Abstract
A systematic summary is presented describing the application of isotope tracer method in detecting seepage flow in a single borehole. In a single borehole, many hydraulic coefficients, such as flow velocity, direction of flow, vertical flow etc., Can be obtained by using isotope tracer method. There are three conditions if a fissure intersects a borehole: vertical, parallel and tilt. According to each different condition, the formulation of flow velocity deduced by isotope dilution method is different. At the same time, well theory of blended borehole about fissure groups including single fissure group and multi-fissure groups, has also been discussed.
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References
Plata, A., Detection of leaks from reservoir and lakes, Using artificial tracer in hydrology, IAEA-TECDOC-601. Vienna: IAEA, 1991: 71.
Chen Jiansheng, Study of isotope tracer theory and method in rock hydraulics, Doctoral dissertation, Hohai university, 2000.
Moser, H., Drost, W., Application of single and multi-well techniques in fractured rocks, Isotope techniques in the study of the hydrology of fractured and fissured rocks, IAEA-AG-329.2/12, Vienna: IAEA, 1989: 223.
Chen Jiansheng, Zhao Weibing, Study of permeability of fractured rock by isotope tracer method, Journal of Hohai University, 2000, 3.
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Chen, J., Dong, H. Study of fissured-rock seepage flow with isotope tracer method in single borehole. Sci. China Ser. E-Technol. Sci. 44 (Suppl 1), 108–113 (2001). https://doi.org/10.1007/BF02916799
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DOI: https://doi.org/10.1007/BF02916799