{"pageNumber":"950","pageRowStart":"23725","pageSize":"25","recordCount":46734,"records":[{"id":72370,"text":"sim2893 - 2005 - Data related to late Quaternary surface faulting on the Eastgate fault, Churchill County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:14:01","indexId":"sim2893","displayToPublicDate":"2005-09-29T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2893","title":"Data related to late Quaternary surface faulting on the Eastgate fault, Churchill County, Nevada","language":"ENGLISH","doi":"10.3133/sim2893","usgsCitation":"Crone, A.J., Kyung, J., Machette, M., Lidke, D.J., Okumura, K., and Mahan, S., 2005, Data related to late Quaternary surface faulting on the Eastgate fault, Churchill County, Nevada (Version 1.0): U.S. Geological Survey Scientific Investigations Map 2893, Pamphlet, 12 p.; Map, 1 sheet : 52 x 36 in., https://doi.org/10.3133/sim2893.","productDescription":"Pamphlet, 12 p.; Map, 1 sheet : 52 x 36 in.","costCenters":[],"links":[{"id":110581,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73905.htm","linkFileType":{"id":5,"text":"html"},"description":"73905"},{"id":193103,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7332,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/2005/2893/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b569","contributors":{"authors":[{"text":"Crone, Anthony J. 0000-0002-3006-406X crone@usgs.gov","orcid":"https://orcid.org/0000-0002-3006-406X","contributorId":790,"corporation":false,"usgs":true,"family":"Crone","given":"Anthony","email":"crone@usgs.gov","middleInitial":"J.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":285501,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kyung, Jai-Bok","contributorId":88224,"corporation":false,"usgs":true,"family":"Kyung","given":"Jai-Bok","email":"","affiliations":[],"preferred":false,"id":285506,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Machette, Michael N.","contributorId":28963,"corporation":false,"usgs":true,"family":"Machette","given":"Michael N.","affiliations":[],"preferred":false,"id":285504,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lidke, David J. 0000-0003-4668-1617 dlidke@usgs.gov","orcid":"https://orcid.org/0000-0003-4668-1617","contributorId":1211,"corporation":false,"usgs":true,"family":"Lidke","given":"David","email":"dlidke@usgs.gov","middleInitial":"J.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":285502,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Okumura, Koji","contributorId":39457,"corporation":false,"usgs":true,"family":"Okumura","given":"Koji","email":"","affiliations":[],"preferred":false,"id":285505,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mahan, Shannon 0000-0001-5214-7774 smahan@usgs.gov","orcid":"https://orcid.org/0000-0001-5214-7774","contributorId":1215,"corporation":false,"usgs":true,"family":"Mahan","given":"Shannon","email":"smahan@usgs.gov","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":false,"id":285503,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70203528,"text":"70203528 - 2005 - Historical subsidence and wetland loss in the Mississippi delta plain","interactions":[],"lastModifiedDate":"2019-05-28T10:53:49","indexId":"70203528","displayToPublicDate":"2005-09-27T10:43:33","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Historical subsidence and wetland loss in the Mississippi delta plain","docAbstract":"<p>Five representative areas of the Mississippi River delta plain were investigated using remote images, marsh elevations, water depths, sediment cores, and radiocarbon dates to estimate the timing, magnitudes, and relative rates of marsh erosion and land subsidence at geological and historical time scales. In the Terrebonne-Lafourche region of rapid interior-wetland loss, former marshes are now submerged beneath water that averages 0.5 to 1.0 m deep. Most of the permanent historical flooding was caused by rapid subsidence and collapse of the delta plain that occurred during the late 1960s and 1970s. Subsequent erosion of the submerged delta-plain marsh was relatively minor at most of the coring sites.<br></p><p>Widespread nearly simultaneous collapse of marshes across the Mississippi delta plain appears to be unprecedented and not repeated in the geological record of the past 1,000 years. Surface and subsurface data strongly indicate that the rapid subsidence and associated wetland loss were largely induced by extraction of hydrocarbons and associated formation water. Average historical rates of subsidence between 1965 and 1993 were about 8 to 12 mm/yr, whereas average geological rates of subsidence for the past 5,000 years were about 1 to 5 mm/yr. Natural processes such as deep-seated salt migration and fault movement cannot be discounted entirely, but there is no compelling evidence that these processes were responsible for the observed historical changes. Results of this study provide a basis for determining the relative importance of subsidence and shoreline erosion as causes of past wetland loss and for predicting sites and probable mechanisms of future wetland loss. This information should improve the selection of project sites and designs for wetland-loss mitigation and coastal restoration in south Louisiana.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Gulf Coast Association of Geological Societies Transactions","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Gulf Coast Association of Geological Societies 55th Annual Convention","conferenceDate":"September 25-27, 2005","conferenceLocation":"New Orleans, Louisiana","language":"English","publisher":"Gulf Coast Association of Geological Societies","usgsCitation":"Morton, R., Bernier, J., Barras, J.A., and Ferina, N.F., 2005, Historical subsidence and wetland loss in the Mississippi delta plain, <i>in</i> Gulf Coast Association of Geological Societies Transactions, v. 55, New Orleans, Louisiana, September 25-27, 2005, p. 555-571.","productDescription":"17 p.; CD-ROM","startPage":"555","endPage":"571","costCenters":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":364008,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":364007,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://store.beg.utexas.edu/gcags/1722-gcags055.html"}],"country":"United States","state":"Louisiana","otherGeospatial":"Mississippi delta","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.87890625,\n              28.9600886880068\n            ],\n            [\n              -90.02197265625,\n              28.9600886880068\n            ],\n            [\n              -90.02197265625,\n              29.7453016622136\n            ],\n            [\n              -90.87890625,\n              29.7453016622136\n            ],\n            [\n              -90.87890625,\n              28.9600886880068\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"55","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Morton, Robert A.","contributorId":88333,"corporation":false,"usgs":true,"family":"Morton","given":"Robert A.","affiliations":[],"preferred":false,"id":763017,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bernier, Julie 0000-0002-9918-5353 jbernier@usgs.gov","orcid":"https://orcid.org/0000-0002-9918-5353","contributorId":3549,"corporation":false,"usgs":true,"family":"Bernier","given":"Julie","email":"jbernier@usgs.gov","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":763018,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barras, John A. jbarras@usgs.gov","contributorId":149332,"corporation":false,"usgs":true,"family":"Barras","given":"John","email":"jbarras@usgs.gov","middleInitial":"A.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":763019,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ferina, Nicholas F.","contributorId":14047,"corporation":false,"usgs":true,"family":"Ferina","given":"Nicholas","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":763020,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":72364,"text":"fs20053079 - 2005 - Water use for irrigation in Michigan, 2001","interactions":[],"lastModifiedDate":"2017-01-20T11:06:21","indexId":"fs20053079","displayToPublicDate":"2005-09-27T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-3079","title":"Water use for irrigation in Michigan, 2001","docAbstract":"<p>Each year, water-use data for Michigan are compiled or estimated by the Michigan Department of Environmental Quality (MDEQ), working in cooperation with the U. S. Geological Survey (USGS). The resulting information provides a category-by-category profile of over 4,200 facilities throughout the State. The data are reported in the Michigan Water Use Reporting Program, which provides needed information for water-resources planning and enhances public understanding of the value of sustaining water resources within the Great Lakes Basin. The primary goal of the program is to inventory, analyze, and report baseline data for major water uses. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20053079","collaboration":"Prepared in cooperation with the Michigan Department of Environmental Quality","usgsCitation":"Morenz, M.L., Van Til, R.L., and Luukkonen, C.L., 2005, Water use for irrigation in Michigan, 2001: U.S. Geological Survey Fact Sheet 2005-3079, 4 p., https://doi.org/10.3133/fs20053079.","productDescription":"4 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":122460,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3079.jpg"},{"id":7327,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3079/","linkFileType":{"id":5,"text":"html"}}],"country":"United 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 \"}}]}\n","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0030","contributors":{"authors":[{"text":"Morenz, Michele L.","contributorId":44244,"corporation":false,"usgs":true,"family":"Morenz","given":"Michele","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":285494,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Til, Ron L.","contributorId":42307,"corporation":false,"usgs":true,"family":"Van Til","given":"Ron","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":285493,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Luukkonen, Carol L. clluukko@usgs.gov","contributorId":3489,"corporation":false,"usgs":true,"family":"Luukkonen","given":"Carol","email":"clluukko@usgs.gov","middleInitial":"L.","affiliations":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285492,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72365,"text":"fs20053071 - 2005 - Nevada water resources data","interactions":[],"lastModifiedDate":"2012-02-02T00:14:01","indexId":"fs20053071","displayToPublicDate":"2005-09-27T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-3071","title":"Nevada water resources data","language":"ENGLISH","doi":"10.3133/fs20053071","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2005, Nevada water resources data: U.S. Geological Survey Fact Sheet 2005-3071, 2 p., https://doi.org/10.3133/fs20053071.","productDescription":"2 p.","costCenters":[],"links":[{"id":7328,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3071/","linkFileType":{"id":5,"text":"html"}},{"id":120836,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3071.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6979d5","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534741,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72362,"text":"sir20055170 - 2005 - Hydrology and simulation of ground-water flow in Cedar Valley, Iron County, Utah","interactions":[],"lastModifiedDate":"2019-12-30T13:58:41","indexId":"sir20055170","displayToPublicDate":"2005-09-27T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5170","title":"Hydrology and simulation of ground-water flow in Cedar Valley, Iron County, Utah","docAbstract":"<p>Cedar Valley, located in the eastern part of Iron County in southwestern Utah, is experiencing rapid population growth. Cedar Valley traditionally has supported agriculture, but the growing population needs a larger share of the available water resources. Water withdrawn from the unconsolidated basin fill is the primary source for public supply and is a major source of water for irrigation. Water managers are concerned about increasing demands on the water supply and need hydrologic information to manage this limited water resource and minimize flow of water unsuitable for domestic use toward present and future public-supply sources.</p><p>Surface water in the study area is derived primarily from snowmelt at higher altitudes east of the study area or from occasional large thunderstorms during the summer. Coal Creek, a perennial stream with an average annual discharge of 24,200 acre-feet per year, is the largest stream in Cedar Valley. Typically, all of the water in Coal Creek is diverted for irrigation during the summer months. All surface water is consumed within the basin by irrigated crops, evapotranspiration, or recharge to the ground-water system.