首页> 外文期刊>Geoderma: An International Journal of Soil Science >Atterberg limits and shrink/swell capacity of soil as indicators for sodium sensitivity within a gradient of soil exchangeable sodium percentage and salinity
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Atterberg limits and shrink/swell capacity of soil as indicators for sodium sensitivity within a gradient of soil exchangeable sodium percentage and salinity

机译:Atterberg限制和收缩/膨胀容量作为钠敏感性的升高率升高百分比和盐度的指标

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摘要

Soil sodification and salinization present a global soil degradation risk to agricultural production since they affect soil hydraulic properties. Soils containing smectite clays have been found to be most sensitive to sodicity although little research exists directly relating sodicity to clay swelling under varying levels of salinity and Exchangeable Sodium Percentage (ESP). The goal of this study is to determine whether soil swelling related measurements can be a proxy to determine soil sensitivity to exchangeable sodium. This study examined the response of three smectitic soils treated with salt solutions having concentrations ranging between 5 and 40 mmol(c) dm(-3) and ESP levels between 0 and 50% to create differing degrees of sodicity. Whole soil Atterberg limits and the coefficient of linear extensibility (COLE) were measured prior to and after treatments. Liquid limit, plasticity index and the coefficient of linear extensibility increased for all three soils after treatment with a salt concentration of 5 mmol(c) dm(-3) at an ESP of 25 and 50% and 10 mmol(c) dm(-3) at an ESP of 50%. Comparing liquid limit of low salinity treatment at 50% ESP to low salinity 0% ESP revealed the presence of swelling smectite clay and the sensitivity of the soils to sodicity and a soil measurement to identify soil sodicity risk.
机译:土壤拟合和盐渍化为农业生产的全球土壤退化风险产生,因为它们影响了土壤液压性能。已发现含有蒙脱石粘土的土壤对钠度最敏感,尽管在不同水平的盐度和可交换钠百分比(ESP)下的粘土肿胀直接与粘土肿胀直接相关的研究。本研究的目标是确定土壤膨胀相关测量是否可以是确定对可交换钠的土壤敏感性的代理。该研究检测了用盐溶液处理的三种透晶土壤的响应,其浓度在5-40mmol(c)dm(-3)和0%至50%之间的eSP水平之间产生不同程度的癸二度。在治疗之前和之后测量整个土壤Atterberg限制和线性伸展系数(COLE)。液体限位,可塑性指数和线性伸展系数在用5mmol(c)dm(-3)的盐浓度为25和50%和10mmol(c)dm( - - 3)ESP为50%。将低盐度处理的液体限制在50%ESP至低盐度0%ESP显示出溶胀蒙脱石粘土的存在和土壤敏感性和土壤测量的敏感性,以鉴定土壤素状风险。

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