structure salinity sodicity Flashcards
soil structure controls
size and arrangement of pores
soil structure is developed by 2 processes
physical and biological processes
Soil structure controls 3 imp properties:
Permeability, pore size and soil strength
Soil structural stability describes the…
ability of soil structure to be retained when stressed (e.g. wetting, traffic)
Two processes that degrade soil structure
DIspersion and slaking
Two ways to enhance structural stability
Increasee OM content, and add sources of Ca, especially gypsum and lime
What changes to soil structure from poor structural stability, and can they be measured?
- generation of finger material on wetting
+eg. slaking produces smaller aggregates
+ e.g. dispersion: colloids (dispersed clay)
-decreaseed permeability
+simple lab tests of hydraulic conductivity - increased strength
+penetrometer resistance
Mechanisms that destroy soil structure
- Tillage
- Compaction
- Grazing
- Raindrop impact
- Slaking
- dispersion
Slaking
Water moves into pores, rapid wetting, air has to go somewhere, starts pushing outwards. Increased water content causes swellling which reduces strength. Agg starts breaking down
Dispersion
Na: Ca ratios. Clay platelets spread apart. Float around when wetting occurs
Conserving soil structure. Maximise soil stability by:
- Avoid soil disturbance (minimum tillage, no traffice, reduce grazying, increase plant cover)
- Increase OM - plant residue rotation, more pasture, reduced tillage
- Calcium amendments (lime (CaCO3), gypsum (CaSO4, 2 H2O)
Restoring soil structure
- maximise plant and biological activity (plants, roots provide glue to stick aggs together)
- OM/ Ca inputs