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Changes in Some Physical and Mechanical Properties of a Structurally Unstable Soil after Flood Irrigation

机译:洪水灌溉后结构不稳定土的某些物理和力学性质的变化。

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Soil tilth is crucial to seedling emergence, plant growth, and crop yield. Soil tilth of unstable soil is very susceptible to change. Internal forces originating from matric suction can change soil physical properties. A laboratory study was conducted on pots of a surface silty clay loam soil of Khomeinishahr series (fine-loamy, mixed, thermic Typic Haplargids, USDA), located in Research Farm of Isfahan University of Technology. Soil surface subsidence, bulk density, cone index, and tensile strength were measured after first flood irrigation. Results showed that the seedbed (0-20 cm) with a bulk density of 1.2 Mg.m-3 will be changed to a massive soil with high values of bulk density, cone index, and tensile strength after soil wetting. Slaking, slumping and coalescence of the soil caused soil surface to subside about 1.5 cm in 20 cm soil layer. After irrigation, cone index and tensile strength increased abruptly with decreasing of moisture content. It is shown that the dominant source of strength (cone index and tensile strength) gain during drying is the effective stress due to matric suction. In the absence of external loads, physical state (tilth) of the soil returned back to the original state. Therefore, soil slaking and slumping and rearrangement of particles along with the internal forces are the factors leading to soil hardness. Keywords: Effective stress, Matric suction, Capillary forces, Settlement, Bulk density, Cone index, Tensile strength. Full-Text Type of Study: Research | Subject: Ggeneral Received: 2008/01/9 Related Websites Scientific Publications Commission - Health Ministry Scientific Publications Commission - Science Ministry Yektaweb Company Site Keywords ?????, Academic Journal, Scientific Article, ???? ????? ??, ???? ????? ??, ???? ????? ??, ???? ????? ??, ???? ????? ??, ???? ????? ??, ???? ?? Vote ? 2015 All Rights Reserved | JWSS - Isfahan University of Technology
机译:土壤倾角对幼苗出苗,植物生长和农作物产量至关重要。不稳定土壤的土壤倾角非常容易发生变化。基质吸力产生的内力会改变土壤的物理性质。对位于伊斯法罕工业大学研究农场的霍梅尼沙赫尔系列(细粒小麦,混合小麦,热典型Typal Haplargids,USDA)的表层粉质粘土壤土盆进行了实验室研究。第一次洪水灌溉后,测量土壤表面沉降,堆积密度,圆锥指数和抗张强度。结果表明,堆积密度为1.2 Mg.m-3的苗床(0-20厘米)在土壤润湿后将变成具有高堆积密度,锥度指数和抗张强度值的块状土壤。土壤的塌陷,塌陷和聚结使土壤表面在20厘米的土壤层中沉降约1.5厘米。灌溉后,锥度指数和抗张强度随着含水量的减少而突然增加。结果表明,干燥过程中强度(圆锥指数和拉伸强度)增加的主要来源是由于基质吸力引起的有效应力。在没有外部负载的情况下,土壤的物理状态(倾斜度)返回到原始状态。因此,土壤的崩解和塌陷以及颗粒的重新排列以及内力是导致土壤硬度的因素。关键字:有效应力,基质吸力,毛细作用力,沉降,堆积密度,锥指数,拉伸强度。全文研究类型:研究|主题:一般收稿日期:2008/01/9相关网站科学出版物委员会-卫生部科学出版物委员会-科学部Yektaweb公司网站关键字??????,Academic Journal,Scientific Article,???? ?????? ??,???? ?????? ??,???? ?????? ??,???? ?????? ??,???? ?????? ??,???? ?????? ??,???? ??投票吗? 2015版权所有| JWSS-伊斯法罕工业大学

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