环境对交河故城破坏机理研究
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摘要
交河故城遗址在自然和人为环境的影响下,已经遭受了严重的破坏,交河故城的环境主要特点是风沙大,温差大,土体耐崩解性差,矿物成分的耐风化、热膨胀系数有差异,位于新构造活动带。它的主要病害有风蚀、雨蚀、裂隙、崩塌等,交河故城的破坏主要是这些因素的综合作用。通过对交河故城赋存环境和病害的调查,分析它的赋存环境因素对土遗址的作用机理,认为风是交河故城破坏的主要外动力,风蚀病害是交河故城的最主要病害,风参与了所有的破坏活动;温差变化大、雨蚀、地质构造和地震是它破坏的因素之一。温度变化引起土体内水分含量的变化是表层土体风化的主要因素;土体中可溶盐、方解石、长石含量高,是它抵抗破坏性能差的主要内因;同时,建议可用PS材料对它进行保护加固。
The Ruins of Jiaohe is a national major preservation unit of cultural relic,It have already been seriously demolished by the natural and artificial environment,The main characteristics of the environment of The Ruins of Jiaohe is big sandstorm,the big difference of temperature,the bad slake durability of soil mass,the resist weathering and heat dilatability coefficient of the mineral is difference,located the new tectonic movement belt.Its primary damages is weathering,rain erode,cranny and collapse etc.The breakage of The Ruins of Jiaohe is these factors to synthesize effect.Pass to investigate the conservational environment and the damages of its,analyzing the action mechanism that the environment factor impact the earthen sites,thinking that the wind is a main outside power to the breakage of The Ruins of Jiaohe,The wind erode is most damage of The Ruins of Jiaohe,the wind participates in all sabotage;The great difference in temperature,rain erode,geology structure and the earthquake is one of the factor of its breakage.It is the primary factor of the surface layer soil weathering that the temperature variety bring on the soil internal water content variety.The bad capability to resist destroyed rest with plenty salt,feldspar,calcite within the soil.So the material PS is suggested to use.
The Ruins of Jiaohe is a national major preservation unit of cultural relic,It have already been seriously demolished by the natural and artificial environment,The main characteristics of the environment of The Ruins of Jiaohe is big sandstorm,the big difference of temperature,the bad slake durability of soil mass,the resist weathering and heat dilatability coefficient of the mineral is difference,located the new tectonic movement belt.Its primary damages is weathering,rain erode,cranny and collapse etc.The breakage of The Ruins of Jiaohe is these factors to synthesize effect.Pass to investigate the conservational environment and the damages of its,analyzing the action mechanism that the environment factor impact the earthen sites,thinking that the wind is a main outside power to the breakage of The Ruins of Jiaohe,The wind erode is most damage of The Ruins of Jiaohe,the wind participates in all sabotage;The great difference in temperature,rain erode,geology structure and the earthquake is one of the factor of its breakage.It is the primary factor of the surface layer soil weathering that the temperature variety bring on the soil internal water content variety.The bad capability to resist destroyed rest with plenty salt,feldspar,calcite within the soil.So the material PS is suggested to use.
引文
[1]郭宏.文物保护环境概论[M].北京:科学出版社,2001.
[2]潘别桐,黄克忠.文物保护与环境地质[M].武汉:中国地质大学出版社,1992.
[3]田琳.交河故城遗址水文地质调查报告[C].解耀华编.交河故城保护与研究·乌鲁木齐:新疆人民出版社,1999:111-130.
[4]解耀华.交河故城的历史及保护修缮工程[C].解耀华编.交河故城保护与研究·乌鲁木齐:新疆人民出版社,1999:34-61.
[5]田琳.交河故城生土建筑遗存保护加固实验报告[C].交河故城保护与研究·乌鲁木齐:新疆人民出版社,1999:146-154.
[6]慕福智.吐鲁番地区大降水的天气动力学特征[J].新疆气象,1995,18(2):4-8.
