scholarly journals Groundwater Assessment and its Implication for Irrigation in Selected Coastal Areas of South-Western Nigeria

Author(s):  
Adeyeye J.A ◽  
Akinyemi O.D ◽  
Akinluyi F.O ◽  
Abiola M.O ◽  
Badmus G. O

Physicochemical and ionic characteristics of groundwater aquifers have been of tremendous importance in water applications. Groundwater in selected coastal communities (Badagry, Epe, Ikorodu, and Ilaje/ese-odo) of south-western Nigeria was assessed for domestic and irrigation suitability. One hundred and ninety-two (192) groundwater samples were obtained and analyzed for chemical composition and major ionic ratio over a period of four seasons using standard methods. Results indicated abundance of ions in the order HCO3– > Cl–> SO42– for anions, and K+ > Na+ > Ca2+> Mg2+ for cations. Piper's diagram revealed calcium (Ca2+) and magnesium (Mg2+) as the dominant cations, while sulphate and chloride were the dominant anions with a mixture of two major groundwater types: Ca–Cl water and mixed Ca–Mg–Cl. The presence of Ca–Cl facies water type suggests potential ion exchange (Na2+ with Ca2+) reaction in these coastal aquifers. Cation exchangeable values (CEV), and molar ratios of Mg/Ca, HCO3/Cl, and Na/Cl, showed high values (>1) across all locations indicating the occurrence of saline water ingression in groundwater samples, especially during the dry spell. The increasing K+, Na+, and Cl– characteristics of the groundwater and calculated ionic indices values indicated the influence of seawater intrusion. However, total hardness values showed that the samples were very soft in nature. Irrigation water quality suitability, as indicated by sodium adsorption ratio (SAR), permeability index (PI), and percentage sodium (PS) varied with seasons and location, showing that water will cause soil deterioration and poor crop performance if intensively used for irrigation without proper precautions.

2020 ◽  
Vol 55 (4) ◽  
pp. 245-252
Author(s):  
C Ogwah ◽  
MO Eyankware

A detail understanding of the hydrogeochemical characteristics and groundwater quality is indispensable for the sustainable utilization of the groundwater sources. This is in line with sustainable development goal of United Nation. The following parameters were analyzed using APHA, 2012 standard: pH, Ec, total dissolved solid (TDS,) total hardness (TH), magnesium (Mg2+), sulphate (SO4 2¯), chloride (Cl¯), bicarbonate (HCO3¯), carbonate (CO3 2¯), nitrate (NO3¯), potassium (K+), sodium (Na2+)and calcium (Ca2+). Findings revealed that pH value reveals that groundwater is acidic. Bivariate plots showed that groundwater quality is influenced by number of factors. Hydrogeochemical assessment of groundwater samples was based on the following model:End-member, Parson’s and Diamond field plots. Results from these plots revealed that silicate and carbonate weathering are the major factors that control groundwater quality and that groundwater samples were of different water type namely, Ca–Mg–SO4, Ca–Mg–Cl, Na–SO4 water type and high Ca+Mg & SO4+Cl respectively. It was observed that 99 % of groundwater within the study area fell within fresh water category and groundwater is influenced by various factors. Bangladesh J. Sci. Ind. Res.55(4), 245-252, 2020


2020 ◽  
Vol 4 (1) ◽  
pp. 12-16
Author(s):  
C. Ogwah ◽  
M. O. Eyankware

A detail understanding of the hydrogeochemical characteristics and groundwater quality is indispensable for the sustainable utilization of the groundwater sources. This is in line with Sustainable development goal of United Nation. The following parameters were analyzed using APHA, 2012 standard: pH, Ec, total dissolved solid (TDS,) total hardness (TH), magnesium (Mg2+), sulphate (SO42¯), chloride (Cl¯), bicarbonate (HCO3¯), carbonate (CO32¯), nitrate ( NO3¯), potassium (K+), sodium (Na2+) and calcium (Ca2+). Findings revealed that pH value reveals that groundwater is acidic. Bivariate plots showed that groundwater quality is influenced by number of factors. Hydrogeochemical assessment of groundwater samples was based on the following model: End-member, Parson’s and Diamond field plots. Results from these plots revealed that that silicate and carbonate weathering are that major factor that control groundwater quality, and that groundwater samples were of different water type namely; Ca–Mg–SO4, Ca–Mg–Cl, Na–SO4 water type and high Ca + Mg & SO4 + Cl respectively. It was observed that 99 % of groundwater within the study area fell within fresh water category and groundwater is influenced by various factors such as weathering.


