溢油胁迫下孔石莼碳氮稳定同位素的变化

为了研究溢油对海岸潮间带重要的大型绿藻孔石莼（Ulva Pertusa）的影响,本文探究了在180#燃料油的原油分散液（WAF）胁迫下,孔石莼的生长速率、叶绿素a以及碳氮稳定同位素的变化。在低WAF浓度（1.43 mg/L、2.87 mg/L和4.30 mg/L）胁迫下,对孔石莼的生长具有促进作用,生长速率均高于对照组,同时叶绿素a和碳氮稳定同位素均呈现上升的趋势;而高浓度WAF（5.72 mg/L和7.17 mg/L）会抑制藻类生长,导致生长速率低于对照组,而叶绿素a含量却高于对照组,孔石莼的δ15N和δ13C相比对照组偏负。对于孔石莼来说,C、N稳定同位素变化的趋势比叶绿素a更明显,这表明在溢油胁迫下,孔石莼的C、N稳定同位素能够更好更快速地评价溢油胁迫毒性大小,因此可以作为海洋环境监测和评价的一种新手段。     

基于在线监测的江河入海径流通量计算方法研究与应用——以辽河口为例

随着入海流量在线监测技术的兴起,本文从流量在线监测技术原理和步骤出发,对入海流量在线监测的主要技术环节进行了梳理,给出了综合、全面的江河入海径流通量流程化计算方案,并将其应用到了辽河入海径流通量计算实例中。本文的研究为江河污染物排海量的准确估算和入海流量在线监测技术的推广提供了支持。     

双区静电除尘器的数值模拟研究

采用数模拟的方法研究了双区静电除尘器内流场分布、颗粒荷电及颗粒运动等难以直接测量的物理过程,构建了双区静电除尘过程完整的数值模型.采用泊松方程、电流连续性方程和匀强电场方程描述电场,采用N-S方程和雷诺应力标准湍流模型描述流场,采用拉格朗日法描述颗粒运动轨迹.通过截面风速与颗粒去除率的模拟值与实验值的对比,验证了数值模型在模拟内部流场和颗粒运动时的准确性.数值模拟结果表明：双区静电除尘器内部流场分布对入口风速的变化非常敏感;颗粒荷电方式占比由颗粒粒径决定;荷电区内颗粒向极板的趋近过程由流体曳力和电场力共同完成,收尘区内的趋近过程则由电场力主导;入口流速通过改变颗粒前进速度和内部流场形态来影响颗粒运动轨迹.     

小流域综合治理新设计研究——猪沼果模式

近年来,小流域综合治理的主旨思想改变了,其工作重心在于巩固和发展治理开发的成果,提升综合治理的科技含量,增加治理带来的经济效益。于是将小流域的治理与生产联系起来成为了当前科研人员的研究方向。文章对目前部分地区大力推广的"猪-沼-果"模式在小流域治理方面的概念、发展及综合效益等方面做了一些综述。总的来说,猪沼果模式能够增加农村的能源,增加农民收入,并保护绿植,促进小流域治理。     

高速铁路选线对生态环境的影响分析研究

高速铁路选线要充分考虑对生态环境的影响,在路基、桥涵、隧道等形式通过环境敏感点时,要从工程技术和生态环境保护的角度出发,避免高速铁路建设和运营对当地的水资源环境、自然保护区造成破坏。根据高速铁路周边的环境信息,在路基填土高度上结合地形、地质和水文自然特征确定合理的填土高度。在高速铁路跨越生态保护区和湖泊等线路中,贯彻生态选线的原则,准确确定桥涵净空,在工程设计、施工上采用系列的生态保护措施。     

Analysing the sensitivity behaviour of two hydrology models

Recently, the New Morris Method has been presented as an effective sensitivity analysis tool for mathematical models. The New Morris Method estimates the sensitivity of an output parameter to a given set of input parameters (first-order effects) and the extent these parameters interact with each other (second-order effects). This method requires the specification of two parameters (runs and resolution) that control the sampling of the output parameter to determine its sensitivity to various inputs. The criteria for these parameters have been set on the analysis of a well-behaved analytical function (see Cropp and Braddock, Reliab. Eng. Syst. Saf. 78:77–83, 2002), which may not be applicable to other physical models that describe complex processes. This paper will investigate the appropriateness of the criteria from (Cropp and Braddock, 2002) and hence the effectiveness of the New Morris Method to determine the sensitivity behaviour of two hydrologic models: the Soil Erosion and Deposition System and Griffith University Representation of Urban Hydrology. In the first case, this paper will separately analyse the sensitivity of an output parameter on a set of input parameters (first- and second-order effects) for each model and discuss the physical meaning of these sensitivities. This will be followed by an investigation into the sampling criteria by exploring the convergence of the sensitivity behaviour for each model as the sampling of the parameter space is increased. By comparing these trends to the convergence behaviour from Cropp and Braddock (2002), we will determine how well the New Morris Method estimates the sensitivity for each model and whether the sampling criteria are appropriate for these models. It will be shown that the New Morris Method can provide additional insight into the functioning of these models, and that, under a different metric, the sensitivity behaviour of these models does converge confirming the sampling criteria set by Cropp and Braddock.     

Mathematical balance models for monitoring the state of Lake Baikal

The global cycles of man-produced pollutants entering the natural environment are reflected in changes of pollutant cycles, even in background regions.The system of mathematical balance simulation models of inorganic pollutant distribution and circulation (some heavy metals and pesticides included in the priority list for integrated background monitoring) has been developed for the Lake Baikal drainage basin. The system consists of the following units: (1) inventory and classification of regional sources of pollutants entering the atmosphere, natural waters and soils; (2) computation of the global atmospheric transfer and depositions; (3) regional spreading with atmospheric fluxes and deposition onto the underlying surfaces; (4) transport with waterflows feeding Lake Baikal; (5) transport with the lake currents and balance in the lake.The models developed have enabled improvement of existing programmes and systems of observations, in particular to substantiate the large-scale snow sampling and analysis network, and to develop the programme of integrated surveys of the state of Lake Baikal. Since 1981 these actions have been included in the operational network observations within the Lake Baikal Monitoring System.