A water-quality reconnaissance study of the Big Bear Lake area in southern California was made by the U.S. Geological Survey from April 1972 through April 1973. The primary purpose of the study was to measure the concentration and distribution of selected primary nutrients, organic carbon, dissolved oxygen, phytoplankton, and water temperature in the lake. Estimates of the nitrogen, phosphorus, and silica loading to the lake from surface-water tributaries and precipitation were also made.
Results of the study indicate that Big Bear Lake is moderately eutrophic, at least in regard to nitrogen, phosphorus, and organic content. Nitrate was found in either trace concentrations or below detectable limits; however, ammonia nitrogen was usually detected in concentrations greater than 0.05 milligrams per liter. Orthophosphate phosphorus was detected in mean concentrations ranging from 0.01 to 0.05 milligrams per liter. Organic nitrogen and phosphorus were also detected in measurable concentrations.
Seasonal levels of dissolved oxygen indicated that the nutrients and other controlling factors were optimum for relatively high primary productivity. However, production varied both seasonally and areally in the lake. Primary productivity seemed highest in the eastern and middle parts of the lake. The middle and western parts of the lake exhibited severe oxygen deficits in the deeper water during the warmer summer months of June and July 1972.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri743","usgsCitation":"Irwin, G.A., and Lemons, M., 1974, A water-quality reconnaissance of Big Bear Lake, San Bernardino County, California, 1972-1973: U.S. Geological Survey Water-Resources Investigations Report 74-3, v, 40 p., https://doi.org/10.3133/wri743.","productDescription":"v, 40 p.","costCenters":[],"links":[{"id":158611,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1974/0003/report-thumb.jpg"},{"id":358908,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1974/0003/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"San Bernardino County","otherGeospatial":"Big Bear Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117.00714111328125,\n 34.214357361365884\n ],\n [\n -116.8234634399414,\n 34.214357361365884\n ],\n [\n -116.8234634399414,\n 34.29636658456932\n ],\n [\n -117.00714111328125,\n 34.29636658456932\n ],\n [\n -117.00714111328125,\n 34.214357361365884\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d87","contributors":{"authors":[{"text":"Irwin, George A.","contributorId":35363,"corporation":false,"usgs":true,"family":"Irwin","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":198777,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lemons, Michael","contributorId":24390,"corporation":false,"usgs":true,"family":"Lemons","given":"Michael","email":"","affiliations":[],"preferred":false,"id":198776,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":63295,"text":"gq1179 - 1974 - Geologic map of the Livingston quadrangle, southeastern Kentucky","interactions":[{"subject":{"id":50749,"text":"ofr7538 - 1975 - Preliminary Geologic Map Of The Livingston Quadrangle, Southeastern Kentucky","indexId":"ofr7538","publicationYear":"1975","noYear":false,"title":"Preliminary Geologic Map Of The Livingston Quadrangle, Southeastern Kentucky"},"predicate":"SUPERSEDED_BY","object":{"id":63295,"text":"gq1179 - 1974 - Geologic map of the Livingston quadrangle, southeastern Kentucky","indexId":"gq1179","publicationYear":"1974","noYear":false,"title":"Geologic map of the Livingston quadrangle, southeastern Kentucky"},"id":1}],"lastModifiedDate":"2012-02-10T00:11:00","indexId":"gq1179","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1179","title":"Geologic map of the Livingston quadrangle, southeastern Kentucky","language":"ENGLISH","doi":"10.3133/gq1179","usgsCitation":"Brown, W.R., and Osolnik, M., 1974, Geologic map of the Livingston quadrangle, southeastern Kentucky: U.S. Geological Survey Geologic Quadrangle 1179, 1 map., https://doi.org/10.3133/gq1179.","productDescription":"1 map.","costCenters":[],"links":[{"id":107610,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10718.htm","linkFileType":{"id":5,"text":"html"},"description":"10718"},{"id":249399,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1179/report.pdf","size":"39","linkFileType":{"id":1,"text":"pdf"}},{"id":252798,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1179/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.25,37.25 ], [ -84.25,37.3675 ], [ -84.11749999999999,37.3675 ], [ -84.11749999999999,37.25 ], [ -84.25,37.