激光点云的多功能风洞施工量测与分析

针对传统皮尺测绘、全站仪在结构复杂的多功能风洞中存在采集作业难、数据精度低、信息不完整等局限性,提出基于高精度、高密度的点云数据开展对风洞施工量测的研究。通过对点云进行预处理及算法的运用,解决风洞数据获取难、信息不完整瓶颈,实现施工量测数据的有效获取及分析。基于点云预处理数据,可获取风洞的二维线划图、立面图、三维信息模型及统计分析等成果;基于点云数据运用算法,能够快速、准确地对风洞内墙面的平整度提取分析,判断施工是否符合要求,这是传统测绘方法无法获取的,验证该技术方法在多功能风洞测量的优越性和必要性。应用结果表明,地面三维激光扫描技术对该风洞的施工量测及建筑信息提取均优于传统方法,成效明显。     

An Actively Controlled Wind Tunnel And Its Application To The Reproduction Of The Atmospheric Boundary Layer

An actively controlled wind tunnel equipped with multiple fansand airfoils has been developed, mainly for the purpose of reproducing the atmospheric boundary layer (ABL) for wind engineering applications. Various fluctuating flows can be achieved in this wind tunnel by altering the input data of the fans and airfoils through computer control. In this study, the ABL is physically simulated in this wind tunnel, and particular attention ispaid to the simulation of the profile of Reynolds stress. The method of generating the fluctuating flow and the experimental results of reproducing the ABL are presented. As the results show, the spatial distribution of Reynolds stress is satisfactorily simulated, and the profiles of other statisticalturbulent parameters, such as mean velocity, turbulent intensity, integral scale and power spectrum are successfully reproduced simultaneously.     

藏东地区新生代构造体系与成矿的关系

区域构造和微构造分析表明，新生代藏东地区构造应力场自印支燕山期的NE-SW向挤压向喜马拉雅山期的NNE-SSW向压扭性转变，表现在：（1）沿昌都地块两侧及古生代一中生代形成的深大断裂带发生了大规模的右旋走滑活动，伴重型较强的碎裂岩化、拉伸线埂和剑鞘褶皱等，沿主断裂两侧叠加一系列NW、NNW及NE向雁行式排列的褶皱和张扭性断裂；（2）在区域上，沿大规模右旋走滑断裂两侧形成一系列雁行式排列的第三系走滑拉分盆地；（3）新生代岩浆活动沿走滑断裂两侧的张扭性次级断裂有规律分布，新生代构造体制的转变造成大规模成矿流体与富集，使新生代成为本区最重要的成矿时期，而北澜沧江，妥坝、温泉断裂带及车所乡断裂带北段是该期矿产最有利的富集部位。     

自喷生产井深层卤水的动态分析

本文以四川盆地中部的P_1井为例,分析自喷型深层卤水生产钻井的开采动态特征,建立生产指标之间的统计关系,并预测钻井自喷阶段的总产量。     

FIELD STUDY ON WIND EROSION IN THE NORTHWESTSHANXI PROVINCE

Field study on wind erosion in the hilly regions with gentle slope in the Northwest Shanxi Province has been carried out from 1983 through 1988. Based on the data observed in the field, quantitative analyses of the wind erosion and the effects of the wind-break forest are presented in this paper in detail. Most of the strong windy days occur in the period of March to May. The coincidence of drought and strong wind in the Spring days with no vegetative cover at all on the loose top soil lead to severe wind erosion in this region. The rate of soil erosion is as high as 12800 t / km2. Major characteristics of wind and other meteorological factors are given in graphs and tables. Wind-break forest reduces the wind velocity by 51. 1 %. Consequently, the amount of wind erosion is reduced by 90% and the dust content in the atmosphere is reduced by 97. 1 % in comparison with those measured in the farmland. This paper provides a preliminary summary on the result of data analyses of wind erosion on the Loess Plateau. It can serve as scientific basis for control of the wind erosion in regions of similar conditions.     

Relationships between deflation and near surface wind velocity in a coastal dune blowout

Detailed field measurements were made of the degree of surface level change in a blowout, situated in the coastal dune area of Meijendel, The Netherlands. A formula was established to express the erosivity of the wind for the corresponding 34 measurement intervals, over a period of about 3 years. Having established, for 12 wind sectors, the relationship between wind velocity at the nearest standard weather station and at five locations in the blowout, correlations were derived between the deflation rate in the blowout and the wind erosivity using standard hourly wind data. The winter season, although the most windy, is by far the least effective season: the threshold shear wind velocity is disproportionally increased because the moisture content of the surface sand is high. The soil moisture conditions are described as a function of the daily precipitation and evaporation rate. The two most relevant upper and lower threshold shear wind velocities are determined empirically. During the summer season, deflation rate is even higher than indicated by the net surface level change because deflation is partly compensated by deposition of sand transported by rainwash from the blowout margin. With regard to spatial variation in the deflation rate within the blowout, it appears that locations with relatively high velocities coincide with higher deflation rates. However, the spatial variation is commonly less than is expected from the horizontal wind velocity distribution. In view of this the role of wind direction, blowout morphology and algal coverage of the soil in the deflation rate is discussed.     

