红层砂岩与砾岩差异风化的湿度应力效应研究

doi:10.13722/j.cnki.jrme.2019.0345

Abstract
Figure/Table
References (0)
Related Citation (15)

Download: PDF (1020 KB) HTML (1 KB)
Export: BibTeX | EndNote (RIS)

Abstract Many researchers attribute the differential weathering of sandstone and conglomerate to differences in their physical and mechanical properties but pay less attention to external dynamic factors involved in differential weathering. We had a field study on twelve arched rock shelters and one natural arch developed in red-bed basins of Zhejiang province，conducted laboratorial wet-dry test and numerical modelling of moisture movement and moisture stress on sandstone and conglomerate. The failure characteristics of sandstone and conglomerate in wet-dry tests are consistent with the results of field investigation. Sandstone tends to collapse with spherical fractures，while conglomerate generally remains intact except that some gravels at surface drop off from the matrix. The disintegration rate of sandstone is much higher than that of conglomerate. Meanwhile，expansion and shrinkage deformation is 0.15–0.18 mm in sandstone，while 0.001–0.002 mm in conglomerate. The numerical modelling also reveals the mechanism of differential weathering of sandstone and conglomerate. Spherical moisture stress distributes in sandstone during water absorption and causes sandstone flaked like an onion. In contrast，moisture and moisture stress concentrate on the interface between gravel and matrix，and cause gravels dropped off from the matrix. The results reveal that moisture stress is the external dynamic factor controlling the differential weathering between red-bed sandstone and conglomerate

Key words： rock mechanics red-bed sandstone and conglomerate differential weathering laboratorial test numerical simulation moisture stress

	Service

	E-mail this article
	Add to my bookshelf
	Add to citation manager
	E-mail Alert
	RSS
	Articles by authors
	TAN Yufang1
	2
	3
	LI Lihui1
	2
	3
	YANG Zhifa1
	2
	3
	LIAO Xiaohui4

Cite this article:

TAN Yufang1,2,3, et al. Moisture stress effect and its control on differential weathering of red-bed sandstone and conglomerate[J]. , 2019, 38(S2): 3481-3492.

URL:

https://rockmech.whrsm.ac.cn/EN/10.13722/j.cnki.jrme.2019.0345 OR https://rockmech.whrsm.ac.cn/EN/Y2019/V38/IS2/3481

