The present is the second of the series of reports on the collection of deep-well samples, the first of which, covering the period from the beginning of the work July 1, 1904, to December 31, 1904, was published as Bulletin No. 264. This report presents the records of a large number of wells from which more or less complete sets of samples have been secured and placed on file at the Survey, and. also many additional records not represented by samples.
The work has been conducted by the eastern section, division of hydrology, the expense being shared with the western section of hydrology and the geologic branch. The writer has continued in charge of the investigations and has been assisted by Messrs. E. F. Lines and Samuel Sanford. The burden of executive details has fallen mainly on Mr. Sanford since his assignment to the work on its relinquishment by Mr. Lines April 1. The methods followed are in most particulars those formulated by Mr. A. C. Veatch on the inauguration of the work in 1904, but to Mr. Sanford is due the credit for materially increasing the usefulness of the work to the driller, especially in furnishing geologic information.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/b298","usgsCitation":"Fuller, M.L., and Sanford, S., 1906, Record of deep-well drilling for 1905: U.S. Geological Survey Bulletin 298, 299 p., https://doi.org/10.3133/b298.","productDescription":"299 p.","numberOfPages":"299","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":167766,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0298/report-thumb.jpg"},{"id":22493,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0298/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a91be","contributors":{"authors":[{"text":"Fuller, Myron Leslie","contributorId":106091,"corporation":false,"usgs":true,"family":"Fuller","given":"Myron","email":"","middleInitial":"Leslie","affiliations":[],"preferred":false,"id":213001,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sanford, Samuel","contributorId":45687,"corporation":false,"usgs":true,"family":"Sanford","given":"Samuel","email":"","affiliations":[],"preferred":false,"id":213000,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70098436,"text":"ar27 - 1906 - Twenty-seventh annual report of the Director of the United States Geological Survey","interactions":[],"lastModifiedDate":"2015-09-03T10:40:44","indexId":"ar27","displayToPublicDate":"1910-01-01T14:29:00","publicationYear":"1906","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":304,"text":"Annual Report","code":"AR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"27","title":"Twenty-seventh annual report of the Director of the United States Geological Survey","docAbstract":"During the last fiscal year the character of the work and the organization of the force remained substantially the same as described in the Twenty-sixth Annual Report. Accounts of the work performed in geology and paleontology, chemistry and physics, topography and geography, and hydrography, hydrology, and hydro-economics, as well as in the lines of publication and administration, will be found on later pages.
\n\n
Appropriations and allotments.--A plan of operations, including an itemized statement of the appropriations, amounting to $1,513,482.30, and the allotments thereof, was approved by the Secretary of the Interior on May 15, 1905. The work of the year conformed to this plan, copies of which are on file at the Department and the Survey.
\n\n
State cooperation.--Many of the States, following a well-established policy, cooperated with the National Survey in geologic, topographic, and hydrographic work; details are given on pages 12, 29, 72, and 74.
","language":"English","publisher":"Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/ar27","usgsCitation":"Walcott, C.D., 1906, Twenty-seventh annual report of the Director of the United States Geological Survey: U.S. Geological Survey Annual Report 27, 104 p., https://doi.org/10.3133/ar27.","productDescription":"104 p.","numberOfPages":"128","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":284181,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ar27.jpg"},{"id":285318,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ar/0027/report.pdf"}],"country":"United 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States\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"535595d3e4b0120853e8c2b4","contributors":{"authors":[{"text":"Walcott, Charles D.","contributorId":7738,"corporation":false,"usgs":true,"family":"Walcott","given":"Charles","email":"","middleInitial":"D.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":491721,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1248,"text":"wsp149 - 1905 - Preliminary list of deep borings in the United States","interactions":[],"lastModifiedDate":"2017-09-12T07:57:57","indexId":"wsp149","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1905","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"149","title":"Preliminary list of deep borings in the United States","docAbstract":"The first preliminary list of deep borings in the United States was issued as Water-Supply Papers Nos. 57 and 61. The present publication includes all of the wells listed in these two papers, together with many additional borings, mostly of recent date. Messrs. M. L. Fuller and A. C. Veatch, of the eastern section of hydrology, and other geologists of the Survey have contributed many new data. Descriptions of borings published in reports issued since 1901 have been incorporated as far as practicable. All the entries are by counties. The wells and borings reported in the paper are all more than 400 feet in depth. The information concerning them has been obtained partly from replies to circular letters sent to all parts of the United States and partly from geological reports and other published sources. Owing to the difficulty of obtaining replies to the circulars, to lack of knowledge on the part of correspondents, and to the incompleteness of published records, doubtless there are borings which have not been reported. In regions of oil and gas wells, where borings are numerous, the individual wells can not be listed here, but representative wells are given. References to logs or records of the wells or extended descriptions of them are given in footnotes, and after the list of wells in each State there is added a list of the principal publications relating to deep borings in that State.
