Nitrogen availability in relation to vegetation changes resulting from grass encroachment in Dutch dry dunes

The encroachment of some tall grass species in open dune vegetation, as observed in a Dutch dry dune area, is considered unfavourable from a conservation viewpoint. This paper investigates differences in vegetation and soil properties between grass-dominated and still existing open dune grassland plots at four locations along the coast. Soil properties studied include nitrogen and phosphorus pools and nitrogen availability by mineralization. Vegetation properties included are above and below-ground biomass and nitrogen and phosphorus concentrations in above-ground biomass. Systematic differences in N-pools between grass-dominated and open dune grassland plots were not observed. However, N-availability by mineralization and its turnover rates are higher in grass-dominated plots than in open dune grassland plots, as well as above and below-ground biomass. In open dune grassland plots, atmospheric N-input is an important source of N, whereas in grass-dominated plots mineralization largely exceeds atmospheric N-input. However, these observations do not explain the mosaic-like vegetation pattern. Grazing intensity is most likely the determinant factor in the dry dune system. It is concluded, that grass encroachment is probably triggered by atmospheric deposition and is enhanced by positive feedbacks in the N-cycle. The relevance of these results for restoration management is briefly discussed.     

松胞素B对人血淋巴细胞和CHL细胞微核率的影响

研究了不同浓度的松胞素Ｂ对人血淋巴细胞和中国仓鼠肺成纤维细胞（ＣＨＬ）分裂吉周期和微核率的影响。结果表明,松胞素Ｂ浓度增高过高能引起细胞微核率增高。在本研究中,对ＣＨＬ细胞微核率试验以３μｇ／ｍＬ松胞素Ｂ较适合;而对人血淋巴细胞微核试验,松胞素Ｂ浓度以２－４μｇ／ｍＬ为宜,松胞表Ｂ浓度过高会提高微核背景值,降低试验的灵敏度和精确性。     

人地协同论：可持续发展模型构建的基础

人地协同论是在陆地系统科学、非线性系统理论基础上建立起来的关于可持续发展的一个数理模型,它以社会与自然的交互作用、交界面性质及其演化规律为研究对象。本文根据系统生态学理论,提出了关于可持续生存的数学定义。     

Variations of denitrification in a farming catchment area

We measured denitrification at 15 sites during 1 year in a agricultural catchment in Brittany, France. Our objective was to assess the relative importance of heterotrophic denitrification on the fate of excess nitrogen at the catchment scale, and to quantify the relative importance of riparian areas on the N₂O emissions. Using the C₂H₂ inhibition technique, denitrification rate on soil core and denitrifying enzyme activity (DEA) were each determined, for samples taken from two soil layers: 0–20 and 20–40 cm. Denitrification rates, ranging from 0 to 417 mg N m⁻² d⁻¹, were significantly higher in riparian areas than for hillslopes (median of 24.87 against 10.38 mg N m⁻² d⁻¹). However, since denitrification rates are significant in the hillslope and given that hillslope surface area is much greater (79% of catchment surface), this domain could be responsible for half of the overall denitrified nitrogen (N). Also, the 20–40 cm deep soil layer was found to account for more than 46% of the denitrification. The DEA indicates the potential for denitrifying activity by the soil under non-limiting conditions, measured values ranged from 76.48 to 530.63 ng N g⁻¹ dry soil h⁻¹. The ratio N₂O/(N₂O + N₂) was about 60% with no clear spatial or temporal trends. Soil moisture appeared to be the main limiting factor for denitrification at the field scale. The results suggest that, for this catchment, denitrification is a major route for nitrogen removal, but a significant proportion of this removal occurs as N₂O.     

沈阳张士污灌区镉循环的分室模型与污染防治对策研究

对沈阳张土污灌区大气、水、土壤和生物各分室中Ｃｄ的库存量和各分室间Ｃｄ的循环通量进行了研究，建立了土壤水稻系统中Ｃｄ流分室模型，该模型表明，Ⅱ闸和Ⅲ闸地区土壤分室中Ｃｄ的库存增量均为正值。可见，该污灌区近年来Ｃｄ污染程度由于污水灌溉仍然处于加剧的趋势，研究最后指出，该污灌区Ｃｄ的污染防治对策主要是减少污水灌溉量、进一步降低灌溉水中Ｃｄ的浓度和通过富Ｃｄ的下降速率分别依次达到２９．４９和２２．８１ｍ     

