{"pageNumber":"458","pageRowStart":"11425","pageSize":"25","recordCount":16446,"records":[{"id":68353,"text":"ha722D - 1992 - Geohydrologic systems in Kansas: Physical framework of the upper aquifer unit in the western interior plains aquifer system","interactions":[],"lastModifiedDate":"2022-07-18T19:29:50.584672","indexId":"ha722D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"722","chapter":"D","title":"Geohydrologic systems in Kansas: Physical framework of the upper aquifer unit in the western interior plains aquifer system","docAbstract":"

The purpose of this Hydrologic Investigations Atlas is to provide a description of the principal geohydrologic systems in Upper Cambrian through Lower Cretaceous rocks in Kansas. This investigation was made as part of the Central Midwest Regional Aquifer-System Analysis (CMRASA). The CMRASA is one of several major investigations by the U.S. Geological Survey of regional aquifer systems in the United States. These regional investigations are designed to increase knowledge of the flow regime and hydrologic properties of major aquifer systems and to provide quantitative information for the assessment, development, and management water supplies. The CMRASA study area includes all or parts of 10 Central Midwestern States (Jorgensen and Signor, 1981), as shown on the envelope cover.
This Hydrologic Investigations Atlas, which consists of a series of nine chapters, presents a description of the physical framework and the geohydrology of principal aquifers and confining systems in Kansas. Chapter D presents maps that show the areal extent, altitude and configuration of the top, and thickness of Mississippian rocks that compose the upper aquifer unit of the Western Interior Plains aquifer system in Kansas, The chapter is limited to the presentation of the physical framework of the upper aquifer unit. The interpretation of the physical framework of the upper aquifer unit is based on selected geophysical and lithologic logs and published maps of stratigraphically equivalent units. Maps indicating the thickness and the altitude and configuration of the top of the upper aquifer unit in the Western Interior Plains aquifer system have been prepared as part of a series of interrelated maps that describe the stratigraphic interval from the Precambrian basement through Lower Cretaceous rocks. A concerted effort was made to ensure that maps of each geohydrologic unit are consistent with the maps of underlying and overlying units. Chapter A of this atlas series (Wolf and others, 1990) describes the relation of principal geohydrologic systems in Kansas and presents a more detailed discussion of the methods and data used to prepare and ensure consistency among the sets of maps.

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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8dd4","contributors":{"authors":[{"text":"Hansen, Cristi V. chansen@usgs.gov","contributorId":435,"corporation":false,"usgs":true,"family":"Hansen","given":"Cristi","email":"chansen@usgs.gov","middleInitial":"V.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":false,"id":278080,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spinazola, Joseph M.","contributorId":102044,"corporation":false,"usgs":true,"family":"Spinazola","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":278083,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Underwood, E. J.","contributorId":22440,"corporation":false,"usgs":true,"family":"Underwood","given":"E.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278082,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wolf, R. J.","contributorId":21518,"corporation":false,"usgs":true,"family":"Wolf","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278081,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":68111,"text":"ha730J - 1992 - Ground Water Atlas of the United States: Segment 9, Iowa, Michigan, Minnesota, Wisconsin","interactions":[{"subject":{"id":68111,"text":"ha730J - 1992 - Ground Water Atlas of the United States: Segment 9, Iowa, Michigan, Minnesota, Wisconsin","indexId":"ha730J","publicationYear":"1992","noYear":false,"chapter":"J","title":"Ground Water Atlas of the United States: Segment 9, Iowa, Michigan, Minnesota, Wisconsin"},"predicate":"IS_PART_OF","object":{"id":68687,"text":"ha730 - 2000 - Ground Water Atlas of the United States","indexId":"ha730","publicationYear":"2000","noYear":false,"title":"Ground Water Atlas of the United States"},"id":1}],"isPartOf":{"id":68687,"text":"ha730 - 2000 - Ground Water Atlas of the United States","indexId":"ha730","publicationYear":"2000","noYear":false,"title":"Ground Water Atlas of the United States"},"lastModifiedDate":"2017-05-30T15:55:08","indexId":"ha730J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"730","chapter":"J","title":"Ground Water Atlas of the United States: Segment 9, Iowa, Michigan, Minnesota, Wisconsin","docAbstract":"

Segment 9, which consists of Minnesota, Iowa, Wisconsin, and Michigan, abuts the Canadian border in the upper Midwest and lies adjacent to or surrounds four of the Great Lakes-Superior, Michigan, Huron, and Erie. Thousands of small to large lakes similar to the one shown in figure 1 dot the landscape, which is drained by numerous rivers and streams tributary primarily to the Mississippi River in the west and to the Great Lakes-St. Lawrence River system in the east. These abundant surface-water sources represent an ample supply of water to large users, such as the cities of Milwaukee, Wis., and Detroit, Mich. However, water stored in unconsolidated and consolidated sedimentary-rock aquifers that underlie the four States also is in abundant supply and is an economical source that can be used for nearly any purpose, usually with little or no treatment. In more than 95 percent of the four-State area, these aquifers supply water to a broad spectrum of consumers-from individual households to cities, such as St. Paul, Minn., Madison, Wis., and Lansing, Mich. These aquifers are the subject of this chapter. The geology and the hydrology of each of the principal aquifers are illustrated and discussed insofar as information was available from the literature. Hydrogeology, ground-water flow, availability and quality of water, and freshwater withdrawals from each of the aquifers are the principal subjects of discussion.

Population in the four States is concentrated in the cities and is thinly dispersed in the broad agricultural areas of the States (fig. 2). Minneapolis-St. Paul, Minn., Des Moines, Iowa, Milwaukee and Madison, Wis., and Detroit and Lansing, Mich., are a few of the principal cities. Many of these cities and other large population centers represent areas of concentrated ground-water withdrawals.