</p><p>Ground water in Cedar Valley generally moves from primary recharge areas along the eastern margin of the basin where Coal Creek enters, to areas of discharge or subsurface outflow. Recharge to the unconsolidated basin-fill aquifer is by seepage of unconsumed irrigation water, streams, direct precipitation on the unconsolidated basin fill, and subsurface inflow from consolidated rock and Parowan Valley and is estimated to be about 42,000 acre-feet per year. Stable-isotope data indicate that recharge is primarily from winter precipitation. The chloride mass-balance method indicates that recharge may be less than 42,000 acre-feet per year, but is considered a rough approximation because of limited chloride concentration data for precipitation and Coal Creek. Continued declining water levels indicate that recharge is not sufficient to meet demand. Water levels in many areas are at or close to historic lows.</p><p>In 2000, withdrawal from wells was estimated to be 36,000 acre-feet per year. About 4,000 acre-feet per year are estimated to discharge to evapotranspiration or as subsurface outflow. Prior to large-scale ground-water development, ground-water discharge by evapotranspiration and discharge to springs was much larger.</p><p>Ground water along the eastern margin of the valley between Cedar City and Enoch is unsuitable for domestic use because of high dissolved-solids and nitrate concentrations. The predominant ions of Ca and SO4 in this area indicate dissolution of gypsum in the Markagunt Plateau to the east. Data collected during this study were compared to historic data; there is no evidence to indicate deterioration in ground-water quality. The spatial distribution of ground water with high nitrate concentration does not appear to be migrating beyond its previously known extent. <br>No single source can be identified as the cause for elevated nitrate concentrations in ground water. Low nitrogen-15 values north of Cedar City indicate a natural geologic source. Higher nitrogen-15 values toward the center of the basin and associated hydrologic data indicate probable recharge from waste-water effluent. Excess dissolved nitrogen gas and low nitrate concentrations in shallow ground water indicate that denitrification is occurring in some areas.</p><p>A computer ground-water flow model was developed to simulate flow in the unconsolidated basin fill. The method of determining recharge from irrigation was changed during the calibration process to incorporate more areal and temporal variability. In general, the model accurately simulates water levels and water-level fluctuations and can be considered an adequate tool to help determine the valley-wide effects on water levels of additional ground-water withdrawals and changes in water use. The model was used to simulated water-level changes caused by projecting current withdrawal rates, increased withdrawal rates, and a 10-year drought. Water levels declined 20 to 275 feet in the southern and central parts of the valley and less than 20 feet north of Enoch</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/sir20055170","collaboration":"Prepared in cooperation with the Central Iron County Water Conservancy District; Utah Department of Natural Resources, Division of Water Resources; Utah Department of Environmental Quality, Division of Water Quality; Cedar City, and City of Enoch","usgsCitation":"Brooks, L.E., and Mason, J.L., 2005, Hydrology and simulation of ground-water flow in Cedar Valley, Iron County, Utah (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5170, x, 114 p., https://doi.org/10.3133/sir20055170.","productDescription":"x, 114 p.","numberOfPages":"127","onlineOnly":"Y","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":193036,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7325,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5170/","linkFileType":{"id":5,"text":"html"}},{"id":334242,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5170/PDF/SIR2005_5170.pdf"}],"country":"United States","state":"Utah","county":"Iron County","otherGeospatial":"Cedar Valley","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-112.4806,38.1474],[-112.4806,38.1379],[-112.4805,38.1293],[-112.481,38.1148],[-112.481,38.1098],[-112.4808,38.0862],[-112.4813,38.0658],[-112.4818,38.0572],[-112.4817,38.0418],[-112.4822,38.0273],[-112.4825,37.9847],[-112.483,37.9788],[-112.4696,37.9789],[-112.4707,37.9635],[-112.4706,37.9462],[-112.4711,37.9349],[-112.4715,37.9059],[-112.489,37.9063],[-112.4895,37.8913],[-112.5075,37.8912],[-112.5245,37.8912],[-112.5256,37.8912],[-112.5623,37.8905],[-112.5909,37.8909],[-112.5909,37.8832],[-112.5815,37.8832],[-112.5812,37.8383],[-112.5815,37.8057],[-112.5949,37.8065],[-112.6275,37.8082],[-112.6491,37.8085],[-112.6567,37.8076],[-112.6928,37.8065],[-112.6931,37.7752],[-112.6934,37.7525],[-112.6931,37.7185],[-112.6902,37.7186],[-112.6877,37.574],[-112.6874,37.545],[-112.7641,37.5445],[-112.7948,37.5448],[-112.8331,37.5449],[-112.8534,37.5448],[-112.9051,37.5449],[-112.9047,37.5154],[-112.9046,37.5005],[-112.9452,37.5006],[-113.0415,37.5007],[-113.0411,37.4744],[-113.0817,37.4745],[-113.1496,37.4748],[-113.1497,37.4803],[-113.2024,37.4807],[-113.2123,37.4806],[-113.2175,37.4805],[-113.2605,37.481],[-113.2601,37.4946],[-113.2604,37.5114],[-113.2601,37.5313],[-113.2775,37.5311],[-113.2955,37.5314],[-113.3153,37.5307],[-113.4772,37.5302],[-113.4779,37.5946],[-113.4784,37.6182],[-113.5144,37.6186],[-113.5324,37.6189],[-113.5353,37.6188],[-113.5539,37.619],[-113.5917,37.619],[-113.592,37.6059],[-113.61,37.6061],[-113.7204,37.6068],[-113.7402,37.6065],[-113.7564,37.6068],[-113.7599,37.6067],[-113.7936,37.6067],[-113.8128,37.6073],[-113.8686,37.6074],[-113.8872,37.6071],[-113.904,37.6068],[-113.9232,37.607],[-114.0539,37.6075],[-114.0541,37.6431],[-114.0541,37.6447],[-114.0539,37.666],[-114.0536,37.7109],[-114.0535,37.7259],[-114.0531,37.7887],[-114.0531,37.7903],[-114.0524,37.9039],[-114.0524,37.9059],[-114.0494,38.0308],[-114.0494,38.0329],[-114.0493,38.1503],[-114.0445,38.1499],[-114.0246,38.1502],[-114.0077,38.1505],[-113.9889,38.1504],[-113.955,38.1505],[-113.9368,38.1503],[-113.9333,38.1508],[-113.9164,38.1506],[-113.8988,38.1509],[-113.8807,38.1507],[-113.8438,38.1508],[-113.8239,38.1507],[-113.8069,38.1505],[-113.787,38.1508],[-113.7688,38.1506],[-113.7343,38.1506],[-113.7144,38.1504],[-113.6957,38.1507],[-113.6781,38.1509],[-113.6594,38.1507],[-113.643,38.151],[-113.6225,38.1508],[-113.605,38.151],[-113.5862,38.1508],[-113.5657,38.1506],[-113.5546,38.1508],[-113.547,38.1504],[-113.5142,38.1508],[-113.4961,38.1506],[-113.4926,38.1506],[-113.4738,38.1504],[-113.4545,38.1506],[-113.4364,38.1504],[-113.4042,38.1498],[-113.3814,38.1501],[-113.3638,38.1498],[-113.3474,38.1496],[-113.3351,38.1497],[-113.3111,38.1495],[-113.2924,38.1488],[-113.2736,38.149],[-113.2034,38.1493],[-113.1999,38.1493],[-113.1812,38.149],[-113.163,38.1488],[-113.1449,38.1485],[-113.1267,38.1491],[-113.108,38.1488],[-113.0717,38.1482],[-113.0536,38.1484],[-113.0325,38.1481],[-113.012,38.1483],[-112.9939,38.1484],[-112.9605,38.1482],[-112.9418,38.1484],[-112.9383,38.1484],[-112.9202,38.1485],[-112.9014,38.1487],[-112.8833,38.1484],[-112.8499,38.1491],[-112.8318,38.1487],[-112.8277,38.1488],[-112.8101,38.1489],[-112.7902,38.149],[-112.7715,38.1487],[-112.7381,38.1489],[-112.7194,38.1481],[-112.7165,38.1485],[-112.6989,38.1482],[-112.6773,38.1483],[-112.6585,38.1484],[-112.6275,38.1486],[-112.6094,38.1491],[-112.6035,38.1492],[-112.5854,38.1488],[-112.5673,38.1489],[-112.5485,38.1485],[-112.5356,38.1486],[-112.5304,38.1481],[-112.5134,38.1478],[-112.4806,38.1474]]]},\"properties\":{\"name\":\"Iron\",\"state\":\"UT\"}}]}","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e865","contributors":{"authors":[{"text":"Brooks, Lynette E. 0000-0002-9074-0939 lebrooks@usgs.gov","orcid":"https://orcid.org/0000-0002-9074-0939","contributorId":2718,"corporation":false,"usgs":true,"family":"Brooks","given":"Lynette","email":"lebrooks@usgs.gov","middleInitial":"E.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285487,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mason, James L.","contributorId":14397,"corporation":false,"usgs":true,"family":"Mason","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":285488,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72319,"text":"sir20055155 - 2005 - Field tests of nylon-screen diffusion samplers and pushpoint samplers for detection of metals in sediment pore water, Ashland and Clinton, Massachusetts, 2003","interactions":[],"lastModifiedDate":"2012-02-02T00:13:55","indexId":"sir20055155","displayToPublicDate":"2005-09-22T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5155","title":"Field tests of nylon-screen diffusion samplers and pushpoint samplers for detection of metals in sediment pore water, Ashland and Clinton, Massachusetts, 2003","docAbstract":"Efficient and economical screening methods are needed to detect and to determine the approximate concentrations of potentially toxic trace-element metals in shallow groundwater- discharge areas (pore water) where the metals may pose threats to aquatic organisms; such areas are likely to be near hazardous-waste sites. Pushpoint and nylon-screen diffusion samplers are two complementary options for use in such environments.\r\n\r\nThe pushpoint sampler, a simple well point, is easy to insert manually and to use. Only 1 day is required to collect samples. The nylon-screen diffusion sampler is well suited for use in sediments that do not allow a pump to draw water into a pushpoint sampler. In this study, both types of devices were used in sediments suitable for the use of the pushpoint sampler. Sampling with the nylon-screen diffusion sampler requires at least two site visits: one to deploy the samplers in the sediment, and a second to retrieve the samplers and collect the samples after a predetermined equilibration period.\r\n\r\nExtensive laboratory quality-control studies, field testing, and laboratory analysis of samples collected at the Nyanza Chemical Waste Dump Superfund site along the Sudbury River in Ashland, Massachusetts, and at a Superfund site-assessment location on Rigby Brook in Clinton, Massachusetts, indicate that these two devices yield comparable results for most metals and should be effective tools for pore-water studies. The nylon-screen diffusion samplers equilibrated within 1-2 days in homogeneous, controlled conditions in the laboratory. Nylon-screen diffusion samplers that were not purged of dissolved oxygen prior to deployment yielded results similar to those that were purged. Further testing of the nylon-screen diffusion samplers in homogeneous media would help to resolve any ambiguities about the data variability from the field studies.\r\n\r\nComparison of data from replicate samples taken in both study areas shows that even samples taken from sites within a half-meter radius of one another have distinct differences in pore-water trace-element concentrations. Sequential replicate samples collected with the pushpoint sampler yield consistent results; moving the pushpoint sampler even 5 to 10 centimeters, however, generally produces a second set of data that differs enough from the first set of data to indicate a heterogeneous environment. High concentration biases for barium and zinc in laboratory and field samples collected with nylon-screen diffusion samplers, however, may make their use inappropriate for studies of these metals.\r\n\r\nAnalyzing samples with high iron concentrations required sample dilution by factors of 2 or 10. Because these dilutions caused increases in the reporting levels by the same proportion, a substantial fraction of the data was censored. The results from undiluted samples, however, indicate that both devices should be useful for sampling ground water with metal concentrations close to reporting limits.","language":"ENGLISH","doi":"10.3133/sir20055155","usgsCitation":"Zimmerman, M.J., Vroblesky, D.A., Campo, K.W., Massey, A.J., and Scheible, W., 2005, Field tests of nylon-screen diffusion samplers and pushpoint samplers for detection of metals in sediment pore water, Ashland and Clinton, Massachusetts, 2003: U.S. Geological Survey Scientific Investigations Report 2005-5155, 51 p., https://doi.org/10.3133/sir20055155.","productDescription":"51 p.","costCenters":[],"links":[{"id":191775,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7273,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5155/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f434b","contributors":{"authors":[{"text":"Zimmerman, Marc J. mzimmerm@usgs.gov","contributorId":3245,"corporation":false,"usgs":true,"family":"Zimmerman","given":"Marc","email":"mzimmerm@usgs.gov","middleInitial":"J.","affiliations":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285420,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vroblesky, Don A. vroblesk@usgs.gov","contributorId":413,"corporation":false,"usgs":true,"family":"Vroblesky","given":"Don","email":"vroblesk@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":285418,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Campo, Kimberly W. kcampo@usgs.gov","contributorId":4690,"corporation":false,"usgs":true,"family":"Campo","given":"Kimberly","email":"kcampo@usgs.gov","middleInitial":"W.