No abstract available.
The Rincon and Mesilla Valleys of New Mexico extend from Caballo Reservoir to El Paso del Norte, west of El Paso, Texas. Water supplies for this area are obtained from the Rio Grande and from the saturated sediments filling the intermontane basins of south-central New Mexico.
The two major aquifers are the Santa Fe Group of Miocene to middle Pleistocene age and the flood-plain alluvium of late Pleistocene and Holocene age. The Santa Fe Group is composed of thick deposits of interbedded clay, silt, sand, and gravel. The flood-plain alluvium, generally less than 80 feet thick, is composed of a basal gravel layer overlain by interbedded sand, silt, and clay.
In the Rincon Valley, the flood-plain alluvium is the principal source of ground water because the underlying Santa Fe is composed predominantly of lacustrine clay deposits. In the Mesilla Valley, thick deposits of fluvial sands and gravels in the Santa Fe Group are hydraulically connected with the flood-plain alluvium. Water-table conditions occur in the flood-plain alluvium, which is recharged primarily by infiltration of surface water from the Rio Grande, irrigation canals, and irrigated fields. Recharge to the Santa Fe Group occurs primarily from downward infiltration of water from the flood-plain alluvium and secondarily from runoff infiltrating upland sediments and mountain-front fan deposits. In the short term, the Santa Fe Group responds as a leaky confined aquifer due to the presence of interbedded clays that reduce vertical permeability.
Aquifer tests were conducted on 58 wells and test holes, most of which were completed in the Santa Fe Group. Transmissivities range from 1.3 to 21,100 feet squared per day. Average well yields range from about 1,050 gallons per minute in the Rincon Valley to about 1,500 gallons per minute in the Mesilla Valley. Yields in the Jornada del Muerto generally are much smaller.
Movement of ground water is generally southward in the Rincon and Mesilla Valleys and toward the valleys in the adjacent upland areas. Ground water moves southeastward beneath the West Mesa area, converging with ground-water flow in the southern end of the Mesilla Valley. Good hydraulic connection exists between sediments of the West Mesa and Mesilla Valley areas. Ground water in the southern end of the Jornada del Muerto moves generally to the northwest, converges with south-flowing ground water near Point of Rocks, and moves westward into Rincon Valley sediments near Rincon. A small amount of ground water flows westward from the southern end of the Jornada del Muerto across a subsurface igneous body into the Mesilla Valley. Ground-water discharge occurs throughout the Rincon and Mesilla Valleys as drain flow to the river and evapotranspiration.
Dissolved-solids concentrations in the water in the flood-plain alluvium of the Rincon and Mesilla Valleys are generally greater than 1,000 milligrams per liter. A freshwater zone, with dissolved-solids concentrations less than 1,000 milligrams per liter, underlies this thin, slightly saline zone beneath much of the Mesilla Valley. This freshwater zone, occurring in the Santa Fe Group, is surrounded by saline water. Within the study area, major dissolved ions in ground water include sodium, calcium, bicarbonate, and sulfate.
The Rio Grande is a gainlng stream in the northern parts of the Rincon and Mesilla Valleys and a losing stream in the southern part of the Mesilla Valley. Gains and losses result from a close interconnection with ground-water flow systems. Large surface-water irrigation allotments increase ground-water recharge. Increased recharge raises ground-water levels and improves shallow ground-water quality adjacent to these recharge areas. Shallow ground-water discharges to drains, which flow into the Rio Grande. Dissolved-solids concentrations in the Rio Grande increase by as much as 60 percent between Caballo Reservoir and the southern end of the study area.
