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F1-F90 :maps, diagrs., tables. ;24 cm.","costCenters":[],"links":[{"id":97159,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1133f/plate-1.pdf","size":"5825","linkFileType":{"id":1,"text":"pdf"}},{"id":97160,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1133f/plate-2.pdf","size":"114","linkFileType":{"id":1,"text":"pdf"}},{"id":97161,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1133f/plate-3.pdf","size":"121","linkFileType":{"id":1,"text":"pdf"}},{"id":97162,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1133f/plate-4.pdf","size":"111","linkFileType":{"id":1,"text":"pdf"}},{"id":167336,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1133f/report-thumb.jpg"},{"id":63938,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1133f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a81b3","contributors":{"authors":[{"text":"Stewart, J. 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(Contour interval 20 feet. 32 by 35 inches), https://doi.org/10.3133/ha46.","productDescription":"1 map. (Contour interval 20 feet. 32 by 35 inches)","costCenters":[],"links":[{"id":186277,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89992,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/046/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.06666666666666,39.9175 ], [ -82.06666666666666,39.98416666666667 ], [ -82,39.98416666666667 ], [ -82,39.9175 ], [ -82.06666666666666,39.9175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635e64","contributors":{"authors":[{"text":"Edelen, George W. Jr.","contributorId":107275,"corporation":false,"usgs":true,"family":"Edelen","given":"George","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":278257,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ruggles, Frederick H. Jr.","contributorId":40628,"corporation":false,"usgs":true,"family":"Ruggles","given":"Frederick","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":278256,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cross, William Perry","contributorId":21137,"corporation":false,"usgs":true,"family":"Cross","given":"William","email":"","middleInitial":"Perry","affiliations":[],"preferred":false,"id":278255,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":68450,"text":"ha45 - 1964 - Floods at Chillicothe, Ohio","interactions":[],"lastModifiedDate":"2012-02-10T00:11:26","indexId":"ha45","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"45","title":"Floods at Chillicothe, Ohio","language":"ENGLISH","doi":"10.3133/ha45","usgsCitation":"Edelen, G.W., Ruggles, F.H., and Cross, W.P., 1964, Floods at Chillicothe, Ohio: U.S. Geological Survey Hydrologic Atlas 45, 1 map. (Contour interval 10 and 20 feet. 28 by 32 inches), https://doi.org/10.3133/ha45.","productDescription":"1 map. (Contour interval 10 and 20 feet. 28 by 32 inches)","costCenters":[],"links":[{"id":186272,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89987,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/045/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.95083333333334,39.333333333333336 ], [ -82.95083333333334,39.333333333333336 ], [ -82.95083333333334,39.333333333333336 ], [ -82.95083333333334,39.333333333333336 ], [ -82.95083333333334,39.333333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e72b9","contributors":{"authors":[{"text":"Edelen, George W. Jr.","contributorId":107275,"corporation":false,"usgs":true,"family":"Edelen","given":"George","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":278244,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ruggles, Frederick H. Jr.","contributorId":40628,"corporation":false,"usgs":true,"family":"Ruggles","given":"Frederick","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":278243,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cross, William Perry","contributorId":21137,"corporation":false,"usgs":true,"family":"Cross","given":"William","email":"","middleInitial":"Perry","affiliations":[],"preferred":false,"id":278242,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70207358,"text":"70207358 - 1964 - Hidden Recharge","interactions":[],"lastModifiedDate":"2019-12-18T10:56:54","indexId":"70207358","displayToPublicDate":"1964-10-31T10:53:38","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1861,"text":"Ground Water","active":true,"publicationSubtype":{"id":10}},"title":"Hidden Recharge","docAbstract":"“Hidden recharge” is defined as subsurface percolation of water from basin‐margin mountains directly into aquifers of the valley basins. It is an important, and sometimes neglected, item in hydrologic equations. Locally, geologic conditions permit inter‐basin circulation of ground water. The concept that ground‐water basins necessarily terminate at the contact between alluvium and hardrock is not tenable. Copyright © 1964, Wiley Blackwell. All rights reserved
