Chemical composition of cabbage (Brassica oleracea L. var. capitata) grown on acid sulfate soils
Identifieur interne : 000478 ( Main/Exploration ); précédent : 000477; suivant : 000479Chemical composition of cabbage (Brassica oleracea L. var. capitata) grown on acid sulfate soils
Auteurs : Rasmus F Ltmarsch [Finlande] ; Peter Österholm [Finlande] ; Gunnar Jacks [Suède]Source :
- Journal of Plant Nutrition and Soil Science [ 1436-8730 ] ; 2010-06.
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Abstract
The purpose of this study was to investigate the influence of soil geochemistry on the concentrations of Ca, K, Mg, P, Co, Ni, Zn, Mn, Cu, and Fe in cabbage (Brassica oleracea L. var. capitata) grown on acid sulfate (AS) soils in Western Finland. A total of 11 topsoil (0–20 cm) and corresponding cabbage samples and three whole‐soil profiles (≈ 0–260 cm) were collected on three agricultural fields. The concentrations of Co and Zn in cabbage were correlated with the NH4Ac‐extractable (easily available) concentrations in the topsoil, indicating that the uptake of these elements in cabbage is largely governed by soil geochemistry. Yet, the concentrations of Co and Zn in cabbage were not in general elevated relative to that of Finnish average values, although some AS soils showed enriched concentrations of these metals in the soil and cabbage. Significant geochemical differences (e.g., oxidation depth, organic‐matter and S content, pH) were observed among the studied AS soils, while, on the other hand, the concentrations of Ca, K, Mg, P, Ni, Mn, Cu, and Fe in cabbage were relatively similar. The hydroxylamine‐extractable concentrations of these elements in the topsoil were not correlated to those in cabbage, suggesting that uptake is not governed by the oxide‐bound fraction of these elements in the soil. Similarly, the easily available concentrations of Ca, P, Ni, Mn, Cu, and Fe in the topsoil were not correlated to those in cabbage, indicating that uptake is independent of the easily available concentrations in the soil. Hence, it is suggested that cabbage can regulate and thus optimize its concentrations of Ca, P, Ni, Mn, Cu, and Fe. Oxidation depth affected neither the easily available concentrations of Co, Ni, Zn, and Mn in the topsoil nor the concentrations in cabbage. However, the subsoil with a lower oxidation depth, which is to a smaller extent affected by leaching, may partly be enriched in these metals. Nevertheless, these showed no increased concentrations in cabbage. Based on these findings, it is suggested that the large amounts of metals mobilized in AS soils are easily lost to drains, subsequently contaminating nearby waterways and estuaries whereas they are only partly enriched in cabbage and other previously studied crops (oat).
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DOI: 10.1002/jpln.200900277
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Pflanzenernähr. Bodenk.</title><idno type="ISSN">1436-8730</idno><idno type="eISSN">1522-2624</idno><imprint><publisher>WILEY‐VCH Verlag</publisher><pubPlace>Weinheim</pubPlace><date type="published" when="2010-06">2010-06</date><biblScope unit="volume">173</biblScope><biblScope unit="issue">3</biblScope><biblScope unit="page" from="423">423</biblScope><biblScope unit="page" to="433">433</biblScope></imprint><idno type="ISSN">1436-8730</idno></series><idno type="istex">C67A9B56046C4E54F3B41E149310F2A994843475</idno><idno type="DOI">10.1002/jpln.200900277</idno><idno type="ArticleID">JPLN200900277</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">1436-8730</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>NH4‐acetate</term><term>leaching</term><term>metal</term><term>nutrient availability</term><term>topsoil</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">The purpose of this study was to investigate the influence of soil geochemistry on the concentrations of Ca, K, Mg, P, Co, Ni, Zn, Mn, Cu, and Fe in cabbage (Brassica oleracea L. var. capitata) grown on acid sulfate (AS) soils in Western Finland. A total of 11 topsoil (0–20 cm) and corresponding cabbage samples and three whole‐soil profiles (≈ 0–260 cm) were collected on three agricultural fields. The concentrations of Co and Zn in cabbage were correlated with the NH4Ac‐extractable (easily available) concentrations in the topsoil, indicating that the uptake of these elements in cabbage is largely governed by soil geochemistry. Yet, the concentrations of Co and Zn in cabbage were not in general elevated relative to that of Finnish average values, although some AS soils showed enriched concentrations of these metals in the soil and cabbage. Significant geochemical differences (e.g., oxidation depth, organic‐matter and S content, pH) were observed among the studied AS soils, while, on the other hand, the concentrations of Ca, K, Mg, P, Ni, Mn, Cu, and Fe in cabbage were relatively similar. The hydroxylamine‐extractable concentrations of these elements in the topsoil were not correlated to those in cabbage, suggesting that uptake is not governed by the oxide‐bound fraction of these elements in the soil. Similarly, the easily available concentrations of Ca, P, Ni, Mn, Cu, and Fe in the topsoil were not correlated to those in cabbage, indicating that uptake is independent of the easily available concentrations in the soil. Hence, it is suggested that cabbage can regulate and thus optimize its concentrations of Ca, P, Ni, Mn, Cu, and Fe. Oxidation depth affected neither the easily available concentrations of Co, Ni, Zn, and Mn in the topsoil nor the concentrations in cabbage. However, the subsoil with a lower oxidation depth, which is to a smaller extent affected by leaching, may partly be enriched in these metals. Nevertheless, these showed no increased concentrations in cabbage. Based on these findings, it is suggested that the large amounts of metals mobilized in AS soils are easily lost to drains, subsequently contaminating nearby waterways and estuaries whereas they are only partly enriched in cabbage and other previously studied crops (oat).</div></front></TEI><affiliations><list><country><li>Finlande</li><li>Suède</li></country><region><li>Svealand</li></region><settlement><li>Stockholm</li></settlement></list><tree><country name="Finlande"><noRegion><name sortKey="F Ltmarsch, Rasmus" sort="F Ltmarsch, Rasmus" uniqKey="F Ltmarsch R" first="Rasmus" last="F Ltmarsch">Rasmus F Ltmarsch</name></noRegion><name sortKey="F Ltmarsch, Rasmus" sort="F Ltmarsch, Rasmus" uniqKey="F Ltmarsch R" first="Rasmus" last="F Ltmarsch">Rasmus F Ltmarsch</name><name sortKey="Osterholm, Peter" sort="Osterholm, Peter" uniqKey="Osterholm P" first="Peter" last="Österholm">Peter Österholm</name></country><country name="Suède"><region name="Svealand"><name sortKey="Jacks, Gunnar" sort="Jacks, Gunnar" uniqKey="Jacks G" first="Gunnar" last="Jacks">Gunnar Jacks</name></region></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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