Rozenite - Wikipedia
Rozenite is a hydrous iron sulfate mineral, Fe 2+ SO 4 ·4(H 2 O). It occurs as a secondary mineral, formed under low humidity at less than 21 °C (70 °F) as an alteration of copper-free melanterite, which is a post mine alteration product of pyrite or marcasite. It also occurs in lacustrine sediments and coal seams.
火星上多水合硫酸盐矿床的候选矿物成分 rozenite (FeSO4·4H2O)
Rozenite (FeSO4·4H2O) 是火星地表和地下多水合硫酸盐沉积物的候选矿物成分。 为了更好地了解其在火星表面普遍存在的温度条件下的行为，并帮助其在正在进行和未来的漫游者任务中进行识别，我们对矿物的结构和特性进行了实验和计算相结合的研究。
Rozenite (Fe(SO4).4H2O) | FeH8O8S | CID 182426 - PubChem
Rozenite (Fe (SO4).4H2O) | FeH8O8S | CID 182426 - structure, chemical names, physical and chemical properties, classification, patents, literature, biological activities, safety/hazards/toxicity information, supplier lists, and more.
Rozenite Mineral Data
Named for Zygmunt Rozen (1874-1936), mineralogist and petrographer, Academy of Mining and Metallurgy, Kracow, Poland. Comments: White powdery rozenite coating with yellow ferrinatrite on purple copiapite. Location: Le Cetine Mine, Siena, Tuscany, Italy. Scale: See Photo.
Low-temperature crystallography and vibrational properties of rozenite …
2023年6月1日 · Rozenite (FeSO 4 ·4H 2 O) is a candidate mineral component of the polyhydrated sulfate deposits on the surface and in the subsurface of Mars. To better understand its behavior at temperature conditions prevailing on the Martian surface and aid its identification in ongoing and future Rover missions, we have carried out a combined experimental ...
Mineral Group: Rozenite group. Occurrence: An uncommon secondary mineral, formed at or below 21 C and under low humidity directly from copper-free melanterite, in turn an alteration product of pyrite or
Rozenite: Mineral information, data and localities.
Rozenite Baur W H (1962) Zur kristallchemie der salzhydrate. Die kristallstrukturen von MgSO4*4H2O (leonhardtit) und FeSO4*4H2O (rozenit) Acta Crystallographica 15 815-826
Spectral and Chemical Characterization of Copiapite and Rozenite …
2021年8月5日 · Copiapite (Fe 2+ Fe 3+4 (SO 4) 6 (OH) 2 ∙ 20 H 2 O) and rozenite (Fe 2+ (SO 4) ∙ 4H 2O) are secondary hydrous sulfate minerals, mostly formed because of oxygenation and weathering events of primary sulfides on Earth.
四水白铁矾Rozenite | 国学百科
四水白铁矾Rozenite. 化学成分：Fe2+SO4．4H2O物理性质：水绿矾若在干热环境下，则脱水而粉化成四水白铁矾，若再不充份之氧化，则转变为叶绿矾。
Raman, MIR, VNIR, and LIBS Spectra of Szomolnokite, Rozenite, …
1997年10月12日 · Jarosite, rozenite (FeSO 4 ·4H 2 O), and szomolnokite (FeSO 4 ·H 2 O) have been proposed to exist on Mars by OMEGA and CRISM [29, 30]. These findings imply that Mars once had conditions favorable for the formation of ferrous sulfate, such as acidic and habitable environments with the presence of liquid water [29, 30, 31, 32].
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