Abstract
Soil acidity is an important soil factor affecting crop growth and development. This ultimately limits crop productivity and the profitability of farmers. Soil acidity increases the toxicity of Al, Fe, H, and Mn. The abundance of Al and Fe ions in weathered soils has been implicated in P fixation. To date, limited research has attempted to unravel the use of charcoal with the incorporation of sago (Metroxylon sagu) bark ash to reduce P fixation. Therefore, an incubation study was conducted in the Soil Science Laboratory of Universiti Putra Malaysia Bintulu Sarawak Campus, Malaysia for 90 days to determine the optimum amounts of charcoal and sago bark ash that could be used to improve the P availability of a mineral acidic soil. Charcoal and sago bark ash rates varied by 25%, whereas Egypt rock phosphate (ERP) rate was fixed at 100% of the recommendation rate. Soil available P was determined using the Mehlich 1 method, soil total P was extracted using the aqua regia method, and inorganic P was fractionated using the sequential extraction method based on its relative solubility. Other selected soil chemical properties were determined using standard procedures. The results reveal that co-application of charcoal, regardless of rate, substantially increased soil total carbon. In addition, application of 75% sago bark ash increased soil pH and at the same time, it reduced exchangeable acidity, Al3+, and Fe2+. Additionally, amending acidic soils with both charcoal and sago bark ash positively enhanced the availability of K, Ca, Mg, and Na. Although there was no significant improvement in soil Mehlich-P with or without charcoal and sago bark ash, the application of these amendments altered inorganic P fractions in the soil. Calcium-bound phosphorus was more pronounced compared with Al-P and Fe-P for the soil with ERP, charcoal, and sago bark ash. The findings of this study suggest that as soil pH decreases, P fixation by Al and Fe can be minimised using charcoal and sago bark ash. This is because of the alkalinity of sago bark ash and the high affinity of charcoal for Al and Fe ions to impede Al and Fe hydrolysis to produce more H+. Thus, the optimum rates of charcoal and sago bark ash to increase P availability are 75% sago bark ash with 75%, 50%, and 25% charcoal because these rates significantly reduced soil exchangeable acidity, Al3+, and Fe2+.
Highlights
Phosphorus is an essential nutrient which serves as a component of many key plant structural compounds and as a catalyst in the conversion of numerous biochemical reactions in plants
The findings demonstrate that dissolution of water soluble fertiliser (TSP) in acidic soils produced Aluminium bound phosphorus (Al-P) and Fe-P, whereas the application of rock phosphate resulted in Calcium bound phosphorus (Ca-P)
Calcium-bound P is more pronounced compared with Al-P and Fe-P in soils with Egypt rock phosphate (ERP), charcoal, and sago bark ash because these soil amendments are able to increase soil pH, and at the same time, they reduce exchangeable acidity, exchangeable Al, and exchangeable Fe
Summary
Phosphorus is an essential nutrient which serves as a component of many key plant structural compounds and as a catalyst in the conversion of numerous biochemical reactions in plants. Phosphorus availability is limited in soils, especially in acidic soils such as highly weathered ultisols and oxisols This limitation is mainly because of the abundance of Al and Fe resulting from high weathering of the soils’ minerals [4,5]. These acidic cations tend to convert P in the soil solution to water-insoluble Fe-P and Al-P. Only a small proportion of the total P (usually
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