{"pageNumber":"3796","pageRowStart":"94875","pageSize":"25","recordCount":185258,"records":[{"id":70018565,"text":"70018565 - 1996 - Growth of the Tongariro volcanic complex: New evidence from K-Ar age determinations","interactions":[],"lastModifiedDate":"2019-06-06T13:16:54","indexId":"70018565","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2869,"text":"New Zealand Journal of Geology and Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Growth of the Tongariro volcanic complex: New evidence from K-Ar age determinations","docAbstract":"New K-Ar age determinations indicate that the exposed portion of the Tongariro volcanic complex has grown steadily since at least 275 ka, with intervals of vigorous cone growth at 210-200.130-70. and 25 ka to the present day.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"New Zealand Journal of Geology and Geophysics","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor and Francis","doi":"10.1080/00288306.1996.9514701","issn":"00288306","usgsCitation":"Hobden, B., Houghton, B.F., Lanphere, M.A., and Nairn, I., 1996, Growth of the Tongariro volcanic complex: New evidence from K-Ar age determinations: New Zealand Journal of Geology and Geophysics, v. 39, no. 1, p. 151-154, https://doi.org/10.1080/00288306.1996.9514701.","productDescription":"4 p.","startPage":"151","endPage":"154","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":479130,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/00288306.1996.9514701","text":"Publisher Index Page"},{"id":227568,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268059,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1080/00288306.1996.9514701"}],"volume":"39","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-03-23","publicationStatus":"PW","scienceBaseUri":"505a2dfbe4b0c8380cd5c1d6","contributors":{"authors":[{"text":"Hobden, B.J.","contributorId":67677,"corporation":false,"usgs":true,"family":"Hobden","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":380056,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Houghton, Bruce F. 0000-0002-7532-9770","orcid":"https://orcid.org/0000-0002-7532-9770","contributorId":140077,"corporation":false,"usgs":false,"family":"Houghton","given":"Bruce","email":"","middleInitial":"F.","affiliations":[{"id":6977,"text":"University of Hawai`i at Hilo","active":true,"usgs":false},{"id":13351,"text":"University of Hawaii Cooperative Studies Unit","active":true,"usgs":false}],"preferred":false,"id":380055,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lanphere, M. A.","contributorId":35298,"corporation":false,"usgs":true,"family":"Lanphere","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":380054,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nairn, I.A.","contributorId":92812,"corporation":false,"usgs":true,"family":"Nairn","given":"I.A.","email":"","affiliations":[],"preferred":false,"id":380057,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70018520,"text":"70018520 - 1996 - Galileo photometry of asteroid 243 Ida","interactions":[],"lastModifiedDate":"2012-03-12T17:19:24","indexId":"70018520","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Galileo photometry of asteroid 243 Ida","docAbstract":"Galileo imaging observations over phase angles 19.5?? to 109.8?? are combined with near-opposition Earth-based data to derive the photometric properties of Ida. To first order these properties are uniform over the surface and well modeled at ?? = 0.55 ??m by Hapke parameters ????0 = 0.22, h = 0.020, B0 = 1.5, g = -0.33, and ?? = 18?? with corresponding geometric albedo p = 0.21??0.030.01 and Bond albedo AB = 0.081??0.0170.008. Ida's photometric properties are more similar to those of \"average S-asteroids\" (P. Helfenstein and J. Veverka 1989, Asteroids II, Univ. of Arizona Press, Tucson) than are those of 951 Gaspra. Two primary color units are identified on Ida: Terrain A exhibits a spectrum with relatively shallower 1-??m absorption and a relatively steeper red spectral slope than average Ida, while Terrain B has a deeper 1-??m absorption and a less steep red slope. The average photometric properties of Ida and Terrain A are similar while those of Terrain B differ mostly in having a slightly higher value of ????0 (0.22 versus 0.21), suggesting that Terrain B consists of slightly brighter, more transparent regolith particles. Galileo observations of Ida's satellite Dactyl over phase angles 19.5?? to 47.6?? suggest photometric characteristics similar to those of Ida, the major difference being Dactyl's slightly lower albedo (0.20 compared to 0.21). ?? 1990 Academic Press, Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Icarus","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1006/icar.1996.0036","issn":"00191035","usgsCitation":"Helfenstein, P., Veverka, J., Thomas, P., Simonelli, D., Klaasen, K., Johnson, T.V., Fanale, F., Granahan, J., McEwen, A.S., Belton, M., and Chapman, C., 1996, Galileo photometry of asteroid 243 Ida: Icarus, v. 120, no. 1, p. 48-65, https://doi.org/10.1006/icar.1996.0036.","startPage":"48","endPage":"65","numberOfPages":"18","costCenters":[],"links":[{"id":479131,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1006/icar.1996.0036","text":"Publisher Index Page"},{"id":227522,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205932,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1006/icar.1996.0036"}],"volume":"120","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a14ade4b0c8380cd54af1","contributors":{"authors":[{"text":"Helfenstein, P.","contributorId":69306,"corporation":false,"usgs":true,"family":"Helfenstein","given":"P.","email":"","affiliations":[],"preferred":false,"id":379920,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Veverka, J.","contributorId":71689,"corporation":false,"usgs":true,"family":"Veverka","given":"J.","email":"","affiliations":[],"preferred":false,"id":379921,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, P.C.","contributorId":32690,"corporation":false,"usgs":true,"family":"Thomas","given":"P.C.","affiliations":[],"preferred":false,"id":379918,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Simonelli, D.P.","contributorId":42373,"corporation":false,"usgs":true,"family":"Simonelli","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":379919,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Klaasen, K.","contributorId":101395,"corporation":false,"usgs":true,"family":"Klaasen","given":"K.","email":"","affiliations":[],"preferred":false,"id":379924,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Johnson, T. 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,{"id":70018462,"text":"70018462 - 1996 - Mass wasting triggered by the 5 March 1987 Ecuador earthquakes","interactions":[],"lastModifiedDate":"2012-03-12T17:19:24","indexId":"70018462","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1517,"text":"Engineering Geology","active":true,"publicationSubtype":{"id":10}},"title":"Mass wasting triggered by the 5 March 1987 Ecuador earthquakes","docAbstract":"On 5 March 1987, two earthquakes (Ms=6.1 and Ms=6.9) occurred about 25 km north of Reventador Volcano, along the eastern slopes of the Andes Mountains in northeastern Ecuador. Although the shaking damaged structures in towns and villages near the epicentral area, the economic and social losses directly due to earthquake shaking were small compared to the effects of catastrophic earthquake-triggered mass wasting and flooding. About 600 mm of rain fell in the region in the month preceding the earthquakes; thus, the surficial soils had high moisture contents. Slope failures commonly started as thin slides, which rapidly turned into fluid debris avalanches and debris flows. The surficial soils and thick vegetation covering them flowed down the slopes into minor tributaries and then were carried into major rivers. Rock and earth slides, debris avalanches, debris and mud flows, and resulting floods destroyed about 40 km of the Trans-Ecuadorian oil pipeline and the only highway from Quito to Ecuador's northeastern rain forests and oil fields. Estimates of total volume of earthquake-induced mass wastage ranged from 75-110 million m3. Economic losses were about US$ 1 billion. Nearly all of the approximately 1000 deaths from the earthquakes were a consequence of mass wasting and/ or flooding.