“Water is the lifeblood of the earth, the source of life, essential to the survival of all living beings”, as [1] , rightly exclaimed. The earth is called the blue planet because that’s how it appears from space, with 70% of its surface covered by water. Although water is abundant, freshwater (surface water and groundwater) represents only 2.53% of the planet’s total water, and only this freshwater sustains terrestrial life, especially human life. Freshwater is therefore a rare and precious resource which, if contaminated, may no longer be able to fulfill its various ecological roles. Its availability in quantity and quality is essential to prevent disease and improve quality of life [2] . Freshwater is a rare and vital resource. In coastal areas, this resource is subject to multiple pressures, notably saline intrusion caused by intensive groundwater exploitation and rising sea levels. These phenomena disrupt the natural balance between fresh and salt water, compromising water quality and the health of local populations. The Grand-Popo district in southern Benin is particularly hard hit by this problem, due to its proximity to the Atlantic Ocean and the increasing use of groundwater for domestic and agricultural purposes. The aim of this study is to assess the impact of the salt wedge on the physico-chemical quality of groundwater in this region.

Generally speaking, the parameters measured do not comply with Beninese standards or WHO guidelines. Indeed, the temperature values measured vary from 28.6˚C to 30.2˚C. compared with those measured by [4] between 26.5˚C and 32˚C and between 28.4˚C and 33˚C during the fieldwork of [5] . On the other hand, they are similar to those reported by [6] and [7] in groundwater from Chad and Burkina Faso. Based on the results, all water temperatures at the various sampling points exceed the quality reference set at 25˚C [8] . Although these values are high, they do not present any danger to human health, but they do pose a problem of acceptability, as cool water is generally more pleasant to the taste than lukewarm water. The pH values recorded range from 7.04 to 8.48. These pH values oscillate within the range of values (6.5 < pH < 8.5) tolerable by Beninese standards [9] , as stipulated in article 17 of Decree N˚2001-094 of February 20, 2001 setting drinking water quality standards in Republic of Benin. These pH values are, for the most part, below those (6.1 and 8) obtained by [5] in the municipality of Grand-Popo. As far as salinity is concerned, the recorded values are not so great compared with those of the seas and oceans on average (34 and 35 PSU) [10] . Electrical conductivity values range from 320 to 3970 µS/cm. This indicates an average mineralization of 1404.6 µS/cm. The maximum value recommended for electrical conductivity by the WHO is 2000 µS/cm. The results show that the conductivities recorded are quite high, although 80% of the sampled wells had electrical conductivities below WHO guidelines. Given that the sampled wells at Yodo-Condji (P7 et P6), Hounssoukoè (P7), Apoutagbo (P9 et P10), Hêvê (P13 et P14) and Toklanhon (P15) have conductivity values in excess of 1000 µS/cm to 3000 µS/cm, they could be classified as “saline water”. If conductivity exceeds 3000 µS/cm, the water is characterized as “seawater” according to water classification based on conductivity [11] . In addition, those sampled at Toklanhon (P16) and Houndjohoundji (P18) show values in excess of 3000 µS/cm. This undoubtedly attests to seawater intrusion. However, it should be noted that the two water points sampled (Toklan-hon and Houndjohoundji) are close to the Grand-Popo lagoon. This configuration could explain the high electrical conductivity values obtained in these two locations, which are also close to the sea. With regard to chloride concentrations, the levels of the water samples analyzed ranged from 38.34 mg/L to 1160.44 mg/L. Water points with high chloride ion values suggest salt water intrusion, as the values obtained at these water points are higher than those recommended by Beninese standards, i.e. 250 mg/L. As for sodium, average sodium levels in the water at the points studied ranged from 10.41 mg/L to 1000.32 mg/L. According to [12] recommendations, the amount of sodium required in water intended for consumption should be less than 200 mg/L. However, the levels obtained for the water points sampled in certain localities are above this value. These waters therefore fail to meet potability standards. As for potassium levels, most of them comply with WHO standards (<12 mg/L). They are similar to those obtained by several authors [13] [14] . Based on the piezometric map [5] , we can say that the piezometric levels in the Grand-Popo district are equivalent to −1 m in the piezometric depressions, testifying to the sensitivity of these sectors to invasion by salt water from the sea and brackish water from the Grand-Popo lagoon. These depressions are found at Hêvê, Apoutagbo, Houndjohoundji and Toklanhon. This further justifies the high conductivity, chloride and sodium concentrations in the water sampled in these localities. The saltwater wedge is therefore located along the Grand-Popo coastal lagoon and the villages of Houndjohoundji and Toklanhon. In addition, the survey results revealed that water-borne diseases such as diarrhoea and infections are largely observed in the villages, although the main use of well water is not for drinking but for cooking. On the other hand, high blood pressure is not so much recorded as a disease. Sustainable water resource management measures, including awareness-raising and control of groundwater use, are needed to limit the effects of saline intrusion.

This study highlights the significant impact of the salt wedge on groundwater quality in the Grand-Popo district. High concentrations of electrical conductivity, chlorides and sodium compromise water potability, with serious implications for public health. Sustainable water resource management measures, including raising public awareness and controlling groundwater exploitation, are needed to limit the effects of saline intrusion.