Cold season CH4, CO2 and N2O fluxes from freshwater marshes in northeast China

Cold season (winter and thaw) CH₄, CO₂ and N₂O fluxes from freshwater marshes (47°35′N, 133°31′E, Northeast China) were measured, using the static chamber method. The mean CH₄ and CO₂ fluxes from Carex lasiocarpa (Cl) were 0.5 ± 0.19 and 6.23 ± 1.36 mg C m⁻² h⁻¹, respectively, and those from Deyeuxia angustifoli (Da) were 0.18 ± 0.15 and 5.22 ± 2.48 mg C m⁻² h⁻¹, respectively in winter. There was no significant difference between Cl and Da (p > 0.05). The contributions of winter CH₄ fluxes were about 5.5% and 3% in the Cl and Da, respectively. Marshes are an important potential N₂O sink in winter season in northeast China. During thaw, the CH₄ and CO₂ emissions rapidly increased, 4.5–6 times of winter emissions. Wetland became a source of N₂O. Cold season gases flux from northern wetlands play an important role in the seasonal gas exchange.     

Cause of PM2.5 pollution during the 2016-2017 heating season in Beijing, Tianjin, and Langfang, China

To investigate the cause of fine particulate matter (particles with an aerodynamic diameter less than 2.5 µm, PM_2.5) pollution in the heating season in the North China Plain (specifically Beijing, Tianjin, and Langfang), water-soluble ions and carbonaceous components in PM_2.5 were simultaneously measured by online instruments with 1-hr resolution, from November 15, 2016 to March 15, 2017. The results showed extreme severity of PM_2.5 pollution on a regional scale. Secondary inorganic ions (SNA, i.e., NO₃^?+SO₄²+ NH₄⁺) dominated the water-soluble ions, accounting for 30%-40% of PM_2.5, while the total carbon (TC, i.e., OC + EC) contributed to 26.5%-30.1% of PM_2.5 in the three cities. SNA were mainly responsible for the increasing PM_2.5 pollution compared with organic matter (OM). NO₃^? was the most abundant species among water-soluble ions, but SO₄^2- played a much more important role in driving the elevated PM_2.5 concentrations. The relative humidity (RH) and its precursor SO₂ were the key factors affecting the formation of sulfate. Homogeneous reactions dominated the formation of nitrate which was mainly limited by HNO₃ in ammonia-rich conditions. Secondary formation and regional transport from the heavily polluted region promoted the growth of PM_2.5 concentrations in the formation stage of PM_2.5 pollution in Beijing and Langfang. Regional transport or local emissions, along with secondary formation, made great contributions to the PM_2.5 pollution in the evolution stage of PM_2.5 pollution in Beijing and Langfang. The favourable meteorological conditions and regional transport from a relatively clean region both favored the diffusion of pollutants in all three cities.     

青藏铁路三岔河特大桥空心薄壁高墩寒季混凝土施工技术

三岔河特大桥地处海拔高、干燥多风的恶劣气候区,是青藏铁路的咽喉工程,按总体部署须跨越寒季施工,依据高墩薄臂特点,优选拆装式大模板施工方法。该项技术采用试验研究、理论计算分析、现场监测分析等手段,使现场量测与设计数据、施工管理等工程信息相结合,并反馈于施工过程中。利用成熟度法对砼早期强度进行预测和估算,以确定下道工序的时间和对混凝土质量进行预测;采用双层保温层及内置供热系统形成高原高寒高墩薄臂负温混凝土保温加热养护技术;选用塔吊配合整体拼装式模板的高墩施工技术,成功解决空心薄臂高墩快速连续施工和寒季砼加热养护的难题,实现了高墩流水化、机械化作业。以温度为主线的信息化监控技术是该技术成果的创新内容,该创新成果对于高寒地区,尤其对青藏铁路、青藏公路桥梁下部结构施工具有广泛应用和借鉴价值。     

龙须草的施肥时期和施肥效果

针对提高纸浆原料植物龙须草的产量进行盆栽和田间施肥试验。结果表明；①龙须草的最佳施肥时期为营养生长旺盛期初期和春季萌发生长期；②对龙须草采用少量多次的施肥方法效果好；③龙须草施用氮肥的效果好，在施氮肥的基础上施磷肥效果显著。     

湖南汛期降水分区和变化规律的探讨

利用湖南５２站汛期降水资料,根据聚类分析方法,进行降水分区,结果共分为Ⅰ区,Ⅲ区（湘北）Ⅲ区（湘东）,Ⅳ区（湘中）和Ⅴ区（湘南）等５个区域,能反映地理位置和地形对降水的影响。然后,通过统计分析,讨论了各区域汛期降水的年际变化趋势,结果表明,Ⅱ区（湘北）汛期降水的年际变化最大;同时,根据各区域汛期降水的距平资料,探讨了它们的变化规律,结果显示,基本上都呈现出上升－下降－上升的特征,只有Ⅴ区（湘南）稍     

