The effect of local cooling upon spontaneous and evoked electrical activity of cerebral cortex

1970 ◽  
Vol 48 (9) ◽  
pp. 640-652 ◽  
Author(s):  
Herbert H. Jasper ◽  
David G. Shacter ◽  
Jacques Montplaisir

The effect of local cooling of the surface of the cerebral cortex by means of a metal chamber implanted in the skull was studied while recording evoked and spontaneous electrical activity from the center of a cooled area of 1 cm2. Direct cortical responses to local stimulation of the cortical surface decreased rapidly and progressively to disappear at surface temperatures of 20–22 °C. Onset and peak latencies were prolonged with a Q10 of 1.4 and 1.7 respectively. Response duration was prolonged with decreasing amplitude, having a Q10 of about 2.6. Surface cooling to 8–12 °C was necessary to abolish all postsynaptic components of somatic and auditory evoked potentials, recruiting responses, and spontaneous barbiturate spindles. Latencies of these responses were also increased with a Q10 of 1.3–1.4 while the Q10 for amplitude was consistently higher (2.0–2.6). Allowing for a gradient of increasing temperature from surface to depth it is concluded that all synaptic processes are blocked at temperatures of 20–22 °C. Synaptic mechanisms determining latency were consistently different from those determining amplitude as judged by consistent differences in the Q10 of latency and amplitude for all postsynaptic responses studied in these experiments.

Author(s):  
Susheel Singh ◽  
Sumanta Acharya ◽  
Forrest Ames

Flow and heat transfer in a low aspect ratio pin-finned channel, representative of an internally cooled turbine airfoil, is investigated using Large Eddy Simulations (LES). To achieve greater control of surface cooling distribution, a novel approach has been recently proposed in which coolant is injected incrementally through a series of holes located immediately behind a specially designed cutout region downstream of the pin-fins. Sheltering the coolant injection behind the pin-fins avoids the impact of the cross-flow buildup that deflects the impingement jet and isolates the surface from cooling. The longitudinal and transverse spacing of the pin-fins, arranged in a staggered fashion, is X/D = 1.046 and S/D = 1.625, respectively. The aspect ratio (H/D) of pin-fin channel is 0.5. Due to the presence of the sequential jets in the configuration, the local cooling rates can be controlled by controlling the jet-hole diameter which impacts the jet mass flow rate. Hence, four different hole diameters, denoted as Large (L), Medium (M) , Small (S), Petite (P) are tested for impingement holes, and their effects are studied. Several patterns of the hole-size distributions are studied. It is shown that the peak Nusselt number in the stagnation region below the jet correlates directly with the jet-velocity, while downstream the Nusselt numbers correlate with the total mass flow rates or the average channel velocity. The local cooling parameter defined as (Nu/Nu0)(1-ε) correlates with the jet/channel mass flow rates.


2012 ◽  
Vol 25 (13) ◽  
pp. 4511-4522 ◽  
Author(s):  
Guang-Shan Chen ◽  
Michael Notaro ◽  
Zhengyu Liu ◽  
Yongqiang Liu

Abstract Afforestation has been proposed as a climate change mitigation strategy by sequestrating atmospheric carbon dioxide. With the goal of increasing carbon sequestration, a Congressional project has been planned to afforest about 18 million acres by 2020 in the Southeast United States (SEUS), the Great Lake states, and the Corn Belt states. However, biophysical feedbacks of afforestation have the potential to counter the beneficial climatic consequences of carbon sequestration. To assess the potential biophysical effects of afforestation over the SEUS, the authors designed a set of initial value ensemble experiments and long-term quasi-equilibrium experiments in a fully coupled Community Climate System Model, version 3.5 (CCSM3.5). Model results show that afforestation over the SEUS not only has a local cooling effect in boreal summer [June–August (JJA)] at short and long time scales but also induces remote warming over adjacent regions of the SEUS at long time scales. Precipitation, in response to afforestation, increases over the SEUS (local effect) and decreases over adjacent regions (remote effect) in JJA. The local surface cooling and increase in precipitation over SEUS in JJA are hydrologically driven by the changes in evapotranspiration and latent heat flux. The remote surface warming and decrease in precipitation over adjacent regions are adiabatically induced by anomalous subsidence. Our results suggest that the planned afforestation efforts should be developed carefully by taking account of short-term (local) and long-term (remote) biophysical effects of afforestation.


1985 ◽  
Vol 57 (2) ◽  
pp. 134-141 ◽  
Author(s):  
W.A. THOMAS ◽  
P.V. COLE ◽  
N.J. ETHERINGTON ◽  
P.F. PRIOR ◽  
S.B. STEFANSSON

Sign in / Sign up

Export Citation Format

Share Document