{"pageNumber":"5019","pageRowStart":"125450","pageSize":"25","recordCount":184617,"records":[{"id":70013216,"text":"70013216 - 1985 - TRANSIENT SOUNDING INVESTIGATION OF NEWBERRY VOLCANO, OREGON.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:39","indexId":"70013216","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"TRANSIENT SOUNDING INVESTIGATION OF NEWBERRY VOLCANO, OREGON.","docAbstract":"Transient electromagnetic soundings were used to map the geoelectrical structure of Newberry Volcano in central Oregon. An extensive conductor was found to underlie the volcano and to have resistivities from 20 OMEGA m to 72 OMEGA m. The depth to the conductor ranges from 410 m to 870 m. Inside the caldera, low basement resistivities are the result of hot fluids. The cause of the conductor outside the caldera is not known; however, we speculate that it is due to the water table.","largerWorkTitle":"Transactions - Geothermal Resources Council","conferenceTitle":"1985 International Symposium on Geothermal Energy. Geothermal Resources Council 1985 Annual Meeting.","conferenceLocation":"Kailua-Kona, HI, USA","language":"English","publisher":"Geothermal Resources Council","publisherLocation":"Davis, CA, USA","issn":"01935933","isbn":"093441260X","usgsCitation":"Fitterman, D.V., and Neev, D.K., 1985, TRANSIENT SOUNDING INVESTIGATION OF NEWBERRY VOLCANO, OREGON., <i>in</i> Transactions - Geothermal Resources Council, v. 9, no. pt 2, Kailua-Kona, HI, USA, p. 407-410.","startPage":"407","endPage":"410","numberOfPages":"4","costCenters":[],"links":[{"id":220023,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"pt 2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba391e4b08c986b31fd6c","contributors":{"authors":[{"text":"Fitterman, David V. dfitterman@usgs.gov","contributorId":1106,"corporation":false,"usgs":true,"family":"Fitterman","given":"David","email":"dfitterman@usgs.gov","middleInitial":"V.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":365562,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neev, Deborah K.","contributorId":35872,"corporation":false,"usgs":true,"family":"Neev","given":"Deborah","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":365563,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1013636,"text":"1013636 - 1985 - Purification of Cyclops cultures by pH shock (Copepoda)","interactions":[],"lastModifiedDate":"2023-09-25T15:15:59.954616","indexId":"1013636","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1348,"text":"Crustaceana","active":true,"publicationSubtype":{"id":10}},"title":"Purification of Cyclops cultures by pH shock (Copepoda)","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Brill","doi":"10.1163/156854085X00864","usgsCitation":"Bulkowski, L., Krise, W.F., and Kraus, K.A., 1985, Purification of Cyclops cultures by pH shock (Copepoda): Crustaceana, v. 48, no. 2, p. 179-182, https://doi.org/10.1163/156854085X00864.","productDescription":"4 p.","startPage":"179","endPage":"182","numberOfPages":"4","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132301,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"48","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a90e4b07f02db655793","contributors":{"authors":[{"text":"Bulkowski, L.","contributorId":88312,"corporation":false,"usgs":true,"family":"Bulkowski","given":"L.","email":"","affiliations":[],"preferred":false,"id":318930,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krise, W. F.","contributorId":50842,"corporation":false,"usgs":true,"family":"Krise","given":"W.","middleInitial":"F.","affiliations":[],"preferred":false,"id":318928,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kraus, K. A.","contributorId":84707,"corporation":false,"usgs":true,"family":"Kraus","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":318929,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012263,"text":"70012263 - 1985 - Water-level changes in the Ogallala aquifer, northwestern Oklahoma.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:03","indexId":"70012263","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2944,"text":"Oklahoma Geology Notes","active":true,"publicationSubtype":{"id":10}},"title":"Water-level changes in the Ogallala aquifer, northwestern Oklahoma.","docAbstract":"The Ogallala aquifer, that part of the High Plains aquifer in Oklahoma, is part of a regional aquifer system that underlies parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming. In 1978 the US Geological Survey began a 5- year study of the High Plains regional aquifer system to provide hydrologic information for evaluation of the effects of long-term development of the aquifer and to develop a capability for predicting aquifer response to various ground-water-management alternatives (Weeks, 1978). -from Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Oklahoma Geology Notes","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00301736","usgsCitation":"Havens, J., 1985, Water-level changes in the Ogallala aquifer, northwestern Oklahoma.: Oklahoma Geology Notes, v. 45, no. 5, p. 205-210.","startPage":"205","endPage":"210","numberOfPages":"6","costCenters":[],"links":[{"id":222127,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bcd4de4b08c986b32dfac","contributors":{"authors":[{"text":"Havens, J.S.","contributorId":12043,"corporation":false,"usgs":true,"family":"Havens","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":363125,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012811,"text":"70012811 - 1985 - The Schwartzwalder uranium deposit. I: Geology and structural controls on mineralization.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:06","indexId":"70012811","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"The Schwartzwalder uranium deposit. I: Geology and structural controls on mineralization.","docAbstract":"Numerous uranium veins occupy fractures and faults in brittle Proterozoic gneisses along the east central Front Range of Colorado. The deposit size correlates with the density and localization of brittle fracture. The largest deposit, the Schwartzwalder, is explained by a singular configuration of complexly broken, deep-reaching brittle gneisses between impervious schists. The gneisses are described as being derived from volcanic rocks, shales, and chemical sediments, including iron, quartz and sulphide formations.-G.J.N.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Economic Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03610128","usgsCitation":"Wallace, A.R., and Karlson, R.C., 1985, The Schwartzwalder uranium deposit. I: Geology and structural controls on mineralization.: Economic Geology, v. 80, no. 7, p. 1842-1857.","startPage":"1842","endPage":"1857","numberOfPages":"16","costCenters":[],"links":[{"id":222620,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"80","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba8dce4b08c986b321ed6","contributors":{"authors":[{"text":"Wallace, A. R.","contributorId":59445,"corporation":false,"usgs":true,"family":"Wallace","given":"A.