EGU25-10100, updated on 15 Mar 2025
https://doi.org/10.5194/egusphere-egu25-10100
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Wednesday, 30 Apr, 10:05–10:15 (CEST)
 
Room 2.44
Reconstructing Atmospheric Chloride Deposition Using Chloride-Tritium Tracers Stored in Deep Loess
Yanan Huang1,2,3, Wangjia Ji2, and Zhi Li2
Yanan Huang et al.
  • 1College of Water Sciences, Beijing Normal University, Beijing, China
  • 2College of Natural Resources and Environment, Northwest A&F University, Yangling, China
  • 3Center for Water Research, Advanced Institute of Natural Sciences, Beijing Normal University at Zhuhai, Zhuhai, China

Atmospheric chloride deposition (ACD) is an essential parameter in estimating potential groundwater recharge. However, ACD observations are still limited to a few sparsely distributed sites and/or short time intervals, which are insufficient to characterize regional distribution over a longer time scale, putting into limitation the usefulness of the easily accessible environmental chloride method for tracking groundwater dynamics in future studies. Considering the mass balance between chloride input from precipitation and soil Cl storage in the unsaturated zone, we combined 3H- and Cl-based tracing techniques to inversely reconstruct the long-term average or historical time series of ACD from the Cl stored in soil profiles. Our results highlight the proposed methods can effectively exclude fertilization impacts and perform satisfactorily in estimating ACD. However climatic and geographic factors had should be taken seriously when reconstructing ACD. A better understanding of groundwater recharge in unsaturated zones is ultimately critical for water resource management, especially in semi-arid environments with deep soils.

How to cite: Huang, Y., Ji, W., and Li, Z.: Reconstructing Atmospheric Chloride Deposition Using Chloride-Tritium Tracers Stored in Deep Loess, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-10100, https://doi.org/10.5194/egusphere-egu25-10100, 2025.