钙长石的

基本解释 (translations)

anorthitic

与钙长石的相关的网络例句 [注：此内容来源于网络，仅供参考]

Plagioclase is a continuous solid solution series of albite anorthite, but its crystal structure is in continuous, which can be divided into several feldspar areas with different structure and attachment .

斜长石是钠长石-钙长石的连续固溶体系列，但在晶体结构上并不连续，可以划分成几种结构和连生不同的长石区。

A large amount of anorthite formed in the slag lumps is the main reason of slag blockage in the Shell gasifier.

大量钙长石的生成是导致安庆石化Shell气化炉产生大块熔渣和堵渣主要原因。

Anorthite and albite are important calcium-containing feldspars.

钙长石与钠长石是重要的含钙长石。

The traditional ceramic semifinished materials are the aluminum silicate system, the production phase are mainly the mullite, the solid phase reaction temperature are quite high, generally in 1200℃ about; But after joining the wollastonite, turns the calcium silicate system, the high temperature resultant for the anorthite and the cristobalite, reduced the solid phase reaction temperature largely, approximately for 1000℃~1050℃, and the anorthite assumes acicular.

传统的陶瓷坯料为硅酸铝系统，生成的物相主要为莫来石，固相反应温度比较高，一般在1200℃左右；而加入硅灰石后变成硅酸钙系统，高温生成物为钙长石和方石英，大幅降低了固相反应温度，大约为1000℃～1050℃，且钙长石呈针状。

The results show that the glass-ceramics with fibroid structure is produced after definite heat treatment, the main crystallization phase is hedenbergite and anorthite is the minor crystallization phase. The optimal process of heat treatment shows as follows: the nucleation temperature is 850 ℃ and hold time is 100 min, and the crystallization temperature is 980 ℃ and hold time is 80 min. With increasing heat treatment temperature, the FT-IR absorption bands appear obvious split, the aluminum-oxide polyhedron in the glass network changes from [AlO4] to [AlO6]. The titanium ion in the glass network gradually transforms to the 6-coordinated, moreover forms minicrystal of MgTi2O5 and Fe2TiO4 which provides the position of heterogeneous nucleation for the growth of crystal.

结果表明：在一定的热处理条件下可以以基础玻璃制备出主晶相为钙铁透辉石，次晶相为钙长石的纤维状结构的微晶玻璃；最佳的热处理工艺为：850 ℃核化100 min，980 ℃晶化80 min；随着热处理温度的升高，红外吸收带发生明显的分裂；玻璃结构中的[AlO4]向[AlO6]转化；网络结构中的钛离子逐渐转变为六配位，形成微晶相——钛酸镁和钛铁晶石，为晶体的生长提供非均匀形核位置。

Secondly, the liquid glass get inside and tine the baddeleyite in the meantime, the corudem separate out to react with the CaO-Al2O3-SiO2 glass ceramic and produce anorthite and gehlenite, and so on.

CAS微晶玻璃发生反应生成钙长石和钙铝黄长石等低共融新相物质；最后在玻璃液的冲刷下脱落。

Slag test indicates that andalusite has no obvious effect on penetration. Slag penetrates along boundaries of bauxite or mullite. Al2O3 from bauxite dissolves into slag to form CA6, anorthite, gehlenite and other low melting phases which precipitate during cooling.

渣蚀试验表明，红柱石时侵蚀无明显影响，熟料液相沿莫来石和矾土骨料晶界向内渗透，氧化铝逐渐浓解与液相、渣中的氧化钙形成CA5和钙长石、黄长石等低熔相，在冷却过程中，钙长石和黄长石从液相中析出。

The author creates the AutomaticallyDiscriminational Model for the Classification of Sandstones System, thatis to say, people can complete the vastly sample s classification of sandstonesaccurately and swiftly, meantime, diminish the possibility of mortal mistake. Based on the study of the basic sandstone component before embedding, the typeof authigenic mineral, and the forming mechanism of porosity in Upper Paleozoicreservoirs in Ordos basin, the author selects the reasonable experiment objects forWater-Rock Interaction modeling study, designs the relatively reactant and resultantduring the diagenesis period, builds the solid-liquid thermodynamics model with theprinciple of thermodynamic phase equilibrium for kinds of primary minerals (potashfeldspar, albite, anorthite, and pyroxene, hornblende) which dissolve in acidic media,and forms the corresponding thermodynamics test database.

在对鄂尔多斯盆地上古生界储层砂岩埋藏前组成、自生矿物类型和孔隙构成研究的基础之上，确定合理的沉积盆地水—岩相互作用模拟研究的实验对象，设计了埋藏成岩过程有关反应的反应物和可能的生成物，并通过热力学相平衡原理，建立了碎屑岩在埋藏成岩过程中各种骨架颗粒(钾长石、钠长石、钙长石以及铁镁暗色矿物中的辉石、角闪石等)在酸性介质条件下发生溶解的固体—流体相化学反应热力学计算模型，并获得了相应的热力学数据库，在此基础上对储层砂岩中主要造岩矿物(钾长石、钠长石、钙长石以及铁镁暗色矿物中的辉石、角闪石等)在埋藏成岩过程的酸性介质条件下发生溶解的热力学习性进行了论述。

As a result, the author discusses the thermodynamics habitus for the minerals either. With the calculation of the thermodynamics modeling, we run the dissolutionmodeling experiments for primary minerals (potash feldspar, albite, anorthite, andpyroxene, hornblende), which is under the conditions of organic acidic and 20 varietytemperature and pressure. The dissolution modeling experiments include 4 anorthitedissolution experiments, 8 pyroxene dissolution experiments, 8 hornblendedissolution experiments. We catch the records on the X ray diffraction, chemistryanalysis, SEMphotos, and the PH parameters. By theway, we discuss the dissolution habitus for the minerals either.

