{"pageNumber":"3846","pageRowStart":"96125","pageSize":"25","recordCount":185189,"records":[{"id":22027,"text":"ofr95456 - 1995 - A preliminary assessment of the occurrence and possible sources of MTBE in ground water of the United States, 1993-94","interactions":[],"lastModifiedDate":"2012-02-02T00:07:45","indexId":"ofr95456","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":"95-456","title":"A preliminary assessment of the occurrence and possible sources of MTBE in ground water of the United States, 1993-94","docAbstract":"The 1990 Clean Air Act Amendments require fuel oxygenates to be added to gasoline used in some metropolitan areas to reduce atmospheric concen- trations of carbon monoxide or ozone. Methyl tert-butyl ether (MTBE), is the most commonly used fuel oxygenate and is a relatively new gasoline additive. Nevertheless, out of 60 volatile organic chemicals analyzed, MTBE was the second most frequently detected chemical in samples of shallow ambient ground water from urban areas that were collected during 1993-94 as part of the U.S. Geological Survey's National Water-Quality Assessment program. Samples were collected from 5 drinking-water wells, 12 springs, and 193 monitoring wells in urban areas. No MTBE was detected in drinking-water wells. At a reporting level of 0.2 ug/L (micrograms per liter), MTBE was detected most frequently in shallow ground water from urban areas (27 percent of 210 wells and springs sampled in 8 areas) as compared to shallow ground water from agricultural areas (1.3 percent of 549 wells sampled in 21 areas) or deeper ground water from major aquifers (1 percent of 412 wells sampled in 9 areas). Only 3 percent of the shallow wells sampled in urban areas had concentrations of MTBE that exceed 20 ug/L, which is the estimated lower limit of the U.S. Environmental Protection Agency draft drinking-water health advisory. Because MTBE is persistent and mobile in ground water, it can move from shallow to deeper aquifers with time. In shallow urban ground water, MTBE generally was not found with benzene, toluene, ethylbenzene, or xylenes (BTEX) compounds which commonly are associated with gasoline spills. This disassociation causes uncertainty as to the source of MTBE. Possible sources of MTBE in ground water include point sources, such as leaking storage tanks, and nonpoint sources, such as recharge of precipitation and storm-water runoff.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95456","issn":"0094-9140","usgsCitation":"Squillace, P.J., 1995, A preliminary assessment of the occurrence and possible sources of MTBE in ground water of the United States, 1993-94: U.S. Geological Survey Open-File Report 95-456, v, 16 p. :ill. ;28 cm., https://doi.org/10.3133/ofr95456.","productDescription":"v, 16 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":152972,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0456/report-thumb.jpg"},{"id":51493,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0456/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab381","contributors":{"authors":[{"text":"Squillace, P. J.","contributorId":8878,"corporation":false,"usgs":true,"family":"Squillace","given":"P.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":186758,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21879,"text":"ofr95813 - 1995 - Hydrologic effects associated with the January 17, 1994 Northridge, California, earthquake","interactions":[],"lastModifiedDate":"2019-09-06T15:49:42","indexId":"ofr95813","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":"95-813","title":"Hydrologic effects associated with the January 17, 1994 Northridge, California, earthquake","docAbstract":"<p>This report compiles hydrologic observations in southern California associated with the 1994 Mw = 6.7 Northridge, California earthquake. In southern California, the largest ground water level change was a drop of 52 cm at Crystalaire. Most of the steplike water-level changes recorded following the Northridge earthquake agreed in direction with the sign of the calculated coseismic volume strain field. A spring discharge increase at Southern Pacific Springs was reported to have preceded the earthquake by several days. Outside of southern California, water-level changes were also observed, but are not consistent in sign or size with the static strain field of the earthquake sequence.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95813","issn":"0566-8174","usgsCitation":"Quilty, E., Farrar, C.D., Galloway, D., Hamlin, S.N., Laczniak, R.J., Roeloffs, E., Sorey, M., and Woodcock, D., 1995, Hydrologic effects associated with the January 17, 1994 Northridge, California, earthquake: U.S. Geological Survey Open-File Report 95-813, ii, 47 p., https://doi.org/10.3133/ofr95813.","productDescription":"ii, 47 p.","numberOfPages":"49","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":51367,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0813/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153744,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0813/report-thumb.jpg"}],"country":"United States","state":"California, Nevada, Oregon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -125.41992187499999,\n              31.615965936476076\n            ],\n            [\n              -113.99414062499999,\n              31.615965936476076\n            ],\n            [\n              -113.99414062499999,\n              43.100982876188546\n            ],\n            [\n              -125.41992187499999,\n              43.100982876188546\n            ],\n            [\n              -125.41992187499999,\n              31.615965936476076\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db607120","contributors":{"authors":[{"text":"Quilty, E.G.","contributorId":87160,"corporation":false,"usgs":true,"family":"Quilty","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":186096,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Farrar, C. D.","contributorId":71978,"corporation":false,"usgs":true,"family":"Farrar","given":"C.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":186094,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Galloway, D. L. 0000-0003-0904-5355","orcid":"https://orcid.org/0000-0003-0904-5355","contributorId":31383,"corporation":false,"usgs":true,"family":"Galloway","given":"D. L.","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"preferred":false,"id":186091,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hamlin, S. N.","contributorId":46560,"corporation":false,"usgs":true,"family":"Hamlin","given":"S.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":186093,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Laczniak, R. J.","contributorId":46104,"corporation":false,"usgs":true,"family":"Laczniak","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":186092,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Roeloffs, E.A.","contributorId":88742,"corporation":false,"usgs":true,"family":"Roeloffs","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":186097,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Sorey, M.L.","contributorId":73185,"corporation":false,"usgs":true,"family":"Sorey","given":"M.L.","affiliations":[],"preferred":false,"id":186095,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Woodcock, D.E.","contributorId":8499,"corporation":false,"usgs":true,"family":"Woodcock","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":186090,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":21863,"text":"ofr9575G - 1995 - Hydrocarbon source rock characterization and maturity based on rock-eval pyrolysis and vitrinite reflectance of Eocene strata, southern Oregon Coast Range, Douglas and Coos