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,{"id":43096,"text":"ofr8951 - 1989 - Ground-water data from selected sites, Grand Teton National Park, Wyoming","interactions":[],"lastModifiedDate":"2021-11-30T22:39:16.931785","indexId":"ofr8951","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-51","title":"Ground-water data from selected sites, Grand Teton National Park, Wyoming","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8951","usgsCitation":"Parliman, D., and Young, H., 1989, Ground-water data from selected sites, Grand Teton National Park, Wyoming: U.S. Geological Survey Open-File Report 89-51, 1 Plate: 37.72 × 25.04 inches, https://doi.org/10.3133/ofr8951.","productDescription":"1 Plate: 37.72 × 25.04 inches","costCenters":[],"links":[{"id":135577,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":392275,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17566.htm"},{"id":80908,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0051/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wyoming","otherGeospatial":"Grand Teton National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.02783203125,\n              43.56447158721811\n            ],\n            [\n              -110.401611328125,\n              43.56447158721811\n            ],\n            [\n              -110.401611328125,\n              44.134913443750726\n            ],\n            [\n              -111.02783203125,\n              44.134913443750726\n            ],\n            [\n              -111.02783203125,\n              43.56447158721811\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cf32","contributors":{"authors":[{"text":"Parliman, D. J.","contributorId":64220,"corporation":false,"usgs":true,"family":"Parliman","given":"D. J.","affiliations":[],"preferred":false,"id":227715,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Young, H.W.","contributorId":68278,"corporation":false,"usgs":true,"family":"Young","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":227716,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":20239,"text":"ofr8949 - 1989 - Biannual water-resources review, White Sands Missile Range, New Mexico, 1986 and 1987","interactions":[],"lastModifiedDate":"2012-02-02T00:07:35","indexId":"ofr8949","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-49","title":"Biannual water-resources review, White Sands Missile Range, New Mexico, 1986 and 1987","docAbstract":"Hydrologic data were collected at White Sands Missile Range, New Mexico in 1986 and 1987. The total groundwater withdrawal in 1986 was 565,462,500 gal and in 1987 it was 620,492,000 gal. The total groundwater withdrawal was 110,971,300 gal less in 1986 than in 1985, but 55,029,500 gal more in 1987 than in 1986. Water samples from five Post Headquarters water supply wells were collected for chemical analysis in 1986. In 1987, water samples were collected from four test wells in the Post Headquarters area for analysis of selected volatile organic compounds. Twenty-eight water samples from wells were collected for analysis of specific conductance in 1986 and 1987. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nCopies of this report can be purchased from Books and Open-File Reports, Federal Center,","doi":"10.3133/ofr8949","usgsCitation":"Myers, R.G., and Sharp, S.C., 1989, Biannual water-resources review, White Sands Missile Range, New Mexico, 1986 and 1987: U.S. Geological Survey Open-File Report 89-49, iv, 36 p. ill., map ;28 cm., https://doi.org/10.3133/ofr8949.","productDescription":"iv, 36 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":152505,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0049/report-thumb.jpg"},{"id":49780,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0049/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62985d","contributors":{"authors":[{"text":"Myers, Robert G.","contributorId":99170,"corporation":false,"usgs":true,"family":"Myers","given":"Robert","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":182306,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sharp, Steven C.","contributorId":89917,"corporation":false,"usgs":true,"family":"Sharp","given":"Steven","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":182305,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14612,"text":"ofr89235 - 1989 - Texture and depositional history of near-surface alluvial deposits in the central part of the western San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2014-07-14T10:46:17","indexId":"ofr89235","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-235","title":"Texture and depositional history of near-surface alluvial deposits in the central part of the western San Joaquin Valley, California","docAbstract":"<p>Saline conditions and associated high levels of selenium and other soluble trace elements in soil, shallow ground water, and agricultural drain water of the western San Joaquin Valley, California, have prompted a study of the texture of near-surface alluvial deposits in the central part of the western valley. Texture is characterized by the percentage of coarse-grained sediment present within a specified subsurface depth interval and is used as a basis for mapping the upper 50 feet of deposits. Resulting quantitative descriptions of the deposits are used to interpret the late Quaternary history of the area.</p>\n<br/>\n<p>Three hydrogeologic units--Coast Range alluvium, flood-basin deposits, and Sierran sand--can be recognized in the upper 50 feet of deposits in the central part of the western San Joaquin Valley. The upper 30 feet of Coast Range alluvium and the adjacent 5 to 35 feet of flood-basin deposits are predominantly fine grained. These fine-grained Coast Range deposits are underlain by coarse-grained channel deposits. The fine-grained flood basin deposits are underlain by coarse-grained Sierran sand. The extent and orientation of channel deposits below 20 feet in the Coast Range alluvium indicate that streams draining the Coast Range may have been tributary to the axial stream that deposited the Sierran sand and that streamflow may have been to the southeast.</p>\n<br/>\n<p>The fining-upward stratigraphic sequence in the upper 50 feet of deposits and the headward retreat of tributary stream channels from the valley trough with time support a recent hypothesis of climatic control of alluviation in the western San Joaquin Valley.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Sacramento, CA","doi":"10.3133/ofr89235","collaboration":"Prepared in cooperation with the San Joaquin Valley Drainage Program","usgsCitation":"Laudon, J., and Belitz, K., 1989, Texture and depositional history of near-surface alluvial deposits in the central part of the western San Joaquin Valley, California: U.S. Geological Survey Open-File Report 89-235, iv, 19 p., https://doi.org/10.3133/ofr89235.","productDescription":"iv, 19 p.","numberOfPages":"25","costCenters":[],"links":[{"id":289877,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":289876,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0235/report.pdf"}],"country":"United States","state":"California","otherGeospatial":"San Joaquin Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.25,36.25 ], [ -121.25,37.25 ], [ -119.75,37.25 ], [ -119.75,36.25 ], [ -121.25,36.