乌尔米亚湖西部地区农村聚落的可持续性分析

A. Nasiri
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摘要

今天,人类与自然环境相互作用的程度和复杂性、年轻的土地、聚落的环境不稳定性比以前更频繁和更严重。根据该地区的形态构造变量,农村聚落的环境可持续性是什么?哪些因素影响了该地区农村住区的可持续性?本研究领域未见相关报道。采用模糊多元空间分析、数据ISO和W、SL、Hi、Ar、SMF等地貌指数及Iat指数评价稳定性。对该地区的地形资料、地震、断裂系统、地质、地貌、形态构造进行了分析,确定了该地区的形态构造带。研究结果表明,研究区内存在由与南北向平行的断裂体系形成的东西向的地堑和地堑体系。研究区确定了A、B、C、D 4种不同的形态构造模式,它们具有不同的特征和形态稳定性系数。根据Iat指数分析结果,该区57%的聚落位于A区,A区形态构造稳定。C区沉降占23.5%,高度不稳定,B区沉降占16%,D区沉降占4.9%,不同系数分别表现为较严重和较严重的形态构造不稳定。结果表明,乌尔米亚湖西部地区环境不稳定的主要原因是该地区的活动断裂系统。
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Sustainability Analysis of Rural Settlements in the Western Region of Lake Urmia
Today, the extent and complexity of human-natural environment interactions, young lands, environmental instabilities of settlements with more frequency and intensity than before and are serious. What is the environmental sustainability of rural settlements according to the morphotectonic variables of the region? What factors affect sustainability of rural settlements the region? No report has been submitted in this research area. Fuzzy multivariate spatial analysis and Data ISO and geomorphic indices such as W, SL, Hi, Ar and SMF and Iat index were used to assess stability. Topographic data, earthquakes, fault systems, geology, geomorphology, morphostructure were analyzed and morphotectonic zones of the region were determined. The results of this study show that in the study area there is a Horst and Graben system with east-west trend which is formed by a system of faults parallel to the north-south trend. 4 different morphotectonic patterns (A, B, C, D) were identified with different characteristics and coefficients of morphotechnical stability in the research area. According to the results of the analysis of the Iat index, 57% of the settlements in the region are located in zone A, which is morphotectonically stable. 23.5% of the settlements are located in zone C with high instability and the settlements of zone B 16% and in zone D 4.9% with different coefficients show more severe and severe morphotectonic instability, respectively. The results show that the main cause of environmental instability in the western region of Lake Urmia is due to the active fault system of the region.
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