mjsa.02.2025.85.90
ABSTRACT
GROWTH AND FRESH YIELD RESPONSE OF SWISS CHARD (BETA VULGARIS L. VAR. CICLA) CV. FORD HOOK GIANT TO ZEOLITE SOIL AMENDMENT
Journal: Malaysian Journal of Sustainable Agriculture (MJSA)
Author: Olwetu Antonia Sindesi, Bongani Ncube, Muinat Nike Lewu, Azwimbavhi Reckson Mulidzi, Francis Bayo Lewu
This is an open access article distributed under the Creative Commons Attribution License CC BY 4.0, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited
DOI: 10.26480/mjsa.02.2025.85.90
KEYWORDS: Zeolite, Swiss chard, sandy soil, growth parameters, fresh yield, soil amendment.
1. INTRODUCTION
Vegetables are essential for health and nutritional benefits in the human diet (Sharma et al. 2021; Noopur et al. 2023). Vegetables supply large amounts of minerals, vitamins, carbohydrates, proteins, dietary fibre and various nutraceutical compounds (Sharma et al., 2021). They are also the cheapest source of protection against various diseases (Kumar et al., 2020). According to, there is an inverse relationship between high vegetable consumption and disease (Noopur et al., 2023). In developing countries, vegetables play an essential role in managing malnutrition, particularly the ones that are easy to cultivate. Swiss chard (Beta vulgaris L., var. cicla) is one of the vegetables that has gained significant interest from farmers due to its ease of cultivation and adaptability to diverse environmental conditions (Franzoni et al. 2024; Ojiewo et al., 2015). Swiss chard is a biennial herbaceous leafy vegetable with nutraceutical properties, and it is one of the most widely consumed leafy vegetables in South Africa (Dumani et al. 2021).
In South Africa, vegetable and other crop producers face numerous challenges, including high input costs, water shortages, and soil degradation (Lötter et al., 2009; Chikozho et al., 2020). Farmers have used organic manures, such as compost and animal manure, to combat high input costs, water shortages, and soil degradation (Atoloye, 2024). However, organic manures are not stable and easily decomposable; they are also bulky and may introduce weed seeds to the farmers’ fields, leading to increased labour requirements (Gamage et al., 2023; Mwangi et al., 2024). Therefore, there is a need to find more stable and innovative soil amendments to reduce farm input costs and ameliorate soil degradation while improving crop yields.
Zeolite is a relatively cheap soil amendment which can be used as an alternative to natural organic amendments (Javaid et al., 2024). Zeolite has been observed to improve soil quality and increase soil moisture holding capacity (Ibrahim et al. 2021; Sindesi et al. 2023a). Zeolites are natural inorganic amendments; they are stable materials that improve soil quality and increase crop productivity (Nur Aainaa et al., 2018; Sindesi et al., 2023b). Zeolites are a group of microporous crystalline aluminosilicate minerals of alkaline nature, with large surface area and ion exchange capacity and a great affinity towards ammonium (NH4+) and potassium (K+) cations (Gül et al. 2005; Ramesh and Reddy, 2011). Due to its benefits and properties, zeolite has gained popularity as a soil amendment. There is also growing research on the positive effects of zeolite as a soil amendment on various crops, including vegetables. However, specific studies it’s the impact on Swiss chard are relatively limited. Nevertheless, based on its known properties of improving soil quality, water retention, and nutrient availability, zeolite has the potential to enhance the growth and yield of Swiss chard and other vegetable crops. This study examined the influence of zeolite on Swiss chard growth and yield over 8 weeks after transplanting.
