{"pageNumber":"423","pageRowStart":"10550","pageSize":"25","recordCount":16445,"records":[{"id":27438,"text":"wri944145 - 1995 - Evaluation of ground-water flow and hydrologic budget for Lake Five-O, a seepage lake in northwestern Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:25","indexId":"wri944145","displayToPublicDate":"1996-07-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"94-4145","title":"Evaluation of ground-water flow and hydrologic budget for Lake Five-O, a seepage lake in northwestern Florida","docAbstract":"Temporal and spatial distributions of ground-water inflow to, and leakage from Lake Five-O, a softwater, seepage lake in northwestern Florida, were evaluated using hydrologic data and simulation models of the shallow ground-water system adjacent to the lake. The simulation models indicate that ground-water inflow to the lake and leakage from the lake to the ground-water system are the dominant components in the total inflow (precipitation plus ground-water inflow) and total outflow (evaporation plus leakage) budgets of Lake Five-O. Simlulated ground-water inflow and leakage were approximately 4 and 5 times larger than precipitation inputs and evaporative losses, respectively, during calendar years 1989-90. Exchanges of water between Lake Five-O and the ground-water system were consistently larger than atmospheric-lake exchanges. A consistent pattern of shallow ground-water inflow and deep leakage was also evident throughout the study period. The mean time of travel from ground-water that discharges at Lake Five-O (time from recharge at the water table to discharge at the lake) was estimated to be within a range of 3 to 6 years. Flow-path evaluations indicated that the intermediate confining unit probably has a negligible influence on the geochemistry of ground-water inflow to Lake Five-O. The hydrologic budgets and flow-path evaluations provide critical information for developing geochemical budgets for Lake Five-O and for improving the understanding of the relative importance of various processes that regulate the acid-neutralizing capacity of softwater seepage lakes in Florida.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri944145","usgsCitation":"Grubbs, J.W., 1995, Evaluation of ground-water flow and hydrologic budget for Lake Five-O, a seepage lake in northwestern Florida: U.S. Geological Survey Water-Resources Investigations Report 94-4145, vi, 42 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944145.","productDescription":"vi, 42 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":2122,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri944145","linkFileType":{"id":5,"text":"html"}},{"id":123720,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_94_4145.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688d3d","contributors":{"authors":[{"text":"Grubbs, J. W.","contributorId":77139,"corporation":false,"usgs":true,"family":"Grubbs","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":198121,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25895,"text":"wri954231 - 1995 - Technique for estimating the 2- to 500-year flood discharges on unregulated streams in rural Missouri","interactions":[],"lastModifiedDate":"2016-08-10T10:49:52","indexId":"wri954231","displayToPublicDate":"1996-07-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"95-4231","title":"Technique for estimating the 2- to 500-year flood discharges on unregulated streams in rural Missouri","docAbstract":"<p>A generalized least-squares regression technique was used to relate the 2- to 500-year flood discharges from 278 selected streamflow-gaging stations to statistically significant basin characteristics. The regression relations (estimating equations) were defined for three hydrologic regions (I, II, and III) in rural Missouri. Ordinary least-squares regression analyses indicate that drainage area (Regions I, II, and III) and main-channel slope (Regions I and II) are the only basin characteristics needed for computing the 2- to 500-year design-flood discharges at gaged or ungaged stream locations. The resulting generalized least-squares regression equations provide a technique for estimating the 2-, 5-, 10-, 25-, 50-, 100-, and 500-year flood discharges on unregulated streams in rural Missouri. The regression equations for Regions I and II were developed from stream-flow-gaging stations with drainage areas ranging from 0.13 to 11,500 square miles and 0.13 to 14,000 square miles, and main-channel slopes ranging from 1.35 to 150 feet per mile and 1.20 to 279 feet per mile. The regression equations for Region III were developed from streamflow-gaging stations with drainage areas ranging from 0.48 to 1,040 square miles. Standard errors of estimate for the generalized least-squares regression equations in Regions I, II, and m ranged from 30 to 49 percent.</p>","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","publisherLocation":"Richmond, Virginia","doi":"10.3133/wri954231","usgsCitation":"Alexander, T.W., and Wilson, G.L., 1995, Technique for estimating the 2- to 500-year flood discharges on unregulated streams in rural Missouri: U.S. Geological Survey Water-Resources Investigations Report 95-4231, iv, 33 p.: maps ;28 cm., https://doi.org/10.3133/wri954231.","productDescription":"iv, 33 p.: maps ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":396,"text":"Missouri Water Science 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,{"id":23725,"text":"ofr95420 - 1995 - Selected environmental and geohydrologic reports for the Fort Wainwright and Fairbanks areas, Alaska as of July 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:08:19","indexId":"ofr95420","displayToPublicDate":"1996-07-01T00:00:00","publicationYear":"1995","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":"95-420","title":"Selected environmental and geohydrologic reports for the Fort Wainwright and Fairbanks areas, Alaska as of July 1995","docAbstract":"As part of its effort to help collect data and gather information for geohydrologic investigations, the U.S. Geological Survey (USGS) collects and reviews environmental and technical reports relating to geology, hydrology, and geohydrology. The USGS investigation efforts are coordinated with ongoing technical investigations by the Water Research Center of the University of Alaska Fairbanks and the U.S. Army Cold Regions Research and Engineering Laboratory. One project objective for Fort Wainwright includes maintaining a library of report references for USGS project use and for use by the U.S. Army, Alaska (USARAK), USARAK contractors, and other Federal and State agencies. This report presents an annotated bibliography of reports relating to the project study area or geohydrologic processes important to investigations in the study area.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95420","issn":"0094-9140","usgsCitation":"Lilly, M.R., DePalma, K., and Benson, S., 1995, Selected environmental and geohydrologic reports for the Fort Wainwright and Fairbanks areas, Alaska as of July 1995: U.S. Geological Survey Open-File Report 95-420, 1 v. 62 p.  :ill., map ;28 cm., https://doi.org/10.3133/ofr95420.","productDescription":"1 v. 62 p.  :ill., map ;28 cm.","costCenters":[],"links":[{"id":157325,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0420/report-thumb.jpg"},{"id":19478,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0420/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52967,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0420/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aade4b07f02db66b4b6","contributors":{"authors":[{"text":"Lilly, M. R.","contributorId":38594,"corporation":false,"usgs":true,"family":"Lilly","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":190609,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DePalma, K.L.","contributorId":80315,"corporation":false,"usgs":true,"family":"DePalma","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":190611,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Benson, S.L.","contributorId":61075,"corporation":false,"usgs":true,"family":"Benson","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":190610,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27185,"text":"wri954091 - 1995 - Geohydrology and simulation of ground-water flow near Los Alamos, north-central New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:26","indexId":"wri954091","displayToPublicDate":"1996-07-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"95-4091","title":"Geohydrology and simulation of ground-water flow near Los Alamos, north-central New Mexico","docAbstract":"An existing model was modified in recognition of new \r\ngeohydrologic interpretations and adjusted to simulate \r\nhydrographs in well fields in the Los Alamos area. Hydraulic-head\r\ndrawdowns at the Buckman well field resulting from two projected\r\nground-water-withdrawal alternatives were estimated with the \r\nmodified model.\r\n\r\n     The Chaquehui formation (informal usage) is the main new \r\nfeature of recent hydrologic interpretations for the Los Alamos \r\narea. The Chaquehui occupies a 'channel' that was eroded or \r\nfaulted into the Tesuque Formation, and the Chaquehui is more \r\npermeable than the Tesuque. The Chaquehui is a major producing \r\nzone in the Pajarito Mesa well field and to a lesser extent in\r\nthe Guaje well field.\r\n\r\n     Model modification included splitting the four layers of the\r\nMcAda-Wasiolek model (McAda, D.P., and Wasiolek, Maryann, 1988, \r\nSimulation of the regional geohydrology of the Tesuque aquifer \r\nsystem near Santa Fe, New Mexico: U.S. Geological Survey Water-\r\nResources Investigations Report 87-4056, 71 p.) into eight layers\r\nto better simulate vertical ground-water movement. Other model \r\nmodifications were limited as much as possible to the area of \r\ninterest near Los Alamos and consisted mainly of adjusting \r\nhydraulic-conductivity values representing the Tesuque Formation,\r\nChaquehui formation (informal usage), and Puye Formation, and \r\nadjusting simulated recharge along the Pajarito Fault Zone west \r\nof Los Alamos. Adjustments were based mainly on simulation of \r\nfluctuations in measured hydraulic heads near Los Alamos.