Abstract

The field experiment was carried out in northern Tanzania to assess the effects of intercropping systems, Rhizobium inoculation, and fertilization with P and K on chemical properties of soybean rhizosphere soil. The experiment was laid out in split-split plot design with 2 × 4 × 7 factorial arrangement replicated thrice. The main plots had two inoculation treatments and the subplots were comprised of four cropping systems which were sole maize, sole soybean, and two intercropping at different soybean spacing (75 × 20 and 75 × 40 cm). The fertilizer levels (kg/ha) control (0 kg/ha); 20 K; 40 K; 26 P; 52 P; 26 P + 20 K; and 52 P + 40 K were assigned to sub-subplots. Statistical analysis was performed using ANOVA. Least Significant Difference was used to compare treatment means at p=0.05 significance level. The results indicated that rhizosphere soil chemical properties such as pH, organic carbon (OC), and macro- and micronutrients (N, P, Ca, Mg, and Na and Fe, Cu, Mn, and Zn, resp.) were significantly increased in the Rhizobium inoculated soybean over the control. The supply of P and K fertilizers significantly increased the rhizosphere content of macronutrients (P, K, Ca, and Mg) and also they altered the pH and EC of the rhizosphere soil relative to control.

Highlights

  • Plants require 17 nutrients to perform different plant functions related to growth, development, and reproduction

  • The results indicated that, except for sodium (Na), cropping systems had no significant effects on the chemical properties of the soybean rhizosphere soil

  • Rhizobium inoculation was observed to alter the most of the chemical properties of the rhizosphere soil of soybean compared with the rhizosphere soil collected

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Summary

Introduction

Plants require 17 nutrients to perform different plant functions related to growth, development, and reproduction. Most soils in sub-Saharan Africa are depleted and are deficient in mineral elements to sustain crop production [1,2,3]. Each of these plant nutrients is needed in deferent amount by plants and they differ in their mobility and availability in the plants and soil. Interactions between roots and soil during plant growth induce changes in the soil that make rhizosphere soil to differ from bulk soil [8, 9] These changes in the rhizosphere may be caused by root uptake of nutrients, microbial activity, and/or components of root exudates [5, 10]. The compounds that are released can lead to dissolution of primary minerals and precipitation or crystallization of secondary compounds and/or minerals and eventually transformation of mineral components in the rhizosphere [6]

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