{"pageNumber":"443","pageRowStart":"11050","pageSize":"25","recordCount":16504,"records":[{"id":1827,"text":"wsp2381C - 1994 - Assessment of nonpoint-source contamination of the High Plains Aquifer in south-central Kansas, 1987","interactions":[{"subject":{"id":19293,"text":"ofr91238 - 1992 - Assessment of nonpoint-source contamination of the High Plains Aquifer in south-central Kansas, 1987","indexId":"ofr91238","publicationYear":"1992","noYear":false,"title":"Assessment of nonpoint-source contamination of the High Plains Aquifer in south-central Kansas, 1987"},"predicate":"SUPERSEDED_BY","object":{"id":1827,"text":"wsp2381C - 1994 - Assessment of nonpoint-source contamination of the High Plains Aquifer in south-central Kansas, 1987","indexId":"wsp2381C","publicationYear":"1994","noYear":false,"chapter":"C","title":"Assessment of nonpoint-source contamination of the High Plains Aquifer in south-central Kansas, 1987"},"id":1}],"lastModifiedDate":"2020-04-30T18:36:16.248829","indexId":"wsp2381C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"2381","chapter":"C","title":"Assessment of nonpoint-source contamination of the High Plains Aquifer in south-central Kansas, 1987","docAbstract":"Ground-water quality was assessed in a 5,000-square-mile area of the High Plains aquifer in south-central Kansas that is susceptible to nonpoint-source contamination from agricultural and petroleum-production activities. Of particular interest was the presence of agricultural chemicals and petroleum-derived hydrocarbons that might have been associated with brines that formerly were disposed into unlined ponds. \r\n\r\nRandom sampling of ground water was done within a framework of discrete land-use areas (irrigated cropland, petroleum-production land containing former brine-disposal ponds, and undeveloped rangeland) of 3-10 square miles. Although true baseline water-quality conditions probably are rare, in this region they are represented most closely by ground water in areas of undeveloped rangeland. The sampling design enabled statistical hypothesis testing, using nonparametric procedures, of the effects of land use, unsaturated-zone lithology, and type of well sampled. \r\n\r\nResults indicate that regional ground-water quality has been affected by prevailing land-use activities, as shown by increased concentrations of several inorganic constituents. Ground water beneath irrigated cropland was characterized by significantly larger concentrations of hardness, alkalinity, calcium, magnesium, potassium, fluofide, and nitrite plus nitrate than was water beneath undeveloped rangeland. Few nondegraded pesticides were detected in the aquifer, probably because of degradation and sorption. Atrazine was the most common, but only in small concentrations. round water beneath petroleum-production land was characterized by significantly larger concentrations of hardness, alkalinity, dissolved solids, sodium, and chloride than was water beneath undeveloped rangeland. Nonpoint-source contamination by oil-derived hydrocarbons was not discernible. The occurrences of trace organic compounds were similar between petroleum-production land and undeveloped rangeland, which indicates a natural origin for these compounds. \r\n\r\nThe unsaturated zone in the study area is lithologically heterogeneous and contains substantial amounts of clay that inhibit the downward movement of water and solutes. Within the aquifer, the rate of lateral regional flow and solute transport is slow enough so that the ground-water quality reflects overlying land use in discrete areas of several square miles, but it is still sufficiently rapid so that the type of well sampled is not important in regional characterizations of water quality beneath irrigated cropland; the seasonal pumping of irrigation wells does not appear to divert regional flow enough to cause substantial local anomalies of more mineralized ground water.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2381C","usgsCitation":"Helgesen, J.O., Stullken, L.E., and Rutledge, A.T., 1994, Assessment of nonpoint-source contamination of the High Plains Aquifer in south-central Kansas, 1987: U.S. Geological Survey Water Supply Paper 2381, v, 51 p. , https://doi.org/10.3133/wsp2381C.","productDescription":"v, 51 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":137075,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2381c/report-thumb.jpg"},{"id":27025,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2381c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"South-central Kansas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -101.700439453125,\n              36.98500309285596\n            ],\n            [\n              -96.2841796875,\n              36.98500309285596\n            ],\n            [\n              -96.2841796875,\n              38.8824811975508\n            ],\n            [\n              -101.700439453125,\n              38.8824811975508\n            ],\n            [\n              -101.700439453125,\n              36.98500309285596\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671ef9","contributors":{"authors":[{"text":"Helgesen, John O.","contributorId":101630,"corporation":false,"usgs":true,"family":"Helgesen","given":"John","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":144219,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stullken, Lloyd E.","contributorId":60609,"corporation":false,"usgs":true,"family":"Stullken","given":"Lloyd","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":144218,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rutledge, A. T.","contributorId":38532,"corporation":false,"usgs":true,"family":"Rutledge","given":"A.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":144217,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":29848,"text":"wri944028 - 1994 - Potential effects of the Hawaii Geothermal Project on ground-water resources on the island of Hawaii","interactions":[],"lastModifiedDate":"2019-05-08T09:09:02","indexId":"wri944028","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-4028","title":"Potential effects of the Hawaii Geothermal Project on ground-water resources on the island of Hawaii","docAbstract":"In 1990, the State of Hawaii proposed the Hawaii Geothermal Project for the development of as much as 500 MW of electric power from the geothermal system in the East Rift Zone of Kilauea Volcano. This report uses data from 31 wells and 8 springs to describe the properties of the ground-water system in and adjacent to the East Rift Zone. Potential effects of this project on ground-water resources are also discussed. Data show differences in ground-water chemistry and heads within the study area that appear to be related to mixing of waters of different origins and ground-water impoundment by volcanic dikes. East of Pahoa, the ground-water system within the rift is highly transmissive and receives abundant recharge from precipitation; therefore, the pumping of freshwater to support geothermal development in that part of the rift zone would have a minimal effect on ground-water levels. To the southwest of Pahoa, dike impoundment reduces the transmissivity of the ground-water system to such an extent that wells might not be capable of supplying sufficient fresh water to support geothermal operations. Contamination of ground-water resources by accidental release of geothermal fluids into shallow aquifers is possible because of corrosive conditions in the geothermal wells, potential well blowouts, and high ground-water velocities in parts of the region. Hydrologic monitoring of water level, temperature, and chemistry in observation wells should continue throughout development of geothermal resources for the Hawaii Geothermal Project for early detection of leakage and migration of geothermal fluids within the groundwater system.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944028","usgsCitation":"Sorey, M., and Colvard, E., 1994, Potential effects of the Hawaii Geothermal Project on ground-water resources on the island of Hawaii: U.S. Geological Survey Water-Resources Investigations Report 94-4028, vi, 35 p., https://doi.org/10.3133/wri944028.","productDescription":"vi, 35 p.","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":58657,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4028/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123942,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4028/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c242","contributors":{"authors":[{"text":"Sorey, M.L.","contributorId":73185,"corporation":false,"usgs":true,"family":"Sorey","given":"M.L.","affiliations":[],"preferred":false,"id":202235,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Colvard, E.M.","contributorId":83553,"corporation":false,"usgs":true,"family":"Colvard","given":"E.M.","affiliations":[],"preferred":false,"id":202236,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16961,"text":"ofr94129 - 1994 - Chemical analyses of ground and surface water from Battle Brook drainage basin, near Princeton, Minnesota","interactions":[],"lastModifiedDate":"2019-12-08T13:56:43","indexId":"ofr94129","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-129","title":"Chemical analyses of ground and surface water from Battle Brook drainage basin, near Princeton, Minnesota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr94129","usgsCitation":"Wanty, R., Tuttle, M.L., Böhlke, J., and Briggs, P., 1994, Chemical analyses of ground and surface water from Battle Brook drainage basin, near Princeton, Minnesota: U.S. Geological Survey Open-File Report 94-129, 25 p. , https://doi.org/10.3133/ofr94129.","productDescription":"25 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":149349,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0129/report-thumb.jpg"},{"id":46072,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0129/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","county":"Mille Lacs County, Sherburne