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首页> 外文期刊>Engineering Geology >Use of fuzzy relations to produce landslide susceptibility map of a landslide prone area (West Black Sea Region, Turkey)
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Use of fuzzy relations to produce landslide susceptibility map of a landslide prone area (West Black Sea Region, Turkey)

机译:使用模糊关系生成易发生滑坡地区(土耳其西黑海地区)的滑坡敏感性图

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Preparation of landslide susceptibility maps is important for engineering geologists and geomorphologists. However, due to complex nature of landslides, producing a reliable susceptibility map is not easy. For this reason, many procedures have been used to produce such maps. In this study, a new attempt is tried to produce landslide susceptibility map of a part of West Black Sea Region of Turkey. To obtain the fuzzy relations for producing the susceptibility map, a landslide inventory database is compiled by both field surveys and airphoto studies. A total of 266 landslides are identified in the study area, and dominant mode of failure is rotational slide while the other mode of failures are soil flow and shallow translational slide. The landslide inventory and the parameter maps are analyzed together using a computer program (FULLSA) developed in this study. The computer program utilizes the fuzzy relations and produces the landslide susceptibility map automatically. According to this map, 9.6 percent of the study area is classified as very high susceptibility, 10.3 percent as high susceptibility, 8.9 percent as moderate susceptibility, 27.5 percent as low susceptibility and 43.8 percent as very low susceptibility or nonsusceptible areas. The prediction performance of the susceptibility map is checked by considering actual landslides in the study area. For this purpose, strength of the relation (r_(ij)) and the root mean square error (RMSE) values are calculated as 0.867 and 0.284, respectively. These values show that the produced landslide susceptibility map in the present study has a sufficient reliability. It is believed that the approach employed in this study mainly prevents the subjectivity sourced from the parameter selection and provides a support to improve the landslide susceptibility mapping studies.
机译:滑坡敏感性图的准备对于工程地质学家和地貌学家很重要。但是,由于滑坡的性质复杂,要生成可靠的磁化率图并不容易。由于这个原因,已经使用了许多过程来产生这样的地图。在这项研究中,尝试进行新的尝试以绘制土耳其西黑海地区一部分的滑坡敏感性图。为了获得产生磁化率图的模糊关系,通过实地调查和航拍研究汇编了滑坡清单数据库。在研究区域内总共发现了266个滑坡,主要的破坏模式是旋转滑动,而其他的破坏模式是土壤流和浅平移滑动。使用本研究开发的计算机程序(FULLSA)一起分析滑坡清单和参数图。该计算机程序利用模糊关系并自动生成滑坡敏感性图。根据这张图,研究区域的9.6%被归类为极高的磁化率,10.3%的高磁化率,8.9%的中等磁化率,27.5%的低磁化率和43.8%的极低磁化率或非磁化率区域。通过考虑研究区域中的实际滑坡来检查敏感性图的预测性能。为此,关系强度(r_(ij))和均方根误差(RMSE)值分别计算为0.867和0.284。这些值表明,本研究产生的滑坡敏感性图具有足够的可靠性。可以相信,本研究中使用的方法主要是防止来自参数选择的主观性,并为改善滑坡敏感性地图研究提供了支持。

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