{"pageNumber":"2715","pageRowStart":"67850","pageSize":"25","recordCount":68807,"records":[{"id":70221774,"text":"70221774 - 1932 - Recent investigations of Thiem's method for determining permeability of water‐bearing materials","interactions":[],"lastModifiedDate":"2021-07-02T13:04:16.594646","indexId":"70221774","displayToPublicDate":"1932-06-01T08:00:46","publicationYear":"1932","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":"Recent investigations of Thiem's method for determining permeability of water‐bearing materials","docAbstract":"<p>This paper presents results obtained in an investigation of the ground-water resources of the Platte River Valley that is being conducted in cooperation between the Conservation and Survey Department of the University of Nebraska and the United States Geological Survey.</p><p>Most quantitative ground-water studies are concerned with the amount of water that percolates into the discharge-area of an investigated region from the recharge-area in order to determine the amount of water that can be safely withdrawn from the discharge-area without an excessive lowering of the ground-water level. D'Arcy found that the quantity of water discharged through a column of water-bearing material was proportional t o the hydraulic gradient, the cross-sectional area, and a constant which depends upon the material. If these three factors are known, the discharge through any cross section of a water-bearing formation may be computed.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR013i001p00313","usgsCitation":"Wenzel, L., 1932, Recent investigations of Thiem's method for determining permeability of water‐bearing materials: Eos, Transactions, American Geophysical Union, v. 13, no. 1, p. 313-317, https://doi.org/10.1029/TR013i001p00313.","productDescription":"5 p.","startPage":"313","endPage":"317","costCenters":[],"links":[{"id":386935,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Wenzel, L.K.","contributorId":18733,"corporation":false,"usgs":true,"family":"Wenzel","given":"L.K.","email":"","affiliations":[],"preferred":false,"id":818682,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221773,"text":"70221773 - 1932 - Investigations of the fluctuations of water‐levels in observation‐wells in Virginia","interactions":[],"lastModifiedDate":"2021-07-02T12:55:15.86234","indexId":"70221773","displayToPublicDate":"1932-06-01T07:48:20","publicationYear":"1932","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":"Investigations of the fluctuations of water‐levels in observation‐wells in Virginia","docAbstract":"<p><span>An automatic&nbsp;</span>water<span>‐stage recorder has been maintained on an&nbsp;</span>observation<span>‐</span>well<span>&nbsp;</span>in<span>&nbsp;Arlington County,&nbsp;</span>Virginia<span>, about 1‐½ miles from the United States Weather Bureau,&nbsp;</span>in<span>&nbsp;Washington, D.C., since June, 1928, but there are a few interruptions&nbsp;</span>in<span>&nbsp;the record. This is a dug&nbsp;</span>well<span>, about 28 feet deep and extends through terrace deposits of gravelly silt or loam. It has not been used for&nbsp;</span>water<span>‐supply during the period of record. The recorder was installed by the United States Geological Survey and the record has been given considerable study by O. E. Meinzer, W. N. White, and L. K. Wensel, all of the Geological Survey.&nbsp;</span>In<span>&nbsp;July, 1931, the study of this&nbsp;</span>well<span>&nbsp;was made a part of a more comprehensive&nbsp;</span>investigation<span>&nbsp;of the ground‐</span>water<span>&nbsp;resources of&nbsp;</span>Virginia<span>&nbsp;</span>in<span>&nbsp;cooperation with the State Geological Survey, which was assigned to the writer. The&nbsp;</span>well<span>&nbsp;is essentially of the&nbsp;</span>water<span>‐table type, and its hydrograph shows approximately the periods of rainfall‐penetration and the relative amounts of recharge&nbsp;</span>in<span>&nbsp;each of these periods. The record is especially instructive because of certain unusual climatic conditions that have existed&nbsp;</span>in<span>&nbsp;the last four years.&nbsp;</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR013i001p00370","usgsCitation":"Cady, R., 1932, Investigations of the fluctuations of water‐levels in observation‐wells in Virginia: Eos, Transactions, American Geophysical Union, v. 13, no. 1, p. 370-373, https://doi.org/10.1029/TR013i001p00370.","productDescription":"4 p.","startPage":"370","endPage":"373","costCenters":[],"links":[{"id":386934,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Virginia","otherGeospatial":"western Virginia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.068603515625,\n              36.53612263184686\n            ],\n            [\n              -75.794677734375,\n              36.53612263184686\n            ],\n            [\n              -75.794677734375,\n              38.69408504756833\n            ],\n            [\n              -79.068603515625,\n              38.69408504756833\n            ],\n            [\n              -79.068603515625,\n              