> index / blog : sratch
;; This buffer is for text that is not saved, and for Lisp evaluation. ;; To create a file, visit it with C-x C-f and enter text in its buffer.
Mon Sep 26 16:24:25 2022. flow through porous media can be disentagled into a fast advective component in the large pores and a slow diffusive component in the soil matrix. kleidon et al. (2013) and zehe et al. (2013) describe preferential flow using thermodynamic principles. in contrast, jackisch & zehe (2018), construct a lagrangian, stochastic—physical model framework.
Tue Sep 20 12:52:42 2022. thermodynamic limits — applied to sequence of energy conversions — can quantify their limits to provide basic estimates for processes on earth. they operate near thermodynamic limits that represents an evolutionary target. steady state is not thermodynamic equilibrium. thermodyn. description of earth processes allows to formulate everything in terms of energy and entropy fluxes. on kleidon et al. (2016).
date unknown. cited from beyer & penna (2021). some of these issues have been discussed in recent works (penna et al., 2018; barbeta et al., 2019, 2020; beyer et al., 2020; sprenger and allen, 2020; von freyberg et al., 2020)
date unknown. matthias literature suggestions:
date unknown. kathi links: