Forestation does not necessarily reduce soil erosion in a karst watershed in southwestern China

• Published in: Progress in physical geography Vol. 45; no. 1; pp. 82 - 97
• Main Authors: Feng, Siwen, Wu, Lu, Liang, Boyi, Wang, Hongya, Liu, Hongyan, Zhu, Chenyi, Li, Shuai
• Format: Journal Article
• Language: English
• Published: London, England SAGE Publications 01-02-2021; Sage Publications Ltd
• Subjects: Agricultural land; Correlation coefficient; Correlation coefficients; Dolomite; Drought; Environmental monitoring; Forest growth; Forest watersheds; Forests; Karst; Limestone; Lithology; River basins; Satellite imagery; Sediment yield; Soil erosion; Tillage; China; WaTEM/SEDEM; Soil erosion; forestation; dynamic factor; karst watershed
• ISSN: 0309-1333; 1477-0296
• DOI: 10.1177/0309133320958613

Forestation as part of the Returning Farmland to Forest Project was implemented to mitigate soil erosion in southwestern China. However, whether forestation has effectively reduced soil erosion in southwestern China remains unclear, mostly because of the lack of monitoring forest cover change and soil erosion at watershed scales. We interpreted forest cover change from satellite images and simulated soil erosion changes for the period of 1986–2018 in the Chong’an River Basin with the Water and Tillage Erosion Model and Sediment Delivery Model. Our results show that the change in forest cover has the highest correlation coefficient with the sediment yield in the watershed, with an obvious inverse phase relationship between them for all the simulated years. From 2002 to 2014, large-scale forestation and frequent droughts caused the forest cover to vary, resulting in significant changes in the annual soil erosion amount. Because crevices favoring tree growth are more developed in limestone than in dolomite, the forest cover reduction on dolomite is significantly higher than that on limestone under severe droughts in karst areas. Our study implied that the function of forestation in preventing soil erosion depends on lithology in karst areas.