ABSTRACT
The worldwide historical carbon (C) losses due to Land Use and Land-Use Change between 1870 and 2014 are estimated at 148 Pg C (1 Pg=1billionton). South America is chosen for this study because its soils contain 10.3% (160 Pg C to 1-m depth) of the soil organic carbon stock of the world soils, it is home to 5.7% (0.419 billion people) of the world population, and accounts for 8.6% of the world food (491milliontons) and 21.0% of meat production (355milliontons of cattle and buffalo). The annual C emissions from fossil fuel combustion and cement production in South America represent only 2.5% (0.25 Pg C) of the total global emissions (9.8 Pg C). However, South America contributes 31.3% (0.34 Pg C) of global annual greenhouse gas emissions (1.1 Pg C) through Land Use and Land Use Change. The potential of South America as a terrestrial C sink for mitigating climate change with adoption of Low-Carbon Agriculture (LCA) strategies based on scenario analysis method is 8.24 Pg C between 2016 and 2050. The annual C offset for 2016 to 2020, 2021 to 2035, and 2036 to 2050 is estimated at 0.08, 0.25, and 0.28 Pg C, respectively, equivalent to offsetting 7.5, 22.2 and 25.2% of the global annual greenhouse gas emissions by Land Use and Land Use Change for each period. Emission offset for LCA activities is estimated at 31.0% by restoration of degraded pasturelands, 25.6% by integrated crop-livestock-forestry-systems, 24.3% by no-till cropping systems, 12.8% by planted commercial forest and forestation, 4.2% by biological N fixation and 2.0% by recycling the industrial organic wastes. The ecosystem carbon payback time for historical C losses from South America through LCA strategies may be 56 to 188years, and the adoption of LCA can also increase food and meat production by 615Mton or 17.6Mtonyear-1 and 56Mton or 1.6Mtonyear-1, respectively, between 2016 and 2050.
Subject(s)
Agriculture/methods , Carbon Sequestration , Food Supply , Animals , Carbon/analysis , Cattle , Climate Change , Ecosystem , Food , Forests , Livestock , Plants/metabolism , Soil , South AmericaABSTRACT
A redução no conteúdo de carbono (C) nas camadas mais profundas do solo indica a estratificação entre a camada superficial e as subsuperficiais, devido à adição contínua de C pelos resíduos culturais na superfície. O objetivo deste trabalho foi avaliar a variação (∆) da relação de estratificação (RE) de carbono como indicadora do sequestro de C total e particulado em macroagregados de dois Latossolos de classes texturais diferentes, manejados em sistema plantio direto. Os ensaios foram desenvolvidos em delineamento inteiramente casualizado com doze repetições. Os fatores analisados foram: (a) dois solos (Latossolo Vermelho Distrófico típico com classe textural franco-argilo-arenosa e Latossolo Vermelho Distrófico típico com classe textural franco-argilosa); (b) duas camadas de amostragem (0-5 e 5-20cm de profundidade); (c) duas épocas de amostragem (E1-outubro de 2007; E2-setembro de 2008). Observou-se relação linear e significativa entre o delta RE com a taxa de sequestro de C total em macroagregados no Latossolo Vermelho com classe textural franco argilo arenosa (R²=0,78**) e franco argilosa (R²=0,81**), indicando ter havido sequestro de C e confirmando ser este um indicador sensível da taxa de sequestro de C no solo em macroagregados.
The decrease in soil organic carbon (SOC) content in deeper layers indicates the occurrence of stratification between the surface layer and subsurface layer of soil due to continuous C addition by crop residues. The objective was to evaluate the change (delta) of stratification (RE) of carbon (C) as an indicator of C sequestration and soil total and particulate soil in macroaggregates of two soils (Typic Hapludox) with different textures, managed in no-tillage system. The tests were developed in completely randomized design twelve repetitions.Analyzed factors were: (a) two soils: Oxisol with medium texture and Oxisol with clay texture, (b) sampling depth: 0-5 and 5-20cm, (c) two sampling times (October 2007-T1, September 2008-T2). The results were submitted to variance analysis by program SISVAR 5.3, using the Tukey test at 5% significance. There was a significant linear relationship between the ∆ RE and carbon sequestration rate total macroaggregates Oxisol with medium texture (R²=0.78**) and Oxisol with clay texture (R²=0.81**) indicating that there was C sequestration confirming to be a sensitive indicator of the rate of C sequestration in soil macroaggregates.
