"mcarpent@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":850573,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sneed, Michelle 0000-0002-8180-382X micsneed@usgs.gov","orcid":"https://orcid.org/0000-0002-8180-382X","contributorId":155,"corporation":false,"usgs":true,"family":"Sneed","given":"Michelle","email":"micsneed@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":850574,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70209190,"text":"70209190 - 2010 - Historical seismograms for unravelling a mysterious earthquake: The 1907 Sumatra Earthquake","interactions":[],"lastModifiedDate":"2020-03-23T09:35:19","indexId":"70209190","displayToPublicDate":"2010-10-01T09:24:57","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1803,"text":"Geophysical Journal International","active":true,"publicationSubtype":{"id":10}},"title":"Historical seismograms for unravelling a mysterious earthquake: The 1907 Sumatra Earthquake","docAbstract":"<p>History of instrumental seismology is short. Seismograms are available only for a little more than 100 years; high-quality seismograms are available only for the last 50 years and the seismological database is very limited in time. To extend the database, seismograms of old events are of vital importance. Many unusual earthquakes are known to have occurred, but their seismological characteristics are poorly known. The 1907 Sumatra earthquake is one of them (1907 January 4,<span>&nbsp;</span><i>M</i>= 7.6). Gutenberg and Richter located this event in the outer-rise area of the Sunda arc. This earthquake is known to be anomalous because of its extensive tsunami, which is disproportionate of its magnitude. The tsunami affected the coastal areas over 950 km along the Sumatran coast. We investigated this earthquake using the historical seismograms we could collect from several seismological observatories. We examined the<span>&nbsp;</span><i>P</i>-wave arrival times listed in the Strassburg Bulletin (1912) and other station bulletins. The scatter of the Observed−Computed traveltime residuals ranges from –30 to 30 s, too large to locate the event accurately. The uncertainty of the epicentre estimated from an S-P grid-search relocation study is at least 1° (∼110 km). We interpreted the Omori seismograms from Osaka, Mizusawa and Tokyo, and the Wiechert seismograms from Göttingen and Uppsala by comparing them with the seismograms simulated from modern broad-band seismograms of the 2002, 2008 and two 2010 Sumatra earthquakes which occurred near the 1907 earthquake. From the amplitude of Rayleigh waves recorded on the Omori seismograms we conclude that the magnitude of the 1907 earthquake at about 30 to 40 s is about 7.8 (i.e. 7.5 to 8.0). The<span>&nbsp;</span><i>SH</i><span>&nbsp;</span>waveforms recorded on the Göttingen and Uppsala seismograms suggest that the 1907 earthquake is a thrust earthquake at a shallow depth around 30 km. The most likely scenario is that the 1907 earthquake initiated on the subduction interface, and slowly ruptured up-dip into the shallow sediments and caused the extensive tsunami. Although their quantity and quality are limited, historical seismograms provide key quantitative information about old events that cannot be obtained otherwise. This underscores the importance of preserving historical seismograms.</p>","language":"English","publisher":"Oxford Academic ","doi":"10.1111/j.1365-246X.2010.04731.x","usgsCitation":"Kanamori, H., Rivera, L., and Lee, W., 2010, Historical seismograms for unravelling a mysterious earthquake: The 1907 Sumatra Earthquake: Geophysical Journal International, v. 183, no. 1, p. 358-374, https://doi.org/10.1111/j.1365-246X.2010.04731.x.","productDescription":"17 p.","startPage":"358","endPage":"374","costCenters":[],"links":[{"id":475662,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1365-246x.2010.04731.x","text":"Publisher Index Page"},{"id":373435,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Indonesia 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Hiroo","contributorId":106120,"corporation":false,"usgs":true,"family":"Kanamori","given":"Hiroo","affiliations":[],"preferred":false,"id":785303,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rivera, Luis","contributorId":102367,"corporation":false,"usgs":true,"family":"Rivera","given":"Luis","email":"","affiliations":[],"preferred":false,"id":785304,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lee, W.H.K.","contributorId":35303,"corporation":false,"usgs":true,"family":"Lee","given":"W.H.K.","affiliations":[],"preferred":false,"id":785305,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70236311,"text":"70236311 - 2010 - Preface: Developments in land subsidence investigation","interactions":[],"lastModifiedDate":"2022-09-01T14:30:11.948251","indexId":"70236311","displayToPublicDate":"2010-10-01T09:21:06","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Preface: Developments in land subsidence investigation","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Eighth International Symposium on Land Subsidence","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"8th International Symposium on Land Subsidence,","conferenceDate":"October 17-22, 2010","conferenceLocation":"Querétaro, Mexico","language":"English","publisher":"International Association of Hydrological Sciences Press","usgsCitation":"Carreon-Freyre, D., Cerca, M., and Galloway, D.L., 2010, Preface: Developments in land subsidence investigation, <i>in</i> Eighth International Symposium on Land Subsidence, Querétaro, Mexico, October 17-22, 2010, p. v-viii.","productDescription":"4 p.","startPage":"v","endPage":"viii","costCenters":[],"links":[{"id":406064,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Carreon-Freyre, Dora","contributorId":203530,"corporation":false,"usgs":false,"family":"Carreon-Freyre","given":"Dora","email":"","affiliations":[{"id":36644,"text":"Centro de Geociencias, Universidad Nacional Autónoma de México, Campus Juriquilla, Queretaro, Mexico","active":true,"usgs":false}],"preferred":false,"id":850567,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cerca, Mariano","contributorId":296082,"corporation":false,"usgs":false,"family":"Cerca","given":"Mariano","email":"","affiliations":[],"preferred":false,"id":850568,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Galloway, Devin L. 0000-0003-0904-5355 dlgallow@usgs.gov","orcid":"https://orcid.org/0000-0003-0904-5355","contributorId":679,"corporation":false,"usgs":true,"family":"Galloway","given":"Devin","email":"dlgallow@usgs.gov","middleInitial":"L.","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true},{"id":5078,"text":"Southwest Regional Director's Office","active":true,"usgs":true},{"id":509,"text":"Office of the Associate Director for Water","active":true,"usgs":true},{"id":5058,"text":"Office of the Chief Scientist for Water","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":850569,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70199988,"text":"70199988 - 2010 - Effects of light and nutrients on seasonal phytoplankton succession in a temperate eutrophic coastal lagoon","interactions":[],"lastModifiedDate":"2018-10-10T09:04:24","indexId":"70199988","displayToPublicDate":"2010-10-01T09:03:46","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1919,"text":"Hydrobiologia","onlineIssn":"1573-5117","printIssn":"0018-8158","active":true,"publicationSubtype":{"id":10}},"title":"Effects of light and nutrients on seasonal phytoplankton succession in a temperate eutrophic coastal lagoon","docAbstract":"<p><span>Rodeo Lagoon, a low-salinity coastal lagoon in the Golden Gate National Recreation Area, California, United States, has been identified as an important ecosystem due to the presence of the endangered goby (</span><i class=\"EmphasisTypeItalic \">Eucyclogobius newberri</i><span>). Despite low anthropogenic impacts, the lagoon exhibits eutrophic conditions and supports annual episodes of very high phytoplankton biomass. Weekly assessments (February–December 2007) of phytoplankton indicated diatoms,&nbsp;</span><i class=\"EmphasisTypeItalic \">Nodularia spumigena</i><span>,&nbsp;</span><i class=\"EmphasisTypeItalic \">Chaetoceros muelleri</i><span>&nbsp;var.&nbsp;</span><i class=\"EmphasisTypeItalic \">muelleri</i><span>, flagellated protozoa, a mixed assemblage, and&nbsp;</span><i class=\"EmphasisTypeItalic \">Microcystis aeruginosa</i><span>&nbsp;dominated the algal community in successive waves. Phytoplankton succession was significantly correlated (</span><i class=\"EmphasisTypeItalic \">r</i><span>&nbsp;</span><sup>2</sup><span>&nbsp;=&nbsp;0.37,&nbsp;</span><i class=\"EmphasisTypeItalic \">p</i><span>&nbsp;&lt;&nbsp;0.001) with averaged daily irradiance (max&nbsp;=&nbsp;29.7&nbsp;kW&nbsp;m</span><sup>−2</sup><span>&nbsp;d</span><sup>−1</sup><span>), water column light attenuation (max&nbsp;=&nbsp;14&nbsp;m</span><sup>−1</sup><span>), and orthophosphate and dissolved inorganic carbon concentrations (max&nbsp;=&nbsp;1.5 and 2920&nbsp;μM, respectively). Negative effects of phytoplankton growth and decay included excessive ammonia concentrations (exceeded EPA guidelines on 77% of sampling days), hypoxia (&lt;3&nbsp;mg&nbsp;l</span><sup>−1</sup><span>dissolved oxygen), and introduction of several microcystins, all in the latter half of the year. Our one-year study suggests that this coastal lagoon is a highly seasonal system with strong feedbacks between phytoplankton and geochemical processes.</span></p>","language":"English","publisher":"Springer Netherlands","doi":"10.1007/s10750-010-0380-y","usgsCitation":"Drake, J.L., Carpenter, E.J., Cousins, M., Nelson, K.L., Guido-Zarate, A., and Loftin, K.A., 2010, Effects of light and nutrients on seasonal phytoplankton succession in a temperate eutrophic coastal lagoon: Hydrobiologia, v. 654, no. 1, p. 177-192, https://doi.org/10.1007/s10750-010-0380-y.","productDescription":"16 p.","startPage":"177","endPage":"192","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":475663,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1007/s10750-010-0380-y","text":"Publisher Index Page"},{"id":358227,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Rodeo Lagoon, Golden Gate National Recreation Area","volume":"654","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-07-30","publicationStatus":"PW","scienceBaseUri":"5c10c655e4b034bf6a7f3e29","contributors":{"authors":[{"text":"Drake, Jeana L.","contributorId":208544,"corporation":false,"usgs":false,"family":"Drake","given":"Jeana","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":747639,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carpenter, Edward J.","contributorId":208545,"corporation":false,"usgs":false,"family":"Carpenter","given":"Edward","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":747640,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cousins, Mary","contributorId":208546,"corporation":false,"usgs":false,"family":"Cousins","given":"Mary","email":"","affiliations":[],"preferred":false,"id":747641,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nelson, Kara L.","contributorId":208547,"corporation":false,"usgs":false,"family":"Nelson","given":"Kara","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":747642,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Guido-Zarate, Alejandro","contributorId":208548,"corporation":false,"usgs":false,"family":"Guido-Zarate","given":"Alejandro","email":"","affiliations":[],"preferred":false,"id":747643,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Loftin, Keith A. 0000-0001-5291-876X kloftin@usgs.gov","orcid":"https://orcid.org/0000-0001-5291-876X","contributorId":868,"corporation":false,"usgs":true,"family":"Loftin","given":"Keith","email":"kloftin@usgs.gov","middleInitial":"A.