Tracing urban drinking water sources: global state of the art and
insights from an IAEA-Coordinated Research Project
Abstract
Climate change, inter-annual precipitation variability, recurrent
droughts, and flash flooding, coupled with increasing water needs, are
shaping the co-evolution of socioeconomic and cultural assemblages,
water laws and regulations, and equitable drinking water access and
allocation worldwide. Recognizing the need for mitigation strategies for
drinking water availability in urban areas, the Isotope Hydrology
Section of the International Atomic Energy Agency (IAEA) coordinated a
state-of-the-art global assessment to evaluate water sources and
distribution of drinking water supply in urban centers, an initiative
entitled “Use of Isotope Techniques for the Evaluation of Water Sources
for Domestic Supply in Urban Areas (2018-2023)”. Here, we report on a)
current research trends for studying urban drinking water systems during
the last two decades and b) the development, testing, and integration of
new methodologies, aiming for a better assessment, mapping, and
management of water resources used for drinking water supply in urban
settings. Selected examples of water isotope applications (Canada, USA,
Costa Rica, Ecuador, Morocco, Botswana, Romania, Slovenia, India, and
Nepal) provide context to the insights and recommendations reported and
highlight the versatility of water isotopes to underpin seasonal and
temporal variations across various environmental and climate scenarios.
The study revealed that urban areas depend on a large spectrum of water
recharge across mountain ranges, extensive local groundwater extraction,
and water transfer from nearby or distant river basins. The latter is
reflected in the spatial isotope snapshot variability. High-resolution
monitoring (hourly and sub-hourly) isotope sampling revealed large
diurnal variations in the wet tropics (Costa Rica) (up to 1.5‰ in δ
18O) and more uniform diurnal variations in urban
centers fed by groundwater sources (0.08 ‰ in δ 18O)
([Ljubljana](https://www.google.com/search?client=firefox-b-1-d&sca_esv=f5a20a2e9138d638&sca_upv=1&sxsrf=ADLYWIKR6-DvBtjaWqFYRhn6VgnegOa8kg:1717189104058&q=Ljubljana&stick=H4sIAAAAAAAAAONgVuLQz9U3SMrNNXnEaMwt8PLHPWEprUlrTl5jVOHiCs7IL3fNK8ksqRQS42KDsnikuLjgmngWsXL6ZJUm5WQl5iUCAAFa64FOAAAA&sa=X&ved=2ahUKEwjMrrz047iGAxWyG9AFHSVwCBgQzIcDKAB6BAgTEAE),
Slovenia). Similarly, while d-excess was fairly close to the
global mean value (+10 ‰) across all urban centers (10-15‰),
reservoir-based drinking water systems show significantly lower values
(up to ~ -20 ‰) (Arlington, TX, USA and Gaborone,
Botswana), as a result of strong evapoconcentration processes. δ
18O time series and depth-integrated sampling
highlighted the influence of the catchment damping ratio in the ultimate
intake water composition. By introducing new, traceable spatial and
temporal tools that span from the water source to the end-user and are
linked to the engineered and socio-economic structure of the water
distribution system, governmental, regional, or community-based water
operators and practitioners could enhance drinking water treatment
strategies (including more accurate surface water blending estimations)
and improve urban water management and conservation plans in the light
of global warming.