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Deliquescence Relative Humidities of Organic and Inorganic Salts Important in the Atmosphere

机译:重要的有机和无机盐的潮解相对湿度

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摘要

The deliquescence relative humidities (DRH) as a function of temperature have been determined for several salts of atmospheric importance using humidity controlled thermogravimetric analysis (HTGA): sodium hydrogen oxalate monohydrate (NaHC2O4H2O), sodium oxalate (Na2C2O4), sodium ammonium sulfate dihydrate (NaNH4SO4.2H(2)O, lecontite), sodium hydrogen malonate monohydrate (NaHC3H2O4.H2O), sodium malonate monohydrate (Na2C3H2O4.H2O), and ammonium hydrogen malonate (NH4HC3H2O4). The temperature dependent onset DRH values (where a dry mixture begins to take up water) were also determined for mixtures of ammonium sulfate with malonic acid, and ammonium sulfate with sodium oxalates and sodium malonates, respectively. We demonstrate that the onset DRH is independent of the ratio of solids in the mixture. In general, onset DRH values were always lower than the pure component DRH values.
机译:已使用湿度控制热重分析(HTGA)确定了几种具有大气重要性的盐的潮解相对湿度(DRH)与温度的关系:草酸氢钠一水合物(NaHC2O4H2O),草酸钠(Na2C2O4),硫酸钠二水合硫酸钠(NaNH4SO4 .2H(2)O,方沸石,丙二酸氢钠一水合物(NaHC3H2O4.H2O),丙二酸一钠水合物(Na2C3H2O4.H2O)和丙二酸氢铵(NH4HC3H2O4)。还分别确定了硫酸铵与丙二酸的混合物和硫酸铵与草酸钠和丙二酸钠的混合物的温度相关的起始DRH值(干燥的混合物开始吸收水)。我们证明,DRH的起始与混合物中固体的比例无关。通常,起始DRH值始终低于纯组分DRH值。

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