长江三峡山地集水区土壤水分空间变异特征
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胡乐心(2000-),女,硕士研究生,主要从事土壤水文研究。E-mail:hlx251964@163.com

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S152.7

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国家自然科学基金项目(41771261,41601215);湖北省自然科学基金重点项目(2015CFA141)


Spatial Variation Characteristics of Soil Moisture in the Three Gorges Mountain Catchment Area of the Yangtze River
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    摘要:

    为阐明亚热带湿润气候区山地坡面土壤水分的时空变化及影响因素,以三峡库区针叶林覆盖的中山凹坡为研究对象,采用经典统计学和地统计学的方法,对2019-2020年5 m×5 m网格点监测的117个点位0-70 cm土层深度的土壤水分数据进行分析,研究了湿润和干旱条件下典型凹坡集水区内土壤含水量的统计学特征与环境因子的相关性,以及土壤含水量的空间变异特征。结果表明:(1)水平方向上,集水区内各层土壤水分均表现为中等变异(10%

    Abstract:

    In order to clarify the spatial and temporal variation and the influencing factors of soil moisture on mountain slopes in the humid subtropical climate zone, taking the mid-mountain concave slopes covered by coniferous forest in the Three Gorges reservoir area as the research object. The soil moisture data of 117 monitoring points at a depth of 0-70 cm in a 5-meter grid during 2019 to 2020 were analyzed by using classical statistics and geostatistics methods. And this study investigated the correlation between the statistical characteristics of soil moisture content and environmental factors and the spatial variability characteristics of soil moisture content in the catchment area of typical concave slopes under wet and dry conditions. The results showed that:(1) Soil moisture of all layers in the catchment area showed moderate variability (10%

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胡乐心, 刘目兴, 赵露, 易军, 张海林, 万金红.长江三峡山地集水区土壤水分空间变异特征[J].水土保持学报,2023,37(5):86~93

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  • 收稿日期:2023-03-13
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  • 在线发布日期: 2023-10-10
  • 出版日期: 2023-10-28