Sand particle lift-off velocity measurements and numerical simulation of mass flux distributions in a wind tunnel

Lift-off velocity of saltating sand particles in wind-blown sand located at 1.0 mm above the sand bed surface was measured using a phase Doppler particle analyzer in a wind tunnel. The results show that the probability distribution of lift-off velocity can be expressed as a lognormal function, while that of lift-off angle follows an exponential function. The probability distribution of lift-off angle conditioned for each lift-off velocity also follows an exponential function, with a slope that becomes steeper with increasing lift-off velocity. This implies that the probability distribution of lift-off velocity is strongly dependent on the lift-off angle. However, these lift-off parameters are generally treated as an independent joint probability distribution in the literature. Numerical simulations were carried out to investigate the effects of conditional versus independent joint probability distributions on the vertical sand mass flux distribution. The simulation results derived from the conditional joint probability distribution agree much better with experimental data than those from the independent ones. Thus, it is better to describe the lift-off velocity of saltating sand particles using the conditional joint probability distribution. These results improve our understanding of saltation processes in wind-blown sand.

CONTROL OF TWO DIMENSIONAL JETS USING MINIATURE ZERO MASS FLUX JETS

Zero mass flux jets, synthesized by acoustic actuators, have been used for the purpose of jet mixing enhancement and jet vectoring. Zero mass flux jets composed of entirely entrained fluid allow momentum transfer into the embedding flow. In the present experiments, miniature scale high aspect ratio actuator jets are placed along the long sides and near the exit plane of a primary two dimensional jet. In different modes, the primary jet can be vectored either towards or away from the actuator jets and the jet mixing is enhanced. The disturbance of the excitation frequency is developed while the unstable frequency of the primary jet is completely suppressed.

Heat and mass flux estimation of modern seafloor hydrothermal activity

Research on heat and mass flux yielded by modern seafloor hydrothermal activity is very important, because it is involved not only in the base of ocean environment research, but also in the historical evolution of seawater properties. Currently, estimating heat flux is based on the observation data of hydrothermal smokers, low-temperature diffusive flow and mid-ocean ridge mainly. But there are some faults, for example, there is lack of a concurrent conductive item in estimating the heat flux by smokers and the error between the half-space cooling model and the observation data is too large. So, three kinds of methods are applied to re-estimating the heat flux of hydrothermal activity resepectively, corresponding estimation is 97. 359 GW by hydrothermal smoker and diffusive flow, 84.895 GW by hydrothermal plume, and 4. 11 TW by exponential attenuation method put forward by this paper. Research on mass flux estimation is relatively rare, the main reason for this is insufficient field observation data. Mass fluxes of different elements are calculated using hydrothermal vent fluid data from the TAG hydrothermal area on the Mid-Atlantic Ridge for the first time. Difference of estimations by different methods reflects the researching extent of hydrothermal activity, and systematically in - situ observation will help to estimate the contribution of hydrothermal activity to ocean chemical environment, ocean circulation and global climate precisely.

MODIFIED MASS FLUX CUMULUS CONVECTIVE PARAMETERIZATION SCHEME AND ITS SIMULATION EXPERIMENT—PART Ⅰ:MASS FLUX SCHEME AND ITS SIMULATION OF THE 1991 FLOOD EVENT

Based on the existing cumulus convective parameterization schemes,a mass flux scheme (MFS)for cumulus convective parameterization has been successfully developed by reference to the work of Chen et al.(1996).The MFS is a comprehensive scheme.In MFS,not only the importance of the large-scale moisture convergence is taken into account,but also it includes the cumulus updrafts and downdrafts,cumulus-induced subsidence in the environmental air. entrainment,detrainment and evaporation.The interaction between the cumulus and the environment is described by using a one-dimensional bulk model.At the same time the scheme includes the penetrative and shallow convections. The MFS has been successfully incorporated into the regional climate model RegCM2 developed by NCAR.The new model has been applied to simulate summer monsoon characteristics and their variations of heavy rainfall process in the Changjiang-Huaihe River Basins for three months from May to July 1991.The results show that the new model can successfully simulate this rainfall prolonged process.By comparising the model outputs of RegCM2.using the Kuo scheme and the MFS.it is found that the MFS is better in simulating the surface temperature,rainfall position and amount,and rainfall duration.

