Insoluble Particles in the Snowpack of the Ob River Basin (Western Siberia) a 2800 km Submeridional Profile

• Published in: Atmosphere
• Main Authors: Vladimir P. Shevchenko, Sergey N. Vorobyev, Ivan V. Krickov, Andrey G. Boev, Artyom G. Lim, Alexander N. Novigatsky, Dina P. Starodymova, Oleg S. Pokrovsky
• Format: Article in Journal/Newspaper
• Language: English
• Published: MDPI AG 2020
• Subjects: insoluble particles; snowpack; West Siberia; scanning microscopy; lithogenic particles; biogenic particles; Meteorology. Climatology; QC851-999; Salekhard; ob river; Siberia
• Online Access: https://doi.org/10.3390/atmos11111184; https://doaj.org/article/87f7b773ac1c45df8ed6ebc24fa12658

Snowpack exhibits properties that make it a unique natural archive of airborne pollution. The data on insoluble particles in the Ob River catchment (Western Siberia) snowpack are limited. Insoluble particles in the snowpack of Western Siberia were studied at 36 sites on a 2800 km submeridional profile from the city of Barnaul to Salekhard in February 2020. Snow samples were collected over the full depth of the snow core, from the surface of the snow cover to the boundary with soil, except for the lower 1–2 cm. After the filtration of melted snow through a 0.45-µm membrane, the particle composition was studied using a scanning electron microscope with an energy microprobe. In the background areas, the concentration of insoluble particles in the snow was below 2 mg/L. Significantly higher particle concentrations were encountered near cities and hydrocarbon production areas. Particulate matter in snow mainly consists of biogenic and lithogenic particles mixed with anthropogenic particles (ash and black carbon aggregates). The proportion of anthropogenic particles increases near cities and areas of active hydrocarbon production.