Acta agriculturae Slovenica, 121/2, 1–12, Ljubljana 2025 doi:10.14720/aas.2025.121.2.22269 Original research article / izvirni znanstveni članek Water quality effects on germination of okra seed (Abelmoschus esculen- tus L.) Arsalan Azeez MARIF 1, 2 Received March 26, 2025; accepted May 29, 2025 Delo je prispelo 26. marec 2025, sprejeto 29. maj 2025 1 Garden Design Department, Bakrajo Technical Institute BTI, Sulaimani Polytechnic University SPU, Sulaimani, Kurdistan Region, Iraq 2 Correspondence Author: arsalan.marif@spu.edu.iq Water quality effects on germination of okra seed (Abel- moschus esculentus L.) Abstract: This study, conducted at Bakrajo Technical In- stitute in 2023, assessed the water quality of 24 resources using the Irrigation Water Quality Index (IWQI). Results revealed two categories: “Excellent” (19 resources, IWQI 91.4-96.5) and “Good” (5 resources, IWQI 70-90). Water in the “Excellent” category was highly suitable for irrigation, while the “Good” category was of lower quality but still acceptable. Electrical conductivity (EC) was identified as a key factor influencing the IWQI, with higher EC correlating with lower water qual- ity. Principal Component Analysis (PCA) and Agglomerative Hierarchical Clustering (AHC) were used to classify resources based on cation, anion, and heavy metal content. A negative correlation between EC and IWQI emphasized the importance of monitoring EC for irrigation purposes. The study also found weak, non-significant correlations between pH, EC, and germi- nation ratio, but noted that higher IWQI values and lower EC levels generally promoted better seed germination. The find- ings highlight the value of advanced models in water quality classification, offering essential insights for agricultural water management. Key words: water quality, germination ratio, okra, irriga- tion water, pH, EC Kakovost vode vpliva na kalitev semen jedilnega osleza (Abel- moschus esculentus L.) Izvleček: V raziskavi, izvedeni na Bakrajo Technical In- stitute, v letu 2023 je bila ocenjena kakovost 24 vodnih virov z indeksom kakovosti vode (IWQI). Rezultati so odkrili dve kategoriji, “odlična” (19 virov, IWQI 91.4-96.5) in “dobra” (5 virov, IWQI 70-90). Voda iz virov “odlična” je bila zelo prim- erna za namakanje, med tem, ko je bila voda iz kategorije “dobra” slabše kakovosti vendar še sprejemljiva. Električna prevodnost (EC) je bila prepoznana kot ključni dejavnik, ki vpliva na indeks kakovosti vode (IWQI), pri čemer so večje vrednosti EC korelirale s slabšo kakovostjo vode. Analiza glavnih komponent (PCA) in hierarhično aglomerativno grozdenje (AHC) sta bila uporabljena za klasifikacijo vodnih virov glede na vsebnost kationov, anionov in težkih kovin. Ugotovljena je bila negativna korelacija med EC in IWQI, kar poudarja pomen monitoringa EC za namene namakanja. Ra- ziskava je tudi odkrila šibko, neznačilno povezavo med pH, EC in deležem kalitve, pri čemer so večje vrednosti IWQI in manjše vrednosti EC navadno pospeševale boljšo kalitev. Ta odkritja pojasnjujejo vrednost naprednejših modelov pri kla- sifikaciji kakovosti vod in ponujajo bistven vpogled v kmeti- jsko upravljanje z vodo. Ključne besede: kakovost vode, kalitev, jedilni oslez, voda za namakanje, pH, EC Acta agriculturae Slovenica, 121/2 – 20252 A. A. MARIF 1 INTRODUCTION Water quality plays a crucial role in determining both agricultural productivity and the overall health of ecosystems. It directly impacts plant growth, germina- tion, and the subsequent development of crops, influenc- ing both yield and quality (Yuan et al., 2024: Wakchaure et al., 2023). The importance of water in agriculture is un- derscored by its effect on various physiological processes within plants, such as nutrient uptake, photosynthesis, and transpiration. For crops like okra (Abelmoschus escu- lentus L.), which is widely cultivated in tropical regions, water quality can significantly alter germination rates and early vegetative growth, ultimately affecting overall crop performance. Okra is a staple vegetable in many countries, with a global cultivation area of approximately 2.5 million hectares, yielding 10.5 million tons annually (Ibrahim, 2024): Food and Agriculture Organization of the United Nations, 2018). Seed priming, a pre-sowing treatment of seeds us- ing water or other solutions, is an important technique to enhance germination and improve early seedling growth. When combined with high-quality irrigation water, seed priming has been shown to accelerate seedling emer- gence, leading to more robust and healthy plants. Water quality, defined by parameters such as salinity, pH, dis- solved oxygen, and presence of contaminants, directly affects seed priming outcomes. Numerous studies have demonstrated that water with high salinity or other un- desirable characteristics can hinder seedling emergence and reduce crop yields. Okra is not only valuable for its role in agriculture but also an important source of nutri- tion, providing essential vitamins, minerals, and dietary fiber. Given