{"pageNumber":"2904","pageRowStart":"72575","pageSize":"25","recordCount":184606,"records":[{"id":51536,"text":"ofr03201 - 2003 - Sequence-Stratigraphic Analysis of the Regional Observation Monitoring Program (ROMP) 29A Test Corehole and Its Relation to Carbonate Porosity and Regional Transmissivity in the Floridan Aquifer System, Highlands County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:11:13","indexId":"ofr03201","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-201","title":"Sequence-Stratigraphic Analysis of the Regional Observation Monitoring Program (ROMP) 29A Test Corehole and Its Relation to Carbonate Porosity and Regional Transmissivity in the Floridan Aquifer System, Highlands County, Florida","docAbstract":"An analysis was made to describe and interpret the lithology of a part of the Upper Floridan aquifer penetrated by the Regional Observation Monitoring Program (ROMP) 29A test corehole in Highlands County, Florida. This information was integrated into a one-dimensional hydrostratigraphic model that delineates candidate flow zones and confining units in the context of sequence stratigraphy. Results from this test corehole will serve as a starting point to build a robust three-dimensional sequence-stratigraphic framework of the Floridan aquifer system. \r\n\r\nThe ROMP 29A test corehole penetrated the Avon Park Formation, Ocala Limestone, Suwannee Limestone, and Hawthorn Group of middle Eocene to Pliocene age. The part of the Avon Park Formation penetrated in the ROMP 29A test corehole contains two composite depositional sequences. A transgressive systems tract and a highstand systems tract were interpreted for the upper composite sequence; however, only a highstand systems tract was interpreted for the lower composite sequence of the deeper Avon Park stratigraphic section. The composite depositional sequences are composed of at least five high-frequency depositional sequences. These sequences contain high-frequency cycle sets that are an amalgamation of vertically stacked high-frequency cycles. Three types of high-frequency cycles have been identified in the Avon Park Formation: peritidal, shallow subtidal, and deeper subtidal high-frequency cycles. \r\n\r\nThe vertical distribution of carbonate-rock diffuse flow zones within the Avon Park Formation is heterogeneous. Porous vuggy intervals are less than 10 feet, and most are much thinner. The volumetric arrangement of the diffuse flow zones shows that most occur in the highstand systems tract of the lower composite sequence of the Avon Park Formation as compared to the upper composite sequence, which contains both a backstepping transgressive systems tract and a prograding highstand systems tract. Although the porous and permeable layers are not thick, some intervals may exhibit lateral continuity because of their deposition on a broad low-relief ramp. A thick interval of thin vuggy zones and open faults forms thin conduit flow zones mixed with relatively thicker carbonate-rock diffuse flow zones between a depth of 1,070 and 1,244 feet below land surface (bottom of the test corehole). This interval is the most transmissive part of the Avon Park Formation penetrated in the ROMP 29A test corehole and is included in the highstand systems tract of the lower composite sequence. \r\n\r\nThe Ocala Limestone is considered to be a semiconfining unit and contains three depositional sequences penetrated by the ROMP 29A test corehole. Deposited within deeper subtidal depositional cycles, no zones of enhanced porosity and permeability are expected in the Ocala Limestone. A thin erosional remnant of the shallow marine Suwannee Limestone overlies the Ocala Limestone, and permeability seems to be comparatively low because moldic porosity is poorly connected. Rocks that comprise the lower Hawthorn Group, Suwannee Limestone, and Ocala Limestone form a permeable upper zone of the Upper Floridan aquifer, and rocks of the lower Ocala Limestone and Avon Park Formation form a permeable lower zone of the Upper Floridan aquifer. On the basis of a preliminary analysis of transmissivity estimates for wells located north of Lake Okeechobee, spatial relations among groups of relatively high and low transmissivity values within the upper zone are evident. Upper zone transmissivity is generally less than 10,000 feet squared per day in areas located south of a line that extends through Charlotte, Sarasota, DeSoto, Highlands, Polk, Osceola, Okeechobee, and St. Lucie Counties. Transmissivity patterns within the lower zone of the Avon Park Formation cannot be regionally assessed because insufficient data over a wide areal extent have not been compiled.","language":"ENGLISH","doi":"10.3133/ofr03201","usgsCitation":"Ward, W.C., Cunningham, K., Renken, R., Wacker, M., and Carlson, J., 2003, Sequence-Stratigraphic Analysis of the Regional Observation Monitoring Program (ROMP) 29A Test Corehole and Its Relation to Carbonate Porosity and Regional Transmissivity in the Floridan Aquifer System, Highlands County, Florida: U.S. Geological Survey Open-File Report 2003-201, 34 p., plus appendixes, https://doi.org/10.3133/ofr03201.","productDescription":"34 p., plus appendixes","costCenters":[],"links":[{"id":4553,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr03-201/","linkFileType":{"id":5,"text":"html"}},{"id":176526,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b07e4b07f02db69ad80","contributors":{"authors":[{"text":"Ward, W. C.","contributorId":8925,"corporation":false,"usgs":false,"family":"Ward","given":"W.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":243874,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cunningham, K.J.","contributorId":39852,"corporation":false,"usgs":true,"family":"Cunningham","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":243875,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Renken, R.A.","contributorId":99161,"corporation":false,"usgs":true,"family":"Renken","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":243878,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wacker, M.A.","contributorId":91168,"corporation":false,"usgs":true,"family":"Wacker","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":243876,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Carlson, J.I.","contributorId":96344,"corporation":false,"usgs":true,"family":"Carlson","given":"J.I.","email":"","affiliations":[],"preferred":false,"id":243877,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":53169,"text":"fs00103 - 2003 - Hubbard Glacier, Alaska: growing and advancing in spite of global climate change and the 1986 and 2002 Russell Lake outburst floods","interactions":[],"lastModifiedDate":"2012-02-02T00:11:46","indexId":"fs00103","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"001-03","title":"Hubbard Glacier, Alaska: growing and advancing in spite of global climate change and the 1986 and 2002 Russell Lake outburst floods","docAbstract":"Hubbard Glacier, the largest calving glacier on the North American Continent (25 percent larger than Rhode Island), advanced across the entrance to 35-mile-long Russell Fiord during June 2002, temporarily turning it into a lake. Hubbard Glacier has been advancing for more than 100 years and has twice closed the entrance to Russell Fiord during the last 16 years by squeezing and pushing submarine glacial sediments across the mouth of the fiord. Water flowing into the cutoff fiord from mountain streams and glacier melt causes the level of Russell Lake to rise. However, both the 1986 and 2002 dams failed before the lake altitude rose enough for water to spill over a low pass at the far end of the fiord and enter the Situk River drainage, a world-class sport and commercial fishery near Yakutat, Alaska.","language":"ENGLISH","doi":"10.3133/fs00103","usgsCitation":"Trabant, D.C., March, R.S., and Thomas, D.S., 2003, Hubbard Glacier, Alaska: growing and advancing in spite of global climate change and the 1986 and 2002 Russell Lake outburst floods: U.S. Geological Survey Fact Sheet 001-03, 4 p., https://doi.org/10.3133/fs00103.","productDescription":"4 p.","costCenters":[],"links":[{"id":120675,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_001_03.jpg"},{"id":4754,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/fs-001-03/ ","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62a70d","contributors":{"authors":[{"text":"Trabant, Dennis C.","contributorId":13965,"corporation":false,"usgs":true,"family":"Trabant","given":"Dennis","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":246814,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"March, Rod S. rsmarch@usgs.gov","contributorId":416,"corporation":false,"usgs":true,"family":"March","given":"Rod","email":"rsmarch@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":246813,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, Donald S.","contributorId":17296,"corporation":false,"usgs":true,"family":"Thomas","given":"Donald","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":246815,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":53995,"text":"fs20043047 - 2003 - Managing floodplain forests for bird diversity","interactions":[],"lastModifiedDate":"2012-02-02T00:11:40","indexId":"fs20043047","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2004-3047","title":"Managing floodplain forests for bird diversity","language":"ENGLISH","doi":"10.3133/fs20043047","usgsCitation":"Knutson, M., 2003, Managing floodplain forests for bird diversity: U.S. Geological Survey Fact Sheet 2004-3047, 2 p., https://doi.org/10.3133/fs20043047.","productDescription":"2 p.","costCenters":[],"links":[{"id":4819,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.umesc.usgs.gov/reports_publications/fact_sheets/forest_birds.html","linkFileType":{"id":5,"text":"html"}},{"id":122728,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2004_3047.