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湖北省2019-2021年岩溶碳汇估算及其驱动因子分析OA北大核心CSTPCD

Estimation of karst carbon sinks and analysis of their driving factors in Hubei Province from 2019 to 2021

中文摘要英文摘要

碳酸盐岩在水循环过程中的碳汇效应显著,加之岩溶地貌在我国分布广泛,所以探求岩溶碳汇潜力的研究对制定区域增汇策略具有重要意义.选取位于西南岩溶区的湖北省为重点研究区域,基于水化学径流法及入渗-平衡化学法进行定量化计算和比较,利用ArcGIS空间分析技术整体评估湖北省2019-2021年岩溶碳汇的空间格局与量级,探索更适宜应用于区域尺度的岩溶作用碳汇估算方法,综合分析岩溶碳汇的驱动因子,发掘更大的增汇潜力.研究结果表明:(1)采用入渗-平衡化学法估算3 a碳汇强度大小为2020年>2019年>2021年,丰水年(2020年)岩溶碳汇总量约为枯水年(2019年)的6倍,3 a年均碳汇强度为12.84 t/(km2·a),碳汇总量达163.89×104t/a;(2)相较于水化学径流法,入渗-平衡化学法计算结果更为准确,获取数据资料较为简单,大小空间尺度都具有一定的普适性;(3)碳汇作用变化是高度动态的,气候变化下变化幅度主要由径流深决定,碳汇强度随径流深增大而变强,土地利用类型调控着岩溶作用碳汇强度;(4)鄂西南地区岩溶作用强烈,可建立岩溶碳汇试验区,定量评估人工干预所带来的增汇效果.研究结果不仅提供了精确易行的岩溶碳汇估算方法,而且确定了湖北省岩溶碳汇的量级与空间格局,摸清了碳汇强度驱动因子的共同耦合作用,体现了岩溶碳汇的人为可调控性以及复杂性,进一步为环境保护政策、人工增汇措施的制定提供了可靠的科学依据.

[Objective]Carbonate rocks have a significant carbon sink effect in water cycle.Since karst landforms are widely distributed in China,research on the potential of karst carbon sinks plays an important role in formula-ting regional strategies for increasing carbon sinks.[Methods]In this study,groundwater monitoring points in Hu-bei Province,which is located in the karst area of Southwest China,were selected.Quantitative calculations and method comparisons were performed based on the hydrochemical runoff method and the infiltration-equilibrium chemistry method.The spatial pattern and magnitude of karst carbon sinks in the hilly mountains of Hubei Province from 2019 to 2021 were evaluated via ArcGIS spatial analysis techniques.Additionally,the most suitable method for estimating karst carbon sinks at the regional scale were explored,the comprehensive analysis of the drivers of karst carbon sinks was performed,and the potential for increasing sinks were explored.[Results]The results showed that:(1)the intensity of carbon sinks estimated by the infiltration-equilibrium chemistry method were 2020>2019>2021.The total amount of karst carbon sinks in wet year(2020)was approximately 6 times of that in dry year(2019).The average annual carbon sink intensity in the three years was 12.84 t/(km2·a)and the annual total amount of carbon reached 163.89x 104 t/a;(2)the infiltration-equilibrium chemistry method was more accu-rate in calculation results and simpler in data acquisition than the hydrochemical runoff method,and had a certain universality at both large and small spatial scales;(3)the change in carbon sinks was highly dynamic.The extent of changes in carbon sinks under climate change was mainly determined by runoff depth,with the intensity of car-bon sinks increasing with runoff depth,while land use regulated the intensity of carbon sinks in karst processes;and(4)the karstification is strong in southwestern Hubei Province,so a pilot field of karst carbon sinks could be established within the area to quantitatively evaluate artificial interventions to increase carbon sinks.[Conclusion]This study not only provides an accurate and easy-to-use method for estimating karst carbon sinks,but also deter-mines the magnitude and spatial pattern of karst carbon sinks in Hubei Province and figures out the coupling effect of the driving factors of carbon sink intensity,which demonstrates the complexity and anthropogenic control lability of karst carbon sinks.The results of this study provides a reliable scientific basis for the formulation of environmen-tal protection policies and artificial sink increase measures.

王懿洁;马传明;郭静;党慧慧;黄鹏;范威

中国地质大学(武汉)环境学院,武汉 430078湖北省地质局资源与生态环境地质湖北省重点实验室,武汉 430034||湖北省地质局湖北省地质环境总站,武汉 430034

地质学

岩溶碳汇水化学径流法入渗-平衡化学法ArcGIS空间分析驱动因子湖北省

karst carbon sinkmethod of solute loadmethod of infiltration-equilibrium chemistryArcGIS spatial analysisdriving factorHubei Province

《地质科技通报》 2024 (002)

330-343 / 14

湖北省地质局项目"湖北地下水-土壤生态环境调查、监测与修复研究"(KJ2022-13);湖北省地质局科技项目

10.19509/j.cnki.dzkq.tb20220534

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