County","city":"Princeton","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-93.8105,46.2412],[-93.4286,46.2443],[-93.428,46.1541],[-93.4321,45.9815],[-93.5212,45.9801],[-93.5133,45.7335],[-93.5106,45.5598],[-93.5093,45.4163],[-93.5138,45.2454],[-93.5158,45.2458],[-93.5216,45.2467],[-93.5235,45.2477],[-93.5261,45.249],[-93.5255,45.2513],[-93.5274,45.2541],[-93.5307,45.2545],[-93.5378,45.2554],[-93.5404,45.2563],[-93.5443,45.2595],[-93.5501,45.265],[-93.5534,45.2691],[-93.554,45.2732],[-93.5547,45.2824],[-93.5566,45.286],[-93.5592,45.2892],[-93.5624,45.2915],[-93.5644,45.2938],[-93.5657,45.297],[-93.5657,45.2984],[-93.5683,45.2988],[-93.5709,45.2979],[-93.5715,45.2961],[-93.5728,45.2929],[-93.5767,45.2924],[-93.5832,45.2924],[-93.5961,45.2924],[-93.6065,45.2929],[-93.6123,45.2933],[-93.6188,45.2947],[-93.6246,45.2951],[-93.6324,45.2942],[-93.6363,45.2951],[-93.6408,45.2969],[-93.6454,45.2969],[-93.6493,45.2969],[-93.6538,45.2969],[-93.6583,45.2965],[-93.6629,45.2965],[-93.6674,45.296],[-93.6726,45.2964],[-93.6765,45.2978],[-93.6791,45.2996],[-93.6804,45.3014],[-93.6823,45.3028],[-93.683,45.3037],[-93.6843,45.3046],[-93.6856,45.3051],[-93.6869,45.3046],[-93.6882,45.3042],[-93.6901,45.3042],[-93.6927,45.3028],[-93.694,45.3014],[-93.6953,45.3001],[-93.6966,45.2996],[-93.7011,45.2991],[-93.705,45.2987],[-93.7082,45.2973],[-93.7134,45.2964],[-93.7167,45.2973],[-93.7212,45.2996],[-93.7264,45.3018],[-93.7283,45.3018],[-93.7303,45.3023],[-93.7322,45.3027],[-93.7355,45.3023],[-93.7387,45.3018],[-93.7413,45.3009],[-93.7439,45.3],[-93.7497,45.2977],[-93.753,45.2972],[-93.7594,45.2972],[-93.7614,45.2972],[-93.7633,45.2977],[-93.7659,45.2986],[-93.7698,45.3004],[-93.7737,45.3027],[-93.7789,45.3045],[-93.7841,45.3072],[-93.7899,45.309],[-93.7964,45.3108],[-93.801,45.3122],[-93.8062,45.3145],[-93.8107,45.3172],[-93.8133,45.3204],[-93.8179,45.3245],[-93.8205,45.3259],[-93.8224,45.3277],[-93.827,45.3304],[-93.8289,45.3322],[-93.8309,45.335],[-93.8322,45.3368],[-93.8342,45.3372],[-93.8374,45.3377],[-93.8407,45.3382],[-93.8445,45.3386],[-93.8497,45.3381],[-93.8549,45.3386],[-93.8601,45.3395],[-93.866,45.3413],[-93.8764,45.3449],[-93.8815,45.3476],[-93.8855,45.3508],[-93.8868,45.3526],[-93.8874,45.3545],[-93.89,45.3572],[-93.8907,45.3609],[-93.8914,45.3631],[-93.894,45.365],[-93.8953,45.3654],[-93.8979,45.3668],[-93.9018,45.3681],[-93.9057,45.37],[-93.9102,45.3718],[-93.9115,45.3731],[-93.9122,45.3754],[-93.9129,45.3782],[-93.9135,45.3809],[-93.9155,45.3818],[-93.9194,45.3836],[-93.9246,45.3859],[-93.9285,45.3863],[-93.9311,45.3854],[-93.9337,45.3845],[-93.9376,45.3845],[-93.946,45.3849],[-93.9479,45.384],[-93.9505,45.3821],[-93.9538,45.3789],[-93.9557,45.378],[-93.9583,45.378],[-93.9609,45.3798],[-93.9648,45.3826],[-93.9707,45.3871],[-93.9739,45.3894],[-93.9759,45.3898],[-93.9778,45.3912],[-93.9811,45.3935],[-93.9831,45.3957],[-93.9844,45.398],[-93.9876,45.3998],[-93.9909,45.4017],[-93.9948,45.4016],[-93.9993,45.4007],[-94.0045,45.4007],[-94.0052,45.4007],[-94.0058,45.4016],[-94.0071,45.4021],[-94.0104,45.402],[-94.0143,45.4025],[-94.0162,45.4025],[-94.0201,45.4029],[-94.0227,45.4043],[-94.026,45.4066],[-94.0299,45.4093],[-94.0338,45.4129],[-94.0371,45.4166],[-94.041,45.4207],[-94.0456,45.4261],[-94.0463,45.4275],[-94.0482,45.4307],[-94.0502,45.4334],[-94.0522,45.4339],[-94.0548,45.4329],[-94.0612,45.4311],[-94.0625,45.432],[-94.0652,45.4343],[-94.0684,45.4365],[-94.0717,45.4365],[-94.0756,45.437],[-94.0769,45.4397],[-94.0769,45.4434],[-94.0789,45.4452],[-94.0835,45.447],[-94.0893,45.4479],[-94.0939,45.4492],[-94.0971,45.452],[-94.0991,45.4547],[-94.0998,45.4579],[-94.0985,45.4625],[-94.0992,45.4657],[-94.1018,45.4693],[-94.1064,45.472],[-94.1084,45.4743],[-94.1136,45.477],[-94.1188,45.4797],[-94.1267,45.4847],[-94.1293,45.4861],[-94.1332,45.4884],[-94.1365,45.4915],[-94.1371,45.4934],[-94.1398,45.4961],[-94.1411,45.4979],[-94.1411,45.5016],[-94.1412,45.5034],[-94.1418,45.5043],[-94.1412,45.5075],[-94.1386,45.5107],[-94.1387,45.5144],[-94.1393,45.518],[-94.1439,45.5231],[-94.1472,45.5281],[-94.1466,45.5331],[-94.1442,45.5482],[-94.1436,45.5537],[-94.1475,45.5591],[-94.0148,45.5602],[-93.9999,45.5589],[-93.7598,45.5604],[-93.7641,45.8202],[-93.7667,45.9812],[-93.8099,45.9812],[-93.8107,46.1551],[-93.8105,46.2412]]]},\"properties\":{\"name\":\"Mille Lacs\",\"state\":\"MN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4b04","contributors":{"authors":[{"text":"Wanty, R. B. 0000-0002-2063-6423","orcid":"https://orcid.org/0000-0002-2063-6423","contributorId":66704,"corporation":false,"usgs":true,"family":"Wanty","given":"R. B.","affiliations":[],"preferred":false,"id":174335,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tuttle, M. L.","contributorId":71992,"corporation":false,"usgs":true,"family":"Tuttle","given":"M.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":174336,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Böhlke, J.K. 0000-0001-5693-6455","orcid":"https://orcid.org/0000-0001-5693-6455","contributorId":96696,"corporation":false,"usgs":true,"family":"Böhlke","given":"J.K.","affiliations":[],"preferred":false,"id":174337,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Briggs, Paul H.","contributorId":107691,"corporation":false,"usgs":true,"family":"Briggs","given":"Paul H.","affiliations":[],"preferred":false,"id":174338,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":29991,"text":"wri934146 - 1994 - Hydrogeologic characterization of a proposed landfill expansion in Pickens County near Easley, South Carolina","interactions":[],"lastModifiedDate":"2023-03-24T20:22:07.958157","indexId":"wri934146","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"93-4146","title":"Hydrogeologic characterization of a proposed landfill expansion in Pickens County near Easley, South Carolina","docAbstract":"This report presents the results of a hydrogeologic study in the Piedmont physiographic province of South Carolina to obtain geologic, hydrologic, and water-quality data from the site of a proposed landfill expansion in Pickens County near Easley, South Carolina.  The geology of the study area is typical of the Piedmont region.  The unconsolidated regolith on the site is soil and saprolite, which is a product of the weathered parent rock.  The soil ranges in thickness from about 5 to 20 feet.  The saprolite ranges in thickness from about 5 to 134 feet.  The most abundant parent rock type in the area is a biotite gneiss.  Ground- and surface-water data were collected at the site.  Slug tests on the saprolite indicate a mean hydraulic conductivity of 3 x 0.000003 feet per second.  Transmissivity ranges from 12 to 27 cubic feet per day per feet (squared per day).  The ground-water velocity for the site ranges from 3 to 6 feet per year.  The closest major stream to the site is Golden Creek. Based on low-flow data for Golden Creek, the estimated minimum 7 consecutive day flow that has a recurrence interval of 10 years (7Q10) at station 02186102 is 2.4 cubic feet per second. Water samples were collected from five monitoring wells at the proposed landfill expansion site and from one stream adjacent to the expansion site. Measured pH units ranged from 5.5 to 8.1, and alkalinity concentrations ranged from 5.1 to 73 milligrams per liter as CaCO3.  Other water- quality data obtained included temperature and specific conductance, and 5-day BOD (biochemical oxygen demand), bicarbonate, ammonia-nitrogen, nitrite-nitrogen, nitrite plus nitrate, organic carbon, calcium, magnesium, sodium, potassium, chloride, sulfate, fluoride, and selected trace metal concentrations.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri934146","usgsCitation":"Stringfield, W.J., 1994, Hydrogeologic characterization of a proposed landfill expansion in Pickens County near Easley, South Carolina: U.S. Geological Survey Water-Resources Investigations Report 93-4146, iv, 28 p., https://doi.org/10.3133/wri934146.","productDescription":"iv, 28 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":414741,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47848.htm","linkFileType":{"id":5,"text":"html"}},{"id":58799,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4146/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123544,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4146/report-thumb.jpg"}],"country":"United States","state":"South Carolina","county":"Pickens County","city":"Easley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.6689,\n              34.8292\n            ],\n            [\n              -82.6689,\n              34.8206\n            ],\n            [\n              -82.6583,\n              34.8206\n            ],\n            [\n              -82.6583,\n              34.8292\n            ],\n            [\n              -82.6689,\n              34.8292\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628b5d","contributors":{"authors":[{"text":"Stringfield, W. J.","contributorId":73236,"corporation":false,"usgs":true,"family":"Stringfield","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":202490,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19114,"text":"ofr94347 - 1994 - Plan of study to determine the effect of changes in herbicide use on herbicide concentrations in Midwestern streams, 1989-94","interactions":[],"lastModifiedDate":"2019-12-17T07:05:33","indexId":"ofr94347","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-347","title":"Plan of study to determine the effect of changes in herbicide use on herbicide concentrations in Midwestern streams, 1989-94","docAbstract":"<p>An approach was developed to determine if recent changes in the use of herbicides has affected herbicide concentrations in Midwestern streams. This approach also provides a plan to determine if the abnormally high rainfall and flooding in 1993 has an effect on nitrate concentrations in 1994 in streams that flooded in 1993. The approach involves sampling 53 stream sites, 50 of which were sampled in 1989 and 1990 as part of a reconnaissance to determine the geographic and seasonal distribution of herbicides in 10 Midwestern States. Sites will be sampled twice, once prior to application of herbicides, in March or early April, and once during the first runoff event after application of herbicides. Samples will be analyzed for 11 herbicide and 2 atrazine metabolites by gas chromatography/mass spectrometry. Samples will also be analyzed for ESA (an alachlor metabolite), two cyanazine metabolites, and nutrients.