An experiment, over 3 years, studied the effects of mineral fertilizers and
organic manures on potassium (K) balances in rainfed lowland rice on a lig
ht-textured Tropaqualf. Two rice Crops were grown each year: the first dire
ct seeded (DS) in moist soil that was later flooded by monsoon rain; the se
cond transplanted (TP) into flooded soil towards the end of the wet season.
A soybean crop followed the TP rice in the first year. In all the fertiliz
er and manure combinations studied, removal of K in the crop exceeded K add
itions and the soil K balance was negative unless crop residues were incorp
orated. For DS rice the relations between grain yield and K uptake fell wit
hin the limits of maximum K dilution and maximum K accumulation expected fo
r well-managed irrigated rice. But those for TP rice tended to fall below t
he limit of maximum accumulation, yield being constrained by factors other
than mineral nutrition, especially water deficit. In the DS rice, grain yie
lds per unit K uptake were close to maximal in the treatments that received
no K, but they were well below that in the K-fertilized treatments. Uptake
was well correlated with exchangeable K in the soil at maximum tillering m
easured by ammonium acetate extraction. The mass balances of K inputs, K up
take and exchangeable K in the soil however, showed that a large part of th
e uptake was from non-exchangeable pools. The mobilization of non-exchangea
ble K was apparently plant-induced and was greater in treatments with great
er growth. A mechanism for root-induced solubilization of non-exchangeable
K, peculiar to rice growing in flooded soil, is proposed. (C) 1999 Elsevier
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