This report summarizes selected water-quality data collected in the Eel River, Calif., during a reconnaissance study from November 1971 through January 1975. It also includes a summary of the major inorganic chemical data collected near Dos Rios, at South Fork, and at Scotia since the early 1950's. The recent reconnaissance involved data collection for nitrogen, phosphorus, total organic carbon, trace elements, and pesticide compounds in the river at Van Arsdale Dam, near Dos Rios, at Fort Seward, and at Scotia.
The number of samples collected during the special reconnaissance is somewhat limited, and therefore the data are only an estimate of conditions that presently exist at selected sites in the river. Results indicate that most of the constituents were low in concentration; although some variability was measured for some constituents. Sampling was designed so that samples collected at each site would represent a large range in discharge. Results indicate that discharge was not the singular factor controlling the concentration variance for most constituents. However, the concentrations of total ammonia, phosphorus, arsenic, chromium, copper, and zinc indicated a direct relation with discharge at some sites.
Statistical analysis indicates that the past sampling program has been adequate to estimate the major chemical constituents of the river. Specific conductance in the river near its headwaters ranges from 110 to 300 micromhos about 98 percent of the time; and at Scotia, near the mouth, the specific conductance ranges from 110 to 340 micromhos about 98 percent of the time.
Results of regression analyses indicate that between 83 and 88 percent of the variance in specific conductance can be explained by discharge.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri765","usgsCitation":"Irwin, G.A., 1976, Water-quality investigation, Eel River, California: U.S. Geological Survey Water-Resources Investigations Report 76-5, iv, 35 p., https://doi.org/10.3133/wri765.","productDescription":"iv, 35 p.","costCenters":[],"links":[{"id":158604,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0005/report-thumb.jpg"},{"id":359110,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0005/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Eel River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -124.49707031249999,\n 39.33854604847979\n ],\n [\n -122.8,\n 39.33854604847979\n ],\n [\n -122.8,\n 40.896905775860006\n ],\n [\n -124.49707031249999,\n 40.896905775860006\n ],\n [\n -124.49707031249999,\n 39.33854604847979\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e54cc","contributors":{"authors":[{"text":"Irwin, George A.","contributorId":35363,"corporation":false,"usgs":true,"family":"Irwin","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":198774,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":65843,"text":"i959 - 1976 - Shaded relief map of the Bach area of Mercury (Australia Albedo Province)","interactions":[],"lastModifiedDate":"2012-02-02T00:13:17","indexId":"i959","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"959","subseriesTitle":"NONE","title":"Shaded relief map of the Bach area of Mercury (Australia Albedo Province)","language":"ENGLISH","doi":"10.3133/i959","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Shaded relief map of the Bach area of Mercury (Australia Albedo Province): U.S. Geological Survey IMAP 959, 1 map :col. ;46 cm. in diameter fold. in envelope 30 x 24 cm., https://doi.org/10.3133/i959.","productDescription":"1 map :col. ;46 cm. in diameter fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190174,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101196,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0959/plate-1.pdf","size":"2449","linkFileType":{"id":1,"text":"pdf"}}],"scale":"4290000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699f30","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":534198,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":65938,"text":"i978 - 1976 - Topographic map of the Oxia Palus Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-10T00:11:05","indexId":"i978","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"978","subseriesTitle":"NONE","title":"Topographic map of the Oxia Palus Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i978","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Topographic map of the Oxia Palus Quadrangle of Mars: U.S. Geological Survey IMAP 978, 1 map :col. ;37 x 53 cm. fold. in envelope 30 x 24 cm., https://doi.org/10.3133/i978.","productDescription":"1 map :col. ;37 x 53 cm. fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190048,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101250,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0978/plate-1.pdf","size":"3824","linkFileType":{"id":1,"text":"pdf"}}],"scale":"5000000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 0,0 ], [ 0,30 ], [ 45,30 ], [ 45,0 ], [ 0,0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629c70","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":534291,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":65948,"text":"i985 - 1976 - Topographic map of the Argyre Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:10","indexId":"i985","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"985","subseriesTitle":"NONE","title":"Topographic map of the Argyre Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i985","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Topographic map of the Argyre Quadrangle of Mars: U.S. Geological Survey IMAP 985, 1 map :col. ;on sheet 86 x 83 cm. fold. in envelope 30 x 24 cm., https://doi.org/10.3133/i985.","productDescription":"1 map :col. ;on sheet 86 x 83 cm. fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190338,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101260,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0985/plate-1.pdf","size":"4736","linkFileType":{"id":1,"text":"pdf"}}],"scale":"46000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699ca3","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":534301,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27839,"text":"wri7661 - 1976 - A model for calculating effects of liquid waste disposal in deep saline aquifer","interactions":[],"lastModifiedDate":"2018-11-16T10:01:44","indexId":"wri7661","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-61","title":"A model for calculating effects of liquid waste disposal in deep saline aquifer","docAbstract":"Injection of liquid industrial wastes into confined underground saline aquifers can offer a good disposal alternative from both environmental and economic considerations. One of the needs in choosing from among several disposal alternatives is a means of evaluating the influence such an injection will have on the aquifer system. This report describes a mathematical model to accomplish this purpose.
