USE OF THE LAVAâ LAMP AS AN ANALOGY IN THE GEOSCIENCE CLASSROOM Stephen G. Tolley Florida Gulf Coast University, College of Arts and Sciences, 10501 FGCU Boulevard South, Fort Myers, Florida 33965-6565, [email protected] Sherry D. Richmond University of Florida, P.O. Box 110410, Gainesville, Florida 32611-0410, [email protected] ABSTRACT We have developed an exercise for the geoscience classroom that uses the LAVA lamp as an analogy to introduce general education undergraduate students to oceanography. The exercise provides a link between previously learned (from their secondary educational experience) and new knowledge by placing basic principles of science within an oceanographic context. Previously learned concepts that are built upon in the exercise address the properties of matter, the transformation of energy, force and motion, and the global processes that shape the Earth. The exercise requires students to compile an extensive list of observations using the lava lamp, to derive meaning from these observations and share this meaning with their peers, and to apply this meaning to new course content. Some of the more common observations recorded by students deal with changes of state in matter, differences in density among the lamp’s components, the influence of temperature on density and thus on buoyancy, the formation of convection cells, and thermal expansion of fluid volume. We have found the exercise to be a useful way of introducing lower-division students to such related processes as adiabatic atmospheric circulation, global warming and sea level rise, and most especially magma movement contributing to global plate tectonics. Keywords: Education geoscience; education precollege; educationscience; education undergraduate; geoscience teaching and curriculum; marine geology and oceanography; plate tectonics. LAVA®, LAVA LITE®, LAVA WORLD INTERNATIONAL® and the configuration of the LAVA® brand motion lamp are registered trademarks of Haggerty Enterprises, Inc. The configuration of the globe and base of the motion lamp are registered trademarks of Haggerty Enterprises, Inc. in the U.S.A. and in other countries around the world. ©2002 Haggerty Enterprises, Inc. All rights reserved. “There is no better, there is no more open door by which you can enter into the study of natural philosophy than by considering the physical phenomena of a candle. There is not a law under which any part of this universe is governed which does not come into play, and is not touched upon, in these phenomena.” Michael Faraday, “The Chemical History of a Candle,” p. 1 Tolley and Richmond - Use of the Lava Lamp INTRODUCTION The burning candle has served not only as a metaphor for science itself (Sagan, 1995; Ho, 1997; Laidler, 1998), but ever since Michael Faraday’s classic discourse (Faraday, 1861), it has also been the subject of examination within the science classroom. Candles were originally burned as a part of the curriculum either to illustrate the inherent complexities of seemingly simple phenomena or to demonstrate the basic principles of combustion (the appropriateness of some of these usages has since been questioned, see Birk and Lawson, 1999). More recently, candles have been used to examine convection (Buchman, 1992), rotation (Mou, 1997) and even microgravity (Ross, 1998, Candle drop, 1999). We have been using the Lava lamp in the geoscience classroom as a contemporary corollary of the burning candle. Like the candle, the lava lamp provides an opportunity for students to compile an extensive list of observations from which they can later infer meaning. The lamp consists of three primary components, each of differing density and each of differing degree of thermal expansion (Figure 1). The first component, a transparent liquid consisting of dyed water (U. S. Patent Office, 1968), is of lesser density than the second– popularly referred to as the lava. The lava itself is described as being comprised of mineral oil and paraffin, with a melting point that allows it to change state from a solid to a liquid at temperatures of 40-50º C (U. S. Patent Office, 1968). Located above these two substances is an air space that can expand or contract in response to the thermal expansion of the more dense liquid and lava. All three of these components are sealed within a glass vessel that sits upon a base. A 40-watt appliance bulb housed in the lamp’s base serves as the energy (heat) source. In a cold lamp (turned off), the lava is in its solid state lying at the bottom of the vessel, the air space at the top of the vessel is at its largest volume, and no movement can be detected in any of the lamp’s major components. After the heat source is turned on and the lamp begins to warm, the solid lava slowly begins to melt, becoming a viscous liquid and maintaining its opacity. As its density is reduced by thermal expansion, the lava begins to rise though the transparent liquid. This rising lava begins to break off from that still at the bottom of the vessel and forms odd shapes. As the lava continues to rise toward the surface of the vessel and away from its heat source, it begins to cool and then sinks, eventually amalgamating with the lava remaining at the bottom of the vessel. This cycle of thermal convection may take from tens of minutes to several hours to fully develop, during which time the air space in the top of the vessel continues to contract in volume. 