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Tracing nitrate in water from the forest to the aquifer using stable isotopes of oxygen and nitrogen
The sources of nitrate in a riparian zone
along a restored corridor of the river Thur in Switzerland are investigated using
oxygen and nitrogen isotope ratios in nitrate. These data contribute to a
better understanding of nitrogen transformation in hydrologic flow paths from
upland agricultural fields to the river passing through different succession
stages of vegetation. The effects of river restoration on water quality in
alluvial and dry hardwood forests are assessed. Tracing nitrate from the forest to the aquifer
Forests usually supply drinking water of
good quality thanks to the filtering of water through the soil. In Switzerland,
about 42% of groundwater protection zones are located in forested areas.
However, the continuous input of atmospheric nitrogen since the 1970s can have
led to the saturation of forest ecosystems and resulted in an increased release
of nitrate to groundwater. Nitrate originating from agriculture lands can also
contribute to increased nitrate leaching into groundwater, even if the
catchment is largely forested. A good understanding of flow paths and nitrate
sources in catchments is therefore important to assess the forest influence on
groundwater quality and to select the most effective practices of land
management (forest, agriculture, river) aiming at a sustainable water supply of
good quality. Numerous studies have investigated either the chemistry of
percolation waters in the forest root zone or the groundwater quality. However,
very few have assessed the biochemical transformation of the water composition
along its flow path from the forest soil to the well and the mixing in the
aquifer with water from other sources within the catchment. Identification of nitrate sourcesThis project aims at identifying the different sources of nitrate (atmospheric deposition, nitrification in forest soils and N-fertilizers) in the saturated and unsaturated zones and at a better understanding of the N transformations along the flow paths from the forest to the aquifer by analyzing the oxygen and nitrogen isotopes in nitrate.
The study is performed in a riparian zone
including different succession stages (gravel bars, river banks, grassland,
alluvial and climax forests) along a restored corridor of the river Thur
(Canton Thurgau, Switzerland). The relative contribution of the different
nitrate sources in water is assessed. The seasonal variations of nitrate concentrations
and of oxygen and nitrogen isotope ratios in nitrate are determined in three
transects across the riparian zone from the riverbank to the upland
agricultural fields, passing through the different succession stages of
vegetation. MethodsThe experimental site is located along a
restored corridor of the river Thur where a monitoring infrastructure (piezometers,
wells) has been installed in the framework of the RECORD project (see below).
Water samples for isotopic analysis are collected in the river Thur and along
three terrestrial transects in the saturated and unsaturated zones. Laboratory
experiments are performed to investigate:
The denitrifier method is used to analyze oxygen and nitrogen isotopes in nitrate.
A national and international projectThis project is financially supported by the Swiss State Secretariat for Education and Research within the framework of the European Cost Action FP601 "Forest Management and the Water Cycle” (FORMAN). It is also integrated in the interdisciplinary RECORD project launched in April 2007 within the Competence Center of Environment and Sustainability (CCES) of the ETH domain. An important question to be addressed is whether river revitalization influences the quality of drinking water pumped from alluvial ecosystems that are hydraulically linked to the river and the runoff of neighboring ecosystems. Links
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