『Abstract
Vulnerability maps are important tools for water decision makers
and land-use planners for protection of aquifers against contamination.
The vulnerability map, according to the parametric method SINTACX
for assessing intrinsic aquifer vulnerability, was validated in
a case study with chlorofluorocarbon tracer technologies (CFC-11,
CFC-12, and CFC-113) of groundwater. The tested area was the 1,295
km2 volcano-sedimentary area of San Miguel de Allende
(SMA), Mexico. From the results of this area, it appears that
the vulnerability map is in parts inconsistent with the underlying
groundwater flow system. Thus, the vulnerability map was corrected
with tracer information. The validated vulnerability map indicates
that the degree of vulnerability varies from low to moderate-high.
Low vulnerability values are found in the graben extending from
north to south along the SMA fault system and high values in recharge
areas southeast and northwest of the study area. The investigation
is a demonstration that the scientific reliability of results
of the parametric method can be improved by validation with tracer
techniques representing the groundwater dynamics. The flexible
structure of SINTACX allows revising and adjusting scores and
weights of the parameter maps to rebuild a new vulnerability map
consistent with the hydrological system.
Keywords: Aquifer vulnerability; SINTACX; Chlorofluorocarbons;
Semi-arid regions; Guanajuato; Mexico』
Introduction
Study area
General description and hydrology
Geology and hydrogeology
Materials and methods
Parameter estimation for parametric methods
Field and laboratory techniques
Interpretation of chlorofluorocarbons
Results and discussion
Groundwater chemistry
Degree of vulnerability
Residence time and modern water percentage
Validation of vulnerability map
Conclusion
Acknowledgments
References