Detection and monitoring of leaked CO2 through sediment, water column and atmosphere in a sub-seabed CCS experiment
Detection and monitoring of leaked CO2 through sediment, water column and atmosphere in a sub-seabed CCS experiment
复制标题
海底 CCS 实验中通过沉积物、水柱和大气泄漏的 CO2 的检测和监测
DOI:
10.1016/j.ijggc.2014.12.011
复制
发表时间:
2015
影响因子:
3.9
通讯作者:
Shitashima K
中科院分区:
文献类型:
--
作者:
Shitashima K
Carbon capture and storage in sub-seabed geological formations (sub-seabed CCS) is currently being studied as a realistic option to mitigate the accumulation of anthropogenic CO2in the atmosphere. In implementing sub-seabed CCS, detecting and monitoring the impact of the sequestered CO2on the ocean environment is highly important. The first controlled CO2release experiment, Quantifying and Monitoring Potential Ecosystem Impacts of Geological Carbon Storage (QICS), took place in Ardmucknish Bay, Oban, in May–September 2012.We applied the in situ pH/pCO2sensor to the QICS experiment for detection and monitoring of leaked CO2, and carried out several observations. The cabled real-time sensor was deployed close to the CO2leakage (bubbling) area, and the fluctuations of in situ pH and pCO2above the seafloor were monitored in a land-based container. The long-term sensor was placed on seafloor in three different observation zones. The sediment pH sensor was inserted into the sediment at a depth of 50 cm beneath the seafloor near the CO2leakage area. Wide-area mapping surveys of pH and pCO2in water column around the CO2leakage area were carried out by using an autonomous underwater vehicle (AUV) installed with sensors. Atmospheric CO2above the leakage area was observed by using a CO2analyzer that was attached to the bow of ship of 50 cm above the sea-surface.The behavior of the leaked CO2is highly dependent on the tidal periodicity (low tide or high tide) during the CO2gas release period. At low tide, the pH in sediment and overlying seawater decreased due to strong eruption of CO2gas bubbles, and the CO2ascended to sea-surface quickly with a little dissolution to seawater and dispersed into the atmosphere. On the other hand, the CO2bubbles release was lower at high tide due to higher water pressure, and slight low pH seawater and high atmospheric CO2were detected. After stopping CO2gas injection, no remarkable variations of pH in sediment and overlying water column were observed for three months.
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影响因子:
3.9
作者:
Y. Maeda;K. Shitashima;A. Sakamoto
通讯作者:
Y. Maeda;K. Shitashima;A. Sakamoto
DOI:
--
发表时间:
1994
期刊:
影响因子:
--
作者:
A. Dickson
通讯作者:
A. Dickson
影响因子:
3.4
作者:
K. Shitashima;Y. Maeda;T. Ohsumi
通讯作者:
K. Shitashima;Y. Maeda;T. Ohsumi
DOI:
10.1109/ut.2002.1002403
发表时间:
2002
期刊:
Proceedings of the 2002 Interntional Symposium on Underwater Technology (Cat. No.02EX556)
影响因子:
--
作者:
K. Shitashima;M. Kyo;Y. Koike;H. Henmi
通讯作者:
H. Henmi
影响因子:
5.8
作者:
Dewar M
通讯作者:
Dewar M