Experimental Time-Lapse Visualization of Mud-Filtrate Invasion and Mudcake Deposition Using X-Ray Radiography

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引用次数: 1

Abstract

Accurate description and modeling of multiphase fluid flow are of paramount importance for subsurface resource engineering. The main source of information to quantify in-situ rock properties are borehole geophysical measurements, which are very often riddled with uncertainty ensuing from rock heterogeneity/anisotropy and mud-filtrate invasion effects. Therefore, experimental methods are needed to accurately describe and quantify the physics of mud-filtrate invasion and mudcake deposition and its effects on borehole geophysical measurements. We developed a new high-resolution (10 to 50 μm) experimental method to investigate the invasion of water- and oil-based drilling muds into rectangular rock samples using X-ray radiography. During mud injection, rock simples are scanned using high-resolution X-ray radiography, enabling the time-lapse visualization of both mud-filtrate invasion and external/internal mudcake deposition. Our experimental method successfully examines the effects of rock heterogeneity, bedding plane orientation, and anisotropy on the spatial distribution of fluids and mudcake formation resulting from mud-filtrate invasion. It also emphasizes the importance of mud properties on the final fluid saturation state once mudcake seals the borehole. The procedure is fast, accurate, and reliable to quantify the process of mud-filtrate invasion at the core scale, enabling an improved understanding of invasion effects on borehole geophysical measurements following drilling operations, especially in spatially complex rocks such as laminated sandstones and carbonates.
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基于x射线摄影的泥滤液侵入和泥饼沉积实验延时可视化
多相流体流动的准确描述和建模对地下资源工程至关重要。量化原位岩石性质的主要信息来源是井内地球物理测量,但由于岩石的非均质性/各向异性和泥浆滤液侵入效应,这些测量常常充满不确定性。因此,需要实验方法来准确描述和量化泥滤侵入和泥饼沉积的物理特性及其对井内地球物理测量的影响。我们开发了一种新的高分辨率(10 ~ 50 μm)实验方法,利用x射线摄影技术研究水基和油基钻井泥浆对矩形岩石样品的侵入。在注入泥浆过程中,使用高分辨率x射线成像技术对岩石进行扫描,实现了泥浆滤液侵入和外部/内部泥饼沉积的时序可视化。我们的实验方法成功地检验了岩石非均质性、层理平面方向和各向异性对泥浆滤液侵入引起的流体空间分布和泥饼形成的影响。它还强调了泥浆性质对泥饼封井后最终流体饱和状态的重要性。该方法快速、准确、可靠,可在岩心尺度上量化泥浆滤液侵入过程,从而更好地了解钻井作业后侵入对井眼地球物理测量的影响,特别是在层状砂岩和碳酸盐岩等空间复杂的岩石中。
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