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利用静态箱-气相色谱法对夏季(7月、8月和9月)长江河口湿地芦苇植被CO_2、CH_4和N_2O的叶面通量、茎秆扩散速率以及沉积物通量的日变化进行研究。结果显示,通过芦苇叶片排放的N_2O与CH_4的量分别为2.99μg/(m~2·h)和15.36μg/(m~2·h),CO_2则呈现白天吸收(-120.86 mg/(m~2·h))、夜间排放(69.39 mg/(m~2·h))的特点。芦苇茎秆N_2O、CH_4和CO_2平均扩散速率分别为1.96μg/h、142.45μg/h和10.69 mg/h,沉积物平均排放通量为N_2O 8.18μg/(m~2·h)、CH_41.58 mg/(m~2·h)、CO_2169.66 mg/(m~2·h)。芦苇茎秆和沉积物界面CH_4和CO_2的排放均呈现出明显的"单峰型"昼夜变化规律,其排放峰值集中在日照及温度最高的9:00至15:00。芦苇植株是影响温室气体排放变化的因素之一。芦苇植株在光合作用下吸收CO_2并促进CH_4的排放,而芦苇发达的根系及茎秆是温室气体排放的主要途径。同时,Pearson相关性分析表明温度对芦苇群落CH_4和NO2的排放影响显著,但与CO_2通量的相关性不明显。土壤氧化还原电位对3种气体的排放均有显著影响。 相似文献
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对昆山市区域7个点位夏秋季的5中水溶性无机阴离子(SO2-4、NO-3、NO-2、Cl-、F-)的污染特征进行了调查,结果表明,昆山市夏季大气PM2.5中5种离子平均值排序为:ρ(SO2-4)ρ(Cl-)ρ(NO-3)ρ(F-)ρ(NO-2);秋季平均值排序为:ρ(SO2-4)ρ(NO-3)ρ(Cl-)ρ(F-)ρ(NO-2)。SO2-4、NO-3和Cl-3者的总量在PM2.5中占比20%。除F-以外各区域离子的平均值秋季比夏季要高。ρ(NO-3)/ρ(SO2-4)表明,固定污染源在昆山市大气颗粒物污染中仍然占很大比重,但大部分测点的比值接近1,说明移动源也是昆山大气颗粒物的重要污染源。 相似文献
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Eimers MC Watmough SA Buttle JM Dillon PJ 《Environmental monitoring and assessment》2007,127(1-3):399-407
Increased sulphate (SO4) export from wetlands following summer droughts in central Ontario, Canada has been associated with the delayed chemical
recovery of downstream surface waters following decreased sulphur (S) emissions. Prolonged summer droughts result in a decrease
or cessation of stream flow, declines in wetland water table level and oxidation of reduced S compounds to SO4, which is subsequently flushed into drainage streams when stream flow resumes. Sulphate input-output budget calculations
(1983–1995 and 1999–2001) at a conifer Sphagnum swamp in the Plastic Lake catchment, indicate that SO4 is retained in most years but is exported on a net basis following particularly severe summer droughts that result in the
cessation of stream flow for more than 54 days (95% CI: 41–72 days). Hindcast calculations using long-term (1916–2000) stream
discharge records from a nearby station indicate that while droughts occurred frequently in south-central Ontario over the
past 85 years, sufficiently dry conditions to cause net SO4 export occurred in only18 of the past 85 years, and indicate a cumulative positive SO4 balance for the swamp (i.e. net SO4 retention). Furthermore, the S pool at the Plastic Lake swamp has been estimated to be ∼1500 kg S/ha in the upper 40 cm peat
layer, which is large compared to the amount of net SO4 export that occurs even in years with particularly dry summers (e.g. −43 kg S/ha in 1987/88). Together, these data suggest
that the wetland S pool at Plastic Lake has not been depleted by previous droughts and will continue to sustain episodic drought-related
SO4 export for the foreseeable future. 相似文献
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Anttila A Leppänen AP Rissanen K Ylipieti J 《Journal of environmental radioactivity》2011,102(7):659-666
Samples of summer pasture plants that reindeer feed on were collected in order to study 137Cs concentrations in different plant species and in species nested in certain site types, and to study the regional distribution of 137Cs in the Finnish reindeer management area. Plant species were categorized by the site types of mineral soil forest (xeric heath forest and mesic heath forest) and peatland. A third category called ’other plant species’ included plants with various site types, poorly determined species and species with poor statistics. The 137Cs concentrations in different site types differed significantly. The mean 137Cs concentrations of the whole reindeer management area in the xeric heath forest plant species was 44 ± 27 Bq/kg dw, in the mesic heath forest plant species 75 ± 59 Bq/kg dw and in the peatland plant species 219 ± 150 Bq/kg dw. The peatland species uptake 137Cs more efficiently than plant species of mineral soil forests. A particularly efficient collector of 137Cs was Trichophorum sp. It is suggested that Trichophorum sp. could be used as an indicator species for reindeer summer fodder plants. The highest concentrations of 137Cs were found in Southern Lapland and the lowest in Northern Lapland. Today, the concentrations of 137Cs in summer pasture plants that reindeer feed on in Finland are at such a level that there is no need to avoid any plant species. In the case of future nuclear fallout, reindeer grazing in peatlands would increase concentrations of 137Cs in reindeer meat. 相似文献
