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首页> 外文期刊>Journal of Volcanology and Geothermal Research >Testing the tunable diode laser system in extreme environments: Measuring high and low CO_2 concentrations in both active volcanic and geothermal settings
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Testing the tunable diode laser system in extreme environments: Measuring high and low CO_2 concentrations in both active volcanic and geothermal settings

机译:在极端环境中测试可调二极管激光器系统:在火山活动和地热活动中测量高和低CO_2浓度

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摘要

Measuring CO2 emissions in geothermal and volcanic areas is sometimes difficult because of large areas to cover and sites often inaccessible. Measuring high levels of CO2 concentration can provide information on hidden structure in geothermal areas and recording changes in CO2 concentration on volcanic areas can help monitor the level of volcanic activity. The purpose of this study was to use the Tunable Laser Diode (TDL) absorption spectroscopy method to test levels of CO2 concentrations at two extreme environments: White Island volcano, the most active volcano of New Zealand, with large and concentrated gas fluxes, and Ngapouri geothermal area, a small geothermal area in the Taupo Volcanic Zone, New Zealand, with relatively low and diffuse gas emissions. In 2017, for the first time using TDL at White Island, CO2 concentration measurements performed across the active fumarole fields had the highest CO2 concentrations of 657 ppm. TDL survey measurements were also conducted across fault strands near the Ngapouri geothermal area, and the results complemented CO2 flux results obtained with the accumulation chamber method. Higher CO2 concentrations were measured close to the mapped Ngapouri splays with a maximum of 484 ppm. The maximum CO2 flux measured in the same area was 100 g M-2 day(-1) however the highest CO2 fluxes measured along the transects and by the mapped faults were less clear, but the CO2 concentrations increased closer to the fault splays. Advantages and disadvantages of using a TDL system have been described and compared to the accumulation chamber method. The results from the TDL system demonstrated that CO2 concentrations can be used as a tool, with other geophysical tools, for both detecting and highlighting geological structures where no obvious thermal activity is present and for monitoring purposes on active volcanoes. (C) 2019 Elsevier B.V. All rights reserved.
机译:有时很难测量地热和火山地区的二氧化碳排放量,因为要覆盖的区域很大,而且常常无法到达站点。测量高水平的二氧化碳浓度可以提供有关地热区域隐藏结构的信息,而记录火山区域二氧化碳浓度的变化可以帮助监测火山活动的水平。这项研究的目的是使用可调谐激光二极管(TDL)吸收光谱法来测试两种极端环境下的CO2浓度水平:怀特岛火山,新西兰最活跃的火山,气体通量大且集中,Ngapouri地热区,是新西兰陶波火山区中的一个较小的地热区,气体排放量相对较低且弥散。 2017年,首次在白岛使用TDL,在整个富马油田中进行的CO2浓度测量的最高CO2浓度为657 ppm。还对Ngapouri地热区域附近的断层股进行了TDL测量测量,其结果补充了用累积室法获得的CO2通量结果。在接近映射的Ngapouri扇形处测得较高的CO2浓度,最大值为484 ppm。在同一区域测得的最大CO2通量为100 g M-2天(-1),但是沿断面和测绘断层测得的最高CO2通量不太清楚,但CO2浓度增加得更接近断层。已经描述了使用TDL系统的优缺点,并将其与累积室方法进行了比较。 TDL系统的结果表明,CO2浓度可以与其他地球物理工具一起用作检测和突出显示不存在明显热活动的地质结构的工具,并可以用于监测活火山的目的。 (C)2019 Elsevier B.V.保留所有权利。

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