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":747644,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70231418,"text":"70231418 - 2010 - Ancient earthquakes from archaeoseismic evidence during the Visigothic and Islamic periods in the archaeological site of “Tolmo de Minateda” (SE Spain)","interactions":[],"lastModifiedDate":"2022-05-10T14:19:36.704814","indexId":"70231418","displayToPublicDate":"2010-10-01T09:01:52","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Ancient earthquakes from archaeoseismic evidence during the Visigothic and Islamic periods in the archaeological site of “Tolmo de Minateda” (SE Spain)","docAbstract":"<p><span>The ruins of the ancient settlement of “El Tolmo de Minateda” are one of the best representative archaeological sites within the Albacete Province (SE Spain), characterized by a well-preserved record for the last ~3800 yr. The present ruins record an almost continuous of occupation from the Late Bronze Age (Iberian Culture, from ca. third century B.C.) to the High Middle Ages, including intervening and successive Roman, Visigoth, and Muslim city remains. The eventual Muslim settlement was abruptly abandoned and destroyed during the ninth–tenth centuries A.D., leaving a lack of any archaeological evidence of war or decay. Another previous anomalous archaeological episode of abrupt city abandonment and destruction is recorded during the Visigothic Period (seventh century). The archaeological record of this city supports evidence for earthquake damage linked to both periods of city abandonment and destruction, including oriented collapse of walls, watchtowers, and columns, oriented cracking of walls and column drums, as well as in situ broken pottery, abrupt abandonment of kilns, and anomalous sedimentary infilling of canals and water-supply facilities. Additionally, large-scale rockfalls containing Visigothic carved tombs are also apparently associated with both episodes, constituting one of the few instances of combined geoarchaeological evidence of earthquake ground effects ever reported. As a means of testing the theoretical archaeoseismic potential of this site, we obtained an archaeoseismic quality factor (AQF) value of 0.074.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Ancient earthquakes","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/2010.2471(15)","usgsCitation":"Rodriguez-Pascua, M., Silva, P.G., Garduno-Monroy, V.H., Perez-Lopez, R., Israde-Alcántara, I., Giner-Robles, J.L., Bischoff, J.L., and Calvo, J.P., 2010, Ancient earthquakes from archaeoseismic evidence during the Visigothic and Islamic periods in the archaeological site of “Tolmo de Minateda” (SE Spain), chap. <i>of</i> Ancient earthquakes, v. 471, p. 100-108, https://doi.org/10.1130/2010.2471(15).","productDescription":"9 p.","startPage":"100","endPage":"108","costCenters":[],"links":[{"id":400387,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Spain","otherGeospatial":"Tolmo de Minateda","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -1.646919250488281,\n              38.43799313099272\n            ],\n            [\n              -1.5686416625976562,\n              38.43799313099272\n            ],\n            [\n              -1.5686416625976562,\n              38.50062390460539\n            ],\n            [\n              -1.646919250488281,\n              38.50062390460539\n            ],\n            [\n              -1.646919250488281,\n              38.43799313099272\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"471","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Rodriguez-Pascua, M. A.","contributorId":67325,"corporation":false,"usgs":true,"family":"Rodriguez-Pascua","given":"M. A.","affiliations":[],"preferred":false,"id":842543,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Silva, P. G.","contributorId":291578,"corporation":false,"usgs":false,"family":"Silva","given":"P.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":842544,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Garduno-Monroy, Victor H.","contributorId":10962,"corporation":false,"usgs":true,"family":"Garduno-Monroy","given":"Victor","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":842545,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Perez-Lopez, R.","contributorId":291579,"corporation":false,"usgs":false,"family":"Perez-Lopez","given":"R.","affiliations":[],"preferred":false,"id":842546,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Israde-Alcántara, I.","contributorId":60422,"corporation":false,"usgs":true,"family":"Israde-Alcántara","given":"I.","affiliations":[],"preferred":false,"id":842547,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Giner-Robles, J. L.","contributorId":22602,"corporation":false,"usgs":true,"family":"Giner-Robles","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":842548,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Bischoff, James L. jbischoff@usgs.gov","contributorId":1389,"corporation":false,"usgs":true,"family":"Bischoff","given":"James","email":"jbischoff@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":842549,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Calvo, J. P.","contributorId":24136,"corporation":false,"usgs":true,"family":"Calvo","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":842550,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70056340,"text":"70056340 - 2010 - Creative use of pilot points to address site and regional scale heterogeneity in a variable-density model","interactions":[],"lastModifiedDate":"2014-04-18T08:45:58","indexId":"70056340","displayToPublicDate":"2010-10-01T08:36:03","publicationYear":"2010","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":12,"text":"Conference publication"},"title":"Creative use of pilot points to address site and regional scale heterogeneity in a variable-density model","docAbstract":"Pilot points for parameter estimation were creatively used to address heterogeneity at both the well field and regional scales in a variable-density groundwater flow and solute transport model designed to test multiple hypotheses for upward migration of fresh effluent injected into a highly transmissive saline carbonate aquifer. Two sets of pilot points were used within in multiple model layers, with one set of inner pilot points (totaling 158) having high spatial density to represent hydraulic conductivity at the site, while a second set of outer points (totaling 36) of lower spatial density was used to represent hydraulic conductivity further from the site. Use of a lower spatial density outside the site allowed (1) the total number of pilot points to be reduced while maintaining flexibility to accommodate heterogeneity at different scales, and (2) development of a model with greater  areal extent in order to simulate proper boundary conditions that have a limited effect on the area of interest. The parameters associated with the inner pilot points were log transformed hydraulic conductivity multipliers of the conductivity field obtained by interpolation from outer pilot points. The use of this dual inner-outer scale parameterization (with inner parameters constituting multipliers for outer parameters) allowed smooth transition of hydraulic conductivity from the site scale, where greater spatial variability of hydraulic properties exists, to the regional scale where less spatial variability was necessary for model calibration. While the model is highly parameterized to accommodate potential aquifer heterogeneity, the total number of pilot points is kept at a minimum to enable reasonable calibration run times.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"PEST Conference 2009 Proceedings","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"conferenceTitle":"PEST Conference","conferenceDate":"2009-11-02T00:00:00","conferenceLocation":"Potomac, MD","language":"English","publisher":"S.S. Papadopulos & Associates, Inc.","usgsCitation":"Dausman, A., Doherty, J., and Langevin, C.D., 2010, Creative use of pilot points to address site and regional scale heterogeneity in a variable-density model.","ipdsId":"IP-016465","costCenters":[{"id":286,"text":"Florida Water Science Center-Ft. Lauderdale","active":false,"usgs":true}],"links":[{"id":286411,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":279193,"type":{"id":15,"text":"Index Page"},"url":"https://www.lulu.com/shop/ss-papadopulos-associates-inc/pest-conference-2009-proceedings-potomac-maryland-color/paperback/product-12914428.html"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53558ffee4b0120853e8be9f","contributors":{"authors":[{"text":"Dausman, Alyssa M.","contributorId":64337,"corporation":false,"usgs":true,"family":"Dausman","given":"Alyssa M.","affiliations":[],"preferred":false,"id":486536,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Doherty, John","contributorId":43843,"corporation":false,"usgs":true,"family":"Doherty","given":"John","affiliations":[],"preferred":false,"id":486535,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Langevin, Christian D. 0000-0001-5610-9759 langevin@usgs.gov","orcid":"https://orcid.org/0000-0001-5610-9759","contributorId":1030,"corporation":false,"usgs":true,"family":"Langevin","given":"Christian","email":"langevin@usgs.gov","middleInitial":"D.","affiliations":[{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"preferred":true,"id":486534,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70176258,"text":"70176258 - 2010 - Improving and integrating data on invasive species collected by citizen scientists","interactions":[],"lastModifiedDate":"2016-09-06T14:22:54","indexId":"70176258","displayToPublicDate":"2010-10-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1018,"text":"Biological Invasions","active":true,"publicationSubtype":{"id":10}},"title":"Improving and integrating data on invasive species collected by citizen scientists","docAbstract":"<p><span>Limited resources make it difficult to effectively document, monitor, and control invasive species across large areas, resulting in large gaps in our knowledge of current and future invasion patterns. We surveyed 128 citizen science program coordinators and interviewed 15 of them to evaluate their potential role in filling these gaps. Many programs collect data on invasive species and are willing to contribute these data to public databases. Although resources for education and monitoring are readily available, groups generally lack tools to manage and analyze data. Potential users of these data also retain concerns over data quality. We discuss how to address these concerns about citizen scientist data and programs while preserving the advantages they afford. A unified yet flexible national citizen science program aimed at tracking invasive species location, abundance, and control efforts could be designed using centralized data sharing and management tools. Such a system could meet the needs of multiple stakeholders while allowing efficiencies of scale, greater standardization of methods, and improved data quality testing and sharing. Finally, we present a prototype for such a system (see </span><span class=\"ExternalRef\"><a rel=\"noopener noreferrer\" href=\"http://www.citsci.org/\" target=\"_blank\" data-mce-href=\"http://www.citsci.org/\"><span class=\"RefSource\">www.citsci.org</span></a></span><span>).</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s10530-010-9740-9","usgsCitation":"Springer, 2010, Improving and integrating data on invasive species collected by citizen scientists: Biological Invasions, v. 12, no. 10, p. 3419-3428, https://doi.org/10.1007/s10530-010-9740-9.","productDescription":"10 p.","startPage":"3419","endPage":"3428","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":328264,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"10","noUsgsAuthors":false,"publicationDate":"2010-03-07","publicationStatus":"PW","scienceBaseUri":"57cfe8b7e4b04836416a0dc4"}
