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Effects of shallow water tables on soil aeration, water quality, and physiological growth of soybean

机译:浅层地下水位对大豆通气,水质和生理生长的影响

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摘要

This study was conducted to investigate the effects shallow water table depths on soil aeration, groundwater quality and on some physiological growth and yield parameters of soybean. The experiments were conducted in two environmentally controlled growth chambers using sixteen lysimeters. Water table (WT) treatments were established on 37 day after planting (DAP), at depths of 0.15-, 0.30-, 0.45- and 0.60-m below the soil surface. Soil aeration status was determined by measuring soil oxygen concentrations at 0.15-, 0.30-, 0.60-m depths in the lysimeters. Effects of water table depths on groundwater quality were determined by observing the movement of residual soil nitrate and applied metolachlor at three different depths (0.20-, 0.40-, and 0.60-m) in the soil profile. Measurements on different physiological parameters (photosynthesis rate, stomatal conductance, transpiration rate, chlorophyll content and intercellular CO[subscript]2) and leaf temperature were taken on a weekly basis;The results of study showed that oxygen concentration was significantly reduced by raising the water table depth. Differences in soil oxygen concentrations for various soil depths were also significant. Soil oxygen concentration at shallow soil depths was always higher compared to deeper soil depths. The variation in soil oxygen concentrations with time was not significant. Significant reductions in both NO[subscript]3-N and metolachlor concentrations were observed by maintaining shallow WT depths. For 0.15-m WT treatment, the NO[subscript]3-N and metolachlor concentrations were 54 and 63%, respectively, lower compared to 0.60-m WT treatment. The analysis of drainage outflow data also supported the fact that shallow WT treatments can reduce the leaching of NO[subscript]3-N and metolachlor to groundwater. A week after the establishment of WT treatments, different physiological parameters of soybean were significantly affected. Photosynthesis rate, stomatal conductance and transpiration rates were significantly reduced when WT was raised to 0.15-m depth. Soybean yield was significantly reduced with the decrease in WT height. The results of this study indicate that, on the average, 48% increase in yield is possible by maintaining WT at 0.60-m depth.
机译:本研究旨在研究浅层地下水位对土壤通气,地下水水质以及大豆某些生理生长和产量参数的影响。实验是在两个环境控制的生长室中使用16辐射力计进行的。种植后第37天(DAP)建立了地下水位(WT)处理,深度为土壤表面以下0.15-,0.30-,0.45-和0.60-m。通过在溶渗仪中分别测量0.15-,0.30-,0.60-m深度的土壤氧浓度来确定土壤通气状态。通过观察土壤剖面中三个不同深度(0.20-,0.40-和0.60-m)的残留土壤硝酸盐和施用的异丙甲草胺,确定地下水位深度对地下水水质的影响。每周测量不同的生理参数(光合作用速率,气孔导度,蒸腾速率,叶绿素含量和细胞间CO 2含量)和叶片温度;研究结果表明,升高水分能显着降低氧气浓度桌子深度。不同土壤深度的土壤氧浓度差异也很明显。与较深的土壤深度相比,浅土深度的土壤氧气浓度始终较高。土壤氧浓度随时间的变化不显着。通过维持较浅的WT深度,观察到NO 3 -N和异丙甲草胺浓度均显着降低。对于0.15-m WT处理,NO 6 -N和甲草胺的浓度分别为54和63%,比0.60-m WT处理低。排水流量数据的分析也支持以下事实:浅水处理可以减少NO [3-] N和异丙甲草胺向地下水的淋溶。 WT处理建立一周后,大豆的不同生理参数受到显着影响。当野生型提高到0.15-m深度时,光合作用,气孔导度和蒸腾速率显着降低。随着WT高度的降低,大豆产量显着降低。这项研究的结果表明,通过将WT保持在0.60-m的深度,平均可以使产量提高48%。

著录项

  • 作者

    Sarwar, Tahir;

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  • 年度 1995
  • 总页数
  • 原文格式 PDF
  • 正文语种 en
  • 中图分类

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