The bearing of the information given in the columns of the lists probably is apparent unless, perhaps, in the one headed \"Height to which the water rises.\" In this column an entry such as \"-45\" indicates that the water rises to within 45 feet of the surface; \"+45\" indicates that it is a flowing well and has sufficient head to raise the water 45 feet above the surface in an open pipe 45 feet or more in height. The yield in gallons per minute usually is estimated. Depths and diameters often have been reported from memory and different sources of publication sometimes give different figures. Most wells which are not stated to be \"for oil,\" \"for gas,\" \"brine,\" \"abandoned,\" etc., in the remarks column, or \"not any\" in the yield column, generally afford more or less water. Many of the gas and oil wells, active or abandoned, yield salt water.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp149","usgsCitation":"Darton, N.H., 1905, Preliminary list of deep borings in the United States (2d ed. with additions.): U.S. Geological Survey Water Supply Paper 149, 175 p., https://doi.org/10.3133/wsp149.","productDescription":"175 p.","numberOfPages":"180","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":26178,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0149/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137257,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0149/report-thumb.jpg"}],"country":"United States","edition":"2d ed. with additions.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d96f","contributors":{"authors":[{"text":"Darton, Nelson Horatio","contributorId":78307,"corporation":false,"usgs":true,"family":"Darton","given":"Nelson","email":"","middleInitial":"Horatio","affiliations":[],"preferred":false,"id":143436,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1442,"text":"wsp110 - 1905 - Contributions to the hydrology of eastern United States, 1904","interactions":[],"lastModifiedDate":"2012-02-02T00:05:14","indexId":"wsp110","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1905","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"110","title":"Contributions to the hydrology of eastern United States, 1904","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp110","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1905, Contributions to the hydrology of eastern United States, 1904: U.S. Geological Survey Water Supply Paper 110, 211 p. ;23 cm., https://doi.org/10.3133/wsp110.","productDescription":"211 p. ;23 cm.","costCenters":[],"links":[{"id":137062,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0110/report-thumb.jpg"},{"id":26535,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0110/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db691294","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527846,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1443,"text":"wsp145 - 1905 - Contributions to the hydrology of Eastern United States, 1905","interactions":[],"lastModifiedDate":"2012-02-02T00:05:14","indexId":"wsp145","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1905","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"145","title":"Contributions to the hydrology of Eastern United States, 1905","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp145","usgsCitation":"Fuller, M.L., 1905, Contributions to the hydrology of Eastern United States, 1905: U.S. Geological Survey Water Supply Paper 145, 220 p. :ill., maps ;23 cm., https://doi.org/10.3133/wsp145.","productDescription":"220 p. :ill., maps ;23 cm.","costCenters":[],"links":[{"id":137063,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0145/report-thumb.jpg"},{"id":26536,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0145/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a7a0","contributors":{"authors":[{"text":"Fuller, M. 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Under the latter term is included that general lowland area which is definitely limited on the north by the San Gabriel and San Bernardino ranges and on the east by the latter range and the San Jacinto group, but whose southern boundary is irregular and difficult to define. In this direction there is an interdigitation of ridges and valleys as the Sierra Madre Range of San Diego County dies out toward the north. The more or less indefinite heights that represent its extension in this direction are separated by lowlands, which in turn are to be regarded as southwest lobes of the well-defined east-west valley that lies along the base of the San Gabriel Range.