Annual variations in composition of the North Dvina River water

• Main Authors: Shevchenko, Vladimir P, Pokrovsky, Oleg S, Filippov, Alexander S, Lisitzin, Alexander P, Bobrov, Vyacheslav A, Bogunov, A Yu, Zavernina, N N, Zolotykh, E O, Isaeva, Alexandra B, Kokryatskaya, Natalya M, Korobov, V B, Kravchishina, Marina D, Novigatsky, Alexander N, Politova, Nadezhda V
• Format: Dataset
• Language: English
• Published: PANGAEA 2010
• Subjects: Archive of Ocean Data; ARCOD; Belaya River (tributary of Pinega); Creek from the llasskoe bog; Ilasskoe bog; Karasozero Lake; Karelka River; Karmozero Lake; Karst depression; Kelda River; North Dvina River; Maimaksa Channel; North Dvina River at Lapominka; North Dvina River at Myudyug Island; North Dvina River at Ust-Pinega; Pinega River; Pinega River at Golubino; Polta River; Saint Spring; Sotka River; VSh-A-1; VSh-A-10; VSh-A-11-12; VSh-A-13; VSh-A-14; VSh-A-15; VSh-A-16; VSh-A-17; VSh-A-18; VSh-A-19; VSh-A-2; VSh-A-20; VSh-A-21; VSh-A-22; VSh-A-23; VSh-A-24; VSh-A-25; VSh-A-26; VSh-A-27; VSh-A-28; VSh-A-29; VSh-A-3; VSh-A-30; VSh-A-31; VSh-A-32; VSh-A-33; VSh-A-34; VSh-A-35; VSh-A-36; Pinega; Sotka; Ust’-Pinega; Karelka; Kelda; Lapominka; dvina
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.746584; https://doi.org/10.1594/PANGAEA.746584

New data on elemental composition of particulate matter from the North Dvina River are presented. In May (period of snowmelt flood) it is similar to the upper layer of the continental crust due to active erosion of crust material in the catchment area. In August (summer low water period) impact of biogenic components increases and elevated concentrations of Cd, Sb, Mn, Zn, Pb, and Cu are observed. At other seasons no significant increase in heavy and rare earth element concentrations is observed.