探索地幔中的热传导

The key to understanding Earth's evolution is to look at how heat is conducted in the deep lower mantle¹ -- a region some 400 to 1,800 miles (660 to 2,900 kilometers) below the surface. Researchers at the Carnegie Institution, with colleagues at the University of Illinois, have for the first time been able to experimentally simulate the pressure conditions in this region to measure thermal² conductivity using a new measurement technique developed by the collaborators and implemented³ by the Carnegie team on the mantle material magnesium⁴ oxide⁵ (MgO). They found that heat transfer is lower than other predictions, with total heat flow across Earth of about 10.4 terawatts, which is about 60 % of the power used today by civilization. They also found that conductivity has less dependence⁶ on pressure conditions than predicted. The research is published in the August 9, online Scientific Reports.

 

Lead author of the study Douglas Dalton explains: "The lower mantle sits on top of the core where pressures range from 230,000 to 1.3 million times the pressure at sea level. Temperatures are like an inferno⁷ -- from about 2,800°F to 6,700 °F. The major constituents⁸ are oxides of magnesium, silicon⁹ and calcium¹⁰. Heat transfer occurs at a higher rate across materials of high thermal conductivity than across materials of low thermal conductivity, thus these low thermal conductivity oxides are insulating."

 

The atoms of the major mantle materials are solid solutions and are in a disordered arrangement, which affects the way they conduct heat. Until now, the effect of this disorder¹¹ on the way heat was conducted could only be estimated with experiments at low pressures. The pressure dependence on thermal conductivity has not been addressed in disordered materials before.

 

"We squeezed the samples between two diamond tips in an anvil¹² cell and measured the thermal conductivity of the samples, debuting¹³ a technique called time-domain thermoreflectance," remarked co-author Alexander Goncharov. "We went up to 600,000 times atmospheric¹⁴ pressure at room temperature. This technique allows us to measure the thermal properties of the material from the change in the reflectance of the material's surface, thus avoiding the need of contacting the material of interest as required by conventional techniques. We then compared the results to theoretical models."

 

The scientists also showed that there is less dependence of thermal conductivity on pressure than had been predicted. Calculations showed that at the core-mantle boundary there is an estimated total heat flow of 10.4 terawatts across Earth.

 

"The results provide important bounds on the degree to which heat is transferred by convection as opposed to conduction in the lower mantle," said Russell J. Hemley, director of Carnegie's Geophysical Laboratory. "The next step will be to examine effects of different mineral components¹⁵ on the thermal conductivity and to better understand the atomic scale basis of convective motion of these materials within the broader context of mantle dynamics¹⁶."

 

"The results suggest that this technique could really advance other high pressure and temperature studies of the deep Earth and provide a better understanding of how Earth is evolving and how materials act under the intense conditions," concluded Goncharov.

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