Impacts of Eucalyptus plantation on soil and water losses in a typical small watershed in mountainous area of southern China.

Unreasonable exploitation oi artificial forest causes severe soil erosion in the mountainous areas of sou¬thern China. The spatial-temporal variations of soil erosion in typical small watershed with artificial forest has signifi¬cant implications for artificial forest exploitation and sustainable development of mountainous ecological environ¬ment. In this study, we used revised universal soil loss equation ( RUSLE) and geographic information system ( GIS) to evaluate the spatial and temporal variations of soil erosion and its key drivers of Dadingshan watershed in mountainous area of western Guangdong. The results showed that the erosion modulus was 1948.1 t ⋅ km^-2 ⋅ a^-1 (belonging to light erosion) in the Dadingshan watershed. However, the spatial variation of soil erosion was sub¬stantial, with variation coefficient of 5.12. The maximal soil erosion modulus was 191127 t ⋅ km^-2 ⋅a^-1. Slight ero¬sion (<500 t ⋅ km^-2 ⋅ a^-1 ) accounted for 80.6% of the total watershed area. The moderate erosion and above ( >2500 t ⋅ km^-2 a^-1) were mainly distributed in young Eucalyptus forest area with less than 30% of the vegeta¬tion coverage, which contributed nearly 75.7% of total soil erosion. During 2014-2019, the interannual variations of mean erosion of Dadingshan catchment was modest, but the spatial variation of soil erosion was large. Vegetation cover, slope, and rainfall were key drivers of such variation. The destruction of natural vegetation resulted by plan¬tation exploitation was the primary cause of soil erosion in afforestation areas. Soil erosion significantly increased with the increases of slope gradient in the young forest area, which was aggravated by extreme rainfall. However, soil erosion gradually decreased with the increases of the age of Eucalypt plantation. Therefore, the hot spot of soil erosion was young forest areas of Eucalypt plantation with slope >25°, and the key period for soil erosion control was the first 2-3 years after Eucalyptus planting. We suggested that reasonable afforestation measures should be used in area with >25° slopes, and that the destruction of natural vegetation should be avoided on hillslope with >35° slope gradient. The road construction standards and forest management should be further improved to address the challenge of extreme rainfalls. [ABSTRACT FROM AUTHOR]