Soil salinity, a critical concern in agriculture, refers to the accumulation of excessive salt in the soil, posing significant challenges to plant growth and overall land fertility. The salts involved include compounds of sodium, potassium, calcium, magnesium, sulfates, chlorides, carbohydrates, and bicarbonates. This salinization process occurs due to various factors, such as mineral weathering, improper farming practices, and the rise in sea levels, among others. The impacts of soil salinity are far-reaching, affecting both the ecological balance and human livelihoods. Notably, it hampers water absorption by plants, leading to dehydration and reduced crop yields. Furthermore, soil salinity negatively influences terrestrial biodiversity, inducing the degradation of natural habitats and fragmentation of wildlife corridors. The salinization of fresh rivers due to dryland salinity also poses challenges to water quality for both drinking and irrigation purposes. Various factors contribute to the causes of soil salinity, including dry climates with low precipitation, high evaporation rates, poor drainage, waterlogging, improper irrigation practices, and human-induced activities like removing deep-rooted vegetation. Addressing soil salinity is crucial for sustaining agricultural productivity and preventing environmental degradation.