首页> 外文期刊>The Journal of Chemical Thermodynamics >Solid-solute phase equilibria in aqueous solution. XVI. Thermodynamic properties of malachite and azurite-predominance diagrams for the system Cu~(2+)-H_2O-CO_2
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Solid-solute phase equilibria in aqueous solution. XVI. Thermodynamic properties of malachite and azurite-predominance diagrams for the system Cu~(2+)-H_2O-CO_2

机译:水溶液中的固溶相平衡。十六。 Cu〜(2 +)-H_2O-CO_2系统的孔雀石和铜绿石优势图的热力学性质

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摘要

The thermodynamic properties of the copper carbonates malachite, Cu_2(OH)_2CO_3, and azurite, Cu_3(OH)_2(CO_3)_2, have been obtained from solubility measurements as a function of temperatures as well as ionic strength of aqueous perchlorate media. First, solubility constants have been determined from T = 288.15 K to T = 338.15 K at constant ionic strength, I = 1.00 mol ·kg~(-1) NaClO_4. Second, solubility experiments have been carried out from I = 1.00 mol·kg~(-1) to I = 3.00 mol·kg~(-1) NaClO_4 at constant temperature. T = 298.15 K. All experimental data have been evaluated by application of the optimization routeine of CheMSage, yielding an internally consistent set of thermodynamic properties for malachite (T = 298.15 K): log ~*K_pso~O(mal.) = (6.34 (+-) 0.10), DELTA_fG_m~o{Cu_2(OH)_2CO_3} = (-0903.3 (+-) 1.2) kJ·mol~(-1), DELTA_fH_m~o{Cu_2(OH)_2CO_3} = (-1067.1 (+-) 3.4) kJ ·mol~(-1), S_m~o{Cu_2(OH)_2CO_3} = (166.3 (+-) 2.5) J·mol~(-1)·K~(-1); and azurite (T = 298.15 K): log ~*K_pso~o(azu.) = (6.30 (+-) 0.10), DELTA_fG_m~o{Cu_2(OH)_2(CO_3)_2} = (-1434.2 (+-) 1.8) kJ·mol~(-1), DELTA_fH_m~o{Cu_3(OH)_2(CO_3)_2} = (-1675.1 (+-) 5.1 ) kJ·mol~(-1), S_M~o{Cu_3(OH)_2(CO_3)_2} = (254.4 (+-) 3.8) J·mol~(-1)·K~(-1). Wheras these results confirm the literature data for the standard molar entropies, new values for the standard molar enthalpy of formation of malachite and azurite are recommended.Moreover the phase relations in the ternary system Cu~(2+) - H_2O -CO_2 are discussed by the construction of two-dimensional as well as three-dimensional predominance diagrams.
机译:碳酸铜孔雀石Cu_2(OH)_2CO_3和蓝铜矿Cu_3(OH)_2(CO_3)_2的热力学性质已根据温度和高氯酸盐水溶液的离子强度从溶解度测量获得。首先,在恒定离子强度I = 1.00 mol·kg〜(-1)NaClO_4的条件下,已从T = 288.15 K到T = 338.15 K确定了溶解度常数。其次,在恒定温度下从I = 1.00 mol·kg〜(-1)到I = 3.00 mol·kg〜(-1)NaClO_4进行了溶解度实验。 T = 298.15K。所有化学实验数据均已通过应用CheMSage优化路线进行了评估,得出了孔雀石的一组内部一致的热力学性质(T = 298.15 K):log〜* K_pso〜O(mal。)=(6.34 (+-)0.10),DELTA_fG_m〜o {Cu_2(OH)_2CO_3} =(-0903.3(+-)1.2)kJ·mol〜(-1),DELTA_fH_m〜o {Cu_2(OH)_2CO_3} =(--1067.1 (+-)3.4)kJ·mol〜(-1),S_m_o {Cu_2(OH)_2CO_3} =(166.3(+-)2.5)J·mol〜(-1)·K〜(-1);和青铜石(T = 298.15 K):log〜* K_pso〜o(azu。)=(6.30(+-)0.10),DELTA_fG_m〜o {Cu_2(OH)_2(CO_3)_2} =(-1434.2(+- )1.8)kJ·mol〜(-1),DELTA_fH_m〜o {Cu_3(OH)_2(CO_3)_2} =(-1675.1(+-)5.1)kJ·mol〜(-1),S_M〜o {Cu_3 (OH)_2(CO_3)_2} =(254.4(+-)3.8)J·mol〜(-1)·K〜(-1)。这些结果证实了标准摩尔熵的文献数据,推荐了孔雀石和蓝铜矿形成的标准摩尔焓的新值。此外,还讨论了三元体系Cu〜(2+)-H_2O -CO_2的相关系。二维和三维优势图的构建。

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