致密砂岩储层流体差异性赋存特征———以鄂尔多斯盆地三叠系延长组为例

In order to explore the differential characteristics of fluid occurrence in tight sandstone reservoirs, theChang 6 and Chang 8 reservoirs in the Triassic Yanchang Formation in HQ and HS areas of the Ordos Basin wereemployed as research objects, the movable and non-movable fluid saturation of reservoir rocks were quantitativelyanalyzed with features including permeability interval, area and target strata by using nuclear magnetic resonance(NMR) test and high-speed centrifugal experiments. Results showed that the total movable fluid saturation, as well asthe main throat intervals of movable fluid were different in reservoirs with different permeability levels. For the highpermeability, movable fluid was mainly controlled by larger throat, while for the low permeability, movable fluid wasmainly controlled by smaller throat. Movable fluid saturation positively correlated to the throat radius in the smallerthroat radius range (＜critical throat radius), and negatively correlated to throat radius in the larger throat radius range(＞critical throat radius). The higher the permeability, the larger the critical throat radius.