Microbiology Procedure
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Geochemical Agents

Geochemical Agents

During the middle of the 19th century, interest was mostly on the role of microorganisms in fermentation and disease. Pasteur's contributions on fermentation clearly showed that microorganisms can serve as specific agents in chemical transformations.

The credit for establishing the role of microorganisms in transformation of nitrogen and sulphur goes to Winogradsky and Beijerinck. Winogradsky (1856-1953) found that there are several distinct groups of bacteria each characterized by their ability to use a particular inorganic energy source. For example, sulphur bacteria oxidize inorganic sulphur and sulphur compounds while nitrifying bacteria oxidize reduced inorganic nitrogen compounds.

Winogradsky also showed that some bacteria, either in. association with higher plants or free living, can use gaseous nitrogen for the synthesis of cell components. Hellriegel and Wilfarth (1888) showed that a mutual beneficial symbiosis exists between bacteria (rhizobia) and leguminous plants. Beijerinck (1901) found the free living nitrogen fixing bacteria Azotobacter and described their usefulness in soil fertility.

 

 

 

 

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