CALCULATION OF THE EFFECTIVE VOLUME HEAT CAPACITY FROM THE WAVE CHARACTERISTICS OF FROZEN SOILS

摘要

A partial empirical relation between the wave characteristics and theoretical estimates of the effective volume heat capacity of frozen layers of sandy soil in Yakutsk is established using the example of an investigation of archive material of design-survey operations. It is shown that it is possible in principle to use ground penetrating radar to solve the problem of determining theoretically, using probability mathematical models, not only the effective volume heat capacity of frozen sandy soils, but also, hypothetically, the residual thermal characteristics for a whole class of frozen dispersed soils in Central Yakutia.