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Mechanism of anomalous low friction phenomenon in deep block rock mass
Deep rock mass has the unique "self-stressed" block-hierarchical structure, anomalous low friction (ALF) was one of the typical nonlinear get-mechanical and dynamic responses in deep block rock mass, which occurred as the result of movements of large-scale get-blocks under the impact of external pul...
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Published in: | Mining science and technology (China) 2009-07, Vol.19 (4), p.409-419 |
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description | Deep rock mass has the unique "self-stressed" block-hierarchical structure, anomalous low friction (ALF) was one of the typical nonlinear get-mechanical and dynamic responses in deep block rock mass, which occurred as the result of movements of large-scale get-blocks under the impact of external pulses (such as a deep confined explosion, earthquakes, rock bursts and etc.). ALF phenomenon obtained its name to describe the curious phenomenon that the friction between interacting get-blocks qua- si-periodically disappears at some discrete points in time along the direction orthogonal to the direction of the external pulse. With the objective to confirm the existence of the ALF phenomenon and study the get-mechanical conditions for its occurrence experi- mentally and theoretically, laboratory tests on granite and cement mortar block models were carried out on a multipurpose testing system developed independently. The ALF phenomenon was realized under two loading schemes, i.e., blocks model and a working block were acted upon jointly by the action of a vertical impact and a horizontal static force, as well as the joint action of both ver- tical and horizontal impacts with differently delayed time intervals. We obtained the rules on variation of horizontal displacements of working blocks when the ALF phenomenon was realized in two tests. The discrete time delay intervals, corresponding to local maxima and minima of the horizontal displacement amplitudes and residual horizontal displacements of the working block, satis- fied canonical sequences multiplied by (√2)'. Some of these time intervals satisfied the quantitative expression (√2)' ,alva. At last, 1D dynamic theoretical model was established, the analytical results agreed better with the test data, while the quantitative expression drawn from test data was not validated well in theoretical analyses. |
doi_str_mv | 10.1016/S1674-5264(09)60077-6 |
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ALF phenomenon obtained its name to describe the curious phenomenon that the friction between interacting get-blocks qua- si-periodically disappears at some discrete points in time along the direction orthogonal to the direction of the external pulse. With the objective to confirm the existence of the ALF phenomenon and study the get-mechanical conditions for its occurrence experi- mentally and theoretically, laboratory tests on granite and cement mortar block models were carried out on a multipurpose testing system developed independently. The ALF phenomenon was realized under two loading schemes, i.e., blocks model and a working block were acted upon jointly by the action of a vertical impact and a horizontal static force, as well as the joint action of both ver- tical and horizontal impacts with differently delayed time intervals. We obtained the rules on variation of horizontal displacements of working blocks when the ALF phenomenon was realized in two tests. The discrete time delay intervals, corresponding to local maxima and minima of the horizontal displacement amplitudes and residual horizontal displacements of the working block, satis- fied canonical sequences multiplied by (√2)'. Some of these time intervals satisfied the quantitative expression (√2)' ,alva. At last, 1D dynamic theoretical model was established, the analytical results agreed better with the test data, while the quantitative expression drawn from test data was not validated well in theoretical analyses.</description><identifier>ISSN: 1674-5264</identifier><identifier>EISSN: 2212-6066</identifier><identifier>DOI: 10.1016/S1674-5264(09)60077-6</identifier><language>eng</language><publisher>Elsevier B.V</publisher><subject>anomalous low friction ; block-hierarchical structure ; canonical sequence ; deep block rock mass ; optical fiber displacement meter ; 摩擦现象 ; 深部岩体</subject><ispartof>Mining science and technology (China), 2009-07, Vol.19 (4), p.409-419</ispartof><rights>2009 China University of Mining and Technology</rights><rights>Copyright © Wanfang Data Co. Ltd. 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ALF phenomenon obtained its name to describe the curious phenomenon that the friction between interacting get-blocks qua- si-periodically disappears at some discrete points in time along the direction orthogonal to the direction of the external pulse. With the objective to confirm the existence of the ALF phenomenon and study the get-mechanical conditions for its occurrence experi- mentally and theoretically, laboratory tests on granite and cement mortar block models were carried out on a multipurpose testing system developed independently. The ALF phenomenon was realized under two loading schemes, i.e., blocks model and a working block were acted upon jointly by the action of a vertical impact and a horizontal static force, as well as the joint action of both ver- tical and horizontal impacts with differently delayed time intervals. We obtained the rules on variation of horizontal displacements of working blocks when the ALF phenomenon was realized in two tests. The discrete time delay intervals, corresponding to local maxima and minima of the horizontal displacement amplitudes and residual horizontal displacements of the working block, satis- fied canonical sequences multiplied by (√2)'. Some of these time intervals satisfied the quantitative expression (√2)' ,alva. At last, 1D dynamic theoretical model was established, the analytical results agreed better with the test data, while the quantitative expression drawn from test data was not validated well in theoretical analyses.