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,{"id":76564,"text":"sir20055266 - 2006 - Hydrogeology and simulation of ground-water flow in the Silurian-Devonian aquifer system, Johnson County, Iowa","interactions":[],"lastModifiedDate":"2016-01-29T15:39:42","indexId":"sir20055266","displayToPublicDate":"2006-04-13T00:00:00","publicationYear":"2006","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":"2005-5266","title":"Hydrogeology and simulation of ground-water flow in the Silurian-Devonian aquifer system, Johnson County, Iowa","docAbstract":"<p>Bedrock of Silurian and Devonian age (termed the &ldquo;Silurian-Devonian aquifer system&rdquo;) is the primary source of ground water for Johnson County in east-central Iowa. Population growth within municipal and suburban areas of the county has resulted in increased amounts of water withdrawn from this aquifer and water-level declines in some areas. A 3-year study of the hydrogeology of the Silurian-Devonian aquifer system in Johnson County was undertaken to provide a quantitative assessment of ground water resources and to construct a ground-water flow model that can be used by local governmental agencies as a management tool.</p>\n<p>Johnson County is underlain by unconsolidated deposits of Quaternary age and Paleozoic-age bedrock units. The bulk of the Quaternary deposits consists of weathered and unweathered glacial till; however, shallow alluvium and buried sand and gravel deposits also are present. Six bedrock hydrogeologic units are present in Johnson County (oldest to youngest): Maquoketa confining unit, Silurian aquifer, Wapsipinicon Group (aquifer and confining unit), Cedar Valley aquifer, Upper Devonian shale confining unit, and Cherokee confining unit. Although separate aquifers and confining units are described, the Silurian- and Devonian-age units are considered as a single aquifer system. The top of the Silurian-Devonian aquifer system is considered as the top of the Cedar Valley aquifer, where present, and the base of the aquifer system is considered as the top of the Maquoketa confining unit.</p>\n<p>The hydraulic properties of the rocks that comprise the Silurian-Devonian aquifer system are highly variable as a result of the variable composition of the rocks and the presence of solution features in some of the carbonate-rock units. For the combined Silurian-Devonian aquifer system, specific capacity averages 2.1 gallons per minute per foot of drawdown, transmissivity averages about 580 feet squared per day, and hydraulic conductivity averages 8.3 feet per day.</p>\n<p>Recharge to the Silurian-Devonian aquifer system in Johnson County is predominantly from infiltration of precipitation to the bedrock. Discharge from the aquifer is primarily to municipal, industrial, and private-development wells. Reliable measurements of the amount of recharge to or discharge from the ground-water system in Johnson County, however, are not available.</p>\n<p>Altitude of the 1996 potentiometric surface ranged from more than 750 feet above the North American Vertical Datum of 1988 (NAVD88) in northern Johnson County to less than 575 feet above NAVD88 in the central part of the county. A large cone of depression within the potentiometric surface is present in the central part of the county, between Coralville and Iowa City. A large limestone quarry is located near the center of this cone of depression. Ground water generally flows from the northern and western parts of Johnson County either toward the cone of depression in the center of the county or south out of the county. Ground water also flows toward the Cedar River in the northeastern part of the county. A ground-water divide in the northeastern part of the county roughly approximates the surface-water divide between the Iowa River and Cedar River drainages.</p>\n<p>A numerical ground-water-flow model of the Silurian-Devonian aquifer system in Johnson County was used to test concepts of ground-water flow, to assess the need for additional data, and to evaluate the potential effects of anticipated increased ground-water development and drought. The 1-layer model was calibrated to average 1996 ground-water conditions, which were assumed to approximate steady-state flow conditions. The model also was used to simulate steady-state conditions for 2004, steady-state conditions using anticipated pumping rates for 2025, and potential future drought conditions.</p>\n<p>The simulated potentiometric surface generally replicated the potentiometric surface for 1996 and 2004 conditions. The calculated root mean squared error values for the 1996 and 2004 simulations were 13.6 and 18.6 feet, respectively. The mean absolute differences between measured and simulated water levels for the 1996 and 2004 simulations were about 11 and 14 feet, respectively.</p>\n<p>Total model-calculated inflow to the ground-water system for the 1996 simulation was 19.6 million gallons per day (Mgal/d), and the largest model-calculated inflow component was areal recharge (15.1 Mgal/d). Total model-calculated outflow from the ground-water system was 19.7 Mgal/d, and the largest outflow component was discharge to wells (10.5 Mgal/d). Model-calculated water-budget components for the 2004 simulation were similar to the 1996 components.</p>\n<p>Potential future steady-state conditions were simulated using anticipated 2025 pumping rates. Pumpage both for existing wells and for assumed new wells, based on anticipated population growth in the northern part of the county and for the nearby municipalities, was included in the model. Simulated 2025 pumpage was about 1.5 Mgal/d greater than simulated 2004 pumpage. Simulated steady-state ground-water levels, using anticipated 2025 pumping rates, were lower than 2004 simulated levels throughout the county, and simulated water-level declines ranged from less than 1 foot near the county boundaries to about 11 feet.</p>\n<p>Potential future drought conditions were simulated by assuming that recharge to the Silurian-Devonian aquifer system is reduced by a factor of 0.75 and that water-supply pumpage is increased by a factor of 1.25 over the anticipated 2025 pumping rates. Overall, simulated water levels for future drought conditions were greater than 5 feet lower than simulated 2004 conditions and were a maximum of about 30 feet lower in the northeastern part of the county.</p>\n<p>The greatest limitation to the model is the lack of measured or estimated water-budget components for comparison to simulated water-budget components. Because the model is only calibrated to measured water levels, and not to water-budget components, the model results are nonunique. Other model limitations include the relatively coarse grid scale, lack of detailed information on pumpage from the quarry and from private developments and domestic wells, and the lack of separate water-level data for the Silurian- and Devonian-age rocks.