首页|黄、渤海沉积物耗氧速率的时空分布特征和环境影响因素

黄、渤海沉积物耗氧速率的时空分布特征和环境影响因素

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沉积物耗氧(SOC)是海洋沉积物重要参数,是海底沉积物有机质矿化速率的重要表征参数,开展沉积物耗氧的研究有助于了解整个海洋的碳循环过程.陆架边缘海作为有机质矿化和埋藏最重要和最活跃的场所之一,在全世界已经受到广泛关注与研究,但是对于具有海洋环境典型季节变化的中国边缘海区域,尤其是黄、渤海仍然缺乏相应的关注.本文使用整柱培养法,分别于2022年4月、7月和10月对黄、渤海沉积物耗氧进行研究,结果表明黄、渤海沉积物耗氧速率为7.11~17.33 mmol/(m2 d).黄海春季沉积物耗氧速率与渤海无显著差异(ANOVA,p>0.05),夏季(ANOVA,p<0.01)和秋季(ANOVA,p<0.01)黄海沉积物耗氧速率低于渤海;黄海春季沉积物耗氧速率最高,秋季次之,夏季最小,渤海夏季和秋季接近,显著高于春季(ANOVA,p<0.05),温度和沉积物Ch1a浓度是主要影响因素.同时,用沉积物耗氧速率来评估海底有机质矿化速率,并与初级生产力相比较,结果表明渤海海底有机质矿化与初级生产力的占比范围为42.8%~74.5%,是渤海碳循环的关键环节之一,黄海海底沉积物有机质矿化在黄海碳循环中作用不如渤海显著.本文系统研究了黄、渤海沉积物耗氧速率及其时空分布特征,探究了黄、渤海地区有机质矿化对初级生产力的贡献,为理解黄、渤海区域有机质矿化和埋藏提供理论支持.
Characteristics of spatial and temporal distribution of sediment oxygen consumption rate and environmental influence factors in the Yellow Sea and Bohai Sea
Sediment oxygen consumption(SOC)is an important parameter of marine sediments and an important characterization parameter of the rate of organic carbon mineralization in seafloor sediments,and the study of SOC can help us to understand the carbon cycling process in the whole ocean.As one of the most important and active sites for organic carbon mineralization and burial,marginal seas have received widespread attention and research around the world,but there is still a lack of relevant attention to the Chinese marginal sea region with typical sea-sonal variations of the marine environment,especially the Yellow Sea and Bohai Sea.In this paper,the intact core incubation was used to study the SOC in the Yellow Sea and Bohai Sea in April,July and October 2022,and the res-ults showed that the rates of SOC ranged from 7.11 mmol/(m2·d)to 17.33 mmol/(m2·d).There was no significant difference between the SOC of the Yellow Sea and the Bohai Sea in spring(ANOVA,p>0.05),and the SOC of the Yellow Sea was lower than Bohai Sea in summer(ANOVA,p<0.01)and autumn(ANOVA,p<0.01);the SOC of the Yellow Sea was the largest in spring and the smallest in summer,and there was no significant difference between the SOC of the Bohai Sea in summer and autumn,which were significantly higher than that of spring(AN-OVA,p<0.05).Temperature and sediment Ch1 a concentration were the influencing factors.Meanwhile,the SOC was used to assess the rate of benthic organic carbon mineralization.When compared with the primary productivity,the results indicated that the contribution of benthic organic carbon mineralization to primary productivity in the Bohai Sea ranged from 42.8%to 74.5%,which was one of the key links in the carbon cycle of the Bohai Sea,while the benthic organic carbon mineralization in Yellow Sea plays a less significant role in the carbon cycle of the Yel-low Sea carbon cycle than Bohai Sea.This paper systematically studied the SOC in the Yellow Sea and Bohai Sea and its spatial and temporal distribution characteristics,exploring the contribution of organic carbon mineralization to primary productivity in the Yellow Sea and Bohai Sea,which provided theoretical support for the understanding of organic carbon mineralization and burial in the Yellow Sea and Bohai Sea.

sediment oxygen consumptionorganic carbon mineralizationtemperaturesediment Ch1 aYellow Sea and Bohai Sea

朱若思、宋国栋、刘素美

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中国海洋大学深海圈层与地球系统前沿科学中心海洋化学理论与工程技术教育部重点实验室,山东青岛 266100

青岛海洋科技中心海洋生态与环境科学功能实验室,山东青岛 266237

中国海洋大学化学化工学院,山东青岛 266100

沉积物耗氧 有机质矿化 温度 沉积物Ch1 a 黄、渤海

2024

海洋学报(中文版)
中国海洋学会

海洋学报(中文版)

CSTPCD北大核心
影响因子:1.044
ISSN:0253-4193
年,卷(期):2024.46(5)