The Long-Term Effects of Wildfire and Post-Fire Vegetation on Sierra Nevada Forest Soils

Forests

Dale W. Johnson¹  Roger F. Walker²  Michelle McNulty²  Benjamin M. Rau² 

[1] Natural Resources and Environmental Science, University of Nevada, Reno, NV 89557, USA;

关键词: carbon;    long-term;    N-fixation;    nutrients;    soils;    vegetation;    wildfire;   

DOI  :  10.3390/f3020398

来源: mdpi

【 摘 要 】

This paper compares carbon (C) and nutrient contents in soils (Alfisols derived from andesite), forest floor and vegetation in a former fire (1960) and an adjacent forest in the Sagehen Watershed in the Sierra Nevada Mountains of California. Soils from the former fire (now occupied predominantly by Ceanothus velutinus, a nitrogen-fixing shrub) had significantly lower contents of extractable SO₄²⁻ and P (both Bray and bicarbonate) but significantly greater contents of exchangeable Ca²⁺ than the adjacent forested site (dominated by Pinus jeffreyii). ¹⁵N data suggested that N fixation had occurred in the former fire site, but N contents did not differ between the two sites. O horizon C and nutrient contents did not differ between the two sites, but vegetation C and nutrient contents were significantly greater in the forested than former fire site. These results contrast with those from a nearby, previous study at Little Valley Nevada, also dominated by P. jeffreyii growing on a different soil type (Entisols derived from granite). In the Little Valley study, soil C, N, Ca²⁺, Mg²⁺, and K⁺ contents within the former fire (1981, now also occupied predominantly by Ceanothus velutinus) were greater than in the adjacent forest (Pinus jeffreyii) but soil extractable P contents either did not differ or were greater in the former fire. We conclude that soil parent material is an indirect but strong mediator of the effects of post-fire vegetation on soils in this region, especially with respect to soil P changes, which vary substantially between andesite- and granite-derived soils.

【 授权许可】

CC BY   
© 2012 by the authors; licensee MDPI, Basel, Switzerland.