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2017-06-26_HYDROLOGY - M1980244
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2017-06-26_HYDROLOGY - M1980244
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Entry Properties
Last modified
12/27/2020 1:25:58 AM
Creation date
6/28/2017 10:03:40 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1980244
IBM Index Class Name
Hydrology
Doc Date
6/26/2017
Doc Name
Demonstration of Compliance with WQCC Regulation No 41
From
Newmont
To
DRMS
Email Name
TC1
Media Type
D
Archive
No
Tags
DRMS Re-OCR
Description:
Signifies Re-OCR Process Performed
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8 - - __._ __._._-_.__.----- ------------___ __.. __.._ __._._.._._. ._.._. -. 18 <br /> 7.8 .... __.._. - _._. __ • 16 <br /> 7.6 _. _._.__. __....___--__—_—____.___-.____-__-_._.____- ---___ <br /> 14 <br /> 7.4 <br /> r 12 <br /> 7.2 <br /> N 10 <br /> • • <br /> 6.8 <br /> n <br /> 8 <br /> n <br /> • 6 <br /> I . • . 4 <br /> 6.46.2 _._.... . <br /> • 2 <br /> 8 S 8 8 8 8 8 8 8 8 8 8 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 <br /> —+—VIN 2A-270 -+—VIN 28-140 + Precip —Poly.(VIN 26-140) —Poly.(Precip) <br /> Figure 13: Precipitation(total between sampling events)and field pH in Vindicator Valley. <br /> 5.4 Poverty Gulch <br /> The Poverty Gulch compliance monitoring well is PGMW 2. However, this well has been dry since it was <br /> constructed 19 December 2001. Two other monitoring wells in Poverty Gulch, PGMW 1A-200 and <br /> PGMW 113-55, were sampled from 31 March 2000 through 10 April 2001, with one additional sample <br /> taken from PGMW 1 B-55 on 9 July 2001 (these wells were subsequently dry until the last attempts were <br /> made to sample them in October 2005). Both of the PGMW 1 wells were plugged and abandoned <br /> sometime after October 2005. In the absence of data from PGMW 2, the data from the other two wells <br /> were used in the analysis. <br /> Groundwater sampled in Poverty Gulch has the fourth highest geometric mean concentration of sulfate, <br /> the lowest field pH, highest zinc, and second highest manganese geometric mean concentrations of the <br /> six drainages, but the time period represented by the data is less than 1.5 years. Identification of trends <br /> for each of the analytes is difficult due to the short record of data. <br /> Sulfate, field pH, and precipitation (measured at the Rigi meteorological station, totaled between sampling <br /> events) data are shown in Figure 14. No clear relationship between precipitation and sulfate or pH is <br /> evident. It appears that sulfate concentrations and pH are relatively stable. <br /> Figure 15 presents the manganese and zinc concentrations, and precipitation totaled between sampling <br /> events, for the Poverty Gulch monitoring wells. No clear relationship is apparent between precipitation <br /> and either manganese or zinc. In general, concentrations are relatively stable, although both manganese <br /> and zinc were declining in PGMW 1 B-55 during the last three sampling events. <br />
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