珠穆朗玛峰地区近200年冰芯草酸根记录及其环境意义

 1997年5月中美联合珠峰地区绒布冰川考察期间，在远东绒布冰川海拔6500m北支冰流粒雪盆内钻取到一支41m长冰芯.该冰芯定年至1814年．远东绒布冰芯中近200年来草酸根浓度变化与Ca²⁺和NH₄浓度变化一致性较差，表明草酸根的来源有别于大气尘埃和生物来源．草酸根浓度与冰芯中气温指标δ¹⁸O的变化具有一致性,说明气温是影响大气中草酸根浓度变化的因素之一，但非主导因素.远东绒布冰芯记录的20世纪以来草酸根浓度的迅速升高反映了人类工业活动对大气环境的污染．20世纪50～80年代，大气中受人类工业活动污染的草酸根浓度约为19世纪自然本底值的3倍，其中60年代人类活动排放的草酸盐类对大气的污染最为严重.     

铸造泥芯废气的治理

通过对铸造泥芯废气排放特性的分析 ,采用自行设计的冷凝水洗处理系统 ,废气治理效果明显 ,达到了国家排放标准。该法可供参考借鉴     

测震数字化观测系统前台机维护的研究

随着地震台站数字化和计算机网络技术的使用,对地震台数字化系统的维护提出了更高的要求。而数字化观测系统前台机的正常与否是整个数字化的核心,前台机的安全和维护工作的成败直接影响数字资料的质量和产出。本文针对在实际工作中所遇到的各种问题,结合地震台的实际情况,归纳和总结了一些方法和见解,提出一些切合实际的解决方法,希望对兄弟台站测震数字化系统的维护有所帮助。     

镉、铅在玉米幼苗中的积累和迁移--X射线显微分析

用扫描电镜-X射线能谱仪及原子吸收分光光度计,测定经不同浓度镉、铅处理的玉米根、叶中镉、铅的积累。结果表明,铅的积累为皮层>中柱;木质部薄壁组织>导管。镉则相反。铅主要以非共质体途径在根内横向迁移,镉主要以共质体途径在根内横向迁移。原于吸收分光光度计测定表明,镉、铅主要在玉米根内沉积,镉铅复合作用促进了玉米根叶对镉、铅的吸收,镉比铅更易为玉米吸收且更易从根向叶迁移。     

渤海湾及其邻近河口区重金属环境背景值和污染历史

用长箱式静压取样器和挖探槽采集了渤海湾及毗邻河口区11个沉积物岩芯样.结合~(210)Pb测年、沉积物重金属分析,测定了沉积速率、重金属环境背景值及渤海湾4个时期(1983,1974,1964,1933年)Cu、Pb、Zn、Cd的人为增量部分.研究表明,测区沉积速率范围为1.8—44.2mm/a.高速沉积区位于蓟运河口、海河口及废黄河口;低速率区位于湾中部.Cu、Pb、Zn、Cd环境背景值分别为24.80—25.63mg/L、15.96—16.55mg/L、72.58—74.61mg/L和0.10—0.12mg/L.经重金属沉积通量计算,人为排放最大负荷量分别为:Cu,73.75t(1964年);Pb,64.57t(1974年);Zn,249.32t(1983年);Cd,5.77t(1983年).     

锰细菌在加拿大海盆、楚科奇海沉积物中的分布

用平板法分别在4℃和25℃时对北极加拿大海盆和楚科奇海10个沉积物岩芯中的锰细菌进行培养,并测定了检出率和含量.分析结果表明,4℃与25cc温度下培养的锰细菌含量范围均为(-)～3.3×108个g-1,锰细菌平均检出率分别为77.78%、86.03%.平均含量分别为5.60×106、7.91×106个g-1;该结果高于太平洋深海沉积物中的锰细菌含量,比北极阿拉斯加淡水湖湖水中的锰细菌含量高1个数量级,比印度洋海岭Carlsberg Ridge区热水区海水样品中的锰细菌含量高3个数量级,证实寒冷北极海同样广布锰细菌.对锰细菌在不同水深、经纬度以及沉积物深度中的分布进行了讨论;结果表明,锰细菌检出率随沉积物深度的增加而增大.含量变化呈现浅层少、下层多之势;纬度分布范围较大,并显出有扩大的趋势.水深对沉积物中锰细菌也有一定影响.尽管锰细菌对温度有较强的适应能力,环境温度的升降对本研究区锰细菌具有双重作用.     

