An underground drip water monitoring network to characterize rainfall recharge of groundwater at different geologies, environments, and climates across Australia
-
Published:2024-05-02
Issue:1
Volume:13
Page:117-129
-
ISSN:2193-0864
-
Container-title:Geoscientific Instrumentation, Methods and Data Systems
-
language:en
-
Short-container-title:Geosci. Instrum. Method. Data Syst.
Author:
Baker AndyORCID, Shanafield MargaretORCID, Timms WendyORCID, Andersen Martin Sogaard, Priestley StaceyORCID, Melo Zurita Marilu
Abstract
Abstract. Understanding when and why groundwater recharge occurs is of fundamental importance for the sustainable use of this essential freshwater resource for humans and ecosystems. However, accurately capturing this component of the water balance is widely acknowledged to be a major challenge. Direct physical measurements identifying when groundwater recharge is occurring are possible by utilizing a sensor network of hydrological loggers deployed in underground spaces located in the vadose zone. Through measurements of water percolating into these spaces from above, we can record the potential groundwater recharge process in action. By using automated sensors, it is possible to precisely determine when recharge occurs (which event, month, or season and for which climate condition). Combined with daily rainfall data, it is possible to quantify the “rainfall recharge threshold”, the amount of rainfall needed to generate groundwater recharge, and its temporal and spatial variability. Australia's National Groundwater Recharge Observing System (NGROS) provides the first dedicated sensor network for observing groundwater recharge at an event scale across a wide range of geologies, environments, and climate types representing a wide range of Australian hydroclimates. Utilizing tunnels, mines, caves, and other subsurface spaces located in the vadose zone, the sensors effectively record “deep drainage”, water that can move beyond the shallow subsurface and root zone to generate groundwater recharge. The NGROS has the temporal resolution to capture individual recharge events, with multiple sensors deployed at each site to constrain the heterogeneity of recharge between different flow paths, and to quantify (including uncertainty bounds) rainfall recharge thresholds. Established in 2022, the network is described here together with examples of data being generated.
Funder
Australian Research Council
Publisher
Copernicus GmbH
Reference48 articles.
1. Ajami, H.: Geohydrology, in: Groundwater. Encyclopedia of Geology, 2nd edn., edited by: Alderton, D. and Elias, S. A., Academic Press, Oxford, 408–415, ISBN 9780081029084, 2021. 2. Baker, A. and Brunsdon, C.: Non-linearities in drip water hydrology: an example from Stump Cross Caverns, Yorkshire, J. Hydrol., 277, 151–163, https://doi.org/10.1016/S0022-1694(03)00063-5, 2003. 3. Baker, A., Berthelin, R., Cuthbert, M. O., Treble, P. C., Hartmann, A., and the KSS Cave Studies Team: Rainfall recharge thresholds in a subtropical climate determined using a regional cave drip water monitoring network, J. Hydrol., 587, 125001, https://doi.org/10.1016/j.jhydrol.2020.125001, 2020. 4. Baker, A., Scheller, M., Oriani, F., Mariethoz, G., Hartmann, A., Wang, Z., and Cuthbert, M. O: Quantifying temporal variability and spatial heterogeneity in rainfall recharge thresholds in a montane karst environment, J. Hydrol., 594, 125965, https://doi.org/10.1016/j.jhydrol.2021.125965, 2021. 5. Baldwin, C., Tan, P. L., White, I., Hoverman, S., and Burry, K.: How scientific knowledge informs community understanding of groundwater, J. Hydrol., 474, 74–83, https://doi.org/10.1016/j.jhydrol.2012.06.006, 2012.
|
|