The soil organic carbon (SOC) pool is the largest carbon (C) pool in terrestrial ecosystems (Grimm et al., 2008). SOC loss due to land-use change is a major contributor to anthropogenic CO 2 emissions (Piao et al., 2009). Urbanization is among the most prominent land-use changes in the 21st century (Hansen et al., 2005;Kuang, 2020), and the expansion of impervious surface area (ISA), which is an artificially hardened surface characterized by buildings, roads, etc., could cause intensive soil disturbances (Montague & Kjelgren, 2004). The global ISA area is approximately 4.5 × 10 5 to 5.8 × 10 5 km 2 (Kuang, 2019;Kuang, Zhang, et al., 2021;Lehmann & Stahr, 2007), and the built-up area is projected to triple in the first half of the 21st century (Seto et al., 2012). China's urbanization rate is twice the world average, and 67% of its urban area is covered by ISAs, which is higher than the global average (Kuang, 2019;Kuang et al., 2020).