\r\n\r\n     Two possible alternative plans for replacing Guaje well field \r\nproduction were suggested by Los Alamos National Laboratory. In \r\nthe first plan (Guaje alternative), the Guaje field would be \r\nrenewed with four new wells replacing the existing production \r\nwells in the Guaje field. In the second plan (Pajarito-Otowi \r\nalternative), the Guaje well field would be retired and its\r\nformer production would be made up by additional withdrawals from the \r\nPajarito Mesa and Otowi well fields. A projection for each of \r\nthese alternatives was made through 2012 using the new eight-\r\nlayer model. In the Guaje field, projected hydraulic heads at the\r\nend of 2012 were as much as 50 feet lower with the Guaje \r\nalternative; in the Pajarito Mesa field, hydraulic heads were as\r\nmuch as 12 feet higher with the Guaje alternative. At the western\r\nend of the Los Alamos well field, projected hydraulic heads were\r\nabout 20 feet higher with the Guaje alternative; at the eastern \r\nend of the Los Alamos field, the difference between alternatives\r\nwas much less. At the Buckman field, projected hydraulic heads \r\nwere about 2 feet higher with the Guaje alternative because the \r\nBuckman field is closer to the Pajarito Mesa field than to the \r\nGuaje field. \r\n\r\n     Ways of improving the understanding of the flow system \r\ninclude developing a more accurate representation of the \r\nstructure and extent of the Tesuque Formation, Chaquehui \r\nformation, and Puye Formation of the Santa Fe Group and obtaining\r\nmore detailed geologic and hydrologic data for the Chaquehui and\r\nPuye. Data that describe water chemistry, hydraulic head, and \r\ndegree of saturation would be valuable for determining the \r\nlocation and quantity of recharge on the Pajarito Plateau, \r\nespecially along the west side of the Plateau and in canyon \r\nbottoms. Chloride concentrations in soil at the top of the \r\nBandelier Tuff could be used to verify the concept that \r\nevapotranspiration accounts for nearly all precipitation over a \r\nlarge area of the plateau.","language":"ENGLISH","publisher":"U.S. Geological Survey, [Water Resources Division, New Mexico District] ;\r\nCan be purchased from U.S. Geological Survey, Earth Science Information Center, Open-File Reports Section,","doi":"10.3133/wri954091","usgsCitation":"Frenzel, P.F., 1995, Geohydrology and simulation of ground-water flow near Los Alamos, north-central New Mexico: U.S. Geological Survey Water-Resources Investigations Report 95-4091, vi, 92 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri954091.","productDescription":"vi, 92 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124047,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4091/report-thumb.jpg"},{"id":56059,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4091/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8c49","contributors":{"authors":[{"text":"Frenzel, P. F.","contributorId":98726,"corporation":false,"usgs":true,"family":"Frenzel","given":"P.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":197706,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31931,"text":"ofr95704 - 1995 - Potentiometric surface of the upper Floridan Aquifer, west-central Florida, May 1995","interactions":[],"lastModifiedDate":"2017-01-24T10:53:53","indexId":"ofr95704","displayToPublicDate":"1996-07-01T00:00:00","publicationYear":"1995","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":"95-704","title":"Potentiometric surface of the upper Floridan Aquifer, west-central Florida, May 1995","docAbstract":"<p>The Floridan aquifer system consists of the Upper and Lower Floridan aquifers separated by a middle confining unit. The middle confining unit and the Lower Floridan aquifer generally contain highly mineralized water. In most reports on the hydrology of southwest Florida, the term \"Floridan aquifer\" has been applied to the water-bearing rocks, herin referred to as the Upper Floridan aquifer. The Upper Floridan aquifer is a productive aquifer and supplies more than 10 times the amount of water pumped from either the surfical aquifer system of the intermediate aquifer system in most of the study area (Duerr and other, 1988).&nbsp;</p><p>This map report depicts the potentiometric surface of the Upper Floridan aquifer in May 1995. The potentipmetric surface represents to the level to which water will rise in tightly cased wells that tap a confined aquifer system. The surface is mapped by determining the altitude of water levels in a network of wells and is represented on maps by contours that connect point of equal altitude. This map represents water-level conditions near the end of the dry season when ground-water withdrawals for agricultural use are usually high. The cumulative rainfall for the study area was 2.98 inches above average for the period from June 1994 through May 1995 (Southwest Florida Water Management District, 1995)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/ofr95704","usgsCitation":"Metz, P.A., and Stelman, K.A., 1995, Potentiometric surface of the upper Floridan Aquifer, west-central Florida, May 1995: U.S. Geological Survey Open-File Report 95-704, 1 map ; 72 x 60 cm., folded to 24 x 24 cm., https://doi.org/10.3133/ofr95704.","productDescription":"1 map ; 72 x 60 cm., folded to 24 x 24 cm.","costCenters":[],"links":[{"id":19574,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0704/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":163812,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"1","country":"United 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,{"id":23765,"text":"ofr95825 - 1995 - Results of geophysical investigations near the Norman, Oklahoma, Municipal Landfill, 1995","interactions":[],"lastModifiedDate":"2019-12-08T12:56:09","indexId":"ofr95825","displayToPublicDate":"1996-07-01T00:00:00","publicationYear":"1995","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":"95-825","title":"Results of geophysical investigations near the Norman, Oklahoma, Municipal Landfill, 1995","docAbstract":"<p>No abstract available.</p>","language":"English ","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr95825","issn":"0094-9140","usgsCitation":"Lucius, J., and Bisdorf, R., 1995, Results of geophysical investigations near the Norman, Oklahoma, Municipal Landfill, 1995: U.S. Geological Survey Open-File Report 95-825, 125 p. , https://doi.org/10.3133/ofr95825.","productDescription":"125 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":52994,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0825/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156372,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0825/report-thumb.jpg"}],"country":"United States","state":"Oklahoma","county":"Cleveland County","city":"Norman","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-97.6733,35.3763],[-97.4076,35.3771],[-97.1442,35.3742],[-97.1405,35.202],[-97.1433,35.2021],[-97.1432,34.9305],[-97.1504,34.9302],[-97.1544,34.9312],[-97.1622,34.9295],[-97.1701,34.9305],[-97.1869,34.9303],[-97.1936,34.9309],[-97.2041,34.936],[-97.213,34.9421],[-97.2208,34.9454],[-97.2263,34.9464],[-97.2314,34.9446],[-97.236,34.9397],[-97.2388,34.9397],[-97.2482,34.9458],[-97.2527,34.9472],[-97.2622,34.9492],[-97.2666,34.9506],[-97.2711,34.9534],[-97.2743,34.9575],[-97.2771,34.9603],[-97.2798,34.9617],[-97.286,34.9627],[-97.2927,34.9628],[-97.2984,34.9615],[-97.3029,34.9607],[-97.3096,34.9594],[-97.3164,34.959],[-97.3214,34.9586],[-97.3265,34.9583],[-97.331,34.9588],[-97.3376,34.9625],[-97.3437,34.9667],[-97.3475,34.9717],[-97.3497,34.9759],[-97.3506,34.9863],[-97.3484,35.0103],[-97.3505,35.0154],[-97.3538,35.0204],[-97.3542,35.0281],[-97.3543,35.0459],[-97.3489,35.0644],[-97.351,35.0699],[-97.3548,35.0758],[-97.3609,35.0818],[-97.3653,35.0842],[-97.376,35.0852],[-97.3799,35.0834],[-97.3833,35.0826],[-97.3878,35.0826],[-97.3934,35.0845],[-97.3984,35.0869],[-97.4034,35.0906],[-97.4072,35.0952],[-97.4077,35.0984],[-97.4071,35.1015],[-97.4059,35.106],[-97.4047,35.1101],[-97.4046,35.1138],[-97.4051,35.1174],[-97.4056,35.1219],[-97.4066,35.1274],[-97.407,35.1329],[-97.4086,35.1379],[-97.4119,35.1411],[-97.4169,35.1434],[-97.4237,35.144],[-97.427,35.1445],[-97.4315,35.1464],[-97.4359,35.1496],[-97.4398,35.1524],[-97.4437,35.1556],[-97.4453,35.1583],[-97.4469,35.1611],[-97.448,35.1638],[-97.4502,35.1661],[-97.4546,35.1698],[-97.4619,35.1744],[-97.4791,35.1865],[-97.4879,35.1925],[-97.4974,35.2003],[-97.5035,35.2031],[-97.5198,35.2033],[-97.5248,35.2052],[-97.5326,35.2117],[-97.5443,35.2177],[-97.5515,35.2255],[-97.5598,35.2315],[-97.5631,35.2352],[-97.5636,35.2384],[-97.5636,35.2402],[-97.5613,35.2429],[-97.5583,35.2483],[-97.5594,35.2542],[-97.5599,35.2574],[-97.5552,35.2669],[-97.5539,35.2732],[-97.5577,35.2805],[-97.5638,35.2892],[-97.5671,35.2934],[-97.5749,35.2953],[-97.591,35.3073],[-97.5933,35.3082],[-97.5973,35.3037],[-97.6035,35.3047],[-97.6086,35.3057],[-97.6142,35.303],[-97.6193,35.3031],[-97.6332,35.3137],[-97.6393,35.3192],[-97.6443,35.326],[-97.6481,35.3306],[-97.6531,35.3339],[-97.6565,35.3357],[-97.6683,35.3368],[-97.6729,35.335],[-97.6733,35.3763]]]},\"properties\":{\"name\":\"Cleveland\",\"state\":\"OK\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ce4b07f02db613c96","contributors":{"authors":[{"text":"Lucius, J.E.","contributorId":12501,"corporation":false,"usgs":true,"family":"Lucius","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":190679,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bisdorf, R.J.","contributorId":42960,"corporation":false,"usgs":true,"family":"Bisdorf","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":190680,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24692,"text":"ofr94306 - 1995 - Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data through September 1993","interactions":[],"lastModifiedDate":"2012-02-02T00:08:29","indexId":"ofr94306","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"94-306","title":"Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data through September 1993","docAbstract":"This report contains hydrologic and climatic data that