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Please use this identifier to cite or link to this item:
http://krishi.icar.gov.in/jspui/handle/123456789/21114
Full metadata record
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Deepesh Machiwal | en_US |
dc.contributor.author | Madan Kumar Jha | en_US |
dc.date.accessioned | 2019-07-03T09:36:41Z | - |
dc.date.available | 2019-07-03T09:36:41Z | - |
dc.date.issued | 2013-03-14 | - |
dc.identifier.citation | Not Available | en_US |
dc.identifier.issn | Not Available | - |
dc.identifier.uri | http://krishi.icar.gov.in/jspui/handle/123456789/21114 | - |
dc.description | Not Available | en_US |
dc.description.abstract | The aim of this study was to investigate rainfall-groundwater dynamics over space and annual time scales in a hard-rock aquifer system of India by employing time series, GIS and geostatistical modeling techniques. Trends in 43-year (1965-2007) annual rainfall time series of ten rainfall stations and 16-year (1991-2006) pre- and post-monsoon groundwater levels of 140 sites were identified by using Mann-Kendall, Spearman rank order correlation, and Kendall rank correlation tests. Trends were quantified by Kendall slope method. Furthermore, the study involves novelty of examining homogeneity of pre- and post-monsoon groundwater levels, for the first time, by applying seven tests. Regression analysis between rainfall and post-monsoon groundwater levels was performed. The pre- and post-monsoon groundwater levels for four periods: (a) 1991-1994, (b) 1995-1998, (c) 1999-2002, and (d) 2003-2006 were subjected to GIS-based geostatistical modeling. The rainfall showed considerable saptio-temporal variations, with a declining trend at the Mavli rainfall station (p-value<0.05). The Levene’s tests revealed spatial homogeneity of rainfall at α = 0.05. Regression analyses indicated significant relationships (r2>0.5) between groundwater level and rainfall for eight rainfall stations. Non-homogeneity and declining trends in the groundwater level, attributed to anthropogenic and hydrologic factors, were found at 5 to 61 more sites in pre-monsoon compared to post-monsoon season. The groundwater declining rates in phyllite-schist, gneiss, schist and granite formations were found to be 0.18, 0.26, 0.21 and 0.14 m year-1 and 0.13, 0.19, 0.16 and 0.02 m year-1 during the pre- and post-monsoon seasons, respectively. The geostatistical analyses for four time periods revealed linkages between the rainfall and groundwater levels. | en_US |
dc.description.sponsorship | Not Available | en_US |
dc.language.iso | English | en_US |
dc.publisher | Wiley | en_US |
dc.relation.ispartofseries | Not Available; | - |
dc.subject | Groundwater dynamics | en_US |
dc.subject | GIS, homogeneity | en_US |
dc.subject | trend | en_US |
dc.subject | geostatistical modeling | en_US |
dc.subject | Udaipur district | en_US |
dc.title | Characterizing rainfall-groundwater dynamics in a hard-rock aquifer system using time series, GIS and geostatistical modeling | en_US |
dc.title.alternative | Not Available | en_US |
dc.type | Research Paper | en_US |
dc.publication.projectcode | Not Available | en_US |
dc.publication.journalname | Hydrological Processes | en_US |
dc.publication.volumeno | 28(5) | en_US |
dc.publication.pagenumber | 2824-2843 | en_US |
dc.publication.divisionUnit | Regional Research Station, Kukma, Bhuj | en_US |
dc.publication.sourceUrl | 10.1002/hyp.9816 | en_US |
dc.publication.authorAffiliation | ICAR::Central Arid Zone Research Institute | en_US |
dc.ICARdataUseLicence | http://krishi.icar.gov.in/PDF/ICAR_Data_Use_Licence.pdf | en_US |
dc.publication.naasrating | 9.26 | en_US |
Appears in Collections: | NRM-CAZRI-Publication |
Files in This Item:
File | Description | Size | Format | |
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Machiwal_and_Jha_rev_final_Krishi_Portal.pdf | 1.93 MB | Adobe PDF | View/Open |
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