Abstract

In the tropics, warm temperatures and high rainfall contribute to acidic soil formation because of the significant leaching of base cations (K+, Ca2+, Mg2+, and Na+), followed by the replacement of the base cations with Al3+, Fe2+, and H+ ions at the soil adsorption sites. The pH buffering capacity of highly weathered acid soils is generally low because of their low pH which negatively impacts soil and crop productivity. Thus, there is a need to amend these soils with the right amount of inorganic liming materials which have relatively high neutralizing values and reactivity to overcome the aforementioned problems. Soil leaching and the pH buffering capacity studies were conducted to determine whether the co-application or co-amendment of a calcium carbonate product (Calciprill) and sodium silicate can improve soil nutrient retention and pH buffering capacity of the Bekenu series (Typic Paleudults). A 30 day soil leaching experiment was carried out using a completely randomized design with 16 treatments and 3 replications after which the leached soil samples were used for a pH buffering capacity study. The Calciprill and sodium silicate treatments significantly improved soil pH, exchangeable NH4+, available P, exchangeable base cations, Effective Cation Exchange Capacity (ECEC), and pH buffering capacity in comparison with the untreated soil. The improvements were attributed to the alkalinity of Calciprill and sodium silicate due to their high inherent K+, Ca2+, Mg2+, and Na+ contents. The neutralizing effects of the amendments impeded the hydrolysis of Al3+ (96.5%), Fe2+ (70.4%), and Mn2+ (25.3%) ions resulting in fewer H+ ions being produced. The co-application of Calciprill and sodium silicate reduced the leaching of Ca2+ (58.7%) and NO3− (74.8%) from the amended soils. This was due to the ability of sodium silicate to reduce soil permeability and protect the Calciprill and available NO3− from being leached. This also improved the longevity of Calciprill to enhance the soil pH buffering capacity. However, the amounts of NH4+, P, and base cations leached from the amended soils were higher compared with the un-amended soils. This was due to the high solubility of sodium silicate. The most suitable combination amendment was 7.01 g Calciprill and 9.26 g sodium silicate (C2S5) per kilogram soil. It is possible for farmers to adopt the combined use Calciprill and sodium silicate to regulate soil nutrient retention and improve the soil pH buffering capacity of highly weathered acidic soils. This will enhance soil and crop productivity.

Highlights

  • The leaching of soil nutrients is a process by which water soluble nutrients move downward through the soil profile below the plant root zone via percolation of water that exceeds the field capacity of soils

  • The Calciprill and sodium silicate significantly suppressed exchangeable Al3+ in the range of 94.1% to 96.5%. These findings suggest that the co-application of Calciprill and sodium silicate was effective in suppressing Al toxicity because these values are below the threshold for Al toxicity which is 0.8 cmol(+) kg−1 [78,79]

  • The co-precipitation of Calciprill in alkaline soils resulted from the rapid solubility of sodium silicate and the adsorption of phosphates onto the surface of CaCO3 reduced leaching of Ca2+

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Summary

Introduction

The leaching of soil nutrients is a process by which water soluble nutrients move downward through the soil profile below the plant root zone via percolation of water that exceeds the field capacity of soils. These highly weathered soils with high kaolinite clay minerals and Al and Fe oxides are generally characterized by a low pH buffering capacity because of low Cation Exchange Capacity (CEC) and base saturations [5] As a result, these soils are prone to nutrient loss through soil erosion, surface runoff, and leaching due to the high rainfall events over long periods [6]. The effectiveness of CaCO3 in ameliorating soil acidity and suppressing Al toxicity is inconsistent due to the impurities and coarse particles in these traditional limes These carbonates exhibit poor solubility in soil water and the excessive use of dolomite causes Mg toxicity [10,11]. Careful selection of the right amendment to effectively suppress exchangeable acidity and manage soil pH is essential

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