Selected Publications
Selected Publications
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Mega-city pumping and preferential flow threaten groundwater quality: insights from Dhaka, Bangladesh
Spatial distribution of (a) probability and (b) standard deviation of the deep (≥150 m) aquifer becoming contaminated in ≤200 years
A workflow to create fine scale static models guided by seismic data in a fluvial system
Combining process-based and surface-based models to simulate subsurface heterogeneity in volcanic aquifers
https://link.springer.com/article/10.1007/s00477-018-1511-7
The impact of geological uncertainty on primary production from a fluvial reservoir
https://link.springer.com/article/10.1007/s12182-018-0229-y
3D view of the reference geological model (realization), b sediments having a permeability more than 1 mD
Multiple-point geostatistical simulation using the bunch-pasting direct sampling method
https://doi.org/10.1016/j.cageo.2013.01.020
Impact of Topography on Groundwater Salinization Due to Ocean Surge Inundation
Synthetic topography of 16 types. (a-l) The upper box includes four isotropic topography categories: crater, random, river, and sine. Each category has three depression scenarios: (a-d) depression removed, (e-h) normal, and (i-l) depression doubled. Crater, random and river categories have five realizations by varying the statistical seed. Sine category has fiverealizations that differ in phase. The lower box (m-p) includes four types of anisotropic topography: shore-perpendicular of crater (m), shore-parallel of crater (n), shore-perpendicular ofriver (o), and shore-parallel of river (p). Each type has five statistically equivalent realizations generated by varying the statistical seeds. The color gradient shows the elevation. The uniform blue color shows the normal sea level at 0 m
Multiple-point geostatistical simulation of dykes: application at Sungun porphyry copper system, Iran
https://link.springer.com/article/10.1007/s00477-014-0857-8
Geologic influence on groundwater salinity drives large seawater circulation through the continental shelf
Example of heterogeneous fields and simulated salinity distributions and fresh and saline groundwater discharge rates (qout) for heterogeneous and equivalent homogeneous models. (a) Low, (b) intermediate, and (c) high horizontal continuity. Area between 10% and 90% salinity contours (white) is defined as the mixing zone, and the black dot indicates the horizontal position of its center of mass. Labels for Figure 2a apply to Figures 2b and 2c.
Reserve Classification Challenges and Modeling of The Kaolin Deposits of Charentes Basin, France
Schema of the procedure of stocks simulation
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