No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94462","usgsCitation":"Savoie, J., 1995, Altitude and configuration of the water table, western Cape Cod aquifer, Massachusetts, March 1993: U.S. Geological Survey Open-File Report 94-462, 1 Plate: 42.00 x 32.00 inches, https://doi.org/10.3133/ofr94462.","productDescription":"1 Plate: 42.00 x 32.00 inches","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":393964,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12539.htm"},{"id":161214,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":21634,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0462/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"50000","country":"United States","state":"Massachusetts","otherGeospatial":"Cape Cod","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.0870361328125,\n 41.372686481864676\n ],\n [\n -70.28503417968749,\n 41.372686481864676\n ],\n [\n -70.28503417968749,\n 41.73852846935917\n ],\n [\n -71.0870361328125,\n 41.73852846935917\n ],\n [\n -71.0870361328125,\n 41.372686481864676\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adde4b07f02db686ab6","contributors":{"authors":[{"text":"Savoie, Jennifer G. jsavoie@usgs.gov","contributorId":1691,"corporation":false,"usgs":true,"family":"Savoie","given":"Jennifer G.","email":"jsavoie@usgs.gov","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":false,"id":207191,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28158,"text":"wri954003 - 1995 - Recharge to the surficial aquifer system in Lee and Hendry counties, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:36","indexId":"wri954003","displayToPublicDate":"1996-03-01T00:00:00","publicationYear":"1995","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":"95-4003","title":"Recharge to the surficial aquifer system in Lee and Hendry counties, Florida","docAbstract":"Protection of ground-water recharge areas against contamination is of great interest in Florida, a State whose population depends heavily on ground water and that is experiencing rapid growth. The Florida Legislature is considering implementation of a tax incentive program to owners of high-rate recharge lands that remain undeveloped. High-rate recharge was arbitrarily set at 10 or more inches per year. The U.S. Geological Survey, in cooperation with the South Florida Water Management District, conducted a study to investigate the efficacy of several methods for estimating recharge to the surficial aquifer system in southwestern Florida and to map recharge at a scale of 1:100,000. Four maps were constructed at a scale of 1:100,000 for Lee and Hendry Counties, depicting the configuration of the water table of the surficial aquifer system, direction of ground-water flow, general soil characteristics, and recharge rates. Point recharge rates calculated for 25 sites in Lee County from comparisons of chloride concentrations in precipitation and in water from the surficial aquifer system ranged from 0.6 to 9.0 inches per year. Local recharge rates estimated by increases in flow along theoretical flow tubes in the surficial aquifer system were 8.0 inches per year in a part of Lee County and 8.2 inches per year in a part of Hendry County. Information on oxygen isotopes in precipitation and water from the surficial aquifer system was used to verify that the source of chlorides in the aquifer system was from precipitation rather than upward leakage of saline water. Soil maps and general topographic and hydrologic considerations were used with calculated point and local recharge rates to regionalize rates throughout Lee and Hendry Counties. The areas of greatest recharge were found in soils of flatwoods and sloughs, which were assigned estimated recharge rates of 0 to 10 inches per year. Soils of swamps and sloughs were assigned values of 0 to 3.0 inches per year; soils of tidal areas and barrier islands, soils of the Everglades, and soils of sloughs and freshwater marshes were assigned values of 0 to 2.0 inches per year; lastly, soils of manmade areas were assigned values of 0.5 to 1.5 inches per year. Small isolated areas of high-rate recharge (greater than 10 inches per year) might exist in Lee and Hendry Counties, but the maximum rate calculated in this study was 9.0 inches per year. Despite low natural recharge rates, lowering of the water table through pumping or canalization could create a potential for induced recharge in excess of 10 inches per year in parts of Lee and Hendry Counties.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nU.S. Geological Survey, Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri954003","usgsCitation":"Krulikas, R., and Giese, G.L., 1995, Recharge to the surficial aquifer system in Lee and Hendry counties, Florida: U.S. Geological Survey Water-Resources Investigations Report 95-4003, iv, 21 p. :ill., maps (some col.) ;28 cm. [PGS - 25 p.], https://doi.org/10.3133/wri954003.","productDescription":"iv, 21 p. :ill., maps (some col.) ;28 cm. [PGS - 25 p.]","costCenters":[],"links":[{"id":158647,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4003/report-thumb.jpg"},{"id":56988,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4003/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56989,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4003/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56990,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4003/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56991,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4003/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56992,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4003/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a72e4b07f02db642d2a","contributors":{"authors":[{"text":"Krulikas, R.K.","contributorId":81102,"corporation":false,"usgs":true,"family":"Krulikas","given":"R.K.","email":"","affiliations":[],"preferred":false,"id":199314,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Giese, G. L.","contributorId":44898,"corporation":false,"usgs":true,"family":"Giese","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":199313,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28245,"text":"wri934069 - 1995 - Hydrology and the effects of selected agricultural best-management practices in the Bald Eagle Creek watershed, York County, Pennsylvania, prior to and during nutrient management: Water-quality study for the Chesapeake Bay Program","interactions":[],"lastModifiedDate":"2023-04-13T20:41:43.614521","indexId":"wri934069","displayToPublicDate":"1996-03-01T00:00:00","publicationYear":"1995","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":"93-4069","title":"Hydrology and the effects of selected agricultural best-management practices in the Bald Eagle Creek watershed, York County, Pennsylvania, prior to and during nutrient management: Water-quality study for the Chesapeake Bay Program","docAbstract":"The U.S. Geological Survey, in cooperation with the Susquehanna River Basin Commission and the Pennsylvania Department of Environmental Resources, conducted a study as part of the U.S. Environmental Protection Agency's Chesapeake Bay Program to determine the effects of nutrient management of surface-water quality by reducing animal units in a 0.43-square-mile agricultural watershed in York County. The study was conducted primarily from October 1985 through September 1990 prior to and during the implementation of nutrient-management practices designed to reduce nutrient and sediment discharges. Intermittent sampling continued until August 1991.
The Bald Eagle Creek Basin is underlain by schist and quartzite. About 87 percent of the watershed is cropland and pasture. Nearly 33 percent of the cropland was planted in corn prior to nutrient management, whereas 22 percent of the cropland was planted in corn during the nutrient-management phase. The animal population was reduced by 49 percent during nutrient management. Average annual applications of nitrogen and phosphorus from manure to cropland were reduced by 3,940 pounds (39 percent) and 910 pounds (46 percent), respectively, during nutrient management. A total of 94,560 pounds of nitrogen (538 pounds per acre) and 26,400 pounds of phosphorus (150 pounds per acre) were applied to the cropland as commercial fertilizer and manure during the 5-year study.
Core samples from the top 4 feet of soil were collected prior to and during nutrient management and analyzed from concentrations of nitrogen and phosphorus. The average amount of nitrate nitrogen in the soil ranged from 36 to 135 pounds per acre, and soluble phosphorus ranged from 0.39 to 2.5 pounds per acre, prior to nutrient management. During nutrient management, nitrate nitrogen in the soil ranged from 21 to 291 pounds per acre and soluble phosphorus ranged from 0.73 to 1.7 pounds per acre. Precipitation was about 18 percent below normal and streamflow was about 35 percent below normal prior to nutrient management, whereas precipitation was 4 percent above normal and streamflow was 3 percent below normal during the first 2 years of nutrient management. Eighty-four percent of the 20.44 inches of streamflow was base flow prior to nutrient management and 54 percent of the 31.14 inches of streamflow was base flow during the first 2 years of the nutrient-management phase. About 31 percent of the measured precipitation during the first 4 years of the study was discharged as surface water; the remaining 69 percent was removed as evapotranspiration or remained in ground-water storage.
