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Spatio-temporal patterns and factors controlling the hydrogeochemistry of the river Jhelum basin, Kashmir Himalaya

机译:克什米尔喜马拉雅山耶鲁姆河流域水文地球化学的时空格局及控制因素

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摘要

River Jhelum is a major source of water for growing population and irrigation in the Kashmir Himalaya. The region is trending towards water scarcity as well as quality deterioration stage due to its highly unregulated development. The existence of few literature on various aspects of the basin prompts us to study the spatio-temporal variability of its physicochemical parameters and thereby to understand the regulating hydrogeochemical mechanisms based on 50 samples collected during high flow (June 2008) and low flow (January 2009) periods. The water chemistry exhibited significant spatial variability reflecting the mixing processes in the basin. The seasonal effect does change the concentration of ions significantly with modest variability in the order of ionic abundance. The Ca2+ ion among cations and HCO3- ion among anions dominate the ionic budget and correlates significantly with the diverse lithology of the basin. Three major water types, i.e., Ca-Mg-HCO3 (72 %), Ca-HCO3 (12 %), and Mg-Ca-HCO3 (16 %), suggest that the chemical composition of water is dominantly controlled by carbonate lithology, besides a significant contribution from silicates. However, at certain sites, the biological processes and anthropogenic activities play a major role. Relatively, the lower ionic concentration during high flow period (summer season) suggested the significant influence of higher discharge via dilution effect. The higher discharge due to higher rainfall and snow melting in response to rising temperature in this period leads to strong flushing of human and agricultural wastes into the river. The factor analysis also reflected the dominant control of varied lithology and anthropogenic sources on the water quality based on the four significant factors explaining collectively about 70-81 % of the total data variance. A two-member chloride mixing model used to estimate the discharge contribution of tributaries to the main river channel showed reliable results. It may be mentioned that the regular and continuous contamination through anthropogenic sources is likely to jeopardize and degrade the water quality in the near future. Thus, critical management approaches and strategies are very imperative for its future sustainability.
机译:杰鲁姆河是克什米尔喜马拉雅山人口增长和灌溉的主要水源。由于该地区高度不受管制的发展,该地区正趋向于缺水和质量恶化阶段。流域各个方面的文献很少,这促使我们研究其理化参数的时空变化,从而根据高流量(2008年6月)和低流量(2009年1月)收集的50个样品来了解调节水文地球化学的机理。 )期间。水化学表现出显着的空间变异性,反映了盆地中的混合过程。季节性影响的确会以离子丰度的顺序以适度的变化显着改变离子浓度。阳离子中的Ca2 +离子和阴离子中的HCO3-离子占主导地位,并且与盆地的不同岩性显着相关。三种主要的水类型,即Ca-Mg-HCO3(72%),Ca-HCO3(12%)和Mg-Ca-HCO3(16%),表明水的化学组成主要受碳酸盐岩岩性控制,除了硅酸盐的重要贡献。但是,在某些地方,生物过程和人为活动起着重要作用。相对而言,在高流量时期(夏季)较低的离子浓度表明较高的放电通过稀释效应的显着影响。在此期间,由于较高的降雨和积雪融化(由于温度升高而导致的较高排放量)导致大量人类和农业废弃物冲入河流。因子分析还反映了基于四个重要因子对各种岩性和人为来源对水质的主要控制,这四个因子共同解释了总数据差异的约70-81%。用于估算支流对主要河道排放贡献的两元氯离子混合模型显示了可靠的结果。可以提到的是,在不久的将来,通过人为来源的定期和连续污染可能会危害和降低水质。因此,关键的管理方法和策略对其未来的可持续性非常重要。

著录项

  • 来源
    《Environmental Monitoring and Assessment》 |2016年第7期|438.1-438.24|共24页
  • 作者单位

    Indian Inst Technol Roorkee, Dept Earth Sci, Roorkee 247667, Uttar Pradesh, India|Geol Survey India, State Unit J&K, Srinagar 190008, Jammu & Kashmir, India;

    Univ Kashmir, Dept Earth Sci, Srinagar 190006, Jammu & Kashmir, India;

    Univ Kashmir, Dept Earth Sci, Srinagar 190006, Jammu & Kashmir, India;

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

    Hydrogeochemistry; Weathering; Spatial; Temporal; River Jhelum basin; Kashmir Himalaya;

    机译:水文地球化学;风化;空间;时空;杰鲁姆河盆地;克什米尔喜马拉雅山;
  • 入库时间 2022-08-17 13:26:14

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