期刊
ENVIRONMENTAL POLLUTION
卷 265, 期 PT A, 页码 -出版社
ELSEVIER SCI LTD
DOI: 10.1016/j.envpol.2020.114909
关键词
Tropospheric O-3; Nitrogen deposition; Isoprene emission; Poplar; Leaf position
资金
- National Natural Science Foundation of China [41907383]
- Key Research Program of Frontier Sciences, CAS [QYZDB-SSW-DQC019]
- National Key Research and Development Program of China [2017YFC0210106]
- Chinese Academy of Sciences President's International Fellowship Initiative (PIFI) for Senior Scientists [2016VBA057]
We investigated isoprene (ISO) emission and gas exchange in leaves from different positions along the vertical canopy profile of poplar saplings (Populus euramericana cv. '74/76'). For a growing season, plants were subjected to four N treatments, control (NC, no N addition), low N (LN, 50 kg N ha(-1)year(-1)), middle N (MN, 100 kg N ha(-1)year(-1)), high N (HN, 200 kg N ha(-1)year(-1)) and three O-3 treatments (CF, charcoal-filtered ambient air; NF, non-filtered ambient air; NF + O-3, NF + 40 ppb O-3). Our results showed the effects of O-3 and/or N on standardized ISO rate (ISOrate) and photosynthetic parameters differed along with the leaf position, with larger negative effects of O-3 and positive effects of N on ISOrate and photosynthetic parameters in the older leaves. Expanded young leaves were insensitive to both treatments even at very high O-3 concentration (67 ppb as 10-h average) and HN treatment. Significant O-3 x N interactions were only found in middle and lower leaves, where ISOrate declined by O-3 just when N was limited (NC and LN). With increasing light-saturated photosynthesis and chlorophyll content, ISOrate was reduced in the upper leaves but on the contrary increased in middle and lower leaves. The responses of ISOrate to AOT40 (accumulated exposure to hourly O-3 concentrations > 40 ppb) and PODY (accumulative stomatal uptake of 0 3 > Y nmol O-3 m(-2) PLA s(-1)) were not significant in upper leaves, but ISOrate significantly decreased with increasing AOT40 or PODY under limited N supply in middle leaves but at all N levels in lower leaves. Overall, ISOrate changed along the vertical canopy profile in response to combined O-3 and N exposure, a behavior that should be incorporated into multi-layer canopy models. Our results are relevant for modelling regional isoprene emissions under current and future O-3 pollution and N deposition scenarios. (C) 2020 Elsevier Ltd. All rights reserved.
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