Abstract

A comprehensive in vitro study on single and sequential extraction methods for Cu exraction by different extractants of distinct chemical nature from some peat soils of Bangladesh was conducted to assess the pattern of metal-extractability in drying and wetting sequences. Samples were collected from peat basins of two different districts of Bangladesh (Gopalgonj and Bagerhat) and an incubation study was designed and conducted in which soils were incubated to three alternate drying and wetting cycles for 21 days. Single and sequentially extracted Cu ions in all three cycles and by all three selective extractants were compared. Maximum amount of Cu was extracted in drying days and 1M HCl extracted the largest proportion of Cu from all the soils in each incubation time. Conversely, 1M NH4Cl was the least effective extractant for extracting Cu by both single and sequential process in either day of incubation. Considerable amount of Cu was extracted by 0.005 M DTPA in dry periods. In general, single extraction was found to be more effective in extracting Cu in the alternate drying and wetting cycles from the peat soil samples except for 1M HCl in initial drying days.

Highlights

  • Peat soils generally consist of partially decomposed organic matter, derived mostly from plant material, which has accumulated under conditions of water logging and oxygen deficiency

  • A comprehensive in vitro study on single and sequential extraction methods for Cu exraction by different extractants of distinct chemical nature from some peat soils of Bangladesh was conducted to assess the pattern of metal-extractability in drying and wetting sequences

  • Maximum amount of Cu was extracted in drying days and 1M HCl extracted the largest proportion of Cu from all the soils in each incubation time

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Summary

Introduction

Peat soils generally consist of partially decomposed organic matter, derived mostly from plant material, which has accumulated under conditions of water logging and oxygen deficiency. These are organic soils containing a minimum of 20% organic matter with as much as 60% of the mineral matter is clay. Peat and mineral layers may occur at the top of the profile. They usually possess highly acidic environment with lower available nutrients, reserved organic matter acts as total nutrient pool

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