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aragonite相关的网络例句

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与 aragonite 相关的网络例句 [注:此内容来源于网络,仅供参考]

"Aragonite: an orthorhombic mineral form of crystalline calcium carbonate, dimorphous with calcite."

霰石: 文石结晶富钙碳化物的一种正交晶矿物,具有方解石的两种晶态。

The authors have summarized relevant data studied by overseas scientists and suggested the definition of chalky texture formation as "Chalky texture formation refers to that magnesium calcite and aragonite are transformed into the framework of micrite and microspar of low-magnesium calcite via neomorphism, and result in and maintain intercrystalline pore and throat networks in it; enhanced chalky texture formation refers to that the micrite and microspar are successively subjected to dissolution and leaching, so that the secondary network of solution voids is formed".

综合各国学者的有关研究资料,建议将白垩状结构化定义为:&碳酸盐沉积物和碳酸盐岩中的镁方解石和文石在不同成岩阶段通过新生变形而转变成低镁方解石微晶和微亮晶格架,并在其中产生和保存晶间孔喉网络的作用;强化白垩状结构化是指微晶和微亮晶格架受到进一步溶蚀和淋滤,从而形成次生溶蚀孔隙网络的作用&。

In Phanerozoic neritic carbonate environments, syndepositional dissolution proceeded at least largely independent from aragonite seas or calcite seas, and appears mainly controlled by site-related factors.

在显生宙浅水碳酸盐环境中,同沉积溶解作用独立于文石海和方解石海,主要有局部环境控制(site-related factors)。

Sanidinite (some have transformed to perthite) and quartz inclusions with radial cracks are often seen in the garnet of eclogite. The geothermal gradient of <10℃/km is recorded in the early stage mineral assemblage of high-pressure metapelitic rocks with relict aragonite. these features imply a possibility that there may be ultra-high-pressure rocks existed in Altun.

根据榴辉岩中石榴石常见透长石和石英包体,并有放射状裂纹的特征,以及高压变泥质岩石早期矿物组合温压条件记录的地温梯度小于10℃/km和残存文石等特征,不排除区内有超高压变质岩石存在的可能性。

Two common types of calcium carbonate crystal are calcite and aragonite. Many calcifying organisms are able to control the respective growth of these two crystal types which have different solubilities.

常见的碳酸钙结晶有方解石及霰石,钙化生物能控制这两种结晶各别的成长率,这两者在水中有不同的溶解度。

Their crystal structure sets them apart: calcite forms hexagons and aragonite forms rhombohedrons.

其晶体结构使它们除了:方解石形式六边形和文石形式的菱面体。

Calcite and aragonite are the two crystal forms of calcium carbonate, a property of minerals geologists call dimorphism.

方解石和文石是两种碳酸钙结晶组成,地质学者称二态性。

The presence of Mg〓 will change the crystallization process of calcium carbonate and produce aragonite scale. The presence of Zn〓 can prevent the formation of the crystal nucleus of calcium carbonate and then prevent the scale.

当水的硬度、温度增加时,水的结垢速率增加;SO〓和NaCl含量增加,能使水的结垢速率略有增加;Mg〓能改变碳酸钙的结晶过程并产生文石状的水垢;Zn〓的参与能明显阻碍碳酸钙微晶核的生成,从而达到阻垢的目的。

The water-scaling rate will increase when the water hardness or temperature is increased. The water-scaling rate will increase slightly when the concentration of SO〓 or NaC1 is increased. The presence of Mg〓 will change the crystallization process of calcium carbonate and produce aragonite scale. The presence of Zn〓 can prevent the formation of the crystal nucleus of calcium carbonate and then prevent the scale.

当水的硬度、温度增加时,水的结垢速率增加;SO〓和NaCl含量增加,能使水的结垢速率略有增加;Mg〓能改变碳酸钙的结晶过程并产生文石状的水垢;Zn〓的参与能明显阻碍碳酸钙微晶核的生成,从而达到阻垢的目的。

Calcium carbonate occurs in the allomorphs calcite and aragonite.

碳酸钙存在于同质异晶的方解石和文石中。

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