The relationship between water-depth and discharge of overbank flows is very different form inbank flow.
水流在天然河道中极
常见,尤其在冲积平原地区。
The relationship between water-depth and discharge of overbank flows is very different form inbank flow.
水流在天然河道中极
常见,尤其在冲积平原地区。
Site soils in southern area of Jiangsu province belong to washland sediment or limnetic facies sediment.The components of sediment are very complex and process of sedimentation is in disorder.
苏南地区场地主要
相、湖沼相或冲湖相新近沉积软弱
,结构松
,沉积零乱,成分复杂,饱水可液化
细砂
及
较
发育,在地震或动力荷载的作用下有可能发生软
震陷或砂
液化。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
The relationship between water-depth and discharge of overbank flows is very different form inbank flow.
漫滩水流天然河道中极为常见,尤
积平原地区。
Site soils in southern area of Jiangsu province belong to washland sediment or limnetic facies sediment.The components of sediment are very complex and process of sedimentation is in disorder.
苏南地区场地土主要为漫滩相、湖沼相或湖相新近沉积软弱土,结构松
,沉积零乱,成分复杂,饱水可液化粉细砂层及粉土层较为发育,
地震或动力荷载的作
有可能发生软土震陷或砂土液化。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
The relationship between water-depth and discharge of overbank flows is very different form inbank flow.
漫滩水流在天然河道中极为常见,尤其在冲积平原地区。
Site soils in southern area of Jiangsu province belong to washland sediment or limnetic facies sediment.The components of sediment are very complex and process of sedimentation is in disorder.
苏南地区场地土主要为漫滩相、湖沼相或冲湖相新近沉积软弱土,结构松,沉积零乱,成分复杂,饱水可液化粉细砂层及粉土层较为发育,在地震或动力荷载的作用下有可能发生软土震陷或砂土液化。
声明:以上、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
The relationship between water-depth and discharge of overbank flows is very different form inbank flow.
漫滩水流在天然河道中极为常见,尤其在冲积平原地区。
Site soils in southern area of Jiangsu province belong to washland sediment or limnetic facies sediment.The components of sediment are very complex and process of sedimentation is in disorder.
苏南地区场地土主要为漫滩、
或冲
新近沉积软弱土,结构松
,沉积零乱,成分复杂,饱水可液化粉细
粉土
较为发育,在地震或动力荷载的作用下有可能发生软土震陷或
土液化。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
The relationship between water-depth and discharge of overbank flows is very different form inbank flow.
漫滩水流在天然河道中极为常见,尤其在冲积区。
Site soils in southern area of Jiangsu province belong to washland sediment or limnetic facies sediment.The components of sediment are very complex and process of sedimentation is in disorder.
苏南区场
土主要为漫滩相、湖沼相或冲湖相新近沉积软弱土,结构松
,沉积零乱,成分复杂,饱水可液化粉细砂层及粉土层较为发育,在
震或动力
作用下有可能发生软土震陷或砂土液化。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件观点;若发现问题,欢迎向我们指正。
The relationship between water-depth and discharge of overbank flows is very different form inbank flow.
漫滩水流在天然河道中极为常见,尤其在冲积平原。
Site soils in southern area of Jiangsu province belong to washland sediment or limnetic facies sediment.The components of sediment are very complex and process of sedimentation is in disorder.
南
场
土主要为漫滩相、湖沼相或冲湖相新近沉积软弱土,结构松
,沉积零乱,成分复杂,饱水可液化粉细砂层及粉土层较为发育,在
震或
载的作用下有可能发生软土震陷或砂土液化。
声明:以上例句、词性分类均由互联网资源自生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
The relationship between water-depth and discharge of overbank flows is very different form inbank flow.
漫滩水流在天然河道中极为常见,尤其在冲积平原地区。
Site soils in southern area of Jiangsu province belong to washland sediment or limnetic facies sediment.The components of sediment are very complex and process of sedimentation is in disorder.
苏南地区场地土主要为漫滩、湖
冲湖
新近沉积软弱土,结构松
,沉积零乱,成分复杂,饱水可液化
层及
土层较为发育,在地震
动力荷载的作用下有可能发生软土震陷
土液化。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
The relationship between water-depth and discharge of overbank flows is very different form inbank flow.
流在天然河道中极为常见,尤其在冲积平原地区。
Site soils in southern area of Jiangsu province belong to washland sediment or limnetic facies sediment.The components of sediment are very complex and process of sedimentation is in disorder.
苏南地区场地土主要为相、湖沼相或冲湖相新近沉积软弱土,结构松
,沉积零乱,成分复杂,饱
可液
粉细砂层及粉土层较为发育,在地震或动力荷载的作用下有可能发生软土震陷或砂土液
。
:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
The relationship between water-depth and discharge of overbank flows is very different form inbank flow.
漫滩流在天然河道中极为常见,尤其在冲积平原地区。
Site soils in southern area of Jiangsu province belong to washland sediment or limnetic facies sediment.The components of sediment are very complex and process of sedimentation is in disorder.
苏南地区场地土主要为漫滩相、湖沼相或冲湖相积软弱土,结构松
,
积零乱,成分复
,
可液化粉细砂层及粉土层较为发育,在地震或动力荷载的作用下有可能发生软土震陷或砂土液化。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。