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Self sealing backfill (SVV) - A salt based material for constructing seals in salt mines

机译:自封回填(SVV) - 一种基于盐矿山密封的盐材料

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A self-sealing salt backfill (S W) based on anhydrous magnesium sulphate has been developed. Fine grained dry initial material (SW) can be emplaced pneumatically Artificial flooding of the pore space with brine initiates a reaction that leads to the formation of a brine tight seal,. The reaction consumes the brine completely and forms an impermeable plug with a new mineralogy and greater volume of solids. The initial high porosity is reduced to 2-5 vol,,-% of isolated pores. Miner alogical assemblages obtained in the experiments and measured by X-ray diffraction agree well with results of geochemical modelling with EQ3/6. The geochemical modelling allows the quantification of the short- and long-term volume changes in the system and demonstrates that in the long run stable mineral assemblages will be obtained. The volume increase leads to a considerable crystallization pressure The porosity/permeability relationship resembles that of highly compacted crushed rock salt backfill The mechanical properties are comparable with the values of undisturbed rock salt. These results indicate that SVV is a self-sealing long-term stable and to wide extend predictable predictable material.
机译:基于无水硫酸镁自密封盐回填(S W)已经研制成功。细粒干燥初始材料(SW)可以布设孔隙空间的气动人工驱用盐水发起的反应,导致盐水紧密密封的形成,。反应完全消耗盐水,并形成一个新的矿物学和固体的体积更大的不可渗透的塞子。初始的高孔隙率减至2-5体积,, - 中分离的孔的%。在实验中获得的,并通过X射线衍射测得的矿工非逻辑组合与EQ3 / 6地球化学模拟的结果吻合良好。地球化学模型允许在系统中的短期和长期的体积变化的定量分析,并表明,从长远来看稳定的矿物组合也会获得。音量增加导致显着的结晶化压力的孔隙率/渗透率的关系类似于高度压实的碎石盐的回填的机械性质与未受干扰的岩盐的值相媲美。这些结果表明,SVV是自密封的长期稳定且宽的延伸可预测的预测的材料。

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