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ab89","contributors":{"authors":[{"text":"Knutson, Melinda","contributorId":27929,"corporation":false,"usgs":true,"family":"Knutson","given":"Melinda","affiliations":[],"preferred":false,"id":248859,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53128,"text":"wri034229 - 2003 - Ground-water resources in the lower Milliken--Sarco--Tulucay Creeks area, southeastern Napa County, California, 2000-2002","interactions":[],"lastModifiedDate":"2012-02-02T00:11:44","indexId":"wri034229","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2003-4229","title":"Ground-water resources in the lower Milliken--Sarco--Tulucay Creeks area, southeastern Napa County, California, 2000-2002","docAbstract":"Ground water obtained from individual private wells is the sole source of water for about 4,800 residents living in the lower Milliken-Sarco-Tulucay Creeks area of southeastern Napa County. Increases in population and in irrigated vineyards during the past few decades have increased water demand. Estimated ground-water pumpage in 2000 was 5,350 acre-feet per year, an increase of about 80 percent since 1975. Water for agricultural irrigation is the dominant use, accounting for about 45 percent of the total. This increase in ground-water extraction has resulted in the general decline of ground-water levels. The purpose of this report is to present selected hydrologic data collected from 1975 to 2002 and to quantify changes in the ground-water system during the past 25 years. \r\n\r\n    The study area lies in one of several prominent northwest-trending structural valleys in the North Coast Ranges. The area is underlain by alluvial deposits and volcanic rocks that exceed 1,000 feet in thickness in some places. Alluvial deposits and tuff beds in the volcanic sequence are the principal source of water to wells.\r\n\r\n    The ground-water system is recharged by precipitation that infiltrates, in minor amounts, directly on the valley floor but mostly by infiltration in the Howell Mountains. Ground water moves laterally from the Howell Mountains into the study area. Although the area receives abundant winter precipitation in most years, nearly half of the precipitation is lost as surface runoff to the Napa River. Evapotranspiration also is high, accounting for nearly one-half of the total precipitation received. Because of the uncertainties in the estimates of precipitation, runoff, and evapotranspiration, a precise estimate of potential ground-water recharge cannot be made.\r\n\r\n    Large changes in ground-water levels occurred between 1975 and 2001. In much of the western part of the area, water levels increased; but in the central and eastern parts, water levels declined by 25 to 125 feet. Ground-water extraction produced three large pumping depressions in the northern and east-central parts of the area. The general decline in ground-water levels is a result of increases in ground-water pumpage and possibly changes in infiltration capacity caused by changes in land use. \r\n\r\nGround-water-level declines during 1960-2002 are evident in the records for 9 of 10 key monitoring wells. In five of these wells, water levels dropped by greater than 20 feet since the 1980s. The largest water-level declines have occurred since the mid 1970s, corresponding with a period of accelerated well construction and ground-water extraction.\r\n\r\n    Analysis of samples from 15 wells indicates that the chemical quality of ground water in the study generally is acceptable. However, arsenic concentrations in samples from five wells exceed the U.S. Environmental Protection Agency primary drinking-water standard of 10 micrograms per liter, and iron concentrations in samples from five wells exceed the U.S. Environmental Protection Agency and the California Department of Health Services secondary drinking-water standard of 300 micrograms per liter. Water from 12 of 15 wells sampled contained concentrations of manganese that exceed the U.S. Environmental Protection Agency and the California Department of Health Services secondary drinking-water standard of 50 micrograms per liter. Two wells produced water that had boron in excess of the California Department of Health Services action level of 1 milligram per liter.\r\n\r\n    Stable isotope, chlorofluorocarbon, and tritium data indicate that ground water in the area is a mixture of waters that recharged the aquifer system at different times. The presence of chlorofluorocarbons and tritium in water from the study area is evidence that modern recharge (post 1950) does take place. Water-temperature logs indicate that ground-water temperatures throughout the study area exceed 30?C at depths in excess of 600 feet. Further, water at ","language":"ENGLISH","doi":"10.3133/wri034229","usgsCitation":"Farrar, C.D., and Metzger, L.F., 2003, Ground-water resources in the lower Milliken--Sarco--Tulucay Creeks area, southeastern Napa County, California, 2000-2002: U.S. Geological Survey Water-Resources Investigations Report 2003-4229, 106 p., https://doi.org/10.3133/wri034229.","productDescription":"106 p.","costCenters":[],"links":[{"id":4707,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri034229/","linkFileType":{"id":5,"text":"html"}},{"id":177858,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696e15","contributors":{"authors":[{"text":"Farrar, Christopher D. cdfarrar@usgs.gov","contributorId":1501,"corporation":false,"usgs":true,"family":"Farrar","given":"Christopher","email":"cdfarrar@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":246714,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Metzger, Loren F. 0000-0003-2454-2966 lmetzger@usgs.gov","orcid":"https://orcid.org/0000-0003-2454-2966","contributorId":1378,"corporation":false,"usgs":true,"family":"Metzger","given":"Loren","email":"lmetzger@usgs.gov","middleInitial":"F.","affiliations":[],"preferred":true,"id":246713,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":51985,"text":"wri034020 - 2003 - Louisiana ground-water map no. 15: Potentiometric surface of the \"1,200-foot\" sand of the Baton Rouge area, Louisiana, spring 2001","interactions":[],"lastModifiedDate":"2012-02-02T00:11:35","indexId":"wri034020","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2003-4020","title":"Louisiana ground-water map no. 15: Potentiometric surface of the \"1,200-foot\" sand of the Baton Rouge area, Louisiana, spring 2001","language":"ENGLISH","doi":"10.3133/wri034020","usgsCitation":"Griffith, J., and Lovelace, J.K., 2003, Louisiana ground-water map no. 15: Potentiometric surface of the \"1,200-foot\" sand of the Baton Rouge area, Louisiana, spring 2001: U.S. Geological Survey Water-Resources Investigations Report 2003-4020, 2 sheets, https://doi.org/10.3133/wri034020.","productDescription":"2 sheets","costCenters":[],"links":[{"id":177252,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":94352,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://la.water.usgs.gov/publications/pdfs/WRI_03-4020.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a73e4b07f02db643d0c","contributors":{"authors":[{"text":"Griffith, J.M.","contributorId":71245,"corporation":false,"usgs":true,"family":"Griffith","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":244611,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lovelace, J. K.","contributorId":64279,"corporation":false,"usgs":true,"family":"Lovelace","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":244610,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":54271,"text":"wdrNJ021 - 2003 - Water Resources Data, New Jersey, Water Year 2002, Volume 1. Surface-Water Data","interactions":[],"lastModifiedDate":"2012-02-02T00:11:36","indexId":"wdrNJ021","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NJ-02-1","title":"Water Resources Data, New Jersey, Water Year 2002, Volume 1. Surface-Water Data","docAbstract":"Water-resources data for the 2002 Water Year for New Jersey are presented in three volumes, and consists of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs; and water levels and water quality of ground water. Volume 1 contains discharge records for 93 gaging stations; tide summaries at 31 gaging stations; and stage and contents at 39 lakes and reservoirs. Also included are stage and discharge for 104 crest-stage partial-record stations and stage-only at 31 tidal crest-stage gages. Locations of these sites are shown in figures 8-11. Additional water data were collected at various sites that are not part of the systematic data-collection program. Discharge measurements were made at 201 low-flow partial-record stations and 121 miscellaneous sites.","language":"ENGLISH","doi":"10.3133/wdrNJ021","usgsCitation":"Reed, T., White, B., Centinaro, G., Dudek, J., Spehar, A., Protz, A., Shvanda, J., Watson, A., and Holzer, G., 2003, Water Resources Data, New Jersey, Water Year 2002, Volume 1. Surface-Water Data: U.S. Geological Survey Water Data Report NJ-02-1, 391 p., https://doi.org/10.3133/wdrNJ021.","productDescription":"391 p.","costCenters":[],"links":[{"id":5383,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdrnj021/","linkFileType":{"id":5,"text":"html"}},{"id":178105,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb261","contributors":{"authors":[{"text":"Reed, T.J. 0000-0002-9943-4081","orcid":"https://orcid.org/0000-0002-9943-4081","contributorId":15224,"corporation":false,"usgs":true,"family":"Reed","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":249711,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, B.T.","contributorId":9710,"corporation":false,"usgs":true,"family":"White","given":"B.T.","email":"","affiliations":[],"preferred":false,"id":249710,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Centinaro, G.L.","contributorId":61892,"corporation":false,"usgs":true,"family":"Centinaro","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":249714,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dudek, J.F.","contributorId":31818,"corporation":false,"usgs":true,"family":"Dudek","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":249712,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Spehar, A.B.","contributorId":76809,"corporation":false,"usgs":true,"family":"Spehar","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":249715,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Protz, A.R.","contributorId":97976,"corporation":false,"usgs":true,"family":"Protz","given":"A.R.","affiliations":[],"preferred":false,"id":249717,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Shvanda, J.C.","contributorId":34999,"corporation":false,"usgs":true,"family":"Shvanda","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":249713,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Watson, A.F.","contributorId":85653,"corporation":false,"usgs":true,"family":"Watson","given":"A.F.","email":"","affiliations":[],"preferred":false,"id":249716,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Holzer, G.K.","contributorId":98803,"corporation":false,"usgs":true,"family":"Holzer","given":"G.K.","email":"","affiliations":[],"preferred":false,"id":249718,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":51543,"text":"ofr03180 - 2003 - Impacts of Hurricane Mitch on water quality and sediments of Lake Izabal, Guatemala","interactions":[],"lastModifiedDate":"2012-02-02T00:11:34","indexId":"ofr03180","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-180","title":"Impacts of Hurricane Mitch on water quality and sediments of Lake Izabal, Guatemala","language":"ENGLISH","doi":"10.3133/ofr03180","usgsCitation":"Michot, T.C., Boustany, R., Arrivillaga, A., and Perez, B., 2003, Impacts of Hurricane Mitch on water quality and sediments of Lake Izabal, Guatemala: U.S. Geological Survey Open-File Report 2003-180, 21 p., https://doi.org/10.3133/ofr03180.","productDescription":"21 p.","costCenters":[],"links":[{"id":4560,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.nwrc.usgs.gov/hurricane/mitch/mckee%20rpt100702.