{"pageNumber":"211","pageRowStart":"5250","pageSize":"25","recordCount":37001,"records":[{"id":70546,"text":"ofr20041251 - 2005 - Mineral commodity profiles: Silver","interactions":[],"lastModifiedDate":"2012-02-02T00:14:04","indexId":"ofr20041251","displayToPublicDate":"2005-05-13T00:00:00","publicationYear":"2005","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":"2004-1251","title":"Mineral commodity profiles: Silver","docAbstract":"Overview -- Silver is one of the eight precious, or noble, metals; the others are gold and the six platinum-group metals (PGM). World mine production in 2001 was 18,700 metric tons (t) and came from mines in 60 countries; the 10 leading producing countries accounted for 86 percent of the total. The largest producer was Mexico, followed by Peru, Australia, and the United States. About 25 percent of the silver mined in the world in 2001 came from silver ores; 15 percent, from gold ores and the remaining 60 percent, from copper, lead, and zinc ores.\r\n\r\nIn the United States, 14 percent of the silver mined in 2001 came from silver ores; 39 percent, from gold ores; 10 percent, from copper and copper-molybdenum ores; and 37 percent, from lead, zinc, and lead-zinc ores. The precious metal ores (gold and silver) came from 30 lode mines and 10 placer mines; the base-metal ores (copper, lead, molybdenum, and zinc) came from 24 lode mines. Placer mines yielded less than 1 percent of the national silver production. Silver was mined in 12 States, of which Nevada was by far the largest producer; it accounted for nearly one-third of the national total. The production of silver at domestic mines generated employment for about 1,100 mine and mill workers. The value of mined domestic silver was estimated to be $290 million. \r\n\r\nOf the nearly 27,000 t of world silver that was fabricated in 2001, about one-third went into jewelry and silverware, one-fourth into the light-sensitive compounds used in photography, and nearly all the remainder went for industrial uses, of which there were 7 substantial uses and many other small-volume uses. By comparison, 85 percent of the silver used in the United States went to photography and industrial uses, 8 percent to jewelry and silverware, and 7 percent to coins and medals. The United States was the largest consumer of silver followed by India, Japan, and Italy; the 13 largest consuming countries accounted for nearly 90 percent of the world total. In the United States, about 30 companies accounted for more than 90 percent of the silver fabricated. The consumption of silver for all fabrication uses is expected to grow slowly through the decade ending in 2010 at about 1.3 percent per year for the world and 2.4 percent per year for the United States.\r\n\r\nWorld and U.S. reserves and reserve bases are more than adequate to satisfy the demand for newly mined silver through 2010. The other components of supply will be silver recovered from scrap, silver from industrial stocks, and silver bullion that is sold into the market from commodity exchange and private stocks.","language":"ENGLISH","doi":"10.3133/ofr20041251","usgsCitation":"Butterman, W., and Hilliard, H.E., 2005, Mineral commodity profiles: Silver (Online only): U.S. Geological Survey Open-File Report 2004-1251, 44 p., https://doi.org/10.3133/ofr20041251.","productDescription":"44 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":193129,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6930,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1251/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635896","contributors":{"authors":[{"text":"Butterman, W. C.","contributorId":13679,"corporation":false,"usgs":true,"family":"Butterman","given":"W. C.","affiliations":[],"preferred":false,"id":282615,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hilliard, Henry E.","contributorId":60278,"corporation":false,"usgs":true,"family":"Hilliard","given":"Henry","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":282616,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70549,"text":"ofr20051182 - 2005 - U.S. Geological Survey 2005 oil and gas resource assessment of the central North Slope, Alaska: Play maps and results","interactions":[],"lastModifiedDate":"2022-10-05T18:22:44.38074","indexId":"ofr20051182","displayToPublicDate":"2005-05-13T00:00:00","publicationYear":"2005","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":"2005-1182","title":"U.S. Geological Survey 2005 oil and gas resource assessment of the central North Slope, Alaska: Play maps and results","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051182","usgsCitation":"Garrity, C.P., Houseknecht, D.W., Bird, K.J., Potter, C.J., Moore, T.E., Nelson, P.H., and Schenk, C.J., 2005, U.S. Geological Survey 2005 oil and gas resource assessment of the central North Slope, Alaska: Play maps and results (Online only): U.S. Geological Survey Open-File Report 2005-1182, Report: 29 p.; ArcGIS Geodatabase, https://doi.org/10.3133/ofr20051182.","productDescription":"Report: 29 p.; ArcGIS Geodatabase","onlineOnly":"Y","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true},{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":193228,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":407981,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_71378.htm","linkFileType":{"id":5,"text":"html"}},{"id":6933,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1182/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -156,\n              68.2\n            ],\n            [\n              -146,\n              68.2\n            ],\n            [\n              -146,\n              70.5167\n            ],\n            [\n              -156,\n              70.5167\n            ],\n            [\n              -156,\n              68.2\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ce4b07f02db613a2e","contributors":{"authors":[{"text":"Garrity, Christopher P. 0000-0002-5565-1818 cgarrity@usgs.gov","orcid":"https://orcid.org/0000-0002-5565-1818","contributorId":644,"corporation":false,"usgs":true,"family":"Garrity","given":"Christopher","email":"cgarrity@usgs.gov","middleInitial":"P.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true},{"id":5061,"text":"National Cooperative Geologic Mapping and Landslide Hazards","active":true,"usgs":true}],"preferred":true,"id":282622,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Houseknecht, David W. 0000-0002-9633-6910 dhouse@usgs.gov","orcid":"https://orcid.org/0000-0002-9633-6910","contributorId":645,"corporation":false,"usgs":true,"family":"Houseknecht","given":"David","email":"dhouse@usgs.gov","middleInitial":"W.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":282623,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bird, Kenneth J. kbird@usgs.gov","contributorId":1015,"corporation":false,"usgs":true,"family":"Bird","given":"Kenneth","email":"kbird@usgs.gov","middleInitial":"J.","affiliations":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"preferred":true,"id":282626,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Potter, Christopher J. 0000-0002-2300-6670 cpotter@usgs.gov","orcid":"https://orcid.org/0000-0002-2300-6670","contributorId":1026,"corporation":false,"usgs":true,"family":"Potter","given":"Christopher","email":"cpotter@usgs.gov","middleInitial":"J.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":282627,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Moore, Thomas E. 0000-0002-0878-0457 tmoore@usgs.gov","orcid":"https://orcid.org/0000-0002-0878-0457","contributorId":1033,"corporation":false,"usgs":true,"family":"Moore","given":"Thomas","email":"tmoore@usgs.gov","middleInitial":"E.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":282628,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Nelson, Philip H. pnelson@usgs.gov","contributorId":862,"corporation":false,"usgs":true,"family":"Nelson","given":"Philip","email":"pnelson@usgs.gov","middleInitial":"H.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":282625,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Schenk, Christopher J. 0000-0002-0248-7305 schenk@usgs.gov","orcid":"https://orcid.org/0000-0002-0248-7305","contributorId":826,"corporation":false,"usgs":true,"family":"Schenk","given":"Christopher","email":"schenk@usgs.gov","middleInitial":"J.","affiliations":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true},{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":282624,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70548,"text":"ofr20051151 - 2005 - Alabama-Mississippi coastal classification maps - Perdido Pass to Cat Island","interactions":[],"lastModifiedDate":"2022-07-18T21:10:40.184032","indexId":"ofr20051151","displayToPublicDate":"2005-05-13T00:00:00","publicationYear":"2005","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":"2005-1151","title":"Alabama-Mississippi coastal classification maps - Perdido Pass to Cat Island","docAbstract":"The primary purpose of the USGS National Assessment of Coastal Change Project is to provide accurate representations of pre-storm ground conditions for areas that are designated high-priority because they have dense populations or valuable resources that are at risk from storm waves. Another purpose of the project is to develop a geomorphic (land feature) coastal classification that, with only minor modification, can be applied to most coastal regions in the United States.\r\n\r\nA Coastal Classification Map describing local geomorphic features is the first step toward determining the hazard vulnerability of an area. The Coastal Classification Maps of the National Assessment of Coastal Change Project present ground conditions such as beach width, dune elevations, overwash potential, and density of development. In order to complete a hazard vulnerability assessment, that information must be integrated with other information, such as prior storm impacts and beach stability. The Coastal Classification Maps provide much of the basic information for such an assessment and represent a critical component of a storm-impact forecasting capability.\r\n\r\nThe map above shows the areas covered by this web site. Click on any of the location names or outlines to view the Coastal Classification Map for that area.