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Engineering Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/0013-7952(95)00024-0","issn":"00137952","usgsCitation":"Schuster, R.L., Nieto, A., O’Rourke, T.D., Crespo, E., and Plaza-Nieto, G., 1996, Mass wasting triggered by the 5 March 1987 Ecuador earthquakes: Engineering Geology, v. 42, no. 1, p. 1-23, https://doi.org/10.1016/0013-7952(95)00024-0.","startPage":"1","endPage":"23","numberOfPages":"23","costCenters":[],"links":[{"id":487309,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/0013-7952(95)00024-0","text":"Publisher Index Page"},{"id":205869,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0013-7952(95)00024-0"},{"id":227207,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"42","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a525ae4b0c8380cd6c354","contributors":{"authors":[{"text":"Schuster, R. L.","contributorId":19135,"corporation":false,"usgs":true,"family":"Schuster","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":379683,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nieto, A.S.","contributorId":30629,"corporation":false,"usgs":true,"family":"Nieto","given":"A.S.","email":"","affiliations":[],"preferred":false,"id":379685,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O’Rourke, T. D.","contributorId":36308,"corporation":false,"usgs":true,"family":"O’Rourke","given":"T.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":379686,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Crespo, E.","contributorId":49123,"corporation":false,"usgs":true,"family":"Crespo","given":"E.","email":"","affiliations":[],"preferred":false,"id":379687,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Plaza-Nieto, G.","contributorId":28387,"corporation":false,"usgs":true,"family":"Plaza-Nieto","given":"G.","email":"","affiliations":[],"preferred":false,"id":379684,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":81516,"text":"81516 - 1996 - Lessons learned from a century of applying research results to management of national parks","interactions":[],"lastModifiedDate":"2022-12-14T17:22:22.926115","indexId":"81516","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"16","title":"Lessons learned from a century of applying research results to management of national parks","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Science and ecosystem management in the national parks","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"University of Arizona Press","publisherLocation":"Tucson, AZ","usgsCitation":"Halvorson, W., and Davis, G.E., 1996, Lessons learned from a century of applying research results to management of national parks, chap. 16 <i>of</i> Science and ecosystem management in the national parks, p. 334-344.","productDescription":"11 p.","startPage":"334","endPage":"344","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":127753,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e5d96","contributors":{"editors":[{"text":"Halvorson, William L.","contributorId":97194,"corporation":false,"usgs":true,"family":"Halvorson","given":"William L.","affiliations":[],"preferred":false,"id":504191,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Davis, Gary E.","contributorId":73235,"corporation":false,"usgs":true,"family":"Davis","given":"Gary","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":504190,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Halvorson, William L.","contributorId":97194,"corporation":false,"usgs":true,"family":"Halvorson","given":"William L.","affiliations":[],"preferred":false,"id":295533,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, Gary E.","contributorId":73235,"corporation":false,"usgs":true,"family":"Davis","given":"Gary","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":295532,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":96691,"text":"96691 - 1996 - Estimating the historical abundance of sea otters in California","interactions":[],"lastModifiedDate":"2012-02-02T00:03:51","indexId":"96691","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Estimating the historical abundance of sea otters in California","docAbstract":"No abstract available at this time","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Endangered Species Update, Special Issue: Conservation and Management of the southern sea otter.","largerWorkSubtype":{"id":9,"text":"Other Report"},"language":"English","usgsCitation":"DeMaster, D., Marzin, C., and Jameson, R., 1996, Estimating the historical abundance of sea otters in California, chap. <i>of</i> Endangered Species Update, Special Issue: Conservation and Management of the southern sea otter., v. 13, p. 79-81.","productDescription":"p. 79-81","startPage":"79","endPage":"81","numberOfPages":"3","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":126949,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc7cb","contributors":{"authors":[{"text":"DeMaster, D.P.","contributorId":93848,"corporation":false,"usgs":true,"family":"DeMaster","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":300077,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marzin, C.","contributorId":68673,"corporation":false,"usgs":true,"family":"Marzin","given":"C.","email":"","affiliations":[],"preferred":false,"id":300076,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jameson, R.J.","contributorId":56581,"corporation":false,"usgs":true,"family":"Jameson","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":300075,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":81514,"text":"81514 - 1996 - Resource issues addressed by case studies of sustained research in national parks","interactions":[],"lastModifiedDate":"2022-12-14T17:00:39.729209","indexId":"81514","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"15","title":"Resource issues addressed by case studies of sustained research in national parks","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Science and ecosystem management in the national parks","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"University of Arizona Press","publisherLocation":"Tucson, AZ","usgsCitation":"Davis, G.E., and Halvorson, W., 1996, Resource issues addressed by case studies of sustained research in national parks, chap. 15 <i>of</i> Science and ecosystem management in the national parks, p. 321-333.","productDescription":"13 p.","startPage":"321","endPage":"333","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":128045,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e5e57","contributors":{"editors":[{"text":"Halvorson, W. L.","contributorId":26246,"corporation":false,"usgs":true,"family":"Halvorson","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":504187,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Davis, G.E.","contributorId":10361,"corporation":false,"usgs":true,"family":"Davis","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":504186,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Davis, Gary E.","contributorId":73235,"corporation":false,"usgs":true,"family":"Davis","given":"Gary","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":295526,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Halvorson, William L.","contributorId":97194,"corporation":false,"usgs":true,"family":"Halvorson","given":"William L.","affiliations":[],"preferred":false,"id":295527,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":81513,"text":"81513 - 1996 - Changes in landscape values and expectations: What do we want and how do we measure it?","interactions":[],"lastModifiedDate":"2022-12-14T15:44:24.168337","indexId":"81513","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"2","title":"Changes in landscape values and expectations: What do we want and how do we measure it?","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"National parks and protected areas: Their role in environmental protection.","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Wiley","usgsCitation":"Halvorson, W.L., 1996, Changes in landscape