globalchange  > 气候变化事实与影响
CSCD记录号: CSCD:6198559
论文题名:
藏北高寒草甸温室气体排放对长期增温的响应
其他题名: Response of Greenhouse Gases Emission Fluxes to Long-term Warming in Alpine Meadow of Northern Tibet
作者: 王学霞1; 高清竹2; 干珠扎布2; 胡国铮2; 栗文瀚2; 罗文蓉2
刊名: 中国农业气象
ISSN: 1000-6362
出版年: 2018
卷: 39, 期:3, 页码:75-79
语种: 中文
中文关键词: 温室气体排放 ; OTC增温 ; 高寒草甸 ; 酶活性 ; 土壤养分
英文关键词: Greenhouse gases emission ; OTC warming ; Alpine meadow ; Enzyme activity ; Soil nutrients
WOS学科分类: AGRICULTURE MULTIDISCIPLINARY
WOS研究方向: Agriculture
中文摘要: 为深入认识高寒草甸温室气体通量对长期气候变暖的响应,利用开顶式生长室(OTC,Open Top Chamber)模拟增温2a(2Y,2015-2016年)和6a(6Y,2011-2016年)对藏北高寒草甸生长季CO_2、CH_4和N_2O通量的影响。结果表明:与对照相比,生长季(6-8月)增温6Y处理和增温2Y处理分别增加和降低高寒草甸土壤CO_2排放通量,其中7月增温6Y处理CO_2排放通量显著高于增温2Y处理;增温6Y和2Y处理增加了高寒草甸CH_4吸收通量,但是处理间差异均不显著;高寒草甸N_2O排放通量表现为增温6Y>2Y>CK,处理间无显著差异。环境因子与温室气体排放通量的相关分析表明,CO_2、CH_4和N_2O排放通量与0~ 5cm土壤温度相关不显著;土壤湿度、植物地上生物量、微生物生物量碳和蔗糖酶是影响高寒草甸CO_2排放通量的关键因子;NO_3~--N是影响CH_4吸收通量的关键因素;脲酶和NO_3~--N是影响N_2O排放通量的主要因子。因此,增温6Y处理通过增加植物地上部生物量、蔗糖酶活性,从而提高了土壤CO_2排放通量,增温6Y和2Y处理通过增加土壤脲酶和NO_3~--N含量,从而促进了土壤N_2O排放和CH_4的吸收通量。
英文摘要: To explore the effects of long-term climate warming on greenhouse gases(GHGs) flux in the alpine meadow,the simulated warming 2 years(2Y,2015-2016) and 6 years(6Y,2011-2016) experiments were conducted by the open top chamber(OTC) in an alpine meadow of Tibetan Plateau,then the dynamics of CO_2,CH_4 and N_2O fluxes were measured during growing season.The observations showed that the CO_2 flux during growing season was increased with 6Y and decreased with 2Y warming treatment,respectively,compared with the control.And the CO_2 flux with 6Y warming treatment was significantly higher than that of 2Y treatment in July.The CH_4 absorption flux was increased with 6Y and 2Y warming treatment,but the differences between treatments were not significant in the growing season.The N_2O emission flux was showed 6Y>2Y>CK in the growing season,and the differences between treatments were not significant.The relationship between environmental factors and GHGs flux were analyzed by using of correlation analysis.The relationship between CO_2,CH_4 and N_2O fluxes and soil temperature(0-5cm) was not obvious.The soil moisture,aboveground biomass,microbial biomass carbon and invertase were key factors regulating the CO_2 fluxes,NO_3~--N was mainly factor affecting the CH_4 absorption flux,and NO_3~--N and soil urease were the main factors promoting N_2O emission flux.Therefore,the CO_2 flux was promoted by increasing plant biomass and invertase activity with 6Y warming treatment,and the N_2O emission and CH_4 absorption flux were improved by increasing the soil urease and NO_3~--N content with 6Y and 2Y warming treatment.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/155292
Appears in Collections:气候变化事实与影响

Files in This Item:

There are no files associated with this item.


作者单位: 1.中国农业科学院农业环境与可持续发展研究所
2.北京市农林科学院植物营养与资源研究所, 农业部农业环境重点实验室
3.,
4., 北京
5.北京 100081
6.100097, 中国
7.中国农业科学院农业环境与可持续发展研究所, 农业部农业环境重点实验室, 北京 100081, 中国

Recommended Citation:
王学霞,高清竹,干珠扎布,等. 藏北高寒草甸温室气体排放对长期增温的响应[J]. 中国农业气象,2018-01-01,39(3):75-79
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[王学霞]'s Articles
[高清竹]'s Articles
[干珠扎布]'s Articles
百度学术
Similar articles in Baidu Scholar
[王学霞]'s Articles
[高清竹]'s Articles
[干珠扎布]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[王学霞]‘s Articles
[高清竹]‘s Articles
[干珠扎布]‘s Articles
Related Copyright Policies
Null
收藏/分享
所有评论 (0)
暂无评论
 

Items in IR are protected by copyright, with all rights reserved, unless otherwise indicated.