Median concentrations of total nitrogen and dissolved nitrate plus nitrite in base flow increased from 4.9 and 4.1 milligrams per liter as nitrogen, respectively, prior to nutrient management to 5.8 and 5.0 milligrams per liter, respectively, during nutrient management. Median concentrations of ammonia nitrogen and organic nitrogen did not change significantly in base flow. Median concentrations of total and dissolved phosphorus in base flow did not change significantly and were 0.05 and 0.03 milligrams per liter as phosphorus, respectively, prior to the management phase, and 0.05 and 0.04 milligrams per liter, respectively, during the management phase.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri934069","usgsCitation":"Langland, M.J., and Fishel, D.K., 1995, Hydrology and the effects of selected agricultural best-management practices in the Bald Eagle Creek watershed, York County, Pennsylvania, prior to and during nutrient management: Water-quality study for the Chesapeake Bay Program: U.S. Geological Survey Water-Resources Investigations Report 93-4069, vii, 72 p., https://doi.org/10.3133/wri934069.","productDescription":"vii, 72 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":415733,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47791.htm","linkFileType":{"id":5,"text":"html"}},{"id":57072,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4069/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119030,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4069/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","county":"York County","otherGeospatial":"Bald Eagle Creek watershed","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -76.4794,\n 39.7567\n ],\n [\n -76.4794,\n 39.7436\n ],\n [\n -76.4639,\n 39.7436\n ],\n [\n -76.4639,\n 39.7567\n ],\n [\n -76.4794,\n 39.7567\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e836","contributors":{"authors":[{"text":"Langland, Michael J. 0000-0002-8350-8779 langland@usgs.gov","orcid":"https://orcid.org/0000-0002-8350-8779","contributorId":2347,"corporation":false,"usgs":true,"family":"Langland","given":"Michael","email":"langland@usgs.gov","middleInitial":"J.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":199460,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fishel, David K.","contributorId":34967,"corporation":false,"usgs":true,"family":"Fishel","given":"David","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":199461,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28532,"text":"wri954186 - 1995 - Geology and hydrology of the Edwards Aquifer in the San Antonio area, Texas","interactions":[],"lastModifiedDate":"2016-08-16T15:35:48","indexId":"wri954186","displayToPublicDate":"1996-03-01T00:00:00","publicationYear":"1995","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":"95-4186","title":"Geology and hydrology of the Edwards Aquifer in the San Antonio area, Texas","docAbstract":"The Edwards aquifer, which is the sole source of water for the city of San Antonio, is one of the most permeable and productive carbonate aquifers in the United States. The aquifer is composed of extensively faulted, fractured, and cavernous limestone and dolomite of Early Cretaceous age lying within the Balcones fault zone a series of normal en echelon strike faults that separate the Edwards Plateau from the Gulf Coastal Plain in south Texas. Along segments of some faults, the entire thickness of the aquifer is displaced vertically, and these faults then act as barriers to downdip ground-water flow.
\nThe large porosity and exceptional permeability of the unconfined part of the Edwards aquifer result from the dissolution of limestone by circulating ground water and development of a cavernous network along fractures. The large porosity and permeability of the freshwater part of the confined Edwards aquifer result primarily from dedolomitization. The small permeability of the saline-water part of the confined aquifer is caused by the limited interconnection between the pores in the rock matrix and by the lack of substantial dissolution along fractures.
\nThe large transmissivity of the Edwards aquifer is indicated by the hundreds of highyielding wells, small hydraulic gradients, and large spring discharges. The determined transmissivity throughout most of the confined freshwater aquifer ranges from 430,000 to 2,200,000 feet squared per day; the determined transmissivity of the unconfined aquifer generally is less than 430,000 feet squared per day. Faulting causes the aquifer to be highly anisotropic, and simulation indicates anisotropy ratios ranging from 0.0:1 to 1:1.
\nThe ground-water-flow system of the Edwards aquifer includes several components. These include a catchment area on the Edwards Plateau where the unconfined aquifer receives direct recharge, an area of confining beds crossed by streams draining the Edwards Plateau, a major recharge area within the Balcones fault zone where streams lose flow directly into the unconfined Edwards aquifer, and the confined Edwards aquifer that consists of the freshwater and salinewater zones.
\nWater entering the Edwards aquifer in the Balcones fault zone moves downdip in a generally southeasterly direction into the confined parts of the aquifer. In the confined aquifer, flow is toward the east and northeast under low hydraulic gradients through fractured, highly transmissive limestone and ultimately discharges at large springs and wells. All of the base flow and some of the storm runoff of streams crossing the recharge area infiltrates to the unconfined aquifer. On the basis of streamflow losses, the average annual recharge for 1934-88 was 635,500 acre-feet.
\nFreshwater discharges from the Edwards aquifer primarily from wells, springs, and seeps. Beginning in 1968, annual discharge from the aquifer has consistently exceeded average annual recharge largely because of a doubling of well pumpage. However, total springflow also increased because of greater-than-average recharge during most years since the late 1960's.
\nThe total volume of circulating freshwater in the Edwards aquifer is about 45 million acrefeet. Long-term hydrographs at San Antonio indicate no net decline in ground-water levels during 1911-87; thus, there was no net loss of water from storage in the freshwater zone of the Edwards aquifer during that long-term period, assuming the San Antonio hydrograph represents the entire aquifer. However, short-term changes in water levels result largely from the variability of precipitation as indicated by severe declines during the drought of the late 1940's to middle 1950's and by rises to record highs during the abnormally wet years in the 1970's and 1980's.
\nThe principal components of the groundwater budget (recharge, springflow, and pumpage) have varied greatly over 55 years (1934-88) of pertinent hydrologic records. Annual recharge varied from about 44,000 to 2,000,000 acre-feet. Annual springflow varied from about 70,000 acrefeet to about 580,000 acre-feet. Pumpage increased from about 100,000 acre-feet annually in the early 1930's to more than 500,000 acre-feet annually during some years in the 1980's. However, the average annual recharge of 635,500 acrefeet is about equal to the sum of the average annual springflow (359,500 acre-feet) and average annual pumpage (273,000 acre-feet), indicating no longterm decrease in ground-water storage because of springflow and pumpage.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri954186","collaboration":"Prepared in cooperation with the San Antonio Water System","usgsCitation":"Maclay, R.W., 1995, Geology and hydrology of the Edwards Aquifer in the San Antonio area, Texas: U.S. Geological Survey Water-Resources Investigations Report 95-4186, Document: v, 64 p.; 12 Plates: 28.00 x 19.39 inches or smaller, https://doi.org/10.3133/wri954186.","productDescription":"Document: v, 64 p.; 12 Plates: 28.00 x 19.39 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":57339,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57340,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57341,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57342,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124992,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4186/report-thumb.jpg"},{"id":57343,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57344,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57345,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57346,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57347,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4186/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57335,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57336,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57337,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57338,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4186/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","otherGeospatial":"Edwards Aquifer","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db68527d","contributors":{"authors":[{"text":"Maclay, Robert W.","contributorId":13210,"corporation":false,"usgs":true,"family":"Maclay","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":199974,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23513,"text":"ofr94533 - 1995 - Documentation of AIR3D, an adaptation of the ground-water-flow code MODFLOW to simulate three-dimensional air flow in the unsaturated zone","interactions":[],"lastModifiedDate":"2020-04-11T17:00:43.725705","indexId":"ofr94533","displayToPublicDate":"1996-03-01T00:00:00","publicationYear":"1995","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":"94-533","title":"Documentation of AIR3D, an adaptation of the ground-water-flow code MODFLOW to simulate three-dimensional air flow in the unsaturated zone","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94533","issn":"0094-9140","collaboration":"The USGS does not support this software or technical questions for the software associated with the publication.","usgsCitation":"Joss, C., and Baehr, A.L., 1995, Documentation of AIR3D, an adaptation of the ground-water-flow code MODFLOW to simulate three-dimensional air flow in the unsaturated zone: U.S. Geological Survey Open-File Report 94-533, Report: viii, 164 p.; Application Site, https://doi.org/10.3133/ofr94533.","productDescription":"Report: viii, 164 p.; Application Site","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":277712,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/of/1994/0533/application.zip"},{"id":52803,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0533/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":155662,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0533/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d70d","contributors":{"authors":[{"text":"Joss, C.J.","contributorId":36964,"corporation":false,"usgs":true,"family":"Joss","given":"C.J.","affiliations":[],"preferred":false,"id":190234,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baehr, A. L.","contributorId":59831,"corporation":false,"usgs":true,"family":"Baehr","given":"A.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":190235,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":19863,"text":"ofr95351 - 1995 - Selected hydrologic data for urban watersheds in South Carolina, 1983-90","interactions":[],"lastModifiedDate":"2017-01-04T12:43:06","indexId":"ofr95351","displayToPublicDate":"1996-03-01T00:00:00","publicationYear":"1995","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":"95-351","title":"Selected hydrologic data for urban watersheds in South Carolina, 1983-90","docAbstract":"Rainfall and streamflow data were collected at 23 gaging stations located in urban watersheds in South Carolina from 1983-90. The site selection process and the instrumentation used to collect the data are described. A compilation of rainfall and streamflow data in graphic and tabular form for seven selected events at each gaging station are presented. A gaging-station description and a listing of certain streamflow and basin characteristics also are included.