From desertification to restoration in the Brazilian semiarid region: Unveiling the potential of land restoration on soil microbial properties.

Land desertification poses a significant challenge in the Brazilian semiarid region, encompassing a substantial portion of the country. Within this region, the detrimental effects of human activities, particularly unsuitable anthropic actions, have resulted in diminished vegetation cover and an accelerated rate of soil erosion. Notably, practices such as overgrazing and the conversion of native forests into pasturelands have played a pivotal role in exacerbating the process of land desertification. Ultimately, land desertification results in significant losses of soil organic matter and microbial diversity. To address this pressing issue and contribute to the existing literature, various land restoration practices, such as grazing exclusion, cover crops, and terracing, have been implemented in the Brazilian semiarid. These practices have shown promising results in terms of enhancing soil fertility and restoring microbial properties. Nonetheless, their effectiveness in improving soil microbial properties in the Brazilian semiarid region remains a subject of ongoing study. Recent advances in molecular techniques have improved our understanding of microbial communities in lands undergoing desertification and restoration. In this review, we focus on assessing the effectiveness of these restoration practices in revitalizing soil microbial properties, with a particular emphasis on the soil microbiome and its functions. Through a critical assessment of the impact of these practices on soil microbial properties, our research aims to provide valuable insights that can help mitigate the adverse effects of desertification and promote sustainable development in this ecologically sensitive region.

Mapeamento da erodibilidade e erosão potencial do solo em uma bacia hidrográfica de encosta / Mapping of erodibility and potential soil erosion in a hillside watershed

RESUMO O objetivo deste estudo foi estimar o potencial de perda de solo por meio da equação universal de perda de solo e identificar os fatores que controlam o processo erosivo em uma bacia hidrográfica de encosta. O fator erosividade da chuva (R) foi calculado por meio de dados normais de precipitação, obtendo-se, assim, índices mensais de erosão. O fator erodibilidade do solo (K) foi obtido a partir de uma amostragem de solo realizada por meio de uma malha de 340 pontos, na qual os valores foram interpolados pelo método da krigagem ordinária. O fator topográfico (LS) foi gerado a partir do Modelo Digital de Elevação (MDE), já os fatores uso e manejo e práticas conservacionistas (CP) foram obtidos por meio de observações de campo e valores tabelados. As maiores taxas de perdas abrangem 27% da área e se concentram em locais de maiores declividades nos quais predominam solos rasos, como Neossolos Litólicos e Neossolos Regolíticos. O fator LS determinou a magnitude do processo erosivo e o fator CP apresentou a maior relação com o controle das perdas de solo. Os resultados encontrados mostram a importância do fator cobertura do solo, em que medidas de manutenção da vegetação e práticas conservacionistas devem ser adotadas e consideradas pelos gestores ambientais em regiões de encosta com predomínio de solos rasos associados a relevo declivoso.

ABSTRACT The objective of this study was to estimate the soil loss potential through the universal soil loss equation and to identify the factors that control the erosive process in a hillside watershed. Rainfall erosivity factor (R) was calculated through normal precipitation data, thus obtaining monthly erosion indexes. The soil erodibility factor (K) was obtained from a soil sampling in an irregular grid of 340 points, in which the values were interpolated by the ordinary kriging method. The topographic factor (LS) was generated from the Digital Elevation Model (MDE) and the use and management and conservationist practices factors (CP) through field observations and tabulated values. The highest loss rates cover around 27% of the area, and are concentrated in places with higher slopes where shallow soils such as Litolics Neosols and Regolithic Neosols predominate. The LS factor determined the magnitude of the erosive process and the CP factor showed the highest relation with the soil loss control. The results found show the importance of the cover-management factor, in which measures of vegetation maintenance and conservation practices should be adopted and considered by the environmental managers in hillside regions with predominance of shallow soils associated to slope relief.