MODIFIED MASS FLUX CUMULUS CONVECTIVE PARAMETERIZATION SCHEME AND ITS SIMULATION EXPERIMENT—PART II:CUMULUS CONVECTION ACTIVITIES SIMULATED FROM THREE SCHEMES AND SENSITIVITY EXPERIMENTS BY USE OF MASS FLUX SCHEME

By comparison of simulated cumulus convection processes in RegCM2,using the Kuo scheme, the Grell scheme and the mass flux scheme (MFS),it is found that the MFS can simulate the cumulus heating and moistening very well.A series of sensitivity tests show that the parameters for specifying the conversion coefficient from cloud droplets to raindrops,the turbulent entrainment and detrainment rates in updrafts anddowndrafts,and the intensity of thedowndrafts have different degrees of influence upon the cumulus convection.Therefore.it is quite important for cumulus parameterization scheme to define these parameters as accurately as possible.

Flow and heat transfer of nanofluid over an exponentially shrinking porous sheet with heat and mass fluxes

Steady boundary layer flow of nanofluid past an exponentially porous shrinking sheet in presence of heat and mass fluxes is presented.In this model the combined effects of Brownian motion and thermophoresis on heat transfer and nanoparticle volume fraction are considered.Similarity transformations are used to obtain the self-similar equations which are then solved numerically using shooting technique along with fourth order Runge-Kutta method.Similarity solution depends on the suction parameter.This investigation reveals that the variable heat flux and mass flux have major significant effects on temperature field and the nanoparticle volume fraction.The wall mass transfer through the porous sheet causes an increase of fluid velocity for the first branch of solution.Temperature as well as nanoparticle volume fraction decreases for both branches of solutions.For the Brownian motion,the temperature increases but the nanoparticle volume fraction decreases.Heat transfer rate becomes lower with the increase of Lewis number.Due to increase in thermophoresis parameter,both the temperature and nanoparticle volume fraction increase.

Re-evaluating the vertical mass-flux profiles of aeolian sediment at the southern fringe of the Taklimakan Desert, China

Reliable estimation of the mass-flux profiles of aeolian sediment is essential for predicting sediment transport rates accurately and designing measures to cope with wind-erosion. Vertical mass-flux profiles from seventeen wind-erosion events were re-evaluated using five typical models based on observed data obtained from a smooth bare field at the southern fringe of the Taklimakan Desert, China. The results showed that the exponential-function model and the logarithmic-function model exhibited the poorest fit between observed and predicted mass-flux profiles. The power-function model and the modified power-function model improved the fit to field data to an equivalent extent, while the five-parameter combined-function model with a scale constant（σ） of 0.00001 m（different from the σ value proposed by Fryear, which represented the height above which 50% of the total mass flux occurred） was verified as the best for describing the vertical aeolian sediment mass-flux profiles using goodness of fit（R2） and the Akaike Information Criterion（AIC） values to evaluate model performance. According to relationships among model parameters, the modified power model played a prominent explanatory role in describing the vertical profiles of the observed data, whereas the exponential model played a coordinating role. In addition, it was found that the vertical profiles could not be extrapolated using the five selected models or easily estimated using an efficient model without field observations by a near-surface sampler at 0 to 0.05 m.

Development and improvement of mass flux convection parameterization scheme and its applications in the seasonal climate predication model

The features of Gregory cumulus parameterization scheme, which is used in British Weather Office, are researched and then this scheme is developed and improved according to the characteristics of area precipitation over China. Firstly, the influence of the large-scale convergence in lower tropopause upon cumulus convection is directly taken into account in a 揵ulk?cloud model. The organized entrainment and detrainment is considered in the model. Secondly, the initial mass flux is revised. Thirdly, the effects of subcooling water upon saturation vapour pressure are considered. Eventually, the drown-draft air is regulated. For several years, the numerical forecast of seasonal precipitation in China has been carried out by using the modified Gregory scheme. The result shows that the model with improved Gregory scheme well simulates the precipitation over China and the prediction result is good.

