No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr90593","usgsCitation":"Wiche, G., Jenson, S., Baglio, J.V., and Domingue, J.O., 1990, Application of digital elevation models to delineate drainage areas and compute hydrologic characteristics for sites in the James River basin, North Dakota: U.S. Geological Survey Open-File Report 90-593, Report: vi, 39 p.; 6 Plates: 15.73 x 20.82 inches or smaller, https://doi.org/10.3133/ofr90593.","productDescription":"Report: vi, 39 p.; 6 Plates: 15.73 x 20.82 inches or smaller","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true},{"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":150293,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0593/report-thumb.jpg"},{"id":383553,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0593/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383554,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0593/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383555,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0593/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383556,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0593/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383558,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0593/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383559,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0593/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383557,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0593/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North 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 -104.0185546875,\n 45.89000815866184\n ],\n [\n -96.6796875,\n 45.89000815866184\n ],\n [\n -96.6796875,\n 48.951366470947725\n ],\n [\n -104.0185546875,\n 48.951366470947725\n ],\n [\n -104.0185546875,\n 45.89000815866184\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67aa52","contributors":{"authors":[{"text":"Wiche, G.J.","contributorId":90715,"corporation":false,"usgs":true,"family":"Wiche","given":"G.J.","affiliations":[],"preferred":false,"id":174103,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jenson, S.K.","contributorId":35291,"corporation":false,"usgs":true,"family":"Jenson","given":"S.K.","email":"","affiliations":[],"preferred":false,"id":174102,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baglio, J. V. Jr.","contributorId":91831,"corporation":false,"usgs":true,"family":"Baglio","given":"J.","suffix":"Jr.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":174104,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Domingue, Julia O.","contributorId":91832,"corporation":false,"usgs":true,"family":"Domingue","given":"Julia","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":174105,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":44153,"text":"ofr90177 - 1990 - Surface-water hydrology of Honey Lake Valley, Lassen County, California, and Washoe County, Nevada","interactions":[{"subject":{"id":44153,"text":"ofr90177 - 1990 - Surface-water hydrology of Honey Lake Valley, Lassen County, California, and Washoe County, Nevada","indexId":"ofr90177","publicationYear":"1990","noYear":false,"title":"Surface-water hydrology of Honey Lake Valley, Lassen County, California, and Washoe County, Nevada"},"predicate":"SUPERSEDED_BY","object":{"id":68382,"text":"ha726 - 1993 - Surface-water hydrology of Honey Lake Valley, Lassen County, California, and Washoe County, Nevada","indexId":"ha726","publicationYear":"1993","noYear":false,"title":"Surface-water hydrology of Honey Lake Valley, Lassen County, California, and Washoe County, Nevada"},"id":1}],"supersededBy":{"id":68382,"text":"ha726 - 1993 - Surface-water hydrology of Honey Lake Valley, Lassen County, California, and Washoe County, Nevada","indexId":"ha726","publicationYear":"1993","noYear":false,"title":"Surface-water hydrology of Honey Lake Valley, Lassen County, California, and Washoe County, Nevada"},"lastModifiedDate":"2022-04-20T17:20:22.914581","indexId":"ofr90177","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-177","title":"Surface-water hydrology of Honey Lake Valley, Lassen County, California, and Washoe County, Nevada","docAbstract":"Honey Lake Valley straddles the state line of California and Nevada, about 35 miles north of Reno; about three-fourths of the area is in California. In this report, Honey Lake Valley (also referred to as the \"basin\") includes the entire area within the hydrographic boundary (fig. 1). Susanville, Calif., in the northwest part of the basin, is the largest town. Population is increasing rapidly both in the Susanville area and in the Reno area of adjacent Washoe County, Nev. Both Lassen and Washoe Counties have identified water resources in Honey Lake Valley as a possible source to meet their needs for future development. An important component of an assessment of the availability of additional long-term supply is an appraisal of surface-water resources.
The U.S. Geological Survey, in cooperation with the California Department of Water Resources and the Nevada Division of Water Resources, began a hydrologic assessment of the area in 1987. The study was primarily an appraisal of ground-water resources, but it also included an assessment of surface-water resources. The purpose of this map report is to present the results of the surface-water assessment, including (1) a broad overview of surface-water conditions in the basin, (2) an estimate of mean annual streamflow to the valley floor, and (3) an evaluation of the characteristics of Honey Lake. This report will be republished by the U.S. Geological Survey as a Hydrologic-Investigations Atlas. Results of this study related to ground-water resources of the basin are discussed in a separate report (Handman and others, 1990) and are summarized in a short \"Water Fact Sheet\" by Handman (1990).
