{"pageNumber":"4024","pageRowStart":"100575","pageSize":"25","recordCount":184938,"records":[{"id":70180349,"text":"70180349 - 1994 - Reproduction and early life history of northern squawfish Ptychocheilus oregonensis in the Columbia River","interactions":[],"lastModifiedDate":"2017-01-27T13:29:51","indexId":"70180349","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Reproduction and early life history of northern squawfish Ptychocheilus oregonensis in the Columbia River","docAbstract":"<p>No abstract available</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"System-wide significance of predation on juvenile salmonids in Columbia and Snake River reservoirs and evaluation of predation control measures","language":"English","publisher":"National Biological Survey","usgsCitation":"Barfoot, C., Gadomski, D., Murphy, A., and Schultz, G., 1994, Reproduction and early life history of northern squawfish Ptychocheilus oregonensis in the Columbia River, 34 p. .","productDescription":"34 p. ","startPage":"7","endPage":"40","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":334197,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"588c6aaae4b08c8121c90994","contributors":{"authors":[{"text":"Barfoot, C.A.","contributorId":51490,"corporation":false,"usgs":true,"family":"Barfoot","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":661329,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gadomski, D.M.","contributorId":37101,"corporation":false,"usgs":true,"family":"Gadomski","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":661330,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Murphy, A.M.","contributorId":178853,"corporation":false,"usgs":false,"family":"Murphy","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":661331,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schultz, G.T.","contributorId":178808,"corporation":false,"usgs":false,"family":"Schultz","given":"G.T.","email":"","affiliations":[],"preferred":false,"id":661332,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":27670,"text":"wri944004 - 1994 - Effects of urban flood-detention reservoirs on peak discharges in Gwinnett County, Georgia","interactions":[],"lastModifiedDate":"2017-01-27T10:34:47","indexId":"wri944004","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-4004","title":"Effects of urban flood-detention reservoirs on peak discharges in Gwinnett County, Georgia","docAbstract":"The effects of flood-detention reservoirs on peak discharges along downstream reaches in six urban drainage basins in Gwinnett County, Georgia, were studied during 1986-93 using the U.S. Geological Survey's Distributed Routing Rainfall-Runoff Model (DR3M). Short-term rainfall-runoff data were collected at selected stations in six urban drainage basins in Gwinnett County. The basins range in size from 0.10 to 0.37 square miles and contain from 15- to 35- percent impervious areas. Each basin contains from two to six flood-detention reservoirs. The DR3M was calibrated using short-term rainfall-runoff data collected (1986-92) at each station. The model then was used to simulate long-term (1898-1980) peak discharges for these stations for conditions representing various amounts of detention ranging from the existing condition with all flood-detention reservoirs in place to the natural condition with no reservoirs. Flood-frequency relations were developed from the simulated annual peak discharges for each of these conditions by fitting the logarithms of the annual peak discharge data to a Pearson type III distribution curve. The effect of each flood-detention reservoir on peak discharges downstream was determined by comparison of peak discharges simulated with and without the flood-detention reservoirs. The cumulative effect of all flood-detention reservoirs in a basin on peak discharges downstream was determined by comparison of peak discharges for a flood with a given recurrence interval simulated with and without the reservoirs. Results of these comparisons indicate that removal of an individual flood-detention reservoir during simulations changes peak discharges from - 1 to 24 percent for the 2-year recurrence interval, from - 1 to 27 percent for the 10-year recurrence interval, and from -2 to 31 percent for the 100-year recurrence interval. The cumulative effect of removing all of the reservoirs from each of the six basins during simulation increases peak discharges from 1 to 38 percent for the 2-year recurrence interval, from 1 to 37 percent for the l O-year recurrence interval, and from 3 to 31 percent for the 100-year recurrence interval.  In this study of six basins, several factors influenced the effect of flood-detention reservoirs on peak discharges downstream. The contributing drainage area, the maximum storage capacity, the outflow-structure capacity, and the elevation-to-storage relation of the flood-detention reservoir affected peak discharges in several basins. The location in the drainage basin and number of flood-detention reservoirs affected peak discharges in some basins.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri944004","usgsCitation":"Hess, G.W., and Inman, E.J., 1994, Effects of urban flood-detention reservoirs on peak discharges in Gwinnett County, Georgia: U.S. Geological Survey Water-Resources Investigations Report 94-4004, v, 35 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944004.","productDescription":"v, 35 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":56521,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4004/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123838,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4004/report-thumb.jpg"}],"country":"United States","state":"Georgia","county":"Gwinnett 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W.","contributorId":43338,"corporation":false,"usgs":true,"family":"Hess","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":198508,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Inman, E. J.","contributorId":44193,"corporation":false,"usgs":true,"family":"Inman","given":"E.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":198509,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":63436,"text":"gq1728 - 1994 - Geologic map of the Gulkana A-1 quadrangle, south-central Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:10:45","indexId":"gq1728","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1728","title":"Geologic map of the Gulkana A-1 quadrangle, south-central Alaska","language":"ENGLISH","doi":"10.3133/gq1728","usgsCitation":"Richter, D.H., Duffield, W.A., Sawyer, D., Ratte, J., and Schmoll, H., 1994, Geologic map of the Gulkana A-1 quadrangle, south-central Alaska: U.S. Geological Survey Geologic Quadrangle 1728, 1 map :col. ;44 x 42 cm., on sheet 87 x 126 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq1728.","productDescription":"1 map :col. ;44 x 42 cm., on sheet 87 x 126 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":102777,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1227.htm","linkFileType":{"id":5,"text":"html"},"description":"1227"},{"id":249529,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1728/report.pdf","size":"72","linkFileType":{"id":1,"text":"pdf"}},{"id":253094,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1728/report-thumb.jpg"}],"scale":"63360","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -144.5,62 ], [ -144.5,62.25 ], [ -144,62.25 ], [ -144,62 ], [ -144.5,62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c677","contributors":{"authors":[{"text":"Richter, Donald H.","contributorId":61021,"corporation":false,"usgs":true,"family":"Richter","given":"Donald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":268844,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Duffield, W. A.","contributorId":71935,"corporation":false,"usgs":true,"family":"Duffield","given":"W.