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Universal Soil Loss Equation Questions and Answers

1.

The soil erodibility factor needs to be determined for use in the universal soil loss equation. The length, in m and slope, in % of the experimental plot to be used for this purpose, respectively are

Exam Year(s)

GATE AG - 2012,

Answer: C

The plot is 22 m long on a 9% slope.

In the universal soil loss equation the erodibility factor K is defined as the soil loss per unit of rainfall erosion index measured on the standard unit plot: 72.6 ft (22.1 m) long on a uniform 9% slope, kept in continuous clean-tilled fallow with tillage up and down the slope. The slope length and steepness factors L and S equal 1 for exactly this plot, which is why the other dimensions are adjusted relative to it.

The other length and slope pairs (19 m and 12%, 21 m and 11%, 23 m and 8%) are not the standard plot, so a K measured on them would have to be corrected through L and S before use.

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2.

For a watershed where no conservation practice is followed, the value of conservation particle factor (P) to the used in universal soil in universal soil loss equation for estimation of soil loss will be?

Exam Year(s)

MP Lab Technician - 2015,

Answer: C

With no conservation practice, the factor P is 1.0.

In the Universal Soil Loss Equation, A = R K L S C P, the support practice factor P is the ratio of soil loss with a practice such as contouring, strip cropping or terracing to the soil loss with straight up-and-down slope farming. With no practice, the two are the same, so P = 1. Practices reduce P below 1, for example to about 0.5 for contouring on moderate slopes.

P = 0 would mean no soil loss at all, which no practice achieves. 0.5 is a typical value with contouring, and 1.5 is impossible, since P never exceeds 1.

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