Thiago Inagaki
Research Scientist
Biography
Dedicated researcher with experience in soil science, sustainable agriculture, and climate change adaptation. Academic journey includes a Ph.D. and postdoctoral research focused on soil organic matter stabilization and carbon sequestration in agriculture. Led and coordinated multiple research projects, utilizing advanced techniques such as isotope labeling and synchrotron-based methods, and collaborated with esteemed professors and international research teams.
Work spans various global initiatives, including projects on organic waste management, diversified cropping systems, and no-tillage practices in tropical and subtropical regions. Contributed to educational efforts by developing teaching materials, assisting students, and writing accessible content for broader audiences.
Deeply interested in multidisciplinary soil science research, particularly focusing on soil structure and the persistence of organic matter. Research interests encompass the functionality of soil organic matter in both agricultural and natural systems, primarily focusing on mechanisms for its persistence through organo-mineral associations.
Authors
Daniel Ruiz Potma Gonçalves Thiago M. Inagaki Luis Gustavo Barioni Newton La Scala Junior Maurício Roberto Cherubin João Carlos de Moraes Sá Carlos Eduardo Pellegrino Cerri Adriano AnselmiAbstract
Soils are the third largest carbon pool on Earth and play a crucial role in mitigating climate change. Therefore, understanding and predicting soil carbon sequestration is of major interest to mitigate climate change globally, especially in countries with strong agricultural backgrounds. In this study, we used a new database composed of 5029 samples collected up to 1-meter depth in three biomes that are most representative of agriculture, Pampas (Prairie), Cerrados (Savanna), and Atlantic Forest (Forest), to explore soil organic carbon (SOC) stocks and its environmental drivers. The Cerrado (Savanna) biome was the only one where croplands presented higher SOC stocks than native vegetation (Native vegetation 121.23 Mg/ha and croplands 127.85 Mg/ha or 5 % higher). From the tested models, the Random Forest outperformed the others, achieving an R2 of 0.64 for croplands and 0.56 for native vegetation. The accuracy of the models varied with soil depth, showing better predictions in shallow layers for croplands and deeper layers for native vegetation. Our results highlight the importance of clay content, precipitation, net primary production (NPP), and temperature as key predictors for soil carbon stocks in the studied biomes. The findings emphasize the importance of protecting the surface layers, especially in the Cerrado biome, to enhance SOC stocks and promote sustainable land management practices. Moreover, the results provide valuable insights for the development of nature-based carbon markets and suggest potential strategies for climate change mitigation. Enhancing our understanding of SOC dynamics and adopting precise environmental predictors will contribute to the formulation of targeted soil management strategies and accelerate progress toward achieving climate goals.
Authors
Luiz Claudio Garcia Guilherme H. Carraro Sandro Felema Allison J. Fornari Leandro J. V. Sformi Thiago M. InagakiAbstract
No abstract has been registered
Authors
Aline Roma Tomaz Ademir de Oliveira Ferreira Rattan Lal Telmo Jorge Carneiro Amado Belchior Oliveira Trigueiro da Silva William Ramos da Silva Felipe José Cury Fracetto Thiago M. Inagaki Maria Betânia Galvão Santos Freire Elves Obede dos Santos NunesAbstract
Land-use change has driven soil carbon stock losses in ecosystems worldwide. Implementing agricultural crops and exploiting forest resources trigger the breakdown of soil aggregates, thus exposing organic matter to microbial decomposition and enhancing carbon dioxide emissions, especially in biomes more susceptible to climate extremes as in the tropical semiarid regions. This study was based on the hypothesis that the undisturbed soil from the dry forest (Caatinga biome under natural revegetation in Brazilian semiarid) would have an improvement in the mass of macroaggregates and recover more than 50% of the soil C stock within 10 years. Thus, a field experiment was conducted to investigate soils from the Caatinga biome under native vegetation, “cowpea cropping” for over 30 years, and soil under natural revegetation for over 10 years, after conventional soil cultivation of maize and cowpea, to determine soil and soil-aggregates carbon stocks and to estimate the recovery rate of these stocks. The proportional mass of aggregates of different sizes and the total stock of particulate organic carbon (POC) were also quantified. The results showed that soil under preserved native vegetation of dry forest Caatinga biome had higher total soil C stock (50.9 Mg ha−1) than that under cowpea cropping (23.2 Mg ha−1) and natural revegetation (45.1 Mg ha−1). The proportional mass of large macroaggregates was higher in soil under native vegetation for all depths. However, soil under cowpea cropping had lower C stocks in macroaggregates, and recovered roughly 63% of the original C stocks, while revegetation recovered 78% of the stock in 10 years. Although the conventional management system for cowpea monoculture aggravated losses in soil carbon stock by more than 50% of the original C stocks, dry forest under natural revegetation recovered 79% of this stock and almost 100% of POC stock in 10 years (~12 Mg ha−1). Furthermore, soil under undisturbed Caatinga dry forest achieved C stock levels equivalent to that of the global average range for semiarid tropical environments. The high recovery rate of C stock in forest soil under natural revegetation indicates the resilience potential of organisms responsible for structural protection of aggregates and the encapsulated soil organic matter content.
Division of Environment and Natural Resources
Conservation of Biodiversity in China in the light of Climate Change
Climate change is becoming an increasingly important pressure on biodiversity, which adds to the burden of other drivers of loss of biodiversity causing negative effects on ecosystems and species
Division of Environment and Natural Resources
AgriCascade
Cascading recycling of organic N-sources with next-generation biochar fertilizer for Norwegian agriculture
Division of Environment and Natural Resources
TerraNordica: Nordic Partnership for Soil Health and Agroecology
Soil health and Ecosystem Services (ES) are assessed through measuring carefully selected physical, chemical, and biological soil indicators related to dynamic soil properties, and compare these to thresholds or standard values that separate healthy from unhealthy conditions.
Division of Environment and Natural Resources
Sinograin III: Smart agricultural technology and waste-made biochar for food security, reduction of greenhouse gas (GHG) emission, and bio-and circular economy
The Sinograin III project’s overall objective is to contribute to the UN SDGs by widely implementing precision agriculture technologies and application of “waste-to-value” biochar products to achieve sustainable food production with minimized GHG emission, improve soil fertility and promote green growth/zero waste in modern agriculture in China.