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PERMFILE109209
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PERMFILE109209
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Last modified
8/24/2016 10:01:51 PM
Creation date
11/24/2007 5:58:20 PM
Metadata
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Template:
DRMS Permit Index
Permit No
C1981014
IBM Index Class Name
Permit File
Doc Date
12/11/2001
Doc Name
TR-14 continued
Section_Exhibit Name
EXHIBIT 15 Part 9a
Media Type
D
Archive
No
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• <br />Art. 17 Shearing Rcsutance of Coheawnleu Sat 107 <br />ART. 17 S[IEARING RESISTAVCE OF COHESIONLESS SOIIS <br />Sand+ and Inorganic Sr1ta <br />The shear characteristics of sands and inorganic silts can, unless the <br />soil is exceptionally loose, be represented reliably by Eq. 17.1. <br />s=(p-u.)tan~=ptan~ (17.1) <br />Deposits of natural sands and silts may be encountered in any state <br />between loose and dense. Depending principally upon the relative <br />density, the value of ~ may range between fairly wide limits; the grain- <br />size distribution and the shape of the grains also have an influence on <br />~. Representative values for ~ under effective pressures p [ass than <br />about 5 kg/cm' are given in Table 17.1. <br />Toble 17.1 <br />Repreaenlalioe Values of ~ /or Sands and SAla <br /> Depreea <br />Material Loose Dtnae <br />• <br />Sand, round grains, uniform 27.5 34 <br />Sand, angular grains, well graded 33 45 <br />Sandy gravels 35 50 <br />Silty sand 27-33 30-34 <br />Inorganic silt 27-30 30-35 <br />Since most of the shearing strength is caused by interlocking of the <br />grains, the values of m are not appreciably different whether the soil <br />is wet or dry. <br />As the pressure p is increased from about 5 to about 50 kg/cm', the <br />values of ~ decrease gradually by about 10°. The decrease is associated <br />with an increase in the percentage of grains that are crushed as the <br />state of failure is approached. <br />Figures 15.3c and a pointed out the tendency of a loose sand to <br />decrease in volume, and of a dense sand to dilate, during shear. The <br />permeability of very fine saturated sand and silt is so low that the <br />rapid application of s shearing stress is associated with a temporary <br />increase of pore pressure u. (Eq. 17.1) if the soil is loose, or with a <br />temporary decrease of u,. if the soil is dense. The strength of the soil is <br />correspondingly temporarily decreased or increased. Hence, for ex- <br />ample, if piles are being driven into one of these materials in a loose <br />saturated state, the piles encounter only a slight resistance which is <br />r1 <br />LJ <br />Terzaghi and Peck, 1967, "Soil Mechanics in Engineering Practice" Second Edition, <br />1967, John Wiley & Sons, Inc. New York, NY. <br />
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