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr90177","collaboration":"Prepared in cooperation with the California Department of Water Resources and the Nevada Division of Water Resources","usgsCitation":"Rockwell, G.L., 1990, Surface-water hydrology of Honey Lake Valley, Lassen County, California, and Washoe County, Nevada: U.S. Geological Survey Open-File Report 90-177, 2 Plates: 41.91 x 44.49 inches and 46.15 x 33.21 inches, https://doi.org/10.3133/ofr90177.","productDescription":"2 Plates: 41.91 x 44.49 inches and 46.15 x 33.21 inches","costCenters":[],"links":[{"id":399188,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0177/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":399187,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0177/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":134680,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0177/report-thumb.jpg"}],"datum":"National Geodetic Vertical Datum of 1929 (NGVD of 1929)","country":"United States","state":"California, Nevada","county":"Lassen County, Washoe County","otherGeospatial":"Honey Lake Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.49942016601562,\n 40.12114052159822\n ],\n [\n -119.91165161132811,\n 40.12114052159822\n ],\n [\n -119.91165161132811,\n 40.36747374615593\n ],\n [\n -120.49942016601562,\n 40.36747374615593\n ],\n [\n -120.49942016601562,\n 40.12114052159822\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a76d","contributors":{"authors":[{"text":"Rockwell, Gerald L.","contributorId":55401,"corporation":false,"usgs":true,"family":"Rockwell","given":"Gerald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":229248,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68463,"text":"ha714 - 1990 - Hydrologic characteristics of soils in the High Plains, northern Great Plains, and Central Texas Carbonates Regional Aquifer Systems","interactions":[],"lastModifiedDate":"2017-09-20T16:41:29","indexId":"ha714","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"714","title":"Hydrologic characteristics of soils in the High Plains, northern Great Plains, and Central Texas Carbonates Regional Aquifer Systems","docAbstract":"Certain physical characteristics of soils, including permeability, available water capacity, thickness, and topographic position, have a measurable effect on the hydrology of an area. These characteristics control the rate at which precipitation infiltrates or is transmitted through the soil, and thus they have an important role in determining the rates of actual evapotranspiration (consumptive water use), groundwater recharge, and surface runoff. In studies of groundwater hydrology, it is useful to differentiate soils spatially according to their physical characteristics and to assign values that indicate their hydrologic responses.
The principal purpose of this report is to describe the relation between the hydrologic characteristics of the soils in the study area and those environmental factors that affect the development and distribution of the soils. This objective will be achieved by (1) defining both qualitatively and quantitatively those soil characteristics that affect hydrology, and (2) classifying and delineating the boundaries of the soils in the study area according to these hydrologic characteristics.
The study area includes the High Plains, Northern Great Plains, the Central Texas Carbonates, and parts of the Central Midwest Regional Aquifer Systems as described by the U.S. Geological Survey Regional Aquifer-System Analysis (RASA) Program (Sun, 1986, p.5and Sun, personal commun., June 1985) and shown in figures 1 through 5. The spatial patterns of the soils classified according to their quantifiable hydrologic characteristics will subsequently serve as an integral component in the analysis of actual evapotranspiration (consumptive water use), consumptive irrigation requirements, and potential ground-water recharge of the study area.
The classification system used to describe the soils in this report is compatible with that of Dugan (1986). Dugan described the same characteristics of soils that are immediately underlain by principal aquifers of Cretaceous or older age in adjacent parts of the Central Midwest Regional Aquifer System. However, map scales and mapping detail are different between this report and the report by Dugan (1986) because of the size of the study area.