Counties, southwest Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:07:44","indexId":"ofr9575G","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":"95-75","chapter":"G","title":"Hydrocarbon source rock characterization and maturity based on rock-eval pyrolysis and vitrinite reflectance of Eocene strata, southern Oregon Coast Range, Douglas and Coos Counties, southwest Oregon","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr9575G","issn":"0566-8174","usgsCitation":"Lillis, P.G., Daws, T., Pawlewicz, M., Niem, A.R., and Ryu, I., 1995, Hydrocarbon source rock characterization and maturity based on rock-eval pyrolysis and vitrinite reflectance of Eocene strata, southern Oregon Coast Range, Douglas and Coos Counties, southwest Oregon: U.S. Geological Survey Open-File Report 95-75, 27 p.; 30 leaves :ill., map ;28 cm., https://doi.org/10.3133/ofr9575G.","productDescription":"27 p.; 30 leaves :ill., map ;28 cm.","costCenters":[],"links":[{"id":153025,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0075g/report-thumb.jpg"},{"id":51349,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0075g/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db6296a1","contributors":{"authors":[{"text":"Lillis, Paul G. 0000-0002-7508-1699 plillis@usgs.gov","orcid":"https://orcid.org/0000-0002-7508-1699","contributorId":1817,"corporation":false,"usgs":true,"family":"Lillis","given":"Paul","email":"plillis@usgs.gov","middleInitial":"G.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":186025,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Daws, T.A.","contributorId":56651,"corporation":false,"usgs":true,"family":"Daws","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":186027,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pawlewicz, M. J.","contributorId":75111,"corporation":false,"usgs":true,"family":"Pawlewicz","given":"M. J.","affiliations":[],"preferred":false,"id":186029,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Niem, A. R.","contributorId":54984,"corporation":false,"usgs":true,"family":"Niem","given":"A.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":186026,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ryu, In-Chang","contributorId":69584,"corporation":false,"usgs":true,"family":"Ryu","given":"In-Chang","email":"","affiliations":[],"preferred":false,"id":186028,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":23780,"text":"ofr95465 - 1995 - Design of monitor wells, hydrogeology, and ground-water quality beneath Country Pond, Kingston, New Hampshire","interactions":[],"lastModifiedDate":"2012-02-02T00:08:18","indexId":"ofr95465","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":"95-465","title":"Design of monitor wells, hydrogeology, and ground-water quality beneath Country Pond, Kingston, New Hampshire","docAbstract":"Ten monitoring well were installed in May 1993 to collect data on the hydrogeology and ground-water quality beneath Country Pond, in Kingston, New Hampshire. Monitoring wells were installed 4 to 48 feet beneath the pond surface in stratified drift that was up to 40 feet thick. The stratified drift is overlain by up to 35 feet of fine-grained, predominantly organic, lake-bottom sediment. The potentiometric head in the aquifer was at or above the pond surface and up to 0.8 foot above the pond surface at one location. Water-quality analyses detected numerous volatile organic compounds including chloroethane, benzene, dichlorobenzenes, and 1,1-dichloroethane at maximum concentrations of 110, 43, 54, and 92 mg/L, respectively. The maximum concentration of total volatile organic compounds detected in ground water from a monitoring well was 550 mg/L in November 1993. Ground-water samples with high concentrations of volatile organic compounds also had elevated specific conductances indicating the presence of other non-organic contaminants. Water-quality analyses indicate that a plume of contaminated ground water extends at least 300 feet in a northeast direction beneath the pond.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S. Geological Survey, Earth Science Information Center [distributor],","doi":"10.3133/ofr95465","issn":"0094-9140","usgsCitation":"Mack, T.J., 1995, Design of monitor wells, hydrogeology, and ground-water quality beneath Country Pond, Kingston, New Hampshire: U.S. Geological Survey Open-File Report 95-465, iv, 16 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr95465.","productDescription":"iv, 16 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157394,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0465/report-thumb.jpg"},{"id":53010,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0465/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667dc5","contributors":{"authors":[{"text":"Mack, Thomas J. 0000-0002-0496-3918","orcid":"https://orcid.org/0000-0002-0496-3918","contributorId":39814,"corporation":false,"usgs":true,"family":"Mack","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":190711,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26008,"text":"wri924192 - 1995 - Geohydrology and water quality of stratified-drift aquifers in the middle Merrimack River basin, south-central New Hampshire","interactions":[],"lastModifiedDate":"2012-02-02T00:08:24","indexId":"wri924192","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":"92-4192","title":"Geohydrology and water quality of stratified-drift aquifers in the middle Merrimack River basin, south-central New Hampshire","docAbstract":"The U.S. Geological Survey, in cooperation with the State of New Hampshire, Department of Environmental Services, Water Resources Division has assessed the geohydrology and water quality of stratified-drift aquifers in the middle Merrimack River basin in south-central New Hampshire. The middle Merrimack River basin drains 469 square miles; 98 square miles is underlain by stratified-drift aquifers. Saturated thickness of stratified drift within the study area is generally less than 40 feet but locally greater than 100 feet. Transmissivity of stratified-drift aquifers is generally less than 2,000 feet squared per day but locally exceeds 6, 000 feet squared per day. At present (1990), ground-water withdrawals from stratified drift for public supply are about 0.4 million gallons per day within the basin. Many of the stratified-drift aquifers within the study area are not developed to their fullest potential. The geohydrology of stratified-drift aquifers was investigated by focusing on basic aquifer properties, including aquifer boundaries; recharge, discharge, and direction of ground-water flow; saturated thickness and storage; and transmissivity. Surficial geologic mapping assisted in the determination of aquifer boundaries. Data from 757 wells and test borings were used to produce maps of water-table altitude, saturated thickness, and transmissivity of stratified drift. More than 10 miles of seismic-refraction profiling and 14 miles of seismic-reflection profiling were also used to construct the water table and saturated-thickness maps. Stratified-drift aquifers in the southern, western, and central parts of the study area are typically small and discontinuous, whereas aquifers in the eastern part along the Merrimack River valley are continuous. The Merrimack River valley aquifers formed in glacial Lakes Merrimack and Hooksett. Many other smaller discontinuous aquifers formed in small temporary ponds during deglaciation. A stratified-drift aquifer in Goffstown was analyzed for aquifer yield by use of a two-dimensional, finite-difference ground-water-flow model. Yield of the Goffstown aquifer was estimated to be 2.5 million gallons per day. Sensitivity analysis showed that the estimate of aquifer yield was most sensitive to changes in hydraulic conductivity. The amount of water induced into the aquifer from the Piscataquog River was most affected by changes in estimates of streambed conductance. Results of analysis of water samples from 10 test wells indicate that, with some exceptions, water in the stratified-drift aquifers generally meets U.S. Environmental Protection Agency primary and secondary drinking-water regulations. Water from two wells had elevated sodium concentrations, waterfront two wells had elevated concentrations of dissolved iron, and waterfront seven wells had elevated concentrations of manganese. Known areas of contamination were avoided during water-quality sampling.