综述与评述

内陆水体初级生产力评估方法研究进展

  • 陆瑶 ,
  • 黄良波 ,
  • 贾珺杰 ,
  • 高扬
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  • 1.中国科学院地理科学与资源研究所,生态网络观测与模拟重点实验室,北京 100101
    2.中国科学院大学资源与环境学院,北京 100049
    3.中国市政工程 中南设计研究总院有限公司,湖北 武汉 430001
陆瑶(1995-),女,山西阳泉人,博士研究生,主要从事内陆水体碳循环与生产力研究. E-mail: luy.18s@igsnrr.ac.cn
高扬(1981-),男,福建长乐人,研究员,主要从事内陆水体碳循环与生产力研究. E-mail: gaoyang@igsnrr.ac.cn

收稿日期: 2021-11-09

  修回日期: 2022-05-16

  网络出版日期: 2023-02-02

基金资助

国家自然科学基金杰出青年科学基金项目“流域碳氮耦合循环及其生态效应”(42225103)

Estimation of Primary Productivity of Inland Water

  • Yao LU ,
  • Liangbo HUANG ,
  • Junjie JIA ,
  • Yang GAO
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  • 1.Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
    2.College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China
    3.Central China Municipal Engineering Design Research Institute Co. , Ltd. , Wuhan 430001, China
LU Yao (1995-), female, Yangquan City, Shanxi Province, Ph. D student. Research area includes inland water productivity and carbon cycle. E-mail: luy.18s@igsnrr.ac.cn
GAO Yang (1981-), male, Changle City, Fujian Province, Professor. Research area includes biogeochemical cycle. E-mail: gaoyang@igsnrr.ac.cn

Received date: 2021-11-09

  Revised date: 2022-05-16

  Online published: 2023-02-02

Supported by

the National Science Foundation for Distinguished Young Scholars of China “Coupling cycle of carbon and nitrogen in watershed and its ecological effects”(42225103)

摘要

内陆水体是全球碳循环的重要参与者,在调节气候变化方面发挥着关键作用。内陆水体初级生产力指内陆水体(包括湖泊、水库、河流和湿地)中初级生产者(包括浮游藻类植物和挺水、浮水、潜水大型植物)单位时间、单位面积上由光合作用产生的有机物质总量,其大小反映了系统有机碳库和无机碳库之间的定量联系。评估内陆水体初级生产力不仅能帮助解析初级生产者光合作用碳固存机理,也有助于量化内陆水体碳吸收量,进而探知不同区域生态环境差异,揭示内陆水体在全球生态系统碳循环中的重要性。内陆水体初级生产力估算方法较多,包括黑白瓶法、垂向归纳模型法和13C法等,各方法都有其适用范围和局限性,对这些方法的不合理使用制约着对内陆水体初级生产力的变异性及其驱动机制的揭示。通过归纳整理近年来国内外内陆水体初级生产力估算方法,对各个方法的机理、优缺点和适用性进行对比和总结,并着重介绍2种新兴的基于溶解氧浓度或氧同位素的方法(即diel O2技术和18/16O技术),进而为深入开展内陆水体新陈代谢、生产力及养分循环方面研究提供重要技术支撑。

本文引用格式

陆瑶 , 黄良波 , 贾珺杰 , 高扬 . 内陆水体初级生产力评估方法研究进展[J]. 地球科学进展, 2023 , 38(1) : 57 -69 . DOI: 10.11867/j.issn.1001-8166.2022.055

Abstract

Inland water is an important component of the global carbon (C) cycle and plays a key role in regulating climate change. The Primary Productivity (PP) of inland water is defined as the amount of organic matter produced by primary producers in inland water bodies through photosynthesis per unit time and unit area, which reflects the quantitative relationship between the organic and inorganic C pools. The assessment of inland water PP can help analyze the C cycle mechanism of photosynthesis and quantify the C absorption of aquatic ecosystems to examine the differences in the ecological environment in different regions and evaluate the importance of inland water bodies in the global ecosystem C cycle. There are many methods for estimating PP in inland water, including the light-dark bottle incubation method, the vertically generalized production model method, and the 13C method. Each of these have application scopes and limitations. The unreasonable use of PP restricts the understanding of its variability and driving mechanism in inland water bodies. The mechanism, advantages, disadvantages, and applicability of each method are compared by summarizing domestic and international research on PP estimation methods in recent years. Two new methods based on dissolved oxygen concentration or oxygen isotopes, namely, diel O2 technology and 18/16O technology, are introduced. This study serves as a reference for research on inland water metabolism, productivity, and nutrient cycles.

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