Precipitation is the source of all water in Segment 9. Average annual precipitation ranges from about 20 to 40 inches across the segment and generally increases from northwest to southeast (fig. 3). Precipitation is least in the northwestern part of the segment because of the orographic effect of the Rocky Mountains, which are hundreds of miles to the west. Annual precipitation in excess of 36 inches that falls south and east of Lakes Superior and Michigan (fig. 3) is a result of the prevailing westerly winds that evaporate moisture from the lakes; this moisture subsequently condenses and falls as precipitation over the land.

Average annual runoff in rivers and streams (fig. 4) generally reflects average annual precipitation patterns (fig. 3). Runoff generally increases from less than 1 to more than 20 inches. Runoff also tends to be substantial downwind from Lakes Superior and Michigan. However, in no part of the segment does runoff exceed precipitation. Much of the water from precipitation is returned to the atmosphere by evapotranspiration-evaporation from the land and water surfaces, and transpiration by plants. Some of the water is stored in aquifers through ground-water recharge or is stored on the land surface in lakes, marshes, and reservoirs. Runoff represents water from precipitation that runs directly off the land surface to streams and water discharged to streams that was stored in lakes, marshes, reservoirs, or aquifers.

","largerWorkTitle":"Ground Water Atlas of the United States","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha730J","isbn":"0607767588","usgsCitation":"Olcott, P.G., 1992, Ground Water Atlas of the United States: Segment 9, Iowa, Michigan, Minnesota, Wisconsin: U.S. Geological Survey Hydrologic Atlas 730, 31 p., https://doi.org/10.3133/ha730J.","productDescription":"31 p.","startPage":"J1","endPage":"J31","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":11487,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ha/ha730/ch_j/index.html","linkFileType":{"id":5,"text":"html"}},{"id":115252,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ha/730j/report.pdf","text":"Report","size":"69.43 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":186516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/730j/report-thumb.jpg"}],"country":"United States","state":"Iowa, Michigan, Minnesota, Wisconsin","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-90.640927,42.508302],[-90.161159,42.106372],[-90.172765,41.866149],[-90.364128,41.579633],[-91.050328,41.400049],[-91.113648,41.241401],[-90.955201,40.986805],[-91.448441,40.378914],[-91.785916,40.611488],[-95.746443,40.584935],[-95.852615,40.702262],[-95.929889,41.415155],[-96.096186,41.547192],[-96.077543,41.777824],[-96.628741,42.757532],[-96.448134,43.104452],[-96.598396,43.495074],[-96.453049,43.500415],[-96.452948,45.268925],[-96.835451,45.586129],[-96.587093,45.816445],[-96.559271,46.058272],[-96.789572,46.639079],[-96.851293,47.589264],[-97.139497,48.153108],[-97.108655,48.691484],[-97.238387,48.982631],[-95.153711,48.998903],[-95.153314,49.384358],[-94.974286,49.367738],[-94.555835,48.716207],[-93.741843,48.517347],[-92.984963,48.623731],[-92.634931,48.542873],[-92.698824,48.494892],[-92.341207,48.23248],[-92.066269,48.359602],[-91.542512,48.053268],[-90.88548,48.245784],[-90.703702,48.096009],[-89.489226,48.014528],[-90.86827,47.5569],[-92.058888,46.809938],[-91.942988,46.679939],[-90.880358,46.957661],[-90.78804,46.844886],[-90.920813,46.637432],[-90.398478,46.575832],[-88.982483,46.99883],[-88.400224,47.379551],[-87.816958,47.471998],[-87.730804,47.449112],[-88.349952,47.076377],[-88.462349,46.786711],[-88.167373,46.9588],[-87.915943,46.909508],[-87.619747,46.79821],[-87.366767,46.507303],[-86.850111,46.434114],[-86.188024,46.654008],[-84.964652,46.772845],[-84.969464,46.47629],[-84.177428,46.52692],[-84.097766,46.256512],[-84.247687,46.17989],[-83.931175,46.017871],[-83.63498,46.103953],[-83.49484,45.999541],[-84.345451,45.946569],[-84.656567,46.052654],[-84.820557,45.868293],[-85.047028,46.020603],[-85.528403,46.087121],[-85.663966,45.967013],[-86.278007,45.942057],[-86.687208,45.634253],[-86.532989,45.882665],[-86.92106,45.697868],[-87.018902,45.838886],[-88.027103,44.578992],[-87.943801,44.529693],[-87.428144,44.890738],[-87.021088,45.296541],[-87.73063,43.893862],[-87.910172,43.236634],[-87.800477,42.49192],[-90.640927,42.508302]]],[[[-88.684434,48.115785],[-88.447236,48.182916],[-89.022736,47.858532],[-89.255202,47.876102],[-88.684434,48.115785]]],[[[-83.880387,41.720089],[-86.824828,41.76024],[-86.24971,42.480212],[-86.226305,42.988284],[-86.540916,43.633158],[-86.25395,44.64808],[-86.066745,44.905685],[-85.780439,44.977932],[-85.540497,45.210169],[-85.641652,44.810816],[-85.520205,44.960347],[-85.477423,44.813781],[-85.355478,45.282774],[-84.91585,45.393115],[-85.110884,45.526285],[-84.94565,45.708621],[-85.011433,45.757962],[-84.204218,45.627116],[-84.095905,45.497298],[-83.488826,45.355872],[-83.316118,45.141958],[-83.435822,45.000012],[-83.277213,44.7167],[-83.335248,44.357995],[-83.890145,43.934672],[-83.909479,43.672622],[-83.618602,43.628891],[-83.227093,43.981003],[-82.915976,44.070503],[-82.617955,43.768596],[-82.423086,42.988728],[-82.509935,42.637294],[-82.648776,42.550401],[-82.630922,42.64211],[-82.780817,42.652232],[-83.431103,41.757457],[-83.880387,41.720089]]],[[[-86.880572,45.331467],[-86.956192,45.351179],[-86.82177,45.427602],[-86.880572,45.331467]]]]},\"properties\":{\"name\":\"Iowa\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dd8c","contributors":{"authors":[{"text":"Olcott, Perry G.","contributorId":17249,"corporation":false,"usgs":true,"family":"Olcott","given":"Perry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":277660,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29363,"text":"wri914085 - 1992 - Reconnaissance investigation of water quality, bottom sediment, and biota associated with irrigation drainage in the Malheur National Wildlife Refuge, Harney County, Oregon, 1988-89","interactions":[],"lastModifiedDate":"2019-12-28T09:50:06","indexId":"wri914085","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"91-4085","title":"Reconnaissance investigation of water quality, bottom sediment, and biota associated with irrigation drainage in the Malheur National Wildlife Refuge, Harney County, Oregon, 1988-89","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri914085","usgsCitation":"Rinella, F.A., and Schuler, C., 1992, Reconnaissance investigation of water quality, bottom sediment, and biota associated with irrigation drainage in the Malheur National Wildlife Refuge, Harney County, Oregon, 1988-89: U.S. Geological Survey Water-Resources Investigations Report 91-4085, vii, 106 p., https://doi.org/10.3133/wri914085.","productDescription":"vii, 106 p.