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2018-05-31_REVISION - C1982056
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2018-05-31_REVISION - C1982056
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Last modified
6/1/2018 8:30:49 AM
Creation date
6/1/2018 7:03:28 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1982056
IBM Index Class Name
Revision
Doc Date
5/31/2018
Doc Name
Adequacy Review
From
DRMS
To
Twentymile Coal Company
Type & Sequence
RN7
Email Name
TNL
Media Type
D
Archive
No
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RN07 <br />Page 23 <br />5/30/18 <br /> <br /> <br />Response: - Please refer to the discussion of “Ground Water Quality Protection” on page 2.05-130 and the extensive <br />discussion of “Potential Mining-Related Impacts on Ground Water Quality and Quantity” on pages 2.05-133 <br />through 2.05-149. The Foidel Creek Mine mining and related operations will all occur within the Twentymile Park <br />groundwater basin, which is an enclosed basin with little or no potential for groundwater movement out of the basin. <br />The CDRMS has recognized this, as documented in the Permit Renewal RN -05 Decision and Findings of <br />Compliance; <br /> <br />“The Wadge overburden and the Twentymile Sandstone are the two major aquifers most likely to be affected <br />by the Foidel Creek Mine….The mine’s annual hydrology reports contain long-term data from these wells. <br />These data show Foidel Creek Mine is in compliance with the Basic Standards for Ground water at the <br />groundwater points of compliance.” <br /> <br />All of the groundwater rights identified in Table 9 are owned by either TC or Sage Creek Land & Minerals, an <br />affiliated Peabody subsidiary company. There are currently no domestic or agricultural uses of groundwater within <br />the Twentymile Park basin, so the applicable groundwater quality classification under Regulation 41, Basic <br />Standards for Groundwater, would be “Potentially Usable Quality”. Based on this cl assification, and the lack of <br />current existing uses, the only applicable water quality standard is TDS, which is 1.25 x background levels. Both <br />the water monitoring discussion in the PAP and Water Monitoring Plan (Exhibit 14) have been revised to clarify <br />points of compliance and this compliance threshold and copies of the revised permit materials are included with <br />these responses for replacement in the PAP. <br /> <br />Resolved <br /> <br />60. Have the proposed wells WC008A and WC013A been installed (monitoring program Exhibit 14A)? They are <br />shown on Map 13A, but have not been acknowledged as current monitoring wells in the monitoring plan. <br /> <br />Response: - The referenced wells have been constructed and are being actively monitored (refer to MR’s 14 -279 <br />and 14-281), and the Hydrologic Monitoring Plan (Exhibit 14) has been reviewed and updated to include these <br />wells. Copies of the revised permit materials are included with these responses for replacement in the PAP. <br /> <br />Resolved <br /> <br />61. The Annual Hydrology Reports (AHRs) reference potentiometric surfaces within the written interpretation of <br />the data and they are referenced within the permit related impacts to the hydrologic balance; however, these <br />potentiometric surfaces are not currently being provided within the AHR. Due to the potential impacts from <br />dewatering to the hydrologic balance, as well as the potential for increased aquifer communication due to <br />subsidence, it is appropriate to include potentiometric surface maps with the annual hydrology report going <br />forward. Please provide the Division with potentiometric surface maps for the Wadge Overburden, Twentymile <br />Sandstone, Trout Creek Sandstone, and Fish Creek Sandstone bedrock units. <br /> <br />Response: - The references to potentiometric surface in the AHR groundwater discussion are generally being used <br />to characterize direction of groundwater movement or as a general reference relative to observed changes for <br />specific monitoring locations. Generally observed variations in water level for groundwater monitoring wells are <br />relatively small and would not be accurately depicted by a potentiometric surface map. In addition, development <br />and updating of potentiometric surface maps for each aquifer being monitored would be unnecessarily time -
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