217 USE IN THE CLASSROOM The lava lamp exercise was developed for an undergraduate general education course to reacquaint students with some basic principles of science so that they might then apply these principles to understand particular oceanographic processes. The lava lamp could also prove useful in introductory geology courses, where a variety of analogies have already been developed in order to teach more effectively principles related to plate tectonics (for a complete listing see Nottis, 1999). Here it could be used not only to introduce such concepts as mantle plume movement and the formation of intrusive igneous bodies, but also to present salt diapir formation and adiabatic processes in the atmosphere. At Florida Gulf Coast University (FGCU), only 10% of the incoming freshmen are from out of state. Therefore, the vast majority of our first-year students have been exposed to Florida’s Sunshine State Standards, a series of learning goals adopted by the State that define expectations of student performance according to both grade level and subject matter (Sunshine State Standards, 2000). These standards also provide a baseline of prior knowledge that post-secondary instructors can use to build upon. Standards relevant to the lava lamp exercise address the following: properties of matter including changes of state; the transformation of energy; the relationship between forces acting on an object and the object’s motion; and “processes in the lithosphere, atmosphere, hydrosphere, and biosphere” that “interact to shape the Earth” (Sunshine State Standards, 2000). Because the lava lamp is immediately recognizable to most students, it engenders a sense a familiarity even before the exercise begins. The exercise is used during the first class meeting and provides students with an opportunity to complete a number of cognitive tasks that fall into several previously recognized categories of learning (Bloom and others, 1956; Marzano, 2001). It also exposes them to a pluralism of ideas through interaction with their peers. As a consequence, we find the exercise to be a valuable, disarming tool that can be used to immediately move students beyond the simplistic authority-oriented view of knowledge that they may still be clinging to at the beginning of their college experience (Perry, 1970) and on to higher levels of cognitive complexity (Lynch and others, 2001). Learning goals are explicit: (1) to help students see the value of making simple, but careful, observations; (2) to reacquaint students with basic principles of science; (3) to introduce students to new course content by relating it to these basic principles; and (4) to stimulate higher order thinking by asking students to function at several levels of intellectual competency. The exercise can be broken down into three parts: individual observation, written questions and student responses coupled with small-group discussion, and large-group discussion facilitated by the instructor that challenges students to apply what they have learned to new course content. Observation - At the beginning of the exercise, students are asked to spend a few minutes individually examining a lava lamp in its cold state and to record these initial observations for use later in the class. Students are restricted in their interaction with the lamp: they may touch the lamp, but may not disturb it in any way. This prevents the lamp’s components from 218 Figure 1. Simplified illustration of a LAVAâ lamp. Primary components include a transparent liquid, a wax-like substancethe lava, and air, all sealed within a glass vessel. Housed in the base of the lamp, below the vessel, is a light bulb with reflector that serves as the energy source driving the motion of the lamp. becoming partially emulsified due to excessive moving or shaking. Furthermore, students are not provided with any information concerning the lamp’s structure or function. As students redirect their attention toward other tasks unrelated to the exercise, several lamps are allowed to warm up. Since the class meets for 2 hours and 15 minutes, this warm-up time allows the instructor to cover other materials related to the class’ first meeting. This shift in focus is facilitated by a combined lecture-laboratory approach to science teaching at FGCU. Science classrooms are designed to be able to move students easily back and forth between laboratoryand lecture-based modes of instruction within the same space. Science courses are then scheduled with lecture and laboratory sections combined. This classroom design allows for flexible teaching and limits the number of students to approximately 30. After a sufficient warm-up period, students assemble into small groups and begin making additional observations of a lamp that is now fully cycling. Typical observations made include the illumination and warming of the lamp itself, the melting of the lava from a solid to a liquid form, the rising and falling of liquid lava, the nature of the shapes that are formed as the lava rises and separates from that remaining at the bottom of the lamp, the apparent immiscibility of the lava and liquid Journal of Geoscience Education, v. 51, n. 2, March, 2003, p. 217-220 components, and the volumetric changes that have concepts regarding the interaction of matter and energy occurred in both the liquid and the airspace since the they infer that thermal expansion has taken place; applying this principle to oceanography, students initial observations of a cold lamp. suggest