Groundwater age is often used to estimate groundwater recharge through a simplified analytical approach. This estimated recharge is thought to be representative of the mean recharge between the point of entry and the sampling point. However, given the complexity in actual recharge, whether the mean recharge is reasonable is still unclear. This study examined the validity of the method to estimate long-term average groundwater recharge and the possibility of obtaining reasonable spatial recharge pattern. We first validated our model in producing reasonable age distributions using a constant flux boundary condition. We then generated different flow fields and age patterns by using various spatially varying flux boundary conditions with different magnitudes and wavelengths. Groundwater recharge was estimated and analysed afterwards using the method at the spatial scale. We illustrated the main findings with a field example in the end. Our results suggest that we can estimate long-term average groundwater recharge with 10% error in many parts of an aquifer. The size of these areas decreases with the increase in both the amplitude
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Groundwater age is often used to estimate groundwater recharge through a
simplified analytical approach. This estimated recharge is thought to be
representative of the mean recharge between the point of entry and the
sampling point. However, given the complexity in actual recharge,
whether the mean recharge is reasonable is still unclear. This study
examined the validity of the method to estimate long-term average
groundwater recharge and the possibility of obtaining reasonable spatial
recharge pattern. We first validated our model in producing reasonable
age distributions using a constant flux boundary condition. We then
generated different flow fields and age patterns by using various
spatially-varying flux boundary conditions with different magnitudes and
wavelengths. Groundwater recharge was estimated and analyzed afterwards
using the method at the spatial scale. We illustrated the main findings
with a field example in the end. Our results suggest that we can
estimate long-term average groundwater recharge with 10% error in many
parts of an aquifer. The size of these areas decreases with the increase
in both the amplitude and the wavelength. The chance of obtaining a
reasonable groundwater recharge is higher if an age sample is collected
from the middle of an aquifer and at downstream areas. Our study also
indicates that the method can also be used to estimate local groundwater
recharge if age samples are collected close to the water table. However,
care must be taken to determine groundwater age regardless of
conditions.
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