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683757","contributors":{"authors":[{"text":"Laudon, Julie","contributorId":68320,"corporation":false,"usgs":true,"family":"Laudon","given":"Julie","email":"","affiliations":[],"preferred":false,"id":169738,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Belitz, Kenneth 0000-0003-4481-2345 kbelitz@usgs.gov","orcid":"https://orcid.org/0000-0003-4481-2345","contributorId":442,"corporation":false,"usgs":true,"family":"Belitz","given":"Kenneth","email":"kbelitz@usgs.gov","affiliations":[{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":169737,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68330,"text":"ha708 - 1989 - Flow characteristics for selected streams in the Great Plains subregion, of the Central Midwest regional aquifer system and selected adjacent areas— Kansas and Nebraska, and parts of Colorado, Iowa, Missouri, New Mexico, Oklahoma, South Dakota, and Texas","interactions":[],"lastModifiedDate":"2021-09-14T18:03:01.429235","indexId":"ha708","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"708","title":"Flow characteristics for selected streams in the Great Plains subregion, of the Central Midwest regional aquifer system and selected adjacent areas— Kansas and Nebraska, and parts of Colorado, Iowa, Missouri, New Mexico, Oklahoma, South Dakota, and Texas","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha708","usgsCitation":"Hedman, E.R., and Engel, G.B., 1989, Flow characteristics for selected streams in the Great Plains subregion, of the Central Midwest regional aquifer system and selected adjacent areas— Kansas and Nebraska, and parts of Colorado, Iowa, Missouri, New Mexico, Oklahoma, South Dakota, and Texas: U.S. Geological Survey Hydrologic Atlas 708, 5 Plates: 39.50 × 58.00 inches or smaller, https://doi.org/10.3133/ha708.","productDescription":"5 Plates: 39.50 × 58.00 inches or smaller","costCenters":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":186602,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89801,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/708/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89798,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/708/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":389213,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16109.htm"},{"id":89800,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/708/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89799,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/708/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89797,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/708/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","country":"United States","state":"Colorado, Iowa, Kansas, Missouri, Nebraska, New Mexico, Oklahoma, South Dakota, Texas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105,34 ], [ -105,43.5 ], [ -94.5,43.5 ], [ -94.5,34 ], [ -105,34 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4783e4b07f02db483b34","contributors":{"authors":[{"text":"Hedman, E. R.","contributorId":71527,"corporation":false,"usgs":true,"family":"Hedman","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":278042,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Engel, Glenn B.","contributorId":70063,"corporation":false,"usgs":true,"family":"Engel","given":"Glenn","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":278041,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28446,"text":"wri894022 - 1989 - Inorganic and organic ground-water chemistry in the Canal Creek area of Aberdeen Proving Ground, Maryland","interactions":[],"lastModifiedDate":"2012-02-02T00:08:52","indexId":"wri894022","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-4022","title":"Inorganic and organic ground-water chemistry in the Canal Creek area of Aberdeen Proving Ground, Maryland","docAbstract":"Groundwater chemical data were collected from November 1986 through April 1987 in the first phase of a 5-year study to assess the possibility of groundwater contamination in the Canal Creek area of Aberdeen Proving Ground, Maryland. Water samples were collected from 87 observation wells screened in Coastal Plain sediments; 59 samples were collected from the Canal Creek aquifer, 18 from the overlying surficial aquifer, and 10 from the lower confined aquifer. Dissolved solids, chloride, iron, manganese, fluoride, mercury, and chromium are present in concentrations that exceed the Federal maximum contaminant levels for drinking water. Elevated chloride and dissolved-solids concentrations appear to be related from contaminant plumes but also could result from brackish-water intrusion. Excessive concentrations of iron and manganese were the most extensive water quality problems found among the inorganic constituents and are derived from natural dissolution of minerals and oxide coatings in the aquifer sediments. Volatile organic compounds are present in the Canal Creek and surficial aquifers, but samples from the lower confined aquifer do not show any evidence of contamination by inorganic or organic chemicals. The volatile organic contaminants detected in the groundwater and their maximum concentrations (in micrograms/L) include 1,1,2,2- tetrachloroethane (9,000); carbon tetrachloride (480); chloroform (460); 1,1,2-trichloroethane (80); 1,2-dichloroethane (990); 1,1-dichloroethane (3.1); tetrachloroethylene (100); trichloroethylene (1,800); 1,2-trans- dichloroethylene (1,200); 1,1-dichloroethylene (4.4); vinyl chloride (140); benzene (70); and chlorobenzene (39). On the basis of information on past activities in the study area, some sources of the volatile organic compounds include: (1) decontaminants and degreasers; (2) clothing-impregnating operations; (3) the manufacture of impregnite material; (4) the manufacture of tear gas; and (5) fuels used in garages and at the air-field. The high density of most of the detected organic compounds in free-product form would have aided their movement into the aquifers by vertical sinking. The outcrop area of the upper confining unit and an area cut by a paleochannel are most susceptible to contamination because a near-surface impermeable layer is not present. