Subsoil organic carbon turnover is dominantly controlled by soil properties in grasslands across China

• Published in: Catena (Giessen) 2021-12, Vol.207, p.105654, Article 105654
• Main Authors: Shi, Yuehong, Tang, Xiaolu, Yu, Peng, Xu, Li, Chen, Guo, Cao, Longxi, Song, Ci, Cai, Chunju, Li, Jingji
• Format: Article
• Language: English
• Subjects: Climate; Soil carbon stock; Soil properties; Structural equation model; Subsoil carbon turnover
• ISSN: 0341-8162; 1872-6887
• DOI: 10.1016/j.catena.2021.105654

•Subsoil τ of main grassland types was studied across China.•The mean values of subsoil τ across grassland types was 129.1 ± 34.2 years.•Subsoil τ is mainly controlled by soil properties, rather than climate. Soil organic carbon turnover time (τ, year) is an important indicator of soil carbon stability and a major factor determining soil carbon sequestration capacity. Many previous studies have investigated τ in the topsoil layers, but little is known about subsoil τ and its environmental drivers. We estimated subsoil τ (the ratio of subsoil organic carbon (OC) stock to net primary production) using field observations from the published literatures and employed regression analysis and the structural equation model (SEM) to identify the effects of climate, soil, and vegetation variables on subsoil τ in China’s grasslands. The results showed that the average subsoil τ over 0.2–1 m varied greatly from 5.5 to 702.2 years, with a mean (±standard deviation) of 118.5 ± 97.8 years. Subsoil τ varied significantly among different grassland types, with 164.0 ± 112.0 years for alpine meadow, 107.0 ± 47.9 years for alpine steppe, 177.0 ± 143.0 years for temperate desert steppe, 96.6 ± 88.7 years for temperate meadow steppe, and 101.0 ± 75.9 years for temperate typical steppe. Subsoil τ was significantly negatively correlated (p