4.3 Article

Using 223Ra and 224Ra to estimate discharges of groundwater and associated nutrients into southeast of Qinghai Lake, in Qinghai-Tibet Plateau

Journal

JOURNAL OF GREAT LAKES RESEARCH
Volume 48, Issue 5, Pages 1171-1179

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.jglr.2022.07.007

Keywords

Qinghai Lake; 223 Ra and 224 Ra; Groundwater discharge; Nutrients

Funding

  1. NSFC program
  2. [41967053]

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Qinghai Lake, with its important geographical location and largest saltwater body in China, is vital for the ecological environment of the northeastern part of the Qinghai-Tibet Plateau. This study used radium isotopes to trace groundwater discharges and nutrients carried into the lake, revealing the influence of shallow groundwater and sediment diffusion on the lake's spatial characteristics. The findings emphasize the significance of monitoring shallow groundwater discharge into Qinghai Lake for water environment protection and prevention of potential ecological risks.
With its important geographical location and status as the largest saltwater body in China, Qinghai Lake plays a vital role in the ecological environment of the northeastern part of the Qinghai-Tibet Plateau. Due to climate change and the subsequent adjustment of Qinghai Lake's tourism policy, it is necessary to understand groundwater discharges in southeast of Qinghai lake both for ecological protection and risk prevention. This study used radium isotopes 223Ra and 224Ra to trace groundwater discharges and nutri-ents carried into the lake. The spatial characteristics of Ra isotopes with greater activity in the upper and bottom layers in the lake indicated that they were influenced by inputs of shallow groundwater and dif-fusion from sediments. The average 224Ra diffusion flux of the sediments in the Lake was 33.54 dpm m-2 d-1. Based on the 224Ra mass balance model, the discharge flux of shallow groundwater in this region was estimated to be 3.49 x 106 ti 3.68 x 106 m3 d-1. The PO43-and SiO2 fluxes carried into the southeastern of the lake by groundwater were 1.78 x 1011 ti 1.88 x 1011 mg/y and 2.22 x 1012 ti 2.34 x 1012 mg/y, respectively. It is thus essential to monitor shallow groundwater discharge into Qinghai Lake for the pro-tection of the water environment and prevention of potential ecological risks.(c) 2022 International Association for Great Lakes Research. Published by Elsevier B.V. All rights reserved.

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