Multibarrier systems are commonly proposed for effective isolation of highly radioactive waste (HLW). Presently considered concepts take the host rock as a barrier claiming it to retard migration of possibly released ...Multibarrier systems are commonly proposed for effective isolation of highly radioactive waste (HLW). Presently considered concepts take the host rock as a barrier claiming it to retard migration of possibly released radionuclides from HLW containers to the biosphere. This capacity is small unless water-bearing fracture zones intersecting the blasted waste-containing tunnels and excavation-disturbance zones around them can be sealed by grouting and construction of bulkheads, but this is effective only for a very limited period of time as explained in the paper. The disturbed zones thence make the entire repository serve as a continuous hydraulic conductor causing quick transport of released radionuclides up to the biosphere. The dilemma can be solved by accepting the shortcircuiting function of the disturbed zones along the tunnels on the condition that totally tight waste containers be used. Deep holes bored in the site selection phase through the forthcoming repository can be effective pathways for radionuclides unless they are properly sealed. They are small-scale equivalents of tunnels but do not have any excavation damage and can be effectively sealed by using clay and concrete of new types. Applying this principle to very deep boreholes with a diameter of a few decimeters would make it possible to safely store slim, tight HLW canisters for any period of time.展开更多
Rock avalanche–debris flows triggered by earthquakes commonly take place in mountainous areas.When entering a body of water,due to good fluidity they can move for some time instead of halting in water.In this study,w...Rock avalanche–debris flows triggered by earthquakes commonly take place in mountainous areas.When entering a body of water,due to good fluidity they can move for some time instead of halting in water.In this study,we proposed a method for calculating the surge height of rock avalanche–debris flows based on momentum balance and designed a series of model tests to validate this method.The experimental variables include the initial water depth,landslide velocity,and landslide volume.According to the experimental results,we analyzed the maximum wave height in sliding zone based on momentum balance.In addition,we investigated the surge height and proposed the calculation method in propagating zone and running up zone.In this way,we can find out the surge height in different areas when a rock avalanche–debris flow impacts into the water,which could provide a basis for analyzing the burst of barrier lakes.展开更多
文摘Multibarrier systems are commonly proposed for effective isolation of highly radioactive waste (HLW). Presently considered concepts take the host rock as a barrier claiming it to retard migration of possibly released radionuclides from HLW containers to the biosphere. This capacity is small unless water-bearing fracture zones intersecting the blasted waste-containing tunnels and excavation-disturbance zones around them can be sealed by grouting and construction of bulkheads, but this is effective only for a very limited period of time as explained in the paper. The disturbed zones thence make the entire repository serve as a continuous hydraulic conductor causing quick transport of released radionuclides up to the biosphere. The dilemma can be solved by accepting the shortcircuiting function of the disturbed zones along the tunnels on the condition that totally tight waste containers be used. Deep holes bored in the site selection phase through the forthcoming repository can be effective pathways for radionuclides unless they are properly sealed. They are small-scale equivalents of tunnels but do not have any excavation damage and can be effectively sealed by using clay and concrete of new types. Applying this principle to very deep boreholes with a diameter of a few decimeters would make it possible to safely store slim, tight HLW canisters for any period of time.
基金supported by the National Program on Key Research Projects of China(Grant No.2016YFC0802206)the National Natural Science Foundation of China(Grant No.41571004)
文摘Rock avalanche–debris flows triggered by earthquakes commonly take place in mountainous areas.When entering a body of water,due to good fluidity they can move for some time instead of halting in water.In this study,we proposed a method for calculating the surge height of rock avalanche–debris flows based on momentum balance and designed a series of model tests to validate this method.The experimental variables include the initial water depth,landslide velocity,and landslide volume.According to the experimental results,we analyzed the maximum wave height in sliding zone based on momentum balance.In addition,we investigated the surge height and proposed the calculation method in propagating zone and running up zone.In this way,we can find out the surge height in different areas when a rock avalanche–debris flow impacts into the water,which could provide a basis for analyzing the burst of barrier lakes.
