No abstract available.
","language":"English","publisher":"American Institute of Hydrology","usgsCitation":"Ames, K.C., 1994, Washington State metals in soils program: Preliminary results: Hydrological Science and Technology, v. 10, no. 1-4, p. 15-30.","productDescription":"16 p.","startPage":"15","endPage":"30","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":321866,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574eb5dee4b0ee97d51a841a","contributors":{"authors":[{"text":"Ames, K. C.","contributorId":20781,"corporation":false,"usgs":true,"family":"Ames","given":"K.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":630836,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70185732,"text":"70185732 - 1994 - Protists from a sewage‐contaminated aquifer on cape cod, Massachusetts","interactions":[],"lastModifiedDate":"2019-02-27T10:16:21","indexId":"70185732","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1800,"text":"Geomicrobiology Journal","active":true,"publicationSubtype":{"id":10}},"title":"Protists from a sewage‐contaminated aquifer on cape cod, Massachusetts","docAbstract":"Several species of flagellates (genera Bodo, Cercomonas, Cryptaulax, Cyathomonas, Goniomonas, Spumella) have been identified in cultures from a plume of organic contamination (treated sewage effluent) within an aquifer on Cape Cod, Massachusetts. Amoebae and numerous unidentifiable 2‐ to 3‐μm flagellates have also been observed. As a rule, flagellates were associated with solid surfaces, or were capable of temporary surface attachment, corroborating earlier observations from in situ and column transport experiments suggesting that protists in the Massachusetts aquifer have a high propensity for association with sediment grain surfaces. Based on the fact that cultures from the uncontaminated part of the aquifer yielded only a few species of protists, it is hypothesized that the greater abundance and variety of food sources in the contaminant plume is capable of supporting a greater number of protistan species.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/01490459409377968","usgsCitation":"Novarino, G., Warren, A., Kinner, N.E., and Harvey, R.W., 1994, Protists from a sewage‐contaminated aquifer on cape cod, Massachusetts: Geomicrobiology Journal, v. 12, no. 1, p. 23-36, https://doi.org/10.1080/01490459409377968.","productDescription":"14 p. ","startPage":"23","endPage":"36","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338474,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58db7637e4b0ee37af29e4de","contributors":{"authors":[{"text":"Novarino, Gianfranco","contributorId":189951,"corporation":false,"usgs":false,"family":"Novarino","given":"Gianfranco","email":"","affiliations":[],"preferred":false,"id":686569,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Warren, Alan","contributorId":189351,"corporation":false,"usgs":false,"family":"Warren","given":"Alan","email":"","affiliations":[],"preferred":false,"id":686570,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kinner, Nancy E.","contributorId":189349,"corporation":false,"usgs":false,"family":"Kinner","given":"Nancy","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":686571,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Harvey, Ronald W. 0000-0002-2791-8503 rwharvey@usgs.gov","orcid":"https://orcid.org/0000-0002-2791-8503","contributorId":564,"corporation":false,"usgs":true,"family":"Harvey","given":"Ronald","email":"rwharvey@usgs.gov","middleInitial":"W.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":686572,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70182197,"text":"70182197 - 1994 - Stream and floodplain restoration in a riparian ecosystem disturbed by placer mining","interactions":[],"lastModifiedDate":"2017-05-19T18:21:42","indexId":"70182197","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1454,"text":"Ecological Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Stream and floodplain restoration in a riparian ecosystem disturbed by placer mining","docAbstract":"Techniques for the hydrologic restoration of placer-mined streams and floodplains were developed in Denali National Park and Preserve Alaska, USA. The hydrologic study focused on a design of stream and floodplain geometry using hydraulic capacity and shear stress equations. Slope and sinuosity values were based on regional relationships. Design requirements include a channel capacity for a 1.5-year (bankfull) discharge and a floodplain capacity for a 1.5- to 100-year discharge. Concern for potential damage to the project from annual flooding before natural revegetation occurs led to development of alder (Alnus crispa) brush bars to dissipate floodwater energy and encourage sediment deposition. The brush bars, constructed of alder bundles tied together and anchored laterally adjacent to the channel, were installed on the floodplain in several configurations to test their effectiveness. A moderate flood near the end of the two-year construction phase of the project provided data on channel design, stability, floodplain erosion, and brush bar effectiveness. The brush bars provided substantial protection, but unconsolidated bank material and a lack of bed armour for a new channel segment led to some bank erosion, slope changes and an increase in sinuosity in several reaches of the study area.
","language":"English","publisher":"Elsevier","doi":"10.1016/0925-8574(94)90041-8","usgsCitation":"Karle, K.F., and Densmore, R.V., 1994, Stream and floodplain restoration in a riparian ecosystem disturbed by placer mining: Ecological Engineering, v. 3, no. 2, p. 121-133, https://doi.org/10.1016/0925-8574(94)90041-8.","productDescription":"13 p.","startPage":"121","endPage":"133","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":335853,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Denali National Park and Preserve, Glen Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -150.7866668701172,\n 63.51779683618753\n ],\n [\n -150.7866668701172,\n 63.58\n ],\n [\n -150.6778335571289,\n 63.58\n ],\n [\n -150.6778335571289,\n 63.51779683618753\n ],\n [\n -150.7866668701172,\n 63.51779683618753\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"3","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58ac0e34e4b0ce4410e7d620","contributors":{"authors":[{"text":"Karle, Kenneth F.","contributorId":37461,"corporation":false,"usgs":true,"family":"Karle","given":"Kenneth","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":669948,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Densmore, Roseann V.","contributorId":24022,"corporation":false,"usgs":true,"family":"Densmore","given":"Roseann","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":669949,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":44749,"text":"wri934215 - 1994 - Water-surface profile and flood boundaries for the computed 100-year flood, Muddy Creek, Northern Cheyenne Indian Reservation, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:10:57","indexId":"wri934215","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"93-4215","title":"Water-surface profile and flood boundaries for the computed 100-year flood, Muddy Creek, Northern Cheyenne Indian Reservation, Montana","docAbstract":"Hydrologic and hydraulic evaluations of Muddy Creek were made to determine the magnitude of the 100-year flood and the extent of flooding that would occur as the result of this flood. Forty-three cross sections were surveyed and 14 cross sections were synthesized along a 6.7-mile reach of Muddy Creek. Data from the surveys were used to calculate the water-surface flood elevation at each cross section using a computer program (WSPRO) developed by the U.S. Geological Survey. The water-surface profile of the computed 100-year flood elevations was then drawn. The profile shows the streambed elevation and the location of one bridge, one culvert, and cross sections. The computed 100-year flood elevation at each