describe the status of ground-water resources at U.S. Navy Support Facility, Diego Garcia. Data are presented through September 1993, one month into the annual wet season. At the end of September 1993, the chloride concentration of the composite water supply was 66 milligrams per liter, well below the 250 milligrams per liter secondary drinking water standard established by the U.S. Environmental Protection Agency. Most of the production wells appeared to be operating at levels consistent with past operations. Several wells at Air Operations remain out of service while they are being used to hydraulically divert the nearby fuel spill. Rainfall thus far in 1993 is 8 percent below the mean annual rainfall of 106 inches. This follows a year when rainfall was 12 percent below the mean annual rainfall. Withdrawal has averaged 856,000 gallons per day during 1993, a decrease from the 1992 average of 936,000 gallons per day. The chloride concentration of pumped water rose during the current quarter (July through September 1993) in most areas, coincident with the annual dry season (March through August). This continues a general trend of increasing chloride concentration that has persisted for more than a year, beginning in the 1992 dry season. Chloride concentration rose progressively during the current quarter in monitoring wells at Cantonment and Air Operations. Chloride concentrations in the deeper monitoring wells have generally been increasing since 1992. A fuel spill at Air Operations caused the shutdown of ten wells in May 1991. Four of the wells have resumed pumping to the water supply, but water from the remaining six wells is being used to hydraulically contain and divert fuel migration.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nFor sale by the Earth Science Information Center, Open-File Reports Section,","doi":"10.3133/ofr94306","issn":"0094-9140","usgsCitation":"Torikai, J., 1995, Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data through September 1993: U.S. Geological Survey Open-File Report 94-306, v, 51 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr94306.","productDescription":"v, 51 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":158179,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0306/report-thumb.jpg"},{"id":53725,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0306/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df2b6","contributors":{"authors":[{"text":"Torikai, J.D.","contributorId":93926,"corporation":false,"usgs":true,"family":"Torikai","given":"J.D.","affiliations":[],"preferred":false,"id":192395,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5062,"text":"fs21695 - 1995 - Mercury contamination of aquatic ecosystems","interactions":[],"lastModifiedDate":"2020-04-11T16:39:50.948014","indexId":"fs21695","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"216-95","title":"Mercury contamination of aquatic ecosystems","docAbstract":"<p>Mercury has been well known as an environmental pollutant for several decades. As early as the 1950's it was established that emissions of mercury to the environment could have serious effects on human health. These early studies demonstrated that fish and other wildlife from various ecosystems commonly attain mercury levels of toxicological concern when directly affected by mercury-containing emissions from human-related activities. Human health concerns arise when fish and wildlife from these ecosystems are consumed by humans. During the past decade, a new trend has emerged with regard to mercury pollution. Investigations initiated in the late 1980's in the northern-tier states of the U.S., Canada, and Nordic countries found that fish, mainly from nutrient-poor lakes and often in very remote areas, commonly have high levels of mercury. More recent fish sampling surveys in other regions of the U.S. have shown widespread mercury contamination in streams, wet-lands, reservoirs, and lakes. To date, 33 states have issued fish consumption advisories because of mercury contamination. These continental to global scale occurrences of mercury contamination cannot be linked to individual emissions of mercury, but instead are due to widespread air pollution. When scientists measure mercury levels in air and surface water, however, the observed levels are extraordinarily low. In fact, scientists have to take extreme precautions to avoid direct contact with water samples or sample containers, to avert sample contamination (Fig 3). Herein lies an apparent discrepancy: Why do fish from some remote areas have elevated mercury concentrations, when contamination levels in the environment are so low?</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs21695","usgsCitation":"Krabbenhoft, D.P., and Rickert, D.A., 1995, Mercury contamination of aquatic ecosystems: U.S. Geological Survey Fact Sheet 216-95, 4 p., https://doi.org/10.3133/fs21695.","productDescription":"4 p.","numberOfPages":"4","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":677,"text":"Wisconsin Water Science 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A.","contributorId":80247,"corporation":false,"usgs":true,"family":"Rickert","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":150357,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24228,"text":"ofr95474 - 1995 - Annual yield and selected hydrologic data for the Arkansas River Basin Compact, Arkansas-Oklahoma, 1994 water year","interactions":[],"lastModifiedDate":"2012-02-02T00:08:06","indexId":"ofr95474","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-474","title":"Annual yield and selected hydrologic data for the Arkansas River Basin Compact, Arkansas-Oklahoma, 1994 water year","docAbstract":"The computed annual yield and deficiency of the subbasins as defined in the Arkansas River Basin Compact, Arkansas-Oklahoma, are given in tables for the 1994 water year. Actual runoff from the subbasins and depletion caused by major reservoirs in the compact area also are given in tabular form. Monthly maximum, minimum, and mean discharges are shown for the 14 streamflow stations used in computing annual yield. Water-quality data are shown for 11 water-quality stations sampled in the Arkansas River Basin.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95474","issn":"0094-9140","usgsCitation":"Porter, J., 1995, Annual yield and selected hydrologic data for the Arkansas River Basin Compact, Arkansas-Oklahoma, 1994 water year: U.S. Geological Survey Open-File Report 95-474, iii, 54 p. :map ;28 cm., https://doi.org/10.3133/ofr95474.","productDescription":"iii, 54 p. :map ;28 cm.","costCenters":[],"links":[{"id":155752,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0474/report-thumb.jpg"},{"id":53362,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0474/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8228","contributors":{"authors":[{"text":"Porter, J.E.","contributorId":51779,"corporation":false,"usgs":true,"family":"Porter","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":191530,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24695,"text":"ofr94479 - 1995 - Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1992 through June 1994","interactions":[],"lastModifiedDate":"2012-02-02T00:08:28","indexId":"ofr94479","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"94-479","title":"Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1992 through June 1994","docAbstract":"This report contains hydrologic and climatic data that describe the status of ground-water resources at U.S. Navy Support Facility, Diego Garcia. Data are presented from January 1992 through June 1994. This report concentrates on data from 1994, and references historic data from 1992 and 1993. Total rainfall for the first half of 1994 was 51 inches which is 48 percent of the mean annual rainfall of 106 inches. In comparison, total rainfall for the first six months of 1993 and 1992 was 56 inches and 51 inches, respectively. Annual rainfall totals in 1993 and 1992 were 95 inches and 93 inches, respectively. Ground-water withdrawal has averaged 975,000 gallons per day through June 1994, while withdrawals in 1993 and 1992 averaged 954,000 gallons per day and 936,000 gallons per day, respectively. In each of the five areas of ground- water production, withdrawals have remained steady since 1991. At the end of June 1994, the chloride concentration of the composite water supply was 68 milligrams per liter, well below the 250 milligrams per liter secondary drinking water standard established by the U.S. Environmental Protection Agency. Chloride concentrations of the composite water supply from January through June 1994 ranged between 37 and 90 milligrams per liter. Chloride concentration of ground water in monitoring wells at Cantonment and Air Operations have increased very slightly since March 1994 coinciding with the start of the dry season. There has been a general trend of increasing chloride concentrations in the deeper monitoring wells since the 1992 dry season, which began in March 1992. A fuel spill at Air Operations caused the shutdown of ten wells in May 1991. Four of the wells resumed pumping for water-supply purposes in April 1992. The remaining six wells are being used to hydraulically contain and divert fuel migration.