Динаміка скорочення ішемізованого камбалоподібного м'яза щура Досліджено характер зміни генерації силової відповіді штучно ішемізованого камбалоподібного м'яза щура при застосуванні електричної стимуляції еферент-сигналом, модульованим за частотою. Показано, що ішемія камбалоподібного м'яза щура (muscle soleus) призводить до зменшення максимальної силової продуктивності та зниження порогової частоти виходу скорочення на тетанічний рівень. Доведено, що при роботі ішемічно ушкодженого камбалоподібного м'яза сила скорочення і час встановлення стаціонарного рівноважного стану залежали від часу розвантажувального сегмента стимуляції.
Thermodynamic parameters such as the change of entropy, internal energy, and enthalpy were calculated as a function of the relative skeletal muscle strain within the framework of a proposed thermodynamic model. A value for the Young's modulus for the skeletal muscle was also estimated. The obtained theoretical values are in a good agreement with available experimental results for the frog skeletal muscle contraction.
Goal. To study the distribution of values of magnetic susceptibility (MS) of soils of agricultural lands of the chernozem zone of the Left Bank of Ukraine and to evaluate their informativeness for control of organic carbon (Corg) of soils at the regional level. Methods. Methods of soil sampling according to DSTU 4287:2004 were used and the humus content was determined according to DSTU 4289:2004. The standard software product Statistica® was used to establish the statistical indicators, and the results of the research were visualized in the environment of MapInfo and Surfer. Results. 90 samples were taken from the upper soil horizon (0-30 cm) of lands of different types (arable land, pastures, forest), their ratio roughly corresponded to the current structure of agricultural lands. For all samples, the specific MS was determined using a kappa-containing KLY2 according to the Evans method. Conclusions. The degree of relationship between the content of sorghum in the soils of the study area did not allow making unambiguous recommendations for the use of MS by interpolation or extrapolation of values at the regional level. This is due to differences in pedogenesis and soil use. The scattering graph of MS and Corg can identify areas that meet different conditions of soil formation: steppe, meadow, gray forest. They did not find regularities in the spatial distribution of soil MS (except for the growth of values with increasing hydrothermal coefficient) and Corg content.
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