三种叠放形式的圆管型人工鱼礁流场效应数值模拟与PIV试验研究

人工鱼礁单体按不同的数量和排列方式组合投放会产生不同的流场效应。圆管型礁为目前黄渤海区增殖礁的重要礁体型式,为优化该礁体的投放数量与排列方式,选择了3种不同叠放个数(1个、3个和6个)的圆管礁,设定了5个流速梯度(4.5、9.0、13.5、18.0和22.5cm/s),利用PIV粒子图像测速技术和Fluent数值模拟软件对圆管型人工鱼礁的流场进行水槽模型试验和数值模拟。结果表明,数值模拟结果与水槽试验结果基本吻合,误差在20%以下,表明数值模拟能够反映人工鱼礁的流场效应;当礁体叠放个数一定时,最大上升流流速、上升流高度和上升流面积均随来流速度的增加而增大,背涡流面积呈现不规则的变化;当来流速度一定时,最大上升流流速、上升流面积、上升流高度和背涡流面积均随礁体叠放个数的增加而增大。     

NUMERICAL EXPERIMENTS FOR THE EFFECTS OF TWO MODEL INITIALIZATION SCHEMES ON RAINFALL FORECAST IN THE 2008 FLOODING SEASON

In this paper, based on heavy rain numerical forecast model AREM （Advanced Regional Eta Model）, two different initialization schemes, LAPS and GRAPES-3DVAR, are used to run assimilation experiments of AREM-LAPS and AREM-3DVAR with the same data source （NCEP forecast field, surface data and radio-soundings） during the period from 21 May to 30 July 2008 to investigate the effect of the two initialization schemes on the rainfall simulation. The result suggests that： （1） the forecast TS score by the AREM-LAPS is higher than that by the AREM-3DVAR for rainfall in different areas, at different valid time and with different intensity, especially for the heavy rain, rainstorm and extremely heavy rain; （2） the AREM-3DVAR can generally simulate the average rainfall distribution, but the forecast area is smaller and rainfall intensity is weaker than the observation, while the AREM-LAPS significantly improves the forecast; （3） the AREM-LAPS gives a better forecast for the south-north shift of rainfall bands and the rainfall intensity variation than the AREM-3DVAR; （4） the AREM-LAPS can give a better reproduction for the daily change in the mean-rainfall-rate of the main rain band, and rainfall intensity changes in the eastern part of Southwest China, the coastal area in South China, the middle-lower valleys of Yangtze river, the Valleys of Huaihe river, and Shandong peninsula, with the rainfall intensity roughly close to the observation, while the rainfall intensity simulated by the AREM-3DVAR is clearly weaker than the observation, especially in the eastern part of Southwest China; and （5） the comparison verification between the AREM-LAPS and AREM-3DVAR for more than 10 typical rainfall processes in the summer of 2008 indicates that the AREM-LAPS gives a much better forecast than AREM-3DVAR in rain-band area, rainfall location and intensity, and in particular, the rainfall intensity forecast is improved obviously.     

Obtaining public support for North-South climate funding: Evidence from conjoint experiments in donor countries

The adoption of the Warsaw mechanism on loss and damage has again highlighted the North-South divide in those parts of UNFCCC negotiations dealing with international climate finance. Current estimates put required funding from rich countries at 50–100 billion Euros per year to induce non-Annex I countries to take on greenhouse gas limitation commitments and to assist highly vulnerable countries. Results from survey-embedded conjoint experiments can help policy-makers anticipate opportunities and pitfalls in designing large-scale climate funding schemes. We implemented such experiments in the United States and Germany to better understand what institutional design characteristics are likely to garner more public support for climate funding among citizens in key developed countries. We find that climate funding receives more public support if it flows to efficient governments, funding decisions are made jointly by donor and recipient countries, funding is used both for mitigation and adaptation, and other donor countries contribute a large share. Contrary to what one might expect, climate change damage levels, income, and emissions in/of potential recipient countries have no significant effect on public support. These findings suggest that finance mechanisms that focus purely on compensating developing countries, without contributing to the global public good of mitigation, will find it hard to garner public support.     

数字摄影测量开放实验室的建设与实践

针对培养创新性人才对高校开放实验室的要求,介绍数字摄影测量实验室的开放形式与管理制度,阐述综合创新性实验设置的特点与具体项目,提出促进实验室社会化发展的一些途径和方法.通过几年的实践表明,实验室开放建设既增强学生的专业实践能力和创新能力,也促进教师的科研与教学能力.     

