Abstract: Based on investingations in-situ to highway tympanites along G218 and G313 , the authors found reasonably maeterial environment for highway tympanites to develop in this paper , i .e clay content is 40 % or so while water content is 25 % or so .Highway tympanites can be classified into two types :climate tympanites and dynamic tympanites . Tympanites pingo are shown for highway tympanites to occur .Tympanites pingo are circle in crankle road and tympaites pingo are ellipse in longitudinal road .In the section of roadbase , tympanites pingo often form below 30 or 40 centimeter of road surface .According to tympanites pingo crack , we can identify the type of tympanites and scale and depth of clay lens

Key words: chill region , highway tympanites , climate tympanites , dynamic tympanites , tympanites pingo

摘要： 笔者基于对新疆国道218线和省道313线道路翻浆的长期现场观测和研究，比较客观地构筑了道路翻浆发 生的物质环境，即路床中40%左右的粘土含量和25%左右的含水量。道路翻浆可以分为气候翻浆和动力翻浆两大 类型，路床中存在粘土透镜是翻浆发育的必备条件。翻浆鼓丘是道路翻浆的直观体现。翻浆鼓丘呈椭圆形及圆 形，椭圆形鼓丘主要出现在平直公路段，圆形鼓丘主要出现在弯曲公路段。路基中道路翻浆通常发生在路面基层 以下30—40cm的路床范围内。根据鼓丘龟裂纹可以反演翻浆类型，并判识粘土透镜的位置

关键词: 高寒地区, 道路翻浆, 动力翻浆, 翻浆鼓丘