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首頁» 過刊瀏覽» 2024» Vol.9» lssue(4) 648-658???? DOI : 10.3969/j.issn.2096-1693.2024.04.049
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基于三維數(shù)字巖心的油頁巖裂解孔隙重構(gòu)及表征研究
王斌, 孫廉賀, 楊兵, 楊睿月, 王海柱, 張?jiān)迄i, 王全, 劉銘盛
1 中國(guó)石油大學(xué)( 北京) 油氣資源與工程全國(guó)重點(diǎn)實(shí)驗(yàn)室,,北京 102249 2 中國(guó)石油大學(xué)( 北京) 石油工程學(xué)院,,北京 102249 3 西安石油大學(xué)石油工程學(xué)院,,西安 710018
Characterization of oil shale pore and fractures during pyrolysis using digital rock reconstruction
WANG Bin, SUN Lianhe, YANG Ruiyue, YANG Bing, WANG Haizhu, ZHANG Yunpeng, WANG Quan, LIU Mingsheng
1 State Key Laboratory of Petroleum Resources and Engineering, China University of Petroleum-Beijing, Beijing 102249, China 2 College of Petroleum Engineering, China University of Petroleum-Beijing, Beijing 102249, China 3 College of Petroleum Engineering, Xi’ an University of Petroleum, Xi’ an 710018, China

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摘要? 油頁巖孔隙結(jié)構(gòu)作為油氣滲流的主要通道,,高溫?zé)峤膺^程中將產(chǎn)生復(fù)雜變化,然而其變化規(guī)律不明嚴(yán)重制約儲(chǔ)集層分類評(píng)價(jià)和高效開發(fā),。因此,,開展不同溫度及不同有機(jī)質(zhì)含量條件下油頁巖熱解對(duì)孔隙結(jié)構(gòu)影響的研究對(duì)于油頁巖的有效開發(fā)具有重要意義。針對(duì)熱解前后油頁巖孔縫結(jié)構(gòu)變化精細(xì)表征難的問題,,本文通過編程方法提出了一種基于三維數(shù)字巖心重構(gòu)的裂縫及孔隙結(jié)構(gòu)表征新方法,,定量分析了熱解過程中樣品裂縫寬度、裂縫方向,、分形維數(shù)及孔隙度等參數(shù)的變化規(guī)律,。研究結(jié)果表明:(1)本文所提出的裂縫性數(shù)字巖心精細(xì)化處理方法結(jié)合等位精細(xì)化中面提取算法,在準(zhǔn)確計(jì)算巖石物性參數(shù)的基礎(chǔ)上可實(shí)現(xiàn)對(duì)縫寬及裂縫方向分布的精確計(jì)算,,可達(dá)到對(duì)裂縫孔隙精細(xì)表征的目的,;(2)隨著熱解溫度的升高,油頁巖樣品孔隙度由18.3%升至20.9%,,且裂縫寬度不斷增大,,油頁巖樣品物性得到持續(xù)改善,但當(dāng)熱解進(jìn)行到一定程度后油頁巖孔隙結(jié)構(gòu)變化趨勢(shì)放緩,;(3)相同溫度條件下隨著有機(jī)質(zhì)含量的升高,,熱解后油頁巖樣品孔隙度由12.1%升至29.3%,但4 種樣品分形維數(shù)未隨著有機(jī)質(zhì)含量升高呈現(xiàn)出單調(diào)遞增趨勢(shì),,表明熱解裂縫復(fù)雜性除受有機(jī)質(zhì)含量影響外,,也受到樣品中有機(jī)質(zhì)初始分布的影響。本文可為油頁巖熱解后孔隙結(jié)構(gòu)精細(xì)表征提供新思路,。
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關(guān)鍵詞 : 數(shù)字巖心,三維重構(gòu),油頁巖,高溫?zé)峤?孔隙結(jié)構(gòu)表征
Abstract

As the primary conduit for oil and gas seepage, the pore and fracture structure of oil shale undergoes intricate changes during pyrolysis. However, the lack of understanding regarding its variations hinders effective reservoir classification and development. Therefore, it is important to investigate the influence of oil shale pyrolysis on pore structure at different temperatures and organic matter content. This paper proposes a new method based on 3D digital core reconstruction to quantify fractures and pore structures. The methodology employs parameters such as fracture width, fracture orientation, fractal dimension, and porosity to assess changes in pore and fracture structures throughout the pyrolysis process. The findings are as follows: (1) The proposed digital rock processing method and midplane extraction algorithm for fractured rock can accurately calculate fracture width and fracture orientation distribution. (2) As pyrolysis temperature increased, the porosity of oil shale samples rose from 18.3% to 20.9%, with a corresponding increase in fracture width, indicating improvements in the physical properties of the samples. However, the rate of change in pore and fracture structures decreased after pyrolysis (3) For fractured oil shale samples, porosity increased from 12.1% to 29.3% with higher organic matter content at consistent temperatures. However, Fractal analysis shows that pyrolysis fracture complexity is governed by both the content and, importantly, the initial spatial distribution of organic matter. This provides a new perspective for the precise characterization of pore structure after fracturing oil shale.


Key words: digital rock; 3D reconstruction; oil shale; high temperature pyrolysis; pore structure characterization
收稿日期: 2024-08-30 ????
PACS: ? ?
基金資助:國(guó)家青年科學(xué)基金項(xiàng)目“粗糙迂曲縫內(nèi)超臨界CO2 微細(xì)支撐劑攜帶機(jī)理研究”(52204021) 和國(guó)家自然科學(xué)基金專項(xiàng)項(xiàng)目“頁巖油儲(chǔ)層超
臨界CO2 聚能壓裂與封存基礎(chǔ)研究”(52341401) 聯(lián)合資助
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王斌, 孫廉賀, 楊兵, 楊睿月, 王海柱, 張?jiān)迄i, 王全, 劉銘盛. 基于三維數(shù)字巖心的油頁巖裂解孔隙重構(gòu)及表征研究. 石油科學(xué)通 報(bào), 2024, 04: 648-658 WANG Bin, SUN Lianhe, YANG Ruiyue, YANG Bing, WANG Haizhu, ZHANG Yunpeng, WANG Quan, LIU Mingsheng. Characterization of oil shale pore and fractures during pyrolysis using digital rock reconstruction. Petroleum Science Bulletin, 2024, 04: 648-658.
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