In this paper, we are concerned with a specific scenario where a large fracture intersects, at its center, a canister that contains spent nuclear fuel. Assuming that a nuclide is free to release from the canister into groundwater flowing through the fracture, a detailed formulation of the volumetric flow rate and the equivalent flow rate are made for the parallel plate model. The formulas proposed have been validated by numerical examinations; they are not only simple in forms but also universal in applications where the flow may be taken normal, inclined or parallel to the axis of the canister. Of great importance, they provide a convenient way to predict the average properties of fluid flow and solute transport through a single fracture with spatially variable apertures.
机构:Hohai Univ, Sch Earth Sci & Engn, Nanjing 210098, Peoples R China
Dou, Zhi
Tang, Songxuan
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Hohai Univ, Sch Earth Sci & Engn, Nanjing 210098, Peoples R ChinaHohai Univ, Sch Earth Sci & Engn, Nanjing 210098, Peoples R China
Tang, Songxuan
Zhang, Xueyi
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Hohai Univ, Sch Earth Sci & Engn, Nanjing 210098, Peoples R China
Eawag, Swiss Fed Inst Aquat Sci & Technol, CH-8600 Dubendorf, SwitzerlandHohai Univ, Sch Earth Sci & Engn, Nanjing 210098, Peoples R China
Zhang, Xueyi
Liu, Richeng
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China Univ Min & Technol, State Key Lab Geomechan & Deep Underground Engn, Xuzhou 221116, Jiangsu, Peoples R China
Nagasaki Univ, Sch Engn, Nagasaki 8528521, JapanHohai Univ, Sch Earth Sci & Engn, Nanjing 210098, Peoples R China
Liu, Richeng
Zhuang, Chao
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Hohai Univ, Sch Earth Sci & Engn, Nanjing 210098, Peoples R ChinaHohai Univ, Sch Earth Sci & Engn, Nanjing 210098, Peoples R China
Zhuang, Chao
Wang, Jinguo
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Hohai Univ, Sch Earth Sci & Engn, Nanjing 210098, Peoples R ChinaHohai Univ, Sch Earth Sci & Engn, Nanjing 210098, Peoples R China
Wang, Jinguo
Zhou, Zhifang
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Hohai Univ, Sch Earth Sci & Engn, Nanjing 210098, Peoples R ChinaHohai Univ, Sch Earth Sci & Engn, Nanjing 210098, Peoples R China