values and expectations: What do we want and how do we measure it?, chap. 2 <i>of</i> National parks and protected areas: Their role in environmental protection., p. 15-30.","productDescription":"16 p.","startPage":"15","endPage":"30","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":128044,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e5e77","contributors":{"editors":[{"text":"Wright, G.","contributorId":111360,"corporation":false,"usgs":true,"family":"Wright","given":"G.","affiliations":[],"preferred":false,"id":504185,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Halvorson, W. L.","contributorId":26246,"corporation":false,"usgs":true,"family":"Halvorson","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":295525,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70018459,"text":"70018459 - 1996 - Semivariogram modeling by weighted least squares","interactions":[],"lastModifiedDate":"2012-03-12T17:19:25","indexId":"70018459","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1315,"text":"Computers & Geosciences","printIssn":"0098-3004","active":true,"publicationSubtype":{"id":10}},"title":"Semivariogram modeling by weighted least squares","docAbstract":"Permissible semivariogram models are fundamental for geostatistical estimation and simulation of attributes having a continuous spatiotemporal variation. The usual practice is to fit those models manually to experimental semivariograms. Fitting by weighted least squares produces comparable results to fitting manually in less time, systematically, and provides an Akaike information criterion for the proper comparison of alternative models. We illustrate the application of a computer program with examples showing the fitting of simple and nested models. Copyright ?? 1996 Elsevier Science Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Computers and Geosciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/0098-3004(95)00095-X","issn":"00983004","usgsCitation":"Jian, X., Olea, R., and Yu, Y., 1996, Semivariogram modeling by weighted least squares: Computers & Geosciences, v. 22, no. 4, p. 387-397, https://doi.org/10.1016/0098-3004(95)00095-X.","startPage":"387","endPage":"397","numberOfPages":"11","costCenters":[],"links":[{"id":487308,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/0098-3004(95)00095-x","text":"Publisher Index Page"},{"id":227117,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205852,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0098-3004(95)00095-X"}],"volume":"22","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8d1ae4b08c986b31826c","contributors":{"authors":[{"text":"Jian, X.","contributorId":70941,"corporation":false,"usgs":true,"family":"Jian","given":"X.","email":"","affiliations":[],"preferred":false,"id":379662,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olea, Ricardo A. 0000-0003-4308-0808","orcid":"https://orcid.org/0000-0003-4308-0808","contributorId":26436,"corporation":false,"usgs":true,"family":"Olea","given":"Ricardo A.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":379661,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yu, Y.-S.","contributorId":98892,"corporation":false,"usgs":true,"family":"Yu","given":"Y.-S.","email":"","affiliations":[],"preferred":false,"id":379663,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70018458,"text":"70018458 - 1996 - Granular-flow rheology: Role of shear-rate number in transition regime","interactions":[],"lastModifiedDate":"2024-04-22T14:34:25.295441","indexId":"70018458","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2252,"text":"Journal of Engineering Mechanics","active":true,"publicationSubtype":{"id":10}},"title":"Granular-flow rheology: Role of shear-rate number in transition regime","docAbstract":"<p><span>This paper examines the rationale behind the semiempirical formulation of a generalized viscoplastic fluid (GVF) model in the light of the Reiner-Rivlin constitutive theory and the viscoplastic theory, thereby identifying the parameters that control the rheology of granular flow. The shear-rate number (&nbsp;</span><strong>N</strong><span>&nbsp;) proves to be among the most significant parameters identified from the GVF model. As&nbsp;</span><strong>N</strong><span>&nbsp;→ 0 and&nbsp;</span><strong>N</strong><span>&nbsp;→∞, the GVF model can reduce asymptotically to the theoretical stress versus shear-rate relations in the macroviscous and grain-inertia regimes, respectively, where the grain concentration (&nbsp;</span><i>C</i><span>&nbsp;) also plays a major role in the rheology of granular flow. Using available data obtained from the rotating-cylinder experiments of neutrally buoyant solid spheres dispersing in an interstitial fluid, the shear stress for granular flow in transition between the two regimes proves dependent on&nbsp;</span><strong>N</strong><span>&nbsp;and&nbsp;</span><i>C</i><span>&nbsp;in addition to some material constants, such as the coefficient of restitution. The insufficiency of data on rotating-cylinder experiments cannot presently allow the GVF model to predict how a granular flow may behave in the entire range of&nbsp;</span><strong>N</strong><span>&nbsp;; however, the analyzed data provide an insight on the interrelation among the relevant dimensionless parameters.</span></p>","language":"English","publisher":"ASCE","doi":"10.1061/(ASCE)0733-9399(1996)122:5(469)","issn":"07339399","usgsCitation":"Chen, C., and Ling, C.#., 1996, Granular-flow rheology: Role of shear-rate number in transition regime: Journal of Engineering Mechanics, v. 122, no. 5, p. 469-479, https://doi.org/10.1061/(ASCE)0733-9399(1996)122:5(469).","productDescription":"11 p.","startPage":"469","endPage":"479","numberOfPages":"11","costCenters":[],"links":[{"id":227116,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"122","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a29c7e4b0c8380cd5ac1a","contributors":{"authors":[{"text":"Chen, Chiu-Lan","contributorId":100979,"corporation":false,"usgs":true,"family":"Chen","given":"Chiu-Lan","email":"","affiliations":[],"preferred":false,"id":379660,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ling, C. #NAME?","contributorId":14133,"corporation":false,"usgs":true,"family":"Ling","given":"C.","email":"","middleInitial":"#NAME?","affiliations":[],"preferred":false,"id":379659,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":96712,"text":"96712 - 1996 - Final report on coastal sage scrub amphibian and reptile autecology study","interactions":[],"lastModifiedDate":"2012-02-02T00:03:58","indexId":"96712","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Final report on coastal sage scrub amphibian and reptile autecology study","docAbstract":"No abstract available at this time","language":"English","collaboration":"Contract report to the California Department of Fish and Game (Contract number:  4188ES).","usgsCitation":"Case, T.J., and Fisher, R., 1996, Final report on coastal sage scrub amphibian and reptile autecology study.","costCenters":[],"links":[{"id":128118,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfed0","contributors":{"authors":[{"text":"Case, T. J.","contributorId":77078,"corporation":false,"usgs":true,"family":"Case","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":300115,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fisher, Robert N. 0000-0002-2956-3240","orcid":"https://orcid.org/0000-0002-2956-3240","contributorId":51675,"corporation":false,"usgs":true,"family":"Fisher","given":"Robert N.