Retention of Dissolved Inorganic Nitrogen by Foliage and Twigs of Four Temperate Tree Species

被引:36
作者
Adriaenssens, Sandy [3 ]
Staelens, Jeroen [1 ,3 ]
Wuyts, Karen [2 ,3 ]
Samson, Roeland [2 ]
Verheyen, Kris [3 ]
Boeckx, Pascal [1 ]
机构
[1] Univ Ghent, Lab Appl Phys Chem ISOFYS, B-9000 Ghent, Belgium
[2] Univ Antwerp, Dept Biosci Engn, B-2020 Antwerp, Belgium
[3] Univ Ghent, Forest & Nat Lab, B-9090 Gontrode, Melle, Belgium
关键词
nitrogen uptake; atmospheric deposition; throughfall; stable isotopes; canopy exchange; CANOPY BUDGET MODEL; ATMOSPHERIC DEPOSITION; PICEA-ABIES; FOREST ECOSYSTEMS; WET DEPOSITION; NORWAY SPRUCE; THROUGHFALL CHEMISTRY; STEMFLOW CHEMISTRY; DRY DEPOSITION; N-15; TRACERS;
D O I
10.1007/s10021-012-9568-5
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Nitrogen (N) retention by tree canopies is believed to be an important process for tree nutrient uptake, and its quantification is a key issue in determining the impact of atmospheric N deposition on forest ecosystems. Due to dry deposition and retention by other canopy elements, the actual uptake and assimilation by the tree canopy is often obscured in throughfall studies. In this study, N-15-labeled solutions ( and ) were used to assess dissolved inorganic N retention by leaves/needles and twigs of European beech, pedunculate oak, silver birch, and Scots pine saplings. The effects of N form, tree species, leaf phenology, and applied to ratio on the N retention were assessed. Retention patterns were mainly determined by foliar uptake, except for Scots pine. In twigs, a small but significant N-15 enrichment was detected for , which was found to be mainly due to physicochemical adsorption to the woody plant surface. The mean retention ratio varied considerably among species and phenological stadia, which indicates that the use of a fixed ratio in the canopy budget model could lead to an over- or underestimation of the total N retention. In addition, throughfall water under each branch was collected and analyzed for , , and all major ions. Net throughfall of was, on average, 20 times higher than the actual retention of by the plant material. This difference in retention could not be attributed to pools and fluxes measured in this study. The retention of was correlated with the net throughfall of K+, Mg2+, Ca2+, and weak acids during leaf development and the fully leafed period, while no significant relationships were found for retention. This suggests that the main driving factors for retention might be ion exchange processes during the start and middle of the growing season and passive diffusion at leaf senescence. Actual assimilation or abiotic uptake of N through leaves and twigs was small in this study, for example, 1-5% of the applied dissolved N-15, indicating that the impact of canopy N retention from wet deposition on forest productivity and carbon sequestration is likely limited.
引用
收藏
页码:1093 / 1107
页数:15
相关论文
共 68 条
  • [1] Nitrogen saturation in temperate forest ecosystems - Hypotheses revisited
    Aber, J
    McDowell, W
    Nadelhoffer, K
    Magill, A
    Berntson, G
    Kamakea, M
    McNulty, S
    Currie, W
    Rustad, L
    Fernandez, I
    [J]. BIOSCIENCE, 1998, 48 (11) : 921 - 934
  • [2] Foliar Nitrogen Uptake from Wet Deposition and the Relation with Leaf Wettability and Water Storage Capacity
    Adriaenssens, Sandy
    Staelens, Jeroen
    Wuyts, Karen
    de Schrijver, An
    Van Wittenberghe, Shari
    Wuytack, Tatiana
    Kardel, Fatemeh
    Verheyen, Kris
    Samson, Roeland
    Boeckx, Pascal
    [J]. WATER AIR AND SOIL POLLUTION, 2011, 219 (1-4) : 43 - 57
  • [3] FOLIAR UPTAKE OF N-15 FROM SIMULATED CLOUD WATER BY RED SPRUCE (PICEA-RUBENS) SEEDLINGS
    BOWDEN, RD
    GEBALLE, GT
    BOWDEN, WB
    [J]. CANADIAN JOURNAL OF FOREST RESEARCH-REVUE CANADIENNE DE RECHERCHE FORESTIERE, 1989, 19 (03): : 382 - 386
  • [4] Negative impact of nitrogen deposition on soil buffering capacity
    Bowman, William D.
    Cleveland, Cory C.
    Halada, Lubos
    Hresko, Juraj
    Baron, Jill S.
    [J]. NATURE GEOSCIENCE, 2008, 1 (11) : 767 - 770
  • [5] Direct canopy nitrogen uptake from N-15-labeled wet deposition by mature red spruce
    Boyce, RL
    Friedland, AJ
    Chamberlain, CP
    Poulson, SR
    [J]. CANADIAN JOURNAL OF FOREST RESEARCH-REVUE CANADIENNE DE RECHERCHE FORESTIERE, 1996, 26 (09): : 1539 - 1547
  • [6] BOYCE RL, 1992, TREES-STRUCT FUNCT, V6, P19
  • [7] Uptake of 15NH3 by Picea abies in Closed Chamber Experiments
    BRUCKNER, G
    GEBAUER, G
    SCHULZE, ED
    [J]. ISOTOPENPRAXIS, 1993, 29 (1-2): : 71 - 76
  • [8] INTERCEPTION AND UPTAKE OF NH4 AND NO3 FROM WET DEPOSITION BY ABOVEGROUND PARTS OF YOUNG BEECH (FAGUS-SILVATICA L) TREES
    BRUMME, R
    LEIMCKE, U
    MATZNER, E
    [J]. PLANT AND SOIL, 1992, 142 (02) : 273 - 279
  • [9] Throughfall chemistry and canopy interactions in a Sitka spruce plantation sprayed with six different simulated polluted mist treatments
    Chiwa, M
    Crossley, A
    Sheppard, LJ
    Sakugawa, H
    Cape, JN
    [J]. ENVIRONMENTAL POLLUTION, 2004, 127 (01) : 57 - 64
  • [10] Distribution of nitrogen-15 tracers applied to the canopy of a mature spruce-hemlock stand, Howland, Maine, USA
    Dail, David Bryan
    Hollinger, David Y.
    Davidson, Eric A.
    Fernandez, Ivan
    Sievering, Herman C.
    Scott, Neal A.
    Gaige, Elizabeth
    [J]. OECOLOGIA, 2009, 160 (03) : 589 - 599