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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

Deposition processes of ionic constituents to snow cover

http://hdl.handle.net/2237/23080
http://hdl.handle.net/2237/23080
3ecb501e-9e12-4f36-84ad-4620d4512317
名前 / ファイル ライセンス アクション
Deposition_processes_of_ionic_constituents_to_snow_cover.pdf Deposition_processes_of_ionic_constituents_to_snow_cover.pdf (308.6 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 Deposition processes of ionic constituents to snow cover
言語 en
著者 Osada, K.

× Osada, K.

WEKO 60730

en Osada, K.

Search repository
Shido, Y.

× Shido, Y.

WEKO 60731

en Shido, Y.

Search repository
Iida, H.

× Iida, H.

WEKO 60732

en Iida, H.

Search repository
Kido, M.

× Kido, M.

WEKO 60733

en Kido, 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 © 2010, Authors. Licensed under the Creative Commons (CC-BY-NC-ND 4.0, http://creativecommons.org/licenses/by-nc-nd/4.0/)
キーワード
主題Scheme Other
主題 Acid deposition
キーワード
主題Scheme Other
主題 Scavenging process
キーワード
主題Scheme Other
主題 Eastern Asia
キーワード
主題Scheme Other
主題 Mountain slope
キーワード
主題Scheme Other
主題 Mount Tateyama
抄録
内容記述 Atmospheric deposition is an important removal process of aerosol particles and gases from the atmosphere. To elucidate the relative contributions of wet and dry processes and in-cloud and below-cloud scavenging based on deposition amounts in winter at Mt. Tateyama, central Japan, we obtained daily samples (December, 2006–March, 2007) of size-segregated aerosol particles and precipitation at Senjyugahara (SJ; 475 m a.s.l.) and vertical samples of spring snow cover at Murododaira (MR, 2450 m a.s.l., 13 km distance from SJ) on the western flank of Mt. Tateyama. The NH4+ and nssSO42− in aerosols were mostly found in the fine fraction (<2 μm), although Na+, NO3−, and nssCa2+ were mainly detected in the coarse fraction (>2 μm). Average ionic concentrations (μg g−1) in precipitation at SJ were higher about 3.8 for Na+ and nssCa2+, 3.4 for NO3−, 3.7 for NH4+, 2.5 for nssSO42− than those at MR, whereas cumulative precipitation amounts at SJ and MR were, respectively, 84 and 175 cm of water equivalent. Wet and dry deposition amounts during the study period were estimated for sites using size-segregated aerosol data, winter averages of HNO3, NH3, and SO2 concentrations, and dry deposition velocities. Particle-dry deposition comprised about 3% (Na+) to 11% (NH4+) of the total deposition at MR. The maximum amounts of gas dry deposition were estimated, respectively, as 4, 13, and 3% of the total deposition at MR for NH4+, NO3−, and nssSO42−. The relative contributions of below-cloud scavenging (BCS) between MR and SJ were estimated as considering the wet only deposition amount at MR. Higher contributions of BCS were obtained for Na+ (56%) and nssCa2+ (45%), whereas BCSs for NH4+, NO3−, and nssSO42− were lower than 28%. Ionic constituents existing predominantly in the coarse fraction showed a large contribution of BCS.
言語 en
内容記述タイプ Abstract
出版者
言語 en
出版者 Elsevier
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 AM
出版タイプResource http://purl.org/coar/version/c_ab4af688f83e57aa
DOI
関連タイプ isVersionOf
識別子タイプ DOI
関連識別子 https://doi.org/10.1016/j.atmosenv.2009.10.031
ISSN
収録物識別子タイプ PISSN
収録物識別子 1352-2310
書誌情報 en : Atmospheric Environment

巻 44, 号 3, p. 347-353, 発行日 2010-01
著者版フラグ
値 author
URI
識別子 http://dx.doi.org/10.1016/j.atmosenv.2009.10.031
識別子タイプ DOI
URI
識別子 http://hdl.handle.net/2237/23080
識別子タイプ HDL
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