来自地球地幔的流量,根据夏威夷烟脱气的估计
概括
研究人员在夏威夷基拉韦亚测量了和二氧化碳的比率. 这些数据表明1 x 10^5原子/cm^2/秒的流,可能源自上层地幔.
科学领域:
- 地质化学 地质化学
- 火山学 火山学是一门学科.
- 地球科学 地球科学 地球科学
背景情况:
- 火山气体为地下过程提供了洞察力.
- 了解气体成分对于监测火山活动和地球地幔动态至关重要.
研究的目的:
- 测量来自夏威夷 Kilauea 的硫银行烟雾中的流量.
- 调查排放的起源及其与地幔过程的关系.
主要方法:
- 系统地收集和分析来自硫库烟雾中的火山气体 (和二氧化碳).
- 估计地球地中的碳含量.
主要成果:
- 确定了与二氧化碳的平均比率.
- 计算出每平方厘米每秒1 x 10^5个原子的流量.
- 这种流量属于先前估计值的较低范围.
结论:
- 测量到的流量可能表明了上层地幔深层来源的贡献.
- 硫银行的烟气体组成可以作为地幔脱气的指标.
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