The objective of the contract was to develop a three-dimensional transient mathematical model which would accurately simulate behavior of waste injection into deep saline aquifers. Fluid properties, density and viscosity are functions of pressure, temperature and composition to provide a comprehensive assessment tool. The model is a finite-difference numerical solution of the partial differential equations describing
The model is not restricted to examining waste disposal operations. It can be used effectively to evaluate fresh water storage in saline aquifers, hot water storage in underground aquifers, salt water intrusion into groundwater flow systems and other similar applications.
The primary advantages of the present model can be summarized as:
The limitations of the present techniques are:
Included in the report are detailed descriptions of the approach used in the model, validation tests of the model, and a typical application of the model. A comparison volume documents the input data requirements, program structure, and an example problem for the model. '
Concentrations of dissolved solids in the Salinas River are variable and range from 164 to 494 milligrams per liter near Bradley and from 170 to 1,090 milligrams per liter near Spreckels. Higher concentrations near Spreckels are caused mainly by sewage inflow about 150 feet (50 meters) upstream. Concentrations of nitrogen, phosphorus, total organic carbon, selected trace elements, and pesticides also generally increase downstream from Pozo to Spreckels and are related to sewage effluent; however, high concentrations occur elsewhere in the river.
Specific conductance and water discharge regression results indicate that relations were all significant at the 1-percent probability level at Paso Robles, Bradley, and Spreckels, with the explained variance ranging from 66 to 74 percent. Concentrations of nitrogen, phosphorus, total organic carbon, and trace elements are only infrequently related to water discharge.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri76110","usgsCitation":"Irwin, G.A., 1976, Water-quality investigation, Salinas River, California: U.S. Geological Survey Water-Resources Investigations Report 76-110, v, 41 p., https://doi.org/10.3133/wri76110.","productDescription":"v, 41 p.","costCenters":[],"links":[{"id":361887,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0110/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158605,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0110/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Salinas River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122,\n 35.5833\n ],\n [\n -120,\n 35.5833\n ],\n [\n -120,\n 36.9\n ],\n [\n -122,\n 36.9\n ],\n [\n -122,\n 35.5833\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa5fc","contributors":{"authors":[{"text":"Irwin, George A.","contributorId":35363,"corporation":false,"usgs":true,"family":"Irwin","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":198775,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4826,"text":"pp978 - 1976 - PACER; data entry, retrieval, and update for the National Coal Resources Data System (Phase I)","interactions":[],"lastModifiedDate":"2012-02-02T00:05:50","indexId":"pp978","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"978","title":"PACER; data entry, retrieval, and update for the National Coal Resources Data System (Phase I)","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp978","usgsCitation":"Cargill, S.M., Olson, A., Medlin, A., and Carter, M., 1976, PACER; data entry, retrieval, and update for the National Coal Resources Data System (Phase I): U.S. Geological Survey Professional Paper 978, 107 p., https://doi.org/10.3133/pp978.","productDescription":"107 p.","costCenters":[],"links":[{"id":117417,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0978/report-thumb.jpg"},{"id":31769,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0978/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689f7c","contributors":{"authors":[{"text":"Cargill, Simon M.","contributorId":7256,"corporation":false,"usgs":true,"family":"Cargill","given":"Simon","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":149847,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olson, A.C.","contributorId":107685,"corporation":false,"usgs":true,"family":"Olson","given":"A.C.","email":"","affiliations":[],"preferred":false,"id":149850,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Medlin, A.L.","contributorId":28226,"corporation":false,"usgs":true,"family":"Medlin","given":"A.L.","email":"","affiliations":[],"preferred":false,"id":149848,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Carter, M.D.","contributorId":31382,"corporation":false,"usgs":true,"family":"Carter","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":149849,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":27611,"text":"wri76101 - 1976 - Water levels in artesian and nonartesian aquifers of Florida, 1973-74","interactions":[],"lastModifiedDate":"2019-08-05T11:05:50","indexId":"wri76101","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-101","title":"Water levels in artesian and nonartesian aquifers of Florida, 1973-74","docAbstract":"Based on measurements of water level in 675 wells selected from a network of about 1,300 observation wells, ground-water levels during May 1973 - May 1974 declined from 2 to 4 feet in the Floridan aquifer through most of north and central peninsular Florida. Hydrographs of 55 wells show the downward trends of ground-water levels continued in several areas of heavy pumping, the most notable area being in west-central Polk County where declines ranged from 18 to nearly 28 feet. In northwest Florida, declines ranged from less than 1 foot to 2 feet in the sand-and-gravel aquifer. In the southeastern coastal part of the State, levels rose 1 to 2 feet. