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mixing

mixing的相关文献在1989年到2022年内共计153篇,主要集中在肿瘤学、数学、化学 等领域,其中期刊论文133篇、专利文献20篇;相关期刊72种,包括地学前缘、中国科学、金属学报:英文版等; mixing的相关文献由441位作者贡献,包括高天寒、Tomomi Uchiyama、Akira Ishikawa等。

mixing—发文量

期刊论文>

论文:133 占比:86.93%

专利文献>

论文:20 占比:13.07%

总计:153篇

mixing—发文趋势图

mixing

-研究学者

  • 高天寒
  • Tomomi Uchiyama
  • Akira Ishikawa
  • Bhrigunandan Prasad Singh
  • Devendra Adhikari
  • Indu Shekhar Jha
  • Jay R. Yablon
  • Jianping Yuan
  • Jitendra Kumar
  • Kazuhisa Nishizawa
  • 期刊论文
  • 专利文献

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    • Jia YOU; Zhenhua XU; Robin ROBERTSON; Qun LI; Baoshu YIN
    • 摘要: Upper ocean mixing plays a key role in the atmosphere-ocean heat transfer and sea ice extent and thickness via modulating the upper ocean temperatures in the Arctic Ocean.Observations of diffusivities in the Arctic that directly indicate the ocean mixing properties are sparse.Therefore,the spatiotemporal pattern and magnitude of diapycnal diffusivities and kinetic energy dissipation rates in the upper Arctic Ocean are important for atmosphere-ocean heat transfers and sea ice changes.These were first estimated from the Ice-Tethered Profilers dataset(2005–2019)using a strain-based fine-scale parameterization.The resultant mixing properties showed signifi cant geographical inhomogeneity and temporal variability.Diapycnal diff usivities and dissipation rates in the Atlantic sector of the Arctic Ocean were stronger than those on the Pacific side.Mixing in the Atlantic sector increased significantly during the observation period;whereas in the Pacific sector,it weakened before 2011 and then strengthened.Potential impact factors include wind,sea ice,near inertial waves,and stratifi cation,while their relative contributions vary between the two sectors of the Arctic Ocean.In the Atlantic sector,turbulent mixing dominated,while in the Pacific sector,turbulent mixing was inhibited by strong stratification prior to 2011,and is able to overcome the stratifi cation gradually after 2014.The vertical turbulent heat fl ux constantly increased in the Atlantic sector year by year,while it decreased in the Pacific sector post 2010.The estimated heat flux variability induced by enhanced turbulent mixing is expected to continue to diminish sea ice in the near future.
    • Aixiang Wu; Zhuen Ruan; Jiandong Wang
    • 摘要: Cemented paste backfill(CPB)has been one of the best practical approaches for tailings management and underground goaf treatment.Paste rheology is a science to study the flow and deformation behaviors of paste or filling body under the effects of stress,strain,temperature,and time during the CPB process.The goal of studying paste rheology is to solve the engineering problems existing in four key processes;that is,paste rheology should meet the engineering demands of thickening,mixing,transportation,and backfilling.However,paste rheology is extremely complicated due to its high concentration,materials complexity,and engineering characteristics of non-stratification,nonsegregation,and non-bleeding.The rheological behavior of full tailings in deep thickening,rheological behavior of paste in mixing and pipeline transportation,and rheological behavior of filling body are introduced and discussed:(1)gel point,compressive yield stress,and the hindered settling function are adopted to characterize the rheological properties of full tailings in deep thickening.Combination of Coe-Clevenger theory and Buscall-White theory can also analyze the thickening performance in the whole area of deep cone thickener;(2)yield stress and viscosity are consistent with the evolution trend of the relative structure coefficient of paste in mixing;(3)coupling effect of wall slip and time-temperature dependency has a significant influence on the rheological properties and pipeline transportation;(4)damage variable is introduced to the Burgers model to describe the creep damage of the filling body.However,in-depth and systematic studies were still needed to establish a complete theoretical system of paste rheology in metal mines.
    • Jun ZHAO; Fan WANG; Shan GAO; Yinglin HOU; Kai LIU