cross section was used to delineate the width of the flood plain at that section. Flood boundaries between cross sections were interpolated using contour lines on topographic maps.","language":"ENGLISH","doi":"10.3133/wri934215","usgsCitation":"Omang, R.J., 1994, Water-surface profile and flood boundaries for the computed 100-year flood, Muddy Creek, Northern Cheyenne Indian Reservation, Montana: U.S. Geological Survey Water-Resources Investigations Report 93-4215, 1 map ; 60 x 18 cm., on sheet 76 x 95 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/wri934215.","productDescription":"1 map ; 60 x 18 cm., on sheet 76 x 95 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":168801,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":82055,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4215/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d60","contributors":{"authors":[{"text":"Omang, R. J.","contributorId":31365,"corporation":false,"usgs":true,"family":"Omang","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":230364,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18540,"text":"ofr9484 - 1994 - Operation of hydrologic data-collection stations by the U.S. Geological Survey in 1993","interactions":[],"lastModifiedDate":"2012-02-02T00:07:27","indexId":"ofr9484","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-84","title":"Operation of hydrologic data-collection stations by the U.S. Geological Survey in 1993","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr9484","usgsCitation":"Condes de la Torre, A., 1994, Operation of hydrologic data-collection stations by the U.S. Geological Survey in 1993: U.S. Geological Survey Open-File Report 94-84, vii, 53 p. :chiefly ill., maps ;28 cm., https://doi.org/10.3133/ofr9484.","productDescription":"vii, 53 p. :chiefly ill., maps ;28 cm.","costCenters":[],"links":[{"id":150730,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0084/report-thumb.jpg"},{"id":47891,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0084/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af1e4b07f02db6917b4","contributors":{"authors":[{"text":"Condes de la Torre, Alberto","contributorId":73570,"corporation":false,"usgs":true,"family":"Condes de la Torre","given":"Alberto","email":"","affiliations":[],"preferred":false,"id":179304,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1002403,"text":"1002403 - 1994 - Recent accretion in two managed marsh impoundments in coastal Louisiana","interactions":[],"lastModifiedDate":"2019-04-29T11:35:56","indexId":"1002403","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1450,"text":"Ecological Applications","active":true,"publicationSubtype":{"id":10}},"title":"Recent accretion in two managed marsh impoundments in coastal Louisiana","docAbstract":"Recent accretion was measured by the feldspar marker horizon method in two gravity-drained, managed, marsh impoundments and unmanaged reference marshes located on the rapidly subsiding coast of Louisiana. Water level management was designed to limit hydrologic exchange to the managed marsh by regulating the direction and rate of water flows. During a drawdown-flooding water management cycle, the unmanaged reference marshes had significantly higher vertical accretion rates, higher soil bulk density and soil mineral matter content, lower soil organic matter content, and higher rates of organic matter accumulation than the managed marsh. The rate of mineral matter accumulation was higher in both reference marshes, but was significantly higher in only one. Spatial variability in accumulation rates was low when analyzed in one managed marsh site, suggesting a primarily autochthonous source of matter. In contrast, the associated reference marsh apparently received allochthonous material that settled out in a distinct spatial pattern as water velocity decreased. The impoundment marshes experienced an accretion deficit of one full order of magnitude (0.1 vs. 1.0 m/yr) based on comparison of accretion and sea level rise data, while the unmanaged reference marshes experienced a five-fold smaller deficit or no deficit. These data suggest that the gravity-drained impoundments likely have a shorter life expectancy than the reference marshes in the rapidly subsiding Louisiana coast.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecological Applications","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2307/1942126","usgsCitation":"Cahoon, D.R., 1994, Recent accretion in two managed marsh impoundments in coastal Louisiana: Ecological Applications, v. 4, no. 1, p. 166-176, https://doi.org/10.2307/1942126.","productDescription":"p. 166-176","startPage":"166","endPage":"176","numberOfPages":"11","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":15418,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.esajournals.org/doi/abs/10.2307/1942126","linkFileType":{"id":5,"text":"html"},"description":"7002.000000000000000"},{"id":133989,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629b9a","contributors":{"authors":[{"text":"Cahoon, Donald R. 0000-0002-2591-5667","orcid":"https://orcid.org/0000-0002-2591-5667","contributorId":65424,"corporation":false,"usgs":true,"family":"Cahoon","given":"Donald","email":"","middleInitial":"R.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":312090,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29991,"text":"wri934146 - 1994 - Hydrogeologic characterization of a proposed landfill expansion in Pickens County near Easley, South Carolina","interactions":[],"lastModifiedDate":"2023-03-24T20:22:07.958157","indexId":"wri934146","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"93-4146","title":"Hydrogeologic characterization of a proposed landfill expansion in Pickens County near Easley, South Carolina","docAbstract":"This report presents the results of a hydrogeologic study in the Piedmont physiographic province of South Carolina to obtain geologic, hydrologic, and water-quality data from the site of a proposed landfill expansion in Pickens County near Easley, South Carolina. The geology of the study area is typical of the Piedmont region. The unconsolidated regolith on the site is soil and saprolite, which is a product of the weathered parent rock. The soil ranges in thickness from about 5 to 20 feet. The saprolite ranges in thickness from about 5 to 134 feet. The most abundant parent rock type in the area is a biotite gneiss. Ground- and surface-water data were collected at the site. Slug tests on the saprolite indicate a mean hydraulic conductivity of 3 x 0.000003 feet per second. Transmissivity ranges from 12 to 27 cubic feet per day per feet (squared per day). The ground-water velocity for the site ranges from 3 to 6 feet per year. The closest major stream to the site is Golden Creek. Based on low-flow data for Golden Creek, the estimated minimum 7 consecutive day flow that has a recurrence interval of 10 years (7Q10) at station 02186102 is 2.4 cubic feet per second. Water samples were collected from five monitoring wells at the proposed landfill expansion site and from one stream adjacent to the expansion site. Measured pH units ranged from 5.5 to 8.1, and alkalinity concentrations ranged from 5.1 to 73 milligrams per liter as CaCO3. Other water- quality data obtained included temperature and specific conductance, and 5-day BOD (biochemical oxygen demand), bicarbonate, ammonia-nitrogen, nitrite-nitrogen, nitrite plus nitrate, organic carbon, calcium, magnesium, sodium, potassium, chloride, sulfate, fluoride, and selected trace metal concentrations.