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PERMFILE53867
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PERMFILE53867
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Entry Properties
Last modified
8/24/2016 10:57:10 PM
Creation date
11/20/2007 3:57:24 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1977004
IBM Index Class Name
Permit File
Doc Date
8/31/1984
Doc Name
Response to Adequacy
From
Homestake
To
DMG
Media Type
D
Archive
No
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-8- <br />Item: Accuracy of the values and units in Table 5-2. <br />Res~ons~e: Table 5-2 incorrectly omits a factor 10-6 in both columns 2 and <br />3, the concentrations in rock material, and in leachate, respectively. The <br />following corrections should be made: (1) in Table 5-2, change 103 to 10-3 <br />in column 2; multiply each number in column 3 by 10-6 (except for Ra values <br />which remain the same; (2) in Table 5-3, multiply mg/ml concentrations in <br />columns 2, 3, and 4 by 10-6 (leave Ra the same). The tables with corrected <br />headings are attached. <br />It is stressed that the projected concentrations of elements in the <br />drainages are extremely low and would likely be undetectable. <br />Item: Two items regarding the projections of leachate: first, the <br />representativeness of the rainfall return event in comparison to snowmelt <br />event in regard to producing leachate on the low-grade stockpiles was queried; <br />secondly, the volume of infiltrating run-off produced and the timing of <br />the peak run-off was discussed. <br />Response: The 1.7 inch rainfall event used was the maximum daily rainfall <br />reported in a two year span of meteorological data accumulation in the 1970's <br />at the project. It is assumed to be a worst-case condition. The relationship <br />between this event and snowmelt event is discussed later in reference to <br />another question. The rainfall event was used to represent conditions during <br />the season when maximum infiltration would be expected or the hypothetical <br />case under consideration. All water falling on the graded low-grade stockpile <br />was discussed to enter the pile. <br />In the absence of other information, the uniform rainfall distribution <br />over the 24-hour period was assumed, as was the coincidence of peak run-off and <br />leachate discharges. The observation regarding the noneven distribution of <br />rainfall is correct. The assumption regarding the average flow, while being <br />approximation to actual conditions, when taken with the other highly conservative <br />assumptions in the analysis such as unrestricted flow of the total volume <br />into the low-grade ore; no evapotranspiration; no dispersion or retardation; <br />and a constant lea hate production rate, (i.e. on the order of 10-10 mg/ml <br />for metals and 10-~ pCi/1 for Ra226) provided estimated concentrations in <br />Indian Creek that were negligibly small. Calculations using higher amounts <br />of inflow into the low-grade ore would have to take into account correspondingly <br />higher rates of run-off and flow in Indian Creek. These factors would maintain <br />the low concentrations. <br />Item: The potential effect of leachate contamination as a result of the Tow <br />grade ore stockpile clay cap rupturing due to settling or construction <br />procedures. <br />Res onse: As noted previously in response to one of Dr. Jim Pendleton's <br />geotechnical concerns, the clay cover did not enter into the calculations <br />of leachate concentrations. The calculations were made assuming no lower- <br />permeability clay cover. A rupture in the clay cover would therefore not <br />result in an increase in infiltration and the leachate concentrations would <br />remain as projected. The clay cover would, of course, reduce infiltration <br />into the low-grade ore material and lessen the flow-through from that used <br />in the hypothetical case. <br />
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