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95351","usgsCitation":"Logan, S., Eckenwiler, M., and Bohman, L.R., 1995, Selected hydrologic data for urban watersheds in South Carolina, 1983-90: U.S. Geological Survey Open-File Report 95-351, xviii, 434 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr95351.","productDescription":"xviii, 434 p. :ill., map ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":152748,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0351/report-thumb.jpg"},{"id":49372,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0351/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South 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R.","contributorId":106518,"corporation":false,"usgs":true,"family":"Bohman","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":181651,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":5196,"text":"fs15995 - 1995 - Water Quality Assessment of the Trinity River Basin, Texas - Pesticides in a Suburban Watershed, Arlington, 1993-94","interactions":[],"lastModifiedDate":"2016-08-17T17:27:14","indexId":"fs15995","displayToPublicDate":"1996-01-10T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"159-95","title":"Water Quality Assessment of the Trinity River Basin, Texas - Pesticides in a Suburban Watershed, Arlington, 1993-94","docAbstract":"The Trinity River Basin was among the first 20 hydrologic systems under full inplementation of the National Water Quality Assessment (NAWQA) Program. Planning and analysis of existing information began in 1991. Intensive water-quality data collection began in 1993. As a part of the NAWQA Program, pesticide samples were taken from surface water, ground water, streambed sediment, and aquatic-organism tissue in the Rush Creek watershed in Arlington, Texas, during 1993?94.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs15995","usgsCitation":"Brown, M.F., 1995, Water Quality Assessment of the Trinity River Basin, Texas - Pesticides in a Suburban Watershed, Arlington, 1993-94: U.S. Geological Survey Fact Sheet 159-95, 4 p., https://doi.org/10.3133/fs15995.","productDescription":"4 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":31931,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1995/0159/report.pdf","text":"Report","size":"1.81 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":11555,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://tx.usgs.gov/projects/trin/pubs/pdf/fs-159-95.pdf","text":"Report-reprint","size":"495.93 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":121781,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1995/0159/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Rush Creek watershed, Trinity River Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -97.2,\n 32.5\n ],\n [\n -97.2,\n 32.8\n ],\n [\n -97,\n 32.8\n ],\n [\n -97,\n 32.5\n ],\n [\n -97.2,\n 32.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd3d6","contributors":{"authors":[{"text":"Brown, Marianna F.","contributorId":57839,"corporation":false,"usgs":true,"family":"Brown","given":"Marianna","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":150590,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70199898,"text":"70199898 - 1995 - Responsibilities and activities of the U.S. Geological Survey related to mining and the environment","interactions":[],"lastModifiedDate":"2018-10-03T08:21:29","indexId":"70199898","displayToPublicDate":"1996-01-01T08:20:32","publicationYear":"1995","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Responsibilities and activities of the U.S. Geological Survey related to mining and the environment","docAbstract":"No abstract available.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Workshop report: Mine waste technical forum","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"conferenceTitle":"Mine Wast Technical Forum","conferenceDate":"July 25-27, 1995","conferenceLocation":"Las Vegas, Nevada","language":"English","publisher":"Environmental Protection Agency","publisherLocation":"Washington, D.C.","usgsCitation":"Alpers, C.N., 1995, Responsibilities and activities of the U.S. Geological Survey related to mining and the environment, chap. of Workshop report: Mine waste technical forum, p. 3-63.","productDescription":"61 p.","startPage":"3","endPage":"63","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":358054,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c110e11e4b034bf6a810d54","contributors":{"authors":[{"text":"Alpers, Charles N. 0000-0001-6945-7365 cnalpers@usgs.gov","orcid":"https://orcid.org/0000-0001-6945-7365","contributorId":411,"corporation":false,"usgs":true,"family":"Alpers","given":"Charles","email":"cnalpers@usgs.gov","middleInitial":"N.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":747193,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70157137,"text":"70157137 - 1995 - Molecular and isotopic tracers used to examine sources of organic matter and its incorporation into the food webs of San Francisco Bay","interactions":[],"lastModifiedDate":"2019-02-25T07:08:10","indexId":"70157137","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2620,"text":"Limnology and Oceanography","active":true,"publicationSubtype":{"id":10}},"title":"Molecular and isotopic tracers used to examine sources of organic matter and its incorporation into the food webs of San Francisco Bay","docAbstract":"Multiple indicators (Chl a, C : N ratios, [δ13C]POC, and two classes of lipid biomarker compounds- sterols and phospholipid ester-linked fatty acids) were used to evaluate spatial and temporal variations in the origin of particulate organic matter (POM) in the San Francisco Bay (SFB) estuary. Comparisons were made between the northern and southern subestuaries of SFB, as well as along the salinity gradient of northern SFB. Two sample types were collected-seston, which was used to characterize the bulk POM, and tissues of the suspension-feeding bivalve Potamocorbula amurensis -in order to evaluate the assimilable portion of the POM. Samples were collected around biological and physical events (phytoplankton blooms and freshwater inflow) thought to be the primary mechanisms controlling temporal variability in organic matter sources. Seston samples indicate that phytoplankton sources of POM are important throughout the entire SFB system, with additional inputs of organic matter from bacterial and terrestrial vascular plant sources delivered to the northern region. Analysis of biomarker compounds in P. amurensis tissues indicates that phytoplankton supply a large fraction of the assimilable carbon to clams throughout SFB, although isotopic analysis of clam tissues suggests that the origin of this reactive carbon varies spatially and that freshwater algae are an important source of reactive organic matter to clams living in northern SFB.
","language":"English","publisher":"Association for the Sciences of Limnology and Oceanography","doi":"10.4319/lo.1995.40.1.0067","usgsCitation":"Canuel, E.A., Cloern, J.E., Ringelberg, D.B., Guckert, J.B., and Rau, G.H., 1995, Molecular and isotopic tracers used to examine sources of organic matter and its incorporation into the food webs of San Francisco Bay: Limnology and Oceanography, v. 40, no. 1, p. 67-81, https://doi.org/10.4319/lo.1995.40.1.0067.","productDescription":"15 p.","startPage":"67","endPage":"81","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1990-01-17","temporalEnd":"1991-04-11","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":307997,"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 -121.67633056640624,\n 38.1734326790354\n ],\n [\n -121.67358398437499,\n 37.99183365313853\n ],\n [\n -122.025146484375,\n 38.0437651074397\n ],\n [\n -122.15972900390624,\n 38.004819966413194\n ],\n [\n -122.2283935546875,\n 38.037275688165614\n ],\n [\n -122.39044189453124,\n 37.94852933714952\n ],\n [\n -122.28607177734376,\n 37.90953361677018\n ],\n [\n -122.08007812499999,\n 37.59464778787345\n ],\n [\n -121.904296875,\n 37.45959832290546\n ],\n [\n -121.94549560546875,\n 37.42252593456307\n ],\n [\n -122.10479736328125,\n 37.42034463389752\n ],\n [\n -122.26959228515624,\n 37.55328764595765\n ],\n [\n -122.39318847656249,\n 37.59247151101911\n ],\n [\n -122.53875732421875,\n 37.883524980871336\n ],\n [\n -122.51953124999999,\n 38.13023573104302\n ],\n [\n -122.27508544921875,\n 38.278078995562105\n ],\n [\n -122.244873046875,\n 38.10430528370985\n ],\n [\n -122.15698242187499,\n 38.078365629967145\n ],\n [\n -122.00317382812499,\n 38.16263584058641\n ],\n [\n -121.9482421875,\n 38.09782123329514\n ],\n [\n -121.79718017578124,\n 38.08701320402273\n ],\n [\n -121.67633056640624,\n 38.1734326790354\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"40","issue":"1","noUsgsAuthors":false,"publicationDate":"2003-12-22","publicationStatus":"PW","scienceBaseUri":"55f15831e4b0dacf699eb96d","contributors":{"authors":[{"text":"Canuel, Elizabeth A.","contributorId":98604,"corporation":false,"usgs":true,"family":"Canuel","given":"Elizabeth","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":571799,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"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":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":571800,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ringelberg, David B.","contributorId":147458,"corporation":false,"usgs":false,"family":"Ringelberg","given":"David","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":571801,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Guckert, James B.","contributorId":147459,"corporation":false,"usgs":false,"family":"Guckert","given":"James","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":571802,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rau, Greg H.","contributorId":78963,"corporation":false,"usgs":false,"family":"Rau","given":"Greg","email":"","middleInitial":"H.","affiliations":[{"id":6949,"text":"University of California, Santa Cruz","active":true,"usgs":false}],"preferred":false,"id":571803,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70156921,"text":"70156921 - 1995 - Seasonal-to-interannual fluctuations in surface temperature over the Pacific: effects of monthly winds and heat fluxes","interactions":[],"lastModifiedDate":"2018-09-10T10:59:14","indexId":"70156921","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Seasonal-to-interannual fluctuations in surface temperature over the Pacific: effects of monthly winds and heat fluxes","docAbstract":"Monthly heat fluxes and wind stresses are used to force the Oberhuber isopycnic ocean general-circulation (OPYC) model of the Pacific basin over a two-decade period from 1970 to 1988. The surface forcings are constructed from COADS marine observations via bulk formulae. Monthly anomalies of the fluxes and stresses are superimposed upon model climatological means of these variables, which were saved from a long spin-up. Two aspects of this work are highlighted, both aimed at a better understanding of the atmosphere-ocean variability and exchanges and at diagnosing the performance of the OPYC model in simulating monthly to decadal-scale variability. The first is the evaluation of the data used to force the model ocean, along with its relationship to other observed data. The second is the diagnosis of the processes revealed in the model that are associated with sea surface temperature (SST) variability, including their seasonal and geographic structure.