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":268846,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sawyer, D.A.","contributorId":107666,"corporation":false,"usgs":true,"family":"Sawyer","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":268847,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ratte, J.C.","contributorId":10416,"corporation":false,"usgs":true,"family":"Ratte","given":"J.C.","affiliations":[],"preferred":false,"id":268843,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schmoll, H. R.","contributorId":71543,"corporation":false,"usgs":true,"family":"Schmoll","given":"H. R.","affiliations":[],"preferred":false,"id":268845,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":27704,"text":"wri934172 - 1994 - Hydrogeology, herbicides and nutrients in ground water and springs, and relation of water quality to land use and agricultural practices near Carlisle, Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-27T11:15:43","indexId":"wri934172","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"93-4172","title":"Hydrogeology, herbicides and nutrients in ground water and springs, and relation of water quality to land use and agricultural practices near Carlisle, Pennsylvania","docAbstract":"Discharge and water-quality data collected in two adjacent karst-spring basins in Cumberland County, Pa., from May 1990 through April 1991 were used to (1) describe the hydrogeology of the area; (2) determine the concentrations of selected herbicides, herbicide-soil metabolites, and nutrients in water from wells and discharges from springs, (3) determine herbicide and nutrient discharges from springs; and (4) determine the relation of ground-water quality to land use and agricultural practices in the spring basins.  The study area is underlain by a regolith-mantled carbonate-rock aquifer system.  Agricultural land, forest, and residential land are the principal land uses.  Herbicides are applied primarily to cornfields. Cyanazine, atrazine, metolachlor, and alachlor account for about 90 percent of the documented herbicide use on cropland.  Daily mean discharge of Alexanders and Mount Rock Springs was 3.8 and 3.7 cubic feet per second, and total discharge was 1,390 and 1,370 cubic feet per second-days.  Increases in discharge were related to individual periods of precipitation, but maximum flow rates lagged precipitation periods by 2 to 5 days.  The recharge area to each spring is estimated to be 2.8 square miles.  Atrazine was the only herbicide in common use that was detected in discharges from springs.  Atrazine and the atrazine soil-metabolite deethylatrazine (DEA) were detected in spring discharges for the duration of the study.  Changes in atrazine and DEA concentrations in the discharges from springs were minimal, and no flush of herbicides from the springs followed application.  Temporal variation in constituent discharges was related mostly to changes in spring flow; the largest daily constituent discharges coincided with periods of increased spring flow during the winter and early spring.  Atrazine and DEA discharged from Alexanders Spring and Mount Rock Spring were about 0.5 and 0.6 percent of the estimated annual atrazine use on row crops in their respective recharge areas.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri934172","usgsCitation":"Hippe, D., Witt, E., and Giovannitti, R., 1994, Hydrogeology, herbicides and nutrients in ground water and springs, and relation of water quality to land use and agricultural practices near Carlisle, Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 93-4172, vi, 66 p. :ill, maps ;28 cm., https://doi.org/10.3133/wri934172.","productDescription":"vi, 66 p. :ill, maps ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":56551,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4172/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123591,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4172/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db61486f","contributors":{"authors":[{"text":"Hippe, D. J.","contributorId":83951,"corporation":false,"usgs":true,"family":"Hippe","given":"D. J.","affiliations":[],"preferred":false,"id":198564,"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":198565,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Giovannitti, R.M.","contributorId":7728,"corporation":false,"usgs":true,"family":"Giovannitti","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":198563,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70187219,"text":"70187219 - 1994 - Giant Hawaiian landslides","interactions":[],"lastModifiedDate":"2019-06-05T10:35:21","indexId":"70187219","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Giant Hawaiian landslides","docAbstract":"<p><span>Sixty-eight landslides more than 20 km long are present along a 2200 km segment of the Hawaiian Ridge from near Midway to Hawaii. Some of the landslides exceed 200 km in length and 5000 km3 in volume, ranking them among the largest on Earth. Most of these giant landslides were discovered during a mapping program of the U.S. Hawaiian Exclusive Economic zone from 1986 to 1991 utilizing the GLORIA side-looking sonar mapping system. Two general types of landslides are present: slumps and debris avalanches. Many intermediate forms occur and some debris avalanches form from oversteepened slumps. The slumps are deeply rooted in the volcanoes and may extend back to volcanic rift zones and down to the base of the volcanic pile at about 10 km depth. Debris avalanches are thinner, longer, and move on lower gradients than slumps. Their rapid movement is indicated by the fact that some have moved uphill for tens of kilometers, and are believed to have produced major tsunamis. The debris avalanches left large amphitheaters at their heads and produce broad hummocky distals lobes at their toes. Commonly, major canyons have incised the amphitheaters. Giant landslides have recently been discovered on many other marine volcanoes where they also can be related to volcanic structure and eruptive activity.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Annual Review of Earth and Planetary Sciences","language":"English","doi":"10.1146/annurev.ea.22.050194.001003","usgsCitation":"Moore, J., Normark, W.R., and Holcomb, R.T., 1994, Giant Hawaiian landslides, chap. <i>of</i> Annual Review of Earth and Planetary Sciences, p. 119-144, https://doi.org/10.1146/annurev.ea.22.050194.001003.","productDescription":"26 p.","startPage":"119","endPage":"144","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":340482,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5901b1c2e4b0c2e071a99bcc","contributors":{"authors":[{"text":"Moore, J.G.","contributorId":67496,"corporation":false,"usgs":true,"family":"Moore","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":693070,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Normark, W. R.","contributorId":87137,"corporation":false,"usgs":true,"family":"Normark","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":693071,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Holcomb, R. T.","contributorId":99146,"corporation":false,"usgs":true,"family":"Holcomb","given":"R.