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri76101","usgsCitation":"Healy, H.G., 1976, Water levels in artesian and nonartesian aquifers of Florida, 1973-74: U.S. Geological Survey Water-Resources Investigations Report 76-101, ix, 115 p. , https://doi.org/10.3133/wri76101.","productDescription":"ix, 115 p. ","costCenters":[],"links":[{"id":158996,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0101/report-thumb.jpg"},{"id":366226,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0101/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -85.20996093749999,\n 24.407137917727667\n ],\n [\n -79.89257812499999,\n 24.407137917727667\n ],\n [\n -79.89257812499999,\n 30.675715404167743\n ],\n [\n -85.20996093749999,\n 30.675715404167743\n ],\n [\n -85.20996093749999,\n 24.407137917727667\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9e0d","contributors":{"authors":[{"text":"Healy, Henry G.","contributorId":89916,"corporation":false,"usgs":true,"family":"Healy","given":"Henry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":198408,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":67116,"text":"i944 - 1976 - Geologic map of the Lamar Quadrangle, Colorado and Kansas","interactions":[],"lastModifiedDate":"2012-02-10T00:11:03","indexId":"i944","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"944","subseriesTitle":"NONE","title":"Geologic map of the Lamar Quadrangle, Colorado and Kansas","language":"ENGLISH","doi":"10.3133/i944","usgsCitation":"Sharps, J., 1976, Geologic map of the Lamar Quadrangle, Colorado and Kansas: U.S. Geological Survey IMAP 944, 1 map :col. ;45 x 70 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i944.","productDescription":"1 map :col. ;45 x 70 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107066,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9832.htm","linkFileType":{"id":5,"text":"html"},"description":"9832"},{"id":189400,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104,38 ], [ -104,39 ], [ -102,39 ], [ -102,38 ], [ -104,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db69713c","contributors":{"authors":[{"text":"Sharps, J.A.","contributorId":44938,"corporation":false,"usgs":true,"family":"Sharps","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":275625,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":65923,"text":"i988 - 1976 - Topographic map of the Cydonia region of Mars","interactions":[],"lastModifiedDate":"2015-07-29T13:17:10","indexId":"i988","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"988","subseriesTitle":"NONE","title":"Topographic map of the Cydonia region of Mars","language":"ENGLISH","doi":"10.3133/i988","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Topographic map of the Cydonia region of Mars: U.S. Geological Survey IMAP 988, 1 map :col. ;on sheet 86 x 77 cm. fold. in envelope 30 x 24 cm., https://doi.org/10.3133/i988.","productDescription":"1 map :col. ;on sheet 86 x 77 cm. fold. in envelope 30 x 24 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":190182,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101237,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0988/plate-1.pdf","size":"6837","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","otherGeospatial":"Mars","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629d6f","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":534276,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":65922,"text":"i976 - 1976 - Topographic map of the Coprates Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:17","indexId":"i976","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"976","subseriesTitle":"NONE","title":"Topographic map of the Coprates Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i976","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Topographic map of the Coprates Quadrangle of Mars: U.S. Geological Survey IMAP 976, 1 map :col. ;37 x 54 cm. fold. in envelope 30 x 24 cm., https://doi.org/10.3133/i976.","productDescription":"1 map :col. ;37 x 54 cm. fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190181,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101236,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0976/plate-1.pdf","size":"4317","linkFileType":{"id":1,"text":"pdf"}}],"scale":"5000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699c83","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":534275,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":65961,"text":"i975 - 1976 - Topographic map of the Margaritifer Sinus Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-10T00:11:09","indexId":"i975","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"975","subseriesTitle":"NONE","title":"Topographic map of the Margaritifer Sinus Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i975","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Topographic map of the Margaritifer Sinus Quadrangle of Mars: U.S. Geological Survey IMAP 975, 1 map :col. ;37 x 54 cm. fold. in envelope 30 x 24 cm., https://doi.org/10.3133/i975.","productDescription":"1 map :col. ;37 x 54 cm. fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189164,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101272,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0975/plate-1.pdf","size":"4378","linkFileType":{"id":1,"text":"pdf"}}],"scale":"5000000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -45,-30 ], [ -45,0 ], [ 0,0 ], [ 0,-30 ], [ -45,-30 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629ccf","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":534314,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27868,"text":"wri7617 - 1976 - Magnitude and frequency of floods in North Carolina, technique for estimating the magnitude and frequency of floods on natural streams in North Carolina","interactions":[],"lastModifiedDate":"2019-11-12T14:49:41","indexId":"wri7617","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-17","title":"Magnitude and frequency of floods in North Carolina, technique for estimating the magnitude and frequency of floods on natural streams in North Carolina","docAbstract":"Methods are provided to estimate the magnitude and frequency of floods on natural North Carolina streams with drainage areas greater than 0.5 square mile (1.3 square kilometers). For 257 gaged sites, the magnitudes of floods having recurrence intervals from 2 to 100 years are provided in tables. For ungaged sites, equations, graphs, and maps allow estimation of flood magnitudes. Multiple regression techniques were used to define the relation between flood peaks and seven basin and climatic variables. Drainage area is the most significant variable. Inclusion of the other six variables reduced the standard error of estimate less than 4 percent. Regression equations gave consistently different results for stations in the Coastal Plain than for stations in the mountains and Piedmont. Accordingly, stations were divided into two groups and estimating equations were developed for each geographic area.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7617","usgsCitation":"Jackson, N., 1976, Magnitude and frequency of floods in North Carolina, technique for estimating the magnitude and frequency of floods on natural streams in North Carolina: U.S. Geological Survey Water-Resources Investigations Report 76-17, v, 26 p. , https://doi.org/10.3133/wri7617.","productDescription":"v, 26 p. 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This aquifer commonly yields 500 to 1,000 gallons per minute (32 to 63 litres per second) and may yield as much as 2,500 gallons per minute (158 litres per second). Based on an estimated average storage coefficient of 0.1, the quantity of water stored in the Ogallala aquifer was computed at approximately 50 million acre-feet (6.17 x 101° cubic metres). Local overdevelopment of this water resource has resulted in water-level declines of more than 40 feet (12 metres) from 1966 to 1972 in some areas of concentrated well development. The amount of ground water in storage has been reduced about 2 percent during this period.
Aquifer tests indicate that transmissivity ranges from 500 to 11,800 feet squared per day (46 to 1,100 metres squared per day), the storage coefficient ranges from 0.002 to 0.11, and hydraulic conductivity ranges from 2.1 to 55 feet per day (0.6 to 16.8 metres per day). In addition to these tests, 802 specific-capacity tests were used to extend transmissivity data.
Recharge to the Ogallala aquifer is primarily from precipitation and may be as much as 1 inch (25 millimetres) per year in areas where catchment and percolation are most favorable. Discharge is primarily from pumping and a small amount of natural discharge.
Aquifers of limited importance are the Dakota Sandstone and the Cheyenne Sandstone Member of the Purgatoire Formation which provide water to irrigation wells in the southwestern part of Cimarron County. Irrigation wells generally are completed jointly in these aquifers and yields of 300 to 500 gallons per minute (19 to 32 litres per second) are common. Water levels in these aquifers have not shown the pronounced declines that have occurred in the Ogallala aquifer. Permian red beds provide only small quantities of water to domestic and stock wells.
Water in the Ogallala aquifer, Dakota Sandstone, and Cheyenne Sandstone Member generally has a dissolved-solids concentration of less than 500 milligrams per litre. The dissolved-solids concentration in water from the Permian red beds generally exceeds 500 milligrams per litre and locally exceeds 2,000 milligrams per litre.
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