{"pageNumber":"1505","pageRowStart":"37600","pageSize":"25","recordCount":46679,"records":[{"id":13796,"text":"ofr8727 - 1987 - The U.S. Geological Survey Federal-State Cooperative Water-Resources Program, fiscal year 1986","interactions":[],"lastModifiedDate":"2012-02-02T00:06:49","indexId":"ofr8727","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-27","title":"The U.S. Geological Survey Federal-State Cooperative Water-Resources Program, fiscal year 1986","docAbstract":"The U.S. Geological Survey 's Federal-State Cooperative Water Resources Program has been in operation for 91 years as of fiscal year (FY) 1986. Hydrologic data collection and interpretive investigations are underway in every State, Puerto Rico, and several territories in cooperation with more than 900 State, regional and local agencies. Federal funds amounted to $49.8 million in this 50-50 matching activity. Total funding was about $106 million, which included $6.9 million furnished by cooperating agencies on an unmatched basis. The Cooperative Program comprised more than 40% of the overall FY 1986 budget of the Survey 's Water Resources Division. The areas of principal emphasis during the year included groundwater contamination, stream quality, water supply and demand, and hydrologic hazards. Information is presented on program priorities and investigations implemented under the merit proposal process. The status of water use information activities, which are being carried out in 48 states and Puerto Rico is reviewed briefly. Standard methods for collecting the data are being developed. Each state has a computerized State Water-Use Data System for storage and retrieval of water-use data for individual users or facilities. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8727","usgsCitation":"Gilbert, B., and Mann, W., 1987, The U.S. Geological Survey Federal-State Cooperative Water-Resources Program, fiscal year 1986: U.S. Geological Survey Open-File Report 87-27, iv, 38 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr8727.","productDescription":"iv, 38 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":146009,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0027/report-thumb.jpg"},{"id":42366,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0027/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db673673","contributors":{"authors":[{"text":"Gilbert, B.K.","contributorId":32167,"corporation":false,"usgs":true,"family":"Gilbert","given":"B.K.","email":"","affiliations":[],"preferred":false,"id":168406,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mann, W.B.","contributorId":60230,"corporation":false,"usgs":true,"family":"Mann","given":"W.B.","affiliations":[],"preferred":false,"id":168407,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16018,"text":"ofr87228 - 1987 - Water-resources report prepared by the U.S. Geological Survey, Texas District, 1973-1986","interactions":[],"lastModifiedDate":"2016-08-12T14:37:51","indexId":"ofr87228","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-228","title":"Water-resources report prepared by the U.S. Geological Survey, Texas District, 1973-1986","docAbstract":"<p>Since 1973, personnel of the Texas District, Water Resources Division of the U.S. Geological Survey have written and published approximately 300 reports concerning the water resources of Texas. These reports vary considerably in subject matter, complexity, format, desired audience, and publication outlet. Some of the reports have been published in different outlets of U.S. Geological Survey formal report series Professional Paper, Water-Supply Paper, and Hydrologic Investigations Atlas and informal report series Water-Resources Investigations, Open-File, and Water-Data Reports. Some have been published by cooperating agencies (hereinafter called \"Cooperator-Published Reports\") in their prescribed report series; occasionally, some reports are published both in a U.S. Geological Survey series and a cooperating agency series.</p>\n<p>This compilation lists reports prepared and published by the Texas District during 1973 through 1986 and is a continuation of a previous report, WRIR 20-75, which listed reports released and published during 1887-1974 (Friebele, 1975). Also included in this compilation are some reports published in 1973 and 1974 and a complete listing of Edwards Underground Water District bulletins and reports which were omitted from WRIR 20-75.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87228","usgsCitation":"1987, Water-resources report prepared by the U.S. Geological Survey, Texas District, 1973-1986: U.S. Geological Survey Open-File Report 87-228, iii, 40 p., https://doi.org/10.3133/ofr87228.","productDescription":"iii, 40 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":44960,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0228/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147923,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0228/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4ded","contributors":{"compilers":[{"text":"Sladek, Gail J. gjsladek@usgs.gov","contributorId":1005,"corporation":false,"usgs":true,"family":"Sladek","given":"Gail","email":"gjsladek@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":645384,"contributorType":{"id":3,"text":"Compilers"},"rank":1}]}}
,{"id":13784,"text":"ofr87500 - 1987 - Gravity profiles across the Uyaijah Ring structure, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2015-09-16T20:47:11","indexId":"ofr87500","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-500","title":"Gravity profiles across the Uyaijah Ring structure, Kingdom of Saudi Arabia","docAbstract":"<p>Three detailed gravity profiles across parts of the Uyaijah ring structure have been completed using an average station spacing of 260 M (giving a total of 217 gravity stations) and level surveys for elevation control. When combined with regional gravity-anomaly data, the profiles are adequate for construction of a structural model of the ring complex based on gravity models.</p>\n<p>The resulting structural model, based on profile fits to gravity responses of three-dimensional models and excess-mass calculations, gives a depth estimate to the base of the complex of 4.75 km. The contacts of the complex are inferred to be steeply dipping inward along the southwest margin of the structure. To the north and east, however, the basal contact of the complex dips more gently inward (about 30 degrees). The ring structure appears to be composed of three laccolith-shaped plutons; two are granitic in composition and make up about 85 percent of the volume of the complex, and one is granodioritic and comprises the remaining 15 percent. The source area for the plutons appears to be in the southwest quadrant of the Uyaijah ring structure. A northwest-trending shear zone cuts the northern half of the structure and contains mafic dikes that have a small but identifiable gravity-anomaly response. The structural model agrees with models derived from geological interpretation except that the estimated depth to which the structure extends is decreased considerably by the gravity results.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr87500","usgsCitation":"Gettings, M.E., and Andreasen, G.E., 1987, Gravity profiles across the Uyaijah Ring structure, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 87-500, i, 19 p., ill., maps, https://doi.org/10.3133/ofr87500.","productDescription":"i, 19 p., ill., maps","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":42355,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0500/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145944,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0500/report-thumb.jpg"}],"country":"Saudi Arabia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              43.5,\n              22\n            ],\n            [\n              43.5,\n              23\n            ],\n            [\n              45,\n              23\n            ],\n            [\n              45,\n              22\n            ],\n            [\n              43.5,\n              22\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db67210d","contributors":{"authors":[{"text":"Gettings, M. E.","contributorId":25148,"corporation":false,"usgs":true,"family":"Gettings","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":168380,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreasen, G. E.","contributorId":105315,"corporation":false,"usgs":true,"family":"Andreasen","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":168381,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":13518,"text":"ofr87633 - 1987 - HVO polling telemetry system for low frequency data acquisition; software users' guide","interactions":[],"lastModifiedDate":"2012-02-02T00:06:38","indexId":"ofr87633","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-633","title":"HVO polling telemetry system for low frequency data acquisition; software users' guide","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87633","usgsCitation":"English, T., 1987, HVO polling telemetry system for low frequency data acquisition; software users' guide: U.S. Geological Survey Open-File Report 87-633, 51 p.  ;28 cm., https://doi.org/10.3133/ofr87633.","productDescription":"51 p.  ;28 cm.","costCenters":[],"links":[{"id":144654,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0633/report-thumb.jpg"},{"id":42002,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0633/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649f11","contributors":{"authors":[{"text":"English, T.T.","contributorId":49799,"corporation":false,"usgs":true,"family":"English","given":"T.T.","email":"","affiliations":[],"preferred":false,"id":167935,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57484,"text":"wdrKY861 - 1987 - Water Resources Data for Kentucky, Water Year 1986","interactions":[],"lastModifiedDate":"2012-02-02T00:12:09","indexId":"wdrKY861","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"KY-86-1","title":"Water Resources Data for Kentucky, Water Year 1986","language":"ENGLISH","doi":"10.3133/wdrKY861","usgsCitation":"Toms, S., Sholar, C., and Zettwoch, D., 1987, Water Resources Data for Kentucky, Water Year 1986: U.S. Geological Survey Water Data Report KY-86-1, 380 p., https://doi.org/10.3133/wdrKY861.","productDescription":"380 p.","costCenters":[],"links":[{"id":181807,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fce78","contributors":{"authors":[{"text":"Toms, S.G.","contributorId":80346,"corporation":false,"usgs":true,"family":"Toms","given":"S.G.","email":"","affiliations":[],"preferred":false,"id":257140,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sholar, C.J.","contributorId":44186,"corporation":false,"usgs":true,"family":"Sholar","given":"C.J.","affiliations":[],"preferred":false,"id":257138,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zettwoch, D.D.","contributorId":44950,"corporation":false,"usgs":true,"family":"Zettwoch","given":"D.D.","affiliations":[],"preferred":false,"id":257139,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":20705,"text":"ofr87373 - 1987 - Granitic-rocks modal data from the southern Sierra Nevada, California","interactions":[],"lastModifiedDate":"2012-02-02T00:07:53","indexId":"ofr87373","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-373","title":"Granitic-rocks modal data from the southern Sierra Nevada, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87373","usgsCitation":"Ross, D.C., 1987, Granitic-rocks modal data from the southern Sierra Nevada, California: U.S. Geological Survey Open-File Report 87-373, 276 p.  :ill., maps ;28 cm., https://doi.org/10.3133/ofr87373.","productDescription":"276 p.  :ill., maps ;28 cm.","costCenters":[],"links":[{"id":154741,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0373/report-thumb.jpg"},{"id":50263,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0373/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672520","contributors":{"authors":[{"text":"Ross, D. C.","contributorId":103681,"corporation":false,"usgs":true,"family":"Ross","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":183098,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20695,"text":"ofr8653 - 1987 - Climatological data for the rice-growing areas along the North Coast of Puerto Rico","interactions":[],"lastModifiedDate":"2012-02-02T00:07:53","indexId":"ofr8653","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"86-53","title":"Climatological data for the rice-growing areas along the North Coast of Puerto Rico","docAbstract":"Rainfall, temperature, wind velocity and pan evaporation data were collected from May 1983 to September 1985, in the rice growing areas of Vega Baja, Manati, and Arecibo in northern Puerto Rico. Daily values and statistics including mean, standard deviation, extremes, and totals for each month of record were compiled. Descriptions of equipment installation and operation, data processing, and significance of climatological data for rice cultivation are presented. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8653","usgsCitation":"Roman-Mas, A., and Green, B., 1987, Climatological data for the rice-growing areas along the North Coast of Puerto Rico: U.S. Geological Survey Open-File Report 86-53, iv, 90 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr8653.","productDescription":"iv, 90 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":154613,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0053/report-thumb.jpg"},{"id":50256,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0053/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de101","contributors":{"authors":[{"text":"Roman-Mas, Angel","contributorId":59816,"corporation":false,"usgs":true,"family":"Roman-Mas","given":"Angel","email":"","affiliations":[],"preferred":false,"id":183081,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Green, Bruce","contributorId":79129,"corporation":false,"usgs":true,"family":"Green","given":"Bruce","email":"","affiliations":[],"preferred":false,"id":183082,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":57397,"text":"wdrPA863 - 1987 - Water resources data for Pennsylvania, water year 1986. Volume 3: Ohio River and St. Lawrence River Basins","interactions":[],"lastModifiedDate":"2020-05-13T17:07:16.969913","indexId":"wdrPA863","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"PA-86-3","title":"Water resources data for Pennsylvania, water year 1986. Volume 3: Ohio River and St. Lawrence River Basins","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrPA863","usgsCitation":"Lescinsky, J., Coll, M., and Siwicki, R., 1987, Water resources data for Pennsylvania, water year 1986. Volume 3: Ohio River and St. Lawrence River Basins: U.S. Geological Survey Water Data Report PA-86-3, viii, 205 p. , https://doi.org/10.3133/wdrPA863.","productDescription":"viii, 205 p. 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc937","contributors":{"authors":[{"text":"Lescinsky, J.B.","contributorId":83197,"corporation":false,"usgs":true,"family":"Lescinsky","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":256906,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coll, M.B.","contributorId":19629,"corporation":false,"usgs":true,"family":"Coll","given":"M.B.","affiliations":[],"preferred":false,"id":256905,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Siwicki, R.W.","contributorId":100060,"corporation":false,"usgs":true,"family":"Siwicki","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":256907,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":14406,"text":"ofr87604 - 1987 - The U.S. Geological Survey instrument for simultaneous multi-element atomic absorption spectrometry; description of the hardware and of the system control and data aquisition software","interactions":[],"lastModifiedDate":"2012-02-02T00:07:03","indexId":"ofr87604","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-604","title":"The U.S. Geological Survey instrument for simultaneous multi-element atomic absorption spectrometry; description of the hardware and of the system control and data aquisition software","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87604","usgsCitation":"Kane, J.S., 1987, The U.S. Geological Survey instrument for simultaneous multi-element atomic absorption spectrometry; description of the hardware and of the system control and data aquisition software: U.S. Geological Survey Open-File Report 87-604, 54 p. :ill. ;28 cm., https://doi.org/10.3133/ofr87604.","productDescription":"54 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":147658,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0604/report-thumb.jpg"},{"id":43089,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0604/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db673154","contributors":{"authors":[{"text":"Kane, J. S.","contributorId":106507,"corporation":false,"usgs":true,"family":"Kane","given":"J.","middleInitial":"S.","affiliations":[],"preferred":false,"id":169400,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18464,"text":"ofr85421 - 1987 - Streamflow characteristics of the Colorado River Basin in Utah through September 1981","interactions":[],"lastModifiedDate":"2017-08-31T16:15:59","indexId":"ofr85421","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"85-421","title":"Streamflow characteristics of the Colorado River Basin in Utah through September 1981","docAbstract":"<p>&nbsp;This report summarizes discharge data and other streamflow characteristics developed from gag ing-station records collected through September 1981 at 337 stations in the Colorado River Basin in Utah. Data also are included for 14 stations in adjacent areas of the bordering states of Arizona, Colorado, and Wyoming (fig. 1). The study leading to this report was done in cooperation with the U.S. Bureau of Land Management, which needs the streamflow data in order to evaluate impacts of mining on the hydrologic system. The report also will be beneficial to other Federal, State, and county agencies and to individuals concerned with water supply and water problems in the Colorado River Basin.