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,{"id":14687,"text":"ofr86250 - 1986 - Hydrologic, lithologic, and chemical data for sediment in the shallow alluvial aquifer at two sites near Fallon, Churchill County, Nevada, 1984-85","interactions":[],"lastModifiedDate":"2012-02-02T00:07:07","indexId":"ofr86250","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-250","title":"Hydrologic, lithologic, and chemical data for sediment in the shallow alluvial aquifer at two sites near Fallon, Churchill County, Nevada, 1984-85","docAbstract":"The U.S. Geological Survey collected an extensive amount of hydrogeologic data from the shallow alluvial aquifer at two study sites near Fallon, Nevada, from 1984 though 1985. These data were collected as part of a study to determine the geochemical controls on the mobility of arsenic and other trace elements in shallow groundwater systems. The main study area is approximately 7 miles south of Fallon. A subsidiary study area is about 8 miles east of Fallon. The data collected include lithologic logs and water level altitudes for the augered sampling wells and piezometers, and determinations of arsenic and selenium content, grain size, porosity, hydraulic conductivity, and mineralogy for sediment samples from cores. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86250","usgsCitation":"Lico, M., Welch, A., and Hughes, J.L., 1986, Hydrologic, lithologic, and chemical data for sediment in the shallow alluvial aquifer at two sites near Fallon, Churchill County, Nevada, 1984-85: U.S. Geological Survey Open-File Report 86-250, v, 43 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr86250.","productDescription":"v, 43 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":148365,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0250/report-thumb.jpg"},{"id":43453,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0250/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db605250","contributors":{"authors":[{"text":"Lico, M.S.","contributorId":36573,"corporation":false,"usgs":true,"family":"Lico","given":"M.S.","affiliations":[],"preferred":false,"id":169849,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Welch, A. H.","contributorId":14836,"corporation":false,"usgs":true,"family":"Welch","given":"A. H.","affiliations":[],"preferred":false,"id":169847,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hughes, J. L.","contributorId":34940,"corporation":false,"usgs":true,"family":"Hughes","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":169848,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":14691,"text":"ofr86452 - 1986 - Log for joint SEPM-Colorado Scientific Society field trip from Westcliffe to Crestone, Colorado, September 20-21, 1986; Late Paleozoic sedimentation and Laramide tectonics of the Sangre de Cristo Range","interactions":[{"subject":{"id":14691,"text":"ofr86452 - 1986 - Log for joint SEPM-Colorado Scientific Society field trip from Westcliffe to Crestone, Colorado, September 20-21, 1986; Late Paleozoic sedimentation and Laramide tectonics of the Sangre de Cristo Range","indexId":"ofr86452","publicationYear":"1986","noYear":false,"title":"Log for joint SEPM-Colorado Scientific Society field trip from Westcliffe to Crestone, Colorado, September 20-21, 1986; Late Paleozoic sedimentation and Laramide tectonics of the Sangre de Cristo Range"},"predicate":"SUPERSEDED_BY","object":{"id":31397,"text":"ofr01249 - 2001 - Log for Joint SEPM-Colorado Scientific Society field trip, September 20-21, 1986: Late Paleozoic sedimentation and Laramide tectonics of the 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,{"id":1712,"text":"wsp2269 - 1986 - Traveltime and longitudinal dispersion in Illinois streams","interactions":[{"subject":{"id":9201,"text":"ofr84468 - 1984 - Traveltime and longitudinal dispersion in Illinois streams","indexId":"ofr84468","publicationYear":"1984","noYear":false,"title":"Traveltime and longitudinal dispersion in Illinois streams"},"predicate":"SUPERSEDED_BY","object":{"id":1712,"text":"wsp2269 - 1986 - Traveltime and longitudinal dispersion in Illinois streams","indexId":"wsp2269","publicationYear":"1986","noYear":false,"title":"Traveltime and longitudinal dispersion in Illinois streams"},"id":1}],"lastModifiedDate":"2022-09-19T18:32:36.31144","indexId":"wsp2269","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"2269","title":"Traveltime and longitudinal dispersion in Illinois streams","docAbstract":"Twenty-seven measurements of traveltime and longitudinal dispersion in 10 Illinois streams made from 1975 to 1982 provide data needed for estimating traveltime of peak concentration of a conservative solute, traveltime of the leading edge of a solute cloud, peak concentration resulting from injection of a given quantity of solute, and passage time of solute past a given point on a stream. These four variables can be estimated graphically for each stream from distance of travel and either discharge at the downstream end of the reach or flow-duration frequency. From equations developed from field measurements, the traveltime and dispersion characteristics also can be estimated for other unregulated streams in Illinois that have drainage areas less than about 1,500 square miles. For unmeasured streams, traveltime of peak