合肥市PM1.0污染特征及与PM2.5污染相关性

对合肥市2014—2019年秋冬季节PM_(1.0)、PM_(2.5)、气象和理化性质等进行分析研究发现,PM_(1.0)质量浓度呈现年度波动性下降趋势,其中2015—2016年度变化最为显著。同一年度内,月度浓度同样呈现波动性变化,总体表现为11、2月PM_(1.0)质量浓度相对较低,12、1月相对较高。无污染情形时(PM_(2.5)浓度不高于75μg/m~3),PM_(1.0)/PM_(2.5)逐小时值相对平稳且比有污染情形(PM_(2.5)浓度大于75μg/m~3)总体高约10%;有污染情形下,PM_(1.0)/PM_(2.5)小时值呈现较明显的日变化特征,09∶00呈现谷值,17∶00呈现峰值,日变化特征显著高于无污染情形。PM_(1.0)质量浓度随着PM_(2.5)级别的上升而逐渐增加,PM_(1.0)/PM_(2.5)值则呈减小的污染特征。严重污染时,PM_(1.0)/PM_(2.5)显著下降,PM_(1.0～2.5)占比增加。传输型污染过程中,PM_(1.0)与OC、PM_(2.5)、SO_4~(2-)等呈现出显著的正相关性,污染来源主要为工业源、燃煤源、道路尘等,共占载荷为83.90%。本地累积型污染过程中,PM_(1.0)与PM_(2.5)、SO_4~(2-)、Ba和Cu等呈现出较好相关性,污染来源主要为烟花爆竹与二次生成,共占载荷为87.94%。     

贵州省旱田土壤N2O释放及其环境影响因素

以贵州省的玉米-油菜轮作田、大豆-冬小麦轮作和休耕地为研究对象,采用密闭箱-气相色谱法,对整个轮作期的土壤N2O释放进行观测,初步研究我国亚热带旱田的N2O释放特征.实验研究结果表明,3试验田N2O释放通量具有相同的规律性日变化形式,秋收作物达通量极大值的时间比越冬作物滞后2h～3h,气温是控制N2O通量日变化的主要环境因子:3试验田N2O释放通量(以N2O中的N计)分别在9.81～433.11,4.00～180.41和9.74～282.00μg·m-2·h-1,高于我国水田和北方旱田的N2O释放通量;进一步分析表明,3试验田N2O释放通量具有相同的季节变化模式,N2O释放峰受降雨事件的直接影响,N2O通量与降雨量和土壤湿度间有显著的正相关性,而与温度的关系不明显.     

甲烷排放源逆向轨迹反演模式研究

基于逆向轨迹计算和单点浓度连续观测资料建立了一个甲烷排放源的反演模式 .经系统调试表明模式具有正确反映边界层物理过程的能力 .在理想条件下 ,模式相当准确地反演出 1 0 0km水平范围内设定的排放源和分布 .用 9天的实际甲烷浓度连续观测资料对北京地区的排放源情况进行个例计算 ,获得主要源块的排放率在0 0 0 66～ 0 0 2 6mg/ (m2 ·s)范围内 ,与区域内的重要排放源 (稻田 )的排放情况相一致 .反演所得源块与区域内的稻田分布亦有一定的空间对应关系     

Effects of elevated atmospheric CO2 concentration and temperature on the soil profile methane distribution and diffusion in rice-wheat rotation system

The aim of this experiment was to determine the impacts of climate change on soil profile concentrations and diffusion effluxes of methane in a rice–wheat annual rotation ecosystem in Southeastern China. We initiated a field experiment with four treatments:ambient conditions(CKs), CO_2 concentration elevated to ~ 500 μmol/mol(FACE),temperature elevated by ca. 2°C(T) and combined elevation of CO_2 concentration and temperature(FACE + T). A multilevel sampling probe was designed to collect the soil gas at four different depths, namely, 7 cm, 15 cm, 30 cm and 50 cm. Methane concentrations were higher during the rice season and decreased with depth, while lower during the wheat season and increased with depth. Compared to CK, mean methane concentration was increased by 42%, 57% and 71% under the FACE, FACE + T and T treatments, respectively, at the 7 cm depth during the rice season(p 0.05). Mean methane diffusion effluxes to the 7 cm depth were positive in the rice season and negative in the wheat season, resulting in the paddy field being a source and weak sink, respectively. Moreover, mean methane diffusion effluxes in the rice season were 0.94, 1.19 and 1.42 mg C/(m~2·hr) in the FACE,FACE + T and T treatments, respectively, being clearly higher than that in the CK. The results indicated that elevated atmospheric CO_2 concentration and temperature could significantly increase soil profile methane concentrations and their effluxes from a rice–wheat field annual rotation ecosystem(p 0.05).     

