African Journal of
Biotechnology

  • Abbreviation: Afr. J. Biotechnol.
  • Language: English
  • ISSN: 1684-5315
  • DOI: 10.5897/AJB
  • Start Year: 2002
  • Published Articles: 12486

Review

Effects of potassium behaviour in soils on crop absorption

Yong-Hong Lin
Kaohsiung District Agricultural Research and Extension Station, Council of Agriculture, Executive Yuan, Pingtung, 90846, Taiwan.
Email: [email protected]

  •  Accepted: 29 June 2010
  •  Published: 31 July 2010

Abstract

Potassium (K) is one of the three major elements that play important roles in plants, such as maintaining 
turgor of cells, promoting activation of enzymes, and improving efficiency of photosynthesis. The types 
of K in soil may affect the plant absorption of K. K in soils includes K minerals, K in layered silicates 
(clay minerals), exchangeable K and K in solution. The former two can provide K very slowly through 
long period and so may be seen as ineffective; the latter two are the major types for K supply to plants. 
The release of the exchangeable K is basically through ionic exchange reactions. In the farm, soils with 
weak acidity to neutral conditions and 90% saturation of salt base, has calcium (Ca) as the most 
important cation among the exchangeable ions, followed sequentially by magnesium (Mg), K and 
sodium (Na). Ca and Mg are the major competitors of K for the exchangeable sites or locations. The 
effectiveness of K ions depends on the competitive absorption of Ca and Mg. However, the exchange 
behaviour of Ca and Mg in soils is quite similar and so they are commonly combined as one cation to 
simplify theoretical and analytical treatments of the processes. In general, quantity/intensity (Q/I) 
diagram of K may serve as an index for the strength and quantity of effective K supply to plants in soils. 
Some parameters such as equilibrium activity ratio (ARe), K selectivity coefficient (KG) and potential 
buffering capacity (PBC) may provide important information for the K behaviour in soils. ARe indicates 
the amount of K that can be provided by solution instantly in the soil. KG, a coefficient for K selectivity, 
indicates higher K selectivity for the soil when its value is higher. Higher PBC shows higher K buffering 
capacity of the soil. Therefore, this information may be based as references for K fertilization.
 
Key words: Potassium (K), quantity/Intensity (Q/I), activity ratio (AR), selectivity coefficient (KG), absorption

Abbreviation

Q/I, Quantity/intensity; ARe, equilibrium activity ratio; KG, potassium selectivity coefficient; PBC, potential 
buffering capacity; AR, activity ratio; ExK, exchangeable potassium; CEC, cation exchange capacity.