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Investigating patterns and controls of groundwater up welling in a lowland river by combining Fibre optic Distributed Temperature Sensing with observations of vertical hydraulic gradients

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Academic year: 2020

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Figure

Fig. 1. (A): field site location in the UK and (B): experimental de-sign at the River Tern with groundwater boreholes (GW), surfacewater gauges (SW) and the streambed piezometer network
Fig. 2. (A): conceptual model of streambed hydrofacies controlling groundwater up-welling in a typical lowland river including their effecton heat transport at the aquifer–river interface (the star indicates the temperature of the surface water)
Fig. 3. Experimental installations at the River Tern with (A): streambed piezometer setup for VHG monitoring, PTS = Permo-Triassic Sand-stone.; (B): FO-DTS cable loop in the investigated meander bend; (C): close-up of cable layout in the streambed sediment
Table 1. Spatial and temporal resolution of environmental parameters monitored during the 2009 sampling period.
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