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2correlation value was 0.76 in relation to the simplifi ed K factor, 0.87 to K1, and 0.86 to K2 (very similar due to the small signifi cance of silt in the equation). This relationship demonstrates that the application of K1 and K2, according to the readiness of the data, is more specifi c and exact than the results obtained by applying the simplifi ed K factor.

Estimation of soil erosionability in the stream basin of Pillahuinco Grande, Province of Buenos Aires, Argentina