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nFor sale by the Earth Science Information Center, Open-File Reports Section,","doi":"10.3133/ofr94479","issn":"0094-9140","usgsCitation":"Torikai, J., 1995, Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1992 through June 1994: U.S. Geological Survey Open-File Report 94-479, v, 41 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr94479.","productDescription":"v, 41 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157822,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0479/report-thumb.jpg"},{"id":53728,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0479/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69764b","contributors":{"authors":[{"text":"Torikai, J.D.","contributorId":93926,"corporation":false,"usgs":true,"family":"Torikai","given":"J.D.","affiliations":[],"preferred":false,"id":192398,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22434,"text":"ofr95450 - 1995 - Bibliography, indices, and data sources of water-related studies, upper Colorado River basin, Colorado and Utah, 1872-1995","interactions":[],"lastModifiedDate":"2026-04-08T19:21:49.813296","indexId":"ofr95450","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-450","title":"Bibliography, indices, and data sources of water-related studies, upper Colorado River basin, Colorado and Utah, 1872-1995","docAbstract":"As part of the U.S. Geological Survey's National Water-Quality Assessment Program, current water-quality conditions in the Upper Colorado River Basin in Colorado and Utah are being assessed. This report is an initial effort to identify and compile information on water-related studies previously conducted in the basin and consists of a bibliography, coauthor and subject indices, and sources of available water-related data. Computerized literature searches of scientific data bases were carried out to identify past water-related studies in the basin, and government agencies and private organizations were contacted regarding their knowledge or possession of water-related publications and data. Categories of information in the bibliography include: aquatic biology, climate, energy development, geology, land use, limnology, runoff, salinity, surface- and ground-water hydrology, water chemistry, water quality and quantity, and water use and management. The approximately 1,400 indexed references date from 1872 through February 1995 and include books, journal articles, maps, and reports. In many instances, an abstract has been provided for a given reference. Sources of water-related data in the basin are included in a table.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95450","issn":"0094-9140","usgsCitation":"Bauch, N., and Apodaca, L., 1995, Bibliography, indices, and data sources of water-related studies, upper Colorado River basin, Colorado and Utah, 1872-1995: U.S. Geological Survey Open-File Report 95-450, v, 282 p. :map ;28 cm., https://doi.org/10.3133/ofr95450.","productDescription":"v, 282 p.","costCenters":[],"links":[{"id":1491,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/ofr95450/index.html","linkFileType":{"id":5,"text":"html"}},{"id":155626,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Colorado, Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ce4b07f02db626289","contributors":{"authors":[{"text":"Bauch, N.J.","contributorId":64688,"corporation":false,"usgs":true,"family":"Bauch","given":"N.J.","email":"","affiliations":[],"preferred":false,"id":188245,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Apodaca, L.E.","contributorId":73635,"corporation":false,"usgs":true,"family":"Apodaca","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":188246,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24604,"text":"ofr93639 - 1995 - Measurements of evapotranspiration, surface-energy fluxes, weather variables, and water-table depths in the closed basin of the San Luis Valley, Alamosa County, Colorado, 1985-88","interactions":[],"lastModifiedDate":"2019-12-07T11:02:12","indexId":"ofr93639","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"93-639","title":"Measurements of evapotranspiration, surface-energy fluxes, weather variables, and water-table depths in the closed basin of the San Luis Valley, Alamosa County, Colorado, 1985-88","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr93639","issn":"0094-9140","usgsCitation":"Stannard, D., and Weaver, H.L., 1995, Measurements of evapotranspiration, surface-energy fluxes, weather variables, and water-table depths in the closed basin of the San Luis Valley, Alamosa County, Colorado, 1985-88: U.S. Geological Survey Open-File Report 93-639, iv, 61 p. , https://doi.org/10.3133/ofr93639.","productDescription":"iv, 61 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":157680,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0639/report-thumb.jpg"},{"id":53651,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0639/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","county":"Alamosa County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-105.4581,37.7517],[-105.454,37.7472],[-105.4517,37.744],[-105.4506,37.7376],[-105.4518,37.7304],[-105.4571,37.7213],[-105.4607,37.7177],[-105.4712,37.7083],[-105.4759,37.7019],[-105.48,37.6938],[-105.4795,37.6906],[-105.4766,37.6856],[-105.4755,37.6802],[-105.4761,37.6747],[-105.4767,37.6711],[-105.4785,37.6634],[-105.4785,37.6625],[-105.4815,37.6566],[-105.4903,37.6349],[-105.4915,37.6286],[-105.4916,37.6227],[-105.4928,37.6186],[-105.4974,37.6159],[-105.4992,37.6141],[-105.498,37.6118],[-105.4917,37.6041],[-105.4929,37.6],[-105.4958,37.5982],[-105.4958,37.591],[-105.4872,37.576],[-105.4896,37.5746],[-105.5036,37.5611],[-105.5421,37.5254],[-105.5468,37.5204],[-105.5503,37.5177],[-105.5596,37.5096],[-105.5969,37.478],[-105.6016,37.4735],[-105.661,37.4234],[-105.6947,37.3963],[-105.7406,37.3583],[-105.7441,37.3551],[-105.7476,37.3551],[-105.7591,37.3551],[-105.8194,37.3553],[-105.9282,37.3549],[-106.0376,37.3554],[-106.0377,37.3998],[-106.0383,37.4905],[-106.0383,37.5199],[-106.0383,37.5761],[-106.0389,37.66],[-106.0384,37.7479],[-105.9267,37.7475],[-105.8149,37.7482],[-105.7078,37.7489],[-105.6374,37.7492],[-105.6182,37.7496],[-105.5198,37.7506],[-105.5163,37.7506],[-105.5,37.751],[-105.4581,37.7517]]]},\"properties\":{\"name\":\"Alamosa\",\"state\":\"CO\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db61128d","contributors":{"authors":[{"text":"Stannard, D.I.","contributorId":100884,"corporation":false,"usgs":true,"family":"Stannard","given":"D.I.","email":"","affiliations":[],"preferred":false,"id":192239,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weaver, H. L.","contributorId":58679,"corporation":false,"usgs":true,"family":"Weaver","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":192238,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23277,"text":"ofr95386 - 1995 - Hydrogeologic and water-quality data for the explosive experimental area, Naval Surface Warfare Center, Dahlgren Site, Dahlgren, Virginia","interactions":[],"lastModifiedDate":"2022-07-20T19:54:53.940777","indexId":"ofr95386","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-386","title":"Hydrogeologic and water-quality data for the explosive experimental area, Naval Surface Warfare Center, Dahlgren Site, Dahlgren, Virginia","docAbstract":"Hydrogeologic and water-quality data were collected at the Explosive Experimental Area, Naval Surface Warfare Center, Dahlgren Site at Dahlgren, Virginia, as part of a hydrogeologic assessment of the shallow aquifer system begun in 1993. The U.S. Geological Survey conducted this study to provide the U.S. Navy with hydrogeologic data to aid in the evaluation of the effects from remediation of contaminated sites and to protect against additional contamination. This report describes the ground-water observation- well network, hydrogeologic, and water-quality data collected between October 1993 and April 1995. The report includes a description of the locations and construction of 28 observation wells on the Explosive Experimental Area. Hydrogeologic data include lithologic logs, geophysical logs, and vertical hydraulic conductivity measurements of selected core intervals. Hydrologic data include synoptic and hourly measurements of ground-water levels, and observation-well slug tests to determine horizontal hydraulic conductivity. Water-quality data include analyses of major dissolved constituents in ground water and surface water.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95386","collaboration":"The USGS does not support this software or technical questions for the software associated with the publication.","usgsCitation":"Hammond, E.C., and Bell, C.F., 1995, Hydrogeologic and water-quality data for the explosive experimental area, Naval Surface Warfare Center, Dahlgren Site, Dahlgren, Virginia: U.S. Geological Survey Open-File Report 95-386, Report: iv, 68 p.; 1 Plate: 19.00 × 17.00 inches; Application Site, https://doi.org/10.3133/ofr95386.","productDescription":"Report: iv, 68 p.; 1 Plate: 19.00 × 17.00 inches; Application Site","costCenters":[],"links":[{"id":404158,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18470.htm","linkFileType":{"id":5,"text":"html"}},{"id":277684,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/of/1995/0386/application.zip"},{"id":52564,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0386/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19444,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0386/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156072,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0386/report-thumb.jpg"}],"country":"United States","state":"Virginia","city":"Dahlgren","otherGeospatial":"Naval Surface Warfare Center, Dahlgren Site","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.070,\n              38.284\n            ],\n            [\n              -77.009,\n              38.284\n            ],\n            [\n              -77.009,\n              38.319\n            ],\n            [\n              -77.070,\n              38.319\n            ],\n            [\n              -77.070,\n              38.284\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628caf","contributors":{"authors":[{"text":"Hammond, E. C.","contributorId":34544,"corporation":false,"usgs":true,"family":"Hammond","given":"E.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":189800,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bell, C. F.","contributorId":14449,"corporation":false,"usgs":true,"family":"Bell","given":"C.