WATER MASS FORMATION IN THE SOUTH INDIAN OCEAN BY AIR-SEA FLUXES

Indian Central Water （ICW） and Subantarctic Mode Water （SAMW） formation rates are estimated from two air-sea flux products, the Comprehensive Ocean-Atmosphere Data Set （COADS） and the Southampton Oceanography Centre （SOC） climatology. The ICW formation is estimated to be 8 Sv (1 Sv = 106m3·s-1 ) from both products, with more contributions from freshwater flux. From the COADS product, the SAMW formation rate is estimated to be 31 Sv in the potential density range of 26.5-26.9σθ, with also a significant contribution from freshwater flux. However, the SAMW formation rate estimated from the SOC product is much smaller, which may be due to bias of the SOC heat flux. Poorer quality of the flux products in the Southern Ocean may also contribute to the difference.

Numerical Solution of MHD Convection and Mass Transfer Flow of Viscous Incompressible Fluid about an Inclined Plate with Hall Current and Constant Heat Flux

The present numerically study investigates the influence of the Hall current and constant heat flux on the Magneto hydrodynamic (MHD) natural convection boundary layer viscous incompressible fluid flow in the manifestation of transverse magnetic field near an inclined vertical permeable flat plate. It is assumed that the induced magnetic field is negligible compared with the imposed magnetic field. The governing boundary layer equations have been transferred into non-similar model by implementing similarity approaches. The physical dimensionless parameter has been set up into the model as Prandtl number, Eckert number, Magnetic parameter, Schmidt number, local Grashof number and local modified Grashof number. The numerical method of Nactsheim-Swigert shooting iteration technique together with Runge-Kutta six order iteration scheme has been used to solve the system of governing non-similar equations. The physical effects of the various parameters on dimensionless primary velocity profile, secondary velocity profile, and temperature and concentration profile are discussed graphically. Moreover, the local skin friction coefficient, the local Nusselt number and Sherwood number are shown in tabular form for various values of the parameters.

Particle flux through the Huanghai Sea cold water mass

Settling particulate matter （SPM） was collected by using sediment traps at four stations in a survey section from Qingdao to Cheju-do, across the Huanghai Sea cold water mass （HSCWM）, in August 2002. The sediment traps were planted in three layers： the upper layer of the thermocline （ULT） above the HSCWM, the lower layer of the thermocline （LLT）, and the bottom layer of water column （BL）. To determine the particle flux, the contents of organic carbon （POC）, organic nitrogen （PON）, total carbon （PC）, and total phosphorous （PP） in SPM were analyzed, and two flux models （Ⅰ and Ⅱ） were improved to calculate the resuspension ratio, with an assumption in Model Ⅰ that the vertical flux of SPM in the LLT equals the net vertical flux of SPM in the whole water column. An X value, i.e., the fraction of the resuspension flux originating from the surficial sediments nearby the sampling station, was deduced from Model Ⅰ to estimate the contribution of lateral currents to the total resuspension flux. The results showed that inorganic particles, fecal pellets, and miscellaneous aggregates were the major types of SPM in the HSCWM, and the contents of POC, PON, PC, and PP all decreased with water depth. A great deal of fecal pellets found in the LLT indicates that the main space producing biogenic SPM is the thermocline, and especially the LLT, where the C/N ratio is lower than that in the ULT. The resuspension ratios, 90%-96% among stations, imply strong impact ofresuspension on particle flux in the BL. These values were not significantly different between the two flux models, suggesting that the hypothesis in Model Ⅰ that the flux in the LLT equaling the net flux to the bottom is acceptable for shallow waters with stratification like the HSCWM. The POC export ratio from the HSCWM ranges from 35% to 68%. It benefits from the short sinking distance in shallow water. The upwelling in the HSCWM enhanced the POC flux through the water mass, and the lateral currents provides up to being greater than 50% ofresuspension flux in the BL according to evaluation of the X value.

