سال 14، شماره 3 - ( پاییز 1403 )
جلد 14 شماره 3 صفحات 82-66 |
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Ghalesardi Gonjanak A, Elmizadeh H, Abbasi A, soleymani A. Evaluation of TWI index and TOPMODEL hydrological model in erosion and runoff (case study: Maroon basin in southwest Iran). E.E.R. 2024; 14 (3) :66-82
URL: http://magazine.hormozgan.ac.ir/article-1-800-fa.html
URL: http://magazine.hormozgan.ac.ir/article-1-800-fa.html
قلعه‌سردی‌گنجانک عارف، علمیزاده هیوا، عباسی علیرضا، سلیمانی آرزو. ارزیابی ﺷﺎﺧﺺ TWI و مدل هیدرولوژیکی TOPMODEL در فرسایش و رواناب (مطالعه موردی: حوضه آبریز مارون در جنوب غرب ایران). پژوهش هاي فرسايش محيطي. 1403; 14 (3) :66-82
گروه زمین شناسی دریایی، دانشکده منابع طبیعی، دانشگاه علوم و فنون دریایی خرمشهر، خرمشهر ، Elmizadeh@kmsu.ac.ir
چکیده: (495 مشاهده)
توپوگرافی یکی از مهم‌ترین عوامل کنترل‌کننده‌ی الگوی مکانی مناطق اشباع و تغییرات در خاک‌ها، فرآیندهای ژئومورفیکی و هیدرولوژیکی و فرم آبراهه‌ها میباشد. هدف این پژوهش ارزیابی ﺷﺎﺧﺺ TWI و مدل هیدرولوژیکی TOPMODEL در فرسایش و رواناب و جهات دامنه شبکه آبراهههای حوضه مارون در جنوب غربی ایران میباشد. در این پژوهش شاخصهای توپوگرافیک و نیمرخ دامنهها (مقعر، محدب و همگرا یا واگرا) بر پایه DEM و شبکه آبراهههای حوضه مطالعاتی، با استفاده از توابع موجود در نرمافزار SAGA محاسبه و مورد تجزیه‌وتحلیل قرار گرفتند. نتایج تحقیق نشان داد که دامنههای واگرا کمترین میزان شاخص رطوبت توپوگرافی را دارند. در این دامنهها آﺑﻬﺎی ﺳﻄﺤﻰ و زﻳﺮﺳﻄﺤﻰ ﺗﻤﺮﻛﺰ ﭘﻴﺪا ﻧﻤﻰﻛﻨﻨﺪ، ﺑﻠﻜﻪ ﭘﺨﺶ ﻣﻰﺷﻮﻧﺪ و آب داﻣﻨﻪ را ﺳﺮﻳﻌﺎً از ﺧﻮد ﻋﺒﻮر ﻣﻰدﻫند. در اﻳﻦ ﺣﺎﻟﺖ ﺗﺸﻜﻴﻞ آﺑﺨﻮان ﻣﻌﻤﻮل ﻧﻴﺴﺖ. همچنین دامنههای مقعر حوضه به علت تمرکز آب در پایین‌ترین نقطه شیب، پیک سیلاب بالاتری دارند و از نظر ژئومورفیکی ناپایدارتر میباشند. با توجه به نتایج، سازگاری شاخص TWI نسبت به شرایط خاک محلی یک مزیت مشخص نسبت به روشهای موجود میباشد. بنابراین شناخت و آگاهی از این شاخصها و خصوصیات از نظر تأثیر بر تغییرپذیری خصوصیات هیدرولیکی خاک و رسوبات سطحی جهت دستیابی به توسعه پایدار و ساماندهی منطقه امری ضروری به نظر میرسد.
نوع مطالعه: مستخرج از پایان‌نامه / رساله / طرح پژوهشی |
موضوع مقاله:
روشهای نوین و دقیق در تهیّه نقشه فرسایش (سنجش از دور و سیستم‌های اطلاعات جغرافیایی)
دریافت: 1402/3/21 | انتشار: 1403/7/10
دریافت: 1402/3/21 | انتشار: 1403/7/10
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