The flow characteristics of deionized water in hydrophilic and hydrophobic microtubes with diameters of 14.9,5.03 and 2.05 μm are investigated experimentally.The results indicate that the flow characteristics of deio...The flow characteristics of deionized water in hydrophilic and hydrophobic microtubes with diameters of 14.9,5.03 and 2.05 μm are investigated experimentally.The results indicate that the flow characteristics of deionized water in microtubes with diameter of 14.9 μm are in agreement with the classical Hagen-Poiseuille(H-P) equation,but for hydrophilic and hydrophobic microtubes with smaller diameters,the results show significant departure from the prediction of conventional theory,and the discrepancies are influenced by wettability of the microtubes and increase as the Reynolds numbers decrease.Besides,flows of fluid in cores are the macroscopic reflection of flows in countless micron-sized pore throats,the influence of wettability on microscale flow in pore throats will cause the change of seepage characteristic in cores.Therefore,flow experiments of brine through cores with different wettabilities are conducted.The results demonstrate that wettability exerts similar influence on water flows in cores and microtubes.展开更多
为确定低渗透岩心速度敏感性实验的合理注入流量,基于喉道半径及其分布建立新的不等径毛细管数学模型,并应用有限差分方法对模型求解.模拟过程中,选取3块低渗透率岩心,模拟微粒释放、表面沉积和微粒堵塞等3种因素对岩心渗透率的影响;选...为确定低渗透岩心速度敏感性实验的合理注入流量,基于喉道半径及其分布建立新的不等径毛细管数学模型,并应用有限差分方法对模型求解.模拟过程中,选取3块低渗透率岩心,模拟微粒释放、表面沉积和微粒堵塞等3种因素对岩心渗透率的影响;选取7块低渗透率岩心,模拟注入流量设置对岩心临界流量判断的影响.模拟结果表明,微粒释放和微粒沉积是低渗透岩心渗透率伤害的主要原因;渗透率越低,渗透率伤害越显著,桥堵和卡堵对渗透率伤害越大;当岩心渗透率为（0.1~1）×10-3μm2,执行标准中注入流量时,临界流量判断结果偏大,建议在0.1 m L/min前添加1或2个流量点.展开更多
基金Supported by the National Natural Science Foundation of China (Grant No.50574060)National Basic Research Program of China (973Program) (Grant No.2005CB221303)
文摘The flow characteristics of deionized water in hydrophilic and hydrophobic microtubes with diameters of 14.9,5.03 and 2.05 μm are investigated experimentally.The results indicate that the flow characteristics of deionized water in microtubes with diameter of 14.9 μm are in agreement with the classical Hagen-Poiseuille(H-P) equation,but for hydrophilic and hydrophobic microtubes with smaller diameters,the results show significant departure from the prediction of conventional theory,and the discrepancies are influenced by wettability of the microtubes and increase as the Reynolds numbers decrease.Besides,flows of fluid in cores are the macroscopic reflection of flows in countless micron-sized pore throats,the influence of wettability on microscale flow in pore throats will cause the change of seepage characteristic in cores.Therefore,flow experiments of brine through cores with different wettabilities are conducted.The results demonstrate that wettability exerts similar influence on water flows in cores and microtubes.
文摘为确定低渗透岩心速度敏感性实验的合理注入流量,基于喉道半径及其分布建立新的不等径毛细管数学模型,并应用有限差分方法对模型求解.模拟过程中,选取3块低渗透率岩心,模拟微粒释放、表面沉积和微粒堵塞等3种因素对岩心渗透率的影响;选取7块低渗透率岩心,模拟注入流量设置对岩心临界流量判断的影响.模拟结果表明,微粒释放和微粒沉积是低渗透岩心渗透率伤害的主要原因;渗透率越低,渗透率伤害越显著,桥堵和卡堵对渗透率伤害越大;当岩心渗透率为（0.1~1）×10-3μm2,执行标准中注入流量时,临界流量判断结果偏大,建议在0.1 m L/min前添加1或2个流量点.
