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1)  carbonatite ['kɑ:bənətait]
碳酸盐矿
1.
Study on the Manufacture and Simulated Grouting Test of Alkali-activated-carbonatite Grouting Material;
碱激发碳酸盐矿灌浆材料的制备与模拟灌浆试验
2.
,on the gelation time of alkali-activated carbonatite-slag cementitious material(AACSCM) was investigated.
研究了一些常用于碱矿渣水泥的缓凝剂,如硝酸铅、硝酸锌和氯化钠等对碱激发碳酸盐矿-矿渣胶凝材料凝胶时间的影响。
3.
The influence of the modulus (n), concentration (C ss ) of water gla ss and the replacement of ground carbonatite with ground blast-furnace slag ( M s) on the strength of alkali carbonatite-slag cementitious material (ACSCM for short) in the presence of retarder were studied in this paper.
在采用缓凝剂的基础上,研究了水玻璃模数(n)、浓度(Css)以及矿渣替代碳酸盐矿质量分数(Ms)等对碱碳酸盐矿渣胶凝材料性能的影响,并对该体系反应产物的微观形貌和胶砂试体的孔分布进行了分析。
2)  carbonate tailings
碳酸盐尾矿
1.
The sintered test used carbonate tailings as main materials composed with fly-ash.
本文采用碳酸盐尾矿作为主要原料,同时使用粉煤灰作为配料进行烧结试验。
3)  Carbonate mineral deposits
碳酸盐矿床
4)  Carbonate mineral
碳酸盐矿物
1.
An elementary description of carbonate mineral grownextensively in gold deposit;
浅谈金矿床广泛发育的碳酸盐矿
2.
The cathodoluminescence and trace elements in carbonate minerals;
碳酸盐矿物的阴极发光性与微量元素的关系
3.
Controlling factors of cathodeluminescence of carbonate minerals
碳酸盐矿物阴极发光性的控制因素分析
5)  carbonate minerals
碳酸盐矿物
1.
X-ray diffraction and petrography analysis showed that the burial depth from 2500 meters to 3000 meters was favorable to diagenetic evolution of clay and carbonate minerals in source rock.
粘土矿物和碳酸盐矿物的转化对烃源岩力学性质产生了影响,导致随埋藏深度的增加岩石由相对塑性向相对脆性转变。
2.
Mineralogical examination and stable isotope analyses for the Lake Qinghai sediments indicate that authigenic carbonate minerals are present either in the form of one type or several types in the sediments, and that large differences in δ18O of up to 6.
青海湖沉积岩芯的矿物学和稳定同位素研究结果显示自生碳酸盐矿物以单种或多种矿物形式保存在沉积物中;不同碳酸盐样品的δ18O值的变化范围为5。
6)  carbonate [英]['kɑ:bəneit]  [美]['kɑrbə,net]
碳酸盐矿物
1.
Silicate minerals and carbonate are the main rock-forming minerals of the earth s crust.
硅酸盐矿物和碳酸盐矿物是构成地壳的主要造岩矿物,论述了两类矿物溶解动力学的研究现状与展望,指出两类矿物的溶解和沉积过程中CO2吸收和释放,对全球环境有重要影响。
2.
The relationship between the formation of some typical mineral (the authigenic pyrite and the ferruginous carbonate) and hydrocarbon is discussed in this paper, based on the correlation of stratigraphic features and diagenetic mineral in different structural belt in the Member 3 of Shahejie Formation from Dongying Depression.
针对自生黄铁矿-碳酸盐矿物-自生石英矿物组合,提出了示烃球的新认识并将其分为两大类,I型示烃球主要分布于含油性较好层段,II型示烃球主要分布于烃类活动相对较弱的非含油层段。
补充资料:盐矿
分子式:
CAS号:

性质:又称盐矿。一种以氯化钠为主要组分的非金属矿产。根据其产出状态分为岩盐、湖盐和天然卤水。共生矿物有钾石盐、杂卤石、光卤石、芒硝、石膏等。一般边界品位(含氯化钠);岩盐10%~15%,湖盐30%;工业品位:岩盐20%~30%,湖盐50%。天然卤水5%~10%。采矿:岩盐用矿井法和水溶法,湖盐用露天开采法,地下卤水用钻井抽卤法。主要用作食盐(民用盐)。还可用于制取烧碱、纯碱、盐酸、氯和提炼金属钠等化工产品。

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