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696e0a","contributors":{"authors":[{"text":"Brown, William Randall","contributorId":34984,"corporation":false,"usgs":true,"family":"Brown","given":"William","email":"","middleInitial":"Randall","affiliations":[],"preferred":false,"id":268626,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Osolnik, M.J.","contributorId":85662,"corporation":false,"usgs":true,"family":"Osolnik","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":268627,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":65023,"text":"i917A - 1974 - Oil and gas data from the upper Paleozoic rocks in the Appalachian basin","interactions":[],"lastModifiedDate":"2012-02-10T00:11:10","indexId":"i917A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"917","subseriesTitle":"NONE","chapter":"A","title":"Oil and gas data from the upper Paleozoic rocks in the Appalachian basin","language":"ENGLISH","doi":"10.3133/i917A","usgsCitation":"De Witt, W., 1974, Oil and gas data from the upper Paleozoic rocks in the Appalachian basin: U.S. Geological Survey IMAP 917, 6 maps :col ;45 x 81 cm. on 4 sheets fold. in envelope 30 x 24 cm., https://doi.org/10.3133/i917A.","productDescription":"6 maps :col ;45 x 81 cm. on 4 sheets fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107050,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9807.htm","linkFileType":{"id":5,"text":"html"},"description":"9807"},{"id":189878,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"2500000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90,32 ], [ -90,44 ], [ -74,44 ], [ -74,32 ], [ -90,32 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691e44","contributors":{"authors":[{"text":"De Witt, Wallace Jr.","contributorId":87521,"corporation":false,"usgs":true,"family":"De Witt","given":"Wallace","suffix":"Jr.","affiliations":[],"preferred":false,"id":272527,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28391,"text":"wri746 - 1974 - Movement and dispersion of soluble materials in Salem Creek, Muddy Creek, and Yadkin River between Winston-Salem and Salisbury, North Carolina","interactions":[],"lastModifiedDate":"2018-11-16T09:55:04","indexId":"wri746","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-6","title":"Movement and dispersion of soluble materials in Salem Creek, Muddy Creek, and Yadkin River between Winston-Salem and Salisbury, North Carolina","docAbstract":"Wastes entering the Yadkin River from the Winston-Salem area, particularly during heavy rains, resulted in several major fish kills in the late 1960's and early 1970's. The actions undertaken to solve this problem, included the collection of data on the time of travel and dispersion characteristics of the tributaries draining the Winston-Salem area and of the main stem of the Yadkin below their confluence.
Fluorescent dye was used to simulate the movement of waterborne wastes under four different flow conditions over a reach of about 41 miles (66 kilometers) beginning at the sewage-treatment plant on Salem Creek and ending on the Yadkin River at High Rock Lake near Salisbury. Total travel time for the entire reach ranges from about 28 hours during periods of high streamflow to about 47 hours during periods of low flow. A soluble substance released as a slug at the sewage-treatment plant disperses longitudinally and laterally as it moves downstream. Longitudinal dispersion, expressed as the time required for a substance released as a slug at the sewage-treatment plant to pass a downstream point, ranges from about 8 hours at the upper end of High Rock Lake during periods of high flow to about 15 hours during periods of low flow. The rate of lateral dispersion also depends on the rate of flow of the Yadkin. During high-flow conditions wastes entering the Yadkin from Winston-Salem disperse across the river in a few miles. Under low-flow conditions lateral dispersion is still incomplete more than 10 miles (16 kilometers) downstream.
Longitudinal dispersion casues the maximum concentrations resulting from slug injections to decrease significantly as the traveltime increases. A relation is presented so the maximum concentration can be estimated at any location downstream from a point of injection at flow rates between about 80 and 500 cubic feet per second (2 and 14 cubic meters per second) at the Muddy Creek gaging station and between about 1,500 and 10,000 cubic feet per second (42 and 280 cubic meters per second) at the Yadkin College gaging station.
Water entering the Yadkin River from Muddy Creek during low-flow periods does not completely disperse laterally for more than 10 miles (16 kilometers) below the confluence, but, when the Yadkin River discharge is above 5,000 cubic feet per second (140 cubic meters per second), lateral mixing is complete within a few miles below the confluence.
