钙

A series of anorthite/glass composites were prepared using electronic ceramics process.

采用电子陶瓷工艺制备了一系列钙长石/玻璃复合材料，并对复合材料进行X射线分析、扫描电镜观察和性能测试。

The results show that the dielectric constant and thermal expansion coefficient increased,the dielectric loss and bending strength desreased with the increasing of anorthite content.

钙长石含量大于50wt%的复合材料中α-石英和方石英的析出增加了材料的热膨胀系数，但对材料的介电性能影响不大。

In different host minerals, the contents of CO2, H2O and CH4 are different.The CO2content is the highest in anorthite, while that in crysolite is in the next place and that in augite is the least.

不同宿主矿物，其包裹体成分中CO2、H2O和CH4的相对含量也不同，其中，钙长石中包裹体的CO2含量最高，贵橄榄石中的次之，普通辉石中的最少。

The amorphous precursor crystallises at 10008C into hexagonal anorthite before transforming into the stable triclinic form.

非晶前驱crystallises在10008C到六角钙长石之前转化为稳定的三表。

At 920 8C, the sample exhibits a high amount of crystalline phase but, at 1050 8C, it is possible to notice a small decrease of the anorthite peak intensity, benefiting the growth of diopside.

在920.8摄氏度下样本中开始出现大面积结晶状态。但在1050.8摄氏度时，我们看到钙长石含量的峰值有所下降，并造成透辉石含量上升。

In the case of frit A, the results have shown that it remains amorphous until 800 8C and only after that it starts to form anorthite and diopside.

样本A的无组织状态直到温度达到800.8摄氏度才被破坏。之后该样本中开始出现钙长石和透辉石。

According to the fluid components and their contents in the studied host minerals,it is inferred that the crystallization order of the studied host minerals are anorthite, crysolite and then augite.It is also concluded that the hydrocarbon and water maybe primarily came from sedimentary strata when lava is arising.

根据这3种宿主矿物中流体成分及其含量变化特点，推断这3种宿主矿物的结晶顺序为钙长石、贵橄榄石、普通辉石，并认为流体包裹体中的烃类和水可能主要来自熔体上升过程中所接触的沉积地层。

As the temperature increases, content of quartz, anhydrite, and hematite in coal ash decrease in reducing conditions and some new mineral phases are formed during heating process. The content of mullite formed in the heating process is the mayor reason of high melting temperature of the ash. Anorthite at high temperature lowers the ash fusion temperature.

随着温度的升高，煤灰中石英、硬石膏、赤铁矿等结晶矿物含量逐渐减少，生成新的矿物质，莫来石的生成是导致淮南煤灰熔点高的主要原因，钙长石起到降低灰熔点的作用。

If we make full use of the mid-infrared spectral features(i.e.,Christiansen Frequency features and reststrahlen bands),we could determine anorthite,olivine,quartz and alkali feldspar on the lunar surface successfully,which could not be accomplished by VIS-NIR spectra.

如果充分利用月球表面硅酸盐的红外光谱特征，即CF特征和Reststrahlen吸收带，将可以用于探测VIS-NIR光谱无法完成的探测目标：钙长石、橄榄石、石英和碱性长石等。

The anorthite component of plagioclase from Kela 2 reservoir was dissolved so completely by the pore fluid that the dissolution made great contribution to the pore volume, and the albite component suffered partially dissolution; by contrast K-feldspar did not dissolved in the ground water at all.

克拉2 气田中斜长石骨架颗粒中的钙长石组分基本上遭受了彻底的溶蚀，对次生孔隙的贡献较大，钠长石溶蚀程度有限，而钾长石基本上不被溶蚀。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。