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Climate change modeling has often been associated with uncertainties.
Ecological niche modeling has often been used to model a species' ecological and geographic distribution.
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The model has often been shown to fit both high activities of the solute and the intermediate range of concentrations.
The model has often successfully fitted high solute activities and the intermediate range of concentrations data well.
However, evaluation of such models has often been very limited due to the lack of necessary field data.
The Weber Morris intraparticle diffusion model has often been used to verify if intraparticle diffusion is the rate-limiting step (Igwe et al. 2005).
The Weber-Morris intra-particle/membrane diffusion model has often been used to determine if intra-particle/membrane diffusion is the rate-limiting step [24, 25].
So far, extremity ischemia and subsequent neovascularization-guided perfusion recovery in animal models has often been evaluated by predominantly anatomic (MRI), invasive (angiography), or limited (LDPI) techniques.
The Weber-Morris intra-particle diffusion model has often been used to determine if intra-particle diffusion is the rate-limiting step [39].
The non-resonant tunneling model has often been used to describe the electron transport process through small molecule, where contact conductance, molecular length, and the tunneling decay constant are the main parameters [17, 18].
This model has often been validated using decay rates of particulate matter concentration; however, in several indoor applications the interest is not in concentration but in the spatial distribution of the deposition flux.
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