呼伦贝尔草原风蚀坑土壤质地与持水能力特征
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张额真(1999-),男,硕士研究生,主要从事荒漠化防治研究。E-mail:nmgzhangezhen@163.com

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S812.1

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内蒙古重点研发和成果转化计划项目(2022YFDZ0055)


Characteristics of Soil Texture and Water-Holding Capacity of Blowout Pits in the Hulunbuir Grassland
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    摘要:

    [目的]为揭示呼伦贝尔草原风蚀坑4个典型部位的土壤质地差异和持水能力变化特征。[方法]将风蚀坑分为边缘区(A区)、沙坑区(B区)、重度积沙区(C区)、轻度覆沙区(D区)4个部位,以天然草地为对照(CK区),对各样地0~200 cm土层土壤粒径、土壤体积质量、田间持水量等指标进行相关性分析和PCA分析。[结果] 1)呼伦贝尔草原风蚀坑0~200 cm土层土壤以中砂为主,不含砾石,平均粒径大小为B区(1.41Φ)>A区(1.48Φ)>C区(1.52Φ)>D区(1.98Φ)>CK区(2.45Φ)。2)风蚀坑4个部位土壤粒度参数存在显著性差异,分选系数总体分选性较差,峰态数值表现为尖窄,偏度都呈极正偏,分形维数总体为2.1~2.2。3)平均粒径沿主害风(西北风)逐渐变细,C区和D区的分选作用较强,而A、B的分选作用较弱。4)风蚀坑土壤体积质量为1.55~1.70 g/cm3,土壤水分体积分数为CK区(4.51%)>A区(4.4%)>D区(4.35%)>B区(4.23%)>C区(4.2%),田间持水量为CK区(17.97%)>D区(16.95%)>A区(15.53%)>B区(15.26%)>C区(14.51%)。5)风蚀坑不同部位的土壤水分体积分数与土壤机械组成中的黏粒、粉粒、细砂、极细砂呈正相关,与土壤机械组成中的中砂、粗砂、极粗砂呈负相关。[结论]风蚀坑总体平均粒度呈沿主风向变细,C区持水能力最弱,D区持水能力最强,为风蚀坑的分部位治理提供理论依据。

    Abstract:

    [Objective] This study aimed to reveal the soil texture difference and water-holding capacity change characteristics of four typical parts of blowout pits in the Hulunbuir grassland.[Methods] The blowout pits were divided into four parts: the edge area(A area), the sand pit area(B area), the severe sand accumulation area(C area), and the mild sand coverage area(D area). The natural grassland was used as the control(CK area). Correlation analysis and PCA analysis of soil properties including soil particle size, bulk density, water-holding capacity, etc. in the 0-200 cm soil layer of each pit were carried out.[Results] 1) The soil in the 0-200 cm soil layer of blowout pits in the Hulunbuir grassland was mainly medium sand, there was no gravel, and the average particle size was B area(1.41Φ)>A area(1.48Φ)>C area(1.52Φ)>D area(1.98Φ)>CK area(2.45Φ). 2) There were significant differences in soil particle size parameters of the four parts of the blowout pits. The sorting coefficient was generally poor, the peak value was sharp and narrow, the skewness was extremely positive, and the fractal dimension was generally distributed around 2.1-2.2. 3) The average particle size gradually decreased along the main wind(northwest wind). The sorting effects of C and D were stronger, while the sorting effects of A and B were weaker. 4) Soil bulk density of wind erosion pits was between 1.55-1.70 g/cm3, soil water content was CK area(4.51%)>A area(4.4%)>D area(4.35%)>B area>(4.23%)>C area(4.2%), and field water-holding capacity was CK area(17.97%)>D area(16.95%)>A area(15.53%)>B area(15.26%)>C area(14.51%). 5) Soil water content in different parts of blowout pits was positively correlated with clay, silt, fine sand, and very fine sand fractions, and negatively correlated with medium sand, coarse sand, and very coarse sand fractions.[Conclusion] The overall average particle size of blowout pits becomes finer along the main wind direction. Water-holding capacity is the weakest in the C area, and strongest in the D area. The findings provide a theoretical basis for the management of blowout pits.

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张额真, 袁立敏, 蒙仲举, 赵阳, 包志鑫.呼伦贝尔草原风蚀坑土壤质地与持水能力特征[J].水土保持学报,2025,39(4):225~234

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  • 收稿日期:2025-02-21
  • 最后修改日期:2025-04-14
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  • 在线发布日期: 2025-09-10
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