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":693072,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3799,"text":"cir1107 - 1994 - Abstracts of the eighth international conference on Geochronology, cosmochronology, and isotope geology","interactions":[],"lastModifiedDate":"2019-06-05T13:29:29","indexId":"cir1107","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1107","title":"Abstracts of the eighth international conference on Geochronology, cosmochronology, and isotope geology","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/cir1107","usgsCitation":"Lanphere, M.A., Dalrymple, G.B., and Turrin, B., 1994, Abstracts of the eighth international conference on Geochronology, cosmochronology, and isotope geology: U.S. Geological Survey Circular 1107, vi, 384 p. , https://doi.org/10.3133/cir1107.","productDescription":"vi, 384 p. ","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":30869,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1994/1107/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123206,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1994/1107/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e5dc","contributors":{"authors":[{"text":"Lanphere, Marvin A. alder@usgs.gov","contributorId":2696,"corporation":false,"usgs":true,"family":"Lanphere","given":"Marvin","email":"alder@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":147620,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dalrymple, G. Brent","contributorId":54564,"corporation":false,"usgs":true,"family":"Dalrymple","given":"G.","email":"","middleInitial":"Brent","affiliations":[],"preferred":false,"id":147621,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Turrin, Brent D.","contributorId":89867,"corporation":false,"usgs":true,"family":"Turrin","given":"Brent D.","affiliations":[],"preferred":false,"id":147622,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27651,"text":"wri924038 - 1994 - Local point sources that affect ground-water quality in the East Meadow area, Long Island, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:08:37","indexId":"wri924038","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"92-4038","title":"Local point sources that affect ground-water quality in the East Meadow area, Long Island, New York","docAbstract":"The extent and chemical characteristics of ground water affected by three local point sources--a stormwater basin, uncovered road-salt-storage piles, and an abandoned sewage-treatment plant--were delineated during a 3-year study of the chemical characteristics and migration of a body of reclaimed wastewater that was applied to the watertable aquifer during recharge experiments from October 1982 through January 1984 in East Meadow. The timing, magnitude, and chemical quality of recharge from these point sources is highly variable, and all sources have the potential to skew determinations of the quality of ambient ground-water and of the reclaimed-wastewater plume if they are not taken into account.  Ground water affected by recharge from the stormwater basin is characterized by low concentrations of nitrate + nitrite (less than 5 mg/L [milligrams per liter] as N) and sulfate (less than 40 mg/L) and is almost entirely within the upper glacial aquifer. The plume derived from road-salt piles is narrow, has high concentrations of chloride (greater than 50 mg/L) and sodium (greater than 75 mg/L), and also is limited to the upper glacial aquifer. The sodium, in high concentrations, could react with aquifer material and exchange for sorbed cations such as calcium, potassium, and magnesium. Water affected by secondary-treated sewage from the abandoned treatment plant extends 152 feet below land surface into the upper part of the Magothy aquifer and longitudinally beyond the southern edge of the study area, 7,750 feet south of the recharge site. Ground water affected by secondary-treated sewage within the study area typically contains elevated concentrations of reactive chemical constituents, such as potassium and ammonium, and low concentrations of dissolved oxygen. Conservative or minimally reactive constituents such as chloride and sodium have been transported out of the study area in the upper glacial aquifer and the intermediate (transitional) zone but remain in the less permeable upper part of the Magothy aquifer.  Identification of the three point sources and delineation of their areas of influence improved definition of ambient ground-water quality and delineation of the reclaimed-wastewater plume.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri924038","usgsCitation":"Heisig, P.M., 1994, Local point sources that affect ground-water quality in the East Meadow area, Long Island, New York: U.S. Geological Survey Water-Resources Investigations Report 92-4038, v, 28 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri924038.","productDescription":"v, 28 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123930,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4038/report-thumb.jpg"},{"id":56508,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4038/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a68e4b07f02db63b219","contributors":{"authors":[{"text":"Heisig, Paul M.","contributorId":95912,"corporation":false,"usgs":true,"family":"Heisig","given":"Paul","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":198472,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70180348,"text":"70180348 - 1994 - Application of DNA technology to the detection and identification of two rhabdoviruses of Pacific salmon","interactions":[],"lastModifiedDate":"2017-06-10T11:37:21","indexId":"70180348","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"title":"Application of DNA technology to the detection and identification of two rhabdoviruses of Pacific salmon","docAbstract":"<p>No abstract available&nbsp;</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Application of DNA technology to the management of Pacific Salmon","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"National Oceanic and Atmospheric Adminstration","usgsCitation":"Arakawa, C., Batts, W., Deering, R., and Winton, J., 1994, Application of DNA technology to the detection and identification of two rhabdoviruses of Pacific salmon, 5 p. .","productDescription":"5 p. ","startPage":"113","endPage":"117","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":334196,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"588c6aaae4b08c8121c90996","contributors":{"editors":[{"text":"Park, L.K.","contributorId":25739,"corporation":false,"usgs":true,"family":"Park","given":"L.K.","email":"","affiliations":[],"preferred":false,"id":661326,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Moran, P.","contributorId":34746,"corporation":false,"usgs":true,"family":"Moran","given":"P.","email":"","affiliations":[],"preferred":false,"id":661327,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Waples, R.S.","contributorId":178852,"corporation":false,"usgs":false,"family":"Waples","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":661328,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Arakawa, C.K.","contributorId":152140,"corporation":false,"usgs":false,"family":"Arakawa","given":"C.K.","email":"","affiliations":[],"preferred":false,"id":661322,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Batts, W.N. 