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":364590,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Karlson, R. C.","contributorId":19524,"corporation":false,"usgs":true,"family":"Karlson","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":364589,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012345,"text":"70012345 - 1985 - Facies in stratigraphy: From 'terrains' to 'terranes'.","interactions":[],"lastModifiedDate":"2024-05-07T16:35:54.846891","indexId":"70012345","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2307,"text":"Journal of Geological Education","active":true,"publicationSubtype":{"id":10}},"title":"Facies in stratigraphy: From 'terrains' to 'terranes'.","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.5408/0022-1368-33.3.175","issn":"00221368","usgsCitation":"Nelson, C., 1985, Facies in stratigraphy: From 'terrains' to 'terranes'.: Journal of Geological Education, v. 33, no. 3, p. 175-187, https://doi.org/10.5408/0022-1368-33.3.175.","productDescription":"13 p.","startPage":"175","endPage":"187","numberOfPages":"13","costCenters":[],"links":[{"id":487209,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.5408/0022-1368-33.3.175","text":"Publisher Index Page"},{"id":221818,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"3","noUsgsAuthors":false,"publicationDate":"2018-02-13","publicationStatus":"PW","scienceBaseUri":"505a0e8de4b0c8380cd534fc","contributors":{"authors":[{"text":"Nelson, C.M.","contributorId":31115,"corporation":false,"usgs":true,"family":"Nelson","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":363330,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70013025,"text":"70013025 - 1985 - Land subsidence: Its impacts and costs in the U.S","interactions":[],"lastModifiedDate":"2012-03-12T17:18:39","indexId":"70013025","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3667,"text":"Underground Space","active":true,"publicationSubtype":{"id":10}},"title":"Land subsidence: Its impacts and costs in the U.S","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Underground Space","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03620565","usgsCitation":"Holzer, T., 1985, Land subsidence: Its impacts and costs in the U.S: Underground Space, v. 9, no. 5-6.","startPage":"260","costCenters":[],"links":[{"id":219888,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"5-6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a41c0e4b0c8380cd65784","contributors":{"authors":[{"text":"Holzer, T.L.","contributorId":35739,"corporation":false,"usgs":true,"family":"Holzer","given":"T.L.","email":"","affiliations":[],"preferred":false,"id":365108,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012361,"text":"70012361 - 1985 - EFFECT OF TEMPERATURE ON THE SORPTION OF CHELATED RADIONUCLIDES.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:05","indexId":"70012361","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"EFFECT OF TEMPERATURE ON THE SORPTION OF CHELATED RADIONUCLIDES.","docAbstract":"Temperature effects in the near-field radioactive waste disposal environment can result in changes in the adsorptive capacity and character of the substrate and the chemistry of the reacting fluids. This work examines the effect of temperature on 1) the kinetics of radionuclide sorption onto clays from 25 degree -75 degree C and 2) the degradation and metal-binding ability of two organic complexing agents found in chelated radioactive wastes and natural groundwaters.","largerWorkTitle":"Materials Research Society Symposia Proceedings","conferenceTitle":"Scientific Basis for Nuclear Waste Management VIII. Held as part of the Fall Meeting of the Materials Research Society.","conferenceLocation":"Boston, MA, USA","language":"English","publisher":"Materials Research Soc","publisherLocation":"Pittsburgh, PA, USA","issn":"02729172","isbn":"093183709X","usgsCitation":"Maest, A.S., Crerar, D.A., Dillon, E.C., Trehu, S.M., and Rountree, T.N., 1985, EFFECT OF TEMPERATURE ON THE SORPTION OF CHELATED RADIONUCLIDES., <i>in</i> Materials Research Society Symposia Proceedings, v. 44, Boston, MA, USA, p. 377-384.","startPage":"377","endPage":"384","numberOfPages":"8","costCenters":[],"links":[{"id":222073,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0457e4b0c8380cd50907","contributors":{"editors":[{"text":"Jantzen Carol M.Stone John A.Ewing Rodney C.","contributorId":128428,"corporation":true,"usgs":false,"organization":"Jantzen Carol M.Stone John A.Ewing Rodney C.","id":536251,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Maest, Ann S.","contributorId":26003,"corporation":false,"usgs":true,"family":"Maest","given":"Ann","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":363368,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crerar, David A.","contributorId":23278,"corporation":false,"usgs":true,"family":"Crerar","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":363367,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dillon, Edward C.","contributorId":70923,"corporation":false,"usgs":true,"family":"Dillon","given":"Edward","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":363369,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Trehu, Stephen M.","contributorId":88488,"corporation":false,"usgs":true,"family":"Trehu","given":"Stephen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":363370,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rountree, Tamara N.","contributorId":97635,"corporation":false,"usgs":true,"family":"Rountree","given":"Tamara","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":363371,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70012309,"text":"70012309 - 1985 - Isotopic and morphologic evidence for the age of the Fordham Gneiss","interactions":[],"lastModifiedDate":"2023-02-08T17:32:46.437502","indexId":"70012309","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":732,"text":"American Journal of Science","active":true,"publicationSubtype":{"id":10}},"title":"Isotopic and morphologic evidence for the age of the Fordham Gneiss","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Journal of Science","doi":"10.2475/ajs.285.5.459","usgsCitation":"Aleinikoff, J.N., 1985, Isotopic and morphologic evidence for the age of the Fordham Gneiss: American Journal of Science, v. 285, no. 5, p. 459-479, https://doi.org/10.2475/ajs.285.5.459.","productDescription":"21 p.","startPage":"459","endPage":"479","numberOfPages":"21","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":480174,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2475/ajs.285.5.459","text":"Publisher Index Page"},{"id":221883,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"285","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3f97e4b0c8380cd6463a","contributors":{"authors":[{"text":"Aleinikoff, John N. 0000-0003-3494-6841 jaleinikoff@usgs.gov","orcid":"https://orcid.org/0000-0003-3494-6841","contributorId":1478,"corporation":false,"usgs":true,"family":"Aleinikoff","given":"John","email":"jaleinikoff@usgs.gov","middleInitial":"N.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":363238,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012265,"text":"70012265 - 1985 - The Dunbar Gneiss-granitoid dome: Implications for early Proterozoic tectonic evolution of northern Wisconsin","interactions":[],"lastModifiedDate":"2024-01-03T00:52:03.874553","indexId":"70012265","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","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 Dunbar Gneiss-granitoid dome: Implications for early Proterozoic tectonic evolution of northern Wisconsin","docAbstract":"<div id=\"15191434\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>The Dunbar dome in northeastern Wisconsin is a critical structural feature in the early Proterozoic Penokean orogen. It provides exposures of gneisses (Dunbar Gneiss) that structurally underlie the voluminous metavolcanic rocks of northeastern Wisconsin, and exposures of abundant granitoid rocks ranging from tonalite to granite. The granitoid rocks cut both the gneisses in the core and the supracrustal (cover) metavolcanic rocks and were emplaced essentially along the core-cover boundary. The Dunbar Gneiss is calc-alkaline and was derived from volcanic and intrusive rocks of intermediate composition. The various intrusive rocks have calcic, calc-alkaline, and alkali to alkali-calcic compositions, and they progress with time to more SiO<sub>2</sub><span>&nbsp;</span>and K<sub>2</sub>-rich compositions. U-Pb zircon ages indicate that accumulation of the layered rocks in the core and cover, deformation and metamorphism, and intrusion of the granitoid rocks spanned a relatively short time, ∼1865–1835 Ma.