</p>\n<br/>\n<p>Changes to the manufacturers' label have decreased the maximum recommended \napplication rate for atrazine on com and sorghum by about 50 percent since the 1989-90 study. Conversely, the use of other herbicides, such as cyanazine, has increased by more than 25 percent since 1989. Statistical procedures such as Wilcoxon signed rank tests for paired samples will be used to determine if the distributions of herbicide and nitrate concentrations in 1994 are different from those measured in 1989 and 1990.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/ofr94347","usgsCitation":"Goolsby, D.A., Boyer, L.L., and Battaglin, W.A., 1994, Plan of study to determine the effect of changes in herbicide use on herbicide concentrations in Midwestern streams, 1989-94: U.S. Geological Survey Open-File Report 94-347, iv, 14 p., https://doi.org/10.3133/ofr94347.","productDescription":"iv, 14 p.","numberOfPages":"19","temporalStart":"1989-01-01","temporalEnd":"1994-12-31","costCenters":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":279464,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0347/report.pdf"},{"id":150695,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0347/report-thumb.jpg"}],"country":"United States","state":"Illinois, Indiana, Iowa, Kansas, Michigan, Minnesota, Missouri, Nebraska, North Dakota, Ohio, South Dakota, Wisconsin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.08,35.98 ], [ -104.08,49.5 ], [ -80.42,49.5 ], [ -80.42,35.98 ], [ -104.08,35.98 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db6844de","contributors":{"authors":[{"text":"Goolsby, Donald A.","contributorId":46083,"corporation":false,"usgs":true,"family":"Goolsby","given":"Donald","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":180327,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boyer, Laurie L.","contributorId":74399,"corporation":false,"usgs":true,"family":"Boyer","given":"Laurie","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":180328,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Battaglin, William A. 0000-0001-7287-7096 wbattagl@usgs.gov","orcid":"https://orcid.org/0000-0001-7287-7096","contributorId":1527,"corporation":false,"usgs":true,"family":"Battaglin","given":"William","email":"wbattagl@usgs.gov","middleInitial":"A.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":180326,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":4493,"text":"cir1120D - 1994 - Major ions, nutrients, and trace elements in the Mississippi River near Thebes, Illinois, July through September 1993","interactions":[],"lastModifiedDate":"2019-12-08T13:50:45","indexId":"cir1120D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1120","chapter":"D","title":"Major ions, nutrients, and trace elements in the Mississippi River near Thebes, Illinois, July through September 1993","docAbstract":"<p>Extensive flooding in the upper Mississippi River Basin during summer 1993 had a significant effect on the water quality of the Mississippi River. To evaluate the change in temporal distribution and transport of dissolved constituents in the Mississippi River, six water samples were collected by a discharge-weighted method from July through September 1993 near Thebes, Illinois. Sampling at this location provided water-quality information from the upper Mississippi, the Missouri, and the Illinois River Basins. </p><p>Dissolved major constituents that were analyzed in each of the samples included bicarbonate, calcium (Ca), carbonate (C03), chloride (Cl), dissolved organic carbon, magnesium (Mg), potassium (K), silica NOD, sodium (Na), and sulfate (S04). Dissolved nutrients included ammonium ion (NH4), nitrate (N03), nitrite (N02), and orthophosphate (P04) . Dissolved trace elements included aluminum (Al), arsenic (As), barium (Ba), boron (B), beryllium (Be), bromide (Br), cadmium (Cd), chromium (Cr), cobalt, (Co), copper (Cu), fluoride (F), iron (Fe), lead, lithium (Li), manganese (Mn), mercury (Hg), molybdenum (Mo), nickel (Ni), strontium (Sr), thallium, uranium (U), vanadium (V), and zinc (Zn). Other physical properties of water that were measured included specific conductance, pH and suspended-sediment concentration (particle size, less than 63 micrometers). </p><p>Results of this study indicated that large quantities of dissolved constituents were transported through the river system. Generally, pH, alkalinity, and specific conductance and the concentrations of B, Br, Ca, Cl, Cr, K, Li, Mg, Mo, Na, S04, Sr, U, and V increased as water discharge decreased, while concentrations of F, Hg, and suspended sediment sharply decreased as water discharge decreased after the crest of the flood. Concentrations of other constituents, such as Al, As, Ba, Be, Co, Cu, Ni, N03, N02, NH4, P04, and Si02, varied with time as discharge decreased after the crest of the flood. </p><p>For most constituents, the load transported during floods generally is much greater than that transported during low-flow conditions. How ever, for Cd, Cr, Fe, Mn, V, and Zn, loads increased substantially as water discharge decreased after the crest of the flood. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/cir1120D","usgsCitation":"Taylor, H.E., Antweiler, R.C., Brinton, T.I., Roth, D.A., and Moody, J.A., 1994, Major ions, nutrients, and trace elements in the Mississippi River near Thebes, Illinois, July through September 1993: U.S. Geological Survey Circular 1120, v, 21 p., https://doi.org/10.3133/cir1120D.","productDescription":"v, 21 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":538,"rank":100,"type":{"id":15,"text":"Index 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,{"id":25961,"text":"wri924046 - 1994 - Geohydrology and simulated ground-water flow in an irrigated area of northwestern Indiana","interactions":[],"lastModifiedDate":"2016-05-09T10:57:36","indexId":"wri924046","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"92-4046","title":"Geohydrology and simulated ground-water flow in an irrigated area of northwestern Indiana","docAbstract":"<p>Water for irrigation in parts of Newton and Jasper Counties and adjacent areas of northwestern Indiana is pumped mostly from the carbonate- bedrock aquifer that underlies glacial drift. To help in managing the ground-water resources of the area, a three-dimensional ground-water model was developed and tested with hydrologic data collected during 1986 and 1988. Two major aquifers and a confining unit were identified. The surficial unconfined outwash aquifer consists of sand and some gravel. Saturated thickness averages about 30 feet. Estimated values of horizontal hydraulic conductivity and storage coefficient are 350 feet per day and 0.07, respectively. The generally continuous confining unit beneath the outwash aquifer is composed predominantly of till and lacustrine silt and clay and is 0 to 125 feet thick. The carbonate-bedrock aquifer is composed of Silurian and Devonian dolomitic limestone; dolomite and has a median transmissivity of 2,000 feet squared per day. A nine-layer digital model was developed to simulate flow in the ground-water system. The mean absolute errors for simulated water levels in the bedrock aquifer ranged from 5 to 7 feet for two recent periods of irrigation. The component of the flow system that most affects water-level drawdowns in the bedrock aquifer is the confining unit which controls the rate of leakage to the bedrock aquifer. The model is most accurate in areas for which data for confining-unit thickness and bedrock water levels are available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/wri924046","collaboration":"INDIANA DEPARTMENT OF NATURAL RESOURCES","usgsCitation":"Arihood, L.D., and Basch, M., 1994, Geohydrology and simulated ground-water flow in an irrigated area of northwestern Indiana: U.S. Geological Survey Water-Resources Investigations Report 92-4046, v, 38 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri924046.","productDescription":"v, 38 p. :ill., maps ;28 cm.","startPage":"1","endPage":"38","numberOfPages":"43","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":54711,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4046/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118978,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4046/report-thumb.jpg"}],"country":"United States","state":"Indiana","county":"Jasper, Newton","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.92108154296875,\n              41.24064190269477\n            ],\n            [\n              -86.9183349609375,\n              40.901057866884024\n            ],\n            [\n              -86.97052001953125,\n              40.901057866884024\n            ],\n            [\n              -86.96914672851562,\n              40.83563216247778\n            ],\n            [\n              -87.07901000976562,\n              40.831475967182925\n            ],\n            [\n              -87.07901000976562,\n              40.72956780913899\n            ],\n            [\n              -87.53082275390625,\n              40.730608477796636\n            ],\n            [\n              -87.5225830078125,\n              41.20655580884106\n            ],\n            [\n              -87.28225708007812,\n              41.225150426206326\n            ],\n            [\n              -87.2149658203125,\n              41.261291493919856\n            ],\n            [\n              -87.14080810546875,\n              41.3025710943056\n            ],\n            [\n              -87.099609375,\n              41.30050773444147\n            ],\n            [\n              -87.03506469726562,\n              41.272645986935586\n            ],\n            [\n              -86.978759765625,\n              41.24270715552139\n            ],\n            [\n              -86.92245483398438,\n              41.24787000204815\n            ],\n            [\n              -86.92108154296875,\n              41.24064190269477\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8c78","contributors":{"authors":[{"text":"Arihood, L. 