Murakami Motohiko
Department of Earth Sciences, ETH Zürich, Zürich, 8025, Switzerland.
Department of Earth and Planetary Materials Science, Graduate School of Science, Tohoku University, Sendai, 980-8578, Japan.
Sci Rep. 2018 Aug 8;8(1):11890. doi: 10.1038/s41598-018-30432-7.
Because of its potentially broad industrial applications, a new synthesis of elastically stiffer and stronger glass has been a long standing interest in material science. Various chemical composition and synthesis condition have so far been extensively tested to meet this requirement. Since hydration of matter, in general, significantly reduces its stiffness, it has long been believed that an anhydrous condition has to be strictly complied in synthesis processes. Here we report elastic wave velocities of hydrous SiO glass determined in-situ up to ultrahigh-pressures of ~180 gigapascals, revealing that the elastic wave velocities of hydrous glass unexpectedly show the rapid increase with pressure and eventually become greater than those of anhydrous glass above ~15 gigapascals. Furthermore, anomalous change in the velocity gradient at ~100 gigapascals, probably caused by the change in Si-O coordination number from 6 to 6+, was also found at ~40 gigapascals lower pressure condition than that previously reported in anhydrous silica glass, implying that water is a highly effective impurity to make SiO glass much denser. This experimental discovery strongly indicates that hydration combined with pressurization is highly effective to synthesize elastically stiffer glass materials, which offers a new insight into the fabrication of industrially useful novel materials.
由于其潜在的广泛工业应用,新型弹性更硬更强的玻璃合成一直是材料科学领域长期关注的问题。迄今为止,人们已经对各种化学成分和合成条件进行了广泛测试以满足这一要求。由于物质的水化通常会显著降低其硬度,长期以来人们一直认为在合成过程中必须严格遵守无水条件。在此,我们报告了在高达约180吉帕斯卡的超高压下原位测定的含水SiO玻璃的弹性波速度,结果表明含水玻璃的弹性波速度出乎意料地随压力快速增加,并且在高于约15吉帕斯卡时最终超过无水玻璃。此外,在比先前报道的无水二氧化硅玻璃低约40吉帕斯卡的压力条件下,还发现了在约100吉帕斯卡处速度梯度的异常变化,这可能是由Si-O配位数从6变为6 +引起的,这意味着水是使SiO玻璃密度显著增加的高效杂质。这一实验发现有力地表明,水化与加压相结合对于合成弹性更硬的玻璃材料非常有效,这为工业上有用的新型材料的制造提供了新的见解。