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285421,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Massey, Andrew J. 0000-0003-3995-8657 ajmassey@usgs.gov","orcid":"https://orcid.org/0000-0003-3995-8657","contributorId":1862,"corporation":false,"usgs":true,"family":"Massey","given":"Andrew","email":"ajmassey@usgs.gov","middleInitial":"J.","affiliations":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285419,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Scheible, Walter","contributorId":88042,"corporation":false,"usgs":true,"family":"Scheible","given":"Walter","email":"","affiliations":[],"preferred":false,"id":285422,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":72318,"text":"sir20055086 - 2005 - Geochemical assessment of metals and dioxin in sediment from the San Carlos Reservoir and the Gila, San Carlos, and San Francisco Rivers, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:13:58","indexId":"sir20055086","displayToPublicDate":"2005-09-22T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5086","title":"Geochemical assessment of metals and dioxin in sediment from the San Carlos Reservoir and the Gila, San Carlos, and San Francisco Rivers, Arizona","docAbstract":"In October 2004, we sampled stream-bed sediment, terrace sediment, and sediment from the San Carlos Reservoir to determine the spatial and chronological variation of six potentially toxic metals-Cu, Pb, Zn, Cd, As, and Hg. Water levels in the San Carlos Reservoir were at a 20-year low at an elevation of 2,409 ft (734.3 m). Four cores were taken from the reservoir: one from the San Carlos River arm, one from the Gila River arm, and two from the San Carlos Reservoir just west of the Pinal County line. Radioisotope chronometry (7Be, 137Cs, and 210Pb) conducted on sediment from the reservoir cores provides a good chronological record back to 1959. Chronology prior to that, during the 1950s, is based on our interpretation of the 137Cs anomaly in reservoir cores. During and prior to the 1950s, the reservoir was dry and sediment-accumulation rates were irregular; age control based on radioisotope data was not possible. We recovered sediment at the base of one 4-m-long core that may date back to the late 1930s. The sedimentological record contains two discrete events, one about 1978-83 and one about 1957, where the Cu concentration in reservoir sediment exceeded recommended sediment quality guidelines and should have had an effect on sensitive aquatic and benthic organisms. Concentrations of Zn determined in sediment deposited during the 1957(?) event also exceeded recommended sediment quality guidelines. Concentration data for Cu from the four cores clearly indicate that the source of this material was upstream on the Gila River.\r\n\r\nLead isotope data, coupled with the geochemical data from a 2M HCl-1 percent H2O2 leach of selected sediment samples, show two discrete populations of data. One represents the dominant sediment load derived from the Safford Valley, and a second reflects sediment derived from the San Francisco River. The Cu concentration spikes in the reservoir cores have chemical and Pb isotope signatures that indicate that deposits in a porphyry copper deposit from the Morenci district is the likely source of these Cu-rich sedimentary deposits. Copper concentrations and Pb isotope data in premining terrace-sediment deposits indicate that the Cu peaks could not have resulted from erosion of premining sediment from terrace deposits downstream on the Gila River. The chemical and Pb isotope data also indicate that agricultural practices in the Safford Valley have resulted in an increased sediment load to the Gila River since large-scale farming began, prior to the time when the San Carlos Reservoir was built.\r\n\r\nAnalyses of dioxin, which is an impurity in one of the herbicides used in the late 1960s and early 1970s, were completed in sediment from one of the cores in the reservoir to determine whether any of these pesticide residues have accumulated in the reservoir sediment. Dioxin concentration is expressed in terms of its toxicity (toxic equivalent concentration or TEQ). Concentrations of dioxin in the sediment ranged from 0.68 to 1.37 pg/g and are less than any of the benchmark concentrations recommended as threshold values for adverse effects of dioxin in sediment (> 2.5-10 pg/g).","language":"ENGLISH","doi":"10.3133/sir20055086","usgsCitation":"Church, S.E., Choate, L.M., Marot, M.E., Fey, D.L., Adams, M., Briggs, P.H., and Brown, Z.A., 2005, Geochemical assessment of metals and dioxin in sediment from the San Carlos Reservoir and the Gila, San Carlos, and San Francisco Rivers, Arizona (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2005-5086, vi, 61 p., https://doi.org/10.3133/sir20055086.","productDescription":"vi, 61 p.","costCenters":[],"links":[{"id":191574,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7217,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5086/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae232","contributors":{"authors":[{"text":"Church, Stan E. schurch@usgs.gov","contributorId":803,"corporation":false,"usgs":true,"family":"Church","given":"Stan","email":"schurch@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":false,"id":285412,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Choate, LaDonna M. 0000-0002-0229-7210 lchoate@usgs.gov","orcid":"https://orcid.org/0000-0002-0229-7210","contributorId":1176,"corporation":false,"usgs":true,"family":"Choate","given":"LaDonna","email":"lchoate@usgs.gov","middleInitial":"M.","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":285413,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Marot, Marci E. 0000-0003-0504-315X mmarot@usgs.gov","orcid":"https://orcid.org/0000-0003-0504-315X","contributorId":2078,"corporation":false,"usgs":true,"family":"Marot","given":"Marci","email":"mmarot@usgs.gov","middleInitial":"E.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":285415,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"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":285411,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Adams, Monique madams@usgs.gov","contributorId":1231,"corporation":false,"usgs":true,"family":"Adams","given":"Monique","email":"madams@usgs.gov","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":285414,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Briggs, Paul H.","contributorId":30973,"corporation":false,"usgs":true,"family":"Briggs","given":"Paul","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":285416,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Brown, Zoe Ann","contributorId":95530,"corporation":false,"usgs":true,"family":"Brown","given":"Zoe","email":"","middleInitial":"Ann","affiliations":[],"preferred":false,"id":285417,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":72315,"text":"ds127 - 2005 - Water-quality and biologic data for the Blue River basin, Kansas City metropolitan area, Missouri and Kansas, October 2000 to October 2004","interactions":[],"lastModifiedDate":"2020-01-26T17:17:00","indexId":"ds127","displayToPublicDate":"2005-09-22T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"127","title":"Water-quality and biologic data for the Blue River basin, Kansas City metropolitan area, Missouri and Kansas, October 2000 to October 2004","docAbstract":"This report presents water-quality and biologic data collected in the Blue River Basin, metropolitan Kansas City, Missouri and Kansas, from October 2000 to October 2004. Data were collected in cooperation with the city of Kansas City, Missouri, Water Services Department as part of an ongoing study designed to characterize long-term water-quality trends in the basin and to provide data to support a strategy for combined sewer overflow control. These data include values of physical properties, fecal indicator bacteria densities, suspended sediment, and concentrations of major ions, nutrients, trace elements, organic wastewater compounds, and pharmaceutical compounds in base-flow and stormflow stream samples and bottom sediments. Six surface-water sites in the basin were sampled 13 times during base-flow conditions and during a minimum of 7 storms. Benthic macroinvertebrate communities are described at 10 sites in the basin and 1 site outside the basin. Water-column and bottom-sediment data from impounded reaches of Brush Creek are provided. Continuous specific conductance, pH, water-quality temperature, turbidity, and dissolved oxygen data are provided for two streams-the Blue River and Brush Creek. Sampling, analytical, and quality assurance methods used in data collection during the study also are described in the report.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds127","usgsCitation":"Wilkison, D.H., Armstrong, D., Brown, R., Poulton, B.C., Cahill, J.D., and Zaugg, S.D., 2005, Water-quality and biologic data for the Blue River basin, Kansas City metropolitan area, Missouri and Kansas, October 2000 to October 2004: U.S. Geological Survey Data Series 127, 166 p., https://doi.org/10.3133/ds127.","productDescription":"166 p.","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":191571,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7215,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/2005/127/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Kansas, Missouri","county":"Cass, Jackson, Johnson, Wyandotte","city":"Kansas City","otherGeospatial":"Kansas River, Missouri River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.6805191040039,\n              39.097828059155134\n            ],\n            [\n              -94.66781616210938,\n              39.09276546806873\n            ],\n            [\n              -94.6592330932617,\n              39.08663658203791\n            ],\n            [\n              -94.6527099609375,\n              39.07890809706475\n            ],\n            [\n              -94.64653015136719,\n              39.07277800696058\n            ],\n           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Center","active":true,"usgs":true}],"preferred":true,"id":285405,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Armstrong, Daniel J. armstron@usgs.gov","contributorId":3823,"corporation":false,"usgs":true,"family":"Armstrong","given":"Daniel J.","email":"armstron@usgs.gov","affiliations":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285404,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, Rebecca E.","contributorId":99233,"corporation":false,"usgs":true,"family":"Brown","given":"Rebecca E.","affiliations":[],"preferred":false,"id":285407,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Poulton, Barry C. 0000-0002-7219-4911 bpoulton@usgs.gov","orcid":"https://orcid.org/0000-0002-7219-4911","contributorId":2421,"corporation":false,"usgs":true,"family":"Poulton","given":"Barry","email":"bpoulton@usgs.gov","middleInitial":"C.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":285403,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cahill, Jeffrey D.","contributorId":22047,"corporation":false,"usgs":true,"family":"Cahill","given":"Jeffrey","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":285406,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Zaugg, Steven D. sdzaugg@usgs.gov","contributorId":768,"corporation":false,"usgs":true,"family":"Zaugg","given":"Steven","email":"sdzaugg@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":285402,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":72324,"text":"sir20055189 - 2005 - Effects of rain gardens on the quality of water in the Minneapolis-St. Paul metropolitan area of Minnesota, 2002-04","interactions":[],"lastModifiedDate":"2016-04-04T11:29:27","indexId":"sir20055189","displayToPublicDate":"2005-09-22T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5189","title":"Effects of rain gardens on the quality of water in the Minneapolis-St. Paul metropolitan area of Minnesota, 2002-04","docAbstract":"<p>Rain gardens are a popular method of managing runoff while attempting to provide aesthetic and environmental benefits. Five rain-garden sites in the Minneapolis &ndash; Saint Paul metropolitan area of Minnesota were instrumented to evaluate the effects of this water-management system on surface and subsurface water quality. Most of these sites were in suburban locations and frequently in newer developments. Because of this they were affected by changing hydrology during the course of this study.</p>\n<p>Less-than-normal precipitation during much of the study may have resulted in samples that may not be representative of normal conditions. However, the resulting data indicate that properly designed rain gardens enhance infiltration and can reduce concentrations of dissolved ions relative to background conditions.</p>\n<p>The runoff events in one rain garden and several runoff events in the other rain gardens produced no sampled overflow during this study because the gardens captured all of the inflow, which subsequently infiltrated beneath the land surface, evaporated, or transpired through garden vegetation. Where measured, overflow had reduced concentrations of suspended solids and most nutrient species associated with particulate material, as compared to inflow. Many of these materials settle to the bottom of the rain garden, and some nutrients may be assimilated by the plant community.