“…The southwestern China karst area centred on Guizhou Province is the world's largest continuous karst area (Li et al, 2017b;Peng et al, 2017) .and the special ecological geological characteristics make this area a typical fragile ecological environment (Wang et al,2004b). With the intensi cation of stone deserti cation, soil erosion in karst areas is becoming increasingly serious ((Febles-González et al, 2014), and the ability to support plant growth is severely weakened, leading to vegetation degradation, which in turn leads to the destruction of the basic structure of karst soils, soil infertile, water-holding capacity reduced, and plants subjected to frequent deteriorating environmental stress, leading to the inability of vegetation to grow normally or eventually to die, increasing the risk of karst stone deserti cation and further leading to the collapse of karst ecosystems, all of which directly or indirectly cause serious challenges to the productivity and sustainability of karst soil resources (Smith et al, 2013) .And the special surface-subsurface dichotomy of the Tongkat region leads to soil erosion in two directions. During the runoff-driven downward loss of soil through the ssure system, part of the soil is temporarily stored in the shallow karst ssures, forming the ssure soil system.…”