Dry-season length and runoff control annual variability in stream DOC dynamics in a small, shallowgroundwater-dominated agricultural watershed
Abstract
As a phenomenon integrating climate conditions and hydrological control of the connection between
streams and terrestrial dissolved organic carbon (DOC) sources, groundwater dynamics control
patterns of stream DOC characteristics (concentrations and fluxes). Influence of intra-annual
variations in groundwater level, discharge and climatic factors on DOC concentrations and fluxes
were assessed over 13 years at the headwater watershed of Kervidy-Naizin (5 km²) in western
France. Four seasonal periods were delineated within each year according to groundwater
fluctuations (A: rewetting, B: high flow, C: recession, and D: drought). Annual and seasonal base
flow vs stormflow DOC concentrations were defined based on daily hydrograph readings. High
inter-annual variability of annual DOC fluxes (5.4-39.5 kg.ha-1.yr-1) indicates that several years of
data are required to encompass variations in water flux to evaluate the actual DOC export capacity of
a watershed. Inter-annual variability of mean annual DOC concentrations was much lower (4.9-7.5
mg C.l-1), with concentrations decreasing within each year from ca. 9.2 mg C.l-1 in A to ca. 3.0 mg
C.l-1 in C. This indicates an intra-annual pattern of stream DOC concentrations controlled by DOC
source characteristics and groundwater dynamics very similar across years. Partial least square
regressions combined with multiple linear regressions showed that the dry season characteristics
(length and drawdown) determine the mean annual DOC concentration while annual runoff
determines the annual flux. Antagonistic mechanisms of production-accumulation and dilution depletion
combined with an unlimited DOC supply from riparian wetland soils can mitigate the
response of stream concentrations to global changes and climatic variations.
Domains
Geochemistry
Origin : Publisher files allowed on an open archive
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