The PH scale is used to register the degree of acidity or alkalinity of a body of water.
The PH scale ranges from 0 extremely acidic, to 14 being extremely alkaline and is based inversely on the concentration of hydrogen ions (H+) in the water in relation to the number of Hydroxel ions (OH-). The more hydrogen ions would make the water more acidic the water will be resulting in a low figured number result.
In their native Japan the winters are very cold however they are also relatively short.