When it is under anaerobic conditions.
They must be buried in the sediment pile and start to decompose aerobically as the pile thickens, they become heated and the decomposition products polymerize to form oils. If the carbon content is high and the organic matter in thick concentrations, solid carbon is also left as a residue (coal).
Bacteria in the soil can cycle essential plant nutrients by decomposing organic matter and releasing nutrients like nitrogen, phosphorus, and sulfur back into the soil in a form that plants can absorb. Some bacteria also form symbiotic relationships with plants, such as nitrogen-fixing bacteria that convert atmospheric nitrogen into a form usable by plants. These processes help maintain the nutrient balance in the soil and promote plant growth.
Cork cambium is the layer of tissue that produces cork cells, which accumulate to form the protective cork layer. This cork layer functions to protect the stem or trunk of a plant from physical damage, pathogens, and water loss. Cork is a natural insulator and has properties that make it resistant to fire and decay, providing additional protection to the plant.
Bacteria in soil play important roles in decomposition, nutrient cycling, and promoting plant growth. They break down organic matter, releasing nutrients that plants can use. Additionally, some bacteria form symbiotic relationships with plant roots to aid in nutrient uptake.
Nitrogen is supplied to the leguminous plant in the nodules found on its roots. This nitrogen-fixing process is carried out by bacteria that form a symbiotic relationship with the plant, converting nitrogen from the air into a form that the plant can use for growth.
Peat is the first form of true coal in the process of coal formation. It is a soft, organic material that forms in waterlogged environments through the partial decay of plant matter. Peat is the precursor to lignite, the lowest rank of true coal.
No. A meteor is an object from space that is falling through the atmosphere. A meteorite is a rock from space that has hit the ground. Coal is neither. It forms underground form dead plant matter.
Plant material :)
No, coal is a non-renewable resource. It takes millions of years for coal to form from dead plant matter, so it cannot be replenished within a human lifespan. Once it is extracted and burned, it is gone.
Yes, coal is a nonrenewable resource because it takes millions of years to form through the decomposition of plant matter. Once coal is extracted and burned for energy, it cannot be easily replenished within a human lifespan.
Bituminous coal is largely the product of ancient plant remains, although some animals would have contributed to a very small percentage of its mass.
Coal is formed from plant material that is subjected to high pressure and heat over millions of years. This process typically involves the burial of plant matter in sedimentary rocks and the removal of oxygen through decomposition, resulting in the formation of coal.
Coal forms from the accumulation of plant material in swamps and marshes, while petroleum and natural gas form from the remains of marine organisms like algae and zooplankton. The main difference lies in the type of organic material and the environment in which it accumulates, resulting in the formation of different fossil fuels.
Coal is derived from plant material which was produced by solar energy during photosynthesis. Photosynthesis is roughly H20 + CO2 + solar energy = Ch20 + O2, which converts CO2 and water to oxygen and plant material as the plant grows.
Coal forms from the accumulation and burial of plant material in oxygen-poor environments, such as swamps and bogs. The lack of oxygen prevents decay and allows the organic matter to undergo transformation into coal through heat and pressure over millions of years.
Coal beds form from the accumulation of plant material in swamps and wetlands over millions of years. The plant material is buried and subjected to heat and pressure, transforming it into coal. This process typically occurs in areas with high plant productivity and slow decomposition rates.
no not all of them for example like Bituminous coal or coal, is form by plant remains