{"pageNumber":"961","pageRowStart":"24000","pageSize":"25","recordCount":46734,"records":[{"id":70197,"text":"sir20055035 - 2005 - Hydrogeology and trichloroethene contamination in the sea-level aquifer beneath the Logistics Center, Fort Lewis, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:14:03","indexId":"sir20055035","displayToPublicDate":"2005-03-11T00:00:00","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":"2005-5035","title":"Hydrogeology and trichloroethene contamination in the sea-level aquifer beneath the Logistics Center, Fort Lewis, Washington","docAbstract":"The U.S. Army disposed of waste trichloroethene (TCE) and other materials in the East Gate Disposal Yard near the Logistics Center on Fort Lewis, Washington, from the 1940s to the early 1970s. As a result, ground water contaminated with primarily TCE extends more than 3 miles downgradient from the East Gate Disposal Yard. The site is underlain by a complex and heterogeneous sequence of glacial and non-glacial deposits that have been broadly categorized into an upper and a lower aquifer (the latter referred to as the sea-level aquifer). TCE contamination was detected in both aquifers. This report describes an investigation by the U.S. Geological Survey (USGS) of the source, migration, and attenuation of TCE in the sea-level aquifer.\r\n\r\nA refined conceptual model for ground-water flow and contaminant migration into and through the sea-level aquifer was developed in large part from interpretation of environmental tracer data. The tracers used included stable isotopes of oxygen (18O), hydrogen (2H), and carbon (13C); the radioactive hydrogen isotope tritium (3H); common ions and redox-related analytes; chlorofluorocarbons; and sulfur hexafluoride. Tracer and TCE concentrations were determined for samples collected by the USGS from 37 wells and two surface-water sites in American Lake during 1999-2000. Ground-water levels were measured by the USGS in more than 40 wells during 2000-01, and were combined with measurements by the U.S. Army and others to create potentiometric-surface maps.\r\n\r\nLocalized ground-water flow features were identified that are of particular relevance to the migration of TCE in the study area. A ridge of ground water beneath American Lake diverts the flow of TCE-contaminated ground water in the sea-level aquifer to the west around the southern end of the lake. Tracer data provided clear evidence that American Lake is a significant source of recharge to the sea-level aquifer that has created that ridge of ground water. High ground-water altitudes at locations north and northeast of the Logistics Center combined with the ridge beneath American Lake prevent TCE contaminated water beneath the Logistics Center from migrating toward municipal water-supply wells northeast of the site.\r\n\r\nThe 1999-2000 TCE concentrations measured by the USGS at older wells screened in the sea-level aquifer were similar to those measured since 1995, but the known downgradient extent of the TCE contamination expanded nearly 2 miles after the Army installed and sampled new wells during 2003-04. Concentrations of TCE in the sea-level aquifer were consistently highest in the upper part of the aquifer throughout the plume, although TCE has spread throughout much of the thickness of the aquifer in the downgradient portions of the plume.\r\n\r\nEnvironmental tracer data indicated that the primary pathway for contaminant migration into the sea-level aquifer is through the previously identified confining unit window, an area where the predominately fine-grained confining unit is relatively coarse grained and more permeable. Other less substantial pathways for contaminant migration also were identified near the East Gate Disposal Yard and the I-5 pump-and-treat facilities. Those areas are near active pumping wells and ground-water reintroduction facilities, but there is no evidence that the contaminant migration was caused or enhanced by those activities.\r\n\r\nWithin the sea-level aquifer, TCE concentrations continue to migrate westward in the flow field strongly influenced by ground-water recharge from American Lake. Historical data are not available to definitively determine if the 5-?g/L leading edge of the current TCE plume is stable or if it is still moving downgradient. However, an evaluation of the available data combined with TCE traveltime estimates indicates that the peak TCE concentrations in the sea-level aquifer may have not yet reached the wells near the currently defined leading edge of the plume. Hypothetically, the 5-?g/L leading edge","language":"ENGLISH","doi":"10.3133/sir20055035","usgsCitation":"Dinicola, R., 2005, Hydrogeology and trichloroethene contamination in the sea-level aquifer beneath the Logistics Center, Fort Lewis, Washington: U.S. Geological Survey Scientific Investigations Report 2005-5035, 59 p.; 1 plate, 42 in. x 30 in., https://doi.org/10.3133/sir20055035.","productDescription":"59 p.; 1 plate, 42 in. x 30 in.","costCenters":[],"links":[{"id":193219,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6915,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5035/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db625210","contributors":{"authors":[{"text":"Dinicola, Richard S. 0000-0003-4222-294X dinicola@usgs.gov","orcid":"https://orcid.org/0000-0003-4222-294X","contributorId":352,"corporation":false,"usgs":true,"family":"Dinicola","given":"Richard S.","email":"dinicola@usgs.gov","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282007,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70182,"text":"sir20045115 - 2005 - Surface-water/ground-water interaction along reaches of the Snake River and Henrys Fork, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"sir20045115","displayToPublicDate":"2005-03-09T00:00:00","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":"2004-5115","title":"Surface-water/ground-water interaction along reaches of the Snake River and Henrys Fork, Idaho","docAbstract":"Declining water levels in the eastern Snake River Plain aquifer and decreases in spring discharges from the aquifer to the Snake River have spurred studies to improve understanding of the surface-water/ground-water interaction on the plain. This study was done to estimate streamflow gains and losses along specific reaches of the Snake River and Henrys Fork and to compare changes in gain and loss estimates to changes in ground-water levels over time. Data collected during this study will be used to enhance the conceptual model of the hydrologic system and to refine computer models of ground-water flow and surface-water/ground-water interactions.\r\n\r\nEstimates of streamflow gains and losses along specific subreaches of the Snake River and Henrys Fork, based on the results of five seepage studies completed during 2001?02, varied greatly across the study area, ranging from a loss estimate of 606 ft3/s in a subreach of the upper Snake River near Heise to a gain estimate of 3,450 ft3/s in a subreach of the Snake River that includes Thousand Springs. Some variations over time also were apparent in specific subreaches. Surface spring flow accounted for much of the inflow to subreaches having large gain estimates. Several subreaches alternately gained and lost streamflow during the study.\r\n\r\nChanges in estimates of streamflow gains and losses along some of the subreaches were compared with changes in water levels, measured at three different times during 2001?02, in adjacent wells. In some instances, a strong relation between changes in estimates of gains or losses and changes in ground-water levels was apparent.","language":"ENGLISH","doi":"10.3133/sir20045115","usgsCitation":"Hortness, J., and Vidmar, P., 2005, Surface-water/ground-water interaction along reaches of the Snake River and Henrys Fork, Idaho (Online only): U.S. Geological Survey Scientific Investigations Report 2004-5115, 27 p. with 3 appendices online, https://doi.org/10.3133/sir20045115.","productDescription":"27 p. with 3 appendices online","onlineOnly":"Y","costCenters":[],"links":[{"id":6885,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2004-5115/","linkFileType":{"id":5,"text":"html"}},{"id":185661,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cee4b07f02db5456f9","contributors":{"authors":[{"text":"Hortness, Jon 0000-0002-9809-2876 hortness@usgs.gov","orcid":"https://orcid.org/0000-0002-9809-2876","contributorId":3601,"corporation":false,"usgs":true,"family":"Hortness","given":"Jon","email":"hortness@usgs.gov","affiliations":[],"preferred":true,"id":281988,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vidmar, Peter","contributorId":25242,"corporation":false,"usgs":true,"family":"Vidmar","given":"Peter","affiliations":[],"preferred":false,"id":281989,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70180,"text":"sir20045254 - 2005 - Chemistry of runoff and shallow ground water at the Cattlemans Detention basin site, South Lake Tahoe, California, August 2000-November 2001","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"sir20045254","displayToPublicDate":"2005-03-09T00:00:00","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":"2004-5254","title":"Chemistry of runoff and shallow ground water at the Cattlemans Detention basin site, South Lake Tahoe, California, August 2000-November 2001","docAbstract":"A study at the Cattlemans detention basin site began in November 2000. The site is adjacent to Cold Creek in South Lake Tahoe, California. The purpose of the study is to evaluate the effects of the detention basin on ground-water discharge and changes in nutrient loads to Cold Creek, a tributary to Trout Creek and Lake Tahoe. The study is being done in cooperation with the Tahoe Engineering Division of the El Dorado County Department of Transportation. This report summarizes data collected prior to and during construction of the detention basin and includes: (1) nutrient and total suspended solid concentrations of urban runoff; (2) distribution of unconsolidated deposits; (3) direction of ground-water flow; and (4) chemistry of shallow ground water and Cold Creek.\r\n\r\nUnconsolidated deposits in the area of the detention basin were categorized into three classes: fill material consisting of a red-brown loamy sand with some gravel and an occasional cobble that was placed on top of the meadow; meadow deposits consisting of gray silt and sand with stringers of coarse sand and fine gravel; and a deeper brown to yellow-brown sand and gravel with lenses of silt and sand. Prior to construction of the detention basin, ground water flowed west-northwest across the area of the detention basin toward Cold Creek. The direction of ground-water flow did not change during construction of the detention basin. \r\n\r\nMedian concentrations of dissolved iron and chloride were 500 and 30 times higher, respectively, in ground water from the meadow deposits than dissolved concentrations in Cold Creek. Median concentration of sulfate in ground water from the meadow deposits was 0.4 milligrams per liter and dissolved oxygen was below the detection level of 0.3 milligrams per liter. The relatively high concentrations of iron and the lack of sulfate in the shallow ground water likely are caused by chemical reactions and biological microbial oxidation of organic matter in the unconsolidated deposits that result in little to no dissolved oxygen in the ground water. The higher chloride concentrations in ground water compared with Cold Creek likely are caused from the application of salt on Pioneer Trail and streets in Montgomery Estates subdivision during the winter. Runoff from these roads contributes to the recharge of the shallow ground water. The range of dissolved constituents generally was greater in the meadow deposits than in the deeper sand and gravel. \r\n\r\nAmmonia plus organic nitrogen were the dominant forms of dissolved nitrogen and concentrations ranged from 0.04 to 18 milligrams per liter as nitrogen. Highest concentration was beneath the middle of the detention basin. Nitrate plus nitrite concentrations were low (<0.33 milligrams per liter as nitrogen) throughout the area and dissolved phosphorus concentrations ranged from 0.001 to 0.34 milligrams per liter. Nitrogen and dissolved organic carbon showed no consistent pattern in the direction of ground-water flow, which suggests that, similar to iron and sulfate, local variations in the chemical and biological reactions within the meadow deposits controlled the variation in nitrogen concentrations. The gradual increase in dissolved phosphorus along the direction of ground-water flow suggest that phosphorus may be slowly dissolving into ground water. Dissolved phosphorus was consistently low in July, which may be the result of greater microbial activity in the unconsolidated deposits or from uptake by roots during the summer.","language":"ENGLISH","doi":"10.3133/sir20045254","usgsCitation":"Prudic, D.E., Sager, S.J., Wood, J.L., Henkelman, K.K., and Caskey, R.M., 2005, Chemistry of runoff and shallow ground water at the Cattlemans Detention basin site, South Lake Tahoe, California, August 2000-November 2001: U.S. Geological Survey Scientific Investigations Report 2004-5254, 48 p., https://doi.org/10.3133/sir20045254.","productDescription":"48 p.","costCenters":[],"links":[{"id":6883,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2004-5254/","linkFileType":{"id":5,"text":"html"}},{"id":185989,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dee4b07f02db5e27a7","contributors":{"authors":[{"text":"Prudic, David E. deprudic@usgs.gov","contributorId":3430,"corporation":false,"usgs":true,"family":"Prudic","given":"David","email":"deprudic@usgs.gov","middleInitial":"E.