We a good story
Quick delivery in the UK

Biogeochemistry of Soil Organic Matter

About Biogeochemistry of Soil Organic Matter

Benefits of MOS in conservation management systems: Physical (structure and aggregation) forming larger structures that favor the root system of cultivated plants.Chemical: By improving the CEC of soils, complexing exchangeable aluminum and reducing the adsorption of P. This is especially helpful in Brazil's tropical soils.Biological: Promotes soil microbiota and enzymesSoil management involving mechanical intervention (plowing, harrowing, scarification, etc.) breaks up soil aggregates, macro- and micro-aggregates, increasing the area of exposure of MOS to microbial attack. In addition, with greater aeration, micro-organisms attack this MOS more easily and contribute to its mineralization.  Grass residues have a higher C/N ratio, often above 30/1, which is why the balance between immobilization and mineralization tends towards microbial immobilization, until this C/N ratio becomes narrower, at which point this balance will tend towards mineralization. Soybean waste has a narrower C/N ratio, below 20/1, which makes mineralization the predominant process

Show more
  • Language:
  • English
  • ISBN:
  • 9786207270552
  • Binding:
  • Paperback
  • Published:
  • March 14, 2024
  • Dimensions:
  • 152x229x4 mm.
  • Weight:
  • 118 g.
Delivery: 1-2 weeks
Expected delivery: December 6, 2024

Description of Biogeochemistry of Soil Organic Matter

Benefits of MOS in conservation management systems: Physical (structure and aggregation) forming larger structures that favor the root system of cultivated plants.Chemical: By improving the CEC of soils, complexing exchangeable aluminum and reducing the adsorption of P. This is especially helpful in Brazil's tropical soils.Biological: Promotes soil microbiota and enzymesSoil management involving mechanical intervention (plowing, harrowing, scarification, etc.) breaks up soil aggregates, macro- and micro-aggregates, increasing the area of exposure of MOS to microbial attack. In addition, with greater aeration, micro-organisms attack this MOS more easily and contribute to its mineralization.  Grass residues have a higher C/N ratio, often above 30/1, which is why the balance between immobilization and mineralization tends towards microbial immobilization, until this C/N ratio becomes narrower, at which point this balance will tend towards mineralization. Soybean waste has a narrower C/N ratio, below 20/1, which makes mineralization the predominant process

User ratings of Biogeochemistry of Soil Organic Matter



Find similar books
The book Biogeochemistry of Soil Organic Matter can be found in the following categories:

Join thousands of book lovers

Sign up to our newsletter and receive discounts and inspiration for your next reading experience.