</p>\n<p>Site design, including capacity relative to drainage area and soil permeability, is an important consideration in the efficiency of rain-garden operation. Vegetation type likely affects the infiltration capacity, nutrient uptake, and evapotranspiration of a rain garden and probably the resulting water quality. The long-term efficiency of rain gardens is difficult to determine from the results of this study because most are still evolving and maturing in relation to their hydrologic, biologic, and chemical setting. Many resource managers have questioned what long-term maintenance will be needed to keep rain gardens operating effectively. Additional or continued studies could address many of these concerns.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View, MN","doi":"10.3133/sir20055189","collaboration":"Prepared in cooperation with the Metropolitan Council of the Twin Cities","usgsCitation":"Tornes, L.H., 2005, Effects of rain gardens on the quality of water in the Minneapolis-St. Paul metropolitan area of Minnesota, 2002-04: U.S. Geological Survey Scientific Investigations Report 2005-5189, iv, 22 p., https://doi.org/10.3133/sir20055189.","productDescription":"iv, 22 p.","numberOfPages":"29","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":319760,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20055189.JPG"},{"id":7277,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5189/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Minnesota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94,\n              45.25\n            ],\n            [\n              -94,\n              44.5\n            ],\n            [\n              -92.75,\n              44.5\n            ],\n            [\n              -92.75,\n              45.25\n            ],\n            [\n              -94,\n              45.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6119bd","contributors":{"authors":[{"text":"Tornes, Lan H.","contributorId":70484,"corporation":false,"usgs":true,"family":"Tornes","given":"Lan","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":285431,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72307,"text":"wri034338 - 2005 - Use of discrete-zone monitoring systems for hydraulic characterization of a fractured-rock aquifer at the University of Connecticut Landfill, Storrs, Connecticut, 1999 to 2002","interactions":[],"lastModifiedDate":"2019-10-17T07:18:45","indexId":"wri034338","displayToPublicDate":"2005-09-21T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2003-4338","title":"Use of discrete-zone monitoring systems for hydraulic characterization of a fractured-rock aquifer at the University of Connecticut Landfill, Storrs, Connecticut, 1999 to 2002","docAbstract":"<p>The U.S. Geological Survey, in cooperation with the University of Connecticut, used a suite of hydraulic methods to characterize the hydrogeology of a fractured-rock aquifer near the former landfill and chemical-waste disposal pits at the University of Connecticut, Storrs, Connecticut. Multiple methods were used to determine head, driving potential, and transmissivity, including manual open-hole water-level and discretezone water-level measurements from 11 boreholes; continuous discrete-zone water-level measurements from 6 of the boreholes; estimated head and transmissivity for 11 boreholes using heat-pulse flowmeter profiles and pumping records; and differential head testing using a straddle-packer apparatus from 4 boreholes. These data were analyzed to identify and characterize relations between long-term water-level patterns and precipitation, topographic setting, contaminant distribution at the site, and a conceptual ground-water flow model. </p><p>Data collected using the heat-pulse flowmeter, the straddle-packer apparatus, and discrete-zone monitoring (DZM) systems helped to establish, refine, and verify a conceptual model of ground-water flow in the study area. Monitoring of DZM systems installed in 11 boreholes provided a method for longterm monitoring of hydraulic head and water quality of the aquifer at fracture zones of different depths. These data were used to help define the conceptual site model for ground-water flow and to determine and explain the distribution of contamination. </p><p>Hydrographs constructed for discretely isolated zones in the boreholes showed the magnitude of seasonal changes of water levels and driving potential in response to precipitation and drought. Heads in discrete zones and in different boreholes varied both in magnitude of response and in timing of response to precipitation. Water levels in open boreholes and in DZM systems showed a semi-diurnal pattern that coincides with gravimetric tidal plots generated for this area. No fluctuations that might indicate pumping were identified in the continuous water-level records. Lack of hydraulic response between boreholes during cross-hole testing in the area of the former chemical-waste disposal pits indicates poor hydraulic connection between the boreholes that were tested. In general, data indicated the presence of downward driving potentials in the recharge areas and in the area of the ground-water divide, and upward driving potentials in discharge areas north and south of the landfill. </p><p>The results of this study illustrate the importance of discrete-zone isolation and monitoring in fractured-rock aquifers to prevent cross contamination while permitting head measurements and water-quality sampling that can be used to identify and characterize contamination or pathways for contaminant migration in a fractured-rock aquifer. Without DZM systems installed in the boreholes, only open-hole heads can be measured. The open-hole heads may be misleading when determining potential flow directions at contamination sites, because they are a composite of the heads associated with each of the fractures intersecting the borehole. The flowmeter tool and straddle-packer apparatus are effective screening tools for generating a snapshot of the hydraulic conditions, including vertical flow, transmissivity, and heads; however, they cannot prevent flow and potential cross-contamination and cannot easily be used to monitor long-term conditions. </p><p>This work was conducted as part of a larger multidisciplinary investigation to characterize the nature and extent of contamination in the soil, surface water, and ground water in the overburden and fractured bedrock in the area of the landfill and former chemical-waste disposal pits near the University of Connecticut. The methods and hydraulic data presented in this report were used along with surface- and borehole-geophysical data and geochemical data to understand and characterize the ground-water flow in overburden and fractured bedrock; to assess possible chemical migration; to develop a site conceptual ground-water flow model; and to assess remediation alternatives.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri034338","usgsCitation":"Johnson, C.D., Kochiss, C.S., and Dawson, C.B., 2005, Use of discrete-zone monitoring systems for hydraulic characterization of a fractured-rock aquifer at the University of Connecticut Landfill, Storrs, Connecticut, 1999 to 2002: U.S. Geological Survey Water-Resources Investigations Report 2003-4338, vi, 105 p., https://doi.org/10.3133/wri034338.","productDescription":"vi, 105 p.","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"links":[{"id":191518,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2003/4338/report-thumb.jpg"},{"id":101653,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2003/4338/report.pdf","size":"18580","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Connecticut","city":"Storrs","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72.27075934410095,\n              41.807708943063126\n            ],\n            [\n              -72.26415038108826,\n              41.807708943063126\n            ],\n            [\n              -72.26415038108826,\n              41.811227582554736\n            ],\n            [\n              -72.27075934410095,\n              41.811227582554736\n            ],\n            [\n              -72.27075934410095,\n              41.807708943063126\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604685","contributors":{"authors":[{"text":"Johnson, Carole D. 0000-0001-6941-1578 cjohnson@usgs.gov","orcid":"https://orcid.org/0000-0001-6941-1578","contributorId":1891,"corporation":false,"usgs":true,"family":"Johnson","given":"Carole","email":"cjohnson@usgs.gov","middleInitial":"D.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":285396,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kochiss, Christopher S.","contributorId":76017,"corporation":false,"usgs":true,"family":"Kochiss","given":"Christopher","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":285398,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dawson, C. 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,{"id":72302,"text":"ofr20051322 - 2005 - Soils infiltration data for selected Wyoming watersheds, 1998-1999","interactions":[],"lastModifiedDate":"2012-02-02T00:13:55","indexId":"ofr20051322","displayToPublicDate":"2005-09-20T00:00:00","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":"2005-1322","title":"Soils infiltration data for selected Wyoming watersheds, 1998-1999","language":"ENGLISH","doi":"10.3133/ofr20051322","usgsCitation":"Miller, K., Elliott, J., and Friday, N., 2005, Soils infiltration data for selected Wyoming watersheds, 1998-1999: U.S. Geological Survey Open-File Report 2005-1322, 74 p., https://doi.org/10.3133/ofr20051322.","productDescription":"74 p.","costCenters":[],"links":[{"id":191872,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7212,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1322/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689bb4","contributors":{"authors":[{"text":"Miller, Kirk","contributorId":81891,"corporation":false,"usgs":true,"family":"Miller","given":"Kirk","affiliations":[],"preferred":false,"id":285387,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elliott, John","contributorId":87638,"corporation":false,"usgs":true,"family":"Elliott","given":"John","email":"","affiliations":[],"preferred":false,"id":285388,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Friday, Nolan","contributorId":9359,"corporation":false,"usgs":true,"family":"Friday","given":"Nolan","email":"","affiliations":[],"preferred":false,"id":285386,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72300,"text":"ds138 - 2005 - Nebraska, Kansas, and Oklahoma aeromagnetic and gravity maps and data: A web site for distribution of data","interactions":[],"lastModifiedDate":"2023-03-31T18:24:28.367778","indexId":"ds138","displayToPublicDate":"2005-09-20T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"138","title":"Nebraska, Kansas, and Oklahoma aeromagnetic and gravity maps and data: A web site for distribution of data","docAbstract":"The Nebraska, Kansas, and Oklahoma aeromagnetic grid is constructed from grids that combine information collected in 28 separate aeromagnetic surveys conducted between 1954 and 1985. The data from these surveys are of varying quality. The design and specifications (terrain clearance, sampling rates, line spacing, and reduction procedures) varied from survey to survey depending on the purpose of the project and the technology of that time. Every attempt was made to acquire the data in digital form. Most of the available digital data were obtained from aeromagnetic surveys flown by the U.S. Geological Survey (USGS), flown on contract with the USGS, or were obtained from other Federal agencies and State universities. The Kansas data were flown by and acquired from the Kansas Geological Survey. Some of the 1954, 1963, and 1964 data are available only on hand-contoured maps and had to be digitized. These maps were digitized along flight-line/contour-line intersections, which is considered to be the most accurate method of recovering the original data. 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,{"id":72301,"text":"ds135 - 2005 - Iowa magnetic and gravity maps and data: A web site for distribution of data","interactions":[],"lastModifiedDate":"2023-03-29T20:00:02.393865","indexId":"ds135","displayToPublicDate":"2005-09-20T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"135","title":"Iowa magnetic and gravity maps and data: A web site for distribution of data","docAbstract":"Magnetic anomalies are due to variations in the Earth's magnetic field caused by the uneven distribution of magnetic minerals (primarily magnetite) in the rocks that make up the upper part of the Earth's crust. The features and patterns of the magnetic anomalies can be used to delineate details of subsurface geology, including the locations of buried faults and magnetite-bearing rocks and the depth to the base of sedimentary basins. This information is valuable for mineral exploration, geologic mapping, and environmental studies.