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp142","usgsCitation":"Mendenhall, W., 1905, The hydrology of San Bernardino Valley, California: U.S. Geological Survey Water Supply Paper 142, Report: 124 p.; 3 Plates: 31.51 x 19.81 inches or smaller, https://doi.org/10.3133/wsp142.","productDescription":"Report: 124 p.; 3 Plates: 31.51 x 19.81 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":316470,"rank":301,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0142/plate-7.pdf","text":"Plate 7","linkFileType":{"id":1,"text":"pdf"}},{"id":28110,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0142/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":316472,"rank":303,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0142/plate-12.pdf","text":"Plate 12","linkFileType":{"id":1,"text":"pdf"}},{"id":316471,"rank":302,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0142/plate-8.pdf","text":"Plate 8","linkFileType":{"id":1,"text":"pdf"}},{"id":409828,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24374.htm","linkFileType":{"id":4,"text":"shapefile"}},{"id":137674,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0142/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Bernardino Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117.5,\n 34\n ],\n [\n -117.5,\n 34.25\n ],\n [\n -117,\n 34.25\n ],\n [\n -117,\n 34\n ],\n [\n -117.5,\n 34\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a85e4b07f02db64d787","contributors":{"authors":[{"text":"Mendenhall, Walter C.","contributorId":34988,"corporation":false,"usgs":true,"family":"Mendenhall","given":"Walter C.","affiliations":[],"preferred":false,"id":144973,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1441,"text":"wsp102 - 1904 - Contributions to the hydrology of eastern United States, 1903","interactions":[],"lastModifiedDate":"2012-02-02T00:05:14","indexId":"wsp102","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1904","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"102","title":"Contributions to the hydrology of eastern United States, 1903","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp102","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1904, Contributions to the hydrology of eastern United States, 1903: U.S. Geological Survey Water Supply Paper 102, 522 p. ;23 cm., https://doi.org/10.3133/wsp102.","productDescription":"522 p. ;23 cm.","costCenters":[],"links":[{"id":137061,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0102/report-thumb.jpg"},{"id":26534,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0102/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db691272","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527845,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70206199,"text":"70206199 - null - Cross-borehole flow tests and insights into hydraulic connections in fractured mudstone and sandstone","interactions":[],"lastModifiedDate":"2020-03-10T14:58:10","indexId":"70206199","displayToPublicDate":"2007-12-31T15:11:34","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Cross-borehole flow tests and insights into hydraulic connections in fractured mudstone and sandstone","docAbstract":"Cross-borehole flow tests provided insights into hydraulic connections in fractured and dipping mudstone and sandstone that were consistent with the lithostratigraphic and structural framework of a VOCcontaminated bedrock research site in west-central New Jersey. Two cross-borehole flow tests were completed. Each test involved measurement and analysis of transient flow in a newly installed deep corehole with a long open interval during short-term pumping and recovery in an adjacent shallow well with a short open interval. The cross-borehole flow test in the mudstone identified a hydraulic connection through a dipping fractured bed between the pumped interval in the well and a flow zone at an intermediate depth in the corehole. The presence of a hydraulic connection between the pumped well and the corehole was not obvious because the water-level response in the corehole was dominated by a shallow zone of high transmissivity, which was hydraulically isolated from the pumped interval. In the sandstone, the cross-borehole flow test identified a hydraulic connection along dipping fractured beds as well as a connection to a deep high-angle fracture that cuts across bedding. These results suggest that application of cross-borehole flow tests at other contaminated fractured-bedrock sites could provide insights into hydraulic connections useful the design and implementation of monitoring and remediation programs.