An investigation of the geohydrologic system in the Ozark Plateaus province (index map and Fenneman, 1938) has been made as part of the Central Midwest Regional Aquifer-System Analysis (Jorgenson and Signor, 1981), a major study that encompasses parts of 10 States. The study is one of several by the U.S. Geological Survey that are designed to increase knowledge of the flow regime and geohydrologic properties of regional aquifer systems in the United States. Because a large quantity of fresh groundwater is available in aquifers underlying the Ozark Plateaus province, a subregional project has been established to study the geohydrologic units of this area in more detail than is practical in the regional study. The stratigraphic relationship among the primary geohydrologic units in the Ozark Plateaus province is discussed in Chapter A of this Hydrologic Investigations Atlas series. This chapter focuses on the Ozark aquifer, a geohydrologic unit within the Ozark Plateaus aquifer system underlying the Ozark Plateaus province.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha711E","usgsCitation":"Imes, J.L., 1990, Major geohydrologic units in and adjacent to the Ozark Plateaus province, Missouri, Arkansas, Kansas and Oklahoma: Ozark aquifer: U.S. Geological Survey Hydrologic Atlas 711, 3 Plates: 40.50 x 35.00 inches, https://doi.org/10.3133/ha711E.","productDescription":"3 Plates: 40.50 x 35.00 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":186549,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89710,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/711e/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89709,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/711e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":411998,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16117.htm","linkFileType":{"id":5,"text":"html"}},{"id":89708,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/711e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"750000","country":"United States","state":"Arkansas, Kansas, Missouri, Oklahoma","otherGeospatial":"Ozark aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -96.25,\n 35.05\n ],\n [\n -96.25,\n 39.667\n ],\n [\n -89.1,\n 39.667\n ],\n [\n -89.1,\n 35.05\n ],\n [\n -96.25,\n 35.05\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64977a","contributors":{"authors":[{"text":"Imes, Jeffrey L. jimes@usgs.gov","contributorId":2983,"corporation":false,"usgs":true,"family":"Imes","given":"Jeffrey","email":"jimes@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":277974,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68196,"text":"ha716 - 1990 - Water resources of the Westfield and Farmington River basins, Massachusetts","interactions":[],"lastModifiedDate":"2015-10-28T12:06:39","indexId":"ha716","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"716","title":"Water resources of the Westfield and Farmington River basins, Massachusetts","docAbstract":"A hydrologic study of the Westfield and Farmington River basins in Massachusetts was conducted by the U.S. Geological Survey, in cooperation with the Commonwealth of Massachusetts Department of Environmental Management, Division of Water Resources, from 1984 to 1986. The study was the final part of a statewide basin-by-basin investigations program designed to provide baseline information on the State's water resources.
The objectives of this report are to: (1) delineate the stratified-drift aquifers of the Westfield and Farmington River basins and present descriptions of their water-yielding characteristics; (2) describe low-flow characteristics, regulation, and diversion of streamflow in the basins; and (3) characterize the quality of ground water and surface water in the basins. The report shows the transmissivity of unconsolidated materials, the availability of ground water, and the surficial geology of the area on a 1:48,000-scale map. High- and low-flow analysis, regional flood-flow equations, diversions, water quality, and water use are also described.
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr90552","usgsCitation":"Kleeschulte, M., and Cross, P.W., 1990, Hydrologic data for the Weldon Spring chemical plant site and vicinity property, St. Charles County, Missouri, 1986-90: U.S. Geological Survey Open-File Report 90-552, vi, 117 p., https://doi.org/10.3133/ofr90552.","productDescription":"vi, 117 p.","costCenters":[],"links":[{"id":152178,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0552/report-thumb.jpg"},{"id":49131,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0552/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":390201,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17969.htm"}],"country":"United States","state":"Missouri","county":"St. Charles County","otherGeospatial":"Weldon Spring Chemical Plant site and vicinity property","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -90.668,\n 38.653\n ],\n [\n -90.783,\n 38.653\n ],\n [\n -90.783,\n 38.75\n ],\n [\n -90.668,\n 38.75\n ],\n [\n -90.668,\n 38.653\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db608256","contributors":{"authors":[{"text":"Kleeschulte, M. J.","contributorId":73222,"corporation":false,"usgs":true,"family":"Kleeschulte","given":"M. J.","affiliations":[],"preferred":false,"id":181301,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cross, P. W.","contributorId":100415,"corporation":false,"usgs":true,"family":"Cross","given":"P.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":181302,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":20394,"text":"ofr90112 - 1990 - Hydrologic and chemical data from selected wells and springs in southern Elmore County, including Mountain Home Air Force Base, southwestern Idaho, Fall 1989","interactions":[],"lastModifiedDate":"2013-11-12T15:51:14","indexId":"ofr90112","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-112","title":"Hydrologic and chemical data from selected wells and springs in southern Elmore County, including Mountain Home Air Force Base, southwestern Idaho, Fall 1989","docAbstract":"Hydrologic and chemical data were collected during September through November 1989 from 90 wells and 6 springs in southern Elmore County, southwestern Idaho. These data were collected to characterize the chemical quality of water in major water-yielding zones in areas near Mountain Home and the Mountain Home Air Force Base. The data include well and spring locations, well-construction and water-level information, and chemical analysis of water from each well and spring inventoried.
