Solute export patterns across the contiguous USA

Author:

Kincaid Dustin W.12,Underwood Kristen L.1,Hamshaw Scott D.13,Li Li4,Seybold Erin C.56,Stewart Bryn4,Rizzo Donna M.127,Haq Ijaz Ul7,Perdrial Julia N.28

Affiliation:

1. Department of Civil & Environmental Engineering University of Vermont Burlington Vermont USA

2. Gund Institute for Environment University of Vermont Burlington Vermont USA

3. U.S. Geological Survey Reston, Virginia USA

4. Department of Civil & Environmental Engineering The Pennsylvania State University University Park Pennsylvania USA

5. Kansas Geological Survey University of Kansas Lawrence Kansas USA

6. Department of Geology University of Kansas Lawrence Kansas USA

7. Department of Computer Science University of Vermont Burlington Vermont USA

8. Department of Geography and Geoscience University of Vermont Burlington Vermont USA

Abstract

AbstractUnderstanding controls on solute export to streams is challenging because heterogeneous catchments can respond uniquely to drivers of environmental change. To understand general solute export patterns, we used a large‐scale inductive approach to evaluate concentration–discharge (C–Q) metrics across catchments spanning a broad range of catchment attributes and hydroclimatic drivers. We leveraged paired C–Q data for 11 solutes from CAMELS‐Chem, a database built upon an existing dataset of catchment and hydroclimatic attributes from relatively undisturbed catchments across the contiguous USA. Because C–Q relationships with Q thresholds reflect a shift in solute export dynamics and are poorly characterized across solutes and diverse catchments, we analysed C–Q relationships using Bayesian segmented regression to quantify Q thresholds in the C–Q relationship. Threshold responses were rare, representing only 12% of C–Q relationships, 56% of which occurred for solutes predominantly sourced from bedrock. Further, solutes were dominated by one or two C–Q patterns that reflected vertical solute–source distributions. Specifically, solutes predominantly sourced from bedrock had diluting C–Q responses in 43%–70% of catchments, and solutes predominantly sourced from soils had more enrichment responses in 35%–51% of catchments. We also linked C–Q relationships to catchment and hydroclimatic attributes to understand controls on export patterns. The relationships were generally weak despite the diversity of solutes and attribute types considered. However, catchment and hydroclimatic attributes in the central USA typically drove the most divergent export behaviour for solutes. Further, we illustrate how our inductive approach generated new hypotheses that can be tested at discrete, representative catchments using deductive approaches to better understand the processes underlying solute export patterns. Finally, given these long‐term C–Q relationships are from minimally disturbed catchments, our findings can be used as benchmarks for change in more disturbed catchments.

Publisher

Wiley

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