</description><subject>anomalous low friction</subject><subject>block-hierarchical structure</subject><subject>canonical sequence</subject><subject>deep block rock mass</subject><subject>optical fiber displacement meter</subject><subject>摩擦现象</subject><subject>深部岩体</subject><issn>1674-5264</issn><issn>2212-6066</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2009</creationdate><recordtype>article</recordtype><recordid>eNqFUEtLAzEQDqJgUX-CEDwpsjrJptnNSUR8geJBPYckO9vGbpOa-P71pla8OswDZr55fYTsMjhiwOTxPZONqMZcin1QBxKgaSq5RkacM15JkHKdjP4gm2Qn5ycoUretYu2IXNyim5rg85zGnpoQ52aIr5kO8Z32ybsXHwNdTLEUigXqA-0QF9QO0c1oWrq5yXmbbPRmyLjzG7fI48X5w9lVdXN3eX12elM53jasUmNhewud5K2wJSHHkpu2aQG7WjnDTG1qy4QQ3DauV6JWTGDHLCrboWG83iKHq7nvJvQmTPRTfE2hbNRfk9ln9_FhNXIABQKAFfR4hXYp5pyw14vk5yZ9agZ6yZ7-YU8vqdGg9A97Wpa-k1UfllfePCadncfgsPMJ3Yvuov93wt7v5mkMk2dfLrXGzXo_oK6ZAFm0_gYURoGR</recordid><startdate>200907</startdate><enddate>200907</enddate><creator>WU, Hao</creator><creator>FANG, Qin</creator><creator>ZHANG, Ya-dong</creator><creator>LU, Yu-sheng</creator><creator>LIU, Jin-chun</creator><general>Elsevier B.V</general><general>Engineering Institute of Engineering Corps, PLA University of Science and Technology, Nanjing, Jiangsu 210007, China</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>~WA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>200907</creationdate><title>Mechanism of anomalous low friction phenomenon in deep block rock mass</title><author>WU, Hao ; FANG, Qin ; ZHANG, Ya-dong ; LU, Yu-sheng ; LIU, Jin-chun</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c2871-954bfb0d6284b8716562a8780ed39ca1a3a3b14442b7cf943914ed1be9bdea123</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2009</creationdate><topic>anomalous low friction</topic><topic>block-hierarchical structure</topic><topic>canonical sequence</topic><topic>deep block rock mass</topic><topic>optical fiber displacement meter</topic><topic>摩擦现象</topic><topic>深部岩体</topic><toplevel>online_resources</toplevel><creatorcontrib>WU, Hao</creatorcontrib><creatorcontrib>FANG, Qin</creatorcontrib><creatorcontrib>ZHANG, Ya-dong</creatorcontrib><creatorcontrib>LU, Yu-sheng</creatorcontrib><creatorcontrib>LIU, Jin-chun</creatorcontrib><collection>中文科技期刊数据库</collection><collection>中文科技期刊数据库-CALIS站点</collection><collection>中文科技期刊数据库-7.0平台</collection><collection>中文科技期刊数据库- 镜像站点</collection><collection>CrossRef</collection><collection>Wanfang Data Journals - Hong Kong</collection><collection>WANFANG Data Centre</collection><collection>Wanfang Data Journals</collection><collection>万方数据期刊 - 香港版</collection><collection>China Online Journals (COJ)</collection><collection>China Online Journals (COJ)</collection><jtitle>Mining science and technology (China)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>WU, Hao</au><au>FANG, Qin</au><au>ZHANG, Ya-dong</au><au>LU, Yu-sheng</au><au>LIU, Jin-chun</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Mechanism of anomalous low friction phenomenon in deep block rock mass</atitle><jtitle>Mining science and technology (China)</jtitle><addtitle>Mining Science and Technology</addtitle><date>2009-07</date><risdate>2009</risdate><volume>19</volume><issue>4</issue><spage>409</spage><epage>419</epage><pages>409-419</pages><issn>1674-5264</issn><eissn>2212-6066</eissn><abstract>Deep rock mass has the unique "self-stressed" block-hierarchical structure, anomalous low friction (ALF) was one of the typical nonlinear get-mechanical and dynamic responses in deep block rock mass, which occurred as the result of movements of large-scale get-blocks under the impact of external pulses (such as a deep confined explosion, earthquakes, rock bursts and etc.). ALF phenomenon obtained its name to describe the curious phenomenon that the friction between interacting get-blocks qua- si-periodically disappears at some discrete points in time along the direction orthogonal to the direction of the external pulse. With the objective to confirm the existence of the ALF phenomenon and study the get-mechanical conditions for its occurrence experi- mentally and theoretically, laboratory tests on granite and cement mortar block models were carried out on a multipurpose testing system developed independently. The ALF phenomenon was realized under two loading schemes, i.e., blocks model and a working block were acted upon jointly by the action of a vertical impact and a horizontal static force, as well as the joint action of both ver- tical and horizontal impacts with differently delayed time intervals. We obtained the rules on variation of horizontal displacements of working blocks when the ALF phenomenon was realized in two tests. The discrete time delay intervals, corresponding to local maxima and minima of the horizontal displacement amplitudes and residual horizontal displacements of the working block, satis- fied canonical sequences multiplied by (√2)'. Some of these time intervals satisfied the quantitative expression (√2)' ,alva. At last, 1D dynamic theoretical model was established, the analytical results agreed better with the test data, while the quantitative expression drawn from test data was not validated well in theoretical analyses.</abstract><pub>Elsevier B.V</pub><doi>10.1016/S1674-5264(09)60077-6</doi><tpages>11</tpages></addata></record> |
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subjects | anomalous low friction block-hierarchical structure canonical sequence deep block rock mass optical fiber displacement meter 摩擦现象 深部岩体 |
title | Mechanism of anomalous low friction phenomenon in deep block rock mass |
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