</p><p>The streamflow characteristics in the report could be useful in many water-related studies that involve the following:</p><p>Definition of baseline-hydrologic conditions; studies of the effects of man's activities on streamflow; frequency analyses of low and high flows; regional analyses of streamflow characteristics; design of water-supply systems; water-power studies; forecasting of stream discharge; time-series analyses of streamflow; design of flood-control structures; stream-pollution studies; and water-chemistry transport studies.</p><p>The basic data used to develop the summaries in this report are records of daily and peak discharge collected by the U.S. Geological Survey and other Federal agencies. Much of the work of the Geological Survey was done in cooperation with Federal, State, and county agencies. Discharge records<br>included in the report generally were for stations with at least 1 complete water year of record and nearby stations that were on the same stream and had different streamflow characteristics. A water year is a 12-month period ending September 30, and it is designated by the calendar year in which it ends. For streams that have had significant changes in regulation by reservoirs or diversions, the records before and after those changes were used separately to provide streamflow characteristics for each period of homogeneous streamflow and to show the change in the characteristics. Summaries for annual peak discharge are included only for stations with 5 or more years of data. The summaries of annual lowest and highest mean-discharge frequency are reported for stations with 10 or more years of daily-discharge record and for which computer-generated frequency curves provided a reasonable fit of the plotted data.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr85421","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Christensen, R., Johnson, E., and Plantz, G., 1987, Streamflow characteristics of the Colorado River Basin in Utah through September 1981: U.S. Geological Survey Open-File Report 85-421, iv, 674 p., https://doi.org/10.3133/ofr85421.","productDescription":"iv, 674 p.","numberOfPages":"678","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":152201,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0421/report-thumb.jpg"},{"id":47822,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0421/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Colorado River basin","publicComments":"This is also Utah Hydrologic-Data Report no. 42","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4e21","contributors":{"authors":[{"text":"Christensen, R.C.","contributorId":56670,"corporation":false,"usgs":true,"family":"Christensen","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":179174,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, E.B.","contributorId":77953,"corporation":false,"usgs":true,"family":"Johnson","given":"E.B.","affiliations":[],"preferred":false,"id":179175,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Plantz, G.G.","contributorId":79103,"corporation":false,"usgs":true,"family":"Plantz","given":"G.G.","affiliations":[],"preferred":false,"id":179176,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":4353,"text":"cir957 - 1987 - Mineralogy and instrumental neutron activation analysis of seven National Bureau of Standards and three Instituto de Pesquisas Tecnologicas clay reference samples","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"cir957","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"957","title":"Mineralogy and instrumental neutron activation analysis of seven National Bureau of Standards and three Instituto de Pesquisas Tecnologicas clay reference samples","docAbstract":"The concentrations of 3 oxides and 29 elements in 7 National Bureau of Standards (NBS) and 3 Instituto de Pesquisas Techno16gicas (IPT) reference clay samples were etermined by instrumental neutron activation analysis. The analytical work was designed to test the homogeneity of constituents in three new NBS reference clays, NBS-97b, NBS-98b, and NBS-679. The analyses of variance of 276 sets of data for these three standards show that the constituents are distributed homogeneously among bottles of samples for 94 percent of the sets of data. \r\n\r\nThree of the reference samples (NBS-97, NBS-97a, and NBS-97b) are flint clays; four of the samples (NBS-98, NBS-98a, NBS-98b, and IPT-32) are plastic clays, and three of the samples (NBS-679, IPT-28, and IPT-42) are miscellaneous clays (both sedimentary and residual). Seven clays are predominantly kaolinite; the other three clays contain illite and kaolinite in the approximate ratio 3:2. Seven clays contain quartz as the major nonclay mineral. The mineralogy of the flint and plastic clays from Missouri (NBS-97a and NBS-98a) differs markedly from that of the flint and plastic clays from Pennsylvania (NBS-97, NBS-97b, NBS-98, and NBS-98b). \r\n\r\nThe flint clay NBS-97 has higher average chromium, hafnium, lithium, and zirconium contents than its replacement, reference sample NBS-97b. The differences between the plastic clay NBS-98 and its replacement, NBS-98b, are not as pronounced. The trace element contents of the flint and plastic clays from Missouri, NBS-97a and NBS-98a, differ significantly from those of the clays from Pennsylvania, especially the average rare earth element (REE) contents. The trace element contents of clay sample IPT-32 differ from those of the other plastic clays. IPT-28 and IPT-42 have some average trace element contents that differ not only between these two samples but also from all the other clays. IPT-28 has the highest summation of the average REE contents of the 10 samples. The uranium content of NBS-98a, 46 parts per million, is very much higher than that of the other clays. \r\n\r\nPlots of average REE contents of the flint and plastic clays, normalized to chondritic abundances, show that the clays from Missouri differ from the same types of clay from Pennsylvania. The plot of REE contents for the miscellaneous clays shows that the normalized means for the elements lanthanum through samarium for IPT-28 are much greater than those for the other miscellaneous clays. The means for the elements europium through lutetium are similar for all three miscellaneous clays.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir957","usgsCitation":"Hosterman, J.W., Flanagan, F., Bragg, A., Doughten, M., Filby, R., Grimm, C., Mee, J.S., Potts, P., and Rogers, N., 1987, Mineralogy and instrumental neutron activation analysis of seven National Bureau of Standards and three Instituto de Pesquisas Tecnologicas clay reference samples: U.S. Geological Survey Circular 957, iv, 38 p. :ill., map ;27 cm., https://doi.org/10.3133/cir957.","productDescription":"iv, 38 p. :ill., map ;27 cm.","costCenters":[],"links":[{"id":124633,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1987/0957/report-thumb.jpg"},{"id":31462,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1987/0957/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699e44","contributors":{"authors":[{"text":"Hosterman, John W.","contributorId":48962,"corporation":false,"usgs":true,"family":"Hosterman","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":148921,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flanagan, F.J.","contributorId":50139,"corporation":false,"usgs":true,"family":"Flanagan","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":148922,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bragg, Anne","contributorId":78600,"corporation":false,"usgs":true,"family":"Bragg","given":"Anne","email":"","affiliations":[],"preferred":false,"id":148923,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Doughten, M. W.","contributorId":101648,"corporation":false,"usgs":true,"family":"Doughten","given":"M. W.","affiliations":[],"preferred":false,"id":148925,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Filby, R.H.","contributorId":26071,"corporation":false,"usgs":true,"family":"Filby","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":148918,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Grimm, Catherine","contributorId":40063,"corporation":false,"usgs":true,"family":"Grimm","given":"Catherine","email":"","affiliations":[],"preferred":false,"id":148920,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Mee, J. S.","contributorId":25168,"corporation":false,"usgs":true,"family":"Mee","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":148917,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Potts, P.J.","contributorId":38416,"corporation":false,"usgs":true,"family":"Potts","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":148919,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Rogers, N.W.","contributorId":83650,"corporation":false,"usgs":true,"family":"Rogers","given":"N.W.","email":"","affiliations":[],"preferred":false,"id":148924,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":2767,"text":"wsp2301 - 1987 - Relations between quality of urban runoff and quality of Lake Ellyn at Glen Ellyn, Illinois","interactions":[],"lastModifiedDate":"2018-01-30T21:05:46","indexId":"wsp2301","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2301","title":"Relations between quality of urban runoff and quality of Lake Ellyn at Glen Ellyn, Illinois","docAbstract":"Comparison of flow and chemical data collected at the principal inlet and at the outlets of Lake Ellynman urban lake in the Chicago metropolitan are--shows that detention storage alters the discharge and the quality of urban runoff. Peak water discharge and variation in the concentration of constituents transported by the runoff are usually reduced. Mass-balance relations based on comparison of measured constituent loads at the inlet and the outlets show that the lake is very efficient in trapping suspended solids, suspended sediment, and sediment-associated metals. Calculated trap efficiencies for many dissolved constituents were negative. However, negative efficiencies appear to be influenced mostly by insufficient sampling in winter. Trap efficiencies for nitrogen and phosphorus are intermediate to those determined for other constituents. \r\n\r\nSolids accumulate on the lake bottom as organic-rich muds that reduce lake storage and cover potential habitat for aquatic organisms. Lake sediments, particularly fine-grained sediments, have elevated concentrations of metals associated with them. Several organic compounds, not detected in inlet- or outlet-water samples, were detected in a lake-sediment sample collected near the inlet. \r\n\r\nConcentrations of many constituents dissolved in lake water are seasonally cyclic, with annual concentration peaks occurring during the winter. Establishment and maintenance of desirable benthic invertebrate and fish populations appear to be inhibited by sediment deposition.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2301","usgsCitation":"Striegl, R.G., and Cowan, E., 1987, Relations between quality of urban runoff and quality of Lake Ellyn at Glen Ellyn, Illinois: U.S. Geological Survey Water Supply Paper 2301, v, 59 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2301.","productDescription":"v, 59 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":29203,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2301/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138605,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2301/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db63465e","contributors":{"authors":[{"text":"Striegl, Robert G. 0000-0002-8251-4659 rstriegl@usgs.gov","orcid":"https://orcid.org/0000-0002-8251-4659","contributorId":1630,"corporation":false,"usgs":true,"family":"Striegl","given":"Robert","email":"rstriegl@usgs.gov","middleInitial":"G.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":36183,"text":"Hydro-Ecological Interactions Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":false,"id":145748,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cowan, Ellen A.","contributorId":103255,"corporation":false,"usgs":true,"family":"Cowan","given":"Ellen A.","affiliations":[],"preferred":false,"id":145749,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25418,"text":"wri874044 - 1987 - Comparison of irrigation pumpage with change in ground-water storage in the High Plains aquifer in Chase, Dundy, and Perkins counties, Nebraska, 1975-83","interactions":[],"lastModifiedDate":"2012-02-02T00:08:09","indexId":"wri874044","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4044","title":"Comparison of irrigation pumpage with change in ground-water storage in the High Plains aquifer in Chase, Dundy, and Perkins counties, Nebraska, 1975-83","docAbstract":"The relation between pumpage and change in storage was evaluated for most of a three-county area in southwestern Nebraska from 1975 through 1983. Initial comparison of the 1975-83 pumpage with change in storage in the study area indicated that the 1 ,042,300 acre-ft of change in storage was only about 30% of the 3,425,000 acre-ft of pumpage. An evaluation of the data used to calculate pumpage and change in storage indicated that there was a relatively large potential for error in estimates of specific yield. As a result, minimum and maximum values of specific yield were estimated and used to recalculate change in storage. Estimates also were derived for the minimum and maximum amounts of recharge that could occur as a result of cultivation practices. The minimum and maximum estimates for specific yield and for recharge from cultivation practices were used to compute a range of values for the potential amount of additional recharge that occurred as a result of irrigation. The minimum and maximum amounts of recharge that could be caused by irrigation in the study area were 953,200 acre-ft (28% of pumpage) and 2,611,200 acre-ft (76% of pumpage), respectively. These values indicate that a substantial percentage of the water pumped from the aquifer is resupplied to storage in the aquifer as a result of a combination of irrigation return flow and enhanced recharge from precipitation that results from cultivation and irrigation practices. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874044","usgsCitation":"Heimes, F., Ferrigno, C., Gutentag, E., Lucky, R., Stephens, D., and Weeks, J., 1987, Comparison of irrigation pumpage with change in ground-water storage in the High Plains aquifer in Chase, Dundy, and Perkins counties, Nebraska, 1975-83: U.S. Geological Survey Water-Resources Investigations Report 87-4044, iv, 34 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874044.","productDescription":"iv, 34 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123377,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4044/report-thumb.jpg"},{"id":54138,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4044/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae383","contributors":{"authors":[{"text":"Heimes, F.J.","contributorId":60654,"corporation":false,"usgs":true,"family":"Heimes","given":"F.J.","affiliations":[],"preferred":false,"id":193606,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ferrigno, C.F.","contributorId":27092,"corporation":false,"usgs":true,"family":"Ferrigno","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":193604,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gutentag, E. D.","contributorId":70015,"corporation":false,"usgs":true,"family":"Gutentag","given":"E. D.","affiliations":[],"preferred":false,"id":193608,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lucky, R.R.","contributorId":89171,"corporation":false,"usgs":true,"family":"Lucky","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":193609,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Stephens, D.M.","contributorId":42970,"corporation":false,"usgs":true,"family":"Stephens","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":193605,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Weeks, J.B.","contributorId":61426,"corporation":false,"usgs":true,"family":"Weeks","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":193607,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":57443,"text":"wdrOR851 - 1987 - Water resources data for Oregon, water year 1985. Volume 1: Eastern Oregon","interactions":[],"lastModifiedDate":"2016-04-25T14:01:44","indexId":"wdrOR851","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"OR-85-1","title":"Water resources data for Oregon, water year 1985. Volume 1: Eastern Oregon","docAbstract":"<p>Water Resources Data for the 1985 water year for Oregon consist of records of stage, discharge, and water quality of streams; and stage, contents, and water quality of lakes and reservoirs. This report, in two volumes , contains discharge records for 259 gaging stations; stage only records for 10 gaging stations; stage and contents for 37 lakes and reservoirs; water quality for 82 stations, and water quality for 3 precipitation stations. Also included are 5 crest-stage, partial-record stations. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S . Geological Survey and cooperating State and Federal agencies in Oregon.