Iron Availability in Tropical Soils and Iron Uptake by Plants

ABSTRACT Given the increase in crop yields and the expansion of agriculture in low fertility soils, deficiency of micronutrients, such as iron, in plants grown in tropical soils has been observed. The aim of this study was to evaluate Fe availability and Fe uptake by corn (Zea mays L.) plants in 13 different soils, at two depths. Iron was extracted by Mehlich-1, Mehlich-3, and CaCl2 (Fe-CC) and was fractionated in forms related to low (Feo) and high (Fed) crystallinity pedogenic oxyhydroxides, and organic matter (Fep) using ammonium oxalate, dithionite-citrate, and sodium pyrophosphate, respectively. In order to relate Fe availability to soil properties and plant growth, an experiment was carried out in a semi-hydroponic system in which part of the roots developed in a nutrient solution (without Fe) and part in the soil (the only source of Fe). Forty-five days after seeding, we quantified shoot dry matter and leaf Fe concentration and content. Fed levels were high, from 5 to 132 g kg-1, and Feo and Fe-CC levels were low, indicating the predominance of Fe as crystalline oxyhydroxides and a low content of Fe readily available to plants. The extraction solutions showed significant correlations with various soil properties, many common to both, indicating that they act similarly. The correlation between the Mehlich-1 and Mehlich-3 extraction solutions was highly significant. However, these two extraction methods were inefficient in predicting Fe availability to plants. There was a positive correlation between dry matter and Fe levels in plant shoots, even within the ranges considered adequate in the soil and in the plant. Dry matter production and leaf Fe concentration and content were positively correlated with Fep concentration, indicating that the Fe fraction related to soil organic matter most contributes to Fe availability to plants.

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Main Authors: Mielki,Guilherme Furlan, Novais,Roberto Ferreira, Ker,João Carlos, Vergütz,Leonardus, Castro,Gustavo Franco de
Format: Digital revista
Language:English
Published: Sociedade Brasileira de Ciência do Solo 2016
Online Access:http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832016000100543
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spelling oai:scielo:S0100-068320160001005432016-10-19Iron Availability in Tropical Soils and Iron Uptake by PlantsMielki,Guilherme FurlanNovais,Roberto FerreiraKer,João CarlosVergütz,LeonardusCastro,Gustavo Franco de Mehlich corn (Zea mays) micronutrient nutrient solution Latossolo ABSTRACT Given the increase in crop yields and the expansion of agriculture in low fertility soils, deficiency of micronutrients, such as iron, in plants grown in tropical soils has been observed. The aim of this study was to evaluate Fe availability and Fe uptake by corn (Zea mays L.) plants in 13 different soils, at two depths. Iron was extracted by Mehlich-1, Mehlich-3, and CaCl2 (Fe-CC) and was fractionated in forms related to low (Feo) and high (Fed) crystallinity pedogenic oxyhydroxides, and organic matter (Fep) using ammonium oxalate, dithionite-citrate, and sodium pyrophosphate, respectively. In order to relate Fe availability to soil properties and plant growth, an experiment was carried out in a semi-hydroponic system in which part of the roots developed in a nutrient solution (without Fe) and part in the soil (the only source of Fe). Forty-five days after seeding, we quantified shoot dry matter and leaf Fe concentration and content. Fed levels were high, from 5 to 132 g kg-1, and Feo and Fe-CC levels were low, indicating the predominance of Fe as crystalline oxyhydroxides and a low content of Fe readily available to plants. The extraction solutions showed significant correlations with various soil properties, many common to both, indicating that they act similarly. The correlation between the Mehlich-1 and Mehlich-3 extraction solutions was highly significant. However, these two extraction methods were inefficient in predicting Fe availability to plants. There was a positive correlation between dry matter and Fe levels in plant shoots, even within the ranges considered adequate in the soil and in the plant. Dry matter production and leaf Fe concentration and content were positively correlated with Fep concentration, indicating that the Fe fraction related to soil organic matter most contributes to Fe availability to plants.info:eu-repo/semantics/openAccessSociedade Brasileira de Ciência do SoloRevista Brasileira de Ciência do Solo v.40 20162016-01-01info:eu-repo/semantics/articletext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832016000100543en10.1590/18069657rbcs20150174
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country Brasil
countrycode BR
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databasecode rev-scielo-br
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libraryname SciELO
language English
format Digital
author Mielki,Guilherme Furlan
Novais,Roberto Ferreira
Ker,João Carlos
Vergütz,Leonardus
Castro,Gustavo Franco de
spellingShingle Mielki,Guilherme Furlan
Novais,Roberto Ferreira
Ker,João Carlos
Vergütz,Leonardus
Castro,Gustavo Franco de
Iron Availability in Tropical Soils and Iron Uptake by Plants
author_facet Mielki,Guilherme Furlan
Novais,Roberto Ferreira
Ker,João Carlos
Vergütz,Leonardus
Castro,Gustavo Franco de
author_sort Mielki,Guilherme Furlan
title Iron Availability in Tropical Soils and Iron Uptake by Plants
title_short Iron Availability in Tropical Soils and Iron Uptake by Plants
title_full Iron Availability in Tropical Soils and Iron Uptake by Plants
title_fullStr Iron Availability in Tropical Soils and Iron Uptake by Plants
title_full_unstemmed Iron Availability in Tropical Soils and Iron Uptake by Plants
title_sort iron availability in tropical soils and iron uptake by plants
description ABSTRACT Given the increase in crop yields and the expansion of agriculture in low fertility soils, deficiency of micronutrients, such as iron, in plants grown in tropical soils has been observed. The aim of this study was to evaluate Fe availability and Fe uptake by corn (Zea mays L.) plants in 13 different soils, at two depths. Iron was extracted by Mehlich-1, Mehlich-3, and CaCl2 (Fe-CC) and was fractionated in forms related to low (Feo) and high (Fed) crystallinity pedogenic oxyhydroxides, and organic matter (Fep) using ammonium oxalate, dithionite-citrate, and sodium pyrophosphate, respectively. In order to relate Fe availability to soil properties and plant growth, an experiment was carried out in a semi-hydroponic system in which part of the roots developed in a nutrient solution (without Fe) and part in the soil (the only source of Fe). Forty-five days after seeding, we quantified shoot dry matter and leaf Fe concentration and content. Fed levels were high, from 5 to 132 g kg-1, and Feo and Fe-CC levels were low, indicating the predominance of Fe as crystalline oxyhydroxides and a low content of Fe readily available to plants. The extraction solutions showed significant correlations with various soil properties, many common to both, indicating that they act similarly. The correlation between the Mehlich-1 and Mehlich-3 extraction solutions was highly significant. However, these two extraction methods were inefficient in predicting Fe availability to plants. There was a positive correlation between dry matter and Fe levels in plant shoots, even within the ranges considered adequate in the soil and in the plant. Dry matter production and leaf Fe concentration and content were positively correlated with Fep concentration, indicating that the Fe fraction related to soil organic matter most contributes to Fe availability to plants.
publisher Sociedade Brasileira de Ciência do Solo
publishDate 2016
url http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832016000100543
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