【24h】

DIFFERENCE OF HYDRATE NUCLEATION IN DISTILLED AND NATURAL WATERS

机译:蒸馏水和天然水中水合物成核的差异

获取原文
获取原文并翻译 | 示例

摘要

Clathrate hydrates are thermodynamically stable under low-temperature and high-pressure conditions. It is well known that the formation of hydrate membrane at the interface between liquid CO_2 and water is difficult to form in the case of water temperature of over 5 Celsius unless a nucleation was forced. We report here some new evidence relating the mechanism of hydrate formation from the experiment using distilled water and natural waters including ion-exchanged water. The solution with hydrate clusters was prepared in advance by injecting a CO_2 droplet into the high-pressure system and forcing it to form hydrate on its surface. Dissolving additional CO_2 in the circulated high-pressure system controlled the concentration of guest molecule. Keeping the pressure constant at 40MPa, the temperature was changed from 4 to 10 Celsius. We measured the time of nucleation occurrence as a parameter of concentration of guest molecule, degree of sub cooling from the dissociation temperature of hydrate. In the case of distilled water, we observed no hydrate formation at above concentration range. This suggests that the cavity-like precursors derived from cluster structures in the solution are not always increased. On the other hand, in the case of ion-exchanged water, we observed the formation of hydrate at high concentrations. Furthermore, we investigated the nucleation behavior of hydrate in surface seawater sampled from the ocean and tap water. As a result, the induction time for the nucleation of hydrate took much longer unless some forcing condition was used. The required concentration to start the nucleation in natural waters was rather small compared with the case of distilled water. This means that the high concentration of CO_2 in natural waters and seawater promotes the hydrate nucleation. These results support the assumption that the concentration of CO_2 in seawater slows the dissolution of hydrate in which a released CO_2 droplet is soon covered with hydrate membrane.
机译:笼形水合物在低温和高压条件下是热力学稳定的。众所周知,如果水温超过5摄氏度,除非强制成核,否则很难在液态CO_2与水之间的界面上形成水合膜。我们在这里报告了一些新的证据,这些证据与使用蒸馏水和包括离子交换水的天然水的实验中水合物形成的机理有关。通过向高压系统中注入CO_2液滴并迫使其在其表面形成水合物,可以预先制备具有水合物簇的溶液。在循环高压系统中溶解额外的CO_2可控制客体分子的浓度。保持压力恒定在40MPa,温度从4摄氏度更改为10摄氏度。我们测量了成核发生的时间,作为来宾分子浓度,水合物离解温度下过冷度的参数。在蒸馏水的情况下,在上述浓度范围内没有观察到水合物的形成。这表明源自溶液中簇结构的腔状前体并不总是增加。另一方面,在离子交换水的情况下,我们观察到高浓度水合物的形成。此外,我们研究了从海洋和自来水采样的地表海水中水合物的成核行为。结果,除非使用某种强迫条件,否则水合物成核的诱导时间要长得多。与蒸馏水相比,在天然水中开始成核所需的浓度很小。这意味着天然水和海水中高浓度的CO_2会促进水合物成核。这些结果支持这样的假设,即海水中CO_2的浓度会减慢水合物的溶解,其中释放的CO_2液滴很快被水合物膜覆盖。

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