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Mapping groundwater quality for irrigation in Punjab, North-West India, using geographical information system

机译:使用地理信息系统绘制印度西北部旁遮普邦的灌溉地下水水质图

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摘要

The state of Punjab-a part of the Indus basin of the Indian subcontinent has an excellent net work of irrigation facilities. However, due to intensive cultivation it is facing a major problem with respect to quality of groundwater for irrigation. In the present investigation, geo-referenced groundwater samples were analysed to map water quality using geographical information system. Electrical conductivity varied from 0.418 to 5.754 dS m~(-1) with an average of 1.365 dS m~(-1) The carbonate ranged between 0 and 120 mg L~(-1), whereas bicarbonate ranged from 5 to 1,000 mg L~(-1). Chloride varied from 7 to 2,347 mg L~(-1). Calcium plus magnesium ranged from 12 to 1,216 mg L~(-1) with a mean value of 169 mg L~(-1). Sodium adsorption ratio ranged between 0.0 and 34.78 with an average of 2.66 meq L~(-1/2). Residual sodium carbonate varied from 0 to 21.30 meq L~(-1) with a standard deviation of 2.24. The Geographic Information System (GIS)-based mapping indicated that water in suitable category spatially covered 45.7 % of the state which is located mostly in the sub-mountain (Siwalik Hills), north-eastern undulating and piedmont and alluvial plain agro-eco-subregions. Marginally suitable groundwater spatially covered 46.1 % in the central alluvial plain and south-western alluvial plain agro-eco-subregions. Unsuitable groundwater covered 8.2 % of the state, mostly in the erstwhile sodic soils areas in the central alluvial plain and south-western alluvial plain agro-eco-subregions. GIS-based maps are effective in identifying hot spots which need immediate attention and call for strategic planning for sustainable management.
机译:旁遮普邦-印度次大陆印度河流域的一部分,拥有极佳的灌溉设施网络。但是,由于精耕细作,灌溉地下水的质量面临着主要问题。在本研究中,使用地理信息系统分析了具有地理参考意义的地下水样品,以绘制水质图。电导率从0.418到5.754 dS m〜(-1)不等,平均为1.365 dS m〜(-1)碳酸盐的范围为0至120 mg L〜(-1),而碳酸氢盐的范围为5至1,000 mg L 〜(-1)。氯化物从7到2,347 mg L〜(-1)不等。钙和镁的范围从12到1,216 mg L〜(-1),平均值为169 mg L〜(-1)。钠的吸附比在0.0和34.78之间,平均为2.66meq L〜(-1/2)。残留碳酸钠的变化范围为0至21.30 meq L〜(-1),标准偏差为2.24。基于地理信息系统(GIS)的地图显示,适当类别的水在空间上覆盖了该州的45.7%,该州主要位于次山(Siwalik Hills),东北起伏和山前以及冲积平原农业生态环境中。次区域。中部冲积平原和西南冲积平原农业生态分区的边缘适宜地下水在空间上占46.1%。不合适的地下水覆盖了该州的8.2%,主要是在中冲积平原和西南冲积平原农业生态分区的旧碱土地区。基于GIS的地图可以有效地识别需要立即引起注意的热点,并要求对可持续管理进行战略规划。

著录项

  • 来源
    《Environmental earth sciences》 |2014年第1期|147-161|共15页
  • 作者单位

    Department of Soil Science, Punjab Agricultural University, Ludhiana 141004, India;

    Department of Soil Science, Punjab Agricultural University, Ludhiana 141004, India;

    Department of Soil Science, Punjab Agricultural University, Ludhiana 141004, India;

    Department of Soil Science, Punjab Agricultural University, Ludhiana 141004, India;

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

    Groundwater; Geospatial quality; Punjab; GIS;

    机译:地下水;地理空间质量;旁遮普地理信息系统;

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