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2013-08-13_HYDROLOGY - M1977348 (2)
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2013-08-13_HYDROLOGY - M1977348 (2)
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Last modified
8/24/2016 5:23:44 PM
Creation date
8/15/2013 8:59:18 AM
Metadata
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Template:
DRMS Permit Index
Permit No
M1977348
IBM Index Class Name
HYDROLOGY
Doc Date
8/13/2013
Doc Name
Groundwater Characterization Field Summary Report.
From
Golder Associates
To
DRMS
Permit Index Doc Type
Hydrology Report
Email Name
ECS
Media Type
D
Archive
No
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August 2013 11 103- 81640A <br />Due to the initial volume of water in monitoring well MW -7 (about 140 gallons), MW -7 was developed by <br />air lift pumping on January 22, 2013 when about 100 gallons were removed before "lift' was lost. <br />Following this, Golder instructed Drilling Engineers to surge and bail the well to complete development. <br />About 10 gallons were removed by bailing. On March 5, 2013, six hours of additional development was <br />conducted by surging monitoring well MW -7 with a 3'/8 -inch diameter surge block and bailing until the well <br />went dry after about 41 gallons were removed. Field parameters were measured during development <br />(Appendix D). As with monitoring well MW -6, low recharge impeded the flushing of the well screen that is <br />necessary to considerably reduce turbidity. <br />3.5 Well Hydraulic Testing <br />After development, rising and falling head (slug) testing was conducted in monitoring well MW -5 by <br />monitoring the water level changes created by rapidly submerging and removing a solid cylinder (slug) <br />into and out of the water column of the well. Slug testing was not performed in monitoring well MW -7 <br />because hydraulic conductivity estimates were obtained from borehole packer injection tests (Section 3.2) <br />and in monitoring well MW -6 due to the long recovery times observed during development. <br />In monitoring well MW -5, a 5 -foot long, 1.25 -inch ID PVC slug was used to displace water in the well, <br />which was monitored with an In -Situ Troll 300 electronic pressure transducer and data logger. However, <br />the initial displacement was insufficient considering a minimum of about 6 inches is required for high <br />conductivity formations (Butler 1998) and recovery to static conditions occurred too rapidly (within one <br />second) to record during several attempts to perform the slug test. Consequently, analyses of these tests <br />could not be performed to estimate hydraulic conductivity. Previous hydraulic testing of monitoring wells <br />MW -1 through MW -4 have yielded hydraulic conductivities in the range of 10 -7 to 10 -10 centimeters per <br />second (cm /sec) (Table 2). Based on the outcome of the hydraulic testing in monitoring well MW -5, it is <br />likely that the hydraulic conductivity there is significantly greater than at monitoring wells MW -1 through <br />MW-4 and is the reason the slug testing was unsuccessful. <br />3.6 Surveying <br />Surveying of the seven monitoring wells was performed on January 10, 2013 to establish groundwater <br />elevations for monitoring flow directions and determining hydraulic gradients. Surveying activities was <br />performed by KRW Consulting, Inc., a Colorado licensed surveyor, and was tied into the same coordinate <br />system used for other surveying at the Site. At each well location, the elevations of the surface of the <br />concrete pad and top of PVC well casing were surveyed to an accuracy of 1/100 foot. The results of the <br />survey of each monitoring well location, and the elevations of each PVC well head casing top and <br />concrete pad are provided in Table 1 and in each monitoring well construction diagram in Appendix D. <br />920Golder <br />i \10 \81640a\ 0400\ gwcharwelhnstallfieldrep_ 09aug13\ gwchanvelhnstallheldrep_09aug13 docx <br />Associates <br />
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