Assessment of groundwater ingress to a partially pressurized water-conveyance tunnel using a conduit-flow process model: a case study in Iran

Construction of a conveyance tunnel through rock often induces the ingress of groundwater into the tunnel, a flow that changes both the hydrogeological regime of the tunnel and its environment. To explore this key interaction, a novel modeling approach using the conduit flow process (CFP) is develop...

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Bibliographic Details
Published in:Hydrogeology journal 2020-11, Vol.28 (7), p.2573-2585
Main Authors: Gholizadeh, Hossein, Behrouj Peely, Ahmad, Karney, Bryan W., Malekpour, Ahmad
Format: Article
Language:English
Subjects:
Aquatic Pollution
Earth and Environmental Science
Earth Sciences
Geology
Geophysics/Geodesy
Hydrogeology
Hydrology/Water Resources
Waste Water Technology
Water Management
Water Pollution Control
Water Quality/Water Pollution
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Summary:Construction of a conveyance tunnel through rock often induces the ingress of groundwater into the tunnel, a flow that changes both the hydrogeological regime of the tunnel and its environment. To explore this key interaction, a novel modeling approach using the conduit flow process (CFP) is developed that considers both the hydraulic head and the ingress of water from the rock matrix during excavation. The resulting flow values are predicted through an adapted MODFLOW numerical model into which the tunnel is introduced with the aid of the new CFP approach. The CFP approach can simulate both laminar and turbulent flow in the tunnel whether the flow is free surface or pressurized. Several simulations, including one for which the permeability of the tunnel perimeter is assumed to be identical to the hydraulic conductivity of the surrounding rock matrix, are then used to explore the sensitivity of the predicted head and flow conditions to the permeability of the tunnel perimeter. Comparisons of the numerical results with field data from the Kerman Water Conveyance Tunnel in Iran show that the proposed approach accurately predicts the spatial variation of both groundwater ingress and hydraulic head.
ISSN:1431-2174
1435-0157
DOI:10.1007/s10040-020-02213-y