\nGround water in the study area is generally suitable for most uses. In localized areas, water is highly mineralized, and pH, concentrations of dissolved sulfate, chloride, or nitrite plus nitrate as nitrogen exceed national public drinking water limits. Fecal coliform and fecal streptococci bacteria were detected in separate water samples. One or more volatile organic compounds were detected in water samples from 15 wells, and the concentration of benzene exceeded the national public drinking water limit in a water sample from one well.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Boise, ID","doi":"10.3133/ofr90112","collaboration":"Prepared in cooperation with Department of the Air Force","usgsCitation":"Parliman, D., and Young, H., 1990, Hydrologic and chemical data from selected wells and springs in southern Elmore County, including Mountain Home Air Force Base, southwestern Idaho, Fall 1989: U.S. Geological Survey Open-File Report 90-112, iii, 35 p. :ill. ;28 cm., https://doi.org/10.3133/ofr90112.","productDescription":"iii, 35 p. :ill. ;28 cm.","numberOfPages":"40","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":153173,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0112/report-thumb.jpg"},{"id":49941,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0112/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","country":"United States","state":"Idaho","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.083333,42.933333 ], [ -116.083333,43.225 ], [ -115.625,43.225 ], [ -115.625,42.933333 ], [ -116.083333,42.933333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6832fc","contributors":{"authors":[{"text":"Parliman, D. J.","contributorId":64220,"corporation":false,"usgs":true,"family":"Parliman","given":"D. J.","affiliations":[],"preferred":false,"id":182578,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Young, H.W.","contributorId":68278,"corporation":false,"usgs":true,"family":"Young","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":182579,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":19048,"text":"ofr90184 - 1990 - Feasibility of privatization of the hydrologic data collection and analysis functions of the U.S. Geological Survey.","interactions":[],"lastModifiedDate":"2012-02-02T00:07:31","indexId":"ofr90184","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-184","title":"Feasibility of privatization of the hydrologic data collection and analysis functions of the U.S. Geological Survey.","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/ofr90184","usgsCitation":"Wahl, K.L., Condes de la Torre, A., Kilpatrick, F.A., Martens, L.A., Mattraw, H., Pollock, D.W., Rosenshein, J.S., and Solley, W.B., 1990, Feasibility of privatization of the hydrologic data collection and analysis functions of the U.S. Geological Survey.: U.S. Geological Survey Open-File Report 90-184, 64 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr90184.","productDescription":"64 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":152005,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0184/report-thumb.jpg"},{"id":48483,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0184/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f71ad","contributors":{"authors":[{"text":"Wahl, Kenneth L.","contributorId":61024,"corporation":false,"usgs":true,"family":"Wahl","given":"Kenneth","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":180215,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Condes de la Torre, Alberto","contributorId":73570,"corporation":false,"usgs":true,"family":"Condes de la Torre","given":"Alberto","email":"","affiliations":[],"preferred":false,"id":180217,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kilpatrick, Frederick A.","contributorId":19306,"corporation":false,"usgs":true,"family":"Kilpatrick","given":"Frederick","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":180213,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Martens, Lawrence A.","contributorId":17973,"corporation":false,"usgs":true,"family":"Martens","given":"Lawrence","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":180212,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mattraw, Harold C.","contributorId":81878,"corporation":false,"usgs":true,"family":"Mattraw","given":"Harold C.","affiliations":[],"preferred":false,"id":180218,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Pollock, David W. dwpolloc@usgs.gov","contributorId":4248,"corporation":false,"usgs":true,"family":"Pollock","given":"David","email":"dwpolloc@usgs.gov","middleInitial":"W.","affiliations":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":180211,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Rosenshein, Joseph S.","contributorId":32904,"corporation":false,"usgs":true,"family":"Rosenshein","given":"Joseph","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":180214,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Solley, Wayne B.","contributorId":61409,"corporation":false,"usgs":true,"family":"Solley","given":"Wayne","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":180216,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":26844,"text":"wri904022 - 1990 - Geohydrology and ground-water geochemistry at a sub-arctic landfill, Fairbanks, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:08:21","indexId":"wri904022","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-4022","title":"Geohydrology and ground-water geochemistry at a sub-arctic landfill, Fairbanks, Alaska","docAbstract":"The Fairbanks-North Star Borough, Alaska, landfill is located on silt, sand, and gravel deposits of the Tanana River flood plain, about 3 miles south of the city of Fairbanks water supply wells. The landfill has been in operation for about 25 years in this sub-arctic region of discontinuous permafrost. The cold climate limits biological activity within the landfill with corresponding low gas and leachate production. Chloride concentrations, specific conductance, water temperature, and earth conductivity measurements indicate a small plume of leachate flowing to the northwest from the landfill. The leachate remains near the water table as it flows northwestward toward a drainage ditch. Results of computer modeling of this local hydrologic system indicate that some of the leachate may be discharging to the ditch. Chemical data show that higher-than-background concentrations of several ions are present in the plume. However, the concentrations appear to be reduced to background levels within a short distance along the path of groundwater flow from the landfill, and thus the leachate is not expected to affect the water supply wells. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri904022","usgsCitation":"Downey, J.S., 1990, Geohydrology and ground-water geochemistry at a sub-arctic landfill, Fairbanks, Alaska: U.S. Geological Survey Water-Resources Investigations Report 90-4022, vi, 25 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri904022.","productDescription":"vi, 25 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124199,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4022/report-thumb.jpg"},{"id":55735,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4022/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688527","contributors":{"authors":[{"text":"Downey, J. S.","contributorId":100013,"corporation":false,"usgs":true,"family":"Downey","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":197105,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":20210,"text":"ofr90389 - 1990 - Manual for comparing methods of designing hydrologic-data-collection networks","interactions":[],"lastModifiedDate":"2012-02-02T00:07:39","indexId":"ofr90389","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-389","title":"Manual for comparing methods of designing hydrologic-data-collection networks","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr90389","usgsCitation":"Moss, M.E., and Tasker, G.D., 1990, Manual for comparing methods of designing hydrologic-data-collection networks: U.S. Geological Survey Open-File Report 90-389, 104 p. :ill. ;28 cm., https://doi.org/10.3133/ofr90389.","productDescription":"104 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":152384,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0389/report-thumb.jpg"},{"id":49756,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0389/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64aebd","contributors":{"authors":[{"text":"Moss, M. E.","contributorId":50500,"corporation":false,"usgs":true,"family":"Moss","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":182254,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tasker, Gary D.","contributorId":83097,"corporation":false,"usgs":true,"family":"Tasker","given":"Gary","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":182255,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27060,"text":"wri894046 - 1990 - Surface-water hydrology and salinity of the Anclote River estuary, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:41","indexId":"wri894046","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"89-4046","title":"Surface-water hydrology and salinity of the Anclote River estuary, Florida","docAbstract":"Direct measurements of streamflow, tides, and salinity in the Anclote River Estuary, Florida were made during the period January 1984 through May 1986; historical streamflow was compared to that measured during the study; the influence of well-field pumpage on streamflow was evaluated; and regression relations between salinity, tide, and average daily streamflow were developed. Mean monthly streamflows during the study period generally were lower than the corresponding long-term monthly averages yet representative of flows that typically enter the estuary. The influence of pumpage from individual well fields in or near the basin on streamflow was not statistically significant; the influence of total well-field pumpage, however, was significant at the 5% level. The upstream daily location of 0.44-, 5.0-, 10-, and 18-parts-per-thousand (ppt) salinity was quantified using multiple regression techniques. Streamflow used in the analysis ranged from 2.3 to 263 cu ft/sec, and high tides ranged from 0.25 ft below to 2.76 ft above sea level. Vertical salinity profiles indicated partially to well-mixed conditions throughout the estuary during the study period. Results of the regression analyses show that streamflow has a large effect on the location of the saltwater- freshwater interface (defined as 0.44 ppt salinity) as well as water having a salinity of 5.0 ppt. The location of water having salinities greater than 5.0 ppt is affected increasingly by tide, with a corresponding decrease in effect by streamflow. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports,","doi":"10.3133/wri894046","usgsCitation":"Fernandez, M., 1990, Surface-water hydrology and salinity of the Anclote River estuary, Florida: U.S. Geological Survey Water-Resources Investigations Report 89-4046, iv, 34 p. :ill. ;29 cm., https://doi.org/10.3133/wri894046.","productDescription":"iv, 34 p. :ill. ;29 cm.","costCenters":[],"links":[{"id":158770,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4046/report-thumb.jpg"},{"id":55935,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4046/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a6fe","contributors":{"authors":[{"text":"Fernandez, Mario Jr.","contributorId":77155,"corporation":false,"usgs":true,"family":"Fernandez","given":"Mario","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":197487,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27087,"text":"wri894089 - 1990 - Hydrology, aquatic macrophytes, and water quality of Black Earth Creek and its tributaries, Dane County, Wisconsin, 1985-86","interactions":[],"lastModifiedDate":"2015-10-20T10:21:39","indexId":"wri894089","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"89-4089","title":"Hydrology, aquatic macrophytes, and water quality of Black Earth Creek and its tributaries, Dane County, Wisconsin, 1985-86","docAbstract":"An intensive data-collection program for the Black Earth Creek basin in southern Wisconsin was conducted from October 1984 through September 1986 to assess the hydrology, aquatic macrophytes, and water quality in Black Earth Creek by the U.S. Geological Survey, in cooperation with the Wisconsin Department of Natural Resources. Three sites on two cold-water trout streams Black Earth Creek at Cross Plains, Black Earth Creek near Cross Plains, and Garfoot Creek near Cross Plains were continuously monitored for streamflow and water-quality data. One site in a warm-water stream, Brewery Creek at Cross Plains, also was monitored. Aquatic macrophyte biomass was determined for three sites on Black Earth Creek.