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055266","usgsCitation":"Tucci, P., and McKay, R.M., 2006, Hydrogeology and simulation of ground-water flow in the Silurian-Devonian aquifer system, Johnson County, Iowa (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5266, 78 p., https://doi.org/10.3133/sir20055266.","productDescription":"78 p.","numberOfPages":"78","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":190834,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7521,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5266/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Iowa","county":"Johnson","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-91.3677,41.8603],[-91.3673,41.7745],[-91.3675,41.6855],[-91.3671,41.5987],[-91.3679,41.5107],[-91.3687,41.4235],[-91.4839,41.4222],[-91.4843,41.4286],[-91.492,41.4405],[-91.5033,41.4493],[-91.5026,41.452],[-91.4989,41.4538],[-91.4988,41.4592],[-91.5145,41.4676],[-91.5156,41.4704],[-91.5136,41.4767],[-91.5038,41.4779],[-91.5029,41.4874],[-91.5039,41.4933],[-91.5076,41.4939],[-91.5107,41.4944],[-91.5112,41.4971],[-91.508,41.5016],[-91.5098,41.5034],[-91.5117,41.5016],[-91.5148,41.4985],[-91.5197,41.4981],[-91.5196,41.5027],[-91.5281,41.5078],[-91.528,41.511],[-91.5991,41.5107],[-91.7138,41.511],[-91.8291,41.5116],[-91.827,41.6001],[-91.8337,41.6006],[-91.8335,41.6865],[-91.8327,41.775],[-91.8318,41.8617],[-91.716,41.862],[-91.5989,41.8612],[-91.4836,41.8608],[-91.3677,41.8603]]]},\"properties\":{\"name\":\"Johnson\",\"state\":\"IA\"}}]}","edition":"Online only","tableOfContents":"<p>Abstract<br />Introduction<br />Previous Studies<br />Physical Setting and Climate<br />Water Use<br />Acknowledgments<br />Hydrogeologic Setting<br />Hydrogeologic Units<br />Quaternary Deposits<br />Bedrock Topography<br />Bedrock Hydrogeologic Units<br />Maquoketa Confining Unit<br />Silurian Aquifer<br />Wapsipinicon Group<br />Cedar Valley Aquifer<br />Upper Devonian Shale Confining Unit<br />Cherokee Confining Unit<br />Geologic Structure<br />Hydraulic Characteristics<br />Recharge and Discharge<br />Ground-Water Occurrence and Movement<br />Simulation of Ground-Water Flow<br />Model Construction and Boundary Conditions<br />1996 Steady-State Calibration and Simulation<br />Model Calibration<br />Simulation Results<br />Model Sensitivity<br />Simulation of Potential Future Withdrawals<br />Simulation of 2004 Conditions<br />Simulation of Potential 2025 Steady-State Pumping<br />Simulation of Potential Future Drought Conditions<br />Model Limitations and Additional Data Needs<br />Summary<br />References Cited<br />Appendix</p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db6252a1","contributors":{"authors":[{"text":"Tucci, Patrick ptucci@usgs.gov","contributorId":926,"corporation":false,"usgs":true,"family":"Tucci","given":"Patrick","email":"ptucci@usgs.gov","affiliations":[],"preferred":true,"id":287387,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McKay, Robert M.","contributorId":91928,"corporation":false,"usgs":true,"family":"McKay","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":287388,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":76552,"text":"sir20065064 - 2006 - Evaluation of the ground-water flow model for northern Utah Valley, Utah, updated to conditions through 2002","interactions":[],"lastModifiedDate":"2017-01-27T10:27:22","indexId":"sir20065064","displayToPublicDate":"2006-04-13T00:00:00","publicationYear":"2006","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":"2006-5064","title":"Evaluation of the ground-water flow model for northern Utah Valley, Utah, updated to conditions through 2002","docAbstract":"<p>This report evaluates the performance of a numerical model of the ground-water system in northern Utah Valley, Utah, that originally simulated ground-water conditions during 1947-1980 and was updated to include conditions estimated for 1981-2002. Estimates of annual recharge to the ground-water system and discharge from wells in the area were added to the original ground-water flow model of the area.</p><p>The files used in the original transient-state model of the ground-water flow system in northern Utah Valley were imported into MODFLOW-96, an updated version of MODFLOW. The main model input files modified as part of this effort were the well and recharge files. Discharge from pumping wells in northern Utah Valley was estimated on an annual basis for 1981-2002. Although the amount of average annual withdrawals from wells has not changed much since the previous study, there have been changes in the distribution of well discharge in the area. Discharge estimates for flowing wells during 1981-2002 were assumed to be the same as those used in the last stress period of the original model because of a lack of new data. Variations in annual recharge were assumed to be proportional to changes in total surface-water inflow to northern Utah Valley. Recharge specified in the model during the additional stress periods varied from 255,000 acre-feet in 1986 to 137,000 acre-feet in 1992.</p><p>The ability of the updated transient-state model to match hydrologic conditions determined for 1981-2002 was evaluated by comparing water-level changes measured in wells to those computed by the model. Water-level measurements made in February, March, or April were available for 39 wells in the modeled area during all or part of 1981-2003. In most cases, the magnitude and direction of annual water-level change from 1981 to 2002 simulated by the updated model reasonably matched the measured change. The greater-than-normal precipitation that occurred during 1982-84 resulted in period-of-record high water levels measured in many of the observation wells in March 1984. The model-computed water levels at the end of 1982-84 also are among the highest for the period. Both measured and computed water levels decreased during the period representing ground-water conditions from 1999 to 2002. Precipitation was less than normal during 1999-2002.</p><p>The ability of the model to adequately simulate climatic extremes such as the wetter-than-normal conditions of 1982-84 and the drier-than-normal conditions of 1999-2002 indicates that the annual variation of recharge to the ground-water system based on streamflow entering the valley, which in turn is primarily dependent upon precipitation, is appropriate but can be improved. The updated transient-state model of the ground-water system in northern Utah Valley can be improved by making revisions on the basis of currently available data and information.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/sir20065064","collaboration":"Prepared in cooperation with the Central Utah Water Conservancy District; Jordan Valley Water Conservancy District representing Draper City; Highland Water Company; Utah Department of Natural Resources, Division of Water Rights; and the municipalities of Alpine, American Fork, Cedar Hills, Eagle Mountain, Highland, Lehi, Lindon, Orem, Pleasant Grove, Provo, Saratoga Springs, and Vineyard","usgsCitation":"Thiros, S.A., 2006, Evaluation of the ground-water flow model for northern Utah Valley, Utah, updated to conditions through 2002 (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2006-5064, iv, 28 p., https://doi.org/10.3133/sir20065064.","productDescription":"iv, 28 p.","numberOfPages":"28","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":190870,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7256,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5064/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Utah","otherGeospatial":"Northern Utah Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.06054687499999,\n              40.04023218690451\n            ],\n            [\n              -112.06054687499999,\n              40.65563874006118\n            ],\n            [\n              -111.4617919921875,\n              40.65563874006118\n            ],\n            [\n              -111.4617919921875,\n              40.04023218690451\n            ],\n            [\n              -112.06054687499999,\n              40.04023218690451\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa402","contributors":{"authors":[{"text":"Thiros, Susan A. 0000-0002-8544-553X sthiros@usgs.gov","orcid":"https://orcid.org/0000-0002-8544-553X","contributorId":965,"corporation":false,"usgs":true,"family":"Thiros","given":"Susan","email":"sthiros@usgs.gov","middleInitial":"A.