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Conservation of prehistoric caves and stability of their inner climate: Lessons from Chauvet and other French caves

机译:保护史前洞穴及其内部气候的稳定性:Chauvet和其他法国洞穴的经验教训

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In the last 150 years, some prehistoric painted caves suffered irreversible degradations due to misperception of conservation issues and subsequent mismanagement. These sites presented naturally an exceptional stability of their internal climate allowing conservation in situ of outstanding fragile remains, some for nearly 40,000 years. This is for a large part due to exchanges of air, CO_2, heat and water with the karstic system in which these caves are included. We introduce the concept of underground confinement, based on the stability of the inner cave climate parameters, especially its temperature. Confined caves present the best conservative properties. It is emphasized that this confined state implies slow exchanges with the surrounding karst and that a stable cave cannot be viewed as a closed system. This is illustrated on four case studies of French caves of various confinement states evidenced by long term continuous monitoring and on strategies to improve their conservation properties. The Chauvet cave presents optimal conservation properties. It is wholly confined as shown by the stability of its internal parameters since its discovery in 1994. In Marsoulas cave, archeological works removed the entrance scree and let a strong opening situation of the decorated zone. Remediation is expected by adding a buffer structure at the entrance. In Pech Merle tourist cave, recurrent painting fading was related to natural seasonal drying of walls. Improvement of the cave closure system restored a confined state insuring optimal visibility of the paintings. In Gargas tourist cave, optimization of closures, lighting system and number of visitors, allowed it to gradually reach a semi-confined state that improved the conservation properties. Conclusions are drawn on the characterization of confinement state of caves and on the ways to improve their conservation properties by restoring their initial regulation mechanisms and to avoid threats to their stability.
机译:在过去的150年中,由于对保护问题的误解以及随后的管理不善,一些史前彩绘洞穴遭受了不可逆转的退化。这些遗址自然呈现出内部气候异常稳定的特性,可以就地保存重要的易碎遗骸,其中一些保存了近40,000年。这很大程度上是由于与包含这些洞穴的岩溶系统进行了空气,CO_2,热量和水的交换。我们基于内部洞穴气候参数(尤其是温度)的稳定性,介绍了地下限制的概念。密闭的洞穴表现出最好的保守性。要强调的是,这种封闭状态意味着与周围岩溶的缓慢交换,并且一个稳定的洞穴不能被视为一个封闭的系统。长期连续监测证明了法国对不同限制状态的洞穴的四个案例研究和改善其保护特性的策略,就可以说明这一点。 Chauvet洞穴具有最佳的保护性质。自从1994年被发现以来,内部参数的稳定性就完全表明了它的局限性。在Marsoulas洞穴中,考古工作去除了入口卵石,使装饰区呈现出强烈的开放状态。有望通过在入口处添加缓冲区结构来进行补救。在Pech Merle旅游洞穴中,经常性的绘画褪色与墙壁的自然季节性干燥有关。洞穴封闭系统的改进恢复了封闭状态,从而确保了绘画的最佳可见性。在加尔加斯旅游山洞中,封闭设施,照明系统和游客数量的优化,使其逐渐达到半封闭状态,从而改善了保护性能。结论是对洞穴的封闭状态的表征,以及通过恢复其初始调控机制并避免对其稳定性的威胁来改善其保护性质的方法。

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