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2012-02-28_REVISION - M1980244 (73)
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2012-02-28_REVISION - M1980244 (73)
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Last modified
8/24/2016 4:49:12 PM
Creation date
3/15/2012 1:40:25 PM
Metadata
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Template:
DRMS Permit Index
Permit No
M1980244
IBM Index Class Name
REVISION
Doc Date
2/28/2012
Doc Name
VOL 5, Appendix F: Surface Water Hydrology
From
CC&V
To
DRMS
Type & Sequence
AM10
Email Name
TC1
Media Type
D
Archive
No
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SOIL TYPES AND RUNOFF CURVE NUMBERS <br />As is required to use the TR 55 method, the surface runoff characteristics of the <br />drainage area were determined based on the natural and "artificial" soil types <br />in Arequa Gulch. Three soil categories were developed and are designated <br />"original ground," "roads and dumps," and "fill slopes." Original ground, as <br />demonstrated over the past years by the limited runoff, has a relatively low <br />runoff coefficient. Fill slopes, as has been evidenced on site by the lack of <br />runoff off from the slopes, also have relatively low runoff coefficients. Haul <br />roads, which comprise the third category, have high runoff coefficients for most <br />precipitation events as a result of compaction. These three categories are <br />further described below. <br />Original Ground: Soil Type B (Moderately Low Runoff Potential - e.g., <br />mostly sandy soils and loess). Consists primarily of 4" <br />to 12" of coarse topsoil covered with grass, brush, or <br />trees and underlain by a loose, rocky sandy soil. <br />Viewed as either thin vegetative stand with limited <br />cover (if rangeland or meadow) or with good vegetative <br />cover (if forest land). This category also includes <br />revegetated ground. (Surface area characterized in this <br />manner_will initially diminish, but then will reappear <br />as reclaimed surfaces are developed.) <br />Roads and Stock Soil Type D (High runoff potential e.g., shallow soils <br />pile Surfaces: with nearly impermeable subhorizons). Consists of haul <br />roads and horizontal surfaces of overburden storage <br />area. Compacted by haul trucks. (Surface area in this <br />category will generally diminish with time.) <br />Fill Slopes: <br />Coefficient: Wooded 66 Grasses 71 <br />Coefficient: 90 <br />Soil Type A (Low runoff potential e.g., deep sands with <br />little silt and clay). Consists of segregated coarse <br />rock overburden faces with high infiltration rate. No <br />runoff is observed from these slopes. (Surface area in <br />this category will remain more or less constant, until <br />completion of the storage area, and will then decrease <br />as the overburden faces are graded and reclaimed.) <br />Coefficient: 50 <br />These coefficients, upon delineation of the area to which they apply in any one <br />subbasin, were developed into a composite coefficient for each subbasin, based <br />on relative areas, to form a single curve number for each the drainage <br />subbasins. <br />AREQUA GULCH OVERBURDEN STORAGE AREA CONSTRUCTION SEQUENCE <br />Because the Arequa Gulch Overburden storage area is to be constructed over a <br />number of years, the drainage control plan has been developed to accommodate the <br />changes that will occur over time. Five points in time were used to assess and <br />modify the drainage controls. These "configurations" of the storage area are <br />presented in five of the six plan views accompanying this documentation (see <br />Attachments). The five plans show approximations of the topographic <br />configurations that would likely develop as the storage area is built. This <br />allows delineation of the drainage areas that will develop and incorporates the <br />changes in surface type as the undisturbed land is disturbed and then <br />revegetated. Field- adaptation of the drainage facilities depicted will occur, <br />given the need to be responsive to changes in the construction or construction <br />3 <br />
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