\nAlthough both random and systematic errors arise from the marine data and the bulk formulations, large signals in the air-sea fluxes are nonetheless consistent with the large-scale atmospheric circulation anomalies over the Pacific. This signal is large in a composite prepared from months with similar circulation modes. Also, latent and sensible heat-flux anomaly patterns correspond well to those of SST anomaly tendencies. Considering short-period variations, SST anomaly tendencies have typical magnitudes of 0.3°C mo-1. These are associated with monthly mean flux anomalies having typical magnitudes of 50 W m-2 and are consistent with observed mixed-layer depths. Decadal anomalies have much smaller magnitudes, perhaps reduced by two orders of magnitude, and it is here that the signal-to-noise problem is more severe. The forcing terms are generally products of variables, so realistic means and fluctuations of these variables are crucial for a successful simulation.
\nThe 19-year simulation of the Pacific basin by the monthly marine data-forced OPYC model displays good skill in reproducing SST variability. These results represent the first hindcast of which we are aware that uses both observed total heat-flux and wind-stress anomalies as forcing for such a long time interval. There is close agreement between the model SSTs and those observed in many regions of the Pacific, including the tropics and the northern extratropics. Besides performing credibly on the monthly time scale, the model captures the essence of low-frequency variability over the North Pacific, including aspects of a marked basin-wide change that occurred in 1976-1977. In the model's detailed heat budget, the anomalous air-sea heat fluxes, entrainment, and to a lesser extent horizontal advection, force thermal-anomaly changes in the mixed layer. Each of these components was apparently involved in the 1976-1977 decadal SST shift.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Natural climate variability on decade-to-century time scales","language":"English","publisher":"The National Academies Press","isbn":"978-0-309-12722-6","usgsCitation":"Cayan, D.R., Miller, A.J., Barnett, T.P., Graham, N.E., Ritchie, J.N., and Oberhuber, J.M., 1995, Seasonal-to-interannual fluctuations in surface temperature over the Pacific: effects of monthly winds and heat fluxes, chap. of Natural climate variability on decade-to-century time scales, p. 133-150.","productDescription":"18 p.","startPage":"133","endPage":"150","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1970-01-01","temporalEnd":"1988-12-31","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":307821,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":307820,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.nap.edu/catalog/5142/natural-climate-variability-on-decade-to-century-time-scales"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"560bb6f9e4b058f706e53e72","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":571147,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Arthur J.","contributorId":147311,"corporation":false,"usgs":false,"family":"Miller","given":"Arthur","email":"","middleInitial":"J.","affiliations":[{"id":13613,"text":"Scripps Institution of Oceanography (University of California, San Diego), La Jolla, CA","active":true,"usgs":false}],"preferred":false,"id":571148,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barnett, Tim P.","contributorId":147312,"corporation":false,"usgs":false,"family":"Barnett","given":"Tim","email":"","middleInitial":"P.","affiliations":[{"id":13613,"text":"Scripps Institution of Oceanography (University of California, San Diego), La Jolla, CA","active":true,"usgs":false}],"preferred":false,"id":571149,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Graham, Nicholas E.","contributorId":147313,"corporation":false,"usgs":false,"family":"Graham","given":"Nicholas","email":"","middleInitial":"E.","affiliations":[{"id":13613,"text":"Scripps Institution of Oceanography (University of California, San Diego), La Jolla, CA","active":true,"usgs":false}],"preferred":false,"id":571150,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ritchie, Jack N.","contributorId":147314,"corporation":false,"usgs":false,"family":"Ritchie","given":"Jack","email":"","middleInitial":"N.","affiliations":[{"id":13613,"text":"Scripps Institution of Oceanography (University of California, San Diego), La Jolla, CA","active":true,"usgs":false}],"preferred":false,"id":571151,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Oberhuber, Josef M.","contributorId":147315,"corporation":false,"usgs":false,"family":"Oberhuber","given":"Josef","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":571152,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70174331,"text":"70174331 - 1995 - Diagnostic modeling of trace metal partitioning in south San Francisco Bay","interactions":[],"lastModifiedDate":"2019-02-25T09:46:22","indexId":"70174331","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2620,"text":"Limnology and Oceanography","active":true,"publicationSubtype":{"id":10}},"title":"Diagnostic modeling of trace metal partitioning in south San Francisco Bay","docAbstract":"The two-dimensional numerical model ELAmet was used to investigate the effect of adsorption kinetics on the apparent distribution coefficients of Cu, Cd, and Zn in south San Francisco Bay, California. The numerical experiments were designed to determine whether adsorption kinetics can control the basin-scale variability of the observed partitioning and to define the conditions under which adsorption kinetics could account for strong interannual variability in partitioning.
\nThe numerical results indicate that aqueous speciation will control basin-scale spatial variations in the apparent distribution coefficient, Kda, if the system is close to equilibrium. However, basin-scale spatial variations in Kda are determined by the location of the sources of metal and the suspended solids concentration of the receiving water if the system is far from equilibrium. The overall spatial variability in Kda also increases as the system moves away from equilibrium.
","language":"English","publisher":"ASLO Publications","doi":"10.4319/lo.1995.40.2.0345","usgsCitation":"Wood, T.W., Baptista, A.M., Kuwabara, J., and Flegal, A., 1995, Diagnostic modeling of trace metal partitioning in south San Francisco Bay: Limnology and Oceanography, v. 40, no. 2, p. 345-358, https://doi.org/10.4319/lo.1995.40.2.0345.","productDescription":"14 p.","startPage":"345","endPage":"358","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":479188,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.4319/lo.1995.40.2.0345","text":"Publisher Index Page"},{"id":324904,"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 -122.42340087890624,\n 37.41598184194613\n ],\n [\n -122.42340087890624,\n 37.81195385919268\n ],\n [\n -121.89331054687499,\n 37.81195385919268\n ],\n [\n -121.89331054687499,\n 37.41598184194613\n ],\n [\n -122.42340087890624,\n 37.41598184194613\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"40","issue":"2","noUsgsAuthors":false,"publicationDate":"2003-12-22","publicationStatus":"PW","scienceBaseUri":"5780ceb4e4b08116168222fe","contributors":{"authors":[{"text":"Wood, T. W.","contributorId":172753,"corporation":false,"usgs":false,"family":"Wood","given":"T.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":641931,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baptista, A. M.","contributorId":172754,"corporation":false,"usgs":false,"family":"Baptista","given":"A.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":641932,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kuwabara, J.S.","contributorId":57905,"corporation":false,"usgs":true,"family":"Kuwabara","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":641933,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Flegal, A.R.","contributorId":64607,"corporation":false,"usgs":true,"family":"Flegal","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":641934,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":22025,"text":"ofr95628 - 1995 - Preliminary analysis of down-core biotic assemblages Bob Allen Keys, Everglades National Park, Florida Bay","interactions":[],"lastModifiedDate":"2022-01-04T17:27:15.453538","indexId":"ofr95628","displayToPublicDate":"1995-12-31T22:00:00","publicationYear":"1995","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":"95-628","displayTitle":"Preliminary Analysis of Down-Core Biotic Assemblages Bob Allen Keys, Everglades National Park, Florida Bay","title":"Preliminary analysis of down-core biotic assemblages Bob Allen Keys, Everglades National Park, Florida Bay","docAbstract":"A series of short piston cores (< 2m) were taken from eleven stations in Florida Bay in May, 1994 by researchers from the U.S. Geological Survey (St. Petersburg, FL., Woods Hole, MA., and Denver CO.) in cooperation with South Florida Water Management District, and the Everglades National Park, and the National Oceanic and Atmospheric Administration (NOAA). Core 6A from Bob Allen Keys (25° 1.391” N, 80°39.41” W) penetrated 172 cm of Holocene sediments in 0.6 m of water on a grass covered mud bank, approximately 1.75 miles (2.82 km) east of the water monitoring station on the southern end of the Bob Allen Keys. Core 6A was sampled for particle size, insoluble residue, water content, loss on ignition, Pb210, Rasup>222, and paleontologic analyses. Here we present the results of the preliminary paleontologic analyses of the biotic components from core #6A.
