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生态学杂志 ›› 2026, Vol. 45 ›› Issue (8): 2581-2587.doi: 10.13292/j.1000-4890.202607.009

• 研究论文 • 上一篇    下一篇

西北荒漠区植物碳储量与土壤有机碳储量及其驱动机制

阚子涵1,2,郭浩1,王明明1,陶冶1,尹本丰1,周晓兵1*,张元明1   

  1. 1中国科学院新疆生态与地理研究所, 新疆干旱区生物多样性保育与应用重点实验室, 乌鲁木齐 830011; 2中国科学院大学, 北京 100049)

  • 出版日期:2026-08-10 发布日期:2026-08-13

Carbon storage of plants and soil organic carbon in the Northwest China desert region and the driving mechanisms.

KAN Zihan1,2, GUO Hao1, WANG Mingming1, TAO Ye1,YIN Benfeng1, ZHOU Xiaobing1*, ZHANG Yuanming1   

  1. (1Key Laboratory of Biodiversity Conservation and Application in Arid Regions of Xinjiang, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China; 2University of Chinese Academy of Sciences, Beijing 100049, China).

  • Online:2026-08-10 Published:2026-08-13

摘要: 荒漠区在全球碳循环中具有重要地位,其植物碳储量(PCS)和土壤有机碳储量(SOCS)对区域生态稳定性和气候调节至关重要。本研究基于中国西北荒漠区56个样点的数据,采用结构方程模型(SEM),量化了气候因子、植物功能性状和土壤性质对PCS和SOCS的影响。结果表明:研究区PCS均值为13.59 g·m-2,变异系数为0.54;SOCS均值为642.38 g·m-2,变异系数为0.27。二者的主要空间变异均来源于样点层级;PCS的主要影响因子为年均降水量、群落加权平均氮含量、群落加权平均高度和土壤含水量,其中植物性状对植被碳储量具有显著正向作用;SOCS主要受到年均气温和土壤总氮影响,气温不仅对SOCS有显著负向效应,还通过影响植物群落氮含量和土壤氮含量产生间接作用;氮循环在荒漠区碳储量的形成和稳定中起到关键作用,土壤总氮在SOCS中起到显著正向作用,植物群落氮含量在PCS也起显著正向作用;研究进一步揭示了荒漠区碳储量的空间异质性,碳储量的主要变异来源为样点差异,显示出强烈的空间变异。研究为理解荒漠区碳循环提供了重要的理论依据,并为增强荒漠区土壤氮素维持与水分利用效率,应对其碳库脆弱性提供了关键策略。


关键词: 西北荒漠区, 碳储量, 驱动要素, 土壤有机碳

Abstract: Deserts play a crucial role in the global carbon cycle, with plant carbon storage (PCS) and soil organic carbon storage (SOCS) being vital for regional ecological stability and climate regulation. We used structural equation modeling (SEM) to assess the effects of climatic factors, plant functional traits, and soil properties on PCS and SOCS across 56 sites in deserts of northwest China. Results showed that the mean PCS was 13.59 g·m-2 (CV=0.54) and the mean SOCS reached 642.38 g·m-2 (CV=0.27), with both exhibiting primary spatial variation at the site level. PCS was primarily influenced by mean annual precipitation, community weighted mean nitrogen content, community weighted mean plant height, and soil water content. Plant traits exerted a significant positive effect on vegetation carbon storage. SOCS was primarily influenced by mean annual temperature and soil total nitrogen. Temperature exerted a significant negative effect on SOCS directly and indirectly through its impact on plant community nitrogen content and soil nitrogen content. Nitrogen cycling played a crucial role in the formation and stabilization of carbon stocks in desert regions. Soil total nitrogen exerted a significant positive effect on SOCS, while plant community nitrogen content also significantly positively influenced PCS. Our results further revealed the spatial heterogeneity of carbon stocks in deserts, with the differences of sampling sites being the primary source of variation, indicating strong spatial variability. This study provides an important theoretical basis for understanding carbon cycling in deserts and offers key strategies for enhancing soil nitrogen retention and water use efficiency in these regions, as well as for addressing the vulnerability of carbon pools.

Key words: northwest China desert region, carbon stock, driving factor, soil organic carbon