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Groundwater residence time.
An apparent link between the tectonic structure and the groundwater residence time zonation can be established.
The key factors in the system are the elevated groundwater residence time and the effect of the evapotranspiration.
A tritium and water balance coupled model was developed and allows for the estimation of lake and groundwater residence time.
The average shallow groundwater residence time is 1.23 years, while the average deep water residence time is 125 years.
Open image in new window Fig. 6 The estimated groundwater recharge indices and groundwater residence times (years) of Pra Basin.
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Temporal patterns of nitrogen speciation and concentration reflect (1) changing NO3− loads over time, (2) groundwater residence-time controls on NH4+ mobilization from solid phases, and (3) groundwater residence-time controls on denitrification.
A typical mineralization conditioned by the sea sprays and the carbonate matrix helped to validate the groundwater weighted residence times from using a binary mixing model.
To contribute to the understanding of this aquifer the assessment of sustainable use of groundwater, the residence time of groundwater in the NP aquifer has been estimated using 3H, 14C and 36Cl.
Lakes, rivers, ice, and groundwaters have residence times lying between these two extremes and are highly variable.
Groundwater age or residence time is the time water has resided in the subsurface since recharge.
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