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":281980,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sager, Sienna J.","contributorId":55082,"corporation":false,"usgs":true,"family":"Sager","given":"Sienna","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":281983,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wood, James L.","contributorId":10059,"corporation":false,"usgs":true,"family":"Wood","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":281981,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Henkelman, Katherine K.","contributorId":26751,"corporation":false,"usgs":true,"family":"Henkelman","given":"Katherine","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":281982,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Caskey, Rachel M.","contributorId":74817,"corporation":false,"usgs":true,"family":"Caskey","given":"Rachel","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":281984,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70184,"text":"sir20055029 - 2005 - Verification of 1921 peak discharge at Skagit River near Concrete, Washington, using 2003 peak-discharge data","interactions":[],"lastModifiedDate":"2012-02-02T00:13:46","indexId":"sir20055029","displayToPublicDate":"2005-03-09T00:00:00","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":"2005-5029","title":"Verification of 1921 peak discharge at Skagit River near Concrete, Washington, using 2003 peak-discharge data","docAbstract":"The 1921 peak discharge at Skagit River near Concrete, Washington (U.S. Geological Survey streamflow-gaging station 12194000), was verified using peak-discharge data from the flood of October 21, 2003, the largest flood since 1921. This peak discharge is critical to determining other high discharges at the gaging station and to reliably estimating the 100-year flood, the primary design flood being used in a current flood study of the Skagit River basin.\r\n\r\nThe four largest annual peak discharges of record (1897, 1909, 1917, and 1921) were used to determine the 100-year flood discharge at Skagit River near Concrete. The peak discharge on December 13, 1921, was determined by James E. Stewart of the U.S. Geological Survey using a slope-area measurement and a contracted-opening measurement. An extended stage-discharge rating curve based on the 1921 peak discharge was used to determine the peak discharges of the three other large floods. Any inaccuracy in the 1921 peak discharge also would affect the accuracies of the three other largest peak discharges. \r\n\r\nThe peak discharge of the 1921 flood was recalculated using the cross sections and high-water marks surveyed after the 1921 flood in conjunction with a new estimate of the channel roughness coefficient (n value) based on an n-verification analysis of the peak discharge of the October 21, 2003, flood. The n value used by Stewart for his slope-area measurement of the 1921 flood was 0.033, and the corresponding calculated peak discharge was 240,000 cubic feet per second (ft3/s). Determination of a single definitive water-surface profile for use in the n-verification analysis was precluded because of considerable variation in elevations of surveyed high-water marks from the flood on October 21, 2003. Therefore, n values were determined for two separate water-surface profiles thought to bracket a plausible range of water-surface slopes defined by high-water marks. The n value determined using the flattest plausible slope was 0.024 and the corresponding recalculated discharge of the 1921 slope-area measurement was 266,000 ft3/s. The n value determined using the steepest plausible slope was 0.032 and the corresponding recalculated discharge of the 1921 slope-area measurement was 215,000 ft3/s. The two recalculated discharges were 10.8 percent greater than (flattest slope) and 10.4 percent less than (steepest slope) the 1921 peak discharge of 240,000 ft3/s. The 1921 peak discharge was not revised because the average of the two recalculated discharges (240,500 ft3/s) is only 0.2 percent greater than the 1921 peak discharge.","language":"ENGLISH","doi":"10.3133/sir20055029","usgsCitation":"Mastin, M.C., and Kresch, D., 2005, Verification of 1921 peak discharge at Skagit River near Concrete, Washington, using 2003 peak-discharge data: U.S. Geological Survey Scientific Investigations Report 2005-5029, 26 p., https://doi.org/10.3133/sir20055029.","productDescription":"26 p.","costCenters":[],"links":[{"id":6908,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5029/","linkFileType":{"id":5,"text":"html"}},{"id":186569,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e482ae4b07f02db4e7635","contributors":{"authors":[{"text":"Mastin, M. C.","contributorId":90782,"corporation":false,"usgs":true,"family":"Mastin","given":"M.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":281992,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kresch, D. L.","contributorId":52559,"corporation":false,"usgs":true,"family":"Kresch","given":"D. L.","affiliations":[],"preferred":false,"id":281991,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70161,"text":"sir20055045 - 2005 - Calibrating a tensor magnetic gradiometer using spin data","interactions":[],"lastModifiedDate":"2025-05-14T18:56:24.226938","indexId":"sir20055045","displayToPublicDate":"2005-03-04T00:00:00","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":"2005-5045","title":"Calibrating a tensor magnetic gradiometer using spin data","docAbstract":"Scalar magnetic data are often acquired to discern characteristics of geologic source materials and buried objects. It is evident that a great deal can be done with scalar data, but there are significant advantages to direct measurement of the magnetic gradient tensor in applications with nearby sources, such as unexploded ordnance (UXO). To explore these advantages, we adapted a prototype tensor magnetic gradiometer system (TMGS) and successfully implemented a data-reduction procedure. One of several critical reduction issues is the precise determination of a large group of calibration coefficients for the sensors and sensor array. To resolve these coefficients, we devised a spin calibration method, after similar methods of calibrating space-based magnetometers (Snare, 2001). The spin calibration procedure consists of three parts: (1) collecting data by slowly revolving the sensor array in the Earth?s magnetic field, (2) deriving a comprehensive set of coefficients from the spin data, and (3) applying the coefficients to the survey data. To show that the TMGS functions as a tensor gradiometer, we conducted an experimental survey that verified that the reduction procedure was effective (Bracken and Brown, in press). Therefore, because it was an integral part of the reduction, it can be concluded that the spin calibration was correctly formulated with acceptably small errors.","language":"ENGLISH","doi":"10.3133/sir20055045","usgsCitation":"Bracken, R.E., Smith, D.V., and Brown, P., 2005, Calibrating a tensor magnetic gradiometer using spin data (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2005-5045, 1 p. online; 9 p. report, https://doi.org/10.3133/sir20055045.","productDescription":"1 p. online; 9 p. report","costCenters":[],"links":[{"id":6875,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5045/","linkFileType":{"id":5,"text":"html"}},{"id":185741,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f93e0","contributors":{"authors":[{"text":"Bracken, Robert E. 0000-0001-7759-2743 rbracken@usgs.gov","orcid":"https://orcid.org/0000-0001-7759-2743","contributorId":2640,"corporation":false,"usgs":true,"family":"Bracken","given":"Robert","email":"rbracken@usgs.gov","middleInitial":"E.","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":281961,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, David V. 0000-0003-0426-4401 dvsmith@usgs.gov","orcid":"https://orcid.org/0000-0003-0426-4401","contributorId":1306,"corporation":false,"usgs":true,"family":"Smith","given":"David","email":"dvsmith@usgs.gov","middleInitial":"V.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":281960,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, Philip J.","contributorId":70483,"corporation":false,"usgs":true,"family":"Brown","given":"Philip J.","affiliations":[],"preferred":false,"id":281962,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70162,"text":"sir20055046 - 2005 - Reducing tensor magnetic gradiometer data for unexploded ordnance detection","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"sir20055046","displayToPublicDate":"2005-03-04T00:00:00","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":"2005-5046","title":"Reducing tensor magnetic gradiometer data for unexploded ordnance detection","docAbstract":"We performed a survey to demonstrate the effectiveness of a prototype tensor magnetic gradiometer system (TMGS) for detection of buried unexploded ordnance (UXO). In order to achieve a useful result, we designed a data-reduction procedure that resulted in a realistic magnetic gradient tensor and devised a simple way of viewing complicated tensor data, not only to assess the validity of the final resulting tensor, but also to preview the data at interim stages of processing. The final processed map of the surveyed area clearly shows a sharp anomaly that peaks almost directly over the target UXO. This map agrees well with a modeled map derived from dipolar sources near the known target locations. From this agreement, it can be deduced that the reduction process is valid, making the prototype TMGS a foundation for development of future systems and processes.","language":"ENGLISH","doi":"10.3133/sir20055046","usgsCitation":"Bracken, R.E., and Brown, P., 2005, Reducing tensor magnetic gradiometer data for unexploded ordnance detection (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2005-5046, 1 p. online; 10 p. report, https://doi.org/10.3133/sir20055046.","productDescription":"1 p. online; 10 p. report","costCenters":[],"links":[{"id":185828,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6876,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5046/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689f40","contributors":{"authors":[{"text":"Bracken, Robert E. 0000-0001-7759-2743 rbracken@usgs.gov","orcid":"https://orcid.org/0000-0001-7759-2743","contributorId":2640,"corporation":false,"usgs":true,"family":"Bracken","given":"Robert","email":"rbracken@usgs.gov","middleInitial":"E.","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":281963,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, Philip J.","contributorId":70483,"corporation":false,"usgs":true,"family":"Brown","given":"Philip J.","affiliations":[],"preferred":false,"id":281964,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70163,"text":"sir20045233 - 2005 - Seepage investigation and selected hydrologic data for the Escalante River drainage basin, Garfield and Kane Counties, Utah, 1909-2002","interactions":[],"lastModifiedDate":"2019-12-30T16:14:37","indexId":"sir20045233","displayToPublicDate":"2005-03-04T00:00:00","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":"2004-5233","title":"Seepage investigation and selected hydrologic data for the Escalante River drainage basin, Garfield and Kane Counties, Utah, 1909-2002","docAbstract":"<p>This report contains the results of an October 2001 seepage investigation conducted along a reach of the Escalante River in Utah extending from the U.S. Geological Survey streamflow-gaging station near Escalante to the mouth of Stevens Canyon. Discharge was measured at 16 individual sites along 15 consecutive reaches. Total reach length was about 86 miles. A reconnaissance-level sampling of water for tritium and chlorofluorcarbons was also done. In addition, hydrologic and water-quality data previously collected and published by the U.S. Geological Survey for the 2,020-square-mile Escalante River drainage basin was compiled and is presented in 12 tables. These data were collected from 64 surface-water sites and 28 springs from 1909 to 2002.