0000-0002-6469-9004","orcid":"https://orcid.org/0000-0002-6469-9004","contributorId":51043,"corporation":false,"usgs":true,"family":"Batts","given":"W.N.","affiliations":[],"preferred":false,"id":661323,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Deering, R.E.","contributorId":178851,"corporation":false,"usgs":false,"family":"Deering","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":661324,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Winton, J. R. 0000-0002-3505-5509","orcid":"https://orcid.org/0000-0002-3505-5509","contributorId":82441,"corporation":false,"usgs":true,"family":"Winton","given":"J. R.","affiliations":[],"preferred":false,"id":661325,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":27519,"text":"wri934115 - 1994 - Yields of bedrock wells in Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:08:39","indexId":"wri934115","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"93-4115","title":"Yields of bedrock wells in Massachusetts","docAbstract":"Six to seven percent of the population of Massachusetts obtains its water from domestic bedrock wells. Additional public, commercial, industrial, and domestic supplies from bedrock will be needed in the future. Information about the factors that are related to large well yields is needed. The factors associated with well yields were identified by use of statistical analysis of reported data from 4,218 bedrock wells.  The median reported yield of all bedrock wells was 7 gallons per minute, and the median depth was 170 feet. Wells in valleys and lowlands had the largest median yield--I0 gallons per minute. The median well yield on hilltops and slopes was 6 gallons per minute. In valleys and lowlands, significant increases in well yields corresponded to increasing thickness of overburden. On hilltops and slopes, only small increases in well yield corresponded to increases in overburden thickness. Increases in well diameter corresponded to significant increases in well yields for all well locations, depths, and use categories.  The common assumptions that fractured crystalline rocks generally yield only small quantities of water to wells and that the fractures that yield water to wells pinch out or are closed because of lithostatic pressure at depths greater than 300 to 400 feet may be in error. Analysis of well data indicates that the median yield of all bedrock wells decreased as well depth increased to 400 feet and increased slightly with well depths greater than 600 feet. The median yield of bedrock wells located in valleys and lowlands reached 50 gallons per minute at depths of 600 to 700 feet. The median yield of wells located on hilltops and slopes reached 15 gallons per minute at depths of 600 to 700 feet.  Carbonate bedrock, with a median well yield of 25 gallons per minute, seemed to be the most productive bedrock type. A reported yield of 1,700 gallons per minute from an industrial well completed in carbonate bedrock is the largest reported yield from a bedrock well in Massachusetts. Yield of wells in sedimentary rocks of the Connecticut Valley increased significantly at depths greater than 400 feet, indicating that this bedrock type may have some primary permeability. Commercial or industrial wells had a median yield of 30 gallons per minute. These wells appear to be preferentially sited, large in diameter, and deeper than average to maximize potential well yields.  The median reported bedrock well yield and depth have changed over time. The median yield of about 20 gallons per minute for 1920-40 decreased to 6 gallons per minute for 1970-80. Well depth increased from 128 feet for 1950- 60 to 250 feet for 1980-90. The period during which well depths began to increase coincides with a change in bedrock-well drilling methods from cable tool to air rotary with percussion.  Four methods of testing the yield of domestic bedrock wells were evaluated: air injection, evacuation and recovery, constant-discharge, and instantaneous discharge or recharge. A constant-discharge test best satisfied the criteria established to evaluate the testing methods.  Further data collection and evaluation are needed for the systematic characterization and appraisal of the bedrock aquifers of Massachusetts. Specific elements include (1) improved and expanded collection and storage of well data, (2) detailed hydrogeologic evaluations of apparent high yield bedrock areas, (3) an evaluation of the relation between the vertical distribution of hydraulic properties measured during well drilling to actual hydraulic properties, (4) an evaluation of the effect of well diameter on well yield, and (5) areal evaluations to characterize the quality of water in bedrock.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri934115","usgsCitation":"Hansen, B.P., and Simcox, A., 1994, Yields of bedrock wells in Massachusetts: U.S. Geological Survey Water-Resources Investigations Report 93-4115, v, 43 p. :ill., map ;28 cm., https://doi.org/10.3133/wri934115.","productDescription":"v, 43 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":123859,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4115/report-thumb.jpg"},{"id":56378,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4115/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4783e4b07f02db483604","contributors":{"authors":[{"text":"Hansen, B. P.","contributorId":45332,"corporation":false,"usgs":true,"family":"Hansen","given":"B.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":198252,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simcox, A.C.","contributorId":46134,"corporation":false,"usgs":true,"family":"Simcox","given":"A.C.","affiliations":[],"preferred":false,"id":198253,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26525,"text":"wri934182 - 1994 - Development and documentation of spatial data bases for the Lake Tahoe Basin, California and Nevada","interactions":[],"lastModifiedDate":"2018-01-12T12:17:59","indexId":"wri934182","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"93-4182","title":"Development and documentation of spatial data bases for the Lake Tahoe Basin, California and Nevada","docAbstract":"A set of spatial data bases consisting of natural- resources and planimetric-base layers has been developed and documented for the Lake Tahoe Basin, California and Nevada. The data bases, in the form of geographic information system coverages, include surface geology, soils, timber type, riparian vegetation, land capability, stream channels, water bodies, roads, political boundaries, the Lake Tahoe Basin boundary, slope, aspect, drainage-basin boundaries, and hydrologic-monitoring sites. The data bases were developed from existing thematic maps, digital data, and hydrographic records. Data were compiled from maps and records of Federal, State, and local agencies. The scale of source materials ranged from 1:24,000 to 1:125,000 and their release dates. from 1964 to 1989. Documen- tation and summary information are included for each spatial data base.