The hydrated silicon dioxide with three layers structure of micron-submicron-millimicron was observed through TEM.
通过电镜实验,观察到水合二氧化硅具有



纳
三次结构。
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Whereas those with lower silica content, like intermediate to mafic volcanic andesite and basalt, tend to make darker iron and magnesium-rich flour, which absorbs more light, making lakes that look greener, grayish, or duller blue, depending on concentration.
而二氧化硅
量较低的岩石,比如中性到镁铁质的火山岩——安山岩和玄武岩,则会形成颜色更深、
铁和镁的岩粉,这类岩粉吸收更多光线,从而使湖泊看起
偏绿、偏灰,或是较为暗淡的蓝色,具体取决于岩粉的浓度。