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Evaluation of Low-solids Mud Reological Behavior during Drilling Shale Formation and Their Effect on the Pay Zone Productivity

机译:泥页岩形成过程中低固泥的生物学行为评价及其对产层生产力的影响

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The present study deals with the evaluation of rheological behavior of lowsolids mud during drilling shale formation and its effect on the pay zone productivity. This study involves the preparation of shale samples (shale formation) requiredfor the shale sloughing tests and preparation of plug samples (reservoir formation) required for the saturation tests. The shale analyzed by X-ray diffraction showed that the main constituents are montmorillonite, small amounts of kaolinite and smectite, with a little bit of illite recorded in a few samples. Also, the low-solids base mud was prepared in form unweighted then weighted by barrite and the rheological properties (density, apparent viscosity, plastic viscosity yield point, gel strength, and thixotropy) were determined for the two types; the weighted low-solids base mud was then circulated with the shale for 12, 24, 36, 48, and 60 hr using the roller oven device to determine the sloughing ratio of the shale and the rheological properties after circulation. This circulation showed that the shale sloughing ratio increased to more than 90%. Afterward, the core samples (reservoir rock) were prepared in the form of plugs according to the test requirements and their physical properties, including porosity, permeability, and resistivity, were determined through clean samples, and after saturation by low-solids mud and shaly low-solids mud, a petrographic study was carried out for the clean and saturated samples by making thin sections to show the change in the porosity. From these it was concluded that the rheological behavior of the low-solids mud during drilling shale formation affected caused formation damage and had an effect on the pay zone productivity. The recommendation for minimizing the shale affect and formation damage is to add specific chemicals to the low-solids mud system during the drilling.
机译:本研究的内容是评估页岩形成过程中低固泥的流变行为及其对产层生产率的影响。这项研究涉及准备页岩泥蚀试验所需的页岩样品(页岩形成)和饱和度试验所需的堵头样品(储层形成)。 X射线衍射分析表明,页岩的主要成分为蒙脱石,少量的高岭土和蒙脱石,少数样品中记录了少量的伊利石。同样,将低固含量的基础泥制备成未加重的形式,然后用重晶石加重,并确定两种类型的流变性能(密度,表观粘度,塑性粘度屈服点,凝胶强度和触变性)。然后,使用辊式烘箱设备,将经过称重的低固含量基础泥浆与页岩一起循环12、24、36、48和60小时,以确定页岩的泥浆塌落率和循环后的流变性。该循环表明,页岩泥浆脱落率增加到90%以上。然后,根据测试要求,以堵塞的形式制备岩心样品(储层岩石),并通过干净的样品以及在低固体泥浆和泥质岩土饱和后确定其物理性质(包括孔隙率,渗透率和电阻率)。对于低固含量的泥浆,通过将其切成薄片以显示孔隙率的变化,对清洁和饱和的样品进行了岩石学研究。由此得出的结论是,低固含量泥浆在钻井页岩形成过程中的流变行为会引起地层破坏,并影响产层产能。减少页岩影响和地层损害的建议是在钻井过程中向低固含量泥浆系统中添加特定的化学物质。

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