Univ.-Prof. Dr.-Ing. habil. Claus Wagner
Head of Group
Frau Colette Wilhelm
Secretary
+49 3677 69 2410
Turbulent Rayleigh-Bénard (RB) convection is frequently used as a canonical model for describing flow phenomena and convective heat transfer in the Earth's atmosphere or in the oceans. In addition to these geophysical flows, however, the model is also applied in the study of indoor airflows or the maintenance of temperature stratification in heat storage systems with liquid media. For a long time, scientific research focused almost exclusively on predicting the global and time-averaged heat flux through the fluid layer heated from below and cooled from above. However, current research questions, such as the dispersion of solid particles or aerosols in the atmosphere or the natural mixing of air in indoor spaces, also require knowledge of the large-scale flow patterns in such convection-driven flows. In the research project proposed here, the global circulation flow in fully turbulent RB convection will be investigated experimentally, with a particular focus on the influence of the aspect ratio Γ (Γ – ratio of the lateral to the vertical extent of the experimental chamber) on the resulting flow pattern. Analogous to the majority of convection-driven flows occurring in nature or engineering, the focus will be on “large” aspect ratios between Γ=2 and Γ=10. The test chamber used is the so-called “Ilmenau barrel,” a large-scale Rayleigh-Bénard experiment (diameter: 7.1 m, height: 0.2…6.3 m) located at the Department of Aerodynamics at the Technical University of Ilmenau. In this facility, Rayleigh numbers up to Ra=10¹² can be achieved. The flow field in the air-filled experimental chamber will be measured using the Lagrangian particle tracking method, and the flow patterns occurring at different aspect ratios will be analyzed. The particular advantage of the planned experimental work lies in a significantly longer observation time compared to direct numerical simulations. This is accompanied by a significant improvement in the statistical accuracy of predictions. In addition to addressing questions regarding the nature of the flow patterns and their typical lifetimes, the proposed research project will also investigate how virus- or pollutant-laden aerosols are distributed in turbulent convective flows as a function of these flow patterns.
Funding Agency: DFG
Period
: January 1, 2025 – December 31, 2027
Principal Investigator:
Thermal convection on a rough or structured surface is a physical process that reflects reality much better in many problems, e.g. in technical systems for heat transfer, in the cooling of electronic components or in research into the urban climate, than the models usually used with smooth surfaces are able to do. Although there have been a large number of publications on this problem in the past, the local transport processes in the immediate vicinity of such a structured wall in particular are still largely misunderstood. This lack is due to the fact that there are only very few convection experiments in which the transport quantities near the wall can be measured with an adequate spatial and temporal resolution and that the computational effort for direct numerical simulations is currently still disproportionately high.
In the planned research project, the local velocity and temperature field during convective heat transfer on a rough surface is to be measured in the "Ilmenau Barrel" convection experiment. Due to the large dimensions of the convection cell, with a diameter of 7.1 m and a total height of 8.0 m, these measurements can be carried out at very high Rayleigh numbers up to Ra = 10^{12}. At the same time, the spatial resolution of these measurements is so high that the functional relationships sought in the fluid layer near the wall can be validated with sufficient certainty. In the course of the research project, different types of roughness patterns are to be investigated, including both uniform and staggered structural elements.
As a result of these investigations, the scientists want to assess in particular the relevance of various flow phenomena, such as the increase in the rate of emitted plumes, the "thinning" of the thermal boundary layer at the surface of the structural elements or the local transition of the convective boundary layer to turbulence, to the changes in convective heat transport on a structured surface observed in the past. A further aim of the planned project is to compare the measurement data on different types of roughness patterns and to search for fundamental similarities with regard to their influence on the flow field and thus on heat transport. Ideally, this search will result in a surface model that is as universally applicable as the hydraulic roughness model for pipe and shear flows.