2. MATERIAL AND METHODS
2.1 Research Design
A greenhouse study was conducted at the Agricultural Research Council,Infruitec-Nietvoorbij, Stellenbosch, South Africa (33.914476° S and18.861322° E) using Swiss chard (Beta vulgaris var. circa cv. Ford HookGiant). The study was conducted over two growing seasons: late autumnto late spring 2018 and early autumn to early spring 2019. The studyassessed the effects of zeolite as a soil amendment on Swiss chard growthrate and Swiss chard fresh yield. Zeolite to sandy soil application wasbased on weight-to-weight ratios of 0:10, 1:9, 2:8, and 3:7. Each plantingpot had 12 kg of soil or soil and zeolite mixture, and the pots werearranged in a randomised complete block design, with six (6) replications.The zeolite used was of clinoptilolite mineralogy composed of 64.30%silicate (SiO2) and 12.70% aluminium oxide (Al2O2). Details about theinitial soil chemical characteristics and other characteristics of the zeoliteused in this study are reported in the work of Sindesi et al. (2023). Thefertiliser applications on each pot are described in the work by Sindesi etal. (2022). Six-week-old Swiss chard plants of about 7 cm were used forthe experiment. One plant was transplanted into each pot.
2.2 Data Collection
Growth parameter data was collected four weeks after the transplantingof the seedlings and continued weekly over four consecutive weeks. Swisschard growth was represented by the number of loose leaves per plant,plant height, leaf width, leaf chlorophyll content index (CCI), and leaflength. Fresh yield was collected 59 days after transplanting.
2.2.1 Number of loose leaves per plant
All the true leaves, fully developed leaves with a petiole or white stalk anda blade that were adequately grown and observed to have moved awayfrom the main growing point, were counted and recorded.
2.2.2 Plant height
Plant height was measured using a transparent ruler, and care was takento ensure that the ruler was vertically placed next to the plant, with theruler’s zero end positioned at the plant’s base, where the stem met the soil.Only the tallest leaf was observed on each plant.
2.2.3 Leaf area
The leaf width (maximum value perpendicular to the midrib) and the leaflength (maximum value along the midrib) were measured and recorded tocalculate the leaf area. These parameters were further used to developratio and regression estimators to calculate the leaf area. The formula forthe Swiss chard leaf area entailed finding the slope of the leaf length andleaf width (linear regression), the Y was represented by leaf width, whilethe X was represented by leaf length. After finding the slope, it (the slope)was multiplied by the leaf length and the leaf width.
LEAF AREA ≈ m * L * W
W was the leaf width
L was the leaf length
m was the slope of the line
2.2.4 Leaf Chlorophyll content index
Leaf chlorophyll content index (CCI) data was collected from the top edgeof the largest leaf on each plant using a CCM-200 plus chlorophyll contentmeter, manufactured by Opti-Sciences, USA.
2.2.5 Growth rates
The growth rates of the observed parameters were calculated by dividingthe difference between the values recorded in the first and fourth weeksby 3.
2.2.6 Fresh yield
Swiss chard was harvested 59 days after transplanting by cutting thestalks at the base of the plants, and the fresh weight (grams/3 plant) was measured immediately using a weighing scale. Swiss chard harvested fromall three pots that represented one replicate were combined beforeweighing.
2.2.7 Statistical analysis
Data were analysed using Statistical Analysis System (SAS) software(version 9.4, SAS Institute Inc., Cary, NC, USA, 2000) for Analysis ofVariance (ANOVA). Seasonal homogeneity of variance was tested withLevene’s test, after which the results of both seasons were merged andstudied in a single overall ANOVA. The Shapiro-Wilk test was conductedfor deviation from normality and insignificant interactions. Fisher’s leastsignificant difference was calculated at the 5% level to compare treatmentmeans. For all tests, a probability level of 5% was considered significant.Pearson correlation coefficients (r), correlating Swiss chard’s growth andyield parameters, were derived using the CORR procedure of SAS 9.4.
