Land‐use change with pasture and short rotation eucalypts impacts the soil C emissions and organic C stocks in the Cerrado biome. (26th December 2019)

• Record Type: Journal Article
• Authors: Teixeira, Rafael da Silva; Fialho, Ricardo Cardoso; Costa, Daniela Cristina; de Sousa, Rodrigo Nogueira; Santos, Rafael Silva; Teixeira, Ana Paula Mendes; Reis, Thalles Guimarães; da Silva, Ivo Ribeiro
• Is Part Of: Land degradation & development. Volume 31:Number 7(2020)
• Page Start: 909
• Page End: 923
• Publication Date: 2019-12-26
• Subjects: 13C -- CH4‐C -- CO2‐C -- mineral‐associated organic matter -- particulate organic matter -- tropical soils, and; Land degradation -- Periodicals; Soil conservation -- Periodicals; Reclamation of land -- Periodicals; Land use -- Periodicals; Economic development -- Environmental aspects -- Periodicals; 333.7315
• DOI: 10.1002/ldr.3480
• Languages: English
• ISSNs: 1085-3278

Abstract

Abstract: The expansion of short rotation eucalypt plantations in low soil organic matter (SOM) sandy soils may offer an alternative to improve soil C sequestration. The goal of this study was to estimate the changes in C stocks and emissions in different SOM fractions following conversion of the native Cerrado to pasture and then to eucalypt plantation. Therefore, we studied soils under native Cerrado, planted pasture (cultivated for 34years following the clearing of the Cerrado) and eucalypt plantation (4years). The C and N stocks in particulate organic matter and mineral‐associated organic matter (MAOM) were determined 4years after eucalypt planting. Soil CO2 ‐C, CH4 ‐C fluxes and CO2 ‐C concentrations in soil profile were measured in different seasons over 4years. Variation in the natural abundance of 13 C was used to partition the SOM‐C. The soil CO2 ‐C and CH4 ‐C fluxes were influenced by soil surface moisture ( r = 0.185 o and r = 0.430 **, respectively), whereas only the soil CH4 ‐C fluxes correlated with soil surface temperature ( r = 0.355 ** ). The highest soil CO2 ‐C flux in soil under eucalypt occurred after 4years of eucalypt planting (2.5 kg ha −1 h −1, approximately 70%). The pasture soil acted as a CH4 ‐C source to the atmosphere. The pasture MAOM‐C losses in the 0.0–1.0‐m soil layers were not compensated by the new eucalypt C inputs (MAOM‐C lost ~9.6 Mg ha −1 ). In summary, the recent worldwide expansion of short rotation eucalypt plantations should be carefully considered, particularly under pasture degraded soil sandy soils, because land uses able to increase SOM are priorities.