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":159445,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4085/report-thumb.jpg"},{"id":58211,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4085/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","county":"Harney County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-118.229,44.0389],[-118.2286,44.0116],[-118.2288,43.9674],[-118.2286,43.9532],[-118.2289,43.9086],[-118.2287,43.8945],[-118.229,43.8653],[-118.23,43.7792],[-118.2338,43.7798],[-118.2335,43.7675],[-118.2337,43.7242],[-118.2333,43.6978],[-118.2337,43.6295],[-118.2343,43.5744],[-118.2343,43.5357],[-118.2341,43.5211],[-118.2346,43.5065],[-118.2353,43.4487],[-118.2351,43.4346],[-118.2349,43.421],[-118.2354,43.4059],[-118.2352,43.3918],[-118.2357,43.3773],[-118.2362,43.3627],[-118.236,43.3486],[-118.2303,43.349],[-118.2302,43.3335],[-118.2301,43.3185],[-118.2293,43.3039],[-118.2298,43.2893],[-118.2295,43.2616],[-118.2293,43.2461],[-118.2287,43.1888],[-118.2286,43.1733],[-118.228,43.1724],[-118.2279,43.1009],[-118.2277,43.0873],[-118.2274,43.0582],[-118.2272,43.0436],[-118.2277,43.029],[-118.2276,43.0145],[-118.2274,43.0004],[-118.2286,43.0009],[-118.2279,42.9276],[-118.2278,42.9131],[-118.2171,42.9129],[-118.2161,42.8119],[-118.2166,42.7969],[-118.2158,42.7255],[-118.2157,42.7109],[-118.2156,42.6373],[-118.2155,42.6227],[-118.2147,42.5504],[-118.2146,42.5359],[-118.2141,42.4927],[-118.2139,42.4632],[-118.2144,42.4486],[-118.2128,42.3622],[-118.2127,42.3477],[-118.2125,42.3336],[-118.2124,42.319],[-118.2116,42.304],[-118.212,42.2754],[-118.1909,42.275],[-118.1916,42.236],[-118.1914,42.2223],[-118.1926,42.1483],[-118.1918,42.1356],[-118.1936,42.0634],[-118.194,42.0493],[-118.1952,41.9965],[-118.2137,41.9964],[-118.2341,41.9963],[-118.3125,41.9958],[-118.3496,41.9956],[-118.3891,41.9954],[-118.4287,41.9952],[-118.5914,41.9943],[-118.7723,41.993],[-118.7764,41.993],[-118.9076,41.9935],[-119.0478,41.9946],[-119.1449,41.9942],[-119.3244,41.9936],[-119.3569,41.9934],[-119.3585,42.0485],[-119.3589,42.1357],[-119.3632,42.1357],[-119.3643,42.2239],[-119.3641,42.3115],[-119.3639,42.3988],[-119.3643,42.4133],[-119.3647,42.4279],[-119.3644,42.4424],[-119.3642,42.4569],[-119.364,42.4715],[-119.3637,42.486],[-119.3641,42.5742],[-119.364,42.6596],[-119.3644,42.7469],[-119.483,42.747],[-119.5417,42.7465],[-119.6004,42.7465],[-119.6335,42.7463],[-119.7028,42.7453],[-119.7028,42.7426],[-119.7059,42.7426],[-119.7259,42.7423],[-119.8258,42.7419],[-119.8439,42.742],[-119.9419,42.7411],[-119.9418,42.8298],[-119.9417,42.9125],[-119.9348,42.9125],[-119.9379,43.0007],[-119.9384,43.0858],[-119.9389,43.1012],[-119.9396,43.1754],[-119.8981,43.1766],[-119.8988,43.2471],[-119.8987,43.2616],[-119.8991,43.2762],[-119.8989,43.3053],[-119.8991,43.3499],[-119.899,43.364],[-119.8995,43.3786],[-119.8994,43.3931],[-119.8992,43.4077],[-119.8996,43.4364],[-119.8996,43.5092],[-119.8995,43.5233],[-119.8994,43.5378],[-119.8988,43.6084],[-119.8986,43.6248],[-119.8982,43.6689],[-119.898,43.6967],[-119.8796,43.6971],[-119.8594,43.697],[-119.8391,43.6973],[-119.779,43.6979],[-119.7793,43.7854],[-119.7787,43.8427],[-119.7778,43.8719],[-119.7763,43.9575],[-119.6778,43.9574],[-119.6587,43.9577],[-119.5577,43.9589],[-119.5373,43.9587],[-119.4878,43.9593],[-119.416,43.9601],[-119.3982,43.9599],[-119.3569,43.96],[-119.2984,43.9599],[-119.1784,43.9602],[-119.0589,43.9612],[-118.9782,43.9612],[-118.9572,43.961],[-118.9363,43.9612],[-118.9185,43.9614],[-118.8676,43.9617],[-118.8174,43.962],[-118.8159,44.0472],[-118.6944,44.047],[-118.5882,44.0473],[-118.5883,44.0409],[-118.5413,44.0407],[-118.4669,44.0405],[-118.3676,44.0407],[-118.3472,44.0409],[-118.3473,44.0391],[-118.3307,44.0392],[-118.3104,44.0389],[-118.29,44.039],[-118.2697,44.0391],[-118.2493,44.0388],[-118.229,44.0389]]]},\"properties\":{\"name\":\"Harney\",\"state\":\"OR\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63eb31","contributors":{"authors":[{"text":"Rinella, F. A.","contributorId":89120,"corporation":false,"usgs":true,"family":"Rinella","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":201411,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schuler, C.A.","contributorId":42627,"corporation":false,"usgs":true,"family":"Schuler","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":201410,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":17240,"text":"ofr92627 - 1992 - Hydrologic and climatic data bases used to assess potential effects of climate change on water resources of American River, Carson River, and Truckee River basins, California-Nevada, and of Gunnison River basin, Colorado","interactions":[],"lastModifiedDate":"2017-12-19T13:26:08","indexId":"ofr92627","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-627","title":"Hydrologic and climatic data bases used to assess potential effects of climate change on water resources of American River, Carson River, and Truckee River basins, California-Nevada, and of Gunnison River basin, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr92627","usgsCitation":"August, M., Jacoboni, J., Jeton, A., Parker, R.S., Pupacko, A., Ruddy, B.C., Smith, J.L., and Redmond, K., 1992, Hydrologic and climatic data bases used to assess potential effects of climate change on water resources of American River, Carson River, and Truckee River basins, California-Nevada, and of Gunnison River basin, Colorado: U.S. Geological Survey Open-File Report 92-627, iv, 72 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr92627.","productDescription":"iv, 72 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":149357,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0627/report-thumb.jpg"},{"id":46390,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0627/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4786","contributors":{"authors":[{"text":"August, M.H.","contributorId":92276,"corporation":false,"usgs":true,"family":"August","given":"M.H.","email":"","affiliations":[],"preferred":false,"id":175560,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jacoboni, J.M.","contributorId":52196,"corporation":false,"usgs":true,"family":"Jacoboni","given":"J.M.","affiliations":[],"preferred":false,"id":175556,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jeton, A.E.","contributorId":61841,"corporation":false,"usgs":true,"family":"Jeton","given":"A.E.","email":"","affiliations":[],"preferred":false,"id":175557,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Parker, R. S.","contributorId":104510,"corporation":false,"usgs":true,"family":"Parker","given":"R.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":175561,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pupacko, Alex","contributorId":107713,"corporation":false,"usgs":true,"family":"Pupacko","given":"Alex","email":"","affiliations":[],"preferred":false,"id":175562,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ruddy, B. C.","contributorId":65098,"corporation":false,"usgs":true,"family":"Ruddy","given":"B.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":175558,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Smith, J. LaRue jlsmith@usgs.gov","contributorId":1863,"corporation":false,"usgs":true,"family":"Smith","given":"J.","email":"jlsmith@usgs.gov","middleInitial":"LaRue","affiliations":[],"preferred":true,"id":175559,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Redmond, K.T.","contributorId":12865,"corporation":false,"usgs":true,"family":"Redmond","given":"K.T.","email":"","affiliations":[],"preferred":false,"id":175555,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":17244,"text":"ofr9267 - 1992 - Hydrologic data for the Big Spring basin, Clayton County, Iowa, water year 1990","interactions":[],"lastModifiedDate":"2016-03-11T15:56:38","indexId":"ofr9267","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-67","title":"Hydrologic data for the Big Spring basin, Clayton County, Iowa, water year 1990","docAbstract":"

