No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha564","usgsCitation":"Prescott, G., 1977, Ground-water favorability and surficial geology of the Windham-Freeport area, Maine: U.S. Geological Survey Hydrologic Atlas 564, 1 Plate: 28.00 × 40.25 inches, https://doi.org/10.3133/ha564.","productDescription":"1 Plate: 28.00 × 40.25 inches","costCenters":[],"links":[{"id":398650,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15955.htm"},{"id":190294,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":91823,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/564/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Maine","otherGeospatial":"Windham-Freeport area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -70.5,\n 43.6420\n ],\n [\n -70,\n 43.6420\n ],\n [\n -70,\n 43.8680\n ],\n [\n -70.5,\n 43.8680\n ],\n [\n -70.5,\n 43.6420\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ce37","contributors":{"authors":[{"text":"Prescott, Glenn C.","contributorId":38126,"corporation":false,"usgs":true,"family":"Prescott","given":"Glenn C.","affiliations":[],"preferred":false,"id":277615,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70162499,"text":"70162499 - 1977 - Earthquake prediction: A perspective for a national program","interactions":[],"lastModifiedDate":"2016-11-30T14:33:21","indexId":"70162499","displayToPublicDate":"1977-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Earthquake prediction: A perspective for a national program","docAbstract":"Earthquake predictions is a rapidly advancing field of research and development. And now is the time to begin planning how we should use the results of this research.
","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Ward, P., 1977, Earthquake prediction: A perspective for a national program: Earthquake Information Bulletin (USGS), v. 9, no. 6, p. 10-13.","productDescription":"4 p.","startPage":"10","endPage":"13","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":314823,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56a75551e4b0b28f1184d817","contributors":{"authors":[{"text":"Ward, P.L.","contributorId":31422,"corporation":false,"usgs":true,"family":"Ward","given":"P.L.","email":"","affiliations":[],"preferred":false,"id":589694,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70162254,"text":"70162254 - 1977 - Relative yield of two transferrin phenotypes in coho salmon","interactions":[],"lastModifiedDate":"2016-01-19T15:27:00","indexId":"70162254","displayToPublicDate":"1977-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Relative yield of two transferrin phenotypes in coho salmon","docAbstract":"Experimental groups of coho salmon (Oncorhynchus kisutch) of transferring types AA and AC were compared to determine relative growth and survival before release, yields from the fishery, and returns of fish to the hatchery as 2- and 3-yr-olds. In the hatchery, growth was faster and survival higher in the AA than in the AC types. However, yields of AA and AC types were equal, although the yield of AC types as 3-yr-olds was greater than that of AA types because more of the AA males matured in 2 years. We concluded that it would be futile to attempt to increase the yield of coho salmon by maximizing the frequency of biochemical phenotypes that display only a temporary advantage over other types.
","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1977)39[175:RYOTTP]2.0.CO;2","usgsCitation":"McIntyre, J.D., and Johnson, A., 1977, Relative yield of two transferrin phenotypes in coho salmon: Progressive Fish-Culturist, v. 39, no. 4, p. 175-177, https://doi.org/10.1577/1548-8659(1977)39[175:RYOTTP]2.0.CO;2.","productDescription":"3 p.","startPage":"175","endPage":"177","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314492,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569f6c53e4b0961cf27fd1c5","contributors":{"authors":[{"text":"McIntyre, John D.","contributorId":152343,"corporation":false,"usgs":false,"family":"McIntyre","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":588989,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, A. Kenneth","contributorId":152344,"corporation":false,"usgs":false,"family":"Johnson","given":"A. Kenneth","affiliations":[],"preferred":false,"id":588990,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":30666,"text":"ofr77649 - 1977 - Mineral resources of the Tracy Arm-Fords Terror Wilderness Study Area and vicinity, Alaska","interactions":[{"subject":{"id":30666,"text":"ofr77649 - 1977 - Mineral resources of the Tracy Arm-Fords Terror Wilderness Study Area and vicinity, Alaska","indexId":"ofr77649","publicationYear":"1977","noYear":false,"title":"Mineral resources of the Tracy Arm-Fords Terror Wilderness Study Area and vicinity, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":33496,"text":"b1525 - 1984 - Mineral resources of the Tracy Arm-Fords Terror Wilderness Study Area and vicinity, Alaska","indexId":"b1525","publicationYear":"1984","noYear":false,"title":"Mineral resources of the Tracy Arm-Fords Terror Wilderness Study Area and vicinity, Alaska"},"id":1}],"supersededBy":{"id":33496,"text":"b1525 - 1984 - Mineral resources of the Tracy Arm-Fords Terror Wilderness Study Area and vicinity, Alaska","indexId":"b1525","publicationYear":"1984","noYear":false,"title":"Mineral resources of the Tracy Arm-Fords Terror Wilderness Study Area and vicinity, Alaska"},"lastModifiedDate":"2024-04-29T21:02:20.040146","indexId":"ofr77649","displayToPublicDate":"1977-01-01T00:00:00","publicationYear":"1977","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":"77-649","title":"Mineral resources of the Tracy Arm-Fords Terror Wilderness Study Area and vicinity, Alaska","docAbstract":"The Wilderness Study Area consists of about 322,300 hectares (1,250 square miles or 796,400 acres) on the southwest side of the Coast Range in southeastern Alaska about 72 km (45 miles) southeast of Juneau, Alaska (fig. 1). An additional 142,800 hectares (550 square miles or 352,900 acres) lying in part between the study area and the International Boundary and in part contiguous to the southwest of the study area were studied because of their importance to the evaluation of the study area itself. Unless otherwise specified, the term Study Area as used in this report includes both the formally designated study area and these contiguous areas. The general area is one of spectacular scenery, with fiords, forests, glacier-covered peaks to 2,470 m (8,095 feet) high, tidewater glaciers, icebergs, and some broad river valleys. No roads or maintained trails or permanent residents are present, and access is only by specially arranged water or air transport. Present human use of the area is related to recreation or mineral-resource exploration.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77649","usgsCitation":"Brew, D.A., Grybeck, D., Johnson, B.R., Jachens, R.C., Nutt, C., Barnes, D., Kimball, A., Still, J., and Rataj, J., 1977, Mineral resources of the Tracy Arm-Fords Terror Wilderness Study Area and vicinity, Alaska: U.S. Geological Survey Open-File Report 77-649, Report: xviii, 282 p.; 4 Plates: 35.54 x 48.45 inches or smaller, https://doi.org/10.3133/ofr77649.","productDescription":"Report: xviii, 282 p.; 4 Plates: 35.54 x 48.45 inches or smaller","costCenters":[],"links":[{"id":428204,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0649/plate-1-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428203,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0649/plate-1-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428202,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0649/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428201,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0649/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428200,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0649/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":163086,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0649/report-thumb.jpg"},{"id":414252,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14491.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","otherGeospatial":"Tracy Arm-Fords Terror Wilderness Study Area and vicinity","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -132.583,\n 58.5\n ],\n [\n -134,\n 58.5\n ],\n [\n -134,\n 57.417\n ],\n [\n -132.583,\n 57.417\n ],\n [\n -132.583,\n 58.5\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a044","contributors":{"authors":[{"text":"Brew, David A. dbrew@usgs.gov","contributorId":3244,"corporation":false,"usgs":true,"family":"Brew","given":"David","email":"dbrew@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":203646,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grybeck, Donald","contributorId":8066,"corporation":false,"usgs":true,"family":"Grybeck","given":"Donald","affiliations":[],"preferred":false,"id":203647,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, Bruce R.","contributorId":100009,"corporation":false,"usgs":true,"family":"Johnson","given":"Bruce","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":203654,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jachens, Robert C.","contributorId":52881,"corporation":false,"usgs":true,"family":"Jachens","given":"Robert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":203652,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Nutt, C.J.","contributorId":52577,"corporation":false,"usgs":true,"family":"Nutt","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":203651,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Barnes, D.F.","contributorId":48960,"corporation":false,"usgs":true,"family":"Barnes","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":203650,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kimball, A.L.","contributorId":68301,"corporation":false,"usgs":true,"family":"Kimball","given":"A.L.","email":"","affiliations":[],"preferred":false,"id":203653,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Still, J.C.","contributorId":32156,"corporation":false,"usgs":true,"family":"Still","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":203649,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Rataj, J.L.","contributorId":20600,"corporation":false,"usgs":true,"family":"Rataj","given":"J.L.","affiliations":[],"preferred":false,"id":203648,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":70162256,"text":"70162256 - 1977 - Immunization of pacific salmon: comparison of intraperitoneal injection and hyperosmotic infiltration of Vibrio anguillarum and Aeromonas salmonicida bacterins","interactions":[],"lastModifiedDate":"2016-01-19T15:37:39","indexId":"70162256","displayToPublicDate":"1977-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Immunization of pacific salmon: comparison of intraperitoneal injection and hyperosmotic infiltration of Vibrio anguillarum and Aeromonas salmonicida bacterins","docAbstract":"Two methods of immunizing fish, intraperitoneal (i.p.) injection and hyperosmotic infiltration, were compared for control of vibriosis and furunculosis in pen-reared coho salmon (Oncorhynchus kisutch) and chinook salmon (O. tshawytscha). Both methods provided significant protection against vibriosis under field test conditions. In coho salmon, hyperosmotic infiltration provided the best protection and fastest rise in antibody titer of seven treatments tested. In chinook salmon, hyperosmotic infiltration of Vibrio anguillarum and Aeromonas salmonicida vaccines resulted in 83.3% survival in comparison with 28.7% survival in controls. Both i.p. injection and hyperosmotic infiltration of V. anguillarum and A. salmonicida bacterins resulted in production of serum antibodies specific for each respective pathogen. Vaccination with bivalent V. anguillarum–A.salmonicida vaccines produced antibodies to both pathogens, and provided protection against vibriosis. Growth rates of vaccinated coho salmon were not significantly different from controls.
","language":"English","publisher":"NRC Research Press","doi":"10.1139/f77-030","usgsCitation":"Antipa, R., and Amend, D.F., 1977, Immunization of pacific salmon: comparison of intraperitoneal injection and hyperosmotic infiltration of Vibrio anguillarum and Aeromonas salmonicida bacterins: Journal of the Fisheries Research Board of Canada, v. 34, no. 2, p. 203-208, https://doi.org/10.1139/f77-030.","productDescription":"6 p.","startPage":"203","endPage":"208","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314494,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569f6c44e4b0961cf27fd1a4","contributors":{"authors":[{"text":"Antipa, Ross","contributorId":152346,"corporation":false,"usgs":false,"family":"Antipa","given":"Ross","email":"","affiliations":[],"preferred":false,"id":588993,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Amend, Donald F.","contributorId":106543,"corporation":false,"usgs":true,"family":"Amend","given":"Donald","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":588994,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26408,"text":"wri7783 - 1977 - A technique for determining depths for T-year discharges in rigid-boundary channels","interactions":[],"lastModifiedDate":"2023-07-14T15:20:50.331973","indexId":"wri7783","displayToPublicDate":"1977-01-01T00:00:00","publicationYear":"1977","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":"77-83","title":"A technique for determining depths for T-year discharges in rigid-boundary channels","docAbstract":"A simplified technique is presented for determining depths for 1-year discharges (the discharge that will occur, on an average, once in T-years-10 years, 50 years, 100 years) for natural channels (channels not significantly affected by manmade structures) having channel-control conditions and rigid boundaries (channels having a low probability of change that would significantly affect the hydraulic characteristics of a T-year discharge). Channel-control conditions usually exist during T-year discharges in natural rigid-boundary channels and, therefore, the simplified technique probably would be applicable for flood-inundation studies for many natural rigid-boundary channels. The technique requires that the T-year discharge for a reach of interest be known or readily available; also, a channel-shape factor, a width at a reference altitude, a channel-bottom slope (or a water-surface slope), and the Manning's roughness factor, n, must be estimated or determined at representative sections having channel-control conditions. The standard error of estimate for depths determined according to the simplified technique is not known; however, it is probably 25-30 percent. In comparison, the standard error of estimate for the depths determined according to the step-backwater procedure and to guidelines and specifications for flood-insurance studies of the Federal Insurance Administration is about 23 percent.