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":178089,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a05e4b07f02db5f8685","contributors":{"authors":[{"text":"Michot, Thomas C. 0000-0002-7044-987X","orcid":"https://orcid.org/0000-0002-7044-987X","contributorId":57935,"corporation":false,"usgs":true,"family":"Michot","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":243899,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boustany, Ronald G.","contributorId":55896,"corporation":false,"usgs":true,"family":"Boustany","given":"Ronald G.","affiliations":[],"preferred":false,"id":243898,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Arrivillaga, Alexandro","contributorId":37004,"corporation":false,"usgs":true,"family":"Arrivillaga","given":"Alexandro","affiliations":[],"preferred":false,"id":243897,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Perez, Brian","contributorId":77224,"corporation":false,"usgs":true,"family":"Perez","given":"Brian","affiliations":[],"preferred":false,"id":243900,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":69632,"text":"i2783 - 2003 - Geologic map of the Rusalka Planitia Quadrangle (V-25), Venus","interactions":[],"lastModifiedDate":"2016-12-28T14:15:48","indexId":"i2783","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2783","title":"Geologic map of the Rusalka Planitia Quadrangle (V-25), Venus","docAbstract":"The Rusalka Planitia quadrangle (herein referred to as V-25) occupies an 8.1 million square kilometer swath of lowlands nestled within the eastern highlands of Aphrodite Terra on Venus. The region (25?-0? N., 150?-180? E.) is framed by the crustal plateau Thetis Regio to the southwest, the coronae of the Diana-Dali chasmata complex to the south, and volcanic rise Atla Regio to the west. Regions to the north, and the quadrangle itself, are part of the vast lowlands, which cover four-fifths of the surface of Venus. \r\n\r\nThe often-unspectacular lowlands of Venus are typically lumped together as ridged or regional plains. However, detailed mapping reveals the mode of resurfacing in V-25's lowlands: a mix of corona-related flow fields and local edifice clusters within planitia superimposed on a background of less clearly interpretable extended flow fields, large volcanoes, probable corona fragments, and edifice-flow complexes. The history detailed within the Rusalka Planitia quadrangle is that of the extended evolution of long-wavelength topographic basins in the presence of episodes of extensive corona-related volcanism, pervasive low-intensity small-scale eruptions, and an early phase of regional circumferential shortening centered on central Aphrodite Terra. Structural reactivation both obscures and illuminates the tectonic development of the region. The data are consistent with progressive lithospheric thickening, although the critical lack of an independent temporal marker on Venus severely hampers our ability to test this claim and correlate between localities. \r\n\r\nTwo broad circular basins dominate V-25 geology: northern Rusalka Planitia lies in the southern half of the quadrangle, whereas the smaller Llorona Planitia sits along the northwestern corner of V-25. Similar large topographic basins occur throughout the lowlands of Venus, and gravity data suggest that some basins may represent dynamic topography over mantle downwellings. Both planitiae include coronae and associated lava flows, as well as fields of volcanic shields. Within each basin, the local geologic histories are relatively well constrained; correlations between the planitiae are difficult without making assumptions. The region between the two basins contains large volcanoes, corona fragments, deformation belts, and shield fields embedded within a topographically higher heterogeneous expanse of rolling plains. \r\n\r\nV-25's most prominent structural grain is a suite of wrinkle ridges that arc around the southwest corner of the quadrangle. A patchy suite of northeast-trending assorted lineaments underlies much of the map area. Although these lineaments originally were narrow fractures, this structural suite appears to have subsequently opened up along extensional troughs near Corpman crater in the southwest corner of the map area and been reactivated as wrinkle ridges at Ran Colles in the middle of the southern boundary of V-25. \r\n\r\nNineteen impact craters dot the quadrangle. Craters Yazruk, du Chatelet, and Caccini contribute large geology- obscuring ejecta halos. Crater densities are too low for either relative or absolute age dating. Ten splotches, presumably associated with meteor airbursts, also occur across V-25.","language":"ENGLISH","doi":"10.3133/i2783","isbn":"0607893796","usgsCitation":"Young, D.A., and Hansen, V.L., 2003, Geologic map of the Rusalka Planitia Quadrangle (V-25), Venus: U.S. Geological Survey IMAP 2783, map, 60 x 42 inches, https://doi.org/10.3133/i2783.","productDescription":"map, 60 x 42 inches","costCenters":[],"links":[{"id":191654,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6286,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i2783/","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60ed26","contributors":{"authors":[{"text":"Young, Duncan A.","contributorId":66358,"corporation":false,"usgs":true,"family":"Young","given":"Duncan","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":280772,"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":280773,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":53282,"text":"wdrAR021 - 2003 - Water resources data, Arkansas, 2002","interactions":[],"lastModifiedDate":"2012-02-02T00:11:41","indexId":"wdrAR021","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"AR-02-1","title":"Water resources data, Arkansas, 2002","docAbstract":"Water resources data for the 2002 water year for Arkansas consist of records of discharge and water quality (physical measurements and chemical concentrations) of streams, water quality of lakes, and groundwater levels and ground-water quality. Data from selected sites in Missouri and Oklahoma also are included. This report contains daily discharge records for 108 surface-water gaging stations and 87 peak-discharge partial-record stations, water-quality data for 65 surface-water stations and 5 wells, and water levels for 15 observation wells. Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements.\r\n\r\n\r\nNote: Historically, this report has been published as a paper report. Beginning with the 2002 water year report, these reports will be available from the World Wide Web at http://ar.water.usgs.gov.","language":"ENGLISH","doi":"10.3133/wdrAR021","usgsCitation":"Brossett, T., and Evans, D., 2003, Water resources data, Arkansas, 2002: U.S. Geological Survey Water Data Report AR-02-1, 465 p., https://doi.org/10.3133/wdrAR021.","productDescription":"465 p.","costCenters":[],"links":[{"id":177298,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4985,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/WDR-AR-02/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f157f","contributors":{"authors":[{"text":"Brossett, T.H.","contributorId":95554,"corporation":false,"usgs":true,"family":"Brossett","given":"T.H.","email":"","affiliations":[],"preferred":false,"id":247172,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Evans, D.A.","contributorId":8551,"corporation":false,"usgs":true,"family":"Evans","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":247171,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":53987,"text":"fs20043036 - 2003 - Pathways of Biological Production in Large Rivers","interactions":[],"lastModifiedDate":"2012-02-02T00:11:40","indexId":"fs20043036","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2004-3036","title":"Pathways of Biological Production in Large Rivers","language":"ENGLISH","doi":"10.3133/fs20043036","usgsCitation":"Gutreuter, S., 2003, Pathways of Biological Production in Large Rivers: U.S. Geological Survey Fact Sheet 2004-3036, 2 p., https://doi.org/10.3133/fs20043036.","productDescription":"2 p.","costCenters":[],"links":[{"id":120625,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2004_3036.jpg"},{"id":4811,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.umesc.usgs.gov/reports_publications/fact_sheets/bio_production.html","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aebd3","contributors":{"authors":[{"text":"Gutreuter, Steve","contributorId":91437,"corporation":false,"usgs":true,"family":"Gutreuter","given":"Steve","affiliations":[],"preferred":false,"id":248847,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50788,"text":"wri024302 - 2003 - Evaluation of candidate rain gages for upgrading precipitation measurement tools for the National Atmospheric Deposition Program","interactions":[],"lastModifiedDate":"2012-02-02T00:11:34","indexId":"wri024302","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2002-4302","title":"Evaluation of candidate rain gages for upgrading precipitation measurement tools for the National Atmospheric Deposition Program","docAbstract":"The National Atmospheric Deposition Program (NADP) was established in 1977 to investigate atmospheric deposition and its effects on the environment. Since its establishment, precipitation records have been obtained at all NADP sites using a gage developed approximately 50 years ago-the Belfort 5-780 mechanical rain gage. In 1998 and 1999, a study was done by the U.S. Geological Survey to evaluate four recently developed, technologically advanced rain gages as possible replacement candidates for the mechanical gage currently (2002) in use by the NADP. The gage types evaluated were the Belfort 3200, Geonor T-200, ETI Noah II, and the OTT PLUVIO. The Belfort 5-780 was included in the study to compare the performance of the rain gage currently (2002) used by NADP to the performance of the more recently developed gages. As a reference gage, the NovaLynx Model 260-2510 National Weather Service type stick gage also was included in the study. Two individual gages of each type were included in the study to evaluate precision between gages of the same type. A two-phase evaluation was completed. Phase I consisted of indoor bench tests with known amounts of simulated rainfall