The Everglades/Florida Bay ecosystem has formed over the last 5000 years at the southern tip of peninsular Florida. Here it has been influenced by Atlantic, Caribbean and Gulf of Mexico waters, and by tropical and subtropical climatic regimes. This location ensures that over time the ecosystem has undergone climatic changes on both a seasonal and long term basis, and that it has been subjected to many major storms. Additionally, in the last century, the hydrologic regime of the region has been altered profoundly through construction of a canal system to control flooding in southern Florida. This system regulates the timing and amount of freshwater flow into Florida Bay. Recently, algal blooms, seagrass, and sponge die-offs, and declining numbers of shellfish, have been reported in Florida Bay; although it has been assumed that these changes have resulted from human alteration of freshwater flow into the bay, this assumption has not been rigorously tested.
The research described here is part of a project designed to examine the history of the Everglades/Florida Bay ecosystem over the last 150 years and to test assumptions of cause and effect. The purpose of the project is two-fold; first, to determine the characteristics of the ecosystem prior to significant human-induced alteration, including the natural range of variation in the ecosystem. This information will establish a baseline for restoration of the system. Second, the project aims to establish the extent, range, and timing of changes to the ecosystem over the last 150 years, and to determine whether these changes correlate with human alteration of the environment, or meteorological patterns, such as precipitation and major storms, or a combination of factors.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr95628","issn":"0094-9140","usgsCitation":"Brewster-Wingard, G., Ishman, S., Cronin, T.M., Edwards, L.E., Willard, D.A., and Halley, R.B., 1995, Preliminary analysis of down-core biotic assemblages Bob Allen Keys, Everglades National Park, Florida Bay: U.S. Geological Survey Open-File Report 95-628, 35 p., https://doi.org/10.3133/ofr95628.","productDescription":"35 p.","numberOfPages":"35","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":362632,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0628/ofr1995628.pdf","text":"Report","size":"257 KB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1995-628"},{"id":152970,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0628/coverthb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Everglades National Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -87.5390625,\n 30.939924331023445\n ],\n [\n -87.51708984375,\n 30.334953881988564\n ],\n [\n -85.8251953125,\n 29.99300228455108\n ],\n [\n -84.17724609375,\n 29.075375179558346\n ],\n [\n -83.1884765625,\n 28.34306490482549\n ],\n [\n -82.4853515625,\n 26.05678288577881\n ],\n [\n -80.57373046875,\n 24.627044746156027\n ],\n [\n -79.7607421875,\n 26.41155054662258\n ],\n [\n -80.04638671875,\n 27.89734922968426\n ],\n [\n -80.9912109375,\n 30.031055426540206\n ],\n [\n -81.40869140625,\n 30.713503990354965\n ],\n [\n -81.82617187499999,\n 30.80791068136646\n ],\n [\n -84.814453125,\n 30.789036751261136\n ],\n [\n -84.990234375,\n 31.109388560814963\n ],\n [\n -87.5390625,\n 30.939924331023445\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
Lake systems continually respond to climatic conditions that vary over broad scales of space and time. The spatial distribution of lakes on the Earth’s surface is indicative of long-term patterns of atmospheric circulation, and the annual cycle of climate over lake basins is reflected in seasonal change in the size and temperature of lakes. Lake size is determined by the balance of water inputs and outputs, and lake temperature is governed by the balance of heat inputs and outputs. The lake hydrological and energy balances are coupled to the atmosphere. In response to the inputs of mass, energy, and momentum (precipitation, radiation, and wind stress), lakes return heat and moisture to the atmosphere through conduction and evaporation. Global, regional, or local change in the hydrological or thermal states of lakes thus represent interactive responses to climatic variation in the supply of water and energy.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Physics and chemistry of lakes","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Springerlink","doi":"10.1007/978-3-642-85132-2_3","usgsCitation":"Hostetler, S.W., 1995, Hydrological and thermal response of lakes to climate: Description and modeling, chap. of Physics and chemistry of lakes, p. 63-82, https://doi.org/10.1007/978-3-642-85132-2_3.","productDescription":"20 p.","startPage":"63","endPage":"82","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":380862,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hostetler, Steven W. 0000-0003-2272-8302 swhostet@usgs.gov","orcid":"https://orcid.org/0000-0003-2272-8302","contributorId":3249,"corporation":false,"usgs":true,"family":"Hostetler","given":"Steven","email":"swhostet@usgs.gov","middleInitial":"W.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":805866,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70206029,"text":"70206029 - 1995 - Assessing the hydrologic impact of land use change in wetland watersheds: A case study from Northern Ohio, USA","interactions":[],"lastModifiedDate":"2019-11-08T12:27:33","indexId":"70206029","displayToPublicDate":"1995-12-31T11:08:16","publicationYear":"1995","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Assessing the hydrologic impact of land use change in wetland watersheds: A case study from Northern Ohio, USA","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Geomorphology and Land management in a Changing Environment","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Wiley","isbn":"0471955116, 9780471955115","usgsCitation":"McClintock, K.A., Harbor, J.A., and Wilson, T.P., 1995, Assessing the hydrologic impact of land use change in wetland watersheds: A case study from Northern Ohio, USA, chap. of Geomorphology and Land management in a Changing Environment.","costCenters":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"links":[{"id":368381,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Ohio","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"McClintock, K. A.","contributorId":219849,"corporation":false,"usgs":false,"family":"McClintock","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":773356,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harbor, J. A.","contributorId":219850,"corporation":false,"usgs":false,"family":"Harbor","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":773357,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilson, Timothy P. 0000-0003-1914-6344 tpwilson@usgs.gov","orcid":"https://orcid.org/0000-0003-1914-6344","contributorId":220370,"corporation":false,"usgs":true,"family":"Wilson","given":"Timothy","email":"tpwilson@usgs.gov","middleInitial":"P.","affiliations":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"preferred":true,"id":773358,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70205972,"text":"70205972 - 1995 - Chemical and biological processes affecting the fate and transport of trichloroethylene in the subsurface at Picatinny Arsenal, New Jersey","interactions":[],"lastModifiedDate":"2019-10-14T09:56:10","indexId":"70205972","displayToPublicDate":"1995-12-31T09:47:50","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1925,"text":"Hydrological Science and Technology","active":true,"publicationSubtype":{"id":10}},"title":"Chemical and biological processes affecting the fate and transport of trichloroethylene in the subsurface at Picatinny Arsenal, New Jersey","docAbstract":"No abstract available.
","language":"English","publisher":"American Institute of Hydrology","usgsCitation":"Imbrigiotta, T.E., Ehlke, T.A., Martin, M., Koller, D., and Smith, J.A., 1995, Chemical and biological processes affecting the fate and transport of trichloroethylene in the subsurface at Picatinny Arsenal, New Jersey: Hydrological Science and Technology, v. 11, no. 1-4, p. 26-50.","productDescription":"25 p.","startPage":"26","endPage":"50","costCenters":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"links":[{"id":368295,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Mew Jersey","otherGeospatial":"Picatinny Arssenal","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -74.49623107910156,\n 40.99544751505735\n ],\n [\n -74.5199203491211,\n 40.99337446752447\n ],\n [\n -74.5865249633789,\n 40.9469729829084\n ],\n [\n -74.5920181274414,\n 40.92570553920497\n ],\n [\n -74.57725524902344,\n 40.91091803848203\n ],\n [\n -74.52644348144531,\n 40.94541706066315\n ],\n [\n -74.51339721679686,\n 40.95293701189724\n ],\n [\n -74.4927978515625,\n 40.99207877971285\n ],\n [\n -74.49623107910156,\n 40.99544751505735\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"11","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Imbrigiotta, Thomas E. 0000-0003-1716-4768 timbrig@usgs.gov","orcid":"https://orcid.org/0000-0003-1716-4768","contributorId":152114,"corporation":false,"usgs":true,"family":"Imbrigiotta","given":"Thomas","email":"timbrig@usgs.gov","middleInitial":"E.","affiliations":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"preferred":true,"id":773124,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ehlke, T. A.","contributorId":106477,"corporation":false,"usgs":true,"family":"Ehlke","given":"T.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":773125,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Martin, Mary","contributorId":7290,"corporation":false,"usgs":true,"family":"Martin","given":"Mary","affiliations":[],"preferred":false,"id":773126,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Koller, David","contributorId":219769,"corporation":false,"usgs":false,"family":"Koller","given":"David","email":"","affiliations":[],"preferred":false,"id":773127,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Smith, J. A.","contributorId":219770,"corporation":false,"usgs":false,"family":"Smith","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":773128,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70185379,"text":"70185379 - 1995 - Assimilation of trace elements ingested by the mussel Mytilus edulis: Effects of algal food abundance","interactions":[],"lastModifiedDate":"2019-02-25T10:34:49","indexId":"70185379","displayToPublicDate":"1995-12-14T00:00:00","publicationYear":"1995","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":"Assimilation of trace elements ingested by the mussel Mytilus edulis: Effects of algal food abundance","docAbstract":"Pulse-chase feeding and multi-labeled radiotracer techniques were employed to measure the assimilation of 6 trace elements (110mAg, 241Am, 109Cd, 57Co, 75Se and 65Zn) from ingested diatoms in the mussel Mytilus edulis feeding at different rates (0.1, 0.49 and 1.5 mg dry wt h-1). Uniformly radiolabeled diatoms Thalassiosira pseudonana were fed to mussels for 0.5 h, and the behavior of the radiotracers in individual mussels was followed for 96 h in a depuration seawater system. Assimilation efficiency (AE) of each element declined with increasing ingestion rate and increased with gut passage time. The importance of extracellular digestion relative to intracellular digestion increased with ingestion activity, which, when coupled with a decline in AE, suggested that extracellular digestion is less efficient in metal absorption. Zn assimilation was most affected by ingestion rate, suggesting that AE may play a role in the physiological regulation of this metal in M. edulis. In an experiment to simulate the effects of an acidic gut, lowered pH (5.5) enhanced the release of elements from intact diatom cells, especially at low particle concentration. These results indicate that both feeding components of the mussel (i.e. gut passage time, digestive partitioning) and metal chemistry (i.e. metal release at lowered pH within the bivalve gut) are responsible for the difference in the assimilation of trace metals at different food quantities observed in mussels.
