Abstract

AbstractThe analysis of concentration‐discharge (C‐Q) relationships from low‐frequency observations is commonly used to assess solute sources, mobilization, and reactive transport processes at the catchment scale. High‐frequency concentration measurements are increasingly available and offer additional insights into event‐scale export dynamics. However, only few studies have integrated inter‐annual and event‐scale C‐Q relationships. Here, we analyze high‐frequency measurements of specific conductance (EC), nitrate (NO3‐N) concentrations and spectral absorbance at 254 nm (SAC254, as a proxy for dissolved organic carbon) over a two year period for four neighboring catchments in Germany ranging from more pristine forested to agriculturally managed settings. We apply an integrated method that adds a hysteresis term to the established power law C‐Q model so that concentration intercept, C‐Q slope and hysteresis can be characterized simultaneously. We found that inter‐event variability in C‐Q hysteresis and slope were most pronounced for SAC254 in all catchments and for NO3‐N in forested catchments. SAC254 and NO3‐N event responses in the smallest forested catchment were closely coupled and explainable by antecedent conditions that hint to a common near‐stream source. In contrast, the event‐scale C‐Q patterns of EC in all catchments and of NO3‐N in the agricultural catchment without buffer zones around streams were less variable and similar to the inter‐annual C‐Q relationship indicating a homogeneity of mobilization processes over time. Event‐scale C‐Q analysis thus added key insights into catchment functioning whenever the inter‐annual C‐Q relationship contrasted with event‐scale responses. Analyzing long‐term and event‐scale behavior in one coherent framework helps to disentangle these scattered C‐Q patterns.

Highlights

  • Anthropogenic activities such as intensive agriculture and waste water discharge deteriorate the quality of water resources

  • We found that inter-event variability in C-Q hysteresis and slope were most pronounced for SAC254 in all catchments and for NO3-N in forested catchments

  • We focus on specific conductance representing geogenic solutes, and the biogeochemically reactive solutes dissolved organic carbon being of biogenic origin and nitrate being of anthropogenic origin

Read more

Summary

Introduction

Anthropogenic activities such as intensive agriculture and waste water discharge deteriorate the quality of water resources. Anthropogenic sources increase the aquatic concentration and fluxes of nutrients like nitrogen, phosphorus and organic carbon, leading to eutrophication in rivers, lakes and coastal waters (Carpenter et al, 2011; Schlesinger, 2009). This can pose a threat to water security and downstream aquatic ecosystem health and functioning (Foley et al, 2005). Reactive transport at the catchment scale, is complex and tends to span a large range of spatial and temporal scales (Gall et al, 2013; Kirchner, 2003; Sivapalan, 2006) This often hinders establishing a unique cause-effect relationship

Objectives
Methods
Results
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call