the crop’s significance, understanding how different water qualities impact okra germination and seedling development is vital for optimizing agricultural practices, particularly in regions where water resources may be limited or of varying quality. Previous studies have highlighted the influence of water quality on seed germination and vegetative growth across different re- gions (Rima, 2021). The aim of the present research is to assess the water quality from 25 different water resources, classifying the irrigation water based on the Sulaimani Irrigation Wa- ter Quality Index (SIWI) proposed by Marif and Esmael (2023), as well as the classification system by Todd (1966). Additionally, this study utilizes advanced statistical tech- niques such as Principal Component Analysis (PCA) and Cluster Analysis to classify the water resources further and investigate their impact on okra seed germination. This research will provide a comprehensive understand- ing of how various water qualities influence the early No. Location GPS Coordinate Altitude 1 Kani Ababaile 35.18235 45.98377 915 2 Well Ababaile 35.18235 45.98377 910 3 Kani Faqe Byara S1 35.2250909 46.11599645 1087 4 Mergapan 35.78892 45.26581 1226.85 5 Peryadi _chm- chamal 35.51728 44.86407 697.58 6 Bakrajo 35.550052 45.358326 743.36 7 Kani panka S1 35.3816374 45.7082884 549 8 Kani panka S2 35.3816374 45.7082884 549 9 Sharbazher S1 35.720167 45.502614 827.28 10 Sharbazher S2 35.695679 45.528932 846.55 11 Krbchna 1 35.283103 45.276888 989 12 Krbchna 2 35.27582 45.26 786 933 13 Khwrmal S1 35.2971744 46.03963419 567 14 Bnawela 35.3647.1 453351.2 1130 15 Sitak 35.593677 45.517543 1126 16 Qarachatan 354410.3 450842.2 807 17 Khwrmal S2 35.30378 46.03852 567 18 Byara S2 35.23021 46.1212 1117 19 Awesar 35.21647 46.18916 1671 20 Tapatolaka 35.29402 45.95852 508 21 Sulaimani Rain water 35.557215 45.47464 1002 22 Kani sard 35.3932.4 453229 896 23 Bakrajo Tap water 35.550052 45.358326 743.36 24 Shene 36.1327 450425 570 Tabel 1: Study area description and GPS Coordination’s Figure 1: Study Area Map Acta agriculturae Slovenica, 121/2 – 2025 3 Water quality effects on germination of okra seed (Abelmoschus esculentus L.) stages of okra cultivation and offer insights into improv- ing irrigation practices for better crop performance. 2 MATERIALS AND METHODS 2.1 STUDY AREA The research was conducted at the Bakrajo Techni- cal Institute Field, located in the Sulaimani Governorate of the Kurdistan Region, Iraq. This field site is situated in Sulaimani City, which lies at an elevation of 888 me- ters above sea level. The geographical coordinates of the location are approximately 35.39705° N latitude and 45.28260° E longitude, as shown in Figure 1 and detailed in Table 1. The specific location’s altitude and geographic position are important factors in determining the cli- mate, soil conditions, and overall environmental char- acteristics of the study area, all of which play significant roles in influencing the results and interpretation of the research. Sulaimani’s climate is influenced by its semi- No. Location PH EC TDS Na Ca 2+ Mg2+ Na+ K+ CO3 - HCO3 - SO4 -- Cl- NO3 - dS m-1 mS.cm-1 % mg l-1 1 Kani Aba- baile 7.3 0.58 368.36 8.0 1.14 1.083 0.172 0.021 0 1.967 0.219 0.014 0.013 2 Well, ababaile 7.1 0.57 362.83 9.1 1.28 1.156 0.234 0.010 0 1.901 0.474 0.199 0.018 3 Kani Faqe Byara S1 7.1 0.54 346.58 8.8 1.17 1.142 0.179 0.044 0 1.820 0.215 0.243 0.075 4 Mergapan 7.1 1.01 645.67 9.1 2.20 1.190 0.335 0.006 0 1.059 1.310 1.029 0.171 5 Shwan _chm- chamal 7.2 0.83 533.85 14.5 1.48 1.124 0.397 0.044 0 1.803 0.077 1.086 0.065 6 Bakrajo 7.3 1.02 649.64 12.8 1.20 1.125 0.190 0.151 0 1.984 0.216 0.329 0.021 7 Kani panka S1 7.4 0.54 344.13 3.5 1.65 1.250 0.101 0.005 0 1.984 0.500 0.429 0.013 8 Kani panka S2 7.3 0.60 386.82 4.5 1.30 1.100 0.108 0.006 0 1.746 0.328 0.191 0.013 9 Shakhasur 7.1 0.45 288.45 6.5 1.24 1.138 0.158 0.008 0 1.910 0.191 0.286 0.022 10 Sharbazher tagaran 7.2 0.44 284.50 6.6 1.30 1.243 0.165 0.014 0 1.929 0.654 0.029 0.032 11 Krbchna 1 7.3 1.48 946.58 16.7 1.95 1.821 0.219 0.536 0 1.115 1.890 1.186 0.129 12 Krbchna 2 7.2 0.70 450.67 3.5 1.35 1.123 0.087 0.003 0 1.931 0.431 0.091 0.023 13 Khwrmal S1 7.1 1.99 1273.61 6.8 2.10 2.103 0.248 0.059 0 1.459 1.550 1.229 0.177 14 Bnawela 7.2 0.69 443.46 5.8 1.30 1.271 0.148 0.010 0 1.820 0.595 0.029 0.022 15 Sitak 7.1 0.74 475.24 8.9 1.12 1.283 0.220 0.015 0 1.900 0.088 0.629 0.013 16 Qarachatan 7.3 0.43 275.03 4.0 1.31 1.212 0.078 0.026 0 1.787 0.398 0.243 0.083 17 Khwrmal S2 7.2 0.50 318.08 19.0 1.81 1.159 0.626 0.070 0 1.838 0.763 0.571 0.099 18 Byara S2 7.1 0.52 329.94 4.7 1.23 1.010 0.104 0.006 0 1.484 0.475 0.243 0.025 19 Awsar 7.1 0.37 237.74 8.1 1.05 0.890 0.143 0.028 0 1.203 0.805 0.029 0.043 20 Tapatolaka 7.2 0.58 372.74 8.8 1.393 0.910 0.200 0.023 0 1.216 0.683 0.322 0.324 21 Rain water 7.1 0.34 218.88 2.2 1.1 0.920 0.030 0.014 0 1.323 0.353 0.280 0.028 22 Kani sard 7.2 0.32 204.80 6.0 0.7 0.430 0.059 0.013 0 0.436 0.446 0.186 0.048 23 Bakrajo Tap water 7.3 0.25 162.56 10.3 0.411 0.410 0.082 0.012 0 0.492 0.165 0.169 0.063 24 Shene 7.1 0.321 205.44 8.5 0.332 0.367 0.054 0.011 0 0.321 0.210 0.154 0.043 Table 2: Water cations and anions analysis Acta agriculturae Slovenica, 121/2 – 20254 A. A. MARIF arid conditions, with distinct seasonal variations that can impact agricultural practices and ecological studies. These geographic and climatic features, combined with the region’s unique environmental factors, provide valu- able insights into the scope of the research, highlighting the importance of this field site in understanding local agricultural systems, climate adaptation, and ecological sustainability in the context of the Kurdistan Region. 