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Soil organic matter and Humic substances
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- 2. SOIL ORGANIC MATTER Substancescontaining carbon are organic matter. Soil organic matter consists of decomposing plant and animal residues. It also includes substances of organic origin either leaving or dead. 11/29/2018 2Sethupathi SIva, M.Sc., In SS & AC
- 3. Importance of SOM Soilorganic matter plays an important role in deciding / maintaining soil physical conditions. It also influences soil chemical properties especially cation exchange capacity. Organic matter supply the energy sources for soil micro organisms. Soil development is another aspect which is influenced by the soil organic matter. 11/29/2018 3Sethupathi SIva, M.Sc., In SS & AC
- 4. SOURCES of SOM Planttissue is the major source. Animals are considered as the secondary sources. They attack original plant tissues, contribute waste products and leave their own bodies after death. 11/29/2018 4Sethupathi SIva, M.Sc., In SS & AC
- 5. Factors affecting soilorganic matter 1. Climate 2. Natural vegetation 3. Texture 4. Drainage 5. Cropping and Tillage 6. Crop rotations, residues and plant nutrients. 11/29/2018 5Sethupathi SIva, M.Sc., In SS & AC
- 6. Composition of organicresidues Plant residues contain 75% moisture and 25% dry matter. This 25% is made up of Carbon (10-12%), Oxygen (9- 10%) , Hydrogen (1.5-2.5%) , N(1-2%) and mineral matter (1-3%). 11/29/2018 6Sethupathi SIva, M.Sc., In SS & AC
- 7. Decomposition Of SoilOrganic Matter 1. Rapidly decomposed : Sugars, starches, proteins etc. 2. Less rapidly decomposed : Hemicelluloses, celluloses etc. 3. Very slowly decomposed: Fats, waxes, resins, lignins etc The general reactions taking place during decomposition are 1. Enzymatic oxidation of the bulk with the release of CO2 , water, energy and heat 2. Essential elements are released (N, P, S etc) and immobilized by a series of reactions. 3. Formation of compounds which are resistant to microbial action. 11/29/2018 7Sethupathi SIva, M.Sc., In SS & AC
- 8. Under aerobic conditionsthe products formed are CO2, NH4, NO3 , H2PO4, SO4, H2O and essential plant nutrients like Ca, Mg, Fe, Cu, Zn etc. Under anaerobic conditions CH4, organic acids like lactic, propionic, butyric, NH4, various amine residues (R-NH2) H2S, ethylene (CH2=CH2) and humic substances. 11/29/2018 8Sethupathi SIva, M.Sc., In SS & AC
- 9. Aerobic Conditions Decomposition ofsoluble substances: When glucose is decomposed under aerobic conditions the reaction is as under: Sugar + Oxygen ----- CO2 + H2O Under partially oxidized conditions, Sugar + Oxygen ----- Aliphatic acids (Acetic, formic etc.) or Hydroxy acids (Citric, lactic etc.) or Alcohols (ethyl alcohol etc.) Some of the reactions involved may be represented as under 11/29/2018 9Sethupathi SIva, M.Sc., In SS & AC
- 10. Ammonification : Organic nitrogenouscompounds (amino acids, amides, ammonium compounds, nitrates etc.) .....Is called ammonification. Hydrolytic and oxidative enzymatic reaction under aerobic conditions by heterotrophic microbes. Nitrification: It is an aerobic process by autotrophic bacteria. Ammonia Ammonia Nitrites (NO2) Denitrification: Nitrates (NO3) Gaseous Nitrogen 11/29/2018 10Sethupathi SIva, M.Sc., In SS & AC
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- 13. Anaerobic Conditions Decomposition ofInsoluble Substances Breakdown of Protein: Aminization : The process of conversion of proteins to amino-acids. Ammonification: The process of conversion of amino-acids and amides to ammonia. Breakdown of cellulose: Breakdown of Hemicellulose Breakdown of Starch 11/29/2018 13Sethupathi SIva, M.Sc., In SS & AC
- 14. Decomposition of ethersoluble substances Fats glycerol + fatty acids Glycerol CO2 + water Decomposition of lignin: Lignin decomposes slowly, much slower than cellulose. Complete oxidation gives rise to CO2 and H2O. 11/29/2018 14Sethupathi SIva, M.Sc., In SS & AC
