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首页> 外文期刊>Journal of Science and Technology of Agriculture and Natural Resources >Estimation of Water Vapor Transport in Unsaturated Soils under Osmotic Potential
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Estimation of Water Vapor Transport in Unsaturated Soils under Osmotic Potential

机译:渗透势下非饱和土壤水汽运移的估算

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摘要

The transport process of chemical-fertilizers, radioactive materials and other solutes in soils and porous media is important to understand the environmental and economic effects of industrial, agricultural and urban waste disposal methods. In unsaturated porous media, large gradient in aqueous osmotic potential derives significant water vapor fluxes towards regions of high solute concentrations. In this research, the effects of osmotic potential (resulting from salinities of 0.5, 1 and 1.5%) on water vapor transport in three soil textures (silty clay loam, loam and sandy loam) were examined by using a physical laboratory model. Then, the experimental results were compared with Kelly and Selker (2001) model for validation of the predicted water vapor transport. The results showed that the rate of water vapor transport reduces significantly as soil texture gets heavier. For example, in salinity of 0.5% and 5th day of experiment, the amount of transported vapor in sandy loam, loam and silty clay loam soils was 0.362, 0.196 and 0.12 kg/m2, respectively. Large osmotic potential near the high solute concentration in soils caused significant vapor movement toward dense solutions. In salinity of 1.5%, transported vapor in these soils was 1.47, 0.723 and 0.38 kg/m2, respectively. Total water vapor movement until the 15th day was more than the 5th day. Comparison of experimental results with Kelly and Selker model results, using Mathcad PLUS 6.0 software, showed a good agreement between the observed and predicted data. Since water vapor delivered from uncontaminated soils to the contaminated soils can result in increased contaminant plume volume, these physical and chemical processes must be included in the predictive models of contaminant transport in the vicinity of concentrated sources Keywords: Porous media, Solute transport, Water potential. Full-Text Type of Study: Research | Subject: Ggeneral Received: 2012/03/17 | Accepted: 2012/09/23 | Published: 2013/09/16 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:化学肥料,放射性物质和其他溶质在土壤和多孔介质中的运输过程对于理解工业,农业和城市废物处理方法对环境和经济的影响非常重要。在不饱和多孔介质中,水渗透势的大梯度会导致大量的水蒸气通向高溶质浓度的区域。在这项研究中,使用物理实验室模型研究了渗透势(0.5、1和1.5%的盐度)对三种土壤质地(粉质壤土壤土,壤土壤土和沙质壤土)中水蒸气传输的影响。然后,将实验结果与Kelly和Selker(2001)模型进行比较,以验证预测的水蒸气传输。结果表明,随着土壤质地变重,水蒸气的输送速率明显降低。例如,在盐度为0.5%和实验第5天时,沙壤土,壤土和粉质粘土壤土中的水蒸气输送量分别为0.362、0.196和0.12 kg / m2。在土壤中高溶质浓度附近的大渗透势会导致大量蒸汽向致密溶液移动。在盐度为1.5%时,这些土壤中的迁移蒸气分别为1.47、0.723和0.38 kg / m2。直到第15天的总水蒸气运动超过第5天。使用Mathcad PLUS 6.0软件将实验结果与Kelly和Selker模型结果进行比较,发现观测数据与预测数据之间有很好的一致性。由于从未受污染的土壤输送到受污染的土壤的水蒸气会导致污染物羽流量增加,因此,这些物理和化学过程必须包括在污染物在浓缩源附近的迁移的预测模型中。关键词:多孔介质,溶质迁移,水势。全文研究类型:研究|主题:一般接收时间:2012/03/17 |接受:2012/09/23 |发布:2013/09/16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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