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":300114,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":96713,"text":"96713 - 1996 - Bullfrog impacts on sensitive wetland herpetofauna and Herpetology of San Bernardino National Wildlife Refuge","interactions":[],"lastModifiedDate":"2012-02-02T00:03:58","indexId":"96713","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Bullfrog impacts on sensitive wetland herpetofauna and Herpetology of San Bernardino National Wildlife Refuge","docAbstract":"No abstract available at this time","language":"English","collaboration":"Report to AGFD Heritage Program, Phoenix, and USDI FWS, San Bernardino National Wildlife Refuge, Douglas, Arizona","usgsCitation":"Rosen, P., and Schwalbe, C., 1996, Bullfrog impacts on sensitive wetland herpetofauna and Herpetology of San Bernardino National Wildlife Refuge, 61 p.","productDescription":"61 p.","startPage":"61","numberOfPages":"61","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":128189,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa67e","contributors":{"authors":[{"text":"Rosen, P.C.","contributorId":107640,"corporation":false,"usgs":true,"family":"Rosen","given":"P.C.","email":"","affiliations":[],"preferred":false,"id":300117,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schwalbe, C.R.","contributorId":35259,"corporation":false,"usgs":false,"family":"Schwalbe","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":300116,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70018455,"text":"70018455 - 1996 - The southern Whidbey Island fault: An active structure in the Puget Lowland, Washington","interactions":[],"lastModifiedDate":"2023-12-22T12:24:37.200255","indexId":"70018455","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"The southern Whidbey Island fault: An active structure in the Puget Lowland, Washington","docAbstract":"<p>Information from seismic-reflection profiles, outcrops, boreholes, and potential field surveys is used to interpret the structure and history of the southern Whidbey Island fault in the Puget Lowland of western Washington. This northwest-trending fault comprises a broad (as wide as 6–11 km), steep, northeast-dipping zone that includes several splays with inferred strike-slip, reverse, and thrust displacement. Transpressional deformation along the southern Whidbey Island fault is indicated by along-strike variations in structural style and geometry, positive flower structure, local unconformities, out-of-plane displacements, and juxtaposition of correlative sedimentary units with different histories.</p><p>The southern Whidbey Island fault represents a segment of a boundary between two major crustal blocks. The Cascade block to the northeast is floored by diverse assemblages of pre-Tertiary rocks; the Coast Range block to the southwest is floored by lower Eocene marine basaltic rocks of the Crescent Formation. The fault probably originated during the early Eocene as a dextral strike-slip fault along the eastern side of a continental-margin rift. Bending of the fault and transpressional deformation began during the late middle Eocene and continues to the present. Oblique convergence and clockwise rotation along the continental margin are the inferred driving forces for ongoing deformation.</p><p>Evidence for Quaternary movement on the southern Whidbey Island fault includes (1) offset and disrupted upper Quaternary strata imaged on seismic-reflection profiles; (2) borehole data that suggests as much as 420 m of structural relief on the Tertiary-Quaternary boundary in the fault zone; (3) several meters of displacement along exposed faults in upper Quaternary sediments; (4) late Quaternary folds with limb dips of as much as ≈9°; (5) large-scale liquefaction features in upper Quaternary sediments within the fault zone; and (6) minor historical seismicity. The southern Whidbey Island fault should be considered capable of generating large earthquakes (M<sub>s</sub><span>&nbsp;</span>≥7) and represents a potential seismic hazard to residents of the Puget Lowland.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1996)108<0334:TSWIFA>2.3.CO;2","issn":"00167606","usgsCitation":"Johnson, S.Y., Potter, C., Armentrout, J., Miller, J.J., Finn, C.A., and Weaver, C., 1996, The southern Whidbey Island fault: An active structure in the Puget Lowland, Washington: Geological Society of America Bulletin, v. 108, no. 3, p. 334-354, https://doi.org/10.1130/0016-7606(1996)108<0334:TSWIFA>2.3.CO;2.","productDescription":"21 p.","startPage":"334","endPage":"354","costCenters":[],"links":[{"id":227029,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Southern Whidbey Island Fault","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -123.06525828676914,\n              48.43268440330638\n            ],\n            [\n              -123.06525828676914,\n              47.816407388473664\n            ],\n            [\n              -122.18715952639644,\n              47.816407388473664\n            ],\n            [\n              -122.18715952639644,\n              48.43268440330638\n            ],\n            [\n              -123.06525828676914,\n              48.43268440330638\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"108","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb053e4b08c986b324dae","contributors":{"authors":[{"text":"Johnson, S. Y.","contributorId":48572,"corporation":false,"usgs":true,"family":"Johnson","given":"S.","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":379647,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Potter, C. J. 0000-0002-2300-6670","orcid":"https://orcid.org/0000-0002-2300-6670","contributorId":89925,"corporation":false,"usgs":true,"family":"Potter","given":"C. J.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":379651,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Armentrout, J.M.","contributorId":16176,"corporation":false,"usgs":true,"family":"Armentrout","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":379646,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, J. J.","contributorId":54588,"corporation":false,"usgs":true,"family":"Miller","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":379648,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Finn, Carol A. 0000-0002-6178-0405 cfinn@usgs.gov","orcid":"https://orcid.org/0000-0002-6178-0405","contributorId":1326,"corporation":false,"usgs":true,"family":"Finn","given":"Carol","email":"cfinn@usgs.gov","middleInitial":"A.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":379650,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Weaver, C.S.","contributorId":57874,"corporation":false,"usgs":true,"family":"Weaver","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":379649,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70018447,"text":"70018447 - 1996 - Groundwater inflow measurements in wetland systems","interactions":[],"lastModifiedDate":"2018-03-08T15:30:04","indexId":"70018447","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","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":"Groundwater inflow measurements in wetland systems","docAbstract":"<p><span>Our current understanding of wetlands is insufficient to assess the effects of past and future wetland loss. While knowledge of wetland hydrology is crucial, groundwater flows are often neglected or uncertain. In this paper, groundwater inflows were estimated in wetlands in southwestern Wisconsin using traditional Darcy's law calculations and three independent methods that included (1) stable isotope mass balances, (2) temperature profile modeling, and (3) numerical water balance modeling techniques. Inflows calculated using Darcy's law were lower than inflows estimated using the other approaches and ranged from 0.02 to 0.3 cm/d. Estimates obtained using the other methods generally were higher (0.1 to 1.1 cm/d) and showed similar spatial trends. An areal map of groundwater flux generated by the water balance model demonstrated that areas of both recharge and discharge exist in what is considered a regional discharge area. While each method has strengths and weaknesses, the use of more than one method can reduce uncertainty in the estimates.