{"title":"天然断裂在微观尺度上对页岩力学性质和断裂模式的影响:以黔北地区下寒武统牛蹄塘地层为例","authors":"Zhong-Hu Wu, Chao Yang, Yu-Jun Zuo, Yi-Li Lou, Huai-Lei Song, Heng-Tao Cui, Mo-Tian Tang","doi":"10.1007/s40948-024-00743-3","DOIUrl":null,"url":null,"abstract":"<p>In order to explore the influence of natural fractures on the mechanical properties and failure modes of shale at the micro scale, uniaxial compression numerical experiments were conducted on the shale of the Niutang Formation in northern Guizhou with different natural fracture angles using a rock failure process system and digital image processing technology. It is shown that the compressive strength of shale increases with the increase of natural crack inclination, and the growth rate of shale compressive strength also increases. Shale's microscopic fractures can generally be classified into four categories. The first category is to sprout along the natural cracks to the outside of the shale, and eventually form a crack similar to the \"X\" type (0°); the second category is to sprout along the natural cracks to the middle and outside of the shale, and eventually form an inverted \"Y\" type crack (15°, 30°); the third category is to sprout along the natural cracks to the middle and outside of the shale, and eventually form an inverted \"Y\" type crack (15°, 30°); the second type sprouts along the natural fractures toward the middle and outside of the shale, forming inverted \"Y\"-type fractures (15°, 30°); the third type cracks along the sides of the natural fractures, forming \"Y\"-type fractures (45°); and the fourth type does not crack along the natural fractures, forming \"S\"-type fractures (60°, 75°, and 90°). In the low natural fracture dip shale model, tensile damage mainly occurs, accompanied by a small amount of compressive shear damage; in the high natural fracture dip shale model, tensile damage and compressive shear damage account for a larger proportion in the fracture process.This suggests that the presence of natural cracks in shale has a significant impact on stress distribution. There are two main types of acoustic emission signal distribution and evolutionary features, the evolutionary features of acoustic emission signal distribution are of two types, 0°-45° test and 60°-90° test, and the difference is mainly reflected in the damage stage, the damage of shale with high natural fracture inclination is more intense, which is manifested by the decrease in the number of acoustic emission events, but the level of acoustic emission events in the damage stage is higher, which can reach 61788, 46605 and 94315, the shale with high natural fracture inclination is more brittle.</p>","PeriodicalId":12813,"journal":{"name":"Geomechanics and Geophysics for Geo-Energy and Geo-Resources","volume":"96 1","pages":""},"PeriodicalIF":3.9000,"publicationDate":"2024-02-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Effect of natural fractures on mechanical properties and fracture patterns of shale at microscopic scale: an example from the Lower Cambrian Niutitang formation in Qianbei region\",\"authors\":\"Zhong-Hu Wu, Chao Yang, Yu-Jun Zuo, Yi-Li Lou, Huai-Lei Song, Heng-Tao Cui, Mo-Tian Tang\",\"doi\":\"10.1007/s40948-024-00743-3\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>In order to explore the influence of natural fractures on the mechanical properties and failure modes of shale at the micro scale, uniaxial compression numerical experiments were conducted on the shale of the Niutang Formation in northern Guizhou with different natural fracture angles using a rock failure process system and digital image processing technology. It is shown that the compressive strength of shale increases with the increase of natural crack inclination, and the growth rate of shale compressive strength also increases. Shale's microscopic fractures can generally be classified into four categories. The first category is to sprout along the natural cracks to the outside of the shale, and eventually form a crack similar to the \\\"X\\\" type (0°); the second category is to sprout along the natural cracks to the middle and outside of the shale, and eventually form an inverted \\\"Y\\\" type crack (15°, 30°); the third category is to sprout along the natural cracks to the middle and outside of the shale, and eventually form an inverted \\\"Y\\\" type crack (15°, 30°); the second type sprouts along the natural fractures toward the middle and outside of the shale, forming inverted \\\"Y\\\"-type fractures (15°, 30°); the third type cracks along the sides of the natural fractures, forming \\\"Y\\\"-type fractures (45°); and the fourth type does not crack along the natural fractures, forming \\\"S\\\"-type fractures (60°, 75°, and 90°). In the low natural fracture dip shale model, tensile damage mainly occurs, accompanied by a small amount of compressive shear damage; in the high natural fracture dip shale model, tensile damage and compressive shear damage account for a larger proportion in the fracture process.This suggests that the presence of natural cracks in shale has a significant impact on stress distribution. There are two main types of acoustic emission signal distribution and evolutionary features, the evolutionary features of acoustic emission signal distribution are of two types, 0°-45° test and 60°-90° test, and the difference is mainly reflected in the damage stage, the damage of shale with high natural fracture inclination is more intense, which is manifested by the decrease in the number of acoustic emission events, but the level of acoustic emission events in the damage stage is higher, which can reach 61788, 46605 and 94315, the shale with high natural fracture inclination is more brittle.