Abstract

The composition of organic waste (OW) and its effect on soil processes may change soil fertility and electrical conductivity (EC). The side effects of waste use in crop fertilization are poorly understood for Brazilian soils. This study examined the effect of the addition of 15 different organic wastes to Oxisols and a Neosol on pH, base saturation, EC, cation exchange capacity (CEC at pH 7), and the availability of Al, macro (P, K, Ca2+, Mg2+ and S) and micronutrients (B, Fe2+, Mn2+, Cu2+ and Zn2+). Soil samples (150 g) were treated with chicken, pig, horse, cattle, and quail manures, sewage sludge 1 and 2, eucalyptus sawdust, plant substrate, coconut fiber, pine bark, coffee husk, peat, limed compost, and biochar. Wastes were added considering a fixed amount of C (2 g kg-1), which resulted in waste rates ranging from 2.5 to 25.6 Mg ha-1. The soil-waste mixtures were incubated for 330 days in laboratory conditions. The waste liming or acidification values were soil-dependent. The use of some manures and compost increased the pH to levels above of those considered adequate for plant growth. The soil EC was slightly increased in the Neosol and in the medium textured Oxisol, but it was sharply changed (from 195 to 394 µS cm-1) by the addition of organic wastes in the clayey Oxisol, although the EC values were below the range considered safe for plant growth. Changes in the soil availability of P, K+, Ca2+ and Zn2+ were highly related to the inputs of these nutrients by the wastes, and other factors in soil changed due to waste use. Organic waste use simultaneously affects different soil fertility attributes; thus, in addition to the target nutrient added to the soil, the soil acidity buffering capacity and the waste liming and agronomic value must be taken into account in the waste rate definition.

Highlights

  • The use of organic wastes in agricultural fields may increase crop yield and soil quality while reducing pollution and increasing farmer profits

  • Compost and alkalinized wastes have excellent potential to increase soil pH to levels above of those considered optimal for plant growth

  • Over-liming of sandy and medium textured soils indicates that the waste rate, in addition to the target nutrient to be added to the soil, must be based on the soil acidity buffering capacity and in the waste liming and agronomic value

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Summary

Introduction

The use of organic wastes in agricultural fields may increase crop yield and soil quality while reducing pollution and increasing farmer profits. The effects of waste application on soil fertility depend on waste chemical composition, which is highly variable and linked to its origin. The waste production system, storage and management of crop residues and postharvest by-products are other key factors controlling the organic waste chemical composition and its value as an agricultural input. The composition and amount of feed furnished to animals are other factors that control the waste agronomic value; post-production treatments of composts and sewage sludge and by-products generated in the industry and agro-industries exert an influence on the waste chemical composition (Melo and Silva, 2008; Silva, 2008). Manures originating from intensive production systems are richer in nutrients than wastes produced by animals raised in extensive pastures or fed with poor nutritional grasses. Besides the amount and chemical composition, the effects of wastes on soil properties are related to the nutrient mineralization rate, which is closely linked to chemical, physical and biological waste properties, humification degree and the biotic and abiotic factors in soil regulating the rate of waste decomposition (Abreu Júnior et al, 2005; Pavinato and Rosolem, 2008)

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