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干旱区地理 ›› 2026, Vol. 49 ›› Issue (9): 1777-1787.doi: 10.12118/j.issn.1000-6060.2025.595 cstr: 32274.14.ALG2025595

• 地表过程研究 • 上一篇    下一篇

古尔班通古特沙漠土壤水分含量与地形-植被因子关系研究

张璐(), 张定海(), 杨甜, 丘月   

  1. 甘肃农业大学理学院数量生物研究所甘肃 兰州 730070
  • 收稿日期:2025-09-25 修回日期:2025-10-24 出版日期:2026-09-25 发布日期:2026-09-07
  • 通讯作者: 张定海(1981-),男,博士,教授,主要从事生态水文模型、统计学在经济学、生态学中的应用研究. E-mail: zhangdh@gsau.edu.cn
  • 作者简介:张璐(1998-),女,硕士研究生,主要从事应用统计学研究. E-mail: 13303846180@163.com
  • 基金资助:
    国家自然科学基金地区基金项目(42361016);内蒙古自治区防沙治沙科技创新重大示范工程“揭榜挂帅”项目(2024JBGS0003);甘肃农业大学青年导师扶持基金(GAU-QDFC-2023-07);甘肃农业大学研究生重点课程建设项目(GAU-ZDKC-202205)

Relationship between soil moisture content and topography-vegetation factors in the Gurbantunggut Desert

ZHANG Lu(), ZHANG Dinghai(), YANG Tian, QIU Yue   

  1. Center for Quantitative Biology, College of Science, Gansu Agricultural University, Lanzhou 730070, Gansu, China
  • Received:2025-09-25 Revised:2025-10-24 Published:2026-09-25 Online:2026-09-07

摘要:

土壤水分是水资源形成、转化和消耗过程中不可或缺的组成部分。以古尔班通古特沙漠固定、半固定和流动沙丘上的土壤水分含量(简称土壤水分)为研究对象,采用偏最小二乘结构方程模型(PLS-SEM)、随机森林模型及沙普利加性解释(SHAP)分析方法,研究了不同深度土壤水分与地形-植被因子之间的关系。结果表明:(1) 除了半固定与流动沙丘上的中层土壤水分分布无显著差异外,研究区其他类型沙丘的土壤水分垂直分布均呈现显著差异。(2) 结构方程模型结果显示,固定沙丘上地形因子高差和植被因子灌木多度对土壤水分影响最为突出,半固定沙丘上坡度和灌木盖度为主导因子,而流动沙丘地形-植被因子对土壤水分的影响不显著。(3) 关键因子交互作用结果进一步显示固定沙丘中草本多度>300株·m-2、灌木多度>2株·m-2的组合可缓解水分胁迫;半固定沙丘中草本多度>200株·m-2、灌木盖度>30%时,能减弱坡度对土壤水分的不利影响;流动沙丘需维持草本盖度>20%、生物量>10 g·m-2以提升水分含量。研究结果可为荒漠化治理提供精细化管理策略。

关键词: 古尔班通古特沙漠, 土壤水分, 地形-植被因子, 偏最小二乘结构方程模型, 随机森林模型

Abstract:

Soil moisture forms an essential component in the formation, transformation, and consumption of water resources. This study investigates soil moisture in fixed, semifixed, and mobile dunes of the Gurbantunggut Desert in Xinjiang, China. The relationship between moisture at different soil depths and topography-vegetation factors was analyzed using partial least squares structural equation model (PLS-SEM), random forest model, and Shapley additive explanations (SHAP) value analysis. The results showed that: (1) Except for soil moisture in the middle layer of semifixed and mobile dunes, the vertical distribution of moisture among dune types varied significantly. (2) Structual equation model indicated that the topography factor—height difference and vegetation factor—shrub abundance—had the most pronounced impacts on soil moisture in fixed dunes; slope degree and shrub coverage were dominant factors in semifixed dunes, whereas topography and vegetation factors had relatively minor effects in mobile dunes. (3) The interaction among key factors revealed that in fixed dunes, a combination of herb and shrub abundance >300 plants·m-2 and >2 plants·m-2, respectively alleviated water stress; in semifixed dunes, >200 plants·m-2 and >30%, respectively mitigated the adverse impacts of slope degree on soil moisture; in mobile dunes, maintaining herb coverage at >20% and biomass at >10 g·m-2 was necessary to enhance soil moisture content. These findings can help formulate refined management strategies for desertification control.

Key words: Gurbantunggut Desert, soil moisture, topography-vegetation factors, partial least squares structural equation model, random forest model