","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1745-6584.1964.tb01780.x","issn":" 0017467X","usgsCitation":"Feth, J.H., 1964, Hidden Recharge: Ground Water, v. 2, no. 4, p. 14-17 , https://doi.org/10.1111/j.1745-6584.1964.tb01780.x.","productDescription":"4 p. ","startPage":"14","endPage":"17 ","costCenters":[],"links":[{"id":370399,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Feth, J. H.","contributorId":50495,"corporation":false,"usgs":true,"family":"Feth","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":777803,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221136,"text":"70221136 - 1964 - The international hydrological decade","interactions":[],"lastModifiedDate":"2021-06-02T19:02:22.503469","indexId":"70221136","displayToPublicDate":"1964-09-01T13:59:52","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"The international hydrological decade","docAbstract":"Work toward establishing a program of international cooperative studies in scientific hydrology began about 4 years ago, and the IHD (International Hydrological Decade) will begin under international auspices in January 1965. This program will be highly important for hydrology and hydrologists, and it should contribute greatly to human welfare in the future. Fortuitously, the opening year coincides with International Cooperation Year of the United Nations Organization. American participation in the program will contribute to the purpose avowed by the President [Johnson, 1964] in a commencement address at Holy Cross early in June 1964: “to dedicate this year to finding new techniques for making Man's knowledge serve Man's welfare. Let this be a year of science.”
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR045i003p00413","usgsCitation":"Nace, R.L., 1964, The international hydrological decade: Eos, Transactions, American Geophysical Union, v. 45, no. 3, p. 413-421, https://doi.org/10.1029/TR045i003p00413.","productDescription":"9 p.","startPage":"413","endPage":"421","costCenters":[],"links":[{"id":386151,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Nace, R. L.","contributorId":11332,"corporation":false,"usgs":true,"family":"Nace","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":816828,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221177,"text":"70221177 - 1964 - Geohydrologic analogies between the Jordan Valleys of Utah and the holy land","interactions":[],"lastModifiedDate":"2021-06-04T17:05:35.301848","indexId":"70221177","displayToPublicDate":"1964-09-01T12:01:39","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5334,"text":"International Association of Scientific Hydrology - Bulletin ","onlineIssn":"2150-3435","printIssn":"0262-6667","active":false,"publicationSubtype":{"id":10}},"title":"Geohydrologic analogies between the Jordan Valleys of Utah and the holy land","docAbstract":"The biblical Jordan River Valley, which extends from Lake Tiberias (the Sea of Galilee) to the Dead Sea, is decidedly similar to the Jordan River Valley of Utah, which joins Lake Utah and Great Salt Lake. Both Jordan Rivers drain relatively large fresh-water lakes and also are major sources of discharge into large salty lakes that have no outlets to the ocean.The two Jordan River valleys and the highlands and mountains that surround them, have many physiographic, geologic, and hydrologic similarities as well as some noteworthy differences. For example, an hypothesis for the formation of the Dead Sea-Jordan Valley rift is that the east Jordan block slid northward with respect to the west Jordan block. The amount of displacement is estimated to be about 65 miles and took place partly in Miocene and possible Pliocène and partly in Pleistocene time. Tectonc activity has also been a major factor in the formation of the Jordan valley of Utah, but the movement here probably was along large normal faults in late Tertiary and Quaternary time. The sediments underlying both Jordan River valleys were deposited in ancestral lacustrine and fluvial environments. Abundant supplies of ground water are found under both valleys, but probably larger supplies of better quality water can be obtained in Utah. Both valleys contain numerous small nonthermal and a few large thermal springs.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666409493666","usgsCitation":"Bradley, E., 1964, Geohydrologic analogies between the Jordan Valleys of Utah and the holy land: International Association of Scientific Hydrology - Bulletin , v. 9, no. 3, p. 12-23, https://doi.org/10.1080/02626666409493666.","productDescription":"12 p.","startPage":"12","endPage":"23","costCenters":[],"links":[{"id":489070,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666409493666","text":"Publisher Index Page"},{"id":386209,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.06005859375,\n 42.00032514831621\n ],\n [\n -114.0380859375,\n 37.07271048132943\n ],\n [\n -109.05029296875,\n 37.03763967977139\n ],\n [\n -109.1162109375,\n 41.0130657870063\n ],\n [\n -111.07177734375,\n 41.02964338716638\n ],\n [\n -111.07177734375,\n 41.983994270935625\n ],\n [\n -114.06005859375,\n 42.00032514831621\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"9","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bradley, Edward","contributorId":67071,"corporation":false,"usgs":true,"family":"Bradley","given":"Edward","email":"","affiliations":[],"preferred":false,"id":816980,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221179,"text":"70221179 - 1964 - The father of modern ground water hydrology","interactions":[],"lastModifiedDate":"2021-06-04T17:17:06.636524","indexId":"70221179","displayToPublicDate":"1964-04-01T12:14:32","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"The father of modern ground water hydrology","docAbstract":"No abstract available.
