Analysis of the Main Factors Controlling the Formation of Subaerial Taliks, Using a One-Dimensional Mathematical Model. A Case Study for the Shestakovka River Basin (Central Yakutia)

• Main Authors: S. Popov V., A. Boronina S., L. Lebedeva S., С. Попов В., А. Боронина С., Л. Лебедева С.
• Other Authors: This study was financially supported by the Russian Science Foundation and Yakut Science Foundation Project No 22-17- 20040 “Subaerial and lake taliks in continuous permafrost in Eastern Siberia: genesis, current state and reaction to climate change”, Работа выполнена при финансовой поддержке гранта Российского научного фонда и Якутского научного фонда Проект № 22-17-20040 “Субаэральные и подозёрные талики в сплошной криолитозоне Восточной Сибири: происхождение, современное состояние и реакция на изменение климата”
• Format: Article in Journal/Newspaper
• Language: Russian
• Published: IGRAS 2024
• Subjects: permafrost; subaerial taliks; mathematical modelling; snow and land covers; многолетняя мерзлота; субаэральные талики; математическое моделирование; снежный и поверхностные покровы; Talik; Ice; wedge*; Yakutia; Якути*; Якутия
• Online Access: https://ice-snow.igras.ru/jour/article/view/1287; https://doi.org/10.31857/S2076673423040130

This study presents a mathematical model of heat transfer in a subaerial talik. The model is based on the concepts presented in classical works on permafrost, as well as on the results of geological and geophysical research carried out in the Shestakovka River basin (Central Yakutia). This model is based on the solution of the classical Stefan problem on the moving of the phase transition boundaries for a multilayer and multiphase medium. The solution was calculated on a unstructured mesh. When the phase boundaries move, thawed or frozen layers of soil are formed or wedged out. The layers include: snow cover, seasonally thawed soil, seasonally frozen and frozen sand deposits, as well as soil-vegetative layer. Published empirical relationships were used to calculate thermophysical coefficients, which are presented in this article. Simple variants of the model were considered to clarify the contribution of various factors to the process of formation and evolution of taliks. It has been established that the presence of snow cover and soil-vegetative layer have the most significant effect on the formation of taliks. Calculations show that taliks are formed in the first years of the modeled period, in the presence of snow and the absence of soil-vegetative layer. The soil-vegetative layer, depending on its composition and moisture content (ice content), can prevent the formation and development of taliks. The authors do not consider cases where shrubs contribute to snow accumulation. The humidity and iciness of the layer of sand sediments located in Central Yakutia have practically no effect on this process. На основе математического моделирования и численных экспериментов дана оценка влияния разных факторов на формирование и термический режим субаэральных таликов. Различные модельные сценарии показали, что наибольший вклад в формирование и развитие таликов вносит снежный покров, препятствующий выхолаживанию грунта в зимний период. Наличие напочвенного слоя с определенными теплофизическими параметрами может ...