Changes in soil organic carbon and soil aggregation due to deforestation for smallholder management in the Brazilian semi-arid region

• Published in: Geoderma Regional Vol. 33; p. e00647
• Main Authors: de Souza Medeiros, Aldair, Gonzaga, Giordano Bruno Medeiros, da Silva, Thamirys Suelle, de Souza Barreto, Bruno, dos Santos, Thiago Cândido, de Melo, Paul Lineker Amaral, de Araújo Gomes, Tâmara Cláudia, Maia, Stoécio Malta Ferreira
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.06.2023
• Subjects: Acrisols; Arenosols; Brazil; Caatinga; CO2 emissions; Conventional tillage; cropland; deforestation; indigenous species; land use; Multiple soil classes; pastures; Regosols; sandy clay loam soils; semiarid zones; soil aggregation; soil degradation; soil organic carbon; soil structure; texture; Water-stable aggregate; Brazil; Multiple soil classes; Caatinga; CO2 emissions; Conventional tillage; Water-stable aggregate
• ISSN: 2352-0094; 2352-0094
• DOI: 10.1016/j.geodrs.2023.e00647

The Brazilian semi-arid region has currently approximately 33.3 million hectares occupied by agriculture, and the inadequate land use and management practices are still predominant, which have been associated with the soil degradation process. Therefore, the aims of this study were to evaluate the effect of conventional agricultural systems (cropland and pasture) on soil structure using water-stable aggregate and aggregation indexes, and to assess the impacts on soil organic carbon (SOC) stocks in different soil types and textures in the Brazilian semi-arid region. The study was carried out in the municipalities of Delmiro Gouveia, Inhapi and Pariconha, in the Brazilian semi-arid region of the state of Alagoas, Brazil. Arenosols, Acrisols and Regosols soil samples were collected at 0–10, 10–20 and 20–30 cm layers. The treatments analyzed were: Cropland with 4, 15 and 30 years and pasture with 10 years. As a reference, native vegetation (Caatinga) was used. Our results show that the maintenance of SOC and structure and soil physical quality in conventional agricultural systems in the Brazilian semi-arid region depend on soil type/texture and climate. In agricultural systems in Acrisols with sandy clay loam texture, a 5.4% non significant increase was observed in SOC stocks after 30 years of use compared to SOC stocks in the native vegetation area; while in soils with sandy texture (Arenosols and Regosols), the SOC stocks were reduced by 16.1% in comparison to areas under native vegetation. The analysis of water-stable aggregate in Acrisols showed great predominance of macroaggregates (>2.0 mm). On the other hand, in sandy soils (Arenosols and Regosols), great predominance of mesoaggregates was observed (<2.00 and > 0.25 mm). •In Acrisols there was a 5.4% increase in SOC stocks after 30 years of use.•Arenosols and Regosols there was an average SOC reduction of 16.1%.•No significant effects of conventional systems on soil aggregation were verified.•It was not possible to verify the relationship between soil aggregation and SOC.