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采用原子吸收光谱和等离子体发射光谱等现代仪器分析方法对大兴安岭泥炭垂直剖面中Ｃｕ、Ｐｂ、Ｚｎ、Ｃｄ、Ｈｇ、Ｃｒ、Ｎｉ、Ｃｏ、Ｍｎ、Ｓｒ、Ｂａ、Ｂ等１２种微量元素进行了测定，结果表明，大兴安岭地区古莲、图强泥炭地和同一泥炭地沼泽泥炭发育的不同阶段，微量元素含量分布规律不十分明显，与俄罗斯典型同类泥炭相比，Ｍｎ含量俄罗斯泥炭明显高于大兴安岭泥炭，Ｚｎ、Ｃｏ、Ｂ含量大兴安岭泥炭明显高于俄罗斯泥炭。大兴安岭高位泥炭中，微量元素特别是与人类活动密切相关的重金属，由下层到上层其含量有明显增高的特点，具有较重要的环境意义。通过不同地区高位泥炭微量元素地球化学谱的研究，可以再现人类活动影响下大气污染的历史
The trace elements such as Cu, Pb, Zn, Cd, Hg, Cr, Ni, Co, Mn, Sr, Ba and B in the vertical profile of the peat in the Daxing’anling were measured by modern instruments such as atomic absorption spectrometry and plasma emission spectrometry The results showed that the distribution of trace elements in different stages of the development of peat in GuLian, Tuqiang peatland and same peatland in Daxinganling area was not obvious. Compared with the typical peat in Russia, the content of Mn in Russian peat was significantly higher than that in Daxinganling Peat, Zn, Co, B content Greater Khingan Range Peat was significantly higher than Russian peat. Among the peat in the Greater Hinggan Mountains, trace elements, especially heavy metals closely related to human activities, have a significantly higher content from the lower layer to the upper layer, and have more important environmental significance. Through the study of trace element geochemical spectra of peat in different areas, we can reproduce the history of air pollution under the influence of human activities