[1]	PENG H，PAN Z X，QIU Z W. Weathering pattern and development process of bedding-controlled caves at Mt. Danxiashan，China[J]. Zeitschrift Fur Geomorphologie，2015，59：165–182.
[2]	ZHU C，WU L，ZHU T，et al. Experimental studies on the Danxia landscape morphogenesis in Mt. Danxiashan，South China[J]. Journal of Geographical Sciences，2015，25(8)：943–966.
[3]	吕文，朱诚，彭华，等. 浙江江山市江郎山岩石岩性特征及其对丹霞地貌形成的影响[J]. 矿物岩石地球化学通报，2009，28(4)：349–355.(LV Wen，ZHU Cheng，PENG Hua，et al. The contribution of lithological characteristics to Danxia landform genesis in Jianglang Mountain，Zhejiang province[J]. Bulletin of Mineralogy，Petrology and Geochemistry，2009，28(4)：349–355.(in Chinese))
[4]	ALDRED J，EPPES M C，AQUINO K，et al. The influence of solar-induced thermal stresses on the mechanical weathering of rocks in humid mid-latitudes[J]. Earth Surface Processes and Landforms，2016，41(5)：603–614.
[5]	COLLINS B D，STOCK G M，EPPES M C，et al. Thermal influences on spontaneous rock dome exfoliation[J]. Nature Communications，2018，9：1–12.
[6]	GOMEZ-HERAS M，SMITH B J，FORT R. Surface temperature differences between minerals in crystalline rocks：Implications for granular disaggregation of granites through thermal fatigue[J]. Geomorphology，2006，78(3/4)：236–249.
[7]	LAMP J L，MARCHANT D R，MACKAY S L，et al. Thermal stress weathering and the spalling of Antarctic rocks[J]. Journal of Geophysical Research-Earth Surface，2017，122(1)：3–24.
[8]	罗炳生. 丹霞地貌形成过程的岩体温度应力效应[J]. 广东工学院学报，1994，11(4)：1–7.(LUO Bingsheng. Temperature stress effect of the rock mass in the formation procedure of Danxia landform[J]. Journal of Guangdong Institute of Technology，1994，11(4)：1–7.(in Chinese))
[9]	黄进，黄瑞红，苏泽霖. 丹霞洞穴地貌的初步研究[C]// 中国地质学会旅游地学与地质公园研究分会，旅游地学的理论与实践——旅游地学论文集第二集. 北京：地质出版社，2006：50–60.(HUANG Jin，HUANG Ruihong，SUI Zelin. A preliminary study on Danxia cave topography[C]// Toursim Geology and Geopark Research，Branch of China Geological Society，The Theory and Practice of Tourism Geology—Second Collection of Eassy on Tourism Geology. Beijing：Geological Publishing House，2006：50–60.(in Chinese))
[10]	冷洋洋，罗炳佳，张磊，等. 岩体温度应力效应及差异性风化对赤水丹霞的破坏作用[J]. 贵州地质，2017，34(2)：123–127.(LENG Yangyang，LUO Bingjia，ZHANG Lei，et al. The destructive effect of Chishui Danxia caused by rock mass temperature stress and differential weathering[J]. Guizhou Geology，2017，34(2)：123–127.(in Chinese))
[11]	BAUER S J，JOHNSON B. Effects of slow uniform heating on the physical properties of the westerly and charcoal granites[C]// Proceedings of the 20th U.S. Symposium on Rock Mechanics (USRMS). Austin，Texas：American Rock Mechanics Association，1979：12.
[12]	YONG C，WANG C. Thermally induced acoustic emission in westerly grainte[J]. Geophysical Research Letters，1980，7(12)：1 089–1 092.
[13]	GRIGGS D T. The factor of fatigue in rock exfoliation[J]. Journal of Geology，1936，44(7)：783–796.
[14]	苏天明. 万州地区近水平岩层高切坡差异风化与边坡崩塌失稳模式研究[博士学位论文][D]. 北京：中国科学院地质与地球物理研究所，2006.(SUI Tianming. Research on differential weathering and collapse model of high cut slope with nearly horizontal strata in Wanzhou district[Ph. D. Thesis][D]. Beijing：Institute of Geology and Geophysics，Chinese Academy of Sciences，2006.(in Chinese))