","language":"English","publisher":"Elsevier","doi":"10.1111/j.1745-6584.1964.tb01749.x","usgsCitation":"Hackett, O.M., 1964, The father of modern ground water hydrology: Groundwater, v. 2, no. 2, p. 2-5, https://doi.org/10.1111/j.1745-6584.1964.tb01749.x.","productDescription":"4 p.","startPage":"2","endPage":"5","costCenters":[],"links":[{"id":386213,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"2","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Hackett, O. M.","contributorId":38527,"corporation":false,"usgs":true,"family":"Hackett","given":"O.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":816986,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010471,"text":"70010471 - 1964 - Tritium-hydrologic research: Some results of the U.S. Geological Survey Research Program","interactions":[],"lastModifiedDate":"2026-02-13T16:21:12.862036","indexId":"70010471","displayToPublicDate":"1964-02-02T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Tritium-hydrologic research: Some results of the U.S. Geological Survey Research Program","docAbstract":"In general tritium is of limited usefulness as a tool in hydrologic studies because the tritium content of ground water, as a result of radioactive decay, becomes too low to be detectable after about 50 years. Nevertheless, a unique study was made of the hydrologic cycle of small stream basins in Wisconsin and New Jersey on the basis of measurements relative to the peak of tritium fallout in the spring of 1958. The continental and the coastal basins received approximately the same tritium fallout. Approximately 30 percent went into ground-water storage, the remainder being exported as runoff and evapotranspiration. The mean residence time for ground-water recharge for the two basins was 45 and 30 days, respectively.","language":"English","publisher":"American Association for the Advancement of Science.","doi":"10.1126/science.143.3608.804","issn":"00368075","usgsCitation":"Carlston, C., 1964, Tritium-hydrologic research: Some results of the U.S. Geological Survey Research Program: Science, v. 143, no. 3608, p. 804-806, https://doi.org/10.1126/science.143.3608.804.","productDescription":"3 p.","startPage":"804","endPage":"806","costCenters":[],"links":[{"id":219076,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Jersey, Wisconsin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -92.65443024683039,\n 47.18686471532902\n ],\n [\n -92.92337344008368,\n 44.76948314682184\n ],\n [\n -91.54422384565291,\n 43.91380985726313\n ],\n [\n -90.40331265602809,\n 42.36186629934298\n ],\n [\n -87.66640475516137,\n 42.473317234890345\n ],\n [\n -86.69378362897187,\n 45.09478563580936\n ],\n [\n -87.76789223463291,\n 45.99366780802788\n ],\n [\n -89.9402097973789,\n 46.41028342019218\n ],\n [\n -89.94150082434655,\n 47.33914537549116\n ],\n [\n -92.65443024683039,\n 47.18686471532902\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -75.03044920156037,\n 41.368918438639554\n ],\n [\n -75.21217801383332,\n 40.6314679025723\n ],\n [\n -74.81474599562263,\n 40.24767874671271\n ],\n [\n -75.6121640073091,\n 39.468177148463866\n ],\n [\n -74.80122580215662,\n 38.82749379603797\n ],\n [\n -74.0060957836949,\n 40.04453424272181\n ],\n [\n -73.96363933005574,\n 41.368918438639554\n ],\n [\n -75.03044920156037,\n 41.368918438639554\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"143","issue":"3608","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb875e4b08c986b327884","contributors":{"authors":[{"text":"Carlston, C.W.","contributorId":26062,"corporation":false,"usgs":true,"family":"Carlston","given":"C.W.","affiliations":[],"preferred":false,"id":358994,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70095523,"text":"70095523 - 1964 - Sedimentology: general introduction and definitions : fluvial sediment and channel morphology","interactions":[],"lastModifiedDate":"2014-03-25T10:35:32","indexId":"70095523","displayToPublicDate":"1964-01-01T13:52:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Sedimentology: general introduction and definitions : fluvial sediment and channel morphology","docAbstract":"Sedimentology, the study of sedimentary rocks and the \nprocesses by which they are formed, includes and is related \nto a large number of phenomena. Sedimentology includes the \nfive fundamental processes defined by the term sediaentation \n--weathering, erosion, transportation, deposition and \ndiagenesis. \nSedimentology shares with geomorphology the study of \nthe surface features of the earth. Sedimentology also \nshares with hydrology the study of river.