Hydrologic data were collected in the Big Spring basin located in Clayton County, Iowa, during the 1990 water year. The data were collected by the U.S. Geological Survey in cooperation with the Iowa Department of Natural Resources, Geological Survey Bureau, to provide information on variation and movement of agricultural chemicals in the hydrologic cycle in the basin. Precipitation, surface-water, and ground-water data were collected.

\n

Rainfall recorded during water year 1990 at a monitoring site on Roberts Creek totaled 43.67 inches. The greatest monthly rainfall (14.45 inches) occurred in August. Calcium and sulfate were the predominant ions in the rain, and the median concentrations of nitrate and ammonia as nitrogen were 0.35 and 0.48 milligrams per liter, respectively.

\n

Stream discharge, specific conductance, pH, and water temperature were monitored continuously, and monthly water-quality samples were collected at three sites in the basin. The predominant ions in samples from Roberts Creek at the point where it leaves the basin were calcium, magnesium, and bicarbonate. Nitrite plus nitrate as nitrogen concentrations in 42 samples ranged from less than 0.10 to 18 milligrams per liter. Pesticide concentrations in 34 samples ranged from less than 0.10 to 12 micrograms per liter. Alachlor was detected in 56 percent of the samples; atrazine in 100 percent; cyanazine in 68 percent; and metolachlor in 47 percent.

\n

At Big Spring, the ground-water discharge point, the daily mean specific conductance ranged from 378 to 796 microsiemens per centimeter at 25 degrees Celsius, the daily median pH ranged from 6.5 to 7.2, and the daily mean water temperature ranged from 5.5 to 11.5 degrees Celsius. Calcium, magnesium, and bicarbonate generally were the predominant ions in solution. Concentrations of nitrite plus nitrate as nitrogen in 32 samples ranged from 3.4 to 16 milligrams per liter. Alachlor was detected in 22 percent of the samples; atrazine in 100 percent; cyanazine in 44 percent, and metplachlor in 6 percent. The maximum atrazine concentration was 4.5 micrograms per liter.

