Mobs
Introduction
Peat is an organic material, dark brown in color and rich in carbon.[1][2] It is formed by a spongy and light mass in which the plant components that originated it can still be seen. It is used as fuel and to obtain organic fertilizers.
Peat is a mineral product. In gardening, peat is often confused with compost, which is fertilizing organic matter. Both are very different since peat is missing certain nutrients, such as nitrogen, phosphorus and potassium. The sale of peat or products mixed with peat is because it is usually more profitable to import peat than for companies that trade in substrates to buy and produce the compost. Some scientists and gardening experts have proposed that peat products be banned because it would be a misleading product and also very harmful to the ecosystem, since its extraction requires "the destruction of valuable peat bog ecosystems to grow ornamental flowers" and that "constitutes an absurd and unnecessary environmental plunder."[3].
Peat is not a renewable energy source, because its extraction rate in industrialized countries far exceeds its slow growth rate of 1 mm per year,[4] and also because new peat growth takes place in only 30-40% of peatlands.[5] Centuries of burning and draining peat by humans have released a significant amount of CO into the atmosphere,[6] and much restoration of peatlands is needed. to help limit climate change.[7].
peat formation
The formation of peat constitutes the first stage of the process by which vegetation is transformed into mineral coal. It is formed as a result of the rotting and partial carbonification of vegetation in the acidic water of swamps, marshes and wetlands. The formation of a peat bog is generally slow as a consequence of low microbial activity, due to the acidity of the water or the low concentration of oxygen. The passing of the years produces an accumulation of peat that can reach several meters thick, at a growth rate that is estimated to be between 10 and 50 centimeters every hundred years.
Peatlands are lacustrine swamps of glacial origin that are currently full of more or less decomposed plant material and which we know as freshwater peat. Peat accumulates because the rotting of plant matter is very slow in cold climates. The plant matter that accumulates below the water level of a lake is in conditions of continuous saturation and low availability of oxygen, thus promoting the activity of the transformers. In these formations we have a histosol type soil.