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Kazi Matin Ahmed

Researcher at University of Dhaka

Publications -  238
Citations -  13366

Kazi Matin Ahmed is an academic researcher from University of Dhaka. The author has contributed to research in topics: Groundwater & Aquifer. The author has an hindex of 53, co-authored 215 publications receiving 11650 citations. Previous affiliations of Kazi Matin Ahmed include Lamont–Doherty Earth Observatory & Columbia University.

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Geological controls on groundwater chemistry and arsenic mobilization: Hydrogeochemical study along an E–W transect in the Meghna basin, Bangladesh

TL;DR: The results of the study clearly indicate geological control (i.e. change in lithofacies) on groundwater chemistry and distribution of redox-sensitive elements such as As along the transect as discussed by the authors.
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Modeling regional-scale groundwater arsenic hazard in the transboundary Ganges River Delta, India and Bangladesh: Infusing physically-based model with machine learning.

TL;DR: Transboundary regional-scale models for computing the probability of groundwater As concentrations to exceed the WHO permissible thresholds for drinking water within the Ganges River delta as a function of the various geomorphologic-(hydro)geologic-hydrostratigraphic-anthropogenic controlling factors are developed and useful in identifying the possible exogenous forcing that may have led to the worst, natural pollution in human history.
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Constraints on sustainable development of arsenic-bearing aquifers in southern Bangladesh.: Part 1: A conceptual model of arsenic in the aquifer

TL;DR: A conceptual model of arsenic in the aquifer is proposed in this paper, as a basis for addressing questions concerning sustainability of groundwater development, which incorporates the conditions of arsenic release to groundwater, the depth distribution of the arsenic source, likely sedimentological controls on the lateral discontinuity of the source, and the hydraulic regime imposed by pumping from the hydrogeologically leaky, multi-layered aquifer.
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Reversible adsorption and flushing of arsenic in a shallow, Holocene aquifer of Bangladesh.

TL;DR: A simple flushing model shows that the increase in As concentrations with depth and groundwater age at this site, and at other sites in the Bengal and Red River Basins, can be attributed to the evolution of the aquifer over 100-1000 years as aquifer sands are gradually flushed of their initial As content.