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The Pliocene Yutengping Sandstone (depth 1642–1882 m) and its overlying caprock shale (depth 1395–1642 m) in Hsinchu City, central Taiwan, were intended for a storage site of CO 2 . Formation water was collected from a gas well located at a depth of 1827–1846 m. This study investigated changes in water chemistry and dissolution of trace elements from the sandstone and shale at 25 MPa and 90 °C...
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