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Acta Prataculturae Sinica ›› 2026, Vol. 35 ›› Issue (10): 1-14.DOI: 10.11686/cyxb2025433

   

Spatial variation of mineral-associated organic carbon in grassland on the northern slopes of the Tianshan Mountains

Jing SI1,2(), Yao WANG1,2, Zhong-lin XU1,3,4,5()   

  1. 1.College of Ecology and Environment,Xinjiang University,Urumqi 830017,China
    2.Institute of Desert Meteorology,China Meteorological Administration,Urumqi 830002,China
    3.Xinjiang Jinghe Observation and Research Station of Temperate Desert Ecosystem,Ministry of Education,Jinghe 833300,China
    4.Technology Innovation Center for Ecological Monitoring and Restoration of Desert-Oasis,Ministry of Natural Resource,Urumqi 830002,China
    5.Key Laboratory of Oasis Ecology,Ministry of Education,Xinjiang University,Urumqi 830017,China
  • Received:2025-10-20 Revised:2025-12-09 Online:2026-10-20 Published:2026-09-09
  • Contact: Zhong-lin XU

Abstract:

Mineral-associated organic carbon (MAOC) is a relatively stable and important fraction of soil organic carbon, and variations in its content directly affect the composition and long-term stability of soil carbon pools. In arid grassland ecosystems in particular, MAOC plays a key role in long-term carbon sequestration and the functioning of carbon sinks. However, studies on the spatial pattern of MAOC in grasslands of the arid and semi-arid regions of central Asia and the main factors controling it remain limited. In this study, we focused on grassland on the northern slope of the Tianshan Mountains in Xinjiang, and examined the spatial distribution characteristics and driving mechanisms of MAOC considering grassland type, soil profile, and topographic-climatic-soil factors. The results show that: 1) The MAOC content decreased with increasing soil depth, with the largest decreases in mountain meadow, followed by typical steppe, and then desert steppe; 2) The MAOC content was significantly negatively correlated with air temperature and soil pH, and significantly positively correlated with elevation, slope, available phosphorus and total nitrogen; 3) The carbon stability index values were higher in deeper soil layers, indicative of higher carbon stability in deeper layers; 4) A spatial prediction model for MAOC based on multiple regression analyses revealed a spatially heterogeneous pattern where the MAOC content increased from northwest to southeast. These results deepen our understanding of the spatial characteristics of MAOC and factors influencing MAOC in arid and semi-arid grassland ecosystems, and provide scientific support for formulating land carbon management policies under the “dual carbon” strategy in Xinjiang and other dryland regions.

Key words: mineral-associated organic carbon (MAOC), spatial distribution, main controlling factors, arid grassland