Organic matter input determines structure development and aggregate formation in artificial soils

Keyphrases

• Incubation 100%
• Aggregate Formation 100%
• Structure Development 100%
• Pomc 100%
• Artificial Soil 100%
• Organic Matter Input 100%
• Microcosm 75%
• Pore System 75%
• Euler number 50%
• Organic Carbon 50%
• C Input 50%
• Interconnected Pores 50%
• Organic Carbon Input 50%
• Organic Matter Type 50%
• Carbon Compounds 25%
• Organic Matter 25%
• Pore Size 25%
• Pore Connectivity 25%
• Water Exchange 25%
• Pore Structure 25%
• Cohesion 25%
• Organic-inorganic 25%
• Size Fraction 25%
• Freeze-thaw Cycles 25%
• Microenvironment 25%
• Highly Connected 25%
• Primary Particles 25%
• Gas-water 25%
• Particle Size Distribution 25%
• Pore Space 25%
• Particle Matter 25%
• Dissolved Organic Matter 25%
• Microbial Decomposition 25%
• Gas Exchange 25%
• Size Composition 25%
• Particulate Organic Matter 25%
• Microaggregates 25%
• Constant Water 25%
• Mineral Particles 25%
• Macroaggregates 25%
• Aggregate Size Distribution 25%
• Soil Matrix 25%
• Cambisols 25%
• Water-stable Macroaggregates 25%
• Soil Microcosm 25%
• Mass Contribution 25%
• Water Tension 25%
• Nutrient Exchange 25%
• Physical Interference 25%
• Controlled Laboratory Conditions 25%
• Mineral Surfaces 25%
• Organic Carbon Addition 25%

Earth and Planetary Sciences

• Organic Matter 100%
• Organic Carbon 100%
• Macroaggregate 40%
• Particle Size Distribution 20%
• Pore Space 20%
• Aggregate Size 20%
• Mineral Surface 20%
• Particulate Organic Matter 20%
• Cambisol 20%
• Microaggregate 20%