| dc.description.abstract | Restoring river-floodplain connectivity has been proposed as an alternative management
measure for natural flood defence through the temporary storage of floodwaters and the
attenuation of flood peaks downstream. Whilst several studies have documented the
associated ecological and landscape amenity values of such hydrological measures, the
water quality benefits to the adjacent water bodies have been inadequately studied. To
date, the focus of scientific research and natural resource management has been on the
role of riparian buffer zones for the alleviation of agricultural diffuse nitrate pollution.
This research investigated the potential for nitrate attenuation in a restored riverfloodplain
system, the River Cole (Coleshill, England), with the aim of informing future
restoration schemes of the best management practices for enhanced nitrate removal.
Following restoration, the increased river-floodplain connectivity has encouraged
overbank flooding of the different land use zones throughout the year. The flood pulse
supplies the floodplain soil with river water nitrate and creates the necessary anaerobic
conditions for the effective removal of nitrate via heterotrophic denitrification, while
organic carbon is supplied mainly through the traditional land use management
practices of grazing and mowing. The conservation of nitrogen via DNRA is of minimal
importance in this lowland agricultural catchment setting, mainly due to the nonlimiting
nitrate supply from the surrounding agricultural land but also the intermittent
saturation regime that restricts the low redox conditions to the low elevation riparian
areas. This presents the added benefit of restricting methane emission to the more
frequently waterlogged riparian soils, while denitrification is effective across the whole
floodplain area. Additionally, more than 90% of nitrate removal occurs in the top 30 cm
of the soil during the flood, while the role of subsurface denitrification is restricted by
the limited availability of organic carbon and nitrate. Based on these findings, this study
demonstrates that, for similar catchments, the nitrate removal capacity of a floodplain
can be assessed by the denitrification capacity of the surface soil. The assessment of the
denitrification capacity can be undertaken inexpensively using a simple empirical model
that requires a single microbial denitrification potential measurement, and a seasonal or
monthly record of soil nitrate content, soil moisture, and temperature. Assessments can
be undertaken as part of the design process to optimise nitrate removal or post
restoration to appraise the functioning of the scheme. | en_US |
