Converting Low-Productivity Pasture to Well-Managed Pasture and Silvopastoral System Cause Relevant Changes in Soil Chemical and Microbiological Characteristics

Author:

Silva Libério Junio da1,Freitas Igor Costa de2,Abreu Luiz Henrique Gomes de2,Oliveira Dener Márcio da Silva3,Barbosa Demerson Luiz de Almeida4ORCID,Figueredo Cléber Cunha5,Camilotti Vagner Luis6,Teixeira Marcus Vinícius3,Frazão Leidivan Almeida2ORCID

Affiliation:

1. Centro de Sensoriamento Remoto, Universidade Federal de Minas Gerais, Belo Horizonte 31270-901, MG, Brazil

2. Instituto de Ciências Agrárias, Universidade Federal de Minas Gerais, Montes Claros 39400-090, MG, Brazil

3. Instituto de Ciências Agrárias, Universidade Federal de Viçosa, Florestal 35690-000, MG, Brazil

4. Faculdade de Ciências Agrárias, Universidade Federal dos Vales do Jequitinhonha e Mucuri, Diamantina 39100-000, MG, Brazil

5. Instituto de Ciências Biológicas, Universidade Federal de Minas Gerais, Belo Horizonte 31270-901, MG, Brazil

6. Instituto Nacional de Pesquisas Espaciais, São José dos Campos 12227-010, SP, Brazil

Abstract

This study evaluated the chemical and microbiological soil attributes in a silvopastoral system compared to well-managed pasture, degraded pasture, and Cerrado vegetation in Brazil. A randomized design with four replications was employed to collect soil samples at seven depths. These samples were analyzed for carbon (C), nitrogen (N), pH, phosphorus (P), potassium (K), calcium (Ca), magnesium (Mg), and cation exchange capacity (CEC). Soil microbial attributes were also evaluated at three depths during the dry and wet seasons. Carbon stocks in the evaluated systems varied (0–100 cm), with the highest stocks found in well-managed pasture (MP) (129.5 Mg C ha−1), followed by the silvopastoral system (SPS) (106.6 Mg C ha−1), and the lowest values in native vegetation (NV) (84.8 Mg C ha−1) and degraded pasture (DP) (63.4 Mg C ha−1). Higher pH and base sum were observed in MP. Soil microbial biomass (Cmic) did not differ between treatments during the wet season but was generally higher in MP and lower in DP during the dry season. MP effectively regulated the chemical and biological quality of the soil. The SPS demonstrated that it is possible to combine the cultivation of trees and pastures in the same area, contributing to the improvement of the chemical and biological attributes of the soil in the Brazilian Cerrado.

Funder

Fundação de Amparo à Pesquisa do Estado de Minas Gerais—Fapemig

Conselho Nacional de Desenvolvimento Científico e Tecnológico—CNPq

Fundação de Amparo à Pesquisa do Estado de São Paulo—FAPESP

Bayer S.A.

Shell Brasil

Publisher

MDPI AG

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2. Francaviglia, R., Almagro, M., and Vicente-Vicente, J.L. (2023). Conservation agriculture and soil organic carbon: Principles, processes, practices and policy options. Soil Syst., 7.

3. Meena, S.K., Ferreira, A.D.O., Meena, V.S., Rakshit, A., Shrestha, R.P., Rao, C.S., and Siddique, K.H.M. (2023). Agricultural management impacts on soil organic carbon storage. Agricultural Soil Sustainability and Carbon Management, Academic Press.

4. Soil microbial community, enzyme activity, C and N stocks and soil aggregation as affected by land use and soil depth in a tropical climate region of Brazil;Sarto;Arch. Microbiol.,2020

5. Dynamics of organic matter molecular composition under aerobic decomposition and their response to the nitrogen addition in grassland soils;Zhao;Sci. Total Environ.,2022

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