Oelmann Yvonne, Kreutziger Yvonne, Temperton Vicky M, Buchmann Nina, Roscher Christiane, Schumacher Jens, Schulze Ernst-Detlef, Weisser Wolfgang W, Wilcke Wolfgang
Institute of Ecology, Department of Soil Science, Berlin University of Technology, Salzufer 11-12, D-10587 Berlin, Germany.
J Environ Qual. 2007 Jan 25;36(2):396-407. doi: 10.2134/jeq2006.0217. Print 2007 Mar-Apr.
Previous research has shown that plant diversity influences N and P cycles. However, the effect of plant diversity on complete ecosystem N and P budgets has not yet been assessed. For 20 plots of artificially established grassland mixtures differing in plant diversity, we determined N and P inputs by bulk and dry deposition and N and P losses by mowing (and subsequent removal of the biomass) and leaching from April 2003 to March 2004. Total deposition of N and P was 2.3 +/- 0.1 and 0.2 +/- 0.01 g m(-2) yr(-1), respectively. Mowing was the main N and P loss. The net N and P budgets were negative (-6.3 +/- 1.1 g N and -1.9 +/- 0.2 g P m(-2) yr(-1)). For N, this included a conservative estimate of atmospheric N(2) fixation. Nitrogen losses as N(2)O were expected to be small at our study site (<0.05 g m(-2) yr(-1)). Legumes increased the removal of N with the harvest and decreased leaching of NH(4)-N and dissolved organic nitrogen (DON) from the canopy. Reduced roughness of grass-containing mixtures decreased dry deposition of N and P. Total dissolved P and NO(3)-N leaching from the canopy increased in the presence of grasses attributable to the decreased N and P demand of grass-containing mixtures. Species richness did not have an effect on any of the studied fluxes. Our results demonstrate that the N and P fluxes in managed grassland are modified by the presence or absence of particular functional plant groups and are mainly driven by the management.
以往的研究表明,植物多样性会影响氮和磷的循环。然而,植物多样性对整个生态系统氮和磷收支的影响尚未得到评估。对于20个植物多样性不同的人工建立的草地混合物样地,我们测定了2003年4月至2004年3月期间通过大气干沉降和湿沉降的氮和磷输入量,以及通过刈割(及随后的生物量移除)和淋溶造成的氮和磷损失量。氮和磷的总沉降量分别为2.3±0.1和0.2±0.01 g m(-2) yr(-1)。刈割是氮和磷损失的主要途径。氮和磷的净收支为负(-6.3±1.1 g N和-1.9±0.2 g P m(-2) yr(-1))。对于氮而言,这包括对大气固氮的保守估计。在我们的研究地点,N2O形式的氮损失预计很小(<0.05 g m(-2) yr(-1))。豆科植物增加了收获时氮的移除量,并减少了冠层中NH4-N和溶解有机氮(DON)的淋溶。含草混合物粗糙度的降低减少了氮和磷的干沉降。由于含草混合物对氮和磷的需求降低,冠层中总溶解磷和NO3-N的淋溶量在有草存在时增加。物种丰富度对任何研究的通量均无影响。我们的结果表明,管理草地中的氮和磷通量会因特定功能植物群的存在与否而改变,且主要受管理措施驱动。