摘要
淤泥质软土是福建地区分布最为广泛的地质条件之一,对其的处理方法和工艺也不尽相同,结合福建地区工程实际,对淤泥质软土地基处理相关问题进行粗浅的分析。
The peaty soils are formed at the late Quaternary geological stage by the deltaic fluvial, marine tidal and lake sedi ments. This is one of the widely distributed soils in Fujian Province. This paper discusses the different soil improvement meth ods that are successfully used in the actual projects.
出处
《土工基础》
2013年第6期78-80,共3页
Soil Engineering and Foundation
关键词
淤泥
地基处理
福建地区
Peaty Soft Soils
Soil Improvement
Fujian Area