","language":"English","publisher":"New Mexico State Engineer","publisherLocation":"Santa Fe, NM","collaboration":"Prepared by the U.S. Geological Survey in cooperation with: New Mexico State Engineer Office; U.S. Bureau of Reclamation; Elephant Butte Irrigation District; City of Las Cruces; New Mexico Water Resources Research Institute","usgsCitation":"Wilson, C.A., White, R., Orr, B.R., and Roybal, R.G., 1981, Water resources of the Rincon and Mesilla Valleys and adjacent areas, New Mexico: Technical Report 43, ix, 514 p.; Plates: 1-16: 24 x 38 inches.","productDescription":"ix, 514 p.; Plates: 1-16: 24 x 38 inches","numberOfPages":"540","costCenters":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"links":[{"id":265519,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70042517.JPG"},{"id":265518,"type":{"id":11,"text":"Document"},"url":"https://www.ose.state.nm.us/Pub/TechnicalReports/TechReport-043.pdf","text":"Report","size":"24.36 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"New Mexico","otherGeospatial":"Mesilla Valley, Rincon Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.05,31.33 ], [ -109.05,37.0 ], [ -103.0,37.0 ], [ -103.0,31.33 ], [ -109.05,31.33 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd7ccee4b0b2908510eff0","contributors":{"authors":[{"text":"Wilson, Clyde A.","contributorId":65464,"corporation":false,"usgs":true,"family":"Wilson","given":"Clyde","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":471680,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, Robert R.","contributorId":16420,"corporation":false,"usgs":true,"family":"White","given":"Robert R.","affiliations":[],"preferred":false,"id":471678,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Orr, Brennon R.","contributorId":18747,"corporation":false,"usgs":true,"family":"Orr","given":"Brennon","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":471679,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Roybal, R. Gary","contributorId":88948,"corporation":false,"usgs":true,"family":"Roybal","given":"R.","email":"","middleInitial":"Gary","affiliations":[],"preferred":false,"id":471681,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70038303,"text":"70038303 - 1981 - Water resources inventory of Connecticut Part 7: upper Connecticut River basin","interactions":[],"lastModifiedDate":"2014-06-27T14:07:44","indexId":"70038303","displayToPublicDate":"2012-04-29T10:03:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":108,"text":"Connecticut Water Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"24","title":"Water resources inventory of Connecticut Part 7: upper Connecticut River basin","docAbstract":"The 508 square miles of the upper Connecticut River basin in north-central Connecticut include the basins of four major tributaries: the Scantic, Park, and Hockanum Rivers, and the Farmington River downstream from Tariffville. Precipitation over this area averaged 44 inches per year during 1931-60. In this period, an additional 3,800 billion gallons of water per year entered the basin in the main stem of the Connecticut River at the Massachusetts state line, about 230 billion gallons per year in the Farmington River at Tariffville, and about 10 billion gallons per year in the Seantic River at the Massachusetts state line. Some water was also imported from outside the basin by water-supply systems. About half the precipitation, 22.2 inches, was lost from the basin by evapotranspiration; the remainder flowed out of the study area in the Connecticut River at Portland.
\nVariations in streamflow at 41 long-term continuous-record gaging stations are summarized in standardized graphs and tables that can be used to estimate streamflow characteristics at other sites. For example, mean-flow and two low-flow characteristics: (1) the 7-day annual minimum flow for 2-year and (2) 10-year recurrence intervals, have been determined for many partial-record stations throughout the basin.
\nOf the 30 principal lakes, ponds, and reservoirs, two have usable storage capacities of more than 1 billion gallons. The maximum safe draft rate (regulated flow) of the largest of these, Shenipsit Lake at Rockville, is 6.5 million gallons per day for the 2-year and 30-year recurrence intervals (median and lowest annual flow).
\nFloods have occurred within each month of the year but in different years. The greatest known flood on the Connecticut River was in March 1936; it had a peak flow of 130,000 cubic feet per second at Hartford. Since then, major floods have been reduced by flood-control measures.
\nThe major aquifers underlying the basin are composed of unconsolidated materials (stratified drift and till) and bedrock. Stratified drift overlies till and bedrock in valleys and lowlands in the eastern and western parts and in most of the broad central valley. The stratified drift generally ranges in thickness from 10 feet in small valleys to more than 200 feet in the Connecticut River Valley. Bedrock underlies the entire basin and is composed of (1) interbedded sedimentary and igneous rocks and (2) crystalline rocks.
\nGround-water sources yield from several million gallons per day from large well fields to 1 gallon per minute from single wells. Yields of 100 gal/min or more are most commonly obtained from screened wells tapping stratified-drift aquifers; amounts can be calculated by use of a series of graphs in conjunction with estimates of aquifer transmissivity and thickness. Eighteen areas underlain by good aquifers are selected as the most favorable locations for large-scale development of ground water. Selection of these areas is based on estimates of aquifer characteristics and the amount of water potentially available from induced infiltration of streamflow at low-flow conditions.
\nSmall to moderate water supplies can generally be obtained from any of the aquifers. Wells in bedrock yield at least a few gallons per minute at most sites. The probability of obtaining an adequate yield for domestic supply is greater in sedimentary than in crystalline bedrock and is also greater in stratified-drift overburden than in till.
\nWhere unaffected by man's activities, the water is of the calcium magnesium bicarbonate type, is generally low to moderate in dissolved-solids concentration, and ranges from soft to hard. In general, streamflow is less mineralized than ground water, particularly when it consists largely of direct runoff. However, streams become more highly mineralized during low-flow conditions, when most flow consists of more highly mineralized water discharged from aquifers. The median dissolved-solids concentration in water from 25 stream sites was 113 mg/L (milligrams per liter) during high flow, and 148 mg/L during low flow within the study period. Iron and manganese occur naturally in objectionable concentrations in some streams draining swamps and in some waters draining from sedimentary bedrock which contains iron- and manganese-bearing minerals.
\nMan's activities have affected the water quality of streams in much of the area, particularly in the Hockanum and Park River basins. The degradation in quality in these streams is shown by wide and erratic changes in dissolved-solids concentration, excessive amounts of trace elements, a low dissolved-oxygen content, and abnormally high temperatures. Ground water within this area is degraded principally by induced infiltration of surface water that contains chemical wastes, by leachate from wastes stored or disposed of on the ground, and by effluents discharged from septic tanks.
