东南大学学报(自然科学版)
東南大學學報(自然科學版)
동남대학학보(자연과학판)
Journal of Southeast University (Natural Science Edition)
2015年
5期
975-979
,共5页
张中琼%吴青柏%刘永智%温智
張中瓊%吳青柏%劉永智%溫智
장중경%오청백%류영지%온지
沥青路面%降雨%透水性%水分%地温
瀝青路麵%降雨%透水性%水分%地溫
력청로면%강우%투수성%수분%지온
asphalt pavement%rainfall%permeability%moisture%ground temperature
通过对青藏高原北麓河地区大气降水以及沥青路面和砂砾路面下部浅层土体水热变化的连续监测,分析路面结构中降水、地温以及水分变化之间的关系.结果表明,在降雨时段,5 cm 深度土体水分增加,沥青路面下部土体的水分增量约为砂砾路面的2倍.砂砾路面20 cm 及以下深度范围水分增加,而沥青路面下部水分变化量小于0.3%.砂砾路面下部土体间存在良好的水力联系,沥青路面结构中的隔水层阻隔了层中水热交换.面层中水分的波动与降水密切相关,基层水分变化受地温控制.路面结构的隔水层增加了面层的蒸发量,同时造成层下水分的大量聚集和路基储热量的增加,表现为基层地温明显高于面层.水热交换的差异是造成沥青路面热效应的重要原因之一.
通過對青藏高原北麓河地區大氣降水以及瀝青路麵和砂礫路麵下部淺層土體水熱變化的連續鑑測,分析路麵結構中降水、地溫以及水分變化之間的關繫.結果錶明,在降雨時段,5 cm 深度土體水分增加,瀝青路麵下部土體的水分增量約為砂礫路麵的2倍.砂礫路麵20 cm 及以下深度範圍水分增加,而瀝青路麵下部水分變化量小于0.3%.砂礫路麵下部土體間存在良好的水力聯繫,瀝青路麵結構中的隔水層阻隔瞭層中水熱交換.麵層中水分的波動與降水密切相關,基層水分變化受地溫控製.路麵結構的隔水層增加瞭麵層的蒸髮量,同時造成層下水分的大量聚集和路基儲熱量的增加,錶現為基層地溫明顯高于麵層.水熱交換的差異是造成瀝青路麵熱效應的重要原因之一.
통과대청장고원북록하지구대기강수이급력청로면화사력로면하부천층토체수열변화적련속감측,분석로면결구중강수、지온이급수분변화지간적관계.결과표명,재강우시단,5 cm 심도토체수분증가,력청로면하부토체적수분증량약위사력로면적2배.사력로면20 cm 급이하심도범위수분증가,이력청로면하부수분변화량소우0.3%.사력로면하부토체간존재량호적수력련계,력청로면결구중적격수층조격료층중수열교환.면층중수분적파동여강수밀절상관,기층수분변화수지온공제.로면결구적격수층증가료면층적증발량,동시조성층하수분적대량취집화로기저열량적증가,표현위기층지온명현고우면층.수열교환적차이시조성력청로면열효응적중요원인지일.
By continuously monitoring the precipitation and soil hydro-thermal changes in a shallow part under the asphalt and sand pavement in Beiluhe area on the Qinghai-Tibetan Plateau,the rela-tionships between precipitation,temperature and moisture change in pavement structure are ana-lyzed.The results show that during the rainfall period,the moisture of the soil of 5 cm depth under pavement increases,and the moisture increment in the soil under asphalt pavement is twice over that under sand pavement.In the deeper part of more than 20 cm depth,the moisture of the soil under sand pavement increases,while that under asphalt pavement varies only by less than 0.3%.Under sand pavement,there is a good hydraulic connection between the soil bodies in roadbed.However, in the asphalt pavement structure,the impermeable layer inhibits hydrothermal exchange obviously. Moisture changes are closely related to precipitation in the surface layer and controlled by the ground temperature in the base course.The impermeable layer of the asphalt pavement structure increases the evaporation capacity in the surface layer and causes abundant moisture accumulation under the impermeable layer and the increase of heat storage in roadbed.As a result,the temperature in the base course is significantly higher than that in the surface layer.Therefore,the difference between hydrothermal exchanges is one of the important reasons for asphalt pavement thermal effects.