Decomposition and composting
 
       Decomposition
 
       Decomposition is the process by which structures and molecules  
         contained in organic matter are broken down into smaller, simpler compounds.  
         Mineralisation describes the complete decomposition of compounds into  
         their component elements. Decomposition is mediated by the activities  
         of decomposer organisms (principally bacteria and fungi) and is regulated  
         by the chemical composition of the material being decomposed and environmental  
         conditions such as temperature, moisture and nutrient availability.
 
       
 
       Figure 1. Decomposition of alder leaves and  
         birch leaves under natural conditions. Alder leaves break down more quickly  
         than birch leaves, perhaps because they contain more nitrogen; a nutrient  
         essential for microorganisms.
 
        
       Composting
 
       During the first few weeks of composting, large numbers of  
         microorganisms consume low and medium molecular weight ‘labile’  
         compounds, such as sugars and amino acids, contained in the organic matter  
         being composted. During this feeding frenzy so much energy is released  
         by their break-down that the temperature of the compost increases to 55  
         degrees centigrade or above (Figure 2).  
         It is this temperature increase that distinguishes composting from natural  
         decomposition of organic matter. 
 
       
 
       
 
       Figure 2. Temperature change when the biodegradable  
         fraction of household rubbish is composted together with green waste collected  
         from municipal parks and gardens. The high temperatures kill harmful microorganisms  
         such as E. coli that may be found in rubbish, but it is not enough  
         to kill the thermophillic  
         microorganisms doing the composting.
 
       
 
         When the supply of labile compounds is diminished, the temperature of  
         the compost decreases and other groups of microorganisms, including basidiomycete  
         fungi (such as white rot fungi) begin to slowly break down high molecular  
         weight compounds, such as lignin and celluloses. The texture, colour and  
         biochemical characteristics of the finished compost are determined largely  
         by these complex compounds, which will themselves decompose, but over  
         a much longer timescale. 
 
       Many detailed explanations of decomposition and composting  
         are available (see links). Cornell  
         University’s composting site provides particularly good background  
         information on the process of decomposition and the factors that regulate  
         it. 
 
       http://compost.css.cornell.edu/Composting_homepage.html