\nThe quantity and quality of water are satisfactory for a wide variety of uses, and, with suitable treatment, the water may be used for most purposes. The total amount of water used in 1968 was more than 100 billion gallons. About 80 percent of this was used for industrial purposes, and 90 percent of the industrial water was obtained from surface-water sources. About 85 percent of the population was supplied with water for domestic use by 15 major public and municipal systems and 25 private associations. Analyses of water from the 13 largest systems show generally good quality.
","language":"English","publisher":"Connecticut Department of Environmental Protection","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Connecticut Department of Environmental Protection","usgsCitation":"Ryder, R.B., Thomas, M.P., and Weiss, L.A., 1981, Water resources inventory of Connecticut Part 7: upper Connecticut River basin: Connecticut Water Resources Bulletin 24, Report: vii, 76 p.; 4 Plates: 37.33 x 50.45 inches and smaller.","productDescription":"Report: vii, 76 p.; 4 Plates: 37.33 x 50.45 inches and smaller","numberOfPages":"83","costCenters":[],"links":[{"id":258813,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ctwrb/0024/report.pdf","size":"17112","linkFileType":{"id":1,"text":"pdf"}},{"id":258814,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ctwrb/0024/report-thumb.jpg"}],"scale":"48000","country":"United States","state":"Connecticut","otherGeospatial":"Connecticut River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.833333,41.533333 ], [ -72.833333,42.058333 ], [ -72.366667,42.058333 ], [ -72.366667,41.533333 ], [ -72.833333,41.533333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc907e4b08c986b32cc15","contributors":{"authors":[{"text":"Ryder, Robert B. rryder@usgs.gov","contributorId":68294,"corporation":false,"usgs":true,"family":"Ryder","given":"Robert","email":"rryder@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":false,"id":463828,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, Mendall P.","contributorId":104314,"corporation":false,"usgs":true,"family":"Thomas","given":"Mendall","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":463830,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weiss, Lawrence A.","contributorId":102528,"corporation":false,"usgs":true,"family":"Weiss","given":"Lawrence","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":463829,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70006937,"text":"70006937 - 1981 - Immunization protects trout against protozoan parasite","interactions":[],"lastModifiedDate":"2012-07-09T01:01:40","indexId":"70006937","displayToPublicDate":"2012-01-01T21:42:40","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":284,"text":"Research Information Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"81-28","title":"Immunization protects trout against protozoan parasite","docAbstract":"No abstract available at this time","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Arlington, VA","collaboration":"None","usgsCitation":"Wolf, K., 1981, Immunization protects trout against protozoan parasite: Research Information Bulletin 81-28, 1 p.","productDescription":"1 p.","startPage":"1","endPage":"1","numberOfPages":"1","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":258261,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3899e4b0c8380cd6161d","contributors":{"authors":[{"text":"Wolf, K.","contributorId":16344,"corporation":false,"usgs":true,"family":"Wolf","given":"K.","email":"","affiliations":[],"preferred":false,"id":355507,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70006490,"text":"70006490 - 1981 - Substrate conditions and abundance of lake trout eggs in a traditional spawning area in southeastern Lake Michigan","interactions":[],"lastModifiedDate":"2012-07-18T01:01:44","indexId":"70006490","displayToPublicDate":"2012-01-01T16:07:18","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Substrate conditions and abundance of lake trout eggs in a traditional spawning area in southeastern Lake Michigan","docAbstract":"Spawning by planted lake trout (Salvelinus namaycush) was documented by sampling with a diver-assisted pump in a traditional spawning area in southeastern Lake Michigan near Saugatuck, Michigan in mid-November in 1978 and 1979. Bottom depths at the 11 locations sampled ranged from 3 to 12 m and substrate size from boulders to sand. Periphyton (Cladophora and associated biota) was several millimeters thick at most stations but sparse at the shallowest. The most eggs recovered from a single sample occurred at the shallowest depth (3 m). In both years, some of the small numbers of eggs collected (9 in 1978, 14 in 1979) were alive and fertilized. Laboratory incubation of viable eggs resulted in successful hatching of larvae. When compared with egg densities measured at spawning sites used by self-sustaining populations of lake trout in other lakes, densities in the study are (0-13/m2) appeared to be critically low. Insufficient numbers of eggs, combined with harsh incubation conditions (turbulence, ice scour, sedimentation), were implicated as prime causes for lake trout reproductive failure in the study area, although other factors, such as inappropriate spawning behavior (selection of suboptimal spawning location, depth, or substrate) also may have reduced survival of eggs and larvae.