    • 摘要: To quantitatively investigate the water mass transport of mesoscale eddies,the mass transport induced by a simulated anticyclonic eddy in the South China Sea was evaluated by using the Regional Ocean Modelling System(ROMS)and a built-in passive tracer module.The results indicate that the eddy can trap and transport 51%of the initial water in the eddy core to 689 km from its origin during its lifetime of 100 days,with a stable loss rate of 6‰per day.During propagation,there is drastic horizontal water exchange between the inside and outside of the eddy.Meanwhile,the vertical mass transport is signifi cant,and 65%of the water initially in the mixed layer of the eddy is eventually detrained into the subsurface.A tracer budget analysis of eddy shows that advection is the dominant dynamic process of transport,while the eff ect of mixing is weak,and horizontal process plays a controlling role.Horizontal and vertical advection exhibit opposite patterns and strongly off set each other.Particularly,a distinct dipole pattern is found in the local velocity fi eld of the eddy,with signifi cant convergence(downwelling)and divergence(upwelling)zones in the anterior and posterior of the eddy,respectively,which is likely related to the driving mechanism of the westward propagation of the eddy.The dipole further induces a vertical overturning cell,through which the surface water in the anterior of the eddy detrains into the subsurface by downwelling and resurface from the posterior of the eddy by upwelling and gradually spreads out of the eddy.The temporal variability in the tracer budget is signifi cant,in which horizontal advection is dominant.The propagation acceleration and temporal derivative of the deformation rate are highly correlated with tracer transport,suggesting the potential eff ect of the temporal instability of eddies on the eddy mass transport.
    • Fang Yang; Wei Zhao; Guiren Wang
    • 摘要: Electrokinetic(EK)micromixers have been widely studied in the past decade for biochemical applications,biological and chemical analysis,etc.Unfortunately,almost all EK mixers require different electrical conductivity between the two fluids to be mixed,which has greatly limited their wide applications,in cases where the two streams to be mixed have equivalent electrical conductivity.Here we show that mixing enhancement between two fluids with identical conductivity can be achieved in an EK micromixer with conductive sidewalls,where the electric field is in transverse direction of the flow.The results revealed that the mixing became stronger with increased conductivity value.This mixing method provides a novel and convenient strategy for mixing two liquids with the same or similar electrical conductivity in microfluidic systems,and could potentially serves as a powerful tool for sample preparation in applications such as liquid biopsy,and environmental monitoring,etc.
    • AUGUSTO SOTO
    • 摘要: ther than being forced to take sides among major countries, what Asia-pacific needs now is pragmatic cooperation in addressing pressing development issues.DURING his May tour of the Republic of Korea (ROK) and Japan, mixing up secu-rity and trade, U.S. President Joe Biden made some announcements based on an a ssumption. So is his administration’s criticism of Chinese State Councilor and Foreign Minister Wang Yi’s recent visit to eight Pacific island countries.
    • Inass A.Al-Mallah; Wasan S.Al-Qurnawi; Hussein B.Ghalib; Adnan B.Al Hawash; Mariam H.Abdulameer
    • 摘要: The Dibdibba aquifer is considered to be the main source in the Al-Zubair area because agriculture depends on it to provide grazing water in the area.The groundwater well samples were collected from the shallow Dibdibba Aquifer in Basra Province,southern Iraq,through the dry and wet period for 37 water samples were collected,to investigate the water quality deterioration,which is a hydrogeochemical modeling study where used to represent the groundwater mixing evaluation.The physicochemical parameter results show the spatial and temporal variations along the groundwater flow path.A Durov diagram of the studied samples shows water type Na-SO_(4),which is represented by mixing waters that may be affected by dissolution.Inverse geochemical model ratio results of the groundwater well samples have shown high mixing ratios in the east and southeast regions of the study area.The stable isotope composition of groundwater samples indicated that the recharge source of the Dibdibba aquifer is meteoric water influenced by vapor water from the Arabian Gulf.The stable isotope results have shown that the enrichment ofδO values is relatively linked with high salinity concentration and indicated the mixing between the upper unconfined and the lower confined,especially in the eastern and southern parts of the study area.These findings of geochemical modeling and isotopes indicated an increasing groundwater quality deterioration.Thus,we recommended avoiding these areas for intensive extraction of groundwater.
