Calculating groundwater recharge in karst aquifers

#aquifer #groundwater recharge #Karst #SWAT #Transfer functions
The figure shows a bar chart. The x-axis shows the years 2000 to 2016, the y-axis shows the precipitation in mm/a on the left side and the groundwater recharge in mm/a on the right side. The groundwater recharge values calculated with the HPTF and the SWAT model as well as the precipitation are displayed as columns in the diagram.
Applied methods to calculate the groundwater recharge of the Western Mountain Aquifer. Groundwater recharge is composed of a fast flow and a slow flow component – since the HPTF only calculate the slow flow component, the fast flow component of the SWAT model was added. © Paul Hepach / Hydrogeology, TU Berlin

The Soil and Water Assessment Tool (SWAT) and Hydro-Pedo Transfer Functions (HPTF) allow for the precise calculation of groundwater recharge in high temporal and spatial resolutions. Both methods were tested for the karstic Western Mountain Aquifer.

SWAT calculates the day-to-day water budget using information on land use, soil properties and topography that form individual Hydrological Response Units (HRUs), as well as climate data. The calculations are based on empirical equations and provide highly accurate information. The SWAT model can be calibrated with observational data such as surface runoff or actual evapotranspiration and adjusts for sensitive parameters such as transmission loss.

The tests showed that SWAT can be used to calculate the groundwater recharge of a karst aquifer with high temporal and spatial resolution. In the Western Mountain Aquifer, on average 34% of precipitation in the recharge zone contributes to groundwater recharge, while the remaining precipitation evaporates or turns into surface runoff. SWAT calculates an average annual recharge of 199mm.

Hydro-Pedo transfer functions (HPTF) were first developed by Wessolek et al. (2008) following Lin's (2003) “Hydropedology” approach – the integration of methods from soil, plant, and water science. HPTF calculate annual percolation rates on a regional scale but were developed for the European continental climate and applied here for the first time to other climates and karst regions. The empirical functions are based on the water budget equation and account for annual precipitation, potential evapotranspiration, soil properties, and vegetation.

HPTF were found to be unable to capture the fast flow component, which is very relevant to infiltration in karst. As a result, groundwater recharge is underestimated. However, by adding the fast flow component from the SWAT model, realistic recharge values can also be calculated using HPTF (Figure 1).

Water resource: Groundwater
Type of product:
  • Modelling & software tools
Application sector: Natural water environment, Water resource management
Funding measure: GRoW
Project: MedWater

Contact and partners

Logo Technische Universität Berlin, Hydrogeologie
  • Technische Universität Berlin, Hydrogeologie,
  • Gebäude BH-N, 3. Stock, Ernst-Reuter-Platz 1,
  • 10587 Berlin

Technische Universität Berlin, Hydrogeologie,
Georg-Augustin-Universität Göttingen, Angewandte Geologie,

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