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"North American Journal of Fisheries Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor & Francis","publisherLocation":"Philadelphia, PA","doi":"10.1577/1548-8659(1981)1<165:SCAAOL>2.0.CO;2","collaboration":"Abstract has subscript/superscript to be fixed","usgsCitation":"Dorr, J.A., O’Connor, D.V., Foster, N.R., and Jude, D.J., 1981, Substrate conditions and abundance of lake trout eggs in a traditional spawning area in southeastern Lake Michigan: North American Journal of Fisheries Management, v. 1, no. 2, p. 165-172, https://doi.org/10.1577/1548-8659(1981)1<165:SCAAOL>2.0.CO;2.","productDescription":"8 p.","startPage":"165","endPage":"172","numberOfPages":"7","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":480557,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://hdl.handle.net/2027.42/140994","text":"External Repository"},{"id":258943,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":258940,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/1548-8659(1981)1<165:SCAAOL>2.0.CO;2","linkFileType":{"id":5,"text":"html"}}],"country":"United States","otherGeospatial":"Lake Michigan","volume":"1","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9d5ae4b08c986b31d7ce","contributors":{"authors":[{"text":"Dorr, John A. III","contributorId":68584,"corporation":false,"usgs":true,"family":"Dorr","given":"John","suffix":"III","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":354610,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Connor, Daniel V.","contributorId":73950,"corporation":false,"usgs":true,"family":"O’Connor","given":"Daniel","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":354611,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Foster, Neal R.","contributorId":67451,"corporation":false,"usgs":true,"family":"Foster","given":"Neal","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":354609,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jude, David J.","contributorId":11986,"corporation":false,"usgs":true,"family":"Jude","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":354608,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70039444,"text":"70039444 - 1981 - Water Resources Research October 1, 1979 - September 30, 1980: Summary statements of research activities by the Water Resources Division","interactions":[],"lastModifiedDate":"2012-08-04T01:01:57","indexId":"70039444","displayToPublicDate":"2012-01-01T15:55:28","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":379,"text":"Report","active":false,"publicationSubtype":{"id":6}},"title":"Water Resources Research October 1, 1979 - September 30, 1980: Summary statements of research activities by the Water Resources Division","docAbstract":"Research in the WRD had its beginnings in the late 1950's when the \"core research\" line item was added to the Congressional budget. Since this time the Federal program has grown from a \"basic sciences\" program to one that includes a broad spectrum of basic and applied scientific investigations. Water resources research in WRD includes the study of water in all its phases and uses the basic sciences of mathematics, chemistry, physics, biology, geology and engineering to gain a fundamental understanding of the processes that affect the movement of water and its chemical constituents through hydrologic systems. The basic knowledge and methodologies derived from water resources research are applicable not only to the solution of current problems associated with the Nation's water resources, but also to anticipated hydrologic issues.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70039444","collaboration":"Compiled by the Office of the Assistant Chief Hydrologist for Research and Technical Coordination, Water Resources Division","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Water Resources Research October 1, 1979 - September 30, 1980: Summary statements of research activities by the Water Resources Division: Report, x, 233 p., https://doi.org/10.3133/70039444.","productDescription":"x, 233 p.","numberOfPages":"247","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":261584,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039444/report.pdf"},{"id":261585,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039444/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc780e4b08c986b32c496","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535304,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70039196,"text":"70039196 - 1981 - The EROS Data Center","interactions":[],"lastModifiedDate":"2017-05-19T18:37:59","indexId":"70039196","displayToPublicDate":"2012-01-01T15:50:15","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"The EROS Data Center","docAbstract":"The Earth Resources Observation Systems (EROS) Program of the U.S. Department of the Interior, administered by the Geological Survey, was established in 1966 to apply remote-sensing techniques to the inventory, monitoring, and management of natural resources. To meet its primary objective, the EROS Program includes research and training in the interpretation and application of remotely sensed data and provides remotely sensed data at nominal cost to scientists, resource planners, managers, and the public.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039196","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, The EROS Data Center: General Information Product, 37 p., https://doi.org/10.3133/70039196.","productDescription":"37 p.","numberOfPages":"40","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":261364,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039196/report.pdf"},{"id":261365,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039196/report-thumb.jpg"}],"country":"United States","state":"South Dakota","city":"Sioux Falls","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -97,43.36666666666667 ], [ -97,43.75 ], [ -96.36666666666666,43.75 ], [ -96.36666666666666,43.36666666666667 ], [ -97,43.36666666666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba70de4b08c986b32133c","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535238,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70006661,"text":"70006661 - 1981 - Synthesis of carbon-14 and deuterium labeled N-nitroso-2 (3',7'-dimethyl-2',6'-octadienyl) aminoethanols","interactions":[],"lastModifiedDate":"2012-08-25T01:02:00","indexId":"70006661","displayToPublicDate":"2012-01-01T14:38:00","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2364,"text":"Journal of Labelled compounds and Radiopharmaceuticals","active":true,"publicationSubtype":{"id":10}},"title":"Synthesis of carbon-14 and deuterium labeled N-nitroso-2 (3',7'-dimethyl-2',6'-octadienyl) aminoethanols","docAbstract":"Methods of preparation of carbon-14 and deuterium labeled N-nitroso-2(3,7-dimethyl-2,6-octadienyl) aminoethanols are described. The primary synthetic method involved alkylation of ethanolamine or ethylglycine with suitable chlorides and subsequent mild nitrosation. Isomeric 14C-nitrosamines were also prepared by selective -cleavage of the di-substituted ethanolamine with nitrous acid.