2.2 WATER SAMPLING COLLECTING The water sampling process for evaluating the water quality index in this research followed these steps: First step: Water samples were collected from 24 different locations or wells (labeled 1 to 24) in the study area. These samples were analyzed and compared based on their electrical conductivity (EC) and pH values. Second step: A total of 24 water samples were se- lected for the study. Third step: The water from the 24 selected wells or water resources was tested for physicochemical proper- ties and some heavy metals. Additionally, 24 of these samples were used for germination experiment with okra seeds. The samples were classified according to various methods outlined in Tables 2 and 3. Each water sample was collected in a 1.5-liter container for physicochemical analysis and was also used for germinating okra seeds in the laboratory at Bakrajo Technical Institute, maintained at a temperature of 25 °C. 2.3 WATER ANALYSIS AND COMPUTING THE IRRIGATION WATER QUALITY INDEX (IWQI). The water analysis was conducted as follows: 2.3.1 pH and electrical conductivity (EC) measure- ment A portable pH meter (Hanna pH H 98107) was used No Location Fe Mn Cu Co Ni Zn Cd Cr mg l-1 1 Kani Ababaile 0.011 0.036 0.02383 0.00150 0.007 0.016 0.00090 0.00156 2 Well ababaile 0.014 0.020 0.01257 0.00105 0.004 0.012 0.00326 0.00152 3 Kani Faqe Byara S1 0.019 0.033 0.02368 0.00201 0.005 0.002 0.00427 0.00300 4 Mergapan 0.031 0.046 0.02214 0.00213 0.005 0.012 0.00105 0.00190 5 Shwan _chmchamal 0.022 0.029 0.02334 0.00195 0.006 0.003 0.00166 0.00115 6 Bakrajo 0.025 0.004 0.03474 0.00184 0.007 0.006 0.00179 0.00210 7 Kani panka S1 0.057 0.014 0.01360 0.00415 0.001 0.046 0.00215 0.00331 8 Kani panka S2 0.016 0.032 0.02377 0.00120 0.004 0.001 0.00158 0.00393 9 Shakhasur 0.017 0.026 0.02286 0.00117 0.004 0.001 0.00275 0.00104 10 Sharbazher tagaran 0.014 0.026 0.01256 0.00111 0.004 0.03110 0.00569 0.00211 11 Krbchna 1 0.045 0.037 0.02890 0.00166 0.001 0.00164 0.00244 0.00664 12 Krbchna 2 0.023 0.016 0.03490 0.00156 0.005 0.00532 0.00530 0.00332 13 Khwrmal S1 0.033 0.039 0.02225 0.00174 0.003 0.00131 0.00353 0.00091 14 Bnawela 0.002 0.023 0.01124 0.00190 0.002 0.00210 0.00231 0.00100 15 Sitak 0.013 0.039 0.01560 0.00138 0.037 0.00313 0.00174 0.00125 16 Qarachatan 0.010 0.014 0.01856 0.00112 0.001 0.00210 0.00171 0.00210 17 Khwrmal S2 0.013 0.038 0.01530 0.00110 0.001 0.00132 0.00217 0.00132 18 Byara S2 0.007 0.002 0.01260 0.00200 0.002 0.00142 0.00132 0.00142 19 Awsar 0.024 0.023 0.01220 0.00416 0.004 0.00673 0.00388 0.00273 20 Tapatolaka 0.029 0.034 0.01490 0.00125 0.006 0.00598 0.00129 0.00218 21 Rain water 0.022 0.033 0.02230 0.00118 0.003 0.00031 0.00140 0.00031 22 Kani sard 0.019 0.035 0.01410 0.00108 0.003 0.00104 0.00138 0.00144 23 Bakrajo Tap water 0.003 0.039 0.01530 0.00196 0.002 0.00091 0.00126 0.00091 24 Shene 0.016 0.034 0.01250 0.00110 0.002 0.00560 0.00135 0.05600 Table 3: Water heavy metals analysis Acta agriculturae Slovenica, 121/2 – 2025 5 Water quality effects on germination of okra seed (Abelmoschus esculentus L.) to measure the pH of the water sample, and an EC me- ter (HI981311) was employed to determine the electrical conductivity, following the standard methods described in the APHA (1998) guidelines for water quality analysis. 2.3.2 Cation and anion analysis The concentrations of various cations calcium (Ca²+), magnesium (Mg²+), potassium (K+), and sodium (Na+)) and anions carbonate (CO₃²-, bicarbonate (HCO₃- ), sulfate (SO₄²-), nitrate (NO₃-), and chloride (Cl-)) were measured to assess the chemical composition of the wa- ter. 2.3.3 Heavy metal concentration analysis The concentrations of heavy metals, including cobalt (Co²+), copper (Cu²+), iron (Fe²+), manganese (Mn²+), zinc (Zn²+), chromium (Cr²+), cadmium (Cd²+), and nickel (Ni²+), were determined using a Shimadzu ICP-9820 inductively coupled plasma atomic emission spectrometer (ICP-AES), made in Japan, which is ca- pable of detecting trace amounts of these metals in the water. The results from these analyses are summarized in Table 3. 