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SOIL MEASUREMENT METHOD AND SOIL MEASUREMENT APPARATUS

机译:土壤测量方法和土壤测量装置

摘要

PROBLEM TO BE SOLVED: To provide a soil measurement method and a soil measurement apparatus capable of reducing the influence on the measurement of the dry density of soil by the proportion of moisture contained in soil while ensuring immediacy.;SOLUTION: A closed space 24 is formed on the soil E by a closed space forming step. A volume change is given to the closed space 24 formed in the closed space forming step by a volume change applying step. In a pressure fluctuation measuring step, the pressure fluctuation of the closed space 24 given the volume change in the volume change applying step by a dry density deriving step is measured. The dry density of the soil E is derived based on the pressure fluctuation of the closed space 24 measured in the pressure fluctuation measuring step by the drying density deriving step. The influence of the proportion of moisture contained in the soil E to the dry density of the soil E derived in the drying density deriving step is extremely small. This makes it possible to reduce the influence on the measurement of the dry density of the soil E by the proportion of moisture contained in the soil E while ensuring immediacy.;SELECTED DRAWING: Figure 3;COPYRIGHT: (C)2019,JPO&INPIT
机译:解决的问题:提供一种土壤测量方法和土壤测量设备,该方法和土壤测量设备能够在确保立即的同时减少土壤中水分含量对土壤干密度测量的影响。通过封闭空间形成步骤在土壤E上形成。通过容积变化施加步骤,对在封闭空间形成步骤中形成的封闭空间24进行容积变化。在压力变动测量步骤中,测量通过干密度推导步骤在体积变化施加步骤中给定体积变化的情况下封闭空间24的压力波动。土壤E的干燥密度是基于由干燥密度导出步骤在压力波动测量步骤中测量的封闭空间24的压力波动而得出的。土壤E中所含水分的比例对在干燥密度导出步骤中导出的土壤E的干燥密度的影响极小。这样就可以减少土壤E中所含水分的比例,同时又确保即时性,从而减少对土壤E干密度测量的影响。;部分制图:图3;版权:(C)2019,JPO&INPIT

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