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri934182","collaboration":"Planning in cooperation with the Tahoe Regional Planning Agency","usgsCitation":"Cartier, K.D., Peltz, L.A., and Smith, J.L., 1994, Development and documentation of spatial data bases for the Lake Tahoe Basin, California and Nevada: U.S. Geological Survey Water-Resources Investigations Report 93-4182, v, 65 p., https://doi.org/10.3133/wri934182.","productDescription":"v, 65 p.","costCenters":[],"links":[{"id":55388,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4182/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119116,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4182/report-thumb.jpg"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Lake Tahoe Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.3,\n              38.7\n            ],\n            [\n              -119.25,\n              38.7\n            ],\n            [\n              -119.25,\n              39.9\n            ],\n            [\n              -120.3,\n              39.9\n            ],\n            [\n              -120.3,\n              38.7\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d530","contributors":{"authors":[{"text":"Cartier, Kenn D.","contributorId":39766,"corporation":false,"usgs":true,"family":"Cartier","given":"Kenn","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":196551,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peltz, Lorri A.","contributorId":29401,"corporation":false,"usgs":true,"family":"Peltz","given":"Lorri","email":"","middleInitial":"A.","affiliations":[{"id":12701,"text":"US Geological Survey","active":true,"usgs":false}],"preferred":false,"id":196552,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, J. LaRue jlsmith@usgs.gov","contributorId":1863,"corporation":false,"usgs":true,"family":"Smith","given":"J.","email":"jlsmith@usgs.gov","middleInitial":"LaRue","affiliations":[],"preferred":true,"id":196553,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":44336,"text":"ofr94164 - 1994 - Aeromagnetic map of parts of the Denver, Greeley, and Pueblo 1 x 2 degree quadrangles, Colorado","interactions":[],"lastModifiedDate":"2022-09-14T21:55:50.749193","indexId":"ofr94164","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-164","title":"Aeromagnetic map of parts of the Denver, Greeley, and Pueblo 1 x 2 degree quadrangles, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94164","usgsCitation":"Riggle, F.E., and Zietz, I., 1994, Aeromagnetic map of parts of the Denver, Greeley, and Pueblo 1 x 2 degree quadrangles, Colorado: U.S. Geological Survey Open-File Report 94-164, 1 Plate: 35.00 × 57.00 inches, https://doi.org/10.3133/ofr94164.","productDescription":"1 Plate: 35.00 × 57.00 inches","costCenters":[],"links":[{"id":168348,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":406740,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12468.htm","linkFileType":{"id":5,"text":"html"}},{"id":21544,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0164/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","projection":"universal transverse Mercator","country":"United States","state":"Colorado","otherGeospatial":"Denver, Greeley, and Pueblo 1 x 2 degrees quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106,\n              38\n            ],\n            [\n              -105,\n              38\n            ],\n            [\n              -105,\n              41\n            ],\n            [\n              -106,\n              41\n            ],\n            [\n              -106,\n              38\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6975b3","contributors":{"authors":[{"text":"Riggle, F. E.","contributorId":93874,"corporation":false,"usgs":true,"family":"Riggle","given":"F.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":229588,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zietz, Isidore","contributorId":76708,"corporation":false,"usgs":true,"family":"Zietz","given":"Isidore","affiliations":[],"preferred":false,"id":229587,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":19873,"text":"ofr9442 - 1994 - Report on the U.S. Geological Survey's evaluation program for standard reference samples distributed in October 1993 : T-127 (trace constituents), M-128 (major constituents), N-40 (nutrients), N-41 (nutrients), P-21 (low ionic strength), Hg-17 (mercury), AMW-3 (acid mine water), and WW-1 (whole water)","interactions":[],"lastModifiedDate":"2012-02-02T00:07:42","indexId":"ofr9442","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-42","title":"Report on the U.S. Geological Survey's evaluation program for standard reference samples distributed in October 1993 : T-127 (trace constituents), M-128 (major constituents), N-40 (nutrients), N-41 (nutrients), P-21 (low ionic strength), Hg-17 (mercury), AMW-3 (acid mine water), and WW-1 (whole water)","docAbstract":"This report presents the results of the U.S. Geological Survey's analytical evaluation program for eight standard reference samples--T-127 (trace constituents), M-128 (major constituents), N-40 (nutrients), N-41 (nutrients), P-21 (low ionic strength), Hg-17 (mercury), AMW-3 (acid mine water), and WW-1 (whole water)--that were distributed in October 1993 to 158 laboratories registered in the U.S. Geological Survey sponsored interlaboratory testing program. Analytical data that were received from 145 of the laboratories were evaluated with respect to: overall laboratory performance and relative laboratory performance for each analyte in the eight reference samples. Results of these evaluations are presented in tabular form. Also presented are tables and graphs summarizing the analytical data provided by each laboratory for each analyte in the eight standard reference samples. The most probable value for each analyte was determined using nonparametric statistics.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr9442","usgsCitation":"Long, H., and Farrar, J., 1994, Report on the U.S. Geological Survey's evaluation program for standard reference samples distributed in October 1993 : T-127 (trace constituents), M-128 (major constituents), N-40 (nutrients), N-41 (nutrients), P-21 (low ionic strength), Hg-17 (mercury), AMW-3 (acid mine water), and WW-1 (whole water): U.S. Geological Survey Open-File Report 94-42, iii, 177 p. :ill. ;28 cm., https://doi.org/10.3133/ofr9442.","productDescription":"iii, 177 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":153414,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0042/report-thumb.jpg"},{"id":49383,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0042/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db610ef6","contributors":{"authors":[{"text":"Long, H.K.","contributorId":50547,"corporation":false,"usgs":true,"family":"Long","given":"H.K.","email":"","affiliations":[],"preferred":false,"id":181671,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Farrar, J.W.","contributorId":26715,"corporation":false,"usgs":true,"family":"Farrar","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":181670,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70730,"text":"fs06694 - 1994 - Technology transfer opportunities : partnerships : controlled-release fertilizers using zeolites","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"fs06694","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"066-94","title":"Technology transfer opportunities : partnerships : controlled-release fertilizers using zeolites","language":"ENGLISH","doi":"10.3133/fs06694","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1994, Technology transfer opportunities : partnerships : controlled-release fertilizers using zeolites: U.S. Geological Survey Fact Sheet 066-94, NA, https://doi.org/10.3133/fs06694.","productDescription":"NA","costCenters":[],"links":[{"id":126298,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_066_94.jpg"},{"id":6625,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.usgs.gov/tech-transfer/factsheets/94-066b.html","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db6859b4","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":534705,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70162680,"text":"70162680 - 1994 - Landslides triggered by the Northridge earthquake","interactions":[],"lastModifiedDate":"2016-02-04T15:38:20","indexId":"70162680","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1437,"text":"Earthquakes & Volcanoes (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Landslides triggered by the Northridge earthquake","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Jibson, R., Harp, E.L., Keefer, D.K., and Wilson, R.C., 1994, Landslides triggered by the Northridge earthquake: Earthquakes & Volcanoes (USGS), v. 25, no. 1, p. 31-41.","productDescription":"11 p.","startPage":"31","endPage":"41","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":315006,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56ab49cbe4b07ca61bfea585","contributors":{"authors":[{"text":"Jibson, R.W.","contributorId":8467,"corporation":false,"usgs":true,"family":"Jibson","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":590121,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harp, E. L.","contributorId":59026,"corporation":false,"usgs":true,"family":"Harp","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":590122,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Keefer, D. K.","contributorId":21176,"corporation":false,"usgs":true,"family":"Keefer","given":"D.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":590123,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wilson, R. C.","contributorId":50889,"corporation":false,"usgs":true,"family":"Wilson","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":590124,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70195437,"text":"70195437 - 1994 - Secondary minerals and acid mine-water chemistry","interactions":[],"lastModifiedDate":"2018-09-12T08:18:26","indexId":"70195437","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesTitle":{"id":5629,"text":"Mineralogical Association of Canada Short Course Volumes","active":true,"publicationSubtype":{"id":24}},"seriesNumber":"22","title":"Secondary minerals and acid mine-water chemistry","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Environmental geochemistry of sulfide mine-wastes (Short course handbook, vol. 22)","largerWorkSubtype":{"id":13,"text":"Handbook"},"language":"English","publisher":"Mineral Association of Canada","usgsCitation":"Alpers, C.N., Blowes, D., Nordstrom, D.K., and Jambor, J., 1994, Secondary minerals and acid mine-water chemistry, chap. <i>of</i> Environmental geochemistry of sulfide mine-wastes (Short course handbook, vol. 22): Mineralogical Association of Canada Short Course Volumes, p. 247-270.","productDescription":"24 p.","startPage":"247","endPage":"270","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":351624,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":351660,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.mineralogicalassociation.ca/index.php?p=25#SC22-E"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff2321e4b0da30c1bfd64a","contributors":{"editors":[{"text":"Blowes, D.W","contributorId":195353,"corporation":false,"usgs":false,"family":"Blowes","given":"D.W","affiliations":[],"preferred":false,"id":728606,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Jambor, J.L.","contributorId":107460,"corporation":false,"usgs":true,"family":"Jambor","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":728607,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Alpers, Charles N. 0000-0001-6945-7365 cnalpers@usgs.gov","orcid":"https://orcid.org/0000-0001-6945-7365","contributorId":411,"corporation":false,"usgs":true,"family":"Alpers","given":"Charles","email":"cnalpers@usgs.gov","middleInitial":"N.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":728602,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blowes, D.W","contributorId":195353,"corporation":false,"usgs":false,"family":"Blowes","given":"D.W","affiliations":[],"preferred":false,"id":728603,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nordstrom, D. Kirk 0000-0003-3283-5136 dkn@usgs.gov","orcid":"https://orcid.org/0000-0003-3283-5136","contributorId":749,"corporation":false,"usgs":true,"family":"Nordstrom","given":"D.","email":"dkn@usgs.gov","middleInitial":"Kirk","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":false,"id":728604,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jambor, J.L.","contributorId":107460,"corporation":false,"usgs":true,"family":"Jambor","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":728605,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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,{"id":19923,"text":"ofr93497 - 1994 - Physical, chemical, and biological data for detailed study of irrigation drainage in the Klamath Basin, California and Oregon, 1990-92","interactions":[],"lastModifiedDate":"2012-02-02T00:07:42","indexId":"ofr93497","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"93-497","title":"Physical, chemical, and biological data for detailed study of irrigation drainage in the Klamath Basin, California and Oregon, 1990-92","docAbstract":"Physical, chemical, and biological data were collected between 1990 and 1992 as part of a detailed study by the U.S. Department of Interior of the effects of irrigation drainage on aquatic resources in the Klamath Basin of California and Oregon. Most of the sites for data collection were in and around the upper and lower sump of Tule Lake, in the Tule Lake National Wildlife Refuge, and along major drains in Lower Klamath National Wildlife Refuge. The physical and chemical data consist of particle-size determinations and concentrations of carbon, mercury, arsenic, chlorophenoxy acid, and organochlorine, organophosphate, and carbamate pesticides in bottom sediment; and concentrations of organophosphate, carbamate, and pyrethroid pesticides, major and trace inorganic constituents, nitrogen, phosphorus, and organic carbon in water. Continuous dissolved oxygen, pH, specific conduc- tance, and temperature data from selected sites in 1991 and 1992 are presented in graphical form to summarize the diel water-quality conditions. The biological data consists of concentrations of inorganic constituents and organochlorine pesticides in tissue, invertebrate and fish population surveys, fish health surveys, frog call surveys, egg shell thickness of avian eggs, and in situ and static toxicity bioassay data collected in 1991 and 1992 using aquatic bacteria, plants, invertebrates, fish, and bird species as test organisms.