Sanches R, Melo W L, Colombo M F
Biochim Biophys Acta. 1986 Nov 7;874(1):19-22. doi: 10.1016/0167-4838(86)90096-8.
The oxygenation and autoxidation of lyophilized human carbonmonoxyhemoglobin (Hb-CO) kept in environments with different relative humidities were followed with time using visible absorption spectroscopy. The sample kept at 68% relative humidity was the one with the greatest formation of methemoglobin (Met-Hb), while for increasing or decreasing hydrations the Met-Hb content decreased gradually. Besides the presence of Met-Hb, it was observed that the samples kept above about 68% relative humidity were converted to oxyhemoglobin (Hb-O2), the samples kept in the range 45-68% relative humidity were a mixture of Hb-CO and Hb-O2, while the samples kept below about 45% relative humidity and the solution sample continued as Hb-CO. Hemoglobin has, therefore, two critical hydration values, 45% and 68% relative humidity, which correspond to about 0.12 and 0.18 g H2O/g protein, respectively.
使用可见吸收光谱法,跟踪在不同相对湿度环境下保存的冻干人碳氧血红蛋白(Hb-CO)的氧化和自氧化随时间的变化情况。保存在相对湿度为68%的样品中高铁血红蛋白(Met-Hb)的生成量最大,而随着湿度增加或降低,Met-Hb含量逐渐降低。除了存在Met-Hb外,还观察到保存在相对湿度约68%以上的样品转化为氧合血红蛋白(Hb-O2),保存在相对湿度45-68%范围内的样品是Hb-CO和Hb-O2的混合物,而保存在相对湿度约45%以下的样品以及溶液样品则保持为Hb-CO。因此,血红蛋白有两个临界水合值,相对湿度分别为45%和68%,分别对应约0.12和0.18 g H2O/g蛋白质。