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri894022","usgsCitation":"Lorah, M., and Vroblesky, D., 1989, Inorganic and organic ground-water chemistry in the Canal Creek area of Aberdeen Proving Ground, Maryland: U.S. Geological Survey Water-Resources Investigations Report 89-4022, vii, 97 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri894022.","productDescription":"vii, 97 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123661,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4022/report-thumb.jpg"},{"id":57246,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1989/4022/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57247,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1989/4022/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57248,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1989/4022/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57249,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4022/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49efe4b07f02db5ede2d","contributors":{"authors":[{"text":"Lorah, M.M.","contributorId":29002,"corporation":false,"usgs":true,"family":"Lorah","given":"M.M.","affiliations":[],"preferred":false,"id":199812,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vroblesky, D.A.","contributorId":101691,"corporation":false,"usgs":true,"family":"Vroblesky","given":"D.A.","affiliations":[],"preferred":false,"id":199813,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":54331,"text":"wdrIL882 - 1989 - Water Resources Data, Illinois, Water Year 1988, Vol. 2","interactions":[],"lastModifiedDate":"2012-02-02T00:11:51","indexId":"wdrIL882","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"IL-88-2","title":"Water Resources Data, Illinois, Water Year 1988, Vol. 2","language":"ENGLISH","doi":"10.3133/wdrIL882","usgsCitation":"Coupe, R., Hayes, P., Richards, T., and Stahl, R., 1989, Water Resources Data, Illinois, Water Year 1988, Vol. 2: U.S. Geological Survey Water Data Report IL-88-2, NA, https://doi.org/10.3133/wdrIL882.","productDescription":"NA","costCenters":[],"links":[{"id":174270,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb954","contributors":{"authors":[{"text":"Coupe, R.H.","contributorId":84778,"corporation":false,"usgs":true,"family":"Coupe","given":"R.H.","affiliations":[],"preferred":false,"id":249928,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hayes, P.D.","contributorId":52644,"corporation":false,"usgs":true,"family":"Hayes","given":"P.D.","email":"","affiliations":[],"preferred":false,"id":249926,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Richards, T.E.","contributorId":64718,"corporation":false,"usgs":true,"family":"Richards","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":249927,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stahl, R.L.","contributorId":35798,"corporation":false,"usgs":true,"family":"Stahl","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":249925,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":19720,"text":"ofr87535 - 1989 - Preparation of average annual runoff map of the United States, 1951-80","interactions":[],"lastModifiedDate":"2015-10-08T13:08:11","indexId":"ofr87535","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-535","title":"Preparation of average annual runoff map of the United States, 1951-80","docAbstract":"<p>Average annual runoff was computed or estimated for 2,148 hydrologic cataloging units in the United States and Puerto Rico , for the period 1951-80. Runoff was computed from the recorded streamflow at 5,951 U.S. Geological Survey gaging stations. The runoff at more than 3,000 of these stations was estimated by correlation with other nearby stations to adjust for missing data.</p>\n<p>These runoff data were used to draw a map depicting the variation of runoff throughout the nation. Average annual runoff varied from less than 0.01 inch in parts of the Great Basin (Utah, parts of Nevada, Oregon, and California) to more than 240 inches in southeastern Alaska. (USGS)</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87535","usgsCitation":"Krug, W., Gebert, W., and Graczyk, D., 1989, Preparation of average annual runoff map of the United States, 1951-80: U.S. Geological Survey Open-File Report 87-535, iii, 414 p., https://doi.org/10.3133/ofr87535.","productDescription":"iii, 414 p.","numberOfPages":"417","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":49195,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0535/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152836,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0535/report-thumb.jpg"}],"country":"United 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,{"id":28280,"text":"wri884031 - 1989 - Water-resources appraisal of the Lake Traverse Indian Reservation in South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:08:48","indexId":"wri884031","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4031","title":"Water-resources appraisal of the Lake Traverse Indian Reservation in South Dakota","docAbstract":"The water resources within the Lake Traverse Indian Reservation consist of streams, lakes, wetlands, and groundwater stored in alluvium and glacial outwash deposits. Streamflow may cease during dry periods and during the winter. Lakes and ponds within the reservation are found predominantly within an internally drained basin. Dissolved-solids concentrations in the lakes generally range from 500 to 10,000 mg/L. Dissolved-solids concentrations in the streams generally ranging from 500 to 1 ,000 mg/L. However, nutrient concentrations tend to be larger than natural background levels in both lakes and streams and indicate unidentified sources of nutrients that effect the quality of water. Major development of surface-water resources is hindered by the lack of storage capacity within the numerous lakes, the lack of sustained streamflow, and the lack of suitable sites for construction or reservoirs. Water within the Coteau des Prairies, a glacial upland, occurs in outwash deposits. The sand and gravel deposits in the Coteau may be as thick as 70 ft. The quality of water from these aquifers generally is suitable for most uses, with calcium, magnesium, and bicarbonate the dominant ions. Water in sand and gravel deposits within the Red River and Minnesota River lowlands tends to have larger concentrations of dissolved solids than the sand and gravel deposits in the Coteau des Prairies. The quality of water in these deposits tends to be more mineralized than water in the sand and gravel deposits in the Coteau des Prairies. The regional flow of groundwater generally is to the east towards the Minnesota and Red River basins and west in the Coteau des Prairies. (USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri884031","usgsCitation":"Lawrence, S., 1989, Water-resources appraisal of the Lake Traverse Indian Reservation in South Dakota: U.S. Geological Survey Water-Resources Investigations Report 88-4031, v, 42 p. :ill. ;28 cm., https://doi.org/10.3133/wri884031.","productDescription":"v, 42 