[15]	李丽慧，刘建立，傅燕，等. 龙游石窟洞室围岩长达8 a的风化速度及风化时限研究[J]. 工程地质学报，2012，20(5)：706–714.(LI Lihui，LIU Jianli，FU Yan，et al. Eight years test results of weathering rates and time limit prediction of chisel imprints on pelitic siltstone inside five Longyou caverns[J]. Journal of Engineering Geology，2012，20(5)：706–714.(in Chinese))
[16]	谌文武，林高潮，刘伟，等. 全风化灰绿色及红色泥岩物理力学性质对比研究[J]. 岩石力学与工程学报，2016，35(12)：2 572–2 582. (CHEN Weiwu，LIN Gaochao，LIU Wei，et al. Physical and mechanical properties of weathered green and red mudstones[J]. Chinese Journal of Rock Mechanics and Engineering，2016，35(12)：2 572–2 582.(in Chinese))
[17]	FAHEY B D，DAGESSE D F. An experimental study of the effect of humidity and temperature variations on the granular disintegration of argillaceous carbonate rocks in cold climates[J]. Arctic and Alpine Research，1984，16(3)：291–298.
[18]	OLIVIER H Some aspects of the influence of mineralogy and moisture redistribution on the weathering behaviour of mudrocks[C]// Proceedings of the 4th International Society for Rock Mechanics(ISRM) Congress. Lisbon：International Society for Rock Mechanics，1979：467–474.
[19]	孙训方，方孝淑，关来泰. 材料力学[M]. 北京：高等教育出版社，2009：387.(SUN Xunfang，FANG Xiaoshu，GUAN Laitai，et al. Mechanics of materials[M]. Beijing：Higher Education Press，2009：387.(in Chinese))
[20]	缪协兴. 湿度应力场理论的耦合方程[J]. 力学与实践，1995，17(6)：22–24.(MIU Xiexing. Coupled equations of theory on moisture stress field[J]. Mechanics in Engineering，1995，17(6)：22–24.(in Chinese))
[21]	缪协兴，杨成永，陈至达. 膨胀岩体中的湿度应力场理论[J]. 岩土力学，1993，14(4)：49–55.(MIU Xiexing，YANG Chengyong，CHENG Zhida. Theory on moisture stress field in swelling rock mass[J]. Rock and Soil Mechanics，1993，14(4)：49–55.(in Chinese))
[22]	朱珍德，张爱军，张勇，等. 基于湿度应力场理论的膨胀岩弹塑性本构关系[J]. 岩土力学，2004，25(5)：700–702.(ZHU Zhende，ZHANG Aijun，ZHANG Yong，et al. Elastoplastic constitutive law of swelling rock based on theory of moisture stress field[J]. Rock and Soil Mechanics，2004，25(5)：700–702.(in Chinese))
[23]	白冰，李小春. 湿度应力场理论的证明[J]. 岩土力学，2007，28(1)：89–92.(BAI Bing，LI Xiaochun. Proof of theory on moisture stress field[J]. Rock and Soil Mechanics，2007，28(1)：89–92.(in Chinese))
[24]	王士天，刘汉超，张倬元，等. 大型水域水岩相互作用及其环境效应研究[J]. 地质灾害与环境保护，1997，8(1)：70–90.(WANG Shitian，LIU Hanchao，ZHANG Zhuoyuan，et al. Research on water-rock interaction and its environmental effect on area with large waterways[J]. Journal of Geological Hazards and Environment Preservation，1997，8(1)：70–90.(in Chinese))
[25]	沈照理，王焰新. 水–岩相互作用研究的回顾与展望[J]. 地球科学，2002，27(2)：127–133.(SHEN Zhaoli，WANG Yanxin. Review and outlook of water-rock interation studies[J]. Earth Science-Journal of China University of Geosciences，2002，27(2)：127–133.(in Chinese))
[26]	徐光黎. 节理张开度水力学分析[J]. 勘察科学技术，1993，(2)：3–6.(XU Guangli. Hydraulic analysis of the joint aperture[J]. Site Investigation Science and Technology，1993，(2)：3–6.(in Chinese))
[27]	黄继忠，袁道先，万力，等. 水岩作用对云冈石窟石雕风化破坏的化学效应研究[J]. 敦煌研究，2010，41(6)：59–63.(HUANG Jizhong，YUAN Daoxian，WAN Li，et al. A study on chemical effect on the water-rock interaction on the weathering of stone sculpture Yungang Grottoes[J]. Dunhuang Research，2010，41(6)：59–63.(in Chinese))
[28]	李黎，王思敬，谷本親伯，等. 龙游石窟岩面水岩作用研究[J]. 工程地质学报，2008，16(6)：798–805.(LI Li，WANG Sijing，CHIKAOSA T，et al. Analysis of chemical interation between water and sandstone at Longyou Grottoes[J]. Journal of Engineering Geolgy，2008，16(6)：798–805.(in Chinese))