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr93497","usgsCitation":"MacCoy, D., 1994, Physical, chemical, and biological data for detailed study of irrigation drainage in the Klamath Basin, California and Oregon, 1990-92: U.S. Geological Survey Open-File Report 93-497, iv, 168 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr93497.","productDescription":"iv, 168 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":153271,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0497/report-thumb.jpg"},{"id":49433,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0497/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685a91","contributors":{"authors":[{"text":"MacCoy, D.E.","contributorId":47814,"corporation":false,"usgs":true,"family":"MacCoy","given":"D.E.","affiliations":[],"preferred":false,"id":181744,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19936,"text":"ofr94321 - 1994 - Water-resources investigations in Wisconsin","interactions":[],"lastModifiedDate":"2022-08-16T20:22:03.911815","indexId":"ofr94321","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-321","title":"Water-resources investigations in Wisconsin","docAbstract":"<p>The statewide average precipitation of 38.79 inches for the 1993 water year was 122 percent of the normal annual precipitation of 31.77 inches for water years 1961-90. Average precipitation values ranged from 103 percent of normal in northwestern Wisconsin to 150 percent of normal in southwestern Wisconsin (Pamela Naber Knox, UW-Extension, Geological and Natural History Survey, written commun., 1993).</p>\n<p>Runoff was variable for rivers throughout the State ranging from 99 percent in northcentral Wisconsin to 278 percent in southwestern Wisconsin. Departure of runoff in the 1993 water year from long-term average runoff is shown in figure 4, along with long-term average runoff for the period 1951-80. Runoff was lowest (99 percent of the average annual runoff from 1936-93) for the Wisconsin River at Rainbow Lake near Lake Tomahawk. Runoff was highest (278 percent of the average annual runoff from 1939-93) for the Pecatonica River at Darlington. The average annual runoff for the 1993 water year was the maximum for the period of record at 33 long-term stations (more than 10 years of record) in the southern half of Wisconsin.</p>\n<p>A comparison of the annual discharge for the individual water years (1916-93) at the Oconto River near Gillett, Jump River at Sheldon, and Sugar River near Brodhead is shown figure 5, The comparisons of monthly and annual discharges for the 1993 water year to discharge for a 78-year base period at the same three gaging stations are shown in figure 6.</p>\n<p>Spring runoff from snowmelt and major storms, in the period March through September 1993, caused floods with discharges that equalled or exceeded those with a recurrence interval of 10 years (Krug and others, 1991) at a number of crest-stage gage and gaging stations.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94321","usgsCitation":"Maertz, D., 1994, Water-resources investigations in Wisconsin: U.S. 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,{"id":39624,"text":"pp1538D - 1994 - Analysis of the origin of landslides in the New Madrid seismic zone","interactions":[],"lastModifiedDate":"2012-02-02T00:09:55","indexId":"pp1538D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1538","chapter":"D","title":"Analysis of the origin of landslides in the New Madrid seismic zone","language":"ENGLISH","doi":"10.3133/pp1538D","usgsCitation":"Jibson, R., and Keefer, D.K., 1994, Analysis of the origin of landslides in the New Madrid seismic zone: U.S. Geological Survey Professional Paper 1538, p. D1-D23, https://doi.org/10.3133/pp1538D.","productDescription":"p. D1-D23","costCenters":[],"links":[{"id":119378,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1538d/report-thumb.jpg"},{"id":67259,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1538d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db680143","contributors":{"authors":[{"text":"Jibson, R.W.","contributorId":8467,"corporation":false,"usgs":true,"family":"Jibson","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":221828,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keefer, D. K.","contributorId":21176,"corporation":false,"usgs":true,"family":"Keefer","given":"D.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":221829,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":67380,"text":"i2409 - 1994 - Geologic map of the Dun Glen Quadrangle, Pershing County, Nevada","interactions":[],"lastModifiedDate":"2012-02-10T00:11:15","indexId":"i2409","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2409","subseriesTitle":"NONE","title":"Geologic map of the Dun Glen Quadrangle, Pershing County, Nevada","language":"ENGLISH","doi":"10.3133/i2409","usgsCitation":"Whitebread, D., 1994, Geologic map of the Dun Glen Quadrangle, Pershing County, Nevada: U.S. Geological Survey IMAP 2409, 1 map :col. ;58 x 44 cm., on sheet 74 x 74 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2409.","productDescription":"1 map :col. ;58 x 44 cm., on sheet 74 x 74 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107416,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10272.htm","linkFileType":{"id":5,"text":"html"},"description":"10272"},{"id":188111,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"48000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118,40.5 ], [ -118,40.75 ], [ -117.75,40.75 ], [ -117.75,40.5 ], [ -118,40.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b07e4b07f02db69b2b1","contributors":{"authors":[{"text":"Whitebread, D. H.","contributorId":96251,"corporation":false,"usgs":true,"family":"Whitebread","given":"D. H.","affiliations":[],"preferred":false,"id":276094,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":64262,"text":"gp1009 - 1994 - Complete Bouguer gravity anomaly, isostatic-residual gravity, horizontal gradient, and terrain maps of Colorado","interactions":[],"lastModifiedDate":"2023-03-20T21:01:41.21553","indexId":"gp1009","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1009","title":"Complete Bouguer gravity anomaly, isostatic-residual gravity, horizontal gradient, and terrain maps of Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp1009","usgsCitation":"Abrams, G.A., and Knepper, D.H., 1994, Complete Bouguer gravity anomaly, isostatic-residual gravity, horizontal gradient, and terrain maps of Colorado: U.S. Geological Survey Geophysical Investigations Map 1009, Report: 1 p.; 2 Plates: 36.24 x 45.13 inches and 31.18 x 43.91 inches, https://doi.org/10.3133/gp1009.","productDescription":"Report: 1 p.; 2 Plates: 36.24 x 45.13 inches and 31.18 x 43.91 inches","costCenters":[],"links":[{"id":414386,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5957.htm","linkFileType":{"id":5,"text":"html"}},{"id":254299,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/1009/report-thumb.jpg"},{"id":250848,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/1009/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250846,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/1009/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250847,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/1009/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","country":"United States","state":"Colorado","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -109.055,\n              41\n            ],\n            [\n              -109.055,\n              37\n            ],\n            [\n              -102,\n              37\n            ],\n            [\n              -102,\n              41\n            ],\n            [\n              -109.055,\n              