2010 ◽  
Vol 7 (3) ◽  
pp. 1033-1039 ◽  
Author(s):  
P. N. Palanisamy ◽  
S. K. Kavitha

Groundwater samples were collected in Erode city, Tamilnadu, from an area having large number of textile dyeing units. Though people residing in this area use river water supplied by local bodies as their major source for drinking, groundwater is also used as complementary source. The samples collected were subjected to systematic analysis using the standard methods and procedures. The values obtained for different physicochemical parameters were compared with the standard values given by ISI/ WHO. Variations in many physicochemical parameters were observed for most of the samples when compared to the standard values. More than half of the samples collected had their EC, TDS, total hardness, calcium, magnesium, sulphate and chloride exceeding their acceptable limits. This attempt has been made to determine the quality of groundwater in the study area confirms the deterioration of groundwater quality in the area and calls for some effective measures to be taken urgently to minimize the adverse impacts that may occur due to the contamination of groundwater.


Irriga ◽  
2006 ◽  
Vol 11 (3) ◽  
pp. 428-440
Author(s):  
Tales Miler Soares ◽  
Sergio Nascimento Duarte ◽  
Cristiano Nascimento Duarte ◽  
Christiano César Dibbern Graf ◽  
Marcelo Zanetti ◽  
...  

IRRIGAÇÃO DE PORTA-ENXERTOS CÍTRICOS COM ÁGUAS SALINAS  Tales Miler Soares1; Sergio Nascimento Duarte1; Christiano César Dibbern Graf2; Marcelo Zanetti2; Silvio Sandoval Zocchi31Departamento de Engenharia Rural, Escola Superior de Agricultura Luiz de Queiroz, Universidade de São Paulo, Piracicaba, SP, [email protected] Mudas, Conchal,  SP3Departamento de Ciências Exatas, Escola Superior de Agricultura Luiz de Queiroz, Universidade de São Paulo, Piracicaba, SP  1 RESUMO Avaliar o desenvolvimento dos porta-enxertos limoeiro ‘Cravo’, tangerineira ‘Cleópatra’ e citrumeleiro ‘Swingle’, irrigados com águas salinas, mensurando se a aplicação de Ca(NO3)2 mitiga eventuais efeitos de íons fitotóxicos, foi objetivo do presente trabalho, conduzido sob ambiente protegido, em Rio Claro-SP. Investigou-se três qualidades de água: água natural (CEa= 1,19 dS m-1), explorada de poço tubular profundo, água dessalinizada (CEa= 0,02 dS m-1), obtida mediante osmose reversa da água natural, e água residual (CEa= 2,11 dS m-1), sub-produto da dessalinização. Os níveis de Ca(NO3)2 avaliados foram 0 e 2,105 g L-1. Averiguando-se os parâmetros usuais do crescimento vegetal, não foram observadas diferenças estatísticas, entre os tratamentos, decorrentes da qualidade da água, embora se tenha registrado que esta contribuiu para o aumento da salinização do substrato, ultrapassando, inclusive, o valor da salinidade limiar (CEes= 1,4 dS m-1) reconhecido para os citros. A adição de Ca(NO3)2 não incrementou o desenvolvimento, atuando negativamente no crescimento inicial das raízes e do caule. O curto período necessário ao crescimento dos porta-enxertos, proporcionado pelo atual sistema de produção, associado às irrigações freqüentes e suas frações de lixiviação podem ter restringido efeitos negativos das águas salinas investigadas. UNITERMOS: Citrus, salinidade, condutividade elétrica, substrato.  SOARES, T.M.; DUARTE, S.N.; GRAF, C.C.D.; ZANETTI, M.; ZOCCHI, S.S.       CITRUS ROOTSTOCKS IRRIGATION WITH SALINE WATER  2 ABSTRACT This research aimed to evaluate the growth of three citrus rootstocks (‘Rangpur’ lime, ‘Cleopatra’ mandarin and ‘Swingle’ citrumelo) irrigated with saline waters, under greenhouse conditions, in order to measure if calcium nitrate mitigates their toxic effects. Three water qualities were investigated: natural water (ECw= 1,19 dS m-1), obtained from a deep tubular well, desalinated water (ECw= 0,02 dS m-1), obtained by reverse osmosis from the natural water, and reject water (ECw= 2,11 dS m-1), resultant from the desalination process. Two Ca(NO3)2 levels were evaluated: 0 and 2,105 g L-1. Usual parameters for plant growth analysis were measured. According to Tukey’s test (5% probability), water quality did not affect rootstocks development, although the water type have contributed to increase the electrical conductivity of substrate saturation extract (ECs) along the experimental period, surpassing the salinity threshold value (ECs = 1,4 dS m-1) reported for citrus. The Ca(NO3)2 addition did not increase the plant growth, but negatively affected the first evaluations of root and stem diameter development. The short time necessary to rootstocks growth provided by new production system, associated to the frequent irrigations and its leaching fractions possible may have restricted the negative effects of saline waters. KEYWORDS: Citrus, salinity, electrical conductivity, substrate.  