2.4 GERMINATION RATIO CALCULATIONS A germination assessment is often the most reliable method to evaluate whether a seed is ready for planting. For this particular test, local varieties of okra seeds were used. Germination in these seeds typically begins after approximately 4 days, provided that the seeds are kept under optimal temperature and humidity conditions. The germination rate can be calculated using a specific equation, which helps to quantify the proportion of seeds that successfully sprout. The data collected during this experiment is summarized in Table 4, where the calcu- lated germination ratio is recorded for each observation. This test is essential for determining the viability of the seeds before planting. ………………………… (1) 2.5 IRRIGATION WATER QUALITY CALCULA- TION 2.5.1 Irrigation water quality calculation according to modified SIWi 2023 (Marif and Esmael, 2023) The irrigation water quality calculation, according to the modified SIWi 2023 as modified by (Marif and Es- mael, 2023), involves a detailed analysis of several water quality parameters, including salinity, pH, sodium, chlo- ride, and other essential factors that affect crop growth and soil health. This method incorporates updated thresholds and classifications to assess the suitability of water for irrigation, ensuring its compatibility with spe- cific soil types and crop needs. In this context, the quality of irrigation water is categorized based on these criteria, which are then cross-referenced with the standards listed in Table 5 of the modified SIWi 2023. This table provides a classification system that ranks water quality into dif- ferent categories, helping to determine whether the wa- ter is suitable for different agricultural purposes, these calculations and classifications are critical for managing Table 4: Germination ratio of the study area No Location Germination Ratio % 1 Kani Ababaile 88.3 2 Well ababaile 90 3 Kani Faqe Byara S1 86.5 4 Mergapan 87.0 5 Shwan _chmchamal 85 6 Bakrajo 88 7 Kani panka S1 81.7 8 Kani panka S2 80 9 Shakhasur 83.0 10 Sharbazher tagaran 85.0 11 Krbchna 1 86.67 12 Krbchna 2 88.3 13 Khwrmal S1 81.0 14 Bnawela 82.0 15 Sitak 80.0 16 Qarachatan 83.3 17 Khwrmal S2 79 18 Byara S2 83.0 19 Awesar 91.7 20 Tapatolaka 88.3 21 Rain water 92 22 Kani sard 83.3 23 Bakrajo Tap water 88.3 24 Shene 87.0 Acta agriculturae Slovenica, 121/2 – 20256 A. A. MARIF irrigation practices, preventing soil degradation, and maximizing crop yield. 2.6 DATA ANALYSIS The data were analyzed using XLSTAT 2019.2.2.59614, a comprehensive statistical software tool. Principal Component Analysis (PCA) was applied to reduce the dimensionality of the data while retaining its most significant features, helping to uncover patterns and structure in complex datasets. Agglomerative Hi- erarchical Clustering (AHC) was also utilized to group similar data points based on their characteristics, allow- ing for the identification of distinct clusters or patterns within the data. Additionally, correlation analysis was performed to examine the relationships between vari- ous variables, helping to understand the strength and di- rection of their associations. Together, these analytical methods provided a thorough exploration of the data, generating valuable insights for further interpretation and decision-making. 3 RESULTS AND DISCUSSIONS 3.1 CLASSIFICATION OF WATER RESOURCES ACCORDING TO MODIFIED SIWI (MARIF & ESMAEL, 2023) The study results classify the water resources into No Location IWQI Classes 1 kani Ababaile 92.1 Excellent 2 Well Ababaile 93.8 Excellent 3 kani Faqe Byara S1 93.1 Excellent 4 Mergapan 90.9 Good 5 Shwan _chmchamal 91.4 Excellent 6 Bakrajo 89.7 Good 7 kani panka S1 84.4 Good 8 kani panka S2 92.4 Excellent 9 Shakhasur 94.0 Excellent 10 sharbazher tagaran 93.3 Excellent 11 Krbchna 1 86.4 Good 12 Krbchna 2 91.5 Excellent 13 Khwrmal S1 85.5 Good 14 Bnawela 93.8 Excellent 15 Sitak 92.3 Excellent 16 Qarachatan 94.7 Excellent 17 khwrmal S2 92.5 Excellent 18 Byara S2 96.0 Excellent 19 Awesar 94.9 Excellent 20 Tapatolaka 92.5 Excellent 21 Rain water 95.0 Excellent 22 kani sard 96.5 Excellent 23 Bakrajo Tap water 96.3 Excellent 24 Shene 91.4 Excellent No Location Classes 1 kani ababaile Suitable for Irrigation 2 well ababaile Suitable for Irrigation 3 kani faqe byara s1 Suitable for Irrigation 4 Mergapan Suitable for Irrigation 5 shwan _chmchamal Suitable for Irrigation 6 Bakrajo Suitable for Irrigation 7 kani panka s1 Suitable for Irrigation 8 kani panka s2 Suitable for Irrigation 9 Shakhasur Suitable for Irrigation 10 sharbazher tagaran Suitable for Irrigation 11 krbchna 1 Suitable for Irrigation 12 krbchna 2 Suitable for Irrigation 13 khwrmal s1 Suitable for Irrigation 14 Bnawela Suitable for Irrigation 15 Sitak Suitable for Irrigation 16 Qarachatan Suitable for Irrigation 17 khwrmal s2 Suitable for Irrigation 18 byara s2 Suitable for Irrigation 19 Awesar Suitable for Irrigation 20 Tapatolaka Suitable for Irrigation 21 rain water Suitable for Irrigation 22 kani sard Suitable for Irrigation 23 bakrajo tap water Suitable for Irrigation 24 Shene Suitable for Irrigation Table 6: Irrigation water quality classification according (Todd,1966) Table 5 Irrigation water quality calculation according to modi- fied SIWi 2023(Marif