高盐度延长了在干燥-湿润周期中稳定土壤结构所需的水循环过程

Kai Chang, Haoxuan Feng, Jiahao Xing, Xiangping Wang, Rongjiang Yao, Xuguang Xing
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摘要

干旱和降雨等气候事件会导致干燥和湿润的循环,从而可能引起土壤结构的变化,导致盐碱土健康状况的恶化。然而,人们对盐分和干燥-湿润(D-W)循环共同影响下土壤结构退化的程度和行为知之甚少。因此,我们系统地研究了盐度(0、5、30 和 100 g/L,标记为 CK、T5、T30 和 T100)和干燥-湿润循环对土壤结构的影响,通过测定土壤体积、收缩和膨胀势以及从土壤收缩特性曲线中获得的土壤孔隙特征,探索干燥-湿润循环和盐度如何影响土壤结构。结果表明,盐碱土和非盐碱土的变形行为随 D-W 周期的次数而变化。在持续的 D-W 周期中,土壤出现了不可逆的变形。经过三个 D-W 循环后,土壤体积增加了 3.75%-15.73%。在垂直方向上,CK、T5、T30 和 T100 各处理的最大膨胀率分别为 29.03%、23.42%、34.23% 和 35.87%。水平方向上的收缩率和膨胀率相等,因为土壤样本始终恢复到原始尺寸。此外,受盐度影响的微孔和毛细孔也有所减少,在 CK、T5、T30 和 T100 中分别为 50%、58.6% 和 70.4%。然而,D-W 循环主要影响大孔隙。高盐度水平增强了膨胀潜能和居住收缩潜能,延长了土壤结构实现稳定所需的水分过程。这项研究的结果强调了了解土壤体积变化滞后性的必要性,并阐明了盐度和 D-W 周期导致土壤结构恶化的机制。这些发现为更健康的土壤管理提供了有价值的参考。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
High salinity prolongs water processes required for soil structure stability during drying–wetting cycles

Climate events, such as drought and rainfall, can lead to a cycle of drying and wetting that may cause changes in soil structure, leading to deteriorations in the health of saline soils. However, little is known about the extent and behavior of soil structure degradation under the combined influences of salinity and drying–wetting (D-W) cycles. Thus, we systematically investigated the effects of salinity (0, 5, 30, and 100 g/L, labeled as CK, T5, T30, and T100) and D-W cycles on soil structure by determining soil volume, shrinkage, and swelling potentials along with soil pore character obtained from soil shrinkage characteristics curve, intending to explore how D-W cycles and salinity affect soil structure. The results showed that soil deformation behaviors in saline and non-saline soils varied with the number of D-W cycles. Irreversible deformation of the soil was observed during continual D-W cycles. The soil volume increased by 3.75%–15.73% after three D-W cycles. In vertical direction, the maximum expansion magnitude for each treatment was reached with the value of 29.03%, 23.42%, 34.23%, and 35.87% in CK, T5, T30, and T100, respectively. The magnitudes of shrinkage and expansion were equal in the horizontal direction since the soil samples consistently returned to their original dimensions. Furthermore, the decrease was observed in the micropores and capillary pores affected by salinity, with values of 50%, 58.6%, and 70.4% in CK, T5, T30, and T100, respectively. However, the D-W cycles primarily affected large pores. High salinity levels enhanced swelling potential and inhabit shrinkage potential, prolonging the water processes required for the soil structure to achieve stability. The results of this study underscore the necessity of understanding the hysteresis of soil volume change and elucidate the mechanisms of soil structure deterioration driven by salinity and D-W cycles. These findings provide a valuable reference for healthier soil management.

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