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PERMFILE44342
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PERMFILE44342
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Entry Properties
Last modified
8/24/2016 10:46:47 PM
Creation date
11/20/2007 11:53:44 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1999002
IBM Index Class Name
Permit File
Doc Date
1/21/1999
Doc Name
PERMIT APPLICATION DRAFT SOIL CONSERVATION EROSION AND SEDIMENT CONTROL RECLAMATION AND REVEGETATION
Section_Exhibit Name
Appendices A-E
Media Type
D
Archive
No
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I~ <br />1 <br /> <br /> <br /> <br /> <br />1 <br /> <br />1 <br /> <br /> <br />1 <br />1 <br />1 <br />1 <br /> <br /> <br /> <br />1 <br />S <br />the trench and partially buried roll will act as asemi-permeable water and sedimem trap, <br />serving to provide an improved growth zone on steep dry slopes. Once rows of vegetation <br />are established they may be expected to create then own habitat and continue to invade the <br />slope. As the rolled blanket deteriorates over time, the vegetation will effectively replace it. <br />Level Spreader <br />A level spreader is a level section of ditch that is used to pool water at the end of a ditch, <br />diversion, or channel. The pool formed by the spreader transforms small concentrated <br />flows into sheet flows when it overflows (Figure C-4). Sheet flow is less erosive than a <br />concentrated flow and it may be used to irrigate vegetation. The gradient of the level <br />spreader ditch must be 0%. The ditch should be at least 6 inches deep and 6 inches wide at <br />the containment level. The lip of the spreader should be of non~rodible material or be <br />protected with erosion control blanket or gravel mulch (Figure C-5). The structure should <br />be inspected and maintained after significant runoff events. Spreaders help to prevent <br />erosion and improve soil moisture content which in turn improves plant growth. <br />Terracing <br />The slope and length of a hillside combined with soil physical characteristics affect its <br />stability. The longer a slope becomes the more susceptible it is to water erosion. Hillsides <br />of equal slopes and lengths, but with different soil physical characteristics will erode at <br />different slope distances. Terraces may be used to limit slope length and effectively control <br />erosion and sedimentation (Figure C-6). Terraces can be built on the level and adequately <br />sized to provide total containment for the slope that drains to them. They can also be placed <br />on low gradient slopes and drain to reconstructed channels. Terrace spacing will be <br />adjusted for slope and soil characteristics. The Revised Universal Soil Loss Equation <br />("RUBLE") may be used to calculate proper spacing for slopes based on site-specific <br />conditions. Factors taken into consideration include rainfall, soil erodibility, and steepness <br />of slope. On very steep slopes (i.e., greater than 2h:ly) terracing may be impracticable <br />because of the amount of material that must be moved and the relatively short distance <br />between structures. Tertaces make good permanent secondary drainage features for <br />reclaimed areas. <br />C-3 <br />
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