火星核心上方有丰富的化层的地质证据
Henri Samuel1, Mélanie Drilleau2, Attilio Rivoldini3
1Université Paris Cité, Institut de physique du globe de Paris, CNRS, Paris, France. samuel@ipgp.fr.
Nature
|October 25, 2023
概括
火星
科学领域:
- 星球科学
- 地震学
- 地质学
背景情况:
- 之前的地震数据显示火星有一个巨大的核心 (1830公里).
- 这种核心大小暗示光元素组成与实验数据不一致.
- 异常缓慢的地震波表明火星上有异质的地幔.
研究的目的:
- 为了研究火星的异质地幔结构假设.
- 将地质数据与核心大小和组成的约束相协调.
- 根据新的模型确定火星核心的大小和组成.
主要方法:
- 对地震相的分析 (反射和衍射的S和P波).
- 模拟地幔结构,包括基底层和化层.
- 综合地震减弱和潮散射数据.
主要成果:
- 一个异质地幔模型适合所有地质观测.
- 火星核心的大小估计为1650公里±20公里.
- 这种核心尺寸和密度 (6.5 g/cm3) 需要较少的轻元素,与约束保持一致.
结论:
- 火星很可能有层层的地幔和基础层.
- 经过修订的核心大小和组成在地化学上是合理的.
- 需要外部来源来解释火星的地磁场.
更多相关视频
11:50Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
Published on: June 13, 2015
12.6K
10:30Soil Lysimeter Excavation for Coupled Hydrological, Geochemical, and Microbiological Investigations
Published on: September 11, 2016
10.8K
相关概念视频
Magnetic Susceptibility and Permeability
1.1K
In linear magnetic materials, like paramagnets and diamagnets, magnetization is proportional to the magnetic field intensity. The constant of proportionality, a dimensionless number, is called magnetic susceptibility. The value of the susceptibility depends on the type of material.
When diamagnetic materials are placed under an external magnetic field, the moments opposite to the field are induced. Hence, the susceptibility for diamagnets has a minimal negative value of 10-5–10-6. Since...
When diamagnetic materials are placed under an external magnetic field, the moments opposite to the field are induced. Hence, the susceptibility for diamagnets has a minimal negative value of 10-5–10-6. Since...
1.1K
Minerals
330
Minerals are essential nutrients that the human body needs in small amounts to work properly. They play a vital role in many bodily functions, such as building strong bones and transmitting nerve impulses. Some minerals are needed for hormone production or to maintain a normal heartbeat. Major minerals include calcium, phosphorus, potassium, sulfur, sodium, chlorine, and magnesium, while trace minerals include iron, manganese, copper, iodine, zinc, cobalt, fluoride, and selenium.
Major...
Major...
330
Energetics of Solution Formation
6.8K
The formation of a solution is an example of a spontaneous process, which is a process that occurs under specified conditions without energy from some external source.
When the strengths of the intermolecular forces of attraction between solute and solvent species in a solution are no different than those present in the separated components, the solution is formed with no accompanying energy change. Formation of the solution requires the solute–solute and solvent–solvent...
When the strengths of the intermolecular forces of attraction between solute and solvent species in a solution are no different than those present in the separated components, the solution is formed with no accompanying energy change. Formation of the solution requires the solute–solute and solvent–solvent...
6.8K
Conditions on Early Earth
93.1K
Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
93.1K
Isothermal Processes
3.7K
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...
3.7K
Porosity in Cement Paste
151
The porosity of concrete is a measure of the void spaces within its structure. These spaces impact its strength and durability significantly. When water and cement interact, a chemical reaction called hydration creates a semi-solid paste. This paste includes combined water, making up approximately 23% of the cement's dry mass, and gel water, which fills minuscule voids known as gel pores, accounting for about 28% of the cement gel volume.
The balance of water to cement in the mix is...
The balance of water to cement in the mix is...
151
