印度洋卡尔斯伯格脊6°48′N附近热液羽状流水化学参数异常和颗粒物成分特征

蒋紫靖; 韩喜球; 王叶剑; 邱中炎

doi:10.3969/j.issn.1001-909X.2017.04.004

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海洋学研究 ›› 2017, Vol. 35 ›› Issue (4) : 34-43. DOI: 10.3969/j.issn.1001-909X.2017.04.004

研究论文

印度洋卡尔斯伯格脊6°48′N附近热液羽状流水化学参数异常和颗粒物成分特征

蒋紫靖^1,2, 韩喜球^1,2, 王叶剑^1,2, 邱中炎^1,2

作者信息 +

Characteristics of water chemistry and constituents of particles in the hydrothermal plume near 6°48′N, Carlsberg Ridge, Northwest Indian Ocean

JIANG Zi-jing^1,2, HAN Xi-qiu^1,2, WANG Ye-jian^1,2, QIU Zhong-yan^1,2

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文章历史 +

摘要

2015年中国大洋33航次在西北印度洋卡尔斯伯格脊6°48′N附近进行了热液异常探测,成功发现了大糦热液区。本文对该热液区附近采集的CTD水样开展了水化学与颗粒物分析。结果表明,在3 150~3 400 m水深范围内水体存在Cl、Br、Mg负异常以及DFe和DMn正异常。其中Cl、Br、Mg的浓度较研究区海水背景值分别亏损2.87%~5.27%、3.21%~4.53%和2.52%~3.82%,Cl和Br的亏损指示海底释放的热液流体曾经发生了相分离。根据Mg的亏损情况,可以估算热液羽状流中热液流体的贡献约3.90%。DFe和DMn的浓度峰值分别为127 nmol/L和29.0 nmol/L,均出现在水深3 150 m层位。颗粒物的电镜观察和能谱分析结果显示,在2 900~3 400 m深度范围内存在热液成因的富铁氧化物(FeO占49.1%~95.2%),与海水样品中发现的高浓度DFe和DMn相印证。根据实测底层流流速与Fe(Ⅱ)扩散半径对研究区的Fe(Ⅱ)氧化半衰期进行了估算,得到大糦热液区Fe(Ⅱ)氧化半衰期为0.56~2.22 h。

Abstract

In 2015, a hydrothermal field named Daxi was discovered during the Chinese DY33 cruise at 6°48′N, Carlsberg Ridge, Northwest Indian Ocean. The chemistry of water samples and particles of a CTD station near Daxi Hydrothermal Field was studied. In the water depth of 3 150~3 400 m, the water chemistry shows slight depletion of Cl, Br, Mg and intense enrichment of DFe and DMn. The concentrations of Cl, Br, Mg deplete 2.87%~5.27%, 3.21%~4.53% and 2.52%~3.82%, respectively, when comparing to background seawater. It is suggested that the hydrothermal fluid has been subjected to phase separation, resulting in the depletion of Cl and Br. The depletion of Mg suggests that the hydrothermal plume has been well mixed with the ambient seawater and the contribution of hydrothermal fluid is account for about 3.90%. The concentrations of DFe and DMn reach to 127 nmol/L and 29.0 nmol/L, respectively, for the sample collected at 3 150 m water depth. The particles have been investigated under scanning electron microscope and analyzed by energy dispersive X-Ray spectrometer. The results show that among the particles in the water depth of 2 900~3 400 m, there are more iron oxides or hydroxides (49.1%~95.2% FeO) present, and this discovery is consistent with the enrichment of DFe and DMn in the water samples. According to the current speed and the diffuse radius of Fe(Ⅱ), the calculated value of Fe(Ⅱ) oxidation half-live in Daxi hydrothermal field is 0.56~2.22 h.

导出引用

蒋紫靖, 韩喜球, 王叶剑, 邱中炎. 印度洋卡尔斯伯格脊6°48′N附近热液羽状流水化学参数异常和颗粒物成分特征[J]. 海洋学研究. 2017, 35(4): 34-43 https://doi.org/10.3969/j.issn.1001-909X.2017.04.004

JIANG Zi-jing, HAN Xi-qiu, WANG Ye-jian, QIU Zhong-yan. Characteristics of water chemistry and constituents of particles in the hydrothermal plume near 6°48′N, Carlsberg Ridge, Northwest Indian Ocean[J]. Journal of Marine Sciences. 2017, 35(4): 34-43 https://doi.org/10.3969/j.issn.1001-909X.2017.04.004

中图分类号： P734.2

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