Tl. Chow et Hw. Rees, EFFECTS OF COARSE-FRAGMENT CONTENT AND SIZE ON SOIL-EROSION UNDER SIMULATED RAINFALL, Canadian Journal of Soil Science, 75(2), 1995, pp. 227-232
Farmers have long considered coarse fragments a hindrance in potato pr
oduction. Rock picking or crushing has become a routine operation. Usi
ng simulated rainfall events and runoff-erosion plots (1 m X 1 m), the
effects of coarse-fragment content (0, 7, 15 and 25% by volume) and s
ize (1.0-1.9, 1.9-5.1 and 5.1-7.6-cm diam) on runoff, infiltration and
soil loss were evaluated on an Orthic Dystric Brunisol. Study objecti
ves were to quantify the influence of coarse fragments on soil erosion
and to convert these relationships into mathematical equations for us
e with existing models to predict soil loss. Although there were only
marginal increases in infiltration and reductions in runoff attributab
le to increasing content and size of coarse fragments, the rate of soi
l loss from the control was higher than that from all other treatments
. In general, the rate of son loss decreased with increasing content a
nd size of coarse fragments. The effects of content and size of coarse
fragments on soil-loss reduction, either individually or in combinati
on, were expressed mathematically with correlation coefficients greate
r than 0.82. The study also revealed that for a given volumetric coars
e-fragment content, the percentage surface cover increased with increa
sing coarse-fragment size. This finding has important practical implic
ations because most reporting of coarse fragments is done on the basis
of volume rather than percentage surface cover.