اثرات حذف کربنات‌ها و ماده آلی بر جذب فسفر در برخی خاک‌های آهکی استان کرمان

آب و خاک

مقاله 9، دوره 34، شماره 3 - شماره پیاپی 71، شهریور 1399، صفحه 637-648   

نوع مقاله: مقالات پژوهشی

شناسه دیجیتال (DOI): 10.22067/jsw.v34i1.81290

نویسندگان

هدی حسینی^* ؛ مجید فکری؛ محمد هادی فرپور؛ مجید محمودآبادی

دانشگاه شهید باهنر کرمان

چکیده

آگاهی از تاثیر اجزای مختلف خاک همانند ماده آلی و کربنات­ها بر قابلیت دسترسی فسفر در خاک جهت تغذیه گیاه و مدیریت حاصلخیزی خاک مهم است. در این مطالعه تاثیر حذف ماده آلی و کربنات­ها بر رفتار جذب فسفر در شش نمونه خاک در سه تکرار و سه تیمار ( تیمار هیپوکلریت سدیم، تیمار استات سدیم و خاک شاهد (بدون تیمار)) مورد مطالعه قرار گرفت. نتایج نشان داد که معادلات لانگمویر و فروندلیچ برازش خوبی بر داده­های جذب فسفر نشان دادند. حذف ماده آلی باعث افزایش حداکثر جذب فسفر (qmax) با دامنه 37 تا 104 میلی­گرم بر کیلوگرم نسبت به خاک­های تیمار نشده شد. برعکس، با حذف کربنات­ها از خاک­ها، حداکثر جذب فسفر (qmax) در محدوده 43 تا 345 میلی­گرم بر کیلو گرم نسبت به خاک­های تیمار نشده کاهش نشان داد. ثابت انرژی پیوند (Kl) بعد از حذف مواد آلی و کربنات­ها به ترتیب 03/17 درصد افزایش و 78/28 درصد کاهش یافت. نیاز استاندارد فسفر در خاک­های مورد مطالعه بعد از حذف مواد آلی 43/14 درصد افزایش و حذف کربنات­ها از خاک­های مورد مطالعه نیاز آن­ها را به فسفر 5/40 درصد کاهش داد. جهت مدیریت کارامد فسفر در خاک­های کشاورزی توجه به میزان کربنات­ها و کاهش آن در خاک اهمیت زیادی دارد و همچنین افزودن مواد آلی به خاک یا حداقل حفظ مواد آلی موجود در آن می­تواند سبب افزایش کارایی مصرف فسفر در خاک شود.

کلیدواژه‌ها

جذب سطحی؛ فسفر؛ مواد آلی؛ نیاز استاندارد؛ هم‌دماها

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