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051151","usgsCitation":"Morton, R., and Peterson, R.L., 2005, Alabama-Mississippi coastal classification maps - Perdido Pass to Cat Island: U.S. Geological Survey Open-File Report 2005-1151, HTML Document; CD-ROM, https://doi.org/10.3133/ofr20051151.","productDescription":"HTML Document; CD-ROM","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":193188,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":403957,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_71379.htm","linkFileType":{"id":5,"text":"html"}},{"id":6932,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1151/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alabama, Mississippi, Florida","otherGeospatial":"Cat Island, Perdido Pass","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.154052734375,\n              29.945415337104453\n            ],\n            [\n              -87.440185546875,\n              29.945415337104453\n            ],\n            [\n              -87.440185546875,\n              30.315987718557867\n            ],\n            [\n              -89.154052734375,\n              30.315987718557867\n            ],\n            [\n              -89.154052734375,\n              29.945415337104453\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db68811d","contributors":{"authors":[{"text":"Morton, Robert A.","contributorId":88333,"corporation":false,"usgs":true,"family":"Morton","given":"Robert A.","affiliations":[],"preferred":false,"id":282621,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, Russell L.","contributorId":55045,"corporation":false,"usgs":true,"family":"Peterson","given":"Russell","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":282620,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70547,"text":"ofr20041410 - 2005 - Generalized geologic map of bedrock lithologies and surficial deposits in the Great Smoky Mountains National Park region, Tennessee and North Carolina","interactions":[{"subject":{"id":70547,"text":"ofr20041410 - 2005 - Generalized geologic map of bedrock lithologies and surficial deposits in the Great Smoky Mountains National Park region, Tennessee and North Carolina","indexId":"ofr20041410","publicationYear":"2005","noYear":false,"title":"Generalized geologic map of bedrock lithologies and surficial deposits in the Great Smoky Mountains National Park region, Tennessee and North Carolina"},"predicate":"SUPERSEDED_BY","object":{"id":70040740,"text":"sim2997 - 2012 - Geologic map of the Great Smoky Mountains National Park region, Tennessee and North Carolina","indexId":"sim2997","publicationYear":"2012","noYear":false,"title":"Geologic map of the Great Smoky Mountains National Park region, Tennessee and North Carolina"},"id":1}],"supersededBy":{"id":70040740,"text":"sim2997 - 2012 - Geologic map of the Great Smoky Mountains National Park region, Tennessee and North Carolina","indexId":"sim2997","publicationYear":"2012","noYear":false,"title":"Geologic map of the Great Smoky Mountains National Park region, Tennessee and North Carolina"},"lastModifiedDate":"2016-04-19T12:19:06","indexId":"ofr20041410","displayToPublicDate":"2005-05-13T00:00:00","publicationYear":"2005","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":"2004-1410","title":"Generalized geologic map of bedrock lithologies and surficial deposits in the Great Smoky Mountains National Park region, Tennessee and North Carolina","docAbstract":"<p><span>The geology of the Great Smoky Mountain National Park (GSMNP) region of Tennessee and North Carolina was studied from 1993 to 2003 as part of a cooperative investigation with the National Park Service (NPS). This work has been compiled as a 1:100,000-scale map derived from mapping done at 1:24,000 and 1:62,500 scale. The geologic data are intended to support cooperative investigations with NPS, the development of a new soil map by the Natural Resources Conservation Service, and the All Taxa Biodiversity Inventory (</span><a href=\"http://www.discoverlifeinamerica.org/\" target=\"_blank\">http://www.discoverlifeinamerica.org/</a><span>). At the request of NPS, we mapped areas previously not visited, revised the geology where stratigraphic and structural problems existed, and developed a map database for use in interdisciplinary research, land management, and interpretive programs for park visitors.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20041410","usgsCitation":"Southworth, S., Schultz, A., and Denenny, D., 2005, Generalized geologic map of bedrock lithologies and surficial deposits in the Great Smoky Mountains National Park region, Tennessee and North Carolina (Online only): U.S. Geological Survey Open-File Report 2004-1410, Report: 109 p.;  Plate: 54.25 x 39.42 inches; Shapefiles; Database, https://doi.org/10.3133/ofr20041410.","productDescription":"Report: 109 p.;  Plate: 54.25 x 39.42 inches; Shapefiles; Database","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":193187,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":110560,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_71380.htm","linkFileType":{"id":5,"text":"html"},"description":"71380"},{"id":6931,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1410/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"North Carolina, Tennessee","otherGeospatial":"Great Smoky Mountains National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84,\n              35.3\n            ],\n            [\n              -84,\n              35.88\n            ],\n            [\n              -83,\n              35.88\n            ],\n            [\n              -83,\n              35.3\n            ],\n            [\n              -84,\n              35.3\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af30b","contributors":{"authors":[{"text":"Southworth, Scott","contributorId":93933,"corporation":false,"usgs":true,"family":"Southworth","given":"Scott","affiliations":[],"preferred":false,"id":282619,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schultz, Art","contributorId":44982,"corporation":false,"usgs":true,"family":"Schultz","given":"Art","email":"","affiliations":[],"preferred":false,"id":282617,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Denenny, Danielle","contributorId":78804,"corporation":false,"usgs":true,"family":"Denenny","given":"Danielle","affiliations":[],"preferred":false,"id":282618,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70545,"text":"ofr20041218 - 2005 - Mineral commodity profiles: Germanium","interactions":[],"lastModifiedDate":"2012-02-02T00:14:04","indexId":"ofr20041218","displayToPublicDate":"2005-05-13T00:00:00","publicationYear":"2005","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":"2004-1218","title":"Mineral commodity profiles: Germanium","docAbstract":"Overview -- Germanium is a hard, brittle semimetal that first came into use a half-century ago as a semiconductor material in radar units and as the material from which the first transistor was made. Today it is used principally as a component of the glass in telecommunications fiber optics; as a polymerization catalyst for polyethylene terephthalate (PET), a commercially important plastic; in infrared (IR) night vision devices; and as a semiconductor and substrate in electronics circuitry.\r\nMost germanium is recovered as a byproduct of zinc smelting, although it also has been recovered at some copper smelters and from the fly ash of coal-burning industrial powerplants. It is a highly dispersed element, associated primarily with base-metal sulfide ores. In the United States, germanium is recovered from zinc smelter residues and manufacturing scrap and is refined by two companies at four germanium refineries. One of the four refineries is dedicated to processing scrap. In 2000, producers sold zone-refined (high-purity) germanium at about $1,250 per kilogram and electronic-grade germanium dioxide (GeO2) at $800 per kilogram. Domestic refined production was valued at $22 million.\r\nGermanium is a critical component in highly technical devices and processes. It is likely to remain in demand in the future at levels at least as high as those of 2000. U.S. resources of germanium are probably adequate to meet domestic needs for several decades.","language":"ENGLISH","doi":"10.3133/ofr20041218","usgsCitation":"Butterman, W., and Jorgenson, J.D., 2005, Mineral commodity profiles: Germanium (Online only): U.S. Geological Survey Open-File Report 2004-1218, 22 p., https://doi.org/10.3133/ofr20041218.","productDescription":"22 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":6929,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1218/","linkFileType":{"id":5,"text":"html"}},{"id":193128,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db63588c","contributors":{"authors":[{"text":"Butterman, W. C.","contributorId":13679,"corporation":false,"usgs":true,"family":"Butterman","given":"W. C.","affiliations":[],"preferred":false,"id":282613,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jorgenson, John D.","contributorId":74087,"corporation":false,"usgs":true,"family":"Jorgenson","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":282614,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70521,"text":"ofr20051165 - 2005 - Particle atlas of World Trade Center dust","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"ofr20051165","displayToPublicDate":"2005-05-06T00:00:00","publicationYear":"2005","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":"2005-1165","title":"Particle atlas of World Trade Center dust","docAbstract":"The United States Environmental Protection Agency (EPA) has begun a reassessment of the presence of World Trade Center (WTC) dust in residences, public buildings, and office spaces in New York City, New York. Background dust samples collected from residences, public buildings, and office spaces will be analyzed by multiple laboratories for the presence of WTC dust. Other laboratories are currently studying WTC dust for other purposes, such as health effects studies. To assist in inter-laboratory consistency for identification of WTC dust components, this particle atlas of phases in WTC dust has been compiled.","language":"ENGLISH","doi":"10.3133/ofr20051165","usgsCitation":"Lowers, H., and Meeker, G.P., 2005, Particle atlas of World Trade Center dust (Version 1.0, online only): U.S. Geological Survey Open-File Report 2005-1165, 6 p. with linked tables and images, https://doi.org/10.3133/ofr20051165.","productDescription":"6 p. with linked tables and images","onlineOnly":"Y","costCenters":[],"links":[{"id":185991,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6898,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1165/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","edition":"Version 1.0, online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db688f46","contributors":{"authors":[{"text":"Lowers, Heather 0000-0001-5360-9264 hlowers@usgs.gov","orcid":"https://orcid.org/0000-0001-5360-9264","contributorId":710,"corporation":false,"usgs":true,"family":"Lowers","given":"Heather","email":"hlowers@usgs.gov","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":false,"id":282574,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meeker, Gregory P.","contributorId":62974,"corporation":false,"usgs":true,"family":"Meeker","given":"Gregory","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":282575,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70525,"text":"ofr20051176 - 2005 - Flooding of the Androscoggin River during December 18-19, 2003, in Canton, Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"ofr20051176","displayToPublicDate":"2005-05-06T00:00:00","publicationYear":"2005","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":"2005-1176","title":"Flooding of the Androscoggin River during December 18-19, 2003, in Canton, Maine","docAbstract":"The Androscoggin River flooded the town of Canton, Maine in December 2003, resulting in damage to and (or) evacuation of 44 homes. Streamflow records at the U.S. Geological Survey (USGS) streamflow-gaging stations at Rumford (USGS station identification number 01054500) and Auburn (01059000) were used to estimate the peak streamflow for the Androscoggin in the town of Canton for this flood (December 18-19, 2003). The estimated peak flood streamflow at Canton was approximately 39,800 ft3/s, corresponding to an estimated recurrence interval of 4.4 years; however, an ice jam downstream from Canton Point on December 18-19 obstructed river flow resulting in a high-water elevation commensurate with an open-water flood approximately equal to a 15-year event. The high water-surface elevations attained during the December 18-19 flood event in Canton were higher than the expected open-water flood water-surface elevations; this verified the assumption that the water-surface elevation was augmented due to the downstream ice jam\r\n\r\nThe change in slope of the riverbed from upstream of Canton to the impoundment at the downstream corporate limits, and the river bend near Stevens Island are principal factors in ice-jam formation near Canton. The U.S. Army