Tracing spatial patterns of lacustrine groundwater discharge in a closed inland lake using stable isotopes

Abstract

Tracing lacustrine groundwater discharge (LGD) is essential for understanding the hydrological cycle and water chemistry behaviour of lakes. LGD usually exhibits large spatial variability, but there are few reports on quantitatively revealing the spatial patterns of LGD at the whole lake scale. This study investigated the spatial patterns of LGD in Daihai Lake, a typical closed inland lake in northern China, based on the stable isotopes (δ²H and δ¹⁸O) of groundwater, surface water, and sediment pore water (SPW). The results showed that there were significant differences between the δ²H and δ¹⁸O values of different water bodies in the Daihai Lake Basin: groundwater < SPW < lake water. The LGD through SPW was found to be an important recharge pathway for the lake. Accordingly, stable isotopes of SPW showed that LGD in the northeastern and northwestern of Daihai Lake was significantly greater both horizontally and vertically than that in the other regions, and the proportions of groundwater in SPW in these two regions were 55.53% and 29.84%, respectively. Additionally, the proportion of groundwater in SPW showed a significant increase with profile depth, and the proportion reached 100% at 50 cm below the sediment surface in the northeastern of the lake where the LGD intensity was strongest. The total LGD to Daihai Lake was 1.47 × 10⁷ m³/a, while the LGD in the northeastern and northwestern of the lake exceeded 1.9 × 10⁶ m³/a. This study provides new insights into assessing the spatial patterns of LGD and water resource management in lakes.

Keywords: Daihai Lake; Lacustrine groundwater discharge; Sediment pore water; Spatial patterns; Stable isotopes.