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根据天山乌鲁木齐河源地区的一个完整年周期的大气降水样品、１ 号冰川连续雪坑样品及浅冰芯样品的ｐ Ｈ 和电导率资料， 初步探讨冰芯ｐ Ｈ 和电导率记录的形成过程和影响因素结果表明， 降水沉积后的粒雪化过程和成冰作用过程中样品的ｐ Ｈ 和电导率有较大的变化， 但两者之间仍基本保持正相关关系这说明在消融率较大和融水渗浸作用较强的内陆地区， 仍可以根据冰芯的ｐ Ｈ 和电导率记录合理地反演沉积时的大气环境状况
According to the p H and conductivity data of a complete annual cycle of precipitation in the Heyuan area, Urumqi, Tianshan Mountains, p H and conductivity data of continuous samples of glaciers in No. 1 glacier and samples of shallow ice cores, the formation process and influence of p H and conductivity records in ice cores Factors The results show that the p H and conductivity of samples during the process of grain snow precipitation and ice formation have a greater change, but still maintain a positive correlation between the two This shows that in the ablation rate Inland areas with large and melt infiltration can still reasonably retrieve the atmospheric conditions during deposition based on the p H and conductivity records of ice cores