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Soil salinity. Soil salinity is the salt content in the soil; the process of increasing the salt content is known as salinization. Salts occur naturally within soils and water. Salination can be caused by natural processes such as mineral weathering or by the gradual withdrawal of an ocean. It can also come about through artificial processes such as irrigation
When your soil have pH dependt charge clays this effect becomes more proeminent (organic matter also has this kind of charge). If you had a pH decrease with increasing soil salinity, it means your soil has predominance of negative charges in soil (predominance of negative charges in pH dependent charges). It is perfectly expected for your soil.