","language":"English","publisher":"U. S. Geological Survey","doi":"10.3133/wri746","usgsCitation":"Lindskov, K., 1974, Movement and dispersion of soluble materials in Salem Creek, Muddy Creek, and Yadkin River between Winston-Salem and Salisbury, North Carolina: U.S. Geological Survey Water-Resources Investigations Report 74-6, iv, 26 p., https://doi.org/10.3133/wri746.","productDescription":"iv, 26 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":359496,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1974/0006/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159381,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1974/0006/report-thumb.jpg"}],"country":"United States","state":"North Carolina","city":"Salisburg, Winston-Salem","otherGeospatial":"Muddy Creek, Salem Creek, Yadkin River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.1667,\n 35.70693497582502\n ],\n [\n -80.1667,\n 36\n ],\n [\n -80.5,\n 36\n ],\n [\n -80.5,\n 35.70693497582502\n ],\n [\n -80.1667,\n 35.70693497582502\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4802","contributors":{"authors":[{"text":"Lindskov, K.L.","contributorId":91077,"corporation":false,"usgs":true,"family":"Lindskov","given":"K.L.","affiliations":[],"preferred":false,"id":199719,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":65139,"text":"i787E - 1974 - Slope-stability map of Anchorage and vicinity, Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:11:05","indexId":"i787E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"787","subseriesTitle":"NONE","chapter":"E","title":"Slope-stability map of Anchorage and vicinity, Alaska","language":"ENGLISH","doi":"10.3133/i787E","usgsCitation":"Schmoll, H., 1974, Slope-stability map of Anchorage and vicinity, Alaska: U.S. Geological Survey IMAP 787, 1 map :col. ;124 x 102 cm. fold. in envelope 30 x 24 cm., https://doi.org/10.3133/i787E.","productDescription":"1 map :col. ;124 x 102 cm. fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":106972,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9617.htm","linkFileType":{"id":5,"text":"html"},"description":"9617"},{"id":189308,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -150.08333333333334,61.06666666666667 ], [ -150.08333333333334,61.333333333333336 ], [ -149.6175,61.333333333333336 ], [ -149.6175,61.06666666666667 ], [ -150.08333333333334,61.06666666666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f0e4b07f02db5ee149","contributors":{"authors":[{"text":"Schmoll, H. R.","contributorId":71543,"corporation":false,"usgs":true,"family":"Schmoll","given":"H. R.","affiliations":[],"preferred":false,"id":272714,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":56701,"text":"wdrUT732 - 1974 - Water resources data for Utah, water year 1973; Part 2: Water quality records","interactions":[],"lastModifiedDate":"2020-11-17T21:09:28.079759","indexId":"wdrUT732","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"UT-73-2","title":"Water resources data for Utah, water year 1973; Part 2: Water quality records","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrUT732","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Water resources data for Utah, water year 1973; Part 2: Water quality records: U.S. Geological Survey Water Data Report UT-73-2, viii, 138 p., https://doi.org/10.3133/wdrUT732.","productDescription":"viii, 138 p.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":380557,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1973/ut-73-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":184233,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1973/ut-73-2/report-thumb.jpg"},{"id":334759,"rank":2,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/wdrUT731","text":"Part 1 of this Report (Surface water records)"}],"country":"United 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Jr.","contributorId":102952,"corporation":false,"usgs":true,"family":"Wood","given":"G.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":276191,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27916,"text":"wri744 - 1974 - Availability of ground water in the Blackstone River area Rhode Island and Massachusetts","interactions":[],"lastModifiedDate":"2013-12-13T15:44:16","indexId":"wri744","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-4","title":"Availability of ground water in the Blackstone River area Rhode Island and Massachusetts","docAbstract":"The Blackstone River study area covers 83 square miles of northern Rhode Island and 5 square miles of adjacent Massachusetts (fig. 1). It includes parts of the Blackstone, Moshassuck, and Tenmile River basins, and a coastal area that drains to the brackish Seekonk and Providence Rivers. In Rhode Island, all or parts of the suburban towns of Cumberland, Lincoln, North Smithfield, and Smithfield and all or parts of the cities of Central Falls, East Povidence, Pawtucket, Providence, and Woonsocket are within the study area. Also included are parts of the towns Attleboro and North Attleborough in Massachusetts. In 1970, total population was about 240,000, which was equivalent to about one-fourth of the total population of Rhode Island. Fresh water usage in 1970 by public-supply systems and self-supplied industry was about 33 mgd (million gallons per day), which was equal to 22 percent of total fresh water use in Rhode Island for all purposes except generation of electric power (fig. 2). Anticipated increases in population and per capita water requirements are likely to cause the demand for water to more than double within the next 50 years. A significant part of this demand can be met from wells that tap the principal streams. This aquifer yielded an average of 10 mgd in 1970 and is capable of sustaining a much higher yield. The primary objectives of the study were to determine and map the saturated thickness and transmissivity of the stratified-drift aquifer and to assess the potential sustained yield of those parts of the aquifer favorable for large-scale development of water. A secondary objective was to describe