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Session A4 - Physics Education and General Theory.
ORAL session, Saturday morning, April 12
4270, BPS

[A4.001] Chaos in Quantum Mechanics: Implications for Quantum Information

Wm. C. McHarris (Michigan State University)

Some of the imponderables associated with the Copenhagen interpretation of quantum mechanics have parallel explanations in terms of nonlinear dynamics and chaos. They include quantization itself, spontaneous breaking of symmetry, the exponential decay law, and interpretations of Bell's inequality. These lead one to infer the possibility of nonlinear, chaotic underpinnings for quantum mechanics. There have been previous nonlinear interpretations and extensions to quantum mechanics, and, of course, quantum chaos, but in general these have applied the nonlinearities to preexisting quantum mechanics and have not examined the possibilities of nonlinearities underlying quantum mechanics itself. This will be examined in terms of quantum mechanics being essentially relativistic in nature, and it will be shown than such an interpretation allows both Einstein and Bohr to be simultaneously correct! Nonlinearities fundamental to quantum mechanics also have implications for the superposition principle and hence for quantum information theory and quantum computing.

[A4.002] Theory of Auditory Thresholds in Primates

Michael J. Harrison (Michigan State University)

The influence of thermal pressure fluctuations at the tympanic membrane has previously been investigated as a possible determinant of the threshold of hearing in humans. More recent work has focussed more precisely on the relation between statistical mechanics and sensory signal processing by biological means in creatures' brains. Clinical data on hearing thresholds in humans and other primates as a function of frequency has long been available. I have derived an expression for hearing thresholds in primates by first calculating the frequency dependence of thermal pressure fluctuations at eardrums from damped normal modes that are thermally excited in model ear canals of given simple geometry. Most of the features of the clinical data may be attributed to the frequency dependence of the ratio of thermal noise pressure arising from frequencies outside to that arising from within a masking bandwidth that coherent signals must dominate in order to be sensed. Normalization of the theoretical threshold sound field pressure to clinical data at a single frequency leads to representation of the clinical data over the complete auditory spectrum.

[A4.003] The quantum/classical interface: spin and qubits

William E. Baylis, Crystal Johnson (Department of Physics, University of Windsor, Windsor, ON, Canada)

Classical relativistic physics in Clifford algebra has a spinorial formulation that is closely related to standard quantum formalism. The algebraic use of spinors and projectors, together with the bilinear relations of spinors to observed currents, gives quantum-mechanical form to many classical results, and the clear geometric content of the algebra makes it an illuminating probe of the quantum/classical interface. The paravector representation of spacetime in algebra of physical space is used in particular to provide insight into spin-1/2 systems and their measurement. Such systems are of particular interest because they represent the qubits of quantum computing.

[A4.004] Core-mantle Mill Theory

Yikun Zhang (Freelance)

Based on radiation mechanics, the history of Earth can be perfectly interpreted by core-mantle mill theory. The theory confesses the inner core as a ferromagnet. The ferromagnetism of inner core is supported by observed anisotropic property of inner core in transmitting seismic waves. Rotation of Earth originates from the magnetic interaction between Earth and Jovian planets. Since the torque caused by the magnetic interaction between Earth and Jovian planets only acts on the iron core of Earth, the core behaves as a rotating engine, tending to change both the rate and axis of Earth's rotation, while the mantle is the resistant to any change of rotation. The interplay between the two leads to the formations of fluid outer core, basalt magmas, oceanic crust, and the differential rotation between the inner core and mantle. Rock materials at the core-mantle boundary are ground into basalt magma due to the differential rotation between the inner core and mantle. Mid-ocean ridge systems are interpreted as the huge dike systems rooted in some principal magma chambers in the core-mantle boundary layer. The anisotropy of background radiation in the polar directions determines the patterns of mid-ocean ridge systems on the Earth's surface and the global tectonic movement of the Earth's crust. The theory also explains the causes of geomagnetic reversals, mass extinctions and global climate changes. The history of Earth is featured by three stages: without oceanic crust (before 2.7Ga), forming oceanic crust (2.7-2.25Ga) and gowth of continents (after 2.25Ga).

[A4.005] A Numerical Study of the Entropy Density Function

William Newby, Adam Lark, John Spencer, Haowen Xi (Bowling Green State University), BG Universal Research Group Team

Entropy plays a very important role in statistical physics and communication theory. There are many degenerate states Pi that correspond to the same value of entropy S. Where:

S = Sum(i=1,N) Pi ln (Pi) We will present a numerical study of the entropy density function for N=2,3,4,5. We have constructed a custom piece of software to calculate the different values and locate possible patterns and groupings.

[A4.006] Studying the Sagnac Effect with Ping

Chris Clymer, Michael Crescimanno (Youngstown State University)

This is experiment is an extension of the earlier experiments done by Dr. Crescimano along with Joel Lepak where the speed of light was measured using conventional computer networks and the common utility, "ping." In this experiment we will be using a modified version of ping to send packets between 3 geographically distant locations across the upper Atlantic. We will be measuring the time it takes for the travel each leg of this journey, and use this to find the length of each cable the packets travel across the Atlantic. Using this information we should be able to calculate the Sagnac Effect.

[A4.007] May the force be with you: student explanations of forces on charges in magnetic fields

Gordon Aubrecht (Department of Physics, Ohio State University at Marion), Cristian Raduta (Department of Physics, Ohio State University)

Although physics is the same worldwide, students belonging to different learning systems (or different cultural environments) may develop different styles of approaching and reasoning out physics problems. We compare student physics problem-solving styles between two different student populations: a group of typical American students (from an OSU calculus-based introductory course) and a group of Romanian students (from a second-year class at Bucharest University). We discuss one of the problems given in a small Eamp;M survey, in which students from both populations were presented with a point charge in a region containing a uniform magnetic field. We asked students to determine the force on the charge for different initial conditions. Their answers depend on an understanding of the Lorentz force and their general knowledge from classical mechanics. Observed similarities and differences in approach between these student groups are discussed, and our study's results described.

[A4.008] Quantum Mechanics without the Hydrogen Atom

Chitra Rangan, Jens Zorn (FOCUS Center, Department of Physics, University of Michigan, Ann Arbor)

Many undergraduate science and engineering majors are interested in quantum information and quantum computing. The traditional undergraduate quantum mechanics course offered by physics departments does not really prepare these students to understand quantum information science. To address this need, we propose an alternative that omits some of the traditional topics, notably the the hydrogen atom, in order to have time for necessary topics (e.g. field interactions with a two-level system, Rabi flopping, entanglement, and questions of quantum measurement) that are usually covered only in more advanced courses.

[A4.009] Building Bridges Towards Physics in the Undergraduate Discrete Math Class

Mihai Caragiu (Department of Mathematics, Ohio Northern University)

We will present various interesting problems with potential implications in physics that can be addressed in an upper undergraduate discrete mathematics class. In the talk we will look for bridges towards physics emerging from various mathematical problems involving Fibonacci and Lucas numbers, transfer matrices, cellular automata, discrete dynamics and algebraic coding theory.

Part A of program listing