Experimental Study on the Influence of Temperature on Salt Expansion of Sodium Sulfate Saline Soil

Xusheng Wan, Mengke Liao, L. Du
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引用次数: 8

Abstract

To find the rule on the effect of different temperatures on salt expansion of sodium sulfate saline soil and ensure the safety of road engineering in areas with sulfate saline soil, we tested saline soil samples in a laboratory. By analyzing the variation in soil samples before and after cooling and the variation in water content under different temperatures, we determined the influence of salt expansion on soil components under different temperatures by using computed tomography. Results show that salt expansion intensifies and tends to stabilize under decreasing temperature. Salt expands mainly from 0℃ to the initial precipitation temperature of salt crystals, and very slight precipitation occurs at a negative temperature; thus, salt expansion is very low at temperatures below 0℃. Moisture content decreases as temperature decreases, and the diminishing trend decreases and gradually stabilizes at 0℃. Damage in soil structure increases as temperature decreases. Change in porosity occupied by air is mainly determined by change in water content. Porosity changes acutely with acute changes in water content, and these parameters show an inverse relationship.
温度对硫酸钠盐渍土盐膨胀影响的实验研究
为了找出不同温度对硫酸钠盐渍土盐膨胀的影响规律,保证硫酸钠盐渍土地区道路工程的安全,在实验室对盐渍土样品进行了测试。通过分析冷却前后土壤样品的变化以及不同温度下土壤含水量的变化,利用计算机断层扫描技术确定不同温度下盐膨胀对土壤组分的影响。结果表明,随着温度的降低,盐的膨胀加剧并趋于稳定。盐主要从0℃膨胀到盐结晶的初始析出温度,负温度下有极轻微的析出;因此,在低于0℃的温度下,盐的膨胀非常低。含水率随温度的降低而减小,在0℃时减小趋势逐渐趋于稳定。土壤结构的破坏随着温度的降低而增加。空气所占孔隙度的变化主要是由含水量的变化决定的。孔隙度随含水率的急剧变化而急剧变化,这些参数呈反比关系。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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