ground-water quality and to evaluate the impact of induced infiltration of polluted stream water on the quality of native ground water. This report is based on analysis of drillers' records of more than 700 wells and borings which include 462 lithologic logs; 35 specific-capacity determinations; 12 aquifer tests, including detailed tests at two sites to determine streambed infiltration rates; chemical analyses of 92 ground-water and 15 stream-water samples; and geologic mapping. Selected base data are published in a separate (Johnston and Dickerman, in press). The authors are indebted to well drillers, especially American Drilling and Boring Company, R.E. Chapman Company, and Layne New England Company, for making their records available; to the water departments of the towns of Cumberland and Lincoln, for allowing aquifer tests of their well fields; to the Rhode Island Department of Health, for providing data on water quality and use; and to many other federal, state, and municipal agencies, companies, and individuals who supplied information. Their contributions are gratefully acknowledged.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri744","collaboration":"Prepared in cooperation with Rhode Island Water Resources Board","usgsCitation":"Johnston, H.E., and Dickerman, D.C., 1974, Availability of ground water in the Blackstone River area Rhode Island and Massachusetts: U.S. Geological Survey Water-Resources Investigations Report 74-4, 2 Plates: 41.74 x 50.88 and 41.40 x 50.46 inches, https://doi.org/10.3133/wri744.","productDescription":"2 Plates: 41.74 x 50.88 and 41.40 x 50.46 inches","costCenters":[],"links":[{"id":158655,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1974/0004/report-thumb.jpg"},{"id":279495,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0004/plate-2.pdf"},{"id":279494,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0004/plate-1.pdf"}],"country":"United States","state":"Massachusetts;Rhode Island","otherGeospatial":"Blackstone River Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.566667,41.75 ], [ -71.566667,42.0 ], [ -71.333333,42.0 ], [ -71.333333,41.75 ], [ -71.566667,41.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db660474","contributors":{"authors":[{"text":"Johnston, Herbert E.","contributorId":16392,"corporation":false,"usgs":true,"family":"Johnston","given":"Herbert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":198894,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dickerman, David C.","contributorId":41047,"corporation":false,"usgs":true,"family":"Dickerman","given":"David","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":198895,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":63484,"text":"gp897 - 1974 - Aeromagnetic map of Connecticut","interactions":[],"lastModifiedDate":"2025-07-16T20:37:50.517861","indexId":"gp897","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"897","title":"Aeromagnetic map of Connecticut","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp897","usgsCitation":"Zietz, I., Kirby, J., and Gilbert, F.P., 1974, Aeromagnetic map of Connecticut: U.S. Geological Survey Geophysical Investigations Map 897, 1 Plate: 54.43 x 40.73 inches, https://doi.org/10.3133/gp897.","productDescription":"1 Plate: 54.43 x 40.73 inches","costCenters":[],"links":[{"id":249589,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0897/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":492372,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6245.htm","linkFileType":{"id":5,"text":"html"}},{"id":253131,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0897/report-thumb.jpg"},{"id":249590,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0897/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698306","contributors":{"authors":[{"text":"Zietz, Isidore","contributorId":76708,"corporation":false,"usgs":true,"family":"Zietz","given":"Isidore","affiliations":[],"preferred":false,"id":268958,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kirby, J.R.","contributorId":6428,"corporation":false,"usgs":true,"family":"Kirby","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":268956,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gilbert, F. P.","contributorId":53033,"corporation":false,"usgs":true,"family":"Gilbert","given":"F.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":268957,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":26655,"text":"wri7410 - 1974 - Water quality in Rhode River at Smithsonian Institution Pier near Annapolis, Maryland, April 1970 through December 1973","interactions":[],"lastModifiedDate":"2018-10-30T09:47:14","indexId":"wri7410","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-10","title":"Water quality in Rhode River at Smithsonian Institution Pier near Annapolis, Maryland, April 1970 through December 1973","docAbstract":"Water temperature, salinity (computed from specific conductance data), turbidity, dissolved oxygen, pH, and water level data were collected by a continuously recording water quality monitor located in the Rhode River, at the Smithsonian Institution's pier near Annapolis, Md., from April 1970 through December 1973. Data, as presented in this report, consist of daily maximum and minimum values summarized by week to give weekly averages and extremes.
Temperatures showed an overall range from 0.7 to 32.6°C. The water temperature data indicate successively warmer winters. Salinity ranged from
1.05 to 14.03 parts per thousand. In June 1972, salinity dropped markedly as fresh water from tropical storm Agnes entered the Rhode River from Chesapeake Bay. Most of the fresh water entering upper Chesapeake Bay as a result of tropical storm Agnes came from the Susquehanna River. Turbidity was usually low, averaging about 14 Jackson Turbidity Units; however, during spring and early summer of 1972, values averaged about 23 Jackson Turbidity Units. This increase in turbidity was due to the high Susquehanna River flows during that period. Extremes of turbidity ranged from about 5 to 80 Jackson Turbidity Units.
