| 长沙东郊第四纪红土红壤粘土矿物组成X射线衍射法分析 |
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| 引用本文： | 蒋健容,宫内信文. 长沙东郊第四纪红土红壤粘土矿物组成X射线衍射法分析[J]. 湖南农业大学学报(自然科学版), 1993, 0(6) |
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| 作者姓名： | 蒋健容 宫内信文 |
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| 作者单位： | 湖南农学院农学系，鹿儿岛大学农学部 长沙，410128，鹿儿岛市，日本 |
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| 摘 要： | 通过X射线衍射分析湖南长沙东郊第四纪红色粘土发育的红壤,结果表明:该地红壤粘土矿物成分以水云母,高岭石,蛭石、蛭石-蒙脱石1.4×10~(-9)m 过渡矿物等3种粘土矿物群为主.
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| 关 键 词： | 红壤 粘土矿物 X射线衍射分析 |
A STUDY ON THE MINERAL COMPOSITION OF CLAY OF THE RED SOIL DEVELOPED FROM QUATERNARY RED CLAY IN THE EAST SUBURBS OF CHANGSHA |
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| Jiang Jianrong Nobufumi Miyauchi. A STUDY ON THE MINERAL COMPOSITION OF CLAY OF THE RED SOIL DEVELOPED FROM QUATERNARY RED CLAY IN THE EAST SUBURBS OF CHANGSHA[J]. Journal of Hunan Agricultural University, 1993, 0(6) |
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| Authors: | Jiang Jianrong Nobufumi Miyauchi |
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| Affiliation: | Jiang Jianrong~1 Nobufumi Miyauchi~2 |
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| Abstract: | X-Ray diffraction Analysis showed that the dominant mineral groups of the redsail were Kaonilite,Illite,Vermiculite and the intermidiate group of Vermiculite andMontmorillonite. |
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| Keywords: | krasnozem clay minerals X-ray diffraction analysis |
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