Assessment of the barrier effect caused by underground constructions on porous aquifers with low hydraulic gradient: A case study of the metro construction in Barcelona, Spain
Abstract
Construction of tunnels can impact aquifers because of the changes produced in the
natural groundwater behavior. The drain effect, which is one of the most important impacts,
can be eliminated using a tunnel-boring machine (TBM) to drill a tunnel with an impervious
lining. However, the use of impermeable linings results in aquifer obstruction, giving rise to
the barrier effect, which may cause an increase and decrease of the hydraulic head upgradient
and downgradient of the tunnel, respectively. This modification of the hydraulic head, which
can be predicted analytically and is proportional to the natural hydraulic gradient of the
aquifer perpendicular to the tunnel ( N i ) (before it is constructed), is negligible for aquifers
with values of N i that are very small or null (approximately 0). In these cases, the analytical
solutions are not useful to estimate the real impact because the head distribution is not largely
affected.
This study proposes a methodology to evaluate the hydrogeological impact produced
by the construction of underground impervious structures in aquifers, which have a small or
null N i . The method, which is based on the analysis of the groundwater response to pumping
tests performed before and after construction, was tested in a stratified porous aquifer and was
used along with numerical modeling to assess the barrier effect in an experimental site (Sant
Cosme, El Prat de Llobregat, Barcelona). The impact on the head distribution was negligible.
However, the reduction of the connectivity was considerable. Pumping tests can determine the
changes in aquifer connectivity caused by the construction of an underground impervious
structure. The behavior of the groundwater during the post-tunneling pumping changes with
regards to the pre-tunneling tests. A delay in the response to the pumping and a decrease of
the drawdown are observed in the piezometers located on the opposite side of the tunnel
where the well is placed, whereas an increase of drawdown occurs in the piezometers situated
on the same side of the well. The procedure explained in this paper reveals a useful tool for
determining the impact caused by underground impermeable constructions in aquifers, where
N i is small or even 0.
Origin : Files produced by the author(s)
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