</p><p>We interpret the dome as being a large-scale, fold-interference structure resulting from polydeformation modified by diapirism. Northeast-oriented folds (F<sub>3</sub>) and a related mylonitic foliation (S<sub>3</sub>), nearly confined to the dome, are superposed on northwest-oriented folds (F<sub>2</sub>) that developed during regional deformation. In the core-cover boundary, these structures are obliterated by a zone of intense deformation—a mylonitic foliation and a steeply plunging stretching lineation—as much as 500 m wide, which we interpret as resulting from diapirism. Metamorphic zoning is concentric: amphibolite facies in inner parts of the mantle and greenschist facies in the outer part of the mantle.</p><p>The Wisconsin magmatic terrane, as represented by the rocks in the Dunbar dome, differs from the epicratonic, early Proterozoic sedimentary-volcanic sequence (Marquette Range Supergroup) in Michigan, to the north, in stratigraphy, structure, and volume and composition of igneous rocks. Whereas the basalts in northern Michigan are compositionally similar to continental rift basalts, the volcanic rocks in the Dunbar dome have over-all island-arc compositional affinities. The over-all calc-alkaline compositions of the intrusive rocks are similar to those in magmatic arcs formed at convergent plate-margin settings. Accordingly, we interpret the Wisconsin magmatic terrane as an oceanic-arc complex that was sutured to the North American continent during development of the Penokean orogen. Similar interpretations based on broad regional observations have been proposed previously.</p></div>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1985)96<1101:TDGDIF>2.0.CO;2","usgsCitation":"Sims, P., Peterman, Z.E., and Schulz, K.J., 1985, The Dunbar Gneiss-granitoid dome: Implications for early Proterozoic tectonic evolution of northern Wisconsin: Geological Society of America Bulletin, v. 96, no. 9, p. 1101-1112, https://doi.org/10.1130/0016-7606(1985)96<1101:TDGDIF>2.0.CO;2.","productDescription":"12 p.","startPage":"1101","endPage":"1112","numberOfPages":"12","costCenters":[],"links":[{"id":222129,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Michigan, Wisconsin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -90.17501031586968,\n              44.73567155837759\n            ],\n            [\n              -86.92305719086939,\n              44.73567155837759\n            ],\n            [\n              -86.92305719086939,\n              47.35804575064864\n            ],\n            [\n              -90.17501031586968,\n              47.35804575064864\n            ],\n            [\n              -90.17501031586968,\n              44.73567155837759\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"96","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba70be4b08c986b321333","contributors":{"authors":[{"text":"Sims, P.K.","contributorId":30191,"corporation":false,"usgs":true,"family":"Sims","given":"P.K.","email":"","affiliations":[],"preferred":false,"id":363127,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterman, Z. E.","contributorId":63781,"corporation":false,"usgs":true,"family":"Peterman","given":"Z.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":363128,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schulz, K. J.","contributorId":79131,"corporation":false,"usgs":true,"family":"Schulz","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":363129,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012791,"text":"70012791 - 1985 - Determination of interstitial chloride in shales and consolidated rocks by a precision leaching technique","interactions":[],"lastModifiedDate":"2019-11-25T13:51:29","indexId":"70012791","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3411,"text":"Society of Petroleum Engineers journal","active":true,"publicationSubtype":{"id":10}},"title":"Determination of interstitial chloride in shales and consolidated rocks by a precision leaching technique","docAbstract":"<p><span>We have devised a technique for determining chloride in interstitial water of consolidated rocks. Samples of rocks ranging from 5 to 10 g are crushed and sieved under controlled conditions and then ground with distilled water to submicron size in a closed mechanical mill. After ultra-centrifugation, chloride content is determined by coulometric titration. The chloride concentrations and total pore-water concentrations, obtained earlier from the same pore-water concentrations, obtained earlier from the same samples by low-temperature vacuum desiccation, are used to arrive at the \"original\" pore-water chloride concentrations by a simple iteration procedure. Interstitial chlorinity results obtained from Cretaceous and Jurassic strata in the Gulf of Mexico coastal areas ranged from 20 to 100 g/kg Cl with reproducibility approaching +/- 1%. We have also applied the technique to igneous and metamorphic bedrocks as well as ocean basalts containing 1 % water or less. Chloride values ranging from 6.7 to 20 g/kg with a reproducibility of about 5% were obtained.</span></p>","language":"English","publisher":"Society of Petroleum Engineers","doi":"10.2118/12724-PA","issn":"01977520","usgsCitation":"Manheim, F., Peck, E., and Lane, C.M., 1985, Determination of interstitial chloride in shales and consolidated rocks by a precision leaching technique: Society of Petroleum Engineers journal, v. 25, no. 5, p. 704-710, https://doi.org/10.2118/12724-PA.","productDescription":"7 p.","startPage":"704","endPage":"710","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":222377,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"5","noUsgsAuthors":false,"publicationDate":"1985-10-01","publicationStatus":"PW","scienceBaseUri":"5059fd43e4b0c8380cd4e71a","contributors":{"authors":[{"text":"Manheim, Frank T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":45294,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank T.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":364536,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peck, E.E.","contributorId":77302,"corporation":false,"usgs":true,"family":"Peck","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":364537,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lane, Candice M.","contributorId":80823,"corporation":false,"usgs":true,"family":"Lane","given":"Candice","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":364538,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012192,"text":"70012192 - 1985 - Terrestrial vs. marine depositional model—A new assessment of subsurface Lower Pennsylvanian rocks of southwestern Virginia","interactions":[],"lastModifiedDate":"2024-01-30T12:28:59.810095","indexId":"70012192","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Terrestrial vs. marine depositional model—A new assessment of subsurface Lower Pennsylvanian rocks of southwestern Virginia","docAbstract":"<div id=\"15569158\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>A reinterpretation of the origin of subsurface rocks in southwestern Virginia and southeastern Kentucky suggests that, contrary to commonly accepted ideas, the Mississippian-Pennsylvanian Systemic boundary is an unconformity and the Lower Pennsylvanian quartz arenite sequences were deposited in a fluvial environment. Because Pennsylvanian strata of the Pocahontas and Lee Formations appear to have been deposited at the same time in adjacent valleys, the Pocahontas, which generally has been considered to be older and to underlie the Lee, is considered here to be equivalent to the basal part of the Middlesboro Member of the Lee Formation.