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891.
892.
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. 相似文献
893.
Due to the lack of data on hydraulic-jump dynamics in very large channels, the present paper describes the main characteristics
of the velocity field and turbulence in a large rectangular channel with a width of 4 m. Although a hydraulic jump is always
treated as a wave that is transversal to the channel wall, in the case of this study it has a trapezoidal front shape, first
starting from a point at the sidewalls and then developing downstream in an oblique manner, finally giving rise to a trapezoidal
shape. The oblique wave front may be regarded as a lateral shockwave that arises from a perturbation at a certain point of
the lateral wall and travels obliquely toward the centreline of the channel. The experimental work was carried out at the
Coastal Engineering Laboratory of the Water Engineering and Chemistry Department of the Technical University of Bari (Italy).
In addition to the hydraulic jump formation, a large recirculating flow zone starts to develop from the separating point of
the lateral shock wave and a separate boundary layer occurs. Intensive measurements of the streamwise and spanwise flow velocity
components along one-half width of the channel were taken using a bidimensional Acoustic Doppler Velocimeter (ADV). The water
surface elevation was obtained by means of an ultrasonic profiler. Velocity vectors, transversal velocity profiles, turbulence
intensities and Reynolds shear stresses were all investigated. The experimental results of the separated boundary layer were
compared with numerical predictions and related work presented in literature and showed good agreement. The transversal velocity
profiles indicated the presence of adverse pressure gradient zones and the law of the wall appears to govern the region around
the separated boundary layer. 相似文献
894.
北京官厅水库中有机氯类农药的分布和来源 总被引:3,自引:1,他引:3
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. 相似文献
895.
对ABR反应器的水力流态进行了示踪剂试验,分析了特征截面面积对ABR水力特性的影响,采用停留时间分布(RTD)法研究了不同进水COD浓度和HRT条件下ABR反应器的水力特性,结果表明不同进水COD浓度时ABR反应器的RTD曲线相似,表明进水COD浓度不是影响ABR水力特性的主要因素;不同HRT条件下RTD曲线差异很大,表明HRT对ABR的水力特性影响较大,随着水力停留时间的延长,N值增大,1/Pe减小,ABR的流态趋于推流流态,随着HRT的缩短,N值减小,1/Pe数增大,ABR反应器趋于完全混合流态. 相似文献
896.
897.
探讨了6组不同的碳氮比(C/N)对分段进水生物脱氮工艺中进水流量分配、每一段中缺氧区好氧区容积比以及脱氮效率的影响.将进水总氮浓度恒定为42mg/L(凯氏氮浓度为40mg/L),以比较出水总氮浓度.结果表明,在一定C/N条件下,通过调整进水流量分配和每一段缺氧区与好氧区容积比可达到高于95%的总氮去除率.同时污泥体积指数也会随着进水流量分配系数的升高而增大.出水总氮浓度主要是由进水流量分配所决定,每一段中缺氧区好氧区的容积比影响不大. 相似文献
898.
899.
Introduction Photosyntheticphotonfluxdensity(PPFD)withinforestcanopiesisintrinsicallyheterogeneousinspaceandtime.Becausesomespeciesaregenotypicallysuitedforspecificlightregimes,understandingtheheterogeneityofthelightregimewithinaforestcanopyisimportantfor… 相似文献
900.
不同粒径垃圾焚烧飞灰重金属分布和浸出性质 总被引:19,自引:0,他引:19
对烟气净化系统飞灰(以下简称飞灰)按粒径进行分级,研究了飞灰重金属含量、形态分布和浸出毒性随粒径的变化,讨论了不同粒径的飞灰对重金属总量和浸出总量的贡献率.结果表明:飞灰中粒径>154 μm和<30 μm的颗粒较少,粒径为38.5~74 μm的颗粒约占总量的50%.除Ni和Cr外,重金属含量随飞灰粒径的减小呈增加趋势,且主要表现在酸溶态Cd,Zn,Pb,Cu和有机结合态Pb以及晶形氧化铁态Pb,Zn含量的增加.随着飞灰粒径的减小,Cr,Ni,Zn,Hg和Pb的浸出量也呈逐渐增加趋势,其中Zn,Hg和Pb的表现尤为突出.尽管细颗粒上的重金属对飞灰的重金属总量贡献不大,但高浸出率使细颗粒飞灰对重金属浸出总量仍具有较大贡献,尤其是Pb,Zn和Hg,在占飞灰质量8%的粒径<30 μm的飞灰中,富集了约40%的水溶性Pb,Zn和Hg. 相似文献