--channels. River \nchannels are formed in part or in total as a result of \nflowing water and sediment transport, commonly called the \n\"work of the rivers.\" \nThis survey of published literature was made to aid in \narriving at definitions which would be acceptable to, and \nrepresentative of, a majority of professional personnel \nactively engaged in laboratory and field investigations \nrelated to the \"work of the river.\" The definitions in this \nlist are intended to explain the terms used in studies of \nfluvial sediment and channel morphology. No set of \ndefinitions can expect universal acceptance, however, i t is \nhoped that this compilation will be considered a summary \nand synthesis of present and past usage and that it will \nserve as a starting point for future usage. \nMultiple references are cited from textbooks, glossaries and dictionaries, scientific journals and u.s. Government \npublications. To obtain a mutual understanding and enhance \nprecision, many of the proposed definitions are a composite \nof those selected from papers or reports covering research \nstudies and field investigations. \n\nA draft of this glossary has been reviewed by a group of \ninterested personnel. The results of this review have been \ncarefully considered and the originally-suggested definitions \nhave been revised accordingly, resulting in the present \ncompilation. \nR. G. Wolff, with the help of Mrs. v. Blatcher, carried \nout the literature search and compilation of terms and the \nreview results. Paul c. Benedict approved or composed the \ndefinitions as presented in this report.","language":"English","publisher":"U.S. Geological Survey, Water Resources Division","publisherLocation":"Washington, DC","doi":"10.3133/70095523","usgsCitation":"Wolff, R.G., and Benedict, P., 1964, Sedimentology: general introduction and definitions : fluvial sediment and channel morphology: Open-File Report, iii, 132 p., https://doi.org/10.3133/70095523.","productDescription":"iii, 132 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":283310,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70095523.jpg"},{"id":284835,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70095523/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5355955fe4b0120853e8c1d4","contributors":{"authors":[{"text":"Wolff, Roger G.","contributorId":19580,"corporation":false,"usgs":true,"family":"Wolff","given":"Roger","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":491227,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Benedict, Paul C.","contributorId":72293,"corporation":false,"usgs":true,"family":"Benedict","given":"Paul C.","affiliations":[],"preferred":false,"id":491228,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70094923,"text":"70094923 - 1964 - Soil mechanics and soil physics symbols and nomenclature useful in hydrologic studies","interactions":[],"lastModifiedDate":"2014-02-25T13:59:49","indexId":"70094923","displayToPublicDate":"1964-01-01T13:50:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Soil mechanics and soil physics symbols and nomenclature useful in hydrologic studies","docAbstract":"The study of hydrology requires an interdisciplinary approach,\nincorporating knowledge from fields such as engineering, geology,\nchemistry, and agriculture. With increasing frequency, the hydrologist\nfinds it necessary to study the literature of the soil mechanics and\nsoil physics disciplines for assistance in the solution of hydrologic\nproblems. Because of the inter-relation between hydrology and soil\nmechanics and soil physics, hydrologists also are preparing an increasing\nnumber of technical papers ·for use by these two disciplines.\nTo permit the hydrologist to better understand specialized literature,\nas well as to assist him in preparing papers for these disciplines,\nthis glossary of soil mechanics and soil physics nomenclature was prepared.\nIt is a compilation from standards, dictionaries, and glossaries published\nby technical societies, and from reports by selected authorities in the\nfields of soil mechanics and soil physics. The variety of symbols and\ndefinitions presented for many of the terms demonstrates the difficulty\nthat has been encountered over the years in reaching agreement on such a\nsubject as nomenclature. Both old and new definitions and symbols are\npresented to assist the hydrologist in reading literature. Whenever\npossible the more recent symbols and nomenclature should be used by the\nhydrologist in writing papers for soil mechanics or soil physics audiences.