Solute export patterns across the contiguous USA

被引:3
作者
Kincaid, Dustin W. [1 ,2 ,9 ]
Underwood, Kristen L. [1 ]
Hamshaw, Scott D. [1 ,3 ]
Li, Li [4 ]
Seybold, Erin C. [5 ,6 ]
Stewart, Bryn [4 ]
Rizzo, Donna M. [1 ,2 ,7 ]
Haq, Ijaz Ul [7 ]
Perdrial, Julia N. [2 ,8 ]
机构
[1] Univ Vermont, Dept Civil & Environm Engn, Burlington, VT USA
[2] Univ Vermont, Gund Inst Environm, Burlington, VT USA
[3] US Geol Survey, Reston, VA USA
[4] Penn State Univ, Dept Civil & Environm Engn, University Pk, PA USA
[5] Univ Kansas, Kansas Geol Survey, Lawrence, KS 66045 USA
[6] Univ Kansas, Dept Geol, Lawrence, KS 66047 USA
[7] Univ Vermont, Dept Comp Sci, Burlington, VT USA
[8] Univ Vermont, Dept Geog & Geosci, Burlington, VT USA
[9] US Geol Survey, Upper Midwest Water Sci Ctr, Madison, WI 20192 USA
基金
美国国家科学基金会;
关键词
Bayesian regression; CAMELS-Chem; catchment; concentration-discharge; CONUS; export; inductive; solute; CONCENTRATION-DISCHARGE RELATIONSHIPS; STREAM-WATER CHEMISTRY; DISSOLVED ORGANIC-CARBON; BIOGEOCHEMICAL RESPONSES; CATCHMENT ATTRIBUTES; POTASSIUM; SEDIMENT; RIVER; VARIABILITY; METEOROLOGY;
D O I
10.1002/hyp.15197
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Understanding 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.
引用
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页数:17
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