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S. Geological Survey, Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri924192","usgsCitation":"Ayotte, J., and Toppin, K.W., 1995, Geohydrology and water quality of stratified-drift aquifers in the middle Merrimack River basin, south-central New Hampshire: U.S. Geological Survey Water-Resources Investigations Report 92-4192, 1 v. (various pagings) :ill., maps (some col.) ;28 cm.;  PGS - 149 p., 4 over-size sheets, scale 1:24,000, https://doi.org/10.3133/wri924192.","productDescription":"1 v. (various pagings) :ill., maps (some col.) ;28 cm.;  PGS - 149 p., 4 over-size sheets, scale 1:24,000","costCenters":[],"links":[{"id":2007,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri924192/","linkFileType":{"id":5,"text":"html"}},{"id":123655,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_92_4192.jpg"},{"id":54767,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4192/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54768,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4192/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54769,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4192/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54770,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4192/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54771,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4192/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54772,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4192/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54773,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4192/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54774,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4192/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8b8c","contributors":{"authors":[{"text":"Ayotte, Joseph D. jayotte@usgs.gov","contributorId":1802,"corporation":false,"usgs":true,"family":"Ayotte","given":"Joseph D.","email":"jayotte@usgs.gov","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":false,"id":195634,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Toppin, Kenneth W. ktoppin@usgs.gov","contributorId":3753,"corporation":false,"usgs":true,"family":"Toppin","given":"Kenneth","email":"ktoppin@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":195635,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29174,"text":"wri954205 - 1995 - Processes controlling dissolved oxygen and pH in the upper Willamette River basin, Oregon, 1994","interactions":[],"lastModifiedDate":"2017-02-07T08:35:34","indexId":"wri954205","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":"95-4205","title":"Processes controlling dissolved oxygen and pH in the upper Willamette River basin, Oregon, 1994","docAbstract":"<p>In July and August of 1994, the U. S. Geological Survey in cooperation with the Oregon Department of Environmental Quality (ODEQ) collected data to document the spatial extent and diel variability of dissolved oxygen (DO) concentrations and pH levels in selected reaches of streams in the upper Willamette River Basin. These data were also collected to identify primary factors that control DO concentrations downstream from major point sources as well as to provide ODEQ with data to refine calibration of their steady-state DO and nutrient models for the upper Willamette River Basin. All of the reaches studied had diel variations in DO and pH. The magnitude of the diel variations in DO ranged from 0.2 to 3.9 milligrams per liter (7 to 50 percent-saturation units based on ambient water temperature and barometric pressure) and in pH from 0.3 to 1.4 units. However, of the reaches studied, only the Coast Fork Willamette River from river mile (RM) 21.7 to 12.5 and the Willamette River from RM 151 to 141.6 had field measured violations of State standards for DO and pH. DO concentration and pH in water depend on many factors. Data were collected to examine several major factors, including BOD (biochemical oxygen demand), carbonaceous BOD, nitrogenous BOD, and measures of photosynthetic activity. Of the four study reaches, only a short stretch of the Coast Fork Willamette River has potential for important levels of oxygen consumption from BOD or nitrification. Additionally, water-column primary-productivity measurements indicated that respiration and photosynthesis by free-floating algae did not explain the observed diel variations in DO in the study reaches. Results from a simple mathematical model incorporating measures of community respiration and net primary productivities indicated that periphyton are capable of producing a diel variation of the order of magnitude observed during the August study period. In the Willamette River near Peoria, the combined periphyton DO consumption and production estimate at RM 151 (2.4 mg/L) and RM 144.6 (1.7 mg/L) would account for 90 and 63 percent, respectively, of the observed diel fluctuation. The estimates for the Corvallis reach at RM 132.6 (0.4 mg/L) and RM 130.7 (2.9 mg/L) had a considerably larger range of 36 to 264 percent of DO saturation, respectively. Therefore, because BOD and phytoplankton do not appear to be important contributors to diel DO fluctuations, periphyton are likely the primary contributor to diel fluctuations in the upper Willamette River Basin during July and August.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/wri954205","collaboration":"Prepared in cooperation with Oregon Department of Environmental Quality and Willamette River Technical Advisory Steering Committee","usgsCitation":"Pogue, T.R., and Anderson, C., 1995, Processes controlling dissolved oxygen and pH in the upper Willamette River basin, Oregon, 1994: U.S. Geological Survey Water-Resources Investigations Report 95-4205, iv, 71 p., https://doi.org/10.3133/wri954205.","productDescription":"iv, 71 p.","numberOfPages":"77","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1994-01-01","temporalEnd":"1994-12-31","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":58047,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4205/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159368,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4205/report-thumb.