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri934146","usgsCitation":"Stringfield, W.J., 1994, Hydrogeologic characterization of a proposed landfill expansion in Pickens County near Easley, South Carolina: U.S. Geological Survey Water-Resources Investigations Report 93-4146, iv, 28 p., https://doi.org/10.3133/wri934146.","productDescription":"iv, 28 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":414741,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47848.htm","linkFileType":{"id":5,"text":"html"}},{"id":58799,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4146/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123544,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4146/report-thumb.jpg"}],"country":"United States","state":"South Carolina","county":"Pickens County","city":"Easley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -82.6689,\n 34.8292\n ],\n [\n -82.6689,\n 34.8206\n ],\n [\n -82.6583,\n 34.8206\n ],\n [\n -82.6583,\n 34.8292\n ],\n [\n -82.6689,\n 34.8292\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628b5d","contributors":{"authors":[{"text":"Stringfield, W. J.","contributorId":73236,"corporation":false,"usgs":true,"family":"Stringfield","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":202490,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23963,"text":"ofr9491 - 1994 - Bibliography of publications from the Toxic Substances Hydrology Program, U.S. Geological Survey","interactions":[],"lastModifiedDate":"2013-12-13T13:25:17","indexId":"ofr9491","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-91","title":"Bibliography of publications from the Toxic Substances Hydrology Program, U.S. Geological Survey","docAbstract":"The U.S. Geological Survey began the Toxic Substances Hydrology Program in 1982 to study, in an interdisciplinary\natmosphere, the fate and effects of toxic substances in the environment. The objective of the Program\nis to provide the earth-science information needed to prevent or mitigate contamination of the Nation's ground\nand surface waters. To achieve this goal, research is conducted in four categories--focused field investigations\nof contaminated sites, additional research on toxic substances hydrology, development of methods to study or\nsample contaminated waters, and investigations of nonpoint sources of contamination. This report contains citations\nof reports on research conducted under the auspices of the Program from the beginning of the Program\nthrough the end of 1993.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Tallahassee, FL","doi":"10.3133/ofr9491","issn":"0094-9140","usgsCitation":"Morganwalp, D.W., 1994, Bibliography of publications from the Toxic Substances Hydrology Program, U.S. Geological Survey: U.S. Geological Survey Open-File Report 94-91, iv, 156 p., https://doi.org/10.3133/ofr9491.","productDescription":"iv, 156 p.","numberOfPages":"161","costCenters":[],"links":[{"id":154955,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0091/report-thumb.jpg"},{"id":279458,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0091/report.pdf"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.8,24.5 ], [ -124.8,49.383333 ], [ -66.95,49.383333 ], [ -66.95,24.5 ], [ -124.8,24.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629866","contributors":{"authors":[{"text":"Morganwalp, David W. dwmorgan@usgs.gov","contributorId":5592,"corporation":false,"usgs":true,"family":"Morganwalp","given":"David","email":"dwmorgan@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":191050,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":17876,"text":"ofr93661 - 1994 - Water-resources activities of the U.S. Geological Survey in New Mexico, fiscal year 1992","interactions":[],"lastModifiedDate":"2018-02-08T16:04:24","indexId":"ofr93661","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"93-661","title":"Water-resources activities of the U.S. Geological Survey in New Mexico, fiscal year 1992","docAbstract":"Awareness of our environment in general, and water resources in particular, has brought increased interest in and support of hydrologic data collection and research. The quantity, quality, and distribution of water are extremely important to the future well-being of New Mexico. The State's surface-water resources are minimal and highly variable due to climate and to regulation and diversion; ground-water resources are subject to development that exceeds natural recharge and to potential contamination by land use. Issues related to global climate change, disposal of hazardous wastes, toxic substances in water, water rights, and ground-water contamination are evolving areas of greater public concern. At the same time there is a continuing need for a better understanding of various hydrologic systems and processes in order to manage these limited water resources for maximum benefit to present and future generations.
The U.S. Geological Survey has collected and disseminated information on the water resources of New Mexico for more than a century. The Survey began to collect records of streamflow in New Mexico in December 1888 when the first discharge measurements were made on the Rio Grande near the present gaging station at Embudo. This site, called the \"birthplace of systematic stream gaging,\" was chosen to be the training center for the first hydrographers of the Irrigation Survey, a bureau within the original Geological Survey. Since that time, in cooperation with Federal, State, local, and tribal agencies, we have monitored streams at hundreds of sites throughout the State and have a current network of more than 200 streamflow-gaging stations. Through the Cooperative Program, we also have established sites where ground-water levels are monitored to document changes in ground-water storage or where surface-water and groundwater samples are collected to determine water chemistry, and we have undertaken investigative studies to define the availability, quality, and distribution of water resources. Information from the data program and results of investigative studies are made available to water-resources managers, regulators, and the public to be used for the effective management of the State's water resources.
This report provides a brief summary of the activities of the New Mexico District for FY (fiscal year) 1992, including our mission, organization, sources of funding, and descriptions of current projects. This report serves to document not only the content of the program, but also the diversity and complexity of that program. Cooperation among water-resources agencies will be essential in effectively dealing with water-related issues facing New Mexico. We look forward to the challenge of addressing these issues by continuing to provide factual hydrologic data and technically sound areal appraisals and interpretive studies.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Albuquerque, NM","doi":"10.3133/ofr93661","usgsCitation":"1994, Water-resources activities of the U.S. Geological Survey in New Mexico, fiscal year 1992: U.S. Geological Survey Open-File Report 93-661, vi, 75 p., https://doi.org/10.3133/ofr93661.","productDescription":"vi, 75 p.","costCenters":[],"links":[{"id":47114,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0661/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149806,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0661/report-thumb.jpg"}],"country":"United States","state":"New 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Mexico\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67abe7","contributors":{"compilers":[{"text":"Allen, Harriet R.","contributorId":94683,"corporation":false,"usgs":true,"family":"Allen","given":"Harriet","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":727920,"contributorType":{"id":3,"text":"Compilers"},"rank":1}]}} ,{"id":17875,"text":"ofr9492 - 1994 - Water-resources activities of the U.S. Geological Survey in Nebraska, fiscal years 1993-94","interactions":[],"lastModifiedDate":"2012-02-02T00:07:21","indexId":"ofr9492","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-92","title":"Water-resources activities of the U.S. Geological Survey in Nebraska, fiscal years 1993-94","docAbstract":"Water-resources activities of the U.S. Geological Survey in Nebraska consist principally of hydro- logic data collection and local, areal, or state- wide interpretive studies. These programs are funded by cooperative agreements with State and local agencies, transfer of funds from other Federal agencies, and direct Federal funds. The data and results of the investigations are published or released either by the U.S. Geological Survey or by cooperating agencies. This report describes the hydrologic data-collection programs and local or areal hydrologic investigations in Nebraska during fiscal yars 1993 and 1994 and provides a list of reports released by the Nebraska District during 1985-93.