CO 2 is the key gas of the greenhouse ones, the effect of its radiation on temperature ascent is 60% of the total greenhouse gases. The elevating CO 2 concentration influences to a great extent the future climate wa...CO 2 is the key gas of the greenhouse ones, the effect of its radiation on temperature ascent is 60% of the total greenhouse gases. The elevating CO 2 concentration influences to a great extent the future climate warming in a regional or global scale. Forest is the main part of carbon cycling in the land ecosystem.. Monitoring CO 2 absorption and emission in the forest ecosystem play a non\| fungible role in study on the global change. Gongga Mountain is located in the southeast margin of the Tibetan Plateau, and there exist intact vertical vegetation zonality, which is advantageous for measuring soil CO\-2 emission on each vertical forest zonality and researching the ecological factors of soil respiration.The east slope of Gongga Mountain develops 5 natural forest vertical zones from lower to higher altitudes: secondary forest, ever\|greened and deciduous broad\|leaved mixed forest, broad\|leaved and coniferous mixed forest, coniferous forest and alpine shrubs. Based on the two\|year’s measurement, the soil respiration of each forest averaged: 5 488, 6 344, 5 912, 4 176 and 3 864μmol CO 2/(m 2·s); the flux of soil CO 2 emission was arranged: 208 628, 241 169, 224 746, 158 752 and 146 891kg CO 2/(hm 2·d), respectively.展开更多
From the middle of 19 century, mountain glacier recession occurs widely and Hailuogou glacier does so on a great scale. There is a primary vegetation succession series on the shrinking glacial area. The enhancement of...From the middle of 19 century, mountain glacier recession occurs widely and Hailuogou glacier does so on a great scale. There is a primary vegetation succession series on the shrinking glacial area. The enhancement of greenhouse gases result in the climate warming. Glacier recession is a response to the global climate warming. Determination on soil respiration plays an important role in the research on the global carbon cycling, which is one key problem for the global climate change studies. The observed values differ in different sites or with different measuring methods or by distinct observers, which add up one indefinite factor to the study on the global carbon balance. There exist different base courses at one same climatic district on the glacier shrinking area in Hailuogou, Gongga Mountain.Comparing the characteristic of different soil CO 2 emissions through the synchronous observation by the analyze ways of on\|the\|spot infrared CO 2(CI\|301) and chromatographic mainframe(HP5890A),and with the achievements of the study on the glacial recession area and vegetation succession, we established a series of soil CO 2 emission flux that can be a reference to emend the determination of soil CO 2 emission on different regions of the globe and that can be a useful parameter for modeling the global carbon cycling . Vegetation succession in the more than 2000m long glacial recession area is serially divided into 6 phases :①exposed shrinking area phase,②herbs phase,③shrubs phase,④deciduous and broad\|leaved mixed forest phase⑤coniferous and broad\|leaved mixed forest phase,⑥coniferous forest phase. Based on the two\|year’s measurement, the series of the mean intensity of soil respiration was arranged: 0, 1 960, 1 136, 2 080, 3 688 and 4 706μmol CO\-2/(m\+2·s); the series of the flux of soil CO\-2 emission was arranged: 0, 74 510, 43 185, 79 071, 140 200 and 178 890kg CO\-2/(hm\+2·d), respectively.Among the effect factors of soil respiration, temperature is the main one. All kinds of temperature influence soil respiration during the 6 succession phases.. The 2nd phase is influenced by atmospheric temperature, the 3rd and 4th phase by near\|surface temperature, the 5th and 6th phases by 5～10cm soil temperature.展开更多
