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2017-04-05_PERMIT FILE - C1982057 (7)
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2017-04-05_PERMIT FILE - C1982057 (7)
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Last modified
5/10/2017 10:20:49 AM
Creation date
5/10/2017 10:19:31 AM
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Template:
DRMS Permit Index
Permit No
C1982057
IBM Index Class Name
Permit File
Doc Date
4/5/2017
Section_Exhibit Name
Tab 17 Probable Hydrologic Consequences
Media Type
D
Archive
No
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005 Trib. DSC = O, 0000469 + 0.0000917 = 3450 mg/1 (494 TDS <br /> 0.0000298 x 0.00136 <br /> increase) <br />005 crib. L = 0.000015 x 3450 x 0.0027 = 0.000140 tons/day (494 <br /> tonnage increase) <br />Dry Creek Alluvium DSC = 0,00014 + 0.000245 = 1038 mg/1 (164 TDS <br /> (0.0000298 + 0.000243) x 0 .00136 <br /> increase due to 005 <br /> spoil discharge) <br />Dry Creek Alluvium L = 0.00014 x 7038 x 0.0027 = 0.000392 tons/day (754 tonnage <br /> increase due to 005 <br /> spoil discharge) <br />Cumulative Dry Cree k Alluvial System Premining: <br />Dry Creek Alluvium DSC = 0.000245 + 0.0000938 = 897 mg/1 <br /> (0.000248 + 0,00002975) x 0. 00136 <br />Dry Creek Alluvium L = 0.00074 x 897 x 0.0027 = 0.00034 tons/day <br />Cumulative Dry Cree k Alluvial System Postmining: <br />Dry Creek Alluvium DSG = 0.000288 + 0,00014 = 1154 mg/1 (294 TDS <br /> (0.000243 + 0.0000298) x 0. 00136 <br /> increase) <br />Dry Creek Alluvium L = 0.0001375 x 7154 x 0.0027 = 0.000428 tons/day (26$ • <br /> tonnage increase) <br />Sage Creek Alluvial System Premining: <br />009 Trib. Dry <br />Sage Creek Alluvium L = 0.0000398 x 955 x 0.0027 = 0.0001016 tons/day <br />Sage Creek Alluvial System Postmining: <br />009 Trib. L = 0.000000463 x 4500 x 0.002 7 = 0.0000056 tons/day <br />Sage Creek Alluvium DSC = 0.0001 + 0.0000056 = 972 mg/1 (1, 7+e TDS increase) <br /> (0.00000092 + 0.000079) x 0.0 0136 <br />Sage Creek Alluvium L = 0.00004 x 972 x 0.0027 = 0.000105 tons/day (24 tonnage <br />increase) <br />The magnitude of the cumulative 705 increase in the Dry Creek alluvium below the 005 <br />tributary confluence is approximately 30 percent. The range of the TDS increase extends <br />from below the 006 pond outfall to probably one mile below the confluence of Dry Creek <br />with the 005 tributary alluvium. The extent of the TDS increase is limited to this range <br />because of the low hydraulic conductivity of the alluvium, additional downg radient <br />geochemi cal changes and dilution from shallow aquifers which discharge to the alluvium, • <br />The duration of the impact over the extent of the Dry Creek alluvial aquifer previously <br />46 <br />
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