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f DER <br />Bright Bright People. Right Solutio - <br />seen in past results. Additional, it should be noted that the HELP model results do not <br />depict seepage until January 2011, also similar to past results. <br />2.4 MODELING OF SEEPAGE THROUGH PRESCRIPTIVE CAP <br />Performance of the Title 27 Prescriptive Cap was modeled using HELP and Test Pad <br />precipitation data collected so far during the 2010/2011 water year. The Prescriptive <br />Cap was setup in HELP using the following values: <br />i <br />Layer 1 (vegetative cover), 12 inches thick, sandy silt (HELP soil texture #7) <br />® Layer 2 (barrier layer), 12 inches thick, clay (HELP soil texture #16, <br />hydraulic conductivity adjusted to 1x10-6 cm/sec) <br />® Layer 3 (foundation layer), 24 inches thick, sandy silt (HELP soil texture 7) <br />The modeled results showed 1,118.15 cu ft seepage. Results of the HELP modeling <br />are summarized in Table 1. The HELP modeling printout can be found in Appendix B. <br />Chart 1 shows the rainfall vs. seepage volume with actual and modeled data. <br />Performance of the ET Test Pad (using seepage out of the bottom of the cap) was <br />compared directly to the modeled performance of the Title 27 Prescriptive Cap. <br />2.5 SOIL MOISTURE MONITORING <br />Soil moisture sensors were installed with the ET Test Pad at the request of RWQCB <br />staff; however, soil moisture is not a criterion for ET cover evaluation. This data <br />presents monitoring data collected since fall 2006. <br />2.6 PREVIOUSRAIN E <br />The ET Test Pad was fitted with soil moisture sensors set at depths of 1, 2 and 3 feet <br />below the ground surface. Soil moistures in 2006/2007 were low, a reflection of the <br />recently constructed ET Final Cover. The variability in the shallowest probe was <br />greatest, as it was influenced most heavily by the cycles of wetting and drying caused <br />47717.11/ST011R193 Page 5 of 9 August 31, 2011 <br />Copyright 2011 Kleinfelder <br />