\r\n\r\nThe Iowa magnetic map is constructed from grids that combine information collected in nine separate magnetic surveys conducted between 1953 and 1972. The data from these surveys are of varying quality. The design and specifications (terrain clearance, sampling rates, line spacing, and reduction procedures) varied from survey to survey depending on the purpose of the project and the technology of that time. Every attempt was made to acquire the data in digital form. All survey grids have been continued to 305 m (1,000 ft) above ground and merged together to form the State compilation.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ds135","usgsCitation":"Kucks, R.P., and Hill, P.L., 2005, Iowa magnetic and gravity maps and data: A web site for distribution of data (Online only, Version 1.0): U.S. Geological Survey Data Series 135, HTML Document, https://doi.org/10.3133/ds135.","productDescription":"HTML Document","onlineOnly":"Y","costCenters":[],"links":[{"id":191871,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414910,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73901.htm","linkFileType":{"id":5,"text":"html"}},{"id":7211,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/2005/135/","linkFileType":{"id":5,"text":"html"}}],"country":"United 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,{"id":72297,"text":"ofr20051328 - 2005 - Seven aeromagnetic surveys in California and Nevada: A web site for distribution of data","interactions":[],"lastModifiedDate":"2024-02-29T17:57:49.481569","indexId":"ofr20051328","displayToPublicDate":"2005-09-20T00:00:00","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":"2005-1328","title":"Seven aeromagnetic surveys in California and Nevada: A web site for distribution of data","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051328","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2005, Seven aeromagnetic surveys in California and Nevada: A web site for distribution of data (Version 1.0): U.S. Geological Survey Open-File Report 2005-1328, HTML Document, https://doi.org/10.3133/ofr20051328.","productDescription":"HTML Document","onlineOnly":"Y","costCenters":[],"links":[{"id":425654,"rank":5,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/2005/1328/readme.txt","text":"Read Me","size":"8.00 KB","linkFileType":{"id":2,"text":"txt"}},{"id":425653,"rank":4,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2005/1328/ofr20051328.zip","size":"492 MB","linkFileType":{"id":6,"text":"zip"}},{"id":7207,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1328/","linkFileType":{"id":5,"text":"html"}},{"id":191827,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":415181,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73896.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California, Nevada","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -114.04596793699903,\n              39.594093152384346\n            ],\n            [\n              -122.76285164888907,\n              39.594093152384346\n            ],\n            [\n              -122.76285164888907,\n              33.118784802083525\n            ],\n            [\n              -114.04596793699903,\n              33.118784802083525\n            ],\n            [\n              -114.04596793699903,\n              39.594093152384346\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f5920","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534737,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72284,"text":"sir20055149 - 2005 - Questa baseline and pre-mining ground-water quality investigation. 12. Geochemical and reactive-transport modeling based on tracer injection-synoptic sampling studies for the Red River, New Mexico, 2001-2002","interactions":[],"lastModifiedDate":"2024-10-30T19:00:48.391857","indexId":"sir20055149","displayToPublicDate":"2005-09-19T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5149","title":"Questa baseline and pre-mining ground-water quality investigation. 12. Geochemical and reactive-transport modeling based on tracer injection-synoptic sampling studies for the Red River, New Mexico, 2001-2002","docAbstract":"<p>Reactive-transport processes in the Red River, downstream from the town of<span>&nbsp;</span>Red River<span>&nbsp;</span>in north-central New Mexico, were simulated using the OTEQ reactive-transport model. The simulations were calibrated using physical and chemical data from synoptic studies conducted during low-flow conditions in August 2001 and during March/April 2002. Discharge over the 20-km reach from the town of Red River to the USGS streamflow-gaging station near the town of Questa ranged from 395 to 1,180 L/s during the 2001 tracer and from 234 to 421 L/s during the 2002 tracer. The pH of the<span>&nbsp;</span>Red River<span>&nbsp;</span>ranged from 7.4 to 8.5 during the 2001 tracer and from 7.1 to 8.7 during the 2002 tracer, and seep and tributary samples had pH values of 2.8 to 9.0 during the 2001 tracer and 3.8 to 7.2 during the 2002 tracer.</p><p>Mass-loading calculations allowed identification of several specific locations where elevated concentrations of potential contaminants entered the<span>&nbsp;</span>Red River<span>&nbsp;</span>. These locations, characterized by features on the north side of the Red River that are known to be sources of low-pH water containing elevated metal and sulfate concentrations, are: the initial 2.4 km of the study reach, including Bitter Creek, the stream section from 6.2 to 7.8 km, encompassing La Bobita well and the Hansen debris fan, Sulphur Gulch, at about 10.5 km, the area near Portal Springs, from 12.2 to 12.6 km, and the largest contributors of mass loading, the 13.7 to 13.9 km stream section near Cabin Springs and the 14.7 to 17.5 km stream section from Shaft Spring to Thunder Bridge, Goathill Gulch, and Capulin Canyon.</p><p>Speciation and saturation index calculations indicated that although solubility limits the concentration of aluminum above pH 5.0, at pH values above 7 and aluminum concentrations below 0.3 mg/L inorganic speciation and mineral solubility controls no longer dominate and aluminum-organic complexing may occur.</p><p>The August 2001 reactive-transport simulations included dissolved iron(II) oxidation, constrained using measured concentrations of dissolved iron(II) and dissolved iron(total). Both simulations included precipitation of amorphous Al(OH)<sub>3</sub><span>&nbsp;</span>and hydrous ferric oxide as Fe(OH)<sub>3</sub>, and sorption of copper and zinc to the precipitated hydrous ferric oxide. Simulations revealed that hydrogen, iron, aluminum, copper, and zinc were non-conservative and that mineral precipitation can account for iron and aluminum concentrations. Copper and zinc concentrations can be accounted for by simulating their sorption to hydrous ferric oxide forming in the water column of the<span>&nbsp;</span>Red River<span>&nbsp;</span>, although hydrous manganese oxides also may be important sorption substrates.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055149","usgsCitation":"Ball, J.W., Runkel, R.L., and Nordstrom, D.K., 2005, Questa baseline and pre-mining ground-water quality investigation. 12. Geochemical and reactive-transport modeling based on tracer injection-synoptic sampling studies for the Red River, New Mexico, 2001-2002: U.S. Geological Survey Scientific Investigations Report 2005-5149, vii, 68 p., https://doi.org/10.3133/sir20055149.","productDescription":"vii, 68 p.","temporalStart":"2001-01-01","temporalEnd":"2002-12-31","costCenters":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":193252,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7153,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5149/","linkFileType":{"id":5,"text":"html"}},{"id":463441,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_86714.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New Mexico","otherGeospatial":"Red River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.55,36.63333333333333 ], [ -105.55,36.733333333333334 ], [ -105.4,36.733333333333334 ], [ -105.4,36.63333333333333 ], [ -105.55,36.63333333333333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685afe","contributors":{"authors":[{"text":"Ball, James W.","contributorId":38946,"corporation":false,"usgs":true,"family":"Ball","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":285352,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Runkel, Robert L. 0000-0003-3220-481X runkel@usgs.gov","orcid":"https://orcid.org/0000-0003-3220-481X","contributorId":685,"corporation":false,"usgs":true,"family":"Runkel","given":"Robert","email":"runkel@usgs.gov","middleInitial":"L.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285351,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nordstrom, D. Kirk 0000-0003-3283-5136 dkn@usgs.gov","orcid":"https://orcid.org/0000-0003-3283-5136","contributorId":749,"corporation":false,"usgs":true,"family":"Nordstrom","given":"D.","email":"dkn@usgs.gov","middleInitial":"Kirk","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":false,"id":285353,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72247,"text":"ofr20051090 - 2005 - Geomorphic Data Collected Within Nebraska Public Power District's Cottonwood Ranch Property, Platte River, Nebraska, Water Year 2004","interactions":[],"lastModifiedDate":"2012-02-02T00:13:58","indexId":"ofr20051090","displayToPublicDate":"2005-09-19T00:00:00","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":"2005-1090","title":"Geomorphic Data Collected Within Nebraska Public Power District's Cottonwood Ranch Property, Platte River, Nebraska, Water Year 2004","language":"ENGLISH","doi":"10.3133/ofr20051090","usgsCitation":"Kinzel, P.J., Parker, R.S., Nelson, J.M., Burman, A.R., and Heckman, A.K., 2005, Geomorphic Data Collected Within Nebraska Public Power District's Cottonwood Ranch Property, Platte River, Nebraska, Water Year 2004: U.S. Geological Survey Open-File Report 2005-1090, 23 p. text + additional files, https://doi.org/10.3133/ofr20051090.","productDescription":"23 p. text + additional files","costCenters":[],"links":[{"id":191524,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7099,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://wwwbrr.cr.usgs.gov/projects/SW_Env_Fluid/downloads.html","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c55f","contributors":{"authors":[{"text":"Kinzel, Paul J. 0000-0002-6076-9730 pjkinzel@usgs.gov","orcid":"https://orcid.org/0000-0002-6076-9730","contributorId":743,"corporation":false,"usgs":true,"family":"Kinzel","given":"Paul","email":"pjkinzel@usgs.gov","middleInitial":"J.","affiliations":[{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285244,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parker, Randolph S.","contributorId":58638,"corporation":false,"usgs":true,"family":"Parker","given":"Randolph","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":285246,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nelson, Jonathan M. 0000-0002-7632-8526 jmn@usgs.gov","orcid":"https://orcid.org/0000-0002-7632-8526","contributorId":2812,"corporation":false,"usgs":true,"family":"Nelson","given":"Jonathan","email":"jmn@usgs.gov","middleInitial":"M.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"preferred":true,"id":285245,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Burman, Aaron R.","contributorId":102960,"corporation":false,"usgs":true,"family":"Burman","given":"Aaron","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":285247,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Heckman, Ashley K.","contributorId":103748,"corporation":false,"usgs":true,"family":"Heckman","given":"Ashley","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":285248,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":72248,"text":"ofr20041316 - 2005 - Water-chemistry data for selected springs, geysers, and streams in Yellowstone National Park Wyoming, 2001-2002","interactions":[],"lastModifiedDate":"2020-02-03T20:18:36","indexId":"ofr20041316","displayToPublicDate":"2005-09-19T00:00:00","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":"2004-1316","title":"Water-chemistry data for selected springs, geysers, and streams in Yellowstone National Park Wyoming, 2001-2002","docAbstract":"<p>Water analyses are reported for one-hundred-twenty-one samples collected from hot springs and their overflow drainages, the Gibbon River, and one ambient-temperature acid stream in Yellowstone National Park (YNP) during 2001-2002. Twenty-five analyses are reported for samples collected during May 2001, fifty analyses are reported for samples collected during September 2001, eleven analyses are reported for samples collected during October 2001, and thirty-five analyses are reported for samples collected during June and July 2002. Water samples were collected and analyzed for major and trace constituents from nine areas of YNP including Norris Geyser Basin, Nymph Lake and Roadside Springs, Lower Geyser Basin, Washburn Springs, Calcite Springs, Crater Hills, Mammoth Hot Springs, West Thumb Geyser Basin, and Brimstone Basin. These water samples were collected and analyzed as part of research investigations in YNP on arsenic redox distribution in hot springs and overflow drainages, the occurrence and distribution of dissolved mercury, and sulfur redox speciation. Most samples were analyzed for major cations and anions, trace metals, and iron, arsenic, nitrogen, and sulfur redox species. Only mercury concentration, pH, and specific conductance were determined for samples collected in October 2001 as they were collected during a reconnaissance field trip. Analyses were performed at the sampling site, in an onsite mobile laboratory, or later in a U.S. Geological Survey laboratory, depending on stability of the constituent and whether it could be preserved effectively.