Laserfiche WebLink
<br />35 <br />I would agree that the angle of internal friction equals the angle of repose only in the case <br />of a theoretical non-cohesive (granular) soil, such as dry well-sorted silica sand. In the <br />realistic case of cohesive soils, such as the colluviaUresidual clay soils and the anticipated <br />spoil at the Lorencito Canyon Mine, this generalization is inappropriate. In my opinion <br />this assumption should be amended to read; "The angle of repose of cohesive soils is <br />considered an indicator of the maximum possible friction angle of these materials. Razely <br />will the friction angle of these materials approach that theoretical maximum limit." <br />Frankly, I do not believe this potentially flawed statement adds to the presentation and <br />might better be deleted. <br />Design and Coustructiou Recommendations <br />As a result of their pazametric analysis, CTL/I'hompson, Inc. forwards detailed <br />recommendations for use in the eventual design and construction of the Lorencito Canyon <br />Mine spoil fills. I concur with the majority of their recommendations. My following <br />comments address only recommendations with which I disagree or which require more <br />detail. <br />Site Prepazation <br />"If reconnaissance indicates localized unstable areas which could affect stability, the best <br />procedure may be excavation of the unstable mass." Caution should be exercised by the <br />operator in applying this suggestion. Excavation of a failed mass may remove the lateral <br />support for adjacent upslope materials and only exacerbate the instability of the upslope <br />material resulting in a lazger failure. <br />"If a localized steep valley side slope results in classification as a valley fill this could <br />require the lazge drains associated with valley fill regulations. It may be advantageous <br />to cut these slopes to less than 20 degrees." Rule 1.04 (148) states; "'Valley fill' means <br />a fill structure consisting of any material other than coal waste and organic matter that is <br />placed in a valley where side slopes of the existiug valley measured at the steepest point <br />aze greater than 20° or the average slope of the profile of the valley from the toe of the <br />fill to the top of the fill is greater than ]0°." (emphasis added) The word "existing" was <br />used in the regulatory definition to disallow this sort of avoidance. However, the <br />Division would measure the side slope gradient over an appropriate chord length. "Slope" <br />is not a point characteristic. There is no written policy for this determination. It is a <br />judgement made by the reviewing professional. Small steep segments may not be <br />significant in completing the determination of slope gradient. Further, I suspect it would <br />not be practical for the operator to attempt to amend large areas of the slope to avoid <br />classification as a "valley 511". <br />Fill Placement <br />On page ]4 of Exhibit #13, CTL/Thompson, Inc. States; "CDMG regulations require that <br />