WestminsterResearch

Patterns of denitrification rates in European alluvial soils under various hydrological regimes

Pinay, Gilles and Gumiero, Bruna and Tabacchi, Eric and Giminez, Olivier and Tabacchi-Planty, Anne Marie and Hefting, Maria Margaretha and Burt, Tim P. and Black, Valerie A. and Nilsson, Christer and Iordache, Virgil and Bureau, Fabrice and Vought, Lena and Petts, Geoffrey E. and Decamps, Henri (2007) Patterns of denitrification rates in European alluvial soils under various hydrological regimes. Freshwater Biology, 52 (2). pp. 252-266. ISSN 0046-5070

Full text not available from this repository.

Official URL: http://dx.doi.org/10.1111/j.1365-2427.2006.01680.x

Abstract

1. Denitrification in floodplain soils is one of the main biological processes emitting and reducing nitrous oxide, a greenhouse gas, and the main process responsible for the buffering capacity of riparian zones against diffuse nitrate pollution. 2. The aim of this study was to measure denitrification rates under a wide range of current climatic conditions and hydrological regimes in Europe (from latitude 64°N to latitude 42°N and from longitude 2°W to longitude 25°E), in order to determine the response patterns of this microbial process under different climatic and hydrological conditions, and to identify denitrification proxies robust enough to be used at the European scale. 3. Denitrification activity was significant in all the floodplain soils studied whatever the latitude. However, we found an increase in rates of an order of magnitude from high to mid latitudes. Maximum rates (above 30 g N m−2 month−1) were measured in the maritime conditions of the Trent floodplain. These rates are similar to mineralisation rates measured in alluvial soils and of the same order of magnitude as the amount of N stored in herbaceous plants in alluvial soils. 4. We used Multivariate Adaptative Regression Splines to relate the response variable denitrification with five relevant predictors, namely soil moisture, temperature, silt plus clay, nitrate content and herbaceous plant biomass. 5. Soil moisture, temperature, and nitrate were the three main control variables of microbial denitrification in alluvial soils in decreasing order of importance. 6. The model developed for denitrification with interaction effects outperformed a pure additive model. Soil moisture was involved in all interactions, emphasising its importance in predicting denitrification. 7. These results are discussed in the context of scenarios for future change in European hydrological regimes.

Item Type:Article
Research Community:University of Westminster > Life Sciences, School of
ID Code:5951
Deposited On:10 Feb 2009 14:40
Last Modified:22 Dec 2009 10:12

Repository Staff Only: item control page