</p></div>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1985)13<786:TVMDMN>2.0.CO;2","issn":"00917613","usgsCitation":"Rice, C.L., 1985, Terrestrial vs. marine depositional model—A new assessment of subsurface Lower Pennsylvanian rocks of southwestern Virginia: Geology, v. 13, no. 11, p. 786-789, https://doi.org/10.1130/0091-7613(1985)13<786:TVMDMN>2.0.CO;2.","productDescription":"4 p.","startPage":"786","endPage":"789","numberOfPages":"4","costCenters":[],"links":[{"id":222122,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba565e4b08c986b320a00","contributors":{"authors":[{"text":"Rice, C. L.","contributorId":60658,"corporation":false,"usgs":true,"family":"Rice","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":362963,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012359,"text":"70012359 - 1985 - QUALITY ASSURANCE PROGRAM FOR WET DEPOSITION SAMPLING AND CHEMICAL ANALYSES FOR THE NATIONAL TRENDS NETWORK.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:07","indexId":"70012359","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"QUALITY ASSURANCE PROGRAM FOR WET DEPOSITION SAMPLING AND CHEMICAL ANALYSES FOR THE NATIONAL TRENDS NETWORK.","docAbstract":"The purpose of the National Trends Network is to delineate the major inorganic constituents in the wet deposition in the United States. The approach chosen to monitor the Nation's wet deposition is to install approximately 150 automatic sampling devices with at least one collector in each state. Samples are collected at one week intervals, removed from collectors, and transported to an analytical laboratory for chemical analysis. The quality assurance program has divided wet deposition monitoring into 5 parts: (1) Sampling site selection, (2) sampling device, (3) sample container, (4) sample handling, and (5) laboratory analysis. Each of these five components is being examined using existing designs or new designs. Each existing or proposed sampling site is visited and a criteria audit is performed.","conferenceTitle":"Transactions - Quality Assurance in Air Pollution Measurements.","conferenceLocation":"Boulder, CO, USA","language":"English","publisher":"APCA (TR-3)","publisherLocation":"Pittsburgh, PA, USA","usgsCitation":"Schroder, L., and Malo, B.A., 1985, QUALITY ASSURANCE PROGRAM FOR WET DEPOSITION SAMPLING AND CHEMICAL ANALYSES FOR THE NATIONAL TRENDS NETWORK., Transactions - Quality Assurance in Air Pollution Measurements., Boulder, CO, USA, p. 254-260.","startPage":"254","endPage":"260","numberOfPages":"7","costCenters":[],"links":[{"id":222012,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a906de4b0c8380cd7fd24","contributors":{"editors":[{"text":"Johnson Ted R.Penkala Stanley J.","contributorId":128455,"corporation":true,"usgs":false,"organization":"Johnson Ted R.Penkala Stanley J.","id":536249,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Schroder, LeRoy J.","contributorId":8454,"corporation":false,"usgs":true,"family":"Schroder","given":"LeRoy J.","affiliations":[],"preferred":false,"id":363364,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Malo, Bernard A.","contributorId":78868,"corporation":false,"usgs":true,"family":"Malo","given":"Bernard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":363365,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70013020,"text":"70013020 - 1985 - Physiography and deposition on a distal deep-sea system: The Valencia Fan (Northwestern Mediterranean)","interactions":[],"lastModifiedDate":"2012-03-12T17:18:23","indexId":"70013020","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"Physiography and deposition on a distal deep-sea system: The Valencia Fan (Northwestern Mediterranean)","docAbstract":"The Valencia Fan developed as the distal fill of a deep-sea valley, detached from the continental slope and the main sedimentary source. A survey of side-scan sonar, Sea Beam and reflection seismics shows that the sediment is largely fed through the Valencia Valley. The upper fan comprises large channels with low-relief levees, and the middle fan has sinuous distributary channels. Depositional bedforms predominate on the valley floor and levees, and erosional bedforms are common in the valley walls. A change to slope on the fan apex and the presence of volcanoes on the upper fan are the main factors influencing fan-growth pattern. ?? 1985 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF02281633","issn":"02760460","usgsCitation":"Maldonado, A., Palanques, A., Alonso, B., Kastens, K., Nelson, C., O'Connell, S., and Ryan, W., 1985, Physiography and deposition on a distal deep-sea system: The Valencia Fan (Northwestern Mediterranean): Geo-Marine Letters, v. 5, no. 3, p. 157-164, https://doi.org/10.1007/BF02281633.","startPage":"157","endPage":"164","numberOfPages":"8","costCenters":[],"links":[{"id":204977,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02281633"},{"id":219828,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7b04e4b0c8380cd791e9","contributors":{"authors":[{"text":"Maldonado, A.","contributorId":90437,"corporation":false,"usgs":true,"family":"Maldonado","given":"A.","affiliations":[],"preferred":false,"id":365095,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Palanques, A.","contributorId":61155,"corporation":false,"usgs":true,"family":"Palanques","given":"A.","email":"","affiliations":[],"preferred":false,"id":365091,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Alonso, B.","contributorId":51014,"corporation":false,"usgs":true,"family":"Alonso","given":"B.","email":"","affiliations":[],"preferred":false,"id":365090,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kastens, K.A.","contributorId":70917,"corporation":false,"usgs":true,"family":"Kastens","given":"K.A.","email":"","affiliations":[],"preferred":false,"id":365092,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Nelson, C.H.","contributorId":88346,"corporation":false,"usgs":true,"family":"Nelson","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":365094,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"O'Connell, S.","contributorId":37060,"corporation":false,"usgs":true,"family":"O'Connell","given":"S.","affiliations":[],"preferred":false,"id":365089,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ryan, William B. F.","contributorId":86486,"corporation":false,"usgs":false,"family":"Ryan","given":"William B. F.","affiliations":[{"id":7135,"text":"Lamont Doherty Earth Observatory, Columbia University, Palisades, NY","active":true,"usgs":false}],"preferred":false,"id":365093,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70012942,"text":"70012942 - 1985 - An underwater instrument for determining bearing capacity of shallow marine sediments","interactions":[],"lastModifiedDate":"2023-11-16T17:49:08.25594","indexId":"70012942","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1824,"text":"Geotechnical Testing Journal","active":true,"publicationSubtype":{"id":10}},"title":"An underwater instrument for determining bearing capacity of shallow marine sediments","docAbstract":"<p><span>A small, portable, underwater instrument for measuring carbonate substrate bearing capacity in situ is described. The device was used in various shallow water (&lt; 9 m) carbonate reef environments. Criteria for design and operation were based on ability to deliver controlled levels of stress to bearing plates of various sizes, operability underwater by scuba divers, transportability, and cost.