","language":"English","publisher":"Inter-Research","doi":"10.3354/meps129165","usgsCitation":"Wang, W., Fisher, N., and Luoma, S., 1995, Assimilation of trace elements ingested by the mussel Mytilus edulis: Effects of algal food abundance: Marine Ecology Progress Series, v. 129, p. 165-176, https://doi.org/10.3354/meps129165.","productDescription":"12 p. ","startPage":"165","endPage":"176","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":479196,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3354/meps129165","text":"Publisher Index Page"},{"id":337942,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"129","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d23b92e4b0236b68f82904","contributors":{"authors":[{"text":"Wang, W.-X.","contributorId":90477,"corporation":false,"usgs":true,"family":"Wang","given":"W.-X.","email":"","affiliations":[],"preferred":false,"id":685386,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fisher, N.S.","contributorId":67668,"corporation":false,"usgs":true,"family":"Fisher","given":"N.S.","email":"","affiliations":[],"preferred":false,"id":685387,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Luoma, S. N.","contributorId":86353,"corporation":false,"usgs":true,"family":"Luoma","given":"S. N.","affiliations":[],"preferred":false,"id":685388,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70195997,"text":"70195997 - 1995 - Accuracy of tretyakov precipitation gauge: Result of wmo intercomparison","interactions":[],"lastModifiedDate":"2018-03-13T10:56:41","indexId":"70195997","displayToPublicDate":"1995-12-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1924,"text":"Hydrological Processes","active":true,"publicationSubtype":{"id":10}},"title":"Accuracy of tretyakov precipitation gauge: Result of wmo intercomparison","docAbstract":"The Tretyakov non-recording precipitation gauge has been used historically as the official precipitation measurement instrument in the Russian (formerly the USSR) climatic and hydrological station network and in a number of other European countries. From 1986 to 1993, the accuracy and performance of this gauge were evaluated during the WMO Solid Precipitation Measurement Intercomparison at 11 stations in Canada, the USA, Russia, Germany, Finland, Romania and Croatia. The double fence intercomparison reference (DFIR) was the reference standard used at all the Intercomparison stations in the Intercomparison. The Intercomparison data collected at the different sites are compatible with respect to the catch ratio (measured/DFIR) for the same gauge, when compared using mean wind speed at the height of the gauge orifice during the observation period.
The Intercomparison data for the Tretyakov gauge were compiled from measurements made at these WMO intercomparison sites. These data represent a variety of climates, terrains and exposures. The effects of environmental factors, such as wind speed, wind direction, type of precipitation and temperature, on gauge catch ratios were investigated. Wind speed was found to be the most important factor determining the gauge catch and air temperature had a secondary effect when precipitation was classified into snow, mixed and rain. The results of the analysis of gauge catch ratio versus wind speed and temperature on a daily time step are presented for various types of precipitation. Independent checks of the correction equations against the DFIR have been conducted at those Intercomparison stations and a good agreement (difference less than 10%) has been obtained. The use of such adjustment procedures should significantly improve the accuracy and homogeneity of gauge-measured precipitation data over large regions of the former USSR and central Europe.
","language":"English","publisher":"Wiley","doi":"10.1002/hyp.3360090805","usgsCitation":"Yang, D., Goodison, B.E., Metcalfe, J.R., Golubev, V.S., Elomaa, E., Gunther, T., Bates, R., Pangburn, T., Hanson, C.L., Emerson, D.G., Copaciu, V., and Milkovic, J., 1995, Accuracy of tretyakov precipitation gauge: Result of wmo intercomparison: Hydrological Processes, v. 9, no. 8, p. 877-895, https://doi.org/10.1002/hyp.3360090805.","productDescription":"19 p.","startPage":"877","endPage":"895","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":352429,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"8","noUsgsAuthors":false,"publicationDate":"2006-07-31","publicationStatus":"PW","scienceBaseUri":"5aff209ce4b0da30c1bfd5bc","contributors":{"authors":[{"text":"Yang, Daqing","contributorId":203286,"corporation":false,"usgs":false,"family":"Yang","given":"Daqing","email":"","affiliations":[],"preferred":false,"id":730855,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goodison, Barry E.","contributorId":203293,"corporation":false,"usgs":false,"family":"Goodison","given":"Barry","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":730856,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Metcalfe, John R.","contributorId":203294,"corporation":false,"usgs":false,"family":"Metcalfe","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":730857,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Golubev, Valentin S.","contributorId":203295,"corporation":false,"usgs":false,"family":"Golubev","given":"Valentin","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":730858,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Elomaa, Esko","contributorId":203296,"corporation":false,"usgs":false,"family":"Elomaa","given":"Esko","email":"","affiliations":[],"preferred":false,"id":730859,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gunther, Thilo","contributorId":203287,"corporation":false,"usgs":false,"family":"Gunther","given":"Thilo","email":"","affiliations":[],"preferred":false,"id":730860,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Bates, Roy","contributorId":203288,"corporation":false,"usgs":false,"family":"Bates","given":"Roy","email":"","affiliations":[],"preferred":false,"id":730861,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Pangburn, Timothy","contributorId":203289,"corporation":false,"usgs":false,"family":"Pangburn","given":"Timothy","email":"","affiliations":[],"preferred":false,"id":730862,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Hanson, Clayton L.","contributorId":203290,"corporation":false,"usgs":false,"family":"Hanson","given":"Clayton","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":730863,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Emerson, Douglas G.","contributorId":40579,"corporation":false,"usgs":true,"family":"Emerson","given":"Douglas","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":730864,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Copaciu, Voilete","contributorId":203291,"corporation":false,"usgs":false,"family":"Copaciu","given":"Voilete","email":"","affiliations":[],"preferred":false,"id":730865,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Milkovic, Janja","contributorId":203292,"corporation":false,"usgs":false,"family":"Milkovic","given":"Janja","email":"","affiliations":[],"preferred":false,"id":730866,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}} ,{"id":70185328,"text":"70185328 - 1995 - Simulation of aerobic and anaerobic biodegradation processes at a crude oil spill site","interactions":[],"lastModifiedDate":"2018-03-08T14:53:55","indexId":"70185328","displayToPublicDate":"1995-12-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Simulation of aerobic and anaerobic biodegradation processes at a crude oil spill site","docAbstract":"A two-dimensional, multispecies reactive solute transport model with sequential aerobic and anaerobic degradation processes was developed and tested. The model was used to study the field-scale solute transport and degradation processes at the Bemidji, Minnesota, crude oil spill site. The simulations included the biodegradation of volatile and nonvolatile fractions of dissolved organic carbon by aerobic processes, manganese and iron reduction, and methanogenesis. Model parameter estimates were constrained by published Monod kinetic parameters, theoretical yield estimates, and field biomass measurements. Despite the considerable uncertainty in the model parameter estimates, results of simulations reproduced the general features of the observed groundwater plume and the measured bacterial concentrations. In the simulation, 46% of the total dissolved organic carbon (TDOC) introduced into the aquifer was degraded. Aerobic degradation accounted for 40% of the TDOC degraded. Anaerobic processes accounted for the remaining 60% of degradation of TDOC: 5% by Mn reduction, 19% by Fe reduction, and 36% by methanogenesis. Thus anaerobic processes account for more than half of the removal of DOC at this site.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/95WR02567","usgsCitation":"Essaid, H.I., Bekins, B.A., Godsy, E.M., Warren, E., Baedecker, M.J., and Cozzarelli, I.M., 1995, Simulation of aerobic and anaerobic biodegradation processes at a crude oil spill site: Water Resources Research, v. 31, no. 12, p. 3309-3327, https://doi.org/10.1029/95WR02567.","productDescription":"19 p.","startPage":"3309","endPage":"3327","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337870,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"12","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"58d0ea1ee4b0236b68f67393","contributors":{"authors":[{"text":"Essaid, Hedeff I. 0000-0003-0154-8628 hiessaid@usgs.gov","orcid":"https://orcid.org/0000-0003-0154-8628","contributorId":2284,"corporation":false,"usgs":true,"family":"Essaid","given":"Hedeff","email":"hiessaid@usgs.gov","middleInitial":"I.