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287363,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":76561,"text":"ofr20061096 - 2006 - Central Texas coastal classification maps - Aransas Pass to Mansfield Channel","interactions":[],"lastModifiedDate":"2022-09-27T19:37:54.988287","indexId":"ofr20061096","displayToPublicDate":"2006-04-13T00:00:00","publicationYear":"2006","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":"2006-1096","title":"Central Texas coastal classification maps - Aransas Pass to Mansfield Channel","docAbstract":"The primary purpose of the USGS National Assessment of Coastal Change Project is to provide accurate representations of pre-storm ground conditions for areas that are designated high priority because they have dense populations or valuable resources that are at risk from storm waves. A secondary purpose of the project is to develop a geomorphic (land feature) coastal classification that, with only minor modification, can be applied to most coastal regions in the United States.\r\n\r\nA Coastal Classification Map describing local geomorphic features is the first step toward determining the hazard vulnerability of an area. The Coastal Classification Maps of the National Assessment of Coastal Change Project present ground conditions such as beach width, dune elevations, overwash potential, and density of development. In order to complete a hazard-vulnerability assessment, that information must be integrated with other information, such as prior storm impacts and beach stability. The Coastal Classification Maps provide much of the basic information for such an assessment and represent a critical component of a storm-impact forecasting capability.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061096","usgsCitation":"Morton, R., and Peterson, R.L., 2006, Central Texas coastal classification maps - Aransas Pass to Mansfield Channel: U.S. Geological Survey Open-File Report 2006-1096, HTML Document; 1 CD-ROM, https://doi.org/10.3133/ofr20061096.","productDescription":"HTML Document; 1 CD-ROM","onlineOnly":"Y","costCenters":[],"links":[{"id":190832,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":407473,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_76218.htm","linkFileType":{"id":5,"text":"html"}},{"id":7519,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1096/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Texas","otherGeospatial":"Aransas Pass to Mansfield Channel","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.58056640625,\n              26.52956523826758\n            ],\n            [\n              -96.8994140625,\n              26.52956523826758\n            ],\n            [\n              -96.8994140625,\n              28.013801376380712\n            ],\n            [\n              -97.58056640625,\n              28.013801376380712\n            ],\n            [\n              -97.58056640625,\n              26.52956523826758\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6eb6","contributors":{"authors":[{"text":"Morton, Robert A.","contributorId":88333,"corporation":false,"usgs":true,"family":"Morton","given":"Robert A.","affiliations":[],"preferred":false,"id":287377,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, Russell L.","contributorId":55045,"corporation":false,"usgs":true,"family":"Peterson","given":"Russell","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":287376,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":76557,"text":"fs20063038 - 2006 - Geography at the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-02-02T00:14:14","indexId":"fs20063038","displayToPublicDate":"2006-04-13T00:00:00","publicationYear":"2006","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":"2006-3038","title":"Geography at the U.S. Geological Survey","docAbstract":"Geography ? the science of place ? is a bridging, integrating, and synthesizing field because place is a pivotal study element in all the natural sciences. We work to combine our talents with USGS scientists in other disciplines in pursuing the USGS mission ? Science for a Changing World.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/fs20063038","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2006, Geography at the U.S. Geological Survey: U.S. Geological Survey Fact Sheet 2006-3038, 2 p., https://doi.org/10.3133/fs20063038.","productDescription":"2 p.","numberOfPages":"4","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":123127,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2006/3038/report-thumb.jpg"},{"id":91192,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2006/3038/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8fc1","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":534777,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":76558,"text":"ofr20061025 - 2006 - Drivers of U.S. mineral demand","interactions":[],"lastModifiedDate":"2012-02-02T00:14:14","indexId":"ofr20061025","displayToPublicDate":"2006-04-13T00:00:00","publicationYear":"2006","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":"2006-1025","title":"Drivers of U.S. mineral demand","docAbstract":"Introduction:   The word 'demand' has different meanings for different people. To some, it means their 'wants and needs,' to others it is what they consume. Yet, when considering economics, demand refers to the specific amounts of goods or services that individuals will purchase at various prices. Demand is measured over a given time period. It is determined by a number of factors including income, tastes, and the price of complementary and substitute goods. In this paper, the term consumption is used fairly synonymously with the term demand. Most mineral commodities, like iron ore, copper, zinc, and gravel, are intermediate goods, which means that they are used in the production of other goods, called final goods. Demand for intermediate goods is called derived demand because such demand is derived from the demand for final goods.\r\n\r\nWhen demand increases for a commodity, generally the price rises. With everything else held constant, this increases the profits for those who provide this commodity. Normally, this would increase profits of existing producers and attract new producers to the market. When demand for a commodity decreases, generally the price falls. Normally, this would cause profits to fall and, as a consequence, the least efficient firms may be forced from the industry.\r\n\r\nDemand changes for specific materials as final goods or production techniques are reengineered while maintaining or improving product performance, for example, the use of aluminum in the place of copper in long distance electrical transmission lines or plastic replacing steel in automobile bumpers. Substitution contributes to efficient material usage by utilizing cheaper or technically superior materials. In this way, it may also alleviate materials scarcity. If a material becomes relatively scarce (and thus more expensive), a more abundant (and less expensive) material generally replaces it (Wagner and others, 2003, p. 91).