基于认知风格的遥感导论实验教学体系的建立与实践

从认知风格理论出发,顺应学习者的认知风格差异,建立多层次、一体化的实验教学体系,并从实验教学的内容、过程、环境与考核出发,构建个性化的学习平台,以培养学习者的实践能力与创新精神。     

建筑爆破倒塌过程的摄影测量分析系统

本文将近景摄影测量分析系统引入工程爆破领域,对建筑物倒塌过程的运动轨迹进行测量分析.本分析系统用非量测用摄影机采集建筑爆破倒塌过程的影像,用直接线性变换解法解析图像,再进行专业化的数据后处理,获得建筑物倒塌过程的构件(或部分结构体)的运动学和动力学参数以及爆破后座、动能、势能、机械能损失率等引申物理量,从而实现各种爆破...     

中职学校工程测量大赛对实践教学的启示

通过对陕西省教育厅举办过的两届中职学校工程测量大赛的结果总结,分析了目前中职学校工程测量教学中存在的问题及形成原因,对产生原因的各个方面进行了探讨,并提出了解决办法。     

Simulated Spatiotemporal Response of Ocean Heat Transport to Freshwater Enhancement in North Atlantic and Associated Mechanisms

The Atlantic Meridional Overturning Circulation(AMOC)transports a large amount of heat to northern high latitudes,playing an important role in the global climate change.Investigation of the freshwater perturbation in North Atlantic(NA)has become one of the hot topics in the recent years.In this study,the mechanism and pathway of meridional ocean heat transport(OHT)under the enhanced freshwater input to the northern high latitudes in the Atlantic are investigated by an ocean-sea ice-atmosphere coupled model.The results show that the anomalous OHT in the freshwater experiment(FW)is dominated by the meridional circulation kinetic and ocean thermal processes.In the FW,OHT drops down during the period of weakened AMOC while the upper tropical ocean turns warmer due to the retained NA warm currents.Conversely,OHT recovers as the AMOC recovers,and the mechanism can be generalized as:1)increased ocean heat content in the tropical Southern Ocean during the early integration provides the thermal condition for the recovery of OHT in NA;2)the OHT from the Southern Ocean enters the NA through the equator alongthe deep Ekman layer;3)in NA,the recovery of OHT appears mainly along the isopycnic layers of 24.70-25.77 below the mixing layer.It is then transported into the mixing layer from the "outcropping points"innorthern high latitudes,and finally released to the atmosphere by the ocean-atmosphere heat exchange.     

An experimental study on using MR damper to mitigate longitudinal seismic response of a suspension bridge

In this paper, the seismic response reduction performance of magnetorheological (MR) damper is experimentally investigated for a suspension bridge. First, the force–displacement and force–velocity curves under a range of excitation frequencies, amplitudes and currents are obtained by mechanical behavior test of the RD1097 type MR damper. Then a new non-linear hysteretic model is proposed to model the mechanical behavior of the MR damper and the model parameters are identified from test data. An experimental method, as well as a set of testing setups with the MR damper for longitudinal seismic response reduction of a SDOF generalized system representing the fundamental longitudinal mode of suspension bridge, is developed. Finally, the seismic response reduction experiment subject to three kinds of earthquake excitations, including the Pingsheng Bridge earthquake wave, the El-Centro wave and the Taft wave, is carried out, and nine control cases, including uncontrolled, six passive control schemes with different input currents and two semi-active Bang–Bang control schemes, are tested. The results verify that the seismic response reduction experimental method is feasible and the good performance of seismic longitudinal response reduction of the suspension bridge can be achieved by MR damper. It is also shown that the passive control with optimum input current outperforms the semi-active Bang–Bang controls.     

Sorption of ortho‐Phenylphenol to Soils

Conflicting sorption coefficients for ortho‐phenylphenol (OPP) have been reported in the literatures, which resulted in the conflicting assessments on OPP mobility in soil. To ascertain the sorption coefficient of OPP, batch experiments were performed based on OECD guideline 106, using three types of soils. Headspace solid‐phase microextraction (HS‐SPME) and GC‐MS were applied to the determination of OPP concentration in the liquid phase. The sorption isotherms obtained for all three soils under equilibrium conditions were described well, assuming linear sorption. The organic carbon normalized distribution coefficients (K_oc) ranged from 894 to 1703 L kg^?1, which suggested that OPP is moderately mobile in soil. The results also showed that the K_oc value of OPP can be predicted precisely from K_ow, whereas it was underestimated by one order of magnitude when water solubility is used.