Deformational behavior and change of micro-fabric of rocks in creep

岩石蠕变变形行为及微结构变化

• 批准号: 08455480
• 负责人: YAMASHITA Shigeru
• 金额: $ 3.2万
• 依托单位: AKITA UNIVERSITY
• 依托单位国家: 日本
• 项目类别: Grant-in-Aid for Scientific Research (B)
• 财政年份: 1996
• 资助国家: 日本
• 起止时间: 1996 至 1997
• 项目状态: 已结题
• 来源: https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-08455480/
• 关键词: Creep; Creep Curve; Axial Strain Rate; Crack; Pore; Agent for Detecting Crack and Pore; Microscopic Observation; Failure Mechanism of Creep; クリープ軸ひずみ速度; 画像解析

Recently, much attention has been paid to the utilization of underground to build the repository for nuclear waste, the underground power house, the facilities for storage of oil, water, air and food, and so on. In the construction, maintenance and management of these structures, it has become important to evaluate the long-term stability of rockmass.In this study, to clarify the failure phenomenon and machanism of creep in rocks, a series of uniaxial compression tests, uniaxial creep tests and the microscopic observations was carried out.Creep tests were done for KIMACHI sandstone, AKIYOSHI marble, OGINO tuff and KURIHASHI granodiorite. Judging from the results of creep tests, secondary region in creep curve, which is divided into 3 regions, is subdivided into 2 regions according to the behavior of axial strain rate. The subdivided former region is characterized by the decrease of axial strain rate, and the latter one is by the increase of it.The thin sections were made from the rock … More specimens loaded until some compressive stress level and observed by the microscope. From the microscopic observations, it was found that the agent for detecting the cracks and pores in rocks has to be selected so that it may be suitable for the fabric and texture of each rock. Then, from the microscopic observations of the thin sections of KURIHASHI granodiorite loaded under creep tests, it was recognized that the intracrystalline microcracks extend mainly, and the number of intercrystalline microcracks increases as creep proceeds.Also, to investigate the relationship between the failure processes of uniaxial compression and uniaxial compressive creep, the uniaxial compression tests were done for the rock specimens after creep load is applied to them during some elapsed time or until a given creep region. From the results of these tests, it was found that the residual uniaxial compressive strengths of rock specimens don't change until the former secondary creep region, and are lower from the latter one with the passage of time. Less

近年来，利用地下建设核废料库、地下发电厂房、石油、水、空气和食品储存设施等的建设、维护和管理受到广泛关注。为了阐明岩石蠕变的破坏现象和机理，开展了一系列的单轴压缩试验、单轴蠕变试验和显微观察，以评价岩体的长期稳定性。 .进行蠕变测试对于KIMACHI砂岩、AKIYOSHI大理石、荻野凝灰岩和栗桥花岗闪长岩，从蠕变试验结果来看，蠕变曲线中的次要区域根据轴向应变率的行为被细分为2个区域。前一区域的特征是轴向应变率的减小，而后一区域的特征是轴向应变率的增加。薄片是由岩石制成的……更多样本加载直到一些从显微观察发现，必须选择适合每种岩石的结构和纹理的检测剂。通过蠕变试验加载的栗桥花岗闪长岩薄片的显微观察，发现晶内微裂纹主要是扩展的，并且晶间微裂纹的数量随着蠕变的进行而增加。为了研究单轴压缩破坏过程和单轴压缩蠕变之间的关系，在一段时间内或直到给定的蠕变区域之前，对岩石样本施加蠕变载荷后进行单轴压缩试验。 ，发现岩石试件的残余单轴抗压强度直到前一个二次蠕变区才发生变化，并且随着时间的推移，其残余单轴抗压强度逐渐低于后者。

项目成果

山下 秀、杉本 文男、デンベレル・ナムスライ、山内 優、鴨志田 直人、菊山 清児: "長期載荷における変形破壊挙動(岩盤の長期安定性)" 資源・素材'97(札幌). 企画発表A-3. 99-103 (1997)

Hide Yamashita、Fumio Sugimoto、Dembele Namsulai、Yu Yamauchi、Naoto Kamoshida、Seiji Kikuyama：“长期荷载下的变形破坏行为（岩体的长期稳定性）”资源和材料 97（札幌）项目演示 A-。 3. 99 -103 (1997)

Shigeru YAMASHITA,Fumio SUGIMOTO,Masaru YAMAUCHI et al.: "Changes of Micro-Structures of a Soft Rock on the Creep Loading Processes-Studies on the creep mechanism under compressive load of rocks (part-1) -" J.of Mining and Materials Processing Institute o

Shigeru YAMASHITA、Fumio SUGIMOTO、Masaru YAMAUCHI 等：“蠕变加载过程中软岩微观结构的变化 - 岩石压缩载荷下蠕变机制的研究（第 1 部分）-” J.of Mining and

S.Yamashita F.Sugimoto,etc.: "Estimation of Long-Term Stability of Mine Pillars in Underground Pit." 15th International Conference on Ground Controll in Mining. (Colorado School of Mines ; August 13-15,1996). (Proceedings). 685-698 (1996)

S.Yamashita F.Sugimoto等：“地下矿坑矿柱长期稳定性的估计”。

山内 優, 山崎貴博, 山下 秀, 杉本文男: "軟岩の圧縮クリープ過程と一軸圧縮破壊過程の関連性-岩石のクリープ破壊機構に関する研究(その2)-" 資源と素材. 114・3(印刷中). (1998)

Yu Yamauchi、Takahiro Yamazaki、Hide Yamashita、Fumio Sugimoto：“软岩压缩蠕变过程与单轴压缩断裂过程的关系 - 岩石蠕变断裂机制研究（第 2 部分）-”资源与材料 114・3（出版中） ））（1998）。

山下 秀, 杉本文男, 山内 優, 森聡, デンベレル・ナムスライ: "軟岩の圧縮クリープ過程と微視的構造の変化-岩石のクリープ破壊機構に関する研究(その1)-" 資源と素材. 113・11. 817-824 (1997)

Hide Yamashita，Fumio Sugimoto，Yu Yamauchi，Satoshi Mori，Dembele Namsulai：“软岩的压缩蠕变过程和微观结构的变化 - 岩石蠕变破裂机制的研究（第1部分）”资源和材料113・11 .817-。 824 (1997)