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相关概念视频

Atomic Orbitals02:44

Atomic Orbitals

An atomic orbital represents the three-dimensional regions in an atom where an electron has the highest probability to reside. The radial distribution function indicates the total probability of finding an electron within the thin shell at a distance r from the nucleus. The atomic orbitals have distinct shapes which are determined by l, the angular momentum quantum number. The orbitals are often drawn with a boundary surface, enclosing densest regions of the cloud.
Energy of a Satellite in a Circular Orbit01:11

Energy of a Satellite in a Circular Orbit

Thousands of artificial satellites orbit the Earth every day at various distances from the Earth. Satellites that orbit the Earth below an altitude of 1,600 km are considered to be orbiting in low-Earth orbit (LEO). Research satellites and Earth observation satellites are usually placed in LEO, and mostly orbit the Earth in elliptical orbits. Navigation satellites are placed in medium-Earth orbit (MEO), ranging from 2,000 km to 36,000 km from the surface of the Earth. Meanwhile, communication...
Circular Orbits and Critical Velocity for Satellites01:16

Circular Orbits and Critical Velocity for Satellites

The Moon orbits around the Earth. In turn, the Earth (and other planets) orbit the Sun. The space directly above our atmosphere is filled with artificial satellites in orbit. One can examine the circular orbit, the simplest kind of orbit, to understand the relationship between the speed and the period of planets and satellites with respect to their positions and the bodies that they orbit.
Nicolaus Copernicus (1473-1543) first suggested that the Earth and all other planets orbit the Sun in...
Gravity between Spherical Bodies01:27

Gravity between Spherical Bodies

Newton's law of gravitation describes the gravitational force between any two point masses. However, for extended spherical objects like the Earth, the Moon, and other planets, the law holds with an assumption that masses of spherical objects are concentrated at their respective centers.
This assumption can be proved easily by showing that the expression for gravitational potential energy between a hollow sphere of mass (M) and a point mass (m) is the same as it would be for a pair of extended...
Minerals01:26

Minerals

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.
π Molecular Orbitals of the Allyl Cation and Anion01:18

π Molecular Orbitals of the Allyl Cation and Anion

An allyl group is a three-carbon conjugated system where the sp³-hybridized allylic carbon is bonded to a CH=CH2 group via a single bond. Allyl anions can be obtained by treating propene with a strong base that can deprotonate methyl groups. Allyl cations are formed as intermediates during substitution reactions involving allylic halides. In both cases, the hybridization of the allylic carbon changes from sp3 to sp2, giving rise to a carbon chain with three sp2-hybridized carbons, each with an...

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相关实验视频

Updated: Jul 12, 2026

Simulating Imaging of Large Scale Radio Arrays on the Lunar Surface
06:14

Simulating Imaging of Large Scale Radio Arrays on the Lunar Surface

Published on: July 30, 2020

月球上的非正方位.

J A Wood, J S Dickey, U B Marvin

    Science (New York, N.Y.)
    |January 30, 1970
    PubMed
    概括

    月球上的异构岩石与海岩石不同,表明高地起源于撞击喷射物. 一个拟议的模型在gabbro上面呈现一个anorthosite地,玛丽亚由岩通过地裂隙上升而形成.

    科学领域:

    • 月球地质学 月球地质学
    • 星球科学 星球科学
    • 石化学 石化学是一门学科.

    背景情况:

    • 月球岩石分析显示,在海玄武岩和土壤岩中发现了明显的异型岩石碎片.
    • 异构体呈现出独特的组成,颜色和特定重力特性.
    • 对Tycho ejecta的Surveyor 7分析显示,其构成与这些anorthosites相似.

    研究的目的:

    • 为了识别和表征月球上的异构体.
    • 为月球地和海洋提出一个结构模型.
    • 为了解释anorthosites的起源及其与月球表面特征的关系.

    主要方法:

    • 对1676个月球岩石碎片的检查.
    • 月球样本的组成分析.
    • 与月球任务 (如Surveyor 7) 的现有数据进行比较.

    主要成果:

    • 鉴定了61个anorthosite碎片,与其他月球材料有很大的不同.
    • 拟议的甲基石是月球高地物质的样本,这些物质是由撞击所抛出的.
    • 一个月球结构模型表明,在加布罗上漂浮着25公里长的正方体岩层.

    更多相关视频

    Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
    11:50

    Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions

    Published on: June 13, 2015

    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 15, 2013

    相关实验视频

    Last Updated: Jul 12, 2026

    Simulating Imaging of Large Scale Radio Arrays on the Lunar Surface
    06:14

    Simulating Imaging of Large Scale Radio Arrays on the Lunar Surface

    Published on: July 30, 2020

    Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
    11:50

    Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions

    Published on: June 13, 2015

    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 15, 2013

    结论:

    • 阿诺托西特可能代表了原始的月球地物质.
    • 拟议的模型解释了玛丽亚的形成,因为岩岩填充了撞击漏洞.
    • 在这种地模型的背景下,Mascons被考虑.