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PERMFILE108040
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PERMFILE108040
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Last modified
8/24/2016 10:00:30 PM
Creation date
11/24/2007 4:11:26 PM
Metadata
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Template:
DRMS Permit Index
Permit No
C1981019
IBM Index Class Name
Permit File
Doc Date
12/11/2001
Doc Name
Sections 10 - 16
Section_Exhibit Name
Exhibit 12 Experimental Part 3
Media Type
D
Archive
No
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- 7- <br /> <br />• strain. I*_ has long been known that a slope stability failure is a plane <br />strain problem and that ideally the strength of ttre material in plane <br />strain shouid be used in analysis. Because of the lack of equipment and <br />convenience, most data on strength is obtained frc~n triaxial testing. <br />blork done oy Lee (9) has mown That there is a significant difference be- <br />t~~:eon the strength obtained from a triaxial test and a plane strain test <br />an granular materials. This ratifier extensive wore indicates that the <br />angle of internal friction obtained from plane strain testing can be up <br />to 3 degrees higher than that obtained from triaxial tests. <br />ble agree with the commentor that "ideally, the appropriate soil testing... <br />shouid be conducted to decrease the necessity for assumption...". However, <br />we Mould like to add that inappropriate soils testing will not only be <br />wasteful tut also misleading. As indicated by Sowers (13), "A realistic <br />test of a rockfill must meet two reouirements: (1) the material tested <br />should be the same as that of the prototype embankment; and (2) the stresses <br />imposed by the testing should simulate these in the dam." The large scale <br />triaxial tests do not meet the first requirement and meet the second re- <br />quirement only partially. Lops (10) indicates that the data available are <br />sufficient only to indicate trends. hlarachi (11) states "the engineer in <br />charge of the design of a rock-'ill dam s•rould have no logical and conclusive <br />means to assess the strength and compressibility of actual rockfill materials <br />on the basis of laboratory test results which are usually performed on the <br />materials consisting of much smaller particles." These comments and our <br />experience indicate the use of standard testing techniques is hardly accept- <br />• able ror spoil material. The heterogeneous character of the spoil as com- <br />pared with the uniform characteristics of the rockfill materials tested <br />;hake it e~!en more dlffi~Ult to obtain strength data from standard testing. <br />The letter mention:, the tests and results of the r•rork done in Kentucky <br />by riuang ;;) as an example of data. in our opinion, there are several <br />pitfalls that must be examined carefully prior io using such data. A <br />fe';I OT =;;252 CG.^,SiGc:"c~i 0ii~ InCIUdc: <br />The samples used in the laboratory testing were all obtained <br />approximately "...1 foot belov; the surface...". It is hardly <br />an acceptable procedure to model the overall strength of the <br />spoil pile r`rcm tests taken at a depth of i fool. .45 a matter <br />of fact, materials which are very near the surface are normally <br />the most weathered and least representative of the fill. <br />2. Tire use of standard test data is not acceptable from an anaineer- <br />ing viewpoint. The character of different materials, as shoti•m <br />by she test da*_a presented can provide widely aifferir.g results. <br />Tile data presented shows variations in cohesion of 0 to 760 psf <br />and friction angle variations of 15.5 to 36.6 degrees. <br />lJ <br />
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