|Monger, H. Curtis - NEW MEXICO STATE UNIV|
Submitted to: Agronomy Society of America, Crop Science Society of America, Soil Science Society of America Meeting
Publication Type: Abstract Only
Publication Acceptance Date: August 9, 2005
Publication Date: November 6, 2005
Citation: Monger, H.C., Bestelmeyer, B.T. 2005. Soil geomorphic change during desertification [abstract]. ASA-CSSA-SSSA International Annual Meetings, November 6-10, 2005, Salt Lake City, Utah. Paper No. 200-5. Interpretive Summary: No interpretive summary required.
Technical Abstract: The objective of this paper is to illustrate the concept of the soil-geomorphic template and its relationship to biotic change. Desertification, as an example of biotic change toward a degraded state, is a common phenomenon in many arid and semiarid regions of the world. Such biotic change is typically accompanied by and linked to geomorphic change. Geomorphic factors that are involved in biotic change are soil, topography, and soil parent material, which together form the soil-geomorphic template. Soil is involved because it is the substrate that provides water, nutrients, anchorage for roots, and habitat for burrowing animals. Topography is involved by its influence on microclimate via elevation, lateral redistribution of water, and slope aspect. Soil parent material is involved by its contribution to the nutrient supply. Numerous linkages and feedback-loops occur between the soil-geomorphic template, microclimate, vegetation, and animals. A perturbation in any of these factors can steer an ecosystem from one state to another. Some soil-geomorphic templates are more prone to change than others. For example, landscapes with sandy soils are more vulnerable to desertification than landscapes with fine-textured soils that receive run-in water and, therefore, require distinct management practices. Desertification involving simultaneous changes in biotic and geomorphic states provides a good example of how biological and geological systems are coupled and co-evolve.