Distribution of phosphorus and the effect of physicochemical properties and clay minerals on phosphorus release in some calcareous soils

Document Type : Full Article

Authors

1 Department of Agriculture, Payame Noor University, Tehran, I. R. Iran

2 Department of Soil and Water Research, Khuzestan Agricultural and Natural Resources Research and Education Center, AREEO, Ahvaz, I. R. Iran

3 Department of Environments, Institute of Science and High Technology and Environmental Sciences, Graduate University of Advanced Technology, Kerman, I. R. Iran

Abstract

Phosphorus (P) is a nutrient essential for plant, which its availability in soils changes with aging process, leaching, precipitation processes, and the landform change. There is limited information available on kinetics release of P in calcareous soils. Therefore, the purpose of this study was to investigate distribution of P and the effect of physicochemical properties and clay minerals on its release in some dominant orders of the calcareous soils in Kohgiluyeh-and-Boyer-Ahmad province, using the 0.01 M calcium chloride ( ) extractant. The results showed that the P released rapidly from the soil and continued slowly. After 72 h, the amount of P released in the studied soils ranged between 3.2 and 25.4 mg kg-1. Evaluation of the fitted different equations on P released in the studied soils revealed that the Simple Elovich and power function equations could well predict the P release process in the studied soils. The results of the correlation between soil properties and released P contents showed that P release coefficients (including the slope and intercept in the Simple Elovich equation) have a significant negative relationship with the amount of smectite and vermiculite minerals. Also, the release coefficient of the parabolic diffusion equation had a significant negative relationship with pH and the amount of illite and palygorskite minerals.

Keywords

Article Title [Persian]

توزیع فسفر و اثر ویژگی‌های فیزیکوشیمیایی و کانی‌های رسی بر آزادسازی فسفر در تعدادی از خاک‌های آهکی

Authors [Persian]

  • سیروس شاکری 1
  • ابوالفضل آزادی 2
  • محبوب صفاری 3
1 گروه کشاورزی، دانشگاه پیام نور، تهران، ج. ا. ایران
2 بخش تحقیقات خاک و آب، مرکز تحقیقات و آموزش کشاورزی و منابع طبیعی استان خوزستان، سازمان تحقیقات، آموزش و ترویج کشاورزی، اهواز، ایران،
3 گروه پژوهشی محیط زیست، پژوهشگاه علوم و تکنولوژی پیشرفته و علوم محیطی، دانشگاه تحصیلات تکمیلی صنعتی و فناوری پیشرفته، کرمان، ایران
Abstract [Persian]

فسفر به عنوان یک عنصر غذایی ضروری برای رشد گیاهان می باشد که دسترسی آن در خاک با گذشت زمان، آبشویی، ترسیب و تغییر زمین­نما تغییر می­کند. اطلاعات در مورد سینتیک آزاد سازی فسفر در خاک­های آهکی محدود است. بنابراین هدف از این تحقیق، بررسی توزیع فسفر و تاثیر ویژگی­های فیزیکوشیمیایی و کانی­های رسی بر آزادسازی فسفر در تعدادی از رده­های غالب خـاک­هـای آهکی اسـتان کهگیلویه و بویر­احمد، با عصاره­گیر کلرید کلسیم 01/0 مولار بود. نتایج این پژوهش نشان داد، رها سازی فسفر از خاک در ابتدا سریع  و سپس به آهستگی ادامه یافت. بعد از گذشت 72 ساعت، مقدار فسفر آزاد شده در خاک­ها در محدوده 2/3 تا 4/25 میلی­گرم در کیلوگرم بود. بر اساس برازش معادلات مختلف بر داده های واجذبی فسفر، معادلات الوویچ و تابع توانی توانستند به خوبی فرایند رهاسازی فسفر را در خاک­های مورد مطالعه پیش­بینی کنند. نتایج مطالعات همبستگی خصوصیات خاک و اجزای رهاسازی فسفر در خاک‌ها نشان داد که برخی ضرایب آزاد شدن فسفر (از جمله شیب و عرض از مبدا معادله الوویچ) ارتباط منفی معنی­داری با مقدار کانی اسمکتیت و ورمی­کولیت دارند. همچنین، ضریب آزاد سازی معادله پخشیدگی پارابولیک رابطه معنی دار منفی با pH ، میزان ایلیت و کانی پالیگورسکیت نشان داد.

Keywords [Persian]

  • آزادسازی فسفر
  • کانی‌های رسی
  • خاک‌های آهکی

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Iran Agricultural Research
Volume 39, Issue 2
December 2020
Pages 79-90

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