TEMPERATURE
MOISTURE
AIR
soil organic matter
Banana decomposition happens when enzymes break down the banana's organic matter, causing it to rot. Factors like temperature, humidity, and presence of microorganisms can influence the speed of decomposition.
Pyrolysis
Decomposition (or rotting) is the process by which organic substances are broken down into simpler forms of matter.
Organic matter is converted into animal and microbial tissue during decomposition. This matter can be then used to fertilize the soil.
Good air flow is necessary for the decomposition of organic matter because decaying matter builds up gases. If the gases are not allowed to escape the area, there could be an explosion.
bacteria and fungi
bacteria or fungi
Soil pH can affect organic matter decomposition by influencing the activity of microorganisms involved in the decomposition process. Most microorganisms responsible for breaking down organic matter thrive in slightly acidic to neutral pH conditions. Extreme pH levels can inhibit microbial activity and slow down decomposition rates. Additionally, pH levels can also impact the availability of essential nutrients for microorganisms, further influencing decomposition.
Organic matter can increase the volume of soil as it decomposes, releasing gases that can cause soil expansion. However, the weight of the soil can decrease with the addition of organic matter, as it is lighter than mineral components like sand, silt, and clay. Overall, the impact of organic matter on soil volume and weight will depend on factors such as decomposition rate, soil texture, and environmental conditions.
Organic matter is formed through the decomposition of living organisms, such as plants, animals, and microbes. When these organisms die, their remains break down and undergo a process called decomposition, where organic compounds are broken down into simpler molecules by fungi, bacteria, and other decomposers. This process eventually results in the formation of organic matter in the soil.
During decomposition, microorganisms break down organic matter, releasing carbon dioxide as a byproduct. This process occurs as the microorganisms feed on the organic material and respire, converting the carbon from the organic matter into carbon dioxide that is released into the atmosphere.