Solute export patterns across the contiguous USA

IF 3.2 3区 地球科学 Q1 Environmental Science Hydrological Processes Pub Date : 2024-06-17 DOI:10.1002/hyp.15197
Dustin W. Kincaid, Kristen L. Underwood, Scott D. Hamshaw, Li Li, Erin C. Seybold, Bryn Stewart, Donna M. Rizzo, Ijaz Ul Haq, Julia N. Perdrial
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Abstract

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.

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美国毗连地区的溶质输出模式
了解对溪流溶质输出的控制具有挑战性,因为不同的集水区会对环境变化的驱动因素做出独特的反应。为了了解一般的溶质输出模式,我们采用了大规模的归纳法来评估不同集水区的浓度-排水量(C-Q)指标,这些集水区跨越了广泛的集水属性和水文气候驱动因素。我们利用了 CAMELS-Chem 中 11 种溶质的配对 C-Q 数据,该数据库建立在现有的集水区和水文气候属性数据集的基础上,数据来源于美国毗连地区相对未受干扰的集水区。由于具有 Q 值阈值的 C-Q 关系反映了溶质输出动态的变化,而且在不同溶质和不同集水区之间的特征并不明显,因此我们使用贝叶斯分段回归法分析了 C-Q 关系,以量化 C-Q 关系中的 Q 值阈值。阈值反应非常罕见,仅占 C-Q 关系的 12%,其中 56%发生在主要来自基岩的溶质上。此外,溶质主要以一种或两种 C-Q 模式为主,这些模式反映了溶质来源的垂直分布。具体来说,主要来源于基岩的溶质在 43%-70% 的集水区具有稀释的 C-Q 反应,而主要来源于土壤的溶质在 35%-51% 的集水区具有更多的富集反应。我们还将 C-Q 关系与流域和水文气候属性联系起来,以了解对输出模式的控制。尽管考虑的溶质和属性类型多种多样,但它们之间的关系普遍较弱。然而,美国中部的集水区和水文气候属性通常会导致溶质出口行为的最大差异。此外,我们还说明了归纳法如何产生新的假设,这些假设可以通过演绎法在离散的、有代表性的集水区进行测试,从而更好地了解溶质输出模式的基本过程。最后,鉴于这些长期的 C-Q 关系来自于干扰最小的集水区,我们的研究结果可以作为基准,用于衡量干扰更大的集水区的变化。
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来源期刊
Hydrological Processes
Hydrological Processes 环境科学-水资源
CiteScore
6.00
自引率
12.50%
发文量
313
审稿时长
2-4 weeks
期刊介绍: Hydrological Processes is an international journal that publishes original scientific papers advancing understanding of the mechanisms underlying the movement and storage of water in the environment, and the interaction of water with geological, biogeochemical, atmospheric and ecological systems. Not all papers related to water resources are appropriate for submission to this journal; rather we seek papers that clearly articulate the role(s) of hydrological processes.
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