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首頁(yè)» 過(guò)刊瀏覽» 2024» Vol.9» lssue(3) 513-524     DOI : 10.3969/j.issn.2096-1693.2024.03.038
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砂巖雙軸壓縮應(yīng)力狀態(tài)下的拉伸強(qiáng)度的實(shí)驗(yàn)研究
鞠盈彤, 陳勉, 楊帥
1 中國(guó)石油大學(xué)( 北京) 石油工程學(xué)院,北京 102249 2 中國(guó)石油勘探開(kāi)發(fā)研究院,北京 100083
Experimental study on tensile strength of sandstone under biaxial compressive stress
JU Yingtong, CHEN Mian, YANG Shuai
1 College of Petroleum Engineering, China University of Petroleum-Beijing, Beijing 102249, China 2 PetroChina Research Institute of Petroleum Exploration & Development, Beijing 100083, China

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摘要  巖石材料的拉伸強(qiáng)度對(duì)于井壁穩(wěn)定校核計(jì)算是一個(gè)比較重要的基礎(chǔ)參數(shù)。一般的,對(duì)于金屬材料,可以通過(guò)拉伸試驗(yàn)機(jī)來(lái)直接獲得抗拉強(qiáng)度;但是對(duì)于巖土類材料,這種方法從第一步制樣上可行性就較差。在實(shí)驗(yàn)室內(nèi)獲得巖石抗拉強(qiáng)度最常用的方法是巴西劈裂法,這是一種間接獲得巖石單軸抗拉強(qiáng)度的方法,目前被ISRM(國(guó)際巖石力學(xué)協(xié)會(huì))推薦并得到了廣泛的應(yīng)用。但這種方法也存在一定的局限性:首先,由于無(wú)法還原巖石的初始?jí)簩?shí)狀態(tài),因此在校核超深層巖石的拉伸強(qiáng)度時(shí)會(huì)有偏差;此外,這種方法的前提假設(shè)是巖石在線彈性階段過(guò)后直接發(fā)生脆性破壞,這與砂巖實(shí)際變形規(guī)律不符。基于以上問(wèn)題,本文從屈服理論出發(fā),通過(guò)雙軸壓縮實(shí)驗(yàn)的方法確定了砂巖在地下的真實(shí)拉伸屈服強(qiáng)度以及極限拉伸強(qiáng)度,實(shí)驗(yàn)表明砂巖的屈服強(qiáng)度隨圍壓增大而增大,符合巖石材料越致密強(qiáng)度越高的普遍認(rèn)識(shí)。通過(guò)擬合外推可以得到等效的砂巖單軸拉伸屈服強(qiáng)度,與巴西實(shí)驗(yàn)數(shù)據(jù)結(jié)果非常接近,驗(yàn)證了這種方法獲得帶圍壓下砂巖拉伸屈服強(qiáng)度的可靠性。通過(guò)研究雙軸壓縮應(yīng)力狀態(tài)下砂巖的拉伸強(qiáng)度,可以為卸載工況下砂巖發(fā)生拉伸破壞提供更準(zhǔn)確的校核依據(jù),為砂巖井壁穩(wěn)定提供理論與實(shí)驗(yàn)支撐。
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關(guān)鍵詞 : 砂巖,拉伸屈服強(qiáng)度,雙軸壓縮應(yīng)力狀態(tài),井壁穩(wěn)定,理論方法
Abstract

The tensile strength of rock material is an important and basic parameter when it comes to wellbore stability. In general, for metal, we can obtain the tensile strength in a direct way – the Tensile Test. However, for geotechnical materials, this method is impractical from the first step of sample preparation. Generally, the most commonly used method to obtain the tensile strength of rocks in the laboratory is using the Brazilian Test, which is an indirect approach. Now, this method is recommended by ISRM and has been extensively accepted by the whole community. However, this method has certain limitations. First, since it cannot restore the initial compacted state of the rock, there may be deviations when determining the tensile strength of ultra-deep rock formation. Additionally, the underlying assumption of this method is that the rock undergoes brittle failure directly after the linear elastic stage, which does not align with the actual deformation behavior of ultra-deep sandstone. Based on the problems mentioned above, in this paper, the real tensile yield strength and ultimate tensile strength of sandstone are determined through Biaxial Compression Tests. The real tensile yield strength and ultimate tensile strength of underground sandstone can be determined by a Biaxial Compression Test. The results show that they both increase along with the confining pressure, which accords with the common understanding that the denser the rock material, the higher the strength. The equivalent uniaxial tensile yield strength of sandstone can be obtained by fitting-extrapolation, which is very close to the results of Brazilian Tests, verifying the reliability of this method. By studying the tensile strength of sandstone under biaxial compressive stress, it can provide a more accurate basis for checking tensile failure under unloading conditions, as well as the theoretical and experimental support for the stability of sandstone wellbores.


Key words: sandstone; tensile yield strength; biaxial compressive stress; wellbore stability; theoretical approach
收稿日期: 2024-06-28     
PACS:    
基金資助:國(guó)家自然科學(xué)基金重點(diǎn)項(xiàng)目“提高超深大斜度井壓裂效率的關(guān)鍵力學(xué)問(wèn)題研究”(52334001) 資助
通訊作者: [email protected]
引用本文:   
鞠盈彤, 陳勉, 楊帥. 砂巖雙軸壓縮應(yīng)力狀態(tài)下的拉伸強(qiáng)度的實(shí)驗(yàn)研究. 石油科學(xué)通報(bào), 2024, 03: 513-524 JU Yingtong, CHEN Mian, YANG Shuai. Experimental study on tensile strength of sandstone under biaxial compressive stress. Petroleum Science Bulletin, 2024, 03: 513-524.
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