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2017-05-10_REVISION - M2002004
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2017-05-10_REVISION - M2002004
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Entry Properties
Last modified
6/16/2021 6:25:34 PM
Creation date
5/11/2017 9:33:01 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M2002004
IBM Index Class Name
REVISION
Doc Date
5/10/2017
Doc Name
Adequacy Review Response
From
GCC Rio Grande
To
DRMS
Type & Sequence
TR6
Email Name
ERR
Media Type
D
Archive
No
Tags
DRMS Re-OCR
Description:
Signifies Re-OCR Process Performed
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9. The Division believes the proposed location for MW-006 is appropriate because it is located <br /> downgradient of the second mine panel (Years 6-15) and is within close proximity of the fault <br /> which bisects the second panel. However, MW-006 is likely not appropriately located for the <br /> first panel (Years 1-5). Located within this first panel is an un-lined sedimentation basin <br /> excavated into the Codell Sandstone. The Division is concerned this in-pit sedimentation basin <br /> could act as a groundwater infiltration gallery and therefore the installation of an additional <br /> monitoring well appears warranted. The location of this additional well would be most <br /> appropriate downgradient of the in-pit sedimentation basin (near Arroyo B). Please <br /> demonstrate how the location of MW-006 is sufficient to demonstrate compliance with the <br /> requirements of Rules 3.1.5(5), (10) and (11), 3.1.6, and 3.1.7 for activities occurring in the <br /> first two mine panels(Years 1-15)or commit to installing an additional well. <br /> GCC agrees that the proposed MW-006 is likely not well suited for the first panel (Years 1-5). The <br /> sedimentation basin was excavated at the very beginning of the life of the Quarry, before the Plant <br /> was erected, and subsequently expanded in 2010. Pursuant to condition 1 of Operations mining <br /> Permit No. M-2002-004, GCC installed six (06) groundwater monitoring wells at the facility: MW- <br /> 001, MW-001A, MW-002, MW-003, MW-004 and MW-005. Monitoring well MW-001 was installed <br /> inside the first panel (Years 1-5), specifically 1,440 feet west and 200 feet north of the southeast <br /> corner of Section 13 Township 22 South, Range 65 West. The purpose of this monitoring well was <br /> to screen across the Codell Sandstone. MW-001 was plugged in April 2008 as mining of panel years <br /> 1-5 progressed. Groundwater was never found. <br /> In order to provide a monitoring point downgradient of the mine limits and an eventual <br /> replacement for MW-001, monitoring well MW-001A was installed early 2003 north of MW-001; <br /> specifically 1,000 feet west and 1,550 feet north of the southeast corner of Section 13 Township 22 <br /> South, Range 65 West (downgradient of panel years 1-5) to further evaluate whether the <br /> limestone/sandstone or sandstone/shale contacts were water-bearing units. No water was noted <br /> during drilling MW-001A and from the time of installation in 2003 until 2013, MW-001A never <br /> produced enough water to sample. Also, no saturation in the Fort Hayes Limestone or the Codell <br /> Sandstone has been noted during mining. <br /> On March 12, 2013 GCC submitted a Technical Revision application to modify the Groundwater <br /> Monitoring Plan. The application elaborated on groundwater sampling events from all Monitoring <br /> Wells present at the time,including MW-001A. In accordance with the provisions of Rule 16.2 of <br /> the State Engineer's Water Well Construction Rules, GCC requested DRMS'approval to plug and <br /> abandon wells MW-001A, MW-002, MW-003 and MW-004. The Technical Revision application was <br /> approved by DRMS on March 20, 2013. <br /> The sedimentation pond is excavated into the upper portion of the Codell Sandstone. The pond is <br /> pumped down after a maximum of 3 days of stormwater accumulation. As noted in the CCG report <br /> (2016), "given the pump setting, the water level in the basin stays below the Fort Hayes/Codell <br /> contact. The limited water that accumulates in the basin primarily evaporates. Some limited <br /> amount of water may persist at times in the basin due the impracticability of pumping it completely <br />
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