硫酸盐
风化作用
环境科学
流域
环境化学
灌溉
地表径流
矿化(土壤科学)
盐度
水文学(农业)
温带气候
城市化
地球化学
地质学
化学
土壤水分
生态学
土壤科学
海洋学
生物
地理
有机化学
岩土工程
地图学
作者
Jiang Wu,Nan Xu,Yichu Wang,Wei Zhang,Alistair G.L. Borthwick,Jinren Ni
标识
DOI:10.1038/s41467-021-26231-w
摘要
Solute-induced river syndromes have grown in intensity in recent years. Here we investigate seven such river syndromes (salinization, mineralization, desalinization, acidification, alkalization, hardening, and softening) associated with global trends in major solutes (Ca2+, Mg2+, Na+, K+, SO42-, Cl-, HCO3-) and dissolved silica in the world's large rivers (basin areas ≥ 1000 km2). A comprehensive dataset from 600 gauge stations in 149 large rivers reveals nine binary patterns of co-varying trends in runoff and solute concentration. Solute-induced river syndromes are associated with remarkable increases in total dissolved solids (68%), chloride (81%), sodium (86%) and sulfate (142%) fluxes from rivers to oceans worldwide. The syndromes are most prevalent in temperate regions (30~50°N and 30~40°S based on the available data) where severe rock weathering and active human interferences such as urbanization and agricultural irrigation are concentrated. This study highlights the urgency to protect river health from extreme changes in solute contents.
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