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Density Change of CO_2-Dissolved Water in Hydrate Forming Region

机译:水合物成形区域CO_2溶解水的密度变化

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The density changes of CO_2 dissolved seawater in hydrate forming region, which determines the diffusion process of dissolved CO_2 around storage site, is one of the properties that influence on the ecosystems. In order to obtain density changes, the authors attempt directly to measure the density of CO_2 dissolved water by using a high-pressure loop that can simulate the pressure up to 3000 meters depth (30 MPa). As a result, the density increase of CO_2 dissolved water was obtained as 2.99, 2.55 and 2.84 kg/m~3/wt% for 5, 12 and 20 Celsius, respectively.
机译:Co_2溶解海水在水合物成形区域中的密度变化,确定储存部位周围溶解的CO_2的扩散过程,是影响生态系统的性质之一。为了获得密度变化,作者试图通过使用高压回路直接测量CO_2溶解水的密度,该高压环可以模拟高达3000米深度的压力(30MPa)。结果,将CO_2溶解水的密度增加分别为2.99,2.55和2.84kg / m〜3 / wt%,分别为5,12和20摄氏度。

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