Back to results

University of Saskatchewan

Variability of soil erodibility: its relationship to topography and soil properties in cultivated landscape

Abstract

dc:description.abstract

The hypothesis of this thesis is that soil erodibility varies systematically with landscape topography. This hypothesis was tested by using a portable rainfall simulator to measure the relative soil erodibility at five slope positions along eleven slope transects on fallow agricultural land in hummocky terrain. Soil erodibility variations among the five slope units were examined for significant differences. The slope units were found to be ranked in descending order by mean soil erodibility as follows: shoulder, midslope, footslope, summit, toeslope. This systematic pattern of erodibility was evident even though topographic characteristics and soil properties varied substantially between the slope transects sampled within the small study area. Differences in erodibility were attributed to soil property differences along the slopes. Correlation and multiple regression indicated that soil properties had a stronger relationship to soil erodibility than did topographic variables. Particle size distribution, bulk density and organic matter had the most significant effect on erodibility variations. Aggregation measures were not found to be good indicators of soil erodibility. Topography was thought to influence erodibility indirectly through its effect on the distribution of soil properties along the slope transects based on the higher correlations between topographic variables and many soil properties. Higher correlations between erodibility and soil and topographic variables were found when analyzed by slope position, especially on the midslope. This indicates that soil properties were more uniform when grouped by slope position than when considered as a single, large data set. This study suggested that the use of a catena approach to examine soil erodibility is an important consideration when studying soil erosion processes in agricultural landscapes.

Degree

thesis:*
Name thesis:degree_name
Master of Science (M.Sc.)
Level thesis:degree_level
Masters
Discipline thesis:degree_discipline
Geography
Grantor
University of Saskatchewan
Year dc:date.issued
1989

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Christianson, Donald Dean
Advisor dc:contributor.advisor
  • Martz, Lawrence
Committee members dc:contributor.committeemember
  • Smith, D.
  • Barr, B.
  • Pooler, J.
  • McLennan, B.D.

Rights

Language dc:language.iso
en_US

Identifiers

dc:identifier.*
OAI identifier oai:identifier
oai:harvest.usask.ca:10388/etd-06052012-084359

Chain of custody

source
Harvested from
University of Saskatchewan
Base URL
harvest.usask.ca/server/oai/request
Last updated
2026-07-24
Source record
OAI-PMH GetRecord
related terms
citation

Christianson, Donald Dean. Variability of soil erodibility: its relationship to topography and soil properties in cultivated landscape. Masters thesis, University of Saskatchewan, 1989. https://hdl.handle.net/10388/etd-06052012-084359