Influence of specific organic compounds on phosphorus sorption and distribution in a tropical soil

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Autoren

  • Wakene Negassa
  • Stefan Dultz
  • André Schlichting
  • Peter Leinweber

Externe Organisationen

  • Universität Rostock
  • Steinbeis-Transferzentrum Soil Biotechnology
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Details

OriginalspracheEnglisch
Seiten (von - bis)587-601
Seitenumfang15
FachzeitschriftSoil Science
Jahrgang173
Ausgabenummer9
PublikationsstatusVeröffentlicht - Sept. 2008

Abstract

Effects of organic matter on phosphorus (P) sorption are not completely understood, among others, because the molecular composition of organic matter seldom has been considered. Our objective was to investigate how surface modification of a tropical soil with specific organic compounds altered the P sorption and distribution of the sorbed P. Samples of an ando-humic Nitisol, original and treated with H2O2 to remove native organic matter, were amended by 50 g C kg from lipids, lignin building blocks, glucose, albumin, tryptophan, histidine, and a mixture of these compounds. Phosphorus sorption was studied by equilibrating 1 g of the treated soil samples in 30 mL of 1 mM CaCl2 • 2H2O containing 0 to 645.71 μmol P L. The P concentrations in the soil solution after 24 h followed the order: histidine > mixture > lignin > albumin > lipid > tryptophan > glucose > control in the original sample and albumin > lignin > lipid > mixture > histidine > tryptophan > glucose > control in the H2O2-treated sample. Phosphorus sorption was lower in the H2O2-treated than in the original sample, which was explained by removal of aluminum and an increase in negative surface charges after native soil organic matter oxidation. The sorbed P distribution, studied by sequentially fractionating the samples with the highest P load, showed that 73 to 96% (original) and 100% (H2O2 treated) of sorbed inorganic P was extracted by the first three fractions (anion exchange membrane-Pi, NaHCO3-Pi, NaOH-Pi). From calculations of P requirements for sufficient P concentrations for plant growth, it was concluded that surface modification by the addition of locally available organic compounds with great molecular complexity and organic P constituents may help to reduce the need for mineral P fertilizer and increase its efficiency in tropical soils.

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Influence of specific organic compounds on phosphorus sorption and distribution in a tropical soil. / Negassa, Wakene; Dultz, Stefan; Schlichting, André et al.
in: Soil Science, Jahrgang 173, Nr. 9, 09.2008, S. 587-601.

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Negassa W, Dultz S, Schlichting A, Leinweber P. Influence of specific organic compounds on phosphorus sorption and distribution in a tropical soil. Soil Science. 2008 Sep;173(9):587-601. doi: 10.1097/SS.0b013e3181847eef
Negassa, Wakene ; Dultz, Stefan ; Schlichting, André et al. / Influence of specific organic compounds on phosphorus sorption and distribution in a tropical soil. in: Soil Science. 2008 ; Jahrgang 173, Nr. 9. S. 587-601.
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abstract = "Effects of organic matter on phosphorus (P) sorption are not completely understood, among others, because the molecular composition of organic matter seldom has been considered. Our objective was to investigate how surface modification of a tropical soil with specific organic compounds altered the P sorption and distribution of the sorbed P. Samples of an ando-humic Nitisol, original and treated with H2O2 to remove native organic matter, were amended by 50 g C kg from lipids, lignin building blocks, glucose, albumin, tryptophan, histidine, and a mixture of these compounds. Phosphorus sorption was studied by equilibrating 1 g of the treated soil samples in 30 mL of 1 mM CaCl2 • 2H2O containing 0 to 645.71 μmol P L. The P concentrations in the soil solution after 24 h followed the order: histidine > mixture > lignin > albumin > lipid > tryptophan > glucose > control in the original sample and albumin > lignin > lipid > mixture > histidine > tryptophan > glucose > control in the H2O2-treated sample. Phosphorus sorption was lower in the H2O2-treated than in the original sample, which was explained by removal of aluminum and an increase in negative surface charges after native soil organic matter oxidation. The sorbed P distribution, studied by sequentially fractionating the samples with the highest P load, showed that 73 to 96% (original) and 100% (H2O2 treated) of sorbed inorganic P was extracted by the first three fractions (anion exchange membrane-Pi, NaHCO3-Pi, NaOH-Pi). From calculations of P requirements for sufficient P concentrations for plant growth, it was concluded that surface modification by the addition of locally available organic compounds with great molecular complexity and organic P constituents may help to reduce the need for mineral P fertilizer and increase its efficiency in tropical soils.",
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AU - Negassa, Wakene

