湖北农业科学 ›› 2025, Vol. 64 ›› Issue (6): 45-52.doi: 10.14088/j.cnki.issn0439-8114.2025.06.009

• 资源·环境 • 上一篇    下一篇

基于土柱模拟的红壤坡耕地耕作土体构型对土壤水运移特征的影响

莫明浩, 刘昭, 石芬芬, 严志伟, 王嘉   

  1. 江西省水利科学院/流域水土保持江西省重点实验室,南昌 330029
  • 收稿日期:2024-11-29 出版日期:2025-06-25 发布日期:2025-07-18
  • 通讯作者: 刘 昭(1989-),男,高级工程师,博士,主要从事水土保持及土壤水分研究,(电子信箱)zhaoliu1989@foxmail.com。
  • 作者简介:莫明浩(1981-),男,江西抚州人,教授级高级工程师,博士,主要从事水土保持与生态环境研究,(电子信箱)mominghao@126.com
  • 基金资助:
    国家自然科学基金项目(42067020); 江西省主要学科学术和技术带头人培养计划青年人才项目(20225BCJ23005); 江西省水利厅科技项目(202325ZDKT02; 202324YBKT08)

The influence of soil configuration on soil water migration characteristics in red soil slope farmland based on soil column simulation

MO Ming-hao, LIU Zhao, SHI fen-fen, YAN Zhi-wei, WANG Jia   

  1. Jiangxi Academy of Water Science and Engineering/Jiangxi Key Laboratory of Watershed Soil and Water Conservation, Nanchang 330029, China
  • Received:2024-11-29 Published:2025-06-25 Online:2025-07-18

摘要: 为探讨红壤坡耕地耕作土体构型对土壤水运移特征的影响,采用一维垂直薄层积水入渗试验研究了不同土体构型和秸秆覆盖措施下土壤水分的入渗特征。结果表明,对于二元非均质土壤,随耕作层土壤容重增大,湿润锋的推进速度和水分入渗率会减慢,导致入渗能力下降;模拟免耕措施的土柱湿润锋运移耗时最长,较耕作层25、35 cm土柱分别延长了64、127 min,且单位时间内其水分累积入渗量与入渗率均最小;秸秆覆盖后土壤水分入渗率下降,降幅在5%~23%,从而增加土壤水分的滞留时间,并进一步提高水分累积入渗量;将非均质土柱概化为均质土体模型发现,当下土层容重一定、上土层容重增大时,其概化均质土体的等效饱和导水率呈减小趋势;上土层厚度增加,等效饱和导水率也相应增大。

关键词: 红壤坡耕地, 土体构型, 土壤水, 运移特征, 耕作, 土柱模拟

Abstract: In order to investigate the influence of soil configuration on soil water migration characteristics in red soil slope farmland, the one-dimensional vertical water infiltration test was used to study soil water infiltration characteristics under different soil configurations and straw mulching measures. The results showed that for binary heterogeneous soil, with the increase of soil bulk density in the cultivated soil layer, the advance velocity of the wetting front and water infiltration rate slowed down, resulting in a decrease in filtration capacity. The wetting front movement's time of the simulated no-tillage measure was the longest, which was 64 min and 127 min longer than that of the 25 cm and 35 cm soil column respectively, and the cumulative infiltration amount and infiltration rate of water per unit time were the lowest. The soil water infiltration rate decreased by 5% to 23% after straw mulching, which increased the retention time of soil water and further increased the cumulative water infiltration amount. When a heterogeneous soil column was generalized into a homogeneous soil model, it showed that if the soil bulk density of the underlying soil layer was constant while the bulk density of the upper soil layer increased, the equivalent saturated water conductivity of the generalized homogeneous soil layer decreased. Additionally, as the thickness of the upper soil layer increased, the equivalent saturated water conductivity also increased.

Key words: red soil slope farmland, soil configuration, soil water, migration characteristics, cultivation, soil column simulation

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