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Analysis of groundwater drought characteristics of Damoh district in Bundelkhand using groundwater drought index

机译:地下水旱营指数对Bundelkhand的达蒙斯地区地下水干旱特征分析

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摘要

Drought is a natural disastrous phenomenon that occurs due to the continuous reduction of rainfall over a short or a long period of time. A deficit in precipitation result in deficit of groundwater recharge, which leads to lower groundwater table andturn in groundwater drought. This is a challenging problem in Bundelkhand region of the Central India, where people mostly suffer from groundwater drought condition. Bearma basin is one of the considerable groundwater resource fields of Bundelkhand in Madhya Pradesh, which is sub-basin of Ken river. In the present study the Bearma basin has been selected with the objective to analyze the groundwater drought condition in Damoh district by using Groundwater Drought Index (GDI). The 26 years (1984-2010) quarterly groundwater levels of 59 observation wells falling in and around of Damoh district has been used. The GDI for all observation wells were computed with the help of groundwater level of each stations. With the help of temporal variations of GDI foreach observation wells, the groundwater drought characteristics of the basin falling under Damoh district were analyzed. Result showed that the maximum number of 9 frequency drought events occurred at Fatehpur, Hatta and Bari-kalan with total durationsvarying between 83 to 134 months and total severity varying between -19.40 to -27.96. The cumulative groundwater drought duration of 134 months has been observed at Devron followed by 116 months at Kusumi. The overall drought intensity in the observationwells was found -0.38.
机译:干旱是一种自然的灾难性现象,由于在短时间或长时间的降雨量持续减少而发生。地下水补给缺陷的降水量缺陷,导致地下水干旱地下水表衰竭。这是印度中部Bundelkhand地区的一个具​​有挑战性的问题,人们主要遭受地下水干旱状况。 Bearma Basin是Madhya Pradesh Bundelkhand的相当大的地下水资源领域之一,是肯河的次盆地。在本研究中,已经选择了Bearma盆地,目的是通过使用地下水干旱指数(GDI)分析达莫区的地下水干旱状况。已经使用了26岁(1984-2010)59个观察井的季度地下水水平落在达摩区周围。在每个站的地下水位的帮助下计算所有观察孔的GDI。借助于GDI Foreach观察井的时间变化,分析了达到达摩区下落下的盆地的地下水干旱特征。结果表明,Fatehpur,Hatta和Bari-Kalan的最大9个频率干旱事件发生的最大频率发生在83至134个月之间,总严重程度在-19.40至-27.96之间。 Devron在Kusumi的116个月后观察到累积地下水干旱期限为134个月。观察威胁中的整体干旱强度被发现-0.38。

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