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Impact of the December 2004 tsunami on soil, groundwater and vegetation in the Nagapattinam district, India

机译:2004年12月海啸对印度Nagapattinam区的土壤,地下水和植被的影响

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摘要

The tsunami of 26 December 2004 struck the Nagapattinam District, Tamil Nadu, India. Sea water inundation from the tsunami caused salinization problems for soil and groundwater in coastal areas of the district, and also induced salt injuries in crops. To document the recovery of the agricultural environment from the tsunami, we conducted observations of the soil, groundwater, and vegetation. Soil electrical conductivity increased sharply after the tsunami, but returned to pre-tsunami levels the following year. Groundwater salinity returned to pre-tsunami levels by 2006. These rapid rates of recovery were due to the monsoon rainfall leaching salt from the highly permeable soils in the area. MODIS NDVI values measured before and after the tsunami showed that vegetation damaged by the tsunami recovered to its pre-tsunami state by the next rice cropping season, called samba, which starts from August to February. From these results, we conclude that the agricultural environment of the district has now fully recovered from the tsunami. Based on the results, we have also identified important management implications for soil, groundwater, and vegetation as follows: 1) due to the heavy monsoon rainfall and the high permeability of soils in this region, anthropogenic inputs like fertilizers should be applied carefully to minimize pollution, and the use of green manure is recommended; 2) areas that were contaminated by sea water extended up to 1000 m from the sea shore and over pumping of groundwater should be carefully avoided to prevent inducing sea water intrusion; and 3) data from a moderate resolution sensor of 250 m, such as MODIS, can be applied to impact assessment in widespread paddy field areas like the Nagapattinam District.
机译:2004年12月26日的海啸袭击了印度泰米尔纳德邦的Nagapattinam区。海啸使海水泛滥,造成该地区沿海地区土壤和地下水的盐碱化问题,并造成农作物盐害。为了记录海啸后农业环境的恢复,我们对土壤,地下水和植被进行了观测。海啸后,土壤电导率急剧上升,但次年又恢复到海啸前的水平。到2006年,地下水盐度恢复到海啸前的水平。这些快速的恢复速度归因于该地区高渗透性土壤中的季风降雨浸出盐分。海啸前后测得的MODIS NDVI值表明,受海啸破坏的植被在下一个水稻种植季节(桑巴)从八月至二月开始恢复到海啸前的状态。从这些结果可以得出结论,该地区的农业环境现已从海啸中完全恢复。根据结果​​,我们还确定了对土壤,地下水和植被的重要管理意义如下:1)由于该地区季风降雨多和土壤渗透性高,应谨慎使用人为投入,如肥料污染,建议使用绿肥; 2)应小心避免被海水污染的区域,该区域从海边延伸至1000 m,并且抽取的地下水过多,以防止引起海水入侵; 3)来自250 m的中等分辨率传感器(例如MODIS)的数据可用于在诸如Nagapattinam地区这样的广泛稻田地区进行影响评估。

著录项

  • 来源
    《Journal of Environmental Management》 |2009年第3期|3147-3154|共8页
  • 作者单位

    Research Institute for Humanity and Nature, 457-4 Kamigamo-Motoyama, Kita-ku, Kyoto, 603-8047, Japan;

    Research Institute for Humanity and Nature, 457-4 Kamigamo-Motoyama, Kita-ku, Kyoto, 603-8047, Japan;

    IWMI-TATA Policy Research Program, International Water Management Institute (IWMI), South Asia Regional Office, ICRISAT campus, Patancheru 502 324, Andhra Pradesh, India;

  • 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

    tsunami; soil salinity; groundwater salinity; NDVI; agricultural environment and management;

    机译:海啸;土壤盐分;地下水盐度;NDVI;农业环境与管理;
  • 入库时间 2022-08-17 13:36:20

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