\nWhen the hydrologist finds it necessary to use symbols or terms not included\nin the present list, he should try to select those not in conflict with the\nrecent systems presented in this report.\nSymbols are listed in alphabetical order to assist readers in finding\nthe term represented by a given symbol. Terms also are listed alphabetically,\nusually followed by recommended symbols and brief definitions.\nWhere two or more symbols or definitions are listed following a term, no\nsignificance should be placed on the order of presentation. The source is\nindicated for each symbol, term, or definition, and the sources are listed\nin the cited references.\nIt is emphasized that this report is only a compilation of nomenclature\ngenerally accepted in the soil mechanics apd soil physics disciplines.\nIt does not necessarily represent the recommendations or usage of such\nnomenclature by the Geological Survey or any part of its organization.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/70094923","usgsCitation":"Johnson, A., 1964, Soil mechanics and soil physics symbols and nomenclature useful in hydrologic studies: Open-File Report, 50 p., https://doi.org/10.3133/70094923.","productDescription":"50 p.","numberOfPages":"53","costCenters":[],"links":[{"id":282776,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70094923.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd732ce4b0b29085108c64","contributors":{"authors":[{"text":"Johnson, A.I.","contributorId":82676,"corporation":false,"usgs":true,"family":"Johnson","given":"A.I.","email":"","affiliations":[],"preferred":false,"id":490965,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221132,"text":"70221132 - 1964 - Hydrologic factors pertinent to ground‐water contamination","interactions":[],"lastModifiedDate":"2021-06-04T12:04:08.414151","indexId":"70221132","displayToPublicDate":"1964-01-01T13:47:53","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Hydrologic factors pertinent to ground‐water contamination","docAbstract":"Predictions of where and how a fluid waste may travel from disposal site to the water table require detailed information on the physical characteristics, location, and extent of all pervious and impervious materials in the unsaturated zone. Principles concerning the flow system in the unsaturated zone indicate the importance of choice of disposal technique in predicting the time required for the fluid waste to traverse the distance to the water table. With appropriate data on the location, extent, and physical properties of water‐bearing materials and on the boundaries of the saturated zone flow system, it is possible to analyze the relative merits of a variety of waste disposal techniques and to describe the probable consequences of each. Environments of consolidated rocks, such as granites, sandstones, and limestones, pose problems in addition to those related to unconsolidated or granular porous media in defining the fluid‐flow regimes that involve joint patterns, fracture patterns, solutional openings, and the rock structure. The consequences of ground‐water contamination can be just as damaging to water users as the pollution of surface streams. In fact it can be argued that the consequences are far more damaging because they persist over much longer periods of time after the contaminating source has been eliminated. It would appear prudent, therefore, to guard against contamination of the ground‐water resource in the first instance, rather than to engage in long expensive rehabilitation measures after the damage has been done. In 1960 Graham Walton presented data concerning contamination, by sewage or other man‐made wastes, of surface and underground waters. The circumstances attending the reported incidents of contamination, especially those involving ground‐water supplies, have aided materially in the choice of a few principles and ideas that will identify the role of some significant hydrologic factors in the underground movement of fluid wastes. Walton's discussion of ground‐water contamination refers often to physical settings into which fluid wastes are discharged at or near the land surface into cesspools, tile‐drain fields, and holding ponds. Furthermore, most reported instances of ground‐water contamination have taken place in relatively humid.
