THEME

Fundamental Physical and Biological Soil Processes
from Pore- to Field-Scale


Examination of seminal contributions made by soil physics pioneers such as Livingston, Buckingham, Haines, Gardner, Richards, and Kirkham reveal a common thread manifested in extremely broad scientific relevance well beyond the boundaries of "soil physics". The establishment of discipline boundaries in the form of specialized jargon, isolation and lack of frequent interactions with scientists from other fields seems to exclude contributions essential to a discipline's own evolution. An important objective of the Kirkham conference is to serve as a platform for expanding and blurring disciplinary boundaries of traditional soil physics by seeking unhindered exchange of ideas (no conference proceedings), and by in-depth exploration of methods developed and tested in other disciplines addressing a wide range of processes taking place in soils and other porous media.

We recognize the synergistic potential of interactions and discussions among active researchers from diverse scientific fields that more than internal discussion are likely to create new opportunities and enhance relevance of participating disciplines and soil physics. The complexity of the living and heterogeneous system we call soil presents endless challenges to soil physics as well as serving as a source of inspiration. The heterogeneous system with its complex biological component and nonlinear physics that make problem solving very difficult, is the same system that offers endless opportunities for new discoveries. New and exciting new areas of research tend to lie either at interfaces among disciplines where large knowledge gaps exist (e.g., scale and scaling issues, pore scale characterization and modeling; integration of physical and biological processes, complex-nonlinear-unstable natural phenomena), or are becoming feasible with rapid technological advancements (e.g., noninvasive measurement techniques, advances in computational method).