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":189799,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24694,"text":"ofr95387 - 1995 - Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1992 through December 1994","interactions":[],"lastModifiedDate":"2012-02-02T00:08:28","indexId":"ofr95387","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-387","title":"Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1992 through December 1994","docAbstract":"This report contains hydrologic and climatic data that describe the status of ground-water resources at U.S. Navy Support Facility, Diego Garcia. Data presented are from January 1992 through December 1994. This report concentrates on data from October through December 1994, and references previous data from 1992 through 1994. Cumulative rainfall for October through December 1994 was 55 inches which is higher than the mean cumulative rainfall of about 31 inches for the same 3 months. Total rainfall for 1994 was 131 inches which is 24 percent higher than the mean annual rainfall of 106 inches. In com- parison, total rainfall in 1992 and 1993 were 93 inches and 95 inches, respectively. Ground-water withdrawal during October through December 1994 averaged 903,000 gallons per day, while the annual withdrawal in 1994 was 942,700 gallons per day. Annual withdrawals in 1992 and 1993 averaged 935,900 gallons per day and 953,800 gallons per day, respectively. At the end of December 1994, the chloride concentration of the composite water supply was 28 milligrams per liter, well below the 250 milligrams per liter secondary drinking-water standard established by the U.S. Environmental Protection Agency. Chloride concentrations of the composite water supply from October through December 1994 ranged between 28 and 86 milligrams per liter. Chloride concentration of ground water in monitoring wells at Cantonment and Air Operations decreased in November and December, and seems to have leveled off by the end of the year. Although chloride concen- trations have decreased during the fourth quarter of 1994, there has been a general trend of increasing chloride concentrations in the deeper monitoring wells since the 1992 dry season, which began in March 1992. A fuel leak at Air Operations caused the shutdown of ten wells in May 1991. Four of the wells resumed pumping for water-supply purposes in April 1992. The remaining six wells are being used to hydraulically contain and divert fuel migration by recirculating 150,000 gallons of water each day.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nFor sale by the Earth Science Information Center, Open-File Reports Section,","doi":"10.3133/ofr95387","issn":"0094-9140","usgsCitation":"Torikai, J., 1995, Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1992 through December 1994: U.S. Geological Survey Open-File Report 95-387, v, 42 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr95387.","productDescription":"v, 42 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157821,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0387/report-thumb.jpg"},{"id":53727,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0387/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699e54","contributors":{"authors":[{"text":"Torikai, J.D.","contributorId":93926,"corporation":false,"usgs":true,"family":"Torikai","given":"J.D.","affiliations":[],"preferred":false,"id":192397,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24693,"text":"ofr94480 - 1995 - Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, 1991-93","interactions":[],"lastModifiedDate":"2012-02-02T00:08:29","indexId":"ofr94480","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"94-480","title":"Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, 1991-93","docAbstract":"This report contains hydrologic and climatic data that describe the status of ground-water resources at U.S. Navy Support Facility, Diego Garcia. Data are presented from January 1991 through December 1993. This report concentrates on data from fourth quarter 1993, and references historic data from 1991 and 1992. Total rainfall for 1993 was 95 inches which is 10 percent below the mean annual rainfall of 106 inches. In comparison, total rainfalls in 1992 and 1991 were 93 inches and 130 inches, respectively. Ground-water withdrawal has averaged 954,000 gallons per day during 1993, while with- drawals in 1992 and 1991 averaged 936,000 gallons per day and 927,000 gallons per day, respectively. In each of the five areas of ground-water produc- tion, withdrawals have remained steady since 1991. At the end of December 1993, the chloride concen- tration of the composite water supply was 36 milligrams per liter, well below the 250 milligrams per liter secondary drinking water standard established by the U.S. Environmental Protection Agency. Chloride concentrations of the composite water supply during the last quarter (October through December 1993) ranged between 35 and 75 milligrams per liter. Chloride concentrations in monitoring wells at Cantonment and Air Operations decreased during the last quarter (October through December 1993) after having risen progressively during the previous quarter (July through September 1993). There has been a general trend of increasing chloride concentrations in the deeper monitoring wells since the 1992 dry season, which began in March 1992. A fuel spill at Air Operations caused the shutdown of ten wells in May 1991. Four of the wells resumed pumping for water supply purposes in April 1992. The remaining six wells are being used to hydraulically contain and divert fuel migration.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nFor sale by the Earth Science Information Center, Open-File Reports Section,","doi":"10.3133/ofr94480","issn":"0094-9140","usgsCitation":"Torikai, J., 1995, Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, 1991-93: U.S. Geological Survey Open-File Report 94-480, v, 41 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr94480.","productDescription":"v, 41 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158180,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0480/report-thumb.jpg"},{"id":53726,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0480/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de895","contributors":{"authors":[{"text":"Torikai, J.D.","contributorId":93926,"corporation":false,"usgs":true,"family":"Torikai","given":"J.D.","affiliations":[],"preferred":false,"id":192396,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29519,"text":"wri924093 - 1995 - Simulation of streamflow and sediment transport in two surface-coal-mined basins in Fayette County, Pennsylvania","interactions":[],"lastModifiedDate":"2022-09-16T21:33:46.050946","indexId":"wri924093","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"92-4093","title":"Simulation of streamflow and sediment transport in two surface-coal-mined basins in Fayette County, Pennsylvania","docAbstract":"The Hydrological Simulation Program - Fortran (HSPF) was used to simulate streamflow and sediment transport in two surface-mined basins of Fayette County, Pa. Hydrologic data from the Stony Fork Basin (0.93 square miles) was used to calibrate HSPF parameters. The calibrated parameters were applied to an HSPF model of the Poplar Run Basin (8.83 square miles) to evaluate the transfer value of model parameters. The results of this investigation provide information to the Pennsylvania Department of Environmental Resources, Bureau of Mining and Reclamation, regarding the value of the simulated hydrologic data for use in cumulative hydrologic-impact assessments of surface-mined basins. \r\n     The calibration period was October 1, 1985, through September 30, 1988 (water years 1986-88). The simulated data were representative of the observed data from the Stony Fork Basin. Mean simulated streamflow was 1.64 cubic feet per second compared to measured streamflow of 1.58 cubic feet per second for the 3-year period. The difference between the observed and simulated peak stormflow ranged from 4.0 to 59.7 percent for 12 storms. The simulated sediment load for the 1987 water year was 127.14 tons (0.21 ton per acre), which compares to a measured sediment load of 147.09 tons (0.25 ton per acre). The total simulated suspended-sediment load for the 3-year period was 538.2 tons (0.30 ton per acre per year), which compares to a measured sediment load of 467.61 tons (0.26 ton per acre per year). \r\n\r\n     The model was verified by comparing observed and simulated data from October 1, 1988, through September 30, 1989. The results obtained were comparable to those from the calibration period. The simulated mean daily discharge was representative of the range of data observed from the basin and of the frequency with which specific discharges were equalled or exceeded.\r\n\r\n     The calibrated and verified parameters from the Stony Fork model were applied to an HSPF model of the Poplar Run Basin. The two basins are in a similar physical setting. Data from October 1, 1987, through September 30, 1989, were used to evaluate the Poplar Run model. In general, the results from the Poplar Run model were comparable to those obtained from the Stony Fork model. The difference between observed and simulated total streamflow was 1.1 percent for the 2-year period. The mean annual streamflow simulated by the Poplar Run model was 18.3 cubic feet per second. This compares to an observed streamflow of 18.15 cubic feet per second. For the 2-year period, the simulated sediment load was 2,754 tons (0.24 ton per acre per year), which compares to a measured sediment load of 3,051.2 tons (0.27 ton per acre per year) for the Poplar Run Basin. Cumulative frequency-distribution curves of the observed and simulated streamflow compared well. The comparison between observed and simulated data improved as the time span increased. Simulated annual means and totals were more representative of the observed data than hourly data used in comparing storm events.\r\n\r\n     The structure and organization of the HSPF model facilitated the simulation of a wide range of hydrologic processes. The simulation results from this investigation indicate that model parameters may be transferred to ungaged basins to generate representative hydrologic data through modeling techniques.