雪 静, 王全九, 毕远杰. 微咸水间歇供水土壤入渗特征[J]. 农业工程学报, 2009, 25(5): 14-19.
    引用本文: 雪 静, 王全九, 毕远杰. 微咸水间歇供水土壤入渗特征[J]. 农业工程学报, 2009, 25(5): 14-19.
    Xue Jing, Wang Quanjiu, Bi Yuanjie. Soil infiltration properties with slight saline water intermittent application[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2009, 25(5): 14-19.
    Citation: Xue Jing, Wang Quanjiu, Bi Yuanjie. Soil infiltration properties with slight saline water intermittent application[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2009, 25(5): 14-19.

    微咸水间歇供水土壤入渗特征

    Soil infiltration properties with slight saline water intermittent application

    • 摘要: 为了合理开发利用微咸水,以缓解农业淡水资源短缺的问题,该文通过室内微咸水垂直一维间歇入渗模拟试验,研究了微咸水矿化度为2、3、4、5和6 g/L,及不同周期和循环率下土壤的间歇入渗特性。根据Philip入渗公式分析了吸湿率S与矿化度间的关系。研究结果表明,微咸水间歇入渗符合间歇入渗的一般规律,但微咸水间歇入渗具有增加湿润深度的特点;不同矿化度微咸水累积入渗量和湿润深度不同,土壤吸湿率随矿化度的增大而增大(矿化度6 g/L除外),间歇入渗第一周期吸湿率最大,以后各周期吸湿率逐步减小,但变化幅度不显著,并趋于稳定。

       

      Abstract: Reasonable development and utilization of slight saline water is an important approach of relieving the agricultural freshwater resource shortage. Soil infiltration properties were studied through laboratory simulation experiments of one-dimensional vertical intermittent infiltration under different periods and circulating rates, when salt concentrations of the slight saline water were 2, 3, 4, 5 and 6 g/L. Philip’s infiltration formula was used to analyze the relationship between the sorptivity and the salt concnentration of slight saline water. The results showed that the intermittent infiltration properties of slight saline water were the same as the properties of freshwater, but the slight saline water intermittent infiltration could increase the wetted depth. The cumulative infiltration and wetted depth changed with the different salt concentrations of slight saline water. The sorptivity increased with the increasing salinity of the slight saline water, and the sorptivity was the maximum at the first period of intermittent infiltration and decrease at the following periods, but the decreasing range was not significant and tended to a stable value.

       

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