
В работе приведено обоснование роли коэффициента котловинности и биоклиматических индексов в формировании условий развития почвенного покрова межгорных степных котловин Горного Алтая. На примере Уймонской, Курайской и Чуйской межгорных степных котловин продемонстрированно, что использованные расчетные показатели играют основную роль при формирование условий образования почвенного покрова указанных территорий.
In article presents validation role of hollows coefficient and bioclimatic indexes in establishing the conditions of development the soil cover of intermountain basins in Altai mountains. On the examples of Uymonskaya, Kurayskaya and Chuyskaya intermountain hollows it was demonstrated that mentioned calculated indexes plays the main role in conditions of formation the soil cover at these territories.
КОЭФФИЦИЕНТ КОТЛОВИННОСТИ,БИОКЛИМАТИЧЕСКИЕ ИНДЕКСЫ,ВЫСОТНАЯ ПОЯСНОСТЬ,ПОЧВЕННЫЙ ПОКРОВ,ГОРНЫЙ АЛТАЙ,HOLLOWS COEFFICIENT,BIOCLIMATIC INDEXES,HIGH-ALTITUDE ZONE,SOIL COVER,ALTAI MOUNTAINS
КОЭФФИЦИЕНТ КОТЛОВИННОСТИ,БИОКЛИМАТИЧЕСКИЕ ИНДЕКСЫ,ВЫСОТНАЯ ПОЯСНОСТЬ,ПОЧВЕННЫЙ ПОКРОВ,ГОРНЫЙ АЛТАЙ,HOLLOWS COEFFICIENT,BIOCLIMATIC INDEXES,HIGH-ALTITUDE ZONE,SOIL COVER,ALTAI MOUNTAINS
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