Formation Dynamics of Groundwater

EasyChair Preprint 15148

Abstract

The formation dynamics of groundwater involve a complex interplay of natural processes and environmental factors that dictate the availability and movement of water beneath the Earth's surface. Groundwater, a vital resource for ecosystems and human activities, is primarily formed through the processes of precipitation, infiltration, and percolation, with aquifers serving as critical reservoirs. This paper explores the key mechanisms of groundwater recharge, emphasizing the influence of soil composition, topography, and climatic conditions.

Additionally, the dynamics of groundwater movement are examined through the lens of hydraulic gradients and Darcy's Law, highlighting the significance of flow types in resource management. The interaction between groundwater and surface water is also discussed, particularly its implications for water quality and ecosystem health.

Keyphrases: Aquifers, Baseflow, Groundwater, Hydraulic gradient, Recharge, infiltration, percolation

@booklet{EasyChair:15148,
  author    = {Edwin Frank},
  title     = {Formation Dynamics of Groundwater},
  howpublished = {EasyChair Preprint 15148},
  year      = {EasyChair, 2024}}