[29]	张中俭. 平遥古城古砖风化机制和防风化方法研究[J]. 工程地质学报，2017，25(3)：619–629.(ZHANG Zhongjian. Weathering mechanism and prevention methods of ancient brick in Pingyao city Shanxi province，China[J]. Journal of Engineering Geology，2017，25(3)：619–629.(in Chinese))
[30]	周翠英，邓毅梅，谭祥韶，等. 软岩在饱水过程中水溶液化学成分变化规律研究[J]. 岩石力学与工程学报，2004，23(22)：3 813–3 817. (ZHOU C Y，DENG Y M，TAN S X，et al. Testing study on variation regularites of solution components in saturation of soft rocks[J]. Chinese Journal of Rock Mechanics and Engineering，2004，23(22)：3 813–3 817.(in Chinese))
[31]	周翠英，邓毅梅，谭祥韶，等. 饱水软岩力学性质软化的试验研究与应用[J]. 岩石力学与工程学报，2005，24(1)：33–38.(ZHOU Cuiying，DENG Yimei，TAN Xiangshao，et al. Experimental research on softening mechanical properties of saturated soft rocks and application[J]. Chinese Journal of Rock Mechanics and Engineering，2005，24(1)：33–38.(in Chinese))
[32]	周翠英，谭祥韶，邓毅梅，等. 特殊软岩软化的微观机制研究[J]. 岩石力学与工程学报，2005，24(3)：394–400.(ZHOU Cuiying，TAN Xiangshao，DENG Yimei，et al. Research on softening micro- mechanism of special soft rocks[J]. Chinese Journal of Rock Mechanics and Engineering，2005，24(3)：394–400.(in Chinese))
[33]	丁瑜，周忠浩，吴立新，等. 重庆地区红层泥岩球状风化剥落特征及其形成机制[J]. 中国地质灾害与防治学报，2015，26(1)：108–112.(DING Yu，ZHOU Zhonghao，WU Lixin，et al. Characteristic and mechanism of spheroidal weathering exfoliation of reded mudstone in Chongqing[J]. The Chinese Journal of Geological Hazard and Control，2015，26(1)：108–112.(in Chinese))
[34]	HEALD M，HOLLINGSWORTH T，SMITH R. Alteration of sandstone as revealed by spheroidal weathering[J]. Journal of Sedimentary Research，1979，49(3)：901–909.
[35]	CHATTERJEE A，RAYMAHASHAY B. Spheroidal weathering of Deccan Basalt：a three-mineral model[J]. Quarterly Journal of Engineering Geology and Hydrogeology，1998，31(3)：175–179.
[36]	MOMENI A，KHANLARI G，HEIDARI M，et al. New engineering geological weathering classifications for granitoid rocks[J]. Engineering Geology，2015，185：43–51.
[37]	RICHARDS L A. Capillary conduction of liquids through porous mediums[J]. Physics，1931，1(5)：318–333.
[38]	FREEZE R A. Three dimensional，transient，saturated unsaturated flow in a groundwater basin[J]. Water Resources Research，1971，7(2)：347–366.
[39]	VAN GENUCHTEN M T. A closed-form equation for predicting the hydraulic conductivity of unsaturated soils 1[J]. Soil Science Society of America Journal，1980，44(5)：892–898.
[40]	WANG H F. Theory of linear poroelasticity: with applications to geomechanics and hydrogeology[M]. New Jersey：Princeton University Press，2000：301.
[41]	STUCK H，PLAGGE R，SIEGESMUND S. Numerical modeling of moisture transport in sandstone：the influence of pore space，fabric and clay content[J]. Environmental Earth Sciences，2013，69(4)：1 161– 1 187.
[42]	BIRD R B，STEWART W E，LIGHTFOOT E N. Transport phenomena[M]. 2nd ed. New York：John Wiley and Sons，Inc.，2002：912.
[43]	CARTER G F，PAUL D E. Materials science and engineering[M]. New York：CRC Press，1991：351.
[44]	徐文杰. 土石混合体细观结构力学及其边坡稳定性研究[博士学位论文][D]. 北京：中国科学院地质与地球物理研究所，2008.(XU Wenjie. Study on meso-structural mechanics(M-SM) of soil-rock mixture (S-RM) and its slope stability[Ph. D. Thesis][D]. Beijing：Institute of Geology and Geophysics，Chinese Academy of Sciences，2008.(in Chinese))