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使用高度便携的差分吸收激光雷达(DIAL)激光系统进行一氧化碳通量测量的新领域。

A new frontier in CO flux measurements using a highly portable DIAL laser system.

作者信息

Queiβer Manuel, Granieri Domenico, Burton Mike

机构信息

School of Earth, Atmospheric and Environmental Sciences, University of Manchester, Oxford Road, Manchester M139PL, UK.

Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione di Pisa, 50126 Pisa, Italy.

出版信息

Sci Rep. 2016 Sep 22;6:33834. doi: 10.1038/srep33834.

Abstract

Volcanic CO emissions play a key role in the geological carbon cycle, and monitoring of volcanic CO fluxes helps to forecast eruptions. The quantification of CO fluxes is challenging due to rapid dilution of magmatic CO in CO-rich ambient air and the diffuse nature of many emissions, leading to large uncertainties in the global magmatic CO flux inventory. Here, we report measurements using a new DIAL laser remote sensing system for volcanic CO (CODIAL). Two sites in the volcanic zone of Campi Flegrei (Italy) were scanned, yielding CO path-amount profiles used to compute fluxes. Our results reveal a relatively high CO flux from Campi Flegrei, consistent with an increasing trend. Unlike previous methods, the CODIAL is able to measure integrated CO path-amounts at distances up to 2000 m using virtually any solid surface as a reflector, whilst also being highly portable. This opens a new frontier in quantification of geological and anthropogenic CO fluxes.

摘要

火山一氧化碳排放是地质碳循环的关键环节,监测火山一氧化碳通量有助于预测火山喷发。由于富含一氧化碳的环境空气中岩浆一氧化碳的快速稀释以及许多排放的扩散性质,一氧化碳通量的量化具有挑战性,这导致全球岩浆一氧化碳通量清单存在很大不确定性。在此,我们报告了使用一种用于火山一氧化碳的新型差分吸收激光雷达(DIAL)遥感系统(CODIAL)的测量结果。对意大利坎皮佛莱格瑞火山带的两个地点进行了扫描,得出用于计算通量的一氧化碳路径总量剖面。我们的结果显示坎皮佛莱格瑞火山的一氧化碳通量相对较高,且呈上升趋势。与以往方法不同,CODIAL能够在距离达2000米处测量积分一氧化碳路径总量,几乎可将任何固体表面用作反射体,同时还具有高度便携性。这为地质和人为一氧化碳通量的量化开辟了新领域。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8a0f/5031984/77743b3772e4/srep33834-f1.jpg

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