a.<\/strong><\/span> Determine the water level in the tap building<\/strong><\/span> b.<\/strong><\/span> Determining the slope of the line in the field,<\/strong><\/span>
\n High water levels in the tap building tertiary primary or secondary channel can be calculated by the following equation:<\/span>
\n P = A + a + b + c + d + e + f + g + \uf044h + z<\/strong><\/span>
\n Where:<\/span>
\n P = water level in the primary or secondary channel<\/span>
\n A = altitude wetland<\/span>
\n a = a layer of stagnant water in paddy fields (10 cm)<\/span>
\n b = loss of high-energy disaluran quarter to rice (5 cm)<\/span>
\n c = high loss of energy in the box for the quarter (5 cm)<\/span>
\n d = high energy loss during drainage in irrigation canals<\/span>
\n e = high loss of energy in the box for<\/span>
\n f = high loss of energy in culvert<\/span>
\n g = high loss of energy in the tap building<\/span>
\n \uf044h = variations in water level<\/span>
\n z = high loss of energy in other tertiary buildings<\/span><\/p>\n
\n<\/strong> The slope of the line follows the slope of the land on topographic maps (contour).<\/span> The best way is to plot the elevation at the point of intersection with a line trace the contour lines<\/span>
\n
<\/a>
\n Figure 17. Determining the slope of the line<\/span><\/p>\n