\n

During a low-flow seepage study, May 29 and 30,1990, the measured discharge lost by streams in the basin was 8.56 cubic feet per second, the measured dissolved nitrogen load lost was 0.29 ton per day, and the measured atrazine load lost was 0.028 pound per day. The total measured discharge and total dissolved nitrogen load leaving the basin in streams were 3.63 cubic feet per second and about 0.04 ton per day, respectively.

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Water-resources activities of the U.S. Geological Survey in Iowa consist of collecting hydrologic data and conducting interpretive studies. Hydrologic investigations in Iowa are made through three basic types of projects: (1) hydrologic data-collection programs; (2) local or areal studies; and (3) statewide or regional investigations. These projects are funded through cooperative joint-funding agreements with Federal, State, and local agencies and direct Federal funds. The data and the results of the interpretive studies are published or released by either the U.S. Geological Survey or by cooperating agencies. This report describes: (1) the hydrologic data-collection programs; (2) the local or areal hydrologic investigations; and (3) statewide or regional studies conducted by the U.S. Geological Survey in Iowa during fiscal year 1992 and provides a list of selected water-resources references for Iowa.

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No abstract available. 

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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae8de","contributors":{"authors":[{"text":"Arvin, Donald V. dvarvin@usgs.gov","contributorId":3210,"corporation":false,"usgs":true,"family":"Arvin","given":"Donald","email":"dvarvin@usgs.gov","middleInitial":"V.","affiliations":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":178355,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18061,"text":"ofr92143 - 1992 - A study of ground-water flow beneath the Massachusetts Military Reservation, Cape Cod, Massachusetts; project description, August 1992","interactions":[],"lastModifiedDate":"2019-12-28T10:07:52","indexId":"ofr92143","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-143","title":"A study of ground-water flow beneath the Massachusetts Military Reservation, Cape Cod, Massachusetts; project description, August 1992","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr92143","usgsCitation":"Barlow, P.M., and LeBlanc, D., 1992, A study of ground-water flow beneath the Massachusetts Military Reservation, Cape Cod, Massachusetts; project description, August 1992: U.S. Geological Survey Open-File Report 92-143, 2 p. , https://doi.org/10.3133/ofr92143.","productDescription":"2 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":149965,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0143/report-thumb.jpg"},{"id":47414,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0143/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Massachusetts","otherGeospatial":"Cape Cod","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -70.6915283203125,\n 41.31907562295139\n ],\n [\n -69.5819091796875,\n 41.31907562295139\n ],\n [\n -69.5819091796875,\n 42.16340342422401\n ],\n [\n -70.6915283203125,\n 42.16340342422401\n ],\n [\n -70.6915283203125,\n 41.31907562295139\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a61f0","contributors":{"authors":[{"text":"Barlow, P. M.","contributorId":63022,"corporation":false,"usgs":true,"family":"Barlow","given":"P.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":178465,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LeBlanc, D.R.","contributorId":87141,"corporation":false,"usgs":true,"family":"LeBlanc","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":178466,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":18229,"text":"ofr92500 - 1992 - Hydrologic data for a study of pre-Illinoian glacial till in Linn County, Iowa, water year 1991","interactions":[],"lastModifiedDate":"2016-03-11T16:17:29","indexId":"ofr92500","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-500","title":"Hydrologic data for a study of pre-Illinoian glacial till in Linn County, Iowa, water year 1991","docAbstract":"

Hydrologic data for a study of pre-lllinoian glacial till were collected during the 1991 water year at a site in Linn County, east-central Iowa. A hydrologic-data-collection network, consisting of a meteorological station, 22 observation wells, and a water-quality minimonitor, was installed at the site to investigate the hydraulic properties of the till. Recorders were installed on 12 of the observation wells to continuously monitor water levels.

\n

Rainfall at the study site from October 1990 to September 1991 was 17.86 inches. The greatest monthly rainfall (4.07 inches) occurred in March. The smallest monthly rainfall (0.06 and 0.04 inch) occurred in June and July, respectively.

\n

The highest water levels measured in 22 observation wells were recorded from March through May 1991. Water levels in three of the deeper wells, completed in the unweathered glacial till, continued to rise from the time the wells were initially installed in November 1989 until they were bailed for water-quality sampling in May 1991. One well had water levels greater than the top of the well casing for most of the period from March to mid-July.

\n

Ten unvented, vibrating-wire pressure transducers with internal thermistors were buried in two boreholes at upgradient and downgradient locations to record hydraulic pressure and water temperature at selected depths.

\n

A water-quality minimonitor was installed near the top of the water table to monitor temporal changes in ground-water quality. For October 1990 through September 1991, the daily mean water temperatures ranged from 7.3 to 14.9 degrees Celsius, and the daily median pH values ranged from 6.9 to 7.5 standard units.