</span></p>","language":"English","publisher":"ASTM","doi":"10.1520/GTJ10516J","usgsCitation":"Circe, R.C., 1985, An underwater instrument for determining bearing capacity of shallow marine sediments: Geotechnical Testing Journal, v. 8, no. 2, p. 96-98, https://doi.org/10.1520/GTJ10516J.","productDescription":"3 p.","startPage":"96","endPage":"98","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":222688,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbb3ee4b08c986b3285b1","contributors":{"authors":[{"text":"Circe, Ronald C.","contributorId":41592,"corporation":false,"usgs":true,"family":"Circe","given":"Ronald","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":364898,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012943,"text":"70012943 - 1985 - Kinetic and thermodynamic factors controlling the distribution of SO32- and Na+ in calcites and selected aragonites","interactions":[],"lastModifiedDate":"2024-03-19T16:54:10.042448","indexId":"70012943","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","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}},"displayTitle":"Kinetic and thermodynamic factors controlling the distribution of SO<sub>3</sub><sup>2-</sup> and Na<sup>+</sup> in calcites and selected aragonites","title":"Kinetic and thermodynamic factors controlling the distribution of SO32- and Na+ in calcites and selected aragonites","docAbstract":"<div id=\"preview-section-abstract\"><div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p>Significant amounts of SO<sub>4</sub><sup>2−</sup>, Na<sup>+</sup>, and OH<sup>−</sup><span>&nbsp;</span>are incorporated in marine biogenic calcites. Biogenic high Mg-calcites average about 1 mole percent SO<sub>4</sub><sup>2−</sup>. Aragonites and most biogenic low Mg-calcites contain significant amounts of Na<sup>+</sup>, but very low concentrations of SO<sub>4</sub><sup>2−</sup>. The SO<sub>4</sub><sup>2−</sup><span>&nbsp;</span>content of non-biogenic calcites and aragonites investigated was below 100 ppm. The presence of Na<sup>+</sup><span>&nbsp;</span>and SO<sub>4</sub><sup>2−</sup><span>&nbsp;</span>increases the unit cell size of calcites. The solid-solutions show a solubility minimum at about 0.5 mole percent SO<sub>4</sub><sup>2−</sup><span>&nbsp;</span>beyond which the solubility rapidly increases. The solubility product of calcites containing 3 mole percent SO<sub>4</sub><sup>2−</sup><span>&nbsp;</span>is the same as that of aragonite. Na<sup>+</sup><span>&nbsp;</span>appears to have very little effect on the solubility product of calcites. The amounts of Na<sup>+</sup><span>&nbsp;</span>and SO<sub>4</sub><sup>2−</sup><span>&nbsp;</span>incorporated in calcites vary as a function of the rate of crystal growth. The variation of the distribution coefficient (<span class=\"math\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>D</mtext></math>\"><span class=\"MJX_Assistive_MathML\">D</span></span></span>) of SO<sub>4</sub><sup>2−</sup><span>&nbsp;</span>in calcite at 25.0°C and 0.50 molal NaCl is described by the equation<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-2-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>D = k</mtext><msub><mi></mi><mn>0</mn></msub><mtext>+ k</mtext><msub><mi></mi><mn>1</mn></msub><mtext>R</mtext></math>\"><span class=\"MJX_Assistive_MathML\">D = k<sub>0</sub>+ k<sub>1</sub>R</span></span></span><span>&nbsp;</span>where<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-3-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>k</mtext><msub><mi></mi><mn>0</mn></msub></math>\"><span class=\"MJX_Assistive_MathML\">k<sub>0</sub></span></span></span><sub><span>&nbsp;</span></sub>and<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-4-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>k</mtext><msub><mi></mi><mn>1</mn></msub></math>\"><span class=\"MJX_Assistive_MathML\">k<sub>1</sub></span></span></span><span>&nbsp;</span>are constants equal to<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-5-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>6.16 &amp;#xD7; 10</mtext><msup><mi></mi><mn>&amp;#x2212;6</mn></msup></math>\"><span class=\"MJX_Assistive_MathML\">6.16 × 10<sup>−6</sup></span></span></span><span>&nbsp;</span>and<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-6-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>3.941 &amp;#xD7; 10</mtext><msup><mi></mi><mn>&amp;#x2212;6</mn></msup></math>\"><span class=\"MJX_Assistive_MathML\">3.941 × 10<sup>−6</sup></span></span></span>, respectively, and<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-7-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>R</mtext></math>\"><span class=\"MJX_Assistive_MathML\">R</span></span></span><span>&nbsp;</span>is the rate of crystal growth of calcite in mg·min<sup>−1</sup>·g<sup>−1</sup><span>&nbsp;</span>of seed. The data on Na<sup>+</sup><span>&nbsp;</span>are consistent with the hypothesis that a significant amount of Na<sup>+</sup><span>&nbsp;</span>occupies interstitial positions in the calcite structure. The distribution of Na<sup>+</sup><span>&nbsp;</span>follows a Freundlich isotherm and not the Berthelot-Nernst distribution law. The numerical value of the Na<sup>+</sup><span>&nbsp;</span>distribution coefficient in calcite is probably dependent on the number of defects in the calcite structure. The Na<sup>+</sup><span>&nbsp;</span>contents of calcites are not very accurate indicators of environmental salinities.</p></div></div></div></div><div id=\"preview-section-introduction\"><br></div><div id=\"preview-section-snippets\"><br></div><div id=\"preview-section-references\"><br></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(85)90166-8","issn":"00167037","usgsCitation":"Busenberg, E., and Plummer, N., 1985, Kinetic and thermodynamic factors controlling the distribution of SO32- and Na+ in calcites and selected aragonites: Geochimica et Cosmochimica Acta, v. 49, no. 3, p. 713-725, https://doi.org/10.1016/0016-7037(85)90166-8.","productDescription":"13 p.","startPage":"713","endPage":"725","numberOfPages":"13","costCenters":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"links":[{"id":222689,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"49","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a40a4e4b0c8380cd64f13","contributors":{"authors":[{"text":"Busenberg, E.","contributorId":56796,"corporation":false,"usgs":true,"family":"Busenberg","given":"E.","affiliations":[],"preferred":false,"id":364899,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":364900,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70013300,"text":"70013300 - 1985 - APPLICATIONS OF BOREHOLE-ACOUSTIC METHODS IN ROCK MECHANICS.