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松散颗粒介质水的渗透率与孔隙率实验研究
引用本文:郝锦志,雷树业,马斌.松散颗粒介质水的渗透率与孔隙率实验研究[J].广西师范大学学报(自然科学版),2003,21(4):15-18.
作者姓名:郝锦志  雷树业  马斌
作者单位:清华大学,热能工程系工程热物理所,北京,100084
基金项目:国家自然科学基金(50176025)
摘    要:以松散颗粒介质渗透率实验出发点,考证多孔介质内流动滑移的同时,将此实验作为考察微孔道流动的方法提出,避开单一微槽道流动测量的困难.实验结果表明,大于0.1mm的孔道内,观测不到水的偏常规层流流动.

关 键 词:松散颗粒介质  渗透率  孔隙率  流动滑移  微细孔道
文章编号:1001-6600(2003)04-0015-04
修稿时间:2003年4月17日

EXPERIMENTAL STUDY OF UNCONSOLIDATED SAND PERMEABILITY AND POROSITY WITH WATER AS FLOW MEDIUM
HAO Jin-zhi,LEI Shu-ye,MA Bin.EXPERIMENTAL STUDY OF UNCONSOLIDATED SAND PERMEABILITY AND POROSITY WITH WATER AS FLOW MEDIUM[J].Journal of Guangxi Normal University(Natural Science Edition),2003,21(4):15-18.
Authors:HAO Jin-zhi  LEI Shu-ye  MA Bin
Abstract:With the purpose of studying slip flow in pores,the experiment of unconsolidated sand perme- ability with water as a flow medium was carried out. The experimental method can facilitate observing statistically flow in micro-channel. The experimental result shows that abnormal laminar flow can not be observed in the pores with their average diameter greater than 0.1 mm.
Keywords:permeability  porosity  slip flow
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