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生态学杂志 ›› 2024, Vol. 43 ›› Issue (6): 1824-1832.doi: 10.13292/j.10004890.202406.040

• 恢复生态 • 上一篇    下一篇

西藏一江两河地区耕地土壤有机碳空间分异及其影响因素

谭格非1,2,王兆锋1,2*,张镱锂1,2,3,宫殿清1,2,胡晓阳1,2   

  1. (1中国科学院地理科学与资源研究所/陆地表层格局与模拟重点实验室, 北京 100101; 2中国科学院大学, 北京 100049; 3中国科学院青藏高原地球科学卓越创新中心, 北京 100101)

  • 出版日期:2024-06-10 发布日期:2024-06-19

Spatial differentiation of cropland soil organic carbon and influencing factors in the Yarlung Zangbo River, Nyangqu River and Lhasa River region of Tibet.

TAN Gefei1,2, WANG Zhaofeng1,2*, ZHANG Yili1,2,3, GONG Dianqing1,2, HU Xiaoyang1,2   

  1. (1Key Laboratory of Land Surface Pattern and Simulation, Institution of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; 2University of Chinese Academy of Sciences, Beijing 100049, China; 3CAS Center for Excellence in Tibetan Earth Sciences, Beijing 100101, China).

  • Online:2024-06-10 Published:2024-06-19

摘要: 耕地土壤有机碳(SOC)在稳定生态环境和粮食安全等方面发挥重要作用,探明其空间分异规律及其影响因素对于生态文明建设和区域农业发展具有重要意义。本研究以西藏“一江两河”地区耕地土壤为对象,基于150个采样点,采用冗余分析和结构方程模型,研究了区域耕地SOC的空间分异特征及其影响因素。结果表明:“一江两河”地区耕地SOC表现为西部地区低、东部高,雅江干流河谷低、南北支流源头高,研究区SOC整体较匮乏;土壤粉粒是区域SOC空间分异的主导因子,解释了SOC变异的14.0%;年均蒸发量比年均气温和年均降水更能解释区域SOC的空间分异;区域SOC含量主要表现出垂直地带性和经向地带性,海拔主要通过影响气温和蒸发量,经度主要通过影响降水和土壤pH间接影响区域耕地SOC含量;空间位置通过影响气候、植被和土壤特性间接影响SOC含量。本研究为SOC空间预测和区域农业发展提供了科学依据。


关键词: 土壤有机碳, 空间分异, 青藏高原, 冗余分析, 结构方程模型

Abstract: Soil organic carbon (SOC) in croplands plays an important role in stabilizing the ecological environment and food security. Exploring the spatial variations and influencing factors of SOC is of great significance for promoting the sustainability of regional agriculture. We analyzed the spatial differentiation characteristics and influencing factors of cropland SOC using redundancy analysis (RDA) and structural equation model (SEM), with 150 sampling points from cropland topsoil across the Yarlung Zangbo River, the Nyangqu River, and the Lhasa River region (the YNL river region) in Tibet. The results showed that cropland SOC in the YNL river region was low in the west and high in the east, and low in the mainstream valley of the Yarlung Zangbo River and high in the source areas of the north and south tributaries. Overall, the average SOC content in the YNL river region was relatively low. Soil silt content was the dominant factor in the regional spatial variations of SOC, explaining 14.0% of total variation. Mean annual evaporation (MAE) could better explain the spatial variations of SOC than mean annual temperature (MAT) and mean annual precipitation (MAP). The SOC content in this region mainly showed vertical and meridional zonality. Altitude affected SOC levels indirectly by affecting temperature and evaporation, while longitude affected it indirectly by affecting precipitation and soil pH. The spatial variations of SOC content were indirectly affected by climate, vegetation, and soil properties. This study provides a scientific basis for the prediction of spatial variations of SOC and regional agricultural development.


Key words: soil organic carbon, spatial differentiation, Qinghai-Tibet Plateau, redundancy analysis (RDA), structural equation modeling (SEM)