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John 0000-0002-6054-6908 jhwillia@usgs.gov","orcid":"https://orcid.org/0000-0002-6054-6908","contributorId":1553,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"jhwillia@usgs.gov","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":773829,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lacombe, Pierre 0000-0002-9596-7622 placombe@usgs.gov","orcid":"https://orcid.org/0000-0002-9596-7622","contributorId":152113,"corporation":false,"usgs":true,"family":"Lacombe","given":"Pierre","email":"placombe@usgs.gov","affiliations":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"preferred":true,"id":773830,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, Carole D. 0000-0001-6941-1578 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aquifer","interactions":[],"lastModifiedDate":"2019-10-14T14:38:34","indexId":"70205983","displayToPublicDate":"2006-10-14T14:38:13","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3420,"text":"Soil Science Society of America Journal","active":true,"publicationSubtype":{"id":10}},"title":"Characterizing the two-dimensional thermal conductivity distribution in a sand and gravel aquifer","docAbstract":"Both hydrologic and thermal transport properties play a significant role in the movement of heat through permeable sedimentary material; however, the thermal conductivity is rarely characterized in detailed spatial resolution. As part of a study of the movement of thermal plumes through a sand and gravel aquifer, we have constructed a two-dimensional profile of thermal conductivity. This work consisted of: (i) measuring the thermal conductivity of the soil solids, λs, for the main stratigraphic units using the steady-state divided-bar apparatus and estimating conductivity from mineral composition; (ii) measuring the volumetric water content and porosity using crosshole ground-penetrating radar; (iii) evaluating four models used to predict the apparent thermal conductivity, λ, of variably saturated soils and selecting the best model using the information-theoretic approach, (iv) calculating the λ field on a 0.25-m square cell grid using measured data and the selected model, and (v) simulating thermal transport within the two-dimensional domain using a finite element numerical model. The apparent thermal conductivity in the saturated aquifer ranges from 2.14 to 2.69 W m−1 K−1 with a mean of 2.42 W m−1 K−1 Numerical simulations show that the heterogeneous thermal conductivity field results in increased thermal dispersion that is most pronounced at the plume front. Our values for λ and λs may be used for glacial soils with similar mineralogy and texture. Our methods may also be used at other sites to construct the thermal conductivity distribution.
","doi":"10.2136/sssaj2005.0293","usgsCitation":"Markle, J.M., Schincariol, R.A., Sass, J., and Molson, J.W., Characterizing the two-dimensional thermal conductivity distribution in a sand and gravel aquifer: Soil Science Society of America Journal, v. 70, no. 4, p. 1281-1294, https://doi.org/10.2136/sssaj2005.0293.","productDescription":"14 p.","startPage":"1281","endPage":"1294","costCenters":[],"links":[{"id":368310,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada","state":"Ontario","otherGeospatial":"Tricks Creek Watershed ","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.0458984375,\n 43.52266348752663\n ],\n [\n -81.6998291015625,\n 43.52266348752663\n ],\n [\n -81.6998291015625,\n 43.94537239244209\n ],\n [\n -82.0458984375,\n 43.94537239244209\n ],\n [\n -82.0458984375,\n 43.52266348752663\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"70","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Markle, Jeff M.","contributorId":219782,"corporation":false,"usgs":false,"family":"Markle","given":"Jeff","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":773164,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schincariol, Robert A.","contributorId":219783,"corporation":false,"usgs":false,"family":"Schincariol","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":773165,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sass, J.H.","contributorId":70749,"corporation":false,"usgs":true,"family":"Sass","given":"J.H.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":773166,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Molson, John W.","contributorId":219784,"corporation":false,"usgs":false,"family":"Molson","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":773167,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70204765,"text":"70204765 - null - Vegetation pattern on channel features in the Passage Creek Gorge, Virginia","interactions":[],"lastModifiedDate":"2019-08-14T10:53:25","indexId":"70204765","displayToPublicDate":"1983-08-14T10:46:13","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1195,"text":"Castanea","active":true,"publicationSubtype":{"id":10}},"title":"Vegetation pattern on channel features in the Passage Creek Gorge, Virginia","docAbstract":"Persistent distribution patterns of woody vegetation within the bottomland forest of Passage Creek, Virginia, were related to fluvial landforms, channel geometry, streamflow characteristics, and sediment-size characteristics. Vegetation patterns were determined from species presence as observed in transects and traverses on landforms developed along the stream. Distinct species distributional patterns were found on four common fluvial geomorphic landforms: depositional bar, active-channel shelf, floodplain, and terrace. Independent hydrologic characteristics (flow duration and flood frequency) were determined for each of the landforms. Vegetation data were analyzed by binary discriminant analysis, principal components analysis, and detrended correspondence analysis. Results and related field observations suggest that certain species are significantly associated with specific fluvial landforms. Vegetation patterns appear to develop more as a result of hydrologic processes associated with each fluvial landform rather than from sediment-size characteristics. Flood disturbance may be an important factor in maintaining the vegetation patterns, which may therefore be used as indicators for particular hydrogeomorphic site conditions.
