工程地质学报
工程地質學報
공정지질학보
2014年
6期
1279-1286
,共8页
孙亚丽%曹冬梅%方建平%李燕
孫亞麗%曹鼕梅%方建平%李燕
손아려%조동매%방건평%리연
衢州通仙门%岩石砌块%风化剥落深度%风化速度
衢州通仙門%巖石砌塊%風化剝落深度%風化速度
구주통선문%암석체괴%풍화박락심도%풍화속도
Tongxian gate of Quzhou%Rock block%Surface recession%Weathering rate
岩石的长期风化作用会造成岩石表面的剥落,这将导致石质文物产生无可挽回的破坏。为了更好地保护它们,需要开展在相同风化环境下岩石风化剥落深度和相对风化速度及其与不同岩性关系的研究。本文以衢州古城墙通仙门的多块岩石砌块为研究对象,利用自制的测量仪器,对不同岩性岩石砌块风化剥落深度和风化速度进行了研究;通过分析量测结果得出凝灰岩、砂岩、砾岩、含砾砂岩和粉砂岩相对灰岩的风化速度分别为0.005~0.059mm·a-1、0.032~0.097mm·a-1、0.004~0.058mm·a-1、0.021~0.033mm·a-1和0.015mm·a-1。研究结果表明:在相同的风化环境之中不同岩石砌块的风化速度从大到小排序为V砂岩>V凝灰岩>V含砾砂岩>V砾岩>V粉砂岩>V灰岩,即岩石抗风化能力从强到弱为:灰岩>粉砂岩>砾岩>含砾砂岩>凝灰岩>砂岩。由此,为石质文物的长期保护以及制定相关的保护措施提供了重要的理论依据。
巖石的長期風化作用會造成巖石錶麵的剝落,這將導緻石質文物產生無可輓迴的破壞。為瞭更好地保護它們,需要開展在相同風化環境下巖石風化剝落深度和相對風化速度及其與不同巖性關繫的研究。本文以衢州古城牆通仙門的多塊巖石砌塊為研究對象,利用自製的測量儀器,對不同巖性巖石砌塊風化剝落深度和風化速度進行瞭研究;通過分析量測結果得齣凝灰巖、砂巖、礫巖、含礫砂巖和粉砂巖相對灰巖的風化速度分彆為0.005~0.059mm·a-1、0.032~0.097mm·a-1、0.004~0.058mm·a-1、0.021~0.033mm·a-1和0.015mm·a-1。研究結果錶明:在相同的風化環境之中不同巖石砌塊的風化速度從大到小排序為V砂巖>V凝灰巖>V含礫砂巖>V礫巖>V粉砂巖>V灰巖,即巖石抗風化能力從彊到弱為:灰巖>粉砂巖>礫巖>含礫砂巖>凝灰巖>砂巖。由此,為石質文物的長期保護以及製定相關的保護措施提供瞭重要的理論依據。
암석적장기풍화작용회조성암석표면적박락,저장도치석질문물산생무가만회적파배。위료경호지보호타문,수요개전재상동풍화배경하암석풍화박락심도화상대풍화속도급기여불동암성관계적연구。본문이구주고성장통선문적다괴암석체괴위연구대상,이용자제적측량의기,대불동암성암석체괴풍화박락심도화풍화속도진행료연구;통과분석량측결과득출응회암、사암、력암、함력사암화분사암상대회암적풍화속도분별위0.005~0.059mm·a-1、0.032~0.097mm·a-1、0.004~0.058mm·a-1、0.021~0.033mm·a-1화0.015mm·a-1。연구결과표명:재상동적풍화배경지중불동암석체괴적풍화속도종대도소배서위V사암>V응회암>V함력사암>V력암>V분사암>V회암,즉암석항풍화능력종강도약위:회암>분사암>력암>함력사암>응회암>사암。유차,위석질문물적장기보호이급제정상관적보호조시제공료중요적이론의거。
Long-term weathering of rock will cause the rock surface recession,which will cause irreparable damage to stone cultural relics.Those precious stone cultural relics are being protected for a long time.But the result is not optimistic.In theory,in order to protect them well,it is important to study the relationship between the rock surface recession and the relative weathering rate with the different lithology in the same environment.The paper is intended to study the surface recession of different lithology rock blocks and their weathering rate.The rock blocks are part of the Tongxian gate of Quzhou ancient walls of national key cultural relics protection sites.An especially designed movable instrument is used.By analyzing the measured data,the weathering rates of different rocks are attained so as to provide an actual basis for the stone cultural relics and the development of relevant protective measures.The measurement results are from tufa,sandstone,conglomerate,pebbly sandstone and siltstone.Their weathering rates with respect to limestone are 0.005~0.059,0.032~0.097,0.004~0.058,0.021 ~0.033 and 0.01 5mm·a-1 , respectively.The results also show that under the same weathering environment,different weathering rates of rock block order from large to small is Vsandstone>Vtufa>Vpebblysandstone>Vconglomerate>Vsiltstone>Vlimestone,which means that the rock weathering resistance from strong to weak is:Vlimestone>Vsiltstone>Vconglomerate>Vpebblysandstone>Vtufa>Vsandstone.This study can provide an important data basis for the long-term protection of stone relics and formulate relevant protective measures.