Submitted to: International Symposium on Gully Erosion Under Global Change Proceedings
Publication Type: Abstract Only
Publication Acceptance Date: 1/30/2003
Publication Date: 11/30/2003
Citation: McCool, D.K., Williams, J.D. Freeze/thaw effects on rill and gully erosion in the northwestern wheat and range region. International Symposium on Gully Erosion Under Global Change Proceedings.
Technical Abstract: Hydrology of the Northwestern Wheat and Range Region (NWRR) of the Pacific Northwest USA is dominated by winter events. Fifty-five to sixty-five percent of the annual precipitation occurs from November through March, and formation of impermeable frost, intensified by excessive tillage and tillage pans, has long been a major factor in rill and gully formation in the region. Saturated zones can form above tillage pans, freeze solid, and significantly reduce infiltration. Frost-heaved surface soils thaw and weaken with warming temperatures or rain. Under these conditions, runoff from rain or snowmelt or a combination of the two is inevitable, concentrating in rills and channels and carrying with it the loosened soil. Slopes are frequently quite steep and there may be little deposition above the toe slope. Classical over-fall head-cut gullies are uncommon. Concentrated flow channels form because of collection of water from impervious areas such as conventionally tilled fall seeded small grain and bare grass seed fields. Gullies are also created by seepage from saturated layers above permanent restrictive layers in the soil. Gullies can also result from terrace failures due to rodent burrows and low compaction at the time of construction. In naturally unconsolidated soil, rodent activity can lead to piping failures that remove large quantities of soil. Rill measurements on conventionally tilled fields in Oregon, Washington, and Idaho were used to determine coefficients for relationships between slope length and steepness and rill size. The steepness relationships differed from those found in the eastern US. Concentrated flow channels seem to exhibit unique characteristics as well. Consideration of the unique hydrological characteristics of the region will improve erosion and sediment transport modeling.