</p><p>None of the 15 consecutive reaches along the Escalante River had a measured loss or gain that exceeded the measurement error. All discharge measurements taken during the seepage investigation were assigned a qualitative rating of accuracy that ranged from 5 percent to greater than 8 percent of the actual flow. Summing the potential error for each measurement and dividing by the maximum of either the upstream discharge and any tributary inflow, or the downstream discharge, determined the normalized error for a reach. This was compared to the computed loss or gain that also was normalized to the maximum discharge. A loss or gain for a specified reach is considered significant when the loss or gain (normalized percentage difference) is greater than the measurement error (normalized percentage error). The percentage difference and percentage error were normalized to allow comparison between reaches with different amounts of discharge.</p><p>The plate that accompanies the report is 36\" by 40\" and can be printed in 16 tiles, 8.5 by 11 inches. An index for the tiles is located on the lower left-hand side of the plate. Using Adobe Acrobat, the plate can be viewed independent of the report; all Acrobat functions are available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/sir20045233","collaboration":"Prepared in cooperation with the U.S. Department of the Interior, Bureau of Land Management, Grand Staircase-Escalante National Monument","usgsCitation":"Wilberg, D.E., and Stolp, B.J., 2005, Seepage investigation and selected hydrologic data for the Escalante River drainage basin, Garfield and Kane Counties, Utah, 1909-2002: U.S. Geological Survey Scientific Investigations Report 2004-5233, Report: vi, 39 p.; 1 Plate: 36.0 x 40.0 inches, https://doi.org/10.3133/sir20045233.","productDescription":"Report: vi, 39 p.; 1 Plate: 36.0 x 40.0 inches","numberOfPages":"45","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":6877,"rank":100,"type":{"id":15,"text":"Index 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,{"id":70156,"text":"sim2868 - 2005 - Water-surface elevation data and flood and floodway boundaries for the upper Yellowstone River, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"sim2868","displayToPublicDate":"2005-03-03T00:00:00","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":"2868","title":"Water-surface elevation data and flood and floodway boundaries for the upper Yellowstone River, Montana","language":"ENGLISH","doi":"10.3133/sim2868","usgsCitation":"Parrett, C., Holnbeck, S.R., and Chase, K.J., 2005, Water-surface elevation data and flood and floodway boundaries for the upper Yellowstone River, Montana (Online only): U.S. Geological Survey Scientific Investigations Map 2868, 5 sheets, 48 in. x 42 in., https://doi.org/10.3133/sim2868.","productDescription":"5 sheets, 48 in. x 42 in.","onlineOnly":"Y","costCenters":[],"links":[{"id":6873,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sim20042868/","linkFileType":{"id":5,"text":"html"}},{"id":185657,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d70","contributors":{"authors":[{"text":"Parrett, Charles","contributorId":9635,"corporation":false,"usgs":true,"family":"Parrett","given":"Charles","email":"","affiliations":[],"preferred":false,"id":281958,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holnbeck, Stephen R. 0000-0001-7313-9298 holnbeck@usgs.gov","orcid":"https://orcid.org/0000-0001-7313-9298","contributorId":1724,"corporation":false,"usgs":true,"family":"Holnbeck","given":"Stephen","email":"holnbeck@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":281957,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chase, Katherine J. 0000-0002-5796-4148 kchase@usgs.gov","orcid":"https://orcid.org/0000-0002-5796-4148","contributorId":454,"corporation":false,"usgs":true,"family":"Chase","given":"Katherine","email":"kchase@usgs.gov","middleInitial":"J.","affiliations":[{"id":685,"text":"Wyoming-Montana Water Science Center","active":false,"usgs":true}],"preferred":true,"id":281956,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70209603,"text":"70209603 - 2005 - Evaluation of groundwater movement in the Frenchman Flat CAU using geochemical and isotopic analysis","interactions":[],"lastModifiedDate":"2020-04-15T13:40:05.420066","indexId":"70209603","displayToPublicDate":"2005-03-01T08:18:22","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":295,"text":"Technical Report","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"DOE/NV/13609-36","title":"Evaluation of groundwater movement in the Frenchman Flat CAU using geochemical and isotopic analysis","docAbstract":"<div class=\"biblio-detail\"><p id=\"citation-abstract\" class=\"description\">The principal pathway for radionuclide migration from underground tests in Frenchman Flat, on the Nevada Test Site, to the accessible environment is groundwater flow. Two potential pathways for radionuclide transport via groundwater have been identified from hydrologic data: (1) radionuclide transport downward from the alluvial and volcanic aquifers into the underlying carbonate aquifer; and (2) radionuclide transport laterally to the carbonate aquifer surrounding Frenchman Flat. This report presents an evaluation of geochemical and environmental isotopic data to test these potential pathways and to identify other groundwater flowpaths in, and out of, Frenchman Flat.</p></div><div class=\"biblio-detail\"><br data-mce-bogus=\"1\"></div>","language":"English","publisher":"Desert Research Institute","doi":"10.2172/839138","usgsCitation":"Hershey, R., Thomas, J., Rose, T., Paces, J.B., Farnham, I.M., and Benedict, F.C., 2005, Evaluation of groundwater movement in the Frenchman Flat CAU using geochemical and isotopic analysis: Technical Report DOE/NV/13609-36, viii, 65 p., https://doi.org/10.2172/839138.","productDescription":"viii, 65 p.","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":477679,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://www.osti.gov/biblio/839138","text":"External Repository"},{"id":374008,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Frenchman Flat","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.09939575195312,\n              36.72017310567465\n            ],\n            [\n              -115.89889526367188,\n              36.72017310567465\n            ],\n            [\n              -115.89889526367188,\n              36.89499795802219\n            ],\n            [\n              -116.09939575195312,\n              36.89499795802219\n            ],\n            [\n              -116.09939575195312,\n              36.72017310567465\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationDate":"2005-03-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Hershey, R.","contributorId":224122,"corporation":false,"usgs":false,"family":"Hershey","given":"R.","affiliations":[],"preferred":false,"id":787103,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, J.","contributorId":224124,"corporation":false,"usgs":false,"family":"Thomas","given":"J.","affiliations":[],"preferred":false,"id":787104,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rose, T.","contributorId":224125,"corporation":false,"usgs":false,"family":"Rose","given":"T.","affiliations":[],"preferred":false,"id":787105,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Paces, James B. 0000-0002-9809-8493 jbpaces@usgs.gov","orcid":"https://orcid.org/0000-0002-9809-8493","contributorId":2514,"corporation":false,"usgs":true,"family":"Paces","given":"James","email":"jbpaces@usgs.gov","middleInitial":"B.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":787106,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Farnham, I. M.","contributorId":224126,"corporation":false,"usgs":false,"family":"Farnham","given":"I.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":787107,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Benedict, F. C.","contributorId":97068,"corporation":false,"usgs":true,"family":"Benedict","given":"F.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":787108,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70184390,"text":"70184390 - 2005 - Geochemistry and the understanding of ground-water systems","interactions":[],"lastModifiedDate":"2018-03-21T15:05:45","indexId":"70184390","displayToPublicDate":"2005-02-25T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1923,"text":"Hydrogeology Journal","active":true,"publicationSubtype":{"id":10}},"title":"Geochemistry and the understanding of ground-water systems","docAbstract":"<p><span>Geochemistry has contributed significantly to the understanding of ground-water systems over the last 50 years. Historic advances include development of the hydrochemical facies concept, application of equilibrium theory, investigation of redox processes, and radiocarbon dating. Other hydrochemical concepts, tools, and techniques have helped elucidate mechanisms of flow and transport in ground-water systems, and have helped unlock an archive of paleoenvironmental information. Hydrochemical and isotopic information can be used to interpret the origin and mode of ground-water recharge, refine estimates of time scales of recharge and ground-water flow, decipher reactive processes, provide paleohydrological information, and calibrate ground-water flow models. Progress needs to be made in obtaining representative samples. Improvements are needed in the interpretation of the information obtained, and in the construction and interpretation of numerical models utilizing hydrochemical data. The best approach will ensure an optimized iterative process between field data collection and analysis, interpretation, and the application of forward, inverse, and statistical modeling tools. Advances are anticipated from microbiological investigations, the characterization of natural organics, isotopic fingerprinting, applications of dissolved gas measurements, and the fields of reaction kinetics and coupled processes. A thermodynamic perspective is offered that could facilitate the comparison and understanding of the multiple physical, chemical, and biological processes affecting ground-water systems.