Abstract:
Total potassium (K) concentration represents the K pool in a soil, and that provides
the required K for plant uptake after making K available through biochemical
changes. Knowledge on K pool in different soil types is important for sustainable
management of crops and soils. Therefore, this research was conducted to estimate
the total K concentration in different rice growing soil types from agro-climatic
zones (ACZs) of Sri Lanka. Total of 200 soil samples representing six ACZs (except
for Upcountry Wet zone) in Sri Lanka were collected though a stratified random
sampling approach. Soil total K concentration was determined through X-ray
florescence (XRF) analyser. Soil total K concentration had a wide range of values i.e.
316-31,153 mg kg−1. The Reddish Brown Earths & Immature Brown Loams (RBE IBL) had the highest soil total K concentration (20,127 mg kg−1) followed by Rock
Knob Plain (RKP), Reddish Brown Earths with high amount of gravel in subsoil &
Low Humic Gley (RBE-LHG), Noncalcic Brown soils & Low Humic Gley soils (NB LHG), Reddish Brown Earths, Noncalcic Brown soils & Low Humic Gley (RBE-NB LHG) and Noncalcic Brown soils, soils on old alluvium & Solonetz (NB-S) soils. All
these soils had total K concentration greater than 13,000 mg kg-1. Soils of Bog and
Half-Bog soils (BHB) and Red-Yellow Podzolic soils with soft or hard laterite (RYP)
reported the lowest total K, i.e. <5,000 mg kg-1. Soil total K concentration was high
in Intermediate Zone Upcountry followed by Dry Zone Low Country, Intermediate
Zone Low Country and Intermediate Zone Mid Country and the lowest in Wet Zone
Low Country. The results confirm that, soil total K concentration in Sri Lankan
paddy growing soils had a clear spatial variability associated with soil type and ACZ.
This information would be important for sustainable K-nutrient management in Sri
Lankan rice fields.
