https://www.selleckchem.com/EGFR(HER).html
At the transition point, the event-size distribution of the avalanches is found to be a power law w_τ(Δn)∼Δn^-τ, with the drop-off exponent τ=(sqrt[17]+1)/2≃2.56. This value is an exact result of the self-consistent model. The edge behavior bears signatures enabling to associate it with the dynamics of a self-organized critical (SOC) state. At the same time the critical exponents, pertaining to this state, are found to be inconsistent with classic models of avalanche transport based on sand piles and their generalizations, suggesting that the