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- W120579423 abstract "In large bodies of sedimentary rock containing salt formations, the groundwater flows over, under, or around the salt but never through it under natural circumstances. The flowing water in the sedimentary rocks may dissolve away the outside edges of the salt. Groundwater could flow through a repository in salt if violent fracturing of the earth's crust took place at some future time in geologic history. This chapter discusses the paths for groundwater flows in hard rock masses containing joints and fractures. The widths of fractures and joint openings vary from locality to locality. They generally decrease with depth in the earth's crust. This is due to the weight of the overburden rock. These widths are commonly small, perhaps less than 0.5 mm. The quantity of flowing water decreases significantly with decreasing width." @default.
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- W120579423 date "1982-01-01" @default.
- W120579423 modified "2023-09-23" @default.
- W120579423 title "Groundwater Flow Near the Repository" @default.
- W120579423 doi "https://doi.org/10.1016/b978-0-08-027608-3.50015-7" @default.
- W120579423 hasPublicationYear "1982" @default.
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