Publications by authors named "Numair Ahmed Siddiqui"

Swelling of shale in clastic reservoirs poses a significant challenge, causing instability in wellbores. Utilizing water-based drilling mud with shale inhibitors is preferable for environmental reasons over oil-based mud. Ionic liquids (ILs) have garnered interest as shale inhibitors due to their customizable properties and strong electrostatic features.

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Article Synopsis
  • The Baraichari Shale Formation in Bangladesh's Bengal Basin is critical for understanding hydrocarbon accumulation, necessitating a detailed facies analysis to reveal its depositional complexities.
  • The research identifies eight sedimentary facies and categorizes them into three main associations: subtidal or estuarine, mixed flats with tidal creeks, and tidal mud flats, each reflecting different energy levels and sediment deposition environments.
  • The findings, including distinct sedimentary structures and cycles, can aid in developing models for subsurface reservoirs, enhancing our understanding of natural resource potential in this region.
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The early to middle Permian Dohol Formation is characterized by a significant presence of shale deposits. While these shales exhibit a low potential to generate hydrocarbons, there is a need to ascertain the possible reasons for the low hydrocarbon generation potential. Also, there are several unidentified properties and attributes associated with these shales in terms of their inorganic geochemical characteristics and their mineralogy.

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Current worldwide projections of sea-level rise show a staggering increase in water level of up to 2 m by 2100 owing to global warming exacerbated by anthropogenically induced climate change. While amplified rates of sea-level rise is an immense hazard to coastal communities, storm surges are expected to increase in intensity and frequency making it an equally significant threat to coastal populations. In France, these hazards are not uncommon with records of extreme tempests every thousand years in the Holocene.

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