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Water supply in the Arctic. Travel Tips

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Как secure water in the Arctic?

Dehydration of the body can occur not only in conditions of high temperatures, when the body is struggling with overheating. At negative temperatures, water losses are very significant due to increased sweating during intense physical activity, and also because of the warm clothing that restricts movement in which this work has to be done. Dehydration of the body occurs as a result of low temperature and dryness of the air entering the lungs, to which it reacts, first of all, with increased urination (cold diuresis). An increase in urination increases the loss of sodium chloride in the body and causes a violation of water-salt metabolism.

In the cold season in the coastal zone and when crossing sea ice, the source of water is the "old ice". In young ice, the gaps between ice crystals are filled with salt cells with brine, which was released during the period of ice formation. The high salinity of young ice makes it completely unsuitable for obtaining fresh water.

Natural "desalination" of ice occurs due to the lowering of the brine into the lower layers during prolonged freezing, so the older the ice, the less salt it contains. The upper part of multi-year pack ice rising above the level of the ice field is often completely fresh. Such ice is found on the coast, it can be recognized by its peculiar blue color, smooth outlines and brilliance. The deeper the blue shade of the ice, the more suitable it is for drinking water. However, old ice that has been exposed to salt spray for a long time should not be consumed.

Fresh sea ice is white, sometimes with greenish hues, and is characterized by sharp edges. This ice is salty and, as mentioned above, is not suitable for drinking water.

Dense, packed snow can also serve as a source of water, but the output of water from it is very small, only 10-12%, and a lot of fuel will be required to melt it. In the tundra and forest-tundra it is best to use the fresh ice of rivers and lakes.

Ice produces twice as much water as snow, with half the amount of heat. To get water from snow, melt a small amount of it in a pot, and then gradually add more snow to it. If you fill the kettle completely, then when the snow melts, a cavity forms at the bottom, which prevents the snow from melting and can lead to the kettle burning out. The surface layer of snow provides less water than the lower layers.

In summer, the problem of drinking water is completely solved by streams, fresh lakes and rivers, as well as accumulations of melt water on snowfields.

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