Abstract
Saturated hydraulic conductivity (K(s)) is one of the most important soil properties that determines water flow behavior in terrestrial ecosystems. However, the K(s) of forest soils is difficult to predict due to multiple interactions, such as anthropological and geomorphic processes. In this study, we examined the impacts of vegetation type on K(s) and associated mechanisms. We found that K(s) differed with vegetation type and soil depth, and the impact of vegetation type on K(s) was dependent on soil depth. K(s) did not differ among vegetation types at soil depths of 0-10 and 20-30 cm, but was significantly lower in managed forest types (mixed evergreen broad-leaved and coniferous forests, bamboo forests, and tea gardens) than native evergreen broadleaf forests at a depth of 10-20 cm. Boosted regression tree analysis indicated that total porosity, non-capillary porosity, and macro water-stable aggregates were the primary factors that influenced K(s). Our results suggested that vegetation type was a key factor that influences hydraulic properties in subtropical forest soils through the alteration of soil properties, such as porosity and macro water-stable aggregates.