\r\n\r\n","language":"ENGLISH","doi":"10.3133/ofr20061025","usgsCitation":"Sznopek, J.L., 2006, Drivers of U.S. mineral demand (Online only, Version 1.0): U.S. Geological Survey Open-File Report 2006-1025, iv, 16 p., https://doi.org/10.3133/ofr20061025.","productDescription":"iv, 16 p.","numberOfPages":"20","onlineOnly":"Y","costCenters":[],"links":[{"id":190910,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7491,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1025/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only, Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5ee4b07f02db633bb0","contributors":{"authors":[{"text":"Sznopek, John L.","contributorId":23936,"corporation":false,"usgs":true,"family":"Sznopek","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":287369,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":76563,"text":"sir20065076 - 2006 - Hydrogeology, water use, and simulated ground-water flow and availability in Campton township, Kane County, Illinois","interactions":[],"lastModifiedDate":"2019-03-20T10:46:24","indexId":"sir20065076","displayToPublicDate":"2006-04-13T00:00:00","publicationYear":"2006","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":"2006-5076","displayTitle":"Hydrogeology, Water Use, and Simulated Ground-Water Flow and Availability in Campton Township, Kane County, Illinois","title":"Hydrogeology, water use, and simulated ground-water flow and availability in Campton township, Kane County, Illinois","docAbstract":"<p>Several aquifers underlying Campton Township in Kane County, Illinois provide virtually all of the water supply to the residents of the township. These aquifers consist of layers of unconsolidated sand and gravel in the glacial drift; dolomite and shale of the Alexandrian Series and the Maquoketa Group (the Silurian-Maquoketa aquifer); dolomite of the Platteville and Galena Groups (the Galena-Platteville aquifer); and sandstones of the Glenwood Formation and the St. Peter Sandstone (the Ancell aquifer). In 2002, total withdrawals from these aquifers underlying Campton Township exceeded 1.36 million gallons day.</p><p>Water-level altitudes in the shallow and deep glacial drift aquifers generally follow surface topography. Comparison of water levels measured in 1995 and 2002 does not indicate large (15 feet or more) water-level declines in these aquifers beneath most of the township.</p><p>Water-level altitudes in the Silurian-Maquoketa aquifer generally decrease from west to east. The potentiometric surface of the aquifer follows the bedrock-surface topography in parts of the township, but local low water-level altitudes and large declines in water levels between 1995 and 2002 indicate that withdrawals from the Silurian-Maquoketa aquifer may exceed recharge in some areas.</p><p>Water-level altitudes in wells completed in the Galena-Platteville aquifer vary by more than 300 ft. Large water-level declines in wells completed in the Galena-Platteville aquifer from 1995 to 2002 indicate that withdrawals from the Galena-Platteville and Silurian-Maquoketa aquifers exceed recharge in the northern part of the township.</p><p>Water-level altitudes in wells completed in the Ancell aquifer are also highly variable. Although there is no indication of large water-level declines in Ancell aquifer between 1995 and 2002, historical data for one well completed in the aquifer indicate large water-level declines over a period of decades.</p><p>Computer simulation of flow in the ground-water system indicates that most of the shallow ground water underlying the township is derived from precipitation near the ground-water divide in the western part of the township. Shallow recharge moves primarily through the glacial drift aquifers and the upper part of the Silurian-Maquoketa aquifer, with minimal flow into the Galena-Platteville and Ancell aquifers. Most of the water in the Ancell aquifer beneath the township originates as surface recharge in the area west of the township. Vertical recharge to the Ancell aquifer from the Galena-Platteville aquifer beneath the township is not substantial. The source of the water withdrawn from the Ancell is inflow through the aquifer from areas west of the township. About 10 percent of ground water flowing through the township in 2002 was withdrawn by wells, with 80 percent flowing through the township and discharging to surface water bodies, including the Fox River. Simulation of additional withdrawals from the Ancell aquifer to supply an additional 605 proposed homes indicates about 17 ft of drawdown in the aquifer in the vicinity of a production well, but virtually no drawdown in any of the overlying aquifers.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20065076","collaboration":"Prepared in cooperation with the Campton Township Board of Trustees","usgsCitation":"Kay, R.T., Arihood, L.D., Arnold, T., and Fowler, K.K., 2006, Hydrogeology, water use, and simulated ground-water flow and availability in Campton township, Kane County, Illinois (Online only): U.S. Geological Survey Scientific Investigations Report 2006-5076, vii, 99 p., https://doi.org/10.3133/sir20065076.","productDescription":"vii, 99 p.","numberOfPages":"109","onlineOnly":"Y","costCenters":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"links":[{"id":7520,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5076/","linkFileType":{"id":5,"text":"html"}},{"id":190833,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sir/2006/5076/coverthb.jpg"},{"id":362135,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2006/5076/pdf/sir20065076.pdf","text":"Report","size":"9.18 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIR 2006–5076"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.83333333333333,42.333333333333336 ], [ -88.83333333333333,42 ], [ -88.41666666666667,42 ], [ -88.41666666666667,42.333333333333336 ], [ -88.83333333333333,42.333333333333336 ] ] ] } } ] }","edition":"Online only","contact":"<p>Director,&nbsp;<a href=\"https://www.usgs.gov/centers/cm-water\" data-mce-href=\"https://www.usgs.gov/centers/cm-water\">Central Midwest Water Science Center</a><br>U.S. Geological Survey<br>405 North Goodwin<br>Urbana, IL 61801</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Geology</li><li>Hydrology</li><li>Water Use</li><li>Simulation of Ground-Water Flow and Availability</li><li>Summary and Conclusions</li><li>Acknowledgments</li><li>References Cited</li><li>Glossary</li><li>Appendix A—Summary of well information ans water-level measurements taken during the survey of residential-supply wells in Campton Township, Illinois, May–June 1995 and June–July 2002</li><li>Appendix B—Geophysical logs collected from wells in Campton Township, Illinois, June 2003</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db614840","contributors":{"authors":[{"text":"Kay, Robert T. 0000-0002-6281-8997 rtkay@usgs.gov","orcid":"https://orcid.org/0000-0002-6281-8997","contributorId":1122,"corporation":false,"usgs":true,"family":"Kay","given":"Robert","email":"rtkay@usgs.gov","middleInitial":"T.","affiliations":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287383,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Arihood, Leslie D. 0000-0001-5792-3699 larihood@usgs.gov","orcid":"https://orcid.org/0000-0001-5792-3699","contributorId":2357,"corporation":false,"usgs":true,"family":"Arihood","given":"Leslie","email":"larihood@usgs.gov","middleInitial":"D.","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true},{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287385,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Arnold, Terri 0000-0003-1406-6054 