Version 7.0 delivers a set of
features that fully support teachers in making learner-directed learning a reality in their classrooms, as well
as in
"distance" settings. It also supports researchers in making their
findings, or thinking-in-process,
available
to colleagues and funding sources in a more hands-on, "discovery
oriented" format.
The major advances in Version 7.0 lie in the
arena of communicating. We've made substantial improvements to the mapping
language
that will render STELLA diagrams more "readable." We've also
increased readability by significantly enhancing the
"storytelling"
capability that first appeared in Version 6.0 of the software. It's now
possible to unfurl a bit of your model and then
to
simulate just that bit to add the associated "behavioral" dimension.
Drop down a little more structure…then simulate to see
what it
has added to the dynamics. By enabling "just what's showing" to
simulate, people can build up their understanding of the
relationship
between structure and dynamic behavior in a systematic fashion-and the pace of
the building up is completely under
the
control of the "reader." Experiential learning at its best!
When students begin to understand
the concepts of stocks, flows, connectors, and converters, you are offering
them a language they
can use to explain the world around them and the interrelationships that impact change.”
You can download the latest version from the above Stella web site or purchase the software for use in the classroom to run the
file “fossilWood.STR” or you can access their Download reader from their web-page at http://www.hps-inc.com/reader.htm
for either the Windows PC or Mac.
What would happen if only two minerals were present? Our
model is simulating the two most common minerals found in petrified wood,
calcite and silica.
Concentration, Flow-Rate, and Volume related to the “Dwell Time” interacts to make the process possible we look at adding
the necessary converter
symbols and links. By adjusting
these values once a buried log has a water source to bring the minerals to the
log we can begin to determine what happens next. Does the log become Permineralized? Are there enough minerals to complete
the Petrification process? The
type minerals involved alter the changing color patterns found in Petrified
wood. What colors might we expect to find if “Calcite” is the dominate
mineral? What colors might we
expect if “Silca” is the dominant and most common mineral? Please refer to Activity 2 on Physical
Properties on Minerals.
Not all teachers may know the answers to the above posed questions, however, nearly all are provided adequate information in the material provided elsewhere in the lessons or activities. The material and questions are furthered supported by University and Government Resources which can be accessed through links in the related Project materials. Access can be found on the web page for “References and Resources.” Additional links allow Teacher or Student to ask an expert in “Inquiry Based” format.
What might be the difference of water & mineral absorption of decaying wood at different depth levels? How much Time is required to complete the petrification process? How might different types of wood change the factors for organic materials to become fossilized and form the petrified rocks we find? I.e., the difference between the Palm trees, Deciduous Hardwoods, or Fir/Pine tree types might alter what petrification processes?
Manipulative web based model file fossilWood allows students to input and see visual changes in the variables
that have general affects on
the petrification processes in a simplified format. Graphs change as the slider
bars alter the data variables. One
can access the resource code “HTML” and make more changes in the data limits.
Current data is from actual government and university research. Time frame is
simplified.