History of the hydrogeochemical study of groundwater in the Netherlands and the research motives
article
An overview is presented of research on the hydrogeochemical aspects of groundwater resources in the Netherlands conducted
since the early nineteenth century. The earliest studies investigated groundwater as a resource for drinking water. The frst
systematic, national study was in 1868 and was motivated by the cholera epidemics at that time. At the beginning of the
twentieth century, research for drinking water production was institutionalised at national level. Since the 1960s, the range of
organisations involved in hydrogeochemical research has broadened. Societal motives are also identifed: shallow, biogenic
methane as fossil fuel (already researched since the 1890s); groundwater contamination; freshening/salinisation of aquifers;
ecohydrology and nature conservation; aquifer thermal energy storage; national and regional groundwater monitoring for
policy evaluation; impact of climate change and weather variability; and occurrence of brackish groundwater and brines in the
deeper subsurface. The last-mentioned has been driven by a series of motives ranging from water supply for recreational spas
and mineral water production to subsurface disposal of radioactive waste. There have been two major scientifc drivers: the
introduction of techniques for using isotopes as tracers, and geochemical computer modelling. Another recent development
has been the increasing capabilities in analytical chemistry in relation to the contamination of groundwater with emerging
pollutants. Many of the motives for research emerged in the 1980s. Overall, the societal and associated technical motives
turn out to be more important than the scientifc motives for hydrogeochemical research on groundwater in the Netherlands.
Once a research motive has emerged, it commonly tends to remain.
since the early nineteenth century. The earliest studies investigated groundwater as a resource for drinking water. The frst
systematic, national study was in 1868 and was motivated by the cholera epidemics at that time. At the beginning of the
twentieth century, research for drinking water production was institutionalised at national level. Since the 1960s, the range of
organisations involved in hydrogeochemical research has broadened. Societal motives are also identifed: shallow, biogenic
methane as fossil fuel (already researched since the 1890s); groundwater contamination; freshening/salinisation of aquifers;
ecohydrology and nature conservation; aquifer thermal energy storage; national and regional groundwater monitoring for
policy evaluation; impact of climate change and weather variability; and occurrence of brackish groundwater and brines in the
deeper subsurface. The last-mentioned has been driven by a series of motives ranging from water supply for recreational spas
and mineral water production to subsurface disposal of radioactive waste. There have been two major scientifc drivers: the
introduction of techniques for using isotopes as tracers, and geochemical computer modelling. Another recent development
has been the increasing capabilities in analytical chemistry in relation to the contamination of groundwater with emerging
pollutants. Many of the motives for research emerged in the 1980s. Overall, the societal and associated technical motives
turn out to be more important than the scientifc motives for hydrogeochemical research on groundwater in the Netherlands.
Once a research motive has emerged, it commonly tends to remain.
TNO Identifier
990420
Source
Hydrogeology Journal, pp. 1-11.
Pages
1-11