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众所周知,Terzaghi固结理论不能确切地解释纤维泥炭的特性。纤维状泥炭中存在两类孔隙,一类是有机物之间的宏观孔隙(外部孔隙),另一类是存在于有机物内部的微观孔隙。本文基于这一事实提出了纤维状泥炭一维固结过程的近似分析方法。该方法与现场观测结果比较后发现,两者具有十分相近的结果。
It is well known that Terzaghi’s theory of consolidation does not exactly explain the properties of fiber peat. There are two kinds of pores in fibrous peat, one is the macroscopic pores (external pores) between organic matter and the other is the micro pores existing in the organic matter. Based on this fact, this paper presents an approximate analysis method for the one-dimensional consolidation process of fibrous peat. Comparing this method with the field observations, we found that the two methods have very similar results.