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2-D tomography of volcanic CO2 from scanning hard-target differential absorption lidar: the case of Solfatara, Campi Flegrei (Italy)

机译:扫描硬目标差分吸收激光雷达的火山二氧化碳二维断层扫描:以索尔法塔拉,坎皮·弗莱格里(意大利)为例

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摘要

Solfatara is part of the active volcanic zone of Campi Flegrei (Italy), adensely populated urban area where ground uplift and increasing groundtemperature are observed, connected with rising rates of CO emission. Amajor pathway of CO release at Campi Flegrei is diffuse soil degassing,and therefore quantifying diffuse CO emission rates is of vitalinterest. Conventional in situ probing of soil gas emissions withaccumulation chambers is accurate over a small footprint but requiressignificant time and effort to cover large areas. An alternative approach isdifferential absorption lidar, which allows for a fast and spatiallyintegrated measurement. Here, a portable hard-target differential absorptionlidar has been used to acquire horizontal 1-D profiles of column-integratedCO concentration at the Solfatara crater. To capture heterogenicfeatures in the CO distribution, a 2-D tomographic map of the COdistribution has been inverted from the 1-D profiles. The scan was performedone-sided, which is unfavorable for the inverse problem. Nonetheless, theresult is in agreement with independent measurements and furthermore confirmsan area of anomalous CO degassing along the eastern edge as well as thecenter of the Solfatara crater. The method may have important implicationsfor measurements of degassing features that can only be accessed from limitedangles, such as airborne sensing of volcanic plumes. CO fluxesretrieved from the 2-D map are comparable, but modestly higher than emissionrates from previous studies, perhaps reflecting an increase in CO fluxor a more integrated measurement or both.
机译:索尔法塔拉(Solfatara)是Campi Flegrei(意大利)活火山区的一部分,这是人口稠密的市区,在该地区观测到地面抬升和地温升高,并伴有CO排放率上升。 Campi Flegrei的CO释放的主要途径是分散的土壤脱气,因此量化扩散的CO排放速率至关重要。使用积聚室进行土壤气体排放的常规原位探测在较小的占地面积上是准确的,但需要大量的时间和精力才能覆盖大面积。另一种方法是使用差分吸收式激光雷达,该技术可实现快速且空间整合的测量。在这里,便携式硬目标差分吸收激光已被用于获取Solfatara火山口的柱积分CO浓度的水平一维分布图。为了捕获CO分布中的异源特征,已将CO分布的二维断层图从一维轮廓中反转了。扫描是单面进行的,这不利于反问题。尽管如此,结果与独立的测量结果是一致的,并且进一步确认了沿东部边缘以及索尔法塔拉火山口中心的一氧化碳异常脱气的区域。该方法对于只能从有限角度访问的脱气特征的测量可能具有重要意义,例如对火山羽流的机载感应。从二维图获取的CO通量具有可比性,但略高于先前研究的排放率,这可能反映了CO通量的增加或更综合的测量结果或两者兼而有之。

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