Geochemical behaviors of metal elements during a single fl ood event in the natural Chishui River,Southwest China  

作　　者：Zhongxuan Liang Keyi Wang Hongming Cai Zhongwei Wang Wei Yuan Jiubin Chen 

机构地区：[1]State Key Laboratory of Environmental Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences,Guiyang 550081,China [2]University of Chinese Academy of Sciences,Beijing 100049,China [3]Institute of Surface-Earth System Science,School of Earth System Science,Tianjin University,Tianjin 300072,China [4]Zunyi Ecological Environment Monitoring Center,Zunyi 563000,China [5]Guangdong Ecological and Environmental Monitoring Center,Guangzhou 510308,China

出　　处：《Acta Geochimica》2025年第2期373-386,共14页地球化学学报(英文)

基　　金：National Natural Science Foundation of China,42103008,Hongming Cai。

摘　　要：The majority(up to 90%)of riverine materials is transported from the continent to the ocean mainly in flood events.It is thus crucial to characterize the geochemistry of elements and their flux in river system in order to better constrain their global biogeochemical cycling and impact on the oceanic ecosystem.However,the geochemical behavior including the distribution,migration and partitioning of typical metal elements amongst diff erent phases,during hydrodynamic flood event remains still to be well explored.Here,we investigated the geochemical behaviors of typical metal elements in dissolved phase and suspended particulate matter collected from a single flood event in the natural Chishui River,Southwest China.The results showed clearly that the geochemistry of metal elements was largely controlled by the hydrodynamic eff ect,of which the diff erent flowrates introduce a natural sorting of diff erent mineral particles transported at diff erent flood stages,depending on their shape,size and density.The maximum concentrations of alkaline and alkaline earth metals(Li,Mg,K,Rb and Sr)in SPM appeared before the flood peak,which was largely controlled by aluminosilicate minerals.However,transition metals(Cr,Mn,Fe,Ni and Cu)showed their abundance peaks lagging behind the flowrate summit,as a result of the late arrival of coarse particles or heavy minerals,evidenced by the mineralogical phase analysis.In addition,the distribution coe fficient(K_(d))between particulate and dissolved loads were lower and stable for soluble alkali/alkaline earth metals which could be aff ected by pH,while higher and fluctuant for transition metals that were largely influenced by SPM content.Overall,the present study reveals clear eff ects of hydrodynamic sorting on the geochemistry of metal elements during the flood event of the natural Chishui River,which should be taken into account when characterizing the riverine flux and their impact on marine ecosystem.

关 键 词：Natural River FLOOD SPM Hydrodynamic sorting Metals 

分 类 号：P59[天文地球—地球化学]