The origin and hydrochemistry of deep well waters from the northern foot of Mt. Fuji, central Japan

摘要

The major chemical and stable isotopic compositions of hydrogen, oxygen, and sulfur (delta D, delta O-18, delta S-34) were analyzed from water samples of wells and natural springs in the northern foot area of Mt. Fuji and the adjacent Misaka and Tanzawa Mountains to investigate the origin of deep well waters and water-rock interactions that affect the water quality.