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Investigation of Archaeological European White Elm (Ulmus laevis) for Identifying and Characterizing the Kind of Biological Degradation

机译:考古欧洲白榆树(Ulmus Laevis)的调查识别和表征生物降解种类

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The current work aims at the study of the biological degradation of archaeological European white elm via microscopy and chemical analysis in order to identify the kind of biological degradation and characterize the state of preservation of this type of wood. Profound knowledge of the chemical constituents and biological degradation in fresh-cut and archaeological elm wood will simplify the process of restoration and conservation of the investigated artifacts. Therefore, fresh-cut and archaeological elm were compared in terms of extractive, chlorite holocellulose, -cellulose, lignin, and ash contents. In the fresh-cut elm wood, the contents of KrschnerHoffer cellulose, chlorite holocellulose, -cellulose, and hemicellulose were significantly higher than that of the archaeological elm, confirmed by the degradation of native wood hemicelluloses by erosion bacteria during soil contact. Naturally, the mass percentage of lignin increases as the amount of chlorite holocellulose in the wood decreases. These wet chemistry results were also confirmed by FTIR analysis, where bands mainly attributed to hemicellulose and cellulose decreased significantly and bands belonging to lignin display higher intensity for the archaeological specimens. Ash and cyclohexaneethanol extract contents of archaeological elm wood were significantly higher due to the movement of mineral components arising out of the soil into the wood specimens. Based on the microscopic investigation and given the fact that wood decay fungi need oxygen to degrade wood and the investigated archaeological elm specimens were buried to a 10 m depth in the soil, we might conclude that the wood degradation was caused by erosion bacteria.
机译:目前的工作旨在通过显微镜和化学分析研究考古欧洲白榆树的生物降解,以识别生物降解的那种,并表征这种类型的木材的保存状态。鲜切和考古榆木木材中化学成分和生物降解的深刻知识将简化调查伪影的恢复和保护过程。因此,根据萃取,亚氯酸酯全纤维素, - 纤维素,木质素和灰分,比较鲜切和考古榆树。在鲜切割的Elm木材中,Krschnerhoffer纤维素,亚氯酸酯全纤维素, - 晶粒和半纤维素的含量显着高于考古榆树,通过土壤接触期间侵蚀细菌的天然木质半纤维素的降解证实。当然,木质素的质量百分比随着木材中的亚氯酸盐含量的量减少而增加。通过FTIR分析还证实了这些湿化学结果,其中主要归因于半纤维素和纤维素的带显着下降,并且属于木质素的带对考古标本的强度显示出更高的强度。由于土壤产生的矿物质组分进入木材标本,灰和环己烷醇提取物的灰分和环己烷醇的含量显着提高。基于显微镜调查并鉴于木腐烂真菌需要氧气降解木材,调查的考古榆树标本被埋入土壤中的10米深处,我们可能会得出结论,木质降解是由侵蚀细菌引起的。

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