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What is Compost? Composting Biology and Core Principals

What is Compost? Composting Biology and Core Principals. David M. Crohn Department of Soil and Environmental Sciences University of California, Riverside. Compost: definition.

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What is Compost? Composting Biology and Core Principals

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  1. What is Compost?Composting Biology and Core Principals David M. CrohnDepartment of Soil and Environmental SciencesUniversity of California, Riverside

  2. Compost: definition • “An accumulation of decaying or decayed organic matter, as from leaves and manure, used to improve soil structure and to provide nutrients.” • Decay is a biological process (not a chemical process) • Properties determine what is a compost (not the production method)

  3. Not all composts are created equal. • Backyard Composting • Vermicomposting • Lasagna Composting • Thermophilic Composting

  4. Thermophilic composting

  5. Actinomycetes Bacteria Fungi Compost microorganisms Illustrations: www.Digitalseed.com

  6. Aerobic processes Microbes, Carbon, & Oxygen Carbon Dioxide, Water, Compost, &Heat

  7. Thermophilic composting • Microbes tend to specialize in the temperatures they prefer. • In California soils and in our bodies mesophiles are most abundant. Pathogens are mesophiles. • Between 110°F and 155°F, thermophiles dominate. • Above about 160°F dieoff begins. • Reliable pathogen kill occurs above 131°F. • Heat greatly accelerates microbial efficiency.

  8. 25x Thermophilic composting • Microbial efficiency approximately doubles for every 18°F increase in temperature • So how much faster will organic matter decompose if it heats from a shady 72°F to a toasty 150°F ?

  9. Active Composting Why compost? • To eliminate disease organisms Animal ● Plant ● Human • To produce a stable and safe soil amendment Nutrients ● Odors ● Phytotoxins Curing

  10. Carbon • Source of energy for microbes • Not all forms are equally available • lignin (less available) • cellulose • fats, waxes, proteins • sugars (more available) C

  11. C

  12. Nitrogen • Vital nutrient for microbes • Needed for protein synthesis • Excess may volatilize as ammonia (NH3) • Other nitrogenous compounds can be odiferous • Also important for plants • C:N ratio • initially about 35:1 • about 10:1 to 20:1 in cured product N

  13. N

  14. Oxygen • Acts as an electron acceptor • Permits efficient liberation of energy from carbon • Energy is used by microbes to grow and reproduce O2

  15. Heat O2 O2 Oxygen: turned windrow

  16. Composting alternatives Turned Windrow In-vessel Static pile Illustration: Rynk et al. 1992

  17. Water • Clings to compost particles • The bath within which microbes grow • Too much fills pores • Oxygen moves slowly into water H2O

  18. Air Water Anaerobic Zone Unavailable Zone Aerobic Zone Compost particle environment

  19. Particle Size Porosity C:N ratio H2O O2 Management parameters

  20. Conclusions • The composter’s success in managing the process will determine • Product quality • Product consistency • Consistent quality increases demand for composts • Increased demand increases product value

  21. Questions?

  22. Mulches, Soil Amendments and Organic Fertilizers David M. CrohnDepartment of Soil and Environmental SciencesUniversity of California, Riverside

  23. Mulches: cover the soil • Protect soils against erosion • Conserve water by slowing evaporation • Control weeds • Control certain plant diseases • Decorate landscapes

  24. Soil amendments: modify soil properties • Improve tilth • Improve water holding capacity • Improve aeration • Improve infiltration capacity • Adjust pH • Promote microbial activity and diversity

  25. Organic fertilizers: slow release sources of • Nitrogen • Phosphorus • Potassium • Micronutrients

  26. Conclusions • Mulches, soil amendments and organic fertilizers are uses, not products. • Composts may serve any of these. • Different composts have different properties, and some will therefore be more suitable for certain uses than for others.

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