Corps of Engineers Ice Jam Database indicates five ice-jam-related floods (including December 2003) for the town of Canton: March 13, 1936; January 1978; March 12, 1987; January 29, 1996; and December 18-19, 2003. There have been more ice-jam-related flood events in Canton than these five documented events, but the exact number and nature of ice jams in Canton cannot be determined without further research.","language":"ENGLISH","doi":"10.3133/ofr20051176","usgsCitation":"Dudley, R.W., 2005, Flooding of the Androscoggin River during December 18-19, 2003, in Canton, Maine (Online only): U.S. Geological Survey Open-File Report 2005-1176, 13 p., https://doi.org/10.3133/ofr20051176.","productDescription":"13 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":6902,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr2005-1176/","linkFileType":{"id":5,"text":"html"}},{"id":186075,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478fe4b07f02db48a621","contributors":{"authors":[{"text":"Dudley, Robert W. 0000-0002-0934-0568 rwdudley@usgs.gov","orcid":"https://orcid.org/0000-0002-0934-0568","contributorId":2223,"corporation":false,"usgs":true,"family":"Dudley","given":"Robert","email":"rwdudley@usgs.gov","middleInitial":"W.","affiliations":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282589,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70523,"text":"ofr20051130 - 2005 - Geologic and hydrogeologic framework of the Espanola basin -- Proceedings of the 4th annual Espanola Basin Workshop, Santa Fe, New Mexico, March 1-3, 2005","interactions":[],"lastModifiedDate":"2022-04-26T21:01:24.783283","indexId":"ofr20051130","displayToPublicDate":"2005-05-06T00:00:00","publicationYear":"2005","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":"2005-1130","title":"Geologic and hydrogeologic framework of the Espanola basin -- Proceedings of the 4th annual Espanola Basin Workshop, Santa Fe, New Mexico, March 1-3, 2005","docAbstract":"<p class=\"textindent\">This report presents abstracts of technical studies that pertain to the hydrogeologic framework of the</p><p class=\"textindent\">This report presents abstracts of technical studies that pertain to the hydrogeologic framework of the Española basin, a major subbasin of the Cenozoic Rio Grande rift. Sediments and interbedded volcanic rocks that fill the Española basin comprise an aquifer system that is an important source of water for many residents of the basin, including people in the cities of Santa Fe, Española, and Los Alamos as well as Native Americans in eleven Pueblos.</p><p class=\"textindent\">The abstracts describe results of technical studies that were presented either as poster exhibits or oral presentations at the forth-annual Española basin workshop, held March 1-2 of 2005 in Santa Fe, New Mexico. The principal goal of this workshop was to share information about ongoing studies.</p><p class=\"textindent\">The Española basin workshop was hosted by the Española basin technical advisory group (EBTAG) and sponsored by the U.S. Geological Survey, the New Mexico Bureau of Geology and Mineral Resources, and both the Water Research Technical Assistance Office and the Groundwater Protection Program of Los Alamos National Laboratory. Abstracts in this report have been grouped into six information themes: Basic Water Data, Water Quality and Water Chemistry, Water Balance and Stream/Aquifer Interaction, Data Integration and Hydrologic Model Testing, Three-Dimensional Hydrogeological Architecture, and Geologic Framework.</p><p class=\"textindent\">Taken together, the abstracts in this report provide a view of the current status of hydrogeologic research within the Española basin.</p><p class=\"textindent\">, a major subbasin of the Cenozoic Rio Grande rift. Sediments and interbedded volcanic rocks that fill the Española basin comprise an aquifer system that is an important source of water for many residents of the basin, including people in the cities of Santa Fe, Española, and Los Alamos as well as Native Americans in eleven Pueblos.</p><p class=\"textindent\">The abstracts describe results of technical studies that were presented either as poster exhibits or oral presentations at the forth-annual Española basin workshop, held March 1-2 of 2005 in Santa Fe, New Mexico. The principal goal of this workshop was to share information about ongoing studies.</p><p class=\"textindent\">The Española basin workshop was hosted by the Española basin technical advisory group (EBTAG) and sponsored by the U.S. Geological Survey, the New Mexico Bureau of Geology and Mineral Resources, and both the Water Research Technical Assistance Office and the Groundwater Protection Program of Los Alamos National Laboratory. Abstracts in this report have been grouped into six information themes: Basic Water Data, Water Quality and Water Chemistry, Water Balance and Stream/Aquifer Interaction, Data Integration and Hydrologic Model Testing, Three-Dimensional Hydrogeological Architecture, and Geologic Framework.</p><p class=\"textindent\">Taken together, the abstracts in this report provide a view of the current status of hydrogeologic research within the Española basin.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051130","usgsCitation":"McKinney, K.C., 2005, Geologic and hydrogeologic framework of the Espanola basin -- Proceedings of the 4th annual Espanola Basin Workshop, Santa Fe, New Mexico, March 1-3, 2005 (Version 1.0): U.S. Geological Survey Open-File Report 2005-1130, 33 p., https://doi.org/10.3133/ofr20051130.","productDescription":"33 p.","costCenters":[],"links":[{"id":186073,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6900,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1130/","linkFileType":{"id":5,"text":"html"}},{"id":399711,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_71262.htm"}],"country":"United States","state":"New Mexico","otherGeospatial":"Española basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.35314941406249,\n              35.66622234103479\n            ],\n            [\n              -105.77636718749999,\n              35.66622234103479\n            ],\n            [\n              -105.77636718749999,\n              36.38149043210595\n            ],\n            [\n              -106.35314941406249,\n              36.38149043210595\n            ],\n            [\n              -106.35314941406249,\n              35.66622234103479\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8237","contributors":{"authors":[{"text":"McKinney, Kevin C. kcmckinney@usgs.gov","contributorId":3406,"corporation":false,"usgs":true,"family":"McKinney","given":"Kevin","email":"kcmckinney@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":282583,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70522,"text":"ofr20051091 - 2005 - Results of chemical and isotopic analyses of sediment and water from alluvium of the Canadian River near a closed municipal landfill, Norman, Oklahoma","interactions":[],"lastModifiedDate":"2020-03-21T12:03:33","indexId":"ofr20051091","displayToPublicDate":"2005-05-06T00:00:00","publicationYear":"2005","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":"2005-1091","title":"Results of chemical and isotopic analyses of sediment and water from alluvium of the Canadian River near a closed municipal landfill, Norman, Oklahoma","docAbstract":"Results of physical and chemical analyses of sediment and water collected near a closed municipal landfill at Norman, Oklahoma are presented in this report. Sediment analyses are from 40 samples obtained by freeze-shoe coring at 5 sites, and 14 shallow (depth <1.3 m) sediment samples. The sediment was analyzed to determine grain size, the abundance of extractable iron species and the abundances and isotopic compositions of forms of sulfur. Water samples included pore water from the freeze-shoe core, ground water, and surface water. Pore water from 23 intervals of the core was collected and analyzed for major and trace dissolved species. Thirteen ground-water samples obtained from wells within a few meters of the freeze-shoe core sites and one from the landfill were analyzed for major and trace elements as well as the sulfur and oxygen isotope composition of dissolved sulfate. Samples of surface water were collected at 10 sites along the Canadian River from New Mexico to central Oklahoma. These river-water samples were analyzed for major elements, trace elements, and the isotopic composition of dissolved sulfate.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051091","usgsCitation":"Breit, G.N., Tuttle, M.L., Cozzarelli, I.M., Christenson, S.C., Jaeschke, J.B., Fey, D.L., and Berry, C.J., 2005, Results of chemical and isotopic analyses of sediment and water from alluvium of the Canadian River near a closed municipal landfill, Norman, Oklahoma (Version 1.0): U.S. Geological Survey Open-File Report 2005-1091, 43 p., illus., https://doi.org/10.3133/ofr20051091.","productDescription":"43 p., illus.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":185992,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6899,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1091/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Oklahoma ","city":"Norman","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -97.55,35.14 ], [ -97.55,35.35 ], [ -97.18,35.35 ], [ -97.18,35.14 ], [ -97.55,35.14 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db6249fe","contributors":{"authors":[{"text":"Breit, George N. 0000-0003-2188-6798 gbreit@usgs.gov","orcid":"https://orcid.org/0000-0003-2188-6798","contributorId":1480,"corporation":false,"usgs":true,"family":"Breit","given":"George","email":"gbreit@usgs.gov","middleInitial":"N.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":282579,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tuttle, Michele L.W. mtuttle@usgs.gov","contributorId":47839,"corporation":false,"usgs":true,"family":"Tuttle","given":"Michele","email":"mtuttle@usgs.gov","middleInitial":"L.W.","affiliations":[],"preferred":false,"id":282582,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cozzarelli, Isabelle M. 0000-0002-5123-1007 icozzare@usgs.gov","orcid":"https://orcid.org/0000-0002-5123-1007","contributorId":1693,"corporation":false,"usgs":true,"family":"Cozzarelli","given":"Isabelle","email":"icozzare@usgs.gov","middleInitial":"M.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":49175,"text":"Geology, Energy & Minerals Science Center","active":true,"usgs":true}],"preferred":true,"id":282580,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Christenson, Scott C. schris@usgs.gov","contributorId":980,"corporation":false,"usgs":true,"family":"Christenson","given":"Scott","email":"schris@usgs.gov","middleInitial":"C.","affiliations":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282578,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Jaeschke, Jeanne B. 0000-0002-6237-6164 jaeschke@usgs.gov","orcid":"https://orcid.org/0000-0002-6237-6164","contributorId":3876,"corporation":false,"usgs":true,"family":"Jaeschke","given":"Jeanne","email":"jaeschke@usgs.gov","middleInitial":"B.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true}],"preferred":true,"id":282581,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Fey, David L. dfey@usgs.gov","contributorId":713,"corporation":false,"usgs":true,"family":"Fey","given":"David","email":"dfey@usgs.gov","middleInitial":"L.","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":282576,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Berry, Cyrus J. cjberry@usgs.gov","contributorId":946,"corporation":false,"usgs":true,"family":"Berry","given":"Cyrus","email":"cjberry@usgs.gov","middleInitial":"J.