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/95WR03724","usgsCitation":"Hunt, R.J., Krabbenhoft, D.P., and Anderson, M.P., 1996, Groundwater inflow measurements in wetland systems: Water Resources Research, v. 32, no. 3, p. 495-507, https://doi.org/10.1029/95WR03724.","productDescription":"13 p.","startPage":"495","endPage":"507","costCenters":[],"links":[{"id":227604,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2da7e4b0c8380cd5bf89","contributors":{"authors":[{"text":"Hunt, Randy J.","contributorId":25903,"corporation":false,"usgs":false,"family":"Hunt","given":"Randy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":379610,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krabbenhoft, David P. 0000-0003-1964-5020 dpkrabbe@usgs.gov","orcid":"https://orcid.org/0000-0003-1964-5020","contributorId":1658,"corporation":false,"usgs":true,"family":"Krabbenhoft","given":"David","email":"dpkrabbe@usgs.gov","middleInitial":"P.","affiliations":[{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true},{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":379611,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Anderson, Mary P.","contributorId":147842,"corporation":false,"usgs":false,"family":"Anderson","given":"Mary","email":"","middleInitial":"P.","affiliations":[{"id":16925,"text":"University of Wisconsin-Madison","active":true,"usgs":false}],"preferred":false,"id":379612,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":96716,"text":"96716 - 1996 - Selected aspects of the ecology of the Arizona ridge-nosed rattlesnake (Crotalus willardi willardi) and the banded rock rattlesnake (Crotalus lepidus klauberi) in Arizona. Report to AGFD Heritage Program, Phoenix","interactions":[],"lastModifiedDate":"2012-02-02T00:03:58","indexId":"96716","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Selected aspects of the ecology of the Arizona ridge-nosed rattlesnake (Crotalus willardi willardi) and the banded rock rattlesnake (Crotalus lepidus klauberi) in Arizona. Report to AGFD Heritage Program, Phoenix","docAbstract":"No abstract available at this time","language":"English","usgsCitation":"McCrystal, H., Schwalbe, C., and Retes, D., 1996, Selected aspects of the ecology of the Arizona ridge-nosed rattlesnake (Crotalus willardi willardi) and the banded rock rattlesnake (Crotalus lepidus klauberi) in Arizona. Report to AGFD Heritage Program, Phoenix, 34 p.","productDescription":"34 p.","startPage":"34","numberOfPages":"34","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":128209,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa6fe","contributors":{"authors":[{"text":"McCrystal, H.K.","contributorId":10748,"corporation":false,"usgs":true,"family":"McCrystal","given":"H.K.","email":"","affiliations":[],"preferred":false,"id":300122,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schwalbe, C.R.","contributorId":35259,"corporation":false,"usgs":false,"family":"Schwalbe","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":300123,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Retes, D.F.","contributorId":54144,"corporation":false,"usgs":true,"family":"Retes","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":300124,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":96718,"text":"96718 - 1996 - Status of the least Bell's vireo and southwestern willow flycatcher at Marine Corps Base Camp Pendleton, 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:03:58","indexId":"96718","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Status of the least Bell's vireo and southwestern willow flycatcher at Marine Corps Base Camp Pendleton, 1995","docAbstract":"No abstract available at this time","language":"English","usgsCitation":"Kus, B., 1996, Status of the least Bell's vireo and southwestern willow flycatcher at Marine Corps Base Camp Pendleton, 1995, 19 p.","productDescription":"19 p.","startPage":"19","numberOfPages":"19","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":128211,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4794e4b07f02db48d1e6","contributors":{"authors":[{"text":"Kus, B.E.","contributorId":99492,"corporation":false,"usgs":true,"family":"Kus","given":"B.E.","email":"","affiliations":[],"preferred":false,"id":300126,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":96719,"text":"96719 - 1996 - Neotropical migratory bird monitoring study at Marine Corps Base Camp Pendleton, California. Second annual progress report, 1996","interactions":[],"lastModifiedDate":"2012-02-02T00:03:58","indexId":"96719","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Neotropical migratory bird monitoring study at Marine Corps Base Camp Pendleton, California. Second annual progress report, 1996","docAbstract":"No abstract available at this time","language":"English","usgsCitation":"Kus, B., 1996, Neotropical migratory bird monitoring study at Marine Corps Base Camp Pendleton, California. Second annual progress report, 1996, 27 p.","productDescription":"27 p.","startPage":"27","numberOfPages":"27","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":128212,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697d54","contributors":{"authors":[{"text":"Kus, B.E.","contributorId":99492,"corporation":false,"usgs":true,"family":"Kus","given":"B.E.","email":"","affiliations":[],"preferred":false,"id":300127,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7000014,"text":"7000014 - 1996 - The geologic story of the Ocoee River : see the river -- see the rapids -- see the rocks!","interactions":[],"lastModifiedDate":"2012-02-02T00:04:33","indexId":"7000014","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":363,"text":"General Interest Publication","active":false,"publicationSubtype":{"id":6}},"title":"The geologic story of the Ocoee River : see the river -- see the rapids -- see the rocks!","language":"ENGLISH","doi":"10.3133/7000014","usgsCitation":"Water Resources Division, U.S. Geological Survey, U.S. Forest Service, and Tennessee River Valley Authority, 1996, The geologic story of the Ocoee River : see the river -- see the rapids -- see the rocks!: General Interest Publication, 1 sheet : col. ill., col. maps ; 23 x 41 cm. folded to 23 x 10 cm., https://doi.org/10.3133/7000014.","productDescription":"1 sheet : col. ill., col. maps ; 23 x 41 cm. folded to 23 x 10 cm.","costCenters":[],"links":[{"id":131502,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":18587,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/gip/ocoee2/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d9c5","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":535076,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"U.S. Forest Service","contributorId":128067,"corporation":true,"usgs":false,"organization":"U.S. Forest Service","id":535075,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tennessee River Valley Authority","contributorId":128090,"corporation":true,"usgs":false,"organization":"Tennessee River Valley Authority","id":535077,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70018626,"text":"70018626 - 1996 - Preflight and in-flight calibration plan for ASTER","interactions":[],"lastModifiedDate":"2024-04-16T22:15:46.09283","indexId":"70018626","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2186,"text":"Journal of Atmospheric and Oceanic Technology","active":true,"publicationSubtype":{"id":10}},"title":"Preflight and in-flight calibration plan for ASTER","docAbstract":"<p>Preflight and in-flight radiometric calibration plans are described for the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) that is a multispectral optical imager of high spatial resolution. It is designed for the remote sensing from orbit of land surfaces and clouds, and is expected to be launched in 1998 on NASA's EOS<span>&nbsp;</span><i>AM-I</i><span>&nbsp;</span>spacecraft. ASTER acquires images in three separate spectral regions, the visible and near-infrared (VNIR), the shortwave infrared (SWIR), and the thermal infrared (TIR) with three imaging radiometer subsystems. The absolute radiometric accuracy is required to be better than 4% for VNIR and SWIR radiance measurements and 1 to 3 K, depending on the temperature regions from 200 to 370 K, for TIR temperature measurements.</p><p>A reference beam is introduced at the entrance pupil of each imaging radiometer to provide the in-flight calibration. Thus, the ASTER instrument includes internal onboard calibration units that comprise incandescent lamps for the VNIR and SWIR and a blackbody radiator for the TIR as reference sources. The calibration reliability of the VNIR and SWIR is enhanced by a dual system of onboard calibration units as well as by high-stability halogen lamps. A ground calibration system of spectral radiances traceable to fixed-point blackbodies is used for the preflight VNIR and SWIR calibration.