Rainforest Regeneration, The Carbon Cycle and Environmental Issues   
STELLA Model Building as a Teaching Tool:
    by Florence Sherrill Duarte
High School Biology
The Lovett School
Atlanta  GA
 
 
I. Introduction VI. Meeting the NSF Standards
II. Objectives VII. Remarks
III. Methods VIII. Aknowledgements
IV. The Models IX. Bibliography
V. Modeling in the Classroom X. About the Author
 

I. Introduction back to top
This project focuses on the process of building two new STELLA models one to study forest recovery rates, the other to study global carbon cycles and  associated environmental issues. The models presented are examples of models that could be developed in a high school classroom studying environmental issues. They are not finished products, but works-in-progress requiring further definition and testing. The central idea is that model building is itself the more valuable teaching tool rather than using a finished model.
The systems approach and the attempt to build  formal models encourage disciplined  analysis and theory development. Modeling forces us to dissect a system into its smallest details and to evaluate the significance of components. Modeling helps us find patterns in seemingly random events and make predictions for outcomes. A well-conceived model must behave plausibly under extreme conditions and should be tested against what we can observe in the real world. This leads to asking questions about what the limiting conditions are to any particular trend or behavior.
 
 
II. Objectives back to top
My long-term goal is to coach my students in building their own STELLA models about environmental problems. I have been inspired by the degree of inquiry and critical thinking that are necessary for the construction of a good model. I hope to inspire my students to question current scientific beliefs and even bad modeling with their own reasoning and research. Sound modeling should help them develop the self-confidence that is needed to create and find original solutions to old problems.
 
 III. Methods back to top
A. Brainstorming
The modeling process began with several brainstorming sessions to define a specific problem, select important variables and suggest theories for system structure. The critical thinking process required at the conceptualization stage is the most demanding and the most revealing for the modeler, especially as a novice. Some of the many questions raised for me during brainstorming for these models are as follows:

On tropical reforestation:

The soil was not considered as a stock of carbon because it is not. The carbon present in decaying litters is  released  back into the atmosphere as carbon dioxide. Nutrients are present in the soil in minute quantities not comparable to the amounts of biomass.

On the global carbon cycle:

B. Computer Modeling
After creating the conceptual foundation of the model, computer modeling began, using the PC version 5.0 of the STELLA software by High Performance Systems. The software symbols are fairly straightforward to use. Stocks and flows need to be defined and the relationship between components established using equations and graphs. The next step is to set the initial amounts of each stock and define flow rates. For the most part, I defined parameters and relationships illustrated in high school text books. For example, in order to explain the effect of temperature on decay I used what we know about how temperature affects microorganisms that aid decay, using a graphic formulation. Two daily consultations with Dr. Forrester took place throughout the model building and model analysis periods. I call these sessions "mental ping-pong". After consultations I was often propelled to the library in search of answers for the many questions that our discussions brought up.
 

IV. The Models back to top
a) A STELLA model of Tropical Forest Regeneration After Deforestation
 
Guiding question:
What will happen to a small patch of tropical rainforest after selective logging and burn?

The reforestation model deals with the forces controlling re-frowth of a small area of tropical forest (1km2)   to climax vegetation after selective logging and burning. The model reflects patterns of temperature and rainfall and their impact on plant growth, litter decay and ecological succession. Early pioneer plants do reestablish under bad conditions and eventually lead to climax growth. Over a few decades biomass recovers to climax levels. Light and genetics turn out to be the limiting factors to plant  growth, not nutrient soil depletion, due to intensive recycling in even semi-mature forests. The model does not include the potential effects of increased concentration of atmospheric carbon dioxide on photosynthesis and growth rates.
                                                                                                           
 

Preliminary results:
Re-growth is predicted under conditions of temperature at 250C and 300 mm rain per year. Decay time for organic material is defined at 1 year. Plant lifetime is defined as a function of biomass: the larger the plant biomass, the longer the lifetime. Nutrient availability is defined as a ratio between decomposition and unlimited growth. The limiting factors on unconstrained growth in this ecosystem are light and genetics. Plants need light to grow and are genetically programmed to reach only a certain height. Initial amounts of plant biomass and forest litter are both set at 1 ton per km2
 

 b) A STELLA Model of the Global Carbon Cycle
Guiding question:
What happens to CO2 after it is dumped into the atmosphere?
The model of the global carbon cycle deals with the forces that act on carbon as it circulates between reservoirs.  The reservoirs of carbon are the earth, the biosphere, the atmosphere and the ocean.  The model should show how what happens to the carbon dioxide temissions in the atmospher from fossil fuel burning and deforestation. Carbon dioxide  emissions are never localized because they are gases and immediately diffuse into the atmosphere. The interaction of carbon with the ocean surface is critical to understanding the carbon cycle because the ocean covers approximately 75% of the earth's surface. Research indicates that of the 5 x 1015 g of C yr-1 released in 1985  by burning of fossil fuels, only 58% remains as what is called the "airborne fraction". No one knows for certain where the remaining 42% are stored. Oceanographers hypothesize that this missing fraction of CO2 is taken in by the oceans, used by aquatic producers for photosynthesis and buffered by the precipitation of marine carbonates.
The key to the "mystery of the missing carbon sink" is linked to the emission and absorption rates of carbon dioxide at various points in the cycle. Remote sensing and GIS data on the vegetative cover on land and in the ocean would be useful to evaluate these processes further. The model below reflects only an initial attempt to describe the carbon cycle; further work is needed.

