1991—2004年东亚温室气体浓度特征及变化趋势

利用NOAA Earth System Research Laboratory提供的1991─2004年Tae-ahn(韩国),Ulaan Uul(蒙古)以及瓦里关(中国)的大气温室气体CO₂和CH₄的数据,对东亚地区大气温室气体的浓度特征及变化趋势进行研究.结果表明:14年来东亚地区大气中φ(CO₂)和φ(CH₄)月和年平均值总体呈明显上升趋势;3个监测站的φ(CO₂)年线性递增率比较接近,平均值为1.91×10-6a-1,季节变化较一致;从沿海到内陆这2种温室气体的浓度均随海拔升高而逐渐降低.      

Urban expansion and its contribution to the regional carbon emissions: Using the model based on the population density distribution

The method is used for calculating regional urban area dynamics and the resulting carbon emissions (from the land-conversion) for the period of 1980 till 2050 for the eight world regions. This approach is based on the fact that the spatial distribution of population density is close to the two-parametric Γ-distribution [Kendall, M.G., Stuart, A., 1958. The Advanced Theory of Statistics, vol. 1.2. Academic Press, New York; Vaughn, R., 1987. Urban Spatial Traffic Patterns, Pion, London]. The developed model provides us with the scenario of urbanisation, based on which the regional and world dynamics of carbon emissions and export from cities, and the annual total urban carbon balance are estimated. According to our estimations, world annual emissions of carbon as a result of urbanisation increase up to 1.25 GtC in 2005 and begin to decrease afterwards. If we compare the emission maximum with the annual emission caused by deforestation, 1.36 GtC per year, then we can say that the role of urbanised territories (UT) in the global carbon balance is of a comparable magnitude. Regarding the world annual export of carbon from UT, we observe its monotonous growth by three times, reaching 505 MtC. The latter, is comparable to the amount of carbon transported by rivers into the ocean (196–537 MtC). The current model shows that urbanisation is inhibited in the interval 2020–2030, and by 2050 the growth of urbanised areas would almost stop. Hence, the total balance, being almost constant until 2000, then starts to decrease at an almost constant rate. By the end of the XXI century, the total carbon balance will be equal to zero, with the exchange flows fully balanced, and may even be negative, with the system beginning to take up carbon from the atmosphere, i.e., becomes a “sink”. The regional dynamics is somewhat more complex, i.e., some regions, like China, Asia and Pacific are being active sources of Carbon through the studied period, while others are changing from source to sink or continue to be neutral in respect the GCC.     

Quantifying Plant Population Persistence in Human-Dominated Landscapes

Abstract:  We assessed population performance of rare plants across a gradient from rural to urban landscapes and evaluated 2 hypotheses central to strategic conservation planning: (1) population performance declines with increasing human dominance and (2) small populations perform poorly relative to larger ones. Assessing these hypotheses is critical to strategic conservation planning. The current conservation paradigm adheres to the well-established ecology theory that small isolated populations, particularly those in human-dominated landscapes, are the least likely to succeed over the long term. Consequently, conservation planning has strongly favored large, remote targets for protection. This shift in conservation toward ecosystem-based programs and protection of populations within large, remote systems has been at the expense of protection of the rarest of the rare species, the dominant paradigm for conservation driven by the endangered species act. Yet, avoiding conservation of small populations appears to be based more on theoretical understanding and expert opinion than empiricism. We used Natural Heritage data from California in an assessment of population performance of rare plants across a landscape with an urban-rural gradient. Population performance did not decrease in urban settings or for populations that were initially small. Our results are consistent with a pattern of few species extinctions within these landscapes over the past several decades. We conclude that these populations within compromised landscapes can contribute to overall biodiversity conservation. We further argue that conservation planning for biodiversity preservation should allocate relatively more resources to protecting urban-associated plant taxa because they may provide conservation benefit beyond simply protecting isolated populations; they may be useful in building social interest in conservation.     

九寨沟自然保护区4种水深梯度下芦苇分株地上生物量的分配与生长

芦苇是世界自然遗产--九寨沟自然保护区的一种重要的湿地植物.本文对该地区芦苇海4个不同水深梯度下芦苇的无性系地上分株的生物量分配、生长与繁殖策略进行了比较研究.结果表明,在47 cm (水在土层表面上)水深环境中,芦苇单株的平均生物量(4.2 g)最大.在-15 cm (水在土层表面下15 cm)的生境中,叶生物量百分比(叶生物量占单株总生物量的百分比, 46.1%)最大.芦苇地上分株高度、地上分株有分枝的单株百分比(茎上有分枝的分株占样地总分株的百分数)也存在明显的差别.茎的生物量分配百分比和生长速率随水深的增加而增加.在滩地生境中,开花率、花序的生物量百分比明显大于水较深的生境.分株株高与分株生物量、茎生物量与叶生物量都表现出较明显的幂指数异速生长规律.在-15 cm水深的生境中,叶生物量的生长快于茎的增长;在其他水深梯度的生境中,则是茎生物量的增加快于叶生物量的增加.     