concentration and of the leading edge of the cloud are related to discharge at the downstream end of the reach and to distance of travel. For both measured and unmeasured streams, peak concentration and passage time are best estimated from the relation of each to traveltime. In measured streams, dispersion efficiency is greater than that predicted by Fickian diffusion theory. The rate of decrease in peak concentration with traveltime is about equal to the rate of increase in passage time. Average velocity in a stream reach, given by the velocity of the center of solute mass in that reach, can be estimated from an equation developed from measured values. The equation relates average reach velocity to discharge at the downstream end of the reach. Average reach velocities computed for 9 of the 10 streams from available equations that are based on hydraulic-geometry relations are high relative to measured values. The estimating equation developed from measured velocities provides estimates of average reach velocity that are closer to measured velocities than are those computed using equations developed from hydraulic-geometry relations.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2269","usgsCitation":"Graf, J.B., 1986, Traveltime and longitudinal dispersion in Illinois streams: U.S. Geological Survey Water Supply Paper 2269, vi, 65 p., https://doi.org/10.3133/wsp2269.","productDescription":"vi, 65 p.","costCenters":[],"links":[{"id":406991,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25457.htm","linkFileType":{"id":5,"text":"html"}},{"id":26788,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2269/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137198,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2269/report-thumb.jpg"}],"country":"United 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,{"id":27245,"text":"wri864153 - 1986 - Hydrogeology, ground-water flow, and tritium movement at low-level radioactive-waste disposal site near Sheffield, Illinois","interactions":[],"lastModifiedDate":"2023-01-05T21:29:02.151914","indexId":"wri864153","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4153","title":"Hydrogeology, ground-water flow, and tritium movement at low-level radioactive-waste disposal site near Sheffield, Illinois","docAbstract":"<p>Groundwater flow and tritium movement are described at and near a low-level radioactive waste disposal site near Sheffield, Illinois. Flow in the shallow aquifer is confined to three basins that ultimately drain into a stripmine lake. Most of the flow from the site is through a buried, pebbly sandfilled channel. Remaining flow is toward alluvium of an existing stream. Conceptual flow models for the two largest basins are used to improve definition of flow velocity and direction. Flow velocities range from about 25 to 2,500 ft/yr. Tritium was found in all three basins. The most extensive migration of tritium is coincident with buried channel. Tritium concentrations ranged from detection level to more than 300 nanocuries/L.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864153","usgsCitation":"Garklavs, G., and Healy, R.W., 1986, Hydrogeology, ground-water flow, and tritium movement at low-level radioactive-waste disposal site near Sheffield, Illinois: U.S. Geological Survey Water-Resources Investigations Report 86-4153, v, 35 p., https://doi.org/10.3133/wri864153.","productDescription":"v, 35 p.","costCenters":[],"links":[{"id":411452,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36580.htm","linkFileType":{"id":5,"text":"html"}},{"id":56108,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4153/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158749,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4153/report-thumb.jpg"}],"country":"United States","state":"Illinios","city":"Sheffield","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -89.796,\n              41.343\n            ],\n            [\n              -89.796,\n              41.3360\n            ],\n            [\n              -89.782,\n              41.3360\n            ],\n            [\n              -89.782,\n              41.343\n            ],\n            [\n              -89.796,\n              41.343\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db614875","contributors":{"authors":[{"text":"Garklavs, George","contributorId":87139,"corporation":false,"usgs":true,"family":"Garklavs","given":"George","email":"","affiliations":[],"preferred":false,"id":197789,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Healy, R. W.","contributorId":89872,"corporation":false,"usgs":true,"family":"Healy","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":197790,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4727,"text":"twri03A12 - 1986 - Fluorometric procedures for dye tracing","interactions":[{"subject":{"id":11690,"text":"ofr84234 - 1984 - Fluorometric procedures for dye tracing","indexId":"ofr84234","publicationYear":"1984","noYear":false,"title":"Fluorometric procedures for dye tracing"},"predicate":"SUPERSEDED_BY","object":{"id":4727,"text":"twri03A12 - 1986 - Fluorometric procedures for dye tracing","indexId":"twri03A12","publicationYear":"1986","noYear":false,"title":"Fluorometric procedures for dye tracing"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:32","indexId":"twri03A12","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"03-A12","title":"Fluorometric procedures for dye tracing","docAbstract":"This manual describes the current fluorometric procedures\r\nused by the U.S. Geological Survey in dye tracer studies such\r\nas time of travel, dispersion, reaeration, and dilution-type discharge\r\nmeasurements. The advantages of dye tracing are (1)\r\nlow detection and measurement limits and (2) simplicity and\r\naccuracy in measuring dye tracer concentrations using\r\nfluorometric techniques.