applied in 20 individual tests. Phase II consisted of outdoor testing by collecting precipitation during a 26-week period near Bay St. Louis, Mississippi. The ETI Noah II, OTT PLUVIO, and NovaLynx stick gages consistently recorded depths more commensurate with the amounts of applied simulated rainfall in Phase I testing than the Geonor T-200, Belfort 5-780, and Belfort 3200 gages. Gages where both the median difference between the measured and applied simulated rainfall and the interquartile range of all of their measured minus applied simulated rainfall differences were small (less than or equal to 0.01 inch) were judged to have performed very well in Phase I testing. The median and interquartile-range values were 0.01 inch or less for each of the ETI Noah II gages, OTT PLUVIO gages, and NovaLynx stick gages. The performance of the Geonor T-200 and Belfort 3200 gages was affected by technical problems during Phase I testing. As part of the evaluation of Phase II results, the average weekly precipitation totals obtained from the Belfort 5-780 gages and from each of the gages under consideration as possible replacements for the Belfort 5-780 gage were all compared with the average precipitation weekly totals obtained from two NovaLynx stick gages. The median absolute differences between a particular gage model and the NovaLynx stick reference gage for the 26 weeks of outdoor testing ranged from 0.04 inch for the ETI Noah II and OTT PLUVIO gages to 0.06 inch for the Geonor T-200. The total absolute difference between a particular gage type and the reference gage ranged from 1.23 inches for the Belfort 5-780 to 1.83 inches for the Geonor T-200 gages. Because the Belfort 3200 gages were inoperable for most of the Phase II testing, it is not meaningful to include the results from that gage type in a calculation of median or total absolute differences. The OTT PLUVIO proved to be the most reliable gage in Phase I and II testing, operating trouble free over the duration of the study.","language":"ENGLISH","doi":"10.3133/wri024302","usgsCitation":"Gordon, J.D., 2003, Evaluation of candidate rain gages for upgrading precipitation measurement tools for the National Atmospheric Deposition Program: U.S. Geological Survey Water-Resources Investigations Report 2002-4302, iv, 30 p. : col. ill., col. map ; 28 cm., https://doi.org/10.3133/wri024302.","productDescription":"iv, 30 p. : col. ill., col. map ; 28 cm.","costCenters":[],"links":[{"id":4571,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024302/","linkFileType":{"id":5,"text":"html"}},{"id":177006,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fae47","contributors":{"authors":[{"text":"Gordon, John D. 0000-0001-8396-8524 jgordon@usgs.gov","orcid":"https://orcid.org/0000-0001-8396-8524","contributorId":347,"corporation":false,"usgs":true,"family":"Gordon","given":"John","email":"jgordon@usgs.gov","middleInitial":"D.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":242306,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53985,"text":"fs20043038 - 2003 - At-Risk Riverine Fishes: Paddlefish and Lake Sturgeon","interactions":[],"lastModifiedDate":"2012-02-02T00:11:40","indexId":"fs20043038","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2004-3038","title":"At-Risk Riverine Fishes: Paddlefish and Lake Sturgeon","language":"ENGLISH","doi":"10.3133/fs20043038","usgsCitation":"Knights, B., and Zigler, S., 2003, At-Risk Riverine Fishes: Paddlefish and Lake Sturgeon: U.S. Geological Survey Fact Sheet 2004-3038, 2 p., https://doi.org/10.3133/fs20043038.","productDescription":"2 p.","costCenters":[],"links":[{"id":120623,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2004_3038.jpg"},{"id":4809,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.umesc.usgs.gov/reports_publications/fact_sheets/paddlefish_lake_sturgeon.html","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ce58","contributors":{"authors":[{"text":"Knights, Brent","contributorId":31824,"corporation":false,"usgs":true,"family":"Knights","given":"Brent","affiliations":[],"preferred":false,"id":248845,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zigler, Steve","contributorId":6124,"corporation":false,"usgs":true,"family":"Zigler","given":"Steve","email":"","affiliations":[],"preferred":false,"id":248844,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":53162,"text":"fs09003 - 2003 - Native plants for effective coastal wetland restoration","interactions":[],"lastModifiedDate":"2024-10-09T14:33:46.413791","indexId":"fs09003","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"090-03","title":"Native plants for effective coastal wetland restoration","docAbstract":"<p>Plant communities, along with soils and appropriate water regimes, are essential components of healthy wetland systems. In Louisiana, the loss of wetland habitat continues to be an issue of major concern. Wetland loss is caused by several interacting factors, both natural and human-induced (e.g., erosion and saltwater intrusion from the construction of canals and levees). Recent estimates of annual coastal land loss rates of about 62 km2 (24 mi2 ) over the past decade emphasize the magnitude of this problem. In an attempt to slow the rate of loss and perhaps halt the overall trend, resource managers in Louisiana apply various techniques to restore damaged or degraded habitats to functioning wetland systems.</p><p>Researchers at the U.S. Geological Survey’s National Wetlands Research Center (NWRC) have cooperated with the Louisiana Department of Natural Resources in studies that address effective restoration strategies for coastal wetlands. The studies have identified differences in growth that naturally exist in native Louisiana wetland plant species and genetic varieties (i.e., clones) within species. Clones of a species have a distinctive genetic identity, and some clones may also have distinctive growth responses under various environmental conditions (i.e., preferences). Indeed, large areas of coastal marsh are typically populated by several clones of a plant species, each growing in a microenvironment suited to its preferences.</p><p>These studies will provide information that will assist resource managers in selecting plant species and clones of species with known growth characteristics that can be matched to environmental conditions at potential restoration sites. </p><p>Before the studies began, a collection of several clones from four plant species native to coastal Louisiana was established. The species collected included saltgrass (Distichlis spicata), common reed (Phragmites australis), giant bulrush (Schoenoplectus californicus), and saltmarsh bulrush (Schoenoplectus robustus). Plants connected by roots were collected from public lands across the coastal zone, and then allowed to grow several months and produce new stems and plants from underground stems called “rhizomes.” These procedures maintained the genetic identity of the clones and allowed the plants to adjust to greenhouse conditions before experimental treatments began.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs09003","usgsCitation":"Howard, R.J., 2003, Native plants for effective coastal wetland restoration: U.S. Geological Survey Fact Sheet 090-03, 2 p., https://doi.org/10.3133/fs09003.","productDescription":"2 p.","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":125713,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2003/090/coverthb.jpg"},{"id":4743,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2003/090/fs09003.pdf","text":"Report","size":"467 KB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 090-03"}],"contact":"<p><a href=\"https://pubs.usgs.gov/contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606361","contributors":{"authors":[{"text":"Howard, Rebecca J. 0000-0001-7264-4364 howardr@usgs.gov","orcid":"https://orcid.org/0000-0001-7264-4364","contributorId":2429,"corporation":false,"usgs":true,"family":"Howard","given":"Rebecca","email":"howardr@usgs.gov","middleInitial":"J.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true},{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":246804,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51545,"text":"ofr03178 - 2003 - Hurricane Mitch: effects on mangrove soil characteristics and root contributions to soil stabilization","interactions":[],"lastModifiedDate":"2012-02-02T00:11:34","indexId":"ofr03178","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-178","title":"Hurricane Mitch: effects on mangrove soil characteristics and root contributions to soil stabilization","language":"ENGLISH","doi":"10.3133/ofr03178","usgsCitation":"McKee, K.L., and McGinnis, T.E., 2003, Hurricane Mitch: effects on mangrove soil characteristics and root contributions to soil stabilization: U.S. Geological Survey Open-File Report 2003-178, 58 p., https://doi.org/10.3133/ofr03178.","productDescription":"58 p.","costCenters":[],"links":[{"id":178091,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4562,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.nwrc.usgs.gov/hurricane/mitch/mckee%20rpt100702.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62a3dc","contributors":{"authors":[{"text":"McKee, Karen L. 0000-0001-7042-670X","orcid":"https://orcid.org/0000-0001-7042-670X","contributorId":8927,"corporation":false,"usgs":true,"family":"McKee","given":"Karen","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":243904,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGinnis, Thomas E. II","contributorId":21219,"corporation":false,"usgs":true,"family":"McGinnis","given":"Thomas","suffix":"II","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":243905,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":51389,"text":"ofr2003305 - 2003 - Sonoran Desert: Fragile Land of Extremes","interactions":[],"lastModifiedDate":"2012-02-02T00:11:46","indexId":"ofr2003305","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-305","title":"Sonoran Desert: Fragile Land of Extremes","docAbstract":"'Sonoran Desert: Fragile Land of Extremes' shows how biologists with the U.S. Geological Survey work with other scientists in an effort to better understand native plants and animals such as desert tortoises, saguaro cacti, and Gila monsters. Much of the program was shot in and around Saguaro National Park near Tucson, Arizona. Genetic detective work, using DNA, focuses on understanding the lives of tortoises. Studies of saguaros over many decades clarify how these amazing plants reproduce and thrive in the desert. Threats from fire, diseases in tortoises, and a growing human population motivate the scientists. Their work to identify how these organisms live and survive is a crucial step for the sound management of biological resources on public lands. This 28-minute program, USGS Open-File Report 03-305, was shot entirely in high definition video and produced by the USGS Western Ecological Research Center and Southwest Biological Science Center; produced and directed by Stephen Wessells, Western Region Office of Communications.