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Stanisław Gołąb, Jan Sobiecki and Janusz Brudecki

Social and Somatic Determinants of Physical Fitness in Men Aged 20-70 Years from Cracow

Purpose. The aim of this study was to determine effects of social and somatic variables on changes of physical fitness in men aged 20-70 years. For this purpose a cross-sectional study of 1,420 industrial workers was carried out. Basic procedures. Correlations were examined between several variables: age, education, physical activity level, BMI, WHR, results of five Eurofit tests (flamingo balance test, plate tapping, sit and reach, standing broad jump, hand grip) and YMCA 3-minute Step Test. ANOVA and step-wise regression were used in the statistical analysis. Main findings. The obtained results point to: (1) a varied regression of motor and cardio-vascular fitness in male subjects between 20 and 70 years of age; (2) high correlation between the standing broad jump results and all the analysed variables; (3) the highest percentage of assignable variation in the results of standing broad jump, hand grip strength tests and % HRmax affected by age and BMI. Conclusions. The significance of the impact of social and somatic variables on motor fitness varies and depends on subjects' age. The regression of motor fitness in men after 50 years of age is a symptom of gradual loss of adaptability to social life concurring with andropause, which is discussed in detail in professional literature.

Open access

Janusz Gołąb, Krzysztof Urban and Elżbieta Badach


Water run-off - a natural part of water circulation in the natural environment - is a harmful and undesired phenomenon for humans. The most spectacular and most serious one is its erosive activity. In adverse conditions, such a runoff has high energy, it causes serious reshaping of a terrain and it destroys the natural environment and infrastructure. In the forest environment, a run-off process occurs basically on roads, skidding trails and in log storage sites, which are areas with soil cover properties changed by humans. The devices used for dehydrating a transport system direct water collected in the form of concentrated streams to a slope, which frequently causes serious linear damage or landslides. The objective of the tests carried out was to determine the spatial distribution of soil moisture on the area behind the outlet of devices dehydrating forest roads within the context of changes in selected soil properties affecting a risk of landslide formation. The tests included four water drains dehydrating a forest slope road with a soil surface. In the area located behind the outlet, according to the model accepted, soil samples were collected for testing a current moisture value, determining grain composition and a hydraulic conductivity coefficient, calculated based on the simplified Hazen formula. There were significant differences in the soil moisture means in the three-measurement series conducted; nevertheless, the highest moisture means were obtained after the lowest precipitation, and the lowest moisture means were obtained after the highest precipitation. It applies to all water drains observed, separately and collectively. Average moisture measures in all dehydrating facilities differed among one another, although in different sessions, this dependence was observed in various facility pairs. The statistical analysis did not demonstrate any significant differences in moisture in terms of the distance of moisture testing location from the road edge, or in locations with different distances from the water run-off line behind the outlet of dehydrating devices. Significant differences could be observed in the analysis of average moisture values in the soil layers. Such an analysis result could be explained by a relatively low soil permeability and low slope gradient on the area examined. Usually, a few percent fluctuation in soil moisture, despite precipitation diversity, in combination with a high amount of granular soil structure, does not create conditions facilitating the formation of landslides.