2018-07-02_PERMIT FILE - C2010089A (19)

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of about 11.9 gpm. As noted, this is based on the situation as is but does not account for the rerouting of 2nd Park Lateral through the HDPE pipeline and the suspension of irrigation during mining which will reduce discharge into the pit. The data from the slug test at GW -N9 (overburden and coal zone combined as described above) show a higher K value (2.1 ft/day) than the averages for the overburden and coal zones. As expected, calculating discharge rates from this test results in higher discharge rates than those calculated from the zone averages. Using the K value from GW -N9, an average gradient of 0.05, a saturated thickness of 25.0 feet and a pit length of 2,197 feet the estimated discharge would be equal to (2.1 ft/day) x (0.05) x (25.Oft x 2197ft) = 5767 ft3 per day or 2.105 x 106 ft3 per year or about 29.9cgpm or a factor of 5 higher than that calculated from the averages of the overburden and coal zones of about 5.7 gpm. However, the GW -N 9 location is only 775 feet directly down gradient (see Map 2.04.7-3) from the 2nd Park Lateral and the test was done on 7/17/86 during the height of the irrigation season and the recharge of the overburden. This suggests that discharge from the highwall after the 2nd Park Lateral has been diverted through the HDPE pipeline will be closer to the lower discharge rate than to the higher rate indicated from the GW - N9 test data (see Table 7-5 a copy of which is contained in Appendix 2.04.7-2). Evapotranspiration Evapotranspiration (ET) is a component of discharge in the NHN permit area. Studies at the New Horizon Mine with similar vegetation types and uses to the NHN permit area (see New Horizon 2 permit Section 2.04.7) indicate that the annual ET rate is on the order of 2.1 acre-ft/acre. Based on the surface area of NHN (328.88 acres) the annual ET is about 674 acre—ft per year. Irrigation run off water contributes to the stream flow of Tuttle Draw and Coal Canyon. The stream flows of Tuttle Draw and Coal Canyon in turn contributes to the flow of the San Miguel River, at the least, two and one half miles downstream of mining and the mining disturbance. The total volume of water that could be evapotranspired from the NHN vegetation study is estimated under ideal conditions. In reality the evapotranspiration rates are less. In many areas shallow soils and rock ledges restrict rooting depths and inhibit maximum plant growth, thereby reducing ET rates. Aquifer Characteristics of the New Horizon North Mining Areas Previous aquifer testing of the Dakota Formation coal strata in the NHN permit area indicates that the overburden, coal and underburden zone transmissivity and hydraulic conductivity values in the NHN permit area are low to very low (see Tables 7-5 and 7-6 in Appendix 2.04.7-2 of this application). The overburden and underburden aquifers have the higher values and the coal aquifer has the lowest transmissive properties. There is approximately one order of magnitude range in the transmissivity and hydraulic conductivity values for the overburden, coal and underburden aquifers. This suggests that there is a high degree of spatial variability within the aquifers. Storage coefficients for the various stratigraphic zones vary from about 10-4 to 10-5 for the overburden and the coal/underburden zones, respectively. Transmissivities (T) for overburden Section 2.04.7 Page 7 March 2018 (TR -16)