Aquifer vulnerability

Identification of the areas where an aquifer is most exposed to contamination from the land surface.

Aquifer vulnerability expresses how easily a contaminant released at the land surface reaches the groundwater. The application maps the protection that soil, unsaturated zone and aquifer provide, and identifies the areas where groundwater requires priority protection.

OutputVulnerability map per category and a combined vulnerability map

DecisionPrioritisation of areas for groundwater protection and monitoring

ScaleAquifer to region

Built forA defined aquifer and contaminant pathway

Default categories

The suggested criteria derive from the input factors of established index methods such as DRASTIC and fall into two categories: the protection above the water table and the conditions that govern contaminant transport. The criteria are suggested inputs, not a pre-configured index; ratings and weights are defined by the user. These default categories can be renamed or removed by the user, and new categories can be added.

Subsurface protection

Thickness and properties of the soil and the unsaturated zone that delay and attenuate contaminants before they reach the water table.

Contaminant transport

Recharge, terrain and aquifer properties that control how fast and how far contaminants travel.

The criteria library is maintained continuously. In each project, criteria can be added, removed or renamed.

Vulnerability concepts

The concept represented by the map depends on the selected criteria. The suggested criteria describe intrinsic vulnerability; contaminant properties and pollution sources can be added as further categories.

Intrinsic

Depends on the hydrogeological setting only, independent of any particular contaminant.

Specific

Adds the behaviour of a contaminant or contaminant group, such as nitrate or pesticides.

Pollution risk

Combines vulnerability with the load from pollution sources such as agriculture, industry or wastewater.

Index methods

Published index methods differ in the aquifer type they address and in the factors they combine. Their factors can be set up as criteria in a project, with the method’s ratings entered as class scores and its weights as analyst weights.

MethodAquifer typeFactorsSource
DRASTICPorous and fracturedDepth to water, net recharge, aquifer media, soil media, topography, impact of the vadose zone, hydraulic conductivityAller et al. (1987)
GODAll types, data-scarce settingsGroundwater confinement, overlying strata, depth to groundwaterFoster (1987)
SINTACSPorous and fracturedSeven DRASTIC-type factors, with weight sets for different hydrogeological settingsCivita (1994)
AVIPorousHydraulic resistance of the layers above the aquifer, from their thickness and hydraulic conductivityVan Stempvoort et al. (1993)
EPIKKarstEpikarst, protective cover, infiltration conditions, karst network developmentDoerfliger et al. (1999)
PIKarst and other aquifersProtective cover, infiltration conditionsGoldscheider et al. (2000)
COPKarstConcentration of flow, overlying layers, precipitationVías et al. (2006)
IKAVKarstPotential vulnerability from rated factors; actual vulnerability from contaminant transport modellingMoreno-Gómez et al. (2022)
Selected index methods for groundwater vulnerability mapping.

Constraints

Vulnerability maps usually cover the whole study area. Constraints serve to mask areas outside the extent of the assessed aquifer or areas without data; the application suggests none.

From criteria to vulnerability

  1. CriteriaStandardised so that high scores consistently mean high vulnerability
  2. Category mapsWeights within each category give its vulnerability map
  3. Vulnerability mapWeights between the categories combine the category maps
  4. Priority areasContiguous areas of very high vulnerability in which no criterion falls below a minimum value

The direction of each criterion usually follows from its role in the contaminant pathway: a shallow water table, permeable soils and high recharge increase vulnerability, while a thick, fine-grained unsaturated zone decreases it. Weights come from the analytic hierarchy process, ranking, rating, the multi-influencing factor method or an anonymous stakeholder survey.

Results

The result classes rank the locations within the study area by their relative vulnerability; they do not predict contaminant concentrations or travel times.

Sensitivity analysis shows which areas keep their class when the weights change. Validation against observed groundwater quality, such as nitrate concentrations in monitoring wells, will follow in a later version.

Typical questions

  • Where is the aquifer least protected by the overlying soil and unsaturated zone?
  • Which wellfields and springs lie in areas of high vulnerability?
  • Where should new monitoring wells be placed?
  • How does vulnerability change between seasonal high and low water tables?

Case stories

No case stories for this application yet.

References

Start a vulnerability project

Select “Aquifer vulnerability” when creating a project. The suggested criteria appear in step 2.