生态与农村环境学报 ›› 2021, Vol. 37 ›› Issue (7): 909-916.doi: 10.19741/j.issn.1673-4831.2020.0779

• 自然保护与生态 • 上一篇    下一篇

广西红树林净生态系统碳交换变化特征及影响因子研究

孙明1,2, 莫伟华2, 谢敏3, 陈燕丽2, 潘良浩1   

  1. 1. 广西科学院广西红树林研究中心/广西红树林保护与利用重点实验室, 广西 北海 536000;
    2. 广西壮族自治区气象科学研究所, 广西 南宁 530022;
    3. 广西壮族自治区气候中心, 广西 南宁 530022
  • 收稿日期:2020-09-16 出版日期:2021-07-25 发布日期:2021-07-23
  • 通讯作者: 莫伟华 E-mail:47562933@qq.com
  • 作者简介:孙明(1986-),男,江苏靖江人,高级工程师,硕士,主要从事生态遥感应用研究。E-mail:517073708@qq.com
  • 基金资助:
    广西红树林保护与利用重点实验室开放基金(GKLMC-201804);中国气象局气候变化专项(CCSF202030);广西区气象局气象科研计划(桂气科2019M02);广西台风与海洋预报服务创新团队

Characteristics of Net Ecosystem Carbon Exchange and Its Influence Factors over the Mangrove in Guangxi

SUN Ming1,2, MO Wei-hua2, XIE Min3, CHEN Yan-li2, PAN Liang-hao1   

  1. 1. Guangxi Mangrove Research Center, Guangxi Academy of Sciences/Guangxi Key Laboratory of Mangrove Conservation and Utilization, Beihai 536000, China;
    2. Guangxi Zhuang Autonomous Region Meteorological Sciences Institute, Nanning 530022, China;
    3. Climate Center of Guangxi Zhuang Autonomous Region, Nanning 530022, China
  • Received:2020-09-16 Online:2021-07-25 Published:2021-07-23

摘要: 为了研究广西红树林CO2通量变化特征及其调控机制,利用2019年北海红树林生态观测试验站涡度相关系统观测的红树林碳通量和气象观测数据,分析红树林净生态系统碳交换变化特征及其与气象因子的响应关系。结果表明,广西红树林净生态系统碳交换的平均日变化曲线呈"U"型分布;在月尺度上,碳汇峰值出现在2月,最小值出现在6月;在季尺度上,不同季节碳汇峰值呈秋季 > 春季 > 冬季 > 夏季的趋势;净生态系统碳交换月累积最大值为11月(-45.23 g·m-2·月-1),最小值为7月(-16.95 g·m-2·月-1);广西红树林净生态系统碳交换、总呼吸和总初级生产力年累积量分别为-386.68、862.49和-1 249.18 g·m-2·a-1,3者均低于福建和广东红树林;光合有效辐射是对净生态系统碳交换产生直接影响的主导因子,饱和水气压差是对净生态系统碳交换产生间接影响的主导因子,降水量是净生态系统碳交换的限制因子。

关键词: 广西, 红树林, 涡度相关系统, 净生态系统碳交换, 影响因子

Abstract: In order to explore the dynamics of CO2 flux exchange and its regulating mechanism of mangrove in Guangxi, the CO2 flux data and the meteorological data of sandy mangrove recorded by the eddy covariance system at the mangrove ecological observation and experiment station in Beihai in 2019 were utilized to analyze the dynamics of net ecosystem carbon exchange (NEE) and its response to meteorological factors. The results suggest that the diurnal variation of NEE on average followed a U-shape pattern in Guangxi. The carbon sink reached the maximum in February and the minimum in June on the monthly scale. On the seasonal scale, the maximum NEE occurred in autumn, followed by spring, winter, and summer. The cumulative monthly NEE reached the maximum of -45.23 g·m-2·mon-1 in November and the minimum of -16.95 g·m-2·mon-1 in July. The total amount of NEE, ecosystem respiration, and gross primary productivity (GPP) were -386.68, 862.49, and -1 249.18 g·m-2·a-1, respectively, which were lower than that in the mixed mangrove in Fujian and Guangdong. The dominant factor of direct influence on the net ecosystem exchange was the photosynthetically active radiation, and that of indirect influence was vapor pressure deficit. Precipitation was the limiting factor of net ecosystem exchange.

Key words: Guangxi, mangrove, eddy covariance system, net ecosystem exchange, influencing factor

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