Yes
Peat moss and vermiculite are used extensively in all-purpose potting soil and many specialized growing mediums. They both contribute to the size of pore spaces in a growing medium, increasing the amount of air around the roots of a plant. Common Uses. Vermiculite and peat moss are often used in conjunction to increase the water-and air-holding capacity of a growing medium. A ratio of 1 part peat moss to 2 parts vermiculite is a common formulation, plus the addition of other ingredients, depending on the purpose of the medium. Vermiculite and peat moss are often used in conjunction to increase the water-and air-holding capacity of a growing medium. Common Uses. Vermiculite and peat moss are often used in conjunction to increase the water-and air-holding capacity of a growing medium. A ratio of 1 part peat moss to 2 parts vermiculite is a common formulation, plus the addition of other ingredients, depending on the purpose of the medium. In a peat profile there is a fossilized record of changes over time in the vegetation, pollen, spores, animals (from microscopic to the giant elk), and archaeological remains that have been deposited in place, as well as pollen, spores and particles brought in by wind and weather. Other words for lands dominated by peat include moors or muskegs. Landscapes covered in peat also have specific kinds of plants, particularly Sphagnum moss, ericaceous shrubs, and sedges (see bog for more information on this aspect of peat). Vermiculite and perlite are common soilless growing mediums that are often added to soils, used as a sprouting medium, or used in hydroponics. Vermiculite is a mineral compound made of mica-like shiny flakes that can sometimes be contaminated with asbestos. Perlite is made from hydrated volcanic ore. Peat moss is cut out of bogs. The lower, dead mosses are separated out, dried, and packaged as peat moss. Although in the past, peat moss was considered a renewable resource, the rate of harvest is currently greater than the production rate of peat bogs. Subscribe. Peat is a renewable, natural, organic material of botanical origin and commercial significance. Peatlands are situated predominately in shallow wetland areas of the Northern Hemisphere, where large deposits developed from the gradual decomposition of plant matter under anaerobic (low oxygen) conditions. In industry, peat is used primarily as a filtration medium to remove toxic materials from process waste streams, pathogens from sewage effluents, and deleterious materials suspended in municipal storm-drain water. In its dehydrated form, peat is a highly effective absorbent for fuel and oil spills on land and water. Background: Peat is the partially decomposed remains of plant material, especially sphagnum moss. It is found in a wetlands environment where the addition of new plant material is faster than the decomposition of the accumulated plant material. As coal formation progresses, volatile materials like water are driven off, and the percentage of carbon content of the material increases, making it increasingly dense and hard. The majority of the peat harvested is called reed-sedge peat. The other harvested forms are sphagnum moss, humus and hypnum moss. Vermiculite. Vermiculite is produced by heating mica, a common soil mineral, to 1,800 degrees Fahrenheit, causing it to puff up to many times its original size. Similar to peat moss, it helps the medium hold large quantities of air, water and nutrients relative to its small size. Common Uses. Vermiculite and peat moss are often used in conjunction to increase the water-and air-holding capacity of a growing medium. A ratio of 1 part peat moss to 2 parts vermiculite is a common formulation, plus the addition of other ingredients, depending on the purpose of the medium. Depending on the agency, peat is not generally regarded as a renewable source of energy, as its extraction rate in industrialized countries far exceeds its slow regrowth rate of 1 mm per year, and as peat regrowth is also reported to take place in only 30-40% of peatlands. Other words for lands dominated by peat include moors or muskegs. Landscapes covered in peat also have specific kinds of plants, particularly Sphagnum moss, ericaceous shrubs, and sedges (see bog for more information on this aspect of peat). Of the peat that is imported into the United States, most comes from Canada. Other significant producers of peat are Belarus, Estonia, Finland, Germany, Sweden, Lithuania and Russia. It is estimated that world resources of peat are 2 trillion tons. As coal formation progresses, volatile materials like water are driven off, and the percentage of carbon content of the material increases, making it increasingly dense and hard. The majority of the peat harvested is called reed-sedge peat. The other harvested forms are sphagnum moss, humus and hypnum moss. Peat is the first material formed in the process that transforms plant matter into coal. As coal formation progresses, volatile materials like water are driven off, and the percentage of carbon content of the material increases, making it increasingly dense and hard. The majority of the peat harvested is called reed-sedge peat. The other harvested forms are sphagnum moss, humus and hypnum moss.
http://homeguides.sfgate.com/peat-moss-vs-vermiculite-86183.html http://homeguides.sfgate.com/peat-moss-vs-vermiculite-86183.html https://en.wikipedia.org/wiki/Peat http://www.gardenguides.com/138085-alternatives-vermiculite-perlite.html http://minerals.usgs.gov/minerals/pubs/commodity/peat/ http://www.mineralseducationcoalition.org/minerals/peat http://homeguides.sfgate.com/peat-moss-vs-vermiculite-86183.html https://en.wikipedia.org/wiki/Peat http://www.mineralseducationcoalition.org/minerals/peat http://www.mineralseducationcoalition.org/minerals/peat
is peat moss considered a mineral