thenardite [θə'nɑ:dait]

thenardite的基本解释

n.

[矿]无水芒硝

与thenardite相关的网络例句 [注：此内容来源于网络，仅供参考]

The evaporating experimental results show that, hydromagnesite is first separated with the lake-water being concentrated, and then halite, thenardite, bloedite, picromerite, epsomite, sylvite and carnallite precipitated successively.

蒸发实验的结果表明：首先析出水菱镁矿，随着湖水继续浓缩进一步析出石盐、无水芒硝、白钠镁矾、软钾镁矾、泻利盐、钾石盐和光卤石。

This paper presents the experimental data of metastable phase equilibrium of Na+, K+, Mg2+∥Cl-, SO2-4-H2O quinary system at 35 ℃, from which the metastable phase diagram is drawn. It consists of nine regions of crystallization saturated with sodium chloride, potassium chloride, glasserite(3K2SO4*Na2SO4), leonite(K2SO4*MgSO4*4H2O), kainite(KCl*MgSO4*2.75H2O), thenardite(Na2SO4), astrankit(MgSO4*Na2SO4*4H2O), carnallite(KCl* MgCl2*6H2O), magnesium sulfate hexahydrite(MgSO4*6H2O) and bischofit(MgCl2*6H2O).

研究得出（Na+， K+， Mg2+∥Cl-， SO2-4-H2O）五元体系35 ℃时的介稳溶解度数据，绘制了该体系35 ℃的介稳相图，共有9个为氯化钠所饱和的结晶区域：氯化钾、钾芒硝（3K2SO4*Na2SO4）、钾镁矾（K2SO4*MgSO4*4H2O）、钾盐镁矾（KCl*MgSO4*2.75H2O）、光卤石（KCl*MgCl2*6H2O）、白钠镁矾（Na2SO4*MgSO4*4H2O）、硫酸钠、六水硫酸镁（MgSO4*6H2O）和水氯镁石（MgCl2*6H2O）。

The ash samples of CS are composed of many sodium rich and fusing temperature low minerals, such as nepheline, thenardite and hauyne.

黑液浆灰样中含有大量的霞石和硫酸钠等低熔融温度富钠化合物，Na是引起沾污结渣的根源。

So, it can be concluded that solution pervasion has great effect on mechanical characteristics of calcium thenardite rock salt.

因此，溶解渗透对钙芒硝盐岩的力学特性有着极大的影响。

It is greatly affected by the solubility of sodium sulfate, and one of the components is calcium thenardite.

实验结果表明，钙芒硝盐岩的渗透率为溶解渗透时间及渗透压的函数。

与thenardite相关的网络解释 [注：此内容来源于网络，仅供参考]

thenardite：无水芒硝

分子式: Na2SO4 CAS号:性质:又称无水芒硝(thenardite)或元明粉. 无色单斜细小结晶或白色粉末. 密度2.68g/cm3. 熔点884℃. 溶于水、甘油. 不溶于醇. 有吸湿性. 由天然芒硝经溶解,澄清,蒸发,增稠,离心分离,干燥制得. 亦可用钙芒硝矿石粉碎,

thenardite：天然无水芒硝

thenard's blue 藤氏蓝 | thenardite 天然无水芒硝 | theobromine 可可碱

thenardite：无水碱芒硝

thematic map 专题图 | thenardite 无水碱芒硝 | theodolite 经纬仪