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":282577,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70500,"text":"ofr20041274 - 2005 - Future petroleum supply - exploration or development?","interactions":[],"lastModifiedDate":"2012-02-02T00:13:32","indexId":"ofr20041274","displayToPublicDate":"2005-04-29T00:00:00","publicationYear":"2005","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":"2004-1274","title":"Future petroleum supply - exploration or development?","docAbstract":"The presentation is titled 'Future Petroleum Supply - Exploration or Development?' and provides a general overview of the magnitude and significance of reserve growth around the world. Reserve growth is defined as the increase in successive estimates of recoverable crude oil, natural gas, and natural-gas liquids and condensates in discovered fields. Analysis of recent exploration and production data shows that petroleum (both crude oil and natural gas) volumes added to reserves by reserve growth in the world are comparable to, if not greater than, the volumes added by new-field discoveries.\r\nThis presentation describes the examination of recoverable volumes of crude oil in 186 giant oil fields (excluding those of the United States (U.S.) and Canada) reported through time from 1981 to 2003 and describes a comparison of the successive increases in these volumes (reserve growth) with recoverable volumes added from new-field discoveries. Examples from the ongoing USGS study of reserve growth in the North Sea also are shown in this presentation.","language":"ENGLISH","doi":"10.3133/ofr20041274","usgsCitation":"Klett, T., 2005, Future petroleum supply - exploration or development? (Version 1.0): U.S. Geological Survey Open-File Report 2004-1274, 38 p., https://doi.org/10.3133/ofr20041274.","productDescription":"38 p.","costCenters":[],"links":[{"id":187698,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6468,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1274/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4224","contributors":{"authors":[{"text":"Klett, Timothy R. 0000-0001-9779-1168 tklett@usgs.gov","orcid":"https://orcid.org/0000-0001-9779-1168","contributorId":709,"corporation":false,"usgs":true,"family":"Klett","given":"Timothy R.","email":"tklett@usgs.gov","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":282545,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70475,"text":"ofr20051128 - 2005 - Water-level altitudes 2005 and water-level changes in the Chicot, Evangeline, and Jasper aquifers and compaction 1973-2004 in the Chicot and Evangeline aquifers, Houston-Galveston region, Texas","interactions":[],"lastModifiedDate":"2017-02-15T17:49:40","indexId":"ofr20051128","displayToPublicDate":"2005-04-27T00:00:00","publicationYear":"2005","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":"2005-1128","title":"Water-level altitudes 2005 and water-level changes in the Chicot, Evangeline, and Jasper aquifers and compaction 1973-2004 in the Chicot and Evangeline aquifers, Houston-Galveston region, Texas","docAbstract":"<p>This report is one in an annual series of reports that depicts water-level altitudes and water-level changes in the Chicot, Evangeline, and Jasper aquifers, and compaction in the Chicot and Evangeline aquifers in the Houston-Galveston region. The Houston-Galveston region comprises Harris, Galveston, Fort Bend, Waller, and Montgomery Counties and adjacent parts of Brazoria, Grimes, Walker, San Jacinto, Liberty, and Chambers Counties. The report was prepared in cooperation with the Harris-Galveston Coastal Subsidence District, the City of Houston, the Fort Bend Subsidence District, and the Lone Star Groundwater Conservation District. For the Chicot and Evangeline aquifers, maps show approximate water-level altitudes in 2005, water-level changes from 2004 to 2005, and approximate water-level changes from 2000 to 2005, from 1990 to 2005, and from 1977 to 2005 (figs. <a href=\"https://pubs.usgs.gov/of/2005/1128/fig1.htm\" data-mce-href=\"https://pubs.usgs.gov/of/2005/1128/fig1.htm\">1</a>, <a href=\"https://pubs.usgs.gov/of/2005/1128/fig2.htm\" data-mce-href=\"https://pubs.usgs.gov/of/2005/1128/fig2.htm\">2</a>, <a href=\"https://pubs.usgs.gov/of/2005/1128/fig3.htm\" data-mce-href=\"https://pubs.usgs.gov/of/2005/1128/fig3.htm\">3</a>, <a href=\"https://pubs.usgs.gov/of/2005/1128/fig4.htm\" data-mce-href=\"https://pubs.usgs.gov/of/2005/1128/fig4.htm\">4</a>, <a href=\"https://pubs.usgs.gov/of/2005/1128/fig5.htm\" data-mce-href=\"https://pubs.usgs.gov/of/2005/1128/fig5.htm\">5</a>, <a href=\"https://pubs.usgs.gov/of/2005/1128/fig6.htm\" data-mce-href=\"https://pubs.usgs.gov/of/2005/1128/fig6.htm\">6</a>, <a href=\"https://pubs.usgs.gov/of/2005/1128/fig7.htm\" data-mce-href=\"https://pubs.usgs.gov/of/2005/1128/fig7.htm\">7</a>, <a href=\"https://pubs.usgs.gov/of/2005/1128/fig8.htm\" data-mce-href=\"https://pubs.usgs.gov/of/2005/1128/fig8.htm\">8</a>, <a href=\"https://pubs.usgs.gov/of/2005/1128/fig9.htm\" data-mce-href=\"https://pubs.usgs.gov/of/2005/1128/fig9.htm\">9</a>, and <a href=\"https://pubs.usgs.gov/of/2005/1128/fig10.htm\" data-mce-href=\"https://pubs.usgs.gov/of/2005/1128/fig10.htm\">10</a>). For the Jasper aquifer, maps show approximate water-level altitudes in 2005 and water-level changes from 2004 to 2005 and 2000 to 2005 (figs. <a href=\"https://pubs.usgs.gov/of/2005/1128/fig11.htm\" data-mce-href=\"https://pubs.usgs.gov/of/2005/1128/fig11.htm\">11</a>, <a href=\"https://pubs.usgs.gov/of/2005/1128/fig12.htm\" data-mce-href=\"https://pubs.usgs.gov/of/2005/1128/fig12.htm\">12</a>, and <a href=\"https://pubs.usgs.gov/of/2005/1128/fig13.htm\" data-mce-href=\"https://pubs.usgs.gov/of/2005/1128/fig13.htm\">13</a>). The report also contains a map showing borehole extensometer (well equipped with compaction monitor) site locations (<a href=\"https://pubs.usgs.gov/of/2005/1128/fig14.htm\" data-mce-href=\"https://pubs.usgs.gov/of/2005/1128/fig14.htm\">fig. 14</a>) and graphs showing measured compaction of subsurface material at these sites from 1973 or later to 2004 (<a href=\"https://pubs.usgs.gov/of/2005/1128/fig15.htm\" data-mce-href=\"https://pubs.usgs.gov/of/2005/1128/fig15.htm\">fig. 15</a>).</p><p>The U.S. Geological Survey (USGS) has published annual reports of water-level altitudes and water-level changes for the Chicot and Evangeline aquifers in the Houston-Galveston region since 1979; and annual reports of same for the Fort Bend subregion (Fort Bend County and adjacent areas) since 1990. The USGS published its first water-level-altitude map for the Jasper aquifer in the greater Houston area (primarily Montgomery County) in 2001. The 2005 water-level-altitude and water-level-change maps for the three aquifers are included in this report.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051128","collaboration":"In cooperation with the Harris-Galveston Coastal Subsidence District, City of Houston, Fort Bend Subsidence District, and Lone Star Groundwater Conservation District","usgsCitation":"Kasmarek, M.C., and Houston, N.A., 2005, Water-level altitudes 2005 and water-level changes in the Chicot, Evangeline, and Jasper aquifers and compaction 1973-2004 in the Chicot and Evangeline aquifers, Houston-Galveston region, Texas: U.S. Geological Survey Open-File Report 2005-1128, HTML Document, https://doi.org/10.3133/ofr20051128.","productDescription":"HTML Document","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":188273,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6432,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1128/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Texas","city":"Galveston, Houston","otherGeospatial":"Chicot Aquifer, Evangeline Aquifer, Jasper Aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.3505859375,\n              29.554345125748267\n            ],\n            [\n              -94.52636718749999,\n              30.031055426540206\n            ],\n            [\n              -94.7021484375,\n              30.29701788337205\n            ],\n            [\n              -94.976806640625,\n              30.675715404167743\n            ],\n            [\n              -95.07568359375,\n              30.829139422013956\n            ],\n            [\n              -95.25970458984374,\n              30.954057859276126\n            ],\n            [\n              -95.614013671875,\n              30.95876857077987\n            ],\n            [\n              -96.064453125,\n              30.798474179567823\n            ],\n            [\n              -96.4434814453125,\n              30.600093873550072\n            ],\n            [\n              -96.2237548828125,\n              30.073847754270204\n            ],\n            [\n              -96.03149414062499,\n              29.410890376109\n            ],\n            [\n              -95.82275390625,\n              29.080175989623203\n            ],\n            [\n              -95.6304931640625,\n              28.9072060763367\n            ],\n            [\n              -95.3558349609375,\n              28.8831596093235\n            ],\n            [\n              -94.7515869140625,\n              29.291189838184863\n            ],\n            [\n              -94.3505859375,\n              29.554345125748267\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e8e4b07f02db5e8cd7","contributors":{"authors":[{"text":"Kasmarek, Mark C. 0000-0003-2808-2506 mckasmar@usgs.gov","orcid":"https://orcid.org/0000-0003-2808-2506","contributorId":1968,"corporation":false,"usgs":true,"family":"Kasmarek","given":"Mark","email":"mckasmar@usgs.gov","middleInitial":"C.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282501,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Houston, Natalie A. 0000-0002-6071-4545 nhouston@usgs.gov","orcid":"https://orcid.org/0000-0002-6071-4545","contributorId":1682,"corporation":false,"usgs":true,"family":"Houston","given":"Natalie","email":"nhouston@usgs.gov","middleInitial":"A.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282500,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70464,"text":"ofr20051072 - 2005 - GWM-a ground-water management process for the U.S. Geological Survey modular ground-water model (MODFLOW-2000)","interactions":[],"lastModifiedDate":"2012-02-02T00:13:32","indexId":"ofr20051072","displayToPublicDate":"2005-04-25T00:00:00","publicationYear":"2005","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":"2005-1072","title":"GWM-a ground-water management process for the U.S. Geological Survey modular ground-water model (MODFLOW-2000)","docAbstract":"GWM is a Ground?Water Management Process for the U.S. Geological Survey modular three?dimensional ground?water model, MODFLOW?2000. GWM uses a response?matrix approach to solve several types of linear, nonlinear, and mixed?binary linear ground?water management formulations. Each management formulation consists of a set of decision variables, an objective function, and a set of constraints. Three types of decision variables are supported by GWM: flow?rate decision variables, which are withdrawal or injection rates at well sites; external decision variables, which are sources or sinks of water that are external to the flow model and do not directly affect the state variables of the simulated ground?water system (heads, streamflows, and so forth); and binary variables, which have values of 0 or 1 and are used to define the status of flow?rate or external decision variables. Flow?rate decision variables can represent wells that extend over one or more model cells and be active during one or more model stress periods; external variables also can be active during one or more stress periods. A single objective function is supported by GWM, which can be specified to either minimize or maximize the weighted sum of the three types of decision variables. Four types of constraints can be specified in a GWM formulation: upper and lower bounds on the flow?rate and external decision variables; linear summations of the three types of decision variables; hydraulic?head based constraints, including drawdowns, head differences, and head gradients; and streamflow and streamflow?depletion constraints.