</p><p>Because of the possibility of nonuniform contamination effects on the partial-aperture onboard calibration, it is desirable to check their results with respect to other methods. Reflectance- and radiance-based vicarious methods have been developed for this purpose. These, and methods involving in-flight cross-calibration with other sensors are also described.</p>","language":"English","publisher":"American Meteorological Society","doi":"10.1175/1520-0426(1996)013%3C0321:PAIFCP%3E2.0.CO;2","issn":"07390572","usgsCitation":"Ono, A., Sakuma, F., Arai, K., Yamaguchi, Y., Fujisada, H., Slater, P., Thome, K.J., Palluconi, F.D., and Kieffer, H.H., 1996, Preflight and in-flight calibration plan for ASTER: Journal of Atmospheric and Oceanic Technology, v. 13, no. 2, p. 321-335, https://doi.org/10.1175/1520-0426(1996)013%3C0321:PAIFCP%3E2.0.CO;2.","productDescription":"15 p.","startPage":"321","endPage":"335","numberOfPages":"15","costCenters":[],"links":[{"id":227172,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8224e4b0c8380cd7b925","contributors":{"authors":[{"text":"Ono, A.","contributorId":21710,"corporation":false,"usgs":true,"family":"Ono","given":"A.","email":"","affiliations":[],"preferred":false,"id":380257,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sakuma, F.","contributorId":100129,"corporation":false,"usgs":true,"family":"Sakuma","given":"F.","email":"","affiliations":[],"preferred":false,"id":380262,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Arai, K.","contributorId":101823,"corporation":false,"usgs":true,"family":"Arai","given":"K.","email":"","affiliations":[],"preferred":false,"id":380263,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Yamaguchi, Y.","contributorId":99317,"corporation":false,"usgs":true,"family":"Yamaguchi","given":"Y.","email":"","affiliations":[],"preferred":false,"id":380261,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fujisada, H.","contributorId":37906,"corporation":false,"usgs":true,"family":"Fujisada","given":"H.","email":"","affiliations":[],"preferred":false,"id":380258,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Slater, P.N.","contributorId":104648,"corporation":false,"usgs":true,"family":"Slater","given":"P.N.","email":"","affiliations":[],"preferred":false,"id":380264,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Thome, K. J.","contributorId":88099,"corporation":false,"usgs":true,"family":"Thome","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":380260,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Palluconi, Frank Don","contributorId":14952,"corporation":false,"usgs":true,"family":"Palluconi","given":"Frank","email":"","middleInitial":"Don","affiliations":[],"preferred":false,"id":380256,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Kieffer, H. H.","contributorId":40725,"corporation":false,"usgs":false,"family":"Kieffer","given":"H.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":380259,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70018466,"text":"70018466 - 1996 - Implications of fault constitutive properties for earthquake prediction","interactions":[],"lastModifiedDate":"2012-03-12T17:19:25","indexId":"70018466","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Implications of fault constitutive properties for earthquake prediction","docAbstract":"The rate- and state-dependent constitutive formulation for fault slip characterizes an exceptional variety of materials over a wide range of sliding conditions. This formulation provides a unified representation of diverse sliding phenomena including slip weakening over a characteristic sliding distance D(c), apparent fracture energy at a rupture front, time- dependent healing after rapid slip, and various other transient and slip rate effects. Laboratory observations and theoretical models both indicate that earthquake nucleation is accompanied by long intervals of accelerating slip. Strains from the nucleation process on buried faults generally could not be detected if laboratory values of D, apply to faults in nature. However, scaling of D(c) is presently an open question and the possibility exists that measurable premonitory creep may precede some earthquakes. Earthquake activity is modeled as a sequence of earthquake nucleation events. In this model, earthquake clustering arises from sensitivity of nucleation times to the stress changes induced by prior earthquakes. The model gives the characteristic Omori aftershock decay law and assigns physical interpretation to aftershock parameters. The seismicity formulation predicts large changes of earthquake probabilities result from stress changes. Two mechanisms for foreshocks are proposed that describe observed frequency of occurrence of foreshock-mainshock pairs by time and magnitude. With the first mechanism, foreshocks represent a manifestation of earthquake clustering in which the stress change at the time of the foreshock increases the probability of earthquakes at all magnitudes including the eventual mainshock. With the second model, accelerating fault slip on the mainshock nucleation zone triggers foreshocks.","largerWorkTitle":"Proceedings of the National Academy of Sciences of the United States of America","language":"English","doi":"10.1073/pnas.93.9.3787","issn":"00278424","usgsCitation":"Dieterich, J.H., and Kilgore, B., 1996, Implications of fault constitutive properties for earthquake prediction, <i>in</i> Proceedings of the National Academy of Sciences of the United States of America, v. 93, no. 9, p. 3787-3794, https://doi.org/10.1073/pnas.93.9.3787.","startPage":"3787","endPage":"3794","numberOfPages":"8","costCenters":[],"links":[{"id":480179,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"text":"External Repository"},{"id":205878,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1073/pnas.93.9.3787"},{"id":227251,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"93","issue":"9","noUsgsAuthors":false,"publicationDate":"1996-04-30","publicationStatus":"PW","scienceBaseUri":"505a3923e4b0c8380cd617fc","contributors":{"authors":[{"text":"Dieterich, James H.","contributorId":81614,"corporation":false,"usgs":true,"family":"Dieterich","given":"James","middleInitial":"H.","affiliations":[],"preferred":false,"id":379699,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kilgore, B.","contributorId":59968,"corporation":false,"usgs":true,"family":"Kilgore","given":"B.","email":"","affiliations":[],"preferred":false,"id":379698,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70017825,"text":"70017825 - 1996 - Diatoms as an aid in identifying late-holocene tsunami deposits","interactions":[],"lastModifiedDate":"2024-01-22T16:06:13.584047","indexId":"70017825","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1905,"text":"Holocene","active":true,"publicationSubtype":{"id":10}},"title":"Diatoms as an aid in identifying late-holocene tsunami deposits","docAbstract":"<p><span>Diatoms (Bacillariophyta) help identify the onshore deposits of tsunamis from earthquakes on the Cascadia subduction zone along the Pacific coast of Oregon, Washington, and British Columbia, and on faults high in the North American plate in the Puget Sound area of Washington. At the Copalis River, Washington, diatom analyses suggest that a tsunami deposit about 300 calendric years old (300 yr BP) originated from sandy shoals of the lower estuary rather than nearby beaches or coastal dunes. At Cultus Bay and West Point, Washington, well-preserved benthic estuarine diatoms in sand sheets overlying tidal-marsh peat indicate that the deposits came from intertidal or nearshore areas of Puget Sound. On an abruptly uplifted mudflat at the landward end of Hood Canal at Lynch Cove, Washington, tidal-flat diatoms refute the possibility of a terrestrial source for the sand. Diatoms in 300-yr-BP tsunami deposits on the Niawiakum River, Washington, confirm that the sand in these deposits had a marine source, and help to identify the landward extent of tsunami inundation. Diatom assemblages in deposits of the 300 yr BP and AD 1964 tsunamis at Port Alberni, British Columbia, consist of different dominant taxa, but both indicate that the sand units originated from Alberni Inlet. Diatoms add to stratigraphic evidence that tsunamis flooded Bradley Lake, a freshwater lake on the south-central Oregon coast, three times during the past 1700 years. Planktonic marine diatoms only found above 1-70-cm-thick sand layers in otherwise clayey lacustrine sediment imply tsunami inundation.