Department of Environment Systems, University of Tokyo, 5-1-5 Kashiwa-no-ha, Kashiwa 277-8563, Japan.
Mar Pollut Bull. 2010 Feb;60(2):215-24. doi: 10.1016/j.marpolbul.2009.09.024. Epub 2009 Oct 23.
A numerical simulation was conducted to predict the change of pCO(2) in the ocean caused by CO(2) leaked from an underground aquifer, in which CO(2) is purposefully stored. The target space of the present model was the ocean above the seafloor. The behavior of CO(2) bubbles, their dissolution, and the advection-diffusion of dissolved CO(2) were numerically simulated. Here, two cases for the leakage rate were studied: an extreme case, 94,600 t/y, which assumed that a large fault accidentally connects the CO(2) reservoir and the seafloor; and a reasonable case, 3800 t/y, based on the seepage rate of an existing EOR site. In the extreme case, the calculated increase in DeltapCO(2) experienced by floating organisms was less than 300 ppm, while that for immobile organisms directly over the fault surface periodically exceeded 1000 ppm, if momentarily. In the reasonable case, the calculated DeltapCO(2) and pH were within the range of natural fluctuation.
进行了数值模拟,以预测因地下含水层中储存的 CO2 泄漏而导致海洋中 pCO2 的变化。本模型的目标空间是海底上方的海洋。对 CO2 气泡的行为、它们的溶解以及溶解的 CO2 的平流扩散进行了数值模拟。这里研究了两种泄漏速率的情况:一种是极端情况,94600 吨/年,假设一个大的断层意外地将 CO2 储层与海底连接;另一种是合理情况,3800 吨/年,基于现有的 EOR 站点的渗流率。在极端情况下,浮游生物经历的计算出的 Delta pCO2 增加量小于 300ppm,而直接在断层表面上方的固定生物周期性地超过 1000ppm,如果只是暂时的。在合理情况下,计算出的 Delta pCO2 和 pH 值在自然波动范围内。