张妙仙, 杨劲松, 李冬顺. 特大暴雨作用下土壤盐分运移特征研究[J]. 中国生态农业学报(中英文), 2004, 12(2): 47-49.
引用本文: 张妙仙, 杨劲松, 李冬顺. 特大暴雨作用下土壤盐分运移特征研究[J]. 中国生态农业学报(中英文), 2004, 12(2): 47-49.
ZHANG Miao-Xian, YANG Jin-Song, LI Dong-Shun. Salt migration characteristics of silt loam soil by rainstorm[J]. Chinese Journal of Eco-Agriculture, 2004, 12(2): 47-49.
Citation: ZHANG Miao-Xian, YANG Jin-Song, LI Dong-Shun. Salt migration characteristics of silt loam soil by rainstorm[J]. Chinese Journal of Eco-Agriculture, 2004, 12(2): 47-49.

特大暴雨作用下土壤盐分运移特征研究

Salt migration characteristics of silt loam soil by rainstorm

  • 摘要: 利用粉砂壤土柱研究特大暴雨过程中土壤盐分运移特征结果表明,当地下水埋深为1.5m 时特大暴雨作用下0~30cm 土层土壤盐分下移至30~105cm 土层段,属浅位脱盐,雨后土壤盐分极易再次升至耕作层;地下水埋深为2.5m 时0~83cm 土层土壤盐分下移至83~200cm 土层段,其淋洗效果最佳;地下水埋深为3.0m 时100~200cm 土层土壤盐分下移至205~255cm 土层段,属深部脱盐。

     

    Abstract: The salt migration characteristics of silt loam soil column were analyzed under the process of leaching by the rainstorm in different groundwater depths under cotton vegetation.The results show that the salinity of 0~30cm soil layer migrates down to 30~105cm when the depth to groundwater is 1.5 m which belongs to shallow desalt,and moves up to topsoil easily again;the salinity of 0~83cm soil layer migrates down to 83~200cm when the depth to groundwater is 2.5m which belongs to central desalt;the salinity of 100~200cm soil layer migrates down to 205~255cm when depth to groundwater is 3m which belongs to deep dealt.

     

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