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利用不同加重材料时钻开地层对滤饼性能的作用

The Role of Drilled Formation in Filter Cake Properties Utilizing Different Weighting Materials.

作者信息

Al Jaber Jaber, Bageri Badr S, Gamal Hany, Elkatatny Salaheldin

机构信息

College of Petroleum Engineering & Geosciences, King Fahd University of Petroleum & Minerals, Dhahran 31261, Saudi Arabia.

出版信息

ACS Omega. 2021 Sep 9;6(37):24039-24050. doi: 10.1021/acsomega.1c03210. eCollection 2021 Sep 21.

Abstract

The filter cake formed during a filtration process plays a vital role in the success of a drilling operation. There are several factors affecting the filter cake build-up such as drilled formation, drilling fluid properties, and well pressure and temperature. The collective impact of these two factors (i.e., formation and the drilling fluid) on the filter cake build-up needs to be fully investigated. In this study, two types of formations represented as limestone and sandstone were used with different weighting materials to assess and compare their impact on the filter cake properties, filtration behavior, and solid invasion. The used weighting materials are manganese tetroxide, ilmenite, barite, and hematite. The filter cake was formed under a temperature of 200 °F and differential pressure of 300 psi. Nuclear magnetic resonance spectroscopy was employed to explore the pore structure of the used core samples. The results showed that the properties (i.e., shape and dimensions) of the different weighting materials are the dominant factors compared to the formation characteristics in most of the investigated filter cake properties. Nevertheless, the formation properties, namely, the permeability and pore structure, have a somehow higher contribution when it comes to the filter cake porosity and thickness. For solid invasion, there were no clear results about the main factor contributing to this issue.

摘要

过滤过程中形成的滤饼对钻井作业的成功起着至关重要的作用。有几个因素会影响滤饼的形成,如钻进地层、钻井液性能以及井内压力和温度。这两个因素(即地层和钻井液)对滤饼形成的综合影响需要进行全面研究。在本研究中,使用了代表石灰岩和砂岩的两种地层,并搭配不同的加重材料,以评估和比较它们对滤饼性质、过滤行为和固相侵入的影响。所使用的加重材料有四氧化锰、钛铁矿、重晶石和赤铁矿。滤饼是在200°F的温度和300 psi的压差下形成的。采用核磁共振光谱法来探究所用岩心样品的孔隙结构。结果表明,在大多数所研究的滤饼性质方面,与地层特性相比,不同加重材料的性质(即形状和尺寸)是主导因素。然而,在地层性质方面,即渗透率和孔隙结构,在滤饼孔隙率和厚度方面的贡献在某种程度上更高。关于导致固相侵入这一问题的主要因素,没有明确的结果。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b0ba/8459423/7b697ef7c7ee/ao1c03210_0002.jpg

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