Carbonization
The renewable energy resource derived from burning organic material such as wood and garbage is called biomass energy. Biomass involves the conversion of organic materials into energy through combustion or other processes, releasing stored energy in the form of heat. This energy can be used for heating, electricity generation, and biofuels. Biomass is considered renewable because it can be replenished through sustainable practices.
It is dissolved salts, gases, and nutrients that are presented in seawater.
imprinted in stone
Organic chemistry (and of course biochemistry) is the branch involving carbon based molecules.
Any thing that is organic and dies
Coal formation is largely a result of the accumulation and compression of organic matter from plants in swampy environments over millions of years. The process involves the burial and transformation of this organic material due to pressure and heat, resulting in the formation of coal.
It is called fossilization or petrification. This process involves minerals replacing the organic material of an organism, resulting in the preservation of its structure in rock.
Silicification is the process by which organic material is converted into stone by impregnation with silica. It is a rare form of fossilization.
If an organic material is converted into stone, it becomes a fossil. The process by which this occurs is called fossilization. Fossils provide valuable information about past life forms and environments.
Coal is primarily produced from the diagenesis of plant material, such as trees and vegetation, that has been buried and subjected to heat and pressure over millions of years. The process involves the gradual transformation of organic material into coal as a result of compaction and biochemical changes.
No, mineral fossilization typically requires water to transport minerals to the remains of the organism and facilitate the crystallization process. Water helps in the replacement of organic material with minerals, forming a fossil.
Mineral fossilization most commonly occurs in the presence of water. Water plays a critical role in transporting mineral ions to replace organic material in the fossilization process. However, in some cases, fossilization can occur in arid or dry environments through other processes like desiccation or replacement by volcanic minerals.
The most common method of fossilization is permineralization. This occurs when minerals in groundwater fill in the empty spaces of organic material, creating a fossilized replica of the original organism. Over time, the minerals in the groundwater harden and preserve the organism's structure.
The process of a dinosaur bone turning into rock over millions of years is a chemical change. This transformation involves the replacement of organic materials in the bone with minerals through a process called fossilization, altering the composition of the original bone.
Fossilization requires quick burial of the organism in sediment or another substance that prevents decomposition. The presence of minerals that can replace the organic material of the organism is also crucial, along with protection from physical and chemical weathering processes. The right environmental conditions, such as low oxygen levels, are also important for fossilization to occur.
Yes, the process of fossilization where the original material is dissolved and replaced by new minerals is called replacement. It occurs when groundwater carrying minerals seeps through the remains of an organism and deposits new mineral materials in place of the original organic material, producing a fossil with the same shape as the original organism.
Oil is formed from organic matter like plankton and algae that is buried and exposed to heat and pressure over millions of years. This organic matter originally obtained its energy from the sun through photosynthesis. The transformation process involves the decomposition of the organic material into compounds that eventually become oil.