In-Situ Stresses in Colorado Group, AB, Calculated from Open-Hole Mini-Fracs and FMI Logs

O CostinSimona, R. Smith, Yanguang Yuan, D. Andjelković, Gabriel Garcia Rosas
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引用次数: 3

Abstract

Open-hole mini-frac tests are seldom performed in the Athabasca and Cold Lake oil sands due to the complexity of operations. In this paper we present the results of open-hole injections tests performed in Cold Lake, Alberta (AB), Canada. The objective of the injection tests was to assess the in-situ stress condition in the Cretaceous Colorado Group. The injection tests results combined with the run of formation image logs (FMI) before and after the injection have enabled not only the determination of the in-situ minimum stress in the rock, but also the full 3-D stress tensor, along with the orientation and inclination of the hydraulic fracture. The tests were performed in IOL 102/08-02-066-03W4 (N10 Passive Seimic Well, ‘PSW’). The injection tests have revealed that the vertical stress in the area is the in-situ minimum stress, consistent with previous measurements. The hydraulically-induced fracture has sub-horizontal to moderate dip angle, mostly owing to the pre-existing fabric of the rock, and peaks in the general NE-SW direction. Numerical modeling of the in-situ stresses has shown that the values of the vertical and the minimum horizontal stresses are close, with the vertical stress consistently being smaller than the minimum horizontal stress in all tested zones.
根据裸眼微型压裂和FMI测井计算科罗拉多组的地应力
由于作业的复杂性,在Athabasca和Cold Lake油砂中很少进行裸眼微型压裂测试。在本文中,我们介绍了在加拿大阿尔伯塔省(AB)的Cold Lake进行的裸眼注入测试结果。注入测试的目的是评估白垩纪Colorado组的地应力状况。注入测试结果与注入前后的地层图像测井(FMI)相结合,不仅可以确定岩石中的原位最小应力,还可以确定全三维应力张量,以及水力裂缝的方向和倾角。试验在IOL 102/08-02-06 -066- 03w4 (N10被动地震井,' PSW ')中进行。注入试验表明,该区域的垂直应力为原位最小应力,与之前的测量结果一致。水力裂缝的倾角为亚水平至中等,主要是由于岩石的预先构造造成的,峰值大致为NE-SW方向。地应力数值模拟结果表明,竖向地应力与最小水平地应力值接近,且各试验区竖向地应力均小于最小水平地应力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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