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Re-search Shrink-Swell Measurement and Relationship with Soil Properties of Black Clayey Tropical Vertisols

机译:重新搜索收缩 - 膨胀测量和黑色粘土性热带活醇土壤性质的关系

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Shrink-swell phenomenon is a complex process in vertic group of soils. Their dynamics in soils has long been presented through various models, field and laboratory methods. The present study finds out a feasible way to measure the shrink-swell potential and the key responsible factors in soil which are most influential in determining this phenomenon. Four shrink- swell parameters such as coefficient of linear extensibility (COLE), coefficient of linear shrinkage (COLS), percent volume change on swelling (PVCsw), percent volume change on shrinkage (PVCs) measured at 25°C (room temperature,RT), 40°C and 110°C were used to quantify shrink - swell phenomenon. Results indicated that heating the soil cake at 110°C over 40°C does not bring higher change (0-10 %) in linear shrinkage, the corresponding value for volume change at 110°C showed greater change (3-61%) hence, COLS at 40°C and PVCs at 110°C amongst others were promising and may be recommended for routine measurement of shrink-swell phenomenon in the laboratory. Out of three the different measurement devices, cube shaped box appeared to be the better option. The soil properties which represent carbon content and soil substrate have significant correlations (p<0.01, p<0.05) with the corresponding shrink-swell parameters. The multiple regression analysis showed 69 percent variation for PVCs 110° C and 63 percent for COLS 40° C
机译:收缩 - 膨胀现象是垂直于土壤中的复杂过程。他们在土壤中的动态长期以来一直通过各种型号,现场和实验室方法提出。本研究发现了一种可行的方法来测量收缩膨胀潜力和土壤中的关键负责因子,这些方法在确定这种现象时最有影响力。四个收缩膨胀参数,如线性伸长系数(COLE),线性收缩系数(COL),肿胀(PVCSW)的体积变化百分比,在25℃下测量的收缩率(PVCs)的体积变化(室温,室温),40℃和110°C用于量化收缩 - 膨胀现象。结果表明,在110℃下加热土壤滤饼在40℃下不会引起更高的变化(0-10%)在线性收缩,相应的体积变化值在110℃下表现出更大的变化(3-61%) ,在其他40°C和110°C的PVC的COL是有前途的,并且可能建议在实验室中进行常规测量收缩膨胀现象。在三个不同的测量装置中,立方体形盒似乎是更好的选择。用相应的收缩膨胀参数,代表碳含量和土壤基质的土壤性质具有显着的相关性(P <0.01,P <0.05)。多元回归分析显示PVCS 110°C的69%,COLS 40°C的63%

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