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":685193,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bekins, Barbara A. 0000-0002-1411-6018 babekins@usgs.gov","orcid":"https://orcid.org/0000-0002-1411-6018","contributorId":1348,"corporation":false,"usgs":true,"family":"Bekins","given":"Barbara","email":"babekins@usgs.gov","middleInitial":"A.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":36183,"text":"Hydro-Ecological Interactions Branch","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":685194,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Godsy, E. Michael","contributorId":45842,"corporation":false,"usgs":true,"family":"Godsy","given":"E.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":685195,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Warren, Ean ewarren@usgs.gov","contributorId":1351,"corporation":false,"usgs":true,"family":"Warren","given":"Ean","email":"ewarren@usgs.gov","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":685196,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Baedecker, Mary Jo mjbaedec@usgs.gov","contributorId":3346,"corporation":false,"usgs":true,"family":"Baedecker","given":"Mary","email":"mjbaedec@usgs.gov","middleInitial":"Jo","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":false,"id":685197,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Cozzarelli, Isabelle M. 0000-0002-5123-1007 icozzare@usgs.gov","orcid":"https://orcid.org/0000-0002-5123-1007","contributorId":1693,"corporation":false,"usgs":true,"family":"Cozzarelli","given":"Isabelle","email":"icozzare@usgs.gov","middleInitial":"M.","affiliations":[{"id":49175,"text":"Geology, Energy & Minerals Science Center","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":685198,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70185358,"text":"70185358 - 1995 - Comment on \"Horizontal aquifer movement in a theis-theim confined system\" by Donald C. Helm","interactions":[],"lastModifiedDate":"2020-04-25T02:26:37.22791","indexId":"70185358","displayToPublicDate":"1995-12-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Comment on \"Horizontal aquifer movement in a theis-theim confined system\" by Donald C. Helm","docAbstract":"In a recent paper, Helm [1994] presents an analysis of horizontal aquifer movement induced by groundwater withdrawal from a confined aquifer in which fluid and grains are incompressible. The analysis considers the aquifer in isolation (ignoring overlying and underlying strata) and assumes that the aquifer deforms purely in the horizontal direction (with no vertical movement). Helm's solution for grain displacement is obtained through introduction of a quantity known as bulk flux, qb, defined as
qb = nvw + (1 - n)vs
where n is porosity, vw is velocity of water, and vs is the velocity of the solid grains. On the basis of the bulk flux concept, Helm develops an explanation for the driving force on the bulk material.
It is our view that Helm's analysis is subject to four limitations. First, Helm's assumption of zero vertical displacement is not supported by field observations and could result in over- estimation of radial displacement. Second, in ignoring the role of overlying and underlying strata, Helm's solution does not yield reliable estimates of aquifer deformation. Third, Helm's solution method works only for problems that involve one spatial coordinate (for example, x or r) but does not generally work for problems involving three-dimensional flow and de- formation. Fourth, Helm's explanation of the driving force on the bulk material is faulty for general three-dimensional problems. The purpose of our comment is to discuss these four issues.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/95WR02713","usgsCitation":"Hsieh, P.A., and Cooley, R.L., 1995, Comment on \"Horizontal aquifer movement in a theis-theim confined system\" by Donald C. Helm: Water Resources Research, v. 31, no. 12, p. 3107-3111, https://doi.org/10.1029/95WR02713.","productDescription":"5 p. ","startPage":"3107","endPage":"3111","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":479198,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/95wr02713","text":"Publisher Index Page"},{"id":337920,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"12","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"58d23b92e4b0236b68f82908","contributors":{"authors":[{"text":"Hsieh, Paul A. 0000-0003-4873-4874 pahsieh@usgs.gov","orcid":"https://orcid.org/0000-0003-4873-4874","contributorId":1634,"corporation":false,"usgs":true,"family":"Hsieh","given":"Paul","email":"pahsieh@usgs.gov","middleInitial":"A.","affiliations":[{"id":39113,"text":"WMA - Office of Quality Assurance","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":685314,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooley, Richard L.","contributorId":8831,"corporation":false,"usgs":true,"family":"Cooley","given":"Richard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":685315,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70185384,"text":"70185384 - 1995 - Eolian transport, saline lake basins, and groundwater solutes","interactions":[],"lastModifiedDate":"2018-03-08T14:58:48","indexId":"70185384","displayToPublicDate":"1995-12-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Eolian transport, saline lake basins, and groundwater solutes","docAbstract":"Eolian processes associated with saline lakes are shown to be important in determining solute concentration in groundwater in arid and semiarid areas. Steady state mass balance analyses of chloride in the groundwater at Double Lakes, a saline lake basin in the southern High Plains of Texas, United States, suggest that approximately 4.5 × 105 kg of chloride is removed from the relatively small (4.7 km2) basin floor each year by deflation. This mass enters the groundwater down the wind gradient from the lake, degrading the water quality. The estimates of mass transport were independently determined by evaluation of solutes in the unsaturated zone and by solute mass balance calculations of groundwater flux. Transport of salts from the lake was confirmed over a short term (2 years) by strategically placed dust collectors. Results consistent with those at Double Lake were obtained from dune surfaces collected upwind and downwind from a sabkha near the city of Abu Dhabi in the United Arab Emirates. The eolian transport process provides an explanation of the degraded groundwater quality associated with the 30–40 saline lake basins on the southern half of the southern High Plains of Texas and New Mexico and in many other arid and semiarid areas.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/95WR02572","usgsCitation":"Wood, W., and Sanford, W.E., 1995, Eolian transport, saline lake basins, and groundwater solutes: Water Resources Research, v. 31, no. 12, p. 3121-3129, https://doi.org/10.1029/95WR02572.","productDescription":"9 p. ","startPage":"3121","endPage":"3129","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337947,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"12","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"58d23b92e4b0236b68f82906","contributors":{"authors":[{"text":"Wood, Warren W.","contributorId":47770,"corporation":false,"usgs":false,"family":"Wood","given":"Warren W.","affiliations":[{"id":6601,"text":"Michigan State University","active":true,"usgs":false}],"preferred":false,"id":685399,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sanford, Ward E. 0000-0002-6624-0280 wsanford@usgs.gov","orcid":"https://orcid.org/0000-0002-6624-0280","contributorId":2268,"corporation":false,"usgs":true,"family":"Sanford","given":"Ward","email":"wsanford@usgs.gov","middleInitial":"E.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"preferred":true,"id":685400,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":21393,"text":"ofr95340 - 1995 - Origin of water that discharges from Calf Creek Spring, Garfield County, Utah","interactions":[],"lastModifiedDate":"2017-08-31T13:35:43","indexId":"ofr95340","displayToPublicDate":"1995-12-01T00:00:00","publicationYear":"1995","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":"95-340","title":"Origin of water that discharges from Calf Creek Spring, Garfield County, Utah","docAbstract":"Calf Creek Spring provides drinking water to users of Calf Creek Campground, which is operated by the Bureau of Land Management in southcentral Utah. Use of all methods and tools available indicates that surface water from Calf Creek does not contribute to the discharge of Calf Creek Spring.
Microscopic Particulate Analysis of spring water indicates that the spring has a low risk of surface-water contamination, which is substantiated by a bacterial test of water from the point of discharge of Calf Creek Spring, the Calf Creek Spring collection box, a tap from the water distribution system, and Calf Creek near the picnic area. Bacteria colonies were found in Calf Creek near the picnic area.
