探地雷达监测路基土壤低温过程

L. Fedorova, D. Savvin, M. Fedorov, A. S. Struchkov
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引用次数: 6

摘要

冻土地区的道路作业需要监测路基土壤,因为其性质的季节性变化以及负低温过程的发展。利用探地雷达监测路基土的性质和状况是最有效的。通过对北方地区道路路基土的理论和试验研究,揭示了探空道路路面变形接收的探地雷达数据的主要波特征。在此基础上,提出了利用季节变化数据识别负低温过程和监测土壤状况的方法。所提出的方法的一个显著特征是在土壤最大冻结和最大解冻期间获得的比较数据的基础上定量确定土壤湿度。通过对雅库特地区道路的探地雷达测量,验证了该方法的可行性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
GPR monitoring of cryogenic processes in subgrade soils
Road operation in areas with frozen soils requires monitoring of subgrade soils due to seasonal changes of their properties as well as development of negative cryogenic processes. Monitoring subgrade soil properties and condition is most effective using GPR. The results of theoretical and experimental studies of subgrade soils of roads in the North revealed the main wave characteristics of GPR data received by sounding road pavement deformations. Based on the characteristics revealed a method to identify negative cryogenic processes and monitor soil condition has been proposed from data of seasonal changes. A distinctive feature of the proposed method is the quantitative determination of soil moisture on the basis of comparative data obtained during maximum freezing and maximum defrosting of the soil. The feasibility of the proposed method is demonstrated by GPR survey of roads in Yakutia.
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