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":123320,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4031/report-thumb.jpg"},{"id":57100,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4031/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47e6e4b07f02db4bbbcf","contributors":{"authors":[{"text":"Lawrence, S.J.","contributorId":67922,"corporation":false,"usgs":true,"family":"Lawrence","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":199521,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57401,"text":"wdrPA882 - 1989 - Water resources data for Pennsylvania, water year 1988. Volume 2: Susquehanna and Potomac River Basins","interactions":[],"lastModifiedDate":"2020-05-13T17:00:08.262491","indexId":"wdrPA882","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"PA-88-2","title":"Water resources data for Pennsylvania, water year 1988. Volume 2: Susquehanna and Potomac River Basins","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrPA882","usgsCitation":"Loper, W., Behrendt, T., and Schaffstall, W., 1989, Water resources data for Pennsylvania, water year 1988. Volume 2: Susquehanna and Potomac River Basins: U.S. Geological Survey Water Data Report PA-88-2, viii, 276 p. , https://doi.org/10.3133/wdrPA882.","productDescription":"viii, 276 p. 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,{"id":7,"text":"wsp2358 - 1989 - Characteristics and trends of streamflow and dissolved solids in the upper Colorado River Basin, Arizona, Colorado, New Mexico, Utah, and Wyoming","interactions":[{"subject":{"id":39640,"text":"ofr87568 - 1988 - Characteristics and trends of streamflow and dissolved solids in the upper Colorado River Basin, Arizona, California, Colorado, Nevada, New Mexico, Utah, and Wyoming","indexId":"ofr87568","publicationYear":"1988","noYear":false,"title":"Characteristics and trends of streamflow and dissolved solids in the upper Colorado River Basin, Arizona, California, Colorado, Nevada, New Mexico, Utah, and Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":7,"text":"wsp2358 - 1989 - Characteristics and trends of streamflow and dissolved solids in the upper Colorado River Basin, Arizona, Colorado, New Mexico, Utah, and Wyoming","indexId":"wsp2358","publicationYear":"1989","noYear":false,"title":"Characteristics and trends of streamflow and dissolved solids in the upper Colorado River Basin, Arizona, Colorado, New Mexico, Utah, and Wyoming"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp2358","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"2358","title":"Characteristics and trends of streamflow and dissolved solids in the upper Colorado River Basin, Arizona, Colorado, New Mexico, Utah, and Wyoming","docAbstract":"Annual and monthly concentrations and loads of dissolved solids and major constituents were estimated for 70 streamflow-gaging stations in the Upper Colorado River Basin. Trends in streamflow, dissolved-solids concentrations, and dissolved-solids loads were identified. Nonparametric trend-analysis techniques were used to determine step trends resulting from human activities upstream and long-term monotonic trends. Results were compared with physical characteristics of the basin and historical water-resource development in the basin to determine source areas of dissolved solids and possible cause of trends. \r\n\r\nMean annual dissolved-solids concentration increases from less than 100 milligrams per liter in the headwater streams to more than 500 milligrams per liter in the outflow from the Upper Colorado River Basin. All the major tributaries that have high concentrations of dissolved solids are downstream from extensive areas of irrigated agriculture. However, irrigation predated the period of record for most sites and was not a factor in many identified trends. Significant annual trends were identified for 30 sites. Most of these trends were related to transbasin exports, changes in land use, salinity-control practices, or reservoir development. The primary factor affecting streamflow and dissolved-solids concentration and load has been the construction of large reservoirs. Reservoirs have decreased the seasonal and annual variability of streamflow and dissolved solids in streams that drain the Gunnison and San Juan River basins. Fontenelle and Flaming Gorge Reservoirs have increased the dissolved-solids load in the Green River because of dissolution of mineral salts from the bank material. The largest trends occurred downstream from Lake Powell. However, the period of record since the completion of filling was too short to estimate the long-term effects of that reservoir.","language":"ENGLISH","publisher":"U.S. G.P.O. ;\r\nBooks and Open- File Reports Section, U.S. Geological Survey [distributor],","doi":"10.3133/wsp2358","usgsCitation":"Liebermann, T.D., Mueller, D.K., Kircher, J.E., and Choquette, A.F., 1989, Characteristics and trends of streamflow and dissolved solids in the upper Colorado River Basin, Arizona, Colorado, New Mexico, Utah, and Wyoming: U.S. Geological Survey Water Supply Paper 2358, vi, 64 p. :ill., map ;28 cm., https://doi.org/10.3133/wsp2358.","productDescription":"vi, 64 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":136298,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2358/report-thumb.jpg"},{"id":24600,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2358/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df6bd","contributors":{"authors":[{"text":"Liebermann, Timothy D.","contributorId":42188,"corporation":false,"usgs":true,"family":"Liebermann","given":"Timothy","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":141807,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mueller, David K. mueller@usgs.gov","contributorId":1585,"corporation":false,"usgs":true,"family":"Mueller","given":"David","email":"mueller@usgs.gov","middleInitial":"K.","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true}],"preferred":true,"id":141806,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kircher, James E. jkircher@usgs.gov","contributorId":248,"corporation":false,"usgs":true,"family":"Kircher","given":"James","email":"jkircher@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":141804,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Choquette, Anne F. achoq@usgs.gov","contributorId":1225,"corporation":false,"usgs":true,"family":"Choquette","given":"Anne","email":"achoq@usgs.gov","middleInitial":"F.","affiliations":[{"id":581,"text":"Tennessee Water Science Center","active":true,"usgs":true}],"preferred":true,"id":141805,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":19706,"text":"ofr89247 - 1989 - Streamflow and water-quality data for Little Clearfield Creek basin, Clearfield County, Pennsylvania, December 1987 - November 1988","interactions":[],"lastModifiedDate":"2017-06-22T10:54:58","indexId":"ofr89247","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-247","title":"Streamflow and water-quality data for Little Clearfield Creek basin, Clearfield County, Pennsylvania, December 1987 - November 1988","docAbstract":"Streamflow and water quality data were collected throughout the Little Clearfield Creek