Vulnerability of Selected Soils in the Different Rainfall Areas to Degradation and Excessive Leaching After Winery Wastewater Application
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Vulnerability of Selected Soils in the Different Rainfall Areas to Degradation and Excessive Leaching after Winery Wastewater Application A.R. Mulidzi1*, C.E. Clarke2, P.A. Myburgh1 1ARC Infruitec-Nietvoorbij, Private Bag X5026, 7599, Stellenbosch, South Africa 2Department of Soil Science, Stellenbosch University, Private Bag X1, Matieland 7602, South Africa. Submitted for publication: November 2019 Accepted for publication: March 2020 Key words: Chemical oxygen demand, Rainfall simulation, Water quality, Winery wastewater A pot trial was conducted to assess the effect of simulated rainfall on six soils with different textures, irrigated with winery wastewater diluted to a chemical oxygen demand (COD) level of 3000 mg/L over one simulated irrigation season. Thereafter, simulated winter rainfall was applied to the pots. The rainfall was simulated according to the long term averages of the regions where the soils originated. Leaching of cations, particularly K+ and Na+ occurred only from four of the six soils when winter rainfall was simulated. In one of the sandy soils, the simulated rainfall was too low to allow leaching. In another soil, high clay content of 35% in combination with low rainfall prevented leaching. In three soils that received the same amount of rainfall, more cations leached from the duplex sandy soil compared to the two other soils. These trends indicated that leaching of cations was a function of soil texture and rainfall. The study showed that in regions with low rainfall, irrigation with winery wastewater would lead to the accumulation of cations thereby increasing soil salinity. The study confirmed that for sustainable use of winery wastewater irrigation in agriculture, different soil types will require individual management in order to avoid or minimize the negative environmental impact on natural resources by wastewater irrigation. INTRODUCTION Studies regarding climate change in the wine growing regions after winery wastewater irrigation may lead to the leaching of the Western Cape Province have shown sharp increases in of nutrients to the groundwater. Changes in soil structure due air temperature, whereas rainfall is expected to decline, or to wastewater irrigation depend on the quality of wastewater, to be differently distributed during the rainy season (Vink i.e. salinity levels, organic matter content, and the amount et al., 2012). In 2017, the Western Cape experienced the of total suspended solids (Muller et al., 2007). The rate worst drought in a decade and this will have a lasting effect and amount of pollutants from winery wastewater reaching on agricultural production in future (Mulidzi et al., 2019). groundwater resources depend on several factors such as: The average annual grape production in South Africa sorption, degradation, chemical properties of the wastewater, was 1.33 million tonnes from 2010 until 2012 and wineries soil characteristics, environmental conditions, rainfall and generate large volumes of poor quality wastewater, water management practices (Mulidzi et al., 2018). Saline- particularly during harvest (Howell & Myburgh, 2018). sodic irrigation water in low rainfall and high evaporation It is estimated that c. 3 to 5 m3 of winery wastewater with areas will increase soil sodicity. Furthermore, a major side high organic load and variable salinity and nutrient levels effect associated with wastewater irrigation is the potentially is produced per tonne of grapes crushed (Howell et al., irreversible deterioration of the groundwater quality (Mulidzi 2018). Most winery wastewater is currently irrigated onto et al., 2016). The electric conductivity (EC) of Fluvisol soils pastures, but because of the drought and climate changes, decreased as a result of leaching of salts by the Autumn- the idea of using winery wastewater to irrigate vineyards Spring rainfall (Mulidzi et al., 2018). However, due to high has been encouraged (Mulidzi et al., 2019). Winter rainfall cation exchange capacity (CEC) and high water retention 1 The Fruit, Vine and Wine Institute of the Agricultural Research Council *Corresponding author: E-mail address: [email protected] Acknowledgements: The Water Research Commission for initiating and funding the project. Winetech, THRIP (TP1208066038) and the Agricultural Research Council for co-funding. Staff of Soil and Water Science at ARC Infruitec-Nietvoorbij for technical support, and in particular Mr Francois Baron for his dedicated effort. Any opinions, findings and conclusions or recommendations expressed in any publication generated through THRIP-supported research, are those of the authors and therefore the NRF/THRIP will not accept any liability in that regard S. Afr. J. Enol. Vitic., Vol. 41, No. 1, 2020 DOI: https://doi.org/10.21548/41-1-3774 99 100 Winery wastewater application to different soils capacity, the soils still retained high levels of Na+. Winter the end of the simulated rainfall period. The chemical status rainfall on soils irrigated with winery wastewater will lead of the