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地下水对旱区湖泊水体溶解性无机碳循环影响的研究进展

陈洁 钱会 李培月 马荣 徐子博 杨雨晨

水文地质工程地质2025,Vol.52Issue(5):10-23,14.
水文地质工程地质2025,Vol.52Issue(5):10-23,14.DOI:10.16030/j.cnki.issn.1000-3665.202503035

地下水对旱区湖泊水体溶解性无机碳循环影响的研究进展

Impact of groundwater on the dissolved inorganic carbon cycle for lakes in arid regions

陈洁 1钱会 1李培月 1马荣 2徐子博 3杨雨晨3

作者信息

  • 1. 长安大学旱区地下水文与生态效应教育部重点实验室,陕西西安 710054||黄土科学全国重点实验室(长安大学),陕西西安 710054||长安大学水利与环境学院,陕西西安 710054
  • 2. 中国地质科学院水文地质环境地质研究所,河北石家庄 050061||中国地质调查局第四纪年代学与水文环境演变重点实验室,河北石家庄 050061
  • 3. 长安大学旱区地下水文与生态效应教育部重点实验室,陕西西安 710054||长安大学水利与环境学院,陕西西安 710054
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摘要

Abstract

Groundwater serves as a crucial source of replenishment for lakes in arid regions.It not only acts as an important link in maintaining the ecological health of these lakes,but also plays a vital role in the terrestrial ecosystem carbon cycle.The unique aquatic environment and hydro-ecological patterns of arid lakes make dissolved inorganic carbon(DIC)a key component in the lake carbon cycle.Dissolved CO2 and HCO3-,the main forms of DIC,are the primary sources for photosynthesis and organic matter production.Phytoplankton absorb DIC to synthesize organic carbon,part of which is oxidized and decomposed by microorganisms,while the rest settles and is buried in the sediment,rendering the lake a"sink"for CO2.However,the formation of calcium carbonate precipitates from Ca2+and HCO3-can increase the partial pressure of CO2 in the lake water,causing the lake to act as a"source"of CO2.This study reviews the critical role of groundwater in the hydrological balance,carbon balance,and ecological balance of arid region lake systems.It identifies the characteristics of DIC in arid regions such as lake water.It elucidates how groundwater affects lake DIC through water cycling,hydrogeochemical interactions,and nutrient input.The applicability of monitoring technologies,carbon isotope techniques,and model simulations in studying lake DIC is also summarized and compared.Finally,future research directions for the DIC cycle in arid region lakes are proposed,focusing on the mechanisms of hydrological and biogeochemical processes influencing lake DIC,the carbon cycle characteristics of artificially replenished lakes,and the effects of lake carbon cycling and adaptive management strategies.

关键词

地表水-地下水相互作用/旱区湖泊/溶解性无机碳/生态环境/碳循环

Key words

surface water-groundwater interaction/lakes in arid regions/DIC/ecological environment/carbon cycle

分类

天文与地球科学

引用本文复制引用

陈洁,钱会,李培月,马荣,徐子博,杨雨晨..地下水对旱区湖泊水体溶解性无机碳循环影响的研究进展[J].水文地质工程地质,2025,52(5):10-23,14.

基金项目

国家自然科学基金项目(42272289 ()

42007184 ()

42341102) ()

中央高校基本科研业务费项目(300102294906 ()

300102294902) ()

水文地质工程地质

OA北大核心

1000-3665

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