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr2003305","usgsCitation":"Produced and Directed by Wessells, S., 2003, Sonoran Desert: Fragile Land of Extremes: U.S. Geological Survey Open-File Report 2003-305, 28 Minutes; Available on videocassette (VHS), DVD-ROM, or online (.WMV), https://doi.org/10.3133/ofr2003305.","productDescription":"28 Minutes; Available on videocassette (VHS), DVD-ROM, or online (.WMV)","costCenters":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true},{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":175016,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9825,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://online.wr.usgs.gov/outreach/desert/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e77ab","contributors":{"authors":[{"text":"Produced and Directed by Wessells, Stephen","contributorId":79165,"corporation":false,"usgs":true,"family":"Produced and Directed by Wessells","given":"Stephen","email":"","affiliations":[],"preferred":false,"id":243431,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51456,"text":"ofr03104 - 2003 - Estimates of deep percolation beneath native vegetation, irrigated fields, and the Amargosa-River Channel, Amargosa Desert, Nye County, Nevada","interactions":[],"lastModifiedDate":"2020-02-10T06:39:14","indexId":"ofr03104","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-104","title":"Estimates of deep percolation beneath native vegetation, irrigated fields, and the Amargosa-River Channel, Amargosa Desert, Nye County, Nevada","docAbstract":"<p>The presence and approximate rates of deep percolation beneath areas of native vegetation, irrigated fields, and the Amargosa-River channel in the Amargosa Desert of southern Nevada were evaluated using the chloride mass-balance method and inferred downward velocities of chloride and nitrate peaks. Estimates of deep-percolation rates in the Amargosa Desert are needed for the analysis of regional ground-water flow and transport. An understanding of regional flow patterns is important because ground water originating on the Nevada Test Site may pass through the area before discharging from springs at lower elevations in the Amargosa Desert and in Death Valley. Nine boreholes 10 to 16 meters deep were cored nearly continuously using a hollow-stem auger designed for gravelly sediments. Two boreholes were drilled in each of three irrigated fields in the Amargosa-Farms area, two in the Amargosa-River channel, and one in an undisturbed area of native vegetation. Data from previously cored boreholes beneath undisturbed, native vegetation were compared with the new data to further assess deep percolation under current climatic conditions and provide information on spatial variability.</p><p>The profiles beneath native vegetation were characterized by large amounts of accumulated chloride just below the root zone with almost no further accumulation at greater depths. This pattern is typical of profiles beneath interfluvial areas in arid alluvial basins of the southwestern United States, where salts have been accumulating since the end of the Pleistocene. The profiles beneath irrigated fields and the Amargosa-River channel contained more than twice the volume of water compared to profiles beneath native vegetation, consistent with active deep percolation beneath these sites. Chloride profiles beneath two older fields (cultivated since the 1960’s) as well as the upstream Amargosa-River site were indicative of long-term, quasi-steady deep percolation. Chloride profiles beneath the newest field (cultivated since 1993), the downstream Amargosa-River site, and the edge of an older field were indicative of recently active deep percolation moving previously accumulated salts from the upper profile to greater depths.</p><p>Results clearly indicate that deep percolation and ground-water recharge occur not only beneath areas of irrigation but also beneath ephemeral stream channels, despite the arid climate and infrequency of runoff. Rates of deep percolation beneath irrigated fields ranged from 0.1 to 0.5 m/yr. Estimated rates of deep percolation beneath the Amargosa-River channel ranged from 0.02 to 0.15 m/yr. Only a few decades are needed for excess irrigation water to move through the unsaturated zone and recharge ground water. Assuming vertical, one-dimensional flow, the estimated time for irrigation-return flow to reach the water table beneath the irrigated fields ranged from about 10 to 70 years. In contrast, infiltration from present-day runoff takes centuries to move through the unsaturated zone and reach the water table. The estimated time for water to reach the water table beneath the channel ranged from 140 to 1000 years. These values represent minimum times, as they do not take lateral flow into account. The estimated fraction of irrigation water becoming deep percolation averaged 8 to 16 percent. Similar fractions of infiltration from ephemeral flow events were estimated to become deep percolation beneath the normally dry Amargosa-River channel. In areas where flood-induced channel migration occurs at sub-centennial frequencies, residence times in the unsaturated zone beneath the Amargosa channel could be longer. Estimates of deep percolation presented herein provide a basis for evaluating the importance of recharge from irrigation and channel infiltration in models of ground-water flow from the Nevada Test Site.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/ofr03104","collaboration":"Prepared in cooperation with the Nevada Operations Office, U.S. Department of Energy, under Interagency Agreement DE - AI08 - 96NV11967 ","usgsCitation":"Stonestrom, D.A., Prudic, D.E., Laczniak, R.J., Akstin, K.C., Boyd, R., and Henkelman, K.K., 2003, Estimates of deep percolation beneath native vegetation, irrigated fields, and the Amargosa-River Channel, Amargosa Desert, Nye County, Nevada: U.S. Geological Survey Open-File Report 2003-104, 88 p., https://doi.org/10.3133/ofr03104.","productDescription":"88 p.","costCenters":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":179304,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4464,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr03-104/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Nevada","county":"Nye County","otherGeospatial":"Amargosa Desert","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-115.9082,39.1615],[-115.5191,38.9578],[-115.4725,38.9325],[-115.4433,38.9162],[-115.3694,38.8769],[-115.363,38.874],[-115.242,38.8093],[-115.0969,38.7309],[-115.0777,38.721],[-115.0604,38.7107],[-115.0291,38.6937],[-114.999,38.6777],[-114.9996,38.592],[-114.9997,38.4315],[-114.9994,38.3894],[-115.0004,38.0507],[-115.1185,38.0508],[-115.1436,38.0508],[-115.326,38.0515],[-115.3453,38.0514],[-115.4003,38.051],[-115.4587,38.0506],[-115.6394,38.0512],[-115.6581,38.051],[-115.8404,38.0504],[-115.8931,38.0507],[-115.8938,37.723],[-115.8969,37.5498],[-115.8975,37.2796],[-115.8982,37.1926],[-115.8942,36.8425],[-115.8941,36.686],[-115.8945,36.6702],[-115.8949,36.598],[-115.8949,36.5962],[-115.8946,36.5858],[-115.8947,36.5005],[-115.8945,36.4806],[-115.8949,36.462],[-115.8944,36.457],[-115.8948,36.3087],[-115.8945,36.2923],[-115.8943,36.1957],[-115.8945,36.1608],[-115.8948,36.1163],[-115.8948,36.0927],[-115.895,36.0015],[-115.9178,36.0192],[-115.9518,36.0457],[-115.9925,36.0773],[-116.049,36.1211],[-116.0624,36.1314],[-116.1039,36.1636],[-116.1287,36.1829],[-116.1702,36.2152],[-116.173,36.2174],[-116.2311,36.2626],[-116.2834,36.3028],[-116.2954,36.3122],[-116.3752,36.373],[-116.5107,36.4764],[-116.5247,36.4871],[-116.5589,36.5131],[-116.574,36.5245],[-116.5946,36.54],[-116.6556,36.5867],[-116.6583,36.5888],[-116.6764,36.6024],[-116.706,36.6248],[-116.7895,36.6877],[-116.8424,36.7276],[-116.8453,36.7298],[-116.8806,36.7568],[-116.8912,36.7648],[-116.9237,36.7891],[-116.9641,36.8193],[-116.9783,36.8299],[-116.981,36.8319],[-117.0046,36.8495],[-117.164,36.9688],[-117.1639,36.9698],[-117.1637,37.0182],[-117.164,37.0894],[-117.1642,37.171],[-117.1641,37.1909],[-117.1641,37.1936],[-117.1665,37.6995],[-117.1664,37.714],[-117.1663,37.7285],[-117.1663,37.7435],[-117.1662,37.7585],[-117.1657,38.0019],[-117.2198,38.0482],[-117.2397,38.0483],[-117.239,38.0641],[-117.2408,38.0705],[-117.2653,38.0932],[-117.6896,38.4731],[-118.0197,38.7599],[-118.197,38.9154],[-118.1972,38.9993],[-117.8559,39.0746],[-117.7748,39.092],[-117.7008,39.1058],[-117.6409,39.1149],[-117.5946,39.1231],[-117.4742,39.1431],[-117.3823,39.1562],[-117.3609,39.1585],[-117.3318,39.1629],[-117.3063,39.1634],[-117.2849,39.1633],[-117.1995,39.1632],[-117.0856,39.1628],[-117.0322,39.1626],[-117.0144,39.1626],[-116.9871,39.1625],[-116.9158,39.1631],[-116.7562,39.1622],[-116.7301,39.1625],[-116.5996,39.1616],[-116.5859,39.162],[-116.4815,39.1616],[-116.3497,39.1618],[-116.2358,39.1616],[-116.0548,39.1624],[-115.9082,39.1615]]]},\"properties\":{\"name\":\"Nye\",\"state\":\"NV\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcb37","contributors":{"authors":[{"text":"Stonestrom, David A. 0000-0001-7883-3385 dastones@usgs.gov","orcid":"https://orcid.org/0000-0001-7883-3385","contributorId":2280,"corporation":false,"usgs":true,"family":"Stonestrom","given":"David","email":"dastones@usgs.gov","middleInitial":"A.","affiliations":[{"id":438,"text":"National Research Program - 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,{"id":51515,"text":"ofr03339 - 2003 - Near field receiving water monitoring of trace metals in clams (Macoma balthica) and sediments near the Palo Alto water quality control plant in south San Francisco Bay, California: 2002","interactions":[],"lastModifiedDate":"2020-02-10T18:42:09","indexId":"ofr03339","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-339","title":"Near field receiving water monitoring of trace metals in clams (Macoma balthica) and sediments near the Palo Alto water quality control plant in south San Francisco Bay, California: 2002","docAbstract":"This report presents trace element concentrations analyzed on samples of fine-grained sediments and clams (Macoma balthica) collected from a mudflat one kilometer south of the discharge of the Palo Alto Regional Water Quality Control Plant in South San Francisco Bay. This report serves as a continuation of the Near Field Receiving Water Monitoring Study, which was started in 1994. The data for 2002, herein, are interpreted within that context. Metal concentrations in both sediments and clam tissue samples have been within the range of values produced by seasonal variability. However, copper and zinc, display continued decreases. Copper in sediment was observed to drop below the ERL (Effects Range-Low) concentration for the third consecutive year and zinc concentrations never exceeded the ERL. Yearly average concentrations of copper, zinc and silver in Macoma balthica for 2002 are some of the lowest recorded since monitoring began in 1975. Mercury and selenium concentrations in sediments and clams at Palo Alto were similar concentrations observed elsewhere in the San Francisco Bay.