\r\nThe manual contains necessary background information\r\nabout fluorescence, dyes, and fluorometers and a description\r\nof fluorometric operation and calibration procedures as a\r\nguide for laboratory and field use. The background information\r\nshould be useful to anyone wishing to experiment with\r\ndyes, fluorometer components, or procedures different from\r\nthose described. In addition, a brief section on aerial photography\r\nis included because of its possible use to supplement\r\nground-level fluorometry.","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;For sale by the Books and Open-File Reports Section, U.S. Geological Survey,","doi":"10.3133/twri03A12","issn":"0565-596X","usgsCitation":"Wilson, J.F., Cobb, E.D., and Kilpatrick, F.A., 1986, Fluorometric procedures for dye tracing (Revision - 1986): U.S. Geological Survey Techniques of Water-Resources Investigations 03-A12, x, 34 p. :ill ;26 cm., https://doi.org/10.3133/twri03A12.","productDescription":"x, 34 p. :ill ;26 cm.","costCenters":[],"links":[{"id":139108,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":355,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri3-a12/","linkFileType":{"id":5,"text":"html"}}],"edition":"Revision - 1986","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cce4b07f02db54411a","contributors":{"authors":[{"text":"Wilson, James F.","contributorId":84737,"corporation":false,"usgs":true,"family":"Wilson","given":"James","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":149692,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cobb, Ernest D.","contributorId":25139,"corporation":false,"usgs":true,"family":"Cobb","given":"Ernest","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":149691,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kilpatrick, F. A.","contributorId":22319,"corporation":false,"usgs":true,"family":"Kilpatrick","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":149690,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27242,"text":"wri854147 - 1986 - Water-quality characteristics and nutrient and suspended-sediment loads, Carson River and Truckee Canal, western Nevada, water year 1980","interactions":[],"lastModifiedDate":"2022-08-23T19:38:27.291403","indexId":"wri854147","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-4147","title":"Water-quality characteristics and nutrient and suspended-sediment loads, Carson River and Truckee Canal, western Nevada, water year 1980","docAbstract":"<p>Lahontan Reservoir is a major recreational site in the Carson River basin in western Nevada. The reservoir is fed by the Carson River and by the Truckee Canal which transports water from the adjacent Truckee River. Water quality in both rivers is influenced by agriculture and urbanization. Specific conductance tended to increase in a downstream direction. Generally, pH values ranged from 7.0 to 8.8. Dissolved-oxygen concentrations were greater than 5 milligrams/L. Calcium and sodium were the dominant cations and bicarbonate the dominant anion. Suspended-sediment concentrations ranged from 3 to 1,790 milligrams/L. Ultimate carbonaceous biochemical oxygen demand ranged from 1.2 to 19.6 milligrams/L. The codominant algal groups were the blue-greens, greens, and diatoms. Background total nutrient and suspended-sediment loads were about 490 tons nitrogen, 130 tons phosphorus, and 200,000 tons suspended sediment. Total nutrient and suspended-sediment loads to Lahontan Reservoir were about 980 tons nitrogen, 300 tons phosphorus, and 300,000 tons suspended sediment. Loads to the lower Carson River from the reservoir were about 820 tons total nitrogen, 180 tons total phosphorus, and 26,000 tons suspended sediment.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854147","usgsCitation":"Garcia, K.T., and Carman, R.L., 1986, Water-quality characteristics and nutrient and suspended-sediment loads, Carson River and Truckee Canal, western Nevada, water year 1980: U.S. Geological Survey Water-Resources Investigations Report 85-4147, vii, 107 p., https://doi.org/10.3133/wri854147.","productDescription":"vii, 107 p.","costCenters":[],"links":[{"id":405483,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36310.htm","linkFileType":{"id":5,"text":"html"}},{"id":56105,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4147/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158744,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4147/report-thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Carson River and Truckee Canal","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120,\n              38.717\n            ],\n            [\n              -119,\n              38.717\n            ],\n            [\n              -119,\n              39.6\n            ],\n            [\n              -120,\n              39.6\n            ],\n            [\n              -120,\n              38.717\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cce4b07f02db544586","contributors":{"authors":[{"text":"Garcia, K. T.","contributorId":52613,"corporation":false,"usgs":true,"family":"Garcia","given":"K.