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,{"id":18713,"text":"ofr94310 - 1994 - Overview of environmental and hydrogeologic conditions at Moses Point, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:07:24","indexId":"ofr94310","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-310","title":"Overview of environmental and hydrogeologic conditions at Moses Point, Alaska","docAbstract":"The Federal Aviation Administration facility at Moses Point is located at the mouth of the Kwiniuk River on the Seward Peninsula in northwestern Alaska. This area has long cold winters and short summers which affect the hydrology of the area. The Federal Aviation Administration owns or operates airport support facilities at the Moses Point site and wishes to consider the subsistence lifestyles of area residents and the quality of the current environment when evaluating options for remediation of environmental contamination at their facilities. Currently no operating wells are in the area, but the vulnerability of the aquifer and other alternative water supplies are being evaluated because the Federal Aviation Administration has a potential liability for the storage and use of hazardous materials in the area.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94310","usgsCitation":"Dorava, J., Ayres, R., and Sisco, W., 1994, Overview of environmental and hydrogeologic conditions at Moses Point, Alaska: U.S. Geological Survey Open-File Report 94-310, iv, 11 p. :maps ;28 cm., https://doi.org/10.3133/ofr94310.","productDescription":"iv, 11 p. :maps ;28 cm.","costCenters":[],"links":[{"id":150971,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0310/report-thumb.jpg"},{"id":48072,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0310/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a318","contributors":{"authors":[{"text":"Dorava, J.M.","contributorId":68756,"corporation":false,"usgs":true,"family":"Dorava","given":"J.M.","affiliations":[],"preferred":false,"id":179607,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ayres, R.P.","contributorId":84782,"corporation":false,"usgs":true,"family":"Ayres","given":"R.P.","email":"","affiliations":[],"preferred":false,"id":179608,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sisco, W.C.","contributorId":100874,"corporation":false,"usgs":true,"family":"Sisco","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":179609,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":17729,"text":"ofr9482 - 1994 - Studies of the San Francisco Bay, California, estuarine ecosystem: Pilot regional monitoring program results, 1993","interactions":[],"lastModifiedDate":"2020-04-12T14:11:52.249972","indexId":"ofr9482","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-82","title":"Studies of the San Francisco Bay, California, estuarine ecosystem: Pilot regional monitoring program results, 1993","docAbstract":"<p>Water samples were collected in the San Francisco Bay estuary during 22 cruises from January through December 1993. Conductivity, temperature, light attenuation, turbidity, oxygen, and in-vivo fluorescence were measured 1ongitudinally and vertically in the main channel of the estuary from south of the Dumbarton Bridge in the southern part of the bay to Rio Vista on the Sacramento River. Discrete water samples were analyzed for chlorophyll a, phaeopigments, suspended particulate matter, and dissolved oxygen. Water density was calculated from values for salinity, temperature, and pressure (depth), and is included in the data summaries. Photosynthetic parameters, water column respiration, and phytoplankton species abundance and cell volume were determined at selected stations every other month.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr9482","usgsCitation":"Caffrey, J., Cole, B., Cloern, J., Rudek, J., Tyler, A., and Jassby, A., 1994, Studies of the San Francisco Bay, California, estuarine ecosystem: Pilot regional monitoring program results, 1993: U.S. Geological Survey Open-File Report 94-82, iv, 411 p. , https://doi.org/10.3133/ofr9482.","productDescription":"iv, 411 p. ","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":46950,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0082/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150555,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0082/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.9974365234375,\n              37.391981943533544\n            ],\n            [\n              -121.79992675781249,\n              37.391981943533544\n            ],\n            [\n              -121.79992675781249,\n              38.29424797320529\n            ],\n            [\n              -122.9974365234375,\n              38.29424797320529\n            ],\n            [\n              -122.9974365234375,\n              37.391981943533544\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699dc0","contributors":{"authors":[{"text":"Caffrey, J.M.","contributorId":98750,"corporation":false,"usgs":true,"family":"Caffrey","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":177624,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cole, B.E.","contributorId":66268,"corporation":false,"usgs":true,"family":"Cole","given":"B.E.","email":"","affiliations":[],"preferred":false,"id":177621,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cloern, J. E.","contributorId":59453,"corporation":false,"usgs":true,"family":"Cloern","given":"J. E.","affiliations":[],"preferred":false,"id":177620,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rudek, J.","contributorId":67904,"corporation":false,"usgs":true,"family":"Rudek","given":"J.","email":"","affiliations":[],"preferred":false,"id":177622,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Tyler, A.C.","contributorId":75169,"corporation":false,"usgs":true,"family":"Tyler","given":"A.C.","email":"","affiliations":[],"preferred":false,"id":177623,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Jassby, A.D.","contributorId":43798,"corporation":false,"usgs":true,"family":"Jassby","given":"A.D.","affiliations":[],"preferred":false,"id":177619,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":18540,"text":"ofr9484 - 1994 - Operation of hydrologic data-collection stations by the U.S. Geological Survey in 1993","interactions":[],"lastModifiedDate":"2012-02-02T00:07:27","indexId":"ofr9484","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-84","title":"Operation of hydrologic data-collection stations by the U.S. Geological Survey in 1993","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr9484","usgsCitation":"Condes de la Torre, A., 1994, Operation of hydrologic data-collection stations by the U.S. Geological Survey in 1993: U.S. Geological Survey Open-File Report 94-84, vii, 53 p. :chiefly ill., maps ;28 cm., https://doi.org/10.3133/ofr9484.","productDescription":"vii, 53 p. :chiefly ill., maps ;28 cm.","costCenters":[],"links":[{"id":150730,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0084/report-thumb.jpg"},{"id":47891,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0084/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af1e4b07f02db6917b4","contributors":{"authors":[{"text":"Condes de la Torre, Alberto","contributorId":73570,"corporation":false,"usgs":true,"family":"Condes de la Torre","given":"Alberto","email":"","affiliations":[],"preferred":false,"id":179304,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18876,"text":"ofr9458 - 1994 - Lithologic descriptions of two cores and ground-water-quality data from five counties in the northeastern part of the coastal plain of South Carolina, 1988 and 1991","interactions":[],"lastModifiedDate":"2017-01-04T12:08:27","indexId":"ofr9458","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-58","title":"Lithologic descriptions of two cores and ground-water-quality data from five counties in the northeastern part of the coastal plain of South Carolina, 1988 and 1991","docAbstract":"This report presents data collected as part of a hydrologic investigation of Darlington, Dillon, Florence, Marion, and Marlboro Counties in the northeastern part of the Coastal Plain of South Carolina. These data include lithologic descriptions of sediment recovered from two continuously cored boreholes and water-quality results for samples collected from 17 existing wells. One continuously cored borehole was drilled near Lake Darpo in the northern part of Darlington County to a total depth of 447 feet below land surface. The other borehole was drilled in Lake City in the south-central part of Florence County to a total depth of 1,090 feet below land surface. Water-quality results presented in this report include specific conductance, dissolved oxygen, temperature, pH, alkalinity, major- and minor-ion chemistry, and hydrogen sulfide.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S. 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F. 0000-0003-2928-9795 wffalls@usgs.gov","orcid":"https://orcid.org/0000-0003-2928-9795","contributorId":60251,"corporation":false,"usgs":true,"family":"Falls","given":"W.","email":"wffalls@usgs.gov","middleInitial":"F.","affiliations":[],"preferred":false,"id":179903,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2439,"text":"wsp2357B - 1994 - Ground-water-quality assessment of the Central Oklahoma Aquifer, Oklahoma; analysis of available water-quality data through 1987","interactions":[{"subject":{"id":20390,"text":"ofr88728 - 1989 - Ground-water quality assessment of the central Oklahoma aquifer, Oklahoma - Analysis of available water-quality data through 1987","indexId":"ofr88728","publicationYear":"1989","noYear":false,"title":"Ground-water quality assessment of the central Oklahoma aquifer, Oklahoma - Analysis of available water-quality data through 1987"},"predicate":"SUPERSEDED_BY","object":{"id":2439,"text":"wsp2357B - 1994 - Ground-water-quality assessment of the Central Oklahoma Aquifer, Oklahoma; analysis of available water-quality data through 1987","indexId":"wsp2357B","publicationYear":"1994","noYear":false,"chapter":"B","title":"Ground-water-quality assessment of the Central Oklahoma Aquifer, Oklahoma; analysis of available water-quality data through 1987"},"id":1}],"lastModifiedDate":"2022-01-24T22:34:26.452319","indexId":"wsp2357B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"2357","chapter":"B","title":"Ground-water-quality assessment of the Central Oklahoma Aquifer, Oklahoma; analysis of available