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相关概念视频

Conditions on Early Earth02:06

Conditions on Early Earth

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.
Nuclear Stability03:18

Nuclear Stability

Protons and neutrons, collectively called nucleons, are packed together tightly in a nucleus. With a radius of about 10−15 meters, a nucleus is quite small compared to the radius of the entire atom, which is about 10−10 meters. Nuclei are extremely dense compared to bulk matter, averaging 1.8 × 1014 grams per cubic centimeter. If the earth’s density were equal to the average nuclear density, the earth’s radius would be only about 200 meters.
To hold positively charged protons together in the...
Conditions on Early Earth02:06

Conditions on Early Earth

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.
Isothermal Processes01:21

Isothermal Processes

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...
Conservation of Mass in Finite Cotrol Volume01:16

Conservation of Mass in Finite Cotrol Volume

The principle of conservation of mass is a fundamental law in fluid mechanics and is applied using the continuity equation. We apply the concept to a finite control volume to derive the continuity equation.
A system is defined as a collection of unchanging contents, and the conservation of mass states that a system's mass is constant.
Conservation of Mass in Fixed, Nondeforming Control Volume01:07

Conservation of Mass in Fixed, Nondeforming Control Volume

The principle of conservation of mass is fundamental in fluid dynamics and is crucial for analyzing flow within fixed control volumes, such as pipes or ducts. This principle states that the total mass within a control volume remains constant unless altered by the inflow or outflow of mass through the control surfaces. This results in a vital relationship for steady, incompressible flow where the mass entering a system equals the mass leaving it.
In the case of a sewer pipe, which can be modeled...

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相关实验视频

Updated: Jul 5, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
06:04

Simulation of the Planetary Interior Differentiation Processes in the Laboratory

Published on: November 16, 2013

从一开始计算的地球核心组成的限制.

Alfe1, Gillan, Price

  • 1Research School of Geological and Geophysical Sciences, Birkbeck College and University College London, UK. d.alfe@ucl.ac.uk

Nature
|May 23, 2000
PubMed
概括

这项研究调查了地球核心的组成,重点是硫等轻元素. 这些发现挑战了外核中简单的铁硫混合物的想法,影响了我们对行星动态的理解.

科学领域:

  • 地质物理学 地质物理学
  • 行星科学 行星科学
  • 计算化学的计算化学

背景情况:

  • 地球核心的组成对于了解其点,内核边界温度和核心-地幔热概况至关重要.
  • 核心中的光元素被认为驱动着组合对流,产生地球的磁场.
  • 外核的较低密度表明,轻元素占比很大,硫,氧和是主要候选元素.

研究的目的:

  • 使用ab initio计算来限制地球核心的组成.
  • 研究轻元素,特别是硫,在地球核心中的作用.

主要方法:

  • 在固体和液体铁中的轻元素的化学潜力的初始计算.
  • 使用地震学数据对外核密度差异的分析.

主要成果:

  • 计算的化学潜力对核心组成提供了约束.
  • 结果强烈表明,外核不是一个简单的二元铁硫混合物.

结论:

  • 地球外核的组成比二进制的铁硫系统更复杂.
  • 了解核心组成对于地力学至关重要,包括产生磁场.

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Last Updated: Jul 5, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
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Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
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