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首页> 外文期刊>Engineering Geology >Pot-hole subsidence in Son-Mahanadi Master Coal Basin
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Pot-hole subsidence in Son-Mahanadi Master Coal Basin

机译:Son-Mahanadi主煤盆地的井底塌陷

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Pot-hole subsidence is an abrupt depression of local ground surface, which occurs due to sudden collapse of the overburden into an underground void. Pot-hole subsidence is a common form of subsidence in Jamuna and Kotma, Hasdeo and Bisrampur areas of Son-Mahanadi Master Coal Basin. Data of 34 cases of pot-hole subsidence were collected from the above areas and analysed from stand point of their causative factors, prediction, mechanism, and suggested mitigative measures. Analysis of these cases revealed that shallow depth, geological discontinuities, weak and saturated overburden are the main causative factors for the pot-holing phenomenon. Movement of eroded materials from saturated and weathered overburden with water along a fault plane into the underground bord and pillar development led to the formation of a pot-hole. Risk of pot-hole subsidence is high when the pot-hole potential ratings of causative factors are between 80 and 100. Suggested mitigative measures of pot-hole subsidence in bord and pillar development as well as unapproachable depillared workings include maintaining a minimum of 15 m un-weathered hard cover, controlled width and height of drivages, installation of suitable support system, back-filling, grouting of underground voids, etc.
机译:坑洼是局部地表突然下陷,这是由于上覆岩突然塌陷到地下空洞中所致。在Son-Mahanadi主煤盆地的Jamuna和Kotma,Hasdeo和Bismrampur地区,井孔沉降是一种常见的沉降形式。从上述地区收集了34例坑洼沉陷的数据,并从其致病因素,预测,机理和建议的缓解措施的角度进行了分析。对这些案例的分析表明,浅埋深度,地质不连续性,薄弱和饱和的上覆层是造成坑洞现象的主要原因。侵蚀后的物料从含水饱和的风化覆盖层沿断层平面运动到地下波德和柱子的发育过程中,导致形成了一个坑洞。当致病因素的坑洼潜在评级在80到100之间时,坑洼沉陷的风险很高。建议的缓和措施是防止线虫和柱子发育以及无法接近的脱毛工作中的坑洼沉陷,包括保持至少15 m未风化的硬覆盖层,可控制的宽度和高度,适当的支撑系统的安装,回填,地下空隙的注浆等。

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