泥炭沼泽微地貌特征及其形成的水动力机制

Forming Environment and Mechanism of High Bog

草丘微地貌是泥炭沼泽重要的景观特征之一．根据对中国和白俄罗斯不同类型泥炭沼泽的野外观测，分析草丘微地貌的类型、结构和形态，论述了其发育和分布的基本规律，并对草丘微地貌形成的水动力机制做了初步探讨．

Formation of high bog environment is controlled by the internal and outer natural factors, and it is result of the factors controlling each other and effect together. In this paper, the formation reasons of high bog environment in Northeast China and Belarus and in the Western Siberia are studied, and the feature and rules of controlling factors of high bog environment in the frigid and temperate zone in the Northern Hemisphere are analysed. Finally, the formation mechanism of high bog environment is discussed.