论文部分内容阅读
1 概述郑州至少林寺高速公路起点为郑州市西南绕城公路马寨村南1km 处,终点在登封市韩村以东约300m 左右,接豫03线,并与在建的少洛高速公路相连,线路全长53.25km,工程于2001年10月开工,预计2003年12月竣工,为河南省在建重点工程。路线通过地区西高东低,相对高差30～80m,丘谷相间,冲沟发育,地表多为耕地。上覆地层为第四系全新统、上更新统冲洪积黄土,具Ⅰ级非自重湿陷性,中更新统棕红色膨胀上,膨胀性弱～中等,局部及沟谷地带常分布有圆砾土、卵石土,下伏地层为寒武系石灰岩、白云质灰岩、白云岩、泥质灰岩及页岩、二迭系泥岩、砂岩。在石灰岩、白云质灰岩、白云岩地段,岩溶较发
1 Overview The starting point of Zhengzhou to Shaolin Expressway is 1km south of Mazhai Village in the southwest ring road of Zhengzhou City. The ending point is about 300m east of Hancun in Dengfeng City, connecting Yu-03 line and connecting with the under-construction Shaoxing Expressway The total length of the line is 53.25km. The project started in October 2001 and is expected to be completed in December 2003. It is a key project under construction in Henan Province. Route through the area west high low, the relative elevation of 30 ~ 80m, mounds and valleys, gully development, the surface mostly for arable land. The overlying strata are Quaternary Holocene, Upper Pleistocene alluvial loess, with Grade I non-weight collapsible, middle-Pleistocene brown-red swelling, weak expansibility ~ moderate, and local and gully areas are often distributed with round gravel Soil, pebble soil, under the formation of Cambrian limestone, dolomitic limestone, dolomite, argillite and shale, Permian mudstone, sandstone. In limestone, dolomitic limestone, dolomite lots, kfa more hair