Minor and major elements in suspended matter in the Rhine and Meuse rivers and estuary |
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| Institution: | 1. School of Chemical Engineering, Northeast Electric Power University, Jilin 132012, PR China;2. Shenzhen Wenirune Electronic Technologies Co., Ltd, Shenzhen 518172, PR China;1. Institute of Green Chemistry and Chemical Technology, School of Chemistry and Chemical Engineering, Jiangsu University, Zhenjiang 212013, PR China;2. College of Chemistry, Jilin Normal University, Siping 136000, PR China;3. College of Chemistry, Liaoning Normal University, Dalian 116029, PR China;1. Institute of Physics, Faculty of Science, The Islamia University of Bahawalpur, Baghdad-ul-Jadid Campus, Bahawalpur, 63100, Pakistan;2. Advanced Functional Materials & Optoelectronics Laboratory (AFMOL), Department of Physics, Faculty of Science, King Khalid University, Abha, 9004, Saudi Arabia;3. Nanosciences and Nanotechnology Department, National Centre for Physics, Quaid-i-Azam University Islamabad, Pakistan;4. Department of Physics, Khawaja Fareed University of Engineering and Information Technology, Rahim Yar Khan, Pakistan;5. Institute of Biochemistry, Biotechnology and Bioinformatics, The Islamia University of Bahawalpur, Baghdad-ul-Jadid Campus, Bahawalpur, 63100, Pakistan;6. Centre for High Energy Physics, The University of Punjab, Lahore, Pakistan |
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| Abstract: | Suspended sediment in the Rhine-Meuse estuary contained as little as one third of the trace metal content of the river-borne suspended matter. It is shown that the strong seawardly decreasing gradient in the trace metal content of the suspended particulate matter is not due to desorption processes, but can be explained simply by the mixing of river-borne and marine-derived suspended sediments. |
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