\r\n\r\nThe Response Matrix Solution (RMS) Package of GWM uses the Ground?Water Flow Process of MODFLOW to calculate the change in head at each constraint location that results from a perturbation of a flow?rate variable; these changes are used to calculate the response coefficients. For linear management formulations, the resulting matrix of response coefficients is then combined with other components of the linear management formulation to form a complete linear formulation; the formulation is then solved by use of the simplex algorithm, which is incorporated into the RMS Package. Nonlinear formulations arise for simulated conditions that include water?table (unconfined) aquifers or head?dependent boundary conditions (such as streams, drains, or evapotranspiration from the water table). Nonlinear formulations are solved by sequential linear programming; that is, repeated linearization of the nonlinear features of the management problem. In this approach, response coefficients are recalculated for each iteration of the solution process. Mixed?binary linear (or mildly nonlinear) formulations are solved by use of the branch and bound algorithm, which is also incorporated into the RMS Package.\r\n\r\nThree sample problems are provided to demonstrate the use of GWM for typical ground?water flow management problems. These sample problems provide examples of how GWM input files are constructed to specify the decision variables, objective function, constraints, and solution process for a GWM run. The GWM Process runs with the MODFLOW?2000 Global and Ground?Water Flow Processes, but in its current form GWM cannot be used with the Observation, Sensitivity, Parameter?Estimation, or Ground?Water Transport Processes. The GWM Process is written with a modular structure so that new objective functions, constraint types, and solution algorithms can be added.","language":"ENGLISH","doi":"10.3133/ofr20051072","usgsCitation":"Ahlfeld, D.P., Barlow, P.M., and Mulligan, A.E., 2005, GWM-a ground-water management process for the U.S. Geological Survey modular ground-water model (MODFLOW-2000): U.S. Geological Survey Open-File Report 2005-1072, 124 p., https://doi.org/10.3133/ofr20051072.","productDescription":"124 p.","costCenters":[],"links":[{"id":188688,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6426,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1072/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b146d","contributors":{"authors":[{"text":"Ahlfeld, David P.","contributorId":49464,"corporation":false,"usgs":true,"family":"Ahlfeld","given":"David","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":282486,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barlow, Paul M. 0000-0003-4247-6456 pbarlow@usgs.gov","orcid":"https://orcid.org/0000-0003-4247-6456","contributorId":1200,"corporation":false,"usgs":true,"family":"Barlow","given":"Paul","email":"pbarlow@usgs.gov","middleInitial":"M.","affiliations":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":282485,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mulligan, Anne E.","contributorId":66789,"corporation":false,"usgs":true,"family":"Mulligan","given":"Anne","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":282487,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70434,"text":"ofr20051007 - 2005 - The difference between the potentiometric surfaces of the Magothy aquifer, September 1975 and September 2003 in southern Maryland","interactions":[],"lastModifiedDate":"2023-03-10T13:11:15.881911","indexId":"ofr20051007","displayToPublicDate":"2005-04-22T00:00:00","publicationYear":"2005","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":"2005-1007","title":"The difference between the potentiometric surfaces of the Magothy aquifer, September 1975 and September 2003 in southern Maryland","docAbstract":"This report presents a map showing the change in the potentiometric surface of the Magothy aquifer in the Magothy Formation of Cretaceous age in Southern Maryland for September 1975 and September 2003. The map, based on water level measurements in 51 wells, shows that during the 28-year period, the potentiometric surface had no change at the outcrop area, which is in the northernmost part of the study area, but declined 71 feet at Waldorf. Waldorf is located near the southwesternmost part of the study area, and approaches the downdip boundary of the aquifer.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051007","usgsCitation":"Curtin, S.E., Andreasen, D., and Wheeler, J.C., 2005, The difference between the potentiometric surfaces of the Magothy aquifer, September 1975 and September 2003 in southern Maryland: U.S. Geological Survey Open-File Report 2005-1007, 1 p., https://doi.org/10.3133/ofr20051007.","productDescription":"1 p.","temporalStart":"1975-09-01","temporalEnd":"2003-09-30","costCenters":[{"id":41514,"text":"Maryland-Delaware-District of Columbia  Water Science Center","active":true,"usgs":true}],"links":[{"id":8907,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1007/","linkFileType":{"id":5,"text":"html"}},{"id":186695,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db6684c5","contributors":{"authors":[{"text":"Curtin, Stephen E. securtin@usgs.gov","contributorId":3703,"corporation":false,"usgs":true,"family":"Curtin","given":"Stephen","email":"securtin@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282422,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreasen, David C.","contributorId":59003,"corporation":false,"usgs":true,"family":"Andreasen","given":"David C.","affiliations":[],"preferred":false,"id":282424,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wheeler, Judith C.","contributorId":13620,"corporation":false,"usgs":true,"family":"Wheeler","given":"Judith","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":282423,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70431,"text":"ofr20051005 - 2005 - The difference between the potentiometric surfaces of the Aquia Aquifer, September 1982 and September 2003 in southern Maryland","interactions":[],"lastModifiedDate":"2023-03-10T13:10:38.726608","indexId":"ofr20051005","displayToPublicDate":"2005-04-22T00:00:00","publicationYear":"2005","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":"2005-1005","title":"The difference between the potentiometric surfaces of the Aquia Aquifer, September 1982 and September 2003 in southern Maryland","docAbstract":"This report presents a map showing the change in the potentiometric surface of the Aquia aquifer in the Aquia Formation of Paleocene age in Southern Maryland for September 1982 and September 2003. The map, based on water level measurements in 56 wells, shows that the potentiometric surface during the 21-year period declined from zero in the northernmost part of the study area, which is the outcrop of the aquifer, to 108 feet at Lexington Park. Lexington Park is near the southeasternmost part of the study area and approaches the downdip boundary of the aquifer.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051005","usgsCitation":"Curtin, S.E., Andreason, D.C., and Wheeler, J.C., 2005, The difference between the potentiometric surfaces of the Aquia Aquifer, September 1982 and September 2003 in southern Maryland: U.S. Geological Survey Open-File Report 2005-1005, 1 p., https://doi.org/10.3133/ofr20051005.","productDescription":"1 p.","temporalStart":"1982-09-01","temporalEnd":"2003-09-30","costCenters":[{"id":41514,"text":"Maryland-Delaware-District of Columbia  Water Science Center","active":true,"usgs":true}],"links":[{"id":186625,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8905,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1005/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668586","contributors":{"authors":[{"text":"Curtin, Stephen E. securtin@usgs.gov","contributorId":3703,"corporation":false,"usgs":true,"family":"Curtin","given":"Stephen","email":"securtin@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282413,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreason, David C.","contributorId":24857,"corporation":false,"usgs":true,"family":"Andreason","given":"David","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":282415,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wheeler, Judith C.","contributorId":13620,"corporation":false,"usgs":true,"family":"Wheeler","given":"Judith","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":282414,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70428,"text":"ofr20041400 - 2005 - Project PROBE Leg II: Final report and archive of swath bathymetric sonar, CTD/XBT and GPS navigation data collected during USGS Cruise 03008 (NOAA Cruise RB0303) Puerto Rico Trench 18 February - 7 March, 2003","interactions":[],"lastModifiedDate":"2022-06-27T21:16:19.118542","indexId":"ofr20041400","displayToPublicDate":"2005-04-22T00:00:00","publicationYear":"2005","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":"2004-1400","title":"Project PROBE Leg II: Final report and archive of swath bathymetric sonar, CTD/XBT and GPS navigation data collected during USGS Cruise 03008 (NOAA Cruise RB0303) Puerto Rico Trench 18 February - 7 March, 2003","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20041400","usgsCitation":"ten Brink, U., Danforth, W., Polloni, C.F., Parker, C.E., Uozumi, T., and Williams, G.F., 2005, Project PROBE Leg II: Final report and archive of swath bathymetric sonar, CTD/XBT and GPS navigation data collected during USGS Cruise 03008 (NOAA Cruise RB0303) Puerto Rico Trench 18 February - 7 March, 2003: U.S. Geological Survey Open-File Report 2004-1400, HTML Document; DVD, https://doi.org/10.3133/ofr20041400.","productDescription":"HTML Document; DVD","onlineOnly":"Y","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":402568,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_70839.htm","linkFileType":{"id":5,"text":"html"}},{"id":7436,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1400/","linkFileType":{"id":5,"text":"html"}},{"id":191061,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"otherGeospatial":"Puerto Rico Trench","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.05859375,\n              11.867350911459308\n            ],\n            [\n              -58.88671875,\n              11.867350911459308\n            ],\n            [\n              -58.88671875,\n              22.958393318086348\n            ],\n            [\n              -75.05859375,\n              22.958393318086348\n            ],\n            [\n              -75.05859375,\n              11.867350911459308\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65daf5","contributors":{"authors":[{"text":"ten Brink, Uri S. 0000-0001-6858-3001 utenbrink@usgs.gov","orcid":"https://orcid.org/0000-0001-6858-3001","contributorId":127560,"corporation":false,"usgs":true,"family":"ten Brink","given":"Uri S.","email":"utenbrink@usgs.gov","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":282402,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Danforth, William","contributorId":49026,"corporation":false,"usgs":true,"family":"Danforth","given":"William","affiliations":[],"preferred":false,"id":282400,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Polloni, Christopher