British Geological Survey, Servicio Nacional de Aguas Subterraneas, Riego y Avenamiento. 1988 The continuation of hydrogeological investigations in the north and east of the Valle Central, Costa Rica : final report 1984-87. Nottingham, UK, British Geological Survey, 132pp. (WD/88/013) (Unpublished)
Abstract
This report is the conclusion of a three year investigation of the
groundwater resources of the Valle Central in Costa Rica carried out jointly
by BGS (British Geological Survey) and SENARA (Servicio Nacional de Aguas,
Riego y Avenamiento) on behalf of ICAyA (Instituto Costarricence de
Acueductos y Alcantarrillados) under the terms of their loan agreement with
the World Bank. The objective of the investigation is to obtain a better
understanding of the complex groundwater regime, principally of the Colima
aquifers, and on this basis to make recommendations for a rational policy of
further groundwater exploitation and the prevention of groundwater
pollution.
The study has been based on new hydrogeological information gained from the
drilling of cored investigation boreholes and trial production boreholes and
re-evaluation of existing data. A variety of hydrogeological techniques
have been employed, including borehole flow logging and laboratory testing
of rock hydraulic properties, and numerous water samples have been analysed
for a wide range of chemical parameters. The laboratory tests of rock
properties have been particularly important in providing new scientific data
about the movement and storage of water in the lavas and pyroclastics.
It is concluded that development of an additional 1000-1500 1/s of
groundwater from the Colima aquifers is possible. The most effective
strategy for development is the construction of new wellfields. Recommended
areas for new groundwater abstraction include an extension of the Valencia
Wellfield, a new wellfield within the area between Pitahaya and Barreal and
a possible well field south of the Aeropuerto Juan Santamaria. The
groundwater quality is generally excellent but there are indications of
deterioration and, in some areas, aquifers are at risk of becoming seriously
contaminated in the future. As groundwater development expands it will be
increasingly important to monitor both groundwater levels and groundwater
quality in order to maintain borehole yields and the potability of
groundwater supplies.
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