tlarnold@usgs.gov","orcid":"https://orcid.org/0000-0003-1406-6054","contributorId":1598,"corporation":false,"usgs":false,"family":"Arnold","given":"Terri","email":"tlarnold@usgs.gov","affiliations":[{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true},{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":35680,"text":"Illinois-Iowa-Missouri Water Science Center","active":true,"usgs":true}],"preferred":false,"id":287384,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fowler, Kathleen K. 0000-0002-0107-3848 kkfowler@usgs.gov","orcid":"https://orcid.org/0000-0002-0107-3848","contributorId":2439,"corporation":false,"usgs":true,"family":"Fowler","given":"Kathleen","email":"kkfowler@usgs.gov","middleInitial":"K.","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true},{"id":27231,"text":"Indiana-Kentucky Water Science Center","active":true,"usgs":true},{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287386,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":76553,"text":"sir20065001 - 2006 - Characteristics of thermal springs and the shallow ground-water system at Hot Springs National Park, Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:14:14","indexId":"sir20065001","displayToPublicDate":"2006-04-13T00:00:00","publicationYear":"2006","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":"2006-5001","title":"Characteristics of thermal springs and the shallow ground-water system at Hot Springs National Park, Arkansas","language":"ENGLISH","doi":"10.3133/sir20065001","usgsCitation":"Yeatts, D.S., 2006, Characteristics of thermal springs and the shallow ground-water system at Hot Springs National Park, Arkansas: U.S. Geological Survey Scientific Investigations Report 2006-5001, 42 p., 17 fig., https://doi.org/10.3133/sir20065001.","productDescription":"42 p., 17 fig.","numberOfPages":"42","costCenters":[],"links":[{"id":190871,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7257,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5001/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4edb","contributors":{"authors":[{"text":"Yeatts, Daniel S.","contributorId":22015,"corporation":false,"usgs":true,"family":"Yeatts","given":"Daniel","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":287364,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":76559,"text":"ofr20061054 - 2006 - A Procedure for the supercritical fluid extraction of coal samples, with subsequent analysis of extracted hydrocarbons","interactions":[],"lastModifiedDate":"2012-02-02T00:14:14","indexId":"ofr20061054","displayToPublicDate":"2006-04-13T00:00:00","publicationYear":"2006","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":"2006-1054","title":"A Procedure for the supercritical fluid extraction of coal samples, with subsequent analysis of extracted hydrocarbons","docAbstract":"Introduction:  \r\nThis report provides a detailed, step-by-step procedure for conducting extractions with supercritical carbon dioxide (CO2) using the ISCO SFX220 supercritical fluid extraction system. Protocols for the subsequent separation and analysis of extracted hydrocarbons are also included in this report. These procedures were developed under the auspices of the project 'Assessment of Geologic Reservoirs for Carbon Dioxide Sequestration' (see http://pubs.usgs.gov/fs/fs026-03/fs026-03.pdf) to investigate possible environmental ramifications associated with CO2 storage (sequestration) in geologic reservoirs, such as deep (~1 km below land surface) coal beds.\r\n\r\nSupercritical CO2 has been used previously to extract contaminants from geologic matrices. Pressure-temperature conditions within deep coal beds may render CO2 supercritical. In this context, the ability of supercritical CO2 to extract contaminants from geologic materials may serve to mobilize noxious compounds from coal, possibly complicating storage efforts. There currently exists little information on the physicochemical interactions between supercritical CO2 and coal in this setting. The procedures described herein were developed to improve the understanding of these interactions and provide insight into the fate of CO2 and contaminants during simulated CO2 injections.","language":"ENGLISH","doi":"10.3133/ofr20061054","usgsCitation":"Kolak, J.J., 2006, A Procedure for the supercritical fluid extraction of coal samples, with subsequent analysis of extracted hydrocarbons (Online only, Version 1.0): U.S. Geological Survey Open-File Report 2006-1054, 29 p., https://doi.org/10.3133/ofr20061054.","productDescription":"29 p.","numberOfPages":"29","onlineOnly":"Y","costCenters":[],"links":[{"id":190911,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7492,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1054/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only, Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4964e4b0b290850ef1f1","contributors":{"authors":[{"text":"Kolak, Jonathan J.","contributorId":59100,"corporation":false,"usgs":true,"family":"Kolak","given":"Jonathan","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":287370,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":76562,"text":"sir20065077 - 2006 - Application of ground-water flow and solute-transport models to simulate selected ground-water management scenarios in coastal Georgia and adjacent parts of South Carolina and Florida, 2000-2100","interactions":[],"lastModifiedDate":"2017-01-12T10:02:43","indexId":"sir20065077","displayToPublicDate":"2006-04-13T00:00:00","publicationYear":"2006","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":"2006-5077","title":"Application of ground-water flow and solute-transport models to simulate selected ground-water management scenarios in coastal Georgia and adjacent parts of South Carolina and Florida, 2000-2100","language":"ENGLISH","doi":"10.3133/sir20065077","usgsCitation":"Payne, D.F., Provost, A., Painter, J.A., Abu Rumman, M., and Cherry, G.S., 2006, Application of ground-water flow and solute-transport models to simulate selected ground-water management scenarios in coastal Georgia and adjacent parts of South Carolina and Florida, 2000-2100: U.S. Geological Survey Scientific Investigations Report 2006-5077, 89 p., https://doi.org/10.3133/sir20065077.","productDescription":"89 p.","numberOfPages":"89","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":190940,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7518,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5077/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Florida, Georgia, South Carolina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.1884765625,\n              29.945415337104453\n            ],\n            [\n              -83.1884765625,\n              34.016241889667015\n            ],\n            [\n              -79.541015625,\n              34.016241889667015\n            ],\n            [\n              -79.541015625,\n              29.945415337104453\n            ],\n            [\n              -83.1884765625,\n              29.945415337104453\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a957","contributors":{"authors":[{"text":"Payne, Dorothy F.","contributorId":88825,"corporation":false,"usgs":true,"family":"Payne","given":"Dorothy","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":287382,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Provost, Alden M.","contributorId":85652,"corporation":false,"usgs":true,"family":"Provost","given":"Alden M.","affiliations":[],"preferred":false,"id":287381,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Painter, Jaime A. 0000-0001-8883-9158 jpainter@usgs.gov","orcid":"https://orcid.org/0000-0001-8883-9158","contributorId":1466,"corporation":false,"usgs":true,"family":"Painter","given":"Jaime","email":"jpainter@usgs.gov","middleInitial":"A.