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生态学杂志 ›› 2021, Vol. 40 ›› Issue (1): 103-114.doi: : 10.13292/j.1000-4890.202101.011

• 研究报告 • 上一篇    下一篇

亚热带河口养殖塘沉积物有机碳矿化及其影响因子

谭季1,2,3,4,杨洋1,2,3,4,孙一萍1,2,3,4,黄佳芳1,2,3,4*   

  1. 1福建师范大学地理研究所, 福州 350007;2福建师范大学, 湿润亚热带生态地理过程教育部重点实验室, 福州 350007; 3福建师范大学地理科学学院, 福州 350007;4闽江河口湿地生态系统国家定位观测研究站(国家林业和草原局), 福州 350007)
  • 出版日期:2021-01-10 发布日期:2021-06-10

Organic carbon mineralization and its influencing factors in the sediments of aquaculture ponds in subtropical estuaries.

TAN Ji1,2,3,4, YANG Yang1,2,3,4, SUN Yi-ping1,2,3,4, HUANG Jia-fang1,2,3,4*#br#   

  1. (1Institute of Geographical Research, Fujian Normal University, Fuzhou 350007, China; 2Key Laboratory of Humid Subtropical Eco-geographical Process, Ministry of Education, Fujian Normal University, Fuzhou 350007, China; 3School of Geographical Sciences, FujianNormal University, Fuzhou 350007, China; 4Wetland Ecosystem Research Station of Minjiang Estuary, State Forestry and Grassland Administration, Fuzhou 350007, China).
  • Online:2021-01-10 Published:2021-06-10

摘要: 亚热带河口的养殖塘是温室气体二氧化碳(CO2)的重要排放源,但其沉积物有机碳矿化动力学特征目前尚未厘清。以我国东南沿海亚热带闽江、木兰溪以及九龙江河口区的6个凡纳滨对虾(Penaeus vannamei)养殖塘为研究对象,对沉积物取样,并进行为期60 d的室内厌氧培养,对养殖塘沉积物CO2累积产量曲线利用一阶动力学模型进行拟合和分析。结果表明:养殖塘沉积物CO2产生期主要发生在培养初期的0~2天,随后迅速降低;潜在碳矿化量(C0)为190.12~480.94 μg·g-1,矿化速率常数(k)为0.17~0.42 d-1;不同盐度养殖塘沉积物有机碳矿化存在显著性差异,表现为低盐养殖塘C0更高而k更低;孔隙水Cl-、SO42-、DOC和NH4+是影响养殖塘沉积物有机碳矿化的主要环境因子;高盐的凡纳滨对虾养殖塘Cl-、SO42-浓度高于低盐养殖塘,而DOC和NH4+浓度低于低盐养殖塘,因此高盐条件养殖凡纳滨对虾能够有效抑制沉积物的有机碳矿化。

关键词: 有机碳矿化 一阶动力学模型, 凡纳滨对虾养殖塘

Abstract: Aquaculture ponds are important sources of greenhouse gas (CO2) emissions in subtropical estuaries. However, the kinetic characteristics of organic carbon mineralization of the sediments in these aquaculture ponds have not been clarified yet. Here, we investigated the CO2 accumulation yields of the sediments collected from six Litopenaeus vannamei  aquaculture ponds in subtropical estuaries (Min River, Mulan River and Jiulong River) in southeast China, after anaerobically incubated for 60 days. The results showed that CO2 production in the sediments mainly occurred in the first two days of incubation, and then decreased rapidly. The cumulative carbon mineralization amounts (C0) ranged between 190.12-480.94 μg·g-1, while the mineralization constants (k) ranged between 0.17-0.42 d-1. There were significant differences in organic carbon mineralization of the sediments among aquaculture ponds with different salinities, with low-salinity aquaculture ponds showing higher value of C0 and lower value of k. Porewater Cl-, SO42-, DOC and NH4+ were the most important environmental factors affecting organic carbon mineralization in the sediments. Ponds with high salinity had higher concentrations of Cl- and SO42- and lower concentrations of DOC and NH4+ in porewater than low-salinity ponds. Hence, the aquaculture of L. vannameiin highsalinity ponds can effectively inhibit the mineralization of organic carbon in sediments.

Key words: organic carbon mineralization, the first-order kinetic model, Litopenaeus vannamei aquaculture pond.