Investigating young water fractions in a small Mediterranean mountain
catchment: both precipitation forcing and sampling frequency matter
Abstract
The young water fraction (Fyw), the proportion of
water younger than 2-3 months, was investigated in soil-, ground- and
stream waters in the 0.56 Km2 sub-humid Mediterranean
Can Vila catchment. Rain water was sampled at 5-mm rainfall intervals.
Mobile soil water and groundwater were sampled fortnightly, using
suction lysimeters and two shallow wells, respectively. Stream water was
dynamically sampled at variable time intervals (30 minutes to 1 week),
depending on flow. A total of 1,529 18O determinations
obtained during 58 months were used. The usual hypothesis of rapid
evapotranspiration of summer rainfall could not be maintained, leading
to discard the use of an “effective precipitation” model. Soil mobile
waters had Fyw up to 34%, while in ground and
stream were strongly related to water table and discharge variations,
respectively. In stream waters, due to the highly skewed flow duration
curve, the flow-averaged young water fraction
(F*yw) was 22.6%, whereas the time-averaged
Fyw was 6.2%. Nevertheless, both
F*yw and its exponential discharge sensitivity
(Sd) showed relevant changes when different
12-month sampling periods were investigated. The availability of
Sd and a detailed flow record allowed us to
simulate the young water fraction that would be obtained with a virtual
thorough sampling (F**yw). This showed that
underestimation of F*yw is associated with
missing the sampling of highest discharges and revealed underestimations
of F*yw by 25% for the dynamic sampling and 66%
for the weekly sampling. These results confirm that the young water
fraction and its discharge sensitivity are metrics that depend more on
precipitation forcing than on physiographic characteristics, so the
comparisons between catchments should be based on mean annual values and
inter-annual variability. They also support the dependence of the young
water fraction on the sampling rate and show the advantages of
flow-weighted F*yw. Water age investigations
should be accompanied by the analysis of flow duration curves. In
addition, the simulation of F**yw is proposed as
a method for checking the adequacy of the sampling rate used.