3. RESULTS AND DISCUSSION
3.1 Effect Of Zeolite On The Growth Parameters Of Swiss Chard
Leaf chlorophyll content, number of leaves, height, leaf width, and lengthwere used as non-destructive growth measures on leafy vegetables. Figure1 (A-D) shows the growth parameters of Swiss chard grown on zeoliteamendedsandy soils at 59 days after transplanting. Leaf chlorophyllcontent index (CCI) had higher values in the second season (2019)compared to the first season (2018). Additionally, the non-amendedtreatment (0%) showed better leaf CCI values compared to the zeoliteamendedtreatment, except for 20% zeolite application in the first seasonand 30% zeolite application in the second season. The leaf CCI is related tothe nitrogen (N) and the water status of the plant, a decrease in leaf CCI atthe end of a crop life is normally associated with leaf senescence (Khaleghiet al., 2012; Sánchez-Sastre et al., 2020). Zeolite, due to its porous natureand affinity towards ammonium (NH4+) cations may regulate plant waterand N uptake (Gül et al. 2005; Ramesh and Reddy, 2011). Zeolite has beenobserved to increase soil water holding capacity (Shahbaz et al., 2019;Mahmoud and Swaefy, 2020).
The study found an increased wheat photosynthetic rate, with zeoliteapplication (100 g kg-1; 50 g kg-1 application). That analysis found higherphotosynthetic rates [μmol/m2/s], on sage plants grown on soils treatedwith nano-zeolite (30 g L-1 zeolite-irrigation water) (Shahbaz et al., 2019;Mohmoud and Swaefy, 2020). In both studies, this was attributed toimproved soil moisture holding capacity with zeolite application. Thefindings of this study contradict these author’s findings and may be due tothe differences in zeolite application rate. The high application of zeolitein this study may have increased zeolite affinity towards NH4+ in the soilsolution, allowing for zeolite to adsorb most of the NH4+ in the soil into itscavities. Zeolite cavities and their high cation exchange capacity may allowzeolite to adsorb cations with a greater force than that of plant roots fornutrient assimilation (Valdivia et al., 2021). However, the benefit of theadsorption is that it allows for significant amounts of essential nutrients,particularly NH4+, to be retained in the soil and prevents them fromleaching (Liu et al., 2023).
Swiss chard number of leaves per plant (Figure 1-B) shows that there wereno differences (p≥0.05) in the first growing season (2018). In the secondgrowing season, there was an increase in the number of leaves per plantwith the increased application of zeolite. The leaf area (cm2) results alsoshow that there were no differences (p≥0.05) among the zeolite-amendedtreatments, while the non-amended treatment had reduced (p≤0.05) leafarea in the first growing season. In the second growing season, the leafarea increased with the increase in zeolite application. This can be linkedto zeolites’ long-term improvement of soil quality, as previously reportedby Sindesi et al. (2023a) (2023b) and (2024). Soil pH, soil total K, soilexchangeable cations (Ca, K, Mg and Na) and cation exchange capacitywere all improved in the study due to zeolite application. Additionally,improved soil water holding may also be attributed to the increase in thenumber of leaves and leaf area in the second growing season. In the initialgrowing season, the zeolite may not fully integrate with the sandy soil,leading to uncertain results and trends in Swiss chard growth. Thesefindings suggest that zeolite may need more time to fully integrate into thesoil system and positively impact plant growth. This phenomenon is alsonoticeable in the results for Swiss chard plant height (Figure 1-D). Plantheight slightly (p≥0.05) decreased on the non-amended treatment from2018 to 2019, while on the zeolite-amended treatments, all the plantheights improved from the initial growing season to the 2019 season.


3.2 Swiss chard yield parameter responses to zeolite application
Swiss chard yield parameters are represented in Figure 2 (A-C) below. In the initial growing season, both fresh and dry matter yield (g/3 plants) showed better weight on the non-amended treatment and the 20% zeolite amended treatment. Generally, these two yield parameters were slightly better on the non-amended treatments in the first growing season. In the second growing season, the two yield parameters were reduced on the non-amended and zeolite-amended treatments compared to the initial season, except for the 30% zeolite treatment. In the second growing season, a general increase was observed with the increase in zeolite application. In the initial growing season, zeolite may have not yet fully integrated into the soil system, and during the process of integration may have reduced some essential plant-required nutrients, such as NH4+ (Omar et al., 2015; Liu et al., 2023; Doni et al., 2024). Zeolite has been noted to adsorb cations such as NH4+ and K+ into its structures and slowly release them into soil for plant use (Louhar, 2020). During the initial integration period, these nutrients may be temporarily unavailable for plant uptake as the zeolite absorbs them. Subsequently, they can be slowly released through a gradual exchange-induced dissolution process (Hartman and Fogler, 2007; Louhar, 2020). Zeolite dissolution can be influenced by factors such as pH, with acidic conditions potentially accelerating the dissolution of the zeolite structure (Hartman and Fogler, 2007). The soil pH of the initial soil used was slightly acidic (5.4KCL).
