浅层地震反射波法在水域地质勘察中的应用
摘要:鉴于传统钻孔勘探确定淤泥层起伏情况的不足,在某一围堤水域地质勘察中利用浅层地震反射波法,确定淤泥层的起伏情况。从本场地反射波法物探映像图中可知,淤泥层与粘土层之间的界限明显,均在30s~(-3)左右产生了明显的反射波,且能清楚的看到基岩面的起伏情况。经过与钻探资料的对比发现,物探结果精度较高,满足了该工程的技术要求。分析表明,浅层地震反射波法是一种速度快、效率高的水域工程物探新方法,在各种水域工程的岩土工程勘察中有着广阔的应用前景。
Abstract:Because of the weakness in determining of the mud layer waving situation in traditional drilling exploration, we always use the shallow seismic reflected wave method in some retaining dike to determin the mud layer's waving situation. From the reflectional geophysical prospecting image of this water area, we know that there's a absolute line between slit layer and clay layer. There's a clear reflective wave in 30m,and it can be easily seem the moving situation of the bedrock surface. Compared with the drilling information, geophysical prospecting is more accuracy, and meets the requirment of this project. It shows that the shallow seismic reflected wave method is the fast, efficient new method in water project geophysical prospecting. It has the broad application prospects in a variety of geotechnical engineering investigation.
中文标题：
浅层地震反射波法在水域地质勘察中的应用
Application of Seismic Reflected Wave Method in the Geotechnical Engineering Investigation
作者：
王霞,马小跃
WANG Xia,MA Xiaoyue
作者简介:王霞,1984年生,女,汉族,山东青岛人,吉林大学勘查技术与工程专业,学士学位,助理工程师,主要从事工程检测工作。E-mail:wangxia_37@163.com
通讯地址：
中船勘察设计研究院有限公司, 上海 200063
ChinaShipbuildingIndustryInstituteoftheEngineeringInvestingation&DesignCo.Ltd,shanghai200063,China
中图分类号:TU195
doi:10.3969/j.issn.1007-2993.2010.06.008
出版物：岩土工程技术
收稿日期:2010-08-16
网络出版日期:2021-07-06
关键词:浅层地震反射波法,数据处理,GPS导航
Key words:seismic reflected wave method,data processing,GPS navigation
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