ارزیابی آبشویی خاکهای شور و سدیمی با کاربرد سطوح مختلف آب خالص و اسیدی در بخشی از اراضی شبکه آبیاری و زهکشی دشت مهاباد

نوع مقاله : مقاله پژوهشی

نویسندگان

1 دانشجوی دکترای آبیاری و زهکشی

2 دانشیار گروه مهندسی آب دانشگاه ارومیه

چکیده

بهسازی خاک‎های شور و سدیمی از دیدگاه حفاظت منابع آب و خاک، اهمیت فراوانی دارد. تجمع و فزونی املاح خاک از رشد و نمو گیاه جلوگیری نموده و به‎طور مستقیم بر عملکرد گیاه تأثیر می‎نهد. مهم‎ترین گام جهت جلوگیری از اثرات سوء شوری خاک، کاهش املاح تا حد بهینه از طریق آبشویی و ممانعت از ماندابی شدن می‎باشد. بهسازی خاک‎های شور-سدیمی به کیفیت و مقدار آب کاربردی، نوع بهساز و وضعیت زهکشی خاک بستگی دارد. در این پژوهش، به‎منظور ارزیابی چگونگی اصلاح خاک‎های شور و سدیمی، تیمارهای مختلف آبشویی با آب خالص و آب اسیدی در سه سطح 25، 50 و 75 سانتی‎متری در قالب طرح آزمایش بلوک‎های کامل تصادفی در سه تکرار انجام شد. پس از آنکه رطوبت خاک به حد ظرفیت مزرعه‎ای رسید، نمونه خاک جهت تجزیه و تحلیل مقدار تغییرات املاح تهیه گردید. نتایج نشان داد تغییر کلاس شوری و قلیائیت خاک از S3A2 (شوری زیاد و قلیائیت نسبتا زیاد) به S1A1 (شوری و قلیائیت کم) پس از انجام آبشویی می‎باشد. کمترین و بیشترین درصد بهبود شوری و قلیائیت مربوط به تیمارهای 25 سانتی‎متر آب خالص و 75 سانتی‎متر آب اسیدی به‎ترتیب با مقادیر کاهش متوسط 7/24 و 2/41درصد برای سدیم قابل تبادل و 9/25 و 69 درصد برای قابلیت هدایت الکتریکی نسبت به شرایط اولیه خاک می‎باشد. در تمامی تیمارها اختلاف بین استفاده از آب خالص و اسیدی معنی‎دار شد که نشان از عملکرد موثر ماده اصلاحی دارد. تجزیه آماری نتایج، بیانگر معنی‎دار بودن تغییرات پارامتر درصد سدیم قابل تبادل و قابلیت هدایت الکتریکی به‎ترتیب در سطح احتمال پنج و یک درصد بود. تیمار 50 سانتی‎متر آب اسیدی از بین تیمارها به‎عنوان مناسب‎ترین تیمار از لحاظ مصرف آب و کارآیی آبشویی شناخته شد. پیشنهاد می‎شود برای استفاده بهینه آب، از تیمار 50 سانتی‎متر آب اسیدی برای اصلاح خاک‎های منطقه استفاده شود.

کلیدواژه‌ها


عنوان مقاله [English]

Assessment of leaching of the salt-affected soils Using different levels of Pure and Acidic Water in Selected Regions of Mahabad Irrigation and Drainage Network

چکیده [English]

Improvement of saline-sodic soils is very important in terms of soil and water resources conversation. Accumulation and increasing of soil salts prevents plant growth and directly affects the crop yield. Soil salts reduction through the leaching and preventing from water logging is among the most important steps to prevent the negative effects of soil salinity. Improvement of saline-sodic soils depends on the quality and amount of applied water, type of amendment material and soil drainage condition. In this study, in order to evaluate how to improve the saline and sodic soils, randomized complete block design were conducted with different leaching treatments by using acidic and pure water in three levels of 25, 50 and 75 cm with three replications. After the soil moisture content reached to field capacity, soil samples were taken to analyze the changes of soil salts. Results indicated that, soil salinity and alkalinity class changed from S3A2 (high salinity and relatively high alkalinity) to S1A1 (low salinity and alkalinity) after leaching. The lowest and highest percentages of salinity and alkalinity improvement were related to the 25 cm of pure water and 75 cm of acidic water treatments, with average reduction of 24.7 and 41.2 percent for exchangeable sodium (ESP) and 25.9 and 69 percent for electrical conductivity (EC), respectively. In all treatments, differences between the use of the pure and acidic water were significant .This suggests that the amendment material is effective. Statistical analysis of results showed significant changes in ESP and EC parameters in 5 and 1 percent levels, respectively. Application of 50 cm acidic water was recognized as the most appropriate treatment in terms of water use and leaching efficiency. It could be recommended that, for efficient use of applied water, 50 cm acidic water to be used for remediation of soils in this region.

کلیدواژه‌ها [English]

  • Leaching
  • Exchangeable sodium
  • Salinity
  • Alkalinity
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