Abstract
The magnitude of difference between the predicted detachment rates and the measured interrill sediment delivery rates decreased with clay content. This suggests that in coarse-textured soils, most of the rain-detached sediments are redistributed within the interrill area. Small differences between detachment rates and sediment delivery rates in clayey soils indicate that the interrill erosion is detachment limited. A rainfdrop-induced interrill transportability parameter is derived by dividing the measured sediment delivery rates with the product of rainfall rate and unit effective kinetic energy. -from Authors
| Original language | English (US) |
|---|---|
| Pages (from-to) | 727-734 |
| Number of pages | 8 |
| Journal | Soil Science Society of America Journal |
| Volume | 59 |
| Issue number | 3 |
| DOIs | |
| State | Published - 1995 |