Drilling Through Shales Below Depleted Sands: Case Study of a Niger Delta HPHT Gas Development Well

S. Ogbodu, B. Tichelaar, Chibueze Amadi, C. Anijekwu, K. Eke, J. Alli-Oluwafuyi, P. Schutjens
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Abstract

To sustain gas supply to NLNG T1-T7, it has become imperative to access deeper, geologically complex HPHT reservoirs in the Niger Delta. These hydrocarbon targets typically lie beneath hydrostatic geological intervals and are overlain by depleted and/or producing reservoirs hence choosing the right casing depth is a key parameter in executing HPHT wells In the wells in Astra East Field, it was decided to set a casing shoe in a homogeneous shale of ~200ft vertical thickness, located between overlying heavily depleted sand and underlying over pressured sand. This poses an interesting question of the direct practical importance: at what depth should the casing shoe be set to minimize the risk of kicks and/or wellbore instability (because of too low mud weight) and losses (because of too high mud weight). To help answer this question, wireline log data and drilling observations in other wells in the same field, where such shales were found, were analyzed, and evaluated. The electrical resistivity in the shales consistently showed the following signature from top to bottom across the shale: Zone 1: Relatively high electric resistivity just below the depleted sand, near constant with depth. Zone 2: The signature gradually decreasing with increasing depth, and finally, at the lower section of the shale. Zone 3: Relatively low electric resistivity just above the over pressured sand, the signal again near-constant with depth. The drilling observations revealed that wells with the casing set in Zone 1 experienced severe mud losses and differential sticking, while wells where the casing set in zones 2 or Zone 3 did not. This observation could be explained as follows - The electric resistivity signature as a function of depth (in the three zones described above) may reflect the pore pressure in the bounding sands: at the top, the shale "feels" the sand depletion, transmitted over the years via pore fluid pressure diffusion, which compacts the shale, presses the grains contacts closer together, thus increasing electrical resistivity. In contrast, at the base, the shale "feels" the overpressure in the sand below, maintained over the millions of years of geologic diagenesis. This keeps the deeper part of the shale at relatively low effective stress (compared to the upper part), with relatively low grain contact pressure, thus reducing electrical resistivity. We postulate that there may be a mechanism-based explanation for the heavy losses and sticking when the casing is set in Zone 1. We also inferred from the drilling data that the tendency to set the casing shoe quite shallow (in Zone 1) in previous wells and in the well in case study was driven by concern of wellbore instability and severe losses experienced while drilling through the intra-reservoir shale. Closer inspection reveals that this concern is probably not justified, as the apparently high risk of wellbore instability at the top of the shale was caused by using a too-high pore fluid pressure (i.e., one unaffected by the depletion of the sand on top of it). For future planned wells in the field, new LWD data acquisition practices have been developed for early detection of the onset of overpressures (top of Zone 2). This will improve the accuracy of casing point selection and the chances of successfully drilling across these intervals without well control issues.
在枯竭砂层下钻穿页岩:尼日尔三角洲高温高压天然气开发井的案例研究
为了维持NLNG T1-T7的天然气供应,必须进入尼日尔三角洲更深、地质复杂的高温高压储层。这些油气目标通常位于静水地质层段之下,并且被枯竭和/或正在生产的油藏覆盖,因此选择合适的套管深度是实施高温高压井的关键参数。在Astra East油田的井中,决定在垂直厚度约200英尺的均匀页岩中设置套管鞋,该页岩位于上覆的严重枯竭砂层和下覆的超压砂层之间。这就提出了一个具有直接实际意义的有趣问题:为了最大限度地减少井涌和/或井眼不稳定(由于泥浆比重过低)和漏失(由于泥浆比重过高)的风险,套管鞋应该安装在什么深度?为了帮助回答这个问题,我们对同一油田发现页岩的其他井的电缆测井数据和钻井观察进行了分析和评估。从上到下,页岩的电阻率一致地显示出以下特征:1区:相对较高的电阻率就在衰竭砂层下方,与深度接近恒定。区域2:随着深度的增加,信号逐渐减弱,最后在页岩下部。第3层:超压砂层上方的电阻率相对较低,信号再次随深度接近恒定。钻井观察显示,套管位于1区的井出现了严重的泥浆漏失和压差卡钻现象,而套管位于2区或3区的井则没有出现这种情况。这一观察结果可以解释如下:电阻率特征作为深度的函数(在上述三个区域)可能反映了边界砂中的孔隙压力:在顶部,页岩“感觉”到了沙子的枯竭,这种枯竭是通过孔隙流体压力扩散多年来传递的,这种扩散使页岩压实,使颗粒接触更紧密,从而增加了电阻率。相反,在底部,页岩“感受到”下面沙子的超压,这种压力在数百万年的地质成岩作用中保持着。这使得页岩深层处于相对较低的有效应力(与上部相比),颗粒接触压力相对较低,从而降低了电阻率。我们假设,在第1层下入套管时,可能存在基于机制的严重漏失和卡钻现象。我们还从钻井数据中推断,在之前的井中,以及在案例研究的井中,由于担心井筒不稳定以及在钻穿储层内页岩时经历的严重损失,套管鞋往往下得很浅(在1区)。仔细观察发现,这种担心可能是不合理的,因为页岩顶部的井眼不稳定风险明显很高,是由于使用过高的孔隙流体压力造成的(即,不受顶部砂土枯竭的影响)。对于油田未来的计划井,已经开发了新的随钻数据采集方法,用于早期检测超压(2区顶部)的开始。这将提高套管点选择的准确性,并提高在这些层段成功钻井的机会,而不会出现井控问题。
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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