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr9492","usgsCitation":"Sojka, A.M., and Fitzpatrick, D., 1994, Water-resources activities of the U.S. Geological Survey in Nebraska, fiscal years 1993-94: U.S. Geological Survey Open-File Report 94-92, vi, 45 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr9492.","productDescription":"vi, 45 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":149805,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0092/report-thumb.jpg"},{"id":47113,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0092/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9e9c","contributors":{"authors":[{"text":"Sojka, A. M. (compiler)","contributorId":107715,"corporation":false,"usgs":true,"family":"Sojka","given":"A.","suffix":"(compiler)","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":178106,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fitzpatrick, D. J.","contributorId":33313,"corporation":false,"usgs":true,"family":"Fitzpatrick","given":"D. J.","affiliations":[],"preferred":false,"id":178105,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29170,"text":"wri944169 - 1994 - An interactive code (NETPATH) for modeling NET geochemical reactions along a flow PATH, version 2.0","interactions":[],"lastModifiedDate":"2020-04-12T14:27:07.34098","indexId":"wri944169","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"94-4169","title":"An interactive code (NETPATH) for modeling NET geochemical reactions along a flow PATH, version 2.0","docAbstract":"NETPATH is an interactive Fortran 77 computer program used to interpret net geochemical mass-balance reactions between an initial and final water along a hydrologic flow path. Alternatively, NETPATH computes the mixing proportions of two to five initial waters and net geochemical reactions that can account for the observed composition of a final water. The program utilizes previously defined chemical and isotopic data for waters from a hydrochemical system. For a set of mineral and (or) gas phases hypothesized to be the reactive phases in the system, NETPATH calculates the mass transfers in every possible combination of the selected phases that accounts for the observed changes in the selected chemical and (or) isotopic compositions observed along the flow path. The calculations are of use in interpreting geochemical reactions, mixing proportions, evaporation and (or) dilution of waters, and mineral mass transfer in the chemical and isotopic evolution of natural and environmental waters. Rayleigh distillation calculations are applied to each mass-balance model that satisfies the constraints to predict carbon, sulfur, nitrogen, and strontium isotopic compositions at the end point, including radiocarbon dating. DB is an interactive Fortran 77 computer program used to enter analytical data into NETPATH, and calculate the distribution of species in aqueous solution. This report describes the types of problems that can be solved, the methods used to solve problems, and the features available in the program to facilitate these solutions. Examples are presented to demonstrate most of the applications and features of NETPATH. The codes DB and NETPATH can be executed in the UNIX or DOS1 environment. This report replaces U.S. Geological Survey Water-Resources Investigations Report 91-4078, by Plummer and others, which described the original release of NETPATH, version 1.0 (dated December, 1991), and documents revisions and enhancements that are included in version 2.0. 1 The use of trade, brand or product names in this report is for identification purposes only and does not constitute endorsement by the U.S. Geological Survey.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944169","usgsCitation":"Plummer, N., Prestemon, E.C., and Parkhurst, D.L., 1994, An interactive code (NETPATH) for modeling NET geochemical reactions along a flow PATH, version 2.0 (Version 2.0): U.S. Geological Survey Water-Resources Investigations Report 94-4169, iv, 130 p. , https://doi.org/10.3133/wri944169.","productDescription":"iv, 130 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":124969,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4169/report-thumb.jpg"},{"id":58044,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4169/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Version 2.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db684566","contributors":{"authors":[{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":201073,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Prestemon, Eric C.","contributorId":45352,"corporation":false,"usgs":true,"family":"Prestemon","given":"Eric","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":201074,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Parkhurst, David L. 0000-0003-3348-1544 dlpark@usgs.gov","orcid":"https://orcid.org/0000-0003-3348-1544","contributorId":1088,"corporation":false,"usgs":true,"family":"Parkhurst","given":"David","email":"dlpark@usgs.gov","middleInitial":"L.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":201072,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":19596,"text":"ofr9456 - 1994 - Hydrologic data for the Big Spring basin, Clayton County, Iowa, water year 1991","interactions":[],"lastModifiedDate":"2016-03-18T11:55:06","indexId":"ofr9456","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-56","title":"Hydrologic data for the Big Spring basin, Clayton County, Iowa, water year 1991","docAbstract":"Hydrologic data were collected in the Big Spring Basin located in Clayton County, Iowa, during the 1991 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.
\nThe largest amount of rainfall during water year 1991 (54.69 inches) was measured at the monitoring site on Unnamed Creek near Luana. The largest monthly rainfall (14.72 inches) occurred in June. Analyses of 39 rain samples indicated that calcium and sulfate were the predominant ions and that median concentrations of nitrate and ammonia as nitrogen were 0.36 and 0.49 mg/L (milligrams per liter), respectively.
\nStream discharge, specific conductance, pH, and water temperature were monitored continuously, and monthly water-quality samples were collected at a site on Roberts Creek and at Big Spring. Nitrite plus nitrate as nitrogen concentrations in 27 samples from Roberts Creek at the point where it leaves the study area ranged from 1.8 to 22 mg/L. Herbicide concentrations in 26 samples from the Roberts Creek site ranged from less than 0.10 μg/L (micrograms per liter) to 43 μg/L. Alachlor was detected in 42 percent of the samples; atrazine in 92 percent; and cyanazine and metolachlor in 35 percent of the samples. The total suspended-sediment load discharged in Roberts Creek was about 160,000 tons. At Big Spring, the ground-water discharge point, the daily mean specific conductance ranged from 414 to 788 microsiemens per centimeter at 25 degrees Celsius, the daily median pH ranged from 6.7 to 7.1, and the daily mean water temperature ranged from 8.5 to 13.0 degrees Celsius. Concentrations of nitrite plus nitrate as nitrogen in 23 samples ranged from 4.2 to 17 mg/L. The total measured suspended-sediment discharged from Big Spring was about 17,000 tons. Alachlor was detected in 26 percent; atrazine in 100 percent; cyanazine in 26 percent, and metolachlor in 9 percent of the samples. The maximum atrazine concentration was 16 μg/L.
