Stable isotope and hydrochemistry reveal source and quality of
groundwater around Qinghai Lake, NE Qinghai-Tibet Plateau, China
Abstract
The integrated use of isotopic and hydrochemical tracers is an effective
approach for investigating complex hydrological processes of
groundwater. Thorough understanding of recharge and quality of the
groundwater is usually a prerequisite for effective groundwater
management. This study investigated the water level, stable isotope and
hydrochemistry of groundwater around the Qinghai Lake to reveal the
recharge sources, hydrochemical evolution and water quality of
groundwater. The relative altitudes of groundwater level ranged from
-1.27 to 122.91 m with hydraulic gradient ranging from -6.20 to
43.14‰relative to the water level of Qinghai Lake, indicating most of
the groundwater was flowing into the lake. Most of the groundwater
points lay close to the local meteoric water line, and the slope of
Local Evaporation Line of groundwater (LEL: δ2H = 6.08 δ18O-3.01) was
lower than the slopes of the LMWL, indicating that the groundwater were
recharged primarily from precipitation at different altitude in the
basin, though it had undergone varying degrees of evaporation. The
hydrochemical analysis showed that the groundwater was mainly freshwater
and its hydrochemical type was Ca-Mg-HCO3. The groundwater chemistry was
mainly controlled by carbonate dissolution around Qinghai Lake.
Furthermore, high TDS and high concentrations of Na+, Mg2+, Cl-, or
SO42- in several groundwater were caused by the recharge source of lake
water, the recharge source of fissure water, or by the dissolution of
evaporite. The main sources of nitrate (NO3-) in groundwater around
Qinghai Lake were animal feces and sewage, suggesting that the pollution
of groundwater should be paid more attention in animal husbandry areas
on the Qinghai-Tibet Plateau, although the industrial and urbanization
rates were relative low on the plateau. The scientific planning and
engineering management of livestock manure and wastewater discharge in
animal husbandry regions are very necessary to be carried out urgently,
which could not only protect water resources for drinking, but also
contribute to human health and sustainable development of the ecological
environment of the Qinghai-Tibet Plateau.