玄武岩台地滑坡与土壤发生学类型研究  

Study on the Relationship between Landslide and Soil Genesis Characteristics in Basalts Platform Region

作　　者：王深法[1] 俞建强[1] 陈和平[1] 陆景冈[1] 

机构地区：[1]浙江大学资源科学系,杭州310029

出　　处：《浙江地质》2002年第1期76-81,共6页Geology of Zhejiang

基　　金：浙江省重点科研项目 (001103213)

摘　　要：本文通过研究浙江省玄武岩台地地区滑坡与土壤发生学类型之间的关系 ,结果表明 :滑坡主要产生在棕泥土 (新明系 )和棕泥田 (城塘系 )土壤上 ,有时也发生在黄粘泥 (大岚系 )土壤上。但是 ,在这个区域内很少有滑坡发生在红粘泥 (沈塘系 )和山黄粘泥 (项白山系 )上。This paper studied the relationships between landslides and soil genesis characteristics in the region of the basalt platform in Zhejiang province.Results showed that landslides mainly occurred on the brown earth(Xing ming xi)and paddy field on brown muddy soil(Cheng xi xi),sometimes they also occur on the yellowish bole soil(De lan xi),but in this region few landslides occur on the bole soil(Shen tang xi)or mountain yellowish bole soil(Xiang bai shan xi).We found the main factor about the occurrence of landslides was the degree of soil development.

关 键 词：玄武岩台地 滑坡 土壤发生学类型 棕泥土 黄粘泥 红粘泥 

分 类 号：P642.22[天文地球—工程地质学] S151[天文地球—地质矿产勘探]