小波熵去噪在微差爆破延时精确识别中的应用

在小波熵去噪理论的基础上,对实际隧道爆破工程采集到的爆破振动信号进行了小波熵方法去噪。利用db8小波对去噪后的信号在尺度a=16进行了连续小波变换得到其模极大值,准确识别了隧道多段别微差爆破实际延期时间间隔,并验证了小波熵方法去噪的可靠性。结果表明,小波熵去噪方法能够有效滤除和抑制爆破振动非线性信号所夹杂的高频噪声分量,并且很好地保留了爆破振动信号的突变细节。对滤波后的信号进行模极大值变换,信号局部奇异点的辨识更准确,可以精确识别隧道微差爆破延时间隔。     

井下采煤影响矿区坡面形态及侵蚀的数值模拟分析

针对井下采煤产生的大范围岩移必然最终改变原有地表形态并影响坡面侵蚀特征及规律这一特殊性,从井下与地表相结合的新视角,结合彬长矿区水土流失特征和典型煤矿采矿条件,以采厚、地表坡面坡度等因素为变量,构建了20个不同类型的数值模型,通过数值模拟方法研究并揭示井下采煤对地表坡面形态及侵蚀的影响规律。结果表明,第一,地表坡面坡度会随采厚增加而呈现增大的趋势,且自然坡度越大,坡度变化量越大;相同采厚条件下,坡度增大率与坡面自然坡度整体上呈负相关。第二,地表坡面坡长会随采厚增加而呈现减小的趋势,且自然坡度越小,坡长变化量越大;随采厚增加,地表坡面坡长减小率与自然坡度呈先正相关后负相关的关系,自然坡度为26.57°是拐点。第三,采厚的增加会提高地表坡面产流产沙的强度,加剧坡面侵蚀,这种效应在坡度较小的坡面更加显著;井下采煤引起地表坡面坡度的增大是产生这一规律的主因。     

Hydro-abrasive erosion in hydro turbines: a review

The flow of sediment particles in rivers is a big challenge to develop hydropower plants across the sediment-laden rivers. Hard particles such as quartz and feldspar are available in high amount in the Asian mountain range. The abrasive action of these particles causes the hydro turbines to suffer from erosion in particular at high- and medium-head hydroelectric power plants. This has become a serious economic issue due to maintenance costs and production losses. The treatment without prevention is simply unsustainable. Facilities for sediment exclusion, typically sand traps as well as turbine design, and materials have been improved considerably. In the present paper, studies have been discussed extensively undertaken by several investigators in this field. Based on literature survey several aspects related to reducing the sediment load on turbines, useful ways to improve the turbine surface performance and various erosion models to characterize the effect of erosion on the performance of turbines have been discussed. To calibrate and validate the developed erosion models, more measurements from both physical model tests in laboratories and continuous monitoring of sediment parameters and their impact on the operational hydro turbines are required. As well as the state-of-art in the modeling and simulation using computational fluid dynamics (CFD) has made it possible to optimize the hydraulic design of hydro turbines in order to minimize the erosion level without much sacrifice in the efficiency. To mitigate the hydro-abrasive erosion effects on the performance of turbines, significant improvements have been achieved so far and development is ongoing.     

航空发动机涡轮叶片热障涂层冲蚀试验装置的研制

目的通过研制热障涂层冲蚀服役环境的模拟装置,来研究冲蚀失效机制。方法通过研制模拟热障涂层高温热冲击的燃气喷枪,在喷枪中设计速度、流量可控的颗粒送料系统,同时在装置中集成裂纹演化实时检测的声发射系统。结果该系统实现了热障涂层冲蚀服役环境的模拟,温度场、裂纹演化损伤参量的同步采集、输出与显示,从而完成了冲蚀服役环境模拟与关键损伤参量实时检测的一体化设计。结论装置能完成热障涂层常温、高温等各种服役温度、各种冲蚀角度、各种冲蚀速度等条件下的模拟试验,并提供较为系统的损伤参量检测数据,为理解热障涂层的冲蚀机理、优化其设计制备提供有效的试验数据。     