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Labelled compounds and Radiopharmaceuticals","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wiley","publisherLocation":"Hoboken, NJ","doi":"10.1002/jlcr.2580180817","collaboration":"None","usgsCitation":"Abidi, S.L., and Idelson, A., 1981, Synthesis of carbon-14 and deuterium labeled N-nitroso-2 (3',7'-dimethyl-2',6'-octadienyl) aminoethanols: Journal of Labelled compounds and Radiopharmaceuticals, v. 18, no. 8, p. 1215-1225, https://doi.org/10.1002/jlcr.2580180817.","productDescription":"11 p.","startPage":"1215","endPage":"1225","numberOfPages":"11","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":259915,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":259892,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/jlcr.2580180817","linkFileType":{"id":5,"text":"html"}}],"volume":"18","issue":"8","noUsgsAuthors":false,"publicationDate":"2006-07-10","publicationStatus":"PW","scienceBaseUri":"505ba352e4b08c986b31fc66","contributors":{"authors":[{"text":"Abidi, S. L.","contributorId":19898,"corporation":false,"usgs":true,"family":"Abidi","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":354965,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Idelson, A.L.","contributorId":105255,"corporation":false,"usgs":true,"family":"Idelson","given":"A.L.","email":"","affiliations":[],"preferred":false,"id":354966,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70006940,"text":"70006940 - 1981 - Book Review: Symposium on Parasitology and Pathology of Marine Organisms, Leningrad, USSR: 13-16 October 1981","interactions":[],"lastModifiedDate":"2012-09-06T01:02:24","indexId":"70006940","displayToPublicDate":"2012-01-01T14:29:00","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1647,"text":"Fish Health News","active":true,"publicationSubtype":{"id":10}},"title":"Book Review: Symposium on Parasitology and Pathology of Marine Organisms, Leningrad, USSR: 13-16 October 1981","docAbstract":"No abstract available at this time","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fish Health News","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Arlington, VA","collaboration":"None","usgsCitation":"Wolf, K., 1981, Book Review: Symposium on Parasitology and Pathology of Marine Organisms, Leningrad, USSR: 13-16 October 1981: Fish Health News, v. 13, no. 1-2, p. iii-iii.","productDescription":"1 p.","startPage":"iii","endPage":"iii","numberOfPages":"1","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":260221,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f203e4b0c8380cd4af77","contributors":{"authors":[{"text":"Wolf, K.","contributorId":16344,"corporation":false,"usgs":true,"family":"Wolf","given":"K.","email":"","affiliations":[],"preferred":false,"id":355510,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70039034,"text":"70039034 - 1981 - United States Geological Survey Yearbook, fiscal year 1980","interactions":[],"lastModifiedDate":"2017-03-08T16:36:34","indexId":"70039034","displayToPublicDate":"2012-01-01T11:52:39","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":392,"text":"Yearbook","active":false,"publicationSubtype":{"id":6}},"title":"United States Geological Survey Yearbook, fiscal year 1980","docAbstract":"It is not very often that a single event is so overwhelming that it changes public perceptions of natural hazards for generations. Perhaps for the U.S. Geological Survey, the explosive volcanic activity of Mount St. Helens began such a change. After 101 years of careful science of the Earth's past and meticulous observations and assessments of the present, predictive earth science was in full public view. However vague and faint the glimpse of the future made possible by earth science, it was enough. Warnings were issued, thousands of lives were saved, and the age of real-time geology began. The Survey's basic mission has not changed, but the power of our analytical tools has increased by several orders of magnitude. The Survey's efforts to understand Earth processes and hydrologic principles continued with the collection, during fiscal year 1980, of valuable new data on the geologic origin and framework, seismicity, and mineral and energy resources of the United States. The Survey is also responsible for classification of the leasable minerals on Federal lands and the regulation of mineral exploration and development activities on Federal and Indian lands. As the principal earth science fact-gathering agency, the Survey provides information for sound decisionmaking by government and private industry. Industry uses the Survey's information in exploring for energy and minerals and improving their efforts to make development of energy and minerals compatible with environmental protection standards. Government uses the Survey's information in conducting leasing operations on public lands, in regulating the safe design and siting of nuclear plants, and in establishing guidelines for determining and locating areas that are subject to geologic hazards such as landslides, earthquakes, and volcanic eruptions. The Yearbook reports a broad range of the Survey's accomplishments during the past fiscal year and provides an overview of future directions. Many of the topics covered will continue to be important natural resource and earth science issues of the 1980's.