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Soil-water characteristics of compacted sandy and cemented soils with and without vegetation

机译:有和没有植被的压实沙质和胶结土壤的土壤水特征

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Experiments were undertaken to study the soil-water characteristics of compacted sandy soil (SS) and cemented soil (CS) in field and laboratory conditions. The influence of vegetation and material density on the development of negative pore-water pressure (PWP) and degree of saturation (Sr) in the studied materials was investigated. The field planting experiments demonstrated a promising survival rate of Schefflera heptaphylla in both types of material, while the (SS) promoted better growth of the seedlings than the cemented one. In the field study, PWP and Sr of the compacted SS responded noticeably and promptly to natural drying-wetting cycles. However, the responses in the CS were relatively mild. When subjected to the same drying-wetting cycles, PWP responded more slowly and to a smaller magnitude compared with that of the uncemented counterpart. In addition, Sr changed little in CS. An increase in the density of the SS promoted rapid development of negative PWP, while an opposite trend was observed for CS. Attempts have been made to explain the observations from the perspectives of material permeability and change in water content during a drying period in both soil types. Furthermore, in SS, the development of PWP (with a measurement limit of -90 kPa) was minimally affected by the presence of vegetation, while vegetation noticeably helped the development of negative PWP in CS. Bounds of the soil-water characteristic curve (SWCCs) of the studied materials were presented based on estimates from the drying and wetting scanning curves derived from the field monitoring. A corresponding laboratory study was carried out in an environmental chamber with controllable temperature and humidity. Monitoring results from the laboratory agreed qualitatively with those obtained from the field.
机译:在野外和实验室条件下,进行了试验以研究压实的沙土(SS)和胶结土(CS)的土壤-水特征。研究了植被和材料密度对研究材料中负孔隙水压力(PWP)和饱和度(Sr)的发展的影响。田间种植实验表明,两种材料中七叶鹅掌柴的成活率都很高,而(SS)促进了幼苗的生长,使其高于固结的。在田间研究中,压实的SS的PWP和Sr对自然的干湿循环反应明显且迅速。但是,CS中的反应相对温和。当进行相同的干湿循环时,PWP的响应比未胶结的PWP响应更慢,幅度更小。另外,Sr在CS中变化不大。 SS密度的增加促进了阴性PWP的快速发展,而CS则观察到相反的趋势。已经尝试从两种土壤类型的干燥期间的材料渗透性和含水量变化的角度来解释这些观察结果。此外,在SS中,PWP的发展(测量极限为-90 kPa)受植被的影响最小,而植被显着地帮助了CS中负PWP的发展。根据野外监测得出的干燥和湿润扫描曲线的估计值,给出了研究材料的土壤-水特征曲线(SWCC)的界限。在温度和湿度可控的环境室内进行了相应的实验室研究。实验室的监测结果与从现场获得的结果在质量上是一致的。

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