Spatial distribution and hydrogeochemical evaluations of groundwater and its suitability for drinking and irrigation purposes in kaligonj upazila of satkhira district of Bangladesh

被引:2
|
作者
Jamal, A. H. M. Shofiul Islam Molla [1 ]
Jhumur, Nisat Taslum [1 ]
Shaikh, Md Aftab Ali [2 ,3 ]
Moniruzzaman, Mohammad [4 ]
Uddin, Md Ripaj [1 ]
Siddique, Md Abu Bakar [1 ]
Al-Mansur, Muhammad Abdullah [1 ]
Akbor, Md Ahedul [1 ]
Tajnin, Jahan [1 ]
Ahmed, Sharmin [1 ]
Mahmud, Rashed [1 ]
机构
[1] Inst Natl Analyt Res & Serv INARS, Bangladesh Council Sci & Ind Res BCSIR, Dhaka 1205, Bangladesh
[2] Univ Dhaka, Dept Chem, Dhaka 1000, Bangladesh
[3] Bangladesh Council Sci & Ind Res BCSIR, Dhaka 1205, Bangladesh
[4] Bangladesh Council Sci & Ind Res BCSIR, Cent Analyt & Res Facil CARF, Dhaka 1205, Bangladesh
关键词
Hydrochemistry; Salinity; Multivariate statistical analysis; Irrigation suitability; Water quality index; Spatial distribution; MULTIVARIATE STATISTICAL TECHNIQUES; POSITIVE MATRIX FACTORIZATION; WATER-QUALITY ASSESSMENT; FINE PARTICULATE MATTER; SOURCE APPORTIONMENT; RIVER-BASIN; ATMOSPHERIC AEROSOL; COASTAL BANGLADESH; BOTTOM SEDIMENTS; KHULNA DISTRICT;
D O I
10.1016/j.heliyon.2024.e27857
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Groundwater is a significant water resource for drinking and irrigation in Satkhira district, Bangladesh. The depletion of groundwater resources and deterioration in its quality are the results of the confluence of factors such as industrialization, intensive irrigation, and rapid population growth. For this reason, this study focused on the evaluation of tubewell water of six unions of Kaligonj upazila in Satkhira district, which is situated in the coastal southwest part of Bangladesh. Major and trace elemental concentrations were assimilated into positive matrix factorization (PMF) to identify potential sources and their respective contributions. Principal component analysis (PCA) revealed that groundwater salinization and manmade activities were the primary causes of heavy metals in the coastal groundwater. Its average pH value was found to be 7.5, while Dissolved oxygen, Total dissolved solids, salinity, and conductivity, with values ranging from 1.18 to 7.38 mg/L, 0.5 - 4.88 g/L, 0.4 - 5%, and 0.95 to 8.56 mS/cm, respectively. The total hardness average value was 561.7 mg/L, classified into the very hard water categories, which is why 90% of the tubewell water samples were unfit for household purposes. All samples had an excessive level of arsenic present. The iron concentration of fifteen (15) samples crossed the standard limit according to WHO 2011 value. Around 63% of the samples were of the Na + -K + - Cl - -SO 4 2- type, and about 72% were sodium -potassium and alkali types. 98% of samples were covered in chloride and bicarbonate. The findings showed that 45.83% of the groundwater samples had negative Chloroalkaline index (CAIs), while 54.16% had positive. The permeability index (PI) was an average of 73%, and residual sodium carbonate (RSC) averaged 260.2 mg/L, and the findings clearly showed that 80% of the samples weren ' t appropriate for irrigation. According to the sodium adsorption ratio (SAR) value, 65% of the samples fell into the unsuitable category. These calculations indicated a high overall salinity hazard in the study area, which may be caused by the intrusion of sea water given that the study area is close to the coastal region. Findings compared to standards revealed that the majority of the samples were deemed unfit for drinking and irrigation purposes. Hence, additional attention must be paid to this area to ensure the availability of drinkable water and to preserve sustainable farming practices.
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页数:25
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