General Interests

My research is currently centered on the statistical physics of sediment particle motions and transport in Earth surface systems, including hillslopes and rivers. It combines theoretical, experimental, computational and field-based approaches. A growing aspect of my work involves examining the epistemology of Earth surface science within the context of critical rationalism and our tepid relationship with probability. I have taught courses in geology, hydrology and geomorphology, transport processes in Earth and environmental systems, fluid dynamics, and probability and statistics. I wrote the text Fluid Physics in Geology (Oxford University Press) and I am currently writing a text entitled Transport Processes in Earth and Environmental Systems: The basic physics and mathematics of how stuff works.

Note: I am no longer accepting new graduate students.

Current Research

Our current research on the probabilistic physics of sediment particle motions has, in addition to interesting technical aspects, an important philosophical basis.

Namely, in learning how to describe the behavior of mechanical systems, mostly we are initially exposed to deterministic examples. We study Newton’s laws as these pertain to simple particle systems, and then move on to the behavior of solids and fluids treated as continuous materials. The formalism is unambiguous, and describing the behavior of a well constrained system is in principle straightforward. Indeed, much of the legacy of geophysics resides in the determinism of continuum mechanics. Perhaps it is therefore natural that we might envision that a mechanistic description of the behavior of a system implies that such a description ought to be, or perhaps only can be, a deterministic one. Such a perception represents a lost opportunity. The most elegant counterpoint example is the field of classical statistical mechanics — devoted specifically to the probabilistic (i.e., non-deterministic) treatment of the behavior of gas particle systems in order to justify the principles of thermodynamics — yet which is no less mechanical in its conceptualization of this behavior than, say, the application of Newton’s laws to the behavior of a deterministic system consisting of the interactions of a few billiard balls or the players of the solar system, or involving the motion of a Newtonian fluid subject to specific initial and boundary conditions.

Once steeped in the language of mechanics, we understandably take comfort in mechanistic descriptions of system behavior. Specifically, we invest trust in the underlying foundation, and implied rigor, provided by classical mechanics. This is a good thing. But given the complexity and the uncertainty in describing the behavior of sediment systems, here it is essential to consider the idea that the concepts and language of probability are well suited to the problem of describing this behavior — precisely because of the complexity and uncertainty involved — relaxing our expectations that a deterministic-like relationship exists between, say, the flux of bed-load sediment and the fluid stress imposed on the streambed, or the flux of sediment on a hillslope and the local land-surface slope. This idea of leaning on probability to describe the behavior of sediment systems is not as straightforward as describing the behavior of idealized gas particle systems. Nonetheless, the objective is the same: to be mechanistic, yet probabilistic. These world views are entirely compatible.

Current Student

Sarah Williams (PhD) Earth and Environmental Sciences

Stuff to Ponder

The crest of the hill
I am writing a book based on the material I have been teaching for nearly twenty years in a one-semester course at Vanderbilt. Here the title and contents of the book do not matter so much as the thoughts that emerge during the effort. This essay has two parts. The first part consists of two paragraphs that will land in the Acknowledgments of the book. These paragraphs provide an ideal set up for what I really want to say in the second part of this essay. The link:
The Crest of the Hill

Six of fifteen outstanding problems in sediment transport science
Here are the slides of an invited talk on this topic. Following the introductory material the first problem involves formulating a dynamically correct Knudsen number (or suitable analogue) for rarefied transport conditions. The link:
Sediment Transport Problems

Rain splash transport and the law of large numbers
So what probabilistic elements underlie a nominally deterministic formula of noise driven sediment transport? Here is an essay on perhaps the “tamest” of surface transport processes: rain splash. The link is here:
Rain Splash and Large Numbers

Reimagining the meaning and potentialities of ‘geophysics’
This short essay was inspired by comments of Douglas Jerolmack (UPenn) on Twitter concerning the traditional narrow meaning of ‘geophysics’ versus the intellectual opportunities that a broader perspective might inspire. The link is here:

Catching up to a 21st century view of statistics in the doing and reporting of research in the Earth sciences
There is a compelling need to reexamine our views and use of statistics in the Earth sciences, and press toward a more informed, measured use of statistical methods in data analysis. This involves moving beyond the false premise that hypothesis testing can be reduced to the dichotomous choice of “significant” or “not significant” decided by arbitrary statistical thresholds, paying increasing attention to the “don’ts” of statistics, and crafting well-reasoned descriptive statistics and analyses with full explanation. Our statistics courses must cover the probabilistic foundation of statistics, not just its applications, giving students the needed insight and thus confidence to critically evaluate their own work as well as what is presented in the literature. Click the link below for an essay on this topic.
21st Century Statistics

The “uncertainty principle” of a Poisson point process
The concept of a Poisson point process is a beautiful thing, with important applications throughout the sciences. This concept involves an “uncertainty principle,” which, although not rivaling Heisenberg’s in its importance, nonetheless is delightful in its implications. Click the link below for a one-page essay that illustrates this uncertainty principle.
Uncertainty Principle

Particle diffusion on a Galton board
Particle motions on a Galton board, also known as a quincunx or bean machine, have inspired the design of toys, descriptions of sediment particle motions, and theories of the statistical physics of a Lorentz gas. Click the link below for a short essay that illustrates particle diffusion on a Galton board, with implications for sediment particle transport.
Gaussian Diffusion on a Galton Board

The severe limitations of stress-based formulae for describing bed load transport
Predictions of the flux of bed load particles in a turbulent shear flow typically involve algebraic formulae that relate the flux to the space-time averaged stress on the bed or an averaged near-bed flow velocity. Yet we do not have a clear theoretical basis for such formulae. Click on the link below for a short essay on why the macroscopic fluid-imposed bed stress in turbulent flows is an empirical heuristic and incorrect for what we expect of it.
Limitations of Stress Based Formulae

The benevolent companionship of failure
Here are some brief thoughts on the topic of failure, inspired by discussions with students, my reading on the matter, and my own experience.
Companionship of Failure

The Brickyard in 2020
In 1963 Bernard K. Forscher published a popular allegorical Letter in Science entitled “Chaos in the Brickyard.” Click the link below to see our update on this letter regarding the doing of science.
The Brickyard in 2020

Probability is a physical thing, not a mathematical thing
Consider the idea that probability, the measure p such that 0 ≤ p ≤ 1, is a physical thing rather than a mathematical thing. Click the link below for a short essay exploring the barest essence of this idea.
Probability is Physical