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We conclude that a series of reinforcing fire, soil and vegetation feedbacks maintain the mosaic of shrubland patches.
The Rim Fire soil burn severity map was developed for the entire burned area and shared with those entities engaged in assessment efforts outside the national forest boundaries.
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The CaCO3 content in the heated soil was significantly higher than in the unburned and direct fire soils.
This is especially common in annual plants that emerge rapidly from the post-fire soil seed bank.
Post peat-fire soil TP concentrations (853 mg/kg) were much higher than surface-burned areas (580 mg/kg).
Soil erosion prediction models are crucial for estimating fire impacts and for planning post-fire soil stabilization measures.
In addition, the fire would produce very similar soil erodibility values for the different land uses, and therefore a homogenizing post-fire soil response in the landscape.
To concluded, topography regulated the effects of fire on soil carbon fluxes and might control the post-fire soil carbon flux feedbacks to climate warming.
The post-fire soil faunal communities are formed both by animals having survived the fire and by colonizers from the surrounding landscape.
These post-peat-fire soil TP concentrations are also much higher than the 650 mg/kg threshold TP level that would promote and accelerate cattail expansion (Wu et al.1997).1997
Field measurements indicated that the loss of surface organic layers in boreal ecosystem fires is a major factor determining post-fire soil temperature changes, depth of thawing, and carbon losses from the mineral topsoil layer.
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