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The data were collected and compiled as part of the studies by the U.S. Geological Survey, in cooperation with the U.S. Department of Energy, to characterize surface-water hydrology in the Yucca Mountain area. Streamflow data include daily-mean discharges and peak discharges at 5 continuous-record gaging stations, and peak discharges at 10 crest-stage, partial-record stations and 2 miscellaneous sites. Precipitation data include cumulative totals at 20 stations maintained by the U.S. Geological Survey and daily totals at 15 stations maintained by the Weather Service Nuclear Support Office, National Oceanic and Atmospheric Administration.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94312","collaboration":"Prepared in cooperation with the Nevada Operations Office of the U.S. Department of Energy","usgsCitation":"Kane, T.G., Bauer, D.J., and Martinez, C.M., 1994, Streamflow and selected precipitation data for Yucca Mountain region, southern Nevada and eastern California, water years 1986-90: U.S. Geological Survey Open-File Report 94-312, iv, 118 p., https://doi.org/10.3133/ofr94312.","productDescription":"iv, 118 p.","temporalStart":"1985-10-01","temporalEnd":"1990-09-30","costCenters":[],"links":[{"id":49065,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0312/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152675,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0312/report-thumb.jpg"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Yucca Mountain","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117,36 ], [ -117,37.5 ], [ -115.5,37.5 ], [ -115.5,36 ], [ -117,36 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4f48","contributors":{"authors":[{"text":"Kane, Thomas G. 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8e0b","contributors":{"authors":[{"text":"Hansen, C. V.","contributorId":116823,"corporation":false,"usgs":true,"family":"Hansen","given":"C.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":278077,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spinazola, J. M.","contributorId":32574,"corporation":false,"usgs":true,"family":"Spinazola","given":"J. M.","affiliations":[],"preferred":false,"id":278079,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wolf, R. J.","contributorId":21518,"corporation":false,"usgs":true,"family":"Wolf","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278078,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":7000094,"text":"7000094 - 1994 - U.S. Geological Survey yearbook, fiscal year 1993: At work across the Nation","interactions":[],"lastModifiedDate":"2018-03-15T14:03:02","indexId":"7000094","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":392,"text":"Yearbook","active":false,"publicationSubtype":{"id":6}},"title":"U.S. Geological Survey yearbook, fiscal year 1993: At work across the Nation","docAbstract":"The need for earth science has never been more paramount. The devastating flooding of the Mississippi River this past year, strikingly portrayed on the cover and discussed in detail in this report (p. 37-42), was a sobering reminder of nature's elemental power. As a Nation, we face many environmental and economic challenges, such as natural hazards, that can be addressed effectively only through science. Water quality, resource assessments, climate change, and toxic wastes are all critical issues that can best be dealt with when approached from a sound scientific base. The goal of the U.S. Geological Survey is to provide hydrologic, geologic, and topographic information and understanding that contribute to the wise management of the Nation's natural resources and that promote the health, safety, and well-being of all Americans. FY1993 has proven to be a particularly challenging one for the USGS. We entered into a time of transition from the long-term leadership of Director Dallas Peck and Associate Director Doyle Frederick to the appointment of a new director. We thank Dallas and Doyle for their many years of service and for their support during the transition.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/7000094","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1994, U.S. Geological Survey yearbook, fiscal year 1993: At work across the Nation: Yearbook, Report: 124 p.; 2 Plates: 17.14 x 10.97 inches and16.93 x 11.02 inches, https://doi.org/10.3133/7000094.","productDescription":"Report: 124 p.; 2 Plates: 17.14 x 10.97 inches and16.93 x 11.02 inches","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":101696,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/yb/1993fy/report.pdf","size":"37003","linkFileType":{"id":1,"text":"pdf"}},{"id":101697,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/yb/1993fy/plate-1.pdf","size":"2354","linkFileType":{"id":1,"text":"pdf"}},{"id":195849,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/yb/1993fy/report-thumb.jpg"},{"id":101698,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/yb/1993fy/plate-2.pdf","size":"1279","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611f19","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535113,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27761,"text":"wri934023 - 1994 - Estimation of water withdrawal and distribution, water use, and wastewater collection and return flow in Cumberland, Rhode Island, 1988","interactions":[],"lastModifiedDate":"2012-02-02T00:08:26","indexId":"wri934023","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"93-4023","title":"Estimation of water withdrawal and distribution, water use, and wastewater collection and return flow in Cumberland, Rhode Island, 1988","docAbstract":"Water-use data collected in Rhode Island by different State agencies or maintained by different public suppliers and wastewater- treatment facilities need to be integrated if these data are to be used in making water- resource management decisions. Water-use data for the town of Cumberland, a small area in northeastern Rhode Island, were compiled and integrated to provide an example of how the procedure could be applied. Integration and reliability assessment of water-use data could be facilitated if public suppliers, wastewater- treatment facilities, and State agencies used a number of standardized procedures for data collection and computer storage. The total surface water and ground water withdrawn in the town of Cumberland during 1988 is estimated to be 15.39 million gallons per day, of which 11.20 million gallons per day was exported to other towns. Water use in Cumberland included 2.51 million gallons per day for domestic use, 0.68 million gallons per day for industrial use, 0.27 million gallons per day for commercial use, and 0.73 million gallons per day for other use, most of which were unmetered use. Disposal of waste- water in Cumberland included 2.03 million gallons per day returned to the hydrologic system and 1.73 million gallons per day exported from Cumberland for wastewater treatment. Consumptive use during 1988 is estimated to be 0.43 million gallons per day.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S., Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri934023","usgsCitation":"Horn, M., Craft, P.A., and Bratton, L., 1994, Estimation of water withdrawal and distribution, water use, and wastewater collection and return flow in Cumberland, Rhode Island, 1988: U.S. Geological Survey Water-Resources Investigations Report 93-4023, v, 54 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri934023.","productDescription":"v, 54 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123840,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4023/report-thumb.jpg"},{"id":56609,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4023/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb1cf","contributors":{"authors":[{"text":"Horn, M.A.","contributorId":92223,"corporation":false,"usgs":true,"family":"Horn","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":198653,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Craft, P. A.","contributorId":102105,"corporation":false,"usgs":true,"family":"Craft","given":"P.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":198654,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bratton, Lisa lbratton@usgs.gov","contributorId":362,"corporation":false,"usgs":true,"family":"Bratton","given":"Lisa","email":"lbratton@usgs.gov","affiliations":[],"preferred":true,"id":198652,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":54648,"text":"wdrMARI931 - 1994 - Water resources data, Massachusetts and Rhode Island, water year 1993","interactions":[],"lastModifiedDate":"2025-09-30T17:56:31.122207","indexId":"wdrMARI931","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MA-RI-93-1","title":"Water resources data, Massachusetts and Rhode Island, water year 1993","docAbstract":"Water resources data for the 1993 water year for Massachusetts and Rhode Island consists of records of stage, discharge, and water quality of streams; contents of lakes and reservoirs; and ground-water levels. This report contains discharge records for 77 gaging stations, month end contents of five lakes and reservoirs, water quality at 10 gaging stations, and water levels for 137 observation wells. Data also are included for 59 low-flow partial-record stations. Miscellaneous hydrologic data were collected at various sites that were not a part of the systematic data-collection program and are published as miscellaneous discharge measurements and quality of ground water. A few pertinent stations in bordering States are also included in this report. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Massachusetts and Rhode Island.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMARI931","collaboration":"Prepared in cooperation with the States of Massachusetts and Rhode Island and with other agencies","usgsCitation":"Gadoury, R., Socolow, R., Girouard, G., and Ramsbey, L., 1994, Water resources data, Massachusetts and Rhode Island, water year 1993: U.S. Geological Survey Water Data Report MA-RI-93-1, xvi, 266 p., https://doi.org/10.3133/wdrMARI931.","productDescription":"xvi, 266 p.","costCenters":[],"links":[{"id":181397,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1993/mari-93-1/report-thumb.jpg"},{"id":496117,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1993/mari-93-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Massachusetts, Rhode Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -73.50297488831188,\n 42.97016577848564\n ],\n [\n -73.50297488831188,\n 41.11994266161375\n ],\n [\n -69.8918541821574,\n 41.11994266161375\n ],\n [\n -69.8918541821574,\n 42.97016577848564\n ],\n [\n -73.50297488831188,\n 42.97016577848564\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb6c2","contributors":{"authors":[{"text":"Gadoury, R.S.","contributorId":88030,"corporation":false,"usgs":true,"family":"Gadoury","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":251029,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Socolow, R.S.","contributorId":17639,"corporation":false,"usgs":true,"family":"Socolow","given":"R.S.","affiliations":[],"preferred":false,"id":251026,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Girouard, G.G.","contributorId":88017,"corporation":false,"usgs":true,"family":"Girouard","given":"G.G.","affiliations":[],"preferred":false,"id":251028,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ramsbey, L.R.","contributorId":78393,"corporation":false,"usgs":true,"family":"Ramsbey","given":"L.R.","email":"","affiliations":[],"preferred":false,"id":251027,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70134540,"text":"70134540 - 1994 - Lake Michigan's late Quaternary limnological and climate history from ostracode, oxygen isotope, and magnetic susceptibility","interactions":[],"lastModifiedDate":"2017-09-06T13:03:43","indexId":"70134540","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2330,"text":"Journal of Great Lakes Research","active":true,"publicationSubtype":{"id":10}},"title":"Lake Michigan's late Quaternary limnological and climate history from ostracode, oxygen isotope, and magnetic susceptibility","docAbstract":"The limnology of Lake Michigan has changed dramatically since the late Pleistocene in response to the expansion and contraction of continental glaciers, to differential isostatic rebound, and to climate change. The lake sediment's stratigraphic trends, magnetic susceptibility, δ18O, and ostracode species abundance ratios provide criteria to identify the lake's response to glacial ice and to differential isostatic rebound. The latter phenomena dominate the lake's late Pleistocene and early Holocene history. The lake's hydrological budget provides the primary linkage between the lake and climate, particularly effective moisture. Dissolved salts were stored in the lake's water column when the lake's output shifted toward evaporation, but were flushed when output shifted toward outflow. The lake's salt storage history may be interpreted from some ostracode, δ18O, and magnetic susceptibility records found in sediment cores. Climate change influenced the entire lake's limnological history, but became the primary limnological driver from about the middle-Holocene to the present. The complex limnological history of Lake Michigan resulted in substantial changes in the ostracode species assemblages; from about 12,000 ka to about 5,500 ka, five ostracode intervals can be identified. These ostracode intervals provide a within-lake biostratigraphy and a stratigraphic reference for reconstruction of the paleoenvironmental dynamics of the lake.
