Change of avalanching parameters in the near zone of explosion site

Spatial variations of avalanche formation parameters in the relation with the explosive mass and its location have been experimentally studied. The charges were installed in five locations: on the ground, in the snow layer at a height of 0.6 m above the ground, on the snow surface, at a height of 1...

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Main Authors: E. G. Mokrov, N. V. Barashev
Format: Article
Language:Russian
Published: Nauka 2015-04-01
Series:Лëд и снег
Subjects:
Online Access:https://ice-snow.igras.ru/jour/article/view/100
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author E. G. Mokrov
N. V. Barashev
author_facet E. G. Mokrov
N. V. Barashev
author_sort E. G. Mokrov
collection DOAJ
description Spatial variations of avalanche formation parameters in the relation with the explosive mass and its location have been experimentally studied. The charges were installed in five locations: on the ground, in the snow layer at a height of 0.6 m above the ground, on the snow surface, at a height of 1 m and 2 m above the snow surface. Mass of explosive was 0.5, 1, 2 and 4 kg. The experiments were in March 2012 on the Suoluayv plateau (600 m a.s.l.) in Khibiny Mountains. Studies have shown that at explosion sites the disturbance of snow structure, its density and shear strength occurs throughout the whole depth of snow cover, depending on the structure and density of snow layers as well as the explosive mass and its location.
format Article
id doaj-art-2f3bfbcba08c48c19e231a357c39685a
institution Kabale University
issn 2076-6734
2412-3765
language Russian
publishDate 2015-04-01
publisher Nauka
record_format Article
series Лëд и снег
spelling doaj-art-2f3bfbcba08c48c19e231a357c39685a2025-08-20T03:59:49ZrusNaukaЛëд и снег2076-67342412-37652015-04-01532485210.15356/2076-6734-2013-2-48-5294Change of avalanching parameters in the near zone of explosion siteE. G. Mokrov0N. V. Barashev1Moscow State UniversityNorth-West Phosphor Company, Koashva, Murmavskaya oblastSpatial variations of avalanche formation parameters in the relation with the explosive mass and its location have been experimentally studied. The charges were installed in five locations: on the ground, in the snow layer at a height of 0.6 m above the ground, on the snow surface, at a height of 1 m and 2 m above the snow surface. Mass of explosive was 0.5, 1, 2 and 4 kg. The experiments were in March 2012 on the Suoluayv plateau (600 m a.s.l.) in Khibiny Mountains. Studies have shown that at explosion sites the disturbance of snow structure, its density and shear strength occurs throughout the whole depth of snow cover, depending on the structure and density of snow layers as well as the explosive mass and its location.https://ice-snow.igras.ru/jour/article/view/100avalanche formation parametersexplosionsnow avalanchesnow densitysnow strength.
spellingShingle E. G. Mokrov
N. V. Barashev
Change of avalanching parameters in the near zone of explosion site
Лëд и снег
avalanche formation parameters
explosion
snow avalanche
snow density
snow strength.
title Change of avalanching parameters in the near zone of explosion site
title_full Change of avalanching parameters in the near zone of explosion site
title_fullStr Change of avalanching parameters in the near zone of explosion site
title_full_unstemmed Change of avalanching parameters in the near zone of explosion site
title_short Change of avalanching parameters in the near zone of explosion site
title_sort change of avalanching parameters in the near zone of explosion site
topic avalanche formation parameters
explosion
snow avalanche
snow density
snow strength.
url https://ice-snow.igras.ru/jour/article/view/100
work_keys_str_mv AT egmokrov changeofavalanchingparametersinthenearzoneofexplosionsite
AT nvbarashev changeofavalanchingparametersinthenearzoneofexplosionsite