泥炭沼泽起源及其发育特征的对比研究

Comparative Study on Origin and Development Feature of Peat Mire

通过对白俄罗斯别列金自然保护区与中国东北长白山地区典型泥炭沼泽的考察研究，从泥炭沼泽形成环境和泥炭层特征方面，详细地分析了道莫日里契科、萨弗斯克－莫赫和金川、哈尼四处泥炭沼泽的地表形态、植被类型以及泥炭剖面结构，泥炭类型等的异同性，提出泥炭沼泽形成实质是自然界中物质－能量转化过程中的必然产物，也是生物循环与地质循环过程中生物化学作用的结果．同时，泥炭沼泽的形成还与两地区特有的冰川和火山作用影响有着密切关系．

Typical kinds of peat mire in Berezinsky Natural Reserve in Belarus and in ChangBai Mountains in Northeast of China are explored and studied in this paper. The differenceand similarity of susrface form, vegetation twe, profile structure and type of peat in Daomorqike and Safusike - Mohe in Berezinsky Natural Reserve and in Jinchuan and Hani inChangBai Mountains are compared and analysed in detail. The formation of peat mire is actually a result of matter and energy transforming each other in the nature, it also is a out comeof biochemital effect.s in the course of biological and geological cycles. In the meantime, itsformation has a close relation to special glacial and volcanic action in two regions.