where Qi - heat energy of water flow before contacting the soil sample, J; QT - heat energy of suspension flow after contacting the soil sample, J, ΔQsolid, ΔQiC - changes in water flow heat energy, J. Erosion resistance potential of frozen soil is determined according to total power required to destroy the unit weight of frozen soil and integral energy and is calculated according to formula where Ai - kinetic energy of water flow before contacting the soil sample, J; At - kinetic energy of suspension flow after contacting the soil sample, J; Qi -heat energy of water flow before contacting the soil sample, J; QT - heat energy of suspension flow after contacting the soil sample, J; ms - weight of soil destroyed, kg. The method provides for measurement of total erosion resistance potential and thawing potential for frozen soils.;EFFECT: measuring total erosion resistance potential and thawing potential for frozen soils.;3 cl, 4 dwg, 1 tbl"/> METHOD FOR MEASURING EROSION RESISTANCE POTENTIAL FOR FROZEN SOIL
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METHOD FOR MEASURING EROSION RESISTANCE POTENTIAL FOR FROZEN SOIL

机译:冻土抗侵蚀能力的测定方法

摘要

FIELD: physics; measurement.;SUBSTANCE: the said utility invention relates to agriculture, in particular, to methods for studying erosion processes on soil surface due to melt waters and can be used in soil science, land reclamation and hydrology. The method implies simulation study of erosion in a water flow table and calculation of power consumed to destroy the sample unit weight by metering water flow height before and after contacting the sample and suspension flow rate. Integral energy consumed for thermal physical and chemical processes during unit weight melting is calculated as a function of the sample initial temperature according to formula where Qi - heat energy of water flow before contacting the soil sample, J; QT - heat energy of suspension flow after contacting the soil sample, J, ΔQsolid, ΔQiC - changes in water flow heat energy, J. Erosion resistance potential of frozen soil is determined according to total power required to destroy the unit weight of frozen soil and integral energy and is calculated according to formula where Ai - kinetic energy of water flow before contacting the soil sample, J; At - kinetic energy of suspension flow after contacting the soil sample, J; Qi -heat energy of water flow before contacting the soil sample, J; QT - heat energy of suspension flow after contacting the soil sample, J; ms - weight of soil destroyed, kg. The method provides for measurement of total erosion resistance potential and thawing potential for frozen soils.;EFFECT: measuring total erosion resistance potential and thawing potential for frozen soils.;3 cl, 4 dwg, 1 tbl
机译:领域:物理学;所述实用新型涉及农业,尤其涉及研究由于融水导致的土壤表面侵蚀过程的方法,可用于土壤科学,土地开垦和水文学。该方法意味着对水流表中的侵蚀进行模拟研究,并通过测量接触样品前后的水流高度和悬浮液流速来计算破坏样品单位重量所消耗的功率。根据公式其中Q i -接触土壤样品J之前水流的热能; Q T -接触土壤样品后悬浮液的热能,J,ΔQ solid ,ΔQ iC -水的变化流动热能,J。冻结土壤的耐蚀性是根据破坏冻结土壤的单位重量所需的总功率和积分能量确定的,并根据公式其中A i -接触土壤样品J之前水流的动能; A t -接触土壤样品后悬浮液的动能,J; Q i -接触土壤样品之前水流的热能,J; Q T -接触土壤样品后悬浮液的热能,J; m s -破坏的土壤重量,kg。该方法提供了对冻土的总抗腐蚀潜力和解冻潜力的测量。效果:测量了冻土的总抗腐蚀潜力和解冻潜力。3cl,4 dwg,1 tbl

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