В ИНГГ СО РАН изучают роль системы вода – горная порода в процессах формирования химического состава природных вод (на примере восточной части Новосибирской области). Свои результаты по этой теме в рамках открытого научного семинара представила м.н.с. лаборатории гидрогеологии осадочных бассейнов Сибири Анастасия Алексеевна Максимова.
Доклад был выполнен по материалам подготовленной диссертации на соискание степени кандидата геолого-минералогических наук по специальности 1.6.6 - гидрогеология. Научным руководителем является заведующий лабораторией гидрогеологии осадочных бассейнов Сибири к.г.-м.н. Дмитрий Анатольевич Новиков.
В ходе работы было проведено комплексное изотопно-гидрогеохимическое исследование природных вод восточной части Новосибирской области.
А.А. Максимова
– Впервые для региона изучен широкий комплекс химических элементов, изотопный состав воды; установлен характер равновесия природных вод с большим количеством минералов горных пород, – отметила А.А. Максимова. – Впервые показано, что для региона исследований химический состав природных вод определяется характером взаимодействия воды с горными породами; установлен генезис и геохимический тип изученных вод; проведена оценка качества природных вод восточной части Новосибирской области.
Также была проведена обработка и интерпретация большого объёма гидрогеохимических данных по нескольким районам Новосибирской области и выполнено численное физико-химическое моделирование процессов, происходящих в системе вода – порода.
Презентация вызвала большой интерес со стороны аудитории. С вопросами выступили д.т.н. А.Г. Плавник; к.г.-м.н. М.А. Фомин, к.г.-м.н. Я.В. Фомина; О.П. Изох; положительный комментарий по работе дал Д.А. Новиков.
В дальнейшем в Институте продолжат развивать охваченные в докладе направления.
Опубликовано пресс-службой ИНГГ СО РАН
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11th International Congress on the Jurassic System