施加磷元素后对小麦抗重金属铜毒性的影响

将小麦幼苗放在含有不同浓度磷元素（1 mmol/L和10 mmol/L）和铜元素（0.16μmol/L、100μmol/L和1 mmol/L）的培养液中处理12 h后,观察植物体内铜元素的含量、叶绿素含量、抗坏血酸循环的变化.结果表明,当培养液中施加的铜元素浓度相同时,施加较高浓度的磷（10 mmol/L）能促进植物根部吸收和积累铜,并能促进铜元素从根部向地上部的运输.此外,实验结果还表明,当培养液中都含有较少量的铜（0.16μmol/L）元素时,比较磷浓度对植物体内生理反应的影响时,发现在含有高浓度磷的培养液中培养的小麦体内的受到较少的膜质过氧化损伤,光合色素的含量保持稳定.但是,当培养液中有较高浓度的铜元素（100μmol/L和1 mmol/L）时,施加高浓度的磷反而加剧了植物体内的膜质过氧化损伤和引起光合色素的分解,从而不利于植物正常的生长发育.     

挥发性有机硫化合物释放的研究与展望

在介绍硫的生物地球化学循环的基础上，概述了几种挥发性有机硫气体ＤＭＳ，ＣＯＳ，ＭＳＨ，ＣＳ２和ＤＭＤＳ从各种自然源（主要是生物源）释放的情况，着重阐述了陆地生态系统中各种生物硫源的释放情况，列举了测定这些释放的硫通量的方法，并且对有机硫气体的大气行为及环境影响也作了论述。     

河流湿地氮循环修复过程中的新型功能微生物

自然生态系统中厌氧氨氧化菌和氨氧化古菌的发现,改变了人们对传统氮循环过程的认识.通过氨氧化古菌和厌氧氨氧化菌在缺氧/厌氧的条件下完成硝化反应和封闭的氮循环,对于河流氮循环生态修复意义显著.通过PCR聚合酶链反应结合水体沉积物理化指标,研究典型河流湿地中厌氧氨氧化菌和氨氧化古菌及其在循环中的作用.结果表明,在海河支流北运河湿地中存在厌氧氨氧化菌和氨氧化古菌,它们对于水体和底泥沉积物的氮转化有较重要作用.通过构建16S rRNA克隆文库生物多样性分析比较,发现湿地中厌氧氨氧化菌的生物多样性相对较低,96个克隆序列只分为3个OTUs;其与基因库(GenBank)中已探明的厌氧氨氧化菌Candidatus"Kuenenia stuttgartiensis"和Candidatus"Brocadia fulgida"的相似度分别为98%和95%.通过建立氨氧化古菌克隆文库发现,96个克隆子共得到5个OTUs,其与GenBank中关系最近序列(土壤/沉积物中)的相似度均大于95%;对本实验样本和水相、土壤/沉积物相中不同氨氧化古菌进行进化谱系分析,发现北运河河流湿地的古菌amoA基因属于土壤/沉积物进化分支.     

好氧硝化颗粒污泥搁置后活性恢复研究

利用气提式内循环间歇反应器(SBAR)考察好氧硝化颗粒污泥搁置2个月后重新投入运行, 其物理性状和微生物活性的恢复情况. 结果表明, 搁置后颗粒由棕黄色转为灰黑色, 粒径及沉降速率无明显变化. 颗粒重新投入反应器, 2周后颜色基本恢复; 污泥浓度、颗粒粒径以及沉降速率迅速增加; 颗粒中异养菌活性在1 d内即可恢复至原水平的86％, COD去除活性5 d后完全恢复, 去除率稳定在80%以上. 活性恢复阶段采用较高的曝气量和较长的循环时间有利于硝化菌的活性恢复, 第41 d曝气量由0.05 m³·h^-1提高到0.10 m³·h^-1后, 亚硝酸菌和硝酸菌活性分别由原水平的88%和82%提高到122%和92%, 氨氮去除率由之前的80% ～ 90%迅速提高到96%以上; 第65 d循环时间由4 h延长至6 h使硝酸菌的活性得到了完全恢复.     

电路板环境应力筛选方法效能分析

论述了对设计、工艺成熟电路板组件的环境应力筛选方法,对比恒定高温、温度循环、温度冲击、振动及其组合筛选的筛选度,并进行效能比分析。通过对比各种应力对有较大共性的电路板组件筛选的分析,对GJB 1032进行适当裁减,提出了不少于10个温度循环加随机振动的筛选组合,以适应电路板板级筛选要求,提高效能比。