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:38","indexId":"70013300","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"APPLICATIONS OF BOREHOLE-ACOUSTIC METHODS IN ROCK MECHANICS.","docAbstract":"Acoustic-logging methods using a considerable range of wavelengths and frequencies have proven very useful in the in situ characterization of deeply buried crystalline rocks. Seismic velocities are useful in investigating the moduli of unfractured rock, and in producing a continuous record of rock quality for comparison with discontinuous intervals of core. The considerable range of frequencies makes the investigation of scale effects possible in both fractured and unfractured rock. Several specific methods for the characterization of in situ permeability have been developed and verified in the field.","largerWorkTitle":"Proceedings - Symposium on Rock Mechanics","conferenceTitle":"Research & Engineering Applications in Rock Masses, Proceedings of the 26th US Symposium on Rock Mechanics.","conferenceLocation":"Rapid City, SD, USA","language":"English","publisher":"A. A. Balkema","publisherLocation":"Rotterdam, Neth","issn":"0085574X","isbn":"9061916011","usgsCitation":"Paillet, F.L., 1985, APPLICATIONS OF BOREHOLE-ACOUSTIC METHODS IN ROCK MECHANICS., <i>in</i> Proceedings - Symposium on Rock Mechanics, v. 1, Rapid City, SD, USA, p. 207-220.","startPage":"207","endPage":"220","numberOfPages":"14","costCenters":[],"links":[{"id":220247,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e631e4b0c8380cd4722c","contributors":{"authors":[{"text":"Paillet, Frederick L.","contributorId":63820,"corporation":false,"usgs":true,"family":"Paillet","given":"Frederick","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":365759,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":94757,"text":"94757 - 1985 - Fish recruitment and movement in a flood control reservoir and tailwater","interactions":[],"lastModifiedDate":"2012-02-02T00:15:14","indexId":"94757","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Fish recruitment and movement in a flood control reservoir and tailwater","docAbstract":"Abstract not submitted to date","language":"English","publisher":"U.S. Army Engineer Waterways Experiment Station","publisherLocation":"Vicksburg, MS","usgsCitation":"Jacobs, K., Swink, W., Nestler, J., and Curtis, L., 1985, Fish recruitment and movement in a flood control reservoir and tailwater, 62.","productDescription":"62","startPage":"62","numberOfPages":"62","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":201288,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5ef674","contributors":{"authors":[{"text":"Jacobs, K.E.","contributorId":57813,"corporation":false,"usgs":true,"family":"Jacobs","given":"K.E.","email":"","affiliations":[],"preferred":false,"id":298506,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swink, W.D.","contributorId":66200,"corporation":false,"usgs":true,"family":"Swink","given":"W.D.","affiliations":[],"preferred":false,"id":298507,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nestler, J.M.","contributorId":85685,"corporation":false,"usgs":true,"family":"Nestler","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":298509,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Curtis, L.T.","contributorId":71670,"corporation":false,"usgs":true,"family":"Curtis","given":"L.T.","email":"","affiliations":[],"preferred":false,"id":298508,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70013214,"text":"70013214 - 1985 - Validation of an automated fluorescein method for determining bromide in water","interactions":[],"lastModifiedDate":"2012-03-12T17:18:39","indexId":"70013214","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3716,"text":"Water Research","onlineIssn":"1879-2448","printIssn":"0043-1354","active":true,"publicationSubtype":{"id":10}},"title":"Validation of an automated fluorescein method for determining bromide in water","docAbstract":"Surface, atmospheric precipitation and deionized water samples were spiked with ??g l-1 concentrations of bromide, and the solutions stored in polyethylene and polytetrafluoroethylene bottles. Bromide was determined periodically for 30 days. Automated fluorescein and ion chromatography methods were used to determine bromide in these prepared samples. Analysis of the data by the paired t-test indicates that the two methods are not significantly different at a probability of 95% for samples containing from 0.015 to 0.5 mg l-1 of bromide. The correlation coefficient for the same sets of paired data is 0.9987. Recovery data, except for the surface water samples to which 0.005 mg l-1 of bromide was added, range from 89 to 112%. There appears to be no loss of bromide from solution in either type of container.Surface, atmospheric precipitation and deionized water samples were spiked with mu g l** minus **1 concentrations of bromide, and the solutions stored in polyethylene and polytetrafluoroethylene bottles. Bromide was determined periodically for 30 days. Automated fluorescein and ion chromatography methods were used to determine bromide in these prepared samples. Analysis of the data by the paired t-test indicates that the two methods are not significantly different at a probability of 95% for samples containing from 0. 015 to 0. 5 mg l** minus **1 of bromide. The correlation coefficient for the same sets of paired data is 0. 9987. Recovery data, except for the surface water samples to which 0. 005 mg l** minus **1 of bromide was added, range from 89 to 112%. Refs.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Water Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/0043-1354(85)90042-9","issn":"00431354","usgsCitation":"Fishman, M.J., Schroder, L., and Friedman, L., 1985, Validation of an automated fluorescein method for determining bromide in water: Water Research, v. 19, no. 4, p. 497-501, https://doi.org/10.1016/0043-1354(85)90042-9.","startPage":"497","endPage":"501","numberOfPages":"5","costCenters":[],"links":[{"id":204999,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0043-1354(85)90042-9"},{"id":220021,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc0fee4b08c986b32a3f6","contributors":{"authors":[{"text":"Fishman, M. J.","contributorId":65069,"corporation":false,"usgs":true,"family":"Fishman","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":365560,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schroder, L.J.","contributorId":31767,"corporation":false,"usgs":true,"family":"Schroder","given":"L.J.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":365558,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Friedman, L.C.","contributorId":57080,"corporation":false,"usgs":true,"family":"Friedman","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":365559,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012342,"text":"70012342 - 1985 - The transverse and oblique cylindrical equal-area projection of the ellipsoid.","interactions":[],"lastModifiedDate":"2013-03-12T21:00:11","indexId":"70012342","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":797,"text":"Annals of the Association of American Geographers","active":true,"publicationSubtype":{"id":10}},"title":"The transverse and oblique cylindrical equal-area projection of the ellipsoid.","docAbstract":"The formulas for the ellipsoidal projection are derived for both forward and inverse computations and consist of modifying the formulas obtained by using the authalic sphere so that the scale along the central line of the projection is constant. Fourier series are used to eliminate recurring numerical integration and other lengthy trigonometric computations of co-ordinates.