,{"id":70003677,"text":"70003677 - 2010 - Quarterly wildlife mortality report April to June 2010","interactions":[],"lastModifiedDate":"2023-10-13T16:22:25.104224","indexId":"70003677","displayToPublicDate":"2010-10-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3769,"text":"Wildlife Disease Association Newsletter","active":true,"publicationSubtype":{"id":10}},"title":"Quarterly wildlife mortality report April to June 2010","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Wildlife Disease Association","publisherLocation":"Lawrence, KS","usgsCitation":"Ballmann, A., White, C.L., and Bradsby, J., 2010, Quarterly wildlife mortality report April to June 2010: Wildlife Disease Association Newsletter, p. 9-11.","productDescription":"3 p.","startPage":"9","endPage":"11","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-024887","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":257856,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -180.17578125,\n              17.14079039331665\n            ],\n            [\n              -180.17578125,\n              72.71190310803662\n            ],\n            [\n              -65.7421875,\n              72.71190310803662\n            ],\n            [\n              -65.7421875,\n              17.14079039331665\n            ],\n            [\n              -180.17578125,\n              17.14079039331665\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a9270e4b0c8380cd8085c","contributors":{"authors":[{"text":"Ballmann, Anne 0000-0002-0380-056X","orcid":"https://orcid.org/0000-0002-0380-056X","contributorId":104631,"corporation":false,"usgs":true,"family":"Ballmann","given":"Anne","affiliations":[],"preferred":false,"id":348297,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, C. LeAnn 0000-0002-5004-5165","orcid":"https://orcid.org/0000-0002-5004-5165","contributorId":29571,"corporation":false,"usgs":true,"family":"White","given":"C.","email":"","middleInitial":"LeAnn","affiliations":[],"preferred":false,"id":348295,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bradsby, Jennifer","contributorId":33664,"corporation":false,"usgs":true,"family":"Bradsby","given":"Jennifer","email":"","affiliations":[],"preferred":false,"id":348296,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70194397,"text":"70194397 - 2010 - A population genetic analysis of the midget faded rattlesnake in Wyoming","interactions":[],"lastModifiedDate":"2017-11-27T15:51:07","indexId":"70194397","displayToPublicDate":"2010-10-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1324,"text":"Conservation Genetics","active":true,"publicationSubtype":{"id":10}},"title":"A population genetic analysis of the midget faded rattlesnake in Wyoming","docAbstract":"<p><span>Little is known about the population biology of midget faded rattlesnakes, a sensitive subspecies of the Western Rattlesnake, despite conservation efforts to protect them. We conducted a molecular genetic study of midget faded rattlesnakes in southwestern Wyoming to investigate population genetic structure in this area, particularly with reference to Flaming Gorge Reservoir and its associated human activities, and to document levels of genetic diversity. We genotyped 229 snakes from 11 sampling sites using 9 microsatellite loci. We found significant levels of genetic structure among sites that were better explained by geographic region and isolation by distance than by position relative to waterways. Sites on either side of the reservoir at its widest point were not significantly different. Six of the sites showed signatures of a population bottleneck using an alpha value of 0.05. Three of these bottlenecked sites (the three most northern) were the most genetically distinct and occur in areas of greatest impact from human activity.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s10592-009-0043-6","usgsCitation":"Oyler-McCance, S.J., and Parker, J., 2010, A population genetic analysis of the midget faded rattlesnake in Wyoming: Conservation Genetics, v. 11, no. 5, p. 1623-1629, https://doi.org/10.1007/s10592-009-0043-6.","productDescription":"7 p.","startPage":"1623","endPage":"1629","ipdsId":"IP-012717","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":349391,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Flaming Gorge Reservoir","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.70123291015625,\n              40.9964840143779\n            ],\n            [\n              -109.2755126953125,\n              40.9964840143779\n            ],\n            [\n              -109.2755126953125,\n              41.62160222224564\n            ],\n            [\n              -109.70123291015625,\n              41.62160222224564\n            ],\n            [\n              -109.70123291015625,\n              40.9964840143779\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"11","issue":"5","noUsgsAuthors":false,"publicationDate":"2010-10-01","publicationStatus":"PW","scienceBaseUri":"5a610aaae4b06e28e9c256c2","contributors":{"authors":[{"text":"Oyler-McCance, Sara J. 0000-0003-1599-8769 sara_oyler-mccance@usgs.gov","orcid":"https://orcid.org/0000-0003-1599-8769","contributorId":1973,"corporation":false,"usgs":true,"family":"Oyler-McCance","given":"Sara","email":"sara_oyler-mccance@usgs.gov","middleInitial":"J.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":723688,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parker, J.M.","contributorId":87497,"corporation":false,"usgs":true,"family":"Parker","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":723689,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70160812,"text":"70160812 - 2010 - Determination of biologically significant hydrologic condition metrics in urbanizing watersheds: an empirical analysis over a range of environmental settings","interactions":[],"lastModifiedDate":"2015-12-31T10:59:15","indexId":"70160812","displayToPublicDate":"2010-10-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1919,"text":"Hydrobiologia","onlineIssn":"1573-5117","printIssn":"0018-8158","active":true,"publicationSubtype":{"id":10}},"title":"Determination of biologically significant hydrologic condition metrics in urbanizing watersheds: an empirical analysis over a range of environmental settings","docAbstract":"<p>We investigated the relations among 83 hydrologic condition metrics (HCMs) and changes in algal, invertebrate, and fish communities in five metropolitan areas across the continental United States. We used a statistical approach that employed Spearman correlation and regression tree analysis to identify five HCMs that are strongly associated with observed biological variation along a gradient of urbanization. The HCMs related to average flow magnitude, high-flow magnitude, high-flow event frequency, high-flow duration, and rate of change of stream cross-sectional area were most consistently associated with changes in aquatic communities. Although our investigation used an urban gradient design with short hydrologic periods of record (&le;1 year) of hourly cross-sectional area time series, these five HCMs were consistent with previous investigations using long-term daily-flow records. The ecological sampling day often was included in the hydrologic period. Regression tree models explained up to 73, 92, and 79% of variance for specific algal, invertebrate, and fish community metrics, respectively. National models generally were not as statistically significant as models for individual metropolitan areas. High-flow event frequency, a hydrologic metric found to be transferable across stream type and useful for classifying habitat by previous research, was found to be the most ecologically relevant HCM; transformation by precipitation increased national-scale applicability. We also investigated the relation between measures of stream flashiness and land-cover indicators of urbanization and found that land-cover characteristic and pattern variables, such as road density, percent wetland, and proximity of developed land, were strongly related to HCMs at both a metropolitan and national scale and, therefore, may be effective land-use management options in addition to wholesale impervious-area reduction.</p>","language":"English","publisher":"Springer","doi":"10.1007/s10750-010-0362-0","usgsCitation":"Steuer, J.J., Stensvold, K.A., and Gregory, M., 2010, Determination of biologically significant hydrologic condition metrics in urbanizing watersheds: an empirical analysis over a range of environmental settings: Hydrobiologia, v. 654, no. 1, p. 27-55, https://doi.org/10.1007/s10750-010-0362-0.","productDescription":"29 p.","startPage":"27","endPage":"55","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-013743","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":313128,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Milwaukee-Green Bay; Boston; Raleigh; Atlanta; Birmingham; Dallas-Fort Worth; Denver; Salt Lake City; Portland","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.08837890625,\n              44.61393394730626\n            ],\n            [\n              -88.65966796875,\n              44.174324837518895\n            ],\n            [\n              -88.74755859375,\n              43.874138181474734\n            ],\n            [\n              -88.406982421875,\n              43.01268088642034\n            ],\n            [\n              -87.82470703125,\n  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PSC"},"noUsgsAuthors":false,"publicationDate":"2010-07-19","publicationStatus":"PW","scienceBaseUri":"56865fbfe4b0e7594ee74cb9","contributors":{"authors":[{"text":"Steuer, Jeffrey J.","contributorId":75136,"corporation":false,"usgs":true,"family":"Steuer","given":"Jeffrey","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":584037,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stensvold, Krista A.","contributorId":48007,"corporation":false,"usgs":true,"family":"Stensvold","given":"Krista","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":584038,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gregory, Mark B.","contributorId":151024,"corporation":false,"usgs":false,"family":"Gregory","given":"Mark B.","affiliations":[],"preferred":false,"id":584039,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70193175,"text":"70193175 - 2010 - Habitat use by fishes in groundwater-dependent streams of southern Oklahoma","interactions":[],"lastModifiedDate":"2017-11-15T16:40:18","indexId":"70193175","displayToPublicDate":"2010-10-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5153,"text":"The American Midland Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Habitat use by fishes in groundwater-dependent streams of southern Oklahoma","docAbstract":"<p><span>Habitat use by fishes in groundwater-dependent ecosystems with springs and spring-fed creeks is not widely studied or well understood. We evaluated habitat use by three disjunct populations of fish species (</span><i>Phoxinus erythrogaster</i><span>,<span>&nbsp;</span></span><i>Nocomis asper</i><span><span>&nbsp;</span>and<span>&nbsp;</span></span><i>Etheostoma microperca</i><span>) and, a widespread species,<span>&nbsp;</span></span><i>E. spectabile</i><span><span>&nbsp;</span>in spring-fed streams draining the Arbuckle-Simpson aquifer of southern Oklahoma. Habitat preference for each species was classified based on depth, velocity, substrate and cover.<span>&nbsp;</span></span><i>Phoxinus erthyrogaster</i><span><span>&nbsp;</span>and<span>&nbsp;</span></span><i>N. asper</i><span><span>&nbsp;</span>were associated with pools with little cover, while<span>&nbsp;</span></span><i>E. microperca</i><span><span>&nbsp;</span>was found in heavily vegetated areas.<span>&nbsp;</span></span><i>Etheostoma spectabile</i><span><span>&nbsp;</span>used habitat in riffles with rapid velocity and large substrate types. We classified habitat selection and avoidance with Chesson's α and observed significant differences in habitat use among species in the study sites. Overall differences in habitat use for<span>&nbsp;</span></span><i>P. erythrogaster</i><span><span>&nbsp;</span>among the three study sites were primarily related to differences in available habitat between springs. Our study provides vital ecological information about disjunct populations of groundwater-dependent fishes in an aquifer that is experiencing development pressure for water abstraction.