</span></p>","language":"English","publisher":"Springer-Verlag","doi":"10.1007/s10040-004-0429-y","usgsCitation":"Glynn, P.D., and Plummer, N., 2005, Geochemistry and the understanding of ground-water systems: Hydrogeology Journal, v. 13, no. 1, p. 263-287, https://doi.org/10.1007/s10040-004-0429-y.","productDescription":"26 p. ","startPage":"263","endPage":"287","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337065,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"1","noUsgsAuthors":false,"publicationDate":"2005-02-25","publicationStatus":"PW","scienceBaseUri":"58c12640e4b014cc3a3d34ca","contributors":{"authors":[{"text":"Glynn, Pierre D. 0000-0001-8804-7003 pglynn@usgs.gov","orcid":"https://orcid.org/0000-0001-8804-7003","contributorId":2141,"corporation":false,"usgs":true,"family":"Glynn","given":"Pierre","email":"pglynn@usgs.gov","middleInitial":"D.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":681277,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":681278,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70113,"text":"ofr20051042 - 2005 - Construction, Geologic, and Hydrologic Data from Five Exploratory Wells on Rota, Commonwealth of the Northern Mariana Islands, 1999","interactions":[],"lastModifiedDate":"2012-03-08T17:16:18","indexId":"ofr20051042","displayToPublicDate":"2005-02-24T00:00:00","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":"2005-1042","title":"Construction, Geologic, and Hydrologic Data from Five Exploratory Wells on Rota, Commonwealth of the Northern Mariana Islands, 1999","docAbstract":"Rota is the southernmost of the 14 small islands that make up the Commonwealth of the Northern Mariana Islands. Reduced springflow at Matan Hanom and As Onan springs occurred during a drought associated with the 1997-98 El Nino. Water from the two developed springs constituted the only municipal water source for the island at that time. In April 1998, reduced water supplies forced the Commonwealth Utilities Corporation to restrict water service in the principal villages of Songsong and Sinapalu for the duration of the dry season.\r\n\r\nIn 1999, Five exploratory wells, EX-1 through EX-5 (CUC wells SP-MW1, SP-1, -2, -3, and SP-MW2), were drilled in the Sinapalu region of Rota to (1) assess the availability of fresh ground-water resources in an area where no other well information were available, and (2) to provide a new water source to help mitigate the impacts of drought associated with recurring El Nino weather events. The wells penetrated mainly light colored (dirty white to brownish), fragmental limestones containing abundant coral remains.\r\n\r\nSustained-rate, recovery, and step-drawdown aquifer tests were attempted at each of the five exploratory wells to estimate aquifer properties in the vicinity of the wells and to assess the potential for new water sources. At wells EX-1 (CUC well SPMW1) and EX-5 (CUC well SP-MW2), attempts to conduct sustained-rate aquifer tests resulted in excessive drawdown to the pump intakes in the vicinity of the wells. At well EX-2 (CUC well SP-1), the maximum drawdown measured in the pumped well was 3.93 ft during 8 days of sustained pumping at an average rate of 187 gal/min. At well EX-3 (CUC well SP-2), the maximum drawdown measured in the pumped well was 2.31 ft during 8 days of sustained pumping at an average rate of 108 gal/min, and at well EX-4 (CUC well SP-3), the maximum drawdown measured in the pumped well was 3.27 ft during 8 days of sustained pumping at an average rate of 139 gal/min. Specific conductance at the end of 8 days of pumping was 403, 358, and 445 ?S/cm at well EX-2, EX-3, and EX-4 (CUC wells SP-1, -2, and -3), respectively.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr20051042","collaboration":"Prepared in cooperation with the Commonwealth Utilities Corporation, Commonwealth of the Northern Mariana Islands","usgsCitation":"Carruth, R., 2005, Construction, Geologic, and Hydrologic Data from Five Exploratory Wells on Rota, Commonwealth of the Northern Mariana Islands, 1999: U.S. Geological Survey Open-File Report 2005-1042, Report: v, 40 p.; 12 Tables; 10 Appendices, https://doi.org/10.3133/ofr20051042.","productDescription":"Report: v, 40 p.; 12 Tables; 10 Appendices","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":193284,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6825,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1042/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 145.08333333333334,14.083333333333334 ], [ 145.08333333333334,14.25 ], [ 145.33333333333334,14.25 ], [ 145.33333333333334,14.083333333333334 ], [ 145.08333333333334,14.083333333333334 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698462","contributors":{"authors":[{"text":"Carruth, Rob 0000-0001-7008-2927 rlcarr@usgs.gov","orcid":"https://orcid.org/0000-0001-7008-2927","contributorId":1162,"corporation":false,"usgs":true,"family":"Carruth","given":"Rob","email":"rlcarr@usgs.gov","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":false,"id":281877,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70122,"text":"sir20055037 - 2005 - Mercury accumulation by lower trophic-level organisms in lentic systems within the Guadalupe River watershed, California","interactions":[],"lastModifiedDate":"2020-02-03T19:52:42","indexId":"sir20055037","displayToPublicDate":"2005-02-24T00:00:00","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":"2005-5037","title":"Mercury accumulation by lower trophic-level organisms in lentic systems within the Guadalupe River watershed, California","docAbstract":"The water columns of four reservoirs (Almaden, Calero, Guadalupe and Lexington Reservoirs) and an abandoned quarry pit filled by Alamitos Creek drainage for recreational purposes (Lake Almaden) were sampled on September 14 and 15, 2004 to provide the first measurements of mercury accumulation by phytoplankton and zooplankton in lentic systems (bodies of standing water, as in lakes and reservoirs) within the Guadalupe River watershed, California. Because of widespread interest in ecosystem effects associated with historic mercury mining within and downgradient of the Guadalupe Riverwatershed, transfer of mercury to lower trophic-level organisms was examined. The propensity of mercury to bioaccumulate, particularly in phytoplankton and zooplankton at the base of the food web, motivated this attempt to provide information in support of developing trophic-transfer and solute-transport models for the watershed, and hence in support of subsequent evaluation of load-allocation strategies. Both total mercury and methylmercury were examined in these organisms. \r\n\r\nDuring a single sampling event, replicate samples from the reservoir water column were collected and processed for dissolved-total mercury, dissolved-methylmercury, phytoplankton mercury speciation, phytoplankton taxonomy and biomass, zooplankton mercury speciation, and zooplankton taxonomy and biomass. The timing of this sampling event was coordinated with sampling and analysis of fish from these five water bodies, during a period of the year when vertical stratification in the reservoirs generates a primary source of methylmercury to the watershed. Ancillary data, including dissolved organic carbon and trace-metal concentrations as well as vertical profiles of temperature, dissolved oxygen, specific conductance and pH, were gathered to provide a water-quality framework from which to compare the results for mercury. This work, in support of the Guadalupe River Mercury Total Maximum Daily Load (TMDL) Study, provides the first measurements of mercury trophic transfer through planktonic communities in this watershed. It is worth reemphasizing that this data set represents a single ?snap shot? of conditions in water bodies within the Guadalupe River watershed to: (1) fill gaps in trophic transfer information, and (2) provide a scientific basis for future process-based studies with enhanced temporal and spatial coverage. This electronic document was unconventionally formatted to enhance the accessibility of information to a wide range of interest groups.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055037","usgsCitation":"Kuwabara, J.S., Topping, B.R., Moon, G.E., Husby, P., Lincoff, A., Carter, J.L., and Croteau, M., 2005, Mercury accumulation by lower trophic-level organisms in lentic systems within the Guadalupe River watershed, California: U.S. Geological Survey Scientific Investigations Report 2005-5037, 59 p., https://doi.org/10.3133/sir20055037.","productDescription":"59 p.","onlineOnly":"Y","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":191699,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6834,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5037/","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","country":"United States","state":"California","otherGeospatial":"Guadalupe River watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.18170166015625,\n              37.801103690609615\n            ],\n            [\n              -121.35498046875,\n              37.801103690609615\n            ],\n            [\n              -121.35498046875,\n              38.24249456800328\n            ],\n            [\n              -122.18170166015625,\n              38.24249456800328\n            ],\n            [\n              -122.18170166015625,\n              37.801103690609615\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db624622","contributors":{"authors":[{"text":"Kuwabara, James S. 0000-0003-2502-1601 kuwabara@usgs.gov","orcid":"https://orcid.org/0000-0003-2502-1601","contributorId":3374,"corporation":false,"usgs":true,"family":"Kuwabara","given":"James","email":"kuwabara@usgs.gov","middleInitial":"S.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":281910,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Topping, Brent R. 0000-0002-7887-4221 btopping@usgs.gov","orcid":"https://orcid.org/0000-0002-7887-4221","contributorId":1484,"corporation":false,"usgs":true,"family":"Topping","given":"Brent","email":"btopping@usgs.gov","middleInitial":"R.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":281908,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moon, Gerald E.","contributorId":11288,"corporation":false,"usgs":true,"family":"Moon","given":"Gerald","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":281911,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Husby, Peter","contributorId":35405,"corporation":false,"usgs":true,"family":"Husby","given":"Peter","email":"","affiliations":[],"preferred":false,"id":281914,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lincoff, Andrew","contributorId":29076,"corporation":false,"usgs":true,"family":"Lincoff","given":"Andrew","email":"","affiliations":[],"preferred":false,"id":281913,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Carter, James L. 0000-0002-0104-9776 jlcarter@usgs.gov","orcid":"https://orcid.org/0000-0002-0104-9776","contributorId":3278,"corporation":false,"usgs":true,"family":"Carter","given":"James","email":"jlcarter@usgs.gov","middleInitial":"L.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":281909,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Croteau, Marie-Noële","contributorId":22863,"corporation":false,"usgs":true,"family":"Croteau","given":"Marie-Noële","affiliations":[],"preferred":false,"id":281912,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70211109,"text":"70211109 - 2005 - Reply to “Commentary: Assessment of past infiltration fluxes through Yucca Mountain on the basis of the secondary mineral record—Is it a viable methodology?” by Y.V. Dublyansky and S.Z. Smirnov","interactions":[],"lastModifiedDate":"2020-07-14T22:09:44.951946","indexId":"70211109","displayToPublicDate":"2005-02-23T16:46:42","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2233,"text":"Journal of Contaminant Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Reply to “Commentary: Assessment of past infiltration fluxes through Yucca Mountain on the basis of the secondary mineral record—Is it a viable methodology?” by Y.V. Dublyansky and S.Z. Smirnov","docAbstract":"<p>Many of the comments by Dublyansky and Smirnov (2005) on Marshall et al. (2003) reflect a longstanding debate over the origin of secondary calcite and opal deposits found in cavities and on fracture surfaces at Yucca Mountain, Nevada, site of a proposed high-level nuclear waste repository (US Department of Energy, 2001). These comments require consideration of data and interpretations beyond the scope of Marshall et al. (2003). Dublyansky et al. (2004) and Dublyansky et al. (2005) also have commented on papers published by Whelan et al. (2002) and Wilson et al. (2003), and we will refer to the replies to those comments (Whelan et al., 2004, Wilson and Cline, 2005) in addressing the comments that go beyond the scope of Marshall et al. (2003).