Nonlinear and threshold‐dominated runoff generation controls DOC export in a small peat catchment. Issue 3 (11th March 2017)

• Record Type: Journal Article
• Authors: Birkel, C.; Broder, T.; Biester, H.
• Is Part Of: Journal of geophysical research. Volume 122:Issue 3(2017)
• Page Start: 498
• Page End: 513
• Publication Date: 2017-03-11
• Subjects: DOC -- peat -- conceptual model -- parsimony -- As -- Pb; Geobiology -- Periodicals; Biogeochemistry -- Periodicals; Biotic communities -- Periodicals; Geophysics -- Periodicals; 577.14
• DOI: 10.1002/2016JG003621
• Languages: English
• ISSNs: 2169-8953

Abstract

Abstract: We used a relatively simple two‐layer, coupled hydrology‐biogeochemistry model to simultaneously simulate streamflow and stream dissolved organic carbon (DOC) concentrations in a small lead and arsenic contaminated upland peat catchment in northwestern Germany. The model procedure was informed by an initial data mining analysis, in combination with regression relationships of discharge, DOC, and element export. We assessed the internal model DOC processing based on stream DOC hysteresis patterns and 3‐hourly time step groundwater level and soil DOC data for two consecutive summer periods in 2013 and 2014. The parsimonious model (i.e., few calibrated parameters) showed the importance of nonlinear and rapid near‐surface runoff generation mechanisms that caused around 60% of simulated DOC load. The total load was high even though these pathways were only activated during storm events on average 30% of the monitoring time—as also shown by the experimental data. Overall, the drier period 2013 resulted in increased nonlinearity but exported less DOC (115 kg C ha −1 yr −1 ± 11 kg C ha −1 yr −1 ) compared to the equivalent but wetter period in 2014 (189 kg C ha −1 yr −1 ± 38 kg C ha −1 yr −1 ). The exceedance of a critical water table threshold (−10 cm) triggered a rapid near‐surface runoff response with associated higher DOC transport connecting all available DOC pools and subsequent dilution. We conclude that the combination of detailed experimental work with relatively simple, coupled hydrology‐biogeochemistry models not only allowed the model to be internally constrained but also provided important insight into how DOC and tightly coupled pollutants or trace elements are mobilized. Key Points: Nonlinear runoff generation controls DOC export Threshold‐dominated water table connects all DOC pools Pb nonlinearly and As linearly related to DOC export Plain Language Summary: Peat soils act as important carbon sinks, but they also release large amounts of dissolved organic carbon (DOC) to the aquatic system. The DOC export is strongly tied to soluble heavy metals and other pollutants, which can pose a threat to human health. However, limited knowledge exists as to how much of these substances are mobilized, how they are mobilized in terms of flow pathways, and under which hydrometeorological conditions. In this regard, models can be useful and here we present a simple, conceptual model coupling the element export to hydrology. We could identify the nonlinear and rapid nature of the runoff generation mechanisms and their overwhelming influence on DOC (>60%) and element export in our small peat catchment. Furthermore, only, if all DOC pools were connected above a certain soil water level, such rapid near‐surface flow paths developed. We concluded that simple models coupling the hydrology to biogeochemistry allowed to gain important insight into how DOC and tightly coupled heavy metals are mobilized in peat soil catchments.