Abstract

In this study, titanium dioxide (TiO2) nanoparticles are immobilized onto rice husk biochar (RHB), as a porous support, for the photodegradation of glyphosate under UV light irradiation. The TiO2/RHB composites are prepared by pyrolysis and the sol-gel method. The SEM, XRD, EDX, and FT-IR results confirm the graphene structure of RHB and the formation of 10.61 nm TiO2 nanoparticles on the catalyst support. The effects of operating conditions, including catalyst dosage (3 g L−1, 5 g L−1, 10 g L−1, and 20 g L−1) and different illumination conditions (9 W lamp, 2 × 9 W lamps), on the removal of glyphosate from aqueous solutions were investigated. The photodegradation efficiency of 15 mg L−1 of commercial glyphosate was up to 99% after 5 h of irradiation at pH 3.0, with a TiO2/RHB dosage of 10 g L−1. However, the mineralization efficiency under this condition was lower than the decomposition efficiency of glyphosate, proving the partial degradation of glyphosate into AMPA and other metabolites after 5 h of reaction.

Highlights

  • SEM was connected with energy dispersive X-ray spectroscopy (EDXS) for chemical element composition analysis

  • Biochar is obtained from the pyrolysis of rice husks in an anaerobic environment

  • The cross-sectional image of the rice husk biochar (RHB) illustrates the appearance of mesopores with an average diameter of about 28 μm

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Summary

Introduction

Glyphosate (N-(phosphonomethyl) glycine, known by the trade name Roundup and Rodeo) has been a dominant herbicide worldwide for many years, since its first commercial introduction in 1974 [1]. This herbicide is non-selective, systemic, and postemergent, which is decisive for removing a wide range of weeds. The residue glyphosate from various sources, such as industrial effluents, agricultural runoff, and spilt chemicals [1], was considered as a pollutant, which contaminates the environment. In areas in the USA where genetically modified glyphosate-resistant crops are grown, glyphosate and its main metabolite aminomethylphosphonic acid (AMPA) were found in soil, surface water, and groundwater at levels from 2 to 430 μg L−1 [2,3,4,5]

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