basin, Clearfield County, Pennsylvania, from December 1987 through November 1988, to determine the existing quality of surface water over a range of hydrologic conditions. This data will assist the Pennsylvania Department of Environmental Resources during its review of coal mine permit applications. A water quality station near the mouth of Little Clearfield Creek provided continuous record of stream stage, pH, specific conductance, and water temperature. Monthly water quality samples collected at this station were analyzed for total and dissolved metals, nutrients, major cations, and suspended sediment concentrations. Seventeen partial record sites, located throughout the basin, were similarly sampled four times during the study. Streamflow and water quality data obtained at these sites during a winter base flow, a spring storm event, a low summer base flow, and a more moderate summer base flow also are presented. (Author 's abstract)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr89247","usgsCitation":"Kostelnik, K.M., and Durlin, R., 1989, Streamflow and water-quality data for Little Clearfield Creek basin, Clearfield County, Pennsylvania, December 1987 - November 1988: U.S. Geological Survey Open-File Report 89-247, vi, 30 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89247.","productDescription":"vi, 30 p. :ill. ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":153870,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0247/report-thumb.jpg"},{"id":49184,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0247/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4e86","contributors":{"authors":[{"text":"Kostelnik, K. M.","contributorId":34951,"corporation":false,"usgs":true,"family":"Kostelnik","given":"K.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":181368,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Durlin, R.R.","contributorId":67116,"corporation":false,"usgs":true,"family":"Durlin","given":"R.R.","affiliations":[],"preferred":false,"id":181369,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44828,"text":"wri884144 - 1989 - Potentiometric-surface map of the Carbonate Aquifer in Silurian and Devonian rocks, Lucas, Sandusky, and Wood Counties, Northwestern Ohio, July 1986","interactions":[],"lastModifiedDate":"2012-02-02T00:10:47","indexId":"wri884144","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4144","title":"Potentiometric-surface map of the Carbonate Aquifer in Silurian and Devonian rocks, Lucas, Sandusky, and Wood Counties, Northwestern Ohio, July 1986","language":"ENGLISH","doi":"10.3133/wri884144","usgsCitation":"Breen, K.J., 1989, Potentiometric-surface map of the Carbonate Aquifer in Silurian and Devonian rocks, Lucas, Sandusky, and Wood Counties, Northwestern Ohio, July 1986: U.S. Geological Survey Water-Resources Investigations Report 88-4144, 1 map : col. ; 52 x 82 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/wri884144.","productDescription":"1 map : col. ; 52 x 82 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":171287,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":82177,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4144/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db681f4e","contributors":{"authors":[{"text":"Breen, Kevin J. 0000-0002-9447-6469 kjbreen@usgs.gov","orcid":"https://orcid.org/0000-0002-9447-6469","contributorId":219,"corporation":false,"usgs":true,"family":"Breen","given":"Kevin","email":"kjbreen@usgs.gov","middleInitial":"J.","affiliations":[{"id":501,"text":"Office of Science Quality and Integrity","active":true,"usgs":true}],"preferred":true,"id":230508,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39648,"text":"pp1403I - 1989 - Geochemistry of the Floridan aquifer system in Florida and in parts of Georgia, South Carolina, and Alabama","interactions":[],"lastModifiedDate":"2025-04-17T18:52:27.70877","indexId":"pp1403I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"1403","chapter":"I","title":"Geochemistry of the Floridan aquifer system in Florida and in parts of Georgia, South Carolina, and Alabama","docAbstract":"The chemical quality of the ground water in the Floridan aquifer system is determined primarily by mineral-water interaction. However, some changes in water quality have been imposed by development, particularly near coastal pumping centers. A total of 601 chemical analyses, all from different wells, most completed in the upper part of the aquifer system, were used to describe the variations in water chemistry and to study the processes responsible for observed changes. \r\n\r\nThe Floridan aquifer system is a vertically continuous sequence of Tertiary carbonate rocks that are of generally high permeability and are hydraulically connected in varying degrees. The rocks are principally limestone and dolomite, but they grade into limy sands and clays near the aquifer system's updip limits. Major minerals in the aquifer system are calcite, dolomite, and, locally, gypsum or quartz; minor minerals include apatite, glauconite, and clay minerals such as kaolinite and montmorillonite. Trace amounts of metallic oxides or sulfides are present in some areas. \r\n\r\nThe aquifer system consists of the Upper and Lower Floridan aquifers, separated in most places by a less permeable confining unit that has highly variable hydraulic properties. Only the Upper Floridan aquifer is present throughout the study area. Freshwater enters the aquifer system in outcrop areas located primarily in central Georgia and north-central Florida. Discharge occurs chiefly to streams and springs and, to a lesser extent, directly into the sea. Most of the flow into and out of the system takes place where it is unconfined or where the upper confining unit is thin. Secondary permeability developed by dissolution of aquifer material is most prominent in these areas of dynamic flow. \r\n\r\nDissolved-solids concentrations in water from the Upper Floridan aquifer generally range from less than 25 milligrams per liter near outcrops to more than 25,000 milligrams per liter along the coasts. The dominant cations in the ground water are Ca2+, Mg2+, and Na+; the dominant anions are HCO3-, Cl-, and SO42-, The concentration of Ca2+ is controlled primarily by calcite saturation. Concentrations of Mg2+, NA+, and Cl- are highest where mixing of freshwater and saltwater occurs. Concentrations of HCO3- reflect the control of calcite solubility. The concentration of SO42- is highest where gypsiferous rock units are present in the aquifer system. \r\n\r\nThe major geochemical processes that occur in the Upper Floridan aquifer, based on water-quality maps and computations using a geochemical model, are (1) dissolution of aquifer minerals toward equilibrium, (2) mixing of ground water with recharge, leakage, or seawater, (3) sulfate reduction, and (4) cation exchange between water and aquifer minerals. \r\n\r\nSimilar processes apparently