Dissolved oxygen ranged from 0.0 to 19.8 milligrams per litre. Large daily changes in oxygen indicated a high state of biological metabolism. Values of pH ranged from 6.8 to 10.1 and daily changes coincided with oxygen changes. Tide-dominated water levels had an overall range of 5.9 feet (1.8 metres) and a mean tidal range of 1.5 feet (0.46 metres).
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7410","usgsCitation":"Cory, R.L., Redding, J.M., and McCullough, M.M., 1974, Water quality in Rhode River at Smithsonian Institution Pier near Annapolis, Maryland, April 1970 through December 1973: U.S. Geological Survey Water-Resources Investigations Report 74-10, v, 67 p., https://doi.org/10.3133/wri7410.","productDescription":"v, 67 p.","costCenters":[],"links":[{"id":358931,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1974/0010/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158202,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1974/0010/report-thumb.jpg"}],"country":"United States","state":"Maryland","otherGeospatial":"Rhode River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76.55,\n 38.8583\n ],\n [\n -76.5083,\n 38.8583\n ],\n [\n -76.5083,\n 38.9\n ],\n [\n -76.55,\n 38.9\n ],\n [\n -76.55,\n 38.8583\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9afa","contributors":{"authors":[{"text":"Cory, Robert L.","contributorId":77967,"corporation":false,"usgs":true,"family":"Cory","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":196783,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Redding, J. Michael","contributorId":100028,"corporation":false,"usgs":true,"family":"Redding","given":"J.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":196785,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McCullough, Martha M.","contributorId":81530,"corporation":false,"usgs":true,"family":"McCullough","given":"Martha","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":196784,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":28266,"text":"wri7361 - 1974 - Water-resources data collected in the Devils Hole area, Nevada, 1972-1973","interactions":[],"lastModifiedDate":"2019-07-16T08:37:36","indexId":"wri7361","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"73-61","title":"Water-resources data collected in the Devils Hole area, Nevada, 1972-1973","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7361","usgsCitation":"Larson, J.D., 1974, Water-resources data collected in the Devils Hole area, Nevada, 1972-1973: U.S. Geological Survey Water-Resources Investigations Report 73-61, v, 14 p. , https://doi.org/10.3133/wri7361.","productDescription":"v, 14 p. ","costCenters":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"links":[{"id":159591,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1973/0061/report-thumb.jpg"},{"id":365554,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1973/0061/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","otherGeospatial":"Devils Hole area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.29577636718749,\n 36.42418314739194\n ],\n [\n -116.28908157348633,\n 36.42418314739194\n ],\n [\n -116.28908157348633,\n 36.429707997599614\n ],\n [\n -116.29577636718749,\n 36.429707997599614\n ],\n [\n -116.29577636718749,\n 36.42418314739194\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4f5e","contributors":{"authors":[{"text":"Larson, J. D.","contributorId":83084,"corporation":false,"usgs":true,"family":"Larson","given":"J.","middleInitial":"D.","affiliations":[],"preferred":false,"id":199497,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":66278,"text":"i823 - 1974 - Geologic map of the Schickard Quadrangle of the Moon","interactions":[{"subject":{"id":42477,"text":"ofr71169 - 1971 - Preliminary geologic map of the Schickard Quadrangle of the Moon","indexId":"ofr71169","publicationYear":"1971","noYear":false,"title":"Preliminary geologic map of the Schickard Quadrangle of the Moon"},"predicate":"SUPERSEDED_BY","object":{"id":66278,"text":"i823 - 1974 - Geologic map of the Schickard Quadrangle of the Moon","indexId":"i823","publicationYear":"1974","noYear":false,"title":"Geologic map of the Schickard Quadrangle of the Moon"},"id":1}],"lastModifiedDate":"2023-03-15T11:05:32.318618","indexId":"i823","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"823","subseriesTitle":"MOON","title":"Geologic map of the Schickard Quadrangle of the Moon","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i823","usgsCitation":"Karlstrom, T., 1974, Geologic map of the Schickard Quadrangle of the Moon: U.S. Geological Survey IMAP 823, 1 Plate: 72.00 × 37.33 inches, https://doi.org/10.3133/i823.","productDescription":"1 Plate: 72.00 × 37.33 inches","costCenters":[],"links":[{"id":439017,"rank":4,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9D80L8Y","text":"USGS data release","linkHelpText":"Geologic map of the Schickard Quadrangle of the Moon"},{"id":439016,"rank":4,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9POVMSJ","text":"USGS data release","linkHelpText":"Interactive Map: USGS IMAP 823 Geologic Map of the Schickard Quadrangle of the Moon"},{"id":189819,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414195,"rank":3,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://doi.org/10.5066/P9POVMSJ","text":"Interactive map","linkHelpText":"- Geologic Map of the Schickard Quadrangle of the Moon, 