Speciation and sorption of phosphorus in agricultural soil profiles of redoximorphic character

被引:0
|
作者
Karen Baumann
Sabry M. Shaheen
Yongfeng Hu
Peter Gros
Elena Heilmann
Mohsen Morshedizad
Jianxu Wang
Shan-Li Wang
Jörg Rinklebe
Peter Leinweber
机构
[1] University of Rostock,Soil Sciences, Faculty for Agriculture and Environmental Sciences
[2] University of Wuppertal,Laboratory of Soil
[3] University of Kafrelsheikh, and Groundwater
[4] University of Saskatchewan,Management, School of Architecture and Civil Engineering, Institute of Foundation Engineering, Water
[5] Chinese Academy of Sciences, and Waste
[6] National Taiwan University,Management
[7] University of Sejong,Department of Soil and Water Sciences, Faculty of Agriculture
来源
Environmental Geochemistry and Health | 2020年 / 42卷
关键词
Controlled drainage; Adsorption isotherm; P mobilization; Redox; Synchrotron; XANES;
D O I
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中图分类号
学科分类号
摘要
Controlled drainage is considered as a soil management tool to improve water supply to crops and reduce nutrient losses from fields; however, its closure may affect phosphorus (P) mobilization in soil. To assess the P mobilization potential, three soil profiles with redoximorphic features were selected along a slight hill in Northern Germany. Soil samples from three depths of each profile were characterized for basic properties, total element content, oxalate- and dithionite-extractable pedogenic Al, Fe and Mn (hydr)oxides, P pools (sequential extraction), P species [P K-edge X-ray absorption near-edge structure (XANES) spectroscopy] and P sorption behavior. In topsoil (~ 10 cm depth), labile P (H2O-P + resin-P + NaHCO3-P) accounted for 26–32% of total P (Pt). Phosphorus K-edge XANES revealed that up to 49% of Pt was bound to Al and/or Fe (hydr)oxides, but sequential fractionation indicated that > 30% of this P was occluded within sesquioxide aggregates. A low binding capacity for P was demonstrated by P sorption capacity and low Kf coefficients (20–33 mg1-nfLnfkg-1\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$${\text{mg}}^{{1 - n_{\text{f}} }} \,{\text{L}}^{{n_{\text{f}} }} \,{\text{kg}}^{ - 1}$$\end{document}) of the Freundlich equation. In the subsoil layers (~ 30 and ~ 65 cm depth), higher proportions of Al- and Fe-bound P along with other characteristics suggested that all profiles might be prone to P mobilization/leaching risk under reducing conditions even if the degree of P saturation (DPS) of a profile under oxic conditions was < 25%. The results suggest that a closure of the controlled drainage may pose a risk of increased P mobilization, but this needs to be compared with the risk of uncontrolled drainage and P losses to avoid P leaching into the aquatic ecosystem.
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页码:3231 / 3246
页数:15
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