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr03339","usgsCitation":"Moon, E., David, C.P., Luoma, S.N., Cain, D.J., Hornberger, M.I., and Lavigne, I.R., 2003, Near field receiving water monitoring of trace metals in clams (Macoma balthica) and sediments near the Palo Alto water quality control plant in south San Francisco Bay, California: 2002: U.S. Geological Survey Open-File Report 2003-339, HTML, https://doi.org/10.3133/ofr03339.","productDescription":"HTML","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":178559,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4520,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr03-339/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","city":"Palo Alto","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.22908020019531,\n              37.39607337878013\n            ],\n            [\n              -122.07939147949217,\n              37.39607337878013\n            ],\n            [\n              -122.07939147949217,\n              37.51299386065851\n            ],\n            [\n              -122.22908020019531,\n              37.51299386065851\n            ],\n            [\n              -122.22908020019531,\n              37.39607337878013\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db697f90","contributors":{"authors":[{"text":"Moon, Edward","contributorId":60309,"corporation":false,"usgs":true,"family":"Moon","given":"Edward","email":"","affiliations":[],"preferred":false,"id":243789,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"David, Carlos Primo C.","contributorId":27907,"corporation":false,"usgs":true,"family":"David","given":"Carlos","email":"","middleInitial":"Primo C.","affiliations":[],"preferred":false,"id":243788,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Luoma, Samuel N. 0000-0001-5443-5091 snluoma@usgs.gov","orcid":"https://orcid.org/0000-0001-5443-5091","contributorId":2287,"corporation":false,"usgs":true,"family":"Luoma","given":"Samuel","email":"snluoma@usgs.gov","middleInitial":"N.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":243786,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cain, Daniel J. 0000-0002-3443-0493 djcain@usgs.gov","orcid":"https://orcid.org/0000-0002-3443-0493","contributorId":1784,"corporation":false,"usgs":true,"family":"Cain","given":"Daniel","email":"djcain@usgs.gov","middleInitial":"J.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":243785,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hornberger, Michelle I. 0000-0002-7787-3446 mhornber@usgs.gov","orcid":"https://orcid.org/0000-0002-7787-3446","contributorId":1037,"corporation":false,"usgs":true,"family":"Hornberger","given":"Michelle","email":"mhornber@usgs.gov","middleInitial":"I.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":243784,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lavigne, Irene R.","contributorId":17683,"corporation":false,"usgs":true,"family":"Lavigne","given":"Irene","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":243787,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":51516,"text":"ofr03334 - 2003 - Historical and projected coastal Louisiana land changes: 1978-2050","interactions":[],"lastModifiedDate":"2016-09-15T11:15:27","indexId":"ofr03334","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-334","title":"Historical and projected coastal Louisiana land changes: 1978-2050","docAbstract":"<p>An important component of the Louisiana Coastal Area (LCA) Comprehensive Coastwide Ecosystem Restoration Study is the projection of a “future condition” for the Louisiana coast if no further restoration measures were adopted. Such a projection gives an idea of what the future might hold without implementation of the LCA plan and provides a reference against which various ecosystem restoration proposals can be assessed as part of the planning process. One of the most fundamental measures of ecosystem degradation in coastal Louisiana has been the conversion of land (mostly emergent vegetated habitat) to open water. Thus, the projection of the future condition of the ecosystem must be based upon the determination of future patterns of land and water. </p><p>To conduct these projections, a multidisciplinary LCA Land Change Study Group was formed that included individuals from agencies and academia with expertise in remote sensing, geographic information systems (GIS), ecosystem processes, and coastal land loss. Methods were based upon those used in prior studies for Coast 2050 (Louisiana Coastal Wetlands Conservation and Restoration Task Force [LCWCRTF] and the Wetlands Conservation and Restoration Authority 1998, 1999) and modified as described here to incorporate an improved understanding of coastal land loss and land gain processes with more advanced technical capabilities. The basic approach is to use historical data to assess recent trends in land loss and land gain and to project those changes into the future, taking into account spatial variations in the patterns and rates of land loss and land gain. This approach is accomplished by developing a base map, assessing and delineating areas of similar land change (polygons), and projecting changes into the future. This report describes the methodology and compares the current land change projection to previous projections. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03334","usgsCitation":"Barras, J., Beville, S., Britsch, D., Hartley, S., Hawes, S., Johnston, J., Kemp, P., Kinler, Q., Martucci, A., Porthouse, J., Reed, D., Roy, K., Sapkota, S., and Suhayda, J., 2003, Historical and projected coastal Louisiana land changes: 1978-2050 (Revised January 2004; See also FS 2005-3101): U.S. Geological Survey Open-File Report 2003-334, v, 39 p., https://doi.org/10.3133/ofr03334.","productDescription":"v, 39 p.","costCenters":[],"links":[{"id":178668,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8316,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://archive.usgs.gov/archive/sites/www.nwrc.usgs.gov/special/NewHistoricalland.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Revised January 2004; See also FS 2005-3101","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62ed39","contributors":{"authors":[{"text":"Barras, John","contributorId":24437,"corporation":false,"usgs":true,"family":"Barras","given":"John","affiliations":[],"preferred":false,"id":243794,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beville, Shelly","contributorId":18842,"corporation":false,"usgs":true,"family":"Beville","given":"Shelly","email":"","affiliations":[],"preferred":false,"id":243793,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Britsch, Del","contributorId":29884,"corporation":false,"usgs":true,"family":"Britsch","given":"Del","email":"","affiliations":[],"preferred":false,"id":243796,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hartley, Stephen 0000-0003-1380-2769","orcid":"https://orcid.org/0000-0003-1380-2769","contributorId":104566,"corporation":false,"usgs":true,"family":"Hartley","given":"Stephen","affiliations":[],"preferred":false,"id":243803,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hawes, Suzanne","contributorId":51376,"corporation":false,"usgs":true,"family":"Hawes","given":"Suzanne","email":"","affiliations":[],"preferred":false,"id":243797,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Johnston, James","contributorId":80748,"corporation":false,"usgs":true,"family":"Johnston","given":"James","email":"","affiliations":[],"preferred":false,"id":243800,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kemp, Paul","contributorId":92743,"corporation":false,"usgs":true,"family":"Kemp","given":"Paul","email":"","affiliations":[],"preferred":false,"id":243801,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Kinler, Quin","contributorId":53031,"corporation":false,"usgs":true,"family":"Kinler","given":"Quin","email":"","affiliations":[],"preferred":false,"id":243799,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Martucci, Antonio","contributorId":52236,"corporation":false,"usgs":true,"family":"Martucci","given":"Antonio","email":"","affiliations":[],"preferred":false,"id":243798,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Porthouse, Jon","contributorId":11692,"corporation":false,"usgs":true,"family":"Porthouse","given":"Jon","email":"","affiliations":[],"preferred":false,"id":243792,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Reed, Denise","contributorId":6128,"corporation":false,"usgs":true,"family":"Reed","given":"Denise","affiliations":[],"preferred":false,"id":243791,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Roy, Kevin","contributorId":27933,"corporation":false,"usgs":true,"family":"Roy","given":"Kevin","email":"","affiliations":[],"preferred":false,"id":243795,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Sapkota, Sijan sapkotas@usgs.gov","contributorId":2995,"corporation":false,"usgs":true,"family":"Sapkota","given":"Sijan","email":"sapkotas@usgs.gov","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":243790,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Suhayda, Joseph","contributorId":101740,"corporation":false,"usgs":true,"family":"Suhayda","given":"Joseph","email":"","affiliations":[],"preferred":false,"id":243802,"contributorType":{"id":1,"text":"Authors"},"rank":14}]}}