</span></p>","language":"English","publisher":"University of Notre Dame","doi":"10.1674/0003-0031-164.2.201","usgsCitation":"Seilheimer, T.S., and Fisher, W.L., 2010, Habitat use by fishes in groundwater-dependent streams of southern Oklahoma: The American Midland Naturalist, v. 164, no. 2, p. 201-216, https://doi.org/10.1674/0003-0031-164.2.201.","productDescription":"16 p.","startPage":"201","endPage":"216","ipdsId":"IP-012120","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":348941,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oklahoma","volume":"164","issue":"2","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a610aaae4b06e28e9c256c4","contributors":{"authors":[{"text":"Seilheimer, Titus S.","contributorId":50772,"corporation":false,"usgs":true,"family":"Seilheimer","given":"Titus","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":722316,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fisher, William L. wfisher@usgs.gov","contributorId":1229,"corporation":false,"usgs":true,"family":"Fisher","given":"William","email":"wfisher@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":718124,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70136147,"text":"70136147 - 2010 - Bison conservation initiative: Bison conservation genetics workshop: Report and recommendations","interactions":[],"lastModifiedDate":"2020-12-02T13:50:56.163269","indexId":"70136147","displayToPublicDate":"2010-10-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":53,"text":"Natural Resource Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"NPS/NRPC/BRMD/NRR—2010/257","title":"Bison conservation initiative: Bison conservation genetics workshop: Report and recommendations","docAbstract":"One of the first outcomes of the Department of the Interior (DOI) Bison Conservation Initiative was the Bison Conservation Genetics Workshop held in Nebraska in September 2008. The workshop brought together scientists from government agencies and non-governmental organizations with professional population geneticists to develop guidance for the genetic management of the federal bison herds. The scientists agreed on the basic tenets of genetic management for the DOI herds and discussed different approaches to meeting those goals. First, the 12 DOI herds are an irreplaceable resource for the long-term conservation of North American plains bison. Most of the herds show low levels of cattle introgression dating from the time when they were saved from extirpation; those herds should not be mixed without careful consideration as to their origin. Herds that show no evidence of cattle ancestry by the current molecular methods are the highest priority for protection from genetic mixing with any other bison herds. Second, despite the fact that most of the herds now managed by the U.S. government were founded with very few bison and have been maintained for many generations at relatively low population sizes, they do not show obvious effects of inbreeding. They have retained significant amounts of genetic variation by the standard measures, heterozygosity and allelic diversity. This may be explained in part by the fact that most of these herds are not remnants of a single population. Third, to preserve genetic variation in federal bison herds over decades and centuries, herds should be managed at a population or metapopulation level of 1,000 animals or more, with a sex ratio that enables competition between breeding bulls. The parks and refuges that currently have bison herds, with the exception of Yellowstone National Park, do not have enough land to support a population of this size. In the short term, it will be important to develop satellite herds to attain population targets, and develop a metapopulation structure between herds.\r\nFourth and finally, the current methods used to evaluate the DOI bison herds, using mitochondrial DNA and a suite of nuclear DNA microsatellites, are highly informative at the herd level. They have confirmed relatedness of herds that we know from historical records have a common origin. They have detected cattle ancestry in most of the herds where it was suspected and have shown some loss of rare alleles. However, they do not sample across the bison genome, and the use of neutral genetic markers as the basis for selection of individual bison—either to breed or move to other herds—would be better supported by more high-resolution molecular methods currently under development.","language":"English","publisher":"National Park Service","usgsCitation":"Gogan, P.J., and Dratch, P., 2010, Bison conservation initiative: Bison conservation genetics workshop: Report and recommendations: Natural Resource Report NPS/NRPC/BRMD/NRR—2010/257, vii, 38 p.","productDescription":"vii, 38 p.","numberOfPages":"50","ipdsId":"IP-025356","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":332333,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":348896,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://permanent.fdlp.gov/gpo131592/Bison_Genetics_Report__nrpc.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"585a51c4e4b01224f329b603","contributors":{"authors":[{"text":"Gogan, Peter J. 0000-0002-7821-133X peter_gogan@usgs.gov","orcid":"https://orcid.org/0000-0002-7821-133X","contributorId":1771,"corporation":false,"usgs":true,"family":"Gogan","given":"Peter","email":"peter_gogan@usgs.gov","middleInitial":"J.","affiliations":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"preferred":true,"id":537155,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dratch, Peter","contributorId":131078,"corporation":false,"usgs":false,"family":"Dratch","given":"Peter","email":"","affiliations":[{"id":7231,"text":"National Park Service, Natural Resource Program Center","active":true,"usgs":false}],"preferred":false,"id":537156,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":70006209,"text":"70006209 - 2010 - Efficacy of commercial canarypox vaccine for protecting Hawai'i 'Amakihi from field isolates of <i>Avipoxvirus</i>","interactions":[],"lastModifiedDate":"2017-06-30T15:31:42","indexId":"70006209","displayToPublicDate":"2010-09-30T14:29:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Efficacy of commercial canarypox vaccine for protecting Hawai'i 'Amakihi from field isolates of <i>Avipoxvirus</i>","docAbstract":"At least three variants of avian pox virus are present in Hawai&#8216;i - Fowlpox from domestic poultry and a group of genetically distinct viruses that cluster within two clades (Pox Variant 1 and Pox Variant 2) that are most similar to Canarypox based on DNA sequence of the virus 4b core protein gene. We tested whether Hawai&#8216;i &#8216;Amakihi can be protected from wild virus isolates with an attenuated live Canarypox vaccine that is closely related to isolates that cluster within clade 1 (Pox Variant 1) based on sequence of the attenuated Canarypox virus 4b core protein. Thirty-one (31) Hawai`i &#8216;Amakihi (<i>Hemignathus virens</i>) with no prior physical evidence of pox infection were collected on Mauna Kea from xeric, high elevation habitats with low pox prevalence and randomly divided into two groups. One group of 16 was vaccinated with Poximmune C&reg; while the other group received a sham vaccination with virus diluent. Four of 15 (27%) vaccinated birds developed potentially life-threatening disseminated lesions or lesions of unusually long duration, while one bird never developed a vaccine-associated lesion or \"take\". After vaccine-associated lesions healed, vaccinated birds were randomly divided into three groups of five and challenged with either a wild isolate of Fowlpox, a Hawai`i `Amakihi isolate of a Canarypox-like virus from clade 1 (Pox Variant 1) or a Hawai`i `Amakihi isolate of a Canarypox-like virus from clade 2 (Pox Variant 2). Similarly, three random groups of five unvaccinated &#8216;Amakihi were challenged with the same virus isolates. Vaccinated and unvaccinated &#8216;Amakihi challenged with Fowlpox had transient infections with no clinical signs of infection. Mortality in vaccinated &#8216;Amakihi that were challenged with Pox Variant 1 and Pox Variant 2 ranged from 0% (0/5) for Pox Variant 1 to 60% (3/5) for Pox Variant 2. Mortality in unvaccinated &#8216;Amakihi ranged from 40% (2/5) for Pox Variant 1 to 100% (5/5) for Pox Variant 2. While the vaccine provided some protection against Pox Variant 1, serious side effects and low efficacy against Pox Variant 2 make it risky to use in captive or wild honeycreepers.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hawaii Cooperative Studies Unit Technical Report HCSU-019","largerWorkSubtype":{"id":9,"text":"Other Report"},"language":"English","publisher":"Hawaii Cooperative Studies Unit, University of Hawaii at Hilo, Pacific Aquaculture and Coastal Resources Center","publisherLocation":"Hilo, HI","usgsCitation":"Atkinson, C.T., Wiegand, K.C., Triglia, D., and Jarvi, S.I., 2010, Efficacy of commercial canarypox vaccine for protecting Hawai'i 'Amakihi from field isolates of <i>Avipoxvirus</i>, iv, 18 p.; Figures.","productDescription":"iv, 18 p.; Figures","costCenters":[{"id":521,"text":"Pacific Island Ecosystems Research Center","active":false,"usgs":true}],"links":[{"id":256976,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":256970,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://hilo.hawaii.edu/hcsu/documents/TRHCSU-019Atkinson_Avian_Pox.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Hawai'i","otherGeospatial":"O'ahu;Maui;Moloka'i","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0858e4b0c8380cd51aad","contributors":{"authors":[{"text":"Atkinson, Carter T. 0000-0002-4232-5335 catkinson@usgs.gov","orcid":"https://orcid.org/0000-0002-4232-5335","contributorId":1124,"corporation":false,"usgs":true,"family":"Atkinson","given":"Carter","email":"catkinson@usgs.gov","middleInitial":"T.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":5049,"text":"Pacific Islands Ecosys Research Center","active":true,"usgs":true},{"id":521,"text":"Pacific Island Ecosystems Research Center","active":false,"usgs":true}],"preferred":true,"id":354065,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wiegand, Kimberly C.","contributorId":94142,"corporation":false,"usgs":true,"family":"Wiegand","given":"Kimberly","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":354068,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Triglia, Dennis","contributorId":77780,"corporation":false,"usgs":true,"family":"Triglia","given":"Dennis","email":"","affiliations":[],"preferred":false,"id":354067,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jarvi, Susan I.","contributorId":47748,"corporation":false,"usgs":true,"family":"Jarvi","given":"Susan","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":354066,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70209636,"text":"70209636 - 2010 - Chemical and textural controls on phosphorus mobility in drylands of southeastern Utah","interactions":[],"lastModifiedDate":"2020-04-16T18:46:53.753027","indexId":"70209636","displayToPublicDate":"2010-09-30T13:40:19","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1007,"text":"Biogeochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Chemical and textural controls on phosphorus mobility in drylands of southeastern Utah","docAbstract":"<p><span>We investigated several forms of phosphorus (P) in dryland soils to examine the chemical and textural controls on P stabilization on a diverse set of substrates. We examined three P fractions including labile, moderately labile, and occluded as determined by a modified Hedley fractionation technique. The P fractions were compared to texture measurements and total elemental concentrations determined by inductively coupled plasma-atomic emission spectroscopy (ICP-AES). Labile P related to the absence of materials involved in P sorption. Moderately labile P was most strongly associated with high total Al &amp; Fe content that we interpret to represent oxides and 1:1 clay minerals. The occluded P fraction was strongly associated with low total Al &amp; Fe environments and interpreted to represent 2:1 clay minerals where ligand exchange tightly sequesters P. The results indicate that the controls on P fraction distribution are initially closely tied to the chemical and physical properties of the bedrock units that contribute to soil formation. Further, these results suggest that the progression of stabilized P forms in dryland areas differs from the progression observed in mesic environments. Soil development in dryland settings, such as the formation of pedogenic carbonates, may lead to differing controls on P availability and the proportional size of the moderately labile fraction.