ABSTRACT: Pierre Perrault, member of a bourgeois provincial family whose roots were in the Touraine region of France, grew up in Paris. One of six illustrious Brothers, all characterized by brilliance and diversity, he was educated as a lawyer but turned to finance and rose to a high position under King Louis XIV. Owing to political naivete and financial imprudence, he fell into disgrace and went bankrupt. He then became an amateur scientist and wrote a book on the origin of springs. This book broke almost wholly with the traditional authoritarianism of 2, 000 years'standing, and set hydrology on the modern path of observation and direct experiment, He developed the concept of the hydrological cycle, correctly accounting for the disposition of rainfall by evaporation, transpiration, ground‐water recharge and runoff. Some of his ideas about specific processes were erroneous, but where he was wrong his errors were logically based. Much of his contribution to the foundation of scientific hydrology has been overlooked or distorted by historians and hydrologists alike. Copyright © 1974, Wiley Blackwell. All rights reserved
","language":"English","publisher":"Wiley Blackwell ","doi":"10.1111/j.1752-1688.1974.tb05623.x","issn":"1093474X","usgsCitation":"Nace, R.L., PIERRE PERRAULT: THE MAN AND HIS CONTRIBUTION TO MODERN HYDROLOGY: JAWRA, v. 10, no. 4, p. 633-647, https://doi.org/10.1111/j.1752-1688.1974.tb05623.x.","productDescription":"15 p. ","startPage":"633","endPage":"647","costCenters":[],"links":[{"id":370202,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"4","noUsgsAuthors":false,"publicationDate":"2007-06-08","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":777276,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220528,"text":"70220528 - null - Effect on evaporation of releases from reservoirs on Salt River, Arizona","interactions":[],"lastModifiedDate":"2021-05-18T17:05:16.62051","indexId":"70220528","displayToPublicDate":"1960-09-30T11:59:52","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":"Effect on evaporation of releases from reservoirs on Salt River, Arizona","docAbstract":"By means of the energy-budget method, measurements of evaporation losses from four reservoirs on Salt River, Ariz., were determined to range from 57.5 to 69.9 inches for the 12-month period April 1958 to March 1959. Water is withdrawn from Roosevelt Lake at considerable depth and released through three run-of-the-river reservoirs. Because the water released from Roosevelt Lake is cold, evaporation losses from the downstream reservoirs are considerably lower than those from Roosevelt Lake. Evaporation pan coefficients computed for the various reservoirs ranged from 0.53 to 0.65. A base evaporation rate was computed for each reservoir as the evaporation rate that would have occurred had there been no change in energy storage and the net advected energy equalled zero during the year.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666009493178","usgsCitation":"Koberg, G., Effect on evaporation of releases from reservoirs on Salt River, Arizona: International Association of Scientific Hydrology - Bulletin , v. 5, no. 3, p. 37-44, https://doi.org/10.1080/02626666009493178.","productDescription":"8 p.","startPage":"37","endPage":"44","costCenters":[],"links":[{"id":480529,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666009493178","text":"Publisher Index Page"},{"id":385715,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Salt River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.2637939453125,\n 33.28921188443142\n ],\n [\n -110.8245849609375,\n 33.28921188443142\n ],\n [\n -110.8245849609375,\n 33.75631505992707\n ],\n [\n -112.2637939453125,\n 33.75631505992707\n ],\n [\n -112.2637939453125,\n 33.28921188443142\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"5","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Koberg, G.E.","contributorId":258181,"corporation":false,"usgs":false,"family":"Koberg","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":815905,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}