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Cation-exchange capacity (CEC) is a measure of how many cations can be retained on soil particle surfaces. [1] Negative charges on the surfaces of soil particles bind positively-charged atoms or molecules (cations), but allow these to exchange with other positively charged particles in the surrounding soil water. [ 2 ]
Download as PDF; Printable version ... For example, base saturation refers to the fraction of exchangeable cations that are base cations. ... Text is available under ...
LX Lixisol (low-activity clays, exchangeable base cations ≥ exchangeable Al) AL Alisol (high-activity clays, exchangeable Al > exchangeable base cations) LV Luvisol (high-activity clays, exchangeable base cations ≥ exchangeable Al) Note: The exchangeable base cations are given in cmol c kg −1. Soils with little or no profile differentiation
The sodium adsorption ratio (SAR) is an irrigation water quality parameter used in the management of sodium-affected soils.It is an indicator of the suitability of water for use in agricultural irrigation, as determined from the concentrations of the main alkaline and earth alkaline cations present in the water.
There are also amphoteric exchangers that are able to exchange both cations and anions simultaneously. However, the simultaneous exchange of cations and anions is often performed in mixed beds, which contain a mixture of anion- and cation-exchange resins, or passing the solution through several different ion-exchange materials. Ion exchanger.
An ion-exchange membrane is generally made of organic or inorganic polymer with charged (ionic) side groups, such as ion-exchange resins. Anion-exchange membranes contain fixed cationic groups with predominantly mobile anions; because anions are the majority species, most of the conductivity is due to anion transport.
Download as PDF; Printable version; ... Pages in category "Cations" ... Text is available under the Creative Commons Attribution-ShareAlike 4.0 License; ...
4) cation produced by urea hydrolysis which is a strongly sorbing cation exchanges with the weakly sorbing Na + cation from the soil structure and Na + is released into water. Thus alkali soils adsorb / consume more urea compared to other soils. To reclaim the soils completely one needs prohibitively high doses of amendments.