6533b7d5fe1ef96bd1264f67

RESEARCH PRODUCT

The relationship between copper accumulated in vineyard calcareous soils and soil organic matter and iron

Jean LévêqueCorinne ParatRémi ChaussodFrancis AndreuxSylvie Dousset

subject

2. Zero hungerchemistry.chemical_classificationTotal organic carbonSoil organic matterSoil Sciencechemistry.chemical_elementMineralogy04 agricultural and veterinary sciencesFractionation15. Life on land010501 environmental sciences01 natural sciencesNitrogenCopperchemistryEnvironmental chemistrySoil water040103 agronomy & agriculture0401 agriculture forestry and fisheriesOrganic matterCarbon0105 earth and related environmental sciences

description

Summary The intensive use for over 100 years of copper sulphate (Bordeaux mixture) to fight mildew in vineyards has led to a substantial accumulation of copper (Cu) in surface soils. To assess the effects of such large concentrations, the surface soils of 10 Burgundy vineyards were sampled and analysed for total organic matter (carbon and nitrogen) and metal (copper and iron) contents. Physical (i.e. size fractionation) and chemical (sequential extraction) methods were used to determine the distribution of these elements. The most Cu-contaminated plots showed the largest accumulation of organic carbon and Cu in the coarse sand and fine sand fractions. Copper was strongly correlated with organic carbon and organic nitrogen in the coarse sand fraction and with organic nitrogen in the fine sand fraction. Copper was also highly correlated with both Fe and organic nitrogen in the clay fraction but not significantly with organic carbon. The sequential extraction showed that Cu was bound mainly to the Fe oxides. However, in the most Cu-contaminated plots, a part of added Cu was bound to organic matter. This study suggests that Cu protected indirectly the organic matter present in the coarse fractions against biodegradation, and therefore modified the distribution of organic carbon among the particle-size fractions. Iron appeared as the main factor responsible for Cu accumulation in the clay fraction, mainly through inclusion of Cu in Fe oxyhydroxides and possibly in clay–humus complexes.

https://doi.org/10.1046/j.1365-2389.2002.00478.x