高级检索

    不同地下水矿化度条件下柽柳土柱的水盐分布特征

    Distribution characteristics of soil moisture and salinity in the soil columns with planting Tamarix chinensis under different groundwater mineralization

    • 摘要: 通过探讨土壤水盐分布特征对地下水矿化度的响应规律,为泥质海岸带盐碱土的合理利用和水土保持防护林的栽植管理提供科学依据。以栽植3 年生柽柳苗木的土壤柱体为研究对象,在1.8 m 的地下水水位下,分别模拟设置淡水(0g/L)、微咸水(3g/L)、咸水(8 g/ L)和盐水(20 g/ L)4 种地下水矿化度,并以不栽植柽柳的土壤柱体为对照,测定分析不同地下水矿化度处理的土壤水分、盐分以及溶液绝对浓度等水盐参数。结果表明:地下水矿化度可显著影响不同剖面的土壤水盐参数。随地下水矿化度的升高,整个土柱的含水量和含盐量均呈现升高趋势,而土壤溶液绝对浓度呈下降趋势。其中:柽柳土柱相对含水量均值在4 种矿化度下,分别比对照下降24.4%、20.6%、11.3%和4.7%;微咸水、咸水和盐水矿化度下,柽柳土柱的含盐量均值,分别比对照下降67%、5.6% 和8.7%。不同地下水矿化度条件下,随土壤深度的增加,土壤水分呈升高趋势,土壤溶液绝对浓度呈下降趋势,土壤盐分则表现为先下降再升高,并在80cm土壤深度下,盐分达最低值。地下水矿化度的升高,有利于盐分随水分向土壤表层迁移。栽植柽柳可显著降低土柱的含水量、含盐量和土壤溶液绝对浓度,但随地下水矿化度的升高,栽植柽柳对土壤水分的降低作用在减弱,而抑制盐分作用在增强。

       

      Abstract: Background Soil salinization is one of the major features of the ecological environment in the Yellow River Delta, and groundwater is the main water resource for plant growth and development in this saline soil. This study aims to provide scientific basis for the rational utilization of saline soil in the muddy coast, and management of planting protection forest for soil and water conservation. Methods In order to investigate the response of the distribution characteristics of soil moisture and salinity under different groundwater salinity, the soil columns with planting 3-year Tamarix chinensis Lour were selected as experimental material, and soil columns without planting as control (CK). The parameters of soil moisture and salinity, such as soil water content, soil salt content and absolute concentration of soil solution, were measured and analyzed under simulating groundwater levels of 1.8 m with 4 groundwater salinity gradients of fresh water (0 g/ L), brackish water (3 g/ L), saline water (8 g/ L) and salt water (20 g/ L), respectively. Results The groundwater salinity significantly affected the parameters of soil moisture and salinity under different soil profiles. With the increase of groundwater salinity, the content of soil moisture and salinity in the whole soil columns increased, while the absolute concentration of soil solution decreased. Compared with CK, the mean relative water contents in soil columns with planting T. chinensis at fresh water, brackish water, saline water and salt water decreased by 24.4%, 20.6%, 11.3% and 4.7%, respectively, and the mean soil salt contents of brackish water, saline water and salt water decreased by 6.7%, 5.6% and 8.7%, respectively. With the increase of soil depth under different groundwater salinity, the soil moisture rose, and the absolute concentration of soil solution decreased, while soil salinity decreased firstly and then increased, and reached the minimum value at the soil depth of 80 cm. Conclusions With the increase of groundwater mineralization, the content of soil moisture and salinity rose rapidly, especially at the top soil, indicating that planting T. chinensis significantly decreased the water content, salt content and absolute concentration of soil solution in soil columns. However, the effect of planting T. chinensis for decreasing soil moisture weakened with groundwater mineralization increasing, while that on salt inhibition enhanced.

       

    /

    返回文章
    返回