water-quality data through 1987","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"National water-quality assessment - Central Oklahoma aquifer","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp2357B","usgsCitation":"Parkhurst, D.L., Christenson, S.C., and Schlottmann, J.L., 1994, Ground-water-quality assessment of the Central Oklahoma Aquifer, Oklahoma; analysis of available water-quality data through 1987: U.S. Geological Survey Water Supply Paper 2357, viii, 74 p., https://doi.org/10.3133/wsp2357B.","productDescription":"viii, 74 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":394792,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25488.htm"},{"id":28509,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2357b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138622,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2357b/report-thumb.jpg"}],"country":"United States","state":"Oklahoma","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.675,\n              34.9320\n            ],\n            [\n              -96.767,\n              34.9320\n            ],\n            [\n              -96.767,\n              36\n            ],\n            [\n              -97.675,\n              36\n            ],\n            [\n              -97.675,\n              34.9320\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a1f5","contributors":{"authors":[{"text":"Parkhurst, David L. 0000-0003-3348-1544 dlpark@usgs.gov","orcid":"https://orcid.org/0000-0003-3348-1544","contributorId":1088,"corporation":false,"usgs":true,"family":"Parkhurst","given":"David","email":"dlpark@usgs.gov","middleInitial":"L.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":145205,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Christenson, Scott C. schris@usgs.gov","contributorId":980,"corporation":false,"usgs":true,"family":"Christenson","given":"Scott","email":"schris@usgs.gov","middleInitial":"C.","affiliations":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"preferred":true,"id":145204,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schlottmann, Jamie L.","contributorId":8830,"corporation":false,"usgs":true,"family":"Schlottmann","given":"Jamie","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":145206,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26974,"text":"wri944018 - 1994 - Development of historic and synthesized unregulated streamflow for the James River in North Dakota and South Dakota, 1983-91","interactions":[],"lastModifiedDate":"2018-03-07T16:24:05","indexId":"wri944018","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-4018","title":"Development of historic and synthesized unregulated streamflow for the James River in North Dakota and South Dakota, 1983-91","docAbstract":"<p>Operation of the Garrison Diversion Unit may have some affect on the hydrology of the James River in North Dakota and South Dakota. The Garrison Diversion Unit Monthly Operations Model was developed to analyze a wide range of streamflow conditions that could occur in the James River Basin. The purpose of this study was to compute monthly streamflows that are required as input to the model.</p><p>Historic streamflow data were complied and record extension methods were used, when necessary, to compute monthly streamflow for 1983-91 for 15 gaging stations on the James River in North Dakota and South Dakota. The record extension methods used include Maintenance of Variance Extension Type 1, Ordinary Least Squares, and drainage-area ratio. </p><p>In addition to the historic streamflow, synthesized unregulated streamflow was computed for the 15 gaging stations on the James River for 1983-91 by eliminating the effects of Jamestown Reservoir, Pipestem Reservoir, Sand Lake National Wildlife Refuge, consumptive surface-water withdrawals, and wastewater withdrawals. Maintenance of Variance Extension Type 1, Ordinary Least Squares regression, water-balance procedures, and drainage-area ratio method were used to compute the unregulated streamflows.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944018","usgsCitation":"Emerson, D.G., and Niehus, C.A., 1994, Development of historic and synthesized unregulated streamflow for the James River in North Dakota and South Dakota, 1983-91: U.S. Geological Survey Water-Resources Investigations Report 94-4018, iv, 33 p., https://doi.org/10.3133/wri944018.","productDescription":"iv, 33 p.","numberOfPages":"38","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":119011,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4018/report-thumb.jpg"},{"id":55862,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4018/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Dakota, South Dakota","otherGeospatial":"James River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -100,\n              42.84777884235988\n            ],\n            [\n              -97.2344970703125,\n              42.84777884235988\n            ],\n            [\n              -97.2344970703125,\n              48\n            ],\n            [\n              -100,\n              48\n            ],\n            [\n              -100,\n              42.84777884235988\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65dec8","contributors":{"authors":[{"text":"Emerson, Douglas G.","contributorId":40579,"corporation":false,"usgs":true,"family":"Emerson","given":"Douglas","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":197344,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Niehus, Colin A.","contributorId":86815,"corporation":false,"usgs":true,"family":"Niehus","given":"Colin","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":197345,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27986,"text":"wri934187 - 1994 - Geohydrology and ground-water quality in the vicinity of a ground-water-contamination site in Rockford, Illinois","interactions":[],"lastModifiedDate":"2023-04-10T20:38:27.710172","indexId":"wri934187","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"93-4187","title":"Geohydrology and ground-water quality in the vicinity of a ground-water-contamination site in Rockford, Illinois","docAbstract":"<p>A geohydrologic investigation was performed by the U.S. Geological Survey, in cooperation with the U.S. Environmental Protection Agency, to determine the distribution of volatile organic compounds in a fractured-rock aquifer near the Southeast Rockford Groundwater Contamination Site in Rockford, Ill. The geologic units of concern are the St. Peter Sandstone and Glenwood Formation; the dolomites of the Platteville and Galena Groups of Ordovician age; and the sands, gravels, silts, and clays of Quaternary age. The hydraulic units of concern are the unconsolidated aquifer, composed of sand and gravel; the fractured- dolomite aquifer, composed of the Galena and Platteville Groups and the dolomitic sections of the Glenwood Formation; and the sandstone aquifer, composed of the St. Peter Sandstone and the sandstone beds in the Glenwood Formation. The dolomite aquifer is well connected hydraulically to the overlying unconsolidated aquifer and the underlying sandstone aquifer. Caliper and acoustic-televiewer logs show several subhorizontal fractures in the dolomite that can be correlated throughout the study area. Comparison of televiewer and flowmeter logs indicates that most of the flow in the dolomite aquifer is through these fractures. Ground-water flow through two of the fractures can be correlated over large parts of the study area. Volatile organic compounds, in concentrations exceeding 2,000 micrograms per liter, were detected within the entire thickness of the dolomite aquifer where flow is measurable. Volatile organic compounds were detected in an area of the aquifer where they were thought to be absent in previous investigations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri934187","usgsCitation":"Kay, R., Prinos, S., and Paillet, F.L., 1994, Geohydrology and ground-water quality in the vicinity of a ground-water-contamination site in Rockford, Illinois: U.S. Geological Survey Water-Resources Investigations Report 93-4187, iv, 28 p., https://doi.org/10.3133/wri934187.","productDescription":"iv, 28 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":415538,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47881.htm","linkFileType":{"id":5,"text":"html"}},{"id":123861,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4187/report-thumb.jpg"},{"id":56809,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4187/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Illinois","city":"Rockford","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -89.1,\n              42.2417\n            ],\n            [\n              -89.1,\n              42.225\n            ],\n            [\n              -89,\n              42.225\n            ],\n            [\n              -89,\n              42.2417\n            ],\n            [\n              -89.1,\n              42.2417\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db6360fa","contributors":{"authors":[{"text":"Kay, R.T.","contributorId":72026,"corporation":false,"usgs":true,"family":"Kay","given":"R.T.","email":"","affiliations":[],"preferred":false,"id":199015,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Prinos, S. T.","contributorId":97537,"corporation":false,"usgs":true,"family":"Prinos","given":"S. T.","affiliations":[],"preferred":false,"id":199016,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Paillet, Frederick L.","contributorId":63820,"corporation":false,"usgs":true,"family":"Paillet","given":"Frederick","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":199014,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":18249,"text":"ofr9435 - 1994 - Water resources on and near Indian lands in northeastern Kansas and southeastern Nebraska; hydrologic data through 1990","interactions":[],"lastModifiedDate":"2012-02-02T00:07:26","indexId":"ofr9435","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-35","title":"Water resources on and near Indian lands in northeastern Kansas and southeastern Nebraska; hydrologic data through 1990","docAbstract":"Four Kansas Indian Tribes, the Iowa, Kickapoo, Potawatomi, and Sac &amp; Fox are interested in developing the water resources on and near their respective tribe lands. This report presents climatic and geohydrologic data that are useful in describing the available water resources in the 4,005-square-mile area in northeastern Kansas and southeastern Nebraska. Climatological data for 1961- 90 include monthly summaries of average temperature, heating degree days, precipitation for the climato- logical stations in Horton and Topeka, Kansas, and average temperature and precipitation for the north- east Climatological Region in Kansas. Geohydrologic data include site descriptions for 18 continuous- record streamflow-gaging stations with 10 or more years of daily discharge records, site descriptions for about 1,900 wells, and water-quality data for surface- and ground-water sampling sites in the study area. Water-quality data for surface- and ground-water sites include specific conductance, pH, bacteria concentrations, hardness, dissolved solids, nutrients, dissolved and total metals, and concen- trations for selected pesticides and other organic substances.