在模拟实验中,从哥纪念碑中分离出来的真菌对砂岩恶化和损坏的微观证据
Tomohiro Inaba1, Tomoyuki Hori1, Megumi Tsuchiya2
1Environmental Management Research Institute, National Institute of Advanced Industrial Science and Technology (AIST), 16-1 Onogawa, Tsukuba, Ibaraki 305-8569, Japan.
The Science of the total environment
|July 3, 2023
概括
菌会对像哥尔瓦特这样的砂岩遗产遗址造成重大破坏. 这项研究揭示了真菌菌如何透和破坏砂岩的稳定性,导致其恶化和腔形成.
科学领域:
- * 地质微生物学
- * 材料科学 材料科学
- * 保护文化遗产 保护文化遗产
背景情况:
- * 砂石结构,包括联合国教科文组织世界遗产安哥尔,面临严重的恶化.
- * 微生物,特别是真菌,是砂岩生物退化的主要代理物.
- *了解真菌生物退化机制对于有效的遗产保护至关重要.
研究的目的:
- * 调查菌殖民和砂岩的生物退化.
- * 用先进的显微镜识别真菌破坏砂岩的机制.
- * 提出一种由真菌活动导致的砂岩生物降解模型.
主要方法:
- *共聚焦反射显微镜 (CRM) 用于可视化真菌-砂岩相互作用.
- *扫描电子显微镜-能量散射X射线光谱 (SEM-EDS) 用于元素分析.
- * 用孤立的真菌菌株 (Aspergillus sp. AW1,Paecilomyces sp. 这种虫子的种类. 通过BY8).
主要成果:
- *观察到真菌菌根 (AW1菌株) 附着在砂岩上并透.
- *砂岩表面的粗度增加,由于真菌生长,洞穴变得更深.
- * SEM-EDS显示Si丰富的矿物质 (石英,地) 从砂岩表面脱离.
结论:
- *真菌生长对砂岩表面粗化和洞穴形成有显著的贡献.
- *真菌菌根会损害砂岩基质,破坏矿物成分的稳定.
- * 提出了一个生物降解模型,其中真菌降解了砂岩,导致结构崩.
关键词:
安哥尔瓦特 (Angkor Wat) 是一个古老的城市.亚斯伯菌 sp. 的情况. 这是AW1菌株的AW1.安哥尔·姆的拜 (Bayon) 是一个安哥尔·姆的拜.这种种类型是Paecilomyces sp. 这是BY8菌株.砂岩的生物恶化更多相关视频
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