4.3 Article

Impact of Biochar Amendment on Soil Properties and Organic Matter Composition in Trace Element-Contaminated Soil

Publisher

MDPI
DOI: 10.3390/ijerph19042140

Keywords

pyrogenic C; soil organic matter; humic acids; heavy metals; carbon sequestration; degraded soil

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The application of biochar as an organic amendment can facilitate the recovery of polluted soils by reducing the availability of contaminants. This study assessed the effect of biochar application on the quantity and composition of soil organic matter, with a focus on soil humic acids. The results showed an increase in soil water holding capacity, total organic carbon content, and soil pH after biochar application. The quantity and composition of oxidisable carbon and extracted humic acids were not altered by biochar addition.
The application of biochar as an organic amendment in polluted soils can facilitate their recovery by reducing the availability of contaminants. In the present work, the effect of biochar application to acid soils contaminated by heavy metal spillage is studied to assess its effect on the quantity and composition of soil organic matter (SOM), with special attention given to soil humic acids (HAs). This effect is poorly known and of great importance, as HA is one of the most active components of SOM. The field experiment was carried out in 12 field plots of fluvisols, with moderate and high contamination by trace elements (called MAS and AS, respectively), that are located in the Guadiamar Green Corridor (SW Spain), which were amended with 8 Mg center dot ha(-1) of olive pit biochar (OB) and rice husk biochar (RB). The results indicate that 22 months after biochar application, a noticeable increase in soil water holding capacity, total organic carbon content, and soil pH were observed. The amounts of oxidisable carbon (C) and extracted HAs in the soils were not altered due to biochar addition. Thermogravimetric analyses of HAs showed an increase in the abundance of the most thermostable OM fraction of the MAS (375-650 degrees C), whereas the HAs of AS were enriched in the intermediate fraction (200-375 degrees C). Spectroscopic and chromatographic analyses indicate that the addition of biochar did not alter the composition of the organic fraction of HAs, while Cu, Fe, and as were considerably accumulated at HAs.

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