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Volumn 194, Issue 1-2, 2001, Pages 213-219

Theoretical relation between water flow rate in a vertical fracture and rock temperature in the surrounding massif

Author keywords

Alps; Fractures; Ground water; Mountains; Numerical analysis; Temperature; Tunnels

Indexed keywords

FRACTURE; GROUNDWATER; NUMERICAL METHOD; TEMPERATURE; TUNNEL; WATER FLOW;

EID: 0035705408     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0012-821X(01)00551-9     Document Type: Article
Times cited : (13)

References (18)
  • 2
    • 0000705713 scopus 로고
    • Temperature gradients in the upper layers of the earth's crust due to convective water flows
    • (1962) J. Geophys. Res , vol.67 , pp. 3449-3459
    • Donaldson, J.G.1
  • 6
    • 0027799550 scopus 로고
    • Evaluation of vertical groundwater fluxes and thermal properties of aquifers based on transient temperature- depth profiles
    • (1993) Water Resour. Res , vol.29 , pp. 2021-2026
    • Taniguchi, M.1
  • 13
    • 0008179995 scopus 로고    scopus 로고
    • Prognosis of rock temperatures and water inflow zones in deep tunneling: Examples from the NEAT-project, Swiss Alps
    • Golser, Hinkel and Schubert (Eds.), Balkema, Rotterdam
    • (1997) Tunnels for People , pp. 9-14
    • Busslinger, A.1    Rybach, L.2
  • 15
    • 0033496774 scopus 로고    scopus 로고
    • Relation between temperature and intensity of groundwater circulation in alpine massifs as a tool for predicting water inflows in tunnels
    • (1999) Rev. Sci. Eau , vol.12 , pp. 515-528
    • Maréchal, J.C.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.