Limestone water mixing process and hydrogen and oxygen …
Table 1 shows that the stable isotopes of groundwater in the area are gradually depleted with the increase of aquifer depth. The range of δD and δ 18 O in limestone groundwater is −72.79‰ ∼ −69.17‰, −10.41‰ ∼ −9.78‰, which is the most depleted in all types of water samples. The hydrogen and oxygen isotope of sandstone …