\n

Herbicide concentrations in rainfall ranged from 0.05 to 1.3 micrograms per liter. Herbicides detected in the largest concentrations included alachlor, atrazine, and metolachlor. Metribuzin was the only herbicide detected in ground-water samples at a concentration of 0.10 micrograms per liter in water from one observation well.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr92500","collaboration":"Prepared in cooperation with the Iowa Department of Natural Resources, Geological Survey Bureau","usgsCitation":"Bowman, P., 1992, Hydrologic data for a study of pre-Illinoian glacial till in Linn County, Iowa, water year 1991: U.S. Geological Survey Open-File Report 92-500, iv, 66 p.: ill.; 28 cm., https://doi.org/10.3133/ofr92500.","productDescription":"iv, 66 p.: ill.; 28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":47591,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0500/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150344,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0500/report-thumb.jpg"}],"country":"United States","state":"Iowa","county":"Linn County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -91.6754150390625,\n 41.860068712839\n ],\n [\n -91.6754150390625,\n 41.87480165983683\n ],\n [\n -91.66189670562744,\n 41.87480165983683\n ],\n [\n -91.66189670562744,\n 41.860068712839\n ],\n [\n -91.6754150390625,\n 41.860068712839\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60ebbf","contributors":{"authors":[{"text":"Bowman, P.R.","contributorId":6076,"corporation":false,"usgs":true,"family":"Bowman","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":178747,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18235,"text":"ofr9289 - 1992 - Hydrologic data for the lower Copper River, Alaska, May to September, 1991","interactions":[],"lastModifiedDate":"2012-02-02T00:07:19","indexId":"ofr9289","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-89","title":"Hydrologic data for the lower Copper River, Alaska, May to September, 1991","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr9289","usgsCitation":"Brabets, T.P., 1992, Hydrologic data for the lower Copper River, Alaska, May to September, 1991: U.S. Geological Survey Open-File Report 92-89, iv, 15 p. ill., map ;28 cm., https://doi.org/10.3133/ofr9289.","productDescription":"iv, 15 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":150367,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0089/report-thumb.jpg"},{"id":47595,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0089/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db6832a8","contributors":{"authors":[{"text":"Brabets, Timothy P. tbrabets@usgs.gov","contributorId":2087,"corporation":false,"usgs":true,"family":"Brabets","given":"Timothy","email":"tbrabets@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":178755,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":69646,"text":"ha722E - 1992 - Geohydrologic systems in Kansas; physical framework of the confining unit in the Western Interior Plains aquifer system","interactions":[],"lastModifiedDate":"2015-10-28T11:45:20","indexId":"ha722E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"722","chapter":"E","title":"Geohydrologic systems in Kansas; physical framework of the confining unit in the Western Interior Plains aquifer system","docAbstract":"

The purpose of this Hydrologic Investigations Atlas is to provide a description of the geohydrologic systems in Upper Cambrian through Lower Cretaceous rocks in Kansas. This investigation was made as part of the Central Midwest Regional Aquifer-System Analysis (CMRASA). The CMRASA is one of several major investigations by the U.S. Geological Survey of regional aquifer systems in the United States. These regional investigations are designed to increase knowledge of the flow regime and hydrologic properties of major aquifer systems and to provide quantitative information for the assessment, development, and management of water supplies. The CMRASA study area includes all or parts of 10 Central Midwestern States (Jorgensen and Signor, 1981), as shown on the envelope cover.

","language":"ENGLISH","doi":"10.3133/ha722E","usgsCitation":"Hansen, C.V., Wolf, R.J., and Spinazola, J., 1992, Geohydrologic systems in Kansas; physical framework of the confining unit in the Western Interior Plains aquifer system: U.S. Geological Survey Hydrologic Atlas 722, 2 sheets; Sheet 1, 46 by 40 1/2 inches; sheet 2, 46 by 34 1/2 inches (all in color), https://doi.org/10.3133/ha722E.","productDescription":"2 sheets; Sheet 1, 46 by 40 1/2 inches; sheet 2, 46 by 34 1/2 inches (all in color)","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":191629,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":266335,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/722e/plate-2.pdf"},{"id":266334,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/722e/plate-1.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8dca","contributors":{"authors":[{"text":"Hansen, C. V.","contributorId":74749,"corporation":false,"usgs":true,"family":"Hansen","given":"C.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":280802,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolf, R. J.","contributorId":21518,"corporation":false,"usgs":true,"family":"Wolf","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":280800,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Spinazola, J. M.","contributorId":32574,"corporation":false,"usgs":true,"family":"Spinazola","given":"J. M.","affiliations":[],"preferred":false,"id":280801,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":49593,"text":"ofr92478 - 1992 - State water-data reports; a digital representation of the hydrologic records of the United States for water years 1990 and 1991","interactions":[],"lastModifiedDate":"2012-02-02T00:11:16","indexId":"ofr92478","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-478","title":"State water-data reports; a digital representation of the hydrologic records of the United States for water years 1990 and 1991","language":"ENGLISH","doi":"10.3133/ofr92478","usgsCitation":"Alt, D., 1992, State water-data reports; a digital representation of the hydrologic records of the United States for water years 1990 and 1991: U.S. Geological Survey Open-File Report 92-478, One CD-ROM, https://doi.org/10.3133/ofr92478.","productDescription":"One CD-ROM","costCenters":[],"links":[{"id":176648,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3c68","contributors":{"authors":[{"text":"Alt, D.F.","contributorId":17653,"corporation":false,"usgs":true,"family":"Alt","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":239933,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18736,"text":"ofr9284 - 1992 - Plan of study for the Black Hills hydrology study, South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:07:24","indexId":"ofr9284","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-84","title":"Plan of study for the Black Hills hydrology study, South Dakota","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr9284","usgsCitation":"Driscoll, D.G., 1992, Plan of study for the Black Hills hydrology study, South Dakota: U.S. Geological Survey Open-File Report 92-84, iv, 10 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr9284.","productDescription":"iv, 10 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":150928,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0084/report-thumb.jpg"},{"id":48097,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0084/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68562b","contributors":{"authors":[{"text":"Driscoll, Daniel G. dgdrisco@usgs.gov","contributorId":1558,"corporation":false,"usgs":true,"family":"Driscoll","given":"Daniel","email":"dgdrisco@usgs.gov","middleInitial":"G.","affiliations":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":179649,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":19357,"text":"ofr92152 - 1992 - Continuous-record networks for collection of hydrologic data in Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:07:29","indexId":"ofr92152","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-152","title":"Continuous-record networks for collection of hydrologic data in Ohio","language":"ENGLISH","publisher":"U.S. Geological Survey, Dept. of the Interior,","doi":"10.3133/ofr92152","usgsCitation":"Hindall, S.M., and Eberle, M., 1992, Continuous-record networks for collection of hydrologic data in Ohio: U.S. Geological Survey Open-File Report 92-152, 2 p. ill. ;28 cm., https://doi.org/10.3133/ofr92152.","productDescription":"2 p. ill. ;28 cm.","costCenters":[],"links":[{"id":151713,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0152/report-thumb.jpg"},{"id":48834,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0152/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699dfd","contributors":{"authors":[{"text":"Hindall, S. 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This report is a compilation of data on surface- and ground-water quality, lake sediment, and lake-level fluctuation collected by the U.S. Geological Survey (USGS) during 1981- 87 on or near the St. Croix Indian Reservation. The purpose of this report is to provide baseline data on selected aspects of the water resources of the St. Croix Indian Reservation as a referenceby which future hydrologic changes can be discerned. The tribal lands are adjacent to Bashaw, BigRound, Big Sand, Clam, Gaslyn, Rice, and Sand Lakes and the Danbury Settlement along the St. Croix River. Water samples from each of these lakes and Bear Lake, which is not adjacent to tribal land, were analyzed for water-quality indicators. Lakelevel fluctuations also were measured for each lake except Big Round Lake. Grain-size and chemical analyses were done on lake-sediment samples from Bashaw, Rice, Clam, Gaslyn, and Bear Lakes. Ground-water samples from wells on or near tribal land in Burnett County (27 wells) and Polk County (3 wells) were collected and analyzed for water quality.

