ECO: A new reference model of dry olivine electrical conductivity

IF 2 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Xiaozhi Yang
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Abstract

Electrically Conductive Olivine, ECO, is presented as a new reference model for the electrical conductivity of dry olivine. The model takes into account the prevailing redox state, temperature and pressure in the upper mantle, as well as their effects on the conductivity, and is based on conductivity analyses of dry single crystal olivine at high pressures. The model demonstrates higher conductivity of olivine than those previously proposed standard olivine models, which rely on the conductivity of olivine measured at room pressure. Accepting that the bulk electrical structure is in general dominated by olivine, the upper mantle is more conductive than the estimates of the previous models. The olivine conductivity is in fact high at the oxidizing conditions of the shallow mantle, but drops at greater depths where the mantle portion is reducing. The model provides a new reference basis for understanding the electrical structure of the upper mantle, and is important for invoking any other conductive candidates to explain enhanced mantle conductivity.

ECO:干橄榄石电导率的新参考模型
导电橄榄石(ECO)是干橄榄石导电性的新参考模型。该模型考虑了上地幔中普遍存在的氧化还原状态、温度和压力,以及它们对电导率的影响,并以高压下干燥单晶橄榄石的电导率分析为基础。与之前提出的标准橄榄石模型相比,该模型证明橄榄石具有更高的电导率,而之前提出的标准橄榄石模型依赖的是橄榄石在常压下测得的电导率。如果认为块体电结构总体上由橄榄石主导,那么上地幔的导电率要高于之前模型的估计值。事实上,在浅地幔的氧化条件下,橄榄石的导电率很高,但在地幔部分处于还原状态的更深处,橄榄石的导电率就会下降。该模型为了解上地幔的电结构提供了一个新的参考依据,对于引用任何其他导电候选物质来解释地幔导电性的增强也很重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Solid Earth Sciences
Solid Earth Sciences GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
3.60
自引率
5.00%
发文量
20
审稿时长
103 days
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