- 15. Factors Affecting Decomposition Temperature Soilmoisture Nutrients Soil pH Soil Texture Other Factors: Toxic levels of elements (Al, Mn, B, Se, Cl), excessive soluble salts, shade and organic phytotoxins in plant materials. 11/29/2018 15Sethupathi SIva, M.Sc., In SS & AC
- 16. Granular condition ofsoil Aeration and permeability Water holding capacity Good infiltration Run off and erosion control Surface mulching with coarse organic matter Soil temperature maintenance Role of organic matter 11/29/2018 16Sethupathi SIva, M.Sc., In SS & AC
- 17. Condn……. Source of energyfor the microbes and as A reservoir of nutrients Food for earthworms, ants and rodents and makes soil P readily available in acid soils. Reduce alkalinity in soils Humus (A highly decomposed organic matter) provides A storehouse for the exchangeable and available cations. It acts as A buffering agent 11/29/2018Sethupathi SIva, M.Sc., In SS & AC 17
- 18. Humic Substances -Fractions, properties,formation of humic substances 11/29/2018 18Sethupathi SIva, M.Sc., In SS & AC
- 19. Soil Organic matter HumusNon-Humus Fulvic Acid Humic Acid Humin Humic acid: medium molecular weight and colour soluble in alkali but not in acid. It is intermediate in resistance to degradation Fulvic acid: Lowest in molecular weight, light in colour. Soluble both in alkali and acid. Highly susceptible for microbial attack. Humin : o Insoluble in both alkali and acid. o Highest molecular weight, darkest in colour. o Most resistant to microbial attack proteins, carbohydrates, lignin’s, fats, waxes, resins, tannins 11/29/2018 19Sethupathi SIva, M.Sc., In SS & AC
- 20. Humus Formation Decomposition: a) Decompositionof original organic residues and converting them into simpler compounds. Synthesis Synthesis of organic compounds of higher molecular weight humic substances. 11/29/2018 20Sethupathi SIva, M.Sc., In SS & AC
- 21. Theories on humusformation There are several theories regarding the formation of soil humus. Lignin theory: Proposed by Waksman (1936). • According to this theory humic substances are formed due to the incomplete degradation of lignin. Kononovas theory: According to this theory humic substances are formed by cellulose decomposing mycobacteria earlier to lignin decomposition. concepts on humus formation link…….11/29/2018 21Sethupathi SIva, M.Sc., In SS & AC
- 22. Polyphenol theory:This theorywas proposed by Flaig and Sochtig (1964). • As per this theory the humic substances are formed by the condensation of phenolic materials. Polyphenols of lignin ------ quinones------- humic molecules 11/29/2018 22Sethupathi SIva, M.Sc., In SS & AC
- 23. Properties of Humus Thetiny colloidal particles are composed of C, H, and O. The colloidal particles are negatively charged (-oh, -cooh or phenolic groups) Very high surface area, Higher CEC (150 – 300 cmol(p+)/kg), 4 - 5 times higher water holding capacity than that of silicate clays. Humus has a very favorable effect on aggregate formation and stability. Impart black colour to soils. 11/29/2018 23Sethupathi SIva, M.Sc., In SS & AC
- 24. Clay – HumusComplex • Humus, the organic amorphous colloid supplies both basic and acidic ions which is transitory and ultimately disappears from soil. • Clay, the inorganic crystalline colloid supplies chiefly the basic nutrient ions is more or less stable. • Both these colloids form the soil colloidal complex and are extremely active and form important sources of plant nutrients. 11/29/2018 24Sethupathi SIva, M.Sc., In SS & AC
- 25. Maintenance of Humus •Addition of organic materials is essential • To maintain adequate level of organic matter in the soil the N level should be maintained by inclusion of legumes in crop rotation • Judicious application of N fertilizers. • Loss of n from the soil is also to be minimized. • Conservation tillage (minimum tillage) • Keeping the land fallow to encourage natural vegetation is also advisable. 11/29/2018 25Sethupathi SIva, M.Sc., In SS & AC