Understanding Low Flow Groundwater Gradients in Dolomite Aquifers: Geological, Hydrological, and Chemical Influences -Buchanan (2023)

Abstract

Low flow groundwater gradients in dolomite aquifers are shaped by a complex interplay of geological, hydrological, and chemical processes over extensive time periods, often spanning billions of years. This paper explores the formation of these gradients, the dynamics of groundwater flow, and the implications for aquifer management. Additionally, it discusses advanced modelling techniques and innovative approaches, such as environmental DNA (eDNA) analysis, to enhance our understanding of groundwater connectivity.