零质量射流下波浪前缘叶片气动性能数值研究

针对垂直轴风机叶片大攻角工况下因流动分离导致的失速及颤振抖振问题,引入零质量射流激励对波浪型前缘叶片进行流动分离控制.采用大涡模拟方法建立了波浪前缘叶片绕流数值模型,探究了主/被动耦合控制下叶片升阻力特性及其流动分离机理,分析了射流参数(射流位置、动量系数)对波浪前缘叶片气动性能及失速特性的影响机制,研究发现:受控前后大攻角下波浪型前缘能诱导产生较小尺度流向涡,降低后方大分离涡尺度,波浪前缘与零质量射流耦合控制对于大攻角下流动分离抑制较单一控制更优;零质量射流吹气时使前缘流向涡有更高的动能抵抗逆压梯度从而延迟流动分离,吸气时会吸走流向涡的低动量流体,抑制流向涡发展成大分离涡;射流布置在距基准前缘0.033c处,即位于前缘流向涡最前端,能最大程度地参与前缘流向涡的生成,升阻比的提升效果最好;且升阻比提升量随着动量系数增大而增大,但控制经济性在动量系数0.018时最优,研究结果为垂直轴风力机失速控制提供了有益参考.

深时源-汇系统要素的常用定量分析方法

源-汇系统研究是构造地质学、沉积学和层序地层学的综合,因其整体性、动态化和半定量-定量的特点受到了广泛关注。首先阐述了目前深时(前第四纪)源-汇系统的关键问题是物质平衡的定量表征及搬运过程对沉积物的控制,由于地层记录缺失和参数获取困难等原因,研究仍极具挑战。随后综述了深时源-汇系统定量分析方法,可分为地质年代学法、将今论古法和沉积学法。各方法通过获取地貌要素、水力学参数、侵蚀速率、沉积通量等信息,建立“源”“汇”之间的定量关系,进而重建盆地沉积充填演化史。通过系统介绍不同方法的基本原理、相关参数,对比其优越性及局限性,认为地质年代学法应用较广,核心在于物源示踪;将今论古法关键是地质背景的类比及地质参数的选择;沉积学法受多变量控制,需兼顾构造-气候背景及研究尺度。最后对深时源-汇系统定量分析的发展进行了展望,在“将今论古”这一重要思想指导下,需着眼于物源体系、沉积物搬运路径、沉积物分配关系、系统内的各要素及其耦合作用,需注重多时间尺度的定量表征、多学科交叉的动态研究。而相较于大陆边缘源-汇系统,陆相湖盆源-汇系统模式与预测模型有待进一步完善。

Characterization of Rayleigh Convection in Interfacial Mass Transfer by Lattice Boltzmann Simulation and Experimental Verification

Concentration gradient induced Rayleigh convection can influence effectively interracial mass transfer processes, but the convection phenomena are known as mesoscopic and complex. In order to investigate this phenomenon, a two-equation Lattice Boltzmann Method （LBM） is proposed to simulate the velocity and the concentra-tion distributions of Rayleigh convection generated in the CO2 absorptlon into ethanol liquid.The simulated results on velocity distributions are experimentally verified by PIV （particle image velocimetry technique） measurements. In order to simplify the analysis, the convection in the simulation as well as in the experiment, the Rayleigh convection was manipulated into a single down flow pattern, The simulated results show that the concentration contours agree qualitatively with the schlieren images in the literature. The experimental and simulated results show that theRayleigh convection under investigation is dominated by the flow in the downward direction and impels exchange of the liquid between the interfacial vicinity and the liquid bulk promoting the renewal of interfacial liquid, and hence enhances mass transfer. The comparison between the simulated and experimental results demonstrated that the proposed LBM is a promising alternative for simulating mass transfer induced Rayleigh convection.