The Global Carbon Cycle: A Model Sketch 

 
 

V. Modeling in the classroom. back to top
A. Introduction to STELLA modeling
After a general introduction to STELLA modeling, students should start by looking at some of the classic simple models that are available for study. Models on ozone depletion, predator-prey relationships, disease epidemics and others should highlight the utility of modeling for high school students.

B. Are all models good models?
Students should be aware that modeling is merely a tool that should be used carefully, with sound thinking as a foundation. Like statistics and speeches, models can be deceiving. Assumptions and structures need to be questioned for consistency and reasonableness. I have adapted from Vanclay a possible checklist to help students evaluate models as follows:

C. Classroom modeling
Classroom modeling would necessarily begin with a discussion on the types of problems and issues that lend themselves to modeling. Problems involving dynamics, or the passage of time, or the flow of physical elements are typical examples. Students should likely come to an agreement on a single topic in order to focus on the model building process and to facilitate coaching. Students should not be limited by their current knowledge but rather stimulated to research their areas of interest in the library and on online resources. A natural consequence of model building is to encourage class discussions around environmental issues paying special attention to the human aspects.

 
 VI. Meeting the NSF Standards: back to top
Some of the  NSF standards that were met in completing this project were

A.  9- 12 content standards on:
a) Biological Evolution.
b) The Interdependence of Organisms.
c) Matter, Energy, and Organization in Living Systems.
d) Bio-geo-chemical Cycles (especially that of the element carbon).
e) Origin and Evolution of the earth system.
 
B.  9-12 Science as Inquiry content standards on :
a) Formulation of testable (or researchable) hypothesis and demonstration of logical connections.
b) The use of mathematics and technology to improve investigations and communications.
c) The formulation and revision of scientific explanations and models using logic and evidence.
d) Recognition and analysis of alternate explanations and models.
e) Communication and defense of a scientific argument.
 
 

VII. Remarks back to top
The process of building models has made me rush to the library for more information on tropical rain forests, plant physiology, terrestrial ecology, systems modeling, the bio-geo-chemical cycle of carbon and even oceanography. I emerged from the libraries with even more questions, but with a sense that the modeling had given a purpose and direction to my research. As a result, I have begun a growing list of books and web sites for anyone who wishes to pursue these topics further. I plan to continue working on the models presented here, and others, over the course of the next year. I hope to be able to introduce my students to aspects of the modeling process .
Presenting finished models to my students would probably be less risky for the teacher but less powerful as a teaching tool. The model building experience presents challenges that bring new relevance and motivation to learning about environmental problems.

I would greatly appreciate any comments or suggestions on how to continue my modeling work and specially on how to transfer it to a high school classroom. Please e-mail me at

       fduarte@lovett.org or click on the envelope for a direct link.       

VIII. Acknowledgments back to top
A special thanks Dr. Nathan Forrester for his assistance in in my modeling efforts.
A special thanks to Ms. Louise Shaffer and Mr. David Goodman at the Biology Library at Guyot Hall, Princeton University for their assistance in my research.
A special thanks to Mary Sherrill Forrester for her editorial assistance.

 IX.Bibliography back to top
Odum, Eugene P.1971. Fundamentals of Ecology. 3rd ed.W.B. Saunders Company

Odum, Howard T. 1994. Ecological and General Systems: An Introduction to Systems Ecology. Newot, Colorado: University Press of Colorado

Edwards, Gerry & Walker, David. 1983. C3, C4: Mechanisms and Cellular and Environmental Regulations of Photosynthesis. Berkeley; University of California Press

Koch, George W. & Mooney, Harold A. 1996. edited by, Carbon Dioxide and Terrestrial Ecosystems. Academic Press

Vanclay, Jerome K. 1994. Modeling Forest Growth and Yield Applications to Mixed Tropical Forests. CAB International

Yunus, Mohammad & Iqbal, Mohammad. 1996. edited by, Plant Responses to Air Pollution. John Wiley & Sons

Nepstad, Daniel C. 1989. Forest Regrowth in Abandon Pastures of Eastern Amazonia: Limitations to Tree Seedling Survival and Growth; A Dissertation Presented to the Faculty of the Graduate School of Yale University in Candidacy for the Degree of Doctor of Philosophy. UMI - Dissertation Services

Edwards, DEW., Booth, WE. and Coy, S.C. 1996. edited by, Tropical Rain forest Research - Current Issues, Kluwer Academic Publishers

Hurtt, George C. 1997. Ocean Ecosystem Models for Use in Studies of the Air-Sea Balance of Carbon Dioxide; A Dissertation Presented to the Faculty of Princeton University in Candidacy for the Degree of Doctor of Philosophy; Princeton University

Schlesinger, William H. 1991. Biogeochemistry An Analysis of Global Change. Academic  Press

Butcher, Samuel S., Charlson Robert J., Orians Gordon H. & Wolfe, Gordon V. 1992. edited by, Global Biogeochemical Cycles, Academic Press
 

X. About the Author back to top
Florence Sherrill Duarte
High School Biology Teacher 

The Lovett School in Atlanta    GA
4075 Paces Ferry Road NW
Atlanta  GA  30327
www.lovett.org
fduarte@lovett.org