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"Willamette River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.914794921875,\n              42.85985981506279\n            ],\n            [\n              -123.914794921875,\n              45.62172169252446\n            ],\n            [\n              -121.025390625,\n              45.62172169252446\n            ],\n            [\n              -121.025390625,\n              42.85985981506279\n            ],\n            [\n              -123.914794921875,\n              42.85985981506279\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e508","contributors":{"authors":[{"text":"Pogue, Ted R. Jr.","contributorId":13998,"corporation":false,"usgs":true,"family":"Pogue","given":"Ted","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":201084,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, Chauncey W. 0000-0002-1016-3781 chauncey@usgs.gov","orcid":"https://orcid.org/0000-0002-1016-3781","contributorId":1151,"corporation":false,"usgs":true,"family":"Anderson","given":"Chauncey W.","email":"chauncey@usgs.gov","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":false,"id":201083,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":27410,"text":"wri944110 - 1995 - Water levels in the Calumet aquifer and their relation to surface-water levels in northern Lake County, Indiana, 1985-92","interactions":[],"lastModifiedDate":"2016-05-24T10:55:16","indexId":"wri944110","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":"94-4110","title":"Water levels in the Calumet aquifer and their relation to surface-water levels in northern Lake County, Indiana, 1985-92","docAbstract":"<p>The U.S. Geological Survey made 2,328 water-level measurements at a total of 96 ground-water and surface-water sites in northern Lake County, Indiana, from August 1985 through September 1992. This report lists and summarizes the significance of the measurements. Northern Lake County is on the southern shore of Lake Michigan and includes the cities of East Chicago, Gary, Hammond, and Whiting. The study area is underlain by the unconfined Calumet aquifer and receives about 36 inches of precipitation per year.</p>\n<p>The U.S. Geological Survey investigated ground-water levels and flow in the Calumet aquifer and the effect of Lake Michigan levels on ground-water and surface-water levels throughout the study area. Summary statistics of the water-level data were computed for each site.</p>\n<p>Ground-water levels annually reach a maximum in June or July and a minimum in September or October. Measured groundwater fluctuations in the Calumet aquifer during the study period ranged from 0.40 to 5.01 feet, and the mean ground-water fluctuation was about 2.3 feet The largest surface-water fluctuations were affected by record setting Lake Michigan levels. Midmonth daily averages for the data-collection period show that Lake Michigan fluctuated 4.14 feet Water-level fluctuations on the Grand Calumet River were from 1.06 to 2.45 feet.</p>\n<p>Analysis of water-level data indicates that the 1988 drought did not substantially affect water levels in the Calumet aquifer, but the deficit in precipitation reversed vertical flow gradients in ground water at three paired deep and shallow wells. High water levels in Lake Michigan during 1985-87 created long-term backwater effects on the Grand Calumet River as far as 11.0 miles upstream from Lake Michigan.</p>\n<p>Analysis of water-level data from the data-collection network indicates that the water table normally slopes toward streams, ditches, sewers, the Indiana Harbor Canal, and Lake Michigan. The slope of the water table toward the Grand Calumet River is greatest in the winter and can decrease to being almost horizontal in the summer. Wells near streams respond quickly to nearby surface-water-level changes. Water-table maps indicate that sewers and dewatering systems are lowering ground-water levels in large areas. Ditches, the Grand Calumet River, and the Indiana Harbor Canal connect the Lake Michigan water level to large parts of the study area. The surface-water stage in the Indiana Harbor Canal, which functions as a ditch, can equal Lake Michigan's stage up to 3.75 miles inland from the lakeshore. Human activity, the stage of Lake Michigan, and the storage capacity of the Calumet aquifer combine to reduce vertical changes in the water table in the study area.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/wri944110","collaboration":"Indiana Department of Environmental Management","usgsCitation":"Greeman, T.K., 1995, Water levels in the Calumet aquifer and their relation to surface-water levels in northern Lake County, Indiana, 1985-92: U.S. Geological Survey Water-Resources Investigations Report 94-4110, v, 61 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944110.","productDescription":"v, 61 p. :ill., maps ;28 cm.","startPage":"1","endPage":"61","numberOfPages":"67","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":158683,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4110/report-thumb.jpg"},{"id":56269,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4110/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana","county":"Lake","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-87.2223,41.6248],[-87.2222,41.6152],[-87.2221,41.6039],[-87.2218,41.5698],[-87.22,41.4632],[-87.2198,41.3747],[-87.2196,41.3601],[-87.22,41.3388],[-87.2198,41.3188],[-87.2197,41.3043],[-87.2189,41.2893],[-87.2187,41.2744],[-87.2193,41.2671],[-87.219,41.2426],[-87.2184,41.2417],[-87.2263,41.2353],[-87.2762,41.2187],[-87.2859,41.2154],[-87.3241,41.1862],[-87.3313,41.1829],[-87.3405,41.1824],[-87.3448,41.1824],[-87.38,41.1726],[-87.394,41.1625],[-87.4,41.1625],[-87.4055,41.1625],[-87.4147,41.1619],[-87.4411,41.1731],[-87.4466,41.174],[-87.4484,41.1744],[-87.4587,41.1702],[-87.4801,41.1701],[-87.5263,41.1661],[-87.5261,41.267],[-87.5265,41.2983],[-87.527,41.4086],[-87.5265,41.4712],[-87.5255,41.5516],[-87.5239,41.6941],[-87.524,41.7135],[-87.5234,41.7131],[-87.5134,41.7054],[-87.5158,41.7027],[-87.5133,41.7004],[-87.4997,41.6914],[-87.4922,41.6865],[-87.4848,41.6843],[-87.4829,41.6811],[-87.4768,41.6789],[-87.4712,41.6753],[-87.4613,41.6718],[-87.4503,41.6741],[-87.4397,41.6647],[-87.436,41.6656],[-87.4355,41.6729],[-87.4245,41.6802],[-87.4177,41.6753],[-87.4396,41.6565],[-87.4228,41.6439],[-87.4167,41.6439],[-87.4099,41.644],[-87.4087,41.644],[-87.4044,41.6413],[-87.392,41.6382],[-87.3748,41.6329],[-87.3711,41.6315],[-87.3538,41.6285],[-87.3384,41.6259],[-87.3274,41.6259],[-87.3218,41.6219],[-87.315,41.6201],[-87.3101,41.6201],[-87.3058,41.6202],[-87.3003,41.6202],[-87.296,41.6198],[-87.2831,41.6203],[-87.2702,41.6208],[-87.2223,41.6248]]]},\"properties\":{\"name\":\"Lake\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9d21","contributors":{"authors":[{"text":"Greeman, Theodore K.","contributorId":30655,"corporation":false,"usgs":true,"family":"Greeman","given":"Theodore","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":198064,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21161,"text":"ofr95274 - 1995 - Potassium-argon apparent ages of rocks from the western Okanogan Range, the Methow Basin, and adjacent areas, north-central Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:07:41","indexId":"ofr95274","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":"95-274","title":"Potassium-argon apparent ages of rocks from the western Okanogan Range, the Methow Basin, and adjacent areas, north-central Washington","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr95274","usgsCitation":"Todd, V.R., 1995, Potassium-argon apparent ages of rocks from the western Okanogan Range, the Methow Basin, and adjacent areas, north-central Washington: U.S. Geological Survey Open-File Report 95-274, 10 p. ;28 cm., https://doi.org/10.3133/ofr95274.","productDescription":"10 p. ;28 cm.","costCenters":[],"links":[{"id":153363,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0274/report-thumb.jpg"},{"id":50752,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0274/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683976","contributors":{"authors":[{"text":"Todd, V. R.","contributorId":89918,"corporation":false,"usgs":true,"family":"Todd","given":"V.