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In-situ and on-line measurement of gas flux at a hydrocarbon seep from the northern South China Sea

机译:原位和在线测量南海北部碳氢化合物渗漏的气体通量

摘要

Natural hydrocarbon seeps in the marine environment are important sources of methane and other greenhouse gases to the ocean and the atmosphere. Accurate quantification of methane flux at hydrocarbon seeps is therefore necessary to evaluate their influence on the global methane budget and climate change. Hydrocarbon seeps on the seabed produce a near-shore gas bubble zone along the shallow western coast of Hainan Island, northern South China Sea. An in-situ and on-line gas flux measuring device was deployed over a hydrocarbon seep to quantify the gas flux by equal volume exchange venting from the seabed offshore of Ledong Town, Hainan Island, over 19 days. The physiochemical parameters and the dissolved methane concentration of the bottom water at the hydrocarbon seep were also measured. The gas flux from the hydrocarbon seep varied from 22 to 771/day with the tidal period and was strongly negatively correlated with water depth. The flux data from the seep suggests that the variation in hydrostatic pressure induced by tidal forcing and ocean swell may control the variation of the gas flux. The bottom water dissolved methane concentration, ranging from 26 to 74 nmol/L, was negatively correlated with temperature and water depth at the seabed and positively with the gas flux. The total gas volume released from the hydrocarbon seep was 30.5 m(3) for the 19-day period, providing an estimated gas flux of 600 m(3)/yr. The 120 known hydrocarbon seeps along the eastern edge of the Yinggehai Basin could vent a large quantity of methane from the seafloor, which suggests that hydrocarbon seeps on the continental margin of the northern South China Sea may be an important natural source of methane to the atmosphere. (C) 2014 Elsevier Ltd. All rights reserved.
机译:海洋环境中的天然碳氢化合物渗漏是甲烷和其他温室气体向海洋和大气的重要来源。因此,有必要对烃渗流处的甲烷通量进行准确定量,以评估其对全球甲烷预算和气候变化的影响。海床上的烃类渗漏沿南海北部海南岛的浅西部海岸产生了近岸的气泡带。在碳氢化合物渗漏上部署了现场在线气体流量测量装置,以通过等量交换从海南岛乐东镇海底海底流出的气体,在19天之内对气体流量进行量化。还测量了烃渗流时底水的理化参数和溶解甲烷浓度。碳氢化合物渗漏产生的气体通量随着潮汐期从22到771 / day变化,并且与水深强烈负相关。来自渗流的通量数据表明,由潮汐强迫和海浪引起的静水压力变化可以控制气体通量的变化。底部水中溶解的甲烷浓度在26至74 nmol / L之间,与海床的温度和水深呈负相关,与气体通量呈正相关。在19天的时间里,从碳氢化合物渗漏释放的总气体量为30.5 m(3),估计气体流量为600 m(3)/年。莺歌海盆地东缘的120个已知烃类渗漏可以从海底排出大量甲烷,这表明南海北部大陆边缘的烃类渗漏可能是大气中甲烷的重要天然来源。 (C)2014 Elsevier Ltd.保留所有权利。

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    Di PF; Feng D; Chen DF;

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  • 年度 2014
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