枯水期环太湖河流溶解态重金属空间分布

文章以环太湖53条出入湖河流为研究对象,测定2009年12月至2010年3月间(枯水季节)溶解态重金属含量,结果表明Mn、Ni、Cu、Zn、Cr、As等六种重金属溶解态浓度含量均较低,且未超标.将53条河流出入湖区域分为无锡常州区、宜兴区、湖州区、苏州区四个区域,无锡常州区除Cd外,其它重金属含量最高;Cd在宜兴区含量...     

河北与京津地区非采暖期大气中的PAHs污染特征

对河北与京津地区42个样点非采暖期大气中多环芳烃(Polycyclic Aromatic Hydrocarbons,PAHs)的研究表明,该区域大气中的PAHs浓度水平较高.2～3环PAHs主要分布在气相当中,颗粒相(大气可吸入颗粒物,PM10)中PAHs以4～6环为主.PAHs的高浓度样点在石家庄、唐山和邯郸地区分布最为集中.县城样点与城市样点的PM10和PAHs污染水平相近.临近区域广泛存在的大气污染很可能对北京市的大气环境造成影响.     

湖水冰封期营养盐及浮游植物的分布特征

研究了长春市南湖冰封期间,冰和水中营养盐、叶绿素a和藻类的浓度变化.实验结果表明:在冰层融化的季节(2月末～4月初),存在营养盐、叶绿素a和藻类首先被释放的现象;在最寒冷时期,营养盐、叶绿素a和藻类在冰的上层浓度较大;在冰封期(11月末～2月中旬),冰-水界面和水-底泥界面水中营养盐等的浓度变化较为缓慢,在1月份,营养盐、叶绿素a和藻类的浓度达到最低值.但是,在冰层融化的过程中,冰-水界面和水-底泥界面水中营养盐等的浓度迅速增大.     

重庆主城区流域邻苯二甲酸酯生态风险评价

以长江、嘉陵江重庆主城区段为研究水域,利用Agilent6890N气相色谱仪对丰水期该研究水域12个采样点水体中五种邻苯二甲酸酯（PAEs）含量进行测定,分析了PAEs在该区域水体中丰水期的分布特征并进行了生态安全评价。结果表明：丰水期水体中∑PAEs的浓度范围为0.87μg/L-55.66μg/L;DBP与DEHP为优先污染物,其浓度范围在0.15μg/L-28.32μg/L与0.26μg/L-26.29μg/L;按商值法对PAEs进行生态安全评价,DMP、DEP对该水域中水生动植物无生态风险,DBP和DEHP存在潜在低风险。     

水旱轮作稻田旱作季种植不同作物对CH4和N2O排放的影响

甲烷（CH4）和氧化亚氮（N2O）是仅次于二氧化碳（CO2）的重要温室气体,农田是大气CH4和N20的重要来源,但目前农业措施对CH4和N2O排放的影响尚不明确。以水旱轮作稻田旱作季休闲为对照,采用静态箱．气相色谱法研究了种植紫云英、黑麦草、冬小麦以及油菜等4种作物对稻田旱作季CH4和N2O排放及其温室效应的影响。结果表明：水旱轮作稻田旱作季CH4排放通量较低,而N2O排放较为明显。稻田旱作季CH4平均排放通量表现为油菜〉黑麦草〉冬小麦〉紫云英〉休闲,依次为8．96、7．19、6．94、6．52和6．02μg·m-2·h-1,季节N20平均排放通量的顺序是油菜（61．1lμg·m-2·h-1）〉冬小麦（52．5lag·m-2·h-1）〉黑麦草（34．0μg·m-2·h。）〉休闲（15.3lμg·m-2·h-1）〉紫云英（13．6lμg·m-2·h-1）。稻田旱作季种植不同作物对CH4和N2O季节总排放量的影响达到极显著水平（P〈0．01）,C144和N2O季节总排放量均以种植油菜为最大,分别达到43．2和294．7mg·m-2,比对照休闲增加49％和299％。种植油菜、冬小麦和黑麦草较对照休闲显著增加稻田旱作季总增温潜势（P〈0．05）,紫云英和休闲处理间总增温潜势无显著差异（P〉0．05）。研究表明,种植油菜、冬小麦和黑麦草等作物由于氮肥的施用增加了水旱轮作稻田旱作季温室效应。