</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jconhyd.2005.01.002","usgsCitation":"Marshall, B.D., Neymark, L., and Peterman, Z.E., 2005, Reply to “Commentary: Assessment of past infiltration fluxes through Yucca Mountain on the basis of the secondary mineral record—Is it a viable methodology?” by Y.V. Dublyansky and S.Z. Smirnov: Journal of Contaminant Hydrology, v. 77, no. 3, p. 219-224, https://doi.org/10.1016/j.jconhyd.2005.01.002.","productDescription":"6 p.","startPage":"219","endPage":"224","costCenters":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":376394,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Yucca Mountain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.48254394531249,\n              36.91352904330221\n            ],\n            [\n              -116.43602371215822,\n              36.91352904330221\n            ],\n            [\n              -116.43602371215822,\n              36.95757376878687\n            ],\n            [\n              -116.48254394531249,\n              36.95757376878687\n            ],\n            [\n              -116.48254394531249,\n              36.91352904330221\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"77","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Marshall, Brian D. 0000-0002-8093-0093 bdmarsha@usgs.gov","orcid":"https://orcid.org/0000-0002-8093-0093","contributorId":520,"corporation":false,"usgs":true,"family":"Marshall","given":"Brian","email":"bdmarsha@usgs.gov","middleInitial":"D.","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":792791,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neymark, Leonid A. 0000-0003-4190-0278 lneymark@usgs.gov","orcid":"https://orcid.org/0000-0003-4190-0278","contributorId":140338,"corporation":false,"usgs":true,"family":"Neymark","given":"Leonid A.","email":"lneymark@usgs.gov","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":792792,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peterman, Zell E. 0000-0002-5694-8082 peterman@usgs.gov","orcid":"https://orcid.org/0000-0002-5694-8082","contributorId":167699,"corporation":false,"usgs":true,"family":"Peterman","given":"Zell","email":"peterman@usgs.gov","middleInitial":"E.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":792793,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70105,"text":"sir20045296 - 2005 - Geological, hydrological, and biological issues related to the proposed development of a park at the confluence of the Los Angeles River and the Arroyo Seco, Los Angeles County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:14:04","indexId":"sir20045296","displayToPublicDate":"2005-02-22T00:00:00","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":"2004-5296","title":"Geological, hydrological, and biological issues related to the proposed development of a park at the confluence of the Los Angeles River and the Arroyo Seco, Los Angeles County, California","docAbstract":"A new park is being considered for the confluence of the Los Angeles River and the Arroyo Seco in Los Angeles County, California. Components of the park development may include creation of a temporary lake on the Los Angeles River, removal of channel lining along part of the Arroyo Seco, restoration of native plants, creation of walking paths, and building of facilities such as a boat ramp and a visitor center. This report, prepared in cooperation with the Mountains Recreation and Conservancy Authority, delineates the geological, hydrological, and biological issues that may have an impact on the park development or result from development at the confluence, and identifies a set a tasks to help address these science issues.\r\n\r\nGeologic issues of concern relate to surface faulting, earthquake ground motions, liquefaction, landsliding, and induced seismicity. Hydrologic issues of concern relate to the hydraulics and water quality of both surface water and ground water. Biological issues of concern include colonization-extinction dynamics, wildlife corridors, wildlife reintroduction, non-native species, ecotoxicology, and restoration of local habitat and ecology. Potential tasks include (1) basic data collection and follow-up monitoring, and (2) statistical and probabilistic analyses and simulation modeling of the seismic, hydraulic, and ecological processes that may have the greatest impact on the park. The science issues and associated tasks delineated for the proposed confluence park will also have transfer value for river restoration in other urban settings.","language":"ENGLISH","doi":"10.3133/sir20045296","usgsCitation":"Land, M., Trenham, P.C., Ponti, D.J., Reichard, E.G., Tinsley, J., Warrick, J., and Meyer, R.W., 2005, Geological, hydrological, and biological issues related to the proposed development of a park at the confluence of the Los Angeles River and the Arroyo Seco, Los Angeles County, California (Online only): U.S. Geological Survey Scientific Investigations Report 2004-5296, 56 p., https://doi.org/10.3133/sir20045296.","productDescription":"56 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":192998,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6791,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2004-5296/","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db68744f","contributors":{"authors":[{"text":"Land, Michael 0000-0001-5141-0307","orcid":"https://orcid.org/0000-0001-5141-0307","contributorId":56613,"corporation":false,"usgs":true,"family":"Land","given":"Michael","affiliations":[],"preferred":false,"id":281867,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trenham, Peter C.","contributorId":11710,"corporation":false,"usgs":true,"family":"Trenham","given":"Peter","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":281866,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ponti, Daniel J. 0000-0002-2437-5144 dponti@usgs.gov","orcid":"https://orcid.org/0000-0002-2437-5144","contributorId":1020,"corporation":false,"usgs":true,"family":"Ponti","given":"Daniel","email":"dponti@usgs.gov","middleInitial":"J.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":281862,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Reichard, Eric G. 0000-0002-7310-3866 egreich@usgs.gov","orcid":"https://orcid.org/0000-0002-7310-3866","contributorId":1207,"corporation":false,"usgs":true,"family":"Reichard","given":"Eric","email":"egreich@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":281863,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Tinsley, John C. III jtinsley@usgs.gov","contributorId":3266,"corporation":false,"usgs":true,"family":"Tinsley","given":"John C.","suffix":"III","email":"jtinsley@usgs.gov","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":281865,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Warrick, Jonathan A. jwarrick@usgs.gov","contributorId":1904,"corporation":false,"usgs":true,"family":"Warrick","given":"Jonathan A.","email":"jwarrick@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":281864,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Meyer, Robert W.","contributorId":69601,"corporation":false,"usgs":true,"family":"Meyer","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":281868,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70085,"text":"wdrVA042 - 2005 - Water resources data, Virginia, water year 2004 volume 2.  Ground-water-level and ground-water-quality records","interactions":[],"lastModifiedDate":"2012-02-02T00:14:03","indexId":"wdrVA042","displayToPublicDate":"2005-02-16T00:00:00","publicationYear":"2005","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":"VA-04-2","title":"Water resources data, Virginia, water year 2004 volume 2.  Ground-water-level and ground-water-quality records","docAbstract":"Water-resources data for the 2004 water year for Virginia consist of records of water levels and water quality of ground-water wells. This report (Volume 2. Ground-Water-Level and Ground-Water-Quality Records) contains water levels at 346 observation wells and water quality at 40 wells. Locations of these wells are shown on figures 4 through 9. The data in this report represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Virginia.","language":"ENGLISH","doi":"10.3133/wdrVA042","usgsCitation":"White, R.K., Powell, E.D., Guyer, J.R., and Owens, J.A., 2005, Water resources data, Virginia, water year 2004 volume 2.  Ground-water-level and ground-water-quality records (Online only): U.S. Geological Survey Water Data Report VA-04-2, 418 p., https://doi.org/10.3133/wdrVA042.","productDescription":"418 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":193182,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6784,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/2004/WDR-VA-04-2/","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688d15","contributors":{"authors":[{"text":"White, Roger K.","contributorId":19624,"corporation":false,"usgs":true,"family":"White","given":"Roger","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":281828,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Powell, Eugene D.","contributorId":80309,"corporation":false,"usgs":true,"family":"Powell","given":"Eugene","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":281831,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Guyer, Joel R.","contributorId":47446,"corporation":false,"usgs":true,"family":"Guyer","given":"Joel","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":281829,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Owens, Joseph A.","contributorId":73690,"corporation":false,"usgs":true,"family":"Owens","given":"Joseph","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":281830,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70081,"text":"ofr20051052 - 2005 - Virginia aeromagnetic and gravity maps and data: A web site for distribution of data","interactions":[],"lastModifiedDate":"2023-04-05T19:47:33.251536","indexId":"ofr20051052","displayToPublicDate":"2005-02-15T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1052","title":"Virginia aeromagnetic and gravity maps and data: A web site for distribution of data","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051052","usgsCitation":"Snyder, S.L., 2005, Virginia aeromagnetic and gravity maps and data: A web site for distribution of data: U.S. Geological Survey Open-File Report 2005-1052, HTML 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,{"id":70083,"text":"wdrIA041 - 2005 - Water resources data, Iowa water year 2004, volume 1: surface water and precipitation","interactions":[],"lastModifiedDate":"2016-02-01T10:23:13","indexId":"wdrIA041","displayToPublicDate":"2005-02-15T00:00:00","publicationYear":"2005","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":"IA-04-1","title":"Water resources data, Iowa water year 2004, volume 1: surface water and precipitation","docAbstract":"<p>This volume of the annual hydrologic data report of Iowa is one of a series of annual reports that document hydrologic data gathered from the U.S. Geological Survey.s surface- and ground-water data-collection networks in each State, Puerto Rico, and the Trust Territories. These records of streamflow, ground-water levels, and quality of water provide the hydrologic information needed by local, State, and Federal agencies, and the private sector for developing and managing our Nation.s land and water resources.