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2013-10-30_REVISION - M1977310 (3)
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2013-10-30_REVISION - M1977310 (3)
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Last modified
6/15/2021 2:28:45 PM
Creation date
11/5/2013 5:47:39 PM
Metadata
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Template:
DRMS Permit Index
Permit No
M1977310
IBM Index Class Name
REVISION
Doc Date
10/30/2013
Doc Name
DRAINAGE DESIGN PLAN FOR THE JD6 MINE
From
COTTER
To
DRMS
Type & Sequence
AM1
Email Name
TC1
SJM
Media Type
D
Archive
No
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JD -6 Mine — Drainage Design Plan 2 <br />2. DESIGN CRITERIA & METHODOLOGY <br />2.1 Design Storms <br />The magnitudes of design storms for the site are shown in Table 2. The rainfall intensities for 24 -hour <br />storms with 2 -year to 100 -year recurrence intervals were interpolated from the NOAA Atlas 2, Vol. III <br />(USDC, 1973), for the purpose of runoff calculations and engineering design. Per DRMS <br />recommendations, control structures for the JD -6 Mine presented in this design report are engineered to <br />contain the 10 -year 24 -hour storm event and safely pass a 100 -year 24 -hour storm event. <br />Table 2. Design Storm Parameters <br />Recurrence <br />Interval <br />Duration <br />(Hours) <br />Storm Magnitude <br />NOAA Atlas <br />inches <br />100-year <br />24 <br />3.0 <br />50-year <br />24 <br />2.7 <br />25-year <br />24 <br />2.4 <br />10-year <br />24 <br />2.0 <br />5-year <br />24 <br />1.6 <br />2-year <br />24 <br />1.2 <br />2.2 Runoff Estimates <br />2.2.1 Volume <br />Catchment runoff was estimated using Technical Release 55 (TR -55) developed by the U. S. Department of <br />Agriculture Natural Resources Conservation Service (NRCS, 1986). TR -55 presents simplified procedures <br />to calculate storm runoff volume, peak rate of discharge, hydrographs, and storage volumes required for <br />floodwater reservoirs in small watersheds. <br />Runoff depth (qd) is calculated in TR -55 by the Curve Number (CN) method, using the following equation: <br />(P — 0.26)2 <br />Rd _ (P +0.8S) <br />where: qd = Runoff depth, inches (qd = 0, if P < 0.2S), <br />P = Rainfall depth, inches <br />S = Potential maximum rainfall retention after runoff begins, inches <br />This method assumes initial abstraction (losses before runoff begins due to retention in surface depressions, <br />interception by vegetation, evaporation, infiltration etc.) is equal to 0.2S. <br />The parameter S is related to curve number (CN) by: <br />S = 1000 _ 10 <br />CN <br />Site soils consist predominantly of Bodot and Ustic Torriorthents, which are listed as hydrologic soil group <br />C in the NRCS Web Soil Survey (NRCS, 2012a, 2012b). Site - specific curve numbers are discussed in <br />Section 3. <br />4148A.131028 Whetstone Associates <br />
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