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":197784,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carman, R. L.","contributorId":16460,"corporation":false,"usgs":true,"family":"Carman","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":197783,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4412,"text":"cir979 - 1986 - Symposium proceedings; a national agenda for coal-quality research","interactions":[],"lastModifiedDate":"2018-09-19T17:47:41","indexId":"cir979","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"979","title":"Symposium proceedings; a national agenda for coal-quality research","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir979","usgsCitation":"Schweinfurth, S., 1986, Symposium proceedings; a national agenda for coal-quality research: U.S. Geological Survey Circular 979, vi, 334 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir979.","productDescription":"vi, 334 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":31517,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1986/0979/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117505,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1986/0979/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687ef4","contributors":{"editors":[{"text":"Garbini, Susan","contributorId":82287,"corporation":false,"usgs":true,"family":"Garbini","given":"Susan","affiliations":[],"preferred":false,"id":745666,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Schweinfurth, S. P.","contributorId":82288,"corporation":false,"usgs":true,"family":"Schweinfurth","given":"S. P.","affiliations":[],"preferred":false,"id":149072,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4403,"text":"cir971 - 1986 - Strong-motion program report, January-December 1983","interactions":[],"lastModifiedDate":"2018-10-22T19:38:24","indexId":"cir971","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"971","title":"Strong-motion program report, January-December 1983","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir971","usgsCitation":"1986, Strong-motion program report, January-December 1983: U.S. Geological Survey Circular 971, vi, 57 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir971.","productDescription":"vi, 57 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":31511,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1986/0971/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117501,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1986/0971/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4b59","contributors":{"editors":[{"text":"Porcella, R. L.","contributorId":102869,"corporation":false,"usgs":true,"family":"Porcella","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":749323,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":65298,"text":"i1785 - 1986 - Controlled photomosaic of part of the Apollinaris Patera Region of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:14","indexId":"i1785","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"1785","subseriesTitle":"NONE","title":"Controlled photomosaic of part of the Apollinaris Patera Region of Mars","language":"ENGLISH","doi":"10.3133/i1785","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, Controlled photomosaic of part of the Apollinaris Patera Region of Mars: U.S. Geological Survey IMAP 1785, 1 remote-sensing image ;63 x 52 cm., sheet 96 x 59 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1785.","productDescription":"1 remote-sensing image ;63 x 52 cm., sheet 96 x 59 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":188952,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100863,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1785/plate-1.pdf","size":"7727","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68abb6","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":533685,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27379,"text":"wri854319 - 1986 - Water quality in the St Croix National Scenic Riverway, Wisconsin","interactions":[],"lastModifiedDate":"2022-09-28T19:14:41.788527","indexId":"wri854319","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-4319","title":"Water quality in the St Croix National Scenic Riverway, Wisconsin","docAbstract":"<p>The U.S. Geological Survey conducted a water-quality study of the St. Croix National Scenic Riverway. This report documents the water quality during the period 1975-83. The water quality is good for most uses and is a calcium bicarbonate type. Concentrations of most constituents analyzed were less than most sites in Wisconsin. Constituent loads and yields were alsg lower in the Sceiilc Riverway than in other Wisconsin streams. Water-quality samples were collected at 10 stations throughout the study area and were compared to analyses of samples from selected National Stream Quality Accounting Network stations (NASQAN) and the Hydrologic Bench-Mark NetWork (HBMN) station in Wisconsin.