control minor dissolved constituents, although quantification is difficult with the available data. Statistical tests of available nutrient data indicate that concentrations of N (nitrogen) species in unconfined recharge areas may be increasing over time; more detailed studies of all N species are needed to test this hypothesis, however. Data on trace metals, radionuclides, and man-made organic contaminants are limited. Available data indicate that most freshwater within the Upper Floridan is potable, but detection of pesticides in a few samples indicates that the system is susceptible to contamination from the land surface in some areas, particularly where its upper confining unit is thin or absent. \r\n\r\nGeochemical models were used to examine changes in major chemical elements along selected ground-water paths within the Upper Floridan aquifer. Water in the Upper Floridan aquifer can be categorized into four hydrochemical facies, whose exact distribution is determined by confined or unconfined conditions of the aquifer and by chloride concentrations. The reaction models are considered plausible based on available chemical, isotopic, and hydrologic information, and they","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/pp1403I","usgsCitation":"Geochemistry of the Floridan aquifer system in Florida and in parts of Georgia, South Carolina, and Alabama; 1989; PP; 1403-I; Sprinkle, Craig L.","productDescription":"Report: 105 p.; 9 Plates: 21.00 x 26.30 inches or smaller; Database","numberOfPages":"105","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":119386,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1403i/coverthb.jpg"},{"id":67334,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1403i/report.pdf","text":"Report","size":"21.6 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":67325,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1403i/plate-1.pdf","text":"Plate 1","size":"1.64 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":67326,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1403i/plate-2.pdf","text":"Plate 2","size":"1.70 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":67330,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1403i/plate-6.pdf","text":"Plate 6","size":"1.81 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":67331,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1403i/plate-7.pdf","text":"Plate 7","size":"1.76 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":67332,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1403i/plate-8.pdf","text":"Plate 8","size":"1.76 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,{"id":20129,"text":"ofr89261 - 1989 - Cyclic injection, storage, and withdrawal of heated water in a sandstone aquifer at St. Paul, Minnesota: Field observations, preliminary model analysis, and aquifer thermal efficiency","interactions":[],"lastModifiedDate":"2018-03-19T10:20:50","indexId":"ofr89261","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-261","title":"Cyclic injection, storage, and withdrawal of heated water in a sandstone aquifer at St. Paul, Minnesota: Field observations, preliminary model analysis, and aquifer thermal efficiency","docAbstract":"<p>In May 1980, the University of Minnesota began a project to evaluate the feasibility of storing heated (150 &deg;C (degree Celsius)) water in the deep (180 to 240 m (meters)) Franconia-Ironton-Galesville aquifer and later recovering it for space heating. The Aquifer Thermal-Energy Storage (ATES) system was doublet-well design in which the injection/withdrawal wells were spaced approximately 250 m apart. High-temperature water from the University's steam-generation facilities supplied heat for injection. Water was pumped from one of the wells through a heat exchanger, where heat was added or removed. Water then was injected back into the aquifer through the other well. The experimental plan for testing the ATES system consisted of a series of short-term hot-water injection, storage, and withdrawal cycles. Each cycle was 24-days long, and each injection, storage, and withdrawal step of the cycle was 8 days.</p>\n<p>The Franconia-Ironton-Galesville aquifer is a consolidated sandstone, approximately 60 m thick, the top of which is approximately 180 m below the land surface. It is confined above by the St. Lawrence Formation--a dolomitic sandstone 8-m thick--and below by the Eau Claire Formation--a shale 30-m thick. Initial hydraulic testing with inflatable packers indicated that the aquifer has four hydraulic zones with distinctly different values of relative horizontal hydraulic conductivity. The thickness of each zone was determined by correlating data from geophysical logs, core samples, and the inflatablepacker tests.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr89261","collaboration":"Prepared in cooperation with the University of Minnesota and the Minnesota Geological Survey","usgsCitation":"Miller, R.T., 1989, Cyclic injection, storage, and withdrawal of heated water in a sandstone aquifer at St. Paul, Minnesota: Field observations, preliminary model analysis, and aquifer thermal efficiency: U.S. Geological Survey Open-File Report 89-261, viii, 97 p., https://doi.org/10.3133/ofr89261.","productDescription":"viii, 97 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":153231,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0261/report-thumb.jpg"},{"id":49670,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0261/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","city":"St. Paul","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.23410034179688,\n              44.83736927811443\n            ],\n            [\n              -93.23410034179688,\n              45.023067895446175\n            ],\n            [\n              -92.92922973632812,\n              45.023067895446175\n            ],\n            [\n              -92.92922973632812,\n              44.83736927811443\n            ],\n            [\n              -93.23410034179688,\n              44.83736927811443\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67eb9c","contributors":{"authors":[{"text":"Miller, Robert T.","contributorId":91892,"corporation":false,"usgs":true,"family":"Miller","given":"Robert","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":182114,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19206,"text":"ofr8934 - 1989 - Ground-water-quality assessment of the Delmarva Peninsula, Delaware, Maryland, and Virginia; analysis of available water-quality data through 1987","interactions":[{"subject":{"id":19206,"text":"ofr8934 - 1989 - Ground-water-quality assessment of the Delmarva Peninsula, Delaware, Maryland, and Virginia; analysis of available water-quality data through 1987","indexId":"ofr8934","publicationYear":"1989","noYear":false,"title":"Ground-water-quality assessment of the Delmarva Peninsula, Delaware, Maryland, and Virginia; analysis