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s10533-010-9408-7","usgsCitation":"Buckingham, S.E., Neff, J., Titiz-Maybach, B., and Reynolds, R.L., 2010, Chemical and textural controls on phosphorus mobility in drylands of southeastern Utah: Biogeochemistry, v. 100, p. 105-120, https://doi.org/10.1007/s10533-010-9408-7.","productDescription":"16 p.","startPage":"105","endPage":"120","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":374062,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Canyonlands National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.5499267578125,\n              37.483576550426996\n            ],\n            [\n              -109.12170410156249,\n              37.483576550426996\n            ],\n            [\n              -109.12170410156249,\n              38.75408327579141\n            ],\n            [\n              -110.5499267578125,\n              38.75408327579141\n            ],\n            [\n              -110.5499267578125,\n              37.483576550426996\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"100","noUsgsAuthors":false,"publicationDate":"2010-02-11","publicationStatus":"PW","contributors":{"authors":[{"text":"Buckingham, Susan E.","contributorId":184077,"corporation":false,"usgs":false,"family":"Buckingham","given":"Susan","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":787299,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neff, Jason","contributorId":167084,"corporation":false,"usgs":false,"family":"Neff","given":"Jason","affiliations":[{"id":6709,"text":"University of Colorado, Denver","active":true,"usgs":false}],"preferred":false,"id":787300,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Titiz-Maybach, Behan","contributorId":224205,"corporation":false,"usgs":false,"family":"Titiz-Maybach","given":"Behan","email":"","affiliations":[],"preferred":false,"id":787301,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Reynolds, Richard L. 0000-0002-4572-2942 rreynolds@usgs.gov","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":147880,"corporation":false,"usgs":true,"family":"Reynolds","given":"Richard","email":"rreynolds@usgs.gov","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true},{"id":271,"text":"Federal Center","active":false,"usgs":true}],"preferred":true,"id":787302,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70043523,"text":"70043523 - 2010 - To burn or not to burn Oriental bittersweet: A fire manager’s conundrum","interactions":[],"lastModifiedDate":"2022-09-02T18:15:05.312539","indexId":"70043523","displayToPublicDate":"2010-09-30T10:44:13","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"To burn or not to burn Oriental bittersweet: A fire manager’s conundrum","docAbstract":"<p>This is the second progress report detailing the research about Oriental bittersweet (<i>Celastrus orbiculatus</i>) and fire which has been ongoing for two years. We highlight the further results from three components of the study: 1) Susceptibility of different habitats to invasion of Oriental bittersweet, 2) The impact of fire on established individuals of Oriental bittersweet, and 3) Modeling Oriental bittersweet invasion proliferation and presence on the basis of fire history and vegetation. </p>","language":"English","publisher":"Joint Fire Science Program","usgsCitation":"Pavlovic, N.B., Leicht-Young, S.A., Frohnapple, K., Morford, D., and Mulconrey, N., 2010, To burn or not to burn Oriental bittersweet: A fire manager’s conundrum, 39 p.","productDescription":"39 p.","ipdsId":"IP-025751","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":406147,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":406146,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.firescience.gov/projects/08-1-2-10/project/08-1-2-10_jfspbittersweetsecondprogressreport2010.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana","otherGeospatial":"Indiana Dunes National Lakeshore","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.3248291015625,\n              41.62493858776385\n            ],\n            [\n              -87.32585906982422,\n              41.60414765107674\n            ],\n            [\n              -87.30113983154297,\n              41.59464832679814\n            ],\n  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Center","active":true,"usgs":true}],"preferred":true,"id":850712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leicht-Young, Stacey A.","contributorId":80506,"corporation":false,"usgs":false,"family":"Leicht-Young","given":"Stacey","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":850713,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Frohnapple, Krystal kfrohnapple@usgs.gov","contributorId":4110,"corporation":false,"usgs":true,"family":"Frohnapple","given":"Krystal","email":"kfrohnapple@usgs.gov","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":850714,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Morford, Dan","contributorId":296127,"corporation":false,"usgs":false,"family":"Morford","given":"Dan","email":"","affiliations":[],"preferred":false,"id":850715,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mulconrey, Neal","contributorId":152092,"corporation":false,"usgs":false,"family":"Mulconrey","given":"Neal","email":"","affiliations":[{"id":18866,"text":"Indiana Dunes National Lakeshore","active":true,"usgs":false}],"preferred":false,"id":850716,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":98761,"text":"sim3099 - 2010 - Geologic map of the Artemis Chasma quadrangle (V-48), Venus","interactions":[],"lastModifiedDate":"2023-03-16T10:55:49.423875","indexId":"sim3099","displayToPublicDate":"2010-09-30T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"3099","title":"Geologic map of the Artemis Chasma quadrangle (V-48), Venus","docAbstract":"Artemis, named for the Greek goddess of the hunt, represents an approximately 2,600 km diameter circular feature on Venus, and it may represent the largest circular structure in our solar system. Artemis, which lies between the rugged highlands of Aphrodite Terra to the north and relatively smooth lowlands to the south, includes an interior topographic high surrounded by the 2,100-km-diameter, 25- to 200-km-wide, 1- to 2-km-deep circular trough, called Artemis Chasma, and an outer rise that grades outward into the surrounding lowland. Although several other chasmata exist in the area and globally, other chasmata have generally linear trends that lack the distinctive circular pattern of Artemis Chasma. The enigmatic nature of Artemis has perplexed researchers since Artemis Chasma was first identified in Pioneer Venus data. Although Venus' surface abounds with circular to quasi-circular features at a variety of scales, including from smallest to largest diameter features: small shield edifices (>1 km), large volcanic edifices (100-1,000 km), impact craters (1-270 km), coronae (60-1,010 km), volcanic rises and crustal plateaus (~1,500-2,500 km), Artemis defies classification into any of these groups. Artemis dwarfs Venus' largest impact crater, Mead (~280 km diameter); Artemis also lacks the basin topography, multiple ring structures, and central peak expected for large impact basins. Topographically, Artemis resembles some Venusian coronae; however Artemis is an order of magnitude larger than the average corona (200 km) and about twice the size of Heng-O Corona (which is 1,010 km in diameter), the largest of Venusian coronae. In map view Artemis' size and shape resemble volcanic rises and crustal plateaus; however, both of these classes of features differ topographically from Artemis. Volcanic rises and crustal plateaus form broad domical regions, and steep-sided regions with flat tops, respectively; furthermore, neither rises nor plateaus include circular troughs. So although it seems clear what Artemis is not, there is little consensus about what Artemis is, much less how Artemis formed. \r\n\r\nDebate during the past decade has resulted in the proposal of at least four hypotheses for Artemis' formation. The first (herein referred to as H1) is that Artemis Chasma represents a zone of northwest-directed convergence and subduction. The second hypothesis (herein referred to as H2) is that Artemis consists of a composite structure with a part of its interior region marking the exposure of deformed ductile deep-crustal rocks analogous to a terrestrial metamorphic core complex. The third (herein referred to as H3) is that Artemis reflects the surface expression of an ancient (>3.5 Ga) huge bolide impact event on cold strong lithosphere. The fourth hypothesis (herein referred to as H4) is that Artemis marks the surface expression of a deep mantle plume. Each of these hypotheses holds different implications for Venus geodynamics and evolution processes, and for terrestrial planet processes in general. Viability of H1 would provide support that terrestrial-like plate-tectonic processes once occurred on Earth's sister planet. The feasibility of H2 would require high values of crustal extension and therefore imply that significant horizontal displacements occurred on Venus-displacement that may or may not be related to terrestrial-like plate-tectonic processes. The possibility of H3 would suggest that Venus' surface is extremely old, and that Venus has experienced very little dynamic activity for the last 3.5 billion years or more; this would further imply that Venus is essentially tectonically dead, and has been for most of its history. This view contrasts strongly with studies that highlight a rich history of Venus including activity at least as young as 750 million years ago, and quite likely up to the present. If H4 has credibility, then Artemis could provide clues to cooling mechanisms of Earth's sister planet. Each of these hypotheses","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sim3099","collaboration":"Prepared for the National Aeronautics and Space Administration","usgsCitation":"Bannister, R.A., and Hansen, V.L., 2010, Geologic map of the Artemis Chasma quadrangle (V-48), Venus: U.S. Geological Survey Scientific Investigations Map 3099, Pamphlet: i, 22 p.; Figures; Tables; Map Sheet: 53.30 inches x 36.78 inches, https://doi.org/10.3133/sim3099.","productDescription":"Pamphlet: i, 22 p.; Figures; Tables; Map Sheet: 53.30 inches x 36.78 inches","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":125986,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sim_3099.jpg"},{"id":14171,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/3099/","linkFileType":{"id":5,"text":"html"}},{"id":414264,"rank":3,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://doi.org/10.5066/P9FYOY6B","text":"Interactive map","linkHelpText":"- Geologic Map of the Artemis Chasma Quadrangle (V–48), Venus, 1:5M. Bannister and Hansen (2010)"}],"scale":"47886","projection":"Lambert Projection","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0be4b07f02db69d937","contributors":{"authors":[{"text":"Bannister, Roger A.","contributorId":31872,"corporation":false,"usgs":true,"family":"Bannister","given":"Roger","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":306398,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hansen, Vicki L.","contributorId":101238,"corporation":false,"usgs":false,"family":"Hansen","given":"Vicki","email":"","middleInitial":"L.","affiliations":[{"id":6915,"text":"University of Minnesota - Duluth","active":true,"usgs":false}],"preferred":false,"id":306399,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":98746,"text":"sir20105175 - 2010 - Status and understanding of groundwater quality in the northern San Joaquin Basin, 2005: California GAMA Priority Basin Project","interactions":[],"lastModifiedDate":"2022-01-03T20:08:50.837427","indexId":"sir20105175","displayToPublicDate":"2010-09-30T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-5175","title":"Status and understanding of groundwater quality in the northern San Joaquin Basin, 2005: California GAMA Priority Basin Project","docAbstract":"Groundwater quality in the 2,079 square mile Northern San Joaquin Basin (Northern San Joaquin) study unit was investigated from December 2004 through February 2005 as part of the Priority Basin Project of the Groundwater Ambient Monitoring and Assessment (GAMA) Program. The GAMA Priority Basin Project was developed in response to the Groundwater Quality Monitoring Act of 2001 that was passed by the State of California and is being conducted by the California State Water Resources Control Board in collaboration with the U.S. Geological Survey and the Lawrence Livermore National Laboratory.\r\nThe Northern San Joaquin study unit was the third study unit to be designed and sampled as part of the Priority Basin Project. Results of the study provide a spatially unbiased assessment of the quality of raw (untreated) groundwater, as well as a statistically consistent basis for comparing water quality throughout California. Samples were collected from 61 wells in parts of Alameda, Amador, Calaveras, Contra Costa, San Joaquin, and Stanislaus Counties; 51 of the wells were selected using a spatially distributed, randomized grid-based approach to provide statistical representation of the study area (grid wells), and 10 of the wells were sampled to increase spatial density and provide additional information for the evaluation of water chemistry in the study unit (understanding/flowpath wells).\r\nThe primary aquifer systems (hereinafter, primary aquifers) assessed in this study are defined by the depth intervals of the wells in the California Department of Public Health database for each study unit. The quality of groundwater in shallow or deep water-bearing zones may differ from quality of groundwater in the primary aquifers; shallow groundwater may be more vulnerable to contamination from the surface. Two types of assessments were made: (1) status, assessment of the current quality of the groundwater resource; and (2) understanding, identification of the natural and human factors affecting groundwater quality.