and Esmael, 2023) Acta agriculturae Slovenica, 121/2 – 2025 7 Water quality effects on germination of okra seed (Abelmoschus esculentus L.) two distinct quality categories based on the Irrigation Water Quality Index (IWQI). Nineteen of the resources were categorized as “Excellent” for irrigation, demon- strating IWQI values above 90, with individual values ranging from 91.4 to 96.5, indicating that these water sources are highly suitable for agricultural use. These resources, spread across various locations (1, 2, 3, 5, 8, 9, 10, 12, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, and 24), exhibit optimal quality for irrigation, as reflected in their consistently high IWQI scores. In contrast, five water sources (locations 4, 6, 7, 11, and 13) were classified as “Good,” with IWQI values between 70 and 90, indicating that they are still suitable for irrigation but with slightly lower quality compared to the “Excellent” category. These lower IWQI scores correspond to higher electrical con- ductivity (EC) values, as seen in the data, with EC emerg- ing as a key factor influencing water quality. Specifically, the study found that water resources with lower EC val- ues tended to have higher IWQI scores, while those with higher EC values showed lower IWQI values. This pat- tern is consistent with findings from Dhaoui et al. (2023) and Benaafi et al. (2024), which also identified a strong correlation between EC levels and IWQI, underlining the critical role of EC in evaluating the suitability of water for irrigation purposes. This classification provides valuable insights into the variability of water quality across differ- ent locations and highlights the importance of monitor- ing EC as a predictor of irrigation water suitability. 3.2 CLASSIFICATION OF WATER RESOURCES ACCORDING TO ACCORDING (TODD,1966) Water classification results indicated that all water resources (1, 2, 3, 4, ... to 24) were initially considered suitable for irrigation, with no variation observed across the resources. However, upon comparing the findings to the classification framework proposed by Todd (1966), it was evident that recent studies have led to significant changes in water classification due to the inclusion of ad- ditional parameters and updated models for calculating the Irrigation Water Quality Index (IWQI). These chang- es in classification can be attributed to the introduction of more comprehensive criteria for assessing water quali- ty, which in turn influenced the classification of water re- sources. The results presented in Table 6 align with recent research conducted by Mahammad and Islam (2024), as well as Laaraj et al. (2024), which highlights the evolv- ing nature of water classification models as they adapt to new data and methodologies. This shift underscores the importance of using more advanced and detailed models to accurately reflect the quality and suitability of water resources for irrigation purposes, as these models pro- vide a more nuanced understanding of water quality and its potential impact on agricultural practices. 3.3 CLASSIFICATION OF WATER RESOURCES ACCORDING TO CATIONS AND ANIONS USING PRINCIPAL’S COMPONENT ANALYSIS PCA The classification of 24 water resources based on their cation and anion content using Principal Compo- nent Analysis (PCA) reveals significant insights into wa- ter quality variations across different locations. As shown in Figure 2, the water resources are divided into seven distinct classes, each represented by a unique shape. Class 1, depicted by a left arrow shape, corresponds to water resource number 13. Class 2, represented by a north arrow shape, includes water resource number 11. Class 3, with a circle shape, includes water resources 4 and 17. Class 4, represented by a pentagon shape, is as- signed to water resource number 20. Class 5, with a cyl- inder shape, corresponds to water location number 19. Class 6, represented by a triangle shape, groups water resources 22, 23, and 24. Finally, Class 7, depicted by a square shape, includes a broad range of water locations, including 1, 2, 3, 5, 6, 7, 8, 9, 10, 12, 14, 15, 16, 18, and 21. PCA analysis indicates that Factor 1 (F1) accounts for 48.17 % of the variation in water classification, while Fac- tor 2 (F2) explains 14.53 %, together making up 62.70 % of the total variance. These findings are consistent with recent studies by Hammoumi et al. (2024), Arıman et al. (2024), and Ali et al. (2024), which similarly applied PCA to classify water resources, highlighting the effectiveness of this statistical approach in understanding water qual- ity and variability across different regions. This analysis emphasizes the substantial influence of the first factor (F1), suggesting that cation-anion concentrations are the primary determinants in classifying water resources. 