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書目名稱Groundwater影響因子(影響力)




書目名稱Groundwater影響因子(影響力)學(xué)科排名




書目名稱Groundwater網(wǎng)絡(luò)公開度




書目名稱Groundwater網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Groundwater被引頻次




書目名稱Groundwater被引頻次學(xué)科排名




書目名稱Groundwater年度引用




書目名稱Groundwater年度引用學(xué)科排名




書目名稱Groundwater讀者反饋




書目名稱Groundwater讀者反饋學(xué)科排名

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Spatio-Temporal Variation and Trend Analysis of Groundwater Level in Raipur City, Chhattisgarhereas deeper GWL has been observed in western and northern part of the city. The groundwater contour maps depict that the groundwater flow direction is towards north and west. The results of trend analysis reveal that no significant trend is detected at 5% significance level except few locations.

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Spatiotemporal Relationship Linking Land Use/Land Cover with Groundwater Levelocations (29 wells) all over the district and created a continuous surface using interpolation with the estimate of error. LULC map of 2003 and 2013 was derived from classification of TM images using supervised, parametric maximum likelihood classifier. Area is broadly categorized into four classes,

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Groundwater System Modelling and Sensitivity of Groundwater Level Prediction in Indo-Gangetic Alluvirt of Sharda Sahayak Canal System in Uttar Pradesh. Visual MODFLOW was calibrated and validated for water level data available for 9?years (2005–2013). The effect of change in recharge rate and withdrawal rate is also investigated to predict the corresponding changes in water levels. Groundwater lev

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Assessing Aquifer Vulnerability Using GIS-Based DRASTIC Model Coupling with Hydrochemical Parametersmolar ratios. The results have recognized four aquifer vulnerability zones based on DRASTIC vulnerability index (DVI), which ranged from 39 to 132. It has been deduced that approximately 18, 25, 34, and 23% of the area lies in negligible, low, medium, and high vulnerability zones, respectively. It s

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