Mechanisms controlling the mobility of dissolved organic matter, aluminium and iron in podzol B horizons

• Published in: European journal of soil science Vol. 56; no. 4; pp. 537 - 550
• Main Authors: Jansen, B, Nierop, K.G.J, Verstraten, J.M
• Format: Journal Article
• Language: English
• Published: Oxford, UK; Malden, USA Blackwell Science Ltd 01.08.2005; Blackwell Science
• Subjects: Agronomy. Soil science and plant productions; aluminum; B horizons; Biological and medical sciences; Chemical, physicochemical, biochemical and biological properties; dissolved organic matter; Earth sciences; Earth, ocean, space; Exact sciences and technology; Fundamental and applied biological sciences. Psychology; genetic soil types; Geochemistry; immobilization in soil; iron; Netherlands; Organic matter; Physical properties; Physics, chemistry, biochemistry and biology of agricultural and forest soils; podzols; Soil and rock geochemistry; Soil genesis; Soil science; Soil surveys, classification and mapping, soil genesis; Water and solute dynamics; Netherlands; Western Europe; mobility; Soil transport processes; Group VIII metal; Immobilization; soil sciences; sandy soils; aluminum; Transport process; Regulation(control); Dissolved organic matter; Anthrosols; Soil science; dissolved materials; soils; mechanism; Soil chemistry; Acid soil; geochemistry; Europe; soil horizons; Group IIIA metal; temperate zone; pedogenesis; Podzols; podzolization; organic materials; iron
• ISSN: 1351-0754; 1365-2389
• DOI: 10.1111/j.1365-2389.2004.00686.x

Summary The processes governing the (im)mobilization of Al, Fe and dissolved organic matter (DOM) in podzols are still subject to debate. In this study we investigated the mechanisms of (im)mobilization of Al, Fe and organic matter in the upper and lower B horizons of two podzols from the Netherlands that are in different stages of development. We equilibrated batches of soil material from each horizon with DOM solutions obtained from the Oh horizon of the corresponding soil profiles. We determined the amount of (im)mobilized Al, Fe and DOM after addition of Al and Fe at pH 4.0 and 4.5 and initial dissolved organic carbon (DOC) concentrations of 10 mg C litre−1 or 30 mg C litre−1, respectively. At the combination of pH and DOC concentrations most realistic for the field situation, organic matter was retained in all horizons, the most being retained in the lower B horizon of the well‐developed soil and the least in the upper B horizon of the younger profile. Organic matter solubility seemed to be controlled mainly by precipitation as organo‐metal complexes and/or by adsorption on freshly precipitated solid Al‐ and Fe‐phases. In the lower B horizons, at pH 4.5, solubility of Al and Fe appeared to be controlled mainly by the equilibrium with secondary solid Al‐ and Fe‐phases. In the upper B horizons, the solubility of Al was controlled by adsorption processes, while Fe still precipitated as inorganic complexes as well as organic complexes in spite of the prevailing more acidic pH. Combined with a previous study of eluvial horizons from the same profiles, the results confirm the important role of organic matter in the transport of Al and Fe to create illuvial B horizons initially and subsequently deepening and differentiating them into Bh and Bs horizons.