Application of fractal model in the Jurassic tight sandstone reservoirs of central Junggar Basin as constrained by mercury ejection curves

The high-pressure mercury intrusion (HPMI) experiment is widely used to assess the pore architecture of tight sandstone reservoirs. However, the conventional analysis of the high-pressure mercury intrusion has always focused on the mercury injection curves themselves, neglecting the important geolog...

Full description

Saved in:
Bibliographic Details
Main Authors: Hongkang Zhao, Xiangchun Chang, Tianchen Ge, Zhiping Zeng, Junjian Zhang, Daiqi Ming, Runye Han
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2025-03-01
Series:Energy Geoscience
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2666759224000751
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1832582099541950464
author Hongkang Zhao
Xiangchun Chang
Tianchen Ge
Zhiping Zeng
Junjian Zhang
Daiqi Ming
Runye Han
author_facet Hongkang Zhao
Xiangchun Chang
Tianchen Ge
Zhiping Zeng
Junjian Zhang
Daiqi Ming
Runye Han
author_sort Hongkang Zhao
collection DOAJ
description The high-pressure mercury intrusion (HPMI) experiment is widely used to assess the pore architecture of tight sandstone reservoirs. However, the conventional analysis of the high-pressure mercury intrusion has always focused on the mercury injection curves themselves, neglecting the important geological information conveyed by the mercury ejection curves. This paper quantitatively describes the fractal characteristics of ejection curves by using four fractal models, i.e., Menger model, Thermodynamic model, Sierpinski model, and multi-fractal model. In comparison with mercury injection curves, we explore the fractal significance of mercury ejection curves and define the applicability of different fractal models in characterizing pore architectures. Investigated tight sandstone samples can be divided into four types (Types A, B, C and D) based on porosity, permeability, and mercury removal efficiency. Type D samples are unique in that they have higher permeability (>0.6 mD) but lower mercury removal efficiency (<35%). Fractal studies of the mercury injection curve show that it mainly reflects the pore throat characteristics, while the mercury ejection curve serves to reveal the pore features, and porosity and permeability correlate well with the fractal dimension of the injection curve, while mercury removal efficiency correlates only with the Ds' value of the ejection curve. The studies on the mercury ejection curves also reveal that the small pores and micropores of the Type C and Type D samples are more developed, with varying pore architecture. The fractal dimension DS’ value of Type D samples is greater than that of Type C samples, and the dissolution of Type D samples is more intense than that of Type C samples, which further indicates that the Type D samples are smaller in pore size, rougher in surface, and with greater difficulty for the hydrocarbon to enter, resulting in their reservoir capacity probably less than that of Type C samples. In this regard, the important information characterized by the mercury ejection curve should be considered in evaluating the tight sandstone reservoirs. Finally, the Menger and Thermodynamic models prove to be more suitable for describing the total pore architecture, while the Sierpinski model is better for characterizing the variability of the interconnected pores.
format Article
id doaj-art-6f4c1b3f089044c0bebfbbee1aede2f2
institution Kabale University
issn 2666-7592
language English
publishDate 2025-03-01
publisher KeAi Communications Co., Ltd.
record_format Article
series Energy Geoscience
spelling doaj-art-6f4c1b3f089044c0bebfbbee1aede2f22025-01-30T05:15:04ZengKeAi Communications Co., Ltd.Energy Geoscience2666-75922025-03-0161100360Application of fractal model in the Jurassic tight sandstone reservoirs of central Junggar Basin as constrained by mercury ejection curvesHongkang Zhao0Xiangchun Chang1Tianchen Ge2Zhiping Zeng3Junjian Zhang4Daiqi Ming5Runye Han6College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao, Shandong, 266590, ChinaCollege of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao, Shandong, 266590, China; Laboratory for Marine Mineral Resources, Qingdao Marine Science and Technology Center, Qingdao, Shandong, 266237, China; Corresponding author. College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao, Shandong, 266590, China.College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao, Shandong, 266590, ChinaResearch Institute of Petroleum Exploration and Development, Shengli Oilfield Company, Sinopec, Dongying, Shandong, 257001, ChinaCollege of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao, Shandong, 266590, ChinaCollege of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao, Shandong, 266590, ChinaCollege of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao, Shandong, 