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true},{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287378,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Abu Rumman, Malek","contributorId":35018,"corporation":false,"usgs":true,"family":"Abu Rumman","given":"Malek","affiliations":[],"preferred":false,"id":287380,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cherry, Gregory S. 0000-0002-5567-1587 gccherry@usgs.gov","orcid":"https://orcid.org/0000-0002-5567-1587","contributorId":1567,"corporation":false,"usgs":true,"family":"Cherry","given":"Gregory","email":"gccherry@usgs.gov","middleInitial":"S.","affiliations":[{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true},{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287379,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":76565,"text":"ofr20061060 - 2006 - Two-dimensional magnetotelluric model of deep resistivity structure in the Bodie-Aurora district of California","interactions":[],"lastModifiedDate":"2012-02-02T00:14:14","indexId":"ofr20061060","displayToPublicDate":"2006-04-13T00:00:00","publicationYear":"2006","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":"2006-1060","title":"Two-dimensional magnetotelluric model of deep resistivity structure in the Bodie-Aurora district of California","docAbstract":"Introduction:  Magnetotelluric data were acquired during October 2001 by the U.S. Geological Survey (USGS) as part of a study to examine the structural nature of basins in the transition zone between the Sierra Nevada Mountains of California and the Basin and Range province of Nevada. Magnetotelluric (MT) geophysical studies assist the mapping of geologic structure and the inference of lithologic packages that are concealed beneath the Earth's surface.\r\n\r\nThe Basin and Range province has a complicated geologic history, which includes extension and compression of the Earth's crust to form the basins and ranges that blanket much of Nevada. The basins and ranges in the vicinity of this study trend northeastward and are bounded by steeply dipping strike slip faults. Interestingly, deep east-west magnetic trends occur in the aeromagnetic data of this study area indicating that the northeast-trending basins and ranges represent only thin-skinned deformation at the surface with an underlying east-west structure. To investigate this issue, MT data were acquired at seven stations in eastern California, 20 km east of Mono Lake. The purpose of this report is to present a two-dimensional apparent resistivity model of the MT data acquired for this study.","language":"ENGLISH","doi":"10.3133/ofr20061060","usgsCitation":"Sampson, J.A., 2006, Two-dimensional magnetotelluric model of deep resistivity structure in the Bodie-Aurora district of California (Online only, Version 1.0): U.S. Geological Survey Open-File Report 2006-1060, 98 p., https://doi.org/10.3133/ofr20061060.","productDescription":"98 p.","numberOfPages":"98","onlineOnly":"Y","costCenters":[],"links":[{"id":190872,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7522,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1060/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only, Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2fe4b07f02db6164d5","contributors":{"authors":[{"text":"Sampson, Jay A.","contributorId":13939,"corporation":false,"usgs":true,"family":"Sampson","given":"Jay","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":287389,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":76556,"text":"sir20065023 - 2006 - Calculation of scour depth at the Parks Highway Bridge on the Tanana River at Nenana, Alaska, using one- and two-dimensional hydraulic models","interactions":[],"lastModifiedDate":"2022-02-14T20:35:48.925333","indexId":"sir20065023","displayToPublicDate":"2006-04-13T00:00:00","publicationYear":"2006","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":"2006-5023","title":"Calculation of scour depth at the Parks Highway Bridge on the Tanana River at Nenana, Alaska, using one- and two-dimensional hydraulic models","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20065023","usgsCitation":"Langley, D.E., 2006, Calculation of scour depth at the Parks Highway Bridge on the Tanana River at Nenana, Alaska, using one- and two-dimensional hydraulic models: U.S. Geological Survey Scientific Investigations Report 2006-5023, iv, 20 p., https://doi.org/10.3133/sir20065023.","productDescription":"iv, 20 p.","numberOfPages":"24","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":190909,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":395930,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_76216.htm"},{"id":7490,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5023/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","city":"Nenana","otherGeospatial":"Parks Highway Bridge on the Tanana River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -149.13803100585938,\n              64.55729124058179\n            ],\n            [\n              -149.07108306884766,\n              64.55729124058179\n            ],\n            [\n              -149.07108306884766,\n              64.5773430898777\n            ],\n            [\n              -149.13803100585938,\n              64.5773430898777\n            ],\n            [\n              -149.13803100585938,\n              64.55729124058179\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9680","contributors":{"authors":[{"text":"Langley, Dustin E.","contributorId":91904,"corporation":false,"usgs":true,"family":"Langley","given":"Dustin","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":287367,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":76555,"text":"sir20065052 - 2006 - Simulation of various management scenarios of the Mississippi River valley alluvial aquifer in Arkansas","interactions":[],"lastModifiedDate":"2012-02-10T00:11:41","indexId":"sir20065052","displayToPublicDate":"2006-04-13T00:00:00","publicationYear":"2006","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":"2006-5052","title":"Simulation of various management scenarios of the Mississippi River valley alluvial aquifer in Arkansas","language":"ENGLISH","doi":"10.3133/sir20065052","usgsCitation":"Czarnecki, J.B., 2006, Simulation of various management scenarios of the Mississippi River valley alluvial aquifer in Arkansas (Online only): U.S. Geological Survey Scientific Investigations Report 2006-5052, 21 p., https://doi.org/10.3133/sir20065052.","productDescription":"21 p.","numberOfPages":"21","onlineOnly":"Y","costCenters":[],"links":[{"id":190908,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7259,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5052/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -92.83333333333333,32.833333333333336 ], [ -92.83333333333333,37.333333333333336 ], [ -89,37.333333333333336 ], [ -89,32.833333333333336 ], [ -92.83333333333333,32.833333333333336 ] ] ] } } ] }","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f1d36","contributors":{"authors":[{"text":"Czarnecki, John B. jczarnec@usgs.gov","contributorId":2555,"corporation":false,"usgs":true,"family":"Czarnecki","given":"John","email":"jczarnec@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":287366,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":76554,"text":"sir20065047 - 2006 - Water quality of eleven lakes in eastern and southern Arkansas from August 2004 - July 2005","interactions":[],"lastModifiedDate":"2012-02-02T00:14:14","indexId":"sir20065047","displayToPublicDate":"2006-04-13T00:00:00","publicationYear":"2006","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":"2006-5047","title":"Water quality of eleven lakes in eastern and southern Arkansas from August 2004 - July 2005","language":"ENGLISH","doi":"10.3133/sir20065047","usgsCitation":"Justus, B., 2006, Water quality of eleven lakes in eastern and southern Arkansas from August 2004 - July 2005 (Online only): U.S. Geological Survey Scientific Investigations Report 2006-5047, 77 p., https://doi.org/10.3133/sir20065047.","productDescription":"77 p.","numberOfPages":"77","onlineOnly":"Y","costCenters":[],"links":[{"id":190907,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7258,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5047/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f99ca","contributors":{"authors":[{"text":"Justus, B. G. 0000-0002-3458-9656 bjustus@usgs.gov","orcid":"https://orcid.org/0000-0002-3458-9656","contributorId":2052,"corporation":false,"usgs":true,"family":"Justus","given":"B. G.","email":"bjustus@usgs.gov","affiliations":[{"id":129,"text":"Arkansas Water Science Center","active":true,"usgs":true}],"preferred":false,"id":287365,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":76566,"text":"fs20063012 - 2006 - Improving earthquake and tsunami warnings for the Caribbean Sea, the Gulf of Mexico, and the Atlantic coast","interactions":[],"lastModifiedDate":"2012-02-02T00:14:14","indexId":"fs20063012","displayToPublicDate":"2006-04-13T00:00:00","publicationYear":"2006","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":"2006-3012","title":"Improving earthquake and tsunami warnings for the Caribbean Sea, the Gulf of Mexico, and the Atlantic coast","language":"ENGLISH","doi":"10.3133/fs20063012","usgsCitation":"McNamara, D., McCarthy, J., and Benz, H., 2006, Improving earthquake and tsunami warnings for the Caribbean Sea, the Gulf of Mexico, and the Atlantic coast (Online only, Version 1.0): U.S. Geological Survey Fact Sheet 2006-3012, 4 p., https://doi.org/10.3133/fs20063012.","productDescription":"4 p.","numberOfPages":"4","onlineOnly":"Y","costCenters":[],"links":[{"id":7523,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2006/3012/","linkFileType":{"id":5,"text":"html"}},{"id":122393,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3012.jpg"}],"edition":"Online only, Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f5c50","contributors":{"authors":[{"text":"McNamara, Dan","contributorId":32895,"corporation":false,"usgs":true,"family":"McNamara","given":"Dan","email":"","affiliations":[],"preferred":false,"id":287391,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCarthy, Jill jmccarthy@usgs.gov","contributorId":2732,"corporation":false,"usgs":true,"family":"McCarthy","given":"Jill","email":"jmccarthy@usgs.gov","affiliations":[],"preferred":true,"id":287390,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Benz, Harley","contributorId":91460,"corporation":false,"usgs":true,"family":"Benz","given":"Harley","affiliations":[],"preferred":false,"id":287392,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":76560,"text":"ofr20061072 - 2006 - Status report: USGS coal assessment of the Powder River Basin, Wyoming","interactions":[],"lastModifiedDate":"2022-01-07T21:22:14.106851","indexId":"ofr20061072","displayToPublicDate":"2006-04-13T00:00:00","publicationYear":"2006","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":"2006-1072","title":"Status report: USGS coal assessment of the Powder River Basin, Wyoming","docAbstract":"Summary:  \r\nThis publication reports on the status of the current coal assessment of the Powder River Basin (PRB) in Wyoming and Montana. This slide program was presented at the Energy Information Agency's 2006 EIA Energy Outlook and Modeling Conference in Washington, DC, on March 27, 2006. The PRB coal assessment will be the first USGS coal assessment to include estimates of both regional coal resources and reserves for an entire coal basin. Extensive CBM and additional oil and gas development, especially in the Gillette coal field, have provided an unprecedented amount of down-hole geological data. Approximately 10,000 new data points have been added to the PRB database since the last assessment (2002) which will provide a more robust evaluation of the single most productive U.S. coal basin. The Gillette coal field assessment, including the mining economic evaluation, is planned for completion by the end of 2006. 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,{"id":76548,"text":"fs20063013 - 2006 - Hawaii Forest Bird Interagency Database Project: Collecting, Understanding, and Sharing Population Data on Hawaiian Forest Birds","interactions":[],"lastModifiedDate":"2012-02-02T00:14:18","indexId":"fs20063013","displayToPublicDate":"2006-04-11T00:00:00","publicationYear":"2006","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":"2006-3013","title":"Hawaii Forest Bird Interagency Database Project: Collecting, Understanding, and Sharing Population Data on Hawaiian Forest Birds","docAbstract":"The forest birds of the Hawaiian Islands are distinguished by\r\nthe diversity of endemic forms derived from a small number of\r\nancestral colonists. However, the avifauna has been decimated\r\nby human activities both before and after Western contact. At\r\nleast 71 species or subspecies disappeared before the arrival of\r\nCapt. James Cook in 1778, and an additional 24 went extinct\r\nafter 1778, of which 11 were lost since the 1960s alone. Many\r\nof the remaining Hawaiian bird populations are declining or are\r\nin danger of extinction. Vigorous efforts to survey and monitor\r\nbird populations over the past 3 decades have generated considerable\r\ninformation from which to assess the current status of the\r\nHawaiian forest birds.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/fs20063013","usgsCitation":"Pratt, T.K., Woodworth, B., Camp, R., and Gorresen, P.M., 2006, Hawaii Forest Bird Interagency Database Project: Collecting, Understanding, and Sharing Population Data on Hawaiian Forest Birds: U.S. Geological Survey Fact Sheet 2006-3013, 4 p., https://doi.org/10.3133/fs20063013.","productDescription":"4 p.","numberOfPages":"2","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":10717,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://biology.usgs.gov/pierc/Native_Birds/Forest_birds.pdf","size":"764","linkFileType":{"id":1,"text":"pdf"}},{"id":122354,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3013.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640e89","contributors":{"authors":[{"text":"Pratt, Thane K. tkpratt@usgs.gov","contributorId":5495,"corporation":false,"usgs":true,"family":"Pratt","given":"Thane","email":"tkpratt@usgs.gov","middleInitial":"K.","affiliations":[{"id":5049,"text":"Pacific Islands Ecosys Research Center","active":true,"usgs":true}],"preferred":true,"id":287359,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Woodworth, Bethany L.","contributorId":66797,"corporation":false,"usgs":true,"family":"Woodworth","given":"Bethany L.