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<br />It is important that the sampling area be representative of the <br />roughness coefficient of the cross section. By examining the cross <br />section closely in the field, a representative-sampling area can be <br />chosen. Another way to better determine the roughness coefficient is to <br />select several representative areas and compare the results. It should <br />be pointed out again that cross sections should be divided into subsec- <br />tions when changes in roughness properties dictate. <br /> <br />All of the trees, including vines, in the sampling area must be <br />counted and the diameter measured to the nearest 0.1 ft. Each tree <br />diameter is measured at a height that will give an average diameter for <br />the expected flow depth of the sample area. <br /> <br />Determining the area of the trees in the sampling area is not very <br />difficult. A sampling area 100 ft along the cross section by 50 ft in <br />the flow direction is generally adequate to determine the vegetation <br />density of an area when the sample area is representative of the flood <br />plain. A 100-ft tape is stretched out perpendicular to the flow direction <br />in the sample area. Every tree within 25 ft along either side of the <br />100-ft tape is counted. 'Ihe position of the tree is plotted on a grid <br />system by measuring the distance to each tree from the centerline along <br />the 100-ft tape and the diameter of the tree is recorded on the grid <br />system. (See fig. 4.) <br /> <br />The area, L Ai, occupied by trees in the sampling area can be <br />computed from the number of trees, their diameter, and the depth of flow <br />in the flood plain. Once the vegetation area, LAi' is determined, the <br />vegetation density can be computed using equation 8 and the n value for <br />the subsection can be determined using equation 7 with appropriate values <br />for no, R, and C*. <br /> <br />where L nidi = <br /> h = <br /> w = <br />and 1 = <br /> <br />Equation 8 can be simplified to <br /> <br />LA. h Ln.d. <br />1 1 1 <br />vegd = AL = hwl <br /> <br />the summation of number of trees multiplied by <br />tree diameter, in feet; <br />height of water on flood plain, in feet; <br />the sample area width, in feet; <br />the sample area length, in feet. <br /> <br />(11) <br /> <br />Example of use of direct technique.--An example of how to compute n <br />for a flood plain using the direct method for vegetation density is shown <br />in figures 4 and 5. A representative sample area along the cross section <br />is chosen. The Vegd of the sample area is determined by measuring the <br />number and diameter of trees in the 100 ft by 50 ft area. 'Ihis is easily <br />done by plotting the location and diameter of the trees, in the sample <br />area on the grid shown in figure 4. The numbers by the dots in figure 4 <br />are the diameters of the trees, in tenths of a foot, except for those <br />numbers underlined. The numbers underlined are the diameters of the <br />trees in feet. <br /> <br />20 <br />