基于数字图像相关方法的石墨高温杨氏模量测试

目的为了得到石墨在高温环境下的杨氏模量,为飞行器热防护系统和高温热结构的设计提供可靠的技术保障。方法基于数字图像相关(DIC)方法和通电电阻加热技术,建立一套测量材料在高温环境下力学性能的测试系统。利用该系统,测量高温下石墨试样的表面应变场和应力-应变曲线,计算相应温度下的杨氏模量。在1400℃实验环境下,采用基于DIC与高温引伸计的方法同时测量超高温陶瓷试件的拉伸应变数据,并进行比较验证。结果在1400℃实验环境下,采用基于DIC与高温引伸计方法测得超高温陶瓷的应变-时间曲线吻合良好,方差为1.3×10-7。1200~1900℃高温环境下,石墨的杨氏模量随温度的升高呈线性增长趋势。结论采用基于DIC方法准确有效,该方法可方便快速地实现对石墨材料在高温环境下杨氏模量的测量。另外,该方法也可应用于其他导电材料杨氏模量的测试。     

Storm impacts along European coastlines. Part 2: lessons learned from the MICORE project

This paper describes the MICORE approach to quantify for nine field sites the crucial storm related physical hazards (hydrodynamic as well as morphodynamic) in support of early warning efforts and emergency response.As a first step historical storms that had a significant morphological impact on a representative number of sensitive European coastal stretches were reviewed and analysed in order to understand storm related morphological changes and how often they occur around Europe. Next, an on-line storm prediction system was set up to enable prediction of storm related hydro- and morphodynamic impacts. The system makes use of existing off-the-shelf models as well as a new open-source morphological model. To validate the models at least one year of fieldwork was done at nine pilot sites. The data was safeguarded and stored for future use in an open database that conforms to the OpenEarth protocols.To translate quantitative model results to useful information for Civil Protection agencies the Frame of Reference approach ( [Van Koningsveld et al., 2005] and [Van Koningsveld et al., 2007] ) was used to derive Storm Impact Indicators (SIIs) for relevant decision makers. The acquired knowledge is expected to be directly transferred to the civil society trough partnerships with end-users at the end of the MICORE project.     

珠江流域河流碳输出通量及变化特征

研究河流碳运移对于研究全球碳循环以及探讨河流对全球气候变化的响应机制具有重要意义.2012年4月和7月选取珠江主流及支流11个代表性断面,分析悬浮颗粒物和碳组分的空间分布和季节变化,同时选取博罗、石角和高要这3个主控断面,对珠江流域的碳通量和侵蚀模数进行了估算.结果表明,珠江流域悬浮颗粒物(TSS)、颗粒有机碳(POC)以及溶解有机碳(DOC)随雨季的到来而质量浓度升高,西江上游TSS和POC的质量浓度增加显著;珠江流域河流碳的4种组分中,溶解无机碳(DIC)的所占质量分数最高,且西江、北江的DIC质量浓度明显高于东江;西江、北江和东江河流中外源POC分别占78%、72%和26%,三大支流的POC均受上游C3植物的影响;珠江流域的TSS、总碳(TC)、POC、颗粒无机碳(PIC)、DOC、DIC、以及颗粒碳(TPC)、总有机碳(TOC)的入海通量分别为134×1012、12.69×1012、2.50×1012、1.01×1012、1.13×1012、8.05×1012、3.51×1012和3.65×1012g·a-1,对应的侵蚀模数分别为:309×106、28.98×106、5.75×106、2.27×106、2.56×106、18.4×106、8.02×106和8.31×106g·(km2.a)-1.与全球主要河流碳侵蚀模数相比,珠江流域河流DOC、POC和TOC的侵蚀模数均高于全球平均值.     

