新疆地质
新疆地質
신강지질
XINJIANG GEOLOGY
2013年
z2期
139-141
,共3页
陈蒲礼%王烁%王丹%贾星亮%潜欢欢
陳蒲禮%王爍%王丹%賈星亮%潛歡歡
진포례%왕삭%왕단%가성량%잠환환
孔隙结构%恒速压汞%常规压汞%喉道
孔隙結構%恆速壓汞%常規壓汞%喉道
공극결구%항속압홍%상규압홍%후도
Pore structure%Constant-speed mercury injection%Conventional mercury injection%Throat
本文从理论模型、实验过程和测量结果等方面阐述恒速压汞法与常规压汞法的异同。恒速压汞法可区分孔隙和喉道,常规压汞法区不能;恒速压汞法可反映喉道与孔隙的数量分布情况。运用恒速压汞法可获得总体毛管压力曲线、孔隙毛管压力曲线及喉道毛管压力曲线,测试所得到的毛细管压力值及喉道半径值更接近真实情况。
本文從理論模型、實驗過程和測量結果等方麵闡述恆速壓汞法與常規壓汞法的異同。恆速壓汞法可區分孔隙和喉道,常規壓汞法區不能;恆速壓汞法可反映喉道與孔隙的數量分佈情況。運用恆速壓汞法可穫得總體毛管壓力麯線、孔隙毛管壓力麯線及喉道毛管壓力麯線,測試所得到的毛細管壓力值及喉道半徑值更接近真實情況。
본문종이론모형、실험과정화측량결과등방면천술항속압홍법여상규압홍법적이동。항속압홍법가구분공극화후도,상규압홍법구불능;항속압홍법가반영후도여공극적수량분포정황。운용항속압홍법가획득총체모관압력곡선、공극모관압력곡선급후도모관압력곡선,측시소득도적모세관압력치급후도반경치경접근진실정황。
This paper profoundly expounded the difference between constant-speed mercury injection and conventional mercury injection technique in the theoretical model,experiment and measurement results.The pore and throat can be dis-tinguished by constant-speed mercury injection technique,but the conventional mercury injection technique is unable to distinguish the pore and throat.The constant-speed mercury injection technique can reflect the distribution of throat and pore.General capillary pressure curve,pore capillary pressure curve and throat capillary pressure cure can be obtained by using Constant-speed mercury injection technique.The obtained capillary pressure and the obtained throat radius is clos-er to the real situation.Constant-speed mercury injection technique is a good method to study rock pore structure.