</p><p>Water samples were filtered and preserved onsite. Water temperature, specific conductance, pH, Eh, and dissolved hydrogen sulfide were measured onsite at the time of sampling. Alkalinity and acidity were determined by titration, usually within a few days of sample collection. Concentrations of thiosulfate (S<sub>2</sub>O<sub>3</sub>) and polythionate (S<sub>n</sub>O<sub>6</sub>) were determined as soon as possible (generally minutes to hours after sample collection) by ion chromatography in an onsite mobile laboratory vehicle. Total dissolved iron and ferrous iron concentrations often were measured onsite in the mobile laboratory.</p><p>Concentrations of aluminum, arsenic, barium, beryllium, boron, cadmium, calcium, chromium, cobalt, copper, iron, lead, lithium, magnesium, manganese, molybdenum, nickel, potassium, selenium, silica, sodium, strontium, vanadium, and zinc were determined by inductively coupled plasma-optical emission spectrometry. Trace concentrations of antimony, cadmium, chromium, cobalt, copper, lead, and selenium were determined by Zeeman-corrected graphite-furnace atomic-absorption spectrometry. Concentrations of total arsenic and arsenite were determined by hydride-generation atomic-absorption spectrometry using a flow-injection analysis system. Concentrations of total mercury were determined by cold-vapor atomic fluorescence spectrometry. Concentrations of bromide, chloride, nitrate, and sulfate were determined by ion chromatography. Concentrations of ferrous and total iron were determined by the FerroZine colorimetric method. Concentrations of nitrite were determined by colorimetry or chemiluminescence. Concentrations of ammonia were determined by ion chromatography, with reanalysis by colorimetry when separation of sodium and ammonia peaks was poor. Dissolved organic carbon concentrations were determined by the wet persulfate oxidation method.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20041316","usgsCitation":"McCleskey, R.B., Ball, J.W., Nordstrom, D.K., Holloway, J.M., and Taylor, H.E., 2005, Water-chemistry data for selected springs, geysers, and streams in Yellowstone National Park Wyoming, 2001-2002: U.S. Geological Survey Open-File Report 2004-1316, 94 p., https://doi.org/10.3133/ofr20041316.","productDescription":"94 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":191525,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7100,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1316/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Wyoming","otherGeospatial":"Yellowstone National Park","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111,44.13333333333333 ], [ -111,45 ], [ -110,45 ], [ -110,44.13333333333333 ], [ -111,44.13333333333333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f0e4b07f02db5ee134","contributors":{"authors":[{"text":"McCleskey, R. Blaine 0000-0002-2521-8052 rbmccles@usgs.gov","orcid":"https://orcid.org/0000-0002-2521-8052","contributorId":147399,"corporation":false,"usgs":true,"family":"McCleskey","given":"R.","email":"rbmccles@usgs.gov","middleInitial":"Blaine","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":285251,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ball, James W.","contributorId":38946,"corporation":false,"usgs":true,"family":"Ball","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":285252,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nordstrom, D. Kirk 0000-0003-3283-5136 dkn@usgs.gov","orcid":"https://orcid.org/0000-0003-3283-5136","contributorId":749,"corporation":false,"usgs":true,"family":"Nordstrom","given":"D.","email":"dkn@usgs.gov","middleInitial":"Kirk","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":false,"id":285253,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Holloway, JoAnn M. 0000-0003-3603-7668 jholloway@usgs.gov","orcid":"https://orcid.org/0000-0003-3603-7668","contributorId":918,"corporation":false,"usgs":true,"family":"Holloway","given":"JoAnn","email":"jholloway@usgs.gov","middleInitial":"M.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":285249,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Taylor, Howard E. hetaylor@usgs.gov","contributorId":1551,"corporation":false,"usgs":true,"family":"Taylor","given":"Howard","email":"hetaylor@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":285250,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":72257,"text":"ofr20051177 - 2005 - Zero-headspace coal-core gas desorption canister, revised desorption data analysis spreadsheets and a dry canister heating system","interactions":[],"lastModifiedDate":"2020-09-27T17:47:22.805164","indexId":"ofr20051177","displayToPublicDate":"2005-09-19T00:00:00","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":"2005-1177","displayTitle":"Zero-Headspace Coal-Core Gas Desorption Canister, Revised Desorption Data Analysis Spreadsheets and a Dry Canister Heating System","title":"Zero-headspace coal-core gas desorption canister, revised desorption data analysis spreadsheets and a dry canister heating system","docAbstract":"Coal desorption techniques typically use the U.S. Bureau of Mines (USBM) canister-desorption method as described by Diamond and Levine (1981), Close and Erwin (1989), Ryan and Dawson (1993), McLennan and others (1994), Mavor and Nelson (1997) and Diamond and Schatzel (1998). However, the coal desorption canister designs historically used with this method have an inherent flaw that allows a significant gas-filled headspace bubble to remain in the canister that later has to be compensated for by correcting the measured desorbed gas volume with a mathematical headspace volume correction (McLennan and others, 1994; Mavor and Nelson, 1997).","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051177","usgsCitation":"Barker, C., and Dallegge, T.A., 2005, Zero-headspace coal-core gas desorption canister, revised desorption data analysis spreadsheets and a dry canister heating system (Version 1.0): U.S. Geological Survey Open-File Report 2005-1177, 9 p., https://doi.org/10.3133/ofr20051177.","productDescription":"9 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":193297,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11368,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1177/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5ddfb1","contributors":{"authors":[{"text":"Barker, Charles E.","contributorId":93070,"corporation":false,"usgs":true,"family":"Barker","given":"Charles E.","affiliations":[],"preferred":false,"id":285281,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dallegge, Todd A.","contributorId":38614,"corporation":false,"usgs":true,"family":"Dallegge","given":"Todd","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":285280,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72266,"text":"ofr20051305 - 2005 - Preliminary integrated geologic map databases for the United States - Western states: California, Nevada, Arizona, Washington, Oregon, Idaho, and Utah","interactions":[],"lastModifiedDate":"2022-05-10T18:59:59.459805","indexId":"ofr20051305","displayToPublicDate":"2005-09-19T00:00:00","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":"2005-1305","title":"Preliminary integrated geologic map databases for the United States - Western states: California, Nevada, Arizona, Washington, Oregon, Idaho, and Utah","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051305","usgsCitation":"Ludington, S., Moring, B.C., 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rjmiller@usgs.gov","contributorId":2516,"corporation":false,"usgs":true,"family":"Miller","given":"Robert","email":"rjmiller@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":285303,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Flynn, Kathryn","contributorId":106995,"corporation":false,"usgs":true,"family":"Flynn","given":"Kathryn","affiliations":[],"preferred":false,"id":285309,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hopkins, Melanie J.","contributorId":95132,"corporation":false,"usgs":true,"family":"Hopkins","given":"Melanie","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":285307,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Stone, Paul 0000-0002-1439-0156 pastone@usgs.gov","orcid":"https://orcid.org/0000-0002-1439-0156","contributorId":273,"corporation":false,"usgs":true,"family":"Stone","given":"Paul","email":"pastone@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":285302,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Bedford, David R.","contributorId":26352,"corporation":false,"usgs":true,"family":"Bedford","given":"David R.","affiliations":[],"preferred":false,"id":285305,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Haxel, Gordon A.","contributorId":42308,"corporation":false,"usgs":true,"family":"Haxel","given":"Gordon","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":285306,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":72268,"text":"ofr20051287 - 2005 - Effects of prescribed fire in the coastal prairies of Texas","interactions":[],"lastModifiedDate":"2019-07-22T14:24:54","indexId":"ofr20051287","displayToPublicDate":"2005-09-19T00:00:00","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":"2005-1287","title":"Effects of prescribed fire in the coastal prairies of Texas","docAbstract":"<p>Prescribed fire is widely applied for habitat management in coastal ecosystems. Fire management plans typically list a variety of objectives for prescribed burning, including succession management, promotion of native flora and fauna, providing habitat for species of importance, wildfire risk reduction (fuels management), as well as reduction and/or prevention of invasive species. In most cases, the information needed to determine the degree to which management objectives are met is not available. This study sought to provide an assessment of key objectives of fire management at the U.S. Fish and Wildlife Service (USFWS) Texas Mid-coast National Wildlife Refuge Complex. The main purpose of this work was to provide information and recommendations that will support Region 2 of the USFWS in the conduct of their fire and habitat management activities in the Western Gulf coast region. </p><p>There were four main components of this project: (1) a historical analysis of the role of fire in this ecosystem, (2) the development of standard methodology for assessing and monitoring fire effects in this system, (3) an evaluation of the effects of prescribed burning on the habitat being managed, and (4) an evaluation of the effects of burning on select fauna of special concern. A team of researchers, including some from the U.S. Geological Survey (USGS), Southeast Missouri State University, and Louisiana State University were involved in the various components of this project. Extensive support by USFWS personnel, both at the Texas Mid-coast National Wildlife Refuge Complex and in the Regional Office (Region 2, USFWS), was a key component in this work. Data from the three years of this study were combined with the results of previous USGS studies performed at the site to strengthen our conclusions. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20051287","usgsCitation":"Grace, J.B., Allain, L.K., Baldwin, H., Billock, A.G., Eddleman, W.R., Given, A.M., Jeske, C.W., and Moss, R., 2005, Effects of prescribed fire in the coastal prairies of Texas: U.S. Geological Survey Open-File Report 2005-1287, 46 p., https://doi.org/10.3133/ofr20051287.","productDescription":"46 p.","costCenters":[],"links":[{"id":193143,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20051287.PNG"},{"id":7139,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://archive.usgs.gov/archive/sites/www.nwrc.usgs.gov/factshts/2005-1287-fire-in-coastal-texas-report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624f2e","contributors":{"authors":[{"text":"Grace, James B. 0000-0001-6374-4726 gracej@usgs.gov","orcid":"https://orcid.org/0000-0001-6374-4726","contributorId":884,"corporation":false,"usgs":true,"family":"Grace","given":"James","email":"gracej@usgs.gov","middleInitial":"B.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":285311,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allain, Larry K. 0000-0002-7717-9761 allainl@usgs.gov","orcid":"https://orcid.org/0000-0002-7717-9761","contributorId":2414,"corporation":false,"usgs":true,"family":"Allain","given":"Larry","email":"allainl@usgs.gov","middleInitial":"K.