    • Dongyi Wei
    • 摘要: In this paper, we first present a Gearhart-Pruss type theorem with a sharp bound for m-accretive operators. Then we give two applications:(1) we give a simple proof of the result proved by Constantin et al. on relaxation enhancement induced by incompressible flows;(2) we show that shear flows with a class of Weierstrass functions obey logarithmically fast dissipation time-scales.
    • Hong-bo Cai; Xin-xin Yan; Pei-lin Yao; Shao-ping Zhu
    • 摘要: Shock-driven hydrodynamic instabilities in a plasma usually lead to interfacial mixing and the generation of electromagnetic fields,which are nonequilibrium processes coupling kinetics with meso-and macroscopic dynamics.The understanding and modeling of these physical processes are very challenging tasks for single-fluid hydrodynamic codes.This work presents a new framework that incorporates both kinetics and hydrodynamics to simulate shock waves and hydrodynamic instabilities in high-density plasmas.In this hybrid code,ions are modeled using the standard particle-in-cell method together with a Monte Carlo description of collisions while electrons are modeled as a massless fluid,with the electron heat flux and fluid–particle energy exchange being considered in the electron pressure equation.In high-density plasmas,Maxwell’s equations are solved using Ohm’s law instead of Ampere’s law.This hybrid algorithm retains ion kinetic effects and their consequences for plasma interpenetration,shock wave propagation,and hydrodynamic instability.Furthermore,we investigate the shock-induced(or gravity-induced)turbulent mixing between a light and a heavy plasma,where hydrodynamic instabilities are initiated by a shock wave(or gravity).This study reveals that self-generated electromagnetic fields play a role in the formation of baroclinic vorticity along the interface and in late-time mixing of the plasmas.Our results confirm the ability of the proposed method to describe shock-driven hydrodynamic instabilities in a plasma,in particular,nonequilibrium processes that involve mixing and electromagnetic fields at the interface.
    • YiPeng Jing
    • 摘要: The self-interacting dark matter(SIDM)model is an ideal candidate for explaining the discrepancy between small-scale structure observations and predictions by the prevailing collisionless cold dark matter(CDM)model.SIDM indicates the existence of a light mediator with a typical mass of 10 MeV.Searching for SIDM particles has therefore become one important alternative to the traditional weakly interacting massive particles(WIMPs)in direct detection experiments such as PandaX.Of note,the constraints obtained from direct detections are associated with the unknown mixing parameter(such as photon kinetic mixing)that describes the strength of the coupling between the mediator and ordinary particles。
    • Jinfeng Ma; Hailong Liu; Pengfei Lin; Haigang Zhan
    • 摘要: The effects of biological heating on the upper-ocean temperature of the global ocean are investigated using two ocean-only experiments forced by prescribed atmospheric fields during 1990–2007,on with fixed constant chlorophyll concentration,and the other with seasonally varying chlorophyll concentration.Although the existence of high chlorophyll concentrations can trap solar radiation in the upper layer and warm the surface,cooling sea surface temperature(SST)can be seen in some regions and seasons.Seventeen regions are selected and classified according to their dynamic processes,and the cooling mechanisms are investigated through heat budget analysis.The chlorophyll-induced SST variation is dependent on the variation in chlorophyll concentration and net surface heat flux and on such dynamic ocean processes as mixing,upwelling and advection.The mixed layer depth is also an important factor determining the effect.The chlorophyll-induced SST warming appears in most regions during the local spring to autumn when the mixed layer is shallow,e.g.,low latitudes without upwelling and the mid-latitudes.Chlorophyll-induced SST cooling appears in regions experiencing strong upwelling,e.g.,the western Arabian Sea,west coast of North Africa,South Africa and South America,the eastern tropical Pacific Ocean and the Atlantic Ocean,and strong mixing(with deep mixed layer depth),e.g.,the mid-latitudes in winter.
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