垂直管内高质量流速超临界CO_(2)换热特性

利用已有的流动传热实验数据,对不同湍流模型预测超临界CO_(2)(S-CO_(2))传热能力进行了评价及选取,确定了SST k-ω湍流模型为最优模型。分析了入口温度、热流密度、质量流速、浮升力和流动加速效应对内径为10mm的垂直加热管内S-CO_(2)的对流传热特性的影响。结果表明:在一些工况条件下Bu<10^(-5)、Bu^(*)<5.6×10^(-7)和K_(v)<3×10^(-6)并不满足,表明浮升力和流动加速度效应并不能解释高质量流速下的数值模拟结果。基于超临界类沸腾理论,建立了垂直加热管内S-CO_(2)类沸腾传热模型,并阐述了S-CO_(2)传热恶化现象,径向方向上S-CO_(2)热物性和湍流的详细分布表明超临界传热受类气膜的厚度、类气膜的热性质和近壁区湍流动能的影响很大,成功解释了SCO_(2)在高质量流速下的传热机理。最后引入超临界沸腾数SBO,提出了适用高质量流速的传热关联式。

A discrete model for prediction of radon flux from fractured rocks

Prediction of radon flux from the fractured zone of a propagating cave mine is basically associated with uncertainty and complexity. For instance, there is restricted access to these zones for field measure- ments, and it is quite difficult to replicate the complex nature of both natural and induced fractures in these zones in laboratory studies. Hence, a technique for predicting radon flux from a fractured rock using a discrete fracture network （DFN） model is developed to address these difficulties. This model quantifies the contribution of fractures to the total radon flux, and estimates the fracture density from a measured radon flux considering the effects of advection, diffusion, as well as radon generation and decay. Radon generation and decay are classified as reaction processes. Therefore, the equation solved is termed as the advection-diffusion-reaction equation （ADRE）. Peclet number （Pe）, a conventional dimensionless parameter that indicates the ratio of mass transport by advection to diffusion, is used to classify the transport regimes. The results show that the proposed model effectively predicts radon flux from a fractured rock. An increase in fracture density for a rock sample with uniformly distributed radon generation rate can elevate radon flux significantly compared with another rock sample with an equivalent increase in radon generation rate. In addition to Pe, two other independent dimensionless parameters （derived for radon transport through fractures） significantly affect radon dimensionless flux. Findings provide insight into radon transport through fractured rocks and can be used to improve radon control measures for proactive mitigation.

基于传热传质理论的路面除冰盐融冰过程及影响因素分析

为了解决不同环境下路面除冰盐的科学有效使用问题,降低由于除冰盐的滥用导致路面病害与环境污染,从路面除冰盐融冰传热传质机理出发,建立道路除冰盐融冰过程中的物质平衡方程与热通量平衡方程。采用COMSOL有限元软件建立了路面除冰盐融冰温度场模型,考虑多种因素如相变过程、风速、初始温度和太阳辐射的影响,分析融冰过程中温度场的变化规律。研究结果表明:在融冰过程中,盐溶液温度呈现先快速下降后缓慢回升的规律,在固态除冰盐完全溶解的时间段内(Ⅰ阶段),盐溶液温度迅速下降;除冰盐完全溶解后(Ⅱ阶段),盐溶液温度缓慢回升。外界环境温度的上升使得单位质量除冰盐的融冰体积增加,且外界环境温度相比风速和除冰盐用量对盐溶液最终温度的影响更大。风速越高,固体盐溶解溶解所需时间越短,Ⅰ阶段结束后盐溶液体系的温度也更低,盐溶液温度随之下降得更快。由于风速增大将加快盐溶液层与外部环境的换热,除冰盐融冰Ⅱ阶段升温明显,溶解后盐溶液的平均温度更高。另外,较高的除冰盐初始温度可以促进固态盐的溶解,且温度越高,这种促进作用更加明显。同时,随着反应初始温度的增加,融冰反应的终止温度也随之升高。除此之外,研究发现,太阳辐射对于除冰盐融冰过程的影响在Ⅰ阶段不显著,在Ⅱ阶段具有显著影响。研究结论可为道路冬季路面除冰盐的科学有效使用提供技术支撑与理论参考。