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, Oregon","doi":"10.3133/wdrOR851","usgsCitation":"Alexander, C., Moffatt, R.L., Boucher, P.R., and Smith, M., 1987, Water resources data for Oregon, water year 1985. Volume 1: Eastern Oregon: U.S. Geological Survey Water Data Report OR-85-1, xi, 218 p., https://doi.org/10.3133/wdrOR851.","productDescription":"xi, 218 p.","numberOfPages":"234","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":174533,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdrOR851.jpg"},{"id":320529,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1985/or-85-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.717529296875,\n              41.9921602333763\n            ],\n            [\n              -121.53076171875,\n              45.69850658738848\n            ],\n            [\n              -120.62988281249999,\n              45.75219336063106\n            ],\n            [\n              -119.80590820312499,\n              45.84410779560204\n            ],\n            [\n              -118.93798828125,\n              46.01985337287634\n            ],\n            [\n              -116.89453125,\n              45.99696161820381\n            ],\n            [\n              -116.77917480468749,\n              45.817315080406246\n            ],\n            [\n              -116.53198242187499,\n              45.744526980468436\n            ],\n            [\n              -116.52099609375,\n              45.6716438522655\n            ],\n            [\n              -116.46606445312499,\n              45.6101948758674\n            ],\n            [\n              -116.597900390625,\n              45.41773242370463\n            ],\n            [\n              -116.7242431640625,\n              45.166547157856016\n            ],\n            [\n              -116.84509277343751,\n              45.01918507438176\n            ],\n            [\n              -116.90551757812499,\n              44.83249999349062\n            ],\n            [\n              -117.05932617187499,\n              44.735027899515465\n            ],\n            [\n              -117.15270996093749,\n              44.51609322284931\n            ],\n            [\n              -117.21313476562499,\n              44.465151013519616\n            ],\n            [\n              -117.1966552734375,\n              44.315987905196906\n            ],\n            [\n              -117.04284667968749,\n              44.24126379833979\n            ],\n            [\n              -116.89453125,\n              44.17038488259618\n            ],\n            [\n              -116.94946289062499,\n              44.000717834282774\n            ],\n            [\n              -116.993408203125,\n              43.8503744993026\n            ],\n            [\n              -117.037353515625,\n              43.83848910616803\n            ],\n            [\n              -117.03186035156251,\n              41.99624282178583\n            ],\n            [\n              -121.717529296875,\n              41.9921602333763\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcb62","contributors":{"authors":[{"text":"Alexander, C.W.","contributorId":76745,"corporation":false,"usgs":true,"family":"Alexander","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":257025,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moffatt, R. L.","contributorId":79889,"corporation":false,"usgs":true,"family":"Moffatt","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":257026,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Boucher, P. R.","contributorId":108088,"corporation":false,"usgs":true,"family":"Boucher","given":"P.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":257027,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, M.L.","contributorId":35386,"corporation":false,"usgs":true,"family":"Smith","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":257024,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1959,"text":"wsp2317 - 1987 - Simulation of flood hydrographs for Georgia streams","interactions":[],"lastModifiedDate":"2017-02-01T10:16:14","indexId":"wsp2317","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2317","title":"Simulation of flood hydrographs for Georgia streams","docAbstract":"Flood hydrographs are needed for the design of many highway drainage structures and embankments. A method for simulating these flood hydrographs at ungaged sites in Georgia is presented in this report. \r\n\r\nThe O'Donnell method was used to compute unit hydrographs and lagtimes for 355 floods at 80 gaging stations. An average unit hydrograph and an average lagtime were computed for each station. These average unit hydrographs were transformed to unit hydrographs having durations of one-fourth, one-third, one-half, and three-fourths lagtime, then reduced to dimensionless terms by dividing the time by lagtime and the discharge by peak discharge. Hydrographs were simulated for these 355 floods and their widths were compared with the widths of the observed hydrographs at 50 and 75 percent of peak flow. The dimensionless hydrograph based on one-half lagtime duration provided the best fit of the observed data. \r\n\r\nMultiple regression analysis was then used to define relations between lagtime and certain physical basin characteristics; of these characteristics, drainage area and slope were found to be significant for the rural-stream equations and drainage area, slope, and impervious area were found to be significant for the Atlanta urban-stream equation. \r\n\r\nA hydrograph can be simulated from the dimensionless hydrograph, the peak discharge of a specific recurrence interval, and the lagtime obtained from regression equations for any site in Georgia having a drainage area of less than 500 square miles. \r\n\r\nFor simulating hydrographs at sites having basins larger than 500 square miles, the U.S. Geological Survey computer model CONROUT can be used. This model routes streamflow from an upstream channel location to a user-defined location downstream. The product of CONROUT is a simulated discharge hydrograph for the downstream site that has a peak discharge of a specific recurrence interval.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wsp2317","usgsCitation":"Inman, E.J., 1987, Simulation of flood hydrographs for Georgia streams: U.S. Geological Survey Water Supply Paper 2317, iv, 26 p :ill. map ;28 cm., https://doi.org/10.3133/wsp2317.","productDescription":"iv, 26 p :ill. map ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":138560,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2317/report-thumb.jpg"},{"id":27312,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2317/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":12062,"text":"ofr87509 - 1987 - Geochemistry and preliminary assessment of resource potential for postorogenic granites of the southwestern Arabian Shield, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2015-09-22T14:45:20","indexId":"ofr87509","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-509","title":"Geochemistry and preliminary assessment of resource potential for postorogenic granites of the southwestern Arabian Shield, Kingdom of Saudi Arabia","docAbstract":"<p>Geochemical data for samples from 55 postorogenic plutons of the southwestern Arabian Shield show that these granitoids are generally less evolved than similar granitoids of the eastern Arabian Shield. Radioelement contents are low to normal relative to typical granitic rocks and uranium contents are distinctly low relative to rocks of the eastern Arabian Shield. The data indicate low favorability for ore deposits of elements that are typically enriched in granites at the end stages of magmatism such as tin, tungsten, niobium, tantalum, molybdenum, rare-earth elements, and radioactive elements.</p>\n<p>Regional geochemical patterns are not consistent with the north-south trending microplate boundary that has been proposed by other workers. Correlation coefficients for trace-element data obtained during the current study also argue against sharp compositional breaks in the protolith for the postorogenic granites. Consideration of the data presented here and similar data for granitoids of the eastern Arabian Shield, suggest the existence of a compositionally gradational protolith of continental affinity to the east and oceanic affinity to the west.