\r\nRelative-concentrations (sample concentrations divided by benchmark concentrations) were used for evaluating groundwater quality for those constituents that have Federal or California regulatory or non-regulatory benchmarks for drinking-water quality. Benchmarks used in this study were either health-based (regulatory and non-regulatory) or aesthetic based (non-regulatory). For inorganic constituents, relative-concentrations were classified as high (equal to or greater than 1.0), indicating relative-concentrations greater than benchmarks; moderate (equal to or greater than 0.5, and less than 1.0); or, low (less than 0.5). For organic and special- interest constituents [1,2,3-trichloropropane (1,2,3-TCP), N-nitrosodimethylamine (NDMA), and perchlorate], relative- concentrations were classified as high (equal to or greater than 1.0); moderate (equal to or greater than 0.1 and less than 1.0); or, low (less than 0.1).\r\nAquifer-scale proportion was used as the primary metric in the status assessment for groundwater quality. High aquifer- scale proportion is defined as the percentage of the primary aquifer with relative-concentrations greater than 1.0; moderate and low aquifer-scale proportions are defined as the percentage of the primary aquifer with moderate and low relative- concentrations, respectively. The methods used to calculate aquifer-scale proportions are based on an equal-area grid; thus, the proportions are areal rather than volumetric. Two statistical approaches - grid-based, which used one value per grid cell, and spatially weighted, which used the full dataset - were used to calculate aquifer-scale proportions for individual constituents and classes of constituents. The spatially weighted estimates of high aquifer-scale proportions were within the 90-percent confidence intervals of the grid-based estimates in all cases. The understanding assessment used statistical correlations between constituent relative-concentrations and","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20105175","usgsCitation":"Bennett, G.L., Fram, M.S., Belitz, K., and Jurgens, B., 2010, Status and understanding of groundwater quality in the northern San Joaquin Basin, 2005: California GAMA Priority Basin Project: U.S. Geological Survey Scientific Investigations Report 2010-5175, x, 67 p., https://doi.org/10.3133/sir20105175.","productDescription":"x, 67 p.","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"2004-12-01","temporalEnd":"2005-02-28","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":125993,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2010_5175.jpg"},{"id":393787,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_94308.htm"},{"id":14156,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2010/5175/","linkFileType":{"id":5,"text":"html"}}],"projection":"Albers Equal Area Conic Projection","country":"United States","state":"California","otherGeospatial":"San Joaquin Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.8528,\n              37.5667\n            ],\n            [\n              -120.6439,\n              37.5667\n            ],\n            [\n              -120.6439,\n              38.5\n            ],\n            [\n              -121.8528,\n              38.5\n            ],\n            [\n              -121.8528,\n              37.5667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dae4b07f02db5e02d6","contributors":{"authors":[{"text":"Bennett, George L. 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V","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":306338,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fram, Miranda S. 0000-0002-6337-059X mfram@usgs.gov","orcid":"https://orcid.org/0000-0002-6337-059X","contributorId":1156,"corporation":false,"usgs":true,"family":"Fram","given":"Miranda","email":"mfram@usgs.gov","middleInitial":"S.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":306337,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Belitz, Kenneth 0000-0003-4481-2345 kbelitz@usgs.gov","orcid":"https://orcid.org/0000-0003-4481-2345","contributorId":442,"corporation":false,"usgs":true,"family":"Belitz","given":"Kenneth","email":"kbelitz@usgs.gov","affiliations":[{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true}],"preferred":true,"id":306336,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jurgens, Bryant C. 0000-0002-1572-113X","orcid":"https://orcid.org/0000-0002-1572-113X","contributorId":22454,"corporation":false,"usgs":true,"family":"Jurgens","given":"Bryant C.","affiliations":[],"preferred":false,"id":306339,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70157334,"text":"70157334 - 2010 - Using selective drainage methods to hydrologically-condition and hydrologically-enforce lidar-derived surface flow","interactions":[],"lastModifiedDate":"2017-05-16T16:08:28","indexId":"70157334","displayToPublicDate":"2010-09-30T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Using selective drainage methods to hydrologically-condition and hydrologically-enforce lidar-derived surface flow","docAbstract":"<p><span>The methods to extract surface flow from coarse elevation data are well documented; however, the methods to extract surface flow from high-resolution, high-vertical accuracy digital elevation models (DEMs) derived from light detection and ranging (lidar) are less documented, but yet more complex. As lidar data are increasingly used to generate DEMS, the demand for lidar-derived surface flow escalates. Thus, the US Geological Survey has developed semi-automated selective drainage methods to extract continuous surface flow from lidar-derived DEMs. This integrated network is important in understanding surface water movement and runoff, flood inundation, and erosion.</span></p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Remote sensing and hydrology","conferenceTitle":"International Commission on Remote Sensing of IAHS","conferenceDate":"September 27-30 2010","conferenceLocation":"Jacksonhole, Wyoming","language":"English","publisher":"IAHS Press","usgsCitation":"Poppenga, S.K., Worstell, B., Stoker, J.M., and Greenlee, S., 2010, Using selective drainage methods to hydrologically-condition and hydrologically-enforce lidar-derived surface flow, <i>in</i> Remote sensing and hydrology, v. 352, Jacksonhole, Wyoming, September 27-30 2010, p. 329-332.","productDescription":"4 p.","startPage":"329","endPage":"332","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-022623","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":308296,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"352","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55fd35c2e4b05d6c4e502c89","contributors":{"authors":[{"text":"Poppenga, Sandra K. 0000-0002-2846-6836 spoppenga@usgs.gov","orcid":"https://orcid.org/0000-0002-2846-6836","contributorId":3327,"corporation":false,"usgs":true,"family":"Poppenga","given":"Sandra","email":"spoppenga@usgs.gov","middleInitial":"K.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true},{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":572726,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Worstell, Bruce 0000-0001-8927-3336","orcid":"https://orcid.org/0000-0001-8927-3336","contributorId":90676,"corporation":false,"usgs":true,"family":"Worstell","given":"Bruce","affiliations":[],"preferred":false,"id":572727,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stoker, Jason M. 0000-0003-2455-0931 jstoker@usgs.gov","orcid":"https://orcid.org/0000-0003-2455-0931","contributorId":3021,"corporation":false,"usgs":true,"family":"Stoker","given":"Jason","email":"jstoker@usgs.gov","middleInitial":"M.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true},{"id":423,"text":"National Geospatial Program","active":true,"usgs":true}],"preferred":true,"id":572728,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Greenlee, Susan","contributorId":48137,"corporation":false,"usgs":true,"family":"Greenlee","given":"Susan","affiliations":[],"preferred":false,"id":572729,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":98750,"text":"ofr20101238 - 2010 - Otolith analysis of pre-restoration habitat use by Chinook salmon in the delta-flats and nearshore regions of the Nisqually River Estuary","interactions":[],"lastModifiedDate":"2012-02-10T00:11:57","indexId":"ofr20101238","displayToPublicDate":"2010-09-30T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-1238","title":"Otolith analysis of pre-restoration habitat use by Chinook salmon in the delta-flats and nearshore regions of the Nisqually River Estuary","docAbstract":"The Nisqually Fall Chinook population is one of 27 salmon stocks in the Puget Sound (Washington) evolutionarily significant unit listed as threatened under the federal Endangered Species Act (ESA). Extensive restoration of the Nisqually River delta ecosystem is currently taking place to assist in recovery of the stock as juvenile Fall Chinook salmon are dependent on the estuary. A pre-restoration baseline that includes the characterization of life history strategies, estuary residence times, growth rates, and habitat use is needed to evaluate the potential response of hatchery and natural origin Chinook salmon to restoration efforts and to determine restoration success. Otolith analysis was selected as a tool to examine Chinook salmon life history, growth, and residence in the Nisqually River estuary. Previously funded work on samples collected in 2004 (marked and unmarked) and 2005 (unmarked only) partially established a juvenile baseline on growth rates and length of residence associated with various habitats (freshwater, forested riverine tidal, emergent forested transition, estuarine emergent marsh, delta-flats and nearshore). However, residence times and growth rates for the delta-flats (DF) and nearshore (NS) habitats have been minimally documented due to small sample sizes. The purpose of the current study is to incorporate otolith microstructural analysis using otoliths from fish collected within the DF and NS habitats during sampling years 2004-08 to increase sample size and further evaluate between-year variation in otolith microstructure. Our results from this analysis indicated the delta-flats check (DFCK) on unmarked and marked Chinook samples in 2005-08 varied slightly in appearance from that seen on samples previously analyzed only from 2004. A fry migrant life history was observed on otoliths of unmarked Chinook collected in 2005, 2007, and 2008. Generally, freshwater mean increment width of unmarked fish, on average, was smaller compared to marked Chinook followed by tidal delta and DF/NS portions respectively. On average, the complete tidal delta growth rate was higher for marked Chinook compared to unmarked Chinook. The DF/NS growth rate was highest for unmarked and marked Chinook during 2008 compared to all other sampling years. The average DF/NS growth rate on unmarked Chinook was consistently lower than marked Chinook during all years; however, sample sizes were small during some years. Unmarked Chinook, on average, spent longer in the tidal delta compared to marked Chinook. Our results from this report suggest that otolith microstructural analysis can be a valuable tool in establishing baseline information on the utilization of Nisqually River estuary habitats by juvenile Chinook salmon prior to the newly funded restoration efforts.