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September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Object-oriented Modeling of Heat and Humidity BudgetsOf Biosphere 2 Using Bond Graphs
François E. Cellier ETH Zürich
Àngela NebotUniversitat Politècnica de Catalunya
Jürgen Greifeneder Universität Kaiserslautern
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
What is Biosphere 2
• Biosphere 2 is an environmental research facility, located in the desert of Southern Arizona, that allows performing experiments in a materially closed ecological system under controlled experimental conditions.
• Biosphere 2 was built around 1990 with private funding and has functioned for almost 15 years already for various ecological experiments.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Why Biosphere 2
• In Biosphere 1 (the Earth ecosystem), it is difficult to perform experiments, because of limited access to control variables.
• In Biosphere 1, it is easy to observe phenomena and report them, but it is difficult to interpret these observations in an objective fashion.
• In Biosphere 1, we are able to correlate data, but correlations per se do not establish cause and effect relationships.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Biosphere 2: Construction• Biosphere 2 was built as a
frame construction from a mesh of metal bars.
• The metal bars are filled with glass panels that are well insulated.
• During its closed operation, Biosphere 2 was slightly over-pressurized to prevent outside air from entering the structure. The air loss per unit volume was about 10% of that of the space shuttle!
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Biosphere 2: Construction II
• The pyramidal structure hosts the jungle biome.
• The less tall structure to the left contains the pond, the marshes, the savannah, and at the lowest level, the desert.
• Though not visible on the photograph, there exists yet one more biome: the agricultural biome.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Biosphere 2: Construction III• The two “lungs” are responsible
for pressure equilibration within Biosphere 2.
• Each lung contains a heavy concrete ceiling that is flexibly suspended and insulated with a rubber membrane.
• If the temperature within Biosphere 2 rises, the inside pressure rises as well.
Consequently, the ceiling rises until the inside and outside pressure values are again identical. The weight of the ceiling is responsible for providing a slight over-pressurization of Biosphere 2.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Biosphere 2: Biomes• The (salt water) pond
of Biosphere 2 hosts a fairly complex maritime ecosystem.
• Visible behind the pond are the marsh lands planted with mangroves. Artificial waves are being generated to keep the mangroves healthy.
• Above the cliffs to the right, there is the high savannah.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Biosphere 2: Biomes II• This is the savannah.• Each biome uses its
own soil composition sometimes imported, such as in the case of the rain forest.
• Biosphere 2 has 1800 sensors to monitor the behavior of the system. Measurement values are recorded on average once every 15 Minutes.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Biosphere 2: Biomes III
• The agricultural biome can be subdivided into three separate units.
• The second lung is on the left in the background.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Living in Biosphere 2• The Biosphere 2 library is
located at the top level of a high tower with a spiral staircase.
The view from the library windows over the Sonora desert is spectacular.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
The Rain Maker
• From the commando unit, it is possible to control the climate of each biome individually.
• For example, it is possible to program rain over the savannah to take place at 3 p.m. during 10 minutes.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Climate Control
• The climate control unit (located below ground) is highly impressive. Biosphere 2 is one of the most complex engineering systems ever built by mankind.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Climate Control II• Beside from the
temperature, also the humidity needs to be controlled.
• To this end, the air must be constantly dehumidified.
• The extracted water flows to the lowest point of the structure, located in one of the two lungs, where the water is being collected in a small lake; from there, it is pumped back up to where it is needed.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
The Conceptual Model
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
The Bond-Graph Model
Temperature Humidity
Evaporation
Condensation
For evaporation, energy is needed. This energy is taken from the thermal domain. In the process, so-called latent heat is being generated.
In the process of condensation, the latent heat is converted back to sensible heat.
The effects of evaporation and condensation cannot be neglected in the modeling of Biosphere 2.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
The Dymola Model
• The overall Dymola model is shown to the left.
• At least, the picture shown is the top-level icon window of the model.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
The Dymola Model IINight Sky Temperature
Ambient TemperatureTemperature of Cover
Air Temperature
Soil Temperature
Vegetation Temperature
Water Temperature
Air Humidity
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
The Dymola Model III
Convection
Evaporation and Condensation
Night Sky Radiation
Solar Radiation
Solar Convection
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
ConvectionRth = R · T
Gth = G / TT
e1 e2
T = e1 + e2
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
RadiationRth = R / T 2
Gth = G · T 2
e1
e1
T = e1
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Evaporation of the Pond
Programmed as equations
Teten’s law
} Sensible heat in = latent heat out
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Condensation in the Atmosphere
Programmed as equations
If the temperature falls below the dew point, fog is created.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Ambient Temperature• The ambient temperature is computed here by
interpolation from a huge temperature data file.
Data were available for the location of Tucson only. Correction factors were used to estimate the effects of the higher altitude of Oracle.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Night Sky Temperature
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Solar Input and Wind Velocity
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Absorption, Reflection, Transmission
Since the glass panels are pointing in all directions, itwould be too hard to compute the physics of absorption, reflection, and transmission accurately, as we did in the last example. Instead, we simply divide the incoming radiation proportionally.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Distribution of Absorbed Radiation
The absorbed radiation is railroaded to the different recipients within the overall Biosphere II structure.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
The Dymola Biosphere PackageWe are now ready to compile and simulate the Biosphere model.
