Seasonal Interaction of River Water-Groundwater-Salt Lake Brine and Its Influence on Water-Salt Balance in the Nalenggele River Catchment in Qaidam Basin, NW China

• Published in: Journal of earth science (Wuhan, China) China), 2022-10, Vol.33 (5), p.1298-1308
• Main Authors: Han, Jibin, Xu, Jianxin, Yi, Lei, Chang, Zheng, Wang, Jianping, Ma, Haizhou, Zhang, Baoyun, Jiang, Hongchen
• Format: Article
• Language: English
• Subjects: Biogeosciences; Brines; Catchment area; Crystallization; Dry season; Earth and Environmental Science; Earth Sciences; Exploitation; Geochemistry; Geology; Geotechnical Engineering & Applied Earth Sciences; Groundwater; Groundwater recharge; Mineral resources; Paleo-environment and Hydrogeology; Potassium chloride; Rainy season; River catchments; River water; Rivers; Salt balance; Salt lakes; Seasons; Sodium sulfate; Surface water; Surface-groundwater relations; Upstream; Water exchange; Water infiltration; Wet season
• ISSN: 1674-487X; 1867-111X
• DOI: 10.1007/s12583-022-1731-0

Identifying interactions among river water, groundwater and salt lake brine is important for sustainable exploitation of brine mineral resources. In this study, we investigated the water exchange rate in dry and wet seasons, and assessed the influence of seasonal water exchange on brine concentration and crystallization process in the Nalenggele (NLGL) catchment of Qaidam Basin, China. The results show that the surface water infiltration and groundwater recharge rates in the wet season were 2.81 × 10 −3 and 1.15 × 10 −3 m 3 /(s·m) in upstream, 1.63 × 10 −2 and 1.53 × 10 −2 m 3 /(s·m) in midstream, and 2.83 × 10 −4 and 6.82 × 10 −5 m 3 /(s·m) in downstream, respectively; while their counterparts in the dry season were 9.81 × 10 −4 and 5.05 × 10 −4 m 3 /(s·m) in upstream, and 8.34 × 10 −3 and 7.78 × 10 −3 m 3 /(s·m) in midstream, respectively. The water exchange strongly influenced brine concentration and crystallinzation process, with brine chemistry belonging to 3K 2 SO 4 ·Na 2 SO 4 and KCl types in wet and dry seasons, respectively. The strong water exchange in wet season destroyed the water-salt balance, while the low water exchange rate in dry season facilitated preparation of KCl products.