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INVESTIGATION OF THE INTERNAL STRUCTURE OF EARTHEN WATER-DEVELOPMENT WORKS BY NONDESTRUCTIVE SEISMIC METHODS

机译:用非破坏性地震方法研究伊甸水开发工程的内部结构

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摘要

Use of the method of seismic tomography permits on-going and highly detailed exposure of weaken sections of structures and their beds. The problem of ensuring the stability of water-development works (WDW) remains one of the most critical in-service problems of these structures. Strong crystalline rocks, which ensure reliable WDW performance throughout their significantly lengthy service lives, are the beds of earth dams and dikes built on the Kola Peninsula. As a rule, damage sustained by water-development works formed from fill soils may be caused by an unfavorable filtration regime in the body of the structure, as a result of which suffosion processes, and, correspondingly, suffosion deformations of the structure develop [1,2]. At the same time, the natural jointing of the beds, and zones of tectonic disturbances and fractures that intersect the WDW may also substantially degrade the in-service operating regime of the dams. Reliable, ongoing information on the internal structure of the earth-dam/bed system will appreciably diminish the risk of appearance of unscheduled emergency situations.
机译:地震层析成像方法的使用允许对结构的弱化部分及其床层进行持续且高度详细的曝光。确保水利开发工程(WDW)稳定性的问题仍然是这些结构在使用中最关键的问题之一。坚固的结晶岩是可乐半岛上修建的土坝和堤坝的基床,可确保WDW在相当长的使用寿命中具有可靠的WDW性能。通常,由填充土形成的注水工程所造成的破坏可能是由于结构体中不利的过滤状态而导致的,其结果是,形成了窒息过程,并相应地导致了结构的窒息变形[1]。 ,2]。同时,与WDW相交的地层的自然接合以及构造扰动和裂缝区域也可能大大降低大坝的运行状态。关于土坝/河床系统内部结构的可靠,持续的信息将显着降低出现计划外紧急情况的风险。

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