266590, ChinaThe high-pressure mercury intrusion (HPMI) experiment is widely used to assess the pore architecture of tight sandstone reservoirs. However, the conventional analysis of the high-pressure mercury intrusion has always focused on the mercury injection curves themselves, neglecting the important geological information conveyed by the mercury ejection curves. This paper quantitatively describes the fractal characteristics of ejection curves by using four fractal models, i.e., Menger model, Thermodynamic model, Sierpinski model, and multi-fractal model. In comparison with mercury injection curves, we explore the fractal significance of mercury ejection curves and define the applicability of different fractal models in characterizing pore architectures. Investigated tight sandstone samples can be divided into four types (Types A, B, C and D) based on porosity, permeability, and mercury removal efficiency. Type D samples are unique in that they have higher permeability (>0.6 mD) but lower mercury removal efficiency (<35%). Fractal studies of the mercury injection curve show that it mainly reflects the pore throat characteristics, while the mercury ejection curve serves to reveal the pore features, and porosity and permeability correlate well with the fractal dimension of the injection curve, while mercury removal efficiency correlates only with the Ds' value of the ejection curve. The studies on the mercury ejection curves also reveal that the small pores and micropores of the Type C and Type D samples are more developed, with varying pore architecture. The fractal dimension DS’ value of Type D samples is greater than that of Type C samples, and the dissolution of Type D samples is more intense than that of Type C samples, which further indicates that the Type D samples are smaller in pore size, rougher in surface, and with greater difficulty for the hydrocarbon to enter, resulting in their reservoir capacity probably less than that of Type C samples. In this regard, the important information characterized by the mercury ejection curve should be considered in evaluating the tight sandstone reservoirs. Finally, the Menger and Thermodynamic models prove to be more suitable for describing the total pore architecture, while the Sierpinski model is better for characterizing the variability of the interconnected pores.http://www.sciencedirect.com/science/article/pii/S2666759224000751Fractal theoryMercury ejection curveMercury removal efficiencyInhomogeneityPore architecture
spellingShingle Hongkang Zhao
Xiangchun Chang
Tianchen Ge
Zhiping Zeng
Junjian Zhang
Daiqi Ming
Runye Han
Application of fractal model in the Jurassic tight sandstone reservoirs of central Junggar Basin as constrained by mercury ejection curves
Energy Geoscience
Fractal theory
Mercury ejection curve
Mercury removal efficiency
Inhomogeneity
Pore architecture
title Application of fractal model in the Jurassic tight sandstone reservoirs of central Junggar Basin as constrained by mercury ejection curves
title_full Application of fractal model in the Jurassic tight sandstone reservoirs of central Junggar Basin as constrained by mercury ejection curves
title_fullStr Application of fractal model in the Jurassic tight sandstone reservoirs of central Junggar Basin as constrained by mercury ejection curves
title_full_unstemmed Application of fractal model in the Jurassic tight sandstone reservoirs of central Junggar Basin as constrained by mercury ejection curves
title_short Application of fractal model in the Jurassic tight sandstone reservoirs of central Junggar Basin as constrained by mercury ejection curves
title_sort application of fractal model in the jurassic tight sandstone reservoirs of central junggar basin as constrained by mercury ejection curves
topic Fractal theory
Mercury ejection curve
Mercury removal efficiency
Inhomogeneity
Pore architecture
url http://www.sciencedirect.com/science/article/pii/S2666759224000751
work_keys_str_mv AT hongkangzhao applicationoffractalmodelinthejurassictightsandstonereservoirsofcentraljunggarbasinasconstrainedbymercuryejectioncurves
AT xiangchunchang applicationoffractalmodelinthejurassictightsandstonereservoirsofcentraljunggarbasinasconstrainedbymercuryejectioncurves
AT tianchenge applicationoffractalmodelinthejurassictightsandstonereservoirsofcentraljunggarbasinasconstrainedbymercuryejectioncurves
AT zhipingzeng applicationoffractalmodelinthejurassictightsandstonereservoirsofcentraljunggarbasinasconstrainedbymercuryejectioncurves
AT junjianzhang applicationoffractalmodelinthejurassictightsandstonereservoirsofcentraljunggarbasinasconstrainedbymercuryejectioncurves
AT daiqiming applicationoffractalmodelinthejurassictightsandstonereservoirsofcentraljunggarbasinasconstrainedbymercuryejectioncurves
AT runyehan applicationoffractalmodelinthejurassictightsandstonereservoirsofcentraljunggarbasinasconstrainedbymercuryejectioncurves