1:1M. Karlstrom (1974)"},{"id":101333,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0823/plate-1.pdf","size":"8549","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae7e4b07f02db68bc58","contributors":{"authors":[{"text":"Karlstrom, T. N. V.","contributorId":84846,"corporation":false,"usgs":true,"family":"Karlstrom","given":"T. N. V.","affiliations":[],"preferred":false,"id":274287,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":66679,"text":"i795 - 1974 - Bedrock topography and thickness of Pleistocene deposits in Union County and adjacent areas, New Jersey","interactions":[],"lastModifiedDate":"2022-11-21T12:56:07.976527","indexId":"i795","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"795","subseriesTitle":"NONE","title":"Bedrock topography and thickness of Pleistocene deposits in Union County and adjacent areas, New Jersey","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i795","usgsCitation":"Nemickas, B., 1974, Bedrock topography and thickness of Pleistocene deposits in Union County and adjacent areas, New Jersey: U.S. Geological Survey IMAP 795, 2 Plates: 72.33 × 48.94 inches and 67.33 × 48.11 inches, https://doi.org/10.3133/i795.","productDescription":"2 Plates: 72.33 × 48.94 inches and 67.33 × 48.11 inches","costCenters":[],"links":[{"id":256048,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0795/plate-2.pdf","size":"19964","linkFileType":{"id":1,"text":"pdf"}},{"id":256047,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0795/plate-1.pdf","size":"23160","linkFileType":{"id":1,"text":"pdf"}},{"id":255414,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0795/report-thumb.jpg"},{"id":255413,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0795/report.pdf","size":"27","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"New Jersey","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -74.2730,\n 40.45\n ],\n [\n -74.2730,\n 40.35\n ],\n [\n -74.0730,\n 40.35\n ],\n [\n -74.0730,\n 40.45\n ],\n [\n -74.2730,\n 40.45\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c4a6","contributors":{"authors":[{"text":"Nemickas, Bronius","contributorId":105733,"corporation":false,"usgs":true,"family":"Nemickas","given":"Bronius","email":"","affiliations":[],"preferred":false,"id":274905,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":67138,"text":"i859 - 1974 - Map showing bedrock topography and subcrop of a selected bed beneath alluvial deposits of part of the Wilson Quadrangle, Henderson County, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:11:16","indexId":"i859","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"859","subseriesTitle":"NONE","title":"Map showing bedrock topography and subcrop of a selected bed beneath alluvial deposits of part of the Wilson Quadrangle, Henderson County, Kentucky","language":"ENGLISH","doi":"10.3133/i859","usgsCitation":"Smith, A.E., and Ball, T., 1974, Map showing bedrock topography and subcrop of a selected bed beneath alluvial deposits of part of the Wilson Quadrangle, Henderson County, Kentucky: U.S. Geological Survey IMAP 859, 1 map., https://doi.org/10.3133/i859.","productDescription":"1 map.","costCenters":[],"links":[{"id":256476,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0859/plate-1.pdf","size":"7598","linkFileType":{"id":1,"text":"pdf"}},{"id":256477,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0859/report.pdf","size":"39","linkFileType":{"id":1,"text":"pdf"}},{"id":256478,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0859/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.75,37.75 ], [ -87.75,37.8675 ], [ -87.61749999999999,37.8675 ], [ -87.61749999999999,37.75 ], [ -87.75,37.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a95e4b07f02db659909","contributors":{"authors":[{"text":"Smith, A. E.","contributorId":58254,"corporation":false,"usgs":true,"family":"Smith","given":"A.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":275660,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ball, T.E.","contributorId":105378,"corporation":false,"usgs":true,"family":"Ball","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":275661,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28219,"text":"wri7436 - 1974 - Chemical and biological quality of Lake Dicie at Eustis, Florida, with emphasis on the effects of storm runoff","interactions":[],"lastModifiedDate":"2018-11-02T10:25:08","indexId":"wri7436","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-36","title":"Chemical and biological quality of Lake Dicie at Eustis, Florida, with emphasis on the effects of storm runoff","docAbstract":"After the construction of a storm drain designed to carry runoff from the southeastern part of the city of Eustis into Lake Dicie, algal blooms occurred in the lake. In order to determine the nature and extent of these blooms, the quality of both the lake and storm runoff into the lake was monitored from March 1971 through June 1973.
Surface runoff makes up about 65 percent of the total input to the lake and the storm drain probably contributes about half of the total input. Average concentrations of the major ions in samples of storm runoff collected from the storm drain were not appreciably different from concentrations found in Lake Dicie. However, the storm runoff contained high concentrations of suspended sediment, nitrogen, phosphorus, lead and other trace elements.