EVALUATION OF RUNOFF,EROSION, AND PHOSPHORUS MODELING SYSTEM—SIMPLE1

ABSTRACT: The purpose of this study was to evaluate the performance of Spatially Integrated Models for Phosphorus Loading and Erosion (SIMPLE) in predicting runoff volume, sediment loss, and phosphorus loading from two watersheds. The modeling system was applied to the 334 ha QOD subwatershed, part of the Owl Run watershed, located in Fauquier County, Virginia, and to the 2240 ha watershed, Battle Branch, located in Delaware County, Oklahoma. Simulation runs were conducted at cell and field scales, and simulation results were compared with observed data. Runoff volume and dissolved phosphorus loading were measured at the Battle Branch watershed. Runoff volume, sediment yield, and total phosphorus loading were measured at the QOD site. SIMPLE tended to underestimate runoff volumes during the dormant period, from November to March. The comparison between observed and predicted dissolved phosphorus showed better correlation than for observed and predicted total phosphorus loading. Cell level simulations provided similar estimates of runoff volume and phosphorus loading when compared to field level simulations for both watersheds. However, observed sediment yields better compared with the values predicted from the cell level simulation when compared to field level simulation. Finally, results of model evaluation indicated that SIMPLE's predictive ability is acceptable for screening applications but not for site-specific quantitative predictions.     

ROLE OF EROSION PROCESSES IN TRANSFER OF RADIONUCLIDES: RESULTS OF FIELD EXPERIMENTS1

ABSTRACT: An experimental one-year fieldwork has been conducted in the vicinity of the Chernobyl NPP, within an agricultural watershed, to study the transfer of radionuclides brought into the environment by the disaster of 1986. Presented are results of observation of the washout of ¹³⁷Cs from the runoff plot both in natural conditions and under artificial rainfalls. Beside traditional hydro-logical methods, new techniques were used allowing to consider microtopographical peculiarities of the runoff plot and their role in the redistribution of radionuclides. The estimate of the annual mass balance for the soil and the radionuclides within the runoff plot has shown that, regardless of significant areal variation of their concentration, the ¹³⁷Cs washout with the solid runoff resulted from artificial rainfalls amounts to some 1 percent of its reserves in the uppermost 5 cm of the topsoil. The same parameter for the natural runoff is lower by an order of magnitude. Both these factors of self-purification are about two times less than natural radioactive decay of ¹³⁷Cs.     

“R1-R4” AND “BOISED” SEDIMENT PREDICTION MODEL TESTS USING FOREST ROADS IN GRANITICS1

ABSTRACT: Erosion and sedimentation data from research watersheds in the Silver Creek Study Area in central Idaho were used to test the prediction of logging road erosion using the R1-R4 sediment yield model, and sediment delivery using the “BOISED” sediment yield prediction model. Three small watersheds were instrumented and monitored such that erosion from newly constructed roads and sediment delivery to the mouths of the watersheds could be measured for four years following road construction. The errors for annual surface erosion predictions for the two standard road tests ranged from +31.2 t/ha/yr (+15 percent) to -30.3 t/ha/yr (-63 percent) with an average of zero t/ha/yr and a standard deviation of the differences of 18.7 t/ha/yr. The annual prediction errors for the three watershed scale tests had a greater range from -40.8 t/ha/yr (-70 percent) to +65.3 t/ha/yr (+38 percent) with a mean of -1.9 t/ha/yr and a standard deviation of the differences of 25.2 t/ha/yr. Sediment yields predicted by BOISED (watershed scale tests) were consistently greater (average of 2.5 times) than measured sediment yields. Hillslope sediment delivery coefficients in BOISED appear to be overly conservative to account for average site conditions and road locations, and thus over-predict sediment delivery. Mass erosion predictions from BOISED appear to predict volume well (465 tonnes actual versus 710 tonnes predicted, or a 35 percent difference) over 15 to 20 years, however mass wasting is more episodic than the model predicts.