A cabled monitoring module for gas seepage: the first experiment in a pockmark (Patras Gulf, Greece)

G. Marinaro, G. Etiope, N. Lo Bue, P. Favali, G. Papatheodorou, D. Christodoulou, F. Furlan, F. Gasparoni, G. Ferentinos, M. Masson, J. Rolin
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引用次数: 2

Abstract

A new seafloor observatory, the Gas Monitoring Module (GMM), has been developed for continuous and long-term measurements of methane concentration in seawater at the benthic boundary layer, as a result of marine environmental geology and technology synergy. The module is designed to host a series of sensors controlled and managed by a data acquisition and control system able to perform first-level data quality checks. The prototype includes semiconductor methane sensors, an H2S sensor and a CTD for temperature, salinity, pressure recording, as well as interfaces for additional sensors. GMM was deployed in April 2004 within an active gas-bearing pockmark in the Gulf of Patras (Greece), at a water depth of 42 m. Through a submarine cable linked to an onshore station, it was possible to remotely check, via direct phone connection, GMM functioning and to receive data in near-real time. Recordings were carried out in two consecutive campaigns over the periods April-July 2004, and September 2004-January 2005, amounting to a combined dataset of ca. 6.5 months. This represents the first long-term monitoring ever done on gas leakage from pockmarks by means of CH4+H2S+T+P sensors. The results show frequent T and P drops associated with gas peaks, more than 60 events in 6.5 months, likely due to intermittent, pulsation-like seepage. This seepage "pulsation" can either be an active process driven by pressure build-up in the pockmark sediments, or a passive fluid release due to hydrostatic pressure drops induced by bottom currents cascading into the pockmark depression. Redundancy and comparison of data from different sensors were fundamental to interpret subtle proxy signals of temperature and pressure which would not be understood using only one sensor.
气体渗漏电缆监测模块:麻坑的第一次实验(希腊帕特雷湾)
由于海洋环境地质学和技术的协同作用,已经开发了一个新的海底观测站,即气体监测模块(GMM),用于连续和长期测量底栖边界层海水中的甲烷浓度。该模块设计用于承载一系列传感器,这些传感器由能够执行一级数据质量检查的数据采集和控制系统控制和管理。该原型包括半导体甲烷传感器、H2S传感器和用于温度、盐度、压力记录的CTD,以及用于附加传感器的接口。GMM于2004年4月在Patras湾(希腊)的一个活跃的含气裂缝中进行了部署,水深42米。通过海底电缆连接到陆上站点,可以通过直接电话连接远程检查GMM的功能并近乎实时地接收数据。在2004年4月至7月期间和2004年9月至2005年1月期间,在两个连续的运动中进行了记录,总计约6.5个月的综合数据集。这是首次利用CH4+H2S+T+P传感器对麻穴气体泄漏进行长期监测。结果表明,频繁的T和P下降与气体峰值有关,在6.5个月内超过60次,可能是由于间歇性的脉动式渗流。这种渗流“脉动”既可以是由麻坑沉积物中的压力积聚驱动的主动过程,也可以是由底流级流到麻坑凹陷引起的静水压力下降引起的被动流体释放。来自不同传感器的数据冗余和比较是解释温度和压力的微妙代理信号的基础,这些信号仅使用一个传感器是无法理解的。
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