Abstract

From a global perspective, drought is a well-known manifestation of climate change. The search for alternative sources of water also brings uncertainties and risks, for example, in relation to wastewater irrigation. We asked ourselves whether and how supplemental irrigation with pre-treated wastewater would affect the subsoil or groundwater quality. We constructed semi-operational models that were loaded with wastewater in a controlled manner over three years of observations. Ammonium nitrogen (NH4+-N) pollution is one of the monitored parameters in wastewater discharge. In specific situations and under strict operating conditions, it can be assumed that ammonia nitrogen may not be a significant problem for groundwater. Already at a depth of 0.5 m below ground level, the average nitrogen levels are below 0.02 mg/L at an irrigation rate of approximately 15.5 mm/day. When monitoring total phosphorus (TP), these values are reduced with more variability—depending on the plant species at the surface, ranging from 0.17 to 0.95 mg/L. The measured values are used to calibrate the numerical model, or to determine the reaction parameters that enter the governing equation to describe the distribution of the solution in the soil environment. The results show an acceptable compliance between the model and real measurements, it will be possible to use them in practice for the design of wastewater irrigation systems.

Highlights

  • The issue of drought development associated with increasing water scarcity is currently a very topical issue

  • No mechanical treatment of the effluent was necessary for the measurements, the wastewater contains a minimum of suspended solids, so micro-spray irrigation is possible and there is no risk of clogging of the irrigation nozzle

  • The pump was submerged below the level of the continuously flowing wastewater at all times, the supply pipe is fitted with a fine filter to prevent clogging of the irrigation sprinklers despite the minimum suspended solids

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Summary

Introduction

The issue of drought development associated with increasing water scarcity is currently a very topical issue. It is estimated that up to 3.2 billion people live in agricultural areas suffering from high water scarcity [1]. There is an increasing need for water resources for economic expansion development, agricultural intensification and improvement of living standards due to population growth [2]. We must consider the impact of climate change, which is manifesting itself in more significant pronounced periods of drought even in areas not primarily classified as arid. Agriculture is one of the socio-economic sectors mostly vulnerable to climate change, affected by precipitation, soil moisture and temperature.

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