Swiss chard leaf moisture % did not significantly differ (p≥0.05) in the initial growing season (Figure 2-C). However, the 10 and 30% zeolite treatments showed slightly better moisture content than the other treatments in season 1. In the second growing season, the moisture content tended to reduce with increased zeolite application, with significance (p≤0.05) observed among some treatments. The 0 and 10% treatments showed higher moisture content than the other treatments. Crop moisture in crops assists in maintaining the protoplasmic contents of the cells as it encourages cellular functions and plant growth (Udousoro and Ekanem, 2013). However, in this study, higher growth was observed on the zeolite-amended treatments for the second growing season. As such, the low moisture content in the zeolite-amended treatments may be linked with the fact that Swiss chard cultivated under these treatments had higher leaf growth, which may have encouraged greater transpiration losses. This is further strengthened by the larger irrigation requirement that the Swiss chard needed in the second season as previously observed in (Sindesi et al., 2023).


3.3 Effect of zeolite on the growth of Swiss chard
As the availability of growth factors such as water and mineral nutrientsincreases, the growth rate and crop yield also increase (Motseki, 2008). Assuch, a faster leaf growth rate in Swiss chard leads to quicker harvests. Inthis study, the rate of increase of the number of leaves and leaf areaincreased (p≤0.05) with increased zeolite application (Figures 3-B and C).This increase can be attributed to improved soil chemical properties (pH,CEC, exchangeable cations and reduced heavy metal availability) andimproved water holding capacity (Sindesi et al., 2023a and 2023b).Additionally, the plant height growth rate (Figure 3-D) was notsignificantly different (p≥0.05) in the first growing season. However, therewas a general increase in the application of zeolite in the second growingseason. The growth rate of plant height may have been influenced byresource allocation by the plants (Miao et al.,2024).
The analysis show if plant growth processes draw on the same resourcesource, such as the phloem tissue carrying products of photosynthesis,then a trade-off might occur between resource allocation to certainaspects of growth (Pyke and Ren, 2023). However, if the growth processesutilise resources from different sources, the trade-offs may not arise. Thegrowth rate of the leaf chlorophyll content index decreased (p≥0.05)between the non-amended treatment and the 20% zeolite treatment in theinitial growing season. It further showed an increasing trend between the10 and 30% zeolite treatments, with the increase observed in the 30%zeolite treatment being significantly more significant than the growth rateobserved in the 10% zeolite treatment. Leaf chlorophyll content index ishighly influenced by nutrient availability (N), temperatures and wateravailability (Hermans and Verbruggen, 2005; Li et al., 2018). Zeolite hasbeen shown to influence soil water holding capacity and nutrientavailability (Mahmoud and Swaefy, 2020)



3.4 Correlation analysis between growth and yield parameters ofSwiss chard as affected by zeolite
The correlation coefficient of growth and yield parameters of Swiss chardcultivated under varying rates of zeolite-amended sandy soil are shown inTable 1. Growth parameter at four weeks of data collection (PHW4, NLW4,LAW4) values correlated strongly (p≤0.001) with the observed Swisschard yields. Interestingly, at four weeks of data collection, the threegrowth parameters negatively correlated with Swiss chard leaf moisturecontent %. Growth parameters at four weeks also had a strong positivecorrelation (p≤0.001) with their linked growth rates. As expected, rapid growth rates of these parameters ensure larger plant leaves. However, plant height at four weeks of data collection did not have such a strong correlation with the rate of leaf area growth over the 4 weeks (LAR) of data collection, although it also had a significant positive correlation (p≤0.01). This may be due to the plants’ allocation of resources to certain plant growth parameters, and as observed on the fresh and dry matter yields, it did not affect the plants’ productivity. also found strong positive correlations between plant height and yield parameters of cabbage (Head weight and head diameter) grown on organic and inorganic fertilisers (Shakirdeen et al., 2019). This strong and positive correlation shows that plant height is a valuable indicator of potential yield in leafy vegetables; however, it should not be used in isolation.