of available water-quality data through 1987"},"predicate":"SUPERSEDED_BY","object":{"id":1787,"text":"wsp2355B - 1991 - Water-quality assessment of the Delmarva Peninsula, Delaware, Maryland, and Virginia— Analysis of available ground-water-quality data through 1987","indexId":"wsp2355B","publicationYear":"1991","noYear":false,"chapter":"B","title":"Water-quality assessment of the Delmarva Peninsula, Delaware, Maryland, and Virginia— Analysis of available ground-water-quality data through 1987"},"id":1}],"supersededBy":{"id":1787,"text":"wsp2355B - 1991 - Water-quality assessment of the Delmarva Peninsula, Delaware, Maryland, and Virginia— Analysis of available ground-water-quality data through 1987","indexId":"wsp2355B","publicationYear":"1991","noYear":false,"title":"Water-quality assessment of the Delmarva Peninsula, Delaware, Maryland, and Virginia— Analysis of available ground-water-quality data through 1987"},"lastModifiedDate":"2013-12-03T11:37:11","indexId":"ofr8934","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-34","title":"Ground-water-quality assessment of the Delmarva Peninsula, Delaware, Maryland, and Virginia; analysis of available water-quality data through 1987","docAbstract":"Regional water quality conditions were analyzed on the basis of available data for the Delmarva Peninsula. A summary of 3 Federal, 5 State, and 14 local agencies, as well as various nonprofit organizations and universities, serving as repositories for water quality data is presented. Also included is information describing the range of chemical constituents, the ease of retrieving the data, and general characteristics of the data for use in a regional groundwater quality assessment. Certain characteristics of the available data limit their usefulness for a regional assessment of groundwater. These include a (1) lack of information on quality control; (2) inconsistent sampling; preservation, and analytical techniques used among and within agencies; (3) the clustering of sampling wells around known or suspected areas of contamination, which can impose a bias on water quality assessments; and (4) lack of information on sampling locations, well depths, well construction, and aquifer characteristics. Despite these limitations, the analysis provides a foundation for more detailed regional assessments of water resources on the Delmarva Peninsula and highlights areas where pertinent data are needed. Results of the analysis indicate that data on trace element and organic compound concentrations in groundwater in the Delmarva Peninsula are scarce, whereas data for nitrate, iron, and manganese concentrations are relatively abundant. The data indicate that elevated concentrations of nitrate, iron, and manganese are prevalent in water throughout the surficial aquifer--an aquifer that not only is important in recharging the underlying confined aquifer system, but in supplying drinking water to the majority of Delmarva Peninsula residents. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8934","usgsCitation":"Hamilton, P.A., Shedlock, R.J., and Phillips, P.J., 1989, Ground-water-quality assessment of the Delmarva Peninsula, Delaware, Maryland, and Virginia; analysis of available water-quality data through 1987: U.S. Geological Survey Open-File Report 89-34, vii, 71 p., https://doi.org/10.3133/ofr8934.","productDescription":"vii, 71 p.","numberOfPages":"81","costCenters":[],"links":[{"id":150754,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0034/report-thumb.jpg"},{"id":278845,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0034/report.pdf"}],"country":"United States","state":"Delaware;Maryl;Virginia","otherGeospatial":"Delmarva Peninsula","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.5,29.5 ], [ -76.5,40.0 ], [ -75.0,40.0 ], [ -75.0,29.5 ], [ -76.5,29.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db648588","contributors":{"authors":[{"text":"Hamilton, P. A.","contributorId":7247,"corporation":false,"usgs":true,"family":"Hamilton","given":"P.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":180491,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shedlock, Robert J. rjshedlo@usgs.gov","contributorId":2616,"corporation":false,"usgs":true,"family":"Shedlock","given":"Robert","email":"rjshedlo@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":180490,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Phillips, P. J.","contributorId":31728,"corporation":false,"usgs":true,"family":"Phillips","given":"P.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":180492,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":55719,"text":"wdrNHVT881 - 1989 - Water resources data, New Hampshire and Vermont, Water Year 1988","interactions":[],"lastModifiedDate":"2019-11-06T14:25:38","indexId":"wdrNHVT881","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"NH-VT-88-1","title":"Water resources data, New Hampshire and Vermont, Water Year 1988","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNHVT881","usgsCitation":"Blackey, F., Cotton, J.E., and Denner, J., 1989, Water resources data, New Hampshire and Vermont, Water Year 1988: U.S. Geological Survey Water Data Report NH-VT-88-1, x, 145 p. , https://doi.org/10.3133/wdrNHVT881.","productDescription":"x, 145 p. ","costCenters":[],"links":[{"id":174159,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/2000/nh-vt-88-1/report-thumb.jpg"},{"id":368992,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/2000/nh-vt-88-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Hampshire, Vermont","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.333740234375,\n              42.73894375124377\n            ],\n            [\n              -70.762939453125,\n              42.73894375124377\n            ],\n            [\n              -70.762939453125,\n              45.36758436884978\n            ],\n            [\n              -73.333740234375,\n              45.36758436884978\n            ],\n            [\n              -73.333740234375,\n              42.73894375124377\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0f39","contributors":{"authors":[{"text":"Blackey, F.E.","contributorId":51797,"corporation":false,"usgs":true,"family":"Blackey","given":"F.E.","email":"","affiliations":[],"preferred":false,"id":254108,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cotton, J. E.","contributorId":52976,"corporation":false,"usgs":true,"family":"Cotton","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":254109,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Denner, J.C.","contributorId":75562,"corporation":false,"usgs":true,"family":"Denner","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":254110,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":55716,"text":"wdrND881 - 1989 - Water resources data, North Dakota, water year 1988","interactions":[],"lastModifiedDate":"2020-12-07T18:34:50.657291","indexId":"wdrND881","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"ND-88-1","title":"Water