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2014-10-21_PERMIT FILE - C1981008A
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2014-10-21_PERMIT FILE - C1981008A
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Last modified
8/24/2016 5:49:07 PM
Creation date
11/14/2014 8:14:21 AM
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Template:
DRMS Permit Index
Permit No
C1981008A
IBM Index Class Name
Permit File
Doc Date
10/21/2014
Doc Name
Protection of the Hydrologic Balance
Section_Exhibit Name
Section 2.05.6(3) Protection of the Hydrologic Balance
Media Type
D
Archive
Yes
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of maximum impact of the flows. at this time, the increase in TDS of the River is from 620 to 652 <br />ppm, or an increase of 5.1 %. It should be noted that Tuttle Draw flows are always higher in TDS <br />than the River, regardless of the spoil springs, therefore, the impact from the spoil springs may be <br />only 2 -3% increase in TDS. During March /April, the River is flowing fast and Tuttle Draw is at low <br />flow, therefore the increase in TDS for the River is only 2 ppm, or an increase of 0.4 %. Also, these <br />impacts are for the time when the spoil material is leaching salts at a maximum. As described <br />earlier, the TDS levels will drop as pyrite and salts are leached out of the spoil, lessening the impact <br />to the waters downstream even further. <br />Calamity Draw is not included in the above table since the spoil springs from both mine areas will <br />not enter this stream. This intermittent stream should not be affected in the long term by the mining <br />and reclamation operation. <br />Overall, the effects of the spoil springs are not significant to the waters downstream. <br />7) Effects of mining on the local geomorphology. Impacts from mining on the local <br />geomorphology will belong term, but appear to be of minimal significance. The reestablished reach <br />of the drainage running south into Pond 007 will result in a shorter, slightly steeper stream channel. <br />The potential for increased sediment loads in the drainage (once pond 007 is removed) should be <br />offset by the stable bank sides and the relatively small change in overall gradient. The reclaimed <br />land will be graded to enhance irrigation and restore similar drainage patterns to those which <br />existed on the area prior to mining. The increased runoff and consequent erosion potential on <br />disturbed basins in the mining area due to the temporary loss of topsoil structure should be of <br />minimal significance since all disturbed areas will be protected by a system of sediment ponds. <br />Contour ripping, mulching and revegetation have been demonstrated to minimize soil erosion and <br />will be used to mitigate the increased runoff potential until the topsoil structure is developed. <br />Irrigation will help this to occur rapidly. <br />8) Effects of sediment ponds on channel characteristics and downstream users. Potential <br />impacts of sediment pond 007 and the other future ponds on downstream users will involve <br />possible reductions in flow due to impounded water. The water augmentation plan discusses the <br />available water which will be used should impacts be identified. WFC currently has rights to a <br />sufficient quantity of water to supply all users associated with the mining activities, plus an <br />additional quantity of water that can be used to mitigate any impact to downstream users. <br />Effects of sediment pond discharge on surface water quality. The effects of sediment ponds <br />on surface water quality will be negligible because each structure has been designed to minimize <br />Revised September 2014 (TR -64) 2.05.6(3) -42 <br />
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