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7783","usgsCitation":"Burkham, D., 1977, A technique for determining depths for T-year discharges in rigid-boundary channels: U.S. Geological Survey Water-Resources Investigations Report 77-83, iv, 38 p., https://doi.org/10.3133/wri7783.","productDescription":"iv, 38 p.","costCenters":[],"links":[{"id":358900,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0083/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158315,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0083/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a5c2b","contributors":{"authors":[{"text":"Burkham, D. E.","contributorId":97073,"corporation":false,"usgs":true,"family":"Burkham","given":"D. E.","affiliations":[],"preferred":false,"id":196336,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":59594,"text":"mf868C - 1977 - Map showing lead-zinc deposits of South America","interactions":[],"lastModifiedDate":"2023-12-04T20:26:26.501064","indexId":"mf868C","displayToPublicDate":"1977-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"868","chapter":"C","title":"Map showing lead-zinc deposits of South America","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf868C","usgsCitation":"1977, Map showing lead-zinc deposits of South America: U.S. Geological Survey Miscellaneous Field Studies Map 868, 1 Plate: 21.47 x 26.31 inches, https://doi.org/10.3133/mf868C.","productDescription":"1 Plate: 21.47 x 26.31 inches","costCenters":[],"links":[{"id":364037,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0868-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":183152,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0868-C/report-thumb.jpg"}],"scale":"15000000","otherGeospatial":"South America","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90,-54 ], [ -90,12 ], [ -30,12 ], [ -30,-54 ], [ -90,-54 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a49d3","contributors":{"compilers":[{"text":"Goudarzi, Gus H.","contributorId":44923,"corporation":false,"usgs":true,"family":"Goudarzi","given":"Gus","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":889499,"contributorType":{"id":3,"text":"Compilers"},"rank":1}]}} ,{"id":2002200,"text":"2002200 - 1977 - Feral burros of San Miguel Island","interactions":[],"lastModifiedDate":"2012-02-02T00:14:57","indexId":"2002200","displayToPublicDate":"1977-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":16,"text":"Contribution","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"CPSU/UNLV 15","title":"Feral burros of San Miguel Island","docAbstract":"No abstract available at this time","language":"English","publisher":"National Park Service","usgsCitation":"Douglas, C.L., 1977, Feral burros of San Miguel Island: Contribution CPSU/UNLV 15, 5 p.","productDescription":"5 p.","startPage":"0","endPage":"5","numberOfPages":"5","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":199124,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fde4b07f02db5f5d37","contributors":{"authors":[{"text":"Douglas, C. L.","contributorId":64586,"corporation":false,"usgs":true,"family":"Douglas","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":326154,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2002199,"text":"2002199 - 1977 - Fire management in the Yosemite mixed conifer ecosystem","interactions":[],"lastModifiedDate":"2012-02-02T00:14:57","indexId":"2002199","displayToPublicDate":"1977-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":32,"text":"General Technical Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"WO-3","title":"Fire management in the Yosemite mixed conifer ecosystem","docAbstract":"No abstract available at this time","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Proc. Symp. Environ. Consequences of Fire and Fuel Manage. in Mediterranean Ecosystems.","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"U.S. Forest Service","usgsCitation":"van Wagtendonk, J., 1977, Fire management in the Yosemite mixed conifer ecosystem: General Technical Report WO-3, p. 459-463.","productDescription":"p. 459-463","startPage":"459","endPage":"463","numberOfPages":"5","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":199272,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f43f5","contributors":{"authors":[{"text":"van Wagtendonk, J. W.","contributorId":85111,"corporation":false,"usgs":true,"family":"van Wagtendonk","given":"J. 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For two-phase systems it is sufficient to match phase boundary loops between adjacent sections. 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The difficulty in obtaining such information has been considered a serious limitation of discrete models, but improved borehole techniques can enable one to obtain the necessary data, at least in shallow systems. The possibility of extending these methods to deeper fracture systems needs more investigation. Such data must be considered when deciding whether to use a continuum or discrete model to represent the interaction of rock and fluid forces in a fractured rock system, especially with regard to the problem of induced seismicity. When one is attempting to alter the pressure distribution in a fault zone by injection or withdrawal of fluids, the extent to which this can be achieved will be controlled in large measure by the behavior of the fractures that communicate with the borehole. Since this is essentially a point phenomenon, i.e., the changes will propagate from a relatively small region around the borehole, the use of a discrete model would appear to be preferable.
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