Calf Creek Spring discharges from fractured Navajo Sandstone where the potential for contamination by animal or human microbes is slight. Calf Creek probably gains water along its entire length from the aquifer in the Navajo Sandstone. Once at the surface, water in Calf Creek is exposed to animal- and human-borne microbes. If the water level in the Navajo aquifer at the spring remains higher than the water level of the creek, mixing is unlikely to occur and contamination is unlikely. The water level of Calf Creek Spring in June 1994 was at least 4 feet above the water level of Calf Creek.
Water from Calf Creek Spring is a mixed type composed of magnesium, calcium, sodium, bicarbonate, and sulfate ions, and water from Calf Creek is a mixed type composed of calcium, magnesium, bicarbonate, sulfate, and chloride ions. Compositional similarity is not unusual if both water sources are derived from the Navajo aquifer.
Discharge and temperature measurements at the spring and in the creek in May and June 1994 vary independently and do not indicate a hydraulic connection. Turbidity measurements, though not conclusive, indicate that no direct hydraulic connection exists between Calf Creek and Calf Creek Spring.
Hydrologic characteristics of Calf Creek provide evidence that the probable long-term, sustainable source of water is the Navajo aquifer and not precipitation-derived runoff. Ground-water leakage from adjacent drainages could contribute to perennial flow in Calf Creek. Fractures modify the movement of ground water to discharge areas, such as Calf Creek Spring.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr95340","collaboration":"Prepared in cooperation with the Bureau of Land Management","usgsCitation":"Wilberg, D.E., 1995, Origin of water that discharges from Calf Creek Spring, Garfield County, Utah: U.S. Geological Survey Open-File Report 95-340, iv, 10 p., https://doi.org/10.3133/ofr95340.","productDescription":"iv, 10 p.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":50963,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0340/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":154039,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0340/report-thumb.jpg"}],"country":"United States","state":"Utah","county":"Garfield County","otherGeospatial":"Calf Creek Campground, Calf Creek Spring","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.41595840454102,\n 37.79154065815569\n ],\n [\n -111.41115188598633,\n 37.79154065815569\n ],\n [\n -111.41115188598633,\n 37.79893346559687\n ],\n [\n -111.41595840454102,\n 37.79893346559687\n ],\n [\n -111.41595840454102,\n 37.79154065815569\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e76a","contributors":{"authors":[{"text":"Wilberg, Dale E.","contributorId":101275,"corporation":false,"usgs":true,"family":"Wilberg","given":"Dale","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":184350,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":20086,"text":"ofr95136 - 1995 - Water-quality assessment of the Albemarle-Pamlico drainage basin, North Carolina and Virginia environmental setting and water-quality issues","interactions":[],"lastModifiedDate":"2021-08-20T21:11:02.359254","indexId":"ofr95136","displayToPublicDate":"1995-12-01T00:00:00","publicationYear":"1995","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":"95-136","title":"Water-quality assessment of the Albemarle-Pamlico drainage basin, North Carolina and Virginia environmental setting and water-quality issues","docAbstract":"The Albemarle-Pamlico drainage study unit is one of 60 units of the U.S. Geological Survey's National Water-Quality Assessment Program, and includes the large river basins which drain into the Albemarle and Pamlico Sounds-the Chowan, Roanoke, Tar-Pamlico, and Neuse River Basins. The study unit includes about 28,000 square miles and has an interrelated set of environmental characteristics which strongly influence water quality. The chemical and physical nature of these characteristics are the dominant controls on baseline water quality in the study area. About 50 percent of the study area is forested, slightly more than 30 percent is agricultural, about 15 percent is wetlands, and less than 5 percent is developed. Three million people live in the study area, and activities related to agriculture and development have caused increased concentrations of constituents such as nutrients, pesticides, and suspended sediment. About two-thirds of the 36 to 52 inches of precipitation in the area reenters the atmosphere by evapotranspiration. About one-third of the remaining precipitation reaches streams by overland runoff; the remainder recharges the water table aquifer, where much of the water eventually discharges to streams as ground water. Thus, ground-water quality has a substantial influence on surface-water quality, particularly during dry weather. In 1990, about 152,900 tons of elemental nitrogen and 10,500 tons of elemental phosphorus either were applied to crops as fertilizer or fixed by biological processes, and in 1987, about 43,500 tons of nitrogen and 12,200 tons of phosphorus were produced as animal wastes. In addition, about 1,300 tons of selected herbicides and 400 tons of selected insecticides were applied to crops in 1990. Some 249 permitted point sources discharged 410 million gallons per day, containing an annual load of 5,800 tons of nitrogen and 1,800 tons of phosphorus, to the study area in 1990. Data from 1970-79 indicate that mean annual suspended-sediment yields for selected forested, agricultural, and developed urban basins in North Carolina are 50, 250, and 550 tons per square mile, respectively. In order to facilitate comparisons, much of the data were compiled by hydrologic unit. Homogeneous areas, or strata, representing the most prevalent combinations of environmental factors, such as land use, soils, and geology, were defined. Future data collection and analyses will be designed to answer objective-related concerns about the relations between important water-quality conditions and these study-unit strata.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95136","usgsCitation":"McMahon, G., and Lloyd, O., 1995, Water-quality assessment of the Albemarle-Pamlico drainage basin, North Carolina and Virginia environmental setting and water-quality issues: U.S. Geological Survey Open-File Report 95-136, vi, 73 p., https://doi.org/10.3133/ofr95136.","productDescription":"vi, 73 p.","costCenters":[],"links":[{"id":388266,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19159.htm"},{"id":49637,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0136/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153492,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0136/report-thumb.jpg"}],"country":"United States","state":"North Carolina, Virginia","otherGeospatial":"Albemarle-Pamlico drainage basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.15625,\n 34.831841149828655\n ],\n [\n -75.08056640625,\n 34.831841149828655\n ],\n [\n -75.08056640625,\n 37.23907530202184\n ],\n [\n -80.15625,\n 37.23907530202184\n ],\n [\n -80.15625,\n 34.831841149828655\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e7006","contributors":{"authors":[{"text":"McMahon, Gerard 0000-0001-7675-777X gmcmahon@usgs.gov","orcid":"https://orcid.org/0000-0001-7675-777X","contributorId":191488,"corporation":false,"usgs":true,"family":"McMahon","given":"Gerard","email":"gmcmahon@usgs.gov","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true},{"id":565,"text":"Southeast Climate Science Center","active":true,"usgs":true}],"preferred":true,"id":182034,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lloyd, Orville B.","contributorId":24378,"corporation":false,"usgs":true,"family":"Lloyd","given":"Orville B.","affiliations":[],"preferred":false,"id":182035,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":19854,"text":"ofr95314 - 1995 - U.S. Geological Survey activities in New Mexico 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:07:36","indexId":"ofr95314","displayToPublicDate":"1995-12-01T00:00:00","publicationYear":"1995","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":"95-314","title":"U.S. Geological Survey activities in New Mexico 1995","docAbstract":"The report provides an overview of the USGS in New Mexico, \r\nincluding activities of the Water Resources, Geologic, and National Mapping \r\nDivisions. Some USGS projects address hydrologic and geologic hazards, \r\nsuch as flood discharges, landslides, and land subsidence. Recent \r\nenvironmental assessments include participation in the Kirtland Air Force \r\nBase Installation Restoration Program, erosion on the Zuni Reservation, \r\nand ground-water contamination in eastern Bernalillo County. Water \r\navailability studies have focused on ground-water depletion in the \r\nAlbuquerque Basin, recharge in the Roswell Basin, and the water \r\nresources of Taos County. Irrigation drainage in the San Juan River area \r\nand trace metals in a reach of the Rio Grande have been investigated. \r\nThe National Water-Quality Assessment (NAWQA) program has two study \r\nunits partly located in New Mexico. Energy and mineral resource assess-\r\nments include gas resources in the San Juan Basin and environmental \r\nimpacts of mining in the Mimbres Resource Area. The USGS is studying the \r\nextent of suitable habitat for Mexican Spotted Owls. Also discussed are \r\ncartographic/thematic products and Geographical Information Systems; \r\nsurface-water, ground-water, and water-quality data-collection net-\r\nworks; and reports published from 1993 to 1995.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95314","usgsCitation":"Livingston, R.K., 1995, U.S. Geological Survey activities in New Mexico 1995: U.S. Geological Survey Open-File Report 95-314, 21 p. ill., col. maps ; 28 cm., https://doi.org/10.3133/ofr95314.","productDescription":"21 p. ill., col. maps ; 28 cm.","costCenters":[],"links":[{"id":152721,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0314/report-thumb.jpg"},{"id":49333,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0314/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db61254e","contributors":{"authors":[{"text":"Livingston, Russell K.","contributorId":69582,"corporation":false,"usgs":true,"family":"Livingston","given":"Russell","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":181634,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}