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039034","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, United States Geological Survey Yearbook, fiscal year 1980: Yearbook, vi, 137 p., https://doi.org/10.3133/70039034.","productDescription":"vi, 137 p.","costCenters":[],"links":[{"id":261273,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039034/report.pdf","text":"Report","size":"49.27 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":261274,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039034/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbc91e4b08c986b328cf5","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535203,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70006721,"text":"70006721 - 1981 - Residues of isobornyl thiocyanoacetate (Thanite) and a metabolite in fish and treated ponds","interactions":[],"lastModifiedDate":"2012-07-07T01:01:38","indexId":"70006721","displayToPublicDate":"2012-01-01T10:27:53","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2149,"text":"Journal of Agricultural and Food Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Residues of isobornyl thiocyanoacetate (Thanite) and a metabolite in fish and treated ponds","docAbstract":"Isobornyl thiocyanoacetate (Thanite) is an insecticide that induces a surfacing response in fish and therefore has been considered to have potential as a fish collection agent. Analyses for residues of Thanite in carp (Cyprinus carpio) and largemouth bass (Micropterus salmoides) exposed to chemical yielded only a trace of the parent compound. A metabolite, isobornyl a-(methylthio)acetate, was isolated and indentified by GC-MS,and a reference standard for the metabolite was synthesized. Residues of the metabolite were present in largemouth bass muscle tissue within 1 h after exposure to Thanite. The metabolite was also observed in the muscle, blood plasma, and bile of carp. Residues of the metaboliteare rapidly elimanated after the fish are transferred to Thanite-free water. Residues of Thanite in water, algae, and from soil from ponds treated with Thanite declined to undetectable levels within 28 days after treatment.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Agricultural and Food Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"ACS Publications","publisherLocation":"Washington, D.C.","doi":"10.1021/jf00105a049","collaboration":"None","usgsCitation":"Allen, J.L., Sills, J., Dawson, V.K., and Amel, R., 1981, Residues of isobornyl thiocyanoacetate (Thanite) and a metabolite in fish and treated ponds: Journal of Agricultural and Food Chemistry, v. 29, no. 3, p. 634-636, https://doi.org/10.1021/jf00105a049.","productDescription":"3 p.","startPage":"634","endPage":"636","numberOfPages":"3","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":258236,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":258224,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/jf00105a049","linkFileType":{"id":5,"text":"html"}}],"volume":"29","issue":"3","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505aa9a9e4b0c8380cd85eea","contributors":{"authors":[{"text":"Allen, J. L.","contributorId":49295,"corporation":false,"usgs":true,"family":"Allen","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":355091,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sills, J.B.","contributorId":55380,"corporation":false,"usgs":true,"family":"Sills","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":355092,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dawson, V. K.","contributorId":48900,"corporation":false,"usgs":true,"family":"Dawson","given":"V.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":355090,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Amel, R.T.","contributorId":46818,"corporation":false,"usgs":true,"family":"Amel","given":"R.T.","email":"","affiliations":[],"preferred":false,"id":355089,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70006967,"text":"70006967 - 1981 - Plasma corticosteroid dynamics in channel catfish, Ictalurus punctatus (Rafinesque), during and after oxygen depletion","interactions":[],"lastModifiedDate":"2012-07-13T01:01:54","indexId":"70006967","displayToPublicDate":"2012-01-01T09:23:00","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2285,"text":"Journal of Fish Biology","active":true,"publicationSubtype":{"id":10}},"title":"Plasma corticosteroid dynamics in channel catfish, Ictalurus punctatus (Rafinesque), during and after oxygen depletion","docAbstract":"Plasma corticosteroid concentrations in channel catfish, Ictalurus punctatus, (normally 1.0 ± 0.3 μg/100 ml) increased significantly (to 5.9 ± 1.2μg/100 ml) in response to acute oxygen depletion and then returned to control levels within 30 min after the dissolved oxygen concentration was increased; however, a secondary increase in plasma corticosteroid levels was observed 6 h after exposure. Corticosteroid levels also increased in fish exposed to dissolved oxygen concentration of <0.2 mg/1 for three days. Methylene blue was not effective in preventing interrenal response to low dissolved oxygen. No diurnal plasma corticosteroid rhythm was observed in fish exposed to diurnal chemical rhythms of culture ponds.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Fish Biology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wiley","publisherLocation":"Hoboken, NJ","doi":"10.1111/j.1095-8649.1981.tb03793.x","collaboration":"None","usgsCitation":"Tomasso J.R., D.K., and Parker, N., 1981, Plasma corticosteroid dynamics in channel catfish, Ictalurus punctatus (Rafinesque), during and after oxygen depletion: Journal of Fish Biology, v. 18, no. 5, p. 519-526, https://doi.org/10.1111/j.1095-8649.1981.tb03793.x.","productDescription":"8 p.","startPage":"519","endPage":"526","numberOfPages":"8","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":258436,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":258427,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1095-8649.1981.tb03793.x","linkFileType":{"id":5,"text":"html"}}],"volume":"18","issue":"5","noUsgsAuthors":false,"publicationDate":"2006-01-24","publicationStatus":"PW","scienceBaseUri":"505a7c10e4b0c8380cd79797","contributors":{"authors":[{"text":"Tomasso J.R., Davis K. B. K. B.","contributorId":66113,"corporation":false,"usgs":true,"family":"Tomasso