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2011-11-15_REVISION - M1980055HR
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2011-11-15_REVISION - M1980055HR
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Entry Properties
Last modified
6/15/2021 2:24:26 PM
Creation date
11/15/2011 1:29:58 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1980055HR
IBM Index Class Name
Revision
Doc Date
11/15/2011
Doc Name
Operator acceptance of amendment requirements (AM-01)
From
Denison Mines
To
DRMS
Type & Sequence
AM1
Email Name
RCO
Media Type
D
Archive
No
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Mine <br />Estimated <br />Hydraulic <br />Gradient <br />Estimated <br />Porosity <br />Estimated <br />Hydraulic <br />Conductivity <br />(cm /sec) <br />Estimated <br />Average Linear <br />Groundwater <br />Velocity <br />(feet/year) <br />Topaz <br />0.004 <br />0.11 <br />1.1 x 10-4 <br />4.1 <br />Topaz <br />0.004 <br />0.14 <br />1.1 x 10-4 <br />3.3 <br />West Sunday <br />0.006 <br />0.11 <br />1.1 x 10 -4 <br />6.2 <br />West Sunday <br />0.006 <br />0.14 <br />1.1 x 10-4 <br />4.9 <br />• linear groundwater velocity, this estimated porosity is assumed to be equivalent to <br />the estimated effective porosity of the Salt Wash member sandstones. <br />Groundwater observed in the West Sunday and Topaz Mines occurs within the Salt <br />Wash member of the Morrison Formation. A hydraulic conductivity of 1.1 x 10- <br />centimeters per second (cm /sec.) is estimated for this unit based on intrinsic <br />permeability values provided by Jobim (1962). <br />Exhibit 7 -3 presents a range of estimated linear groundwater velocity for the Salt <br />Wash Member of the Morrison Formation in the vicinity of the mines based on the <br />hydraulic conductivity, effective porosity and hydraulic gradient information <br />described above. <br />Exhibit 7 - 3. Estimated Linear Groundwater Velocit <br />Based on the evaluation presented above, the rate of groundwater flow is estimated <br />to range from approximately 3.3 to 6.2 feet per year. This suggests that, if pathways <br />are present for groundwater to travel towards the Dolores River, the travel time for <br />groundwater in the vicinity of the mine affected areas to reach the Dolores River may <br />be on the order of 2600 to 3300 years. However, the complex structural displacement <br />of the Salt Wash aquifer and other hydrogeologic units likely increases the complexity <br />of groundwater pathways, which may affect the travel time towards the Dolores <br />River. <br />C: \Documents ant Settinos\ woodward .DMClDesktop\Environmental Protection Plan Sunday Mines Revised November 2011 revl (2) 11 10 11.docx <br />Section 7 <br />Groundwater Information <br />7 -9 <br />
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