</p>\n<p>The average suspended-sediment concentration for 9 of the 10 stations in this study was 7.7 milligrams per liter. This compared with an average suspended-sediment concentration of 11 milligrams per liter for two other stations in the scenic riverway and an average suspended-sediment concentration of 110 milligrams per liter for Wisconsin. Concentrations of major cations and anions were generally below concentrations at other stations in the State. The concentrations of major cations and anions at two of the stations were similar to concentrations at the HBMN station Popple River near Fence. Mean total phosphorus concentrations ranged from 0. 02 to 0. 08 milligram per liter at the study stations and from 0.03 to 0.16 milligram per liter at selected NASQAN stations. Concentrations of trace metals were below safe drinking water standards at all the study sites except for iron and manganese which exceeded drinking water standards at some of the study sites. Pesticides were sampled at the St. Croix River at St. Croix Falls and above and below cranberry bogs that drain into the Namekagon River. No pesticides were detected in the water/suspended-sediment mixture or bottom material.</p>\n<p>Average annual loads of suspended sediment, total phosphorus, total nitrogen, and dissolved solids were calculated by a flow-duration curve method. Annual suspended-sediment loads ranged from 580 to 25,000 tons per year at the study stations. Annual suspended-sediment loads at the HBMN station and NASQAN stations ranged from 720 tons at the Popple River near Fence to 443,000 tons at the Chippewa River near Durand. Average annual total phosphorus loads ranged from 6,800 to 900,000 pounds at the study stations compared with 145,000 to 1 ,600,000 pounds at selected Wisconsin NASQAN stations.</p>\n<p>Yields for suspended sediment, total phosphorus, total nitrogen, and dissolved solids at the study stations were consistently lower than at other stations in the State. Suspendedsediment yields ranged from 1.9 to 13.3 tons per square mile. The average suspended-sediment yield for Wisconsin is 80 tons per square mile. Total phosphorous and the other constituents exhibited the same trend.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854319","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Graczyk, D., 1986, Water quality in the St Croix National Scenic Riverway, Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 85-4319, iv, 48 p., https://doi.org/10.3133/wri854319.","productDescription":"iv, 48 p.","numberOfPages":"53","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":407536,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36449.htm","linkFileType":{"id":5,"text":"html"}},{"id":56239,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4319/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158980,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4319/report-thumb.jpg"}],"country":"United States","state":"Wisconsin, Minnesota","otherGeospatial":"St. Croix National Scenic Riverway","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.05419921875,\n              44.69989765840318\n            ],\n            [\n              -93.05419921875,\n              46.64189395892874\n            ],\n            [\n              -91.021728515625,\n              46.64189395892874\n            ],\n            [\n              -91.021728515625,\n              44.69989765840318\n            ],\n            [\n              -93.05419921875,\n              44.69989765840318\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9a3c","contributors":{"authors":[{"text":"Graczyk, D.J.","contributorId":108119,"corporation":false,"usgs":true,"family":"Graczyk","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":198012,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":34982,"text":"b1680 - 1986 - Geochemical reconnaissance of late Proterozoic volcanic and mafic plutonic rocks of the Al'Awshaziyah Quadrangle and related rocks in the Qufar Quadrangle, Northern Arabian Shield","interactions":[],"lastModifiedDate":"2012-02-02T00:09:49","indexId":"b1680","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1680","title":"Geochemical reconnaissance of late Proterozoic volcanic and mafic plutonic rocks of the Al'Awshaziyah Quadrangle and related rocks in the Qufar Quadrangle, Northern Arabian Shield","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1680","usgsCitation":"Leo, G.W., 1986, Geochemical reconnaissance of late Proterozoic volcanic and mafic plutonic rocks of the Al'Awshaziyah Quadrangle and related rocks in the Qufar Quadrangle, Northern Arabian Shield: U.S. Geological Survey Bulletin 1680, iii, 16 p. ill., maps ;28 cm., https://doi.org/10.3133/b1680.","productDescription":"iii, 16 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":165421,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1680/report-thumb.jpg"},{"id":62933,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1680/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ade82","contributors":{"authors":[{"text":"Leo, Gerhard W.","contributorId":26307,"corporation":false,"usgs":true,"family":"Leo","given":"Gerhard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":213930,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}