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Bridging Particle Size Distribution in Drilling Fluid and Formation Damage

机译:钻井液和形成损伤的桥接粒度分布

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It is commonly understood that a reservoir drilling fluid must be compatible with the reservoir rock, both chemically and physically. One important aspect in optimizing drilling fluid is distribution of bridging particle sizes. Appropriate particle sizes can limit fluid loss to the formation and minimize solid plugging into reservoir pores. Reservoir rocks have complicated fluid- flow systems and it is important to understand pore characteristics of the rocks including pore type, size distribution and connectivity; and, secondary changes such as dissolution and fracturing. If inter-particle pores are the dominant fluid-flow channels for the sandstone and pore distribution is relatively homogeneous, a full range of particle-size distribution of bridging material may effectively bridge all pore spaces. But for many types of sandstone, natural dissolution of feldspar, rock fragments, or carbonate material has created oversized pores. Appropriately sized particles should be used to bridge them, and smaller particles should be retained in fluids to bridge smaller pores and to improve filtercake quality. For carbonate rocks, fracturing and/or dissolution may have created large pores or fluid-flow channels. They are usually inhomogeneous in space. Their sizes vary greatly and could be up to centimeter scale. The bridging particle size distribution should be comparable to the inhomogeneous pores or channels, if practical. Differential pressure between wellbore and formation pore fluid is also a factor which influences bridging size selection. At high differential pressure, relatively large particle sizes may help limit the solids plugging into pore spaces and decrease the effect of filtercake compaction. However, a combination of pore size, fluid property, and filtercake quality considerations are needed to achieve the most effective particle size distribution.
机译:通常理解的是,储层钻井液必须与水化学和物理的储层岩石兼容。优化钻井液中的一个重要方面是桥接粒径的分布。适当的粒度可以将流体损失限制在地层上,并使固体堵塞到储层孔中。储层岩石具有复杂的流量系统,重要的是要理解岩石的孔隙特性,包括孔式,尺寸分布和连接;并且,次要变化如溶解和压裂。如果颗粒孔是用于砂岩的主要流体流动通道和孔分布相对均匀,则桥接材料的全系列粒度分布可以有效地桥接所有孔隙空间。但对于许多类型的砂岩,长石,岩石片段或碳酸盐材料的自然溶解已经造成过大孔。适当尺寸的颗粒应该用于桥接它们,并且较小的颗粒应保留在流体中以弥合较小的孔并提高滤饼质量。对于碳酸盐岩石,压裂和/或溶解可能产生大的孔或流体流动通道。它们通常在太空中不均匀。它们的尺寸大大变化,可以高达厘米。桥接粒度分布应与非均匀孔隙或通道相媲美,如果实用。井眼和形成孔隙流体之间的差压也是影响桥接尺寸选择的因素。在高分压力下,相对大的颗粒尺寸可以有助于将固体限制为孔隙空间并降低滤饼压实的效果。然而,需要组合孔径,流体性能和滤饼质量考虑来实现最有效的粒度分布。

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