Funded by: DFG
Period 01.05.2022 - 31.01.2025
Researcher:
The Earth's climate and weather are significantly influenced by thermal convection currents that form in relatively shallow fluid layers, such as the Earth's atmosphere or oceans. These and many other natural and technical convective flows exhibit an aspect ratio Γ—that is, the ratio of lateral to vertical extent—of several thousand. Phenomenological theories of convective heat transport are based on this assumption and make predictions that, strictly speaking, are valid only for such systems with infinitely large lateral dimensions. However, the experimental and numerical evaluation of these theories, particularly in the range of high Rayleigh numbers, takes place almost exclusively in geometries with an aspect ratio less than or equal to one, where the side walls have a significant influence on the flow field and thus also on turbulent energy transport. In the proposed project, therefore, the convective heat flux and the dissipation rate in turbulent Rayleigh-Bénard convection (“Ilmenau barrel”) are to be measured at a large aspect ratio and simultaneously high Rayleigh number. For the first time, the convective heat flux at the surfaces of the heating and cooling plates will be measured directly and without the influence of side walls. This represents a significant qualitative advance over previous measurements, in which this quantity is typically determined from the heating power fed into the system. In addition, the applicants intend to measure the thermal dissipation rate using a miniaturized probe with four ultra-small thermistors arranged in a Cartesian configuration. Due to the size of the experimental setup—the “Ilmenau barrel” measures seven meters in diameter—even the smallest dissipative structures in the range of the Kolmogorov length scale \eta=1.1 mm and the Kolmogorov time scale \tau_eta=76 ms, and phenomenological scale theories for heat transport can be directly validated. As a special highlight of the project, it is planned to fill the “Ilmenau barrel” with sulfur hexafluoride and thereby achieve, for the first time, Rayleigh numbers on the order of Ra=10^11 at an aspect ratio of \Gamma=8.
Funding agency: DFG
Period
: October 1, 2017 – July 31, 2021
Project team:
youtu.beIn the atmospheric boundary layer near the ground, intense vortices with a vertical axis frequently form over flat terrain under convective conditions. These are known as dust devils, and it is believed that they contribute significantly to the production of continental aerosols. Very little is still known today about the origin and properties of these atmospheric vortices. In their natural environment, they are very difficult to measure, as stationary sensors provide an insufficient data set and remote sensing methods have too low a resolution. To numerically simulate such structures, models are needed that capture both the large scales of the atmospheric boundary layer and the small scales of dissipative processes. This has not yet been possible, even though Large Eddy Simulations (LES) can now compute simulation domains with more than one billion grid points and a 2-meter grid spacing.
The goal of this project is to conduct systematic numerical studies, which will be accompanied by laboratory experiments for the first time. They aim to uncover the mechanisms by which dust devils form and how they contribute to the vertical transport of heat and dust in the atmosphere. Based on the PALM (PArallelized LES Model) simulation package developed in recent years at the Institute of Meteorology and Climatology at Leibniz University Hannover, both LES and Direct Numerical Simulations (DNS) will be conducted. In parallel, laboratory experiments are being conducted at the Institute of Thermal and Fluid Dynamics at the Technical University of Ilmenau in the “Ilmenau Barrel,” an eight-meter-tall, seven-meter-diameter convection experiment. In this classic Rayleigh-Bénard experiment, in which enclosed air is heated from below and cooled from above (similar to the atmosphere), intense vortices with a vertical axis have been observed multiple times in the past under certain conditions. These are to be measured and characterized within the scope of the project. The data obtained will, for the first time, allow for a comparison and verification of the DNS in a Rayleigh number range up to 10^12. The planned LES studies for an atmospheric boundary layer will reach Rayleigh numbers up to 10^18, thereby ensuring the transferability of the results from the DNS and laboratory experiments to the atmosphere. To overcome current limitations in the numerical resolution of the simulations, the grid spacing in the near-surface region will be reduced to 0.1 m using a model nesting procedure. The problem of identifying moving vortices within the extremely large LES datasets, both during the formation phase and as they continue to develop and move, will also be addressed.
Funding Agency: DFG
Period
: January 1, 2018 – May 31, 2022
Partner:
Leibniz University Hannover, Associate Professor Dr. Siegfried Raasch
Principal Investigator:
Website:http://www.euhit.org
Period: April 1, 2013 – March 31, 2017
What is EuHIT?
EuHIT is an association whose goal is to integrate highly specialized, experimental facilities in the field of turbulence research into a European infrastructure. The aim is to strengthen the competitiveness of European turbulence research and to build a common knowledge base.
Who are we?
EuHIT currently comprises 21 partner institutions from 10 European countries. The consortium is based on 14 cutting-edge turbulence experiments, which are operated by the members and made available to other scientists for their own research. The project is coordinated by the Max Planck Institute for Dynamics and Self-Organization, represented by Prof. Eberhard Bodenschatz. He is supported by a Steering Committee and overseen by the General Assembly of members.

A three-dimensional “Particle Tracking Velocimetry” (PTV) method is being further developed to measure velocity in large-scale circulation flows and for specific applications in the “Ilmenauer Fass” convection cell.
To capture flows using optical measurement methods, artificially introduced particles (tracers) are necessary. A proven tool for visualizing transparent gas flows are helium-filled soap bubbles, which can follow the flow with virtually no slip. However, the use of ordinary soap bubbles is severely limited due to their short lifespan (1–2 minutes). For investigations of turbulent convective flows, however, measurement series ranging from several tens of minutes to several hours are necessary.