城市雾天单个矿物颗粒物理和化学特征

应用场发射扫描电镜(FESEM)和带能谱的扫描电镜(SEM-EDX)对北京冬季雾天和正常天气下收集的4个样品进行研究.雾天中矿物颗粒的数量-粒度分布的峰值出现在0.1～0.3 μm和1～2.5 μm之间,并且发现雾天出现的二次矿物颗粒的数量百分含量(4.67%)高于正常天气条件(0.12%).单个矿物颗粒的EDX能谱显示,雾天和正常天气中单个矿物颗粒的主要化学成分有一定的差别,尤其是S元素.矿物颗粒分为9种不同类型:"富Si"、"富Ca"、"富S"、"富Fe""富Mg"、"富Al"、"富Ti"、"富K"和"富Cl",其中雾天"富Ca"中55%的颗粒含有Ca(50%±1.2%)和S(37%±1.6%),"富S"中72%的颗粒含有S(44%±1.5%)和Ca(33%±2%),说明了雾天中绝大部富集S的颗粒物中同时富集Ca,这在一定程度上说明了北京市大气中这些含Ca的碱性矿物对雾水酸性有一定的缓冲作用.雾天样品中S/Ca的平均比值为6.11,如果以冬季正常天气条件下S/Ca的均值0.73为背景值,雾天中S/Ca的比值是冬季正常天气的8倍,可见雾天中颗粒物表面的硫化现象相当严重,同时也显示出雾天SO2向硫酸盐的转化率比较高.     

Historical trends of PCBs and PBDEs as reconstructed in a lake sediment from southern Tibetan Plateau

High-altitude lake sediment can be used as a natural archive to reconstruct the history of pollutants. In this work, the temporal distribution of polychlorinated biphenyls (PCBs) and polybrominated diphenyl ethers (PBDEs) were determined using a high-resolution gas chromatography coupled with high-resolution mass spectrometer (HRGC/HRMS) in an alpine lake sediment core collected from the southern Tibetan Plateau (TP) to examine whether the expected decreasing trends due to the implementation of the international Conventions could be observed. The concentrations of PCBs and PBDEs in the sediment core were in the range of 11.8–142 pg/g dw and ND-457 pg/g dw, and their fluxes were in the range of 2.51–31.7 ng/(m²·yr) and ND-43.2 ng/(m²·yr), respectively. The prevalence of low-chlorinated (tri-CB) PCBs and low-brominated (tri- to tetra-) PBDEs in most sections of the sediment profiles was observed, suggesting that the light molecular weight PCBs and PBDEs have most likely reached lake sediments by long-range atmospheric transport from distant sources. Despite the restrictions on their applications, the sediment records for the concentrations and fluxes showed no corresponding decreasing trend with restrictions for PCBs, which suggested that these POPs (e.g., PCBs) were still emitted to the environment owing to the influence of primary or secondary emissions. To our knowledge, this is the first report on input history of atmospheric PCBs and PBDEs recorded in TP Lake sediment.     

云南稻核心种质苗期耐冷性及其地理生态差异

采用Nagamine等(1991)法研究了598份云南稻核心种质在稻作区划间、地州间苗期耐冷性强弱、变异程度及其地理生态差异。结果表明,稻作区划间苗期耐冷强弱差异较大,平均耐冷级别为:I(4.70)>II(4.78)>V(4.79)>III(5.34)>IV(5.36),40份强耐冷种质频率为II(45%)>I(25%)>III(22.5%)>V(5.0%)>IV(2.5%),其变异系数为II(32.22%)>I(31.28%)>V(29.65%)>III(19.66%)>IV(19.59%);揭示了苗期耐冷性与低温胁迫下水稻冬春育秧、冷泉水密切相关,其耐冷基因源是云南南部地区冬季育秧和滇中一带苗期倒春寒长期协同进化的结果;苗期耐冷种质广泛存在于热带、亚热带和温带地区,品种间苗期耐冷差异也明显。云南稻核心种质16个地州平均苗期耐冷强弱差异较大。根据气候、生态、云南稻种多样性及其苗期耐冷性等将云南稻作区划分为重冷害多样性贫乏区、冷害多样性中区和轻冷害区三部分。其中,曲靖、大理、楚雄、昆明和丽江5个地州平均耐冷级别3.65~4.32,0—2级苗期强耐冷种质占27.5%(2.5%~10%)和高海拔冷泉水苗期灌溉,属于重冷害多样性贫乏区;文山、红河、思茅、保山、德宏和临沧6个地州平均耐冷级别4.45~5.40,0—2级苗期耐冷种质占70%(5%~30%)和冬春育秧,属于冷害多样性中区;怒江、玉溪、昭通、迪庆和西双版纳5个地州平均耐冷级别5.05~5.87,0—2级苗期耐冷种质占2.5%(0~2.5%),属于轻冷害多样性扩散区。水稻冬春育秧和高海拔冷泉水灌溉在云南稻核心种质苗期耐冷基因源演化中起了重要作用。     

Use of Water Clarity to Monitor the Effects of Climate Change and other Stressors on Oligotrophic Lakes

We present evidence from studies oflakes in Killarney Park, Ontario, Canada that waterclarity is a key variable for monitoring theeffects of climate change, high UV exposure andacidification. In small oligotrophic lakes, thesestressors affect water clarity primarily byaltering the concentration of DOC in lake water. Clear lakes (<2 mg L^-1 DOC) proved to be highlysensitive indicators of stressors, exhibiting largethermal and optical responses to small changes inDOC. Extremely clear (<0.5 mg L^-1 DOC) acidic lakesshowed the effects of climate change and solarbleaching in recent decades. These lakes becamemuch clearer even though they were slowlyrecovering from acidification.