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Analiza obciążeń kończyny dolnej podczas wykonywania ćwiczeń na stepie

100%

Jochymczyk-Woźniak K. , Bonk A.

tom z. 8

51--56

Grupę badawczą stanowiły cztery studentki bez jakiegokolwiek doświadczenia w step aerobiku. Zadanie ruchowe polegało na 15-krotnym powtórzeniu, bez przerwy, kroku basic step dla dwóch wysokości stepu-10 cm i 15cm. Parametry, które zostały wykorzystane do oceny obciążeń działających na kończyny dolne oraz stopy człowiek, to: składowa pionowa siły reakcji podłoża, współczynnik obciążenia oraz siły nacisku stopy na podłoże. Badania przeprowadzono z wykorzystaniem platform dynamometrycznych AMTI oraz wkładek do pomiaru sił reakcji podłoża MEDILOGIC.

Step aerobics is a very intense and exhausting physical activity. Classes are led with using the platform, which height is being regulated behind the help so-called floors. Aim of this study is to analyze the loads acting on the human movement during basic step. The studies are preliminary research introducing into issues connected from burdens of human movement during exercise on the step.

Comparing Varve Counting And 14C-Ams Chronologies In The Sediments Of Lake Żabińskie, Northeastern Poland: Implications For Accurate 14C Dating Of Lake Sediments

70%

Bonk A. , Tylmann W. , Goslar T. , Wacnik A. , Grosjean M.

tom Vol. 42, no.1

159--171

Varved lake sediments from Lake Żabińskie (northeastern Poland) provide a highresolution calendar-year chronology which allows validation of 14C dating results. Microscopic analysis of the varve microfacies revealed that laminations found in Lake Żabińskie were biogenic (calcite) varves. Three independent counts indicated a good preservation quality of laminae in the 348 cm long sediment profile which contained 1000+12/-24 varves. The varve chronology was validated with the 137Cs activity peaks, the tephra horizon from the Askja eruption at AD 1875 and with the timing of major land-use changes of known age inferred from pollen analysis. 32 AMS 14C dates of terrestrial macrofossils distributed along the profile were compared with the varve chronology. After identification of outliers, the free-shape model performed with 21 14C dates provided the best possible fit with the varve chronology. We observed almost ideal consistency between both chronologies from the present until AD 1250 while in the lower part (AD 1000–1250) the difference increases to ca. 25 years. We demonstrate that this offset can be explained by too old radiocarbon ages of plant remains transported to the lake by the inflowing creek. Results of this study highlight that careful interpretation of radiocarbon age-depth models is necessary, especially in lakes where no annual laminations are observed and no independent method are used for cross-validation.