胶州湾大气降水水溶性离子组成特征及来源解析

基于2019年6月至2020年8月胶州湾沿岸的大气降水样品,分析降水主要水溶性离子(Na^(+)、K^(+)、Ca^(2+)、Mg^(2+)、NH^(4+)、F-、Cl^(-)、SO_(4)^(2-)、NO_(3)^(-)、MAS-(甲基磺酸根))的组成特征和湿沉降通量,评估其对近海营养成分输入的贡献和潜在生态效应,并利用气团后向轨迹和正定矩阵因子分解法(PMF)解析其主要来源.结果表明,观测期间,胶州湾大气降水雨量加权平均(Volume-weighted Mean,VWM)pH为6.41,电导率的VWM值为19.3μS/cm,降水中水溶性离子以Na^(+)、NH^(4+)、NO_(3)^(-)、Cl^(-)和SO_(4)^(2-)为主,在季节上呈现出冬春季浓度明显高于夏秋季的特征,而湿沉降通量则因受降水量的控制而主要集中在夏季(约占55%).胶州湾区域大气降水共清除7274.6t水溶性离子,营养盐(主要为NH^(4+)和NO_(3)^(-),以氮计)沉降入海量达951.9t/a,表明降水在清洁大气的同时也加剧了海洋环境的污染和海洋生态系统的失衡.气团后向轨迹分析得到了观测期间控制胶州湾降水的4类主要气团,在不同季节,降水过程受到不同气团的影响,其中以来自华东地区和东北方向的气团的影响较大.基于PMF的源解析结果显示,胶州湾大气降水水溶性离子受到农业源、海洋源、扬尘源、生物质和垃圾燃烧源、工业和交通源5种来源的共同控制,其中以农业源排放的贡献最为突出(26.7%),而其他4种源的贡献大致相当.研究证实胶州湾大气环境受到复杂人为源排放、矿物沙尘以及海洋源排放的综合制约,而人为排放的贡献占主导地位.

混合澄清槽中硝酸传质对分散相存留分数的影响

混合澄清槽是一种重要的液-液萃取设备,分散相存留分数是混合澄清槽混合室中的一个重要水力学参数。传质条件下分散相存留分数的变化情况是一个重要的研究方向。针对2套不同尺寸的混合澄清槽开展了水力学和硝酸传质实验。获得了水力学条件下泵轮转速、两相流比、料液停留时间对于分散相存留分数影响的实验结果。在传质条件下,发现2套混合澄清槽的级效率均>90%。该研究条件下传质通量集中在10-5~10-4数量级,在该数量级上传质通量很难对水力学性能产生影响,上述计算结果解释了传质条件下分散相存留分数未出现明显变化的根本原因。

长湖地下水排泄及其携带营养盐通量的季节性变化

为揭示地下水对湖泊水量和营养盐平衡的贡献及季节性变化,以长江中游的长湖为研究对象,通过丰、枯水期野外采样,结合电导率(EC)、稳定同位素(~2H和^(18)O)、水化学元素(Ca^(2+)、Mg^(2+))和氡(^(222)Rn)同位素对湖底地下水排泄(lacustrine groundwater discharge,简称LGD)进行了多手段示踪,并基于^(222)Rn质量平衡模型量化了不同季节的LGD及其携带的营养盐通量。结果显示:丰、枯水期LGD速率分别为64.52 mm/d和14.95 mm/d,丰水期显著大于枯水期;丰、枯水期地下水携带的总氮(TN)输入通量分别为25.68×10^(6) g/d和5.58×10^(6) g/d,总磷(TP)输入通量分别8.14×10^(6) g/d和0.17×10^(6) g/d。丰、枯水期LGD强度的差异导致了地下水携带TN、TP输入的差异,丰水期TP的输入量还受该时期农业活动的影响;丰水期较强的降水和蒸发驱动了更大的LGD强度及其携带的TN、TP通量。本研究可为长湖区域水资源管理和水生态保护提供重要理论依据。