18.1 The discovery of the rare gases 18.4 The rare gas compounds 18.3 The existence and recovery of the rare gases 18.2 Properties and uses of the rare gases 18.5 Summarry on the main group elements

Petroleum Natural Gases and Oilfield Waters Section 1石油(Petroleum) Section 2天然气(Natural Gases) 3 Section油、气的稳定同位素 (Stable Isotopes of Petroleum, gases) Section4油田水(Oilfield Waters)

Modified Atmospheric Packaging(MAP)is a precise description of this shelf- life extension technique (Bennett 1995). In the UK, MAP mainly involves the use of three gases-carbon dioxide, nitrogen and oxygen although other gases are used elsewhere. Products are packed in various combinations of these three gases depending on the physical and chemical properties of the food

1.1 The states of gases 1.2 The gas laws Real gases 1.3 Molecular interactions 1.4 The Van der Waals equation 1.5 The principle of corresponding states

Chapter 16 Kinetic Theory of Gases Chapter 16 Kinetic Theory of Gases (气体动理论) 1. Molecular interpretation of Temperature Distribution of Molecular Speed Mean Free Path

一、 General Properties: 1.它们都是单原子分子(monatomic molecular,,在通常条件下,它们都是气体,也称为惰性气体(noble or inert gases)

1. D: Interpretation of Entropy on the Microscopic Scale- The Connection between Randomness and entropy 1. D I Entropy Change in Mixing of Two ldeal gases Consider an insulated rigid container of gas separated into two halves by a heat conducting partition so the temperature of the gas in each part is the same. One side contains air, the other side another gas, say argon, both regarded as ideal gases. The mass of gas in each side is such

6-1 Essential Concept of the Kinetic Theory of Gases气体动理论的基本概念 6-2 State Parameters Equilibrium State Ideal GasLaw状态参量平衡态理想气体状态方程 6-3 Representation of Pressure for Ideal Gas气体动理论的压强公式 6-4 Average Translational Kinetic Energy and Temperature理想气体的平均平动动能和温度公式

1.气体的性质 2.液体的性质 3.溶液的性质

The atmosphere The atmosphere is a thin blanket of gas that envelops the earth The gases that make up the atmosphere are held close to the earth by the pull of gravity With increasing distance from the earth's surface, the temperature, density, and composition of the atmosphere gradually change