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C <br />ExxonMobil Global Services <br />Colony Shale Oil Project <br />ESR Reclamation Studies <br />Weighing Lysimeter Performance 1990-2003 <br />Project No. 353 <br />Page 23 <br />5.0 RECAP OF FINDINGS AND CONCLUSIONS <br />Conclusions from this compilation of the observations at the weighing lysimeter for the years <br />1990- 2003 are summarized below. <br />Percolation Canture and Consumption <br />1) The "A" Treatment, nominally 20.22" native topsoil over a 6-inch thick mixed wne of 2 <br /> <br /> <br />parts native topsoil to 1 part raw un-leached ESR combusted shale, over loosely placed ESR <br />combusted shale, appears capab]e of capturing and consuming all summer rainfall water that does not <br />runoff, regardless of the maturity of the plant cover. In the early years before the reclamation cover is <br />mature, the consumption appears to be carried out by hydration of percolation water as it enters the <br />yet-to-be-hydrated ESR combusted shale. After the reclamation vegetation cover is mature, summer <br />rainfall appears to be captured and consumed in the plant root zone, as Wymore (1974) suggested <br />might indeed occur in thissemi-arid climate. <br />2) The "A" Treatment with an immature native species reclamation plant cover (1990.YE <br />1993) can capture and consume spring melt but only until the mineral hydration capacity of the <br />relatively thin (39 inches) combusted ESR shale layer has been satisfied. After that, the mechanical <br />capillary capacity of that 39-inch layer combusted shale will continue to retain infiltrating moisture, <br />but once its capillary capacity is exczeded, additional spring melt water that reaches the ESR <br />combusted shale will continue deeper into the pile. In this experiment, because of the practical <br />limitation of lysimeter tub depth, the infiltrating percolation water is removed and collected after <br />passing through only 39" of ESR combusted shale. In a prototype pile, it would require <br />proportionately longer time to satisfy the hydration capacity and the capillary capacity of the thicker <br />combusted shale zone. <br />LACHEL FELICE & Associates <br />