F.","contributorId":93087,"corporation":false,"usgs":true,"family":"Polloni","given":"Christopher","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":282403,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Parker, Castle Eugene","contributorId":108202,"corporation":false,"usgs":true,"family":"Parker","given":"Castle","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":282404,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Uozumi, Toshihiko","contributorId":14518,"corporation":false,"usgs":true,"family":"Uozumi","given":"Toshihiko","email":"","affiliations":[],"preferred":false,"id":282399,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Williams, Glynn F.","contributorId":83618,"corporation":false,"usgs":true,"family":"Williams","given":"Glynn","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":282401,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70433,"text":"ofr20051009 - 2005 - The difference between the potentiometric surfaces of the upper Patapsco aquifer, September 1990 and September 2003 in southern Maryland","interactions":[],"lastModifiedDate":"2021-09-24T14:15:44.003009","indexId":"ofr20051009","displayToPublicDate":"2005-04-22T00:00:00","publicationYear":"2005","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":"2005-1009","title":"The difference between the potentiometric surfaces of the upper Patapsco aquifer, September 1990 and September 2003 in southern Maryland","docAbstract":"This report presents a map showing the change in the potentiometric surface of the Upper Patapsco aquifer in the Upper Patapsco Formation of Cretaceous age in Southern Maryland for September 1990 and September 2003. The map, based on water level measurements in 32 wells, shows that during the 13-year period, the potentiometric surface changed from an increase of 6 feet at Arnold, which is located just north of Annapolis, to a decline of 25 feet at Waldorf and Lexington Park and 20 feet at LaPlata and the Chalk Point powerplant.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051009","usgsCitation":"Curtin, S.E., Andreasen, D., and Wheeler, J.C., 2005, The difference between the potentiometric surfaces of the upper Patapsco aquifer, September 1990 and September 2003 in southern Maryland: U.S. Geological Survey Open-File Report 2005-1009, 1 p., https://doi.org/10.3133/ofr20051009.","productDescription":"1 p.","temporalStart":"1990-09-01","temporalEnd":"2003-09-30","costCenters":[],"links":[{"id":186627,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8912,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1009/","linkFileType":{"id":5,"text":"html"}},{"id":389714,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_78442.htm"}],"country":"United States","state":"Maryland","otherGeospatial":"upper Patapsco aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.2667,\n              38.1\n            ],\n            [\n              -76.25,\n              38.1\n            ],\n            [\n              -76.25,\n              39.2333\n            ],\n            [\n              -77.2667,\n              39.2333\n            ],\n            [\n              -77.2667,\n              38.1\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db6684de","contributors":{"authors":[{"text":"Curtin, Stephen E. securtin@usgs.gov","contributorId":3703,"corporation":false,"usgs":true,"family":"Curtin","given":"Stephen","email":"securtin@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282419,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreasen, David C.","contributorId":59003,"corporation":false,"usgs":true,"family":"Andreasen","given":"David C.","affiliations":[],"preferred":false,"id":282421,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wheeler, Judith C.","contributorId":13620,"corporation":false,"usgs":true,"family":"Wheeler","given":"Judith","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":282420,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70432,"text":"ofr20051004 - 2005 - Potentiometric surface of the Aquia Aquifer in southern Maryland, September 2003","interactions":[],"lastModifiedDate":"2023-03-10T13:10:06.189313","indexId":"ofr20051004","displayToPublicDate":"2005-04-22T00:00:00","publicationYear":"2005","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":"2005-1004","title":"Potentiometric surface of the Aquia Aquifer in southern Maryland, September 2003","docAbstract":"This report presents a map showing the potentiometric surface of the Aquia aquifer in the Aquia Formation of Paleocene age in Southern Maryland during September 2003. The map is based on water-level measurements in 91 wells. The highest measured water level was 40 feet above sea level near the northern boundary and outcrop area of the aquifer in the central part of Anne Arundel County, and was below sea level just south of this area and in the remainder of the study area. The hydraulic gradient increased southeastward toward an extensive cone of depression around well fields at Lexington Park and Solomons Island. Another cone of depression occurred in northern Calvert County due to pumpage at and near North Beach and Chesapeake Beach. The water level measured in this area has declined to 48 feet below sea level. The lowest water level measured was 156 feet below sea level at the center of a cone of depression at Lexington Park.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051004","usgsCitation":"Curtin, S.E., Andreason, D.C., and Wheeler, J.C., 2005, Potentiometric surface of the Aquia Aquifer in southern Maryland, September 2003: U.S. Geological Survey Open-File Report 2005-1004, 1 p., https://doi.org/10.3133/ofr20051004.","productDescription":"1 p.","temporalStart":"2003-09-01","temporalEnd":"2003-09-30","costCenters":[{"id":41514,"text":"Maryland-Delaware-District of Columbia  Water Science Center","active":true,"usgs":true}],"links":[{"id":186626,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8904,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1004/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db683080","contributors":{"authors":[{"text":"Curtin, Stephen E. securtin@usgs.gov","contributorId":3703,"corporation":false,"usgs":true,"family":"Curtin","given":"Stephen","email":"securtin@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282416,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreason, David C.","contributorId":24857,"corporation":false,"usgs":true,"family":"Andreason","given":"David","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":282418,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wheeler, Judith C.","contributorId":13620,"corporation":false,"usgs":true,"family":"Wheeler","given":"Judith","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":282417,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70426,"text":"ofr20041329 - 2005 - Ground-water quality in the Chemung River Basin, New York, 2003","interactions":[],"lastModifiedDate":"2017-04-04T13:33:40","indexId":"ofr20041329","displayToPublicDate":"2005-04-22T00:00:00","publicationYear":"2005","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":"2004-1329","title":"Ground-water quality in the Chemung River Basin, New York, 2003","docAbstract":"<p>Water samples were collected from 24 public-supply wells and 13 private residential wells during the summer of 2003 and analyzed to describe the chemical quality of ground water throughout the Chemung River basin, upgradient from Waverly, N.Y, on the Pennsylvania border. Wells were selected to represent areas of heaviest ground-water use and greatest vulnerability to contamination, and to obtain a geographical distribution across the 1,130 square-mile basin. Samples were analyzed for physical properties, inorganic constituents, nutrients, metals and radionuclides, pesticides, volatile organic compounds, and bacteria.</p><p>The cations that were detected in the highest concentrations were calcium and sodium; the anions that were detected in the greatest concentrations were bicarbonate, chloride, and sulfate. The predominant nutrient was nitrate. Nitrate concentrations in samples from wells finished in sand and gravel were greater than in those from wells finished in bedrock, except for one bedrock well, which had the highest nitrate concentration of any sample in this study. The most commonly detected metals were aluminum, barium, iron, manganese, and strontium. The range of tritium concentrations (0.6 to 12.5 tritium units) indicates that the water ages ranged from less than 10 years old to more than 50 years old. All but one of the 15 pesticides detected were herbicides; those detected most frequently were atrazine, deethylatrazine, and two degradation products of metolachlor (metachlor ESA and metachlor OA), which were the pesticides detected at the highest concentrations. Not every sample collected was analyzed for pesticides, and pesticides were detected only in wells finished in sand and gravel. Volatile organic compounds were detected in 15 samples, and the concentrations were at or near the analytical detection limits. Total coliform were detected in 12 samples; fecal coliform were detected in 7 samples; and Escherichia coli was detected in 6 samples. These bacteria were detected in water from bedrock as well as sand-and-gravel aquifers.</p><p>Federal and State water-quality standards were exceeded in several samples. Two samples exceeded the chloride U.S. Environmental Protection Agency Secondary Maximum Contaminant Level of 250 milligrams per liter. The U.S. Environmental Protection Agency Drinking Water Advisory for sodium (30 to 60 milligrams per liter) was exceeded in 11 samples. The upper limit of the Secondary Maximum Contaminant Level range for aluminum (200 micrograms per liter) was exceeded in one sample. The Maximum Contaminant Level for barium (2,000 micrograms per liter) was exceeded in one sample. The Secondary Maximum Contaminant Level for iron (300 micrograms per liter) was exceeded in 11 samples. The Secondary Maximum Contaminant Level for manganese (50 micrograms per liter) was exceeded in 20 samples. The proposed Maximum Contaminant Level for radon (300 picocuries per liter) was exceeded in 34 samples.</p>","language":"English","publisher":"U.S Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20041329","collaboration":"Prepared in cooperation with the New York State Department of Environmental Conservation","usgsCitation":"Hetcher-Aguila, K.K., 2005, Ground-water quality in the Chemung River Basin, New York, 2003: U.S. Geological Survey Open-File Report 2004-1329, iv, 19 p., https://doi.org/10.3133/ofr20041329.","productDescription":"iv, 19 p.