摩天气候过程对城市文化遗址的影响

ساجدة الجوهر, سرحان نعيم الخفاجي
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引用次数: 0

摘要

该研究分析了形态气候过程对Al -Warkaa城市地区的影响,该城市代表了伊拉克南部地区最重要的考古城市。本研究旨在分析自然地理最重要的特征及其对影响考古遗址的形态气候过程的作用,研究表明,Al-Warkaa历史区域的形态气候过程对考古遗址的影响最为有效,其表现为化学、生物和机械风化过程及其不同的作用。机械风化被认为是该地区最活跃的风化类型之一,除了风雨过程侵蚀及其对考古纪念碑的突出影响。通过野外考察和运用数学方程,测量了形态气候过程的活动性。以雨蚀和风蚀过程以及对风蚀的年气候敏感性率为代表,萨马瓦和纳西里耶气候站的侵蚀证据非常高。雨水侵蚀过程对以碰撞和板块侵蚀为代表的考古遗址以及水体和沟槽的侵蚀具有明显而显著的影响,以雨和风降水为代表的沉积形态气候过程对历史区域内许多考古遗址的掩埋具有明显而显著的影响,各种环境干扰也起了作用。气候和地质扰动在很大程度上影响了这些形态气候的不稳定性及其对研究区的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
تأثير العمليات المورفومناخية على المواقع الأثرية في منطقة الوركاء الحضارية
The research dealt with analyzing the impact of morphoclimatic processes on the urban area of Al -Warkaa city, which represents the most important archaeological cities in southern Iraq region. The study aims to analyze the most important characteristics of natural geography and its role in the activity or weakness of morphoclimatic processes affecting archaeological sites, and the studies showed that the morphoclimatic processes on the Al-Warkaa historical region are most effective on the historical sites, which represented by chemical, biological and mechanical weathering processes and their different effects, Mechanical weathering is considered one of the most active types of weathering in the region, in addition to wind and rain processes erosion and its prominent impact on archaeological monuments. Through field work and the use of mathematical equations, the activity of morphoclimatic processes was measured. Represented by the processes of rain and wind erosion and the rates of annual climatic susceptibility to wind erosion, the evidence of erosion in the Samawah and Nasiriyah climatic stations was very high. It became clear that the processes of rain erosion have a clear and significant impact on the archaeological sites represented by collision and plate erosion and the erosion of water bodies and grooves, and the sedimentary morphoclimatic processes represented by rain and wind precipitation have a clear and significant effect represented by the burial of many archaeological sites in the historical region, and various environmental disturbances contribute, such as fluctuation and change Climatic and geological disturbances to a very large extent in the instability of those morpho-climatic and its effects on the study area.
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