Decadal patterns of anthropogenic salinisation in typical mountain streams in northeastern China: Increased rates and sources. (May 2020)

• Record Type: Journal Article
• Authors: Zhao, Qian; Zhang, Yuan; Guo, Fen; Jia, Xiaobo; Ding, Sen
• Is Part Of: Chemosphere. Volume 246(2020)
• Publication Date: 2020-05
• Subjects: Anthropogenic salinisation -- Drastic change -- Increase rates -- Ionic composition -- Driving factor -- Mountain streams; Pollution -- Periodicals; Pollution -- Physiological effect -- Periodicals; Environmental sciences -- Periodicals; Atmospheric chemistry -- Periodicals; 551.511
• DOI: 10.1016/j.chemosphere.2019.125789
• Languages: English
• ISSNs: 0045-6535

Abstract

Abstract: Salt pollution and anthropogenic-accelerated weathering is globally shifting the ionic composition and increasing salinisation of fresh water. We analyzed a 40-year data set (1970s–2010s) to characterize the drastic change of dissolved ionic composition, conductivity and pH levels. We also identified causative factors in these highly polluted mountain streams in northeastern China. Dissolved salt ions (Ca 2+, Mg 2+ and SO4 2− ) increased by 3.02–5.21 fold and conductivity (a proxy for salinisation) increased by 3.09 fold. The average pH values increased from 7.08 to 8.49. The dominant ions, Ca 2+, Mg 2+, SO4 2− and HCO3 − + CO3 2−, accounted for ∼90% of ionic composition based on mass concentration. Between the 1970s and 2010s, the dominant anion shifted from HCO3 − + CO3 2− to a mixture of SO4 2− and HCO3 − + CO3 2− . Increasing mining and land development appear to be the primary driving factors for the change of Ca 2+, Mg 2+, SO4 2− and HCO3 − + CO3 2− concentrations; whereas, agricultural land was the main driving factor for the variation in K +, Na + and Cl − concentrations. The source of ions has shifted from a more natural weathering of carbonate rocks to one of mineral dissolution that is affected by anthropogenic activities. Our study shows that freshwater mountain streams are at risk of long lasting anthropogenic salinisation and should be considered in future management and conservation plans. Highlights: Salinisation and pH have significantly increased during the past four decades. ∼90% of ions are Ca 2+, Mg 2+, SO4 2− and HCO3 − in mountainous northeastern China. The ionic composition shifted from HCO3 − to a mixture of SO4 2− and HCO3 − . Sources are attributed to mining and agricultural practices. Most streams in the region are at risk of long lasting anthropogenic salinisation.