</p>\n<p>This report is the culmination of a concerted effort by dedicated personnel of the U.S. Geological Survey who collected, compiled, analyzed, verified, and organized the data, and who typed, edited, and assembled the report. 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 \"}}]}","tableOfContents":"<p>Preface<br />Surface-water stations, in downstream order, for which records&nbsp;are published in this volume<br />Discontinued surface-water discharge or stage-only stations<br />Discontinued surface-water quality stations<br />Introduction<br />Cooperation<br />Summary of hydrologic conditions<br />&nbsp; &nbsp; &nbsp;Precipitation<br />Special networks and programs<br />Explanation of Stage- and Water Discharge Records<br />&nbsp; &nbsp; &nbsp;Discontinued surface-water<br />&nbsp; &nbsp; &nbsp;Data Presentation<br />&nbsp; &nbsp; &nbsp;Identifying Estimated Daily Discharge<br />&nbsp; &nbsp; &nbsp;Accuracy of Field Data and Computed Results<br />&nbsp; &nbsp; &nbsp;Other Data Records Available<br />Explanation of Precipitation Records<br />&nbsp; &nbsp; &nbsp;Data Collection and Computation<br />&nbsp; &nbsp; &nbsp;Data Presentation<br />Explanation of Water-Quality Records<br />&nbsp; &nbsp; &nbsp;Collection and Examination of Data<br />&nbsp; &nbsp; &nbsp;Water Analysis<br />Surface-Water-Quality Records<br />&nbsp; &nbsp; &nbsp;Classification of Records<br />&nbsp; &nbsp; &nbsp;Accuracy of the Records<br />&nbsp; &nbsp; &nbsp;Arrangement of Records<br />&nbsp; &nbsp; &nbsp;On-Site Measurements and Sample Collection<br />&nbsp; &nbsp; &nbsp;Water Temperature<br />&nbsp; &nbsp; &nbsp;Sediment<br />&nbsp; &nbsp; &nbsp;Laboratory Measurements<br />&nbsp; &nbsp; &nbsp;Data Presentation<br />&nbsp; &nbsp; &nbsp;Remark Codes<br />&nbsp; &nbsp; &nbsp;Water-Quality Control Data<br />&nbsp; &nbsp; &nbsp;Blank Samples<br />&nbsp; &nbsp; &nbsp;Reference Samples<br />&nbsp; &nbsp; &nbsp;Replicate Samples<br />&nbsp; &nbsp; &nbsp;Spike Samples<br />Access to USGS Water Data<br />Definition of Terms<br />Techniques of Water-Resources Investigations of the U.S. Geological Survey.<br />Surface water records<br />Crest-stage partial-record stations<br />Index</p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f0e4b07f02db5ee125","contributors":{"authors":[{"text":"Nalley, Greg M. 0000-0002-0151-0219","orcid":"https://orcid.org/0000-0002-0151-0219","contributorId":69650,"corporation":false,"usgs":true,"family":"Nalley","given":"Greg","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":281825,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gorman, Joseph G.","contributorId":52665,"corporation":false,"usgs":true,"family":"Gorman","given":"Joseph G.","affiliations":[],"preferred":false,"id":281823,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goodrich, Robert D.","contributorId":54293,"corporation":false,"usgs":true,"family":"Goodrich","given":"Robert","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":281824,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, Von E.","contributorId":102551,"corporation":false,"usgs":true,"family":"Miller","given":"Von","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":281827,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Housel, Kevin S.","contributorId":80754,"corporation":false,"usgs":true,"family":"Housel","given":"Kevin","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":281826,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70080,"text":"sir20055017 - 2005 - Evaluation of drainage-area ratio method used to estimate streamflow for the Red River of the North Basin, North Dakota and Minnesota","interactions":[],"lastModifiedDate":"2018-03-07T16:30:27","indexId":"sir20055017","displayToPublicDate":"2005-02-15T00:00:00","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":"2005-5017","title":"Evaluation of drainage-area ratio method used to estimate streamflow for the Red River of the North Basin, North Dakota and Minnesota","docAbstract":"<p>The drainage-area ratio method commonly is used to estimate streamflow for sites where no streamflow data were collected. To evaluate the validity of the drainage-area ratio method and to determine if an improved method could be developed to estimate streamflow, a multiple-regression technique was used to determine if drainage area, main channel slope, and precipitation were significant variables for estimating streamflow in the Red River of the North Basin. A separate regression analysis was performed for streamflow for each of three seasons-- winter, spring, and summer. Drainage area and summer precipitation were the most significant variables. However, the regression equations generally overestimated streamflows for North Dakota stations and underestimated streamflows for Minnesota stations. To correct the bias in the residuals for the two groups of stations, indicator variables were included to allow both the intercept and the coefficient for the logarithm of drainage area to depend on the group. Drainage area was the only significant variable in the revised regression equations. The exponents for the drainage-area ratio were 0.85 for the winter season, 0.91 for the spring season, and 1.02 for the summer season.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055017","usgsCitation":"Emerson, D.G., Vecchia, A.V., and Dahl, A.L., 2005, Evaluation of drainage-area ratio method used to estimate streamflow for the Red River of the North Basin, North Dakota and Minnesota (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5017, iv, 13 p., https://doi.org/10.3133/sir20055017.","productDescription":"iv, 13 p.","onlineOnly":"Y","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":185929,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6780,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5017/","linkFileType":{"id":5,"text":"html"}},{"id":352316,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5017/pdf/sir20055017.pdf"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 0.0025,46 ], [ 0.0025,49 ], [ 0.0025,49 ], [ 0.0025,46 ], [ 0.0025,46 ] ] ] } } ] }","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fae36","contributors":{"authors":[{"text":"Emerson, Douglas G.","contributorId":40579,"corporation":false,"usgs":true,"family":"Emerson","given":"Douglas","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":281819,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vecchia, Aldo V. 0000-0002-2661-4401","orcid":"https://orcid.org/0000-0002-2661-4401","contributorId":41810,"corporation":false,"usgs":true,"family":"Vecchia","given":"Aldo","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":281820,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dahl, Ann L.","contributorId":15278,"corporation":false,"usgs":true,"family":"Dahl","given":"Ann","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":281818,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70069,"text":"sir20045295 - 2005 - Effects of decreased ground-water withdrawal on ground-water levels and chloride concentrations in Camden County, Georgia, and ground-water levels in Nassau County, Florida, from September 2001 to May 2003","interactions":[],"lastModifiedDate":"2017-01-17T17:13:30","indexId":"sir20045295","displayToPublicDate":"2005-02-11T00:00:00","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":"2004-5295","title":"Effects of decreased ground-water withdrawal on ground-water levels and chloride concentrations in Camden County, Georgia, and ground-water levels in Nassau County, Florida, from September 2001 to May 2003","docAbstract":"During October 2002, the Durango Paper Company formerly Gillman Paper Company) in St. Marys, Georgia, shut down paper-mill operations; the shutdown resulted in decreased ground-water withdrawal in Camden County by 35.6 million gallons per day. The decrease in withdrawal resulted in water-level rise in wells completed in the Floridan aquifer system and the overlying surficial and Brunswick aquifer systems; many wells in the St. Marys area flowed for the first time since the mill began operations during 1941. \r\n\r\nPumping at the mill resulted in the development of a cone of depression that coalesced with a larger adjacent cone of depression at Fernandina Beach, Florida. Since closure of the mill, the cone at St. Marys is no longer present, although the cone still exists at Fernandina Beach, Florida. Historical water-level data from the production wells at the mill indicate that the pumping water level ranged from 68 to 235 feet (ft) below North American Vertical Datum of 1988 (NAVD 88) and averaged about 114 ft when the mill was operating. Since the shutdown, it is estimated that water levels at the mill have risen about 140 ft and are now at about 30 ft above NAVD 88. The water-level rise in wells in outlying areas in Camden County was less pronounced and ranged from about 5 to 10 ft above NAVD 88. Because of the regional upward water-level trend in the Upper Floridan aquifer that started during 1999\u00132000 in most of the coastal area, combined with a steeper upward trend beginning during October 2002, it was not possible to determine if the 5\u001310 ft rise in water levels in wells away from St. Marys was due to the mill closure. In addition to water-level rise of 22\u001326 ft in the Floridan aquifer system, water-level rises in the overlying surficial and Brunswick aquifer systems at St. Marys after the shutdown indicate upward leakage of water. Water levels had stabilized in the confined surficial and Upper and Lower Floridan aquifers by April\u0013May 2003; however, the water level in the upper Brunswick aquifer was still rising as of May 2003.\r\n\r\nChloride concentrations in the Upper Floridan aquifer in Camden County do not exceed the State and Federal drinking-water standard of 250 milligrams per liter (mg/L). With the exception of three wells located at St. Marys, all of the wells sampled during this study (from September 2002 to May 2003) had chloride concentrations ranging from 30 to 50 mg/L, which are considered within background levels for the Upper Floridan aquifer in this area. The three wells\u0014two at the Durango Paper Company and the other an old unused City of St. Marys well\u0014had chloride concentrations that ranged from 74 to 175 mg/L, which are above the background level, but were still below the 250-mg/L drinking-water standard. The source has not been determined for the elevated chloride concentration in these wells; the chloride concentration in one of the wells has decreased slightly since the paper-mill shutdown. Chloride concentrations throughout Camden County showed little change after the paper-mill shutdown.","language":"ENGLISH","doi":"10.3133/sir20045295","usgsCitation":"Peck, M., McFadden, K.W., and Leeth, D.C., 2005, Effects of decreased ground-water withdrawal on ground-water levels and chloride concentrations in Camden County, Georgia, and ground-water levels in Nassau County, Florida, from September 2001 to May 2003 (Online only): U.S. Geological Survey Scientific Investigations Report 2004-5295, vi, 31 p., https://doi.org/10.3133/sir20045295.","productDescription":"vi, 31 p.","onlineOnly":"Y","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":186487,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6740,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2004-5295/","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","country":"United States","state":"Florida, Georgia","county":"Camden County, Nassau County","otherGeospatial":"Brunswick aquifer system, Floridan aquifer system","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.15576171875,\n              30.56226095049944\n            ],\n            [\n              -82.15576171875,\n              31.12819929911196\n            ],\n            [\n              -81.36474609375,\n              31.12819929911196\n            ],\n            [\n              -81.36474609375,\n              30.56226095049944\n            ],\n            [\n              -82.15576171875,\n              30.56226095049944\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af2e4b07f02db6918fd","contributors":{"authors":[{"text":"Peck, Michael F. mfpeck@usgs.gov","contributorId":1467,"corporation":false,"usgs":true,"family":"Peck","given":"Michael F.","email":"mfpeck@usgs.gov","affiliations":[],"preferred":false,"id":281805,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McFadden, Keith W. keithmc@usgs.gov","contributorId":1446,"corporation":false,"usgs":true,"family":"McFadden","given":"Keith","email":"keithmc@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":281804,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leeth, David C. cleeth@usgs.gov","contributorId":1403,"corporation":false,"usgs":true,"family":"Leeth","given":"David","email":"cleeth@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":281803,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70073,"text":"wdrIA042 - 2005 - Water resources data, Iowa, water year 2004, volume 2: ground water and quality of precipitation","interactions":[],"lastModifiedDate":"2016-02-01T10:29:18","indexId":"wdrIA042","displayToPublicDate":"2005-02-11T00:00:00","publicationYear":"2005","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":"IA-04-2","title":"Water resources data, Iowa, water year 2004, volume 2: ground water and quality of precipitation","docAbstract":"<p>Water resources data for Iowa for the 2004 water year consists of records of ground water levels and water quality of ground-water wells. This report volume contains water-level records for 163 ground-water observation wells; water-quality data for 147 municipal wells; and precipitation-quality data for 2 precipitation sites.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrIA042","collaboration":"Prepared in cooperation with the Iowa Department of Natural Resources-Iowa Geological Survey, Iowa Department of Transportation, and Federal agencies","usgsCitation":"Nalley, G., Linhart, S.M., Littin, G.R., Miller, V., and Housel, K., 2005, Water resources data, Iowa, water year 2004, volume 2: ground water and quality of precipitation: U.S. Geological Survey Water Data Report IA-04-2, xii, 132 p., https://doi.org/10.3133/wdrIA042.","productDescription":"xii, 132 p.","onlineOnly":"Y","additionalOnlineFiles":"N","temporalStart":"2003-10-01","costCenters":[{"id":351,"text":"Iowa Water Science 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 \"}}]}","tableOfContents":"<p>Preface<br />&nbsp; &nbsp; &nbsp;Figures<br />&nbsp; &nbsp; &nbsp;Ground-Water Wells, by County, for which Records are Published in this Volume<br />Introduction<br />Cooperation<br />Summary of Hydrologic Conditions<br />&nbsp; &nbsp; &nbsp;Precipitation<br />&nbsp; &nbsp; &nbsp;Ground-Water-Level Observation Network<br />&nbsp; &nbsp; &nbsp;Ground-Water Quality<br />&nbsp; &nbsp; &nbsp;Ground-Water Monitoring Network<br />Numbering system for wells and miscellaneous sites<br />Special Networks and Programs<br />Explanation of Ground-Water-Level Records<br />&nbsp; &nbsp; &nbsp;Data Collection and Computation<br />&nbsp; &nbsp; &nbsp;Data Presentation<br />Explanation of precipitation records<br />&nbsp; &nbsp; &nbsp;Data Collection and Computation<br />&nbsp; &nbsp; &nbsp;Data Presentation<br />Explanation of Water-Quality Records<br />&nbsp; &nbsp; &nbsp;Collection and Examination of Data<br />&nbsp; &nbsp; &nbsp;Water Analysis<br />Ground-Water-Quality Data<br />&nbsp; &nbsp; &nbsp;Data Collection and Computation<br />&nbsp; &nbsp; &nbsp;Laboratory Measurements<br />&nbsp; &nbsp; &nbsp;Blank Samples<br />&nbsp; &nbsp; &nbsp;Reference Samples<br />&nbsp; &nbsp; &nbsp;Replicate Samples<br />&nbsp; &nbsp; &nbsp;Spike Samples<br />Access to USGS Water Data<br />Definition of Terms<br />Techniques of Water-Resources Investigations of the U.S. Geological Survey<br />Ground-Water Levels<br />Ground-Water-Quality Monitoring Program.<br />Quality of Precipitation<br />Index</p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f1424","contributors":{"authors":[{"text":"Nalley, G.M.","contributorId":23535,"corporation":false,"usgs":true,"family":"Nalley","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":281813,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Linhart, S. Michael","contributorId":67932,"corporation":false,"usgs":true,"family":"Linhart","given":"S.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":281815,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Littin, G. R.","contributorId":95924,"corporation":false,"usgs":true,"family":"Littin","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":281816,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, V.E.","contributorId":43423,"corporation":false,"usgs":true,"family":"Miller","given":"V.E.","email":"","affiliations":[],"preferred":false,"id":281814,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Housel, K.S.","contributorId":22625,"corporation":false,"usgs":true,"family":"Housel","given":"K.S.","email":"","affiliations":[],"preferred":false,"id":281812,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70066,"text":"sir20045264 - 2005 - Summary of hydraulic properties of the Floridan Aquifer system in coastal Georgia and adjacent parts of South Carolina and Florida","interactions":[],"lastModifiedDate":"2017-01-17T12:49:26","indexId":"sir20045264","displayToPublicDate":"2005-02-11T00:00:00","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":"2004-5264","title":"Summary of hydraulic properties of the Floridan Aquifer system in coastal Georgia and adjacent parts of South Carolina and Florida","docAbstract":"Hydraulic-property data for the Floridan aquifer system and equivalent clastic sediments in a 67-county area of coastal Georgia and adjacent parts of South Carolina and Florida were evaluated to provide data necessary for development of ground-water flow and solute-transport models. Data include transmissivity at 324 wells, storage coefficient at 115 wells, and vertical hydraulic conductivity of 72 core samples from 27 sites.\r\n\r\nHydraulic properties of the Upper Floridan aquifer vary greatly in the study area due to the heterogeneity (and locally to anisotropy) of the aquifer and to variations in the degree of confinement provided by confining units. Prominent structural features in the area\u0014the Southeast Georgia Embayment, the Beaufort Arch, and the Gulf Trough\u0014influence the thickness and hydraulic properties of the sediments comprising the Floridan aquifer system. Transmissivity of the Upper Floridan aquifer and equivalent updip units was compiled for 239 wells and ranges from 530 feet squared per day (ft2/d) at Beaufort County, South Carolina, to 600,000 ft2/d in Coffee County, Georgia. In carbonate rock settings of the lower Coastal Plain, transmissivity of the Upper Floridan aquifer generally is greater than 20,000 ft2/d, with values exceeding 100,000 ft2/d in the southeastern and southwestern parts of the study area (generally coinciding with the area of greatest aquifer thickness). Transmissivity of the Upper Floridan aquifer generally is less than 10,000 ft2/d in and near the upper Coastal Plain, where the aquifer is thin and consists largely of clastic sediments, and in the vicinity of the Gulf Trough, where the aquifer consists of low permeability rocks and sediments. Large variability in the range of transmissivity in Camden and Glynn Counties, Georgia, and Nassau County, Florida, demonstrates the anisotropic distribution of hydraulic properties that may result from fractures or solution openings in the carbonate rocks. Storage coefficient of the Upper Floridan aquifer was compiled for 106 wells and ranges from about 0.00004 at Beaufort County, South Carolina, to 0.04 in Baker County, Florida. \r\n\r\nTransmissivity of the Lower Floridan aquifer and equivalent updip clastic units was compiled for 53 wells and ranges from about 170 ft2/d in Barnwell County, South Carolina, to about 43,000 ft2/d in Camden County, Georgia. Transmissivity of the Lower Floridan aquifer is greatest where the aquifer is thickest\u0014 in southeastern Georgia and northeastern Florida\u0014where estimates are greater than 10,000 ft2/d; at one well in southeastern Georgia transmissivity was estimated to be as high as 200,000 ft2/d. Storage-coefficient data for the Lower Floridan aquifer are limited to three estimates in Barnwell and Allendale Counties, South Carolina, and to estimates determined from six multi-aquifer tests in Duval County, Florida. In the South Carolina tests, storage coefficient ranges from 0.0003 to 0.0004; this range is indicative of a confined aquifer. The storage coefficient for the combined Upper and Lower Floridan wells in Duval County, Florida, ranges from 0.00002 to 0.02. \r\n\r\nVertical hydraulic conductivity was compiled from core samples collected at 27 sites. For the Upper Floridan confining unit, values from 39 core samples at 17 sites range from 0.0002 to 3 feet per day (ft/d). For the Lower Floridan confining unit, values from 10 core samples at 9 sites range from about 0.000004 to 0.16 ft/d. Vertical hydraulic conductivity of the Upper Floridan aquifer was compiled from 16 core samples at five sites, mostly in the Brunswick, Georgia, area and values range from 0.00134 to 160.4 ft/d. Vertical hydraulic conductivity for the semiconfining unit separating the upper and lower water-bearing zones of the Upper Floridan at Brunswick, Georgia, compiled from 6 core samples at three sites ranges from 0.000008 to 0.000134 ft/d. The vertical hydraulic conductivity of the Lower Floridan aquifer in a core sample from a well at Brunswick, G","language":"ENGLISH","doi":"10.3133/sir20045264","usgsCitation":"Clarke, J.S., Leeth, D.C., Taylor-Harris, D., Painter, J.A., and Labowski, J.L., 2005, Summary of hydraulic properties of the Floridan Aquifer system in coastal Georgia and adjacent parts of South Carolina and Florida (Online only): U.S. Geological Survey Scientific Investigations Report 2004-5264, 54 p., https://doi.org/10.3133/sir20045264.","productDescription":"54 p.","onlineOnly":"Y","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":186486,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6739,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2004/5264/","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","country":"United States","state":"Florida, 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cleeth@usgs.gov","contributorId":1403,"corporation":false,"usgs":true,"family":"Leeth","given":"David","email":"cleeth@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":281799,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Taylor-Harris, DaVette","contributorId":67977,"corporation":false,"usgs":true,"family":"Taylor-Harris","given":"DaVette","email":"","affiliations":[],"preferred":false,"id":281801,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"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":281800,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Labowski, James L.","contributorId":87631,"corporation":false,"usgs":true,"family":"Labowski","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":281802,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70074,"text":"sir20055022 - 2005 - Initial-phase investigation of multi-dimensional streamflow simulations in the Colorado River, Moab Valley, Grand County, Utah, 2004","interactions":[],"lastModifiedDate":"2017-01-27T15:41:03","indexId":"sir20055022","displayToPublicDate":"2005-02-11T00:00:00","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":"2005-5022","title":"Initial-phase investigation of multi-dimensional streamflow simulations in the Colorado River, Moab Valley, Grand County, Utah, 2004","docAbstract":"<p><span>A multi-dimensional hydrodynamic model was applied to aid in the assessment of the potential hazard posed to the uranium mill tailings near Moab, Utah, by flooding in the Colorado River as it flows through Moab Valley. Discharge estimates for the 100- and 500-year recurrence interval and for the Probable Maximum Flood (PMF) were evaluated with the model for the existing channel geometry. These discharges also were modeled for three other channel-deepening configurations representing hypothetical scour of the channel at the downstream portal of Moab Valley. Water-surface elevation, velocity distribution, and shear-stress distribution were predicted for each simulation.