It is shown that expansible ettringite forms in the topochemical reaction,and crystallizes in-situ on the surface of unhydrated aluminate minerals and orients radially.
发现能够产生膨胀的钙矾石是由局部应所生成;它们在未水的铝酸盐矿物表面原地结晶,呈放射生长。
It is shown that expansible ettringite forms in the topochemical reaction,and crystallizes in-situ on the surface of unhydrated aluminate minerals and orients radially.
发现能够产生膨胀的钙矾石是由局部应所生成;它们在未水的铝酸盐矿物表面原地结晶,呈放射生长。
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