Processes affecting groundwater chemistry in a zone of saline intrusion into an urban sandstone aquifer

Samples have been collected from inflows into railway tunnels in the Triassic sandstone aquifer beneath Liverpool and the Mersey Estuary, England, U.K. These provide a profile through a saline-freshwater mixing zone. Analyses were made of major anions and cations, delta(34)S and delta(18)O in SO4, delta(13)C in dissolved inorganic C and Sr-87/Sr-86. The data demonstrate that the presence of a low permeability fault exerts a strong control on the local groundwater chemistry. On the estuary side of the fault, groundwater-chemistry is dominated by mixing of intruding estuary water, which is modified by SO4 reduction and calcite dissolution, with fresh groundwater. The environment of SO4 reduction in the tidal estuary is one of repeated reduction and re-oxidation of S in an open system and has resulted in virtually no change in S isotopic composition, but an enrichment in residual SO4 delta(18)O of 1.5 parts per thousand. Groundwater chemistry on the landward side of the fault is primarily the result of recharge in an urban environment. There is also evidence that saline water has been present in this region of the aquifer in the past and that this has now been flushed by fresh groundwaters. This saline water was either transported along the landward side of the fault from nearer the estuary or more probably transmitted across the fault. Both mechanisms would have been driven by large landward head gradients caused by heavy industrial abstraction earlier this century. This has produced a zone of groundwaters depleted in Ca and radiogenic;Sr and enriched in Na as a result of ion exchange between the fresh groundwaters and the aquifer previously occupied by more saline water. Sulphur isotopic composition, however, shows no variation since SO4 does not undergo significant ion exchange. A tracer test from a borehole to the tunnels showed multiple breakthroughs to some locations indicating a;number of different how paths through the aquifer. The maximum flow velocity recorded in this test was 140 m/d suggesting flow along fractures. (C) 1998 Elsevier Science Ltd. All rights reserved.