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T.","contributorId":59046,"corporation":false,"usgs":true,"family":"Krohelski","given":"J.","email":"","middleInitial":"T.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":181381,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":19785,"text":"ofr92132 - 1992 - Hydrologic Instrumentation Facility of the U.S. Geological Survey; annual report 1991","interactions":[],"lastModifiedDate":"2012-02-02T00:07:35","indexId":"ofr92132","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-132","title":"Hydrologic Instrumentation Facility of the U.S. Geological Survey; annual report 1991","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr92132","usgsCitation":"Latkovich, V., 1992, Hydrologic Instrumentation Facility of the U.S. Geological Survey; annual report 1991: U.S. Geological Survey Open-File Report 92-132, vi, 76 p. ill. ;28 cm., https://doi.org/10.3133/ofr92132.","productDescription":"vi, 76 p. ill. ;28 cm.","costCenters":[],"links":[{"id":152536,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0132/report-thumb.jpg"},{"id":49261,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0132/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a37d","contributors":{"authors":[{"text":"Latkovich, V.J.","contributorId":52576,"corporation":false,"usgs":true,"family":"Latkovich","given":"V.J.","email":"","affiliations":[],"preferred":false,"id":181507,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":20628,"text":"ofr92168 - 1992 - Acid rain and its effects on streamwater quality on Catoctin Mountain, Maryland","interactions":[],"lastModifiedDate":"2017-01-19T14:34:24","indexId":"ofr92168","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-168","title":"Acid rain and its effects on streamwater quality on Catoctin Mountain, Maryland","docAbstract":"

The U.S. Geological Survey (USGS) is the Nation's largest water-science and water-information agency. The mission of the Water Resources Division of the USGS is to provide the hydrologic information and understanding needed for the best management of the Nation's water resources. To fulfill this mission, the USGS conducts water-quality and other types of investigations of the Nation's surface- and ground-water resources.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Towson, MD","doi":"10.3133/ofr92168","usgsCitation":"Rice, K.C., and Bricker, O., 1992, Acid rain and its effects on streamwater quality on Catoctin Mountain, Maryland: U.S. Geological Survey Open-File Report 92-168, 2 p., https://doi.org/10.3133/ofr92168.","productDescription":"2 p.","numberOfPages":"2","costCenters":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"links":[{"id":152376,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0168/report-thumb.jpg"},{"id":50155,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0168/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Maryland","county":"Frederick","otherGeospatial":"Catoctin Mountain","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -77.52021789550781,\n 39.57049901310693\n ],\n [\n -77.52021789550781,\n 39.69001640474053\n ],\n [\n -77.3880386352539,\n 39.69001640474053\n ],\n [\n -77.3880386352539,\n 39.57049901310693\n ],\n [\n -77.52021789550781,\n 39.57049901310693\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a351d","contributors":{"authors":[{"text":"Rice, Karen C. 0000-0002-9356-5443 kcrice@usgs.gov","orcid":"https://orcid.org/0000-0002-9356-5443","contributorId":1998,"corporation":false,"usgs":true,"family":"Rice","given":"Karen","email":"kcrice@usgs.gov","middleInitial":"C.","affiliations":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"preferred":false,"id":182969,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bricker, O.P.","contributorId":33717,"corporation":false,"usgs":true,"family":"Bricker","given":"O.P.","affiliations":[],"preferred":false,"id":182968,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":20654,"text":"ofr92173 - 1992 - Selected hydrologic data for Cache Valley, Utah and Idaho, 1969-91","interactions":[],"lastModifiedDate":"2017-08-31T14:29:54","indexId":"ofr92173","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-173","title":"Selected hydrologic data for Cache Valley, Utah and Idaho, 1969-91","docAbstract":"

This report contains hydrologic data collected in Cache Valley from 1969 to 1991. The report area is in north-central Utah and southeast Idaho, within the Basin and Range physiographic province described by Fenneman (1931), and includes about 660 square miles.

Most of the data in this report were collected by the U.S. Geological Survey in cooperation with the Utah Department of Natural Resources, Divisions of Water Resources and Water Rights. Some of the data collected before 1969 were previously published by McGreevy and Bjorklund (1970).

The purpose of this report is to provide hydrologic data for use by the general public and by officials managing the area's water resources, and to supplement interpretive reports for the area. Tables 1 to 7 contain selected well, spring, and surface-water data. The numbering systems used in this report for hydrologic-data sites are illustrated in figure 1. Hydrologic-data sites are shown on plate 1.

