众所周知,纤维泥炭的性状不能通过太沙基原理获得满意的解释。基于纤维泥炭的孔隙由有机体之间的大(外)孔隙和有机体内的微(内)孔隙组成。本文提出了纤维泥炭一维固结的近似分析方法。此法通过与现场观测数据对比,不雄看出,由推荐的模型得出的沉降结果与观测结果非常接近。 It is well known that the properties of fiber peat cannot be satisfactorily explained by the Taischiji principle. Fiber peat-based pores consist of large (outer) pores between organisms and micro (intra) pores within organisms. This paper presents an approximate analysis method for one-dimensional consolidation of fiber peat. This method compares with on-the-spot observational data, and does not see that the settling results obtained by the proposed model are very close to the observed results.