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri924093","usgsCitation":"Sams, J.I., and Witt, E., 1995, Simulation of streamflow and sediment transport in two surface-coal-mined basins in Fayette County, Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 92-4093, vi, 52 p., https://doi.org/10.3133/wri924093.","productDescription":"vi, 52 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":406891,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47658.htm","linkFileType":{"id":5,"text":"html"}},{"id":58357,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4093/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159722,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4093/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","county":"Fayette County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.6,\n              39.75\n            ],\n            [\n              -79.425,\n              39.75\n            ],\n            [\n              -79.425,\n              40.0667\n            ],\n            [\n              -79.6,\n              40.0667\n            ],\n            [\n              -79.6,\n              39.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e492de4b07f02db57ef5c","contributors":{"authors":[{"text":"Sams, J. I. III","contributorId":50548,"corporation":false,"usgs":true,"family":"Sams","given":"J.","suffix":"III","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":201654,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Witt, E. C. III","contributorId":105746,"corporation":false,"usgs":true,"family":"Witt","given":"E. C.","suffix":"III","affiliations":[],"preferred":false,"id":201655,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23742,"text":"ofr95701 - 1995 - Quality assurance plan for discharge measurements using broadband acoustic Doppler current profilers","interactions":[],"lastModifiedDate":"2012-02-02T00:08:15","indexId":"ofr95701","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-701","title":"Quality assurance plan for discharge measurements using broadband acoustic Doppler current profilers","docAbstract":"The recent introduction of the Acoustic Doppler Current Profiler (ADCP) as an instrument for measuring velocities and discharge in the riverine and estuarine environment promises to revolutionize the way these data are collected by the U.S. Geological Survey. The ADCP and associated software, however, compose a complex system and should be used only by qualifies personnel. Standard procedures should be rigorously followed to ensure that the quality of data collected is commensurate with the standards set by the Water Resources Division for all its varied activities in hydrologic investigations.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section,","doi":"10.3133/ofr95701","issn":"0094-9140","usgsCitation":"Lipscomb, S.W., 1995, Quality assurance plan for discharge measurements using broadband acoustic Doppler current profilers: U.S. Geological Survey Open-File Report 95-701, iii, 7 p. ;28 cm., https://doi.org/10.3133/ofr95701.","productDescription":"iii, 7 p. ;28 cm.","costCenters":[],"links":[{"id":156824,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":13679,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/ofr95-701/ ","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db6552df","contributors":{"authors":[{"text":"Lipscomb, S. W.","contributorId":65083,"corporation":false,"usgs":true,"family":"Lipscomb","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":190635,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22276,"text":"ofr95315 - 1995 - Water-quality data for the Santa Clara-Calleguas hydrologic unit, Ventura County, California, October 1989 through December 1993","interactions":[],"lastModifiedDate":"2012-02-02T00:08:02","indexId":"ofr95315","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-315","title":"Water-quality data for the Santa Clara-Calleguas hydrologic unit, Ventura County, California, October 1989 through December 1993","docAbstract":"More than 700 water samples were collected from 232 wells and 34 surface-water sites in the Santa Clara-Calleguas Hydrologic Unit, Ventura County, California, from October 1989 through December 1993 as part of the U.S. Geological Survey's Southern California Regional Aquifer-System Analysis study. Most samples were analyzed for major ions, nutrients, selected trace elements, oxygen-18, and deuterium. Selected samples were analyzed for one or more of the following isotopes: carbon-13/12, carbon-14, strontium-87/86, sulfur-34/32, and tritium. Other samples were analyzed for one or more of the following dissolved gases: hydrogen, methane, oxygen, and freon-11. Location of sampling sites is shown on maps and the results are presented in tables.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95315","issn":"0094-9140","usgsCitation":"Izbicki, J., Martin, P.M., Densmore, J., and Clark, D.A., 1995, Water-quality data for the Santa Clara-Calleguas hydrologic unit, Ventura County, California, October 1989 through December 1993: U.S. Geological Survey Open-File Report 95-315, iv, 124 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr95315.","productDescription":"iv, 124 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":155776,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0315/report-thumb.jpg"},{"id":51698,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0315/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db64858c","contributors":{"authors":[{"text":"Izbicki, J. A. 0000-0003-0816-4408","orcid":"https://orcid.org/0000-0003-0816-4408","contributorId":28244,"corporation":false,"usgs":true,"family":"Izbicki","given":"J. A.","affiliations":[],"preferred":false,"id":187904,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, P. M.","contributorId":39003,"corporation":false,"usgs":true,"family":"Martin","given":"P.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":187905,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Densmore, J.N. 0000-0002-5345-6613","orcid":"https://orcid.org/0000-0002-5345-6613","contributorId":100882,"corporation":false,"usgs":true,"family":"Densmore","given":"J.N.","affiliations":[],"preferred":false,"id":187907,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Clark, D. A.","contributorId":57488,"corporation":false,"usgs":false,"family":"Clark","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":187906,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":24710,"text":"ofr95375 - 1995 - Real-Time Mapping alert system; characteristics and capabilities","interactions":[],"lastModifiedDate":"2012-02-02T00:08:24","indexId":"ofr95375","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-375","title":"Real-Time Mapping alert system; characteristics and capabilities","docAbstract":"The U.S. Geological Survey has an extensive hydrologic network that records and transmits precipitation, stage, discharge, and other water-related data on a real-time basis to an automated data processing system. Data values are recorded on electronic data collection platforms at field sampling sites. These values are transmitted by means of orbiting satellites to receiving ground stations, and by way of telecommunication lines to a U.S. Geological Survey office where they are processed on a computer system. Data that exceed predefined thresholds are identified as alert values. The current alert status at monitoring sites within a state or region is of critical importance during floods, hurricanes, and other extreme hydrologic events. This report describes the characteristics and capabilities of a series of computer programs for real-time mapping of hydrologic data. The software provides interactive graphics display and query of hydrologic information from the network in a real-time, map-based, menu-driven environment.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95375","issn":"0094-9140","usgsCitation":"Torres, L., Lambert, S., and Liebermann, T., 1995, Real-Time Mapping alert system; characteristics and capabilities: U.S. Geological Survey Open-File Report 95-375, iv, 18 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr95375.","productDescription":"iv, 18 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157518,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0375/report-thumb.jpg"},{"id":53742,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0375/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db64474c","contributors":{"authors":[{"text":"Torres, L.A.","contributorId":19195,"corporation":false,"usgs":true,"family":"Torres","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":192413,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lambert, S.C.","contributorId":92289,"corporation":false,"usgs":true,"family":"Lambert","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":192415,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Liebermann, T.D.","contributorId":23569,"corporation":false,"usgs":true,"family":"Liebermann","given":"T.D.","email":"","affiliations":[],"preferred":false,"id":192414,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30259,"text":"wri954113 - 1995 - Ground-Water Availability from the Hawi Aquifer in the Kohala Area, Hawaii","interactions":[],"lastModifiedDate":"2012-03-08T17:16:15","indexId":"wri954113","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"95-4113","title":"Ground-Water Availability from the Hawi Aquifer in the Kohala Area, Hawaii","docAbstract":"A ground-water study consisting of test-well drilling, aquifer tests, and numerical simulation was done to investigate ground-water availability in the basal part of the Hawi aquifer between the western drainage divide of Pololu Valley and Upolu Point in Kohala, Hawaii. The test-well drilling provided information on geology, water levels, water quality, vertical extent of the freshwater, and the thickness of the freshwater-saltwater transition zone in that aquifer. A total of 12 test wells were drilled at eight locations. Aquifer tests were done at five locations to estimate the hydraulic conductivity of the aquifer. Using information on the distribution of recharge, vertical extent of freshwater, hydraulic conductivity, and geometry of the basal aquifer, a numerical model was used to simulate the movement of water into, through, and out of the basal aquifer, and the effect of additional pumping on the water levels in the aquifer.