1) sandstone strength
砂岩强度
1.
In view of the key issue that the development effectiveness of low permeability reservoir is enhanced by fracturing,sandstone reservoir is taken as research object,based on sandstone strength analysis,the reaction process and mechanism of the typical minerals in sandstone and acid liquid system are studied.
针对压裂改造提高低渗透油气藏开采效果的关键问题,以砂岩储层为研究对象,从砂岩强度的本质分析出发,研究了砂岩典型单矿物与酸液体系的反应过程和机理;利用矿物结构分析、离子浓度测定、衍射、能谱分析等实验研究手段,研究了砂岩酸损伤通过改变砂岩矿物成分、晶体结构,降低岩石强度的机理。
2) RES
岩石嵌入砂子的强度
3) sandstone thickness
砂岩厚度
1.
Using sedimentary facies control of reservoir physical properties, the paper puts forward a facies-controlled model to predict physical property parameters of sandstone reservoirs between wells and to research sandstone thickness as well as lateral distribution of reservoir porosity and permeability by building a model of reservoir physical property parameters.
据此 ,针对砂岩储集层进行井间参数预测 ,研究砂岩厚度、孔隙度、渗透率的平面分布 ,提出建立井间储集层参数模型的相控模型法 ,其实质是进行带地质约束的井间参数预估 ,即由井间沉积相地质信息提取储集层参数软信息 ,增补井间约束条件 ,与井点数据共同预测井间储集层参数。
2.
the method , s precision(70%)was proved through predicting sandstone thickness of different sand body and well pattern density of Beierdong dense well pattern testing area.
通过对北二东密井网试验区不同类型砂体、不同井网密度砂岩厚度的预测 ,检验了此方法的精度 (为 70 %左右 )。
4) sandstone grain size
砂岩粒度
1.
We studied the relationship between sandstone grain size and log responses on cores from block 2,3,4 and 5 in Ningdong in the west of Mahuangshan working area.
勘探实践证实麻黄山西探区的砂岩粒度对储层的物性和含油性有较大的控制作用。
5) highly weathered sandstone
强风化砂岩
1.
Physical properties of highly weathered sandstone at Hongshanyao;
红山窑强风化砂岩试验特性
6) cement mortar strength
胶砂强度
1.
At the equal w/c ratio,the fluidity and the cement mortar strength of the coarser separated fly ash were low.
在相同水胶比的条件下,掺分选粗粉煤灰的水泥胶砂流动度及强度均低;分选粗粉煤灰磨细后,不仅减少了颗粒的粘连,增加了比表面积,而且提高了粉煤灰的反应活性和水泥胶砂流动度及强度,虽其水泥胶砂流动度仍小于掺分选细粉煤灰的水泥,3d水泥胶砂强度也略低,但其28d水泥胶砂强度略高于掺分选细粉煤灰的水泥;在相同水泥胶砂流动度的条件下,掺磨细粉煤灰配制的水泥胶砂3d强度低于掺分选细粉煤灰的水泥,但随着水化龄期的增长,其差距逐步缩小,至60d时可超过后者。
补充资料:粉砂岩
| 粉砂岩 siltstone 由粒径为0.0625~0.0039毫米(mm)的粉砂的含量占50%以粉砂岩标本的一种碎屑沉积岩。除粉砂以外其它由砂、粘土或化学沉淀物组成。按粒度划分为粗粉砂岩(0.0625~0.0312mm)和细粉砂岩(0.0312~0.0039mm)。按碎屑成分划分为石英粉砂岩、长石粉砂岩、岩屑粉砂岩(少见)和它们间的过渡类型。根据胶结物成分划分为粘土质粉砂岩、铁质粉砂岩、钙质粉砂岩和白云质粉砂岩。黄土也是一种疏松的或半固结的粉砂质沉积物。粉砂岩多形成于河漫滩、三角洲、潟湖和海洋的较深水部位。
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