</span></p>","language":"English","publisher":"Sage","doi":"10.1177/095968369600600406","issn":"09596836","usgsCitation":"Hemphill-Haley, E., 1996, Diatoms as an aid in identifying late-holocene tsunami deposits: Holocene, v. 6, no. 4, p. 439-448, https://doi.org/10.1177/095968369600600406.","productDescription":"10 p.","startPage":"439","endPage":"448","numberOfPages":"10","costCenters":[],"links":[{"id":228725,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"4","noUsgsAuthors":false,"publicationDate":"1996-12-01","publicationStatus":"PW","scienceBaseUri":"505a00aee4b0c8380cd4f868","contributors":{"authors":[{"text":"Hemphill-Haley, E.","contributorId":69309,"corporation":false,"usgs":true,"family":"Hemphill-Haley","given":"E.","email":"","affiliations":[],"preferred":false,"id":377670,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70018605,"text":"70018605 - 1996 - Kinetic and mineralogic controls on the evolution of groundwater chemistry and 87Sr/86Sr in a sandy silicate aquifer, northern Wisconsin, USA","interactions":[],"lastModifiedDate":"2019-02-20T10:20:07","indexId":"70018605","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Kinetic and mineralogic controls on the evolution of groundwater chemistry and 87Sr/86Sr in a sandy silicate aquifer, northern Wisconsin, USA","docAbstract":"Substantial flowpath-related variability of 87Sr/86Sr is observed in groundwaters collected from the Trout Lake watershed of northern Wisconsin. In the extensive shallow aquifer composed of sandy glacial outwash, groundwater is recharged either by seepage from lakes or by precipitation that infiltrates the inter-lake uplands. 87Sr/86Sr of groundwater derived mainly as seepage from a precipitation-dominated lake near the head of the watershed decreases with progressive water chemical evolution along its flowpath due primarily to enhanced dissolution of relatively unradiogenic plagioclase. In contrast, 87Sr/86Sr of groundwater derived mainly from precipitation that infiltrates upland areas is substantially greater than that of precipitation collected from the watershed, due to suppression of plagioclase dissolution together with preferential leaching of Sr from radiogenic phases such as K-feldspar and biotite. The results of a column experiment that simulated the effects of changing residence time of water in the aquifer sand indicate that mobile waters obtain relatively unradiogenic Sr, whereas stagnant waters obtain relatively radiogenic Sr. Nearly the entire range of strontium-isotope composition observed in groundwaters from the watershed was measured in the experimental product waters. The constant mobility of water along groundwater recharge flowpaths emanating from the lakes promotes the dissolution of relatively unradiogenic plagioclase, perhaps due to effective dispersal of clay mineral nuclei resulting from dissolution reactions. In contrast, episodic stagnation in the unsaturated zone along the upland recharge flowpaths suppresses plagioclase dissolution, perhaps due to accumulation of clay mineral nuclei on its reactive surfaces. Differences in redox conditions along these contrasting flowpaths probably enhance the observed differences in strontium isotope behavior. This study demonstrates that factors other than the calculated state of mineral saturation must be considered when attempting to simulate chemical evolution along flowpaths, and that reaction models must be able to incorporate changing contributions from reacting minerals in the calculations.","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(96)00052-X","issn":"00167037","usgsCitation":"Bullen, T., Krabbenhoft, D., and Kendall, C., 1996, Kinetic and mineralogic controls on the evolution of groundwater chemistry and 87Sr/86Sr in a sandy silicate aquifer, northern Wisconsin, USA: Geochimica et Cosmochimica Acta, v. 60, no. 10, p. 1807-1821, https://doi.org/10.1016/0016-7037(96)00052-X.","productDescription":"15 p.","startPage":"1807","endPage":"1821","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":227526,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205934,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0016-7037(96)00052-X"}],"volume":"60","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a40a3e4b0c8380cd64f0d","contributors":{"authors":[{"text":"Bullen, T.D.","contributorId":79911,"corporation":false,"usgs":true,"family":"Bullen","given":"T.D.","email":"","affiliations":[],"preferred":false,"id":380202,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krabbenhoft, D. P. 0000-0003-1964-5020","orcid":"https://orcid.org/0000-0003-1964-5020","contributorId":90765,"corporation":false,"usgs":true,"family":"Krabbenhoft","given":"D. P.","affiliations":[],"preferred":false,"id":380203,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kendall, C. 0000-0002-0247-3405","orcid":"https://orcid.org/0000-0002-0247-3405","contributorId":35050,"corporation":false,"usgs":true,"family":"Kendall","given":"C.","affiliations":[],"preferred":false,"id":380201,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70018604,"text":"70018604 - 1996 - Compressive and tensile failure at high fluid pressure where preexisting fractures have cohesive strength, with application to the San Andreas fault","interactions":[],"lastModifiedDate":"2024-11-06T17:25:45.378445","indexId":"70018604","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Compressive and tensile failure at high fluid pressure where preexisting fractures have cohesive strength, with application to the San Andreas fault","docAbstract":"<p><span>In thrusting and strike-slip situations, when the maximum principal horizontal stress&nbsp;</span><i>S</i><sub>1</sub><span>&nbsp;acts nearly normal to a fault (a misoriented fault, such as the San Andreas), pore-fluid pressure &gt; the lithostatic load,&nbsp;</span><i>P<sub>f</sub></i><span>&nbsp;&gt;&nbsp;</span><i>S<sub>v</sub></i><span>, is required to reactivate movement on that fault.&nbsp;</span><i>P<sub>f</sub></i><span>&nbsp;&gt;&nbsp;</span><i>S<sub>v</sub></i><span>&nbsp;may be achieved without causing hydraulic tensile fracturing if (1) previously existing cracks have regained cohesive strength by chemical processes, (2) subcritical crack growth has been blunted, and (3) the least principal horizontal stress&nbsp;</span><i>S</i><sub>3</sub><span>&nbsp;nearly equals&nbsp;</span><i>S<sub>v</sub></i><span>. Where&nbsp;</span><i>P<sub>f</sub></i><span>&nbsp;&gt;&nbsp;</span><i>S<sub>v</sub></i><span>&nbsp;has been attained within a misaligned fault, increasing the stress difference (</span><i>S</i><sub>1</sub><span>&nbsp;–&nbsp;</span><i>S</i><sub>3</sub><span>) at constant&nbsp;</span><i>P<sub>f</sub></i><span>&nbsp;&gt;&nbsp;</span><i>S<sub>v</sub></i><span>&nbsp;will not lead to shear failure, while a decrease in (</span><i>S</i><sub>1</sub><span>&nbsp;–&nbsp;</span><i>S</i><sub>3</sub><span>) can lead to shear failure of that fault. However, where the cohesive strength of material in a broad misaligned fault zone is less than that of the surrounding intact rock, increasing (</span><i>S</i><sub>1</sub><span>&nbsp;–&nbsp;</span><i>S</i><sub>3</sub><span>) while&nbsp;</span><i>P<sub>f</sub></i><span>&nbsp;&gt;&nbsp;</span><i>S<sub>v</sub></i><span>&nbsp;can result in shear failure of fractures at near optimum angles to&nbsp;</span><i>S</i><sub>1</sub><span>, but confined within this weak fault zone. If this faulting results in the local short-lived attainment of&nbsp;</span><i>P<sub>f</sub></i><span>&nbsp;&gt;&nbsp;</span><i>S<sub>v</sub></i><span>&nbsp;(cataclastic deformation and frictional heating overcoming dilation) and a simultaneous decrease in (</span><i>S</i><sub>1</sub><span>&nbsp;–&nbsp;</span><i>S</i><sub>3</sub><span>), this combination of effects can trigger movement along the main trace of the misaligned fault. When increasing&nbsp;</span><i>P<sub>f</sub></i><span>&nbsp;results in hydraulic failure, anisotropy in tensile strength or fracture toughness resulting from foliation within faults allows fractures to propagate along the planes of weakness rather than across the foliation perpendicular to&nbsp;</span><i>S</i><sub>3</sub><span>.