نویسندگان
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دانشیار، بخش تحقیقات حفاظت خاک و آبخیزداری، مرکز تحقیقات و آموزش کشاورزی و منابع طبیعی استان فارس، سازمان تحقیقات، آموزش و ترویج
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استادیار بخش تحقیقات بیابان، مؤسسه تحقیقات جنگلها و مراتع کشور، سازمان تحقیقات آموزش و ترویج کشاورزی، تهران، ایران.
3
استادیار بخش تحقیقات حفاظت خاک و آبخیزداری، مرکز تحقیقات و آموزش کشاورزی و منابع طبیعی استان کردستان، سازمان تحقیقات، آموزش و
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نویسندهی مسئول و کارشناس آبخیزداری اداره منابع طبیعی و آبخیزداری شهرستان بهاباد، یزد، ایران.
چکیده
بهمنظور پایش دقیق وضعیت منابع آب زیرزمینی و مدیریت بهینه آن ضروری است که نوسانات تراز سطح آب زیرزمینی و به دنبال آن، تأثیرپذیری کیفیت آب مورد ارزیابی قرار گیرد. پژوهش حاضر با هدف بررسی نوسانات سطح تراز آب زیرزمینی بر کیفیت آن در حوزه آبخیز زرند واقع در استان کرمان انجامشده است. به همین منظور، ویژگی 14 پارامتر کیفی آب زیرزمینی از جمله غلظت کاتیونهای سدیم، پتاسیم، کلسیم و منیزیم، غلظت آنیونهای کلر، سولفات، کربنات و بیکربنات، نسبت جذب سدیم، درصد سدیم، سختی کل، کل مواد جامد محلول، اسیدیته و هدایت الکتریکی، طی بازهی زمانی 82-1381 تا 98-1397 مورد ارزیابی قرار گرفت. با توجه به اینکه کیفیت آب زیرزمینی تحت تأثیر کمیت آن قرار میگیرد؛ تغییرات پارامترهای کیفی آب با توجه به سطح تراز سفرهی زیرزمینی بررسی شد. مطابق نتایج، رابطهی خطی معنیداری میان EC و TDS با میزان R2 بالای 0/9 وجود دارد. پایش تغییرات شوری در طول زمان نشان داد که در بازهی زمانی موردمطالعه، روند تغییرات شوری در این حوزه آبخیز، افزایشی بوده است. نمودار کموگراف بهمنظور بررسی رابطهی میان پارامترهای کیفی و سطح تراز آب زیرزمینی نشان داد که آبخوان با 19/32 متر افت مواجه شده است که افزایش شوری 229/37 میکرو زیمنس بر سانتیمتر را در پی داشته است. همچنان که بررسی تغییرات شوری و سطح تراز آب به تفکیک سال، نشاندهندهی رابطهی منفی (0/007) میان دو پارامتر است و از لحاظ آماری قابلقبول نمیباشد. یافتههای پژوهش حاضر میتواند اطلاعات مهمی را برای بهبود راهبردها مدیریت آب، برای اطمینان از مدیریت پایدار آب و استفاده ایمن ارائه دهد.
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