,{"id":50744,"text":"wri034140 - 2003 - Sediment-water interactions affecting dissolved-mercury distributions in Camp Far West Reservoir, California","interactions":[],"lastModifiedDate":"2020-02-11T07:23:50","indexId":"wri034140","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2003-4140","title":"Sediment-water interactions affecting dissolved-mercury distributions in Camp Far West Reservoir, California","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri034140","usgsCitation":"Kuwabara, J.S., Alpers, C.N., Marvin-DiPasquale, M., Topping, B.R., Carter, J.L., Stewart, A., Fend, S.V., Parcheso, F., Moon, G.E., and Krabbenhoft, D.P., 2003, Sediment-water interactions affecting dissolved-mercury distributions in Camp Far West Reservoir, California: U.S. Geological Survey Water-Resources Investigations Report 2003-4140, 61 p., https://doi.org/10.3133/wri034140.","productDescription":"61 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":176854,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4235,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri034140/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California ","otherGeospatial":"Camp Far West Reservoir","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.75,38.75 ], [ -121.75,39.5 ], [ -120.5,39.5 ], [ -120.5,38.75 ], [ -121.75,38.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbdff","contributors":{"authors":[{"text":"Kuwabara, James S. 0000-0003-2502-1601 kuwabara@usgs.gov","orcid":"https://orcid.org/0000-0003-2502-1601","contributorId":3374,"corporation":false,"usgs":true,"family":"Kuwabara","given":"James","email":"kuwabara@usgs.gov","middleInitial":"S.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":242210,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alpers, Charles N. 0000-0001-6945-7365 cnalpers@usgs.gov","orcid":"https://orcid.org/0000-0001-6945-7365","contributorId":411,"corporation":false,"usgs":true,"family":"Alpers","given":"Charles","email":"cnalpers@usgs.gov","middleInitial":"N.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":242205,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Marvin-DiPasquale, Mark","contributorId":57423,"corporation":false,"usgs":true,"family":"Marvin-DiPasquale","given":"Mark","affiliations":[],"preferred":false,"id":242213,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Topping, Brent R. 0000-0002-7887-4221 btopping@usgs.gov","orcid":"https://orcid.org/0000-0002-7887-4221","contributorId":1484,"corporation":false,"usgs":true,"family":"Topping","given":"Brent","email":"btopping@usgs.gov","middleInitial":"R.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":242206,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Carter, James L. 0000-0002-0104-9776 jlcarter@usgs.gov","orcid":"https://orcid.org/0000-0002-0104-9776","contributorId":3278,"corporation":false,"usgs":true,"family":"Carter","given":"James","email":"jlcarter@usgs.gov","middleInitial":"L.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":242209,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Stewart, A. Robin 0000-0003-2918-546X","orcid":"https://orcid.org/0000-0003-2918-546X","contributorId":82436,"corporation":false,"usgs":true,"family":"Stewart","given":"A. Robin","affiliations":[],"preferred":false,"id":242214,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Fend, Steven V. 0000-0002-4638-6602 svfend@usgs.gov","orcid":"https://orcid.org/0000-0002-4638-6602","contributorId":3591,"corporation":false,"usgs":true,"family":"Fend","given":"Steven","email":"svfend@usgs.gov","middleInitial":"V.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":242211,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Parcheso, Francis 0000-0002-9471-7787 parchaso@usgs.gov","orcid":"https://orcid.org/0000-0002-9471-7787","contributorId":2590,"corporation":false,"usgs":true,"family":"Parcheso","given":"Francis","email":"parchaso@usgs.gov","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":false,"id":242208,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Moon, Gerald E.","contributorId":11288,"corporation":false,"usgs":true,"family":"Moon","given":"Gerald","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":242212,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Krabbenhoft, David P. 0000-0003-1964-5020 dpkrabbe@usgs.gov","orcid":"https://orcid.org/0000-0003-1964-5020","contributorId":1658,"corporation":false,"usgs":true,"family":"Krabbenhoft","given":"David","email":"dpkrabbe@usgs.gov","middleInitial":"P.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true},{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true},{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":242207,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":50745,"text":"ofr03224 - 2003 - Near-field receiving water monitoring of a benthic community near the Palo Alto Water Quality Control Plant in South San Francisco Bay:  February 1974 through December 2002","interactions":[],"lastModifiedDate":"2020-02-10T20:00:59","indexId":"ofr03224","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-224","title":"Near-field receiving water monitoring of a benthic community near the Palo Alto Water Quality Control Plant in South San Francisco Bay:  February 1974 through December 2002","docAbstract":"<p>Analyses of the benthic community structure over a 28-year period show that changes in the community have occurred concurrent with reduced concentrations of metals in the sediment and in the tissues of the biosentinal clam Macoma balthica from the same area. The community has shifted from being dominated by several opportunistic species to a community where the species are more similar in abundance, a pattern that could be indicative of a more stable community that is subjected to less stress. In addition, two of the opportunistic species (Ampelisca abdita and Streblospio benedicti) that brood their young and live on the surface of the sediment in tubes have shown a continual decline in dominance coincident with the decline in metals. Heteromastus filiformis, a subsurface polychaete worm that lives in the sediment, consumes sediment and organic particles residing in the sediment, and reproduces by laying their eggs on or in the sediment has shown a concurrent increase in dominance. These changes in species dominance reflect a change in the community from one dominated by surface dwelling, brooding species to one with species with varying life history characteristics. Analysis of the reproductive activity of Macoma balthica shows increases in reproductive activity concurrent with the decline in metal concentrations in the tissue of this organism. Reproductive activity is presently stable with almost all animals reproducing during the two reproductive seasons (spring and fall) of most years. These findings are consistent with findings previously reported for the 1974 through 2000 period.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr03224","usgsCitation":"Shouse, M.K., Parcheso, F., and Thompson, J.K., 2003, Near-field receiving water monitoring of a benthic community near the Palo Alto Water Quality Control Plant in South San Francisco Bay:  February 1974 through December 2002: U.S. Geological Survey Open-File Report 2003-224, 41 p., https://doi.org/10.3133/ofr03224.","productDescription":"41 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":175294,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4236,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr03-224/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","city":"Palo Alto","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.947998046875,\n              37.31775185163688\n            ],\n            [\n              -121.904296875,\n              37.31775185163688\n            ],\n            [\n              -121.904296875,\n              38.151837403006766\n            ],\n            [\n              -122.947998046875,\n              38.151837403006766\n            ],\n            [\n              -122.947998046875,\n              37.31775185163688\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c9c3","contributors":{"authors":[{"text":"Shouse, Michelle K. mkshouse@usgs.gov","contributorId":5407,"corporation":false,"usgs":true,"family":"Shouse","given":"Michelle","email":"mkshouse@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":242217,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parcheso, Francis 0000-0002-9471-7787 parchaso@usgs.gov","orcid":"https://orcid.org/0000-0002-9471-7787","contributorId":2590,"corporation":false,"usgs":true,"family":"Parcheso","given":"Francis","email":"parchaso@usgs.gov","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":false,"id":242216,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thompson, Janet K. 0000-0002-1528-8452 jthompso@usgs.gov","orcid":"https://orcid.org/0000-0002-1528-8452","contributorId":1009,"corporation":false,"usgs":true,"family":"Thompson","given":"Janet","email":"jthompso@usgs.gov","middleInitial":"K.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":36183,"text":"Hydro-Ecological Interactions Branch","active":true,"usgs":true}],"preferred":true,"id":242215,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":50755,"text":"wri034049 - 2003 - Ground-Water Resources in the Black Hills Area, South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:11:20","indexId":"wri034049","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2003-4049","title":"Ground-Water Resources in the Black Hills Area, South Dakota","docAbstract":"The availability of ground-water resources in the Black Hills area is influenced by many factors including location, local recharge and ground-water flow conditions, and structural features. Thus, the availability of ground water can be extremely variable throughout the Black Hills area, and even when water is available, it may not be suitable for various uses depending on the water quality. \r\n\r\nThe major bedrock aquifers in the Black Hills area are the Deadwood, Madison, Minnelusa, Minnekahta, and Inyan Kara aquifers. Minor bedrock aquifers occur in other hydrogeologic units, including confining units, due to fracturing and interbedded permeable layers.\r\n\r\nVarious information and maps are presented in this report that describe availability and quality of ground-water resources in the Black Hills area. However, there is no guarantee of obtaining usable water at any location due to the extreme potential variability in conditions that can affect the availability and quality of ground water in the area. Maps presented in this report include the distribution of hydrogeologic units; depth to the top of the five formations that contain major aquifers; thickness of the five formations that contain major aquifers; potentiometric maps for the five major aquifers; saturated thickness of the Madison and Minnelusa aquifers; water temperature in the Madison aquifer; specific conductance in the Madison, Minnelusa, and Inyan Kara aquifers; hardness in the Inyan Kara aquifer; sulfate concentrations in the Minnelusa aquifer; and radon concentrations in the Deadwood aquifer.\r\n\r\nWater quality of the major aquifers generally is very good in and near outcrop areas but deteriorates progressively with distance from the outcrops. In the Minnelusa aquifer, an abrupt increase in concentrations of dissolved sulfate occurs downgradient from outcrop areas, where a zone of active anhydrite dissolution occurs.