One possible solution may lie in the use of a special bubble solution designed to produce long-lasting, density-neutral, stable soap bubbles (“stubbles”). “Stubbles” are stable bubbles that can be touched, stacked, and linked together. Based on an existing laboratory model, a prototype for generating these stable soap bubbles is being further developed and optimized. After testing the stubble generator, a suitable imaging system with four digital cameras and a volumetric lighting system will be set up and tested.
Funding Body: EuHIT - European High Performance Infrastructures in Turbulence
Period
: April 1, 2013 – March 31, 2017
Project team:
The national DFG Research Group (FOR 1182) "Wall-near transport and structure formation processes in turbulent Rayleigh-Bénard, Taylor-Couette, and pipe flows" was approved by the DFG on October 24, 2012, and began its second funding period on March 1, 2013.
Information about the project
Subprojects:
RB-1: Experimental investigation of near-wall transport and structure formation processes in turbulent Rayleigh-Bénard convection
RB-2: Numerical investigation of transport and structure formation processes near the wall in turbulent Rayleigh-Bénard convection
TC-1: Experimental investigations of turbulence transition and transport processes in turbulent Taylor-Couette flows
TC-2: Transport and structure formation in Taylor-Couette flow: Theory/Simulation
RS-1: Experimental investigations of the kinematics and dynamics of transitional flow structures generated by optimized disturbances in a pipe
RS-2: Transport and structure formation in pipe flow: Theory/Simulation
Funding Agency: DFG
Period
: March 1, 2013 – February 28, 2016
Partners:
BTU Cottbus, Prof. Dr. C. Egbers
University of Marburg, Prof. B. Eckhardt
University of Erlangen, Prof. M. Avila, Dr. Ö. Ertunc
IST Austria, Prof. B. Hof
Principal Investigator:
Period:
March
1, 2013 – February 28, 2016
Abstract: |
The description of turbulent flows remains one of the greatest challenges in engineering and classical physics. The large spatial-temporal fluctuations and the strong couplings between structures on different length and time scales limit the flow velocities achievable in fully resolved calculations today and place special demands on the modeling of turbulence. Exact statements are possible only in ideal cases, such as with the Kármán–Howarth equation for velocity correlations in homogeneous isotropic turbulence or with the upper bounds on energy dissipation in simple flow geometries. The interactions between structures across many length scales dominate particularly near solid walls, as occurs in virtually all flows. Based on Prandtl’s boundary layer considerations, refined by symmetry considerations, important statements regarding the mean velocity profiles have been derived. However, when calculating global transport quantities, such as the heat flux in thermal convection at the “Ilmenau Barrel” turbulence research facility, uncertainties in the profiles and scale exponents easily lead to variations in the predictions by several orders of magnitude. |
Heat transfer from a solid surface to an adjacent fluid is relevant to a wide range of natural and engineering flow processes. Although the physical fundamentals of convective heat transfer have been studied intensively for nearly 100 years, we are still far from a comprehensive understanding of the processes involved.
Using the large-scale “Ilmenau Barrel”—a globally unique facility where turbulent convective flows can be studied with unmatched spatial and temporal resolution—this project aims to investigate the role of coherent structures in convective heat transfer. A snapshot of such a complex flow structure on the surface of a heated aluminum plate was captured using flow visualization and can be seen in the figure below.
The unique approach of the DFG Research Group FOR 1182 is to utilize mathematical analogies for describing transport processes in turbulent Rayleigh-Bénard convection, Taylor-Couette flow, and pipe flow to comparatively investigate the global scaling properties of turbulent transport as well as the local dynamic processes near the solid walls. The diagram below provides a qualitative overview of the fluid dynamics analogies in the three model flows.
Initial results providing insight into the flow structure near the wall in turbulent Rayleigh-Bénard convection are summarized in the video below. The visualization shows that, contrary to common belief, even at low Rayleigh numbers, the flow in the so-called boundary layer is not uniform and laminar but extremely unstable and complex.
Contact: Dr. Ronald du Puits
Ronald du Puits
Thermal convection is a ubiquitous process in our daily lives. The climatic conditions in our latitudes are influenced, for example, on the one hand by warm, humid air masses over the Azores, which bring us hot summer days, and on the other hand by cold, dry air masses from northern regions, which cause bitter cold in winter. The underlying processes are based on the warming of cold air over seawater or landmasses and its subsequent cooling at higher altitudes. This mechanism, known as thermal convection, is systematically studied in Rayleigh-Bénard convection cells, in which a temperature gradient similar to that in the atmosphere is generated. Of central interest here is the vertical heat transport of moving fluid packets against the force of gravity.
