Formation and deposition of ozone in a red pine forest

• Published in: Water, air, and soil pollution air, and soil pollution, 2004, Vol.151 (1-4), p.53-70
• Main Authors: UTIYAMA, Masahiro, FUKUYAMA, Tsutomu, MARUO, Yasuko Yamada, ICHINO, Toshihiro, IZUMI, Katsuyuki, HARA, Hiroshi, TAKANO, Kenichi, SUZUKI, Haruko, AOKI, Masatoshi
• Format: Article
• Language: English
• Subjects: Air pollution; Air temperature; Applied sciences; Atmospheric pollution; Autumn; Canopies; Coniferous forests; Deposition; Diurnal variations; Environmental monitoring; Evergreen trees; Exact sciences and technology; Forests; Hydrocarbons; Leaves; Nitrogen; Nitrogen oxides; Ozone; Photochemicals; Pine trees; Pinus densiflora; Pollutants physicochemistry study: properties, effects, reactions, transport and distribution; Pollution; Radiation; Radiation measurement; Soil pollution; Solar radiation; Summer; Trees; Trunks; Upper atmosphere
• ISSN: 0049-6979; 1573-2932
• DOI: 10.1023/b:wate.0000009891.12108.b9

Concentrations of ozone and nitrogen oxides, together with air temperature and solar radiation intensity, were measured at several heights on a tower standing through the canopy of a red pine forest in summer and in autumn. In the summer observation, the diurnal variation patterns of ozone concentration both above and below the canopy were all similar and parallel to the solar radiation intensity. Using the data collected immediately above the canopy, deviation from the Leighton relationship and variations of concentration sums [O sub(3)] + [NO] and [NO sub(2)] + [NO] were examined, and as a result, it was supposed that ozone was photochemically formed there in the daytime, probably because hydrocarbons emitted from pine trees broke the photostationary state among ozone and nitrogen oxides. The vertical temperature profile exhibited an inversion at the leaf-layer, which must have hindered vertical mixing of the air and made the trunk space more or less isolated from the upper atmosphere. These observations led to an idea that the similarity of the ozone variation pattern at every height was caused by the photochemical formation that proceeded simultaneously above and below the canopy rather than by vertical transport. Such situations of ozone formation were supported by observation of two maximums in the ozone vertical profile, one immediately above the canopy and another in the trunk space. Another feature of the ozone profile was a deep minimum in the leaf layer, which indicated ozone deposition onto leaf surfaces. This study thus revealed concurrence of ozone formation and deposition, and left two potentially important implications worthy of further investigation: (1) a forest is not always a sink but can be a source of ozone in sunlit conditions, and (2) deposition of ozone to trees can take place not only from outside but also from inside of a forest. In the autumn observation, however, the ozone formation was barely recognizable above the canopy and no longer found in the trunk space; in addition, the ozone concentration minimum in the leaf layer disappeared, suggesting that the deposition or removal was dependent on temperature.