模拟氮沉降对大豆萌发和幼苗生长的影响

氮沉降是当今倍受关注的全球性环境问题.采用大田试验和室内培养的方法,研究大豆种子萌发和幼苗生长对氮沉降的响应.实验设4组处理(CK、T1、T2、T3),所施氮肥为NH4NO3,在室内培养实验中,4组处理的浓度分别为0、0.08、0.16、0.24mol/L.大田实验中,4组处理的氮施入量分别为0,50,100,150 kg·hm-2·a-1.结果表明:过量氮沉降对种子萌发有一定的抑制作用,降低了种子的发芽速度和发芽率;抑制了幼苗的生长速度,降低了植株的株高、叶面积和生物量,并减小了根冠比;随着氮施入量的增加幼苗的蒸腾速率逐渐降低,但叶片叶绿素含量逐渐增加.     

天津蓟运河故道消落带土壤种子库特征与土壤理化性质分析

为确定蓟运河故道消落带土壤种子库特征与土壤理化性质之间的关系,开展土壤萌发试验并测定了土壤理化性质. 结果表明:①土壤物种呈3个聚类组,聚类组1分布在土壤含水率为50%~100%、w(全盐)为0.8~1.4 g/kg的区域,聚类组2分布在土壤含水率为40%~50%、w(全盐)为0.4~0.8 g/kg的区域,聚类组3分布在土壤含水率为25%~40%、w(全盐)为0.2~0.4 g/kg的区域;②土壤w(有机质)、w(全盐)和含水率对土壤种子库物种的分布影响较大,而w(速效K)、w(速效N)、w(速效P)和pH对其影响不大;③随着土壤w(全盐)、含水率的增加及w(有机质)的减少,土壤种子库物种中一年生植物所占比例呈增加趋势,二年生植物比例先减少后增加,多年生植物比例先增加后减少;④随着土壤w(全盐)、含水率的增加以及w(有机质)的减少,消落带土壤种子库的Shannon-Wiener指数和Margalef丰富度指数呈下降趋势,而生态优势度和Pielou均匀度指数随着水位的降低有增大的趋势. 研究得出天津蓟运河故道消落带土壤种子库特征与土壤理化性质有重要关系,适当地进行人为管理和调控对土壤环境的改善及土壤种子库多样性增加有积极作用.      

Effects of seed aerosols on the growth of secondary organic aerosols from the photooxidation of toluene

Hydroxyl radical （.OH）-initiated photooxidation reaction of toluene was carried out in a self-made smog chamber. Four individual seed aerosols such as ammonium sulfate, ammonium nitrate, sodium silicate and calcium chloride, were introduced into the chamber to assess their influence on the growth of secondary organic aerosols （SOA）. It was found that the low concentration of seed aerosols might lead to high concentration of SOA particles. Seed aerosols would promote rates of SOA formation at the start of the reaction and inhibit its formation rate with prolonging the reaction time. In the case of ca. 9000 pt/cm^3 seed aerosol load, the addition of sodium silicate induced a same effect on the SOA formation as ammonium nitrate. The influence of the four individual seed aerosols on the generation of SOA decreased in the order of calcium chloride〉sodium silicate and ammonium nitrate〉ammonium sulfate.     

Second organic aerosol formation from the ozonolysis of -pinene in the presence of dry submicron ammonium sulfate aerosol

An indoor chamber facility is described for investigation of atmospheric aerosol chemistry. Two sets of α-pinene ozonolysisexperiments were conducted in the presence of dry ammonium sulfate seed particle: ozone limited experiments and α-pinene limitedexperiments. The concentration of gas phase and particle phase species was monitored continuously by on-line instruments andrecorded automatically by data sampling system. The evolution of size distribution was measured by a scanning mobility particlesizer (SMPS), and α-pinene consumed was measured using GC-FID. Secondary organic aerosol (SOA) produced for seed-free systemis 100% organic in content, resulting from a sufficient supersaturation of low volatility organics to produce homogeneous nucleationfollowed by condensation to the aerosol. Secondary organic aerosol produced in seeded system is a mixture of organic and inorganicconstituents, initially forms via condensation onto the inorganic particles, and subsequent growth occurs via absorption into the organicsurface coating the inorganic core. Although the formation process and the size distribution for seed-free system and seeded system isdifferent, the ultimate mass of SOA formed is equal, and SOA yield for the two system located in the same regression line when usingone-product model, suggesting that the presence of dry ammonium sulfate seed has no measurable effect on the total aerosol yield, and the dry seed particle acts solely as a site upon which organic deposition occurs.     

土霉素对小麦种子发芽与幼苗生长发育的生态毒性

研究了土霉素对小麦种子发芽以及早期幼苗生长发育的生态毒性效应.结果表明,土霉素对小麦种子芽长及根长的抑制效应显著(p<0.01),而且它们之间具有良好的剂量-效应关系.根据线性回归方程得出土霉素对小麦种子芽长和根长的半抑制浓度为65.5 mg/L和34.7 mg/L.然而,土霉素对小麦种子的发芽率并没有显著的影响.研究还表明,0.15~2.4 mg/L土霉素暴露21 d后,小麦叶片中的叶绿素含量降低了35.6%~47.3%,叶片及根部的可溶性蛋白含量也均呈显著下降趋势.暴露7 d后,0.15~2.4 mg/L土霉素对小麦叶片和根部SOD与POD活性的抑制效应不显著,但随着暴露时间的延长,土霉素对小麦的SOD与POD酶活性抑制率显著下降;2.4 mg/L土霉素暴露21 d后,小麦根部的SOD活性下降72.3%,说明土霉素对小麦幼苗体内的抗氧化系统具有破坏作用.该实验结果显示,低浓度土霉素长期暴露对小麦幼苗的生长发育具有不良的生态毒性效应.     