Most of the sediment and trace elements and much of the phosphorus carried into the lake by storm runoff were trapped in the bottom sediments. The only appreciable change in the quality of the lake since it was first sampled in 1969 is a reduction in the concentration of phosphorus.
The amount of inorganic nitrogen and soluble orthophosphate carried into the lake during this investigation was equivalent to about 3,500 pounds (1,600 kilograms) of 6-6-6 commercial fertilizer. Most of these nutrients were taken up by the large phytoplankton population and eventually incorporated into the bottom sediments in Lake Dicie.
During much of the year Lake Dicie is thermally stratified and the water near the bottom becomes enriched with nutrients, particularly nitrogen, from the decomposition of algal cells and other organic matter. In the winter months, the water cools and the lake slowly \"turns over.\" The mixing of the nitrogen-rich bottom water with the water in the upper part of the lake where the dissolved oxygen and light penetration are sufficient to support algae often results in explosive algal growth, commonly called a bloom. The two highest concentrations of phytoplankton observed in Lake Dicie during the investigation occurred in December when the lake was not stratified.
In Big Bass Lake, a control lake which receives no street runoff, the phytoplankton population is much smaller than in Lake Dicie. Variations in the concentration of phytoplankton appear to be more closely related to rainfall (the major source of nitrogen and phosphorus for Big Bass Lake) than to the seasonal turnover in the lake.
","language":"English","publisher":"U. S. Geological Survey","doi":"10.3133/wri7436","usgsCitation":"Lamonds, A.G., 1974, Chemical and biological quality of Lake Dicie at Eustis, Florida, with emphasis on the effects of storm runoff: U.S. Geological Survey Water-Resources Investigations Report 74-36, iv, 61 p., https://doi.org/10.3133/wri7436.","productDescription":"iv, 61 p.","costCenters":[],"links":[{"id":159398,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1974/0036/report-thumb.jpg"},{"id":359108,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1974/0036/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","otherGeospatial":"Lake Dicie, West Crooked Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.6857099533081,\n 28.82234230721012\n ],\n [\n -81.65777206420898,\n 28.82234230721012\n ],\n [\n -81.65777206420898,\n 28.839937123160688\n ],\n [\n -81.6857099533081,\n 28.839937123160688\n ],\n [\n -81.6857099533081,\n 28.82234230721012\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e48ea","contributors":{"authors":[{"text":"Lamonds, A. G.","contributorId":8450,"corporation":false,"usgs":true,"family":"Lamonds","given":"A.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":199413,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27917,"text":"wri7418 - 1974 - Availability of ground water in the Branch River basin; Providence County, Rhode Island","interactions":[],"lastModifiedDate":"2015-12-03T12:43:06","indexId":"wri7418","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-18","title":"Availability of ground water in the Branch River basin; Providence County, Rhode Island","docAbstract":"Stratified glacial drift consisting largely of sand and gravel constitutes the only aquifer capable of supporting continuous yields of 100 gpm (6.3 1/s) or more to individual wells. The aquifer covers about a third of the 79 mi 2 (205 km2) study area, occurring mainly in stream valleys that are less than a mi le wide. Its saturated thickness is commonly 40 to 60ft (12 to 18 m); its transmissivity is commonly 5,000 to 8,000 ft 2/day (460 to 740m2 /day). The aquifer is hydraulically connected to streams that cross it and much of the water from heavily pumped wells will consist of infiltration induced from them. Potential sustained yield from most parts of the aquifer is limited chiefly by the rate at which infiltration can be induced from streams or low streamflow, whichever is smaller. Ground-water withdrawals deplete streamflow; and if large-scale development of ground water is not carefully planned and managed, periods of no streamflow may result during dry weather. Potential sustained yield varies with the scheme of well development, and is evaluated for selected areas by mathematically simulating pumping from assumed schemes of well Is in models of the stream-aquifer system. Results indicate that sustained yields of 5.5, 3.4, 1.6, and 1.3 mgd (0.24, 0.15, 0.07, and 0.06 m3 /s) can be