","language":"English","publisher":"Elsevier","doi":"10.1016/S0380-1330(94)71134-5","usgsCitation":"Forester, R.M., Colman, S.M., Reynolds, R.L., and Keigwin, L.D., 1994, Lake Michigan's late Quaternary limnological and climate history from ostracode, oxygen isotope, and magnetic susceptibility: Journal of Great Lakes Research, v. 20, no. 1, p. 93-107, https://doi.org/10.1016/S0380-1330(94)71134-5.","productDescription":"15 p.","startPage":"93","endPage":"107","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":296394,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Indiana, Illinois, Michigan, Wisconsin","otherGeospatial":"Lake Michigan","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": 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Center","active":false,"usgs":true}],"preferred":false,"id":526146,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Colman, Steven M. 0000-0002-0564-9576","orcid":"https://orcid.org/0000-0002-0564-9576","contributorId":77482,"corporation":false,"usgs":true,"family":"Colman","given":"Steven","email":"","middleInitial":"M.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":526147,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reynolds, Richard L. 0000-0002-4572-2942 rreynolds@usgs.gov","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":441,"corporation":false,"usgs":true,"family":"Reynolds","given":"Richard","email":"rreynolds@usgs.gov","middleInitial":"L.","affiliations":[{"id":271,"text":"Federal Center","active":false,"usgs":true}],"preferred":true,"id":526148,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Keigwin, Loyd D.","contributorId":46790,"corporation":false,"usgs":false,"family":"Keigwin","given":"Loyd","email":"","middleInitial":"D.","affiliations":[{"id":6706,"text":"Woods Hole Oceanographic Institution,","active":true,"usgs":false}],"preferred":false,"id":526149,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70179038,"text":"70179038 - 1993 - Ground-water hydrology of the upper Sevier River Basin, south-central Utah, and simulation of ground-water flow in the valley-fill in Panguitch Valley.","interactions":[],"lastModifiedDate":"2016-12-14T09:31:32","indexId":"70179038","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"102","title":"Ground-water hydrology of the upper Sevier River Basin, south-central Utah, and simulation of ground-water flow in the valley-fill in Panguitch Valley.","docAbstract":"The ground-water hydrology of the upper Sevier River basin, primarily of the unconsolidated valley-fill aquifers, was studied from 1988 to 1989. Recharge to the valley-fill aquifers is mostly by seepage from surface-water sources. Changes in soil-moisture content am water levels were measured in Panguitch Valley both at a flood-irrigated and at a sprinkler-irrigated alfalfa field to quantify seepage from unconsumed irrigation water. Lag time between irrigation and water-level response decreased from 6 to 2 days in the flood-irrigated field as the soil-moisture content increased. Water levels measured in the sprinkler-irrigated field did not respond to irrigation. Discharge from the valley-fill aquifer to the Sevier River in Panguitch Valley is about 53,570 acre-feet per year.
Water levels measured in wells from 1951 to 1989 tend to fluctuate with the quantity of precipitation falling at higher elevations. Ground-water discharge to the Sevier River in Panguitch Valley causes a general increase in the specific conductance of the river in a downstream direction.
A three-layered ground-water-flow model was used to simulate the effects of changes in irrigation practices am increased ground-water withdrawals in Panguitch Valley. The establishment of initial conditions consisted of comparing simulated water levels and simulated gains and losses from the Sevier River and selected canals with values measured during the 1988 irrigation season. The model was calibrated by comparing water-level changes measured from 1961 to 1963 to simulated changes. A simulated change from flood to sprinkler irrigation resulted in a maximum decline in water level of 0.9 feet after the first year of change. Simulating additional discharge from wells resulted in drawdowns of about 20 feet after the first year of pumping.