\nStreamflow at Black Earth Creek at Black Earth during the 1985 and 1986 water years (WY) were 44 and 60 percent greater than the long-term mean discharge of 33.3 ft3/s (cubic feet per second) for the period 1955-86. Water year 1986 had the highest annual mean discharge, 53.4 ft3/s, since records began in 1954 at the most downstream site Black Earth Creek at Black Earth. Although there have been considerable fluctuations in streamflow, it has tended to increase since WY 1965 as a result of above-average precipitation and consequent rising ground-water levels.
\nTrout population densities may be related to annual mean streamflow. A regression analysis of adult trout populations and the 3-year moving annual mean discharge had a correlation coefficient of 0.75 with a standard error of 83 percent.
\nAquatic macrophyte biomass in Black Earth Creek was substantially less in 1986 than in 1985 as a result of substrate scouring from the flood of July 25, 1985. The frequency of occurrence of species during 1985 and 1986 was similar to that of 1981, and seasonal succession of species also was similar; Potamogeton crispus dominated early in the year and senesced in July. P. crispus and P. pectinatus, both indicative of eutrophic conditions, dominated upstream and downstream, respectively; neither species is native to the area. In 1985, the greatest biomass was found upstream from Cross Plains. This large biomass caused diurnal fluctuations in dissolved-oxygen concentration of 5 to 6 mg/L (milligrams per liter) as a result of photosynthesis and respiration. Many of the dissolved-oxygen minimums, recorded at night, were less than the State 6.0-mg/L water-quality standard for trout waters. Discharge from point sources may adversely affect Black Earth Creek's water quality. Warm water discharged to Black Earth Creek from a gravel pit operation upstream from Cross Plains increased water temperatures 2 to 4 degrees Celsius and decreased the dissolved oxygen about 1 mg/L at a site 1.8 miles downstream. Runoff from a settling pond from a landfill operation in the headwaters of the Black Earth Creek basin drains through a wetland that drains to Black Earth Creek and contained as much as 60 mg/L ammonia nitrogen, 980 mg/L biochemical oxygen demand, and 1,300 mg/L chemical oxygen demand, which may be detrimental to trout.
\nGarfoot Creek had the highest suspended-sediment and phosphorus yields per unit area of the three upstream basins during low to moderate runoff. Detention ponds in the Brewery Creek basin appear to be less effective in controlling suspended-sediment and phosphorus loads during periods of high runoff than during moderate runoff. Brewery Creek had the highest concentrations of suspended sediment and total phosphorus during low and high flows. The water quality at the Black Earth Creek gaging station at Black Earth was affected by Garfoot Creek and unnamed tributaries. As a result, yields of suspended sediment, phosphorus, and nitrogen increased between Cross Plains and Black Earth. High streamflows during WY 1985 resulted in suspendedsediment yields at Black Earth Creek at Black Earth that were 29 percent greater than the 12-year (1955-65, 85-86) mean; yields ranged from 69.5 ton/mi2 (tons per square mile) in Black Earth Creek at Cross Plains to 116 ton/mi2 in the Brewery Creek basin. Phosphorus yields ranged from 312 lb/mi2 (pounds per square mile) in Black Earth Creek at Cross Plains to 628 lb/mi2 in the Brewery Creek basin. Total nitrogen yields ranged from 3,280 lb/mi2 in the Brewery Creek basin to 6,920 lb/mi2 in the Garfoot Creek basin.
\nAn increase in oxygen demand, caused by agricultural runoff, has resulted in reduced dissolved-oxygen content of the water in both Black Earth and Garfoot Creeks. The most substantial reduction occurred at Black Earth Creek at Cross Plains on July 25, 1985, as a result of the largest storm runoff event during the study. A rainfall of 5.54 inches caused streamflow discharges to increase from 9 to 122 ft3/s and dissolved-oxygen concentrations to decline to 3.0 mg/L; the dissolved-oxygen concentration was less than 6.0 mg/L for 30 hours.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri894089","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Field, S.J., and Graczyk, D., 1990, Hydrology, aquatic macrophytes, and water quality of Black Earth Creek and its tributaries, Dane County, Wisconsin, 1985-86: U.S. Geological Survey Water-Resources Investigations Report 89-4089, vi, 38 p., https://doi.org/10.3133/wri894089.","productDescription":"vi, 38 p.","numberOfPages":"44","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":55953,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4089/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122886,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4089/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","county":"Dane County","otherGeospatial":"Black Earth Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -89.72911834716797,\n 43.18440150752066\n ],\n [\n -89.791259765625,\n 43.09170711357466\n ],\n [\n -89.66697692871094,\n 43.06838615478111\n ],\n [\n -89.54132080078125,\n 43.04555812998933\n ],\n [\n -89.53239440917969,\n 43.11401670811261\n ],\n [\n -89.51934814453125,\n 43.13130731581085\n ],\n [\n -89.52587127685547,\n 43.14082759275761\n ],\n [\n -89.72911834716797,\n 43.18440150752066\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc71d","contributors":{"authors":[{"text":"Field, S. J.","contributorId":50540,"corporation":false,"usgs":true,"family":"Field","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":197532,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Graczyk, D.J.","contributorId":108119,"corporation":false,"usgs":true,"family":"Graczyk","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":197533,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":18913,"text":"ofr89623 - 1990 - Hydrologic data collected in the vicinity of the proposed gamma-ray and neutrino detector site, Hot Spring County, Arkansas, 1988-89","interactions":[],"lastModifiedDate":"2012-02-02T00:07:31","indexId":"ofr89623","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"89-623","title":"Hydrologic data collected in the vicinity of the proposed gamma-ray and neutrino detector site, Hot Spring County, Arkansas, 1988-89","docAbstract":"An abandoned barite mine in Hot Spring County, Arkansas, has been selected as the location for a proposed gamma-ray and neutrino detector site. As part of the hydrologic evaluation of the site, the U.S. Geological Survey in cooperation with the Arkansas Geological Commission collected hydrologic data at selected locations in the vicinity of the abandoned barite mine. Data collected as part of the project included water quality, pond-evaluation, and precipitation data within the abandoned barite mine and flow and water quality data at selected sites in the vicinity of the mine. Water quality samples from within the abandoned mine were collected at three locations in the pond at selected depths. These data included field measurements of specific conductance, pH, water temperature, dissolved oxygen, major ions, and trace metals. Major ion and trace-metal samples were collected at six stream sites, one lake site, and two wastewater pond sites. Pond elevation and precipitation data from within the abandoned barite mine were measured during the period between July 1, 1988 and June 30, 1989. Twevle discharge measurements during the period between June 21, 1988, and June 26, 1989, were collected at six sites in the vicinity of the abandoned barite mine. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr89623","usgsCitation":"Fitzpatrick, D., and Westerfield, P., 1990, Hydrologic data collected in the vicinity of the proposed gamma-ray and neutrino detector site, Hot Spring County, Arkansas, 1988-89: U.S. Geological Survey Open-File Report 89-623, iv, 17 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89623.","productDescription":"iv, 17 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":151601,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0623/report-thumb.jpg"},{"id":48311,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0623/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f7ed","contributors":{"authors":[{"text":"Fitzpatrick, D. J.","contributorId":33313,"corporation":false,"usgs":true,"family":"Fitzpatrick","given":"D. J.","affiliations":[],"preferred":false,"id":179972,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Westerfield, P.W.","contributorId":50546,"corporation":false,"usgs":true,"family":"Westerfield","given":"P.W.","email":"","affiliations":[],"preferred":false,"id":179973,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27128,"text":"wri864195 - 1990 - Technique for estimating depths of 100-year floods in Pennsylvania","interactions":[],"lastModifiedDate":"2017-07-05T11:24:39","indexId":"wri864195","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"86-4195","title":"Technique for estimating depths of 100-year floods in Pennsylvania","docAbstract":"Techniques are developed for estimating 100-year flood depths in natural channels of unregulated Pennsylvania streams that drain less than 2,200 square miles. Equations and graphs are presented relating the depth of the 100-year flood above median stage and drainage area in five defined hydrologic areas in the State. Another graph defines the relation between drainage area and median depth of flow over the low point of riffles. Thus 100-year depths on riffles can be estimated by summing depth values derived from two simple relations.
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The hydrologic cycle is the natural pathway of water from evaporation to precipitation to infiltration or runoff and to storage from which evaporation can again occur. The science of water use is the study of human influences on the hydrologic cycle. Human activities affect the hydrologic cycle by changing the quantity, distribution, and quality of available water. Quantifying return flow is useful to water managers in evaluating such changes. Return flow is often thought of as what runs down the drain, or what is leftover after the water's purpose has been served. As innocuous as that may sound, return flow plays a significant part in the overall water-use picture.
