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<br /> <br />.. <br /> <br />I\) <br />w <br />I\) <br />t.lJ <br /> <br />Table 1. Volume-Weights of Soils <br /> <br />Soi 1 Texture <br /> <br />Volume-Weight <br /> <br />Clay <br />Silt <br />Sand <br />Gravel <br />Loam' <br />Sandy loam <br />Gravelly loam <br /> <br />60-70 pcf <br />75-90 <br />90-110 <br />110-120 <br />80-100 <br />90-110 <br />110-120 <br /> <br />SAMPLE CALCULATIONS <br /> <br />1. There are 12 miles of first order streams in the Doodad Watershed. You go <br />out to sample one mile of a first order stream. One bank is grassed and <br />noneroding. The other bank is a sandy loam soil and three spots are bare. <br />Two of the spots are 600 and 800 feet long. The banks are bare with a few <br />roots exposed and some rills. There is no grass overhang above the two <br />spots and the bare areas are about 10 feet high. The third spot is on the <br />outside edge of a curve in the stream. It is 1,200 feet long and the bare <br />banks are 12 feet high. Two fence posts are lying at the base of the bare <br />bank and two trees have fallen into the channel. Most of the bank has <br />rills and a~out 2 inches of grass overhang is at the top of the bank. <br />Based on your sample, how much streambank erosion is occurring on 1st <br />order streams in the Doodad Watershed? <br /> <br />Use direct volume method: <br /> <br />(eroding area) (lateral recession rate)(density) i <br />- eros on <br />2000 pounds/ton <br /> <br />1400 ft x 10 ft x 0.06 ft/yr x 100 pcf _ 42 tons/yr/sample <br />2000 pounds/ton <br /> <br />1200 ft x 12 it x 0~4 ft/vr x 100 pcf _ 288 tons/yr erosion <br />2000 pounds/tDn 330 tons/yr erosion <br /> <br />2600 ft. eroding _ 25% of sample was eroding <br />2 bank miles sampled <br /> <br />330 tons/yr erosion _ 660 tons/yr/bank mile is erosion rate <br />~ mile eroding : <br />12 miles of 1st order streams x 25% - 3 total miles eroding <br />3 miles x 2 banks/mile - 6 total bank miles eroding <br />6 bank miles eroding x 660 tons/yr/bank mile - 3960 tons/yr bank erosion <br /> <br />23 <br />