...
首页> 外文期刊>Energy >A hybrid numerical model system of LCO_2 and CO_2 enriched seawater dynamics in the ocean induced by moving-ship releasing
【24h】

A hybrid numerical model system of LCO_2 and CO_2 enriched seawater dynamics in the ocean induced by moving-ship releasing

机译:船舶释放引起海洋中富含LCO_2和CO_2的海水动力学混合数值模型系统

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

A numerical modeling system has been developed, based on an engineering background, of the direct disposal of liquid carbon dioxide into the ocean by a moving-ship, to predict the physico-chemical dynamics of liquid carbon dioxide droplets and carbon dioxide enriched seawater in the ocean. This is a hybrid simulation model system consisting of a three-dimensional small-scale near-field model and a two-dimensional horizontal turbulent dispersion model. The dynamics near to release sites include double-plume creation, interaction, evolution, and coupling with ocean currents; these are described by using two-fluid large-eddy simulation technology. The further development of carbon dioxide enriched sea-water, as a passive-inert scalar, in relatively larger spatial and time scales (28 x 28 km and up to 100 h) is then simulated by a horizontal turbulent dispersion model. For the case of liquid carbon dioxide release at a depth of 2000 m with mass flow rate of 100 kg/s and initial droplet diameter of 8.0 mm, and with ship speed of 3.0 m/s, the model predicts a vertically separated carbon dioxide enriched seawater plume, 330 m in height and 40 m in width at time about 1 h after release with a minimum pH of 6.20 corresponding to carbon dioxide concentration of 0.18 kg/m~3, in the surrounding area. This carbon dioxide enriched seawater plume diffused turbulently in the horizontal surface to an area of 9.8 x 10.5 km~2 after 100 h.
机译:基于工程背景,已经开发了一种数值模型系统,该系统通过机动船将液态二氧化碳直接排放到海洋中,以预测液态二氧化碳液滴和富二氧化碳海水中的物理化学动力学。海洋。这是一个混合仿真模型系统,由三维小规模近场模型和二维水平湍流弥散模型组成。释放地点附近的动力包括双羽的创造,相互作用,演化以及与洋流的耦合。这些是通过使用双流体大涡流仿真技术来描述的。然后,通过水平湍流弥散模型,模拟了相对较大的空间和时间范围(28 x 28 km,长达100 h)中作为被动惰性标量的富含二氧化碳的海水的进一步发展。对于在深度为2000 m,质量流量为100 kg / s,初始液滴直径为8.0 mm,船速为3.0 m / s的情况下释放液态二氧化碳的情况,该模型预测垂直分离的二氧化碳富集释放后约1 h时高330 m,宽40 m的海水羽流,其周围环境中的最低pH值为6.20,对应于二氧化碳浓度为0.18 kg / m〜3。这种富含二氧化碳的海水羽流在100 h后在水平面湍流扩散到9.8 x 10.5 km〜2的面积。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号