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بررسی فرونشست دشت کبودراهنگ بر مبنای تکنیک تداخل سنجی راداری و تغییرات تراز آب های زیرزمینی | ||
دانش آب و خاک | ||
مقاله 12، دوره 33، شماره 2، تیر 1402، صفحه 183-201 اصل مقاله (984.29 K) | ||
شناسه دیجیتال (DOI): 10.22034/ws.2021.48295.2442 | ||
نویسندگان | ||
عادل قاسمی1؛ امید بهمنی* 1؛ سمیرا اخوان2؛ حمیدرضا پورقاسمی3 | ||
1گروه مهندسی آب/دانشکده کشاورزی/دانشگاه بوعلی سینا/همدان/ایران | ||
2گروه مهندسی آب/دانشکده کشاورزی/دانشگاه بوعلی سینا | ||
3دانشیار دانشکده کشاورزی و محیط زیست؛ دانشگاه شیراز | ||
چکیده | ||
فرونشست با توجه به ماهیت زمین شناسی و ارتباط آن با بهرهبرداری از آبهای زیرزمینی مورد توجه محققین حوزه های مدیریت منابع آب و زمین شناسی قرار گرفته است. در این راستا بررسی فرونشست آبخوان کبودراهنگ در استان همدان با استفاده از تکنیک تداخل سنجی راداری و بررسی تغییرات آب زیرزمینی این دشت مورد مطالعه قرار گرفت. از سویی ارتباط بین فرونشست و تغییرات آب زیرزمینی با استفاده از روابط رگرسیونی در نظر گرفته شد. نتایج حاکی از فرونشست دشت طی سالیان 1393 تا 1398 به میزان 124/7 میلیمتر و نرخ متوسط 13 میلیمتر در هر 6 ماه بود. با توجه هدایت هیدرولیکی متفاوت آبخوان در کنار ساختارهای زمین شناسی متفاوت دشت، بین بهرهبرداری از آب زیرزمینی و پدیده فرونشست تأخیر وجود داشت که با استفاده از رگرسیون تأخیری، زمان تأخیر فرونشست و بهره برداری از آب زیرزمینی به میزان متوسط 1/5 سال تعیین گردید. همچنین تأثیر بیشتر فرونشست بر اراضی کشاورزی به دلیل بهرهبرداری از آب زیرزمینی به منظور کشت مورد تأکید قرار گرفت. | ||
کلیدواژهها | ||
آب های زیرزمینی؛ تداخل سنجی راداری؛ زمان تاخیر؛ دشت کبودراهنگ؛ فرونشست | ||
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