Area of a level cross-section (embankment or cutting)
A=Bd+sd2B = formation width; d = depth or height at centre; s = side slope (s horizontal : 1 vertical)
Mid-sectional area method
V=L(Bdm+sdm2),dm=2d1+d2L = distance between sections; d1, d2 = depths at the two ends
Mean (average) area method
V=L⋅2A1+A2A1, A2 = end areas; L = distance between them
Same as the end-area (trapezoidal) rule for one interval
Trapezoidal (end-area) rule for a series of sections
V=D[2A1+An+A2+A3+⋯+An−1]D = common interval; A1 … An = cross-sectional areas
Prismoidal formula (two end sections)
V=6L(A1+4Am+A2)Am = area of the mid-section (not the mean of A1 and A2)
Prismoidal (Simpson's) rule for a series of sections
V=3D[A1+An+4(A2+A4+⋯)+2(A3+A5+⋯)]D = common interval; n must be odd
Requires an even number of intervals
Prismoidal correction (level sections)
Cp=6Ls(d1−d2)2s = side slope; d1, d2 = end depths
Prismoidal volume = trapezoidal volume − Cp
Volume from spot levels (borrow pit, grid of squares)
V=4A(∑h1+2∑h2+3∑h3+4∑h4)A = area of one square; h1, h2, h3, h4 = depths common to 1, 2, 3 and 4 squares