E. Salomon, EXTRACTION OF SOIL POTASSIUM WITH 0.01M CALCIUM-CHLORIDE COMPARED TO OFFICIAL SWEDISH METHODS, Communications in soil science and plant analysis, 29(19-20), 1998, pp. 2841-2854
In Sweden the official method for estimating plant available potassium
(K) is well calibrated to Swedish soils, but mainly provides informat
ion about exchangeable K. The objective was to evaluate a 0.01 M calci
um chloride (CaCl2) solution (K-CaCl2), with regard to its compatibili
ty with standard laboratory procedures, and the relationship between t
he K-CaCl2 method and official Swedish methods depending on soil and f
ertilizing strategy. Soil was taken from long-term field experiments w
ith no K application or with applications of 160-240 K kg ha(-1) y(-1)
at Vojakkala, Ultuna, and Radde. The soil samples, air-dried or at fi
eld moisture content, were extracted by 0.01 M CaCl2 at two different
soil:extractant ratios (1:2 and 1:10), and analyzed by inductively cou
pled plasma emission spectrometry (ICP) for K content. In Sweden, the
official method for estimating plant available soil K is the ammonium
lactate/acetic acid (AL) method and non-exchangeable K is estimated in
2M HCl (K-HCl). Amounts of K-CaCl2 from field-moist and air-dried soi
l were significantly affected by soil:extractant ratio 1:2 or 1:10. Th
is indicated that the same fraction of K in soil was not always extrac
ted and that the amount depended on soil and fertilizing strategy, a s
oil:extractant ratio of 1:10 was preferable in order to get clear extr
acts. Air-dried soil samples were most suitable for Swedish laboratory
procedures. Overall, CaCl2 extraction gave smaller amounts of K than
AL and HCl extraction. However, at Vojakkala and Radde treatments with
K application considerably increased amounts of K-CaCl2 and K-AL, com
pared with no K application. In treatments with no K application, amou
nts of K-CaCl2 and K-AL were largest at Ultuna. There was a clear diff
erence among sites in amounts of K-HClI. There seemed to be a good rel
ationship between the K-CaCl2 and the K-AL methods. However, the K-CaC
l2 method extracted smaller amounts indicating that mostly K in soil s
olution was extracted. In Sweden, CaCl2 could be a good complement to
AL and HCI extractable K and give a more complete description of K ava
ilability on different soil types and under different fertilizing stra
tegies and could easily be incorporated into Swedish laboratory proced
ures.