冬季降温对菹草叶片光合荧光特性的影响

将菹草(Potamogeton cripus)石芽种植于室外水体中,萌发后选择发育程度相近的幼苗,在冬季降温期间利用水下饱和脉冲荧光仪(DIVING-PAM)测定幼苗叶片的FV/Fm和光响应恢复曲线.结果表明,在冬季水温低于7℃的条件下菹草叶片FV/Fm显著降低(P<0.01).水温回复到9～10℃后,FV/Fm逐渐增大;光强的降低有利于FV/Fm的恢复.进一步研究植株的光响应恢复曲线发现,第4-10天,水温<7℃,菹草叶片有效荧光产量(ΔFV'/Fm)的光响应能力和暗恢复能力显著下降;同时,热耗散能力和暗恢复能力也显著降低,发生光抑制的可能性增大.当水温升高到9～10℃时,ΔFV/Fm和非光化学淬灭(NPQ)随光强降低和实验天数的增加逐渐得到恢复.因而,水温9～10℃可能是冬季菹草进行正常光合作用的临界温度;菹草在低温(<7℃)、高光照条件下易发生光抑制,导致PSII受到伤害.     

酸性条件下红壤表面Pb反应动力学的能量特征

用自行设计的动力学装置研究了酸性条件下Pb在红壤表面的反应动力学能量特征.结果表明,酸性条件下,Pb吸附分为快反应和慢反应.用一级动力学方程拟合的Pb最大吸附量,随酸度增加显著下降,随温度升高提前达到平衡.用扩散速率常数计算的活化能(△E*)随酸度的增加而增加,Pb扩散需克服的能障加大;△H值为正,温度升高可促进Pb的扩散;AS值均为负,说明吸附反应使体系有序度增加.原液pH为4.5和5.6时,流出液的pH急剧下降;pH3.8和3.3时流入液比流出液的pH高,是由于土壤的缓冲作用和土壤表面质子化;当溶液中H+超过一定数量后,反应初期的H+消耗是快反应过程.H+对矿物的溶蚀成为速率控制步骤.     

海洋硅藻三角褐指藻经黑暗与UV辐射后的补偿生长(英文)

补偿生长是生物体对环境变化的一种适应性反应,主要指生物体遭受到不良环境胁迫后其生长及生理机能受到制约,但当不良环境胁迫解除后,生物体的生长能力会得到不同程度的恢复,表现出相对未受不良环境胁迫生物体超常生长的现象.迄今为止,补偿生长研究的对象主要集中在水生动物、反刍动物和高等植物上,而针对体积微小的海洋浮游植物的研究非常有限.海洋微藻是海洋生态系统最主要的初级生产者,在自然界物质和能量流动中扮演着至关重要的角色;同时,它们可以广泛应用在水产养殖、食品加工、医药保健、环境保护和生物制能等各种行业,具有非常好地开发利用前景.本文利用海洋硅藻三角褐指藻为试验材料,设置黑暗胁迫和UV辐射胁迫处理,着重测定微藻在恢复生长时期的藻生物量,叶绿素a含量和蛋白质含鼍等指标,探讨经黑暗与UV辐射胁迫后三角褐指藻的补偿生长现象.结果显示,无论是先经正常光照处理还是2 d黑暗处理,UV辐射0.1 rain和0.8 rain的微藻生物量都明显高于不经UV辐射胁迫的微藻生物置;此外,经过不同程度的黑暗与UV辐射处理后,微藻在恢复生长期的叶绿素a和蛋白质含量在某特定生长时期中明显高于对照组的叶绿素a和蛋白质含最.结果表明,三角褐指藻对外界环境变化具有适应能力,一旦不良环境胁迫被解除,微藻会表现出一定的补偿生长效应.我们的研究结果不但拓展和丰富了目前补偿生长的研究对象范围,而且还能为当前赤潮的形成、预测和防治提供一个新的研究思路,为有益经济微藻的高效率培养与利用提供理论指导.     

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.     

全球地表水中全氟和多氟烷基化合物污染特征演替

综述了全氟和多氟烷基化合物（PFASs）在国内外地表水环境中的空间分布及污染特征,总结归纳了PFASs的来源和特征变化趋势。针对地表水中PFASs的监测种类、监测技术及风险评估等方面存在的问题,提出未来需加强日常监测,重点加强对水环境中新型PFASs的关注;针对流域中不同种类PFASs建立高特异性、高灵敏度监测新技术;筛选适合的水生生物作为环境污染指示物以应用于新污染物的评估等建议。为今后我国地表水环境 PFASs污染的现状调查及治理工作提供确实可行的科学参考。     

北京官厅水库中有机氯类农药的分布和来源

采用气相色谱/电子捕获检测器法(GC/ECD)对官厅水库表层水体中18种有机氯农药进行分析.结果表明:官厅水库9个采样点水样中18种有机氯农药残留水平为10.06～87.37 ng·L-1,其中∑HCHs和∑DDTs分别为3.93～38.94和3.71～16.03 ng·L-1.官厅水库及其支流水体受到有机氯农药轻度污染,上游工业区废水排放以及各支流周边地区农田排水是官厅水库中有机氯农药的重要来源.与国内外其他地区相比较,官厅水库表层水体中有机氯农药含量较低,∑DDTs、γ-HCH和七氯环氧均未超过GB 3838-2002地表水环境质量标准限值.