\r\n\r\nMost limitations for the use of ground water are related to aesthetic qualities associated with hardness and high concentrations of chloride, sulfate, sodium, manganese, and iron. Very few health-related limitations exist for ground water; most limitations are for radionuclides, such as radon and uranium. In addition, high concentrations of arsenic have been measured in a few samples from the Minnelusa aquifer.","language":"ENGLISH","doi":"10.3133/wri034049","usgsCitation":"Carter, J.M., Driscoll, D.G., and Sawyer, J.F., 2003, Ground-Water Resources in the Black Hills Area, South Dakota: U.S. Geological Survey Water-Resources Investigations Report 2003-4049, 36 p., https://doi.org/10.3133/wri034049.","productDescription":"36 p.","costCenters":[],"links":[{"id":4184,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri034049/","linkFileType":{"id":5,"text":"html"}},{"id":176672,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698683","contributors":{"authors":[{"text":"Carter, Janet M. 0000-0002-6376-3473 jmcarter@usgs.gov","orcid":"https://orcid.org/0000-0002-6376-3473","contributorId":339,"corporation":false,"usgs":true,"family":"Carter","given":"Janet","email":"jmcarter@usgs.gov","middleInitial":"M.","affiliations":[{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true},{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":false,"id":242233,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Driscoll, Daniel G. dgdrisco@usgs.gov","contributorId":1558,"corporation":false,"usgs":true,"family":"Driscoll","given":"Daniel","email":"dgdrisco@usgs.gov","middleInitial":"G.","affiliations":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":242234,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sawyer, J. Foster","contributorId":80344,"corporation":false,"usgs":true,"family":"Sawyer","given":"J.","email":"","middleInitial":"Foster","affiliations":[],"preferred":false,"id":242235,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":51528,"text":"ofr03264 - 2003 - Saturation overland flow estimated from TOPMODEL for the conterminous United States","interactions":[],"lastModifiedDate":"2012-02-02T00:11:13","indexId":"ofr03264","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-264","title":"Saturation overland flow estimated from TOPMODEL for the conterminous United States","docAbstract":"This 5-kilometer resolution raster (grid) dataset for the conterminous United States represents the average percentage of saturation overland flow in total streamflow estimated by the watershed model TOPMODEL. Saturation overland flow is simulated in TOPMODEL as precipitation that falls on saturated land-surface areas and enters the stream channel.\r\n\r\nTOPMODEL was applied to 5- by 5-kilometer areas across the conterminous United States using national climate, soils, and terrain GIS datasets. The model was run for 1,000 days for each 5- by 5-kilometer area. The average percentage of saturation overland flow in total streamflow was computed for the 1,000-day simulation in each grid cell.","language":"ENGLISH","doi":"10.3133/ofr03264","usgsCitation":"Wolock, D.M., 2003, Saturation overland flow estimated from TOPMODEL for the conterminous United States: U.S. Geological Survey Open-File Report 2003-264, raster digital data, https://doi.org/10.3133/ofr03264.","productDescription":"raster digital data","costCenters":[],"links":[{"id":4548,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://water.usgs.gov/lookup/getspatial?satof48","linkFileType":{"id":5,"text":"html"}},{"id":176328,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdba9","contributors":{"authors":[{"text":"Wolock, David M. 0000-0002-6209-938X dwolock@usgs.gov","orcid":"https://orcid.org/0000-0002-6209-938X","contributorId":540,"corporation":false,"usgs":true,"family":"Wolock","given":"David","email":"dwolock@usgs.gov","middleInitial":"M.","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":243853,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51538,"text":"ofr03195 - 2003 - Quality-Assurance Plan for Water-Quality Activities of the U.S. Geological Survey in Miami, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:11:34","indexId":"ofr03195","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-195","title":"Quality-Assurance Plan for Water-Quality Activities of the U.S. Geological Survey in Miami, Florida","docAbstract":"In accordance with guidelines set forth by the Office of Water Quality in the Water Resources Discipline of the U.S. Geological Survey, a quality-assurance plan has been created for use by the U.S. Geological Survey (USGS) in Miami to conduct water-quality activities. This quality-assurance plan documents the standards, policies, and procedures used by the Miami USGS for activities related to the collection, processing, storage, analysis, and publication of water-quality data. The policies and procedures that are documented in this quality-assurance plan for water-quality activities are meant to complement the Miami USGS quality-assurance plans for surface-water and ground-water activities.","language":"ENGLISH","doi":"10.3133/ofr03195","usgsCitation":"Lietz, A.C., 2003, Quality-Assurance Plan for Water-Quality Activities of the U.S. Geological Survey in Miami, Florida: U.S. Geological Survey Open-File Report 2003-195, 72 p., https://doi.org/10.3133/ofr03195.","productDescription":"72 p.","costCenters":[],"links":[{"id":4555,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr03-195/","linkFileType":{"id":5,"text":"html"}},{"id":178023,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ae4b07f02db651521","contributors":{"authors":[{"text":"Lietz, A. C. (compiler)","contributorId":43847,"corporation":false,"usgs":true,"family":"Lietz","given":"A.","suffix":"(compiler)","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":243882,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51539,"text":"ofr03184 - 2003 - Hurricane Mitch: impacts on mangrove sediment elevation dynamics and long-term mangrove sustainability","interactions":[],"lastModifiedDate":"2012-02-02T00:11:34","indexId":"ofr03184","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-184","title":"Hurricane Mitch: impacts on mangrove sediment elevation dynamics and long-term mangrove sustainability","language":"ENGLISH","doi":"10.3133/ofr03184","usgsCitation":"Cahoon, D.R., Hensel, P., Rybczyk, J., and Perez, B.C., 2003, Hurricane Mitch: impacts on mangrove sediment elevation dynamics and long-term mangrove sustainability: U.S. Geological Survey Open-File Report 2003-184, 75 p., https://doi.org/10.3133/ofr03184.","productDescription":"75 p.","costCenters":[],"links":[{"id":178024,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4556,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.nwrc.usgs.gov/hurricane/mitch/Cahoon%20Mangrove%20Sediment%20Final%20Revised.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62a3a2","contributors":{"authors":[{"text":"Cahoon, Donald R. 0000-0002-2591-5667 dcahoon@usgs.gov","orcid":"https://orcid.org/0000-0002-2591-5667","contributorId":3791,"corporation":false,"usgs":true,"family":"Cahoon","given":"Donald","email":"dcahoon@usgs.gov","middleInitial":"R.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":243883,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hensel, Philippe","contributorId":26009,"corporation":false,"usgs":true,"family":"Hensel","given":"Philippe","affiliations":[],"preferred":false,"id":243884,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rybczyk, John","contributorId":105793,"corporation":false,"usgs":true,"family":"Rybczyk","given":"John","affiliations":[],"preferred":false,"id":243886,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Perez, Brian C.","contributorId":42286,"corporation":false,"usgs":true,"family":"Perez","given":"Brian","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":243885,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":51542,"text":"ofr03181 - 2003 - Impacts of Hurricane Mitch on seagrass beds and associated shallow reef communities along the Carribbean coast of Honduras and Guatemala","interactions":[],"lastModifiedDate":"2012-02-02T00:11:34","indexId":"ofr03181","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-181","title":"Impacts of Hurricane Mitch on seagrass beds and associated shallow reef communities along the Carribbean coast of Honduras and Guatemala","language":"ENGLISH","doi":"10.3133/ofr03181","usgsCitation":"Michot, T.C., Burch, J.N., Arrivillaga, A., Rafferty, P.S., Doyle, T.W., and Kemmerer, R.S., 2003, Impacts of Hurricane Mitch on seagrass beds and associated shallow reef communities along the Carribbean coast of Honduras and Guatemala: U.S. Geological Survey Open-File Report 2003-181, 65 p., https://doi.org/10.3133/ofr03181.","productDescription":"65 p.","costCenters":[],"links":[{"id":178088,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4559,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.nwrc.usgs.gov/hurricane/mitch/finalallseagrass.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a05e4b07f02db5f8656","contributors":{"authors":[{"text":"Michot, Thomas C. 0000-0002-7044-987X","orcid":"https://orcid.org/0000-0002-7044-987X","contributorId":57935,"corporation":false,"usgs":true,"family":"Michot","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":243895,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burch, James N.","contributorId":106193,"corporation":false,"usgs":true,"family":"Burch","given":"James","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":243896,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Arrivillaga, Alejandro","contributorId":44614,"corporation":false,"usgs":true,"family":"Arrivillaga","given":"Alejandro","email":"","affiliations":[],"preferred":false,"id":243893,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rafferty, Patricia S.","contributorId":55895,"corporation":false,"usgs":true,"family":"Rafferty","given":"Patricia","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":243894,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Doyle, Thomas W. 0000-0001-5754-0671 doylet@usgs.gov","orcid":"https://orcid.org/0000-0001-5754-0671","contributorId":703,"corporation":false,"usgs":true,"family":"Doyle","given":"Thomas","email":"doylet@usgs.gov","middleInitial":"W.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":243891,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kemmerer, R. Scott","contributorId":43028,"corporation":false,"usgs":true,"family":"Kemmerer","given":"R.","email":"","middleInitial":"Scott","affiliations":[],"preferred":false,"id":243892,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
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