Electrical Conductivity of H2O-Rich Silicate Melt: Implications for Subduction Zone Magnetotelluric Anomalies

IF 3.9 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Jiale Ding, Xuan Guo, Li Zhang, Yunguo Li, Zhu Mao, Huaiwei Ni
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Abstract

Magnetotelluric surveys reveal high conductivity anomalies in the deep Earth, which can be attributed to the presence of silicate melt, aqueous fluid, or supercritical fluid with intermediate water content. Electrical conductivity data of all of these liquids are needed to interpret magnetotelluric results and place constraints on the composition and volume fraction of the liquid phase. Electrical conductivity experiments to date are limited to silicate melt with H2O < 12 wt% or aqueous fluid with H2O > 92 wt%, leaving a vast gap with regard to H2O content. This study reports the electrical conductivity of two K2O-Al2O3-SiO2 melts with H2O content up to 35 wt% at 1.5 GPa and 900–1500°C. We find that the strong increase of electrical conductivity with H2O content becomes more gradual after H2O reaches 10 wt%. However, electrical conductivity at 1100°C can approach as high as 40 S/m at 35 wt% H2O, in contrast with electrical conductivity of <10 S/m for most silicate melts with several wt% H2O. The variation of electrical conductivity with H2O correlates with the variation of viscosity and diffusivity, which is rooted in the modification of melt structure and dynamics by H2O. Application of the electrical conductivity data to interpretation of the magnetotelluric results in the Cascadia subduction zone reveals that the presence of 3 vol% of the extremely water-rich melt could account for the 0.5 S/m electrical anomaly detected at subarc depth on top of the subducted slab.

富水硅酸盐熔体的电导率:对俯冲带大地电磁异常的启示
大地电磁测量揭示了地球深部的高电导率异常,这可归因于硅酸盐熔体、含水流体或具有中等含水量的超临界流体的存在。所有这些液体的电导率数据都需要解释大地电磁结果,并对液相的组成和体积分数进行限制。迄今为止的电导率实验仅限于硅酸盐与水的熔体;12 wt%或含H2O的含水流体;92% wt%,在水的含量方面留下了巨大的差距。本研究报告了两种水含量高达35 wt%的k20 - al2o3 - sio2熔体在1.5 GPa和900-1500℃下的电导率。我们发现电导率随水含量的增加而增强,在水达到10 wt%后变得更加缓慢。然而,在1100°C时,在35 wt% H2O下的电导率可高达40 S/m,而大多数含有数wt% H2O的硅酸盐熔体的电导率为10 S/m。电导率随H2O的变化与粘度和扩散率的变化有关,其根源在于H2O对熔体结构和动力学的改变。利用电导率数据解释卡斯卡迪亚俯冲带大地电磁结果表明,3 vol%的极富水熔体的存在可以解释在俯冲板块顶部次弧深度检测到的0.5 S/m电异常。
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来源期刊
Journal of Geophysical Research: Solid Earth
Journal of Geophysical Research: Solid Earth Earth and Planetary Sciences-Geophysics
CiteScore
7.50
自引率
15.40%
发文量
559
期刊介绍: The Journal of Geophysical Research: Solid Earth serves as the premier publication for the breadth of solid Earth geophysics including (in alphabetical order): electromagnetic methods; exploration geophysics; geodesy and gravity; geodynamics, rheology, and plate kinematics; geomagnetism and paleomagnetism; hydrogeophysics; Instruments, techniques, and models; solid Earth interactions with the cryosphere, atmosphere, oceans, and climate; marine geology and geophysics; natural and anthropogenic hazards; near surface geophysics; petrology, geochemistry, and mineralogy; planet Earth physics and chemistry; rock mechanics and deformation; seismology; tectonophysics; and volcanology. JGR: Solid Earth has long distinguished itself as the venue for publication of Research Articles backed solidly by data and as well as presenting theoretical and numerical developments with broad applications. Research Articles published in JGR: Solid Earth have had long-term impacts in their fields. JGR: Solid Earth provides a venue for special issues and special themes based on conferences, workshops, and community initiatives. JGR: Solid Earth also publishes Commentaries on research and emerging trends in the field; these are commissioned by the editors, and suggestion are welcome.
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