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true},{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":285312,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baldwin, Heather Q. 0000-0003-1939-5439","orcid":"https://orcid.org/0000-0003-1939-5439","contributorId":52678,"corporation":false,"usgs":true,"family":"Baldwin","given":"Heather Q.","affiliations":[],"preferred":false,"id":285316,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Billock, Arlene G.","contributorId":57966,"corporation":false,"usgs":true,"family":"Billock","given":"Arlene","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":285317,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Eddleman, William R.","contributorId":40685,"corporation":false,"usgs":true,"family":"Eddleman","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":285314,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Given, Aaron M.","contributorId":49474,"corporation":false,"usgs":true,"family":"Given","given":"Aaron","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":285315,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Jeske, Clint W.","contributorId":107797,"corporation":false,"usgs":true,"family":"Jeske","given":"Clint","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":285318,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Moss, Rebecca 0000-0002-7599-9758","orcid":"https://orcid.org/0000-0002-7599-9758","contributorId":18466,"corporation":false,"usgs":true,"family":"Moss","given":"Rebecca","affiliations":[],"preferred":false,"id":285313,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":72272,"text":"ds124 - 2005 - Mining Claim Activity on Federal Land for the Period 1976 through 2003","interactions":[],"lastModifiedDate":"2012-02-02T00:13:59","indexId":"ds124","displayToPublicDate":"2005-09-19T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"124","title":"Mining Claim Activity on Federal Land for the Period 1976 through 2003","docAbstract":"Previous reports on mining claim records provided information and statistics (number of claims) using data from the U.S. Bureau of Land Management's (BLM) Mining Claim Recordation System. Since that time, BLM converted their mining claim data to the Legacy Repost 2000 system (LR2000). \r\n\r\nThis report describes a process to extract similar statistical data about mining claims from LR2000 data using different software and procedures than were used in the earlier work. A major difference between this process and the previous work is that every section that has a mining claim record is assigned a value. This is done by proportioning a claim between each section in which it is recorded. Also, the mining claim data in this report includes all BLM records, not just the western states. \r\n\r\nLR2000 mining claim database tables for the United States were provided by BLM in text format and imported into a Microsoft? Access2000 database in January, 2004. Data from two tables in the BLM LR2000 database were summarized through a series of database queries to determine a number that represents active mining claims in each Public Land Survey (PLS) section for each of the years from 1976 to 2002. For most of the area, spatial databases are also provided. The spatial databases are only configured to work with the statistics provided in the non-spatial data files. They are suitable for geographic information system (GIS)-based regional assessments at a scale of 1:100,000 or smaller (for example, 1:250,000).","language":"ENGLISH","doi":"10.3133/ds124","usgsCitation":"Causey, J.D., 2005, Mining Claim Activity on Federal Land for the Period 1976 through 2003: U.S. Geological Survey Data Series 124, 28 p. text + data files, https://doi.org/10.3133/ds124.","productDescription":"28 p. text + data files","costCenters":[],"links":[{"id":193205,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7142,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/124/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb727","contributors":{"authors":[{"text":"Causey, J. Douglas","contributorId":41398,"corporation":false,"usgs":true,"family":"Causey","given":"J.","email":"","middleInitial":"Douglas","affiliations":[],"preferred":false,"id":285325,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72282,"text":"sir20055087 - 2005 - Analysis of borehole-radar reflection data from Machiasport, Maine, December 2003","interactions":[],"lastModifiedDate":"2019-10-17T07:19:26","indexId":"sir20055087","displayToPublicDate":"2005-09-19T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5087","displayTitle":"Analysis of Borehole-Radar Reflection Data from Machiasport, Maine, December 2003","title":"Analysis of borehole-radar reflection data from Machiasport, Maine, December 2003","docAbstract":"In December 2003, the U.S. Geological Survey, in cooperation with the U.S. Army Corps of Engineers, collected borehole-radar reflection logs in two boreholes in Machiasport, Maine. These bedrock boreholes were drilled as part of a hydrogeologic investigation of the area surrounding the former Air Force Radar Tracking Station site on Howard Mountain near Bucks Harbor. The boreholes, MW09 and MW10, are located approximately 50 meters (m) from, and at the site of, respectively, the locations of former buildings where trichloroethylene was used as part of defense-site operations. These areas are thought to be potential source areas for contamination that has been detected in downgradient bedrock wells.\r\n\r\nThis investigation focused on testing borehole-radar methods at this site. Single-hole radar-reflection surveys were used to identify the depth, orientation, and spatial continuity of reflectors that intersect and surround the boreholes. In addition, the methods were used to (1) identify the radial depth of penetration of the radar waves in the electrically resistive bimodal volcanic formation at the site, (2) provide information for locating additional boreholes at the site, and (3) test the potential applications of borehole-radar methods for further aquifer characterization and (or) evaluation of source-area remediation efforts.\r\n\r\nBorehole-radar reflection logging uses a pair of downhole transmitting and receiving antennas to record the reflected wave amplitude and transit time of high-frequency electromagnetic waves. For this investigation, 60- and 100-megahertz antennas were used. The electromagnetic waves emitted by the transmitter penetrate into the formation surrounding the borehole and are reflected off of a material with different electromagnetic properties, such as a fracture or change in rock type. Single-hole directional radar surveys indicate the bedrock surrounding these boreholes is highly fractured, because several reflectors were identified in the radar-reflection data. There are several steeply dipping reflectors with orientations similar to the fracture patterns observed with borehole imaging techniques and in outcrops. The radar-reflection data showed that the vitrophyre in borehole MW09 was more highly fractured than the underlying gabbroic unit.\r\n\r\nThe velocities of radar waves in the bedrock surrounding the boreholes were determined using single-hole vertical radar profiling. Velocities of 114 and 125 meters per microsecond were used to determine the distance to reflectors, the radial depth of penetration, and the dip of reflectors. The bimodal volcanic units appear to be ideal for radar-wave propagation. For the radar surveys collected at this site, radar reflections were detected up to 40 m into the rock from the borehole. These results indicate that boreholes could conservatively be spaced about 15-20 m apart for hole-to-hole radar methods to be effective for imaging between the boreholes and monitoring remediation. Integrated analysis of drilling and borehole-geophysical logs indicates the vitrophyric formation is more fractured than the more mafic gabbroic units in these boreholes. There does not, however, appear to be a quantifiable difference in the radar-wave penetration in these two rock units.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055087","usgsCitation":"Johnson, C.D., and Joesten, P.K., 2005, Analysis of borehole-radar reflection data from Machiasport, Maine, December 2003: U.S. Geological Survey Scientific Investigations Report 2005-5087, v, 38 p., https://doi.org/10.3133/sir20055087.","productDescription":"v, 38 p.","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"links":[{"id":192863,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7151,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://water.usgs.gov/ogw/bgas/publications/SIR2005-5087/SIR2005-5087-embedded.pdf","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Maine","city":"Machiasport","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -67.39623069763184,\n              44.618088532560364\n            ],\n            [\n              -67.37674713134766,\n              44.618088532560364\n            ],\n            [\n              -67.37674713134766,\n              44.64362048303464\n            ],\n            [\n              -67.39623069763184,\n              44.64362048303464\n            ],\n            [\n              -67.39623069763184,\n              44.618088532560364\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad0e4b07f02db680cad","contributors":{"authors":[{"text":"Johnson, Carole D. 0000-0001-6941-1578 cjohnson@usgs.gov","orcid":"https://orcid.org/0000-0001-6941-1578","contributorId":1891,"corporation":false,"usgs":true,"family":"Johnson","given":"Carole","email":"cjohnson@usgs.gov","middleInitial":"D.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":285347,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Joesten, Peter K. pjoesten@usgs.gov","contributorId":1929,"corporation":false,"usgs":true,"family":"Joesten","given":"Peter","email":"pjoesten@usgs.gov","middleInitial":"K.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true},{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true}],"preferred":true,"id":285348,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72283,"text":"sir20055106 - 2005 - Quality of nutrient data from streams and ground water sampled during water years 1992-2001","interactions":[],"lastModifiedDate":"2012-02-02T00:13:59","indexId":"sir20055106","displayToPublicDate":"2005-09-19T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5106","title":"Quality of nutrient data from streams and ground water sampled during water years 1992-2001","docAbstract":"Proper interpretation of water-quality data requires consideration of the effects that bias and variability might have on measured constituent concentrations. In this report, methods are described to estimate the bias due to contamination of samples in the field or laboratory and the variability due to sample collection, processing, shipment, and analysis. Contamination can adversely affect interpretation of measured concentrations in comparison to standards or criteria. Variability can affect interpretation of small differences between individual measurements or mean concentrations. Contamination and variability are determined for nutrient data from quality-control samples (field blanks and replicates) collected as part of the National Water-Quality Assessment (NAWQA) Program during water years 1992-2001. Statistical methods are used to estimate the likelihood of contamination and variability in all samples. Results are presented for five nutrient analytes from stream samples and four nutrient analytes from ground-water samples. Ammonia contamination can add at least 0.04 milligram per liter in up to 5 percent of all samples. This could account for more than 22 percent of measured concentrations at the low range of aquatic-life criteria (0.18 milligram per liter). Orthophosphate contamination, at least 0.019 milligram per liter in up to 5 percent of all samples, could account for more than 38 percent of measured concentrations at the limit to avoid eutrophication (0.05 milligram per liter). Nitrite-plus-nitrate and Kjeldahl nitrogen contamination is less than 0.4 milligram per liter in 99 percent of all samples; thus there is no significant effect on measured concentrations of environmental significance. Sampling variability has little or no effect on reported concentrations of ammonia, nitrite-plus-nitrate, orthophosphate, or total phosphorus sampled after 1998. The potential errors due to sampling variability are greater for the Kjeldahl nitrogen analytes and for total phosphorus sampled before 1999. The uncertainty in a mean of 10 concentrations caused by sampling variability is within a small range (1 to 7 percent) for all nutrients. These results can be applied to interpretation of environmental data collected during water years 1992-2001 in 52 NAWQA study units. ","language":"ENGLISH","doi":"10.3133/sir20055106","usgsCitation":"Mueller, D.K., and Titus, C.J., 2005, Quality of nutrient data from streams and ground water sampled during water years 1992-2001: U.S. Geological Survey Scientific Investigations Report 2005-5106, v, 27 p. : ill. (some col.), col. map ; 28 