-from Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Annals of the Association of American Geographers","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1467-8306.1985.tb00077.x","usgsCitation":"Snyder, J., 1985, The transverse and oblique cylindrical equal-area projection of the ellipsoid.: Annals of the Association of American Geographers, v. 75, no. 3, p. 431-442, https://doi.org/10.1111/j.1467-8306.1985.tb00077.x.","startPage":"431","endPage":"442","numberOfPages":"12","costCenters":[],"links":[{"id":222715,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269222,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1467-8306.1985.tb00077.x"}],"volume":"75","issue":"3","noUsgsAuthors":false,"publicationDate":"2010-03-15","publicationStatus":"PW","scienceBaseUri":"505bb13ae4b08c986b325285","contributors":{"authors":[{"text":"Snyder, J.P.","contributorId":79235,"corporation":false,"usgs":true,"family":"Snyder","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":363325,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012343,"text":"70012343 - 1985 - Wavelike movement of bedload sediment, East Fork River, Wyoming","interactions":[],"lastModifiedDate":"2012-03-12T17:18:47","indexId":"70012343","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1540,"text":"Environmental Geology and Water Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Wavelike movement of bedload sediment, East Fork River, Wyoming","docAbstract":"Bedload is moved down the East Fork River in distinct wavelike pulses that have the form of composite dune fields The moving material consists mostly of coarse sand and fine gravel The wavelengths of the pulses are about 500-600 m, a distance that is predetermined by the pattern of stoage of bed sediment in the river during low water As the river discharge increases, the bed sediment is scoured from the storage areas, and it is moved onto and across the interventing riffles As the river discharge decreases, the bed sediment is scoured off the riffles and moved into the next storage area downstream Each successive pulse of water discharge sets into motion a wave of bedload that continues to move unitil it reaches the next storage area ?? 1985 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Geology and Water Sciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF02509922","issn":"00990094","usgsCitation":"Meade, R., 1985, Wavelike movement of bedload sediment, East Fork River, Wyoming: Environmental Geology and Water Sciences, v. 7, no. 4, p. 215-225, https://doi.org/10.1007/BF02509922.","startPage":"215","endPage":"225","numberOfPages":"11","costCenters":[],"links":[{"id":205289,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02509922"},{"id":222716,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bcfa3e4b08c986b32ea06","contributors":{"authors":[{"text":"Meade, R.H.","contributorId":27449,"corporation":false,"usgs":true,"family":"Meade","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":363326,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70013092,"text":"70013092 - 1985 - MARINE MINERAL RESOURCES - AN UPDATE AND INTRODUCTION.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:25","indexId":"70013092","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2678,"text":"Marine Technology Society Journal","active":true,"publicationSubtype":{"id":10}},"title":"MARINE MINERAL RESOURCES - AN UPDATE AND INTRODUCTION.","docAbstract":"This article briefly traces the status of marine minerals development, and it describes papers presented in this special issue on the subject. Subjects covered include types of deposits, marine mining in Canada, Manganese nodules, metalliferous sulfides as seabed minerals, metallurgical processes for reducing sulfide minerals, U. S. phosphate industry, construction materials and placers, and industry problems.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Technology Society Journal","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00253324","usgsCitation":"Cruickshank, M.J., and Siapno, W., 1985, MARINE MINERAL RESOURCES - AN UPDATE AND INTRODUCTION.: Marine Technology Society Journal, v. 19, no. 4, p. 3-5.","startPage":"3","endPage":"5","numberOfPages":"3","costCenters":[],"links":[{"id":219776,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4ab7e4b0c8380cd68faa","contributors":{"authors":[{"text":"Cruickshank, Michael J.","contributorId":97627,"corporation":false,"usgs":true,"family":"Cruickshank","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":365265,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Siapno, William","contributorId":38278,"corporation":false,"usgs":true,"family":"Siapno","given":"William","email":"","affiliations":[],"preferred":false,"id":365264,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012344,"text":"70012344 - 1985 - Simulated fissioning of uranium and testing of the fission-track dating method","interactions":[],"lastModifiedDate":"2013-03-06T20:03:53","indexId":"70012344","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2913,"text":"Nuclear Tracks and Radiation Measurements (1982)","active":true,"publicationSubtype":{"id":10}},"title":"Simulated fissioning of uranium and testing of the fission-track dating method","docAbstract":"A computer program (FTD-SIM) faithfully simulates the fissioning of 238U with time and 235U with neutron dose. The simulation is based on first principles of physics where the fissioning of 238U with the flux of time is described by Ns = ??f 238Ut and the fissioning of 235U with the fluence of neutrons is described by Ni = ??235U??. The Poisson law is used to set the stochastic variation of fissioning within the uranium population. The life history of a given crystal can thus be traced under an infinite variety of age and irradiation conditions. A single dating attempt or up to 500 dating attempts on a given crystal population can be simulated by specifying the age of the crystal population, the size and variation in the areas to be counted, the amount and distribution of uranium, the neutron dose to be used and its variation, and the desired ratio of 238U to 235U. A variety of probability distributions can be applied to uranium and counting-area. The Price and Walker age equation is used to estimate age. The output of FTD-SIM includes the tabulated results of each individual dating attempt (sample) on demand and/or the summary statistics and histograms for multiple dating attempts (samples) including the sampling age. An analysis of the results from FTD-SIM shows that: (1) The external detector method is intrinsically more precise than the population method. (2) For the external detector method a correlation between spontaneous track count, Ns, and induced track count, Ni, results when the population of grains has a stochastic uranium content and/or when the counting areas between grains are stochastic. For the population method no correlation can exist. (3) In the external detector method the sampling distribution of age is independent of the number of grains counted. In the population method the sampling distribution of age is highly dependent on the number of grains counted. (4) Grains with zero-track counts, either in Ns or Ni, are in integral part of fissioning theory and under certain circumstances must be included in any estimate of age. (5) In estimating standard error of age the standard error of Ns and Ni and ?? must be accurately estimated and propagated through the age equation. Several statistical models are presently available to do so. ?? 1985.