• The research results of the effect of covered soil density on reducing radon emanation rate are introduced.

    介绍了覆土密度对降低氡析出率影响的试验研究结果。

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  • Model tests of large driven pile jacked into sands were conducted to obtain the soil density changes due to the compaction.

    通过砂土中的大型沉桩模型试验,得出了桩周土体相对密度的变化规律。

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  • The soil density is decreased, and the disperse coefficient and porosity are increased in the sites where were burnt in successive years.

    连年火烧使土壤密度比未烧林地下降,而孔隙度和分散系数升高。

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  • The soil density of control area of every soil layers of four sample plots in the meadow steppe and typical steppe is lower than the severe degeneration area;

    草甸草原、典型草原样地各土层对照区土壤密度均低于重度退化区。

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  • In thiS model, non-uniformly variations of soil density and shear modulus with depth are taken into consideration. Numerical computations are conducted for typical cases.

    在本模型中考虑了土壤特性(如密度与剪切模量) 沿深度的非均匀变化,通过对典型场地剖面的数值计算探讨了有关因素对场地地震反应的影响。

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  • Saturation of silty clay is related with soil density, condition of experimentation, moisture contents, transportation and preservative condition of soil sample and so on.

    粉质粘土饱和度与其密度、含水量、试验条件及土样运输和保存等因素密切相关。

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  • The results showed that after skidding operation, the soil density increased, the soil moisture condition got bad, the soil porosity and the contents of soil nutrients decreased.

    通过对半悬索道集材后林地土壤理化性质的分析,结果表明:半悬索道集材后土壤容重增加,土壤结构和水分性能变差,土壤养分含量下降。

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  • Taking the soil density and water content into account, a numerical model of moisture migration in unsaturated loess subgrade was given, and parameters of the model were obtained.

    考虑含水率和密度影响,给出了非饱和黄土路基水分场的计算模型,探讨和确定了模型参数。

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  • After that it is pointed out that compared with soil density changes, water content change can result in more variations of coefficient of thermal conductivity and specific volume heat of loess.

    相对于随密度的变化,黄土导热系数和比热容随含水量的变化尤为显著,含水量变化可以引起热参数较大的变化。

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  • Soil density and soil particle of the loam are decreased but those of the sand are increased.

    壤土的土壤密度、比重降低,而砂土的土壤密度、比重增高。

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  • Using the latter, with the correlativity of soil 'density and the velocity of the Rayleigh surface wave, we can obtain the compaction of the subgrade.

    后者则是用已得到的各层瑞雷波速度值,利用土密度与瑞雷波速的相关关系计算各层的压实度。

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  • Using the latter, with the correlativity of soil 'density and the velocity of the Rayleigh surface wave, we can obtain the compaction of the subgrade.

    后者则是用已得到的各层瑞雷波速度值,利用土密度与瑞雷波速的相关关系计算各层的压实度。

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