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首页> 外文期刊>Frontiers of environmental science & eng >Influence of the sewage irrigation on the agricultural soil properties in Tongliao City, China
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Influence of the sewage irrigation on the agricultural soil properties in Tongliao City, China

机译:通辽市污水灌溉对农业土壤性质的影响

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摘要

Increasing shortages of fresh water has led to greater use of treated wastewater for irrigation of crops. This study evaluates the spatial variability of soil properties after irrigation with wastewater and freshwater. Geostatistical techniques were used to identify the variability of soil properties at the different sites. A set of physical and chemical soil properties were measured including total nitrogen (TN), total phosphorus (TP), organic matter (OM) and soil moisture. The TN concentration levels varied from 567 to 700 mg·kg~(-1), while OC levels ranged from 7.3 to 16.3mg·kg~(-1) in wastewater-irrigated zones. The concentration levels of TP were between 371.53 and 402.88 mg·kg~(-1) for the wastewater-irrigated sites. Wastewater irrigation resulted in higher TN, TP and OM concentrations by 18.4%, 8% and 25%, respectively. The highest TN and OM occurred along the wastewater trunk. It was also observed that nitrogen concentrations correlate with the soil's organic matter. The increase of salinity may be associated with the increase of pH, which might suggest that a reduction of pH will be beneficial for plant growth due to the decrease of salinity. The average concentrations of nitrogen in topsoil were higher than those in subsurface soils in irrigated areas. Such differences of the N profile might be due to variations in organic matter content and microbial populations. Consistent with TN and OM, soil C:N decreased significantly with an increase of depth. This phenomenon possibly reflects a greater degree of breakdown and the older age of humus stored in the deeper soil layers. The analysis of pH levels at different depths for the three sites showed that pH values for wastewater irrigation were slightly lower than the controlled sites at the same depths.
机译:淡水的日益增加导致人们更多地使用经过处理的废水灌溉农作物。本研究评估了废水和淡水灌溉后土壤性质的空间变异性。地统计学技术用于确定不同地点土壤性质的变化性。测量了一组物理和化学土壤特性,包括总氮(TN),总磷(TP),有机质(OM)和土壤湿度。污水灌溉区的总氮含量在567至700 mg·kg〜(-1)之间,而OC含量在7.3至16.3mg·kg〜(-1)之间。污水灌溉场地的TP浓度水平在371.53和402.88 mg·kg〜(-1)之间。废水灌溉导致TN,TP和OM浓度分别升高了18.4%,8%和25%。最高TN和OM发生在废水干线上。还观察到氮浓度与土壤有机质相关。盐度的增加可能与pH值的升高有关,这可能表明由于盐度的降低,pH值的降低将有利于植物的生长。灌区表层土壤中氮的平均浓度高于地下土壤。 N分布的这种差异可能是由于有机物含量和微生物种群的变化。与TN和OM一致,土壤C:N随深度增加而显着下降。这种现象可能反映了更大程度的破坏,并且腐殖质年龄更大,储存在更深的土壤层中。对三个地点不同深度的pH值进行分析表明,在相同深度处,废水灌溉的pH值略低于受控地点。

著录项

  • 来源
    《Frontiers of environmental science & eng》 |2013年第2期|273-280|共8页
  • 作者单位

    School of Civil Engineering and Architecture, Beijing Jiaotong University, Beijing 100044, China;

    School of Civil Engineering and Architecture, Beijing Jiaotong University, Beijing 100044, China;

    School of Civil Engineering and Architecture, Beijing Jiaotong University, Beijing 100044, China;

    School of Civil Engineering and Architecture, Beijing Jiaotong University, Beijing 100044, China;

    Department of Soil and Water Sciences, College of Resources and Environmental Sciences, China Agricultural University, Beijing 100094, China;

    School of Civil Engineering and Architecture, Beijing Jiaotong University, Beijing 100044, China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    spatial variability; soil properties; ground-water and sewage irrigation;

    机译:空间变异性土壤性质;地下水和污水灌溉;

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