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Different from the global equilibration, it takes a longer time to reach the equilibrium at each point in the space (or local equilibration).
In Fig. 6, the bottom panel shows the S-to-P energy ratio at three receivers with normalized distances of 0.2, 1 and 2. The top panel shows the S-to-P energy ratio in all the space (or global equilibration) for comparison.
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A re-equilibration of δ following the decay of global [Ca2+] accounts for the observation of a simultaneous return of PPR and covariance values to baseline as a function of interpulse interval (Fig. 2c, e), because these two parameters depend on δ.
(2) Small bodies impact a pre-existing global magma ocean, created by an earlier giant impact, and metal-silicate equilibration takes place near the base of this magma ocean.
After equilibration perfusion, the heart was subjected to 30 min of global no-flow ischemia followed by 45 min of reperfusion.
We have used this model to calculate the melt volume produced by 1000 2000 impacts that occur during each of three "Grand Tack" N-body accretion simulations (Walsh et al. 2011; Jacobson and Morbidelli 2014) and have determined the corresponding metal-silicate equilibration pressures at the base of the resulting melt pools and global magma oceans.
After an equilibration period of 15 minutes, hearts were subjected to 15 minutes of global, normothermic, stopped-flow ischemia and then reperfused under the same condition as before ischemia.
This measure also shows clearly that for the apo1 simulation EV1 describes an equilibration to a significantly different conformation from the starting structure, whilst in contrast concerted global change in the ligand-bound protein is not as marked.
Energy equilibration was checked for these steps.
time is allowed for equilibration.
Effect of metal particle size on the Fermi level equilibration.
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