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Dongyou Wu Tenglong Shi Xiaoying Niu Ziqi Chen Jiecan Cui Yang Chen Xueying Zhang Jun Liu Mingxia Ji Xin Wang Wei Pu 《环境科学学报(英文版)》2022,34(4):53-65
The Asian Tropopause Aerosols Layer (ATAL) refers to an accumulation of aerosols in the upper troposphere and lower stratosphere during boreal summer over Asia, which has a fundamental impact on the monsoon system and climate change. In this study, we primarily analyze the seasonal to sub-seasonal variations of the ATAL and the factors potentially influencing those variations based on MERRA2 reanalysis. The ability of the reanalysis to reproduce the ATAL is well validated by CALIPSO observations from May to October 2016. The results reveal that the ATAL has a synchronous spatiotemporal pattern with the development and movement of the Asian Summer Monsoon. Significant enhancement of ATAL intensity is found during the prevailing monsoon period of July–August, with two maxima centered over South Asia and the Arabian Peninsula. Owing to the fluctuations of deep convection, the ATAL shows an episodic variation on a timescale of 7–12 days. Attribution analysis indicates that deep convection dominates the variability of the ATAL with a contribution of 62.7%, followed by a contribution of 36.6% from surface pollutants. The impact of precipitation is limited. The ATAL further shows a clear diurnal variation: the peak of ATAL intensity occurs from 17:30 to 23:30 local time (LT), when the deep convection becomes strongest; the minimum ATAL intensity occurs around 8:30 LT owing to the weakened deep convection and photochemical reactions in clouds. The aerosol components of the ATAL show different spatiotemporal patterns and imply that black carbon and organic carbon come mainly from India, whereas sulfate comes mainly from China during the prevailing monsoon period. 相似文献
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Wolfgang Cramer Uta Fritsch Rik Leemans Sabine Lütkemeier Dagmar Schröter Allan Watt 《Regional Environmental Change》2008,8(3):125-134
Biodiversity is essential for multiple aspects of human life and well-being, but many current assessments of the functioning
of biodiversity and ecosystems, understanding of risks posed by environmental change and the best practice of their management
of ecosystems are lacking a unified scientific and conceptual basis. Methods such as scenario analysis, and terms such as
ecosystem services, are widely used, but their meaning is understood in many different ways depending on context, user needs
and experience of researchers. In order to advance the conceptual basis for ecosystem analysis and management in a rapidly
changing world, as well as the ability of young scientists to reflect upon these concepts, we have organised five 2-week-long
summer schools in Peyresq, a remote village in the Southern French Alps. In total 173 participants have worked intensively
with 69 experienced researchers and a team of conveners and tutors in order to discuss a broad range of views on topics on
ecosystem analysis and functioning. Topics ranged from conditions of and threats to various ecosystems due to environmental
change, models and scenarios for assessment, stakeholder perceptions and needs for information, to the social and economic
contexts for biodiversity. We report our experience from these schools, present the training concept which has emerged from
them and suggest lines of further development.
相似文献
Wolfgang CramerEmail: |