AU - Dultz, Stefan

AU - Schlichting, André

AU - Leinweber, Peter

N1 - Copyright: Copyright 2009 Elsevier B.V., All rights reserved.

PY - 2008/9

Y1 - 2008/9

N2 - Effects of organic matter on phosphorus (P) sorption are not completely understood, among others, because the molecular composition of organic matter seldom has been considered. Our objective was to investigate how surface modification of a tropical soil with specific organic compounds altered the P sorption and distribution of the sorbed P. Samples of an ando-humic Nitisol, original and treated with H2O2 to remove native organic matter, were amended by 50 g C kg from lipids, lignin building blocks, glucose, albumin, tryptophan, histidine, and a mixture of these compounds. Phosphorus sorption was studied by equilibrating 1 g of the treated soil samples in 30 mL of 1 mM CaCl2 • 2H2O containing 0 to 645.71 μmol P L. The P concentrations in the soil solution after 24 h followed the order: histidine > mixture > lignin > albumin > lipid > tryptophan > glucose > control in the original sample and albumin > lignin > lipid > mixture > histidine > tryptophan > glucose > control in the H2O2-treated sample. Phosphorus sorption was lower in the H2O2-treated than in the original sample, which was explained by removal of aluminum and an increase in negative surface charges after native soil organic matter oxidation. The sorbed P distribution, studied by sequentially fractionating the samples with the highest P load, showed that 73 to 96% (original) and 100% (H2O2 treated) of sorbed inorganic P was extracted by the first three fractions (anion exchange membrane-Pi, NaHCO3-Pi, NaOH-Pi). From calculations of P requirements for sufficient P concentrations for plant growth, it was concluded that surface modification by the addition of locally available organic compounds with great molecular complexity and organic P constituents may help to reduce the need for mineral P fertilizer and increase its efficiency in tropical soils.

AB - Effects of organic matter on phosphorus (P) sorption are not completely understood, among others, because the molecular composition of organic matter seldom has been considered. Our objective was to investigate how surface modification of a tropical soil with specific organic compounds altered the P sorption and distribution of the sorbed P. Samples of an ando-humic Nitisol, original and treated with H2O2 to remove native organic matter, were amended by 50 g C kg from lipids, lignin building blocks, glucose, albumin, tryptophan, histidine, and a mixture of these compounds. Phosphorus sorption was studied by equilibrating 1 g of the treated soil samples in 30 mL of 1 mM CaCl2 • 2H2O containing 0 to 645.71 μmol P L. The P concentrations in the soil solution after 24 h followed the order: histidine > mixture > lignin > albumin > lipid > tryptophan > glucose > control in the original sample and albumin > lignin > lipid > mixture > histidine > tryptophan > glucose > control in the H2O2-treated sample. Phosphorus sorption was lower in the H2O2-treated than in the original sample, which was explained by removal of aluminum and an increase in negative surface charges after native soil organic matter oxidation. The sorbed P distribution, studied by sequentially fractionating the samples with the highest P load, showed that 73 to 96% (original) and 100% (H2O2 treated) of sorbed inorganic P was extracted by the first three fractions (anion exchange membrane-Pi, NaHCO3-Pi, NaOH-Pi). From calculations of P requirements for sufficient P concentrations for plant growth, it was concluded that surface modification by the addition of locally available organic compounds with great molecular complexity and organic P constituents may help to reduce the need for mineral P fertilizer and increase its efficiency in tropical soils.

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KW - Organic matter

KW - Phosphate availability

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VL - 173

SP - 587

EP - 601

JO - Soil Science

JF - Soil Science

SN - 0038-075X

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