首页 | 本学科首页   官方微博 | 高级检索  
     检索      

Subsurface Airflow Induced by Natural Forcings
引用本文:JiuJ.Jiao LIHai-long.Subsurface Airflow Induced by Natural Forcings[J].地球科学进展,2004,19(3):415-421.
作者姓名:JiuJ.Jiao  LIHai-long
作者单位:University of
基金项目:CommitteeonResearchandConferenceGrants (CRCG)attheUniversityofHongKong .
摘    要:Subsurface airflow can be induced by natural processes,such as atmospheric or barometric pressure changes, water table fluctuations,topographic effects,and rainfall infiltration.Barometric pressure fluctuations are the most common cause of subsurface airflow,which can be significant under favourable geological conditions.This process has been studied most extensively because of its application to passive soil vapor extraction.Soil airflow induced by water table fluctuations can be significant,particularly where the fluctuations are of high frequency,for example,in tidal-influenced coastal areas.Top-ographic effects can lead to strong subsoil airflow in areas with great elevation differences.Rainfall infiltration usually produces only weak airflow.Air flow induced by these natural processes has important environmental and engineering implications.Among the different processes,airflow induced by tidal fluctuations has been studied the least,although it has exciting applications to coastal engineering projects and environmental remediation.

关 键 词:Airflow  Unsaturated  zone  Natural  forcings

Subsurface Airflow Induced by Natural Forcings
Jiu J.Jiao,LI Hai-long.Subsurface Airflow Induced by Natural Forcings[J].Advance in Earth Sciences,2004,19(3):415-421.
Authors:Jiu JJiao  LI Hai-long
Institution:University of HongKong,HongKong,China;Anshan Normal University,Anshan 114005,Liaoning,China
Abstract:Subsurface air flow can be induced by natural processes, such as atmospheric or barometric pressure changes, water table fluctuations, topographic effects, and rainfall infiltration. Barometric pressure fluctuations are the most common cause of subsurface air flow, which can be significant under favourable geological conditions. This process has been studied most extensively because of its application to passive soil vapor extraction. Soil air flow induced by water table fluctuations can be significant, particularly where the fluctuations are of high frequency, for example, in tidal-influenced coastal areas. Topographic effects can lead to strong subsoil air flow in areas with great elevation differences. Rainfall infiltration usually produces only weak airflow. Air flow induced by these natural processes has important environmental and engineering implications. Among the different processes, air flow induced by tidal fluctuations has been studied the least, although it has exciting applications to coastal engineering projects and environmental remediation.
Keywords:Airflow Unsaturated zone Natural forcings
本文献已被 CNKI 维普 万方数据 等数据库收录!
点击此处可从《地球科学进展》浏览原始摘要信息
点击此处可从《地球科学进展》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号