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr9435","usgsCitation":"Brewer, L., Trombley, T.J., and Pomes, M., 1994, Water resources on and near Indian lands in northeastern Kansas and southeastern Nebraska; hydrologic data through 1990: U.S. Geological Survey Open-File Report 94-35, vi, 424 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr9435.","productDescription":"vi, 424 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":150803,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0035/report-thumb.jpg"},{"id":47605,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0035/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa560","contributors":{"authors":[{"text":"Brewer, L.D.","contributorId":97513,"corporation":false,"usgs":true,"family":"Brewer","given":"L.D.","email":"","affiliations":[],"preferred":false,"id":178779,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trombley, T. J.","contributorId":75161,"corporation":false,"usgs":true,"family":"Trombley","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":178777,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pomes, M.L.","contributorId":84393,"corporation":false,"usgs":true,"family":"Pomes","given":"M.L.","affiliations":[],"preferred":false,"id":178778,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":28851,"text":"wri934212 - 1994 - Hydrogeology and hydrologic system of Pinal Creek Basin, Gila County, Arizona","interactions":[],"lastModifiedDate":"2019-12-08T13:28:48","indexId":"wri934212","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"93-4212","title":"Hydrogeology and hydrologic system of Pinal Creek Basin, Gila County, Arizona","docAbstract":"Acidic water that contains elevated concentrations of metals has contaminated a stream and alluvial aquifer in a mining district near Globe, Arizona. The contaminated aquifer is a narrow layer of unconsolidated alluvium along Miami Wash and Pinal Creek.  The alluvium overlies basin fill, which extends throughout most of the Pinal Creek basin. The alluvium and basin fill compose the primary aquifer in the basin.  Horizontal hydraulic con- ductivities were estimated at about 200 meters per day in the alluvium, and average linear ground- water flow velocities are about 5 meters per day. Water levels in the aquifer respond rapidly to periods of extended runoff in the basin and variable rates of ground-water pumping. Fluctuations of as much as 2.5 meters in 6 months have been measured.  Ground-water levels were near record highs during spring 1985 and declined as much as 13 meters by spring 1989.  Measured hydraulic gradients indicate that flow is generally upward from the basin fill to the alluvium.  From 1980 to 1984, seepage of 155 liters per second from Webster Lake and 279 liters per second streamflow infiltration were estimated to be the two largest sources of inflow to the regional aquifer.  Major outflows from the aquifer were 166 liters per second of pumpage and 240 liters per second of natural ground-water discharge to Pinal Creek.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri934212","usgsCitation":"Neaville, C., and Brown, J.G., 1994, Hydrogeology and hydrologic system of Pinal Creek Basin, Gila County, Arizona: U.S. Geological Survey Water-Resources Investigations Report 93-4212, v, 32 p., https://doi.org/10.3133/wri934212.","productDescription":"v, 32 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology 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,{"id":2051,"text":"wsp2413 - 1994 - Herbicides and nitrate in near-surface aquifers in the midcontinental United States, 1991","interactions":[],"lastModifiedDate":"2020-04-30T18:41:47.334948","indexId":"wsp2413","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"2413","title":"Herbicides and nitrate in near-surface aquifers in the midcontinental United States, 1991","docAbstract":"<p>The occurrence and distribution of selected herbicides, atrazine metabolites, and nitrate were determined for near-surface aquifers (within 50 feet of land surface) in the corn- and soybean-producing region of the midcontinental United States. The study region included all or parts of Illinois, Indiana, Iowa, Kansas, Michigan, Minnesota, Missouri, Nebraska, North Dakota, Ohio, South Dakota, and Wisconsin. Water samples were collected during the spring and summer of 1991 from 303 wells completed in near-surface unconsolidated and near-surface bedrock aquifers. At least one herbicide or atrazine metabolite was detected in 24 percent of 579 water samples analyzed for herbicides, based on a reporting limit of 0.05 microgram per liter. However, no herbicide concentration exceeded the U.S. Environmental Protection Agency's maximum contaminant levels or health advisory levels for drinking water. The most frequently detected herbicide compound was desethylatrazine, an atrazine metabolite (18.1 percent), followed by atrazine (17.4 percent); deisopropylatrazine, an atrazine metabolite (5.7 percent); prometon (5.0 percent); metolachlor (2.7 percent); alachlor (1.7 percent); simazine (1.0 percent); metribuzin (1.0 percent); and cyanazine (0.7 percent). The herbicides ametryn, prometryn, propazine, and terbutryn were not detected during this study. Nitrate concentrations equal to or greater than 3.0 milligrams per liter (excess nitrate) were detected in 29 percent of the 599 nitrate analyses, and ammonium concentrations equal to or greater than 0.01 milligram per liter were detected in 78 percent of the 584 ammonium analyses. Nitrate concentrations equal to or greater than the U.S. Environmental Protection Agency's maximum contaminant level for drinking water of 10 milligrams per liter were found in 6 percent of the samples.</p>\n<p>The frequency of herbicide detection was, in part, affected by the analytical method's reporting limit. Results from this study show that the frequency of atrazine detection increases as the reporting limit decreases. Herbicide metabolite concentrations are critical to understanding the detection of herbicide residues. The frequency of detection of atrazine residue (atrazine + desethylatrazine + deisopropylatrazine) was 22.1 percent, which was more than the frequency of detection of atrazine alone (17.4 percent).</p>\n<p>Prometon was detected more frequently than every other herbicide except atrazine. The prometon appears to be derived from areas of nonagricultural land use, such as golf courses and residential areas. Herbicides and excess nitrate were both rarely detected in the eastern part of the study region, even though this is an area of intense herbicide and nitrogen-fertilizer use.</p>\n<p>Hydrogeologic factors, land use, agricultural practices, local features, and water chemistry were analyzed for possible relation to herbicide and excess-nitrate detections. Herbicides and excess nitrate were detected more frequently in near-surface unconsolidated aquifers than in nearsurface bedrock aquifers. The depth to the top of the aquifer was inversely related to the frequency of detection of herbicides and excess nitrate. The proximity of streams to sampled wells also affected the frequency of herbicide detection. Significant seasonal differences were determined for the frequency of herbicide detection, but not for the frequency of excess nitrate.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2413","usgsCitation":"Kolpin, D.W., Burkart, M.R., and Thurman, E.M., 1994, Herbicides and nitrate in near-surface aquifers in the midcontinental United States, 1991: U.S. Geological Survey Water Supply Paper 2413, v, 34 p., https://doi.org/10.3133/wsp2413.","productDescription":"v, 34 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology 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Charles A. ckaehler@usgs.gov","contributorId":210,"corporation":false,"usgs":true,"family":"Kaehler","given":"Charles","email":"ckaehler@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":144515,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hsieh, Paul A. 0000-0003-4873-4874 pahsieh@usgs.gov","orcid":"https://orcid.org/0000-0003-4873-4874","contributorId":1634,"corporation":false,"usgs":true,"family":"Hsieh","given":"Paul","email":"pahsieh@usgs.gov","middleInitial":"A.","affiliations":[{"id":39113,"text":"WMA - Office of Quality Assurance","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":144516,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29269,"text":"wri924182 - 1994 - Ground-water resources of southern Tangipahoa Parish and adjacent areas, Louisiana","interactions":[],"lastModifiedDate":"2012-02-02T00:08:35","indexId":"wri924182","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"92-4182","title":"Ground-water resources of southern Tangipahoa Parish and adjacent areas, Louisiana","docAbstract":"Groundwater resources in southern Tangipahoa Parish and adjacent areas were studied to determine their potential for development as an alternative to the Mississippi River as a water-supply source for Jefferson Parish. Eight major aquifers consisting of thick sand units that underlie the study area are, in descending order: (1) shallow, (2) upper Ponchatoula, (3) lower Ponchatoula, (4) Abita, (5) Covington, (6) Tchefuncta, (7) Hammond, and (8) Amite. A fault zone, referred to as the Baton Rouge fault, crosses southern Tangipahoa Parish. Analyses of geophysical logs indicated that the deep aquifers south of the fault zone had been displaced from 350 to 400 feet, and that the deeper aquifers were not in hydraulic connection with the flow system north of the fault. The groundwater resources of southeastern Louisiana are immense and the quality of groundwater in Tangipahoa Parish is suitable for most uses. The quality of water in these aquifers generally meets the U.S. Environmental Protection Agency's standards for public supply. The hydrologic system underlying Tangipahoa Parish and adjacent areas in 1990 supplied about 19 Mgal/d of water that was suitable for public supply. However, substantial increases in pumping from the aquifer system would result in renewed water-level declines throughout the hydrologic system until a new equilibrium is established. A test we11 in southern Tangipahoa Parish, penetrated all eight aquifers. Total thickness of freshwater sand beds penetrated by the 3003-ft test hole was more than 1900 ft. Resistivity values from an electric log of the test typically averaged 200 ohm-meters, which indicates that the water has low dissolved-solids and chloride concentrations. An analysis of the Abita aquifer at Ruddock in St. John the Baptist Parish, for two of three hypothetical well fields, indicated that for a hypothetical we11 field with a pumping rate of 112 Mgal/d, the freshwater/saltwater interface could arrive at the outer perimeter we11 in 10 to 14 years. The 1990 location of the interface in the Abita aquifer is 1.9 mi from the southernmost part of the potential location of the 112 Mgal/d well field.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri924182","usgsCitation":"Rapp, T., 1994, Ground-water resources of southern Tangipahoa Parish and adjacent areas, Louisiana: U.S. Geological Survey Water-Resources Investigations Report 92-4182, v, 47 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri924182.","productDescription":"v, 47 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123962,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4182/report-thumb.jpg"},{"id":58121,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4182/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d5d7","contributors":{"authors":[{"text":"Rapp, T.R.","contributorId":51784,"corporation":false,"usgs":true,"family":"Rapp","given":"T.R.","email":"","affiliations":[],"preferred":false,"id":201249,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25709,"text":"wri934144 - 1994 - Pore-water extraction from unsaturated tuff by triaxial and one-dimensional compression methods, Nevada Test Site, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:15","indexId":"wri934144","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"93-4144","title":"Pore-water extraction from unsaturated tuff by triaxial and one-dimensional compression methods, Nevada Test Site, Nevada","docAbstract":"Study of the hydrologic system at Yucca Mountain, Nevada, requires the extraction of pore-water samples from welded and nonwelded, unsaturated tuffs. Two compression methods (triaxial compression and one-dimensional compression) were examined to develop a repeatable extraction technique and to investigate the effects of the extraction method on the original pore-fluid composition.  A commercially available triaxial cell was modified to collect pore water expelled from tuff cores. The triaxial cell applied a maximum axial stress of 193 MPa and a maximum confining stress of 68 MPa. Results obtained from triaxial compression testing indicated that pore-water samples could be obtained from nonwelded tuff cores that had initial moisture contents as small as 13 percent (by weight of dry soil). Injection of nitrogen gas while the test core was held at the maximum axial stress caused expulsion of additional pore water and reduced the required initial moisture content from 13 to 11 percent. Experimental calculations, together with experience gained from testing moderately welded tuff cores, indicated that the triaxial cell used in this study could not apply adequate axial or confining stress to expel pore water from cores of densely welded tuffs. This concern led to the design, fabrication, and testing of a one-dimensional compression cell.  The one-dimensional compression cell used in this study was constructed from hardened 4340-alloy and nickel-alloy steels and could apply a maximum axial stress of 552 MPa. The major components of the device include a corpus ring and sample sleeve to confine the sample, a piston and base platen to apply axial load, and drainage plates to transmit expelled water from the test core out of the cell. One-dimensional compression extracted pore water from nonwelded tuff cores that had initial moisture contents as small as 7.6 percent; pore water was expelled from densely welded tuff cores that had initial moisture contents as small as 7.7 percent. Injection of nitrogen gas at the maximum axial stress did not produce additional pore water from nonwelded tuff cores, but was critical to recovery of pore water from densely welded tuff cores. Gas injection reduced the required initial moisture content in welded tuff cores from 7.7 to 6.5 percent.  Based on the mechanical ability of a pore-water extraction method to remove water from welded and nonwelded tuff cores, one-dimensional compression is a more effective extraction method than triaxial compression. However, because the effects that one-dimensional compression has on pore-water chemistry are not completely understood, additional testing will be needed to verify that this method is suitable for pore-water extraction from Yucca Mountain tuffs.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey :\r\nU.S. Geological Survey, Earth Science Information Center, Open-File Reports Section, [distributor],","doi":"10.3133/wri934144","usgsCitation":"Mower, T.E., Higgins, J.D., Yang, I., and Peters, C.A., 1994, Pore-water extraction from unsaturated tuff by triaxial and one-dimensional compression methods, Nevada Test Site, Nevada: U.S. Geological Survey Water-Resources Investigations Report 93-4144, vi, 78 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri934144.","productDescription":"vi, 78 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123761,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4144/report-thumb.jpg"},{"id":54469,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4144/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db68428c","contributors":{"authors":[{"text":"Mower, Timothy E.","contributorId":34171,"corporation":false,"usgs":true,"family":"Mower","given":"Timothy","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":194750,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Higgins, Jerry D.","contributorId":35353,"corporation":false,"usgs":true,"family":"Higgins","given":"Jerry","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":194751,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yang, In C.","contributorId":70424,"corporation":false,"usgs":true,"family":"Yang","given":"In C.","affiliations":[],"preferred":false,"id":194752,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Peters, Charles A. capeters@usgs.gov","contributorId":214,"corporation":false,"usgs":true,"family":"Peters","given":"Charles","email":"capeters@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":194749,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":38343,"text":"pp1551E - 1994 - The Loma Prieta, California, Earthquake of October 17, 1989 — Hydrologic disturbances","interactions":[{"subject":{"id":38343,"text":"pp1551E - 1994 - The Loma Prieta, California, Earthquake of October 17, 1989 — Hydrologic disturbances","indexId":"pp1551E","publicationYear":"1994","noYear":false,"chapter":"E","title":"The Loma Prieta, California, Earthquake of October 17, 1989 — Hydrologic disturbances"},"predicate":"IS_PART_OF","object":{"id":77047,"text":"pp1551 - 1992 - The Loma Prieta, California, Earthquake of October 17, 1989: Strong ground motion and ground failure","indexId":"pp1551","publicationYear":"1992","noYear":false,"title":"The Loma Prieta, California, Earthquake of October 17, 1989: Strong ground motion and ground failure"},"id":1}],"isPartOf":{"id":77047,"text":"pp1551 - 1992 - The Loma Prieta, California, Earthquake of October 17, 1989: Strong ground motion and ground failure","indexId":"pp1551","publicationYear":"1992","noYear":false,"title":"The Loma Prieta, California, Earthquake of October 17, 1989: Strong ground motion and ground failure"},"lastModifiedDate":"2025-07-09T19:47:58.957446","indexId":"pp1551E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"1551","chapter":"E","title":"The Loma Prieta, California, Earthquake of October 17, 1989 — Hydrologic disturbances","docAbstract":"Seismic events have long been known to cause changes in the level of oceans, streams, lakes, and the water table. The great San Francisco earthquake of 1906 induced significant hydrologic changes that were qualitatively similar to those changes observed for the Loma Prieta earthquake. What is different is that the hydrologic data sets collected from the Loma Prieta event have enough detail to enable hypotheses on the causes for these changes to be tested. The papers in this chapter document changes in ocean level, stream morphology and flow, water table height, and ground-water flow rates in response to the earthquake. Although hydrologic disturbances may have occurred about 1 hour before the main shock, the papers in this chapter deal strictly with postevent hydrologic changes. The hydrologic responses reported here reflect changes that are not the result of surface rupture. They appear to be the result of landslides, the static displacements induced by the earthquake, and changes in the permeability of the near surface.