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Nuclear Tracks and Radiation Measurements (1982)","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0735-245X(85)90126-7","issn":"0735245X","usgsCitation":"McGee, V., Johnson, N., and Naeser, C.W., 1985, Simulated fissioning of uranium and testing of the fission-track dating method: Nuclear Tracks and Radiation Measurements (1982), v. 10, no. 3, p. 365-379, https://doi.org/10.1016/0735-245X(85)90126-7.","startPage":"365","endPage":"379","numberOfPages":"15","costCenters":[],"links":[{"id":221817,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268862,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0735-245X(85)90126-7"}],"volume":"10","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8fa8e4b08c986b319073","contributors":{"authors":[{"text":"McGee, V.E.","contributorId":36295,"corporation":false,"usgs":true,"family":"McGee","given":"V.E.","email":"","affiliations":[],"preferred":false,"id":363328,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, N.M.","contributorId":105429,"corporation":false,"usgs":true,"family":"Johnson","given":"N.M.","email":"","affiliations":[],"preferred":false,"id":363329,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Naeser, C. W.","contributorId":17582,"corporation":false,"usgs":true,"family":"Naeser","given":"C.","middleInitial":"W.","affiliations":[],"preferred":false,"id":363327,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012346,"text":"70012346 - 1985 - Scarp degraded by linear diffusion: Inverse solution for age","interactions":[],"lastModifiedDate":"2024-06-27T15:48:21.2876","indexId":"70012346","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6453,"text":"Journal of Geophysical Research Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Scarp degraded by linear diffusion: Inverse solution for age","docAbstract":"<p><span>Under the assumption that landforms unaffected by drainage channels are degraded according to the linear diffusion equation, a procedure is developed to invert a scarp profile to find its “diffusion age.” Diffusion age, having dimension [length]</span><sup>2</sup><span>, is the product of diffusivity times chronological age. The second moment of scarp slope grows linearly with age. This fact, together with an assumption about initial scarp shape, allows the inverse determination of diffusion age. Age found assuming a vertical initial scarp is termed “apparent age”; any nonvertical initial scarp profile has a nonzero initial apparent age. True diffusion age differs from apparent age by a fraction of scarp offset squared. The inverse procedure applied to synthetic data yields the following rules of thumb. Evidence of initial scarp shape has been lost when apparent age reaches twice its initial value. If a scarp is formed by two events, the inversion gives their offset-weighted-mean age with an error that is a fraction of offset squared. A scarp that appears to have been formed by one event may have been formed by two with an interval between them as large as apparent age. After scarps of two fault traces have diffused to appear as one, the error in inferred age may be as large as half the apparent age. Variation of apparent age along strike would indicate multiple fault traces. The simplicity of scarp profile measurement and this inversion makes profile analysis attractive. If linearity of the flow law, time for a free face to be reduced to the angle of repose, and variation of diffusivity with climate and material could be established, profile analysis would become a reliable dating technique.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB090iB12p10193","issn":"01480227","usgsCitation":"Andrews, D., and Hanks, T.C., 1985, Scarp degraded by linear diffusion: Inverse solution for age: Journal of Geophysical Research Solid Earth, v. 90, no. B12, p. 10193-10208, https://doi.org/10.1029/JB090iB12p10193.","productDescription":"16 p.","startPage":"10193","endPage":"10208","costCenters":[],"links":[{"id":221819,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"90","issue":"B12","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505b872ce4b08c986b316359","contributors":{"authors":[{"text":"Andrews, D.J.","contributorId":7416,"corporation":false,"usgs":true,"family":"Andrews","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":363331,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanks, Thomas C.","contributorId":35763,"corporation":false,"usgs":true,"family":"Hanks","given":"Thomas","middleInitial":"C.","affiliations":[],"preferred":false,"id":363332,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012699,"text":"70012699 - 1985 - Osmosis: A cause of apparent deviations from Darcy's law","interactions":[],"lastModifiedDate":"2023-08-31T16:32:16.030827","indexId":"70012699","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1166,"text":"Canadian Geotechnical Journal","active":true,"publicationSubtype":{"id":10}},"title":"Osmosis: A cause of apparent deviations from Darcy's law","docAbstract":"<p><span>Recent evidence for deviations from Darcy's law at very low gradients provides a reminder that the origin of similar deviations reported during the last three decades has not been fully clarified. In most of these studies, the potential significance of osmosis was not considered. This review of the existing evidence shows that osmosis causes intercepts in flow rate versus hydraulic gradient relationships that are consistent with the observed deviations from Darcy's law at very low gradients. Moreover, it is suggested that a natural cause of osmosis in laboratory samples could be chemical reactions such as those involved in aging effects. This hypothesis is analogous to the previously proposed occurrence of electroosmosis in nature generated by geochemical weathering reactions.&nbsp;</span></p>","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/t85-032","usgsCitation":"Olsen, H.W., 1985, Osmosis: A cause of apparent deviations from Darcy's law: Canadian Geotechnical Journal, v. 22, no. 2, p. 238-241, https://doi.org/10.1139/t85-032.","productDescription":"4 p.","startPage":"238","endPage":"241","numberOfPages":"4","costCenters":[],"links":[{"id":222738,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6a1ce4b0c8380cd73fda","contributors":{"authors":[{"text":"Olsen, Harold W.","contributorId":28985,"corporation":false,"usgs":true,"family":"Olsen","given":"Harold","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":364250,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012288,"text":"70012288 - 1985 - LORAN-C LATITUDE-LONGITUDE CONVERSION AT SEA: PROGRAMMING CONSIDERATIONS.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:04","indexId":"70012288","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"LORAN-C LATITUDE-LONGITUDE CONVERSION AT SEA: PROGRAMMING CONSIDERATIONS.","docAbstract":"Comparisons are made of the precision of arc-length routines as computer precision is reduced. Overland propagation delays are discussed and illustrated with observations from offshore New England. Present practice of LORAN-C error budget modeling is then reviewed with the suggestion that additional terms be considered in future modeling. Finally, some detailed numeric examples are provided to help with new computer program checkout.","conferenceTitle":"Proceedings of the National Technical Conference - Institute of Navigation.","conferenceLocation":"San Diego, CA, USA","language":"English","publisher":"Inst of Navigation","publisherLocation":"Washington, DC, USA","usgsCitation":"McCullough, J.R., Irwin, B.J., and Bowles, R.M., 1985, LORAN-C LATITUDE-LONGITUDE CONVERSION AT SEA: PROGRAMMING CONSIDERATIONS., Proceedings of the National Technical Conference - Institute of Navigation., San Diego, CA, USA, p. 127-153.","startPage":"127","endPage":"153","numberOfPages":"27","costCenters":[],"links":[{"id":222471,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a40efe4b0c8380cd65176","contributors":{"authors":[{"text":"McCullough, James R.","contributorId":95619,"corporation":false,"usgs":true,"family":"McCullough","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":363191,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Irwin, Barry J. birwin@usgs.gov","contributorId":3889,"corporation":false,"usgs":true,"family":"Irwin","given":"Barry","email":"birwin@usgs.gov","middleInitial":"J.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":363189,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bowles, Robert M.","contributorId":26447,"corporation":false,"usgs":true,"family":"Bowles","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":363190,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}