4: Soil Structure Flashcards
Soil structure
Defines how soil mineral particles (sand, silt and clay) are bound together and arranged in the three dimensional space
Peds or aggregates
Are the structural units in soil formed by particles bound together
Why is soil structure important?
Determines soil capacity to hold water and air
Provides habitat for microorganisms
Provides physical protection of organic matter/C sequestration
Granular
A good, healthy soil structure
Aggregates look like “cookie crumbs”
Particles held together by organic substances
Wedge
Elongated shape; polished surface (slickensides)
Caused by the shrink-swell process
Platy
Thin, flat, horizontal plates
Compacted surface soils
Blocky
Irregular blocks
1.5-5.0 cm in diameter
Particles held together by clay
Prismatic
Vertical columns
Particles cemented by shrink/swell (smectitic) clay
Columnar
Vertical columns with rounded tops
Massive
Structureless
Have fine texture, essentially making them massive clumps
Single grain
Mostly made of sand
Balance between micro and macropores
Micropores hold water more tightly than macropores. Macropores and structure are critical for good drainage and aeration.
The balance between them determines if a soil drains well but also holds enough water