Morris和他的同事正在建模，关于那些不含水的矿物和层状硅酸盐的星盘的红外光谱特征。
Morris and her colleagues began by modeling the infrared emission features of dust that did not contain hydrated minerals, or phyllosilicates.
验证层状硅酸盐存在的一个最简单证据就是粘土矿物。
One of the simplest examples of phyllosilicates is clay minerals.
粘土类矿物因具有独特的层状结构而表现出良好的吸附和离子交换性能，在废水处理中有广阔的应用前景。
Clay minerals possess better adsorption and ion exchange capacity for their sandwich structure, so exhibit wider application prospect in wastewater treatment.
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