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2011-06-13_REVISION - C1981019
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2011-06-13_REVISION - C1981019
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Entry Properties
Last modified
8/24/2016 4:34:27 PM
Creation date
6/14/2011 7:51:57 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981019
IBM Index Class Name
REVISION
Doc Date
6/13/2011
Doc Name
Ground Water Review (Memo)
From
Tom Kaldenbach
To
Janet Binns
Type & Sequence
PR3
Email Name
TAK
JHB
Media Type
D
Archive
No
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STATE OF COLORADO <br />DIVISION OF RECLAMATION, MINING AND SAFETY <br />Department of Natural Resources <br />1313 Sherman St., Room 215 <br />Denver, Colorado 80203 <br />Phone: (303) 866-3567 <br />FAX: (303) 832-8106 <br />MEMO <br />DATE: June 13, 2011 Ifiz <br />FROM: Tom Kaldenbach <br />To: Janet Binns <br />Re: Colowyo Mine (C-1981-019), PR-3, Ground Water Review <br />Follow-up comments to the operator's responses of May 20, 2011 are provided below. <br />2.05.6(3)(a) Protection of the Hydrologic Balance <br />1. Response is adequate. <br />COLORADO <br />D IV IS I ON Of <br />RECLAMATION <br />MINING <br />- SAFETY <br />John W. Hickenlooper <br />Governor <br />Mike King <br />Executive Director <br />Loretta E. Pineda <br />Director <br />2. No further further response is needed for this comment, as pitwall seepage in Collom Lite pit is <br />addressed elsewhere in this letter. <br />5. As previously requested, please use in the calculations of spoil saturation time a reasonable <br />surface infiltration rate into Collom Lite spoil of 3.1 inches per year, calculated as 18% X 17 <br />inches per year average precipitation. In order to reflect the 3.1 inches per year infiltration, <br />please change the 0.016 cfs value on page 133 to 0.31 cfs, and change the 0.75 inches per year <br />recharge rate at the bottom of page 136 to 3.1 inches per year. <br />Our letter of April 22, 2011 explained that the 18% factor is based on Williams and Clark's <br />(1994) spoil lysimeter study which found that approximately 18% of annual precipitation <br />recharge spoil at a Routt County mine. The lithologic differences between the Danforth Hills <br />area and the lower Williams Fork Formation that are cited on page 23 of your 5/20/11 response <br />letter would not cause a significant difference in spoil permeability ( and, consequently, spoil <br />saturation rate) because the effective porosity in spoil is between particles of spoil, rather than <br />inside the particles of spoil. Also, a spoil infiltration study found the Colowyo spoil infiltration <br />rate was not less than infiltration rates at mines developed in the lower Williams Fork coal <br />sequence (Table 10, item 6 of Exhibit 7 of the Colowyo permit application). <br />6. Our original comment was a request to use in the Collom Lite pit backfill saturation calculation <br />that currently is on page 137, a value for effective porosity of 15% (based on spoil swell of that <br />amount), rather than the total porosity of 35% that is shown on that page. Most of the flow and <br />resulting saturation in spoil will occur between particles of spoil, rather than through particles of <br />spoil; therefore; the porosity between spoil particles is the effective porosity, and effective <br />porosity is the appropriate porosity value for performing a spoil saturation calculation. It seems <br />reasonable in a spoil saturation calculation to add 5 percentage points for ineffective porosity <br />inside spoil particles that may become partially saturated, resulting in 20% porosity for the <br />percentage of spoil backfill that will become saturated (15% effective porosity between particles, <br />plus 5% partially saturated particles). A value of 20% is consistent with the value of 20% that is <br />Office of Office of <br />Mined Land Reclamation Denver • Grand Junction Durango Active and Inactive Mines <br />j
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