3.4 CLASSIFICATION OF WATER RESOURCES ACCORDING TO CATIONS AND ANIONS USING AGGLOMERATIVE HIERARCHICAL CLUSTERING (AHC) The classification of water resources according to their cation and anion concentrations using Agglom- erative Hierarchical Clustering (AHC) provides a struc- tured approach to grouping water samples based on their chemical composition. As shown in Table 7 and Figure 3, the AHC analysis divided the water resources into five distinct classes. Class 1, which includes 16 water resourc- es (locations 1, 2, 3, 7, 8, 9, 10, 16, 17, 18, 19, 20, 21, 22, Acta agriculturae Slovenica, 121/2 – 20258 A. A. MARIF 23, and 24), exhibited relatively low variation in terms of ion concentration. In contrast, Classes 2 and 3 each included fewer resources, with Class 2 comprising only locations 4 and 6, and Class 3 encompassing resources 5, 12, 14, and 15. Both Class 4 and Class 5 contained only one water resource each, located at positions 11 and 13, respectively. The lower variation observed in Classes 1 and 3 suggests a more homogeneous ionic composition, whereas the higher variation in Classes 4 and 5 can be at- tributed to the greater influence of electrical conductivity (EC), which likely caused more significant differentiation in the clustering. The impact of EC on water classifica- tion is well-documented in previous studies (Marif and Esmail, 2023; Mishra et al., 2023; Djaafri et al., 2024), supporting the findings of this research. This clustering technique thus underscores the complex interplay of cations, anions, and EC in determining the quality and characteristics of water resources. 3.5 CLASSIFICATION OF WATER RESOURCES ACCORDING TO HEAVY METAL CONTENTS USING PRINCIPAL’S COMPONENT ANALYSIS PCA The classification of water resources based on heavy metal content using Principal Component Analysis (PCA) offers a comprehensive approach to understand- ing the variability and quality of water bodies in relation to pollutants. In this study, 24 water resources were cat- egorized into six distinct classes according to their heavy metal profiles, as demonstrated in Figure 4. These classes are represented by different geometric shapes, each cor- responding to specific water resource locations. Class 1, marked by a circle, includes water resources at locations 6 and 12, while Class 2, represented by a north arrow, encompasses resources at locations 5, 3, 8, 9, 11, 13, 16, and 21. Class 3, shown with a rectangular shape, includes resources at locations 1, 2, 4, 14, 15, 17, 18, 20, 22, and 23. Class 4, marked by a pentagon, represents locations 10 and 19, while Class 5, identified by a triangle, cor- responds to location 7. Finally, Class 6, represented by a cylinder shape, is composed of resource 24. The PCA results, as depicted in Figure 2, show that the first factor (F1) accounts for 26.68% of the total variability affect- ing water classification, while the second factor (F2) con- tributes 16.59%. Together, these factors explain 43.28 % of the variance in the water classification, highlighting the significant influence of heavy metal content on wa- ter quality. These findings align with previous research by Hammoumi et al. (2024) and Arıman et al. (2024), validating the effectiveness of PCA in classifying water Figure 2: Classification of water resources according to cations and anions using principal’s component analysis PCA Classes Class 1 Class 2 Class 3 Class 4 Class 5 Number of classes 16 2 4 1 1 Water Resources or Locations 1, 2, 3, 7, 8, 9, 10, 16, 17, 18, 19, 20, 21, 22, 23 and 24 4 and 6 5, 12, 14, and 15 11 13 Table 7: Classification of water resources according to cations and anions using agglomerative hierarchical clustering (AHC) Figure 3: Classification of water resources according to cations and anions using agglomerative hierarchical clustering (AHC) Acta agriculturae Slovenica, 121/2 – 2025 9 Water quality effects on germination of okra seed (Abelmoschus esculentus L.) resources based on their contamination levels. This anal- ysis underscores the importance of understanding the principal factors contributing to water quality variations and their implications for environmental monitoring and management. 3.6 CLASSIFICATION OF WATER RESOURCES ACCORDING TO HEAVY METAL CONTENTS USING AGGLOMERATIVE HIERARCHICAL CLUSTERING (AHC) The classification of water resources based on heavy metal contents, utilizing Agglomerative Hierarchical Clustering (AHC), groups the water sources into nine distinct classes, as shown in Table 8 and Figure 5. Class 1, which includes water sources 1, 3, 5, 8, 9, 17, 21, 22, and 23, represents the largest cluster with nine water re- sources. Class 2, containing four locations (2, 14, 16, and 19), and Class 3, which includes locations 4, 11, 13, and 20, each contain four water resources. Class 4, consisting of only two locations (6 and 12), demonstrates a more limited variation in heavy metal content. In contrast, Classes 5, 6, 7, 8, and 9 are more distinct, each contain- ing a single water resource—specifically, water sources 7, 10, 15, 18, and 24, respectively. The classification shows low variability in heavy metal concentrations for Class 1 and Class 3, which are likely influenced by similar en- vironmental or anthropogenic factors, while a greater degree of variability is observed in Classes 5 through 9. This greater variation can be attributed to factors such as electrical conductivity (EC), which significantly impacts water quality classification by affecting the solubility and mobility of heavy metals in aquatic environments. These findings align with previous studies by Marif and Esmail (2023) and Mohsine et al. (2023), confirming that clustering based on heavy metal content provides a reli- able method for assessing water quality, revealing both regional differences and the influence of chemical pro- cesses on water resources. 