J.R.","given":"Davis","suffix":"K. B.","email":"","middleInitial":"K. B.","affiliations":[],"preferred":false,"id":355564,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parker, N. C.","contributorId":101209,"corporation":false,"usgs":true,"family":"Parker","given":"N. C.","affiliations":[],"preferred":false,"id":355565,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70039567,"text":"70039567 - 1981 - Studying the Earth from space","interactions":[],"lastModifiedDate":"2012-08-13T17:03:59","indexId":"70039567","displayToPublicDate":"2012-01-01T00:12:25","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"Studying the Earth from space","docAbstract":"Space age technology contains a key to increased knowledge about the Earth's resources; this key is remote sensing detecting the nature or condition of something without actually touching it. An early and still most useful form of remote sensing is photography which records the\nscene, as man sees it, on film sensitive to that part of the electromagnetic spectrum called visible energy. Electromagnetic energy travels in waves of various lengths; most are invisible to the human eye. Wavelengths progressively longer than those that the eye can see are infrared and microwave. Wavelengths progressively shorter than the eye can see are ultraviolet, X-rays, and gamma rays.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039567","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Studying the Earth from space: General Information Product, 24 p., https://doi.org/10.3133/70039567.","productDescription":"24 p.","numberOfPages":"28","costCenters":[],"links":[{"id":259582,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"otherGeospatial":"Earth","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9ceae4b08c986b31d518","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535367,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70012020,"text":"70012020 - 1981 - Earth fissures and localized differential subsidence","interactions":[{"subject":{"id":70012020,"text":"70012020 - 1981 - Earth fissures and localized differential subsidence","indexId":"70012020","publicationYear":"1981","noYear":false,"title":"Earth fissures and localized differential subsidence"},"predicate":"SUPERSEDED_BY","object":{"id":9554,"text":"ofr79951 - 1979 - Earth fissures and localized differential subsidence","indexId":"ofr79951","publicationYear":"1979","noYear":false,"title":"Earth fissures and localized differential subsidence"},"id":1}],"supersededBy":{"id":9554,"text":"ofr79951 - 1979 - Earth fissures and localized differential subsidence","indexId":"ofr79951","publicationYear":"1979","noYear":false,"title":"Earth fissures and localized differential subsidence"},"lastModifiedDate":"2019-07-17T16:10:35","indexId":"70012020","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1981","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":"Earth fissures and localized differential subsidence","docAbstract":"Long linear tension cracks associated with declining groundwater levels at four sites in subsiding areas in south-central Arizona, Fremont Valley, California, and Las Vegas Valley, Nevada, occur near points of maximum convex-upward curvature in subsidence profiles oriented perpendicular to the cracks. Profiles are based on repeated precise vertical control surveys of lines of closely spaced bench marks. Association of these fissures with zones of localized differential subsidence indicates that linear earth fissures are caused by horizontal tensile strains probably resulting from localized differential compaction. Horizontal tensile strains across the fissures at the point of maximum convex-upward curvature, ranging from approximately 100 to 700 microstrains (0.01 to 0.07% per year), were indicated based on measurements with a tape or electronic distance meter.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR017i001p00223","usgsCitation":"Holzer, T.L., and Pampeyan, E.H., 1981, Earth fissures and localized differential subsidence: Water Resources Research, v. 17, no. 1, p. 223-227, https://doi.org/10.1029/WR017i001p00223.","productDescription":"5 p.","startPage":"223","endPage":"227","additionalOnlineFiles":"N","costCenters":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":222334,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona, California, Idaho, Nevada, Utah","otherGeospatial":"Fremont Valley, Las Vegas Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.8,31.3 ], [ -124.8,43.5 ], [ -109.0,43.5 ], [ -109.0,31.3 ], [ -124.8,31.3 ] ] ] } } ] }","volume":"17","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"505a0499e4b0c8380cd50a9a","contributors":{"authors":[{"text":"Holzer, Thomas L. tholzer@usgs.gov","contributorId":2829,"corporation":false,"usgs":true,"family":"Holzer","given":"Thomas","email":"tholzer@usgs.gov","middleInitial":"L.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":362535,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pampeyan, Earl H.","contributorId":54698,"corporation":false,"usgs":true,"family":"Pampeyan","given":"Earl","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":362536,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70046351,"text":"70046351 - 1981 - Improved methods for national water assessment, water resources contract: WR15249270","interactions":[],"lastModifiedDate":"2013-07-08T12:50:12","indexId":"70046351","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Improved methods for national water assessment, water resources contract: WR15249270","docAbstract":"The purpose of our research is to develop methods to make National Water Assessment more useful in estimating water availability for economic growth and more helpful in determining the effect of water resource development upon the environmental quality of related land resources. There are serious questions pertaining to the 1975 Water Assessment and these amplify the significance of decisions made as to the planning and scheduling of the next