Small-scale topography explains patterns and dynamics of dissolved organic carbon exports from the riparian zone of a temperate, forested catchment

Export of dissolved organic carbon (DOC) from riparian zones (RZs) is an important component of temperate catchment carbon budgets, but export mechanisms are still poorly understood. Here we show that DOC export is predominantly controlled by the microtopography of the RZ (lateral variability) and by riparian groundwater level dynamics (temporal variability). From February 2017 until July 2019 we studied topography, DOC quality and water fluxes and pathways in the RZ of a small forested catchment and the receiving stream in central Germany. The chemical classification of the riparian groundwater and surface water samples (n=66) by Fourier transform ion cyclotron resonance mass spectrometry revealed a cluster of plant-derived, aromatic and oxygen-rich DOC with high concentrations (DOCI) and a cluster of microbially processed, saturated and heteroatom-enriched DOC with lower concentrations (DOCII). The two DOC clusters were connected to locations with distinctly different values of the high-resolution topographic wetness index (TWIHR; at 1 m resolution) within the study area. Numerical water flow modeling using the integrated surface–subsurface model HydroGeoSphere revealed that surface runoff from high-TWIHR zones associated with the DOCI cluster (DOCI source zones) dominated overall discharge generation and therefore DOC export. Although corresponding to only 15 % of the area in the studied RZ, the DOCI source zones contributed 1.5 times the DOC export of the remaining 85 % of the area associated with DOCII source zones. Accordingly, DOC quality in stream water sampled under five event flow conditions (n=73) was closely reflecting the DOCI quality. Our results suggest that DOC export by surface runoff along dynamically evolving surface flow networks can play a dominant role for DOC exports from RZs with overall low topographic relief and should consequently be considered in catchment-scale DOC export models. We propose that proxies of spatial heterogeneity such as the TWIHR can help to delineate the most active source zones and provide a mechanistic basis for improved model conceptualization of DOC exports.

Patterns and dynamics of dissolved organic carbon exports from a riparian zone of a temperate, forested catchment

Export of dissolved organic carbon (DOC) from riparian zones (RZs) is an important, but poorly understood component of temperate catchment carbon budgets. This paper delineates explicit DOC source zones within the RZ of a small forested catchment in central Germany, and identifies and quantifies their dominant DOC export mechanism at high spatio-temporal resolution. Stream water DOC samples from differing hydrological situations were compared to riparian DOC groundwater and surface water samples and classified chemically (via Fourier-transform ion cyclotron resonance mass spectrometry) and spatially via a small-scale topographic analysis of the RZ at a resolution of 1 m. Explicit water fluxes from the resulting riparian DOC source zones were then simulated by a physically-based, fully-integrated numerical flow model (HydroGeoSphere). Chemical classification revealed two distinct DOC pools (DOCI and DOCII) in the RZ. The comparison of stream and riparian water samples indicated a predominant export of DOCI during wet conditions and high groundwater levels. The two DOC pools were spatially separated and mapped using a threshold value in high-resolution topographical wetness index (TWIHR). Hydrological modelling revealed that surface runoff from DOCI source zones with high TWIHR values dominated overall discharge generation and therefore DOC export. Although corresponding to only 15 % of the area in the studied RZ, the high TWIHR zones provided in total 1.5 times the load of DOC from the remaining 85 % of the area associated with the DOCII pool. Our results suggest that surface DOC export can play a dominant role for DOC export in RZs with overall low topographic relief and should be considered in DOC export models. We propose that proxies of spatial heterogeneity (here: TWIHR) can delineate the most active riparian source zones and provide a meaningful basis for improved model conceptualization of surficial DOC export.

Uranium Vertical and Lateral Distribution in a German Forested Catchment

The natural measurements of uranium (U) are important for establishing natural baseline levels of U in soil. The relations between U and other elements are important to determine the extent of geological origin of soil U. The present study was aimed at providing a three-dimensional view of soil U distribution in a forested catchment (ca. 38.5 ha) in western Germany. The evaluated data, containing 155 sampled points, each with four major soil horizons (L/Of, Oh, A, and B), were collected from two existing datasets. The vertical U distribution, the lateral pattern of U in the catchment, and the occurrence of correlations between U and three groups of elements (nutrient elements, heavy metals, and rare earth elements) were examined. The results showed the median U concentration increased sevenfold from the top horizon L/Of (0.14 mg kg−1) to the B horizon (1.01 mg kg−1), suggesting a geogenic origin of soil U. Overall, soil U concentration was found to be negatively correlated with some plant macronutrients (C, N, K, S, Ca) but positively with others (P, Mg, Cu, Zn, Fe, Mn, Mo). The negative correlations between U and some macronutrients indicated a limited accumulation of plant-derived U in soil, possibly due to low phytoavailability of U. Positive correlations were also found between U concentration and heavy metals (Cr, Co, Ni, Ga, As, Cd, Hg, Pb) or rare earth elements, which further pointed to a geogenic origin of soil U in this forested catchment.