Fire Effects on Soils and Water Flashcards
3 factors of fire effects on soil
- Direct heating of soil from fire (radiative heat)
- Removal/consumption of vegetation, litter, and duff
- Development of hydrophobic soils
Direct heating depends on:
- amount released during burning (higher intensity = more heating)
- duration heat system stays in one place (residence time); slow-moving/smoldering = more heating
- moisture content of soil (wetter soil = more heating)
Fire impact on soil chemistry
Higher intensity = increased damage to soil microbes
Legacy carbon
Fires are releasing legacy carbon into atmosphere from soil carbon sink
- higher fire frequency = more legacy carbon released
- fires have predominantly negative effect on soil carbon and nitrogen pools (more significant in high-severity fires, i.e. wildfire vs. prescribed/slash & burn)
- micronutrients increase, release of nutrients (potassium and calcium in needleleaf forests)
Change in soil color
More color change = higher severity fire
Rainsplash erosion
High-severity fires remove forest canopy and litter layer (expose mineral soil to rainfall)
- decreased interception, infiltration, and transpiration
- increased overland flow
- denser vegetation lowers risk of rainsplash erosion
Hydrophobocity
Water-repellent layer of soil that prevents infiltration, derived from plant material burned during fire
Effects on water
- increased water temp (direct heating, reduced shading as vegetation cover decreases)
- decreased water quality (erosion sediment enters streams, concentration of nutrients)