Groundwater Recharge of Fractured Rock Aquifers in SE Australia Is Episodic and Controlled by Season and Rainfall Amount

Abstract Sustainable management of groundwater resources requires a comprehensive understanding of groundwater recharge; including when and under what conditions groundwater recharge occurs. However, recharge is one of the least understood hydrologic processes. Here we show how event‐scale rainfall...

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Published in:Geophysical Research Letters
Main Authors: Stacey C. Priestley, Andy Baker, Margaret Shanafield, Wendy Timms, Martin S. Andersen, Maria deLourdes Melo Zurita
Format: Article
Language:English
Published: Wiley 2025-03-01
Subjects:
Online Access:https://doi.org/10.1029/2024GL113503
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author Stacey C. Priestley
Andy Baker
Margaret Shanafield
Wendy Timms
Martin S. Andersen
Maria deLourdes Melo Zurita
author_facet Stacey C. Priestley
Andy Baker
Margaret Shanafield
Wendy Timms
Martin S. Andersen
Maria deLourdes Melo Zurita
author_sort Stacey C. Priestley
collection DOAJ
container_title Geophysical Research Letters
description Abstract Sustainable management of groundwater resources requires a comprehensive understanding of groundwater recharge; including when and under what conditions groundwater recharge occurs. However, recharge is one of the least understood hydrologic processes. Here we show how event‐scale rainfall recharge thresholds vary over a year using a novel network of subterranean drip loggers installed in caves, mines, and tunnels to observe groundwater recharge events. These cannot be used to directly estimate groundwater recharge volumes, but instead detail temporal aspects, such as the rainfall amount required to trigger recharge. We describe how these thresholds vary over time and space from a range of geological, environmental, and climatic conditions. At our Southeast Australian sites, median rainfall recharge thresholds of 10–20 mm in 48 hr were needed to activate recharge. Rainfall events of this magnitude are infrequent, they are expected to change with climate change, and they are fundamentally important for informing groundwater recharge.
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spelling doaj-art-85612df2e2c44fc4b7d2d6d520b9f65f2025-08-20T02:16:05ZengWileyGeophysical Research Letters0094-82761944-80072025-03-01525n/an/a10.1029/2024GL113503Groundwater Recharge of Fractured Rock Aquifers in SE Australia Is Episodic and Controlled by Season and Rainfall AmountStacey C. Priestley0Andy Baker1Margaret Shanafield2Wendy Timms3Martin S. Andersen4Maria deLourdes Melo Zurita5CSIRO Environment Adelaide SA AustraliaSchool of Biological, Earth and Environmental Sciences UNSW Sydney Sydney NSW AustraliaCollege of Science and Engineering Flinders University Adelaide SA AustraliaSchool of Engineering Deakin University Waurn Ponds VIC AustraliaSchool of Civil and Environmental Engineering UNSW Sydney Sydney NSW AustraliaEnvironment and Society Group Faculty of Arts Design and Architecture UNSW Sydney Sydney NSW AustraliaAbstract Sustainable management of groundwater resources requires a comprehensive understanding of groundwater recharge; including when and under what conditions groundwater recharge occurs. However, recharge is one of the least understood hydrologic processes. Here we show how event‐scale rainfall recharge thresholds vary over a year using a novel network of subterranean drip loggers installed in caves, mines, and tunnels to observe groundwater recharge events. These cannot be used to directly estimate groundwater recharge volumes, but instead detail temporal aspects, such as the rainfall amount required to trigger recharge. We describe how these thresholds vary over time and space from a range of geological, environmental, and climatic conditions. At our Southeast Australian sites, median rainfall recharge thresholds of 10–20 mm in 48 hr were needed to activate recharge. Rainfall events of this magnitude are infrequent, they are expected to change with climate change, and they are fundamentally important for informing groundwater recharge.https://doi.org/10.1029/2024GL113503fractured rock aquifersgroundwater rechargerainfall recharge thresholds
spellingShingle Stacey C. Priestley
Andy Baker
Margaret Shanafield
Wendy Timms
Martin S. Andersen
Maria deLourdes Melo Zurita
Groundwater Recharge of Fractured Rock Aquifers in SE Australia Is Episodic and Controlled by Season and Rainfall Amount
fractured rock aquifers
groundwater recharge
rainfall recharge thresholds
title Groundwater Recharge of Fractured Rock Aquifers in SE Australia Is Episodic and Controlled by Season and Rainfall Amount
title_full Groundwater Recharge of Fractured Rock Aquifers in SE Australia Is Episodic and Controlled by Season and Rainfall Amount
title_fullStr Groundwater Recharge of Fractured Rock Aquifers in SE Australia Is Episodic and Controlled by Season and Rainfall Amount
title_full_unstemmed Groundwater Recharge of Fractured Rock Aquifers in SE Australia Is Episodic and Controlled by Season and Rainfall Amount
title_short Groundwater Recharge of Fractured Rock Aquifers in SE Australia Is Episodic and Controlled by Season and Rainfall Amount
title_sort groundwater recharge of fractured rock aquifers in se australia is episodic and controlled by season and rainfall amount
topic fractured rock aquifers
groundwater recharge
rainfall recharge thresholds
url https://doi.org/10.1029/2024GL113503
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