马玉莹, 雷廷武, Xiusheng Yang. 体积置换法测量土石混合物组分含量[J]. 农业工程学报, 2015, 31(9): 85-91. DOI: 10.11975/j.issn.1002-6819.2015.09.014
    引用本文: 马玉莹, 雷廷武, Xiusheng Yang. 体积置换法测量土石混合物组分含量[J]. 农业工程学报, 2015, 31(9): 85-91. DOI: 10.11975/j.issn.1002-6819.2015.09.014
    Ma Yuying, Lei Tingwu, Xiusheng Yang. Volume replacement method for partitioning contents of rocks, soil particles and water mixture[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2015, 31(9): 85-91. DOI: 10.11975/j.issn.1002-6819.2015.09.014
    Citation: Ma Yuying, Lei Tingwu, Xiusheng Yang. Volume replacement method for partitioning contents of rocks, soil particles and water mixture[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2015, 31(9): 85-91. DOI: 10.11975/j.issn.1002-6819.2015.09.014

    体积置换法测量土石混合物组分含量

    Volume replacement method for partitioning contents of rocks, soil particles and water mixture

    • 摘要: 土石混合物组分含量测量在农业生产、建筑施工及水利工程等方面都有重要的意义。该文根据体积置换原理测量土石混合物比例、土壤含水率、容重、孔隙度/孔隙比等一系列土壤物理参数。给出了测量原理、设备、试验方法与过程。采用陕西杨凌的黏黄土、吉林黑土以及粒径为5~10 mm的石砾,预制不同体积含水率(10%、15%、20%)、石砾体积比例(10%、15%、20%)和土壤颗粒体积比例(40%、45%、50%)的土样。首先采用体积置换法测得土样中石砾、土壤颗粒和土壤水的总体积,随后取出土样中的石砾,用体积置换法测得石砾体积,进而得到土壤颗粒和土壤水的体积,并据此得到土壤含水率、土壤容重、土中气体含量、土壤孔隙度和孔隙比。用烘干法测量得到土壤容重和含水率,将2种方法测得的结果对比分析表明,使用体积置换法测得的土壤含水率比烘干法测量的结果大,相对误差在5%左右,测量的土壤容重偏小约1%,土壤气体含量的测量相对误差约为2%。测量土壤孔隙度的相对误差约为1%,土壤孔隙比的测量误差为1%~1.5%。表明体积置换法可以较为准确地测量土石混合物中各组分的相对含量,具有操作便捷、测量精度高、有普遍适用性等优点,可以为相关研究和测量提供基础。

       

      Abstract: Abstract: The effective measurement of the components in soil and rock mixture composition is of great importance in such studies and applications as agricultural production, civil and hydraulic engineering. This paper presents a volume replacement method for accurate measurement of soil, water and rock mixture components, including a series soil physical parameters measurement such as rock content and density, water content, soil bulk density, volume of soil air, porosity and void ratio. The measurement principle is based on the physic model of gas-liquid-solid composition in soils. Typically, soil consists of soil particles, rock fragments, water and air. A clay loam from Yangling of Shaanxi Province and a black soil from Jilin Province were used for the demonstrational measurements. The cleaned and dried rock fragments with the particle sizes of 5-10 mm were used for the experiments. Soil samples were prepared at 3 volumetric moisture contents as 10%, 15%, and 20%. The percentage volumes of rock mass were about 10%, 15%, and 20%. And the volumes of soil particles were designed as 40%, 45%, and 50%. Soil samples prepared were packed into the sampling rings of 100 cm3 in volume. The samples were placed into a constant volume container (CVC) with a known volume before it was weighted. Then the CVC was filled full of distilled water to replace air-filled space in the soil sample and the container, before it was weighted to determine the replaced air-filled space, and the total volume of rock, soil particles and soil water. The rock fragments were cleaned and dried before were weighted and put into the CVC to be filled full of water, so as to determine their volumes. The volumes and mass of soil particles and soil water were calculated after the volume and mass of rocks were determined. The volume of air was computed by the difference between the volume of sampling ring and the total volume of rocks, soil particles and soil water. After the soil samples were measured by volume replacement method, they were put into an oven to dry under 105℃ for 72 h to determine the mass of soil particles and soil water, to determine the soil moisture content and bulk density by using conventional oven-dry method. The air-filled volume in soil, as well as soil porosity and void ratio could be determined after measuring the volume of rocks, soil particles and soil water. The results measured by these two methods were compared. The results showed that the soil water contents measured by the volume replacement method with a CVC were higher than those obtained by the oven-dry method, with the relative errors about 5%. The measurement errors in soil bulk densities between the two methods were about 1%. The air-filled volumes of the soil measured by the 2 methods produced errors of about 2%. Compared with conventional oven-dry method, the relative errors in the measured soil porosities by applying volume replacement method were about 1%, and the measurement errors of void ratios were 1%-1.5%. The results indicate the feasibilities of accurate and effective measurement of soil particle and rock mixture components using the volume replacement method, which is the expansion and improvement for the previous measurement method by using fine-grained soils. Generally, for the measurement of soil particle and rock mixture composition, the proposed volume replacement method by using a CVC for a group measurement of soil physical parameters (soil water content, bulk density, soil air-filled volume, porosity and void ratio) in this study has such advantages as simple operation procedure, time efficient and low energy consumption. Besides, this volume replacement method with a CVC also can provide a helpful tool for the related experiments and measuring methods.

       

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