Sequestration of maize crop straw C in different soils: role of oxyhydrates in chemical binding and stabilization as recalcitrance

While biophysical controls on the sequestration capacity of soils have been well addressed with physical protection, chemical binding and stabilization processes as well as microbial community changes, the role of chemical binding and stabilization has not yet well characterized for soil organic carbon (SOC) sequestration in rice paddies. In this study, a 6-month laboratory incubation with and without maize straw amendment (MSA) was conducted using topsoil samples from soils with different clay mineralogy and free oxy-hydrate contents collected across Southern China. The increase in SOC under MSA was found coincident with that in Fe- and Al-bound OC (Fe/Al-OC) after incubation for 30 d (R(2)=0.90, P=0.05), and with sodium dithionate-citrate-bicarbonate (DCB) extractable Fe after incubation for 180 d (R(2)=0.99, P<0.01). The increase in SOC under MSA was found higher in soils rich in DCB extractable Fe than those poor in DCB extractable Fe. The greater SOC sequestration in soils rich in DCB extractable Fe was further supported by the higher abundance of (13)C which was a natural signature of MSA. Moreover, a weak positive correlation of the increased SOC under MSA with the increased humin (R(2)=0.87, P=0.06) observed after incubation for 180 d may indicate a chemical stabilization of sequestered SOC as humin in the long run. These results improved our understanding of SOC sequestration in China's rice paddies that involves an initial chemical binding of amended C and a final stabilization as recalcitrant C of humin.     

农业气象灾害分析网络服务系统

以大量翔实的农业气象灾害资料为基础,结合实时农业气象灾情分析,在ｗｉｎｄｏｗｓＮＴＳｅｒｖｅｒ网络环境下,研制出具有网络功能的农业气象灾害分析服务系统,系统在Ｉｎｔｅｒｎｅｔ的ＮｅｔｓｃａｐｅＮａｖｉｇａｔｏｒ或Ｅｘｐｌｏｒｅｒｔｏ览器下运行,简便实用．系统以灾害服务为宗旨,体现了信息量大、服务迅速的特点。内容包括农业气象灾害类型库、逐年农业气象灾害评判库、实时农业气象灾害分析及灾情服务流程．     

“安全公正空间”框架在区域环境管理中的应用——以太白湖流域为例

近年兴起的“安全公正空间”（Safe and Just Operating Space）理论框架突出了环境安全上限,兼顾了社会发展主要指标的达成度,对区域环境安全和社会可持续发展具有重要意义。选择长江中下游太白湖这一典型湖泊流域,整合周边县市社会调查数据及过去近150余年来的沉积记录（包括地球化学、孢粉、硅藻等多指标）,分别从环境安全及社会基础两个方面,构建了该流域社会-生态系统安全公正空间。结果显示：目前,流域内水质、空气质量、耕地面积和水土保持这4个指标超越了环境上限,处于危险状态;清洁能源、产业创新的社会基础完成度相对较低。该框架有助于流域系统的管理和决策,同时也有利于公众理解环境上限和社会基础之间交互复杂的关系。本研究亦展示了多源环境数据,特别是古湖沼学记录,能为区域生态环境管理提供重要的长期背景资料。     

Study of Asian Dust Phenomena in 2001–2003 Using A Network of Continuously Operated Polarization Lidars

We have conducted dust observations at a number of locations including Beijing, Hefei, Suwon, Fukue, Nagasaki, Tsukuba, and Sapporo using automated two-wavelength polarization lidars o study Asian dust phenomena, including generation, transport, and change during transport. We developed a method using the depolarization ratio for estimating the contributions of Asian dust and spherical air-pollution aerosols in observed aerosol mixtures. We analyzed the dust profiles statistically to derive climatological characteristics and year-on-year variations. We also studied dust source and transport path for each dust event using the regional chemical transport model CFORS. The statistical analysis clearly demonstrated the year-on-year variation of dust phenomena and the characteristics depending on the locations of the observational sites. Most major dust events in 2001 and 2002 originated in Inner Mongolia and/or Mongolia at the southern edge of a low-pressure area located in Siberia and were transported by strong westerlies. In 2003, the typical meteorological pattern for heavy dust cases accompanying a strong low in Siberia was not seen, except for one case in April. Furthermore, the lidar observation in Beijing suggests that less dust was generated in the source regions in Inner Mongolia and/or Mongolia, probably due to higher precipitation in 2003.     

Effect of long-term fertilization on C mineralization and production of CH4 and CO2 under anaerobic incubation from bulk samples and particle size fractions of a typical paddy soil

Impacts of nutrient management on C mineralization and greenhouse gas (GHGs) emission from soils have been of much concern in global change. Using laboratory incubation, the production of CH₄ and CO₂ were studied from both bulk samples and the particle size fractions (PSF) of topsoil from a paddy under a long-term different fertilization trial (including non (NF), chemical without (CF) and with manure (CFM) fertilization, respectively) in the Tai Lake Region, China. Four PSFs (2000–200, 200–20, 20–2, <2 μm) were separated from undisturbed samples collected after rice harvest by a low-energy ultrasonic dispersion procedure. Both the bulk samples and PSFs were incubated under submerged condition for 72 days. The concentration of CH₄ and CO₂ evolved during incubation were determined by gas chromatography. C mineralization rates ranged from 0.13 to 0.52 mg C g⁻¹ C day⁻¹, with different fertilizations and size of the PSFs, and were not correlated with C/N ratio. While CO₂ production predominated over CH₄ from C mineralization from both bulk samples and the size fractions, CH₄ production played a predominant role in the total global warming potential (GWP) under all treatments. C mineralization of bulk soil was significantly higher under CF than under CFM and NF. CH₄ production, however, was 3 times as under CFM and 27 times as under NF, indicating a tremendous effect of chemical fertilization alone on the total GWP. CO₂ production from the PSFs differed from CH₄ under a single treatment, which was notably from the coarse PSFs larger than 200 μm. Higher C mineralization and CH₄ production with a higher metabolic quotient under CF implicated a vulnerability of soil functioning of GHGs mitigation in the paddy receiving chemical fertilizers only. Thus, rational organic amendments should be undertaken for mitigating the climate change.