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METHOD OF DETERMINING CHANGE IN STABILITY OF FROZEN SOIL BASES

机译:确定冻土基层稳定性变化的方法

摘要

FIELD: geology.;SUBSTANCE: invention relates to engineering-geological survey, in particular, to methods of determining change in stability of frozen soil bases. According to the disclosed method, a ground base accommodates probes, each of which comprises a heating element, a receiving acoustic transducer and a thermometer. With the help of probes the ground base is thawed and the resulting acoustic emission (AE) is recorded. Samples of soil are taken from the examined base. Compliance of AE parameters with stages of deformed condition of soil and its characteristics by standardized methods, for example according to GOST 12248, is determined on them. Determine the values of activity ṄΣ and pulse duration Dimp AE averaged during thawing time M(ṄthΣ), M(Dimpth) and melting ground heating M(ṄhΣ), M(Dimph). Calculating an indicator Rtgr=[M(ṄhΣ) · M(Dimph) / [M(ṄthΣ) · M(Dimpth)]. Comparing the full-scale values Rtgrm with obtained on samples values of RtgrL, state of surveyed soil base is determined.;EFFECT: possibility of monitoring stability of frozen soil bases in monitoring mode.;1 cl, 2 dwg
机译:技术领域本发明涉及工程地质勘测,尤其涉及确定冻土基础稳定性变化的方法。根据所公开的方法,地基容纳探针,每个探针包括加热元件,接收声换能器和温度计。借助探头将地基融化,并记录所产生的声发射(AE)。从被检查的基地中获取土壤样品。通过标准化方法(例如,根据GOST 12248)确定AE参数与土壤变形条件阶段及其特性的符合性,例如根据GOST 12248。确定解冻时间M(Ṅ th Σ)期间平均的活动ṄΣ和脉冲持续时间D imp AE的值),M(D imp th )和融化地热M(Ṅ h Σ),M(D imp h )。计算指标R tgr = [M(Ṅ h Σ)·M(D imp h )/ [M(Ṅ th Σ)·M(D imp th )]]。比较满量程值R tgr m 与在采样值R tgr L 上获得的测量状态进行比较确定了土壤基础;效果:以监测模式监测冻土基础稳定性的可能性。1cl,2 dwg

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