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پهنهبندی خطر وقوع زمینلغزش در حوضهآبریز رودخانه زرد با استفاده از منطق فازی | ||
هیدروژئومورفولوژی | ||
دوره 9، شماره 30، خرداد 1401، صفحه 48-25 اصل مقاله (2.5 M) | ||
نوع مقاله: پژوهشی | ||
شناسه دیجیتال (DOI): 10.22034/hyd.2021.43189.1560 | ||
نویسندگان | ||
سیده معصومه موسوی* 1؛ محمد حسین رضایی مقدم2؛ معصومه رجبی3 | ||
1دانشجوی دکترا دانشگاه تبریز | ||
2استاد تمام گروه ژئومورفولوژی دانشگاه تبریز | ||
3استاد تمام گروه ژئومورفولوژی تبریز | ||
چکیده | ||
زمینلغزش هر ساله جان هزاران نفر را در سراسر جهان میگیرد و خسارتهای هنگفتی را به مردم و دولتها تحمیل میکند. پهنهبندی خطر زمینلغزش، نواحی سطح زمین را به مناطق ویژه و تفکیک شدهای از درجات بالقوه و بالفعل به لحاظ خطرپذیری تقسیمبندی میکند. این امر میتواند مبنایی برای برنامهریزیهای بلندمدت در سطح منطقهای و محلی محسوب شود. هدف از انجام این پژوهش، بررسی و پهنهبندی خطر زمینلغزش در حوضه رود زرد واقع در شرق استان خوزستان با استفاده از روش منطق فازی است. بدین منظور ابتدا از طریق بازدیدهای میدانی، نقشههای زمینشناسی و توپوگرافی و با مرور منابع قبلی و بررسی شرایط منطقه، نه عامل طبقات ارتفاعی، شیب، جهت شیب، فاصله از گسل، فاصله از رودخانه، فاصله از جاده، بارش، لیتولوژی و کاربری اراضی به عنوان عوامل مؤثر، بررسی و انتخاب شدند. پس از طبقهبندی دادهها و مرحله فازیسازی، نقشههای پهنهبندی خطر زمینلغزش با استفاده از عملگر گامای فازی با مقادیر 7/0، 8/0، 9/0 تهیه شدند. نقشههای به دست آمده در 5 کلاس بسیار زیاد، زیاد، متوسط، کم و بسیار کم طبقهبندی شدند. نتایج حاصل از جمع کیفی نشان داد که عملگر گامای 9/0 فازی در مقایسه با دیگر عملگرهای فازی مناسبتر است. تحلیل نقشههای طبقهبندی شده نشان داد که 56/21 درصد از مساحت منطقه در پهنه با خطر زیاد و 24/43 درصد از مساحت منطقه در پهنه با خطر کم قرار گرفته است. در مجموع، میتوان گفت که بخشی از مناطق مرکزی و شمال غربی منطقه در معرض خطر بالا قرار گرفته و مناطق غربی و شرقی حوضه در پهنه خطر متوسط تا پایین میباشند. | ||
کلیدواژهها | ||
مخاطرات ژئومورفولوژیکی؛ منطق فازی؛ سیستم اطلاعات جغرافیایی؛ حوضه رود زرد؛ شرق استان خوزستان | ||
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مراجع | ||
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