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    黄河三角洲盐碱地造林对土壤水分特性的影响

    Effect of afforestation on soil moisture characteristics of saline-alkali soil in the Yellow River Delta

    • 摘要: 为明确造林对盐碱地土壤水分特性的影响,采用室内测试与离心机法,对黄河三角洲盐碱地造林后的土壤水分特征曲线、土壤物理性质及其相关性进行分析。结果表明:1)造林改善了土壤结构,降低了盐分含量,不同造林地土壤密度、非毛管孔隙度、凋萎含水量、含盐量均低于对照荒地,而总孔隙度、毛管孔隙度均高于荒地,造林地土壤水分特征曲线除受土壤质地、土壤密度、土壤孔隙度影响外,还受到土壤含盐量的影响;2)土壤含水量与土壤吸力之间存在显著相关关系,经验方程θ= AS -B对该地区的土壤水分特征曲线有良好的模拟性,参数A 随着造林地的不同而呈现规律性的变化,土壤持水力表现为杨树林> 白蜡林> 冬枣林> 荒地,且各地块不同层次间随土层深度自上而下呈递减趋势;3)土壤密度与总孔隙度、非毛管孔隙度呈极显著负相关,毛管孔隙度与凋萎含水量呈极显著负相关,30 与300 kPa 水吸力下的含水量呈极显著正相关,二者均与凋萎含水量呈极显著负相关。研究结果可为滨海盐碱地造林和林地的经营管理提供参考。

       

      Abstract: order to elucidate the effect of afforestation on soil moisture characteristics of saline-alkali soil in the Yellow River Delta, a combination of field sampling, laboratory measurements and centrifugation method was used to measure the soil moisture characteristics, soil physical properties and their correlation. The results indicated that: 1) The afforestation measures were beneficial for changing the soil structure and reducing the salt content; soil bulk density, capillary porosity, wilting moisture content and salt content on different afforestation lands were lower than contrast wasteland, but the total porosity and capillary porosity were higher than wasteland. In addition to the soil texture, bulk density and porosity are the main factors influencing the curve of soil moisture characteristics, and the salt content is also an important influencing factor. 2) There was a significant correlation between the soil moisture and the potential of soil moisture. The mathematical model θ= AS -B could well simulate the water characteristic curve. The value A and water retending capacities in different afforestation lands ranged from high to low as follows: Populus, Fraxinus chinensis, Zizyphus jujube, wasteland. The water retending capacity in different layers on four afforestation lands ranged from high to low with soil depth representing a downward trend. 3) The correlation analysis indicated that there was a negative significant correlation between the soil bulk density, total porosity and non-capillary porosity, between the capillary porosity and wilting moisture content, but a significantly positive correlation was observed between the water content at the water suction of 30 and 300 kPa, and both were negatively correlated with wilting moisture content. The results provide reference for the forest management and improvement of saline-alkali land in the Yellow River Delta.

       

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