Targeting critical zones: A review of heterogeneity identification methods and driving mechanisms of watershed phosphorus transport

IF 5.5 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES
Journal of contaminant hydrology Pub Date : 2026-02-01 Epub Date: 2026-01-19 DOI:10.1016/j.jconhyd.2026.104857
Qingxuan Wu , Rang Wang , Jing Yang , Hao Wang , Simin Li , Xin Jin
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引用次数: 0

Abstract

Non-point source phosphorus (P) transport is characterized by pronounced heterogeneity manifested in spatial clustering, temporal intermittency, and structural coupling, which together pose critical challenges for watershed management. Based on a systematic synthesis of existing studies, this review proposes a three-dimensional identification framework of hotspots-hot moments-critical source areas (H-M-C) and refines it into the concept of high-risk heterogeneous core units to characterize functional units that are co-activated by multidimensional conditions at the event scale and dominate phosphorus flux outputs. Methodologically, we trace the evolution of approaches from threshold-based criteria, distributed modeling, stable isotopes and geochemical fingerprinting, to intelligent data-driven methods, highlighting their complementarities and limitations in dimensional coverage, mechanistic interpretation, and cross-scale applicability. Furthermore, we summarize the “activation-amplification-regulation-feedback” mechanism chain from four perspectives: hydrological disturbances, land-use practices, geomorphic regulation, and multi-source feedbacks. This review emphasizes the necessity of perceiving non-stationary processes, developing scale-adaptive identification granularity, and constructing strategy-oriented feedback loops, thereby providing a structural framework and methodological pathways to bridge the gap between mechanistic understanding of phosphorus transport and practical management responses.

Abstract Image

针对关键区域:流域磷转运异质性识别方法及驱动机制综述
非点源磷(P)输运具有明显的异质性,表现为空间聚类、时间间歇性和结构耦合,这对流域管理构成了重大挑战。本文在系统综合现有研究的基础上,提出了热点-热点时刻-关键源区(H-M-C)的三维识别框架,并将其细化为高风险异质性核心单元的概念,以表征在事件尺度上被多维条件共同激活并主导磷通量输出的功能单元。在方法上,我们追溯了从基于阈值的标准、分布式建模、稳定同位素和地球化学指纹到智能数据驱动方法的演变,强调了它们在维度覆盖、机制解释和跨尺度适用性方面的互补性和局限性。在此基础上,从水文扰动、土地利用实践、地貌调节和多源反馈四个方面总结了“激活-放大-调节-反馈”机制链。这篇综述强调了感知非平稳过程、开发规模自适应识别粒度和构建面向策略的反馈回路的必要性,从而提供了一个结构框架和方法途径,以弥合对磷运输的机制理解与实际管理响应之间的差距。
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来源期刊
Journal of contaminant hydrology
Journal of contaminant hydrology 环境科学-地球科学综合
CiteScore
6.80
自引率
2.80%
发文量
129
审稿时长
68 days
期刊介绍: The Journal of Contaminant Hydrology is an international journal publishing scientific articles pertaining to the contamination of subsurface water resources. Emphasis is placed on investigations of the physical, chemical, and biological processes influencing the behavior and fate of organic and inorganic contaminants in the unsaturated (vadose) and saturated (groundwater) zones, as well as at groundwater-surface water interfaces. The ecological impacts of contaminants transported both from and to aquifers are of interest. Articles on contamination of surface water only, without a link to groundwater, are out of the scope. Broad latitude is allowed in identifying contaminants of interest, and include legacy and emerging pollutants, nutrients, nanoparticles, pathogenic microorganisms (e.g., bacteria, viruses, protozoa), microplastics, and various constituents associated with energy production (e.g., methane, carbon dioxide, hydrogen sulfide). The journal''s scope embraces a wide range of topics including: experimental investigations of contaminant sorption, diffusion, transformation, volatilization and transport in the surface and subsurface; characterization of soil and aquifer properties only as they influence contaminant behavior; development and testing of mathematical models of contaminant behaviour; innovative techniques for restoration of contaminated sites; development of new tools or techniques for monitoring the extent of soil and groundwater contamination; transformation of contaminants in the hyporheic zone; effects of contaminants traversing the hyporheic zone on surface water and groundwater ecosystems; subsurface carbon sequestration and/or turnover; and migration of fluids associated with energy production into groundwater.
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