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Měření půdní vlhkosti metodou EIS a teplotní stratifikace půdy v oblastech Khan Khentii strictly protected area a Khowsgol lake v Mongolsku
 Sobotka, Milan
In July 2014, the Strictly Protected Area of Khan Khentii and Lake Khowsgol in Mongolia carried out moisture and soil temperature measurements in July 2014 to determine the link between these variables and permafrost. Measurement of soil moisture was performed by EIS (electrical impedance spectrometry). A total of 146 measurements were performed and 49 soil probes were digested. It is always measured in the A and B soil horizons. Measurements up to exceptions did not exceed 30 cm in depth with respect to the content of the skeleton whose skeletal content increased. The direct relationship of permafrost to thermal stratification of soil horizons has been demonstrated. The occurrence of permafrost up to 150 cm from the first measurement was characterized by a difference in temperature between the steps of up to 2 °C. In the case of permafrost deeper, the transition between the measuring steps was smoother, on average by 0.6 °C. By measuring the soil moisture Found by the highest average soil moisture at the nearest tenth, Goricho. Abnormally high soil moisture at this site may be due to the growth of the active layer of permafrost in the primary phase of its melting in the severe anthropogenic damage to the Gorkhy-Terelch National Park landscape.
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