resources data, North Dakota, water year 1988","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrND881","usgsCitation":"Harkness, R., Haffield, N., Ryan, G., and Wesolowski, E.A., 1989, Water resources data, North Dakota, water year 1988: U.S. Geological Survey Water Data Report ND-88-1, xi, 380 p., https://doi.org/10.3133/wdrND881.","productDescription":"xi, 380 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,{"id":30621,"text":"wri884036 - 1989 - Simulation of steady-state ground water and spring flow in the upper Floridan aquifer of coastal Citrus and Hernando Counties, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:09:00","indexId":"wri884036","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4036","title":"Simulation of steady-state ground water and spring flow in the upper Floridan aquifer of coastal Citrus and Hernando Counties, Florida","docAbstract":"A digital groundwater flow model was developed to approximate steady-state predevelopment flow conditions in the Upper Floridan aquifer of coastal west-central Florida. The aquifer is the major source of water and natural spring flow in the area. The aquifer was simulated as a one-layer system with constant vertical recharge and discharge rates. Calibrated transmissivities ranged from 8,640 sq ft/day in the northern part of the area to nearly 13,000,000 sq ft/day near large springs. Calibrated inflows were about 2,708 cu ft/sec; of this, about 2,565 cu ft/sec discharged as natural spring flow and 137 cu ft/sec discharged as upward leakage along the coast. The model was used to show how the system might respond to large manmade stresses. Withdrawal of 116 cu ft/sec from a hypothetical regional well field resulted in potentiometric-surface drawdowns ranging from 0.1 to 1.7 ft and declines of generally less than 0.2 ft along the coast. Total spring flow decreased 5%, and the effect on individual springs varied from 0.1 to 8.0%. Withdrawal of 62 cu ft/sec from the 4-sq-mi node at each spring resulted in six of seven springs to the south of the Chassahowitzka River contributing 50% of their flow to pumpage. Springs located north of the Chassahowitzka River contributed as much as 18% of their flow to pumpage. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nCopies of this report can be purchased from U.S. Geological Survey, Books and Open-File Reports Section,","doi":"10.3133/wri884036","usgsCitation":"Yobbi, D.K., 1989, Simulation of steady-state ground water and spring flow in the upper Floridan aquifer of coastal Citrus and Hernando Counties, Florida: U.S. Geological Survey Water-Resources Investigations Report 88-4036, iv, 33 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884036.","productDescription":"iv, 33 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159879,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4036/report-thumb.jpg"},{"id":59386,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4036/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699d40","contributors":{"authors":[{"text":"Yobbi, D. K.","contributorId":56622,"corporation":false,"usgs":true,"family":"Yobbi","given":"D.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":203554,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30618,"text":"wri884116 - 1989 - Effects of river discharge and high-tide stage on salinity intrusion in the Weeki Wachee, Crystal, and Withlacoochee River estuaries, southwest Florida","interactions":[],"lastModifiedDate":"2023-01-11T19:20:43.62085","indexId":"wri884116","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4116","title":"Effects of river discharge and high-tide stage on salinity intrusion in the Weeki Wachee, Crystal, and Withlacoochee River estuaries, southwest Florida","docAbstract":"<p>The Weeki Wachee, Crystal, and Withlacoochee Rivers are coastal streams flowing into the Gulf of Mexico that may be affected by either future surface water or groundwater withdrawals. Reduction of river discharge will affect the upstream extent of saltwater intrusion in the rivers; however, under certain reduced low-flow discharges, the estimated change in upstream extent of saltwater intrusion is on the order of several tenths of a mile and frequently is within the range of predicted error. Data on flow, tides, and salinity describe the physical characteristics of the Weeki Wachee, Crystal, and Withlacoochee River systems. Vertical and longitudinal salinity profiles indicate that salinity of the rivers increases downstream and varies substantially at any given location. The Weeki Wachee River system is the best mixed of the three. The Crystal River system exhibited the next best mixed system, and the Withlacoochee River system exhibited the most variation in its salinity regime. The daily maximum upstream extent of salinity intrusion is described by multiple linear-regression analysis based on daily mean streamflow of each river and high-tide stage of the gulf. The equations are used to show the effects of discharge on the daily maximum upstream extent of salinity intrusion in the rivers.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884116","usgsCitation":"Yobbi, D.K., and Knochenmus, L.A., 1989, Effects of river discharge and high-tide stage on salinity intrusion in the Weeki Wachee, Crystal, and Withlacoochee River estuaries, southwest Florida: U.S. Geological Survey Water-Resources Investigations Report 88-4116, v, 63 p., https://doi.org/10.3133/wri884116.","productDescription":"v, 63 p.","costCenters":[],"links":[{"id":411726,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47032.htm","linkFileType":{"id":5,"text":"html"}},{"id":59383,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4116/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123856,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4116/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Weekee, Crystal, and Withlacoochee River estuaries","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.75,\n              29.1167\n            ],\n            [\n              -82.75,\n              28.4364\n            ],\n            [\n              -82.4217,\n              28.4364\n            ],\n            [\n              -82.4217,\n              29.1167\n            ],\n            [\n              -82.75,\n              29.1167\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae8ea","contributors":{"authors":[{"text":"Yobbi, D. K.","contributorId":56622,"corporation":false,"usgs":true,"family":"Yobbi","given":"D.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":203549,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knochenmus, L. A.","contributorId":60683,"corporation":false,"usgs":true,"family":"Knochenmus","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":203550,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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