脱硫石膏对盐碱土一维水平吸渗特征及水分运动参数的影响

高小龙; 王幼奇; 白一茹; 阮晓晗

doi:10.13870/j.cnki.stbcxb.2022.03.015

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脱硫石膏对盐碱土一维水平吸渗特征及水分运动参数的影响

更新时间：2026-04-09

- 脱硫石膏对盐碱土一维水平吸渗特征及水分运动参数的影响
- Effects of Desulfurized Gypsum on One-dimensional Horizontal Imbibition Characteristics and Water Movement Parameters of Saline-alkali Soil
- 水土保持学报 2022年36卷第3期页码：100-106
- 作者机构：
  
  1. 宁夏大学地理科学与规划学院,银川,750021
  2. 宁夏大学生态环境学院,银川,750021
  3. 西北土地退化与生态恢复国家重点实验室培育基地,银川,750021
  4. 西北退化生态系统恢复与重建教育部重点实验室,银川,750021
- 作者简介：
  
  [ "高小龙(1996-),男,在读硕士研究生,主要从事土壤改良和土壤水分运动研究。E-mail:gxl0612sj@163.com" ]
- 基金信息：
  
  国家自然科学基金项目(41761049,41867003);宁夏自然科学基金项目(2020AAC03049);国家重点研发计划重点项目(2018YFC1802906)
- DOI：10.13870/j.cnki.stbcxb.2022.03.015
  中图分类号： S152.7
- 网络首发：2022-05-27，
  
  纸质出版：2022
- 稿件说明：
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高小龙, 王幼奇, 白一茹, 等. 脱硫石膏对盐碱土一维水平吸渗特征及水分运动参数的影响[J]. 水土保持学报, 2022,36(3):100-106.

GAO Xiaolong, WANG Youqi, BAI Yiru, et al. Effects of Desulfurized Gypsum on One-dimensional Horizontal Imbibition Characteristics and Water Movement Parameters of Saline-alkali Soil[J]. 2022, 36(3): 100-106.
高小龙, 王幼奇, 白一茹, 等. 脱硫石膏对盐碱土一维水平吸渗特征及水分运动参数的影响[J]. 水土保持学报, 2022,36(3):100-106. DOI： 10.13870/j.cnki.stbcxb.2022.03.015.

GAO Xiaolong, WANG Youqi, BAI Yiru, et al. Effects of Desulfurized Gypsum on One-dimensional Horizontal Imbibition Characteristics and Water Movement Parameters of Saline-alkali Soil[J]. 2022, 36(3): 100-106. DOI： 10.13870/j.cnki.stbcxb.2022.03.015.

摘要

为探明添加脱硫石膏对盐碱土水分运动参数的影响

以改善和提高银川北部地区土壤结构和土地生产力

进行了室内一维水平土柱吸渗试验。选取6种脱硫石膏添加比例0

1.5%

4.5%

6%和7.5%

探究不同脱硫石膏添加比例下盐碱土水平吸渗特征及水分运动参数的变化。结果表明:脱硫石膏添加减缓了土壤水分入渗过程

随着脱硫石膏添加比例增加

各处理累积入渗量与湿润锋运移距离均逐渐减小。幂函数与Philip模型能较好地拟合不同脱硫石膏添加比例下盐碱土水分吸渗特征

吸渗率随脱硫石膏配比增加逐渐减小

毛管力对水的吸持作用减弱。随着脱硫石膏配比增加

土壤饱和含水率依次增加

饱和导水率依次减小

土壤持水能力明显提高。在Brooks—Corey模型中

形状系数n逐渐增加

进气吸力hd逐渐减小

土壤通气性增强。在相同含水率情况下

随着脱硫石膏配比增加

土壤水分扩散率减小。添加脱硫石膏增加了土壤持水性能

改变了土壤水分分布状况

对土壤水分运动参数有显著影响。研究结果可为合理利用脱硫石膏改良盐碱地提供参考依据。

Abstract

In order to explore the effect of adding desulfurized gypsum on the water movement parameters of saline-alkali soil

and improve and increase the soil productivity in the Yinbei Plain area

through an indoor one-dimensional soil column absorption test

6 desulfurized gypsum treatments were selected:0

1.5%

4.5%

6% and 7.5%

to study the horizontal infiltration characteristics and water movement parameters of saline-alkali soil. The results showed that the addition of desulfurized gypsum slowed down the process of soil moisture infiltration. As the proportion of desulfurized gypsum increased

the cumulative infiltration amount and the movement distance of the wet front of each treatment gradually decreased. Power function and Philip model could better fit the water movement characteristics of saline-alkali soil under different desulfurized gypsum addition ratios

and the absorption rate decreased with the increase of the desulfurization gypsum ratios

and the capillary force's water holding effect weakened. As the proportion of desulfurized gypsum increased

the saturated water content of the soil increased and the saturated hydraulic conductivity decreased

the soil water holding capacity was significantly improved. The shape coefficient hd in the Brooks-Corey model gradually decreased

and the intake suction hd gradually increased

and soil aeration was enhanced. Under the same moisture content

the soil unsaturated water diffusivity gradually decreased with the increase of the desulfurization gypsum ratios. The addition of desulfurized gypsum increased the soil water holding capacity

changed the soil moisture distribution

and had a significant impact on soil water movement parameters. This study could provide theoretical support for the rational use of desulfurized gypsum to improve saline-alkali land.

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Keywords

references

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