that increasing heat input into the global ocean Written Questions and Student Responses - As will result in sea-level rise; finally, students predict a rise students assemble into their small groups to examine in sea level as one of the potential outcomes of global their lava lamp, they are provided a handout with a set of warming. In a similar fashion, change of state, the effect questions (Table 1) that asks them to record carefully of temperature on density, the relationship between their observations, to explain the underlying processes density and buoyancy, and thermal convection can all be that they think are at work, and to break down these combined to introduce adiabatic processes in both the processes into their component parts in order to explore mantle and the atmosphere that drive large-scale the relationships among them. These questions are circulation and that transport heat. The effect of meant to stimulate student responses that demonstrate temperature on density can also be used to illustrate the different levels of competency relevant to the concepts formation of deep water at high latitudes. A more being explored, specifically knowledge, comprehension, complete listing of examples in which the lamp has been application, and analysis as described by Bloom and used as an analogy to place basic scientific principles others (1956). After responding to these questions, within an oceanographic context is presented in Table 2. students are encouraged to discuss what they see with other members of their group and to observe the other CONCLUSION lava lamps that are set up in the classroom. It is at this stage of the exercise that students begin to connect their Recent research suggests that a portion of the Earth’s observations with previously learned scientific concepts: interior, the deep mantle, behaves as a sort of lava lamp melting lava is framed within the context of changes of set on low (Kellogg and others, 1999; Kerr, 1999). It seems state; the rising and sinking of lava is expressed in terms appropriate then that the lava lamp exercise be used in of the effects of heating and cooling on density and of the the oceanography classroom, for it is this very process of formation of convection cells; and changes in the volume global plate tectonics that is responsible for the continual of the liquid and of the air space at the top of the lamp are creation and renewal of the ocean basins themselves. The viewed in light of thermal expansion. By using the lava lava lamp provides a striking reference point at the lamp to reacquaint students with these basic principles beginning of the course that can be used later on by the of science, we set the stage for introducing new material instructor to stimulate student thinking about a variety related to oceanography in a manner that is both of concepts that are integral to the study of reinforcing and disarming. oceanography. As such it can be referred to whenever one or more of these concepts need to be applied to Large-group Discussion - After the students have had understand new course content. As unveiled in class time to respond in writing to the above questions and to discussions, students also find the exercise useful and discuss these responses with other members of their continue to refer back to it as an analogy for small group, the class is reconvened as a whole in order understanding oceanographic principles. Furthermore, to share and compare work. It is during this stage of the students’ references to the exercise on exams given exercise that students begin to develop a common weeks later suggest that the lava lamp has proven vocabulary and to apply the principles under discussion helpful to them in the learning process. Just as the to course content. Specifically, the last question on the burning candle has served as science’s symbol, so too the student handout“What processes related to lava lamp can be a useful metaphor, especially in the oceanography do you think might be explained using geosciences. some of these same principles?”is used as a lead-in to begin introducing students to oceanographic principles ACKNOWLEDGMENTS and phenomena. This transition to course content is facilitated by the instructor and begins with a modified We thank José Barreto, Win Everham, Jerry Jackson, brainstorming session in which students offer concepts Rebecca Totaro, and Aswani Volety for their comments assembled from an examination of the lava lamp that on and careful reviews of early drafts of the manuscript might be applied toward oceanography. A large list of as well as Joseph Tolley for his illustration of the lamp. ideas is developed and is then sorted and grouped by the We also thank Journal of Geoscience Education instructor based upon some of the major oceanographic reviewers Marek Cichanski, Ralph Dawes, Robert themes that are to be introduced as part of the course. Hooper, and Jeffrey Noblett for their valuable The lava lamp is a useful analogy that helps students suggestions on how to strengthen the work. The senior relate previously learned concepts such as changes of author expresses his gratitude to Michael McDonald for state, the effect of temperature on density, the influence lengthy discussions regarding both learning outcomes of density on buoyancy, thermal convection, and thermal and lava lamps. This represents contribution 14 from the expansion, to oceanography. 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