36.53612263184686\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"13","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Cady, R.C.","contributorId":44905,"corporation":false,"usgs":true,"family":"Cady","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":818680,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70220411,"text":"70220411 - 1932 - Investigations of underground water problems in Arizona, California, New Mexico, and Oregon","interactions":[],"lastModifiedDate":"2021-05-12T12:34:20.907919","indexId":"70220411","displayToPublicDate":"1932-05-12T07:26:58","publicationYear":"1932","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":"Investigations of underground water problems in Arizona, California, New Mexico, and Oregon","docAbstract":"<div id=\"article__content\" class=\"col-sm-12 col-md-8 col-lg-8 article__content article-row-left\"><div class=\"article__body \"><div class=\"article-section__content en main\"><p>This report is a summary of investigations in progress in 1932 in the southwestern portion of the United States. It covers only those investigations that deal with water in the zone of saturation, and excludes those that deal primarily with water in the zone of aeration. Arizona H. C. Schwalen, Irrigation Engineer, Agricultural Experiment‐Station, Tucson, Arizona, has proposed to undertake a study of the effect of pumping from wells, and of the capacity of water‐bearing strata, but no report of progress is available. Several other hydrologic investigations are now being made by the Agricultural Experiment‐ Station, but relate primarily to infiltration and transpiration.</p></div></div></div>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR013i001p00308","usgsCitation":"Piper, A., 1932, Investigations of underground water problems in Arizona, California, New Mexico, and Oregon: Eos, Transactions, American Geophysical Union, v. 13, no. 1, p. 308-310, https://doi.org/10.1029/TR013i001p00308.","productDescription":"3 p.","startPage":"308","endPage":"310","costCenters":[],"links":[{"id":385583,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona, California, New Mexico, 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 \"}}]}","volume":"13","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Piper, Arthur M.","contributorId":65060,"corporation":false,"usgs":true,"family":"Piper","given":"Arthur M.","affiliations":[],"preferred":false,"id":815472,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25079,"text":"wsp638A - 1932 - A preliminary report on the artesian water supply of Memphis, Tennessee","interactions":[{"subject":{"id":25079,"text":"wsp638A - 1932 - A preliminary report on the artesian water supply of Memphis, Tennessee","indexId":"wsp638A","publicationYear":"1932","noYear":false,"chapter":"A","title":"A preliminary report on the artesian water supply of Memphis, Tennessee"},"predicate":"IS_PART_OF","object":{"id":3212,"text":"wsp638 - 1932 - Contributions to the hydrology of the United States 1931","indexId":"wsp638","publicationYear":"1932","noYear":false,"title":"Contributions to the hydrology of the United States 1931"},"id":1}],"isPartOf":{"id":3212,"text":"wsp638 - 1932 - Contributions to the hydrology of the United States 1931","indexId":"wsp638","publicationYear":"1932","noYear":false,"title":"Contributions to the hydrology of the United States 1931"},"lastModifiedDate":"2024-02-05T21:04:52.046067","indexId":"wsp638A","displayToPublicDate":"1932-01-01T00:00:00","publicationYear":"1932","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":"638","chapter":"A","title":"A preliminary report on the artesian water supply of Memphis, Tennessee","docAbstract":"Memphis is located in the part of the Gulf Coastal Plain known as the Mississippi embayment. It is underlain by unconsolidated sand and clay formations of Tertiary and Cretaceous age. The Wilcox group, of Tertiary age, and the Ripley formation, of Cretaceous age, are excellent aquifers, and all the water consumed in Memphis is derived from them. The maximum pumpage from the Wilcox group was reached about 1920; in that year an estimated average of 37,575,000 gallons a day was pumped. In 1928 the average daily pumpage from the Wilcox group was about 33,984,000 gallons, and in addition to this the Memphis Artesian Water Department pumped an average of 4,616,000 gallons a day from the Ripley formation. \r\n\r\nThe static level at Memphis varies with the pumpage and the stage of the Mississippi River. The original static level was about 235 feet above mean sea level. In 1928 the average static level at the Auction Avenue plant was 202 feet above mean sea level, which was about 33 feet lower than the original level. The yield is therefore about a million gallons a day for each foot of drawdown. The drawdown is not excessive, and additional pumpage can be developed without undue lowering of head. \r\n\r\nThe water from both the Wilcox group and the Ripley formation is fairly soft and has a moderately low content of dissolved mineral matter. 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