Oxyanion Concentrations in Eastern Sierra Nevada Rivers – 2. Arsenic and Phosphate

Water samples were collected from the Truckee River-Pyramid Lake system, the Walker River-Walker Lake system, and the Carson River, all located in eastern California and western Nevada, U.S.A., at three different times (i.e., summer 1991, spring 1992, and autumn 1992) over a two year period. The concentrations of As, Na, Cl, PO4, and pH were measured in these river samples and the associated terminal lakes. Arsenic values ranged from below 13 nmol/kg near Truckee, California to 160 nmol/kg at Nixon, Nevada in the Truckee River, from 40 nmol/kg in the headwaters of both West and East Walker Rivers to 270 nmol/kg below Weber Reservoir on the main branch of the Walker River, and from <27 nmol/kg to 234 nmol/kg for the lower Carson River system. Arsenic concentrations in Steamboat Creek (0.91 mol/kg–1.80 mol/kg) in the Truckee River catchment are above the U.S. EPA drinking water maximum contaminant level of 0.67 mol/kg, as are the As concentrations in both Pyramid Lake (1.33 mol/kg–1.57 mol/kg ) and Walker Lake (13.7 mol/kg–18.7 mol/kg). Sources of As for all three rivers include weathering of As-rich rocks and/or regolith and input of high-As geothermal spring waters, both processes primarily, although not exclusively, adding As to the headwater regions of these rivers. Steamboat Hot Springs (29 mol/kg As 54.5 mol/kg), for example, is identified as a source of As to the Truckee River via Steamboat Creek. The high As concentrations in Pyramid and Walker Lakes are likely due to (1) desorption of arsenate from aquatic particulate matter in these high pH waters (9.0 pH 9.5), (2) limited biologic uptake of arsenate, and (3) evaporative concentration of the lake waters. Evaluation of molar PO4}/As ratios of river waters and geothermal spring waters (e.g., Steamboat Hot Springs), indicates that phosphate is substantially enriched in Steamboat Creek as well as the mid to lower reaches of the Walker and Carson Rivers. These regions of each river are dominated by agricultural interests and, additionally, in the case of Steamboat Creek, residential areas and golf courses. Our data strongly imply that phosphate-rich agricultural return flow has likely added P to these streams and, consequently, increased their respective P:As ratios.     

Three-dimensional multilayer cylindrical tunnel model for calculating train-induced dynamic stress in saturated soils

This study proposes an improved tunnel model for evaluating train-induced dynamic stress in saturated soils, which can consider multiple moving loads, grouting layer and pore-water pressure. Using Shanghai Metro’s actual parameters for train speed, tunnel, grouting layer and soils, the analysis of the spatial distribution of dynamic stress for soils and stress state of various locations under moving train loads shows that neglecting effects such as pore-water pressure can lead to underestimating dynamic normal stress and overestimating dynamic shear stress in the soils below tunnel. This model can be further extended to investigate principal stress axes rotations and tunnel settlement.     

Review of Methodologies for Offshore Wind Resource Observation and Assessment

Observation and assessment of wind resources is a prerequisite for wind farm construction. Due to the investment cost of offshore wind farm is very expensive, more accurate assessment of wind resources is needed to reduce their investment risks. From traditional field observation to multi-platform remote sensing and from ordinary mathematical statistics to coupled numerical model simulation, abundant offshore wind data and evolving assessment methods make the results of offshore wind resource assessment more and more reliable. Poor station observations and rich remote sensing data are distinct characteristics of offshore wind data. Technology integration of applying multi-scale coupled models to assimilate multi-source remote sensing and station data is a mainstream development direction of offshore wind resource assessment methods. The wind resource assessment for offshore wind farm should focus on data quality and method selections of data interpolation, wind speed calculation of return period and wind energy parameters adjusted for a long term condition because these factors can significantly affect the operating efficiency of future wind farm.     

Study on the Long-term Settlement of Subway Tunnel in Soft Soil Area

The long-term settlement of a subway tunnel, especially the differential settlement affects the safe operation of the subway. In this article, the settlement of a subway tunnel was studied from the theoretical and numerical analyses based on the monitoring data. According to the monitoring data, the deformation of segments at different locations is different, and the deformation around a channel is larger than other places. The settlements of tunnel calculated by two theoretical methods are consistent with that obtained in the centrifuge model test. The numerical simulation indicates that the vertical displacement is much bigger than the horizontal displacement.