","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United State Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Thiros, S.A., and Brothers, W.C., 1993, Ground-water hydrology of the upper Sevier River Basin, south-central Utah, and simulation of ground-water flow in the valley-fill in Panguitch Valley.: Technical Publication 102, vii, 121 p.","productDescription":"vii, 121 p.","numberOfPages":"129","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":332093,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":332091,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-6-511"},{"id":332092,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/y920/y920000a.pdf"}],"country":"United States","state":"Utah","otherGeospatial":"Sevier River Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.862548828125,\n 37.400710068740565\n ],\n [\n -111.6046142578125,\n 37.36579146999664\n ],\n [\n -111.4947509765625,\n 39.56758783088905\n ],\n [\n -111.7034912109375,\n 39.56758783088905\n ],\n [\n -112.532958984375,\n 38.14319750166766\n ],\n [\n -112.862548828125,\n 37.400710068740565\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"585268e5e4b0e2663625eca2","contributors":{"authors":[{"text":"Thiros, Susan A. 0000-0002-8544-553X sthiros@usgs.gov","orcid":"https://orcid.org/0000-0002-8544-553X","contributorId":965,"corporation":false,"usgs":true,"family":"Thiros","given":"Susan","email":"sthiros@usgs.gov","middleInitial":"A.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":655852,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brothers, William C.","contributorId":68891,"corporation":false,"usgs":true,"family":"Brothers","given":"William","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":655853,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70175166,"text":"70175166 - 1993 - Coupled effects of vertical mixing and benthic grazing on phytoplankton populations in shallow, turbid estuaries","interactions":[],"lastModifiedDate":"2019-03-06T06:11:07","indexId":"70175166","displayToPublicDate":"2016-03-07T06:15:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2379,"text":"Journal of Marine Research","active":true,"publicationSubtype":{"id":10}},"title":"Coupled effects of vertical mixing and benthic grazing on phytoplankton populations in shallow, turbid estuaries","docAbstract":"Coastal ocean waters tend to have very different patterns of phytoplankton biomass variability from the open ocean, and the connections between physical variability and phytoplankton bloom dynamics are less well established for these shallow systems. Predictions of biological responses to physical variability in these environments is inherently difficult because the recurrent seasonal patterns of mixing are complicated by aperiodic fluctuations in river discharge and the high-frequency components of tidal variability. We might expect, then, less predictable and more complex bloom dynamics in these shallow coastal systems compared with the open ocean. Given this complex and dynamic physical environment, can we develop a quantitative framework to define the physical regimes necessary for bloom inception, and can we identify the important mechanisms of physical-biological coupling that lead to the initiation and termination of blooms in estuaries and shallow coastal waters? Numerical modeling provides one approach to address these questions. Here we present results of simulation experiments with a refined version of Cloern's (1991) model in which mixing processes are treated more realistically to reflect the dynamic nature of turbulence generation in estuaries. We investigated several simple models for the turbulent mixing coefficient. We found that the addition of diurnal tidal variation to Cloern's model greatly reduces biomass growth indicating that variations of mixing on the time scale of hours are crucial. Furthermore, we found that for conditions representative of South San Francisco Bay, numerical simulations only allowed for bloom development when the water column was stratified and when minimal mixing was prescribed in the upper layer. Stratification, however, itself is not sufficient to ensure that a bloom will develop: minimal wind stirring is a further prerequisite to bloom development in shallow turbid estuaries with abundant populations of benthic suspension feeders.
","language":"English","publisher":"Sears Foundation for Marine Research","doi":"10.1357/0022240933223954","usgsCitation":"Koseff, J.R., Holen, J.K., Monismith, S., and Cloern, J.E., 1993, Coupled effects of vertical mixing and benthic grazing on phytoplankton populations in shallow, turbid estuaries: Journal of Marine Research, v. 51, no. 4, p. 843-868, https://doi.org/10.1357/0022240933223954.","productDescription":"26 p.","startPage":"843","endPage":"868","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":325890,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"51","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57a072b1e4b060ce18fb2d94","contributors":{"authors":[{"text":"Koseff, Jeffrey R.","contributorId":37915,"corporation":false,"usgs":false,"family":"Koseff","given":"Jeffrey","email":"","middleInitial":"R.","affiliations":[{"id":6986,"text":"Stanford University","active":true,"usgs":false}],"preferred":false,"id":644182,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holen, Jacqueline K.","contributorId":173302,"corporation":false,"usgs":false,"family":"Holen","given":"Jacqueline","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":644183,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Monismith, Stephen G.","contributorId":57228,"corporation":false,"usgs":true,"family":"Monismith","given":"Stephen G.","affiliations":[],"preferred":false,"id":644184,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cloern, James E. 0000-0002-5880-6862 jecloern@usgs.gov","orcid":"https://orcid.org/0000-0002-5880-6862","contributorId":1488,"corporation":false,"usgs":true,"family":"Cloern","given":"James","email":"jecloern@usgs.gov","middleInitial":"E.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":644185,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70174578,"text":"70174578 - 1993 - Organic carbon sources and sinks in San Francisco Bay: variability induced by river flow","interactions":[],"lastModifiedDate":"2019-03-01T07:23:40","indexId":"70174578","displayToPublicDate":"2016-01-05T10:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2663,"text":"Marine Ecology Progress Series","active":true,"publicationSubtype":{"id":10}},"title":"Organic carbon sources and sinks in San Francisco Bay: variability induced by river flow","docAbstract":"Salinity in the San Francisco Bay Estuary almost always experiences its yearly maximum during late summer, but climate variability produces marked interannual variations. The atmospheric circulation pattern impacts the estuary primarily through variations of runoff from rainfall and snowmelt from the Sierra Nevada and, secondarily, through variations in the near-surface salinity in the coastal ocean. While winter precipitation is the primary influence upon salinity in the estuary, spring climate variations also contribute importantly to salinity fluctuations. Spring atmospheric circulation influences both the magnitude and the timing of freshwater flows, through anomalies of precipitation and temperature. To help discriminate between the effects of these two influences, the record is divided into subsets according to whether spring conditions in the region are cool and wet, warm and wet, cool and dry, or warm and dry. Warm springs promote early snowmelt-driven flows, and cool springs result in delayed flows. In addition to effects of winter and spring climate variability operating on the watershed, there are more subtle effects that are transmitted into the estuary from the coastal ocean. These influences are most pronounced in cool and dry springs with high surface salinity (SS) in the coastal ocean versus cool and wet springs with low SS in the coastal ocean. A transect of SS records at stations from the mouth to the head of the bay suggests that the coastal ocean anomaly signal is attenuated from the mouth to the interior of the estuary. In contrast, a delayed, postsummer signal caused by winter and spring runoff variations from the upstream watershed are most pronounced at the head of the estuary and attenuate toward the mouth.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/92WR02152","usgsCitation":"Cayan, D.R., and Peterson, D., 1993, Spring climate and salinity in the San Francisco Bay Estuary: Water Resources Research, v. 29, no. 2, p. 293-303, https://doi.org/10.1029/92WR02152.","productDescription":"11 p.","startPage":"293","endPage":"303","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":307823,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.52777099609375,\n 37.41816326969145\n ],\n [\n -122.52777099609375,\n 38.171273439283084\n ],\n [\n -121.90155029296875,\n 38.171273439283084\n ],\n [\n -121.90155029296875,\n 37.41816326969145\n ],\n [\n -122.52777099609375,\n 37.41816326969145\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"29","issue":"2","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"560bb6fee4b058f706e53ea8","contributors":{"authors":[{"text":"Cayan, Daniel R. 0000-0002-2719-6811 drcayan@usgs.gov","orcid":"https://orcid.org/0000-0002-2719-6811","contributorId":1494,"corporation":false,"usgs":true,"family":"Cayan","given":"Daniel","email":"drcayan@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":false,"id":571153,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, David H.","contributorId":82776,"corporation":false,"usgs":true,"family":"Peterson","given":"David H.","affiliations":[],"preferred":false,"id":571154,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70018223,"text":"70018223 - 1993 - Mapping playa evaporite minerals with AVIRIS data: A first report from Death Valley, California","interactions":[],"lastModifiedDate":"2025-07-17T14:54:08.82958","indexId":"70018223","displayToPublicDate":"2003-04-07T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3254,"text":"Remote Sensing of Environment","printIssn":"0034-4257","active":true,"publicationSubtype":{"id":10}},"title":"Mapping playa evaporite minerals with AVIRIS data: A first report from Death Valley, California","docAbstract":"Efflorescent salt crusts in Death Valley, California, were mapped by using Airborne Visible/Infrared Imaging Spectrometer (AVIRIS) data and a recently developed least-squares spectral band-fitting algorithm. Eight different saline minerals were remotely identified, including three borates, hydroboracite, pinnoite, and rivadavite, that have not been previously reported from the Death Valley efflorescent crusts. The three borates are locally important phases in the crusts, and at least one of the minerals, rivadavite, appears to be forming directly from brine. Borates and other evaporite minerals provide a basis for making remote chemical measurements of desert hydrologic systems. For example, in the Eagle Borax Spring area, the AVIRIS mineral maps pointed to elevated magnesium and boron levels in the ground waters, and to the action of chemical divides causing subsurface fractionation of calcium. Many other chemical aspects of playa brines should have an expression in the associated evaporite assemblages. Certain anhydrous evaporites, including anhydrite, glauberite, and thenardite, lack absorption bands in the visible and near-infrared wavelength range, and crusts composed of these minerals could not be characterized by using AVIRIS. In these situations, thermal-infrared remote sensing data may complement visible and near-infrared data for mapping evaporites. Another problem occurred in wet areas of Death Valley, where water absorption caused low signal levels in the 2.0-2.5 ??m wavelength region that obscured any spectral features of evaporite minerals. Despite these difficulties, the results of this study demonstrate the potential for using AVIRIS and other imaging spectrometer data to study playa chemistry. Such data can be useful for understanding chemical linkages between evaporites and ground waters, and will facilitate studies of how desert ground-water regimes change through time in response to climatic and other variables.
