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  1. D300 大学院環境学研究科
  2. D300a 雑誌掲載論文
  3. 学術雑誌

Factors controlling sea salt modification and dry deposition of nonsea-salt components to the ocean

http://hdl.handle.net/2237/23081
http://hdl.handle.net/2237/23081
16bff72a-a390-410f-aa5d-0dac10650e67
名前 / ファイル ライセンス アクション
Kawakami_et_al-2008-Journal_of_Geophysical_Research_Atmospheres_1984-2012.pdf Kawakami_et_al-2008-Journal_of_Geophysical_Research_Atmospheres_1984-2012.pdf (864.0 kB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2015-11-04
タイトル
タイトル Factors controlling sea salt modification and dry deposition of nonsea-salt components to the ocean
言語 en
著者 Kawakami, N.

× Kawakami, N.

WEKO 60734

en Kawakami, N.

Search repository
Osada, K.

× Osada, K.

WEKO 60735

en Osada, K.

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Nishita, C.

× Nishita, C.

WEKO 60736

en Nishita, C.

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Yabuki, M.

× Yabuki, M.

WEKO 60737

en Yabuki, M.

Search repository
Kobayashi, H.

× Kobayashi, H.

WEKO 60738

en Kobayashi, H.

Search repository
Hara, K.

× Hara, K.

WEKO 60739

en Hara, K.

Search repository
Shiobara, M.

× Shiobara, M.

WEKO 60740

en Shiobara, M.

Search repository
アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
権利
言語 en
権利情報 ©2008. American Geophysical Union.
抄録
内容記述 [1] Modification of sea salt aerosol particles (SSA particles) by HNO3 and SO2 is an important process for changing phase partitioning of acidic gases from industrial regions to the ocean. During 12–29 September 2005, size-segregated aerosol particles and acidic gases were sampled around the western part of the Japanese Islands to elucidate controlling factors of modification of SSA particles by acidic gases and to estimate dry deposition flux over the ocean. For coarse (>2 μm diameter) SSA particles, the amount of Cl− deficiency from the seawater ratio was comparable to the sum of the equivalent concentrations of NO3− and nonsea-salt (nss) SO42−, suggesting Cl− displacement of SSA particles by acidic gases such as HNO3 and SO2. The Cl− deficiency of SSA particles varied according to the size range and wind speed. Decreasing modification occurred with increasing wind speed for particles of 2–8 μm. Under high (low) wind conditions, the NO3− concentration per unit surface area of coarse SSA particles was lower (higher) for particles >8 μm than for those of 2–8 μm diameter. The respective dry deposition fluxes (Fdry) of NO3−, nss-SO42−, HNO3, and SO2 were estimated according to the wind speed and size of aerosol particles. On average, the Fdry of particulate NO3− was 10 times larger than that of HNO3, but Fdry of nss-SO42− was almost equal to that of SO2. Phase partitioning of dry deposition for NO3− and nss-SO42− over the ocean differs from that of coastal marine areas.
言語 en
内容記述タイプ Abstract
出版者
言語 en
出版者 Wiley
言語
言語 eng
資源タイプ
資源タイプresource http://purl.org/coar/resource_type/c_6501
タイプ journal article
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
DOI
関連タイプ isVersionOf
識別子タイプ DOI
関連識別子 https://doi.org/10.1029/2007JD009410
ISSN
収録物識別子タイプ PISSN
収録物識別子 2169-897X
書誌情報 en : Journal of Geophysical Research: Atmospheres

巻 113, 号 D14, p. D14216-D14216, 発行日 2008-07
著者版フラグ
値 publisher
URI
識別子 http://dx.doi.org/10.1029/2007JD009410
識別子タイプ DOI
URI
識別子 http://hdl.handle.net/2237/23081
識別子タイプ HDL
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