雷达探测分析广西丘陵坡耕地整地措施对土壤水分的影响
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倪晓庆(2000-),女,硕士研究生,主要从事土壤水分研究。E-mail:nixiaoqing_1001@163.com

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S152.7

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国家自然科学基金项目(41701248);广西科技计划项目(AD25069074);广西自然科学基金项目(2017GXNSFBA198102);广西研究生教育创新计划项目(YCSW2022307);桂林理工大学博士科研启动基金项目(GUTQDJJ2017001)


Radar Detection Analysis of the Effects of Land Preparation Measures on Soil Moisture in Hilly Sloping Farmland in Guangxi
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    摘要:

    [目的] 整地是丘陵山区农业生产中的关键措施,明确整地后土壤属性的变化与田间土壤水分空间变异特征的响应关系,对于提升农业生产效益具有重要意义。[方法] 以广西丘陵山区水平和反坡2种典型整地措施为研究对象,将野外雷达探测试验与室内土壤分析试验相结合,利用图像解析、统计分析等方法,深入探讨整地措施对坡耕地田间土壤水分变异特征的作用。[结果] 在相同外部供水条件下,水平整地后的土壤水分空间变化显著发生在0~30 cm土层,反坡整地集中在20~40 cm土层,坡耕地贯穿整个0~50 cm土层。水平整地的田间土壤水分空间分布变化程度最强(平均偏离程度0.052),反坡整地变化程度最弱。水平整地的田间土壤水分空间运动稳定(反射系数0.33,瞬时功率变化速率8.41×1011 dB/ns)且相对均匀(雷达结构相似性指数0.77),而反坡整地与坡耕地的田间土壤水分运动程度均相对剧烈,空间运动状态变化较大。坡耕地的土壤水分空间变异最大(综合指数1.45),其次为反坡整地(综合指数1.53),水平整地的土壤水分空间变异最小(综合指数1.57),土壤水分环境相对最稳定。相较坡耕地,整地后的土壤粉粒质量分数对土壤水分空间变异影响最大。[结论] 在相同外部供水环境下,水平和反坡整地后田间土壤属性和土壤水分状况均相对坡耕地起到调控作用,且水平整地下的田间土壤水分蓄存状况相对更好。

    Abstract:

    [Objective] Land preparation is a key measure in agricultural production in hilly and mountainous areas. It is of great significance to clarify the response relationship between the changes of soil properties after land preparation and the spatial variation characteristics of soil moisture in the field for improving the efficiency of agricultural production. [Methods] Two typical land preparation measures,i. e. horizontal and reverse slopes in hilly and mountainous areas of Guangxi,were taken as the research objects. Field radar detection experiment was combined with indoor soil analysis tests, and the effects of land preparation measures on the variation characteristics of soil moisture in sloping farmland were discussed in depth by means of image analysis and statistical analysis. [Results] Under the same external water supply conditions,the spatial variation of soil moisture after horizontal land preparation significantly occurred in the 0―30 cm soil layer,that after reverse slope preparation was concentrated in the 20―40 cm soil layer,while sloping farmland exhibited moisture variation throughout the entire 0―50 cm soil layer. The spatial distribution of soil moisture in the field of horizontal land preparation was the strongest(average deviation degree 0.052),and the change degree of land preparation on the reverse slope was the weakest. The spatial movement of soil moisture in the field of horizontal land preparation was stable(reflection coefficient 0.33,instantaneous power change rate 8.41×1011 dB/ns)and relatively uniform (radar structure similarity index 0.77),while the degree of soil moisture movement in the field of reverse slope land preparation and sloping farmland was more intense,and the spatial movement state changed greatly. The spatial variation of soil moisture in sloping farmland was the largest(comprehensive index 1.45),followed by reverse slope preparation(comprehensive index 1.53),and the spatial variation of soil moisture in horizontal preparation was the smallest(comprehensive index 1.57),and the soil moisture environment was relatively stable. Compared with sloping farmland,the soil silt content after land preparation had the greatest influence on the spatial variation of soil moisture. [Conclusion] Under the same external water supply conditions,the soil moisture condition in the field after horizontal and reverse slope land preparation is better than that in sloping farmland,and the soil moisture storage condition in the field after horizontal land preparation is better.

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倪晓庆, 陈晓冰, 张详曙, 义轩, 刘雍鑫, 杨婷, 许昊.雷达探测分析广西丘陵坡耕地整地措施对土壤水分的影响[J].水土保持学报,2025,39(5):367~377

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  • 收稿日期:2025-01-03
  • 最后修改日期:2025-02-20
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  • 在线发布日期: 2025-10-20
  • 出版日期: 2025-10-28
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