obtained from the stratified-drift aquifer near Slatersville, Oakland, Harrisville, and Chepachet, respectively. Pumping at these rates will not cause streams to go dry, if the water is returned to streams near points of withdrawal. A larger ground-water yield can be obtained, if periods of no streamflow along reaches of principal streams are acceptable. Inorganic chemical quality of water in the stream-aquifer system is suitable for most purposes; the water is soft, slightly acidic, and generally contains less than 100 milligrams per litre of dissolved sol ids. Continued good quality ground water depends on maintenance of good quality of water in streams, because much of the water pumped from wells will be infiltrated from streams.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7418","collaboration":"Prepared in cooperation with the Rhode Island Water Resources Board","usgsCitation":"Johnston, H., and Dickerman, D., 1974, Availability of ground water in the Branch River basin; Providence County, Rhode Island: U.S. Geological Survey Water-Resources Investigations Report 74-18, Report: v, 39 p.; 1 Plate: 34.54 x 39.14 inches, https://doi.org/10.3133/wri7418.","productDescription":"Report: v, 39 p.; 1 Plate: 34.54 x 39.14 inches","numberOfPages":"46","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":158656,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri7418.jpg"},{"id":311731,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1974/0018/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":311732,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0018/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Rhode Island","county":"Providence County","otherGeospatial":"Branch River","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-71.4983,42.0169],[-71.4266,42.0187],[-71.3797,42.0191],[-71.3806,41.985],[-71.3817,41.9427],[-71.3824,41.8915],[-71.3386,41.8983],[-71.3373,41.8937],[-71.3386,41.891],[-71.3398,41.8874],[-71.3392,41.8824],[-71.3368,41.8733],[-71.3356,41.8678],[-71.3337,41.861],[-71.3331,41.8574],[-71.3337,41.8538],[-71.3356,41.8497],[-71.3387,41.8429],[-71.3393,41.841],[-71.3387,41.8392],[-71.3381,41.8374],[-71.3369,41.8351],[-71.3369,41.8329],[-71.3387,41.8302],[-71.3406,41.8279],[-71.3437,41.8242],[-71.3437,41.8211],[-71.3443,41.8174],[-71.3425,41.8129],[-71.3406,41.8093],[-71.3406,41.8056],[-71.3406,41.8029],[-71.3406,41.7997],[-71.3394,41.797],[-71.3376,41.7952],[-71.3345,41.7925],[-71.3314,41.7897],[-71.3302,41.7865],[-71.329,41.7838],[-71.3271,41.7811],[-71.3259,41.7793],[-71.318,41.7759],[-71.3518,41.7534],[-71.3537,41.7502],[-71.3604,41.7493],[-71.3604,41.7566],[-71.3635,41.7625],[-71.3684,41.7638],[-71.3715,41.767],[-71.3672,41.7761],[-71.3696,41.7829],[-71.3727,41.7911],[-71.377,41.7993],[-71.3868,41.807],[-71.388,41.8083],[-71.3862,41.8147],[-71.3812,41.8224],[-71.3744,41.8324],[-71.3701,41.8401],[-71.3695,41.8474],[-71.3689,41.8533],[-71.375,41.8583],[-71.3806,41.8506],[-71.3812,41.8469],[-71.3824,41.8429],[-71.3825,41.8392],[-71.3855,41.8356],[-71.388,41.8306],[-71.393,41.8179],[-71.3966,41.8174],[-71.4028,41.8197],[-71.4047,41.8179],[-71.3985,41.8065],[-71.3967,41.8025],[-71.393,41.7997],[-71.3887,41.7984],[-71.3856,41.7952],[-71.3838,41.7929],[-71.3844,41.7902],[-71.3887,41.787],[-71.3893,41.782],[-71.3881,41.7752],[-71.3863,41.7689],[-71.385,41.7639],[-71.3857,41.7607],[-71.3881,41.7634],[-71.3924,41.7666],[-71.3979,41.7711],[-71.3998,41.7707],[-71.4016,41.768],[-71.409,41.7671],[-71.4146,41.7648],[-71.4177,41.7639],[-71.4207,41.7648],[-71.4244,41.7607],[-71.4306,41.7603],[-71.4343,41.7607],[-71.4373,41.7598],[-71.4392,41.7575],[-71.441,41.7539],[-71.4417,41.7525],[-71.4435,41.7516],[-71.446,41.7498],[-71.446,41.748],[-71.4447,41.7421],[-71.4472,41.7394],[-71.4521,41.7358],[-71.4583,41.7308],[-71.6102,41.7275],[-71.7904,41.7232],[-71.7937,41.8154],[-71.7963,41.9184],[-71.7968,41.9376],[-71.7971,41.9588],[-71.7979,42.0089],[-71.6681,42.0122],[-71.5588,42.0153],[-71.5366,42.0159],[-71.4983,42.0169]]]},\"properties\":{\"name\":\"Providence\",\"state\":\"RI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e241","contributors":{"authors":[{"text":"Johnston, H.E.","contributorId":27070,"corporation":false,"usgs":true,"family":"Johnston","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":198896,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dickerman, D.C.","contributorId":48601,"corporation":false,"usgs":true,"family":"Dickerman","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":198897,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}