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C.","contributorId":63410,"corporation":false,"usgs":true,"family":"Trotta","given":"L.","email":"","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":183983,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Horn, M.S.","contributorId":107720,"corporation":false,"usgs":true,"family":"Horn","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":183984,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29135,"text":"wri904069 - 1990 - Geology, hydrology, and water quality of the surficial aquifer system in Volusia County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri904069","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-4069","title":"Geology, hydrology, and water quality of the surficial aquifer system in Volusia County, Florida","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri904069","usgsCitation":"Phelps, G.G., 1990, Geology, hydrology, and water quality of the surficial aquifer system in Volusia County, Florida: U.S. Geological Survey Water-Resources Investigations Report 90-4069, vi, 67 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri904069.","productDescription":"vi, 67 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119733,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4069/report-thumb.jpg"},{"id":58004,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4069/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c639","contributors":{"authors":[{"text":"Phelps, G. G.","contributorId":82346,"corporation":false,"usgs":true,"family":"Phelps","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":200999,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68577,"text":"ha715 - 1990 - Reconnaissance study of the thickness of the unsaturated zone in the western conterminous United States","interactions":[{"subject":{"id":12617,"text":"ofr86402W - 1986 - Reconnaissance study of the thickness of the unsaturated zone in the western conterminous United States","indexId":"ofr86402W","publicationYear":"1986","noYear":false,"chapter":"W","title":"Reconnaissance study of the thickness of the unsaturated zone in the western conterminous United States"},"predicate":"SUPERSEDED_BY","object":{"id":68577,"text":"ha715 - 1990 - Reconnaissance study of the thickness of the unsaturated zone in the western conterminous United States","indexId":"ha715","publicationYear":"1990","noYear":false,"title":"Reconnaissance study of the thickness of the unsaturated zone in the western conterminous United States"},"id":1}],"lastModifiedDate":"2015-10-28T12:04:10","indexId":"ha715","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"715","title":"Reconnaissance study of the thickness of the unsaturated zone in the western conterminous United States","docAbstract":"In 1984, the U.S. Geological Survey began a study of the geologic and hydrologic characteristics of the unsaturated zone in the western conterminous United States. The study area extends from the eastern edge of the Rocky Mountains westward and includes all or parts of the 12 westernmost conterminous States. The goal of the study is to characterize unsaturated flow systems to aid in identifying environments in the western United States that may merit further study for isolation of hazardous waste, including high- and low-level radioactive waste and other toxic waste.
The major physiographic areas discussed in this report (see index map below thickness map) are: (1) Rocky Mountain System consisting of the Southern, Middle, and Northern Rocky Mountains, and the Wyoming Basin; (2) Intermontane Plateaus consisting of the Basin and Range province, and the Colorado and Columbia Plateaus; and (3) Pacific Mountain System (Fenneman, 1946). Two of these areas, the Colorado and Columbia plateaus, exhibit a variety of geohydrologic conditions, and therefore are further subdivided in the discussions that follow.
Outstanding features peculiar to the mountainous area of the Rocky Mountain and the Pacific Mountain Systems are the high rugged mountains and steep relief. These mountains receive greater precipitation than do the lower parts of the otherwise dry western United States. Generally moisture-laden air masses move eastward across the continent, and the mountains force them to higher, cooler altitudes. As the air cools, moisture condenses and precipitates. As a result, the Rocky Mountain and Pacific Mountain Systems have annual precipitation in excess of 30 in.
The Wyoming Basin of the Rocky Mountain System and the Basin and Range province, Colorado Plateaus, and Columbia Plateaus of the Intermontane Plateaus generally have lower altitudes and less relief than do the mountainous areas. The climate throughout most of these provinces generally is semiarid to arid. Annual precipitation is generally less than 16 in. throughout most of the area, and is less than 4 in. in some parts. The mean annual free-water-surface evaporation ranges from 20 to 100in. A large part of the study area is subject to a water deficit because potential evapotranspiration exceeds precipitation. As a consequence of the large water deficit, ground-water recharge generally is small, surface runoff is small, perennial streams and lakes are few, and the depth to ground water commonly is large. The generalized thickness of the unsaturated zone (the depth to ground water), in the western conterminous United States is presented on the map.
This Hydrologic Investigations Atlas, which consists of a series of chapters, presents a description of (1) the physical frameworks and (2) the geohydrology of the principal aquifers and confining systems in Kansas. The report is the result of an investigation that has been made as part of the Central Midwest Regional Aquifer System Analysis (CMRASA), one of several major investigations by the U.S. Geological Survey to define regional aquifer systems. These regional analyses are designed to increase knowledge of major flow regimes and provide data for assessing, developing, and managing water supplies. The CMRASA is an investigation of water in Upper Cambrian through Lower Cretaceous rocks in parts of 10 Central Midwestern States, as shown by the map on the envelope cover.
","language":"ENGLISH","doi":"10.3133/ha722A","usgsCitation":"Wolf, R.J., Hansen, C.V., McGovern, H., and Spinazola, J., 1990, Geohydrologic systems in Kansas with emphasis on systems in Upper Cambrian through Lower Cretaceous rocks: U.S. Geological Survey Hydrologic Atlas 722, 8 maps on 2 sheets :some col. ;sheets 84 x 99 cm. and 120 x 105 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/ha722A.","productDescription":"8 maps on 2 sheets :some col. ;sheets 84 x 99 cm. and 120 x 105 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":90426,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/722a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90427,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/722a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":188196,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ha722A.PNG"}],"scale":"2000000","country":"United 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