3.7 CORRELATION COEFFICIENT BETWEEN PH, EC, IWQI AND GERMINATION RATIO The correlation analysis presented in Tables 4 and 9 reveals intriguing insights into the relationships between Figure 4: Classification of water resources according to heavy metal contents using principal’s component analysis PCA Classes Class 1 Class 2 Class 3 Class 4 Class 5 Class 6 Class 7 Class 8 Class 9 Number of classes 9 4 4 2 1 1 1 1 1 Water resources or Locations 1, 3, 5, 8, 9, 17, 21, 22, and 23 2, 14, 16, and 19 4, 11, 13, and 20 6 and 12 7 10 15 18 24 Table 8: Classification of water resources according to cluster analysis of heavy metal contents Figure 5: Classification of water resources according to heavy metal contents using agglomerative hierarchical clustering (AHC) Acta agriculturae Slovenica, 121/2 – 202510 A. A. MARIF pH, electrical conductivity (EC), irrigation water quality index (IWQI), and germination ratio. Notably, the study found a positive but non-significant relationship between the germination ratio and IWQI, with a correlation coef- ficient (r) of 0.218, suggesting that although IWQI may have some influence on germination, its effect is weak and not statistically meaningful (Lal et al., 2024). Addition- ally, a similarly weak but negative correlation between pH and the germination ratio (-0.157), and EC and the germination ratio (-0.196), indicates that as pH and EC increase, there is a slight decrease in the germination ra- tio. However, these correlations are also non-significant, implying that other factors may be influencing the ger- mination rate more strongly. A more robust and signifi- cant negative correlation was observed between EC and IWQI, with an r value of -0.727, which implies a strong inverse relationship. This suggests that as EC (a measure of salinity) increases, the overall quality of irrigation wa- ter as indicated by the IWQI declines. This negative sig- nificant relationship is critical because high EC typically denotes saline water, which can have detrimental effects on plant growth and germination. In summary, while the correlations between pH, EC, and germination ratio are weak and non-significant, the strong negative relation- ship between EC and IWQI underscores the importance of monitoring EC levels in maintaining irrigation water quality and optimizing germination success. 3.8 EFFECTS OF WATER QUALITY ON GERMINA- TION RATIO The data presented in Tables 10 and 4 provides valu- able insights into the relationship between water quality and the germination ratio of okra seeds. The maximum germination ratio recorded was 92  %, observed under excellent water quality conditions with an electrical con- ductivity (EC) of 0.34 dS m-¹ and a standard deviation of 3.72. In contrast, the minimum germination ratio of 79 % was observed at a slightly higher EC of 0.5 dS m-¹, accompanied by the same standard deviation, indicating that even small variations in EC can influence seed ger- mination. This decline in germination is likely due to the combined effects of EC and pH on water quality, which have been shown to impact the osmotic potential and the uptake of water by seeds, ultimately affecting their abil- ity to sprout. Higher EC levels can cause osmotic stress, making it more difficult for the seed to absorb sufficient water, which is crucial for the germination process. This aligns with the findings of Seymen et al. (2023), Singh et al. (2023), and Nautiyal et al. (2023), who demonstrated that water quality parameters such as EC and pH are critical factors in seed viability and germination. In this study, the mean values for pH, EC, and IWQI (Irrigation Water Quality Index) were 7.19, 0.66 dS m-1, and 92.28, respectively, indicating that maintaining water quality within optimal ranges is essential for maximizing germi- nation rates and ensuring successful crop establishment. 