Data

University of New South Wales (UNSW) Raw Groundwater Levels Data (2012-2024)

AuScope
Martin Andersen ; Evan Jensen
Viewed: [[ro.stat.viewed]] Cited: [[ro.stat.cited]] Accessed: [[ro.stat.accessed]]
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Maules Creek has both losing and gaining reaches and infrastructure (including two weather stations) has been installed in this part of the catchment and to provide permanent monitoring of the system. The Upper part of Maules Creek has been instrumented to estimate groundwater recharge from ephemeral streams. * The Wellington site focuses on fractured rock aquifers. Fractured and cavernous limestone at the Wellington Caves has a combination of boreholes, a weather station and instrumented caves, uniquely using caves as an observatory of vadose zone processes. Fractured granites at Baldry have surface water, ground water, climate and tree water use all instrumented. Fractured Ordovician volcanics and metasediments at the UNSW Wellington Research Station have a borefield of over 40 bores in both alluvial sediments and the adjacent fractured rock aquifer. Abstraction bores in both aquifers facilitate experiments such as aquifer tests (pumping tests) and tracer experiments.Statement: Groundwater data is produced with Solinst Level-loggers and In-Situ Rugged TROLL dataloggers. These dataloggers are pressure transducers that hang down into the water column inside the borehole and measure the water pressure above the logger typically at 30 minute intervals. The pressure is measured as water head in meters above the logger. Some loggers are vented to the atmosphere (In-Situ Rugged TROLL) meaning that they measure relative to the atmosphere. Other loggers are non-vented (Solinst Level-loggers) and measure absolute pressure (water + atmosphere) and needs to be corrected for the atmospheric pressure using a barometric logger (Baro-logger data is provide in separate files for each catchment) to provide the water pressure only. Together with manual dip measurements from a known reference level (typically the top of casing) to the groundwater table one can calculate the absolute groundwater elevation (hydraulic head) relative to a known datum (typically Australian Height Datum) over time. 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Brief description

The Groundwater Infrastructure Program aims to enable long-term groundwater resource research in a variable and changing climate to inform sustainable groundwater management. This dataset contains the groundwater levels and temperature (plus corresponding manual dip measurements) across selected NCRIS sites in New South Wales collected by the Groundwater Research at UNSW: * The Namoi valley infrastructure has been established to develop an improved understanding of groundwater interaction with the Namoi, and Cockburn Rivers, and Maules Creek. A profile of double piezometers has been installed on the banks of the Namoi, close to the Maules Creek confluence. Maules Creek has both losing and gaining reaches and infrastructure (including two weather stations) has been installed in this part of the catchment and to provide permanent monitoring of the system. The Upper part of Maules Creek has been instrumented to estimate groundwater recharge from ephemeral streams. * The Wellington site focuses on fractured rock aquifers. Fractured and cavernous limestone at the Wellington Caves has a combination of boreholes, a weather station and instrumented caves, uniquely using caves as an observatory of vadose zone processes. Fractured granites at Baldry have surface water, ground water, climate and tree water use all instrumented. Fractured Ordovician volcanics and metasediments at the UNSW Wellington Research Station have a borefield of over 40 bores in both alluvial sediments and the adjacent fractured rock aquifer. Abstraction bores in both aquifers facilitate experiments such as aquifer tests (pumping tests) and tracer experiments.

Lineage

Statement: Groundwater data is produced with Solinst Level-loggers and In-Situ Rugged TROLL dataloggers. These dataloggers are pressure transducers that hang down into the water column inside the borehole and measure the water pressure above the logger typically at 30 minute intervals. The pressure is measured as water head in meters above the logger. Some loggers are vented to the atmosphere (In-Situ Rugged TROLL) meaning that they measure relative to the atmosphere. Other loggers are non-vented (Solinst Level-loggers) and measure absolute pressure (water + atmosphere) and needs to be corrected for the atmospheric pressure using a barometric logger (Baro-logger data is provide in separate files for each catchment) to provide the water pressure only. Together with manual dip measurements from a known reference level (typically the top of casing) to the groundwater table one can calculate the absolute groundwater elevation (hydraulic head) relative to a known datum (typically Australian Height Datum) over time. Details for data processing are in the metadata folder.

Notes

Credit
Credit to the UNSW Water Research Laboratory and all the researchers and technicians involved in community building, supervising of well drilling, sensor installation & maintenance, dip measurements, data downloads, organization, driving and everything else needed to produce this robust dataset. The project is supported by the Australian Government through the National Collaborative Research Infrastructure Strategy (NCRIS) program.

Created: 01 10 2024

Data time period: 2012-01-01 to 2024-10-01

This dataset is part of a larger collection

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Subjects
AuScope Data Repository | GROUND WATER | GROUND WATER PROCESSES/MEASUREMENTS | GROUNDWATER MANAGEMENT | Groundwater Levels | Groundwater Temperature | Groundwater hydrology | Groundwater quality processes and contaminated land assessment | HYDROLOGIC AND TERRESTRIAL WATER CYCLE MODELS | Hydrology | KARST HYDROLOGY |

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