Characterizing seasonal variability of storm events based on very high frequency monitoring of hydrological and chemical variables: comparing patterns in hot spots and hot moments for nutrient and sediment export
Abstract
Storm events are critical hot moments of emission for several dissolved and particulate chemical species at major
stake for water quality (e.g. dissolved organic carbon DOC, suspended sediments, phosphorus). During such
events, the solutes or particles are exported from heterogeneous sources through various pathways to stream leading
to specific integrated signals at the outlet characterized by very short dynamics. This is merely true in headwater
catchments where the total duration of such events ranges over 10h to 3 days, with very quick variations in stream
flow and concentrations at the outlet occurring in a few hours. Thus for investigating properly event processes,
high frequency monitoring of flow and water quality is required.We analysed 103 storm events in a 5 km2 agricultural
headwater catchment, part of the AgrHys Observatory, on the basis of a 3-year-long data set which combined
meterological (Rainfall), hydrological (flow and piezometry), and water quality (turbidity, conductivity, DOC and
NO3 concentrations) data recorded at very high frequencies (from 1 to 20 min) thanks to dedicated sensors. We
proposed a range of quantitative storm descriptors for characterizing input (rainfall), antecedent and initial conditions
(groundwater levels and saturated area), and stream response in terms of level and dynamics of flow (Q),
groundwater levels, and concentrations (C) but also the C-Q relationships. Three intra annual periods have been
previously defined for base flow dynamic according to shallow groundwater table variations so that they correspond
to different connectivity status in the catchment. The seasonal and inter-annual variability of the storm events have
been analysed using the descriptors and based on these predefined periods. Results show that the hydrological
flowpaths and the consequent storm chemistry were controlled by the hydrological base flow regime rather than
by the rain input characteristics. This highlights that the exports of NO3, DOC and sediments during storms may
be either synchronized or desynchronized depending on the season. This temporal dynamic of the ratios between
species may be at major stake for the aquatic ecosystems response and structure.