沉淀--吸附处理双氯灭痛高浓度有机废水的工艺研究

介绍了用沉淀－吸附法处理双氯灭痛高浓度有机废水的工艺。先用废盐酸将废水的ｐＨ调节到４,沉淀、过滤,然后将滤液依次经过炉渣、生炭串级吸附,处理后的废水ＣＯＤＣｒ、ｐＨ、ＳＳ均达到ＧＢ８９７８－８８污水综合排放制药行业二级标准。     

提供生物稳定饮用水的最佳工艺

研究由预处理、常规处理和深度处理组合而成的 7种不同工艺对饮用水源水中可生物同化有机碳 ( AOC)的去除效果 .试验表明 :生物陶粒预处理对 AOC具有较高的去除率 ,达到 45%左右 ,如果在它之前先经过预臭氧化 ,生物处理的去除率可增大到 58.4% ;常规处理对 AOC的去除非常有限 ,去除率平均在 2 0 %左右 ;新活性炭单元因其吸附作用对 AOC的去除效果稳定在30 %左右 ,如和臭氧氧化连用 ,去除效果能提高到 50 %以上 ;包括了常规处理、生物预处理、预臭氧和臭氧活性炭的组合工艺对AOC的去除效果最好 ,达到 86% .因此臭氧氧化、生物炭和生物处理是提高饮用水生物稳定性的重要手段 ,并以本试验结果为依据提出了对于不同的水源水所采用的最佳工艺 .     

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.      

Eventual saturation of the climate–carbon cycle feedback studied with a conceptual model

A saturation of climate–carbon cycle feedback was found earlier in the simulations with the IAP RAS climate model of intermediate complexity. Here, this eventual saturation is interpreted by using a conceptual linearised coupled model. It is shown that this saturation is due to weak, logarithmic, dependence of the carbon dioxide radiative forcing on its atmospheric concentration. This eventual saturation leads to the non-monotonic behaviour of climate–carbon cycle parameter f   in time. If the time scale of the atmospheric CO₂${\text{CO}}_2$ build up is _tp$t_{\text{p}}$ then, starting from an initial equilibrium, f   approaches maximum in time ?_tp$?t_{\text{p}}$. Afterwards, climate–carbon cycle parameter decreases and eventually tends to unity. The time scale of the latter decrease is _t1=(1−5)_tp$t_1=(1-5)t_{\text{p}}$. A dependence of _tm$t_{\text{m}}$ and _t1$t_1$ on governing parameters of the conceptual model is studied. It is argued that an eventual saturation of the climate–carbon cycle feedback is expected to occur also in the other integrations of sufficient length with coupled climate–carbon cycle models.     

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.     

Importance of Habitat Quality and Landscape Connectivity for the Persistence of Endangered Natterjack Toads

Abstract: The natterjack toad (Bufo calamita) is endangered in several parts of its distribution, including Belgium, where it occurs mainly in artificial habitats. We parameterized a general model for natterjack population viability analysis (PVA) and tested its sensitivity to changes in the values of basic parameters. Then we assessed the relative efficiency of various conservation measures in 2 situations: a small isolated population and a system of 4 populations connected by rare dispersal movements. We based the population viability analysis on a stage‐structured model of natterjack population dynamics. We parameterized the model in the RAMAS GIS platform with vital rates obtained from our own field experience and from published studies. Simulated natterjack populations were highly sensitive to habitat quality (particularly pond drying), to dispersal from surrounding local populations, and to a lesser extent to values of fecundity and survival of terrestrial stages. Population trajectories were nearly insensitive to initial abundances, carrying capacities, and the frequency of extreme climatic conditions. The simulations showed that in habitats with highly ephemeral ponds, where premetamorphosis mortality was high, natterjack populations nearly always had a very high extinction risk. We also illustrated how low dispersal rates (<1 dispersing individual/generation) efficiently rescued declining local populations. Such source‐sink dynamics demonstrate that the identification and management of source populations should be a high priority.     

土地利用方式对紫色土丘陵区土壤剖面碳、氮影响

采取野外调查与室内分析相结合的方法研究了紫色土丘陵区林地、撂荒地、水田、旱地土壤剖面(0～40 cm)有机碳、全氮变化特征.结果表明.有机碳、全氮均随土层深度增加而逐渐减小,且林地、撂荒地有机碳递减幅度高于水田、旱地.相对于撂荒地和旱地,水田、林地更利于有机碳、全氮的积累.林地有机碳和全氮在0～5 cm土层表现出绝对优势;随土层递增,与水田、撂荒地和旱地的差异逐渐减小.水田有机碳和全氮在大于10 cm土层显示最大值.而撂荒地有机碳和全氮仅在土壤表层高于旱地.有机碳与全氮存在显著正相关关系;w(C)/w(N)随土层深度增加而降低,且林地、撂荒地降低幅度较大.因此相对于水田、旱地,林地和撂荒地w(C)/w(N)仅在0～10 cm显示较大值.可见,土地利用方式对陆地生态系统碳、氮蓄积有明显影响,通过旱地还林或撂荒可以增加土壤特别是表层土壤对碳、氮的积累.     

颗粒活性炭对水中邻苯二甲酸二甲酯的吸附特性

研究了颗粒活性炭(GAC)对水中邻苯二甲酸二甲酯(DMP)的静态与动态吸附特性.结果表明,Freundlich和Langmuir等温线模型可以较好的拟合GAC对DMP的吸附.GAC对DMP的吸附容量较大,溶液初始浓度为200mg/L时,GAC对DMP的动态和最大静态吸附容量分别为484.60,450.89mg/g.考察了不同流速条件下(0.65～4.00mL/min)GAC吸附DMP的穿透特性,Yoon-Nelson模型能很好地拟合DMP在GAC柱中的穿透曲线,根据试验数据和Yoon-Nelson模型计算出穿透参数K′、T和穿透点t1以及平衡点t2.在建立了进水流量与Yoon-Nelson穿透模型的参数之间的关系基础上,得到了活性炭柱出水浓度与进水流量和穿透时间之间的动态关系模型.     

活性炭应用测试新技术——微型快速穿透实验

进行了微型快速穿透(MCRB)实验与中小型、小型传统穿透实验方法的对照实验,结果表明,MCRB实验适用于模拟大型活性炭床的穿透情况,预测处理费用以及精选活性炭.MCRB实验加快了实验速度,避免了传统穿透实验中常见的问题.空床接触时间(EBCT)、活性炭粒径对MCRB实验有一定影响.使用粒径120～180目的活性炭,MCRB实验的压力一般小于3.03×10⁵Pa.MCRB实验对2,4-二氯苯酚(2,4-DCP)和甲基叔丁基醚(MTBE)模拟废水的吸附处理获得合理的研究结果.