全球变暖已经成为不争的事实,陆地生态系统碳循环的研究受到了各界广泛关注,是当前全球变化研究中的重点。土壤CO_(2)排放是陆地生态系统与大气间二氧化碳交换的最大通量之一,当前陆地生态系统中土壤CO_(2)排放如何响应全球气候变暖及...全球变暖已经成为不争的事实,陆地生态系统碳循环的研究受到了各界广泛关注,是当前全球变化研究中的重点。土壤CO_(2)排放是陆地生态系统与大气间二氧化碳交换的最大通量之一,当前陆地生态系统中土壤CO_(2)排放如何响应全球气候变暖及其影响因素仍不清楚,限制了对土壤碳循环过程及影响机制的深入认识。旨在明确全球变暖背景下陆地生态系统中土壤CO_(2)排放格局及影响因素。基于Web of Science、PubMed和中国知网等中英文期刊数据库,充分收集全球范围内的相关野外试验文献81篇,提取出65个研究位置和213组相关研究数据,采用Meta分析方法探讨陆地生态系统土壤CO_(2)排放对增温的响应特征,分析其与海拔、气候、土壤含水量、容重(BD)、pH、全氮(TN)和土壤有机碳(SOC)的相关关系。结果表明:陆地生态系统中土壤CO_(2)排放对增温整体有显著的正向响应,在农、林、草生态系统中,增温使土壤CO_(2)排放分别显著增加13.1%、18.0%、5.9%(P<0.05),森林生态系统对增温响应的正效应最强烈;增温能在短时期内促进土壤呼吸,但随着增温持续时间增加,土壤呼吸对温度的敏感性会降低,对温度变化产生适应性,从而使其对增温的响应能力减弱;响应特征受到环境因子、土壤特性以及其他试验条件等的影响,绝大多数条件下对增温表现出显著的正响应特征,不同影响因子之间共同作用、相互影响。增温通常能够改变植物生物量、土壤养分含量及微生物数量和活性,从而影响到植被根际呼吸和土壤呼吸速率。相关分析表明,海拔对土壤CO_(2)排放有显著负向影响,而年均气温、年均降水量、土壤含水量和仪器嵌入土壤深度则对土壤CO_(2)排放产生显著正向影响。这些结果对于理解全球土壤CO_(2)排放的时空变化格局有重要意义,也为准确评价全球变暖背景下土壤碳汇功能及其持续性提供理论依据。展开更多
【目的】明确不同土地利用方式土壤氧化亚氮(N_(2)O)排放系数的差异并评估区域N_(2)O排放,为评估南方红壤丘陵区N_(2)O排放清单提供基础数据和参考依据。【方法】选择南方红壤丘陵区4种常见的土地利用方式(油茶林、旱地农田、稻田和松...【目的】明确不同土地利用方式土壤氧化亚氮(N_(2)O)排放系数的差异并评估区域N_(2)O排放,为评估南方红壤丘陵区N_(2)O排放清单提供基础数据和参考依据。【方法】选择南方红壤丘陵区4种常见的土地利用方式(油茶林、旱地农田、稻田和松林),通过分析土壤不施肥与施氮肥时N_(2)O排放速率和排放量的差异,计算排放系数,并用^(15)N同位素标记方法探究硝化作用和反硝化作用对土壤排放N_(2)O的相对贡献。【结果】不同土地利用方式土壤理化性质差异明显,稻田全氮含量最高(2.22 g/kg),显著高于其他3种土地利用方式土壤(P<0.05,下同)。土壤不施肥时,N_(2)O排放速率在0~227.80μg/(kg·h),施氮量为200 kg N/ha时,N_(2)O排放速率在0~4213.27μg/(kg·h)。4种土地利用方式的土壤N_(2)O排放系数均随土壤孔隙含水量(WPFS)增加而增加,WPFS为75%时,稻田、旱地农田、油茶林和松林土壤N_(2)O排放系数分别为2.47%、0.39%、2.31%和0.91%。4种土地利用方式土壤N_(2)O排放系数主要受全氮含量影响,N_(2)O累积排放量均与潜在反硝化潜势呈显著正相关,除稻田外,其他3种土地利用方式土壤N_(2)O累积排放量也与潜在硝化势呈显著正相关,以NO_(3)^(-)-N为底物的反硝化作用对N_(2)O排放的相对贡献平均大于90.00%,远高于硝化作用。【结论】南方红壤丘陵区土壤以NO_(3)^(-)-N为底物的反硝化作用主导N_(2)O排放,施用氨基氮肥可能有效减少氮肥N_(2)O排放损失,为国家执行碳中和政策提供理论依据。展开更多
文摘CO 2 is the key gas of the greenhouse ones, the effect of its radiation on temperature ascent is 60% of the total greenhouse gases. The elevating CO 2 concentration influences to a great extent the future climate warming in a regional or global scale. Forest is the main part of carbon cycling in the land ecosystem.. Monitoring CO 2 absorption and emission in the forest ecosystem play a non\| fungible role in study on the global change. Gongga Mountain is located in the southeast margin of the Tibetan Plateau, and there exist intact vertical vegetation zonality, which is advantageous for measuring soil CO\-2 emission on each vertical forest zonality and researching the ecological factors of soil respiration.The east slope of Gongga Mountain develops 5 natural forest vertical zones from lower to higher altitudes: secondary forest, ever\|greened and deciduous broad\|leaved mixed forest, broad\|leaved and coniferous mixed forest, coniferous forest and alpine shrubs. Based on the two\|year’s measurement, the soil respiration of each forest averaged: 5 488, 6 344, 5 912, 4 176 and 3 864μmol CO 2/(m 2·s); the flux of soil CO 2 emission was arranged: 208 628, 241 169, 224 746, 158 752 and 146 891kg CO 2/(hm 2·d), respectively.
