Горный институт УрО РАН, Пермь, Россия

Барях А. А., научный руководитель института, академик РАН, д-р техн. наук, bar@mi-perm.ru
Евсеев А. В., научный сотрудник, канд. техн. наук
Глебова П. А., младший научный сотрудник
Васильева Е. Л., младший научный сотрудник

Предложена технологически оперативная методическая схема контроля и прогноза оседаний земной поверхности, основанная на шахтных измерениях горизонтальной конвергенции очистных камер. Установлена устойчивая связь между горизонтальной и вертикальной деформациями междукамерных целиков. На основе анализа представительных экспериментальных данных показано, что скорость оседания земной поверхности определяется суммой вертикальных деформаций междукамерных целиков на отработанных рабочих пластах.

Исследование выполнено при финансовой поддержке Министерства науки и образования РФ (регистрационный номер 122012000403-1).

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