Zmiany w strukturze osadów piaszczystych i pylastych po 1000 cyklach zamarzania i rozmarzania – wstępne wyniki eksperymentu laboratoryjnego
DOI:
https://doi.org/10.26485/AGL/2023/113/6Słowa kluczowe:
permafrost, krioturbacje, cykle zamrażania-rozmrażania, eksperyment laboratoryjny, reorganizacja ziarenAbstrakt
Eksperyment laboratoryjny obejmował analizę zmian zachodzących w strukturze osadów, które wynikają z reorganizacji ziaren osadów poddawanych powtarzającym się cyklom zamarzania i rozmarzania. Wykorzystano do tego urządzenie zamrażająco-rozmrażające pracujące w zakresie temperatur od –5°C do +10°C. W pięciu przeźroczystych cylindrach z pleksi umieszczono w kolejności od dna następujące osady: piasek gruboziarnisty, piasek drobnoziarnisty, pył i ponownie piasek drobnoziarnisty. W każdym z cylindrów stopień wilgotności osadów był inny. Obserwacje zmian przeprowadzono makroskopowo na podstawie fotograficznej dokumentacji cylindrów wykonanej przed rozpoczęciem eksperymentu oraz po 250, 500, 750 i 1000 cyklach zamarzania i rozmarzania. Wykazano, iż największą reorganizacją cechuje się osad pyłowy, a najmniejszą piasek gruboziarnisty. Ponadto, istotny wpływ na reorganizację ziaren miała wilgotność próbki. Największa liczba struktur powstała na granicach pomiędzy piaskiem drobnoziarnistym i pyłem w cylindrach o największej wilgotności
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