Geological Survey Professional Paper Volume 497, PT. 4
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Geological Survey Professional Paper Volume 497, PT. 4

Geological Survey Professional Paper Volume 497, PT. 4


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This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. Excerpt: ...pressures in the adjacent sands and gravels. Another effect that may limit the use of the void-ratio measurements is the expansive rebound that probably takes place when the overburden load is removed from the sediments as they are cored (Poland, 1963).The actual amount of rebound involved, however, is not easily determined. For laboratory tests made of compression and rebound of 48 of the fine clayey sediments from the San Joaquin and Santa Clara Valleys, rebound from the simulated field effective load to the unloaded condition was accompanied by an average increase in void ratio of about 0.1 (from 0.56 to 0.67). This rebound, however, took place in the presence of excess water over rather long periods of time. Saturated clays must imbibe water in order to swell, and the silts and clays whose void ratios are used in this study were not exposed to excess water long enough to swell to their full rebound capacity during the coring process. I suspect, therefore, that the increases in void ratio related to rebound experienced by these samples are considerably less than the 0.1 observed in the laboratory compression and rebound tests. The relation between void ratio and the logarithm of effective overburden load is assumed to be linear. This assumption is based on the data of Hedberg (1936, p. 256, 262) and Storer (1959, p. 520-523), which are summarized together by Engelhardt (1960, p. 39-42). These data suggest that the relation between void ratio and the logarithm of depth is linear in the depth range between 1,500 and 10,000 feet. Using these data to support the assumption of a linear relation between void ratio and the logarithm of effective load in the sediments of the San Joaquin and Santa Clara Valleys involves two further assumptions: (1) that the relation b...


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Product Details
  • ISBN-13: 9781231241325
  • Publisher: Rarebooksclub.com
  • Publisher Imprint: Rarebooksclub.com
  • Height: 246 mm
  • No of Pages: 28
  • Spine Width: 2 mm
  • Width: 189 mm
  • ISBN-10: 1231241322
  • Publisher Date: 01 May 2012
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Weight: 68 gr


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