ORGANIC MATTER DECOMPOSITION

1. ORGANIC MATTER DECOMPOSITION CHAPTER 6

2. OBJECTIVES • Process of organic matter decomposition • Factors affecting organic matter decomposition • Relate the activities of microorganism with soil fertility

3. SOIL • There are three major properties of soil. • Physical – soil structure and texture • Chemical – chemical components; pH, nutrients • Biological – micro and macro fauna/flora • Soil organic matter (OM) is any material produced originally by living organisms (plant or animal) that is returned to the soil and goes through the decomposition process

4. Contain five major groups of microorganisms • Bacteria • Actinomycetes • Fungi • Algae • Protozoa

5. All these microorganisms participate in the various activities that take place in the soil. • Among the activities are; • Decomposition of organic matter • Nutrient Cycling • Nutrients transport/flow • Protection

6. ESSENTIAL PLANT NUTRIENTS • There are at least 16 essential chemical elements for plant growth • Plant must have these nutrients to performance the various physiological functions • C, H and oxygen (O), (from air & water) • N, phosphorus (P), potassium (K), Ca, Mg, sulfur (S), iron (Fe), manganese (Mn), Zn, copper (Cu), boron (B), molybdenum (Mo), and chlorine (Cl) (from soil) • Sodium (Na), silicon (Si), and nickel (Ni) Cobalt (Co) (required by certain plants)

7. SOURCES OF PLANT NUTRIENTS IN THE SOIL 1) weathering of soil minerals 2) decomposition of plant residues, animal remains, and soil microorganisms 3) application of fertilizers and liming materials, 4) application of manures, composts, biosolids (sewage sludge) and other organic amendments

8. 5) N-fixation by legumes 6) ground rock powders or dusts including greensand, basalt, and rock phosphate 7) inorganic industrial byproducts 8) atmospheric deposition, such as N and S from acid rain or N-fixation by lightning discharges, 9) deposition of nutrient-rich sediment from erosion and flooding

10. Basic Plant Nutrient Cycle • The basic nutrient cycle highlights the central role of soil organic matter and microorganisms. • Cycling of many plant nutrients, especially N, P, S, and micronutrients, closely follows the Carbon Cycle. • Plant residues and manure from animals that are fed forage, grain, and other plant-derived foods are returned to the soil.

11. This OM pool of carbon compounds becomes food for bacteria, fungi, and other decomposers. • As OM is broken down to simpler compounds, plant nutrients are released in available forms for root uptake and the cycle begins again. • Plant-available nutrients such as K, Ca, Mg, P, and trace metal micronutrients are also released when soil minerals dissolve.

12. DECOMPOSITION OF OM • Definitions: • Breakdown of dead plant and animal material and release of inorganic nutrients • Decomposition is a biological process that includes the physical breakdown and biochemical transformation of complex organic molecules of dead material into simpler organic and inorganic molecules (Juma, 1998).

14. SOURCE OF ORGANIC MATTER • Plant remains • Animal tissues and excretory products • Cells of microorganisms • However, plant is the main contributor to OM

15. ORGANIC CONSTITUENTS OF PLANTS • Cellulose, most abundant 15 to 60% of dry weight • Hemicelluloses, 10 to 30% • Lignin, 5 to 30% • Water soluble fraction include simple sugar, amino acids, and aliphatic acids, 5 to 30% of tisue weight • Ether and alcohol-soluble constituents; fats, oils, waxes, resins and a number of pigments • Proteins

17. WHY MICROORGANISMS DECOMPOSE OM • Supplying energy for growth • Supplying carbon for new cell synthesis • The cells of most microorganisms commonly contain approximately 50% carbon. This is derived mainly from the substrates.

18. WHY DO WE CARE ABOUT DECOMPOSITION? Decomposition is important in releasing nutrients tied up in dead organic matter and return it back to the soil.

19. WHO ARE THE DECOMPOSERS? A. Soil fauna (e.g., earthworms, arthropods): physical • fragmentation (cominution) increases surface area, • distributes OM within soil profile, doesn’t alter litter chemistry B. Soil microorganisms: heterotrophic bacteria and fungi • derive energy, carbon, and nutrients from dead OM; in the process they release CO2 through respiration; RESPONSIBLE FOR BULK OF DECOMPOSITION!!

21. DECOMPOSITION PROCESSES There are three main processes 1. Assimilation = conversion of substrate materials into protoplasmic materials. Eg. OM carbon to microbial carbon. Protein to microbial protein. 2. Mineralization = conversion of organic substance to inorganic form. Eg. Protein from the OM will be converted to inorganic nitrogen (NH4, NO3) in the soil. 3. Immobilization = conversion of inorganic form into organic form. Eg. Inorganic nitrogen from the soil converted into microbial protein.

23. FACTORS AFFECTING RATE OF DECOMPOSITION 1. Temperature • Microbial activity responds exponentially to increased temperature until enzymes denature, etc. 2. Moisture • Microbial activity has optimum moisture • Low moisture = desiccation, slow diffusion • High moisture = low O2 availability; no lignin degradation 3. pH • Most microbes exhibit optimum activity near pH 7. • Fungi most active in acid soil and bacteria in moderate soil pH.

24. Substrate Quality: Carbon • Different carbon compounds are decomposed at different rates. • Cellulose faster • Lignin slower decomposition as compared to cellulose. • C:Nof the OM determine the rate: • high slower, this is due to insufficient of N for microorganisms to assimilate carbon; • low faster, nitrogen is sufficient for rapid assimilation of carbon.

25. WHAT IS THE C:N RATIO? • The carbon-to-nitrogen (C:N) ratio is often used as an indication of whether mineralization or immobilization will occur. • The C:N ratio is the total concentration of C divided by the total concentration of N.

26. C:N RATION RANGE • Because there is a suite of microorganism and OM quality, generally we can predict whether mineralization or immobilization will take place base on the C:N ration range • When surface of soil layer have a: • C:N > 30:1 => immobilization highly likely to occur • C:N < 20:1 => mineralization is likely to occur • C:N between 20-30:1 => both processes may occur but will generally in balance

27. C:N OF SOME ORGANIC MATTER

28. The C:N ratio is the most commonly used in soils because N is the most limiting element. • A microbe with a C:N ratio of 8:1 would require OM with a C:N ratio of 24:1. • The C:N ratio in lower in microorganisms and = 8. • Since microbes incorporate only about 1/3 of the C metabolized into biomass, the substrate material must have C:N ratio = 24 to satisfy the N requirement of microbes. • If the C:N ratio > 24, available soil N is consumed by microbes and plant available N decrease.