[7]高国英,聂晓红.吐鲁番地区地震活动与应力场特征分析[J].地震地磁观测与研究,2000,21(6):39-44.
[8]邓起东,冯先岳,张培震.天山活动构造[M].北京:地震出版社,2000.
[9]李锁在,廖立兵.矿物热膨胀的晶体化学研究综述[J].高校地质学报,2002,6(2):333-339.
[10]刘均荣,等.岩石热增渗机理初探[J].石油钻采工艺,2003,25(5):43-46.
[11]王永华,刘文荣.矿物学[M].北京:地质出版社,1985.
[12]史謌,等.结晶岩的水化膨胀研究[J].地球物理学报,2000,43(6):798-804.
[13]费雪良,李斌.硫酸盐渍土压实特性及盐胀机理研究[J].中国公路学报,1995,8(1):44-49.
[14]赵晓光,石辉.水蚀作用下土壤抗蚀能力的表征[J].干旱区地理,2003,26(1):12-15.
[15]郭耀文.雨滴侵蚀特征分析[J].中国水土保持,1997,4:15-18.
[16]柳洪亮.交河故城城市布局调查[C].解耀华编.交河故城保护与研究·乌鲁木齐:新疆人民出版社,1999:235-240.
[17]李最雄.丝绸之路古遗址保护[M].北京:科学出版社,2003.
[18]袁传勋.土遗址保护材料综述[J].敦煌研究,2002,(6):103-105.
[19]王旭东.中国西北干旱环境下石窟及土建筑遗址保护加固研究[D].兰州:兰州大学,2003.
[2]潘别桐,黄克忠.文物保护与环境地质[M].武汉:中国地质大学出版社,1992.
[3]田琳.交河故城遗址水文地质调查报告[C].解耀华编.交河故城保护与研究·乌鲁木齐:新疆人民出版社,1999:111-130.
[4]解耀华.交河故城的历史及保护修缮工程[C].解耀华编.交河故城保护与研究·乌鲁木齐:新疆人民出版社,1999:34-61.
[5]田琳.交河故城生土建筑遗存保护加固实验报告[C].交河故城保护与研究·乌鲁木齐:新疆人民出版社,1999:146-154.
[6]慕福智.吐鲁番地区大降水的天气动力学特征[J].新疆气象,1995,18(2):4-8.
[7]高国英,聂晓红.吐鲁番地区地震活动与应力场特征分析[J].地震地磁观测与研究,2000,21(6):39-44.
[8]邓起东,冯先岳,张培震.天山活动构造[M].北京:地震出版社,2000.
[9]李锁在,廖立兵.矿物热膨胀的晶体化学研究综述[J].高校地质学报,2002,6(2):333-339.
[10]刘均荣,等.岩石热增渗机理初探[J].石油钻采工艺,2003,25(5):43-46.
[11]王永华,刘文荣.矿物学[M].北京:地质出版社,1985.
[12]史謌,等.结晶岩的水化膨胀研究[J].地球物理学报,2000,43(6):798-804.
[13]费雪良,李斌.硫酸盐渍土压实特性及盐胀机理研究[J].中国公路学报,1995,8(1):44-49.
[14]赵晓光,石辉.水蚀作用下土壤抗蚀能力的表征[J].干旱区地理,2003,26(1):12-15.
[15]郭耀文.雨滴侵蚀特征分析[J].中国水土保持,1997,4:15-18.
[16]柳洪亮.交河故城城市布局调查[C].解耀华编.交河故城保护与研究·乌鲁木齐:新疆人民出版社,1999:235-240.
[17]李最雄.丝绸之路古遗址保护[M].北京:科学出版社,2003.
[18]袁传勋.土遗址保护材料综述[J].敦煌研究,2002,(6):103-105.
[19]王旭东.中国西北干旱环境下石窟及土建筑遗址保护加固研究[D].兰州:兰州大学,2003.
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