2019 ◽  
Vol 16 (1) ◽  
pp. 0088
Author(s):  
Hussein Ilaibi Zamil Al-Sudani

A groundwater quality assessment has been carried out in northeast part of Anbar governorate in western Iraq. We analyzed hydrochemical parameters such as pH, electrical conductivity, total dissolved solids presence of ions to describe groundwater quality. The study area has the only confined aquifer within the geological formation extended in area. Values of groundwater hydrochemical parameters were ranged from (7) to (7.9) for ph, (1599) to (6800) µmhos/cm for electrical conductivity (EC) and (1048) to (4446) mg/l for total dissolved solids (TDS). The origins and types of groundwater in the area were of marine origin and MgCl2 water type while only (6) samples were of continental origin and Na2SO4 water type. Groundwater utilization indicated that it can't be used for drinking purposes, while few groundwater wells can be used for agricultural and (33) groundwater samples can be used for animal purposes. However, the nature of the soil in the area and the depth of the groundwater qualified water for agricultural uses in significant and wide ranges.


2009 ◽  
Vol 6 (2) ◽  
pp. 523-530 ◽  
Author(s):  
C. R. Ramakrishnaiah ◽  
C. Sadashivaiah ◽  
G. Ranganna

The present work is aimed at assessing the water quality index (WQI) for the groundwater of Tumkur taluk. This has been determined by collecting groundwater samples and subjecting the samples to a comprehensive physicochemical analysis. For calculating the WQI, the following 12 parameters have been considered: pH, total hardness, calcium, magnesium, bicarbonate, chloride, nitrate, sulphate, total dissolved solids, iron, manganese and fluorides. The WQI for these samples ranges from 89.21 to 660.56. The high value of WQI has been found to be mainly from the higher values of iron, nitrate, total dissolved solids, hardness, fluorides, bicarbonate and manganese in the groundwater. The results of analyses have been used to suggest models for predicting water quality. The analysis reveals that the groundwater of the area needs some degree of treatment before consumption, and it also needs to be protected from the perils of contamination


Water ◽  
2020 ◽  
Vol 12 (9) ◽  
pp. 2387
Author(s):  
José Garcés-Vargas ◽  
Wolfgang Schneider ◽  
Andre Pinochet ◽  
Andrea Piñones ◽  
Francisco Olguin ◽  
...  

The Valdivia River estuary (VRE) located in south-central Chile is known as one of the largest estuarine ecosystems on the Pacific coast. This research aims to determine the intra-tidal and sub-tidal variability of saline intrusions into the VRE between November 2017 and March 2019 derived from salinity sensors located along the VRE. Complementary hydrographic measurements were conducted during flood and ebb conditions of the spring and neap tides for each of the four seasons of the year along the central axis of the VRE. The results of the salinity time series showed that saline intrusions (values greater than 0.5 Practical Salinity Units) occurred ~20 km from the estuary mouth, when the total flow of the Cruces and Calle-Calle rivers (main tributaries of the estuary) was low, around 280–300 m3 s−1. During the same period, the best co-variability was observed between the saline intrusions and the mixed-semidiurnal tide and the fortnightly and monthly periods of the tide. Regression analyses indicated that salinity intrusion length (L) is best correlated to discharge (D) with a fractional power model L α D−1/2.64 (R2 = 0.88). The decreasing discharge trend, found between 2008–2019, implies that saline water intrusions would negatively impact the Valdivia’s main drinking water intake during the low rainfall season under future climate conditions.


2019 ◽  
Vol 45 (2) ◽  
pp. 217-228
Author(s):  
Masuma Chowdhury ◽  
Sarmin Sultana ◽  
Md Atikul Islam ◽  
Aziz Hasan ◽  
Kazi Matin Uddin Ahmed

This paper compares the hydrogeochemical signatures between naturally flowing wells with methane (FWs) and non-flowing wells (require pumping) without methane (NFWs) by analyzing a total of 59 groundwater samples to find possible links for methane gas generation. Relatively higher concentration of HCO3 ⁻ indicates oxidation of organic matter (OM) for both the cases which is corroborated by the dominance of Na-Mg-HCO3 and Na- Mg-HCO3-Cl water type. Low concentrations of redox sensitive parameters i.e., NO3 ⁻, SO4 2⁻, Fe2+ and Mn2+ are indicating prevalence of extremely reducing condition and relatively lower concentrations of SO₄²⁻ in FWs suggest microbial sulphate reduction reaching final stage of redox ladder i.e., methanogenesis. Comparatively higher temperature and subsequent higher electrical conductivity (EC) in FWs possibly attributed by the chemical reactions of methane generation or vice versa. Low geothermal gradient, presence of OM and distribution of the FWs over a paleo valley in the deep confined aquifer zone refer to the existence of favourable environment for biogenic methane production rather than the upward migration or leakage of thermogenic gas from the reservoir below. Asiat. Soc. Bangladesh, Sci. 45(2): 217-228, December 2019


