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ارزیابی دقت برآورد تغذیه آب زیرزمینی توسط SWAT و MODFLOW در اراضی شالیزاری (مطالعه موردی : آبخوان آستانه- کوچصفهان) | ||
| تحقیقات آب و خاک ایران | ||
| دوره 54، شماره 10، دی 1402، صفحه 1541-1564 اصل مقاله (2.44 M) | ||
| نوع مقاله: مقاله پژوهشی | ||
| شناسه دیجیتال (DOI): 10.22059/ijswr.2023.363264.669547 | ||
| نویسندگان | ||
| ایمان مهدی دوست رودبنه1؛ سمیه جنت رستمی* 2؛ افشین اشرف زاده1؛ سامان جوادی3 | ||
| 1گروه مهندسی آب، دانشکده علوم کشاورزی، دانشگاه گیلان، رشت، ایران. | ||
| 2گروه مهندسی آب، دانشکده علوم کشاورزی، دانشگاه گیلان، رشت، گیلان. | ||
| 3عضو هیات علمی گروه مهندسی آب پردیس ابوریحان دانشگاه تهران | ||
| چکیده | ||
| در این مطالعه، دقت برآورد مقادیر تغذیه آبخوان کم عمق آستانه-کوچصفهان، با استفاده از دو کد مدل‌سازی SWAT (به عنوان مدل هیدرولوژیکی آب سطحی) و MODFLOW (به عنوان مدل آب زیرزمینی) مقایسه شد. علاوه بر این، ضرورت استفاده از SWAT در مدل‌سازی-های جریان آب زیرزمینی که توسط MODFLOWانجام می‌گیرد، مورد بررسی قرار گرفت. بدین منظور شبیه‌سازی آبخوان آستانه-کوچصفهان در MODFLOW انجام شد. سپس SWAT برای حوضه‌ی آبریز آستانه-کوچصفهان تهیه و اجرا شد و توسط الگوریتم SUFI2 در نرم‌افزار SWAT-CUP مورد واسنجی قرار گرفت. در ادامه بعد از تعیین محدوده‌ی مکانی و زمانی مشترک دو مدل، اقدام به استخراج مقادیر تغذیه به آبخوان از خروجی‌های دو مدل گردید. نتایج نشان داد که کل تغذیه به آبخوان و تغذیه از رودخانه به آبخوان در سال آبی 92-1391 در MODFLOW به ترتیب برابر با 71/102 میلیون متر مکعب و 71/23 میلیون متر مکعب بدست آمد. بیشترین مقادیر تغذیه در اواخر فصل پاییز و ماه آذر 1391 رخ داده است و کمترین مقادیر تغذیه در اوایل فصل بهار و ماه فروردین 1392 اتفاق افتاده است. در SWAT نیز مقادیر تغذیه به آبخوان و تغذیه از رودخانه به آبخوان به ترتیب برابر با 34/138 میلیون متر مکعب و 09/35 میلیون متر مکعب برآورد شده است. بیشترین مقادیر تغذیه در اواخر فصل پاییز و ماه آذر 1391 رخ داده است و کمترین مقادیر تغذیه در اواخر فصل تابستان و ماه شهریور 1392 اتفاق افتاده است. SWAT با استفاده از به کارگیری پارامترهای آب سطحی و موثر بر تغذیه مانند تاثیر سد و کانال‌های انتفال آب، خصوصیات خاک و کاربری اراضی، اطلاعات اقلیمی و هواشناسی، اطلاعات مربوط به مدیریت کشاورزی و آبیاری و غیره مقادیر قابل اطمینان‌تری از پارامتر تغذیه به آب زیرزمینی را با توجه به واقعیت‌های موجود در منطقه، به‌دست می‌آورد، لذا استفاده از خروجی قابل اطمینان تغذیه از SWAT در مدل‌های آب زیرزمینی مانند MODFLOW نتایج بهتر و قابل اطمینان‌تری از وضعیت آبخوان می‌دهد. | ||
| کلیدواژه‌ها | ||
| آبخوان کم‌عمق؛ بیلان آب؛ تغذیه سطحی؛ SWAT؛ MODFLOW | ||
| عنوان مقاله [English] | ||
| Accuracy assessment of groundwater recharge estimation using SWAT and MODFLOW in paddy fields (Case study: Astane-Kouchsefahan aquifer) | ||
| نویسندگان [English] | ||
| Iman Mehdidoost Roudbaneh1؛ Somaye Janatrostami2؛ Afshin Ashrafzadeh1؛ Saman Javadi3 | ||
| 1Department of Water Engineering, Faculty of Agricultural Sciences, University of Guilan, Rasht, Iran. | ||
| 2Department of Water Engineering, College of Agriculture, University of Guilan, Rasht, Guilan. | ||
| 3Department of Water Engineering, College of Aburaihan, University of Tehran, Tehran, Iran | ||
| چکیده [English] | ||
| In this study, the accuracy of estimating shallow aquifer recharge values in Astane-Kouchsefahan using two models: SWAT (a surface water hydrological model) and MODFLOW (a groundwater flow model) was evaluated. Then the need for using SWAT in the modeling of groundwater flow, which is typically done by MODFLOW, was evaluated. For this purpose, the simulation of the Astane-Kouchsefahan aquifer was done by MODFLOW using GMS graphical user interface. Then the SWAT model was built for the Astane-Kochsefahan watershed and calibrated by the SUFI2 algorithm in SWAT-CUP software. In the following, after determining the two models' common spatial and temporal range, the aquifer recharge amounts were compared according to the outputs of the two models. MODFLOW results showed that the total aquifer recharges including recharge from the river in 1391-1392 were equal to 102.71 and 23.71 million m3, respectively. The highest and the lowest amounts of aquifer recharge occurred in December and April, respectively. The results of SWAT showed that the amounts of aquifer recharges including recharge from the river are estimated to be 138.34 and 35.09 million m3, respectively. So, the highest and the lowest recharge amount occurred in December and September, respectively. Based on the regional circumstances, SWAT offers more dependable estimates of the groundwater recharge parameters by considering surface water parameters and factors like the influence of dams and water transfer channels, soil characteristics, land use, climatic and meteorological data, and information regarding agriculture and irrigation management. Consequently, integrating the precise recharge results from SWAT into groundwater models such as MODFLOW leads to enhance and more reliable evaluations of the aquifer's state. | ||
| کلیدواژه‌ها [English] | ||
| Shallow aquifer, Water balance, surface recharge, SWAT, MODFLOW | ||
| مراجع | ||
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