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":185676,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2004/1329/coverthb.jpg"},{"id":323423,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2004/1329/ofr20041329.pdf","text":"Report ","size":"2.45 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2004-1329"}],"contact":"<p>Director, New York Water Science Center<br>U.S. Geological Survey<br> 425 Jordan Rd<br> Troy, NY 12180<br> (518) 285-5695&nbsp;<br> <a href=\"http://ny.water.usgs.gov\" data-mce-href=\"http://ny.water.usgs.gov\">http://ny.water.usgs.gov/</a></p>","tableOfContents":"<ul>\n<li>Abstract</li>\n<li>Introduction</li>\n<li>Methods</li>\n<li>Ground Water Quality</li>\n<li>Summary&nbsp;</li>\n<li>References Cited</li>\n</ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69783d","contributors":{"authors":[{"text":"Hetcher-Aguila, Kari K.","contributorId":92753,"corporation":false,"usgs":true,"family":"Hetcher-Aguila","given":"Kari","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":282395,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70414,"text":"ofr20051150 - 2005 - Data for selected gaging stations in the upper Red River of the North Basin in Minnesota, September 2001 through September 2003","interactions":[],"lastModifiedDate":"2018-02-16T16:12:45","indexId":"ofr20051150","displayToPublicDate":"2005-04-21T00:00:00","publicationYear":"2005","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":"2005-1150","title":"Data for selected gaging stations in the upper Red River of the North Basin in Minnesota, September 2001 through September 2003","docAbstract":"Surface-water and water-quality data were collected to use in development of upper Red River of the North Basin Total Maximum Daily Loads (TMDLs). This report presents the data that were collected. \r\n\r\n \r\n\r\nDuring September 2001 through September 2003, data were collected at 13 selected gaging stations in the upper Red River of the North Basin. Continuous streamflow data were collected at three of the gaging stations. Water-quality samples were collected at all 13 gaging stations; and, simultaneous with sample collection, in-stream specific conductance, pH, water temperature, dissolved oxygen, and turbidity were measured. Samples were analyzed for selected nutrients, selected bacteria, chlorophyll a, and suspended sediment.\r\n\r\n \r\n\r\nContinuous in-stream water-quality monitors were installed at two gaging stations to measure specific conductance, pH, water temperature, dissolved oxygen, and turbidity.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20051150","usgsCitation":"Damschen, W., and Nustad, R.A., 2005, Data for selected gaging stations in the upper Red River of the North Basin in Minnesota, September 2001 through September 2003: U.S. Geological Survey Open-File Report 2005-1150, 93 p., https://doi.org/10.3133/ofr20051150.","productDescription":"93 p.","onlineOnly":"Y","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":185516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6969,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr2005-1150/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c918","contributors":{"authors":[{"text":"Damschen, William C. wcdamsch@usgs.gov","contributorId":1610,"corporation":false,"usgs":true,"family":"Damschen","given":"William C.","email":"wcdamsch@usgs.gov","affiliations":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282379,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nustad, Rochelle A. 0000-0002-4713-5944 ranustad@usgs.gov","orcid":"https://orcid.org/0000-0002-4713-5944","contributorId":1811,"corporation":false,"usgs":true,"family":"Nustad","given":"Rochelle","email":"ranustad@usgs.gov","middleInitial":"A.","affiliations":[{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282380,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70415,"text":"ofr20041412 - 2005 - Correlation analysis of a ground-water level monitoring network, Miami-Dade County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:13:47","indexId":"ofr20041412","displayToPublicDate":"2005-04-21T00:00:00","publicationYear":"2005","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":"2004-1412","title":"Correlation analysis of a ground-water level monitoring network, Miami-Dade County, Florida","docAbstract":"The U.S. Geological Survey cooperative ground-water monitoring program in Miami-Dade County, Florida, expanded from 4 to 98 continuously recording water-level monitoring wells during the 1939-2001 period. Network design was based on area specific assessments; however, no countywide statistical assessments of network coverage had been performed for the purpose of assessing network redundancy.\r\n\r\nTo aid in the assessment of network redundancy, correlation analyses were performed using S-PLUS 2000 statistical analysis software for daily maximum water-level data from 98 monitoring wells for the November 1, 1973, to October 31, 2000 period. Because of the complexities of the hydrologic, water-supply, and water-management systems in Miami-Dade County and the changes that have occurred to these systems through time, spatial and temporal variations in the degree of correlation had to be considered. To assess temporal variation in correlation, water-level data from each well were subdivided by year and by wet and dry seasons. For each well, year, and season, correlation analyses were performed on the data from those wells that had available data. For selected wells, the resulting correlation coefficients from each year and season were plotted with respect to time. To assess spatial variation in correlation, the coefficients determined from the correlation analysis were averaged. These average wet- and dry-season correlation coefficients were plotted spatially using geographic information system software.\r\n\r\nWells with water-level data that correlated with a coefficient of 0.95 or greater were almost always located in relatively close proximity to each other. Five areas were identified where the water-level data from wells within the area remained correlated with that of other wells in the area during the wet and dry seasons. These areas are located in or near the C-1 and C-102 basins (2 wells), in or near the C-6 and C-7 basins (2 wells), near the Florida Keys Aqueduct Authority Well Field (2 wells), near the Hialeah-Miami Springs Well Field (6 wells), and near the West Well Field (21 wells). Data from the remaining 65 wells (most of the wells in the network) generally were not correlated with those of other wells during both the wet and dry seasons with an average coefficient of 0.95 or greater for the comparison.\r\n\r\nBecause many of the wells near the West Well Field and some near the Hialeah-Miami Springs Well Field had not been in operation for very long (most having been installed in 1994), the averaged correlation coefficients for these wells were often determined using only a few seasons of data. For the few instances where water-level data were found to be well correlated on average for a lengthy period of record, short-term declines in correlation were often identified. In general, it would be beneficial to compare data for longer periods of record than currently available.","language":"ENGLISH","doi":"10.3133/ofr20041412","usgsCitation":"Prinos, S.T., 2005, Correlation analysis of a ground-water level monitoring network, Miami-Dade County, Florida: U.S. Geological Survey Open-File Report 2004-1412, 3 p. online publication, illus., https://doi.org/10.3133/ofr20041412.","productDescription":"3 p. online publication, illus.","costCenters":[],"links":[{"id":6970,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr2004-1412/","linkFileType":{"id":5,"text":"html"}},{"id":185517,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684974","contributors":{"authors":[{"text":"Prinos, Scott T. 0000-0002-5776-8956 stprinos@usgs.gov","orcid":"https://orcid.org/0000-0002-5776-8956","contributorId":4045,"corporation":false,"usgs":true,"family":"Prinos","given":"Scott","email":"stprinos@usgs.gov","middleInitial":"T.","affiliations":[{"id":156,"text":"Caribbean Water Science Center","active":true,"usgs":true},{"id":269,"text":"FLWSC-Ft. Lauderdale","active":true,"usgs":true}],"preferred":true,"id":282381,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70394,"text":"ofr20041392 - 2005 - The stability of chlorofluorocarbons (CFCs) in ground-water samples archived in borosilicate ampoules","interactions":[],"lastModifiedDate":"2020-02-09T16:30:58","indexId":"ofr20041392","displayToPublicDate":"2005-04-15T00:00:00","publicationYear":"2005","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":"2004-1392","title":"The stability of chlorofluorocarbons (CFCs) in ground-water samples archived in borosilicate ampoules","docAbstract":"The U.S. Geological Survey (USGS) Chlorofluorocarbon (CFC) Laboratory in Reston, Va., has been measuring concentrations of CFCs in ground-water samples since 1989 to estimate the year that a water sample was recharged to a ground-water flow system. The water samples have been collected in flame-sealed borosilicate ampoules. Typically for each site, three samples were analyzed within days to a few months after collection, and additional samples were archived for extended periods of time (up to four years). The stability of CFC concentrations in the archived water samples from the USGS CFC Laboratory was investigated by analyzing the CFC concentrations in archived water samples and comparing them with the CFC concentrations that were obtained soon after the samples were collected. The archived samples selected for analysis were chosen from sites with a wide variety of hydrogeologic and geochemical conditions. For CFC-11 and CFC-12 concentrations, approximately 14% and 10.5%, respectively, of the archived samples were statistically different (both higher and lower) from the concentrations obtained from analyses conducted soon after the sample collection. Most of the extraneous values were attributed to natural variability of CFC concentrations originally in the water discharged from wells, rather than to microbial degradation within the ampoule on storage.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20041392","usgsCitation":"Shapiro, S.D., Busenberg, E., and Plummer, N., 2005, The stability of chlorofluorocarbons (CFCs) in ground-water samples archived in borosilicate ampoules: U.S. Geological Survey Open-File Report 2004-1392, HTML, https://doi.org/10.3133/ofr20041392.","productDescription":"HTML","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":6941,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr20041392/","linkFileType":{"id":5,"text":"html"}},{"id":192611,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Virginia ","county":"Fairfax County","city":"Reston","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.40898132324219,\n              38.92843409820933\n            ],\n            [\n              -77.31834411621094,\n              38.92843409820933\n            ],\n            [\n              -77.31834411621094,\n              38.982897808179985\n            ],\n            [\n              -77.40898132324219,\n              38.982897808179985\n            ],\n            [\n              -77.40898132324219,\n              38.92843409820933\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc7cd","contributors":{"authors":[{"text":"Shapiro, Stephanie Dunkle","contributorId":82738,"corporation":false,"usgs":true,"family":"Shapiro","given":"Stephanie","email":"","middleInitial":"Dunkle","affiliations":[],"preferred":false,"id":282339,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Busenberg, Eurybiades ebusenbe@usgs.gov","contributorId":2271,"corporation":false,"usgs":true,"family":"Busenberg","given":"Eurybiades","email":"ebusenbe@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":282337,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":282338,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70392,"text":"ofr20051148 - 2005 - Acid-rock drainage at Skytop, Centre County, Pennsylvania, 2004","interactions":[],"lastModifiedDate":"2018-10-29T10:04:08","indexId":"ofr20051148","displayToPublicDate":"2005-04-15T00:00:00","publicationYear":"2005","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":"2005-1148","title":"Acid-rock drainage at Skytop, Centre County, Pennsylvania, 2004","docAbstract":"Recent construction for Interstate Highway 99 (I?99) exposed pyrite and associated Zn-Pb sulfide minerals beneath a >10-m thick gossan to oxidative weathering along a 40-60-m deep roadcut through a 270-m long section of the Ordovician Bald Eagle Formation at Skytop, near State College, Centre County, Pennsylvania. Nearby