Weathering, soil formation and chemical export
Mechanical weathering changes fragment size; chemical weathering transforms or dissolves minerals through reactions such as hydrolysis and oxidation.
Key knowledge
Mechanical weathering changes fragment size; chemical weathering transforms or dissolves minerals through reactions such as hydrolysis and oxidation. Soil formation combines weathered mineral material, organic processes, water/air and transport. Climate, organisms, parent material, relief and time influence the resulting profile.
Conditions and scope
- Soils do not all have one mineral/organic/pore percentage or fixed thickness.
- A mineral's weathering rate depends on accessibility and solution conditions, not solely mineral name.
Sources · 2
References
Sources retain their recorded scope. A source link alone does not establish verification of every statement.
Steven Earle — Physical Geology, 2nd edition, BCcampus Open Education2 sources
Evidence and review
Read weathering controls/hydrolysis/oxidation and soil mixture/texture/profile controls; excluded unbalanced illustrative equation and universal composition numbers.
2026-10-10 · Independent AI editorial review: All36 Life-authored Earth compact statements/conditions/displayed equations and all81 origin semantic links read; all36 author exact-source matrix rows and exclusions assessed. All18 inherited Earth compact records read for combined inventory. Targeted independent actual primary sections listed below; not every source body or proof independently reread. AI editorial reference review, not human certification/field proficiency or whole-field completion. Receipt: earth-life-independent-content-review.1.
Entry details
Permanent link to this entry ↗- Record identity
- uni-earth-weathering-soils
- Revision
- core.1
- Structured reference record
- University core expansion