地质富磷流域水体中磷的迁移规律研究——以黄麦岭矿区为例
Phosphorus Migration in Water Bodies of a Geologically Phosphorus-Enriched Watershed—A Case Study of the Huangmailing Mine
摘要: 本研究以黄麦岭矿区所在的澴河流域为对象，通过在流域内合理布设21个采样点，对水体主要离子、总磷、微量元素、进行系统分析，并运用相关性分析，探究该流域内磷迁移的规律。主要结论如下：通过相关性分析得到P与Mn、ORP显著正相关，中游P还与pH呈强负相关，反映地质作用、氧化还原环境及酸碱条件对磷迁移起主导作用；研究揭示了澴河流域磷迁移受地质背景、人类活动及环境因子共同驱动，为矿区水体污染防治提供了科学依据。
Abstract: This study focuses on the Huan River Basin, where the Huangmailing phosphate mining area is located. Twenty-one sampling sites were strategically established throughout the basin to systematically analyze major ions, total phosphorus (TP), and trace elements in the water. Correlation analysis was employed to investigate the migration behavior of phosphorus within the basin. The main conclusions are as follows: Phosphorus (P) shows a significant positive correlation with Mn and ORP, and in the middle reaches, P is strongly negatively correlated with pH, indicating that geological processes, redox conditions, and acidity-alkalinity jointly play dominant roles in controlling phosphorus migration. The study reveals that phosphorus migration in the Huan River Basin is jointly driven by geological background, human activities, and environmental factors, providing a scientific basis for water pollution prevention and control in mining areas.
文章引用：廖杨. 地质富磷流域水体中磷的迁移规律研究——以黄麦岭矿区为例[J]. 环境保护前沿, 2025, 15(11): 1570-1578. https://doi.org/10.12677/aep.2025.1511171

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