低中放废物处置场的岩体渗透特性分析

Analysing the Rockmass Permeation of a Low-medium Radioactive Waste Disposal Field

在基岩地区,研究地下水运动特征和污染物迁移的前提条件是研究基岩介质中裂隙的分布特征和裂隙岩体的渗透性能,其中包括导水裂隙优势方位研究、基岩裂隙水的活跃带分布研究和基岩裂隙渗透参数的计算。为此,结合我国西北某放射性废物处置场丰富的地质资料,对该处置场裂隙发育分布特征、导水裂隙优势方位及其渗透性参数进行了比较系统的分析。通过统计、分析、比较和计算发现,基岩裂隙水活跃带是核素向外界迁移的活跃通道,某低中放废物处置场内的导水裂隙有一个优势方位。并且还求出了某低中放废物处置场基岩裂隙的渗透系数张量。

The fractures distribution and fracture rock mass permeation research is the premise condition that to study groundwater movement and pollutant migration in fracture rock mass in bed rock area, which includes the dominance orientation of fracture that groundwater fluxes in it, the brisk zone distribution of fracture water and the permeability calculation of rock mass. This paper mainly analyzes the fracture distribution and the dominance orientation of fracture and the permeability of a low-medium radioactive waste disposal field based on its rich geologic record. The following results are found through Statistical analysis and comparison calculation.The active zone of fractural water in bed rock is an active channel of active nucleus migration. Tthe headrace fracture of disposition have a dominant orientation. The penetrating coefficient tensor in bed rock fracture is also calculated.