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Clay minerals and quartz are the chief constituents of most sedimentary rocks in this category. To answer why, clay minerals are the most abundant product of the chemical weathering of silicate minerals, especially the feldspars. Clays are fine-grained minerals with sheetlike crystalline structures similar to the micas. Quartz is abundant because it is extremely durable and very resistant to chemical weathering. Thus, when igneous rocks such as granite are attacked by weathering processes, individual quartz grains are freed.
A horizon is often darker than B horizon or C horizon because it is the topsoil and the topsoil might be covered with litter. The litter decompose and as you know become soil and it will be fresh soil. So the fresh soil is darker than B and C horizon
This mineral is called glauconite, an iron potassium silicate with very low weathering resistance.
Clay is a fine-grained detrital rock that breaks into chucks or blocks. It is the most abundant product of chemical weathering of silicate minerals.
Feldspar breaks down giving us Al, Si and O in solution. You also get clay minerals left behind.
China clay is a type of clay that is rich in kaolinite, which is a layered silicate mineral. Silicate minerals are a type of rock-forming mineral.
O-horizon (surface litter)=mainly partially decaying organic matter A-horizon (Topsoil)= mainly contains organic matter, living organisms, inorganic minerals. E-horizon (Eluviated zone)= low quantities of minerals,clay and organic matter due to leeching. B-horizon (Subsoil)= accumulation of iron, aluminium and clay leached down from the A and E horizons. C-horizon (Regolith)= partially broken down inorganic minerals Bedrock
it is the primary clay minerals
Clay minerals are the product of chemical weathering of silicate minerals, such as feldspars. Clays are silicate minerals.
An allophane is an amorphous hydrous aluminium silicate clay mineral.
An albeluvisol is a form of soil with a thin, dark surface horizon on a bleached subsurface horizon which tongues into a clay illuviation horizon.
The most common metalloid elements (those behaving between the metals and non-metals) are: B, Si, Ge, Te, As, & Sb. Of these common ones only Si (silicon) occurs in sand, quartz (Silicon dioxide), granite (feldspar + quartz + mica), feldspar (alumino silicate), and clay (oxidized alumino silicate.) So the answer is Silicon.
The C horizon contains mainly parent material, while the B horizon contains mainly clay particles and the A horizon; mainly silt sized particles and humus
Graphite and clay binder - no actual 'lead'. Graphite is an allotrope of carbon C Clay is aluminum silicate Al2(SiO3)3
The A horizon is the top layer and is made out of sand, clay silt, and humus. It is where most plants grow. =-) Hope that helped.
It is a fine-grained unstratified accumulation of clay and silt deposited by the wind
two types?I only know the 6 main types of clays used in ceramics which are: China clay (kaolin - silicate clay), Ball Clay,Fireclays, Earthenware clays, Stoneware clays,Porcelain clays..