assessment.","language":"English","publisher":"Harvard Water Resources Group","doi":"10.3133/70046351","usgsCitation":"Thomas, H., 1981, Improved methods for national water assessment, water resources contract: WR15249270, 59 p., https://doi.org/10.3133/70046351.","productDescription":"59 p.","costCenters":[],"links":[{"id":273507,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70046351/report-thumb.jpg"},{"id":274618,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70046351/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b6f568e4b0097a7158e5c6","contributors":{"authors":[{"text":"Thomas, Harold A. Jr.","contributorId":82206,"corporation":false,"usgs":true,"family":"Thomas","given":"Harold A.","suffix":"Jr.","affiliations":[],"preferred":false,"id":479538,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70006392,"text":"70006392 - 1981 - \"Duck stamp\" dollars reserve native prairie tracts","interactions":[],"lastModifiedDate":"2017-11-16T10:19:25","indexId":"70006392","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3230,"text":"Rangelands","active":true,"publicationSubtype":{"id":10}},"title":"\"Duck stamp\" dollars reserve native prairie tracts","docAbstract":"Ducks and wetlands are inseparable in the prairies. Hunters know this, bird watchers know this, wildlife managers know this, and most importantly people who manage the croplands and rangelands know this. The 1,746 tracts of native prairie within these upland-wetland complexes known as Waterfowl Production Areas are not the only lands purchased with \"duck stamp\" dollars. Considerable acreages have also been purchased in central and southern parts of the United States to provide staging, resting, and wintering areas for waterfowl. Since 1934, when \"duck stamps\" were first sold, nearly 2.5 million acres of waterfowl habitats have been acquired or taken under easement within the United States with revenue from these sales. By purchasing \"duck stamps\", more than 2.2 million people provide over $16.5 million in annual revenue. It is certainly gratifying to know that some of the remaining native prairie remnants in the Northern Great Plains are being reserved for the future with \"duck stamp\" dollars.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Rangelands","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"University of Arizona","publisherLocation":"Tucson, AZ","usgsCitation":"Higgins, K., 1981, \"Duck stamp\" dollars reserve native prairie tracts: Rangelands, v. 3, no. 5, p. 190-191.","productDescription":"2 p.","startPage":"190","endPage":"191","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":263631,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":263630,"type":{"id":11,"text":"Document"},"url":"https://journals.uair.arizona.edu/index.php/rangelands/article/view/11685/10958"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 172.5,18.9 ], [ 172.5,71.4 ], [ -66.9,71.4 ], [ -66.9,18.9 ], [ 172.5,18.9 ] ] ] } } ] }","volume":"3","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50bd1353e4b069d93eefc4bb","contributors":{"authors":[{"text":"Higgins, K.F.","contributorId":55767,"corporation":false,"usgs":true,"family":"Higgins","given":"K.F.","email":"","affiliations":[],"preferred":false,"id":354434,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5221724,"text":"5221724 - 1981 - Report of the Conservation Committee--1980. 1980, The Year of the Coast: Birds","interactions":[],"lastModifiedDate":"2012-02-02T00:14:52","indexId":"5221724","displayToPublicDate":"2010-06-16T12:19:34","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3783,"text":"The Wilson Bulletin","printIssn":"0043-5643","active":true,"publicationSubtype":{"id":10}},"title":"Report of the Conservation Committee--1980. 1980, The Year of the Coast: Birds","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wilson Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Bolen, E., Chapman, B., Wilson, M., Weller, M., Jahn, L., Robbins, C., and Samson, F.B., 1981, Report of the Conservation Committee--1980. 1980, The Year of the Coast: Birds: The Wilson Bulletin, v. 93, no. 3, p. 438-456.","productDescription":"438-456","startPage":"438","endPage":"456","numberOfPages":"19","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":199165,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18526,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://elibrary.unm.edu/sora/Wilson/v093n03/p0438-p0456.pdf","linkFileType":{"id":1,"text":"pdf"}}],"volume":"93","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad1e4b07f02db681140","contributors":{"authors":[{"text":"Bolen, E.G.","contributorId":84036,"corporation":false,"usgs":true,"family":"Bolen","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":334532,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chapman, B.R.","contributorId":56762,"corporation":false,"usgs":true,"family":"Chapman","given":"B.R.","email":"","affiliations":[],"preferred":false,"id":334530,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilson, M.M.","contributorId":12149,"corporation":false,"usgs":true,"family":"Wilson","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":334527,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Weller, M.W.","contributorId":54562,"corporation":false,"usgs":true,"family":"Weller","given":"M.W.","email":"","affiliations":[],"preferred":false,"id":334529,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Jahn, L.R.","contributorId":100101,"corporation":false,"usgs":true,"family":"Jahn","given":"L.R.","email":"","affiliations":[],"preferred":false,"id":334533,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Robbins, C.S.","contributorId":53907,"corporation":false,"usgs":true,"family":"Robbins","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":334528,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Samson, F. B.","contributorId":77880,"corporation":false,"usgs":true,"family":"Samson","given":"F.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":334531,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ]}