of heat transfer liquid on the inner\nsurface of the mantle under the effect of the centrifugal forces\ngenerated by the rotation of the mantle, the layer of heat transfer\nliquid being divided into separate annular sections, and controlling\nthe temperature of the heat transfer liquid layer ...
图2. “THE MANTLE”即斗篷策略 颈静脉血氧饱和度SvjO₂、脑组织氧压PtiO₂、脑灌注压CPP;收缩动脉血压SABP,潮气量VT、呼吸频率RR、平台压PP、驱动压力DP、呼吸做功MP、颅内压ICP、50%动脉血氧分压下的氧分压p50、视神经鞘直径ONSD、脉动指数PI...
图2. “THE MANTLE”即斗篷策略 颈静脉血氧饱和度SvjO₂、脑组织氧压PtiO₂、脑灌注压CPP;收缩动脉血压SABP,潮气量VT、呼吸频率RR、平台压PP、驱动压力DP、呼吸做功MP、颅内压ICP、50%动脉血氧分压下的氧分压p50、视神经鞘直径ONSD、脉动指数PI、计算机断层扫描CT。 THE MANTLE策略的主要内容及要点 T Tem...
112 °F) at the boundary with the underlying mantle. The temperature increases by as much as 30 °C (54 °F) for every kilometer locally in the upper part of the crust.
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Adiabatic temperature profile in the mantleGeothermMantleAdiabatic temperature gradientThermal expansionSeismic discontinuityThe temperature at the 410-km discontinuity is re-evaluated by comparing the depth of the discontinuity with the olivine–wadsleyite transition pressure obtained usingin situX-ray ...
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THE velocities of compressional ( V P ) and distortional ( V S ) seismic waves, through the Earth's upper mantle, were computed with much detail by Gutenberg 1 , who found the existence of a low-velocity layer at depths greater than about 70 km....
The two main global mantle transition zone (MTZ) discontinuities, near 410 km and 660 km depth, and their topography are largely compatible with, respectively, exothermic and endothermic phase transformations in an olivine-rich composition at a potential temperature of ~1,600 K. In a few...