| Abstrakt: |
Studies on the effects of wildfires on soil are common in mixed-conifer forests worldwide; however, such studies are less frequent in the context of high-altitude mixed-conifer forests. In this research, we analyzed the soil physicochemical properties over a span of 14 years following a high-intensity wildfire. Soil samples were collected from a depth of 0-10 cm across 100 composite samples, representing both control (unburned) and burned areas. Our findings revealed significant changes in soil characteristics in the burned area compared to the control area. Specifically, the average soil pH, electrical conductivity, and available potassium increased by 3%, 81%, and 53%, respectively, in the burned area, while available phosphorus decreased by 6%. Conversely, the average total nitrogen and organic matter showed non-significant decreases of 20% and 12% in the burned area compared to the control area. No significant differences were found in slope aspects. Electrical conductivity and available potassium varied significantly among upper (3300-3500 m), middle (3100-3300 m), and lower (2900-3100 m) altitude ranges. Principal component analysis explained a total of 50.1% of the variance, with approximately 27.4% explained by the first axis and 22.7% by the second axis. Consequently, post-fire restoration efforts should consider potential changes in soil nutrient availability to facilitate successful vegetation recovery. This study enhances the formulation of more precise post-fire land management strategies, improves forest restoration initiatives, and promotes sustainable land-use practices by comparing unburned natural forests. Further research is needed to explore the physical, chemical, and biological properties that could influence the dynamics of soil variables in post-fire environments. |
