n.[矿物]黄钾铁矾
jarosites───n.[矿物]黄钾铁矾
Aaronite───硅灰石
Maronite───n.马龙派教徒（流行于黎巴嫩的天主教教派）
amosite───n.[矿物]铁石棉
favosite───腐殖石
jarovise───雅罗维斯
jarovize───vt.实施人工方法使植物早熟
parasite───n.寄生虫；食客
jargonise───vt.用术语讲；vi.用术语讲
But jarosite on Earth incorporates all kinds of microorganisms into its crystalline structure.───但地球上黄钾铁矾的晶体结构中含有各种微生物。
an exploration robot discovered jarosite.───一个探索机器人发现了黄钾铁矾。
Jarosite is a yellowish-brown mineral with a crystalline structure that's also found on earth.───黄钾铁矾是一种黄褐色的矿物，它的晶体结构也存在于地球上。
Adsorption and Coprecipitation of Dissolved Metals with Jarosite under Conditions Simulating Sewage Sludge Bioleaching───污泥生物淋滤过程中黄铁矾对重金属离子的吸附与共沉淀作用的模拟研究
The formation conditions of jarosite and its environmental significance───黄钾铁矾的形成条件研究及其环境意义
Biosynthesis and Characterization of Jarosite───黄钾铁矾的生物合成与鉴定
Application of Neural Network in Jarosite Process of Zinc Hydrometallurgy───神经网络技术在湿法炼锌矾法除铁中的应用
Behavior of Antimony in Jarosite Precipitation───锑在沉矾过程中的行为
Preparation of Ni-Zn ferrite from sodium jarosite residue───用黄钠铁矾渣制备复合镍锌铁氧体
Most iron can be removed through jarosite process. The content of zinc sulfate can reach more than 98% by evaporating , cooling, crystallization and centrifuging.
The preparation of Ni - Zn ferrite from sodium jarosite residue was studied.
Because of using zinc hydrometallurgy process of jarosite process, the leaching rate of zinc may reach 97% and this line can produce high quality zinc continuously and steadily.
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The industrial tests show that the jarosite process can be used to handle the zinc calcine with high concentration of Sb by controlling the leaching rate of Sb in the neutral leaching process.
This paper covers production practice of jarosite process in hot-acid leaching and comparison between iron hydroxide process and jarosite process that are used for iron removal.
Jarosite process was selected for iron removal due to the characteristics of the solution originated from the reduction leaching of manganese nodules by pyrite in chloride system.
Jarosite is a major secondary mineral formed in acid supergene environment by oxidation of metal sulphide.
The bulk of the native aluminium occurs in cracks in and along boundaries of jarosite, and only a small amount is present in and along the grain boundaries of quartz.