\r\n\r\nResults of the modeling indicate that ground-water withdrawal of 20 million gallons per day above the existing withdrawal of 0.6 million gallons per day from the basal aquifer is hydrologically feasible, but that spacing, depth, and pumping rates of individual wells are important. If pumping is concentrated, the likelihood of saltwater intrusion is increased. The additional withdrawal of 20 million gallons per day would result in a reduction of ground-water discharge to the ocean by an amount equal to pumpage. Although model-calculated declines in water-level outside the area of pumping are small, pumping could cause some reduction of streamflow near the mouth of Pololu Stream.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/wri954113","usgsCitation":"Underwood, M.R., Meyer, W., and Souza, W.R., 1995, Ground-Water Availability from the Hawi Aquifer in the Kohala Area, Hawaii: U.S. Geological Survey Water-Resources Investigations Report 95-4113, vi, 57 p., https://doi.org/10.3133/wri954113.","productDescription":"vi, 57 p.","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":123867,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4113/report-thumb.jpg"},{"id":59048,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4113/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cee4b07f02db5457af","contributors":{"authors":[{"text":"Underwood, Mark R.","contributorId":45354,"corporation":false,"usgs":true,"family":"Underwood","given":"Mark","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":202949,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, William","contributorId":87538,"corporation":false,"usgs":true,"family":"Meyer","given":"William","affiliations":[],"preferred":false,"id":202950,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Souza, William R.","contributorId":90295,"corporation":false,"usgs":true,"family":"Souza","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":202951,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":25731,"text":"wri954110 - 1995 - Quantity and quality of ground-water discharge to the South Platte River, Denver to Fort Lupton, Colorado, August 1992 through July 1993","interactions":[],"lastModifiedDate":"2012-02-02T00:08:13","indexId":"wri954110","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"95-4110","title":"Quantity and quality of ground-water discharge to the South Platte River, Denver to Fort Lupton, Colorado, August 1992 through July 1993","docAbstract":"Water-quality studies conducted by the Metro Wastewater Reclamation District have indicated that during low flow in segments of the South Platte River between Denver and Fort Lupton, concentrations of dissolved oxygen are less than minimum concen- trations set by the State of Colorado. Low dissolved-oxygen concentrations are observed in two reaches of the river-they are about 3.3 to 6.4 miles and 17 to 25 miles downstream from the Metro Waste- water Reclamation District effluent outfalls. Concentrations of dissolved oxygen recover between these two reaches. Studies conducted by the U.S. Geological Survey have indicated that ground-water discharge to the river may contribute to these low dissolved-oxygen concentrations. As a result, an assessment was made of the quantity and quality of ground-water discharge to the South Platte River from Denver to Fort Lupton. Measurements of surface- water and ground-water discharge and collections of surface water and ground water for water-quality analyses were made from August 1992 through January 1993 and in May and July 1993. The quantity of ground-water discharge to the South Platte River was determined indirectly by mass balance of surface-water inflows and outflows and directly by instantaneous measurements of ground-water discharge across the sediment/water interface in the river channel. The quality of surface water and ground water was determined by sampling and analysis of water from the river and monitoring wells screened in the alluvial aquifer adjacent to the river and by sampling and analysis of water from piezometers screened in sediments underlying the river channel. The ground-water flow system was subdivided into a large-area and a small-area flow system. The precise boundaries of the two flow systems are not known. However, the large-area flow system is considered to incorporate all alluvial sediments in hydrologic connection with the South Platte River. The small- area flow system is considered to incorporate the alluvial aquifer in the vicinity of the river. Flow-path lengths in the large-area flow system were considered to be on the order of hundreds of feet to more than a mile, whereas in the small-area flow system, they were considered to be on the order of feet to hundreds of feet. Mass-balance estimates of incremental ground-water discharge from the large- area flow system ranged from -27 to 17 cubic feet per second per mile in three reaches of the river; the median rate was 4.6 cubic feet per second per mile. The median percentage of surface-water discharge derived from ground-water discharge in the river reaches studied was 13 percent. Instantaneous measurements of ground-water discharge from the small-area flow system ranged from -1,360 to 1,000 cubic feet per second per mile, with a median value of -5.8 cubic feet per second per mile. Hourly measurements of discharge from the small-area flow system indicated that the high rates of discharge were transient and may have been caused by daily fluctuations in river stage due to changing effluent-discharge rates from the Metro Wastewater Reclamation District treatment plant. Higher river stages caused surface water to infiltrate bed sediments underlying the river channel, and lower river stages allowed ground water to discharge into the river. Although stage changes apparently cycled large quantities of water in and out of the small- area flow system, the process probably provided no net gain or loss of water to the river. In general, mass balance and instantaneous measurements of ground-water discharge indicated that the ground- water flow system in the vicinity of the river consisted of a large-area flow system that provided a net addition of water to the river and a small- area flow system that cycled water in and out of the riverbed sediments, but provided no net addition of water to the river. The small-area flow system was superimposed on the large-area flow system. The median values of pH and dissolved oxygen ","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri954110","usgsCitation":"McMahon, P., Lull, K., Dennehy, K., and Collins, J., 1995, Quantity and quality of ground-water discharge to the South Platte River, Denver to Fort Lupton, Colorado, August 1992 through July 1993: U.S. Geological Survey Water-Resources Investigations Report 95-4110, v, 71 p. :ill., map ;28 cm., https://doi.org/10.3133/wri954110.","productDescription":"v, 71 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":157131,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4110/report-thumb.jpg"},{"id":54491,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4110/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54492,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4110/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a57e4b07f02db62e4fe","contributors":{"authors":[{"text":"McMahon, P.B. 0000-0001-7452-2379","orcid":"https://orcid.org/0000-0001-7452-2379","contributorId":10762,"corporation":false,"usgs":true,"family":"McMahon","given":"P.B.","affiliations":[],"preferred":false,"id":194833,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lull, K.J.","contributorId":19591,"corporation":false,"usgs":true,"family":"Lull","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":194834,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dennehy, K.F.","contributorId":41841,"corporation":false,"usgs":true,"family":"Dennehy","given":"K.F.","affiliations":[],"preferred":false,"id":194835,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Collins, J.A.","contributorId":72412,"corporation":false,"usgs":true,"family":"Collins","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":194836,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":26584,"text":"wri954097 - 1995 - Geochemical processes in ground water resulting from surface mining of coal at the Big Sky and West Decker Mine areas, southeastern Montana","interactions":[],"lastModifiedDate":"2025-01-08T21:55:11.888669","indexId":"wri954097","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"95-4097","title":"Geochemical processes in ground water resulting from surface mining of coal at the Big Sky and West Decker Mine areas, southeastern Montana","docAbstract":"A potential hydrologic effect of surface mining of coal in southeastern Montana is a change in the quality of ground water. Dissolved-solids concen- trations in water in spoils aquifers generally are larger than concentrations in water in the coal aquifers they replaced; however, laboratory experiments have indicated that concentrations can decrease if ground water flows from coal-mine spoils to coal. This study was conducted to determine if decreases in concentrations occur onsite and, if so, which geochemical processes caused the decreases. Solid-phase core samples of spoils, unmined over- burden, and coal, and ground-water samples were collected from 16 observation wells at two mine areas. In the Big Sky Mine area, changes in ground- water chemistry along a flow path from an upgradient coal aquifer to a spoils aquifer probably were a result of dedolomitization. Dissolved-solids concentrations were unchanged as water flowed from a spoils aquifer to a downgradient coal aquifer. In the West Decker Mine area, dissolved-solids concentrations apparently decreased from about 4,100 to 2,100 milligrams per liter as water moved along an inferred flow path from a spoils aquifer to a downgradient coal aquifer. Geochemical models were used to analyze changes in water chemistry on the basis of results of solid-phase and aqueous geochemical characteristics. Geochemical processes postulated to result in the apparent decrease in dissolved-solids concentrations along this inferred flow path include bacterial reduction of sulfate, reverse cation exchange within the coal, and precipitation of carbonate and iron-sulfide minerals.