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تحلیل روند تغییرات کیفیت آب زیرزمینی با شاخص کیفی آب زیرزمینی (منطقه مورد مطالعه: آبخوان قزوین) | ||
| آبخوان و قنات | ||
| دوره 6، شماره 1 - شماره پیاپی 10، شهریور 1404، صفحه 107-130 اصل مقاله (1.34 M) | ||
| نوع مقاله: مقاله پژوهشی | ||
| شناسه دیجیتال (DOI): 10.22077/jaaq.2025.9864.1120 | ||
| نویسندگان | ||
| محمد مفیدی1؛ فرهاد هوشیاری پور* 1؛ حمید کاردان مقدم2؛ روح اله نوری3 | ||
| 1گروه علمی مدیریت ساخت و آب، واحد علوم و تحقیقات، دانشگاه آزاد اسلامی، تهران، ایران. | ||
| 2مؤسسه تحقیقات آب، وزارت نیرو، تهران، ایران. | ||
| 3دانشکده تحصیلات تکمیلی محیط زیست، دانشگاه تهران، تهران، ایران | ||
| چکیده | ||
| شاخص کیفیت آب زیرزمینی (GWQI) برای ارزیابی کیفیت آبهای زیرزمینی و مناسب بودن آن برای اهداف مختلف استفاده میشود. این شاخص توسط یکپارچه سازی دادهها و تولید یک عدد که بیانگر کلی کیفیت آب است بکار میرود. در این تحقیق تغییرات کیفیت آب زیرزمینی در آبخوان قزوین در یک دوره 15 ساله منتهی به سال 1400 با استفاده از GWQI مورد بررسی قرار گرفت. برای این منظور طیف وسیعی از پارامترهای شیمیایی آب شامل Na ,K، Mg، Ca، SO4، Cl، HCO3، pH، TDS، EC و TH استفاده شدند. نتایج نشان میدهد که حداقل مقدار GWQI از 6/18 تا 2/24 و مقدار حداکثری آن از 1/118 تا 2/205 متغیر بود. در میان پارامترهای کیفی EC و K به ترتیب بیشترین و کمترین تاثیر را در مقدار GWQI داشتند. نتایج آزمون روند من کندال نیز نشان دهنده عدم وجود یک روند معنادار در شاخص GWQI بود. همچنین آنالیز مکانی نتایج نشان داد که محدوده مینیمم GWQI در قسمت شمال و شمال غرب آبخوان و محدوده ماکزیمم آن در غرب آبخوان قرار داشتند. ذکر این نکته ضروریست که محدوده جغرافیایی مربوط به مینیمم GWQI بسیار گسترده تر از محدوده ماکزیمم آن بود که نشان دهنده کیفیت مناسب آب زیرزمینی در اکثر نواحی بود. | ||
| کلیدواژهها | ||
| آب زیرزمینی؛ آبخوان قزوین؛ کیفیت آب؛ تحلیل روند؛ GWQI | ||
| مراجع | ||
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