日本立山山murrodoaira积雪中的甲醛和过氧化氢浓度

IF 1 Q4 GEOGRAPHY, PHYSICAL Bulletin of glaciological research Pub Date : 2012-01-01 DOI:10.5331/BGR.30.33
Koichi Watanabe, Daiki Nishimoto, Sachie Ishita, Nagisa Eda, Yoshitoshi Uehara, Goichiro Takahashi, N. Kunori, T. Kawakami, W. Shimada, Kazuma Aoki, K. Kawada
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引用次数: 6

摘要

. 引言,渡边光一,西本大纪,石田Sachie, EDA Nagisa UEHARA, Goichiro TAKAHASHI, Noriyasu KUNORI, Tomonori KAWAKAMI, Wataru SHIMADA, Kazuma AOKI和Kunio KAWADA在日本丰山县murrodoaira积雪中的甲醛和过氧化氢浓度33 ' s冰川研究通报()日本冰雪学会富山县立大学,黑川,富山,日本地球顾问有限公司,富山,日本,福冈,九州大学,福冈,日本富山大学,福冈,日本(获2月;4月,改稿被接受,封面被测量。测量雪坑中甲醛(HCHO)和过氧化氢(h2o)以及主要离子的浓度(。今年4月,在日本中部日本海海岸附近的立山山murrodoaira(海拔,米)进行了3米深的试验。HCHO的峰值对应于a以上的高nsso层。米深度。沉积的HCHO浓度可能相对较好地保存在春季地层中。含硫酸盐气溶胶的HCHO可能从亚洲大陆输送到立山山。在颗粒状雪(粗粒、熔融形式)层中检测到的h2o浓度最高。压实雪层(细粒、圆粒)和固体型深度雪层(多面晶体)中h2o浓度较低。高寒地区积雪中h2o的沉积后修正作用可能比HCHO的沉积后修正作用更为显著。
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Formaldehyde and hydrogen peroxide concentrations in the snow cover at Murododaira, Mt. Tateyama, Japan
. Introduction , , Koichi WATANABE , Daiki NISHIMOTO , Sachie ISHITA , Nagisa EDA Yoshitoshi UEHARA , Goichiro TAKAHASHI , Noriyasu KUNORI , Tomonori KAWAKAMI , Wataru SHIMADA , Kazuma AOKI and Kunio KAWADA Formaldehyde and hydrogen peroxide concentrations in the snow cover at Murododaira, Mt. Tateyama, Japan 33 s Bulletin of Glaciological Research ( ) Japanese Society of Snow and Ice Toyama Prefectural University, Kurokawa, Imizu, Toyama , Japan Earth Consultant Co., Ltd., Hibari, Imizu, Toyama , Japan Kasuya Research Forest, Kyushu University, Kasuya, Fukuoka , Japan University of Toyama, Gofuku, Toyama , Japan (Received February , ; Revised manuscript accepted April , ) cover was measured. Measurements of snow chemistry Measurements of the concentrations of formaldehyde (HCHO) and hydrogen peroxide (H O ) as well as major ions in the snow pit ( . m deep) at Murododaira (altitude, m), Mt. Tateyama near the coast of the Japan Sea in Central Japan, were performed in April . The peaks of HCHO corresponded to the high nssSO layers above a . m depth. The concentrations of deposited HCHO might have been relatively well preserved in the spring layers. HCHO with sulfate aerosols may be transported to Mt. Tateyama from the Asian mainland. The highest concentration of H O was detected in the granular snow (coarse grain, melt forms) layer. The concentrations of H O were low in the layers of compacted snow (fine grain, rounded grains) and solid-type depth hoar (faceted crystals). Post-depositional modification of H O may be more significant than that of HCHO in snow in an alpine region.
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来源期刊
Bulletin of glaciological research
Bulletin of glaciological research GEOGRAPHY, PHYSICAL-
CiteScore
2.20
自引率
20.00%
发文量
1
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