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• W2598678332 abstract "The amount of precipitation that infiltrates mountain bedrock is poorly quantified, yet known to strongly influence alpine stream baseflow, landslide initiation, lowland aquifer recharge and, potentially, fault strength. Groundwater discharge in a 355 m tunnel through the western flank of the Southern Alps, New Zealand, was monitored from April 2012 to January 2013 and compared with rainfall records at a nearby rain gauge in order to advance understanding of rainwater infiltration into schist bedrock. Tunnel discharge responded rapidly to 21 distinct rainfall events, with their discharge hydrographs characterised by steeply rising limbs and exponential declines following peak discharges. Two anomalous discharge events (ADE) were recorded when discharge increased despite the absence of associated rainfall. A significant ADE during July 2012 is attributed to snowmelt. Calculated cumulative tunnel discharge and proportions of rainfall infiltration (derived from rainfall versus discharge) indicate that from September 2012 to January 2013 greater volumes of water entered the tunnel, per unit of rainfall, than from April to August 2012. Differences in the magnitude and timing of peak discharge relative to rainfall were also observed between the two periods. Differences in volume and flow rate are thought to reflect seasonal rise of the water table intersecting the tunnel to induce lateral flow and elevate observed discharge. Estimates of the proportion of rainfall that infiltrated bedrock vary between events, from 0.3 to 20%." @default.
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• W2598678332 date "2015-01-01" @default.
• W2598678332 modified "2023-09-26" @default.
• W2598678332 title "Seasonal infiltration and groundwater movement in schist bedrock, Southern Alps, New Zealand" @default.
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• W2598678332 hasPublicationYear "2015" @default.
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