Groundwater resources on the Caribbean Islands of Aruba, Bonaire and Curaca
o are limited and of poor quality. The groundwater of the islands is bracki
sh, due to both seawater mixing and the semi-arid climate of the islands. T
wo hundred and thirty water samples were collected to relate chemical varia
tions in the groundwater of the three islands to the underlying differences
in geology, and to define the natural versus anthropogenic influences. Bot
h the chemical and isotopic (delta 18O, deltaD, and delta 37Cl) composition
s of samples were determined.
Several geochemical processes are recognised in the chemistry of the ground
water samples. The most important processes are calcite dissolution, cation
exchange, silicate weathering and potassium fixation. In (sub)urban areas
anthropogenic influences affect the groundwater quality: high nitrate conce
ntrations were measured. Infiltrating domestic and agricultural (waste)wate
r replenishes the aquifer, and has a desalinization effect on the groundwat
er quality. This phenomenon is primarily seen on Curacao, the most populate
d island.
Oxygen and hydrogen isotopic compositions of groundwaters from Curacao and
Bonaire show that the samples are either meteoric water, or are affected by
evaporation or seawater mixing. No distinction could be made between the l
ast two processes. Only a few samples were measured for the Cl-isotope comp
osition; all showed that no physical processes have taken place.