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Ammonification Video Lecture - NEET

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1. What is ammonification?
Ans. Ammonification is the process by which organic nitrogen compounds, such as proteins and urea, are converted into ammonia (NH3) by the action of decomposer organisms, primarily bacteria and fungi. This process occurs during the decomposition of dead plants and animals, as well as the breakdown of waste materials.
2. How does ammonification contribute to the nitrogen cycle?
Ans. Ammonification plays a crucial role in the nitrogen cycle as it converts organic nitrogen compounds into ammonia, which can further undergo nitrification or assimilation by plants. This conversion releases ammonium ions (NH4+) into the soil, making nitrogen available for plants to uptake and incorporate into their tissues.
3. Which organisms are responsible for ammonification?
Ans. Ammonification is primarily carried out by decomposer organisms, including bacteria and fungi. These microorganisms break down organic matter, such as dead plants and animals, and release ammonia as a byproduct. Some common examples of ammonifying bacteria include Proteus, Bacillus, and Clostridium.
4. What are the environmental factors influencing ammonification?
Ans. Several environmental factors can influence the rate of ammonification. Temperature, moisture content, and pH of the soil are important factors that affect the activity of ammonifying organisms. Generally, higher temperatures and moisture levels promote faster ammonification, while extreme pH conditions can inhibit the process.
5. How does excessive ammonification impact the environment?
Ans. Excessive ammonification can lead to an accumulation of ammonia in the soil and surrounding ecosystems. High levels of ammonia can be toxic to plants and aquatic organisms, causing nutrient imbalances and impairing their growth and survival. Additionally, excess ammonia can contribute to air and water pollution, leading to eutrophication and other environmental problems.
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