","language":"English","publisher":"NGWA The Groundwater Association","doi":"10.1111/j.1745-6584.1964.tb01739.x","usgsCitation":"Brown, R., 1964, Hydrologic factors pertinent to ground‐water contamination: Groundwater, v. 2, no. 1, p. 5-12, https://doi.org/10.1111/j.1745-6584.1964.tb01739.x.","productDescription":"8 p.","startPage":"5","endPage":"12","costCenters":[],"links":[{"id":386191,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Brown, R.","contributorId":101419,"corporation":false,"usgs":true,"family":"Brown","given":"R.","affiliations":[],"preferred":false,"id":816940,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221133,"text":"70221133 - 1964 - Hydrologic factors pertinent to ground‐water contamination","interactions":[],"lastModifiedDate":"2021-06-02T18:50:54.556763","indexId":"70221133","displayToPublicDate":"1964-01-01T13:47:53","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Hydrologic factors pertinent to ground‐water contamination","docAbstract":"Predictions of where and how a fluid waste may travel from disposal site to the water table require detailed information on the physical characteristics, location, and extent of all pervious and impervious materials in the unsaturated zone. Principles concerning the flow system in the unsaturated zone indicate the importance of choice of disposal technique in predicting the time required for the fluid waste to traverse the distance to the water table. With appropriate data on the location, extent, and physical properties of water‐bearing materials and on the boundaries of the saturated zone flow system, it is possible to analyze the relative merits of a variety of waste disposal techniques and to describe the probable consequences of each. Environments of consolidated rocks, such as granites, sandstones, and limestones, pose problems in addition to those related to unconsolidated or granular porous media in defining the fluid‐flow regimes that involve joint patterns, fracture patterns, solutional openings, and the rock structure. The consequences of ground‐water contamination can be just as damaging to water users as the pollution of surface streams. In fact it can be argued that the consequences are far more damaging because they persist over much longer periods of time after the contaminating source has been eliminated. It would appear prudent, therefore, to guard against contamination of the ground‐water resource in the first instance, rather than to engage in long expensive rehabilitation measures after the damage has been done. In 1960 Graham Walton presented data concerning contamination, by sewage or other man‐made wastes, of surface and underground waters. The circumstances attending the reported incidents of contamination, especially those involving ground‐water supplies, have aided materially in the choice of a few principles and ideas that will identify the role of some significant hydrologic factors in the underground movement of fluid wastes. Walton's discussion of ground‐water contamination refers often to physical settings into which fluid wastes are discharged at or near the land surface into cesspools, tile‐drain fields, and holding ponds. Furthermore, most reported instances of ground‐water contamination have taken place in relatively humid.
","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1745-6584.1964.tb01739.x","usgsCitation":"Brown, R., 1964, Hydrologic factors pertinent to ground‐water contamination: Groundwater, v. 2, no. 1, p. 5-12, https://doi.org/10.1111/j.1745-6584.1964.tb01739.x.","productDescription":"8 p.","startPage":"5","endPage":"12","costCenters":[],"links":[{"id":386147,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Brown, R.","contributorId":101419,"corporation":false,"usgs":true,"family":"Brown","given":"R.","affiliations":[],"preferred":false,"id":816821,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010816,"text":"70010816 - 1964 - Ground water in North America","interactions":[],"lastModifiedDate":"2017-03-27T12:47:37","indexId":"70010816","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Ground water in North America","docAbstract":"The fast-growing demands on this natural resource expose a need to resolve many hydrologic unknowns.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.143.3610.1001","issn":"00368075","usgsCitation":"Thomas, H.E., and Leopold, L.B., 1964, Ground water in North America: Science, v. 143, no. 3610, p. 1001-1006, https://doi.org/10.1126/science.143.3610.1001.","productDescription":"6 p.","startPage":"1001","endPage":"1006","costCenters":[],"links":[{"id":218743,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"North America","volume":"143","issue":"3610","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2ad0e4b0c8380cd5b4a7","contributors":{"authors":[{"text":"Thomas, Harold E.","contributorId":36116,"corporation":false,"usgs":true,"family":"Thomas","given":"Harold","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":359714,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":359715,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}