Not bad!
(The compilation is still fairly slow, because Dymola isn’t geared yet to deal with such large measurement data files.)
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Simulation Results I• The program works with weather
data that record temperature, radiation, humidity, wind velocity, and cloud cover for an entire year.
• Without climate control, the inside temperature follows essentially outside temperature patterns.
• There is some additional heat accumulation inside the structure because of reduced convection and higher humidity values.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Simulation Results II
• Since water has a larger heat capacity than air, the daily variations in the pond temperature are smaller than in the air temperature.
• However, the overall (long-term) temperature patterns still follow those of the ambient temperature.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Simulation Results III• The humidity is much higher
during the summer months, since the saturation pressure is higher at higher temperature.
• Consequently, there is less condensation (fog) during the summer months.
• Indeed, it can be frequently observed that during spring or fall evening hours, after sun set, fog starts to build over the high savannah, which then migrates to the rain forest, which eventually gets totally fogged in.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Simulation Results IV
• Daily temperature variations in the summer months.
• The air temperature inside Biosphere 2 would vary by approximately 10oC over the duration of one day, if there were no climate control.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Simulation Results V• Temperature variations during the winter
months. Also in the winter, daily temperature variations are approximately 10oC.
The humidity variations follow the temperature variations almost exactly. This observation shall be explained at once.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Simulation Results VI• The relative humidity is computed as
the quotient of the true humidity and the humidity at saturation pressure.
• The atmosphere is almost always saturated. Only in the late morning hours, when the temperature rises rapidly, will the fog dissolve so that the sun may shine quickly.
• However, the relative humidity never decreases to a value below 94%.
• Only the climate control (not included in this model) makes life inside Biosphere II possible.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
Simulation Results VII
• In a closed system, such as Biosphere 2, evaporation necessarily leads to an increase in humidity.
• However, the humid air has no mechanism to ever dry up again except by means of cooling. Consequently, the system operates almost entirely in the vicinity of 100% relative humidity.
• The climate control is accounting for this. The air extracted from the dome is first cooled down to let the water fall out, and only thereafter, it is reheated to the desired temperature value.
• However, the climate control was not simulated here.
• Modeling of the climate control of Biosphere 2 is still in the works.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
References I
• Brück, D., H. Elmqvist, H. Olsson, and S.E. Mattsson (2002), “Dymola for Multi-Engineering Modeling and Simulation,” Proc. 2nd International Modelica Conference, pp. 55:1-8.
• Cellier, F.E. (1991), Continuous System Modeling, Springer-Verlag, New York.
• Cellier, F.E. and J. Greifeneder (2003), “Object-oriented Modeling of Convective Flows Using the Dymola Thermo-Bond-Graph Library,” Proc. ICBGM’03, 6th Intl. Conference on Bond Graph Modeling and Simulation, Orlando, Florida, pp. 198-204.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
References II• Cellier, F.E. and R.T. McBride (2003), “Object-oriented
Modeling of Complex Physical Systems Using the Dymola bond-graph library,” Proc. ICBGM’03, Intl. Conference on Bond Graph Modeling and Simulation, Orlando, Florida, pp.157-162.
• Cellier, F.E. and A. Nebot (2005), “The Modelica Bond Graph Library,” Proc. 4th Modelica Conference, Hamburg, Germany, Vol. 1, pp. 57-65.
• Greifeneder, J. (2001), Modellierung thermodynamischer Phänomene mittels Bondgraphen, MS Thesis, Institut für Systemdynamik und Regelungstechnik, Universität Stuttgart, Germany.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
References III• Greifeneder, J. and F.E. Cellier (2001), “Modeling
Convective Flows Using Bond Graphs,” Proc. ICBGM’01, 5th Intl. Conference on Bond Graph Modeling and Simulation, Phoenix, Arizona, pp. 276-284.
• Greifeneder, J. and F.E. Cellier (2001), “Modeling Multi-phase Systems Using Bond Graphs,” Proc. ICBGM’01, 5th Intl. Conference on Bond Graph Modeling and Simulation, Phoenix, Arizona, pp. 285-291.
• Greifeneder, J. and F.E. Cellier (2001), “Modeling Multi-element Systems Using Bond Graphs,” Proc. ESS’01, 13th European Simulation Symposium, Marseille, France, pp. 758-766.
September 9, 2005 Start PresentationEnviroInfo 2005: Brno
References IV
• Nebot, A., F.E. Cellier, and F. Mugica (1999), “Simulation of Heat and Humidity Budgets of Biosphere 2 Without Air Conditioning,” Ecological Engineering, 13, pp. 333-356.
• Cellier, F.E. (2005), The Dymola Bond Graph Library, Version 1.1.
• Cellier, F.E. (1997), Tucson Weather Data for Matlab.