单斜晶系
四面体
结晶学
晶体结构
Crystal(编程语言)
矿物
链条(单位)
分子
Atom(片上系统)
化学
群(周期表)
强度(物理)
材料科学
物理
光学
计算机科学
有机化学
天文
程序设计语言
嵌入式系统
作者
Judith A. Konnert,Howard T. Evans
摘要
The crystal structure of the new mineral erdite, NaFeS2.2H2O, has been determined from 263 counter-measured intensity data. The mineral is monoclinic, space group A/c, with a : 10.693(l), D : 9.1l5(l), c : s.507(4)4, B : 92.t7(2), Z : 4, D (X-ray) :2.217 g/cm3. Because of the poor quality of the crystals, the reliability index after anisotropic refinement was not better than 0.170, but the structure is clearly defined. FeSo tetrahedra form chains along the c direction by sharing edges. Each Na atom is coordinated to one edge of an FeSo tetrahedron, and to four HrO molecules. The Fe-S bond length is 2.25(l)A. The (FeSr), chain is very regular and consistent with the dimensions of similar chains previously described in KFeSr, RbFeSr, CsFeSr, and TlFeSr.
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