The cation exchange capacity (CEC) shows how well a soil can hold onto and store cations, so a soil with a high CEC would be able to hold more nutrients. A soil with low CEC for example would not only be missing some important nutrients but would also not be able to hold onto nutrients as well as a soil with a higher CEC. So even adding nutrients to a soil with a low CEC would not be very effective in improving fertility unless soil conditioning was applied that would help improve the CEC as well. Soils with a lot of cations can also hold onto water better since water is a polar molecule and is therefore attracted to the positively charged cations (hydrogen bonding).
Plants that grow in soils with a high CEC value do not have to spend as much energy looking for minerals and water and therefore are able to devote it towards growth. Microorganisms that are essential for good soil health also thrive in these conditions.
However, a soil with a high CEC can also hold more of the acidic hydrogen cations (H+). So when the soil pH of a soil with a high CEC needs to be adjusted it often acts as a buffer and therefore more acid or base is need to change the pH.
mineralogy, soil organic matter, soil texture, type of clay, cation exchange capacity, base saturation
Soil colloids have large surface areas which can be used as sights for cation exchange, increasing the soils cation exchange capacity. The higher the cation exchange capacity in a soil, the more the soil is able to retain nutrients because the cations are suspended in the soil and are then able to be used by organisms in the soil.
A cation exchange capacity of the acid soil refers to the measure of the soil's capacity to hold and release positively charged ions that form acidic substances. It is based on a given pH level.
Well really depends on your anabatic lapse rates because that is directly relevant to the erosion of topsoil and the density of which is eroded at, also if the Cation exchange capacity is greater than the pH of the soil the effect of aeolian processes is greatly maximised. Hope this helps :)
cation
mineralogy, soil organic matter, soil texture, type of clay, cation exchange capacity, base saturation
Soil colloids have large surface areas which can be used as sights for cation exchange, increasing the soils cation exchange capacity. The higher the cation exchange capacity in a soil, the more the soil is able to retain nutrients because the cations are suspended in the soil and are then able to be used by organisms in the soil.
Soil colloids have large surface areas which can be used as sights for cation exchange, increasing the soils cation exchange capacity. The higher the cation exchange capacity in a soil, the more the soil is able to retain nutrients because the cations are suspended in the soil and are then able to be used by organisms in the soil.
Cation exchamnge capacity is directly related to the clay fraction within the soil. For lateritic soil, the surface of clay fracion is coated with the gels of sesquioxides which inturn reduces the surface activity of clay particles...
W. A. Beetem has written: 'Use of cesium-137 in the determination of cation exchange capacity' -- subject(s): Analysis, Soils, Cations, Clay, Cesium, Ion exchange
Appreciate that cation exchange is of importance in the natural environment.
A cation exchange capacity of the acid soil refers to the measure of the soil's capacity to hold and release positively charged ions that form acidic substances. It is based on a given pH level.
Cation-exchange resin has a variety of uses in automotive manufacturing and construction; it contains negatively charged radicals that attracts and isolates cations. It is also called a cation deionization resin or water softening resin.
It is used as an alternative to cation exchange membrane.
"Dowex 50" is a type of ion-exchange resin, called a strongly acidic cation exchanger, used for ion-exchange chromatography. It is useful for swapping a metal cation for a proton (eg. Na+ for H+) or one metal cation for another (eg. K+ for Na+). This can be an important way for purifying amino acids, carboxylate salts or removing unwanted metal ions from water solutions.
= cation =An ion or group of ions having a positive charge and characteristically moving toward the negative electrode in electrolysis.An atom, or group of atoms with a positive charge. Cation exchange is the process whereby a cation in solution is absorbed by a solid, replacing a different cation. Thus, in soil science, if a potassium salt is dissolved in water and applied to a soil, potassium cations are absorbed by soil particles, and sodium and calcium cations are released.
Well really depends on your anabatic lapse rates because that is directly relevant to the erosion of topsoil and the density of which is eroded at, also if the Cation exchange capacity is greater than the pH of the soil the effect of aeolian processes is greatly maximised. Hope this helps