在热力学模拟计算的基础之上，进行20个不同温度和压力条件下，以有机酸作为溶解介质的储层砂岩骨架颗粒(钾长石、钠长石、钙长石以及铁镁暗色矿物中的辉石、角闪石等)的水—岩相互作用的溶解模拟实验，包括：4个钙长石的溶解实验、8个辉石的溶解实验和8个角闪石的溶解实验，获得了溶解模拟实验前后全部参与实验矿物的X射线衍射分析、化学全分析数据、扫描电镜照片，以及介质流体在实验过程中化学参数pH值的检测，在此基础上讨论了铁镁暗色矿物、长石等铝硅酸盐矿物在埋藏成岩过程中酸性介质条件下的溶解习性。

In the condition of keeping F、 K、Na content fixed, To improve slag structure and raise slag melting point and viscosity, MgO content is raised and TiO〓 is added. the main content is as follows:(1) Keeping CaO/SiO〓 fixed, MgO content rises from 10% to 16%, the free running temperature goes up 106℃, the viscosity goe down at bigger than 1425℃, but difference is little; keeping /SiO〓 fixed, MgO content rises from 10% to 16%, the free running temperature rises 87℃, the viscosity rises too; adding TiO〓 to 5%, the free running temperature goes up 98℃, the viscosity rise a little.(2) Powder crystal x ray diffraction and microscopic analysis shows: increasing MgO content, the cuspidine will decreace or even disappear, the monticellite goes up with MgO content rising, keeping /SiO〓 fixed, Akermanite content goes up, for high melting point minerals appear or go up, the free running temperature of the slag bearing F is raised; Adding TiO〓, high melting point mineral—Perovskite forms, it can making other minerals'crystalling fast, it is the reason that TiO〓 raises the free running temperature of the slag bearing F.

2对测定粘度的冷凝渣所进行的X粉晶衍射及显微分析和鉴定表明，增加MgO含量，渣中枪晶石将减少甚至消失，而钙镁橄榄石则随MgO含量增加而增加，在／SiO〓不变时，黄长石含量也有所增加，高熔点矿物的出现和增加，提高了含氟熔渣的熔化性温度；加入TiO〓熔渣中将形成高熔点矿物-钙钛矿，钙钛矿的形成还促使黄长石的结晶，这是TiO〓提高含氟熔渣熔化性温度的根本原因。

与钙长石的相关的网络解释 [注：此内容来源于网络，仅供参考]

albite：钠长石

斜长石则是以钙和钠的互相取代为主,依照纳和钙的比例,可分为钠长石(albite)、富钠长石(oligocalse)、中钠长石(andesine)、中钙长石(labradorite)、富钙长石(bytownte)、钙长石(anorthoite)等.

anorthite：钙长石

长石拥有一种常见的晶体矿物结构,家族成员虽然属同一晶体结构,但亦会因应晶体内不同的化学成份,而形成不同的长石类别;最常见和重要的为含钾的正长石(orthoclase)丶含钠的钠长石(albite)和含钙的钙长石(anorthite).

anorthite：钙长石,钙斜长石

三斜的 anorthic | 钙长石,钙斜长石 anorthite | 钙长安山岩 anorthite andesite

oligoclase：奥长石

再回归到宝石领域来看奥瑞冈日光石,事实上日光石(Sunstone)是来自于拉长石(又称中钙长石,英文名称 Labradorite)或是奥长石(Oligoclase)分类之中的一员,折射率约为 1.53 1.56(spot)之间,比重约为 2.65 2.70,硬度为 6 6.5,韧度稍差,

anorogenic：非造山运动的

非造山运动的 anorogenic | 三斜的 anorthic | 钙长石,钙斜长石 anorthite

anorthic：三斜的

anorogenic 非造山期的 | anorthic 三斜的 | anorthite 钙长石

anorthitic：[矿]钙长石的

plastic tab 塑料薄片 | anorthitic [矿]钙长石的 | desk copy 赠阅本(尤指供教师个人用的赠阅本)

anorthitic：钙长石的

anorthite 钙长石 | anorthitic 钙长石的 | anorthosite 火成岩

calcicosis：灰石沉着病, 钙尘肺

calcicole | 钙生植物 钙生植物的,生长于钙质土壤的 | calcicosis | 灰石沉着病, 钙尘肺 | calcielase | 钙长石

desk copy：赠阅本(尤指供教师个人用的赠阅本)

anorthitic [矿]钙长石的 | desk copy 赠阅本(尤指供教师个人用的赠阅本) | exclusive rithts 专有权