</p>\",\"PeriodicalId\":12813,\"journal\":{\"name\":\"Geomechanics and Geophysics for Geo-Energy and Geo-Resources\",\"volume\":\"96 1\",\"pages\":\"\"},\"PeriodicalIF\":3.9000,\"publicationDate\":\"2024-02-08\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geomechanics and Geophysics for Geo-Energy and Geo-Resources\",\"FirstCategoryId\":\"5\",\"ListUrlMain\":\"https://doi.org/10.1007/s40948-024-00743-3\",\"RegionNum\":2,\"RegionCategory\":\"工程技术\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"ENERGY & FUELS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geomechanics and Geophysics for Geo-Energy and Geo-Resources","FirstCategoryId":"5","ListUrlMain":"https://doi.org/10.1007/s40948-024-00743-3","RegionNum":2,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"ENERGY & FUELS","Score":null,"Total":0}
引用次数: 0
摘要
为了在微观尺度上探讨天然裂隙对页岩力学性质和破坏模式的影响,利用岩石破坏过程系统和数字图像处理技术,对贵州北部牛塘地层不同天然裂隙角的页岩进行了单轴压缩数值实验。结果表明,页岩的抗压强度随天然裂隙倾角的增大而增大,页岩抗压强度的增长率也随之增大。页岩的微观裂缝一般可分为四类。第一类是沿天然裂缝向页岩外侧萌生,最终形成类似 "X "型的裂缝(0°);第二类是沿天然裂缝向页岩中部和外侧萌生,最终形成倒 "Y "型裂缝(15°、30°);第三类是沿天然裂缝向页岩中部和外侧萌生,最终形成倒 "Y "型裂缝(15°、30°);第二类沿天然裂缝向页岩中部和外侧萌生,形成倒 "Y "型裂缝(15°、30°);第三类沿天然裂缝两侧开裂,形成 "Y "型裂缝(45°);第四类不沿天然裂缝开裂,形成 "S "型裂缝(60°、75°和 90°)。在低天然断裂倾角页岩模型中,主要发生拉伸破坏,同时伴有少量压缩剪切破坏;在高天然断裂倾角页岩模型中,拉伸破坏和压缩剪切破坏在断裂过程中占较大比例。声发射信号分布及演化特征主要有两种类型,声发射信号分布的演化特征有0°-45°试验和60°-90°试验两种类型,其差异主要体现在破坏阶段上,天然断裂倾角高的页岩破坏强度较大,表现为声发射事件数量减少,但破坏阶段声发射事件水平较高,可达61788、46605和94315,天然断裂倾角高的页岩脆性较大。
Effect of natural fractures on mechanical properties and fracture patterns of shale at microscopic scale: an example from the Lower Cambrian Niutitang formation in Qianbei region
In order to explore the influence of natural fractures on the mechanical properties and failure modes of shale at the micro scale, uniaxial compression numerical experiments were conducted on the shale of the Niutang Formation in northern Guizhou with different natural fracture angles using a rock failure process system and digital image processing technology. It is shown that the compressive strength of shale increases with the increase of natural crack inclination, and the growth rate of shale compressive strength also increases. Shale's microscopic fractures can generally be classified into four categories. The first category is to sprout along the natural cracks to the outside of the shale, and eventually form a crack similar to the "X" type (0°); the second category is to sprout along the natural cracks to the middle and outside of the shale, and eventually form an inverted "Y" type crack (15°, 30°); the third category is to sprout along the natural cracks to the middle and outside of the shale, and eventually form an inverted "Y" type crack (15°, 30°); the second type sprouts along the natural fractures toward the middle and outside of the shale, forming inverted "Y"-type fractures (15°, 30°); the third type cracks along the sides of the natural fractures, forming "Y"-type fractures (45°); and the fourth type does not crack along the natural fractures, forming "S"-type fractures (60°, 75°, and 90°). In the low natural fracture dip shale model, tensile damage mainly occurs, accompanied by a small amount of compressive shear damage; in the high natural fracture dip shale model, tensile damage and compressive shear damage account for a larger proportion in the fracture process.This suggests that the presence of natural cracks in shale has a significant impact on stress distribution. There are two main types of acoustic emission signal distribution and evolutionary features, the evolutionary features of acoustic emission signal distribution are of two types, 0°-45° test and 60°-90° test, and the difference is mainly reflected in the damage stage, the damage of shale with high natural fracture inclination is more intense, which is manifested by the decrease in the number of acoustic emission events, but the level of acoustic emission events in the damage stage is higher, which can reach 61788, 46605 and 94315, the shale with high natural fracture inclination is more brittle.
期刊介绍:
This journal offers original research, new developments, and case studies in geomechanics and geophysics, focused on energy and resources in Earth’s subsurface. Covers theory, experimental results, numerical methods, modeling, engineering, technology and more.