leachate from each soil was determined in samples to the reduction of soil electrolyte concentrations regardless collected from the pooled leachate. of soil type. Low rainfall areas are likely to experience less soil structural hazard, which is linked to high exchangeable Water sampling and analyses monovalent cation concentrations while high rainfall areas Water samples were collected from the river water and will experience more soil structural hazard (Suarez et al., wastewater tanks prior to each irrigation (Table 2). The pH, 2008). electrical conductivity (EC), Na+, K+, Ca2+, Mg2+, Fe, Cl-, - 2- - The objective of the study was to investigate the effect HCO3 , SO4 , B and COD were determined at a commercial of simulated winter rainfall on leaching of basic cations in laboratory (BEMLAB, Strand). Details of the analytical soils irrigated with diluted winery wastewater. procedures were described previously by Mulidzi et al. (2015). MATERIALS AND METHODS Soils used Soil sampling and analyses Six pedogenetically different soils commonly found in the After six irrigations, i.e. one simulated winery wastewater Western Cape province of South Africa were included in the irrigation season, soil samples were collected from the 0 to study (Table 1). The taxonomic classification of the soils 19 cm soil layer. Soil sampling was again carried out after is given according to the South African soil classification the simulated winter rainfall had been applied. All analyses system (Soil Classification Work Group, 1991) as well were carried out at a commercial laboratory (BEMLAB, as World Reference Base (IUSS Working Group WRB, Strand). Details of the analytical procedures were described 2014). For the purpose of this article, soils will be referred previously by Mulidzi et al. (2016). to as Rawsonville sand, Lutzville sand, Stellenbosch shale, Stellenbosch granite, Stellenbosch sand and Robertson clay. Soil characterization The soil was packed into PVC pots to a specific predetermined The six selected soils represent soils dominant in three of the bulk density as described by Mulidzi et al, (2016). main South African wine producing regions. It was expected that the effect of winter rainfall after winery wastewater Application of water to the soils irrigation would differ between different soils. The results For the control treatment, the soils were irrigated with of the chemical properties of the six soils are presented in water abstracted from the Holsloot River near Rawsonville Table 3. The pH of the six soils ranged between 4.2 and 6.6, in the Breede River valley. Water used for the wastewater whereas the electrical conductivity of the saturated extract treatment was collected from the wastewater pit at a winery (ECe) ranged between 20 and 70 mS/m. The cation exchange -1 near Rawsonville. The winery wastewater was then diluted capacity (CEC) ranged between 2.9 and 8.3 cmolc.kg to a chemical oxygen demand (COD) level of 3000 mg/L. (Table 3). The Robertson soil had the highest clay content, Six irrigations were applied over one simulated season. It i.e. 35%, whereas the Lutzville sand contained only 0.4% was estimated that six is the number of irrigations a micro- clay (Table 4). sprinkler irrigated vineyard would require during the harvest period, i.e. when the highest volumes of wastewater are Composition and amount of simulated winter rainfall produced. Irrigation was applied when c. 50% of the water applied had evaporated (Fig. 1). The latter was considered to be the The overall average chemical composition of the Holsloot recommended level of depletion for vineyards to obtain a river water used to simulate winter rainfall was within the balance between yield and wine quality. acceptable range for irrigation water (Table 2). The pH After one simulated irrigation season, simulated winter levels were below the recommended pH for irrigation water rainfall was applied to all treatments. Since the pot ranging from 6.5 to 8.4 (DWAF, 1996). The amount of experiment was carried out in summer, there was no source rainfall applied was calculated from the long term average of uncontaminated rainwater available. It was decided not to winter rainfall in the region where each soil was collected use distilled or de-ionized water for the rainfall simulations, (Table 5). Rawsonville soils received the highest amount of since using distilled water changes the ionic balances and rainfall per day (13.8 mm) followed by the three soils from may flocculate or disperse the clay in the soil (Amezketa Stellenbosch (9.3 mm), while the Robertson and Lutzville et al., 2004). Soil water contains solutes which are in soils received the least rainfall (4.5 & 3.8 mm, respectively) balance with ions on exchange sites of the clay. Based on (Table 5). the forgoing, “rainwater” for the study was also abstracted from the Holsloot River, i.e. from a natural source where Statistical procedures contamination is least expected. The amount of rainfall The study was carried out under a 20 m × 40 m translucent applied to each soil was based on the long term mean fiberglass rain shelter at ARC Infruitec-Nietvoorbij near winter rainfall for each of the different regions where the Stellenbosch.