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1)  Relaxed rockmass
松动岩体
1.
According to abundant prospecting data of irrigation works and hydropower stations and various reports of monographic study,it has been testified that there is relaxed rockmass over an extensive area at Dalushu dam site.
根据大量的水利水电勘察资料和各方面的专题研究成果,证明大柳树坝址存在、大范围的松动岩体
2)  loose rock mass
松动岩体
3)  dynam relaxed rockmass
松动岩体
1.
Because of its special compositions and structure characteristics of Daliushu in Heishanxia Gorge of Yellow River, the dynam relaxed rockmass shows the seepage characteristics differ from the normal rockmass, namely, the strong permeability of water and a deep water table .
黄河黑三峡大柳树松动岩体由于其特殊的物质组成、结构特征而表现出不同于正常岩体的渗透特性 ,即岩体的透水性强、地下水位埋深大。
2.
The dynam relaxed rockmass at Daliushu in Heishanxia Gorge on the Yellow River contains a great quantity of weak intercalations, which control the dynam relaxed rockmass physical and mechanical properties to a great extent.
黄河黑山峡大柳树松动岩体中含有大量的软弱层带 ,这些软弱层带在很大程度上控制了松动岩体的物理、力学性质 ,而且软弱层带在未来的高水位情况下可能发生的渗透变形与破坏更是直接威胁大坝的安全和正常的使用。
4)  dynamo-relaxed rock mass
松动岩体
1.
Different from the general rock mass,it is characterized by dynamo-relaxed rock mass.
大柳树坝址位于VIII级潜在震源区,岩体受到多次历史地震的破坏,其特征与一般岩体有明显区别,为松动岩体
5)  loosened rock mass
松动岩体
1.
At present,the steep slope of the Grand Buddha is in a dangerous situation because of its broken and loosened rock mass.
根据太原晋阳西山大佛所处的地形地貌、地质构造、气象水文条件和场地工程地质条件,分析影响大佛边坡岩体稳定性的主要因素,建立大佛松动岩体边坡稳定性分析概化模型,提出大佛边坡岩体所处的主要工况类型。
6)  dynam-relaxed rock mass
岩体松动
1.
There is a large scale of dynam-relaxed rock mass lies in Daliushu dam site.
大柳树坝址区存在大面积、大范围的岩体松动破坏现象。
2.
There is a large scale of dynam-relaxed rock mass lies in DaLiushu dam site of Yellow River.
大柳树坝址区存在大面积、大范围的岩体松动现象。
3.
There is a large scale of dynam-relaxed rock mass lies in DaLiushu dam site of Huanghe River.
 黄河黑山峡大柳树坝址区存在大范围的岩体松动破坏现象,其主要特征是岩体应力释放,结构面张开,密度显著下降。
补充资料:高温岩体发电
      利用地表深层高温干岩体所含的热量发电(见高温岩体电站)。
  

说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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