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20101238","collaboration":"Final Report Presented to the Nisqually Indian Tribe","usgsCitation":"Lind-Null, A., and Larsen, K., 2010, Otolith analysis of pre-restoration habitat use by Chinook salmon in the delta-flats and nearshore regions of the Nisqually River Estuary: U.S. Geological Survey Open-File Report 2010-1238, iv, 28 p., https://doi.org/10.3133/ofr20101238.","productDescription":"iv, 28 p.","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"2005-01-01","temporalEnd":"2008-12-31","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":125999,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1238.jpg"},{"id":14160,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1238/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.66666666666667,47 ], [ -122.66666666666667,47.25 ], [ -122.5,47.25 ], [ -122.5,47 ], [ -122.66666666666667,47 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a4a7","contributors":{"authors":[{"text":"Lind-Null, Angie","contributorId":9369,"corporation":false,"usgs":true,"family":"Lind-Null","given":"Angie","affiliations":[],"preferred":false,"id":306350,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Larsen, Kim","contributorId":101762,"corporation":false,"usgs":true,"family":"Larsen","given":"Kim","affiliations":[],"preferred":false,"id":306351,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":98751,"text":"fs20103069 - 2010 - Groundwater resources of Mosteiros basin, island of Fogo, Cape Verde, West Africa","interactions":[],"lastModifiedDate":"2018-03-21T15:13:26","indexId":"fs20103069","displayToPublicDate":"2010-09-30T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-3069","title":"Groundwater resources of Mosteiros basin, island of Fogo, Cape Verde, West Africa","docAbstract":"Groundwater resources in Cape Verde provide water for agriculture, industry, and human consumption. These resources are limited and susceptible to contamination. Additional groundwater resources are needed for continued agricultural development, particularly during times of drought, but increased use and (or) climatic change may have adverse effects on the quantity and quality of freshwater available. In volcanic island aquifers such as those of Cape Verde, a lens of fresh groundwater typically ?floats? upon a layer of brackish water at the freshwater/saltwater boundary, and increased pumping may cause salt water intrusion or other contamination. A recent U.S. Geological Survey study assessed baseline groundwater conditions in watersheds on three islands of Cape Verde to provide the scientific basis for sustainably developing water resources and minimizing future groundwater depletion and contamination.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20103069","collaboration":"Prepared in cooperation with the Millennium Challenge Corporation","usgsCitation":"Heilweil, V.M., Gingerich, S.B., Plummer, N., and Verstraeten, I.M., 2010, Groundwater resources of Mosteiros basin, island of Fogo, Cape Verde, West Africa: U.S. Geological Survey Fact Sheet 2010-3069, 3 p.; PDF do Relatório em Português (PDF of Report in Portuguese), https://doi.org/10.3133/fs20103069.","productDescription":"3 p.; PDF do Relatório em Português (PDF of Report in Portuguese)","numberOfPages":"3","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":125996,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2010_3069.jpg"},{"id":334722,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2010/3069/pdf/fs20103069Port.pdf","text":"Relatório em Português (Report in Portuguese)","size":"1.1 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":334721,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2010/3069/pdf/fs20103069Eng.pdf","text":"Report in English","size":"1.1 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":14161,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2010/3069/","linkFileType":{"id":5,"text":"html"}}],"scale":"1","projection":"Cabo Verde National Grid Projection","country":"Cape Verde","otherGeospatial":"Island of Fogo, Mosteiros Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -25.333333333333332,14.75 ], [ -25.333333333333332,17.333333333333332 ], [ -22.666666666666668,17.333333333333332 ], [ -22.666666666666668,14.75 ], [ -25.333333333333332,14.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a91e4b07f02db656979","contributors":{"authors":[{"text":"Heilweil, Victor M. heilweil@usgs.gov","contributorId":837,"corporation":false,"usgs":true,"family":"Heilweil","given":"Victor","email":"heilweil@usgs.gov","middleInitial":"M.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":306352,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gingerich, Stephen B. 0000-0002-4381-0746 sbginger@usgs.gov","orcid":"https://orcid.org/0000-0002-4381-0746","contributorId":1426,"corporation":false,"usgs":true,"family":"Gingerich","given":"Stephen","email":"sbginger@usgs.gov","middleInitial":"B.","affiliations":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true},{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":306353,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":306355,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Verstraeten, Ingrid M. imverstr@usgs.gov","contributorId":3630,"corporation":false,"usgs":true,"family":"Verstraeten","given":"Ingrid","email":"imverstr@usgs.gov","middleInitial":"M.","affiliations":[{"id":5066,"text":"Office of the Director USGS","active":true,"usgs":true}],"preferred":true,"id":306354,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":98766,"text":"ofr20101159 - 2010 - Effects of the 2008 high-flow experiment on water quality in Lake Powell and Glen Canyon Dam releases, Utah-Arizona","interactions":[],"lastModifiedDate":"2024-04-22T20:29:16.159935","indexId":"ofr20101159","displayToPublicDate":"2010-09-30T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-1159","title":"Effects of the 2008 high-flow experiment on water quality in Lake Powell and Glen Canyon Dam releases, Utah-Arizona","docAbstract":"<p>Under the direction of the Secretary of the Interior, the U.S. Geological Survey‘s Grand Canyon Monitoring and Research Center (GCMRC) conducted a high-flow experiment (HFE) at Glen Canyon Dam (GCD) from March 4 through March 9, 2008. This experiment was conducted under enriched sediment conditions in the Colorado River within Grand Canyon and was designed to rebuild sandbars, aid endangered humpback chub (<i>Gila cypha</i>), and benefit various downstream resources, including rainbow trout (<i>Oncorhynchus mykiss</i>), the aquatic food base, riparian vegetation, and archaeological sites. During the experiment, GCD discharge increased to a maximum of 1,160 m<sup>3</sup>/s and remained at that rate for 2.5 days by near-capacity operation of the hydroelectric powerplant at 736 m<sup>3</sup>/s, augmented by discharge from the river outlet works (ROW) at 424 m<sup>3</sup>/s. The ROW releases water from Lake Powell approximately 30 m below the powerplant penstock elevation and bypasses the powerplant turbines. During the HFE, the surface elevation of Lake Powell was reduced by 0.8 m.</p><p>This report describes studies that were conducted before and after the experiment to determine the effects of the HFE on (1) the stratification in Lake Powell in the forebay immediately upstream of GCD and (2) the water quality of combined GCD releases and changes that occurred through the tailwater below the dam. The effects of the HFE to the water quality and stratigraphy in the water column of the GCD forebay and upstream locations in Lake Powell were minimal, compared to those during the beach/habitat-building flow experiment conducted in 1996, in which high releases of 1,273 m<sup>3</sup>/s were sustained for a 9-day period. However, during the 2008 HFE, there was evidence of increased advective transport of reservoir water at the penstock withdrawal depth and subsequent mixing of this withdrawal current with water above and below this depth. Reservoir hydrodynamics during the HFE period were largely being controlled by a winter inflow density current, which was moving through the deepest portion of the reservoir and approaching GCD near the end of the experiment. Compared to the beach/habitat-building flow experiment of 1996, the 2008 HFE had less affect on the reservoir because of the decreased volume of discharge from the dam and the different behavior of the winter inflow density current.</p><p>The operation of the ROW increased the dissolved oxygen (DO) concentration of GCD releases and resulted in DO supersaturation at higher release volumes. The jets of water discharged from the ROW caused these increases. Elevated DO concentrations persisted through the tailwater of the dam to Lees Ferry. At maximum ROW operation, downstream DO concentrations increased to approximately 120 percent of saturation.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20101159","collaboration":"Grand Canyon Monitoring and Research Center","usgsCitation":"Vernieu, W., 2010, Effects of the 2008 high-flow experiment on water quality in Lake Powell and Glen Canyon Dam releases, Utah-Arizona: U.S. Geological Survey Open-File Report 2010-1159, Report: vi, 25 p.; 2 Tables, https://doi.org/10.3133/ofr20101159.","productDescription":"Report: vi, 25 p.; 2 Tables","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"links":[{"id":428018,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_94314.htm","linkFileType":{"id":5,"text":"html"}},{"id":126000,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1159.jpg"},{"id":14176,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1159/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Arizona, Utah","otherGeospatial":"Glen Canyon Dam, Lake Powell","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -110.74228148200983,\n              37.13046910286759\n            ],\n            [\n              -110.90379403048038,\n              37.28054922868934\n            ],\n            [\n              -111.46370419851155,\n              37.145490543222394\n            ],\n            [\n              -111.63598425021337,\n              37.001591608787834\n            ],\n            [\n              -111.63914616667464,\n              36.826120184758096\n            ],\n            [\n              -111.54373095479677,\n              36.77966129375976\n            ],\n            [\n              -110.87969176773697,\n              37.025057949831876\n            ],\n            [\n              -110.74228148200983,\n              37.13046910286759\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db6105ef","contributors":{"authors":[{"text":"Vernieu, William S.","contributorId":49068,"corporation":false,"usgs":true,"family":"Vernieu","given":"William S.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":false,"id":306411,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":98755,"text":"fs20103036 - 2010 - PAGER--Rapid assessment of an earthquakes impact","interactions":[{"subject":{"id":80797,"text":"fs20073101 - 2007 - PAGER - Rapid Assessment of an Earthquake's Impact","indexId":"fs20073101","publicationYear":"2007","noYear":false,"title":"PAGER - Rapid Assessment of an Earthquake's Impact"},"predicate":"SUPERSEDED_BY","object":{"id":98755,"text":"fs20103036 - 2010 - PAGER--Rapid assessment of an earthquakes impact","indexId":"fs20103036","publicationYear":"2010","noYear":false,"title":"PAGER--Rapid assessment of an earthquakes impact"},"id":1}],"lastModifiedDate":"2019-07-11T07:23:23","indexId":"fs20103036","displayToPublicDate":"2010-09-30T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-3036","title":"PAGER--Rapid assessment of an earthquakes impact","docAbstract":"PAGER (Prompt Assessment of Global Earthquakes for Response) is an automated system that produces content concerning the impact of significant earthquakes around the world, informing emergency responders, government and aid agencies, and the media of the scope of the potential disaster. PAGER rapidly assesses earthquake impacts by comparing the population exposed to each level of shaking intensity with models of economic and fatality losses based on past earthquakes in each country or region of the world. Earthquake alerts--which were formerly sent based only on event magnitude and location, or population exposure to shaking--now will also be generated based on the estimated range of fatalities and economic losses.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20103036","usgsCitation":"Wald, D., Jaiswal, K., Marano, K.D., Bausch, D., and Hearne, M., 2010, PAGER--Rapid assessment of an earthquakes impact: U.S. Geological Survey Fact Sheet 2010-3036, 4 p., https://doi.org/10.3133/fs20103036.","productDescription":"4 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true},{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"links":[{"id":125982,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2010_3036.jpg"},{"id":14165,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2010/3036/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689f3e","contributors":{"authors":[{"text":"Wald, D.J. 0000-0002-1454-4514","orcid":"https://orcid.org/0000-0002-1454-4514","contributorId":43809,"corporation":false,"usgs":true,"family":"Wald","given":"D.J.","affiliations":[],"preferred":false,"id":306365,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jaiswal, K.","contributorId":89260,"corporation":false,"usgs":true,"family":"Jaiswal","given":"K.","affiliations":[],"preferred":false,"id":306367,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Marano, K. D.","contributorId":92390,"corporation":false,"usgs":false,"family":"Marano","given":"K.