","language":"English","publisher":"Elsevier","doi":"10.1016/0034-4257(93)90025-S","issn":"00344257","usgsCitation":"Crowley, J., 1993, Mapping playa evaporite minerals with AVIRIS data: A first report from Death Valley, California: Remote Sensing of Environment, v. 44, no. 2-3, p. 337-356, https://doi.org/10.1016/0034-4257(93)90025-S.","productDescription":"20 p.","startPage":"337","endPage":"356","costCenters":[],"links":[{"id":226973,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Death Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -117.68655810627652,\n 36.921398315526645\n ],\n [\n -117.68655810627652,\n 35.9185137883743\n ],\n [\n -116.61296354270263,\n 35.9185137883743\n ],\n [\n -116.61296354270263,\n 36.921398315526645\n ],\n [\n -117.68655810627652,\n 36.921398315526645\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"44","issue":"2-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5070e4b0c8380cd6b6be","contributors":{"authors":[{"text":"Crowley, J.K.","contributorId":103690,"corporation":false,"usgs":true,"family":"Crowley","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":378916,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":19991,"text":"ofr9461 - 1993 - Policy and procedures for the management and archival storage of data collected for hydrologic investigations, U.S. Geological Survey, Indiana District","interactions":[],"lastModifiedDate":"2016-06-01T12:38:09","indexId":"ofr9461","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-61","title":"Policy and procedures for the management and archival storage of data collected for hydrologic investigations, U.S. Geological Survey, Indiana District","docAbstract":"This report describes the policy and procedures used by the Indiana District of the U.S. Geological Survey, Water Resources Division, to manage and store data collected during hydrologic investigations. It is the policy of the Indiana District that data collected to meet the objectives of projects for hydrologic investigations be documented, organized, and archieved in a manner that (1) facilitates retrieval, evaluation, and use by other District personnel, and (2) enables verifi- cation of data contained in all reports and computer data bases.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db68491f","contributors":{"authors":[{"text":"Martin, Jeffrey D. 0000-0003-1994-5285 jdmartin@usgs.gov","orcid":"https://orcid.org/0000-0003-1994-5285","contributorId":1066,"corporation":false,"usgs":true,"family":"Martin","given":"Jeffrey","email":"jdmartin@usgs.gov","middleInitial":"D.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":27231,"text":"Indiana-Kentucky Water Science Center","active":true,"usgs":true}],"preferred":true,"id":181864,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cohen, David A.","contributorId":30198,"corporation":false,"usgs":true,"family":"Cohen","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":181865,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":30475,"text":"wri934163 - 1993 - Hydrology of the Estancia Basin, central New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:58","indexId":"wri934163","displayToPublicDate":"1995-04-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"93-4163","title":"Hydrology of the Estancia Basin, central New Mexico","docAbstract":"The Estancia Basin of central New Mexico is a topographically closed basin that ranges in altitude from 6,000 feet to more than 10,000 feet above sea level. In the center of the basin a valley-fill aquifer of Quaternary age is as much as 400 feet thick. Limestone of the Madera Group of Pennsylvanian and Permian age crops out over most of the southwestern part of the basin. Large-scale ground-water withdrawals for irrigation began about 1950. Between 1950 and 1985, water levels declined 50 to 60 feet in a number of places. From 1985 to the present (1989), however, a small rise in water level has been measured in a number of wells; this rise can be attributed to decreased ground-water withdrawals resulting from a government crop- reduction program and also to several years of heavy winter snowfall. Continuous water-level recorders were placed on three wells from 1986 to 1988. Two of these wells showed short-term water-level changes characteristic of unconfined aquifers, whereas the other showed changes characteristic of confined aquifers. All three wells showed water-level changes caused by barometric-pressure changes. Six series of miscellaneous measurements and two gain-and-loss (seepage) studies were made in streams in the south- western part of the basin. These measurements showed an extreme variability in discharge under different climatic conditions. The specific conductance of water in much of the southwestern part of the basin ranges from 350 to 550 microsiemens per centimeter at 25 degrees Celsius. East of State Highway 41 in the area of the salt lakes, water quality is highly dependent on depth in the aquifer. Specific- conductance values ranging from about 4,000 to 6,000 microsiemens were measured in water samples from wells in the center of the basin during this study, but previous studies have identified water samples having specific-conductance values of as much as 187,000 microsiemens. A comparison of specific- conductance measurements and laboratory analyses of well water shows that water quality has changed in the past several decades. In many places, increases in spedtic conductance can be correlated with deelines in water level.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri934163","usgsCitation":"White, R., 1993, Hydrology of the Estancia Basin, central New Mexico: U.S. Geological Survey Water-Resources Investigations Report 93-4163, v, 83 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri934163.","productDescription":"v, 83 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123475,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4163/report-thumb.jpg"},{"id":59259,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4163/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59260,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4163/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601f9b","contributors":{"authors":[{"text":"White, R.R.","contributorId":52568,"corporation":false,"usgs":true,"family":"White","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":203315,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}