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri954097","usgsCitation":"Clark, D., 1995, Geochemical processes in ground water resulting from surface mining of coal at the Big Sky and West Decker Mine areas, southeastern Montana: U.S. Geological Survey Water-Resources Investigations Report 95-4097, vi, 80 p., https://doi.org/10.3133/wri954097.","productDescription":"vi, 80 p.","costCenters":[],"links":[{"id":123515,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4097/report-thumb.jpg"},{"id":55453,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4097/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":465912,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48202.htm","text":"Big Sky Mine area","linkFileType":{"id":5,"text":"html"}},{"id":465913,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48203.htm","text":"West Decker Mine area","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Montana","otherGeospatial":"Big Sky and West Decker Mine areas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -107,\n              46\n            ],\n            [\n              -107,\n              45\n            ],\n            [\n              -106,\n              45\n            ],\n            [\n              -106,\n              46\n            ],\n            [\n              -107,\n              46\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adefa","contributors":{"authors":[{"text":"Clark, D.W.","contributorId":22765,"corporation":false,"usgs":true,"family":"Clark","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":196660,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24698,"text":"ofr95722 - 1995 - Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1993 through June 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:08:28","indexId":"ofr95722","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-722","title":"Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1993 through June 1995","docAbstract":"This report contains hydrologic and climatic data that describe the status of ground-water resources at U.S. Navy Support Facility, Diego Garcia. Data presented are from January 1993 through June 1995, although the report focuses on hydrologic events from April through June 1995. Cumulative rainfall for April through June 1995 was about 14 inches which is 70 percent of the mean cumulative rainfall of about 20 inches for the same 3 months in a year. April through June is within the annual dry season. Rainfall for each month was below average from the respective mean monthly rainfall. All mean rainfall values are calculated for the fixed base period 1951-90. Ground-water withdrawal during April through June 1995 averaged 833,700 gallons per day. Withdrawal for the same 3 months in 1994 averaged 950,000 gallons per day.  At the end of June 1995, the chloride concentration of the composite water supply was 57 milligrams per liter, well below the 250 milligrams per liter secondary drinking-water standard established by the U.S. Environmental Protection Agency. Chloride concentrations of the composite water supply from April through June 1995 ranged between 26 and 62 milligrams per liter. Chloride concentration of ground water in monitoring wells at Cantonment and Air Operations increased since April 1995, with water from the deepest monitoring wells increasing in chloride concentra- tion by about 1000 milligrams per liter. A fuel leak at Air Operations caused the shutdown of ten wells in May 1991. Four of the wells resumed pumping for water-supply purposes in April 1992. The remaining six wells are being used to hydraulically contain and divert fuel migration away from water-supply wells by recirculating about 150,000 gallons of water each day.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nFor sale by the Earth Science Information Center, Open-File Reports Section,","doi":"10.3133/ofr95722","issn":"0094-9140","usgsCitation":"Torikai, J., 1995, Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1993 through June 1995: U.S. Geological Survey Open-File Report 95-722, v, 42 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr95722.","productDescription":"v, 42 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157835,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0722/report-thumb.jpg"},{"id":53731,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0722/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bf31","contributors":{"authors":[{"text":"Torikai, J.D.","contributorId":93926,"corporation":false,"usgs":true,"family":"Torikai","given":"J.D.","affiliations":[],"preferred":false,"id":192401,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23700,"text":"ofr95435 - 1995 - Bibliography for Hayes, Spurr, Crater Peak, Redoubt, Iliamna, Augustine, Douglas, and Aniakchak volcanoes, Alaska","interactions":[],"lastModifiedDate":"2019-06-05T12:34:31","indexId":"ofr95435","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-435","title":"Bibliography for Hayes, Spurr, Crater Peak, Redoubt, Iliamna, Augustine, Douglas, and Aniakchak volcanoes, Alaska","docAbstract":"Alaska has more than 40 active volcanoes, many of which are close to the major population centers of south-central Alaska. This bibliography was compiled to assist in the preparation of volcano hazard evaluations at Cook Inlet volcanoes. It lists articles, reports, and maps about the geology and hydrology of Hayes, Spurr, Redoubt, Iliamna, Augustine, and Douglas volcanoes in the Cook Inlet region as well as Aniakchak Volcano on the Alaska Peninsula. References on the biology and archaeology of areas surrounding each volcano also are included because they may provide useful background information.","language":"English","publisher":"U.S. Geological Survey ","publisherLocation":"Reston, VA","doi":"10.3133/ofr95435","issn":"0094-9140","usgsCitation":"Lemke, K., May, B., and Vanderpool, A., 1995, Bibliography for Hayes, Spurr, Crater Peak, Redoubt, Iliamna, Augustine, Douglas, and Aniakchak volcanoes, Alaska: U.S. Geological Survey Open-File Report 95-435, iii, 32 p. , https://doi.org/10.3133/ofr95435.","productDescription":"iii, 32 p. ","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":52948,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0435/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156311,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0435/report-thumb.jpg"}],"country":"United States","state":"Alaska","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629ac5","contributors":{"authors":[{"text":"Lemke, K.J.","contributorId":12519,"corporation":false,"usgs":true,"family":"Lemke","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":190566,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"May, B.A.","contributorId":8872,"corporation":false,"usgs":true,"family":"May","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":190565,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vanderpool, A.M.","contributorId":14451,"corporation":false,"usgs":true,"family":"Vanderpool","given":"A.M.","affiliations":[],"preferred":false,"id":190567,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":24696,"text":"ofr95118 - 1995 - Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1992 through September 1994","interactions":[],"lastModifiedDate":"2012-02-02T00:08:28","indexId":"ofr95118","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-118","title":"Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1992 through September 1994","docAbstract":"This report contains hydrologic and climatic data that describe the status of ground-water resources at U.S. Navy Support Facility, Diego Garcia. Data are presented from January 1992 through September 1994. This report concentrates on data from July through September 1994, and references historic data from 1992 through June 1994. Total rainfall for the first nine months of 1994 was about 77 inches which is 72 percent of the mean annual rainfall of 106 inches. In comparison, total rainfall for the first nine months of 1992 and 1993 was 67 inches and 69 inches, respectively. Annual rainfall totals in 1992 and 1993 were 93 inches and 95 inches, respectively. Ground-water withdrawal during July through September 1994 has averaged 919,400 gallons per day, while annual withdrawals in 1992 and 1993 averaged 935,900 gallons per day and 953,800 gallons per day, respectively. At the end of September 1994, the chloride concentration of the composite water supply was 56 milligrams per liter, well below the 250 milligrams per liter secondary drinking-water standard established by the U.S. Environmental Protection Agency. Chloride concentrations of the composite water supply from July through September 1994 ranged between 51 and 78 milligrams per liter. Chloride concentration of ground water in monitoring wells at Cantonment and Air Operations increased in July and August, but have leveled off or decreased in September. There has been a general trend of increasing chloride concentrations in the deeper monitoring wells since the 1992 dry season, which began in March 1992. A fuel leak at Air Operations caused the shutdown of ten wells in May 1991. Four of the wells resumed pumping for water-supply purposes in April 1992. The remaining six wells are being used to hydraulically contain and divert fuel migration by recirculating 150,000 gallons of water each day.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nFor sale by the Earth Science Information Center, Open-File Reports Section,","doi":"10.3133/ofr95118","issn":"0094-9140","usgsCitation":"Torikai, J., 1995, Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1992 through September 1994: U.S. Geological Survey Open-File Report 95-118, v, 42 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr95118.","productDescription":"v, 42 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157833,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0118/report-thumb.jpg"},{"id":53729,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0118/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697578","contributors":{"authors":[{"text":"Torikai, J.D.","contributorId":93926,"corporation":false,"usgs":true,"family":"Torikai","given":"J.D.","affiliations":[],"preferred":false,"id":192399,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}