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Water balance assessment of different substrates on potash tailings piles using non-weighable lysimeters

机译:使用不可称量的溶渗仪评估钾盐尾矿堆中不同基质的水平衡

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摘要

Water balance is an important tool to evaluate water deficit or excess in crop systems. However, few studies have evaluated the water balance of vegetation grown on the residues from potash mining because the high sodium chloride levels of the residues hinder agricultural development Therefore, this study aims to measure the water balance components in eight non-weighing lysimeters installed on a potash tailings pile in Heringen (Werra), Germany. These lysimeters were filled with different mixtures of household waste incineration slags and coal combustion residues, resulting in 4 different substrates with two repetitions. Manual seeding was performed using 65% perennial ryegrass (Lolium perenne L.), 25% red fescue (Festuca rubra L) and 10% Kentucky bluegrass (Poa pratensis L.). Environmental conditions were monitored using an automatic weather station; ground-level and 1-m-high rain gauges. Precipitation and drainage were recorded weekly following the initial saturation of the lysimeters. Water balance components were determined for two hydrological years based on the expression: ET (mm) = P - D, where ET = evapotranspiration, P = precipitation and D = drainage. In addition, evapotranspiration was studied using the standard FAO Penman-Monteith equation and Haude's method. The lysimeter water balance measured in 2014 revealed an actual evapotranspiration rate of 66.4% for substrate 1, 66.9% for substrate 2, 65.1% for substrate 3 and 64.1% for substrate 4. In 2015, evapotranspiration ranged from 65.7% for substrate 4 to 70.2% for substrate 1. We observed that the FAO Penman-Monteith and Haude's evapotranspiration models generally overestimated the water use of the green coverage by 67% and 23%, respectively. Our study suggests that an evapotranspiration cover for potash tailings piles may decrease brine drainage from these piles and reduce soil and water contamination.
机译:水分平衡是评估作物系统缺水或过量的重要工具。但是,很少有研究评估钾盐开采残渣上生长的植被的水分平衡,因为这些残渣的高氯化钠含量会阻碍农业发展。因此,本研究旨在测量安装在钾盐矿上的八个非称重测渗仪中的水分平衡成分。钾盐尾矿堆在德国黑灵根(韦拉)。这些蒸渗仪充满了生活垃圾焚烧炉渣和燃煤残渣的不同混合物,从而产生了4种不同的基质,并重复了两次。使用65%的多年生黑麦草(黑麦草),25%的红羊茅(Festuca rubra L)和10%的肯塔基草(Poa pratensis L.)进行人工播种。使用自动气象站监测环境状况;地面高度和1米高的雨量计。溶渗仪初始饱和后,每周记录一次降水和排水情况。根据以下表达式确定两个水文学年的水平衡分量:ET(mm)= P-D,其中ET =蒸散量,P =降水量,D =排水量。此外,利用标准的粮农组织Penman-Monteith方程和Haude方法研究了蒸散量。 2014年测得的溶氧仪水平衡显示,底物1的实际蒸散率为66.4%,底物2为66.9%,底物3为65.1%,底物4为64.1%。2015年,底物4的蒸散量为65.7%至70.2。基质1的百分比。我们观察到,粮农组织Penman-Monteith和Haude的蒸散模型通常分别高估了绿色覆盖物的用水量67%和23%。我们的研究表明,钾盐尾矿堆的蒸散覆盖物可以减少这些堆中的盐水排放,并减少土壤和水的污染。

著录项

  • 来源
    《Journal of Environmental Management》 |2017年第1期|633-643|共11页
  • 作者单位

    Department of Agricultural Engineering - University of Kassel, Nordbahnhofstraβe la, D-37213 Witzenhausen, Germany;

    Department of Agricultural Engineering - University of Kassel, Nordbahnhofstraβe la, D-37213 Witzenhausen, Germany;

    Department of Agricultural Engineering - University of Kassel, Nordbahnhofstraβe la, D-37213 Witzenhausen, Germany;

    Department of Agricultural Engineering - University of Kassel, Nordbahnhofstraβe la, D-37213 Witzenhausen, Germany;

    Schmeisky Environmental Consultancy, Steinstrasse 21, D-37213 Witzenhausen, Germany;

    Department of Soil Science - University of Kassel, Nordbahnhofstraβe la, D-37213 Witzenhausen, Germany;

    Department of Soil Science - University of Kassel, Nordbahnhofstraβe la, D-37213 Witzenhausen, Germany;

  • 收录信息 美国《科学引文索引》(SCI);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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