首页> 外文期刊>Geology of Ore Deposits: A Journal of Theoretical and Applied Papers on All Aspects of Ore Genesis >Cocrystallization of Isomorphic Components in Solutions and Crystal Zoning:An Example of the (Bia,Pb)(NO3)2 Series
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Cocrystallization of Isomorphic Components in Solutions and Crystal Zoning:An Example of the (Bia,Pb)(NO3)2 Series

机译:溶液中同晶组分的共结晶和晶体分区:(Bia,Pb)(NO3)2系列的一个例子

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摘要

The phase equilibrium and growth of mixed (Ba,Pb)(NO3)2 crystals in aqueous solutions were investigated.The microcrystallization method was adapted to systems with isomorphic components,where crystal composition deviates from the thermodynamic equilibrium even at a low supercooling.The solid phase is characterized by continuous miscibility of the components within the analyzed ranges of temperature and solution composition.The diagram is characterized by substantial nonlinearity of the solubility isotherms and nonuniformity of the solid isocomposite location.Quasiequilibrium paths change their slope depending on solution enrichment in Ba(NO3)2 and depletion in Pb(NO3)2.The area of curvature of quasiequilibrium paths is coordinated with the area of the changing isotherm slope,i.e.,the area of "remarkable" points,where the behavior of the system changes drastically.Examples of theoretical zoning of a crystal approximated to a sphere were calculated for paths at a temperature decreasing from 50 to 15°C.The content of the Ba component decreases toward the periphery with the consecutive overgrowing of zones.Each zone corresponds to one gram of (Ba,Pb)(NO3)2.Crystals grown from different initial solutions consist of different numbers of zones owing to the nonlinearity of solubility isotherms.Specific features of mixed crystal formation should be taken into account in genetic interpretation of natural minerals of mixed composition.
机译:研究了混合(Ba,Pb)(NO3)2晶体在水溶液中的相平衡和生长。微晶化方法适用于具有同晶成分的系统,即使在低过冷度下,其晶体组成也会偏离热力学平衡。相的特征是在所分析的温度和溶液组成范围内,各组分具有连续的可混溶性;该图的特征是溶解度等温线存在很大的非线性,以及固相复合物位置的不均匀性。准平衡路径的变化取决于Ba( NO3)2和Pb(NO3)2中的耗尽。准平衡路径的曲率面积与等温线变化斜率的面积(即“显着”点的面积)协调,系统的行为会发生剧烈变化。计算了温度降低f时路径的近似于球形的晶体的理论分区数在50至15°C范围内,随着区域的连续过度生长,钡成分的含量向外围降低,每个区域对应一克(Ba,Pb)(NO3)2克。由于溶解等温线是非线性的,因此区域的数目会增加。在混合成分天然矿物的遗传解释中应考虑混合晶体形成的特定特征。

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