z-logo
Premium
Spatial variability of nitrous oxide emissions in an unmanaged old‐growth beech forest
Author(s) -
Jungkunst Hermann F.,
Bargsten Anika,
Timme Marc,
Glatzel Stephan
Publication year - 2012
Publication title -
journal of plant nutrition and soil science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.644
H-Index - 87
eISSN - 1522-2624
pISSN - 1436-8730
DOI - 10.1002/jpln.201100412
Subject(s) - beech , flux (metallurgy) , nitrous oxide , environmental science , greenhouse gas , atmospheric sciences , hydrology (agriculture) , chemistry , forestry , ecology , geography , physics , geotechnical engineering , organic chemistry , engineering , biology
Abstract Nitrous oxide (N 2 O) is a high‐impact greenhouse gas. Due to the scarcity of unmanaged forests in Central Europe, its long‐term natural background emission level is not entirely clear. We measured soil N 2 O emissions in an unmanaged, old‐growth beech forest in the Hainich National Park, Germany, at 15 plots over a 1‐year period. The average annual measured N 2 O flux rate was (0.49 ± 0.44) kg N ha –1  y –1 . The N 2 O emissions showed background‐emission patterns with two N 2 O peaks. A correlation analysis shows that the distance between plots (up to 380 m) does not control flux correlations. Comparison of measured data with annual N 2 O flux rates obtained from a standard model (Forest‐DNDC) without site‐specific recalibration reveals that the model overestimates the actual measured N 2 O flux rates mainly in spring. Temporal variability of measured N 2 O flux was better depicted by the model at plots with high soil organic C (SOC) content. Modeled N 2 O flux rates were increased during freezing only when SOC was > 0.06 kg C kg –1 . The results indicate that the natural background of N 2 O emissions may be lower than assumed by most approaches.

This content is not available in your region!

Continue researching here.

Having issues? You can contact us here