Quasi-liquid layer controls growth mechanisms of ice-like materials
Why it matters: Better understanding clathrate hydrates could unlock new technologies and energy solutions.
- Clathrate hydrates are crystalline structures formed by water molecules trapping other molecules, found on seafloors.
- A University of Oklahoma researcher is contributing to a deeper understanding of these materials.
- The 'quasi-liquid layer' is identified as a key factor controlling the growth mechanisms of ice-like materials such as clathrate hydrates.
University of Oklahoma research is advancing our understanding of clathrate hydrates, crystalline structures found on seafloors that trap molecules like methane and carbon dioxide. This work focuses on the 'quasi-liquid layer' that dictates how these ice-like materials grow, a critical step toward unlocking their potential technological applications.