These data could not have been collected without the cooperation of local residents and officials of irrigation companies and municipalities, that permitted access to their wells, springs, and canals to measure water levels in wells and flow in springs and canals. The Idaho Department of Water Resources also provided valuable assistance and data.

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No abstract available.

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L.","contributorId":20778,"corporation":false,"usgs":true,"family":"Baker","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":183609,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":20980,"text":"ofr92297 - 1992 - Applying the DRASTIC model: A review of county-scale maps","interactions":[],"lastModifiedDate":"2019-12-28T09:39:41","indexId":"ofr92297","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-297","title":"Applying the DRASTIC model: A review of county-scale maps","docAbstract":"

The potential for contamination of ground water has become an issue of great concern to citizens and government alike, especially in the last decade. Numerous methods for assessing ground water vulnerability to contamination have been proposed and used. These methods include field-scale deterministic models that predict the rate of migration and fate of specific chemicals, and regional models that attempt to show general trends of ground-water vulnerability to contamination. To address regional ground-water vulnerability, a model may focus on characteristics of the soil, the geologic materials at and above the unconfined water table, or on the larger part of the geologic framework containing aquifers. A model's focus significantly affects the characteristics and, therefore, the utility of maps produced by the model. For example, a model focusing on the soil or vadose zone cannot adequately characterize the contamination potential of confined aquifers.

The most commonly-used method for regional assessment of ground-water vulnerability is called \"DRASTIC,\" an acronym for the seven factors that comprise the model. The U.S. Environmental Protection Agency (EPA) funded the development of the DRASTIC model, and used it as an assessment tool in their National Pesticide Survey (USEPA, 1992). In that Survey and in other assessments of contamination potential from application of agricultural chemicals, the pesticide version of DRASTIC is used; it differs from the standard DRASTIC model only in the degree of weighting applied to the seven factors. The DRASTIC model was developed by a committee of technical advisors who used the consensus approach to specify the relative significance of each factor. DRASTIC was designed primarily as a regional tool for prioritization, or screening, to indicate those areas (of at least 100 acres in size) which are generally more sensitive to contamination and, therefore, in need of more detailed mapping and evaluation or monitoring. The committee also intended DRASTIC to support decisions on allocation of scarce monitoring or remediation resources, and to serve as an educational tool.

A detailed user's manual for the DRASTIC model (Aller and others, 1987) provides descriptions of common hydrogeologic settings across the United States and expected values for the seven factors; with this information and a specified \"weight\" or multiplier applied to each factor, DRASTIC scores can be calculated for each setting, and a map of these DRASTIC scores generated. The authors of this model intended it to be sufficiently objective and straightforward that it could be effectively used by persons with but a rudimentary knowledge of hydrogeologic principles. By adjusting the factor values for actual or interpreted local conditions a more knowledgeable person should be able to produce a somewhat more realistic and, therefore, reliable map of ground water vulnerability than by using the expected values for a given hydrogeologic setting.

Other models for evaluating regional ground-water vulnerability have been developed; of importance to this report are models developed by the Illinois State Geological Survey (ISGS), the Wisconsin Department of Natural Resources (WDNR), and a joint effort between the U.S. Geological Survey (USGS) and the ISGS. All of these models, as well as DRASTIC, can only estimate the relative potential for contamination, either with a numerical scheme or a hierarchy of contamination potential map units.

The model developed by WDNR (Schmidt, 1987) is based on a numerical scheme. It was used to generate a statewide contamination susceptibility map of Wisconsin (Schmidt and Kessler, 1987); Schmidt (1987) defines ground water contamination susceptibility as the \"ease with which water (and, presumably, accompanying contaminants) at the surface can reach the water table.\" The model is not limited to aquifers, but rather considers all unconfined ground water whether in sandy surface aquifers or low-permeability glacial till. Ground water in confined aquifers is not addressed. Contamination susceptibility is estimated by a factor-weighting scheme similar in concept to DRASTIC. The factors (soil texture, surficial deposits, depth to the water table, bedrock type, and glacial drift thickness) are assigned an arbitrary value based on perceived importance. These numbers are then weighted and summed to produce the contamination susceptibility score. This model is compared and contrasted with other models elsewhere in this report.

In contrast, the ISGS method avoids the use of a numerical system to rate the relative potential for contamination, and instead orders the map units in a hierarchy from relatively low to relatively high contamination potential. Also in contrast to the two models described above, the ISGS model relies solely on the textural character of the geologic framework to a specified depth. For example, a statewide map (Berg and others, 1984, scale 1:500,000) addresses land burial of wastes, and shows the contamination potential of aquifers within geologic units in the upper 50 feet. Another ISGS map (Keefer and Berg, 1990) addresses the contamination of major, economically important aquifers, and therefore evaluates contamination potential to greater depths (to greater than 300 feet). In general, the ISGS contamination potential maps evaluate aquifers, and do not evaluate potential for contamination of ground water at the unconfined water table in geologic units that are not aquifers (for example, in glacial till or finegrained lake sediments).

With the cooperation of the ISGS, I have developed a model (Seller and Berg, in press) for the regional assessment of aquifer contamination potential that is based on ISGS techniques, adapted to a broader map area where detailed information may be unavailable. This model was used to generate a map of aquifer contamination potential for an area encompassing parts of five states near southern Lake Michigan and Lake Erie; the model and map are currently being refined and evaluated.

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The platform allows continuous water sampling over the entire storm-runoff hydrogrpah. The platform was developed for a site in southern Illinois.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr92149","usgsCitation":"Tarte, S.R., Schmidt, A., and Sullivan, D.J., 1992, Floating sample-collection platform with stage-activated automatic water sampler for streams with large variation in stage: U.S. Geological Survey Open-File Report 92-149, iv, 14 p. , https://doi.org/10.3133/ofr92149.","productDescription":"iv, 14 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":50685,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0149/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":154762,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0149/report-thumb.jpg"}],"country":"United States","state":"Illinois 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