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长白山火山区温泉温室气体排放通量研究
引用本文:张茂亮,郭正府,成智慧,张丽红,郭文峰,杨灿尧,付庆州,温心怡.长白山火山区温泉温室气体排放通量研究[J].岩石学报,2011,27(10):2898-2904.
作者姓名:张茂亮  郭正府  成智慧  张丽红  郭文峰  杨灿尧  付庆州  温心怡
作者单位:1. 中国科学院地质与地球物理研究所,新生代地质与环境重点实验室,北京100029
2. 台湾大学地质科学系,台北
基金项目:本文受国家自然科学基金委重大国际合作研究项目 (41020124002) 资助.
摘    要:温泉是深部岩浆活动在地表的直接表现,并且向大气圈排放大量的温室气体.然而,国内尚无火山区温泉排放的温室气体通量研究报道.我国长白山火山区水热活动强烈,主要有湖滨温泉带、聚龙温泉群、锦江温泉以及火山口外围的十八道沟温泉.本文利用数字皂膜流量计测量温泉气体排放通量,并结合前人对长白山火山区温泉气体成分的研究成果,估算了研究区温泉所排放的温室气体通量.结果表明,长白山火山区温泉排放的CO2通量为6.9×104t·a-1,CH4排放通量为428.44t·a-1,与意大利Pantelleria Island火山区温泉排放的温室气体通量规模相当.本文的测试结果表明:数字皂膜流量计在火山区温室气体排放通量估算研究中的应用是可行的.

关 键 词:温泉气体  温室气体  通量  长白山火山区  中国东北
收稿时间:7/1/2011 12:00:00 AM
修稿时间:9/1/2011 12:00:00 AM

Greenhouse gases flux estimation of hot springs in Changbaishan volcanic field,NE China
ZHANG MaoLiang,GUO ZhengFu,CHENG ZhiHui,ZHANG LiHong,GUO WenFeng,YANG CanYao,FU QingZhou and WEN XinYi.Greenhouse gases flux estimation of hot springs in Changbaishan volcanic field,NE China[J].Acta Petrologica Sinica,2011,27(10):2898-2904.
Authors:ZHANG MaoLiang  GUO ZhengFu  CHENG ZhiHui  ZHANG LiHong  GUO WenFeng  YANG CanYao  FU QingZhou and WEN XinYi
Institution:Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;Department of Geosciences, Taiwan University, Taipei, China;Department of Geosciences, Taiwan University, Taipei, China;Department of Geosciences, Taiwan University, Taipei, China
Abstract:Hot springs, which belong to the direct manifestations of deep-derived magma activities, are ample and intensive in Changbaishan volcanic field, NE China. Greenhouse gases emitting from hot springs take up an important part of the total flux contributed by the whole volcanic field. However, there remains no research on greenhouse gases flux estimation of hot springs in volcanic fields of China. A new apparatus named GL-103B digital bubble/liquid flowmeter is used to measure the gas fluxes of the Lake shoreline hot spring belt, Julong hot spring area, Jinjiang hot springs and 18daogou hot springs in changbaishan volcanic field. Combining with the previous studies on gas compositions, the total flux of greenhouse gases emitting from hot springs in Changbaishan volcanic field has been estimated. The results of greenhouse gases flux in this area, 6.9×104 t·a-1 for CO2 and 428.44t·a-1 for CH4, could be compared to that of Pantelleria Island volcano in Sicily, Italy. As is revealed by this study, the digital bubble/liquid flowmeter could be considered as a suitable choice for greenhouse gases flux estimation of hot springs in volcanic fields.
Keywords:Hot springs gases  Greenhouse gases  Flux  Changbaishan volcanic field  NE China
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