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":183950,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21671,"text":"ofr94523 - 1995 - Chemical data for water samples collected during four upriver cruises on the Mississippi River between New Orleans, Louisiana, and Minneapolis, Minnesota, May 1990-April 1992","interactions":[],"lastModifiedDate":"2018-10-22T18:45:05","indexId":"ofr94523","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":"94-523","title":"Chemical data for water samples collected during four upriver cruises on the Mississippi River between New Orleans, Louisiana, and Minneapolis, Minnesota, May 1990-April 1992","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr94523","issn":"0566-8174","usgsCitation":"1995, Chemical data for water samples collected during four upriver cruises on the Mississippi River between New Orleans, Louisiana, and Minneapolis, Minnesota, May 1990-April 1992: U.S. Geological Survey Open-File Report 94-523, xii, 297 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr94523.","productDescription":"xii, 297 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":154405,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0523/report-thumb.jpg"},{"id":51215,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0523/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3c50","contributors":{"editors":[{"text":"Moody, J. A.","contributorId":32930,"corporation":false,"usgs":true,"family":"Moody","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":749279,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"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":21786,"text":"ofr95353 - 1995 - Flow duration of Kentucky streams through 1990; historical and monthly flow characteristics, including the effects of reservoirs","interactions":[],"lastModifiedDate":"2012-02-02T00:07:50","indexId":"ofr95353","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":"95-353","title":"Flow duration of Kentucky streams through 1990; historical and monthly flow characteristics, including the effects of reservoirs","docAbstract":"This report presents flow-duration tables and plots for selected streamflow sites in Kentucky with three or more years of continuous record through 1990. Flow duration describes the frequency with which given streamflows are equalled or exceeded. The flow-duration tables were computed using daily mean discharge values for the entire period specified and for each month of the period specified. Only complete years of record were used for the computation. For sites where the streamflow is affected by regulation, separate tables are presented for the period before regulation (unregulated), the period of record after regulation (regulated) and the entire period of record (historical). Flow-duration plots are also presented for each station using the data for the entire period specified. Where practicable, several flow-duration plots are shown together. This includes stations on the same stream, such as main-stem stations, and stations within the same watershed. For stations affected by regulation, which have up to three sets of data available for one station (unregulated, regulated, and historical), the three plots are shown together to clearly illustrate the influence of regulation in augmenting low flows and reducing high flows.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S. Geological Survey, Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95353","issn":"0566-8174","usgsCitation":"Ruhl, K., Burns, R., Martin, G.R., and Allgeier, D., 1995, Flow duration of Kentucky streams through 1990; historical and monthly flow characteristics, including the effects of reservoirs: U.S. Geological Survey Open-File Report 95-353, iii, 291 p. (1 folded) :ill., maps ;28 cm., https://doi.org/10.3133/ofr95353.","productDescription":"iii, 291 p. (1 folded) :ill., maps ;28 cm.","costCenters":[],"links":[{"id":153766,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0353/report-thumb.jpg"},{"id":51285,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0353/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d7e4b07f02db5deb48","contributors":{"authors":[{"text":"Ruhl, K.J.","contributorId":35322,"corporation":false,"usgs":true,"family":"Ruhl","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":185677,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burns, R.J.","contributorId":50930,"corporation":false,"usgs":true,"family":"Burns","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":185678,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Martin, G. R.","contributorId":14004,"corporation":false,"usgs":true,"family":"Martin","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":185675,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Allgeier, D.P.","contributorId":27881,"corporation":false,"usgs":true,"family":"Allgeier","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":185676,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":24601,"text":"ofr95317 - 1995 - Standard procedures and quality-control practices for the U.S. Geological Survey National Field Quality Assurance Program from 1982 through 1993","interactions":[],"lastModifiedDate":"2012-02-02T00:08:06","indexId":"ofr95317","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":"95-317","title":"Standard procedures and quality-control practices for the U.S. Geological Survey National Field Quality Assurance Program from 1982 through 1993","docAbstract":"The U.S. Geological Survey operates the National Field Quality Assurance Program to provide quality- assurance reference samples to field personnel who make water-quality field measurements. The program monitors the accuracy and precision of pH, specific conductance, and alkalinity field measurements. This report documents the operational procedures and quality-control techniques used in operating the quality-assurance program.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95317","issn":"0094-9140","usgsCitation":"Stanley, D., 1995, Standard procedures and quality-control practices for the U.S. Geological Survey National Field Quality Assurance Program from 1982 through 1993: U.S. Geological Survey Open-File Report 95-317, iv, 75 p. :ill. ;28 cm., https://doi.org/10.3133/ofr95317.","productDescription":"iv, 75 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":155470,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0317/report-thumb.jpg"},{"id":53649,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0317/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de44a","contributors":{"authors":[{"text":"Stanley, D.L.","contributorId":36171,"corporation":false,"usgs":true,"family":"Stanley","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":192231,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":27608,"text":"wri954098 - 1995 - Water-quality characteristics of selected public recreational lakes and ponds in Connecticut","interactions":[],"lastModifiedDate":"2012-02-02T00:08:42","indexId":"wri954098","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":"95-4098","title":"Water-quality characteristics of selected public recreational lakes and ponds in Connecticut","docAbstract":"Reconnaissance limnological and lakebed-sediment surveys were conducted in Connecticut during 1989-91 by the U.S. Geological Survey, in cooperation with the Connecticut Department of Environmental Protec- tion, to evaluate water-quality characteristics of selected public recreational lakes and ponds in the State. Limnological surveys were conducted on 49 lakes and ponds selected from a list of 105 publicly owned waterbodies that qualified for water- quality assessments under Section 314 of the Federal Clean Water Act. Lakebed-sediment surveys were conducted in 9 river impoundments and 1 riverine lake below industrial areas and 2 headwater lakes in relatively pristine areas. The limnological surveys consisted of two sampling events--during spring turnover and during the summer stratifi- cation. Each sampling event included depth profiles of water temperature, specific conductance, hydrogen-ion activity, and dissolved oxygen concen- trations; measurements of Secchi disc transparency; and the collection of samples for the analyses of