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/96JB02293","issn":"01480227","usgsCitation":"Fournier, R., 1996, Compressive and tensile failure at high fluid pressure where preexisting fractures have cohesive strength, with application to the San Andreas fault: Journal of Geophysical Research B: Solid Earth, v. 101, no. B11, p. 25499-25509, https://doi.org/10.1029/96JB02293.","productDescription":"11 p.","startPage":"25499","endPage":"25509","numberOfPages":"11","costCenters":[],"links":[{"id":227482,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"101","issue":"B11","noUsgsAuthors":false,"publicationDate":"1996-11-10","publicationStatus":"PW","scienceBaseUri":"5059f948e4b0c8380cd4d540","contributors":{"authors":[{"text":"Fournier, R.O.","contributorId":73584,"corporation":false,"usgs":true,"family":"Fournier","given":"R.O.","email":"","affiliations":[],"preferred":false,"id":380200,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70018603,"text":"70018603 - 1996 - Identification of groundwater parameters at Columbus, Mississippi, using a 3D inverse flow and transport model","interactions":[],"lastModifiedDate":"2012-03-12T17:19:25","indexId":"70018603","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1934,"text":"IAHS-AISH Publication","active":true,"publicationSubtype":{"id":10}},"title":"Identification of groundwater parameters at Columbus, Mississippi, using a 3D inverse flow and transport model","docAbstract":"An extensive amount of data including hydraulic heads, hydraulic conductivities and concentrations of several solutes from controlled injections have been collected during the MADE 1 and MADE 2 experiments at a heterogeneous site near Columbus, Mississippi. In this paper the use of three-dimensional inverse groundwater models including simultaneous estimation of flow and transport parameters is proposed to help identify the dominant characteristics at the site. Simulations show that using a hydraulic conductivity distribution obtained from 2187 borehole flowmeter tests directly in the model produces poor matches to the measured hydraulic heads and tritium concentrations. Alternatively, time averaged hydraulic head maps are used to define zones of constant hydraulic conductivity to be estimated. Preliminary simulations suggest that in the case of conservative transport many, but not all, of the major plume characteristics can be explained by large-scale heterogeneity in recharge and hydraulic conductivity.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"IAHS-AISH Publication","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"01447815","usgsCitation":"Barlebo, H., Rosbjerg, D., and Hill, M.C., 1996, Identification of groundwater parameters at Columbus, Mississippi, using a 3D inverse flow and transport model: IAHS-AISH Publication, v. 237, p. 189-208.","startPage":"189","endPage":"208","numberOfPages":"20","costCenters":[],"links":[{"id":227481,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"237","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3829e4b0c8380cd6147f","contributors":{"authors":[{"text":"Barlebo, H.C.","contributorId":90484,"corporation":false,"usgs":true,"family":"Barlebo","given":"H.C.","email":"","affiliations":[],"preferred":false,"id":380198,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosbjerg, D.","contributorId":108266,"corporation":false,"usgs":true,"family":"Rosbjerg","given":"D.","affiliations":[],"preferred":false,"id":380199,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hill, M. C.","contributorId":48993,"corporation":false,"usgs":true,"family":"Hill","given":"M.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":380197,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":96732,"text":"96732 - 1996 - The effects of off-road vehicles on animal populations and habitats: A review of the literature. For the U S Bureau of Land Management, Riverside","interactions":[],"lastModifiedDate":"2012-02-02T00:03:58","indexId":"96732","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"The effects of off-road vehicles on animal populations and habitats: A review of the literature. For the U S Bureau of Land Management, Riverside","docAbstract":"No abstract available at this time","language":"English","usgsCitation":"Berry, K., 1996, The effects of off-road vehicles on animal populations and habitats: A review of the literature. For the U S Bureau of Land Management, Riverside, 104 p.; appendices.","productDescription":"104 p.; appendices","costCenters":[],"links":[{"id":128321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65def9","contributors":{"authors":[{"text":"Berry, K.H.","contributorId":17934,"corporation":false,"usgs":true,"family":"Berry","given":"K.H.","email":"","affiliations":[],"preferred":false,"id":300148,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70018602,"text":"70018602 - 1996 - Southern Ocean monthly wave fields for austral winters 1985-1988 by Geosat radar altimeter","interactions":[],"lastModifiedDate":"2024-04-30T16:39:36.246291","indexId":"70018602","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2315,"text":"Journal of Geophysical Research C: Oceans","active":true,"publicationSubtype":{"id":10}},"title":"Southern Ocean monthly wave fields for austral winters 1985-1988 by Geosat radar altimeter","docAbstract":"<p><span>Four years of monthly averaged wave height fields for the austral winters 1985–1988 derived from the Geosat altimeter data show a spatial variability of the scale of 500–1000 km that varies monthly and annually. This variability is superimposed on the zonal patterns surrounding the Antarctic continent and characteristic of the climatology derived from the&nbsp;</span><i>U.S. Navy</i><span>&nbsp;[1992] Marine Climatic Atlas of the World. The location and the intensity of these large-scale features, which are not found in the climatological fields, exhibit strong monthly and yearly variations. A global underestimation of the climatological mean wave heights by more than 1 m is also found over large regions of the Southern Ocean. The largest monthly averaged significant wave heights are above 5 m and are found during August of every year in the Indian Ocean, south of 40°S. The monthly wave fields show more variability in the Atlantic and Pacific Oceans than in the Indian Ocean. The Seasat data from 1978 and the Geosat data from 1985 and 1988 show an eastward rotation of the largest wave heights. However, this rotation is absent in 1986 and 1987; the former was a year of unusually low sea states, and the latter was a year of unusually high sea states, which suggests a link to the El Niño-Southern Oscillation event of 1986.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/95JC02963","issn":"01480227","usgsCitation":"Josberger, E., and Mognard, N.M., 1996, Southern Ocean monthly wave fields for austral winters 1985-1988 by Geosat radar altimeter: Journal of Geophysical Research C: Oceans, v. 101, no. C3, p. 6689-6696, https://doi.org/10.1029/95JC02963.","productDescription":"8 p.","startPage":"6689","endPage":"6696","numberOfPages":"8","costCenters":[],"links":[{"id":227434,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"101","issue":"C3","noUsgsAuthors":false,"publicationDate":"1996-03-15","publicationStatus":"PW","scienceBaseUri":"505b93eee4b08c986b31a773","contributors":{"authors":[{"text":"Josberger, E.G.","contributorId":61161,"corporation":false,"usgs":true,"family":"Josberger","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":380196,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mognard, N. M.","contributorId":27612,"corporation":false,"usgs":false,"family":"Mognard","given":"N.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":380195,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}