1) diaspore
[英]['daiəspɔ:] [美]['daɪə,spɔr]
重水铝石
2) gibbsite
['ɡibzait]
三水铝石
1.
Studies on the surface acid-base properties and phosphate adsorption behavior of gibbsite (γ-Al(OH)_3) and α-Al_2O_3;
三水铝石(γ-Al(OH)_3)和α-Al_2O_3表面酸碱性质与磷酸根吸附研究
2.
Investigation of Raising Silicon to Aluminum Ratio of Gibbsite by Flotation;
浮选方法提高三水铝石铝硅比的研究
3.
Prospects for Comprehensive Utilization of Gibbsite from Accumulated Bauxite in Western Guangxi Province;
桂西堆积型铝土矿中三水铝石矿综合利用前景
3) boehmite
[英]['beimait] [美]['be,maɪt, 'bo-]
薄水铝石
1.
Rehydration of pseudoboehmite-derived γ-Al_2O_3 at lower temperature;
拟薄水铝石脱水产物γ-Al_2O_3在较低温度下的再水合过程研究
2.
Studies on Hydrothermal Behavior of Alumina Ⅲ.-Rehydration of Aluminas Derived from Boehmite;
氧化铝的水热化学研究 Ⅲ──薄水铝石脱水产物的再水合现象
3.
Synthesis and characterization of ovel 3D urchin-like boehmite(AlOOH) superstructures;
三维海胆状薄水铝石(AlOOH)的合成与表征
4) hibschite
水铝榴石
5) diaspore
[英]['daiəspɔ:] [美]['daɪə,spɔr]
硬水铝石
1.
Preparation chemistry study of the high temperature and high surface area Al_2O_3 Ⅰ Preparation of high surface area α-Al_2O_3 from diaspore decomposition;
高温高表面氧化铝新材料制备的化学研究Ⅰ.硬水铝石法制高表面α-Al_2O_3
2.
It was proved in the past few years that the accumulation bauxite deposits in Pingguo and other places in western Guangxi are large-scale paragenetie deposits of gibbsite and diaspore.
近年证实平果等地堆积铝土矿是三水铝石硬水铝石共生的大型矿床。
3.
The mineral feature and its genesis mechanism of diaspore and gibbsite in Sanhe Mine of Jingxi County are studied with observation of polished thin section,X ray diffraction and electronic probe in the paper.
以光薄片观察、X射线衍射分析及电子探针等先进方法为手段,对靖西县三合铝土矿的硬水铝石和三水铝石的矿物特征进行研究,并探讨其成因机制。
6) Allophane
[英]['æləfein] [美]['ælə,fen]
水铝英石
1.
The Preparation of Rubber/Allophane Nanocomposites;
水铝英石/橡胶纳米复合材料的制备
2.
Preparation and properties of allophane/SBR nanocomposite
中空球状水铝英石/SBR纳米复合材料的制备与性能研究
3.
In the 29 Si MAS NMR spectra, the weak 29 Si signal of allophane near - 79.
0×10－6位置附近的水铝英石的特征29Si信号，说明在一定的自然条件下，经过水的化学作用，变高岭石可以转变成水铝英石。
补充资料：三水铝石
化学组成为Al(OH)3、晶体属单斜晶系 P21/n空间群的氢氧化物矿物。与拜三水铝石(bayerite)和诺三水铝石 (nordstrandite)成同质多象。旧称三水铝矿或水铝氧石。以矿物收藏家C.G.吉布斯 (Gibbs)的姓于1822年命名。晶体结构与水镁石相似,由夹心饼干式的(OH)-Al-(OH)配位八面体层平行叠置而成，只是Al3+不占满夹层中的全部八面体空隙,仅占据其中的2/3。三水铝石的晶体一般极为细小，呈假六方片状，并常成双晶；通常以结核状、豆状、土状集合体产出。白色，或因杂质染色而呈淡红至红色。玻璃光泽，解理面显珍珠光泽。底面解理极完全。摩斯硬度2.5～3.5，比重2.40。三水铝石主要是长石等含铝矿物化学风化的次生产物，是红土型铝土矿的主要矿物成分。但也可为低温热液成因。俄罗斯南乌拉尔的兹拉托乌斯托夫斯克的热液脉中产出有达5厘米大小的晶体。用途见铝土矿。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条