Effect of seed sludge on characteristics and microbial community of aerobic granular sludge

Aerobic granular sludge was cultivated by using different kinds of seed sludge in sequencing batch airlift reactor.The influence of seed sludge on physical and chemical properties of granular sludge was studied;the microbial community structure was probed by using scanning electron microscope and polymerase chain reaction-denaturing gradient gel electrophoresis(PCR-DGGE).The results showed that seed sludge played an important role on the formation of aerobic granules.Seed sludge taken from beer wastewater treatment plant(inoculum A) was more suitable for cultivating aerobic granules than that of sludge from municipal wastewater treatment plant(inoculum B).Cultivated with inoculum A, large amount of mature granules formed after 35 days operation, its SVI reached 32.75 mL/g, and SOUR of granular sludge was beyond 1.10 mg/(g·min).By contrast, it needed 56 days obtaining mature granules using inoculum B.DGGE profiles indicated that the dominant microbial species in mature granules were 18 and 11 OTU when inoculum A and B were respectively employed as seed sludge.The sequencing results suggested that dominant species in mature granules cultivated by inoculum A were Paracoccus sp., Devosia hwasunensi, Pseudoxanthomonas sp., while the dominant species were Lactococcus raffinolactis and Pseudomonas sp.in granules developed from inoculum B.     

氯化钙种子气溶胶对甲苯二次有机气溶胶与氨形成含氮有机物的影响

苯系物光氧化反应形成的二次有机气溶胶(SOA)是大气细粒子的重要组成部分.SOA羧酸和二元醛组分能与氨反应形成有机酸铵和咪唑类含氮有机物,它们能够吸收205 nm和270 nm的紫外辐射,是棕色碳的主要组分.氯化钙等无机种子气溶胶具有较大的比表面积,可为气相羰基化合物和氨提供凝结与反应载体,从而影响含氮有机物的形成.基于此,本文利用烟雾腔研究氯化钙种子气溶胶存在时甲苯SOA与氨的反应,采用紫外-可见分光光度计测量产物溶液在205 nm和270 nm处的吸光度,并定性研究不同浓度、湿度和酸度的氯化钙种子气溶胶对含氮有机物形成的影响.结果表明:氯化钙种子气溶胶能够促进甲苯SOA含氮有机物的形成;含氮有机物的生成浓度随着氯化钙种子气溶胶浓度和pH值的增加而逐渐增大.但当氯化钙种子气溶胶为碱性时,OH~-会与凝结的有机酸发生酸碱中和反应并抑制二元醛化合物水合形成四醇产物,从而不利于含氮有机物的生成;水分子的增加占据了氯化钙种子气溶胶表面的吸附活性位点,氨被吸附和凝结的量减少,从而导致含氮有机物的生成浓度随着相对湿度的增大而降低.本研究可为人为源SOA棕色碳的形成机制和化学组成研究提供实验依据.     

土壤种子库研究的几个热点问题

土壤种子库是指存在于土壤表层凋落物和土壤中全部活性种子的总和。土壤中有活性的种子是植物群落的一部分,是新植株的来源。土壤种子库可以分为瞬时土壤种子库和持久土壤种子库。随着群落生态学的发展,土壤种子库的研究已经成为植物生态学重要的一部分,研究内容主要包括:(1)土壤种子库的组成和分布;(2)土壤种子库的动态;(3)地上植被与土壤种子库的关系;(4)干扰对土壤种子库的作用;(5)土壤种子库在生态恢复中的作用。文章在对目前土壤种子库的研究方法、主要研究内容方面总结的基础上,认为土壤种子库在合适的干扰作用下对退化生态系统的恢复以及植被更新发挥重要的作用,同时需进一步加强对这一过程中种子萌发、幼苗建立限制因素的研究。     

4个岷江柏种群的球果和种子形态特征及其地理空间差异

研究了我国四川和甘肃地区特有珍稀濒危植物岷江柏(Cupressus chenggiana S.Y.Hu)的4个地理种群球果和种子的形态特征，分析了不同生境条件下岷江柏的地理差异．结果表明：岷江柏球果呈椭球形，长(l)为1．5～2．5cm，宽(6)为1．5～2．0cm，重(m)为1．5～4．5g，球果鳞片数为8～11片，球果内种子粒数为40～70粒．在调查的4个岷江柏种群中，小金县种群的球果最大、球果内种子数最多，马尔康县种群和金川县种群的球果重量、球果内种子数居中，理县种群的球果最小、球果内种子数最少．讨论认为，4个种群球果和种子大小特征存在极显著差异，不同种群球果和种子的形态差异与岷江柏的种群遗传特征、气候特征和生境特征有着密切的关系．图3表7参25     

濒危植物疏花水柏枝种子萌发的生态学特性

疏花水柏枝Myricaria laxiflora分布于我国三峡从宜昌至重庆段长江干流的消落带,分布区十分狭小.三峡工程兴建后,疏花水柏枝将失去绝大部分的生境而成为濒危物种.通过设置一系列控制实验测试了土壤水质量分数,温度和土壤类型对疏花水柏枝种子萌发的生态学的影响.实验结果表明,土壤水质量分数、温度和土壤类型对种子萌发率都有显著影响.其中种子萌发率随土壤水质量分数增加而增大,土壤水质量分数达到饱和程度时萌发率达到最大值;高温条件下的种子萌发率高于低温,种子萌发率在21～27℃达到最大值;种子在河沙基质上萌发好于在沙土基质上.结合分布区萌发季节的环境条件分析,土壤水质量分数是限制该物种分布于消落带的关键作用因子.据此就该物种的种群保护与重建提出了一些建议.