Zn-Pb deposits hosted in associated sandstone and limestone in Blair and Centre Counties were prospected in the past; however, these deposits generally were not viable as commercial mines. The pyritic sandstone from the roadcut was crushed and used locally as road base and fill for adjoining segments of I?99. Within months, acidic (pH<3), metal-laden seeps and runoff from the exposed cut and crushed sandstone raised concerns about surface- and ground-water contamination and prompted a halt in road construction and the beginning of costly remediation. Mineralized sandstones from the cut contain as much as 34 wt. % Fe, 28 wt. % S, 3.5 wt. % Zn, 1% wt. Pb, 88 ppm As, and 32 ppm Cd. A composite of <2 mm material sampled from the cut face contains 8.1 wt. % total sulfide S, 0.6 wt. % sulfate S, and is net acidic by acid-base accounting (net neutralization potential ?234 kg CaCO3/t). Primary sulfide minerals include pyrite, marcasite, sphalerite (2 to 12 wt. % Fe) and traces of chalcopyrite and galena. Pyrite occurs in mm- to cm-scale veinlets and disseminated grains in sandstone, as needles, and in a locally massive pyrite-cemented breccia along a fault. Inclusions (<10 ?m) of CdS and Ni-Co-As minerals in pyrite and minor amounts of Cd in sphalerite (0.1 wt. % or less) explain the primary source of trace metals in the rock and in associated secondary minerals and seepage. Wet/dry cycles associated with intermittent rainfall promoted oxidative weathering and dissolution of primary sulfides and their oxidation products. Resulting sulfate solutions evaporated during dry periods to form intermittent ?blooms? of soluble, yellow and white efflorescent sulfate salts (copiapite, melanterite, and halotrichite) on exposed rock and other surfaces. Salts coating the cut face incorporated Fe, Al, S, and minor Zn. They readily dissolved in deionized water in the laboratory to form solutions with pH <2.5, consistent with field observations. In addition to elevated dissolved Fe and sulfate concentrations (>1,000 mg/L), seep waters at the base of the cut contain >100 mg/L dissolved Zn and >1 mg/L As, Co, Cu, and Ni. Lead is relatively immobile (<10 ?g/L in seep waters). The salts sequester metals and acidity between rainfall events. Episodic salt dissolution then contributes pulses of contamination including acid to surface runoff and ground water. The Skytop experience highlights the need to understand dynamic interactions of mineralogy and hydrology in order to avoid potentially negative environmental impacts associated with excavation in sulfidic rocks.","language":"ENGLISH","doi":"10.3133/ofr20051148","usgsCitation":"Hammarstrom, J.M., Brady, K., and Cravotta, C.A., 2005, Acid-rock drainage at Skytop, Centre County, Pennsylvania, 2004 (Online Version 1.0): U.S. Geological Survey Open-File Report 2005-1148, 45 p., https://doi.org/10.3133/ofr20051148.","productDescription":"45 p.","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":192569,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6939,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1148/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699d86","contributors":{"authors":[{"text":"Hammarstrom, Jane M. 0000-0003-2742-3460 jhammars@usgs.gov","orcid":"https://orcid.org/0000-0003-2742-3460","contributorId":1226,"corporation":false,"usgs":true,"family":"Hammarstrom","given":"Jane","email":"jhammars@usgs.gov","middleInitial":"M.","affiliations":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true},{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":282333,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brady, Keith","contributorId":92764,"corporation":false,"usgs":true,"family":"Brady","given":"Keith","affiliations":[],"preferred":false,"id":282335,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cravotta, Charles A. III, 0000-0003-3116-4684 cravotta@usgs.gov","orcid":"https://orcid.org/0000-0003-3116-4684","contributorId":2193,"corporation":false,"usgs":true,"family":"Cravotta","given":"Charles","suffix":"III,","email":"cravotta@usgs.gov","middleInitial":"A.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":false,"id":282334,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70377,"text":"ofr20051134 - 2005 - Organic petrography of coals from a coalbed methane test well, Ouachita Parish, Louisiana","interactions":[],"lastModifiedDate":"2018-07-31T11:26:19","indexId":"ofr20051134","displayToPublicDate":"2005-04-08T00:00:00","publicationYear":"2005","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":"2005-1134","title":"Organic petrography of coals from a coalbed methane test well, Ouachita Parish, Louisiana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051134","usgsCitation":"Hackley, P.C., and Warwick, P.D., 2005, Organic petrography of coals from a coalbed methane test well, Ouachita Parish, Louisiana (Online only - Version 1.0): U.S. Geological Survey Open-File Report 2005-1134, 22 p., https://doi.org/10.3133/ofr20051134.","productDescription":"22 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":186410,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6535,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1134/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only - Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68acba","contributors":{"authors":[{"text":"Hackley, Paul C. 0000-0002-5957-2551 phackley@usgs.gov","orcid":"https://orcid.org/0000-0002-5957-2551","contributorId":592,"corporation":false,"usgs":true,"family":"Hackley","given":"Paul","email":"phackley@usgs.gov","middleInitial":"C.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true},{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"preferred":true,"id":282313,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Warwick, Peter D. 0000-0002-3152-7783 pwarwick@usgs.gov","orcid":"https://orcid.org/0000-0002-3152-7783","contributorId":762,"corporation":false,"usgs":true,"family":"Warwick","given":"Peter","email":"pwarwick@usgs.gov","middleInitial":"D.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":282314,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70364,"text":"ofr20051062 - 2005 - Reconnaissance gas measurements on the East Rift Zone of Kilauea Volcano, Hawai'i by Fourier transform infrared spectroscopy","interactions":[],"lastModifiedDate":"2019-05-07T09:53:01","indexId":"ofr20051062","displayToPublicDate":"2005-04-06T00:00:00","publicationYear":"2005","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":"2005-1062","title":"Reconnaissance gas measurements on the East Rift Zone of Kilauea Volcano, Hawai'i by Fourier transform infrared spectroscopy","docAbstract":"We report the results of a set of measurements of volcanic gases on two small ground level plumes in the vicinity of Pu`u `O`o cone on the middle East Rift Zone (ERZ) of Kilauea volcano, Hawai`i on 15 June 2001 using open-path Fourier transform infrared (FTIR) spectroscopy. The work was carried out as a reconnaissance survey to assess the monitoring and research value of FTIR measurements at this volcano. Despite representing emissions of residual volatiles from lava that has undergone prior degassing, the plumes contained detectable amounts of CO2, CO, SO2, HCl, HF and SiF4. Various processes, including subsurface cooling, condensation of water in the atmospheric plume, oxidation, dissolution in water, and reactions with wall rocks at plume vents affect the abundance of these gases. Low concentrations of volcanic CO2 measured against a high ambient background are not well constrained by FTIR spectroscopy. Although there appear to be some differences between these gases and Pu`u `O`o source gases, ratios of HCl/SO2, HF/SO2 and CO/SO2 determined by FTIR measurements of these two small plumes compare reasonably well with earlier published analyses of ERZ vent samples. The measurements yielded emission rate estimates of 4, 11 and 4 t d-1","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051062","usgsCitation":"McGee, K.A., Elias, T., Sutton, A.J., Doukas, M.P., Zemek, P.G., and Gerlach, T.M., 2005, Reconnaissance gas measurements on the East Rift Zone of Kilauea Volcano, Hawai'i by Fourier transform infrared spectroscopy (Version 1.0): U.S. Geological Survey Open-File Report 2005-1062, 28 p., https://doi.org/10.3133/ofr20051062.","productDescription":"28 p.","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":186326,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6526,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1062/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Hawaii","otherGeospatial":"Kılauea volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -155.3144073486328,\n              19.276146935787732\n            ],\n            [\n              -155.1605987548828,\n              19.276146935787732\n            ],\n            [\n              -155.1605987548828,\n              19.47241867420536\n            ],\n            [\n              -155.3144073486328,\n              19.47241867420536\n            ],\n            [\n              -155.3144073486328,\n              19.276146935787732\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a73e4b07f02db643f0e","contributors":{"authors":[{"text":"McGee, Kenneth A. kenmcgee@usgs.gov","contributorId":2135,"corporation":false,"usgs":true,"family":"McGee","given":"Kenneth","email":"kenmcgee@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":282290,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elias, Tamar 0000-0002-9592-4518 telias@usgs.gov","orcid":"https://orcid.org/0000-0002-9592-4518","contributorId":3916,"corporation":false,"usgs":true,"family":"Elias","given":"Tamar","email":"telias@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":282292,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sutton, A. 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,{"id":70369,"text":"ofr20051137 - 2005 - Role of rock/fluid characteristics in carbon (CO<sub>2</sub>) storage and modeling","interactions":[],"lastModifiedDate":"2012-02-02T00:13:46","indexId":"ofr20051137","displayToPublicDate":"2005-04-06T00:00:00","publicationYear":"2005","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":"2005-1137","title":"Role of rock/fluid characteristics in carbon (CO<sub>2</sub>) storage and modeling","docAbstract":"The presentation ? Role of Rock/Fluid Characteristics in Carbon (CO2) Storage and Modeling ? was prepared for the meeting of the Environmental Protection Agency (EPA) in Houston, Tex., on April 6?7, 2005. It provides an overview of greenhouse gases, particularly CO2, and a summary of their effects on the Earth?s atmosphere. It presents methods of mitigating the effects of greenhouse gases, and the role of rock and fluid properties on CO2 storage mechanisms. It also lists factors that must be considered to adequately model CO2 storage.","language":"ENGLISH","doi":"10.3133/ofr20051137","usgsCitation":"Verma, M., 2005, Role of rock/fluid characteristics in carbon (CO<sub>2</sub>) storage and modeling (Version 1.0): U.S. Geological Survey Open-File Report 2005-1137, 27 p., https://doi.org/10.3133/ofr20051137.","productDescription":"27 p.","costCenters":[],"links":[{"id":6531,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1137/","linkFileType":{"id":5,"text":"html"}},{"id":186247,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fe22a","contributors":{"authors":[{"text":"Verma, Mahendra K. mverma@usgs.gov","contributorId":1027,"corporation":false,"usgs":true,"family":"Verma","given":"Mahendra K.","email":"mverma@usgs.gov","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":282305,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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