3.9 RELATION BETWEEN GERMINATION RATIO AND EC DS M-1 Figure 6 illustrates the inverse relationship be- tween the germination ratio and electrical conductiv- ity (EC, measured in dS m-1), showing a significant negative correlation. As EC increases, the germina- tion ratio decreases dramatically, which can be at- tributed to the detrimental effects of high salinity on seed germination. Electrical conductivity in soil is a direct measure of its salinity, and when the EC is high, it indicates that the soil solution has a higher concen- tration of dissolved salts. These salts can create an os- motic pressure that reduces the availability of water to seeds, impairing their ability to absorb water and thus hindering the germination process. This negative rela- tionship is supported by the correlation coefficient (r = -0.07), which highlights the weak yet consistent in- verse trend between EC and germination. These find- ings align with those of Hossain et al. (2023) and Na- her et al. (2024), who also observed similar impacts of salinity on seed germination. High salinity can induce Variables pH EC dS m-1 IWQI Germina- tion Ratio pH 1 EC dS m-1 -0.012 1 IWQI -0.322 -0.727 1 Germination Ratio -0.157 -0.196 0.218 1 Table 9: Correlation between pH, EC, IWQI and germination ratio Variable Observa- tions Mini- mum Maxi- mum Mean Std. deviation PH 24 7.1 7.4 7.19 0.01 EC 24 0.26 1.2 0.66 0.40 IWQI 24 84.43 96.55 92.28 3.18 Germina- tion Ratio 24 79 92 85.36 3.72 Table 10: Summary of water quality effect on germination ratio Acta agriculturae Slovenica, 121/2 – 2025 11 Water quality effects on germination of okra seed (Abelmoschus esculentus L.) physiological stress in seeds, affecting enzyme activ- ity, cell membrane integrity, and nutrient uptake, all of which are essential for successful germination and early seedling development. 3.10 RELATION BETWEEN GERMINATION RATIO AND IRRIGATION WATER QUALITY INDEX (IWQI) Figure 7 illustrates a positive correlation between germination ratio and the Irrigation Water Quality Index (IWQI), demonstrating that as the germination ratio increases, so does the IWQI, indicating better water quality. This relationship suggests that higher IWQI values, which reflect cleaner, more suitable wa- ter for irrigation, promote better seed germination and overall plant growth. Conversely, a decrease in IWQI corresponds to lower germination ratios, high- lighting the detrimental effects of poor water quality on seedling establishment. This finding is consistent with previous studies, such as those by Marif and Es- mail (2023) and Mezlini et al. (2024), which empha- size the significant role of water quality in agricultural productivity. Poor-quality irrigation water, character- ized by high salinity, contamination, or imbalanced nutrient content, can impede seedling growth by cre- ating osmotic stress, altering nutrient availability, or introducing toxic compounds, all of which negatively affect germination. Thus, maintaining a high IWQI is critical for ensuring successful crop establishment and maximizing agricultural yields. 4 CONCLUSIONS The study of irrigation water quality (IWQ) from various locations or water sources reveals significant varia- tions in water quality parameters, with conductivity being one of the most influential factors. Electrical conductiv- ity (EC) serves as an indicator of the ion concentration in water, reflecting the level of dissolved salts or minerals. In agricultural practices, water with high EC values can lead to salinity stress, which adversely affects plant growth and seed germination. Conversely, water with lower EC values, indicating fewer dissolved salts, tends to be more favorable for seedling establishment and plant growth. The observed variations in water quality across different sources can thus be attributed to the local environmental conditions, such as soil composition and water sources, which influence the ion concentrations and overall quality of irrigation water. Furthermore, the study demonstrates a positive cor- relation between irrigation water quality and the germina- tion rate of okra seeds. As the IWQ index increases, par- ticularly in relation to lower EC values, the germination ratio of okra seeds also increases. This suggests that water with lower salt concentrations provides a more conducive environment for seed sprouting, likely due to reduced os- motic stress and enhanced water uptake. High-quality irri- gation water, characterized by low EC values, ensures that seeds receive the optimal conditions necessary for proper germination, leading to higher success rates in seedling emergence. This finding underscores the importance of maintaining high-quality water for irrigation to promote healthy crop development and improve agricultural pro- ductivity. Therefore, the results highlight that managing Figure 6: Relation between germination ratio and EC dS m-1 Figure 7: Relation between germination ratio and IWQI Acta agriculturae Slovenica, 121/2 – 202512 A. A. MARIF water salinity, by monitoring and controlling EC levels, is crucial for optimizing crop germination and growth. 5 REFERENCES Ahmad, T., Muhammad, S., Umar, M., Azhar, M. U., Ahmed, A., Ahmed, A., & Ullah, R. (2024). Spatial distribution of physicochemical parameters and drinking and irrigation water quality indices in the Jhelum River, Pakistan. Envi- ronmental Geochemistry and Health, 46(8), 263. Ali, S., Verma, S., Agarwal, M. B., Islam, R., Mehrotra, M., Deo- lia, R. K., . . . Raj, D. (2024). 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