alkalinity, chlorophyll, phosphorus, and nitrogen concentrations. Areal extent and population density of the dominant aquatic macrophytes were qualita- tively noted during the summer sampling event. These water-quality data were used to determine the trophic classification and acidification status of the 49 lakes. The trophic classification yielded the following results: 2 oligotrophic, 8 early mesotrophic, 13 mesotrophic, 5 late mesotrophic, 10 eutrophic, and 11 highly eutrophic lakes. In terms of acidification status, 7 lakes were classified as acid threatened and 42 as not threatened. A Wilcoxon two-tailed signed rank test was used to compare data for 13 lakes and ponds from the present survey with data from the 1973-75 or 1978-79 surveys conducted by the Connecticut Agricultural Experiment Station and Connecticut Department of Environmental Protection. The test showed no significant difference at the 90 percent confidence level for spring nitrogen and summer chlorophyll-a concen- trations, a significant increase at the 90 percent confidence level in summer phosphorus concentra- tions, and a significant decrease at the 95 percent confidence level in summer transparency. For the lakebed-sediment surveys, composite-grab samples were collected from the deepest part of each lake. Samples were analyzed for arsenic, cyanide, organic and inorganic carbon, selected metals, and methylene-extractable, synthetic organic compounds classified by the U.S. Environmental Protection Agency as semi-volatile priority pollutants. Hanover Pond, Eagleville Lake, and West Thompson Lake had three of the four highest concentrations of cadmium, chromium, copper, lead, nickel, zinc, and cyanide. The four lakes with the highest concentrations of arsenic (Aspinook Pond, Fitchville Pond, Mashapaug Pond, and West Thompson Lake) are located in the eastern part of Connecticut. The three samples with the highest mercury concentrations were from Lake Lillinonah and Lake Zoar. There appears to be a positive correlation between the concentrations of cadmium, chromium, copper, lead, nickel, zinc, and cyanide. Only 15 of the 54 synthetic organic compounds analyzed for were detected in 9 of the 12 lakes sampled. Of these 15 compounds, 14 are polycyclic aromatic hydrocarbons and the 15th is a phthalate ester. Hanover Pond had the most compounds detected (9), and phenanthrene was the compound detected in the most lakes (8).","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri954098","usgsCitation":"Healy, D.F., and Kulp, K., 1995, Water-quality characteristics of selected public recreational lakes and ponds in Connecticut: U.S. Geological Survey Water-Resources Investigations Report 95-4098, ix, 277 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri954098.","productDescription":"ix, 277 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159026,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4098/report-thumb.jpg"},{"id":56474,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4098/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fafec","contributors":{"authors":[{"text":"Healy, D. F.","contributorId":97120,"corporation":false,"usgs":true,"family":"Healy","given":"D.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":198405,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kulp, K.P.","contributorId":49791,"corporation":false,"usgs":true,"family":"Kulp","given":"K.P.","email":"","affiliations":[],"preferred":false,"id":198404,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24264,"text":"ofr95805B - 1995 - Time drill; an introduction to geologic time","interactions":[],"lastModifiedDate":"2012-02-02T00:08:00","indexId":"ofr95805B","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":"95-805","chapter":"B","title":"Time drill; an introduction to geologic time","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr95805B","issn":"0094-9140","usgsCitation":"Purcell, K.P., 1995, Time drill; an introduction to geologic time: U.S. Geological Survey Open-File Report 95-805, 1 computer disk ;3 1/2 in., https://doi.org/10.3133/ofr95805B.","productDescription":"1 computer disk ;3 1/2 in.","costCenters":[],"links":[{"id":154985,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b741","contributors":{"authors":[{"text":"Purcell, Kevin P.","contributorId":101279,"corporation":false,"usgs":true,"family":"Purcell","given":"Kevin","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":191592,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6610,"text":"fs19995 - 1995 - Environmental effects of mineral deposits and mines in the Prescott National Forest, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:05:53","indexId":"fs19995","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":"199-95","title":"Environmental effects of mineral deposits and mines in the Prescott National Forest, Arizona","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/fs19995","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, Environmental effects of mineral deposits and mines in the Prescott National Forest, Arizona: U.S. Geological Survey Fact Sheet 199-95, 1 sheet : ill., map ; 28 cm. ill., map ;, https://doi.org/10.3133/fs19995.","productDescription":"1 sheet : ill., map ; 28 cm. ill., map ;","costCenters":[],"links":[{"id":126833,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1995/0199/report-thumb.jpg"},{"id":34057,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1995/0199/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db6023da","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528752,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21988,"text":"ofr95819 - 1995 - Onshore-offshore wide-angle seismic recording in October 1994 near Cape Blanco, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:07:54","indexId":"ofr95819","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":"95-819","title":"Onshore-offshore wide-angle seismic recording in October 1994 near Cape Blanco, Oregon","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr95819","issn":"0094-9140","usgsCitation":"Brocher, T., Davis, M., Clark, S., and Geist, E., 1995, Onshore-offshore wide-angle seismic recording in October 1994 near Cape Blanco, Oregon: U.S. Geological Survey Open-File Report 95-819, 69 p. :ill. ;28 cm., https://doi.org/10.3133/ofr95819.","productDescription":"69 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":154320,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0819/report-thumb.jpg"},{"id":51458,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0819/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db6919e1","contributors":{"authors":[{"text":"Brocher, T.M. 0000-0002-9740-839X","orcid":"https://orcid.org/0000-0002-9740-839X","contributorId":69994,"corporation":false,"usgs":true,"family":"Brocher","given":"T.M.","affiliations":[],"preferred":false,"id":186563,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, M.J.","contributorId":96718,"corporation":false,"usgs":true,"family":"Davis","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":186565,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clark, S.H. Jr.","contributorId":30250,"corporation":false,"usgs":true,"family":"Clark","given":"S.