Using the fundamental experiments presented here in a rectangular convection cell, high-resolution heat flux images have been successfully measured for the first time (see figure above). To achieve this, a thin layer with known thermal conductivity was applied to the heated base plate, with its surface following the temperature of the flow (see diagram). When this layer is examined using an infrared camera, the surface temperature is determined, and the distribution of the wall heat flux can be calculated using Fourier’s law for heat conduction. In combination with measurements of the local flow field (small figure in the lower diagram), it was found that two counter-rotating vortices form when the main flow strikes the base plate. As a result of this effective mixing, the wall heat flux is locally increased, which is clearly visible as a red spot in the heat flux image. As the flow continues, a boundary layer forms, with convective and diffusive heat transfer processes playing a decisive role. Finally, the heated air rises, and localized pockets of hot air, known as plumes, detach from the floor slab.

Turbulent thermal convection occurs in numerous flow processes in nature and engineering. Due to its high degree of turbulence and geometric complexity, this type of flow is very difficult to predict accurately. This is due, among other things, to insufficient knowledge of the exact structure of the temperature field in the thermal boundary layers. With the large-scale “Ilmenau Barrel” facility, the Technical University of Ilmenau has a globally unique turbulence research facility at its disposal that can overcome this shortcoming. The goal of this project is to measure the structure of the two horizontal thermal boundary layers in the cylindrical air volume of the Ilmenau Barrel—heated from below and cooled from above—with unprecedented spatial and temporal resolution. To this end, for variable Rayleigh numbers and aspect ratios, the profiles of temperature, temperature fluctuation, skewness, and kurtosis will be measured at several points on the heating plate and systematically compared with analogous measurements on the cooling plate. These investigations have been made possible by a precision heating plate approved in 2005 as a DFG major instrument. They are methodologically enhanced by the use of a novel micro-temperature sensor, which allows for spatial resolution that is nearly two orders of magnitude better than in previous temperature measurements. Funding Agency: DFG Duration Partner: University of Oldenburg, Prof. Dr. A. Kittel Principal Investigator:
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3D Particle Tracking Velocimetry (PTV) is a flow measurement technique in which multiple cameras record the movement of tracer particles within a volume of interest and use this data to reconstruct the instantaneous velocity field. To date, this technique has been used only in relatively small measurement volumes and primarily in liquids. --- Principle of the 3D PTV Method The 3D PTV method is a flexible technique for determining time-resolved, spatial velocity fields, which are visualized using suitable particles. By recording and analyzing a sequence of images, particle trajectories can be reconstructed. --- Phase I: "Ilmenau Model Room" Test Cell The initial research was conducted in a rectangular cell measuring (L/W/H) 4.2 m x 3.0 m x 3.6 m. During this phase, the individual components of the 3D PTV system were tested, followed by validation measurements using model flows. Cameras Illumination Particles We use helium-filled soap bubbles as density-neutral particles. To produce these, Prof. Müller’s group at TU Berlin developed a bubble generator capable of producing a sufficient quantity of bubbles over several hours. Phase II: "Ilmenau Barrel" In preparation! Funding agency: DFG Duration Partners: TU Dresden, Prof. Dr. H.-G. Maas, DI T. Putze Project team:
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As a result of the first funding period, three powerful tools for investigating turbulent thermal convection are now available: the large-scale Ilmenau Flue, a newly developed pseudo-spectral simulation program, and a small water cell constructed outside the scope of DFG funding. These will be used in the second funding period to advance the understanding of the statistical properties of turbulent velocity and temperature boundary layers as well as coherent structures. This will be achieved through a combination of (i) high-resolution local velocity and temperature measurements at the Ilmenau barrel for variable Rayleigh numbers and aspect ratios, (ii) direct numerical simulations of convection in the presence of shear flows at the University of Bayreuth, (iii) visualization of coherent wall-near convective structures in a water cell at the University of Göttingen. The interconnection among the three research groups, as well as with the other groups in the package proposal, is reflected in the analysis of the Ilmenau data in Göttingen and Oldenburg, through the use of the microsensors developed in Oldenburg and Ilmenau at the Ilmenau flume, and through the application of the simulation program to calculate coherent structures in the Göttingen water cell. Funding agencies: DFG, Thuringian Ministry of Science, Research, and the Arts, City of Langewiesen Timeframe Partners: University of Bayreuth, Prof. F. Busse Project Leader:
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