2020 ◽  
Vol 24 (3) ◽  
pp. 511-517
Author(s):  
O.B. Ovonramwen

Physicochemical analyses of surface and groundwater samples from eleven different locations in Ugbomro and Iteregbi, Delta State, Nigeria were sampled and analyzed for physicochemical parameters according to standard methods for the examination of water and wastewater. The following  mean and standard deviation were obtained from the groundwater of the communities: temp (oC) 22.46 ± 0.50 and 23.23 ± 0.99, pH 6.63 ± 0.68 and6.69 ± 0.24, dissolved oxygen (DO) (mg/L) 5.91 ± 0.46 and 5.73 ± 0.46, chemical oxygen demand (COD) (mg/L) 4.24 ± 0.01 and 4.43 ± 0.10, biochemical oxygen demand (BOD) (mg/L) 3.51 ± 0.38 and 3.84 ± 0.21, Turbidity (NTU) 1.22 ± 1.07 and 3.56 ± 0.77, electrical conductivity (EC) (μs/cm) 748.9 ± 215.79 and 786.67 ± 226.77, color (TCU) 1.22 ± 2.12 and 6.11 ± 2.11, total alkalinity (TA) (mg/L) 6.22 ± 7.38 and 14.11 ± 11.19, HCO3- (mg/L) 6.22 ± 7.38 and 14.11 ± 11.19, NO3 - (mg/L) 1.13 ± 0.62 and 2.89 ± 1.25, total solids (TS) (mg/L) 489.09 ± 180.17 and 664.95 ± 373.37, total suspended solids (TSS) (mg/L) 32.25 ± 24.29 and 123.86 ± 82.79, total dissolved solids (TDS) (mg/L) 456.78 ± 163.73 and 542.20 ± 450.66, Cl- (mg/L) 21.20 ± 3.20 and 20.10 ± 3.89, total hardness (TH) (mg/L) 26.67 ± 22.83 and 46.78 ± 36.17, Na (mg/L) 1.26 ± 0.06 and 1.16 ± 0.04, K (mg/L) 0.04 ± 0.01 and 0.06 ± 0.03, Mg (mg/L) 4.32 ± 3.23 and 6.96 ± 5.49, Ca (mg/L) 8.68 ± 9.35 and 18.12 ± 13.71 respectively. The results obtained were subjected to statistical analysis and compared with the standard set by the Standards Organization of Nigeria (SON) and the World Health Organization (WHO) for water samples. Some of the parameters did not meet the standards, hence the need for treatment. The present physio-chemical analyses of surface and groundwater quality of the two neighboring university areas, Ugbomro and Iteregbi, were done to assess the environmental status of  the environment before socio-economic impacts. Keywords: physicochemical, surface water, groundwater, water quality


2020 ◽  
Vol 108 (6) ◽  
pp. 499-508
Author(s):  
Tuba Özdemir Öge ◽  
Firdevs Banu Özdemir

AbstractIn this study, radon concentration measurements and chemical analyses of groundwater samples were performed in four sampling locations of Bartın Province of Western Black Sea Region, Turkey. 222Rn analysis was carried out in groundwater samples with liquid scintillation counting system in accordance with ASTM D5072 standard. The pH, total hardness, alkalinity and dissolved oxygen parameters of the groundwater samples were also determined. The radon concentrations for the water samples ranged between <3.00 Bq/L–12.03 Bq/L. Thirty eight percentage of the samples slightly exceeded the permissible limit of 11.1 Bq/L specified by USEPA for drinking waters. The annual effective doses of groundwater samples were calculated in the range of 7.41–30.74 μSv/y for ingestion of water (Ew.Ig), and in the range of 7.31–30.31 μSv/y for inhalation of radon released from water (Ew.Ih). The total calculated annual effective doses due to ingestion and inhalation were found to be below the limit value of 100 μSv/y specified by the World Health Organization (WHO). The radioactivity measurement results significantly varied for three sampling points but not for one sampling point on two different measurement dates, which is attributed to the differences in geological structure. The chemical analysis results, except for total hardness in two sampling points, were within the permissible limits specified by international standards.


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