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":186562,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Geist, E.L. 0000-0003-0611-1150","orcid":"https://orcid.org/0000-0003-0611-1150","contributorId":71993,"corporation":false,"usgs":true,"family":"Geist","given":"E.L.","affiliations":[],"preferred":false,"id":186564,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":22277,"text":"ofr95429 - 1995 - Water-quality, bed-sediment, and biological data (October 1993 through September 1994) and statistical summaries of data for streams in the Upper Clark Fork basin, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:08:02","indexId":"ofr95429","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":"95-429","title":"Water-quality, bed-sediment, and biological data (October 1993 through September 1994) and statistical summaries of data for streams in the Upper Clark Fork basin, Montana","docAbstract":"Water, bed sediment, and biota were sampled in streams from Butte to below Missoula as part of a program to characterize aquatic resources in the upper Clark Fork basin of western Montana. Water- quality data were obtained periodically at 16 stations during October 1993 through September 1994 (water year 1994); daily suspended-sediment data were obtained at six of these stations. Bed-sediment and biological data were obtained at 11 stations in August 1994. Sampling stations were located on the Clark Fork and major tributaries. The primary constituents analyzed were trace elements associated with mine tailings from historical mining and smelting activities. Water-quality data include concentrations of major ions, trace elements, and suspended sediment in samples collected periodically during water year 1994. Daily values of streamflow, suspended-sediment concentration, and suspended- sediment discharge are given for six stations. Bed- sediment data include trace-element concentrations in the fine and bulk fractions. Biological data include trace-element concentrations in whole-body tissue of aquatic benthic insects. Quality-assurance data are reported for analytical results of water, bed sediment, and biota. Statistical summaries of bed sediment, and biological data are provided for the period of record at each station since 1985.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95429","issn":"0094-9140","usgsCitation":"Lambing, J., Hornberger, M.I., Axtmann, E., and Dodge, K.A., 1995, Water-quality, bed-sediment, and biological data (October 1993 through September 1994) and statistical summaries of data for streams in the Upper Clark Fork basin, Montana: U.S. Geological Survey Open-File Report 95-429, iv, 104 p. :map ;28 cm., https://doi.org/10.3133/ofr95429.","productDescription":"iv, 104 p. :map ;28 cm.","costCenters":[],"links":[{"id":155793,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0429/report-thumb.jpg"},{"id":51699,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0429/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cbe4b07f02db54397d","contributors":{"authors":[{"text":"Lambing, J. H.","contributorId":100860,"corporation":false,"usgs":true,"family":"Lambing","given":"J. H.","affiliations":[],"preferred":false,"id":187911,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hornberger, Michelle I. 0000-0002-7787-3446","orcid":"https://orcid.org/0000-0002-7787-3446","contributorId":23574,"corporation":false,"usgs":true,"family":"Hornberger","given":"Michelle","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":187908,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Axtmann, E.V.","contributorId":30652,"corporation":false,"usgs":true,"family":"Axtmann","given":"E.V.","email":"","affiliations":[],"preferred":false,"id":187909,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dodge, K. A.","contributorId":40615,"corporation":false,"usgs":true,"family":"Dodge","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":187910,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":22940,"text":"ofr95323 - 1995 - Flood magnitude and frequency of Eightmile Branch tributary at the culvert on New Jersey route 72, at Stafford Township, New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:07:55","indexId":"ofr95323","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":"95-323","title":"Flood magnitude and frequency of Eightmile Branch tributary at the culvert on New Jersey route 72, at Stafford Township, New Jersey","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95323","issn":"0094-9140","usgsCitation":"Dunne, P., 1995, Flood magnitude and frequency of Eightmile Branch tributary at the culvert on New Jersey route 72, at Stafford Township, New Jersey: U.S. Geological Survey Open-File Report 95-323, iv, 10 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr95323.","productDescription":"iv, 10 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":154281,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0323/report-thumb.jpg"},{"id":52341,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0323/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eeff9","contributors":{"authors":[{"text":"Dunne, Paul","contributorId":86794,"corporation":false,"usgs":true,"family":"Dunne","given":"Paul","email":"","affiliations":[],"preferred":false,"id":189166,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23794,"text":"ofr94521 - 1995 - Water-use data by category, county, and water management district in Florida, 1950-90","interactions":[],"lastModifiedDate":"2012-02-02T00:08:16","indexId":"ofr94521","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":"94-521","title":"Water-use data by category, county, and water management district in Florida, 1950-90","docAbstract":"The population for Florida in 1990 was estimated at 12.94 million, an increase of nearly 10.17 million (370 percent) from the population of 2.77 million in 1950. Consequently, water use (fresh and saline) in Florida increased nearly 510 percent (15,175 million gallons per day) between 1950 and 1990. The resident population of the State is projected to surpass 20 million by the year 2020. Through the cooperation of the Florida Department of Environ- mental Protection and the U.S. Geologial Survey, water-use data for the period between 1950 and 1990 has been consolidated into one publication. This report aggregates and summarizes the quantities of water withdrawn annually for all water-use categories (public supply, self-supplied domestic, self-supplied commercial-industrial, agriculture, and thermoelectric power generation), by counties, and water management districts in Florida from 1950 through 1990. Total water withdrawn in Florida increased from 2,923 million gallons per day in 1950 to 17,898 million gallons per day in 1990. Surface- water withdrawals during 1950 totaled 2,333 million gallons per day but were not differentiated between fresh and saline, therefore, comparisons between fresh and saline water were made beginning with 1955 data. Freshwater withdrawals increased 245 percent between 1955 and 1990. Saline water withdrawals increased more than 1,500 percent between 1955 and 1990. In 1955, more than 47 percent of the fresh- water used was withdrawn from ground-water sources and 53 percent was withdrawn from surface-water sources. In 1990, nearly 62 percent of the fresh- water withdrawn was from ground-water sources, while 38 percent was withdrawn from surface-water sources. The steady increase in ground-water withdrawals since the 1950's primarily is a result of the ability to drill and pump water more economically from large, deep wells and the reliability of both the quality and quantity of water from these wells. Water withdrawn for public supply in Florida increased 1,030 percent between 1950 and 1990. The population served by public supply increased from 1.66 million in 1950 to 11.23 million in 1990, and the percentage of the population served by public supply increased from 60 percent in 1950 to nearly 88 percent in 1990. Freshwater withdrawn for self- supplied domestic use in Florida increased 1,010 percent, self-supplied commercial-industrial uses increased 170 percent, and agriculture increased 915 percent between 1950 and 1990. Freshwater with- drawals for thermoelectric power generation decreased 8 percent between 1955 and 1990, while saline water withdrawals increased nearly 1,540 percent between 1955 and 1990. Between 1965 and 1990, total freshwater withdrawals increased in 58 of the 67 counties in Florida. Fresh ground-water was withdrawn in all 67 counties in 1965 through 1990, and increased in 65 counties between 1965 and 1990. Fresh surface-water was withdrawn in 60 counties from 1965 to 1990, and increased in 42 counties between 1965 and 1990. The change in total freshwater withdrawals within the water management districts between 1975 and 1990 were as follows: Northwest Florida Water Management District increased 3 percent, St. Johns River Water Management District decreased 6 percent, South Florida Water Management District increased 37 percent, Southwest Florida Water Management District decreased 1 percent, and Suwannee River Water Management District increased 8 percent.