首页 | 本学科首页   官方微博 | 高级检索  
     检索      

神农架大九湖泥炭湿地能量通量及平衡分析
引用本文:周颖,葛继稳,彭凤姣,李艳元,李金群,李永福,翁文畅.神农架大九湖泥炭湿地能量通量及平衡分析[J].水生态学杂志,2019,40(4):14-21.
作者姓名:周颖  葛继稳  彭凤姣  李艳元  李金群  李永福  翁文畅
作者单位:中国地质大学盆地水文过程与湿地生态恢复学术创新基地;中国地质大学湿地演化与生态恢复湖北省重点实验室;中国地质大学生态环境研究所;中国电力工程顾问集团中南电力设计院有限公司
基金项目:中国地质大学(武汉)中央高校基本科研业务费专项(1323521225,1323521325);环境保护 部生态环境十年变化遥感调查与评估项目(2012046151;2012046395)
摘    要:研究大九湖泥炭湿地通量,为准确评估泥炭地生态系统与大气间的物质和能量交换提供基础数据。利用涡度相关系统对神农架大九湖2015年9月~2016年8月的净辐射、显热通量、潜热通量及土壤热通量进行了为期1年的连续观测。结果表明:1)泥炭地全年净辐射为3 146.91MJ/m2,显热通量为931.79MJ/m2,潜热通量为1 762.40MJ/m2,土壤热通量为22.26MJ/m2;能量分配主要以潜热为主,占净辐射的56%。潜热通量为能量散失的主要形式,土壤表现为热汇。2)各能量分量季节变化明显,10月、1月、4月及7月的日变化均以净辐射为基础,呈相似的单峰型曲线变化。3)波文比逐月变化不规律,月平均波文比为0.65、波动在0.34~1.06,年波文比为0.53,全年能量分配潜热通量大于显热通量。4)神农架大九湖泥炭地年能量闭合度为0.86,存在14%的能量不闭合。不闭合的原因可能与下垫面状况、季节变化及平流的影响产生的波动等相关。

关 键 词:泥炭地  能量通量  涡度协方差  大九湖
收稿时间:2017/7/9 0:00:00
修稿时间:2019/7/16 0:00:00

Energy Flux and Balance Analysis of Dajiuhu Peatland in Shennongjia
ZHOU Ying,GE Ji-wen,PENG Feng-jiao,LI Yan-yuan,LI Jin-qun,LI Yong-fu and WENG Wen-chang.Energy Flux and Balance Analysis of Dajiuhu Peatland in Shennongjia[J].Journal of Hydroecology,2019,40(4):14-21.
Authors:ZHOU Ying  GE Ji-wen  PENG Feng-jiao  LI Yan-yuan  LI Jin-qun  LI Yong-fu and WENG Wen-chang
Institution:Hubei Key Laboratory of Wetland Evolution and Ecological Restoration, China University of Geoscience, Wuhan 430074, P. R. China; 2. Laboratory of Basin Hydrological and Wetland Eco-restoration, China University of Geosciences, Wuhan 430074, P. R. China; Institute of Ecology and Environmental Sciences, China University of Geosciences, Wuhan 430074, P. R. China;,Hubei Key Laboratory of Wetland Evolution and Ecological Restoration, China University of Geoscience, Wuhan 430074, P. R. China; 2. Laboratory of Basin Hydrological and Wetland Eco-restoration, China University of Geosciences, Wuhan 430074, P. R. China; Institute of Ecology and Environmental Sciences, China University of Geosciences, Wuhan 430074, P. R. China;,Central Southern China Electric Power Design Institute Co., Ltd. of China Power Engineering Consulting Group, Wuhan 430071, P. R. China,Central Southern China Electric Power Design Institute Co., Ltd. of China Power Engineering Consulting Group, Wuhan 430071, P. R. China,Hubei Key Laboratory of Wetland Evolution and Ecological Restoration, China University of Geoscience, Wuhan 430074, P. R. China; Laboratory of Basin Hydrological and Wetland Eco-restoration, China University of Geosciences, Wuhan 430074, P. R. China; Institute of Ecology and Environmental Sciences, China University of Geosciences, Wuhan 430074, P. R. China;,Hubei Key Laboratory of Wetland Evolution and Ecological Restoration, China University of Geoscience, Wuhan 430074, P. R. China; 2. Laboratory of Basin Hydrological and Wetland Eco-restoration, China University of Geosciences, Wuhan 430074, P. R. China; Institute of Ecology and Environmental Sciences, China University of Geosciences, Wuhan 430074, P. R. China; and Hubei Key Laboratory of Wetland Evolution and Ecological Restoration, China University of Geoscience, Wuhan 430074, P. R. China; 2. Laboratory of Basin Hydrological and Wetland Eco-restoration, China University of Geosciences, Wuhan 430074, P. R. China; Institute of Ecology and Environmental Sciences, China University of Geosciences, Wuhan 430074, P. R. China;
Abstract:
Keywords:peatland  energy flux  eddy covariance  Dajiuhu peatland
本文献已被 CNKI 等数据库收录!
点击此处可从《水生态学杂志》浏览原始摘要信息
点击此处可从《水生态学杂志》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号