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":287362,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Camp, Richard J.","contributorId":27392,"corporation":false,"usgs":true,"family":"Camp","given":"Richard J.","affiliations":[],"preferred":false,"id":287360,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gorresen, P. Marcos mgorresen@usgs.gov","contributorId":37020,"corporation":false,"usgs":true,"family":"Gorresen","given":"P.","email":"mgorresen@usgs.gov","middleInitial":"Marcos","affiliations":[],"preferred":false,"id":287361,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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,{"id":76542,"text":"wdrWY052 - 2006 - Water resources data, Wyoming, water year 2005; Volume 2. Ground water","interactions":[],"lastModifiedDate":"2012-02-10T00:11:43","indexId":"wdrWY052","displayToPublicDate":"2006-04-10T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WY-05-2","title":"Water resources data, Wyoming, water year 2005; Volume 2. Ground water","language":"ENGLISH","doi":"10.3133/wdrWY052","usgsCitation":"Watson, K., Woodruff, R.E., Laidlaw, G., Clark, M.L., and Miller, K.A., 2006, Water resources data, Wyoming, water year 2005; Volume 2. Ground water (Online only): U.S. Geological Survey Water Data Report WY-05-2, 186 p., https://doi.org/10.3133/wdrWY052.","productDescription":"186 p.","numberOfPages":"186","onlineOnly":"Y","costCenters":[],"links":[{"id":194967,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7484,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/2005/wdr-wy-05/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111,41 ], [ -111,45 ], [ -104,45 ], [ -104,41 ], [ -111,41 ] ] ] } } ] }","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0a2a","contributors":{"authors":[{"text":"Watson, K.R.","contributorId":79544,"corporation":false,"usgs":true,"family":"Watson","given":"K.R.","email":"","affiliations":[],"preferred":false,"id":287338,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Woodruff, R. E.","contributorId":102556,"corporation":false,"usgs":true,"family":"Woodruff","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":287340,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Laidlaw, G.A.","contributorId":31819,"corporation":false,"usgs":true,"family":"Laidlaw","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":287337,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Clark, M. L.","contributorId":19595,"corporation":false,"usgs":true,"family":"Clark","given":"M.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":287336,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Miller, K. A.","contributorId":81848,"corporation":false,"usgs":true,"family":"Miller","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":287339,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
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,{"id":76546,"text":"wdrLA051 - 2006 - Water resources data, Louisiana, water year 2005","interactions":[],"lastModifiedDate":"2019-08-27T08:27:11","indexId":"wdrLA051","displayToPublicDate":"2006-04-10T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"LA-05-1","title":"Water resources data, Louisiana, water year 2005","docAbstract":"<p><span>Water resources data for the 2005 water year for Louisiana consist of records of stage, discharge, and water quality of streams; stage and contents of lakes; and water levels and water quality of ground water. This report contains stage and discharge records for 77 stations, stage records for 92 stations, water-quality records for 54 surface-water stations and 137 wells, and water-level records for 277 wells. Also included are data for 158 crest-stage and flood-profile partial-record stations and additional water data were collected at miscellaneous sites. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Louisiana.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrLA051","usgsCitation":"Water resources data, Louisiana, water year 2005; 2006; WDR; LA-05-1; Baumann, Todd; Goree, Burl B.; Lovelace, Wendell M.; Montgomery, Pamela A.; Ross, Garron B.; Walters, David J.; Ward, Aub N.","productDescription":"909 p.","numberOfPages":"909","costCenters":[{"id":369,"text":"Louisiana Water Science Center","active":true,"usgs":true}],"links":[{"id":7488,"rank":100,"type":{"id":25,"text":"Version History"},"url":"https://pubs.usgs.gov/wdr/2005/wdr-la-05-1/versionHist.txt","text":"Version History","size":"1 KB","linkFileType":{"id":2,"text":"txt"},"description":"WDR LA-05-01 Version 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"nation\":\"USA  \"}}]}","contact":"<p>Contact Pubs Warehouse<br><a href=\"https://pubs.er.usgs.gov/contact\" target=\"_blank\" rel=\"noopener\" data-mce-href=\"../contact\">https://pubs.er.usgs.gov/<wbr><span class=\"il\">contact</span></a></p>","tableOfContents":"<ul><li>Preface</li><li>Report document page</li><li>List of surface-water stations, in downstream order, for which records are published in this volume</li><li>List of ground-water wells, by parish, for which records are published in this volume</li><li>List of discontinued surface-water discharge, elevation, or stage-only stations</li><li>List of discontinued surface-quality-water stations</li><li>Introduction</li><li>Cooperation</li><li>Summary of hydrologic conditions</li><li>Downstream order and station number</li><li>Numbering system for wells and miscellaneous sites</li><li>Special networks and programs</li><li>Explanation of stage- and water-discharge records</li><li>Explanation of water-quality records</li><li>Surface-water-quality records</li><li>Explanation of ground-water-level records</li><li>Ground-water-quality data</li><li>to USGS water data</li><li>Station records, surface water</li><li>Station records, ground-water levels</li><li>Ground-water quality</li><li>Index</li></ul>","publishedDate":"2006-01-01","revisedDate":"2019-08-23","noUsgsAuthors":false,"publicationDate":"2006-01-01","publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f12a1","contributors":{"authors":[{"text":"Baumann, Todd","contributorId":7769,"corporation":false,"usgs":true,"family":"Baumann","given":"Todd","affiliations":[],"preferred":false,"id":287352,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goree, Burl B. 0000-0003-3278-0403 bbgoree@usgs.gov","orcid":"https://orcid.org/0000-0003-3278-0403","contributorId":3508,"corporation":false,"usgs":true,"family":"Goree","given":"Burl","email":"bbgoree@usgs.gov","middleInitial":"B.","affiliations":[{"id":369,"text":"Louisiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287351,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lovelace, Wendell M.","contributorId":56750,"corporation":false,"usgs":true,"family":"Lovelace","given":"Wendell","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":287355,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Montgomery, Pamela A.","contributorId":16114,"corporation":false,"usgs":true,"family":"Montgomery","given":"Pamela","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":287353,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ross, Garron B.","contributorId":50220,"corporation":false,"usgs":true,"family":"Ross","given":"Garron","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":287354,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Walters, David J.","contributorId":102450,"corporation":false,"usgs":true,"family":"Walters","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":287356,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ward, Aub N.","contributorId":102575,"corporation":false,"usgs":true,"family":"Ward","given":"Aub","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":287357,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
]}