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":306369,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bausch, D.","contributorId":90423,"corporation":false,"usgs":true,"family":"Bausch","given":"D.","email":"","affiliations":[],"preferred":false,"id":306368,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hearne, M.","contributorId":86873,"corporation":false,"usgs":true,"family":"Hearne","given":"M.","email":"","affiliations":[],"preferred":false,"id":306366,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":98760,"text":"ofr20101180 - 2010 - Description of extreme-wave deposits on the northern coast of Bonaire, Netherlands Antilles","interactions":[],"lastModifiedDate":"2012-02-02T00:15:44","indexId":"ofr20101180","displayToPublicDate":"2010-09-30T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-1180","title":"Description of extreme-wave deposits on the northern coast of Bonaire, Netherlands Antilles","docAbstract":"To develop a better understanding of the origins of extreme-wave deposits and to help assess the potential risk of future overwash events, a field mapping survey was conducted in November 2006 on the northern coast of Bonaire, Netherlands Antilles. Deposits were mapped and analyzed to help develop a systematic sedimentological approach to distinguish the type of extreme-wave event (tsunamis or storms) or combination of events that formed and modified the deposits over time. \r\n\r\nExtreme-wave deposits on the northern coast of Bonaire between Boka Onima and Boka Olivia have formed sand sheets, poly-modal ridge complexes, and boulder fields on a Pleistocene limestone platform 3?8 meters above sea level. The deposits exhibit characteristics that are consistent with both large storm and tsunami processes that often overlap one another. Sand sheets occur as low-relief features underlying and incorporated with boulder field deposits. The seaward edge of ridge complexes are deposited up to 70 m from the shoreline and can extend over 200 m inland. Over 600 clasts were measured in fields and range in size from coarse gravel to fine block, weigh up to 165 metric tons, and are placed over 280 m from the shoreline. \r\n\r\nOur analyses indicate that the deposits may have been produced by a combination of hurricane and tsunami events spanning 10s to 1000s of years. Comparing the different deposit morphologies between study sites highlights the importance of shoreline orientation to the distribution of extreme-wave deposits onshore. However, further investigation is required to fully understand the processes that have produced and modified these deposits over time. \r\n","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20101180","usgsCitation":"Watt, S.G., Jaffe, B.E., Morton, R., Richmond, B.M., and Gelfencaum, G., 2010, Description of extreme-wave deposits on the northern coast of Bonaire, Netherlands Antilles: U.S. Geological Survey Open-File Report 2010-1180, vi, 64 p., https://doi.org/10.3133/ofr20101180.","productDescription":"vi, 64 p.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":125985,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1180.jpg"},{"id":14170,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1180/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cc2a","contributors":{"authors":[{"text":"Watt, Steven G.","contributorId":48675,"corporation":false,"usgs":true,"family":"Watt","given":"Steven","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":306395,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jaffe, Bruce E. 0000-0002-8816-5920 bjaffe@usgs.gov","orcid":"https://orcid.org/0000-0002-8816-5920","contributorId":2049,"corporation":false,"usgs":true,"family":"Jaffe","given":"Bruce","email":"bjaffe@usgs.gov","middleInitial":"E.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":306393,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morton, Robert A.","contributorId":88333,"corporation":false,"usgs":true,"family":"Morton","given":"Robert A.","affiliations":[],"preferred":false,"id":306396,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Richmond, Bruce M. 0000-0002-0056-5832 brichmond@usgs.gov","orcid":"https://orcid.org/0000-0002-0056-5832","contributorId":2459,"corporation":false,"usgs":true,"family":"Richmond","given":"Bruce","email":"brichmond@usgs.gov","middleInitial":"M.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":306394,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gelfencaum, Guy","contributorId":96389,"corporation":false,"usgs":true,"family":"Gelfencaum","given":"Guy","email":"","affiliations":[],"preferred":false,"id":306397,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":98764,"text":"ofr20101168 - 2010 - Surface-wave site characterization at 52 strong-motion recording stations affected by the Parkfield, California, M6.0 earthquake of 28 September 2004","interactions":[],"lastModifiedDate":"2024-07-01T18:52:46.89902","indexId":"ofr20101168","displayToPublicDate":"2010-09-30T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-1168","title":"Surface-wave site characterization at 52 strong-motion recording stations affected by the Parkfield, California, M6.0 earthquake of 28 September 2004","docAbstract":"<p><span>We present one-dimensional shear-wave velocity (</span><i>V<sub>S</sub></i><span>) profiles at 52 strong-motion sites that recorded the 28 September 2004 Magnitude 6.0 Parkfield, Calif., earthquake. We estimate the&nbsp;</span><i>V<sub>S</sub></i><span>&nbsp;profiles with the Spectral Analysis of Surface-Waves (SASW) method. The SASW method is a noninvasive method that indirectly estimates the&nbsp;</span><i>V<sub>S</sub></i><span>&nbsp;at depth from variations in the Rayleigh wave phase velocity at the surface. To address the uncertainty associated with these measurements, we compare the SASW profiles to surface-source downhole-receiver (SSDR) profiles at four sites. Three of the four SSDR sites are in close agreement with the adjacent SASW site, while the SASW profile is considerably slower than the SSDR profile at one site.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20101168","collaboration":"In Cooperation with Tufts University","usgsCitation":"Thompson, E., Kayen, R., Carkin, B., and Tanaka, H., 2010, Surface-wave site characterization at 52 strong-motion recording stations affected by the Parkfield, California, M6.0 earthquake of 28 September 2004: U.S. Geological Survey Open-File Report 2010-1168, Report: iii, 10 p.; Data Package, https://doi.org/10.3133/ofr20101168.","productDescription":"Report: iii, 10 p.; Data Package","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":430681,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_94315.htm","linkFileType":{"id":5,"text":"html"}},{"id":14174,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1168/","linkFileType":{"id":5,"text":"html"}},{"id":125998,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1168.jpg"}],"country":"United States","state":"California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -120.71036426400353,\n              35.589603573785055\n            ],\n            [\n              -120.12290885089635,\n              35.589603573785055\n            ],\n            [\n              -120.12290885089635,\n              36.05690143110107\n            ],\n            [\n              -120.71036426400353,\n              36.05690143110107\n            ],\n            [\n              -120.71036426400353,\n              35.589603573785055\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a458","contributors":{"authors":[{"text":"Thompson, Eric M.","contributorId":79193,"corporation":false,"usgs":false,"family":"Thompson","given":"Eric M.","affiliations":[{"id":6608,"text":"San Diego State University","active":true,"usgs":false}],"preferred":false,"id":306407,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kayen, Robert E. rkayen@usgs.gov","contributorId":2787,"corporation":false,"usgs":true,"family":"Kayen","given":"Robert E.","email":"rkayen@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":306405,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carkin, Brad","contributorId":65555,"corporation":false,"usgs":true,"family":"Carkin","given":"Brad","affiliations":[],"preferred":false,"id":306406,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tanaka, Hajime","contributorId":104344,"corporation":false,"usgs":true,"family":"Tanaka","given":"Hajime","email":"","affiliations":[],"preferred":false,"id":306408,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":98763,"text":"ofr20091254 - 2010 - Preliminary bedrock geologic map of the Seward Peninsula, Alaska, and accompanying conodont data","interactions":[],"lastModifiedDate":"2022-04-14T21:52:37.369414","indexId":"ofr20091254","displayToPublicDate":"2010-09-30T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2009-1254","title":"Preliminary bedrock geologic map of the Seward Peninsula, Alaska, and accompanying conodont data","docAbstract":"This 1:500,000-scale geologic map depicts the bedrock geology of Seward Peninsula, western Alaska, on the North American side of the Bering Strait. The map encompasses all of the Teller, Nome, Solomon, and Bendeleben 1:250,000-scale quadrangles, and parts of the Shishmaref, Kotzebue, Candle, and Norton Bay 1:250,000-scale quadrangles (sheet 1; sheet 2). \r\n\r\nThe geologic map is presented on Sheet 1. The pamphlet includes an introductory text, unit descriptions, tables of geochronologic data, and an appendix containing conodont (microfossil) data and a text about those data. Sheet 2 shows metamorphic and tectonic units, conodont color alteration indices, key metamorphic minerals, and locations of geochronology samples listed in the pamphlet.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20091254","usgsCitation":"Till, A.B., Dumoulin, J.A., Werdon, M., and Bleick, H.A., 2010, Preliminary bedrock geologic map of the Seward Peninsula, Alaska, and accompanying conodont data: U.S. Geological Survey Open-File Report 2009-1254, Report: iv, 43 p.; Appendices; 2 Plates: 48.28 inches x 24.61 inches and 35.83 inches x 24.61 inches, https://doi.org/10.3133/ofr20091254.","productDescription":"Report: iv, 43 p.; Appendices; 2 Plates: 48.28 inches x 24.61 inches and 35.83 inches x 24.61 inches","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":386,"text":"Mineral Resources - Alaska","active":false,"usgs":true}],"links":[{"id":125980,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2009_1254.jpg"},{"id":398791,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_94317.htm"},{"id":14173,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2009/1254/","linkFileType":{"id":5,"text":"html"}}],"scale":"500000","projection":"Universal Transverse Mercator Zone","country":"United States","state":"Alaska","otherGeospatial":"Seward Peninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -168.9614,\n              64.3214\n            ],\n            [\n              -161,\n              64.3214\n            ],\n            [\n              -161,\n              66.5981\n            ],\n            [\n              -168.9614,\n              66.5981\n            ],\n            [\n              -168.9614,\n              64.3214\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c95a","contributors":{"authors":[{"text":"Till, Alison B. atill@usgs.gov","contributorId":2482,"corporation":false,"usgs":true,"family":"Till","given":"Alison","email":"atill@usgs.gov","middleInitial":"B.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":306402,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dumoulin, Julie A. 0000-0003-1754-1287 dumoulin@usgs.gov","orcid":"https://orcid.org/0000-0003-1754-1287","contributorId":203209,"corporation":false,"usgs":true,"family":"Dumoulin","given":"Julie","email":"dumoulin@usgs.gov","middleInitial":"A.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":306401,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Werdon, Melanie B.","contributorId":53345,"corporation":false,"usgs":true,"family":"Werdon","given":"Melanie B.","affiliations":[],"preferred":false,"id":306404,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bleick, Heather A. hbleick@usgs.gov","contributorId":2484,"corporation":false,"usgs":true,"family":"Bleick","given":"Heather","email":"hbleick@usgs.gov","middleInitial":"A.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"preferred":true,"id":306403,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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