| 引用本文: | 汪宇菲,张云鹏,金苗,张荣飞,韩超.水环境中无机还原态磷的研究进展与展望.湖泊科学,2024,36(6):1626-1638. DOI:10.18307/2024.0602 |
| Wang Yufei,Zhang Yunpeng,Jin Miao,Zhang Rongfei,Han Chao.The research progress and prospects of inorganic reduced phosphorus in aquatic environments. J. Lake Sci.2024,36(6):1626-1638. DOI:10.18307/2024.0602 |
|
| 本文已被：浏览 828次 下载 1465次 |
码上扫一扫！ |
|
|
| 水环境中无机还原态磷的研究进展与展望 |
|
汪宇菲1,2, 张云鹏2,3, 金苗2, 张荣飞1, 韩超2,3
|
|
1.湖州师范学院生命科学学院, 湖州 313000;2.中国科学院南京地理与湖泊研究所, 湖泊与环境国家重点实验室, 南京 210008;3.中国科学院大学, 北京 100049
|
|
| 摘要: |
| 磷(P)的生物地球化学循环是整个生物圈物质能量循环的重要组成部分,在水环境质量变化和生命演替过程中起着决定性作用。传统理论普遍认为磷循环是以+Ⅴ价态的磷酸盐(P+Ⅴ)为主导的沉积型循环,忽略了磷化氢(P-Ⅲ)、次磷酸盐(P+Ⅰ)和亚磷酸盐(P+Ⅲ)等价态低于+Ⅴ的无机还原态磷(IRP, inorganic reduced phosphorus)形态,致使当前对水体P循环的认识存在明显的“缺失”。本综述在目前获得的新研究和新发现的背景下,对水环境中IRP的赋存形态、来源和组成、检测方法、时空分布、迁移转化、环境行为与效应等方面的研究现状进行阐述并对IRP的发展态势进行展望,以期丰富和完善湖泊磷循环理论并提供关键信息,推动对磷循环相关研究的发展,为湖泊水环境保护和治理提供参考。 |
| 关键词: 无机还原态磷 产生机制 分布特征 迁移转化 环境效应 |
| DOI：10.18307/2024.0602 |
| 分类号: |
| 基金项目:国家重点研发计划项目(2023YFE0100500)、鄱阳湖环境与资源利用教育部重点实验室开放课题(2022Y02)和国家自然科学基金项目(42077360,42277463)联合资助。 |
|
| The research progress and prospects of inorganic reduced phosphorus in aquatic environments |
|
Wang Yufei1,2, Zhang Yunpeng2,3, Jin Miao2, Zhang Rongfei1, Han Chao2,3
|
|
1.School of Life Science, Huzhou University, Huzhou 313000, P. R. China;2.State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, P. R. China;3.University of Chinese Academy of Sciences, Beijing 100049, P. R. China
|
| Abstract: |
| The biogeochemical cycling of phosphorus(P) plays a pivotal role in the material-energy cycle of the biosphere, profoundly influencing the quality of water environments and the process of life succession. While traditional theories often consider the phosphorus cycle to be primarily sedimentary, with orthophosphate(P+Ⅴ) as the primary driver, this neglects the presence of inorganic reduced phosphorus(IRP) forms such as phosphine(P-Ⅲ), hypophosphite(P+Ⅰ), and phosphite(P+Ⅲ), which have lower valences than +Ⅴ. This oversight results in a significant knowledge gap in our understanding of P cycling in water bodies. The aim of this paper is to summarize our current understanding of IRP's sources, compositions, detection methods, spatial and temporal distribution, transport and transformation processes, as well as its bioavailability. It is expected to enrich and improve the lake phosphorus cycle theory to provide key information and a scientific basis for lake water environmental protection and management. |
| Key words: Inorganic reduced phosphorus generation mechanism distribution features migration and transformation ecological environment effect |
