Physical simulation experiment on porosity evolution and controlling factors of Miocene reservoir in Ledong-Lingshui Dep

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ORIGINAL PAPER

Physical simulation experiment on porosity evolution and controlling factors of Miocene reservoir in Ledong-Lingshui Depression, Qiongdongnan Basin, South China Sea Xiyu Qu 1,2 & Yangchen Zhang 1 & Xiu Chen 1 & Xibing Yang 3 & Li You 3 & Jia Zhong 3 Received: 12 June 2020 / Accepted: 2 September 2020 / Published online: 24 September 2020 # Saudi Society for Geosciences 2020

Abstract Considering the high-temperature and overpressure in Miocene reservoirs of Ledong-Lingshui Depression, physical simulation experiments and other methods were adopted to identify the effect of overpressure on reservoir quality and the controlling factors of high-quality reservoir in porosity evolution process. In this paper, the temperature-pressure fields were divided into hightemperature normal-pressure (HTNP) zone, high-temperature overpressure (HTOP) zone, and high-temperature high-overpressure (HTHO) zone. The research findings are as follows: (1) The overpressure has a certain protective effect on primary pores. The visible porosity obtained from overpressure compaction simulation experiment is much higher than that obtained from normal compaction simulation experiment in the same diagenetic stage. The differences of visible porosity between normal compaction and overpressure compaction and high overpressure compaction can reach 1.55% and 6.74% respectively. (2) The organic acid dissolution contributes greatly to the formation of secondary pores in reservoir. The difference of visible porosity between organic acid dissolution and normal compaction is 0.96–7.38%. But the meteoric water leaching has a limited impact on reservoir porosity with a difference of merely 0.19% between meteoric water leaching and normal compaction. (3) Organic acid dissolution has the greatest constructive effect on diagenesis under the HTNP. However, overpressure protection to primary pores is the leading contributor to high-quality reservoir under the HTOP and HTHO, and the protective effect is positively correlated with the increase of overpressure. Overall, this work provides new insights into the porosity evolution and controlling factors in reservoirs. Keywords Overpressure protection . Organic acid dissolution . Meteoric water leaching . Porosity evolution . Ledong-Lingshui Depression

Introduction

This article is part of the Topical Collection on Big Data and Intelligent Computing Techniques in Geosciences * Xiyu Qu [email protected] 1

School of Geosciences, China University of Petroleum, Qingdao 266580, China

2

Shandong Provincial Key Laboratory of Depositional Mineralization & Sedimentary Minerals, Shandong University of Science and Technology, Qingdao 266590, China

3

CNOOC (China) Co., Ltd. Zhanjiang Branch, Zhanjiang 524057, China

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