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Loma Prieta, California, Earthquake of October 17, 1989: Strong ground motion and ground failure","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/pp1551E","collaboration":"Prepared in cooperation with the National Science Foundation","usgsCitation":"1994, The Loma Prieta, California, Earthquake of October 17, 1989 — Hydrologic disturbances: U.S. Geological Survey Professional Paper 1551, iii, 64 p., https://doi.org/10.3133/pp1551E.","productDescription":"iii, 64 p.","costCenters":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":491955,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_76953.htm","text":"Hydrologic changes associated with the earthquake in the San Lorenzo and Pescadero drainage basins","linkFileType":{"id":5,"text":"html"}},{"id":491954,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_76952.htm","text":"Effects of the earthquake on surface waters in Waddell Valley [San Mateo County, California]","linkFileType":{"id":5,"text":"html"}},{"id":491953,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_76951.htm","text":"Stream-channel adjustment in Fern Canyon near Watsonville, California, after the earthquake","linkFileType":{"id":5,"text":"html"}},{"id":3429,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/pp1551/pp1551e/","linkFileType":{"id":5,"text":"html"}},{"id":402065,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_76950.htm","text":"The origin of the tsunami excited by the earthquake -- faulting and slumping [Loma Prieta earthquake, central California coast]","linkFileType":{"id":5,"text":"html"}},{"id":124514,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/pp_1551_e.jpg"}],"country":"United States","state":"California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.420654296875,\n              36.47872381162464\n            ],\n            [\n              -121.73950195312499,\n              36.47872381162464\n            ],\n            [\n              -121.73950195312499,\n              37.068327517596586\n            ],\n            [\n              -122.420654296875,\n              37.068327517596586\n            ],\n            [\n              -122.420654296875,\n              36.47872381162464\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e56da","contributors":{"editors":[{"text":"Rojstaczer, Stuart A.","contributorId":79536,"corporation":false,"usgs":true,"family":"Rojstaczer","given":"Stuart","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":749491,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":21453,"text":"ofr9471 - 1994 - National Water-Quality Assessment Program--Southern High Plains, Texas and New Mexico","interactions":[],"lastModifiedDate":"2012-02-10T00:10:07","indexId":"ofr9471","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-71","title":"National Water-Quality Assessment Program--Southern High Plains, Texas and New Mexico","docAbstract":"BACKGROUND\r\n\r\nIn 1991, the U.S. Geological Survey (USGS) began a National Water-Quality Assessment (NAWQA) program. The long-term goals of the NAWQA program are to describe the status of, and trends in, the quality of a large, representative part of the Nation's surface- and ground-water resources and to identify the major natural and human factors that affect the quality of these resources. In addressing these goals, the program will produce a wealth of water-quality information that will be useful to policy makers and managers at the National, State, and local levels.\r\n\r\nThe NAWQA program emphasis is on regional water-quality problems. The program will not diminish the need for smaller studies and monitoring designed and currently being conducted by Federal, State, and local agencies to meet their individual needs. The NAWQA program, however, will provide a large-scale framework for conducting many of these activities and an understanding about National and regional water-quality conditions that cannot be acquired from individual, small-scale programs and studies.\r\n\r\nStudies of 60 hydrologic systems that include parts of most major river basins and aquifer systems (study-unit investigations) are the building blocks of the National assessment. The 60 study units range in size from 1,000 mi 2 (square miles) to more than 60,000 mi 2 and represent 60 to 70 percent of the Nation's water use and population served by public water supplies. Twenty study-unit investigations were started in 1991, 20 additional are starting in 1994, and 20 more are planned to start in 1997. The Southern High Plains study unit was selected as one of 20 study units to begin assessment activities in 1994. This study will be run from the New Mexico District office of the USGS in Albuquerque, New Mexico.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr9471","usgsCitation":"Woodward, D., and Diniz, C.G., 1994, National Water-Quality Assessment Program--Southern High Plains, Texas and New Mexico: U.S. Geological Survey Open-File Report 94-71, 2 p., https://doi.org/10.3133/ofr9471.","productDescription":"2 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":153848,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":51016,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0071/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":51017,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0071/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104,31.5 ], [ -104,35.5 ], [ -100,35.5 ], [ -100,31.5 ], [ -104,31.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698485","contributors":{"authors":[{"text":"Woodward, Dennis G. woody@usgs.gov","contributorId":232,"corporation":false,"usgs":true,"family":"Woodward","given":"Dennis G.","email":"woody@usgs.gov","affiliations":[],"preferred":true,"id":184454,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Diniz, Cecilia G.","contributorId":99577,"corporation":false,"usgs":true,"family":"Diniz","given":"Cecilia","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":184455,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":43689,"text":"ofr93368 - 1994 - Hydrologic features of the Truckee and Carson River Basins and adjacent areas, western Nevada and eastern California","interactions":[],"lastModifiedDate":"2023-08-30T18:17:55.921283","indexId":"ofr93368","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"93-368","title":"Hydrologic features of the Truckee and Carson River Basins and adjacent areas, western Nevada and eastern California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr93368","usgsCitation":"Trionfante, J.V., and Peltz, L.A., 1994, Hydrologic features of the Truckee and Carson River Basins and adjacent areas, western Nevada and eastern California: U.S. Geological Survey Open-File Report 93-368, 1 Plate: 14.79 x 22.67 inches, https://doi.org/10.3133/ofr93368.","productDescription":"1 Plate: 14.79 x 22.67 inches","costCenters":[],"links":[{"id":420311,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_40305.htm","linkFileType":{"id":5,"text":"html"}},{"id":81273,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0368/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":161802,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0368/report-thumb.jpg"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Truckee and Carson River Basins","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -120.5,\n              40.5\n            ],\n            [\n              -120.5,\n              38.25\n            ],\n            [\n              -118,\n              38.25\n            ],\n            [\n              -118,\n              40.5\n            ],\n            [\n              -120.5,\n              40.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606ad9","contributors":{"authors":[{"text":"Trionfante, Jeffrey V.","contributorId":46577,"corporation":false,"usgs":true,"family":"Trionfante","given":"Jeffrey","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":228562,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peltz, Lorri A.","contributorId":29401,"corporation":false,"usgs":true,"family":"Peltz","given":"Lorri","email":"","middleInitial":"A.","affiliations":[{"id":12701,"text":"US Geological Survey","active":true,"usgs":false}],"preferred":false,"id":228561,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44302,"text":"ofr94380 - 1994 - Map showing major drainage basins and stream-gaging stations in Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:11:03","indexId":"ofr94380","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-380","title":"Map showing major drainage basins and stream-gaging stations in Massachusetts","docAbstract":"This map report shows the 27 major drainage basins, locations of the 71 permanent stream- gaging stations, and the primary rivers, lakes, and reservoirs of Massachusetts.  These features are presented at a scale of 1:400,000 (map size about 36 by 24 inches).  The map also lists uses of streamflow data.  The map was produced from a digital data base using a Geographic Information System (GIS).  It shows information about the stream-gaging stations that can be accessed from the digital data base--stream-gaging station number and name, telemetry code, and cooperating agency.  By use of GIS and the major basin divides from the data base, additional data bases could be grouped to produce other hydrologic planning maps. The drainage divides were digitized from paper maps into the GIS at a scale of 1:24,000. The map was compiled from original maps that was produced by the USGS in cooperation with the Massachusetts Department of Environment Management.","language":"ENGLISH","doi":"10.3133/ofr94380","usgsCitation":"Rader, J.C., 1994, Map showing major drainage basins and stream-gaging stations in Massachusetts: U.S. Geological Survey Open-File Report 94-380, 1 map : photocopy ; 53 x 77 cm., on sheet 72 x 92 cm., folded to 18 x 23 cm., https://doi.org/10.3133/ofr94380.","productDescription":"1 map : photocopy ; 53 x 77 cm., on sheet 72 x 92 cm., folded to 18 x 23 cm.","costCenters":[],"links":[{"id":168658,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":21609,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0380/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a49e9","contributors":{"authors":[{"text":"Rader, J. C.","contributorId":95107,"corporation":false,"usgs":true,"family":"Rader","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":229510,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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