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- W31784712 abstract "This chapter provides an overview of the groundwater flow through the disposal rooms to the surface. During transport, radionuclides are diluted by fresh waters from the surrounding rocks and from infiltration from surface waters. Local changes in the flow velocity due to fractures in the rock improve the mixing. Although some radionuclides are still dangerous, the levels of concentration can be decreased by dilution to less than those existing in nature. Finally, there is the natural ability of minerals in rocks to attract radionuclide particles in such a way that they become attached to each other. This process is known as “sorbtion.” It retards the movement of the particles through the rock. The sorbtion abilities of rocks vary from rock type to rock type. Some are good; particularly when clay minerals coat the fracture walls as often happens in nature. Some are poor unless it contains thin layers of clay and shale." @default.
- W31784712 created "2016-06-24" @default.
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- W31784712 date "1982-01-01" @default.
- W31784712 modified "2023-09-25" @default.
- W31784712 title "Groundwater Flow Through the Disposal Rooms and to the Surface" @default.
- W31784712 doi "https://doi.org/10.1016/b978-0-08-027608-3.50016-9" @default.
- W31784712 hasPublicationYear "1982" @default.
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