Studies on budget of water vapor and carbon dioxide in Rasyomon doline
Studies on budget of water vapor and carbon dioxide in Rasyomon doline
批准号:
09480133
负责人:
MAITANI Toshihiko
金额:
$6.08万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for Scientific Research (B)
财政年份:
1997
资助国家:
日本
项目状态:
已结题
起止时间:
1997 至 1998
中文摘要
测定了罗生门碱的微气象因子(如气温、湿度、气流、光合有效辐射)和植物的生理因子(如光合速率和蒸腾速率)。在峡谷的最低点,侵蚀形成了一个微弱的呼吸,吹洞穴,在温暖的季节排出冷空气。低气压底部的特征是夏季白天温度低于15ºC左右。在整个暖季,doline形成了非常稳定的热层,保持了过湿润的气候,这是苔藓最喜欢的环境。为了弄清从洞穴中流出的空气与洞穴中干燥的关系,我们在1997年夏天两次人工封闭了洞穴最窄的部分。封闭期的空气温度和土壤温度比开放期高3 ~ 4个‰。水汽在封闭期较开放期增加4 ~ 5 hPa。溶洞开放期CO_2浓度约为700 ppm,封闭期CO_2浓度上升至1000 ppm左右。这些结果定量地表明,带有冷但去湿空气的强化空气与石灰石的干燥密切相关。洞穴的关闭也导致了海底CO_2浓度的显著升高,这是苔藓最适宜的生长环境。考虑到这些结果,我们现在计划减少通过洞穴的气流,以防止洞穴干燥,并更新苔藓林。生长在碱底的植物大多具有阴生植物的生理特性,适应了碱底的特定环境。
英文摘要
Micrometeorological factors( such as air temperature, humidity, air flow, and photosynthesis available radiation) and physiological factors of plants ( such as photosynthesis and transpiration rates) were measured in Rasyomon doline. At the lowest point in the doline, erosion created a weak breathing, blowing cavetunnel, draining a cold air in warmer seasons. The bottom in the depression was characterized by daytime summer temperatures below about 15゚C.Throughout warm seasons, very stable thermal layer was formed in the doline and it maintained a perhumid climate, which was a favorite environment to mosses.To clarify how the air flow from the cave relates to the drying in the doline, we artificially closed the narrowest section of the cave 2 times in the summer of 1997. Air temperature and soil temperature were higher by 3-4゚C in the closed period than in the opened period of cave. However, water, vapor increased by 4-5 hPa in the closed period than that in the opened period. The CO_2 concentration were about 700 ppm in the opened period and increased high levels near 1000 ppm in the closed period of cave. These results demonstrate quantitatively that the strengthned air with a cool but dehumified air is closely related to drying of the doline. The closure of cave also induced a significant rise of CO_2 concentration at the bottom of the doline, which is a favorite environment for mosses to grow. Considering these results, we are now planning to reduce an air flow through the cave to prevent from drying of caveand to renew the moss forest. Most of plants growing at the bottom of the doline had physiological charactersitics of shade plant, adopting to the specific environment of doline.
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Maitani, T.and Miyashita, K.: "Vertical structure of temperatures of tree's leaves and gate wall at Rasyomon doline." Bull.Res.Inst.for Bioresources, Okayama Univ.5 (2). 169-181 (1998)
Maitani, T. 和 Miyashita, K.:“罗生门天坑树叶和门墙温度的垂直结构。”
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宮下晃一、米谷俊彦: "羅生門ドリーネにおける樹木の葉温と壁面温度の鉛直構造" 岡山大学資源生物科学研究所報告. 6巻1号(印刷中). (1998)
Koichi Miyashita,Toshihiko Yonetani:“罗生门天坑树木的垂直结构”报告,第 6 卷,第 1 期(出版中)。
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米谷俊彦・宮下晃一: "羅生門ドリーネにおける樹木の葉温と壁面温度の鉛直構造について" 岡大資生研報. 6巻1号. 169-181 (1998)
Toshihiko Yonetani和Koichi Miyashita:“罗生门天坑树木的叶温和壁温的垂直结构”冈谷大学资生研究报告第6卷第1. 169-181 (1998)。
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米谷俊彦・宮下晃一・山地一代・Roger H.Show・柏木良明: "新見市草間の羅生門ドリーネにおける微気象観測" 日本農業気象学会1997年度全国大会講演要旨. 20-21 (1997)
Toshihiko Yonetani、Koichi Miyashita、Kazuyo Yamaji、Roger H.Show、Yoshiaki Kashiwagi:“新见市草间罗生门天坑的微气象观测”日本农业气象学会 1997 年全国会议摘要 20-21 (1997)。
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山地一代・米谷俊彦・宮下晃一・田中丸重美: "羅生門ドリーネにおける微気象の高度変化と植物の光合成・蒸散量の測定" 中国と四国の農業気象. 10号. 46-49 (1997)
Kazuyo Yamaji、Toshihiko Yonetani、Koichi Miyashita、Shigemi Tanakamaru:“罗生门天坑小气候和植物光合作用和蒸腾作用的海拔变化测量”中国和四国农业气象 10. 46-49 (1997)。
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共 22 条
Study on Honami wave and turbulent transports within and above plant canopie
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批准号:05640477
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项目类别:Grant-in-Aid for General Scientific Research (C)
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资助金额:$1.34万
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财政年份:1993
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负责人:MAITANI Toshihiko
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依托单位:
海外基金