文摘From the middle of 19 century, mountain glacier recession occurs widely and Hailuogou glacier does so on a great scale. There is a primary vegetation succession series on the shrinking glacial area. The enhancement of greenhouse gases result in the climate warming. Glacier recession is a response to the global climate warming. Determination on soil respiration plays an important role in the research on the global carbon cycling, which is one key problem for the global climate change studies. The observed values differ in different sites or with different measuring methods or by distinct observers, which add up one indefinite factor to the study on the global carbon balance. There exist different base courses at one same climatic district on the glacier shrinking area in Hailuogou, Gongga Mountain.Comparing the characteristic of different soil CO 2 emissions through the synchronous observation by the analyze ways of on\|the\|spot infrared CO 2(CI\|301) and chromatographic mainframe(HP5890A),and with the achievements of the study on the glacial recession area and vegetation succession, we established a series of soil CO 2 emission flux that can be a reference to emend the determination of soil CO 2 emission on different regions of the globe and that can be a useful parameter for modeling the global carbon cycling . Vegetation succession in the more than 2000m long glacial recession area is serially divided into 6 phases :①exposed shrinking area phase,②herbs phase,③shrubs phase,④deciduous and broad\|leaved mixed forest phase⑤coniferous and broad\|leaved mixed forest phase,⑥coniferous forest phase. Based on the two\|year’s measurement, the series of the mean intensity of soil respiration was arranged: 0, 1 960, 1 136, 2 080, 3 688 and 4 706μmol CO\-2/(m\+2·s); the series of the flux of soil CO\-2 emission was arranged: 0, 74 510, 43 185, 79 071, 140 200 and 178 890kg CO\-2/(hm\+2·d), respectively.Among the effect factors of soil respiration, temperature is the main one. All kinds of temperature influence soil respiration during the 6 succession phases.. The 2nd phase is influenced by atmospheric temperature, the 3rd and 4th phase by near\|surface temperature, the 5th and 6th phases by 5～10cm soil temperature.
文摘全球变暖已经成为不争的事实,陆地生态系统碳循环的研究受到了各界广泛关注,是当前全球变化研究中的重点。土壤CO_(2)排放是陆地生态系统与大气间二氧化碳交换的最大通量之一,当前陆地生态系统中土壤CO_(2)排放如何响应全球气候变暖及其影响因素仍不清楚,限制了对土壤碳循环过程及影响机制的深入认识。旨在明确全球变暖背景下陆地生态系统中土壤CO_(2)排放格局及影响因素。基于Web of Science、PubMed和中国知网等中英文期刊数据库,充分收集全球范围内的相关野外试验文献81篇,提取出65个研究位置和213组相关研究数据,采用Meta分析方法探讨陆地生态系统土壤CO_(2)排放对增温的响应特征,分析其与海拔、气候、土壤含水量、容重(BD)、pH、全氮(TN)和土壤有机碳(SOC)的相关关系。结果表明:陆地生态系统中土壤CO_(2)排放对增温整体有显著的正向响应,在农、林、草生态系统中,增温使土壤CO_(2)排放分别显著增加13.1%、18.0%、5.9%(P<0.05),森林生态系统对增温响应的正效应最强烈;增温能在短时期内促进土壤呼吸,但随着增温持续时间增加,土壤呼吸对温度的敏感性会降低,对温度变化产生适应性,从而使其对增温的响应能力减弱;响应特征受到环境因子、土壤特性以及其他试验条件等的影响,绝大多数条件下对增温表现出显著的正响应特征,不同影响因子之间共同作用、相互影响。增温通常能够改变植物生物量、土壤养分含量及微生物数量和活性,从而影响到植被根际呼吸和土壤呼吸速率。相关分析表明,海拔对土壤CO_(2)排放有显著负向影响,而年均气温、年均降水量、土壤含水量和仪器嵌入土壤深度则对土壤CO_(2)排放产生显著正向影响。这些结果对于理解全球土壤CO_(2)排放的时空变化格局有重要意义,也为准确评价全球变暖背景下土壤碳汇功能及其持续性提供理论依据。
文摘【目的】明确不同土地利用方式土壤氧化亚氮(N_(2)O)排放系数的差异并评估区域N_(2)O排放,为评估南方红壤丘陵区N_(2)O排放清单提供基础数据和参考依据。【方法】选择南方红壤丘陵区4种常见的土地利用方式(油茶林、旱地农田、稻田和松林),通过分析土壤不施肥与施氮肥时N_(2)O排放速率和排放量的差异,计算排放系数,并用^(15)N同位素标记方法探究硝化作用和反硝化作用对土壤排放N_(2)O的相对贡献。【结果】不同土地利用方式土壤理化性质差异明显,稻田全氮含量最高(2.22 g/kg),显著高于其他3种土地利用方式土壤(P<0.05,下同)。土壤不施肥时,N_(2)O排放速率在0~227.80μg/(kg·h),施氮量为200 kg N/ha时,N_(2)O排放速率在0~4213.27μg/(kg·h)。4种土地利用方式的土壤N_(2)O排放系数均随土壤孔隙含水量(WPFS)增加而增加,WPFS为75%时,稻田、旱地农田、油茶林和松林土壤N_(2)O排放系数分别为2.47%、0.39%、2.31%和0.91%。4种土地利用方式土壤N_(2)O排放系数主要受全氮含量影响,N_(2)O累积排放量均与潜在反硝化潜势呈显著正相关,除稻田外,其他3种土地利用方式土壤N_(2)O累积排放量也与潜在硝化势呈显著正相关,以NO_(3)^(-)-N为底物的反硝化作用对N_(2)O排放的相对贡献平均大于90.00%,远高于硝化作用。【结论】南方红壤丘陵区土壤以NO_(3)^(-)-N为底物的反硝化作用主导N_(2)O排放,施用氨基氮肥可能有效减少氮肥N_(2)O排放损失,为国家执行碳中和政策提供理论依据。
