Formation processes of brine drainage channels in sea ice
Formation processes of brine drainage channels in sea ice
复制标题
海冰中盐水排放通道的形成过程
DOI：
10.1029/jc092ic07p07195
复制
发表时间：
1987
期刊：
影响因子：
--
通讯作者：
T. Kawamura
中科院分区：
文献类型：
--
作者：
M. Wakatsuchi;T. Kawamura
本文对海冰中卤水排水通道形成的晶体环境进行了实验研究。研究表明，卤水通道总是在冰片两侧生长的晶界处形成，而不是在冰片倾斜的晶界处形成。这些观测结果表明，盐水排出和重力排水是海冰淡化的主要因素。
This paper is an experimental study of the crystallographic circumstances governing the formation of brine drainage channels in sea ice. The study shows that brine channels always form in the grain boundaries toward which the ice platelets grow from both sides and that they do not form at the boundaries from which the platelets slant away. These observations imply that brine expulsion and gravity drainage are the major contributors to sea ice desalination.