| 珍珠陶石的夹层化合物法鉴定 |
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| 引用本文： | 沈忠悦,叶瑛.珍珠陶石的夹层化合物法鉴定[J].矿物学报,1996,16(1):89-91. |
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| 作者姓名： | 沈忠悦 叶瑛 |
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| 作者单位： | 浙江大学地球科学系!杭州，310027，浙江大学地球科学系!杭州，310027 |
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| 摘 要： | 应用联氨、使珍珠陶石形成其夹层物，然后再用水洗获是水合珍珠陶石，这种水合珍珠陶石具有十分特征的０．８３５ｎｍＸ射线衍射峰，而高岭石族的其它矿物却保持不变，利用这一明显的特征，可以容易地区分出混合在高岭石中的少量珍珠陶石。
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| 关 键 词： | 珍珠陶石 夹层化合物 联氨 水合珍珠陶石 |
IOENTIFICATION OF NACRITE BY HYDRAZINE INTERCALATION |
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| Shen Zhongyue, Ye Ying.IOENTIFICATION OF NACRITE BY HYDRAZINE INTERCALATION[J].Acta Mineralogica Sinica,1996,16(1):89-91. |
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| Authors: | Shen Zhongyue Ye Ying |
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| Abstract: | An intercalation complex of hydrated nacrite is formed by initial nacrite intercalated withhydrazine, and then replaced with water tholecules by washing with water. The nacrite intercalatedcomplex is of cbaracteristic of 0. 835 nm diffraction peak,while other minerals of the kaolinite family rfmain unchanged. This is an unambiguous way to distinguish minor nacrite component from themixture of kaolinite minerals. |
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| Keywords: | nacrite intercalation hydrazine |
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