上层地幔的热扩散率的异性变异性
A Tommasi1, B Gibert, U Seipold
1Laboratoire de Tectonophysique, CNRS/Université de Montpellier II, France. deia@dstu.univ-montp2.fr
Nature
|July 19, 2001
概括
上层地幔岩石的变形会产生热异质性,使热量在流动方向上转移得更快. 这种压力诱导的异构性影响着地球的动态,影响温度分布和质学.
科学领域:
- 地质物理学 地质物理学
- 矿物物理 矿物物理
- 固体地球科学 固体地球科学
背景情况:
- 地球地幔中的热量转移对行星动力学至关重要.
- 橄石表现出热异质性,地震数据揭示了上层地幔中大规模的橄石方向.
- 在高温下地幔矿物质的热异质性及其与变形的联系仍然不太清楚.
研究的目的:
- 在高温下研究变形的地幔岩石的热异质性.
- 了解变形如何影响最上层地幔的热扩散性.
- 评估应变诱导的热异构对地幔动态的影响.
主要方法:
- 在变形地幔岩石 (2901,250 K) 中测量热扩散率的实验室测量.
- 在上层地幔的热传递的石化物理建模.
- 对地震异性质数据的分析,以推断橄树的方向.
主要成果:
- 变形会在最上层的地幔中产生显著的热异质性.
- 与流动方向平行的热传输速度高达30%比垂直的热传输速度快.
- 应变诱导的热异质性会影响上层地幔的温度,质和动态.
结论:
- 变形历史是控制上层地幔热结构和动态的一个关键因素.
- 海洋和大陆环境显示出热异性对传热和地质过程的明显影响.
- 在地幔羽毛上方的异型加热可能会影响大陆的地质活动.
相关概念视频
Thermal Sigmatropic Reactions: Overview
1.6K
Sigmatropic rearrangements are a class of pericyclic reactions in which a σ bond migrates from one part of a π system to another. These are intramolecular rearrangements where the total number of σ and π bonds remain unchanged.
Sigmatropic shifts are classified based on an order term [i, j ], where i and j indicate the number of atoms across which each end of the σ bond migrates. Below are examples of a [3,3] sigmatropic shift in...
Sigmatropic shifts are classified based on an order term [i, j ], where i and j indicate the number of atoms across which each end of the σ bond migrates. Below are examples of a [3,3] sigmatropic shift in...
1.6K
Atomic Nuclei: Nuclear Spin State Population Distribution
1.7K
Near absolute zero temperatures, in the presence of a magnetic field, the majority of nuclei prefer the lower energy spin-up state to the higher energy spin-down state. As temperatures increase, the energy from thermal collisions distributes the spins more equally between the two states. The Boltzmann distribution equation gives the ratio of the number of spins predicted in the spin −½ (N−) and spin +½ (N+) states.
1.7K
Isothermal Processes
3.8K
A thermodynamic process that occurs at constant temperature is called an isothermal process. Heat slowly flows into the system or out of the system to maintain thermal equilibrium. Processes involving phase changes like water evaporation into steam or freezing water into ice at a constant temperature are examples of Isothermal Processes.
An ideal gas can also undergo isothermal expansion or compression.
For example, consider 1 mole of an ideal gas inside an isolated cylinder at initial volume V...
An ideal gas can also undergo isothermal expansion or compression.
For example, consider 1 mole of an ideal gas inside an isolated cylinder at initial volume V...
3.8K
Joule-Thomson Effect
11.7K
The Joule-Thomson effect, also known as the Joule-Kelvin effect, describes the temperature change of a fluid when it is forced through a valve or porous plug while keeping it in a thermally insulated environment. This experiment is called a throttling process. This is an important effect widely used in refrigeration and the liquefaction of gases.
This experiment forces high-pressure gas through a throttle valve or a porous plug to a lower-pressure region. The gas expands as it passes through to...
This experiment forces high-pressure gas through a throttle valve or a porous plug to a lower-pressure region. The gas expands as it passes through to...
11.7K
Boundary Conditions for Current Density
1.5K
Current density becomes discontinuous across an interface of materials with different electrical conductivities. The normal component of the current density is continuous across the boundary.
1.5K
Thermal Strain
3.2K
Thermal strain is a concept that arises when we consider how temperature changes affect structures. Unlike the conventional assumption that structures remain constant under load, real-world scenarios often involve temperature fluctuations that can significantly impact these structures. Consider a homogeneous rod with a uniform cross-section resting freely on a flat horizontal surface. If the rod's temperature increases, the rod elongates. This elongation is proportional to the temperature...
3.2K


