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2008-12-05_REVISION - C1980007 (2)
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2008-12-05_REVISION - C1980007 (2)
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Entry Properties
Last modified
8/24/2016 3:38:40 PM
Creation date
12/8/2008 4:27:09 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1980007
IBM Index Class Name
REVISION
Doc Date
12/5/2008
Doc Name
Summary of Review
From
TAK
To
File
Type & Sequence
TR115
Media Type
D
Archive
No
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Calculation of runoff volumes using Rational Method (for TR-115) <br />Accumulated Curve <br />precipitation, Number, <br />P, in inches CN <br />(acreage- <br />Pond weighted <br />back- <br />calculation <br />10-yr, 24-hr. <br />MB-1 1.9 <br />MB-2R 1.9 <br />MB-3 1.9 <br />MB-5 1.9 <br />SGA 1.9 <br />RPE 1.9 <br />25-yr, 24-hr. <br />MB-1 2.3 <br />MB-2R 2.3 <br />MB-3 2.3 <br />MB-5 2.3 <br />SG-1 2.3 <br />RPE 2.3 <br />S=(1000/ Accumulated Accumulated <br />CN) - 10 runoff, Q, in runoff w/o <br />inches = [(P- initial <br />(0.2XS)j^/[P+( abstractions, <br />0.8)(S) Q', in inches = <br /> PA 2/P <br />No. of acres in Accumulated For <br />contributing acre-feet of <br /> <br />drainage area runoff for comparison: <br /> Accumulated <br />drainage = acre-feet of <br />(Q/12)Xacres <br /> runoff for <br /> drainage per <br /> TR-115 <br /> submittal <br />71 4.08 0.227 1.900 91.2 1.72 1.705 <br />82 2.20 0.584 1.900 100.6 4.89 4.918 <br />83 2.05 0.628 1.900 8.3 0.43 0.443 <br />66 5.15 0.126 1.900 12.4 0.13 0.126 <br />61 6.39 0.055 1.900 2717.4 12.46 12.522 <br />71 4.08 0.227 1.900 61.7 1.17 1.2 <br />72 3.89 0.428 2.300 91.2 3.25 2.713 <br />82 2.20 0.854 2.300 100.6 7.16 7.106 <br />83 2.05 0.907 2.300 8.3 0.62 0.647 <br />66 5.15 0.251 2.300 12.4 0.26 0.251 <br />61 6.39 0.141 2.300 2717.4 31.86 29.33 <br />71 4.08 0.395 2.300 61.7 2.03 1.988 <br />Prepared by T. Kaldenbach, 12/5/08 <br />Initial abstraction(0.2 X <br />S) <br />0.82 inches <br />0.78 inches <br />Note: The SCS CN method assumes that the initial <br />abstraction (losses before runoff begins) = 0.2 S, with S <br />calculated as (1000/CN) - 10. If P<0.2 S, then no runoff <br />occurs because all precipitation is lost to initial abstraction <br />(i.e. evaporation, plant consumption, storage in depressions, <br />and infiltration)
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