The chlorophyll content index (CW4) and chlorophyll content index growth rate (CR) did not significantly correlate with any other growth and yield parameters. However, these two parameters showed a strong positive correlation (p≤0.001). The absence of a significant correlation between CW4 and CR with the yield parameters contradicts the findings observed in the work by (Goggs et al., 2003; Blackmer and Schepers, 1995). The study found a significant correlation between leaf chlorophyll and cotton yield (Goggs et al., 2003). The analysis also found significant positive correlations between chlorophyll content and maise grain yields(Blackmer and Schepers, 1995). The difference in plant species and plant resource allocation may lead to differences in these correlations. These results show that CCI cannot be effectively used to predict Swiss chard growth and final yield.
Swiss chard leaf moisture content % (LM) showed a significant (p≤0.001) correlation with all the observed parameters apart from the chlorophyll-related parameters. All parameters that significantly correlated with Swiss chard leaf moisture content showed negative correlations. The negative correlation between Swiss chard’s moisture content and its growth and yield parameters indicates that the plant prioritises allocating resources towards growth and tissue production rather than water storage. Nevertheless, plants lose water during growth through transpiration. This process occurs when stomata tiny leaf surface pores open to facilitate gas exchange. As the stomata open, water vapour escapes from the leaf’s interior into the atmosphere (Hernandez-Candia and Michaelian, 2010). Generally, larger leaves tend to have more stomata, and while this can facilitate greater gas exchange, it also increases the plant’s susceptibility to water loss (Kouwenberg et al., 2007). Therefore, the correlation between the growth parameter and the LM can be due to increased stomata and plant growth, leading to increased transpiration.

CW4 Chlorophyll Content Index, PHW4 Plant Height, NLW4 Number of Leaves, LAW4 Leaf Area (All those with W4 are actual values on the fourth week of data collection), CR Chlorophyll Content Index Growth Rate, PHR Plant Height Growth Rate, NLR Number of Leaves Growth Rate, LAR Leaf Area Growth Rate, DMY Dry Matter Yield, FY Fresh Yield, LM Leaf Moisture Content.* Correlation is significant ≤ 0.05 level, **Correlation is significant ≤ 0.01 level, ***Correlation is significant ≤ 0.001 level.
4.CONCLUSION
This study examined the influence of zeolite on Swiss chard growth and yield at the end of two months over two growing seasons. The study showed that zeolite soil application improved the leaf area and number of leaves at four weeks of data collection in the second growing season. Furthermore, zeolite also improved the fresh and dry yield of Swiss chard in the second growing season. This demonstrates that zeolite may require a fallowing period before fully integrating into the soil system. The study also showed that decreased leaf moisture (%) does not necessarily lead to reduced dry matter yields. It is also clear that plant growth parameters such as plant height, the number of leaves and the leaf area are good indicators of yield potential in leafy vegetables. Future research is still needed to investigate longer zeolite influences on vegetable crops such as Swiss chard.
ACKNOWLEDGMENTS
The authors would like to thank the National Research Foundation (NRF) of South Africa for financial support for this research. Under NRF grant number: 114405. Any opinion, findings and conclusions, or recommendations expressed in this article are those of the author(s), and the NRF accepts no liability whatsoever in this regard.
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Pages | 85-90 |
Year | 2025 |
Issue | 2 |
Volume | 9 |