Biochar is a product with high content of aromatic carbon. It is produced when biomass is pyrolyzed at hypoxic or anoxic conditions and relatively low temperatures. On biochar's surface functional groups with oxygen are deprotonated and are therefore carrier of negative charge. The amount of said charge directly affects cation exchange capacity (CEC), which is used to express the ability of biochar to accept or retain cations. CEC values are very much affected by pyrolysis temperature and type of used biomass. With increasing pyrolysis temperature, the removal of functional groups with oxygen occurs, leading to a decrease in CEC. The effect of biomass can be observed in the experimental part of my diploma thesis, as the analysed biochar samples produced from different types of biomass had very different CEC.
Biochar types with high CEC values have positive impact on soil quality. In soils, containing biochar, better nutrient retention, air and water availability, higher CEC and better adsorption of heavy metals was observed. Biochar in soil is also able to enhance CO2 sequestration and growth of some microorganisms.
There are many different methods for determination of CEC in organic compounds. In diploma thesis I determined CEC of biochar with two methods: with ammonium acetate (at pH 7) and by summation of base cations (Na+, K+, Ca2+, Mg2+). Firstly, I adjusted the pH value of samples to about 7 and then saturated them with NH4+ ions. This caused the exchange of base cations, which I determined in leached solution by atomic spectroscopic methods (AAS, AES). In the last step I exchanged NH4+ ions absorbed on biochar with K+ ions and determined them with spectrophotometer. I then compared the results obtained with these two methods and found that the sum of base cations is substantially larger than the amount of negative charge on biochar determined with NH4OAc. When comparing CEC values of biochar, we must therefore consider the method used.
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