Origin and Geochemical Processes of Porewater in Clay-Rich Deposits in the North Jiangsu Coastal Plain, China

<div>Solute concentrations and stable isotopes (<i>δ</i><sup>18</sup>O, <i>δ</i><sup>2</sup>H) of porewater versus depth.</div>

Geofluids

Figure 5: Origin and Geochemical Processes of Porewater in Clay-Rich Deposits in the North Jiangsu Coastal Plain, China 