41\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8362","contributors":{"authors":[{"text":"Abrams, G. A.","contributorId":27047,"corporation":false,"usgs":true,"family":"Abrams","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":270343,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knepper, D. H. Jr.","contributorId":106129,"corporation":false,"usgs":true,"family":"Knepper","given":"D.","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":270344,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":62527,"text":"gq1723 - 1994 - Geologic map of the Lopez Mountain quadrangle, San Luis Obispo County, California","interactions":[{"subject":{"id":46921,"text":"ofr90650 - 1990 - Geologic map of the Lopez Mountain quadrangle, San Luis Obispo County, California","indexId":"ofr90650","publicationYear":"1990","noYear":false,"title":"Geologic map of the Lopez Mountain quadrangle, San Luis Obispo County, California"},"predicate":"SUPERSEDED_BY","object":{"id":62527,"text":"gq1723 - 1994 - Geologic map of the Lopez Mountain quadrangle, San Luis Obispo County, California","indexId":"gq1723","publicationYear":"1994","noYear":false,"title":"Geologic map of the Lopez Mountain quadrangle, San Luis Obispo County, California"},"id":1}],"lastModifiedDate":"2012-02-10T00:10:44","indexId":"gq1723","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1723","title":"Geologic map of the Lopez Mountain quadrangle, San Luis Obispo County, California","language":"ENGLISH","doi":"10.3133/gq1723","usgsCitation":"McLean, H., 1994, Geologic map of the Lopez Mountain quadrangle, San Luis Obispo County, California: U.S. Geological Survey Geologic Quadrangle 1723, 1 map :col. ;58 x 48 cm., on sheet 84 x 102 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq1723.","productDescription":"1 map :col. ;58 x 48 cm., on sheet 84 x 102 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":102011,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_389.htm","linkFileType":{"id":5,"text":"html"},"description":"389"},{"id":248690,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1723/report.pdf","size":"70","linkFileType":{"id":1,"text":"pdf"}},{"id":253917,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1723/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.61749999999999,35.25 ], [ -120.61749999999999,35.3675 ], [ -120.5,35.3675 ], [ -120.5,35.25 ], [ -120.61749999999999,35.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696dcf","contributors":{"authors":[{"text":"McLean, Hugh","contributorId":73977,"corporation":false,"usgs":true,"family":"McLean","given":"Hugh","affiliations":[],"preferred":false,"id":267500,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25691,"text":"wri934194 - 1994 - Organic compounds downstream from a treated-wastewater discharge near Dallas, Texas, March 1987","interactions":[],"lastModifiedDate":"2021-05-27T15:43:34.728934","indexId":"wri934194","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"93-4194","title":"Organic compounds downstream from a treated-wastewater discharge near Dallas, Texas, March 1987","docAbstract":"<p>Water and streambed-sediment samples were collected on March 9 and 10,1987 from one site upstream and three sites downstream of the discharge from a municipal wastewater-treatment plant on Rowlett Creek near Dallas, Texas. To extract and separate organic compounds, purgeand-trap, closed-loop stripping, and pH-adjusted solvent extraction methods were used for water samples; and a Soxhlet-solvent extraction method was used for streambed sediment. These methods were combined with gas chromatography/mass spectrometry to identify organic compounds in Rowlett Creek. Results from this study confirm the persistence of many organic compounds in water as far as 13.5 kilometers downstream of the wastewater discharge. These include: (1) the volatile organic compounds chloroform, 1,2-dichlorobenzene, 1,4-dichlorobenzene, tetrachloroethene, and trichloroethene; (2) several linear alkylbenzene compounds, octyl phenol, and a tetramethylbutyl phenol isomer that are related to detergent use; (3) 9-phenyl-9H-carbazole, a compound related to coal tars and coal combustion residues; and (4) caffeine. The only compound present in water in concentrations greater than U.S. Environmental Protection Agency maximum contaminant levels for drinking water was tetrachloroethene (6.0 micrograms per liter) in a sample collected 13.5 kilometers downstream from the waste water discharge. Compounds identified from the streambed-sediment samples include a xylene isomer at 7.7 kilometers downstream and chrysene, fluoranthene, pyrene, and a xylene isomer at 13.5 kilometers downstream from the wastewater discharge.</p>\n<p>Comparison of instantaneous flux values of selected organic compounds in water from downstream sites indicates: (1) the formation of chloroform in the stream following the discharge of the treated effluent, and that (2) instream biodegradation may be decreasing concentrations of linear alkylbenzene compounds in water. The relative persistence of many of the selected organic compounds in Rowlett Creek downstream from the municipal wastewater-treatment plant indicates that they could be transported into Lake Ray Hubbard, a source of municipal water supply.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri934194","usgsCitation":"Buszka, P., Barber, L., Schroeder, M., and Becker, L., 1994, Organic compounds downstream from a treated-wastewater discharge near Dallas, Texas, March 1987: U.S. Geological Survey Water-Resources Investigations Report 93-4194, iv, 19 p., https://doi.org/10.3133/wri934194.","productDescription":"iv, 19 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true},{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":118851,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4194/report-thumb.jpg"},{"id":54456,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4194/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","city":"Dallas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.78199768066406,\n              32.7872745269555\n            ],\n            [\n              -96.78199768066406,\n              33.19790226259598\n            ],\n            [\n              -96.38992309570311,\n              33.19790226259598\n            ],\n            [\n              -96.38992309570311,\n              32.7872745269555\n            ],\n            [\n              -96.78199768066406,\n              32.7872745269555\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db610607","contributors":{"authors":[{"text":"Buszka, P.M.","contributorId":49001,"corporation":false,"usgs":true,"family":"Buszka","given":"P.M.","affiliations":[],"preferred":false,"id":194680,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barber, L.B. II","contributorId":6097,"corporation":false,"usgs":true,"family":"Barber","given":"L.B.","suffix":"II","affiliations":[],"preferred":false,"id":194678,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schroeder, M.P.","contributorId":41453,"corporation":false,"usgs":true,"family":"Schroeder","given":"M.P.","email":"","affiliations":[],"preferred":false,"id":194679,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Becker, L.D.","contributorId":84797,"corporation":false,"usgs":true,"family":"Becker","given":"L.D.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":194681,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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