Conclusions

Soil erosion involves complex, heterogeneous hydrological processes and models can only simulate these processes. USLE model is simple to use and conceptually easy to understand, but the greatest criticism of this model has

TopograpKc map

Slope & Slope kngth itt^s

Saielli*? daia (m^LD^JSSHI)

Slope & Slope kngth itt^s

Kllíl TVUfll

1

K-Factor

nqi

Meteorological <Lic>

Ii»iiliw mm

C-Factor mop

ITSTF ÜSOn.FlíOfilONTHOnFT,

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