cm., https://doi.org/10.3133/sir20055106.","productDescription":"v, 27 p. : ill. (some col.), col. map ; 28 cm.","costCenters":[],"links":[{"id":192864,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7152,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5106/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a68e4b07f02db63b24b","contributors":{"authors":[{"text":"Mueller, David K. mueller@usgs.gov","contributorId":1585,"corporation":false,"usgs":true,"family":"Mueller","given":"David","email":"mueller@usgs.gov","middleInitial":"K.","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true}],"preferred":true,"id":285349,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Titus, Cindy J.","contributorId":61913,"corporation":false,"usgs":true,"family":"Titus","given":"Cindy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":285350,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72290,"text":"sir20055158 - 2005 - Trends in surface-water quality at selected National Stream Quality Accounting Network (NASQAN) stations, in Michigan","interactions":[],"lastModifiedDate":"2017-02-06T09:35:02","indexId":"sir20055158","displayToPublicDate":"2005-09-19T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5158","title":"Trends in surface-water quality at selected National Stream Quality Accounting Network (NASQAN) stations, in Michigan","docAbstract":"<p>To demonstrate the value of long-term, water-quality monitoring, the Michigan Department of Environmental Quality (MDEQ), in cooperation with the U.S. Geological Survey (USGS), initiated a study to evaluate potential trends in water-quality constituents for selected National Stream Quality Accounting Network (NASQAN) stations in Michigan. The goal of this study is to assist the MDEQ in evaluating the effectiveness of water-pollution control efforts and the identification of water-quality concerns. </p><p>The study included a total of nine NASQAN stations in Michigan. Approximately 28 constituents were analyzed for trend tests. Station selection was based on data availability, land-use characteristics, and station priority for the MDEQ Water Chemistry Monitoring Project. Trend analyses were completed using the uncensored Seasonal Kendall Test in the computer program Estimate Trend (ESTREND), a software program for the detection of trends in water-quality data. The parameters chosen for the trend test had (1) at least a 5-year period of record (2) about 5 percent of the observations censored at a single reporting limit, and (3) 40 percent of the values within the beginning one-fifth and ending one-fifth of the selected period. In this study, a negative trend indicates a decrease in concentration of a particular constituent, which generally means an improvement in water quality; whereas a positive trend means an increase in concentration and possible degradation of water quality. </p><p>The results of the study show an overall improvement in water quality at the Clinton River at Mount Clemens, Manistee River at Manistee, and Pigeon River near Caseville. The detected trend for these stations show decreases in concentrations of various constituents such as nitrogen compounds, conductance, sulfate, fecal coliform bacteria, and fecal streptococci bacteria. The negative trend may indicate an overall improvement in agricultural practices, municipal and industrial wastewater-treatment processes, and effective regulations. </p><p>Phosphorus data for most of the study stations could not be analyzed because of the data limitations for trend tests. The only station with a significant negative trend in total phosphorus concentration is the Clinton River at Mount Clemens. However, scatter-plot analyses of phosphorus data indicate decreasing concentrations with time for most of the study stations. </p><p>Positive trends in concentration of nitrogen compounds were detected at the Kalamazoo River near Saugatuck and Muskegon River near Bridgeton. Positive trends in both fecal coliform and total fecal coliform were detected at the Tahquamenon River near Paradise. Various different point and nonpoint sources could produce such positive trends, but most commonly the increase in concentrations of nitrogen compounds and fecal coliform bacteria are associated with agricultural practices and sewage-plant discharges. </p><p>The constituent with the most numerous and geographically widespread significant trend is pH. The pH levels increased at six out of nine stations on all the major rivers in Michigan, with no negative trend at any station. The cause of pH increase is difficult to determine, as it could be related to a combination of anthropogenic activities and natural processes occurring simultaneously in the environment. </p><p>Trends in concentration of major ions, such as calcium, sodium, magnesium, sulfate, fluoride, chloride, and potassium, were detected at eight out of nine stations. A negative trend was detected only in sulfate and fluoride concentrations; a positive trend was detected only in calcium concentration. The major ions with the most widespread significant trends are sodium and chloride; three positive and two negative trends were detected for sodium, and three negative and two positive trends were detected for chloride. The negative trends in chloride concentrations outnumbered the positive trends. This result indicates a slight improvement in surface-water quality because chloride as a point source in natural water comes from deicing salt, sewage effluents, industrial wastes, and oil fields. </p><p>For other major ions, such as magnesium and potassium, both positive and negative trends were detected. These changes in trends indicate changes in surface-water quality caused by a variety of point and non-point sources throughout Michigan, as well as natural changes in the environment.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055158","collaboration":"In cooperation with the Michigan Department of Environmental Quality","usgsCitation":"Syed, A.U., and Fogarty, L., 2005, Trends in surface-water quality at selected National Stream Quality Accounting Network (NASQAN) stations, in Michigan: U.S. Geological Survey Scientific Investigations Report 2005-5158, v, 38 p., https://doi.org/10.3133/sir20055158.","productDescription":"v, 38 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":191769,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20055158.JPG"},{"id":7202,"rank":100,"type":{"id":15,"text":"Index 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,{"id":72292,"text":"sir20055185 - 2005 - Pre- and post-reservoir ground-water conditions and assessment of artificial recharge at Sand Hollow, Washington County, Utah, 1995-2005","interactions":[],"lastModifiedDate":"2017-01-27T16:04:53","indexId":"sir20055185","displayToPublicDate":"2005-09-19T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5185","title":"Pre- and post-reservoir ground-water conditions and assessment of artificial recharge at Sand Hollow, Washington County, Utah, 1995-2005","docAbstract":"<p>Sand Hollow, Utah, is the site of a surface-water reservoir completed in March 2002, which is being operated by the Washington County Water Conservancy District primarily as an aquifer storage and recovery project. The reservoir is an off-channel facility receiving water from the Virgin River, diverted near the town of Virgin, Utah. It is being operated conjunctively, providing both surface-water storage and artificial recharge to the underlying Navajo aquifer. The U.S. Geological Survey and the Bureau of Reclamation conducted a study to document baseline ground-water conditions at Sand Hollow prior to the operation of the reservoir and to evaluate changes in ground-water conditions caused by the reservoir.</p><p>Pre-reservoir age dating using tritium/helium, chlorofluorocarbons, and carbon-14 shows that shallow ground water in the Navajo Sandstone in some areas of Sand Hollow entered the aquifer from 2 to 25 years before sample collection. Ground water in low-recharge areas and deeper within the aquifer may have entered the aquifer more than 8,000 years ago. Ground-water levels in the immediate vicinity of Sand Hollow Reservoir have risen by as much as 80 feet since initial filling began in March 2002. In 2005, ground water was moving laterally away from the reservoir in all directions, whereas the pre-reservoir direction of ground-water flow was predominantly toward the north.</p><p>Tracers, or attributes, of artificial recharge include higher specific conductance, higher dissolved-solids concentrations, higher chloride-to-bromide ratios, more-depleted stable isotopes (<img src=\"https://pubs.usgs.gov/sir/2005/5185/images/snake.gif\" alt=\"Snake\" width=\"16\" height=\"15\" data-mce-src=\"https://pubs.usgs.gov/sir/2005/5185/images/snake.gif\"><sup>2</sup>H and <img src=\"https://pubs.usgs.gov/sir/2005/5185/images/snake.gif\" alt=\"Snake\" width=\"16\" height=\"15\" data-mce-src=\"https://pubs.usgs.gov/sir/2005/5185/images/snake.gif\"><sup>18</sup>O), and higher total-dissolved gas pressures. These tracers have been detected at observation and production wells close to the reservoir. About 15,000 tons of naturally occurring salts that previously accumulated in the vadose zone beneath the reservoir are being flushed into the aquifer. Except for the shallowest parts of the aquifer, this is generally not affecting water quality, largely because of the large saturated thickness of the Navajo aquifer. Since the initial filling of Sand Hollow Reservoir, arsenic concentrations have risen to exceed U.S. Environmental Protection Agency standards only in some shallow observation wells. These increases in arsenic concentration are likely caused by increasing pH associated with artificial recharge beneath the reservoir, rather than flushing of previously accumulated salts in the vadose zone. There has been no trend of increasing arsenic concentration in deeper production wells.</p><p>Estimated evaporation rates for Sand Hollow Reservoir, calculated by the Jensen-Haise method with data from the Sand Hollow weather station, range from about 55 to 61 inches per year and result in a total evaporative loss of about 6,000 acre-feet of water from March 2002 to September 2004. Rates of artificial recharge of ground water beneath Sand Hollow Reservoir have ranged from about 0.02 to 0.44 feet per day, with an average rate excluding the initial 3-month wetting period of about 0.06 feet per day. A total of about 28,000 acre-feet of recharge to the underlying Navajo aquifer occurred from March 2002 to September 2004.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/sir20055185","collaboration":"Prepared in cooperation with the Washington County water conservancy district, Bureau of Reclamation, and the University of Utah Department of Geology and Geophysics","usgsCitation":"Heilweil, V.M., Susong, D.D., Gardner, P.M., and Watt, D.E., 2005, Pre- and post-reservoir ground-water conditions and assessment of artificial recharge at Sand Hollow, Washington County, Utah, 1995-2005 (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5185, viii, 74 p., https://doi.org/10.3133/sir20055185.","productDescription":"viii, 74 p.","numberOfPages":"85","onlineOnly":"Y","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":191824,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":334243,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5185/pdf/SIR2005_5185.pdf"},{"id":7204,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5185/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Utah","county":"Washington County","otherGeospatial":"Sand Hollow","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.393499,37.102437 ], [ -113.393499,37.127407 ], [ -113.359917,37.127407 ], [ -113.359917,37.102437 ], [ -113.393499,37.102437 ] ] ] } } ] }","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db681dc2","contributors":{"authors":[{"text":"Heilweil, Victor M. heilweil@usgs.gov","contributorId":837,"corporation":false,"usgs":true,"family":"Heilweil","given":"Victor","email":"heilweil@usgs.gov","middleInitial":"M.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285364,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Susong, David D. ddsusong@usgs.gov","contributorId":1040,"corporation":false,"usgs":true,"family":"Susong","given":"David","email":"ddsusong@usgs.gov","middleInitial":"D.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285366,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gardner, Philip M. 0000-0003-3005-3587 pgardner@usgs.gov","orcid":"https://orcid.org/0000-0003-3005-3587","contributorId":962,"corporation":false,"usgs":true,"family":"Gardner","given":"Philip","email":"pgardner@usgs.gov","middleInitial":"M.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true},{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285365,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Watt, Dennis E.","contributorId":55286,"corporation":false,"usgs":true,"family":"Watt","given":"Dennis","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":285367,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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