Oil Production and CCUS Potential in La Luna Shale in Colombia

Claudia Marcela Herrera Tellez, A. Fragoso, R. Aguilera
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Abstract

La Luna Shale in Colombia is the main source rock in the Middle Magdalena Valley (MMV) and the Catatumbo Basins. La Luna shale is a high-quality source rock and its potential has been investigated by several authors. This paper presents geological, geochemical, and petrophysical description of La Luna shale with the dual objective of (1) utilizing CO2 for improving oil recovery through Huff-n-Puff (HnP) gas injection, and (2) storing CO2 safely and without leaks. The overall approach includes verifying that geologic fluid containment exists in the shale reservoir. The present work shows that this is indeed the case in La Luna shale. Geologic containment is valuable as it permits maximizing oil recovery from La Luna shale and safe storage of CO2 with negligible possibilities of fluid leakage, thus providing a valuable contribution to solve problems related to climate change. Consequently, the procedure described in this paper conforms well to CCUS: Carbon capture, utilization and storage of CO2. The Eagle Ford shale in Texas is a good analog of La Luna shale. In both reservoirs, sedimentation and development of the source rock start at about the same time in the late Cretaceous, about 93 million years ago. It is not surprising then that in both Eagle Ford and La Luna shales, oil, condensate and natural gas are in the same location where they were generated, gas is at the bottom, condensate in the middle and crude oil at the top of the structure. Thus, the hydrocarbon fluids have been upside down or inverted position through millions of years. This constitutes geologic containment. The paper describes the following activities once geologic containment is established: (1) drill a pilot horizontal well (HW), (2) stimulate the HW with multi-stage hydraulic fractures and investigate the environmental impact (if the pilot is successful, drill another pilot(s)), (3) produce oil by primary means for a maximum of 2-3 years, (4) implement HnP CO2 injection, (5) store the CO2 in the shale reservoir once the HnP reaches economic limit. Regular pressure monitoring throughout the life of the HnP project guarantees the lack of leaks, a major concern when CO2 is stored in other types of depleted reservoirs or aquifers. The novelty of the paper is demonstrating geologic containment in La Luna shale in both the MMV and Catatumbo Basins of Colombia. This provides the basis for implementing CCUS. The geological, geochemical and petrophysical description allow to construct a simulation model to investigate primary recovery as well as EOR by HnP CO2 injection. CO2 can be stored safely, without leaks, in the shale reservoir once the HnP project reaches economic limit.
哥伦比亚La Luna页岩的石油产量和CCUS潜力
La Luna页岩是哥伦比亚中部Magdalena山谷(MMV)和Catatumbo盆地的主要烃源岩。La Luna页岩是一种优质的烃源岩,其潜力已被多位作者研究过。本文介绍了La Luna页岩的地质、地球化学和岩石物理描述,其双重目标是(1)利用CO2通过hff -n- puff (HnP)注气提高采收率;(2)安全、无泄漏地储存CO2。总体方法包括验证页岩储层中存在地质流体密封。目前的工作表明,这确实是拉月神页岩的情况。地质密封是有价值的,因为它可以最大限度地提高La Luna页岩的石油采收率,并在流体泄漏的可能性很小的情况下安全储存二氧化碳,从而为解决与气候变化有关的问题做出宝贵贡献。因此,本文所描述的过程非常符合CCUS:碳捕获,利用和储存二氧化碳。德克萨斯州的Eagle Ford页岩与La Luna页岩非常相似。在这两个储层中,沉积和烃源岩的发育在大约9300万年前的白垩纪晚期几乎同时开始。因此,在Eagle Ford和La Luna页岩中,石油、凝析油和天然气都位于它们产生的同一个位置,天然气在底部,凝析油在中间,原油在顶部,这一点也不奇怪。因此,数百万年来,碳氢化合物流体一直处于颠倒或倒置的位置。这就构成了地质密封。本文介绍了地质密封建立后的以下活动:(1)钻一口试验水平井(HW),(2)用多级水力压裂对HW进行压裂,并调查环境影响(如果试验成功,再钻一次试验),(3)通过主要手段采油,最长可达2-3年,(4)实施HnP CO2注入,(5)一旦HnP达到经济极限,将二氧化碳储存在页岩储层中。在HnP项目的整个生命周期内定期监测压力,确保不发生泄漏,这是将二氧化碳储存在其他类型的枯竭水库或含水层时的一个主要问题。该论文的新颖之处在于展示了哥伦比亚MMV和Catatumbo盆地的La Luna页岩的地质密封。这为CCUS的实现提供了基础。地质、地球化学和岩石物理描述允许建立模拟模型,以研究HnP CO2注入的一次采收率和EOR。一旦HnP项目达到经济极限,二氧化碳就可以安全地储存在页岩储层中,不会泄漏。
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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