</span><br><br><span>The hydrodynamic model was developed from measured channel topography and over-bank topographic data acquired from several sources. A limited calibration of the hydrodynamic model was conducted. The extensive presence of tamarisk or salt cedar in the over-bank regions of the study reach presented challenges for determining roughness coefficients.</span><br><br><span>Predicted water-surface elevations for the current channel geometry indicated that the toe of the tailings pile would be inundated by about 4 feet by the 100-year discharge and 25 feet by the PMF discharge. A small area at the toe of the tailings pile was characterized by velocities of about 1 to 2 feet per second for the 100-year discharge. Predicted velocities near the toe for the PMF discharge increased to between 2 and 4 feet per second over a somewhat larger area. The manner to which velocities progress from the 100-year discharge to the PMF discharge in the area of the tailings pile indicates that the tailings pile obstructs the over-bank flow of flood discharges. The predicted path of flow for all simulations along the existing Colorado River channel indicates that the current distribution of tamarisk in the over-bank region affects how flood-flow velocities are spatially distributed. Shear-stress distributions were predicted throughout the study reach for each discharge and channel geometry examined. Material transport was evaluated by applying these shear-stress values to empirically determined critical shear-stress values for grain sizes ranging from very fine sands to very coarse gravels.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055022","collaboration":"Prepared in cooperation with the Utah Department of Environmmental Quality, Division of Radiation Control; and the U.S. Environmental Protection Agency","usgsCitation":"Kenney, T.A., 2005, Initial-phase investigation of multi-dimensional streamflow simulations in the Colorado River, Moab Valley, Grand County, Utah, 2004: U.S. Geological Survey Scientific Investigations Report 2005-5022, viii, 69 p., https://doi.org/10.3133/sir20055022.","productDescription":"viii, 69 p.","numberOfPages":"80","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":6778,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir20055022/","linkFileType":{"id":5,"text":"html"}},{"id":185843,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":334238,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5022/pdf/SIR2005_5022.pdf"}],"scale":"5000000","country":"United States","state":"Utah","county":"Grand County","otherGeospatial":"Colorado River, Moab Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66da0a","contributors":{"authors":[{"text":"Kenney, Terry A. 0000-0003-4477-7295 tkenney@usgs.gov","orcid":"https://orcid.org/0000-0003-4477-7295","contributorId":447,"corporation":false,"usgs":true,"family":"Kenney","given":"Terry","email":"tkenney@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":281817,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70015,"text":"ofr20051019 - 2005 - Preliminary geologic map of the Los Angeles 30' x 60' quadrangle, Southern California","interactions":[{"subject":{"id":24937,"text":"ofr95800 - 1995 - Preliminary geologic map of the Newhall 7.5' quadrangle, southern California: a digital database","indexId":"ofr95800","publicationYear":"1995","noYear":false,"title":"Preliminary geologic map of the Newhall 7.5' quadrangle, southern California: a digital database"},"predicate":"SUPERSEDED_BY","object":{"id":70015,"text":"ofr20051019 - 2005 - Preliminary geologic map of the Los Angeles 30' x 60' quadrangle, Southern California","indexId":"ofr20051019","publicationYear":"2005","noYear":false,"title":"Preliminary geologic map of the Los Angeles 30' x 60' quadrangle, Southern California"},"id":1}],"lastModifiedDate":"2019-11-19T06:56:09","indexId":"ofr20051019","displayToPublicDate":"2005-02-10T00:00:00","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":"2005-1019","title":"Preliminary geologic map of the Los Angeles 30' x 60' quadrangle, Southern California","docAbstract":"<p>This data set maps and describes the geology of the Los Angeles 30? x 60? quadrangle, southern California. Compilation of the Los Angeles quadrangle is based upon published mapping at scales of 1:12,000 and smaller, unpublished mapping at scales of 1:12,000 and smaller, with reconnaissance mapping by the compilers to resolve some edge-matching problems. The Los Angeles 30' x 60' quadrangle covers approximately 5,000 km2 including some of the most densely populated urban and suburban areas of the southern California megalopolis. It extends about 90 km E-W and about 55 km N-S, from Fillmore and Thousand Oaks in the west to Vincent in the northeast and Montebello in the southeast, and includes urban San Gabriel Valley and San Gabriel Mountain foothill communities from Monrovia to Pasadena, as well as Glendale, downtown Los Angeles, Hollywood, Santa Monica, Malibu, in addition to all the communities in the San Fernando Valley, Simi Valley, and the upper Santa Clara River Valley. From the 2000 Census, the population of these urban and suburban areas totals approximately 5.6 million, and estimates of property value total hundreds of billions of dollars. Residents and transient visitors are subject to potential hazards from earthquakes, debris flows and other landslides, floods, wildfires, subsidence from ground water and petroleum withdrawal, and swelling soils; and coastal areas are exposed to flooding and erosion by storm and tsunami waves. Topographic relief ranges from about one hundred meters sub sea (in Santa Monica Bay) to more than 2,000 meters above sea level at Pacifico Mountain in the high San Gabriel Mountains. In addition to the populated area, the quadrangle includes significant areas of wilderness in the Angeles and Los Padres National Forests, in the Santa Monica Mountains National Recreation Area, and the Sespe Condor Sanctuary. The geologic map illustrates the general distribution of the rocks and surficial deposits in the area and their structural and stratigraphic relations to one another. The principal characteristics of the map units are described and are part of the database. The map provides a regional geologic framework as an aid to better evaluations of the potential for hazard from active earth processes. It synthesizes and combines studies by many earth scientists. Most of the source maps are at more detailed scales than 1:100,000, and we utilized the most detailed source materials available. We have not attempted to resolve all problems of stratigraphic correlation and nomenclature. In most areas we have retained the unit designations of source-map authors, but in some areas, particularly in the igneous-metamorphic complex of the San Gabriel Mountains, some unit designations have been changed. Hopefully, this map will stimulate further work to describe and correlate the many units within the scope of a more coherent, more accurate geologic history.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20051019","usgsCitation":"complied by Yerkes, R.F., Campbell, R., Alvarez, R.M., and Bovard, K.R., 2005, Preliminary geologic map of the Los Angeles 30' x 60' quadrangle, Southern California (Version 1.0): U.S. Geological Survey Open-File Report 2005-1019, HTML, https://doi.org/10.3133/ofr20051019.","productDescription":"HTML","costCenters":[],"links":[{"id":188709,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6246,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1019/","linkFileType":{"id":5,"text":"html"}},{"id":110546,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_70332.htm","linkFileType":{"id":5,"text":"html"},"description":"70332"}],"scale":"1","country":"United States","state":"California","city":"Los Angeles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.00,\n              34.30\n            ],\n            [\n              -118.00,\n              34.30\n            ],\n            [\n              -118.00,\n              34.00\n            ],\n            [\n              -119.00,\n              34.00\n            ],\n            [\n              -119.00,\n              34.30\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b117","contributors":{"authors":[{"text":"complied by Yerkes, Robert F.","contributorId":93136,"corporation":false,"usgs":true,"family":"complied by Yerkes","given":"Robert","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":281669,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, Russell H.","contributorId":91074,"corporation":false,"usgs":true,"family":"Campbell","given":"Russell H.","affiliations":[],"preferred":false,"id":281667,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Alvarez, Rachel M.","contributorId":66354,"corporation":false,"usgs":true,"family":"Alvarez","given":"Rachel","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":281666,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bovard, Kelly R.","contributorId":91577,"corporation":false,"usgs":true,"family":"Bovard","given":"Kelly","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":281668,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70006,"text":"ds110 - 2005 - Flow velocity, water temperature, and conductivity at selected locations in Shark River Slough, Everglades National Park, Florida; July 1999 - July 2003","interactions":[],"lastModifiedDate":"2012-02-02T00:13:35","indexId":"ds110","displayToPublicDate":"2005-02-10T00:00:00","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":"110","title":"Flow velocity, water temperature, and conductivity at selected locations in Shark River Slough, Everglades National Park, Florida; July 1999 - July 2003","docAbstract":"Flow-velocity, water-temperature, and conductivity data were collected at five locations in Shark River Slough, Everglades National Park (ENP), Florida, from 1999 to 2003. The data were collected as part of the U.S. Geological Survey Priority Ecosystems Science Initiative in support of the Comprehensive Everglades Restoration Plan. This report contains digital files and graphical plots of the processed, quality-checked, and edited data. Information pertinent to the locations and monitoring strategy also is presented.","language":"ENGLISH","doi":"10.3133/ds110","usgsCitation":"Schaffranek, R.W., and Riscassi, A.L., 2005, Flow velocity, water temperature, and conductivity at selected locations in Shark River Slough, Everglades National Park, Florida; July 1999 - July 2003: U.S. Geological Survey Data Series 110, data files and text, https://doi.org/10.3133/ds110.","productDescription":"data files and text","costCenters":[],"links":[{"id":6241,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ds110/","linkFileType":{"id":5,"text":"html"}},{"id":188091,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de819","contributors":{"authors":[{"text":"Schaffranek, Raymond W.","contributorId":86314,"corporation":false,"usgs":true,"family":"Schaffranek","given":"Raymond","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":281657,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Riscassi, Ami L.","contributorId":24399,"corporation":false,"usgs":true,"family":"Riscassi","given":"Ami","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":281656,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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