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr87509","usgsCitation":"Stuckless, J., VanTrump, G., Bush, C.A., Vaughn, R.B., and Bartel, A., 1987, Geochemistry and preliminary assessment of resource potential for postorogenic granites of the southwestern Arabian Shield, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 87-509, i, 59 p., https://doi.org/10.3133/ofr87509.","productDescription":"i, 59 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":144358,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0509/report-thumb.jpg"},{"id":40078,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0509/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Saudi Arabia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              41.5,\n              18\n            ],\n            [\n              38.4,\n              22\n            ],\n            [\n              44,\n              22\n            ],\n            [\n              44,\n              18\n            ],\n            [\n              41.5,\n              18\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab6e1","contributors":{"authors":[{"text":"Stuckless, J. S.","contributorId":6060,"corporation":false,"usgs":true,"family":"Stuckless","given":"J. S.","affiliations":[],"preferred":false,"id":164897,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"VanTrump, George Jr.","contributorId":54193,"corporation":false,"usgs":true,"family":"VanTrump","given":"George","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":164901,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bush, C. A.","contributorId":43344,"corporation":false,"usgs":true,"family":"Bush","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":164900,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Vaughn, R. B.","contributorId":27043,"corporation":false,"usgs":true,"family":"Vaughn","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":164898,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bartel, A.J.","contributorId":34508,"corporation":false,"usgs":true,"family":"Bartel","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":164899,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":61034,"text":"mf1834C - 1987 - Maps showing anomalous copper concentrations in stream sediments and heavy-mineral concentrates from the Ajo and Lukeville 1 degree by 2 degrees quadrangles, Arizona","interactions":[],"lastModifiedDate":"2016-08-23T10:01:25","indexId":"mf1834C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1834","chapter":"C","title":"Maps showing anomalous copper concentrations in stream sediments and heavy-mineral concentrates from the Ajo and Lukeville 1 degree by 2 degrees quadrangles, Arizona","docAbstract":"<p>This map is part of a folio of maps of the Ajo and Lukeville 1 &deg; x 2&deg; quadrangles, Arizona, prepared under the Conterminous United States Mineral Assessment Program. Other publications in this folio include U.S. Geological Survey Miscellaneous Field Studies Maps MF-1831-A and MF-1831-B and Open-File Reports 82-119, 82&ndash;599, and 83&ndash;734. Open-File Reports 82-119 and 83&ndash;731 constitute the basic data and initial interpretation on which this discussion is predicated.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1834C","usgsCitation":"Theobald, P., and Barton, H.N., 1987, Maps showing anomalous copper concentrations in stream sediments and heavy-mineral concentrates from the Ajo and Lukeville 1 degree by 2 degrees quadrangles, Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 1834, Plate: 35.48 x 32.10 inches, https://doi.org/10.3133/mf1834C.","productDescription":"Plate: 35.48 x 32.10 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326167,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1834C.JPG"},{"id":327546,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1834-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","country":"United States","state":"Arizona","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,32 ], [ -114,33 ], [ -112,33 ], [ -112,32 ], [ -114,32 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db60468c","contributors":{"authors":[{"text":"Theobald, P. K.","contributorId":45293,"corporation":false,"usgs":true,"family":"Theobald","given":"P. K.","affiliations":[],"preferred":false,"id":264870,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barton, H. N.","contributorId":99546,"corporation":false,"usgs":true,"family":"Barton","given":"H.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":264871,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60994,"text":"mf1975 - 1987 - Seismicity map of the state of Ohio","interactions":[{"subject":{"id":60993,"text":"mf1142 - 1979 - Seismicity map of the State of Ohio","indexId":"mf1142","publicationYear":"1979","noYear":false,"title":"Seismicity map of the State of Ohio"},"predicate":"SUPERSEDED_BY","object":{"id":60994,"text":"mf1975 - 1987 - Seismicity map of the state of Ohio","indexId":"mf1975","publicationYear":"1987","noYear":false,"title":"Seismicity map of the state of Ohio"},"id":1}],"lastModifiedDate":"2025-05-27T16:39:33.291861","indexId":"mf1975","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1975","title":"Seismicity map of the state of Ohio","docAbstract":"<p>This map is one of a series of seismicity maps produced by the U. S. Geological Survey that show earthquake data of individual states or groups of states at the scale of 1:1,000,000. This map shows only those earthquakes with epicenters located within the boundaries of Ohio, even though earthquakes in nearby states or countries may have been felt or may have caused damage in Ohio.</p>\n<p>The data in table 1 were used to compile the seismicity map; these data are a corrected, expanded, and updated (through 1983) version of the data used by Algermissen (1969) for a study of seismic risk in the United States. The locations and intensities of some earthquakes were revised and intensities were assigned where none had been before. Many earthquakes were added to the original list from new data sources as well as from some old data sources that had not been previously used. The data in table 1 represent best estimates of the location of the epicenter, magnitude, and intensity of each earthquake on the basis of historical and current information. Some of the aftershocks from large earthquakes are listed, but not all, especially for earthquakes that occurred before seismic instruments were universally used.</p>\n<p>The latitude and longitude coordinates of each epicenter were rounded to the nearest tenth of a degree and sorted so that all identical locations were grouped and counted . These locations are represented on the map by a triangle. The number of earthquakes at each location is shown on the map by the arabic number to the right of the triangle. A Roman numeral to the left of a triangle is the maximum Modified Mercalli intensity (Wood and Neumann, 1931) of all earthquakes at that geographic location. The absence of an intensity value indicates that no intensities have been assigned to earthquakes at that location. The year shown below each triangle is the latest year for which the maximum intensity was recorded.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1975","usgsCitation":"Stover, C.W., Reagor, B., and Algermissen, S.T., 1987, Seismicity map of the state of Ohio (Supercedes MF-1142): U.S. Geological Survey Miscellaneous Field Studies Map 1975, 1 Plate: 38.28 x 24.84 inches, https://doi.org/10.3133/mf1975.","productDescription":"1 Plate: 38.28 x 24.84 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":486595,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5546.htm","linkFileType":{"id":5,"text":"html"}},{"id":327562,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1975/plate-1.pdf","text":"Plate","size":"9.28 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,{"id":27093,"text":"wri874073 - 1987 - Estimation of streamflow characteristics and assessment of trends in the Niobrara River at Mariaville, Nebraska","interactions":[],"lastModifiedDate":"2012-02-02T00:08:36","indexId":"wri874073","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4073","title":"Estimation of streamflow characteristics and assessment of trends in the Niobrara River at Mariaville, Nebraska","docAbstract":"A computer model was used to synthesize a long-term streamflow record for the Niobrara River at Mariaville, Nebraska. The record was developed on the basis of 30-plus years of streamflow data from 3 upstream sites, and the U. S. Geological Survey 's CONROUT model was calibrated using 294 days of measured flow at Mariaville; for the calibration period, 87% of the synthesized daily discharges were within 15% of the measured values. The synthesized record was analyzed for trends in streamflow characteristics. A marked decrease in the average consecutive-day, low-flow discharges was detected after 1964, ranging between 162 cu ft/sec less for the 1-day low flow and 200 cu ft/sec less for the 14-day low flow. The decrease probably was caused by the start-up of operations at Merritt Reservoir. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874073","usgsCitation":"Fischer, E., 1987, Estimation of streamflow characteristics and assessment of trends in the Niobrara River at Mariaville, Nebraska: U.S. Geological Survey Water-Resources Investigations Report 87-4073, iv, 25 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874073.","productDescription":"iv, 25 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119852,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4073/report-thumb.jpg"},{"id":55959,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4073/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb188","contributors":{"authors":[{"text":"Fischer, E.E.","contributorId":102480,"corporation":false,"usgs":true,"family":"Fischer","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":197541,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25423,"text":"wri874191 - 1987 - A conceptual framework for ground-water solute-transport studies with emphasis on physical mechanisms of solute movement","interactions":[],"lastModifiedDate":"2012-02-02T00:08:10","indexId":"wri874191","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4191","title":"A conceptual framework for ground-water solute-transport studies with emphasis on physical mechanisms of solute movement","docAbstract":"Analysis of solute transport in groundwater systems involves a complex, multi-discipline study that requires intensive and costly investigation. Groundwater contamination, particularly from point sources, has been growing in importance in recent years. This report examines the physical mechanisms of solute transport, advection and dispersion, and explains how they relate to one another and the scale of study. The approach uses a preliminary analysis prior to collection of new data to focus on the technical problems to be addressed and to direct the initial collection of new data if warranted. The field investigation (collection of new data) progresses in stages that use the new knowledge and understanding gained from the preceding data collection to aid in further data collection as the study proceeds. A major premise of the approach is that the foundation of any analysis is a detailed quantitative definition of: (1) the groundwater flow field in three dimensions, and (2) the distribution of solutes in the contaminant plume in three dimensions at one point in time, or preferably at more than features of the groundwater flow field, and is an important tool for analysis. However, the scale of analysis for solute transport studies is usually much finer than the scale of analysis for groundwater flow alone. Therefore, an increase in detail of the velocity field is needed to provide for accurate calculations of pathlines in three-dimensional heterogeneous groundwater systems. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874191","usgsCitation":"Reilly, T.E., Franke, O.L., Buxton, H.T., and Bennett, G.D., 1987, A conceptual framework for ground-water solute-transport studies with emphasis on physical mechanisms of solute movement: U.S. Geological Survey Water-Resources Investigations Report 87-4191, v, 44 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874191.","productDescription":"v, 44 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122834,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_87_4191.jpg"},{"id":1807,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri874191/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b26e4b07f02db6affac","contributors":{"authors":[{"text":"Reilly, Thomas E. tereilly@usgs.gov","contributorId":1660,"corporation":false,"usgs":true,"family":"Reilly","given":"Thomas","email":"tereilly@usgs.gov","middleInitial":"E.","affiliations":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":193628,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Franke, O. Lehn","contributorId":63357,"corporation":false,"usgs":true,"family":"Franke","given":"O.","email":"","middleInitial":"Lehn","affiliations":[],"preferred":false,"id":193631,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Buxton, Herbert T. hbuxton@usgs.gov","contributorId":1911,"corporation":false,"usgs":true,"family":"Buxton","given":"Herbert","email":"hbuxton@usgs.gov","middleInitial":"T.","affiliations":[{"id":5056,"text":"Office of the AD Energy and Minerals, and Environmental Health","active":true,"usgs":true}],"preferred":true,"id":193629,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bennett, Gordon D.","contributorId":18740,"corporation":false,"usgs":true,"family":"Bennett","given":"Gordon","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":193630,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25968,"text":"wri854246 - 1987 - An assessment of low flows in streams in northeastern Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:28","indexId":"wri854246","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"85-4246","title":"An assessment of low flows in streams in northeastern Wyoming","docAbstract":"Low flows were assessed and summarized in the following basins in northeastern Wyoming: Little Bighorn, Tongue, Powder, Little Missouri, Belle Fourche, Cheyenne, and Niobrara River, and about 200 river miles of the North Platte River and its tributaries. Only existing data from streamflow stations and miscellaneous observation sites during the period, 1930-80, were used. Data for a few stations in Montana and South Dakota were used in the analysis. Data were available for 56 perennial streams, 38 intermittent streams, and 34 ephemeral streams. The distribution of minimum observed flows of record at all stations and sites and the 7-day, 10-year low flows at mountain stations and main-stem plains stations are shown on a map. Seven day low flows were determined by fitting the log Pearsons Type III distribution to the data; results are tabulated only for the stations with at least 10 years of record that included at least one major drought. Most streams that originate in the foothills and plains have no flow during part of every year, and are typical of much of the study area. For stations on these streams , the frequency of the annual maximum number of consecutive days of no flow was determined, as an indicator of the likelihood of extended periods of no flow or drought. For estimates at ungaged sites on streams in the Bighorn Mountains only, a simple regression of 7-day, 10-year low flow on drainage area has a standard error of 64%, based on 19 stations with drainage areas of 2 to 200 sq mi. The 7-day, 10-year low flow in main-stem streams can be interpolated from graphs of 7-day, 10-year low flow versus distance along the main channel. Additional studies of low flow are needed. The data base, particularly synoptic baseflow information, needs considerable expansion. Also, the use of storage-analysis procedures should be considered as a means of assessing the availability of water in streams that otherwise are fully appropriated or that are ephemeral. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854246","usgsCitation":"Armentrout, G., and Wilson, J., 1987, An assessment of low flows in streams in northeastern Wyoming: U.S. Geological Survey Water-Resources Investigations Report 85-4246, iv, 30 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854246.","productDescription":"iv, 30 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124210,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4246/report-thumb.jpg"},{"id":54713,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4246/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54714,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4246/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684e34","contributors":{"authors":[{"text":"Armentrout, G.W.","contributorId":12890,"corporation":false,"usgs":true,"family":"Armentrout","given":"G.W.","affiliations":[],"preferred":false,"id":195560,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, J.F.","contributorId":100881,"corporation":false,"usgs":true,"family":"Wilson","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":195561,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25958,"text":"wri834247 - 1987 - Roughness coefficients for densely vegetated flood plains","interactions":[],"lastModifiedDate":"2012-02-02T00:08:25","indexId":"wri834247","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"83-4247","title":"Roughness coefficients for densely vegetated flood plains","docAbstract":"Although much research has been done on Manning 's roughness coefficients for stream channels, very little has been done on the selection of roughness values for densely vegetated flood plains. In this report four method for determining roughness coefficients for flood plains are examined and evaluated. Field data were collected at 13 sites on wide, densely vegetated flood plains where verified n values were known. The ' vegetation density ' of representative sample areas was measured at each site for use in determining roughness coefficients. The vegetation density method, proved to be useful in determining n values for wide, densely wooded plains. By measuring the area occupied by tree trunks and vegetation in a representative sample area, the vegetation density can be determined. Using the vegetation density in an equation developed from Manning 's formula, the Manning 's n can be determined for the representative sample area. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834247","usgsCitation":"Arcement, G., and Schneider, V., 1987, Roughness coefficients for densely vegetated flood plains: U.S. Geological Survey Water-Resources Investigations Report 83-4247, viii, 62 p. :ill. ;28 cm., https://doi.org/10.3133/wri834247.","productDescription":"viii, 62 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":157555,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4247/report-thumb.jpg"},{"id":54708,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4247/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fe1ee","contributors":{"authors":[{"text":"Arcement, G.J.","contributorId":59058,"corporation":false,"usgs":true,"family":"Arcement","given":"G.J.","affiliations":[],"preferred":false,"id":195546,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schneider, V.R.","contributorId":75129,"corporation":false,"usgs":true,"family":"Schneider","given":"V.R.","email":"","affiliations":[],"preferred":false,"id":195547,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27289,"text":"wri874167 - 1987 - Application of National Stream Quality Accounting Network (NASQAN) station data for assessing water quality in the Peace River basin, Florida","interactions":[],"lastModifiedDate":"2022-02-10T22:22:54.990951","indexId":"wri874167","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4167","title":"Application of National Stream Quality Accounting Network (NASQAN) station data for assessing water quality in the Peace River basin, Florida","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri874167","usgsCitation":"German, E.R., and Schiffer, D., 1987, Application of National Stream Quality Accounting Network (NASQAN) station data for assessing water quality in the Peace River basin, Florida: U.S. Geological Survey Water-Resources Investigations Report 87-4167, vii, 73 p., https://doi.org/10.3133/wri874167.","productDescription":"vii, 73 p.","costCenters":[],"links":[{"id":395826,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_46825.htm"},{"id":56171,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4167/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120054,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4167/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Peace River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.99920654296875,\n              27.18379900243671\n            ],\n            [\n              -81.6448974609375,\n              27.18379900243671\n            ],\n            [\n              -81.6448974609375,\n              28.22455005047019\n            ],\n            [\n              -81.99920654296875,\n              28.22455005047019\n            ],\n            [\n              -81.99920654296875,\n              27.18379900243671\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a914","contributors":{"authors":[{"text":"German, E. R.","contributorId":86315,"corporation":false,"usgs":true,"family":"German","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":197858,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schiffer, D. M.","contributorId":102103,"corporation":false,"usgs":true,"family":"Schiffer","given":"D. M.","affiliations":[],"preferred":false,"id":197859,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2025,"text":"wsp2306 - 1987 - Application of the precipitation-runoff model in the Warrior coal field, Alabama","interactions":[{"subject":{"id":14452,"text":"ofr85678 - 1986 - Application of the precipitation-runoff model in the Warrior Coal Field, Alabama","indexId":"ofr85678","publicationYear":"1986","noYear":false,"title":"Application of the precipitation-runoff model in the Warrior Coal Field, Alabama"},"predicate":"SUPERSEDED_BY","object":{"id":2025,"text":"wsp2306 - 1987 - Application of the precipitation-runoff model in the Warrior coal field, Alabama","indexId":"wsp2306","publicationYear":"1987","noYear":false,"title":"Application of the precipitation-runoff model in the Warrior coal field, Alabama"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:19","indexId":"wsp2306","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2306","title":"Application of the precipitation-runoff model in the Warrior coal field, Alabama","docAbstract":"A deterministic precipitation-runoff model, the Precipitation-Runoff Modeling System, was applied in two small basins located in the Warrior coal field, Alabama. Each basin has distinct geologic, hydrologic, and land-use characteristics. Bear Creek basin (15.03 square miles) is undisturbed, is underlain almost entirely by consolidated coal-bearing rocks of Pennsylvanian age (Pottsville Formation), and is drained by an intermittent stream. Turkey Creek basin (6.08 square miles) contains a surface coal mine and is underlain by both the Pottsville Formation and unconsolidated clay, sand, and gravel deposits of Cretaceous age (Coker Formation). Aquifers in the Coker Formation sustain flow through extended rainless periods. \r\n\r\nPreliminary daily and storm calibrations were developed for each basin. Initial parameter and variable values were determined according to techniques recommended in the user's manual for the modeling system and through field reconnaissance. Parameters with meaningful sensitivity were identified and adjusted to match hydrograph shapes and to compute realistic water year budgets. When the developed calibrations were applied to data exclusive of the calibration period as a verification exercise, results were comparable to those for the calibration period. \r\n\r\nThe model calibrations included preliminary parameter values for the various categories of geology and land use in each basin. The parameter values for areas underlain by the Pottsville Formation in the Bear Creek basin were transferred directly to similar areas in the Turkey Creek basin, and these parameter values were held constant throughout the model calibration. Parameter values for all geologic and land-use categories addressed in the two calibrations can probably be used in ungaged basins where similar conditions exist. The parameter transfer worked well, as a good calibration was obtained for Turkey Creek basin.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2306","usgsCitation":"Kidd, R.E., and Bossong, C., 1987, Application of the precipitation-runoff model in the Warrior coal field, Alabama: U.S. Geological Survey Water Supply Paper 2306, v, 42 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2306.","productDescription":"v, 42 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":137627,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2306/report-thumb.jpg"},{"id":27494,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2306/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a5e3","contributors":{"authors":[{"text":"Kidd, Robert E.","contributorId":21523,"corporation":false,"usgs":true,"family":"Kidd","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":144546,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bossong, C. R.","contributorId":39762,"corporation":false,"usgs":true,"family":"Bossong","given":"C. R.","affiliations":[],"preferred":false,"id":144547,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":48980,"text":"ofr87300B - 1987 - Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska, February 1987","interactions":[],"lastModifiedDate":"2012-02-02T00:10:41","indexId":"ofr87300B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-300","chapter":"B","title":"Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska, February 1987","language":"ENGLISH","doi":"10.3133/ofr87300B","usgsCitation":"Townshend, J.B., O’Connell, R.V., and Torrence, L., 1987, Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska, February 1987: U.S. Geological Survey Open-File Report 87-300, 17 p. ill., map ; 28 cm., https://doi.org/10.3133/ofr87300B.","productDescription":"17 p. ill., map ; 28 cm.","costCenters":[],"links":[{"id":171561,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0300b/report-thumb.jpg"},{"id":21239,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0300b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db673db7","contributors":{"authors":[{"text":"Townshend, John B.","contributorId":70383,"corporation":false,"usgs":true,"family":"Townshend","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":238765,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Connell, R. V.","contributorId":88755,"corporation":false,"usgs":true,"family":"O’Connell","given":"R.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":238766,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Torrence, L.Y.","contributorId":62587,"corporation":false,"usgs":true,"family":"Torrence","given":"L.Y.","email":"","affiliations":[],"preferred":false,"id":238764,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}