(USGS)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94521","issn":"0094-9140","usgsCitation":"Marella, R., 1995, Water-use data by category, county, and water management district in Florida, 1950-90: U.S. Geological Survey Open-File Report 94-521, x, 114 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr94521.","productDescription":"x, 114 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":156862,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0521/report-thumb.jpg"},{"id":53016,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0521/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ad8e","contributors":{"authors":[{"text":"Marella, R. L.","contributorId":34164,"corporation":false,"usgs":true,"family":"Marella","given":"R. L.","affiliations":[],"preferred":false,"id":190737,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24242,"text":"ofr95817B - 1995 - Bibliography of well-log applications annual update, October 1, 1994 to September 30, 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:08:06","indexId":"ofr95817B","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":"95-817","chapter":"B","title":"Bibliography of well-log applications annual update, October 1, 1994 to September 30, 1995","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr95817B","issn":"0094-9140","usgsCitation":"Prensky, S.E., 1995, Bibliography of well-log applications annual update, October 1, 1994 to September 30, 1995: U.S. Geological Survey Open-File Report 95-817, 1 computer disk ;3 1/2 in., https://doi.org/10.3133/ofr95817B.","productDescription":"1 computer disk ;3 1/2 in.","costCenters":[],"links":[{"id":155494,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627d20","contributors":{"authors":[{"text":"Prensky, Stephen E.","contributorId":96703,"corporation":false,"usgs":true,"family":"Prensky","given":"Stephen","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":191551,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24240,"text":"ofr95817A - 1995 - Bibliography of well-log applications annual update, October 1, 1994 to September 30, 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:08:06","indexId":"ofr95817A","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":"95-817","chapter":"A","title":"Bibliography of well-log applications annual update, October 1, 1994 to September 30, 1995","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr95817A","issn":"0094-9140","usgsCitation":"Prensky, S.E., 1995, Bibliography of well-log applications annual update, October 1, 1994 to September 30, 1995: U.S. Geological Survey Open-File Report 95-817, ii, 136 leaves ;28 cm., https://doi.org/10.3133/ofr95817A.","productDescription":"ii, 136 leaves ;28 cm.","costCenters":[],"links":[{"id":155492,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0817a/report-thumb.jpg"},{"id":53372,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0817a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627d29","contributors":{"authors":[{"text":"Prensky, Stephen E.","contributorId":96703,"corporation":false,"usgs":true,"family":"Prensky","given":"Stephen","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":191549,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24426,"text":"ofr95445 - 1995 - Nitrate concentrations in ground water of the central Columbia Plateau","interactions":[],"lastModifiedDate":"2012-02-02T00:08:12","indexId":"ofr95445","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":"95-445","title":"Nitrate concentrations in ground water of the central Columbia Plateau","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr95445","issn":"0094-9140","usgsCitation":"Ryker, S.J., and Jones, J.L., 1995, Nitrate concentrations in ground water of the central Columbia Plateau: U.S. Geological Survey Open-File Report 95-445, [4] p. on 1 folded sheet : col. ill., col. maps ; 43 x 28 cm., folded to 22 x 28 cm., https://doi.org/10.3133/ofr95445.","productDescription":"[4] p. on 1 folded sheet : col. ill., col. maps ; 43 x 28 cm., folded to 22 x 28 cm.","costCenters":[],"links":[{"id":156262,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0445/report-thumb.jpg"},{"id":19504,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0445/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19505,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0445/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53505,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0445/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8b70","contributors":{"authors":[{"text":"Ryker, Sarah J. 0000-0002-1004-5611 sryker@usgs.gov","orcid":"https://orcid.org/0000-0002-1004-5611","contributorId":4100,"corporation":false,"usgs":true,"family":"Ryker","given":"Sarah","email":"sryker@usgs.gov","middleInitial":"J.","affiliations":[{"id":505,"text":"Office of the AD Climate and Land-Use Change","active":true,"usgs":true}],"preferred":true,"id":191900,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, Joseph L. jljones@usgs.gov","contributorId":3492,"corporation":false,"usgs":true,"family":"Jones","given":"Joseph","email":"jljones@usgs.gov","middleInitial":"L.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":191899,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25974,"text":"wri954157 - 1995 - Water quality of selected wetland streams in central and eastern Massachusetts, 1988-89","interactions":[],"lastModifiedDate":"2012-02-02T00:08:17","indexId":"wri954157","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":"95-4157","title":"Water quality of selected wetland streams in central and eastern Massachusetts, 1988-89","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri954157","usgsCitation":"Armstrong, D.S., and Lent, R.M., 1995, Water quality of selected wetland streams in central and eastern Massachusetts, 1988-89: U.S. Geological Survey Water-Resources Investigations Report 95-4157, iv, 43 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri954157.","productDescription":"iv, 43 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157377,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4157/report-thumb.jpg"},{"id":54729,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4157/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9999","contributors":{"authors":[{"text":"Armstrong, David S. 0000-0003-1695-1233 darmstro@usgs.gov","orcid":"https://orcid.org/0000-0003-1695-1233","contributorId":1390,"corporation":false,"usgs":true,"family":"Armstrong","given":"David","email":"darmstro@usgs.gov","middleInitial":"S.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":195569,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lent, Robert M. rmlent@usgs.gov","contributorId":284,"corporation":false,"usgs":true,"family":"Lent","given":"Robert","email":"rmlent@usgs.gov","middleInitial":"M.","affiliations":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"preferred":true,"id":195568,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}