File - Respiratory Therapy Files

advertisement

Physical Principles of

Respiratory Care

Egan Chapter 6

I.

Physical Principles of Respiratory Care

II.

III.

IV.

States of Matter

Change of State

Gas Behavior Under Changing Conditions

Fluid Dynamics

II. Change of State

A.

B.

1.

2.

5.

6.

3.

4.

1.

2.

Liquid-Solid Phase

Changes

Melting

Freezing

Properties of Liquids

Pressure in Liquids

Buoyancy (Archimedes’

Principle)

Viscosity

Cohesion and Adhesion

Surface Tension

Capillary Action

C.

D.

1.

2.

1.

2.

3.

4.

5.

6.

Liquid-Vapor Phase

Changes

Boiling

Evaporation, Vapor Pressure, and Humidity

Properties of Gases

Kinetic Activity of Gases

Molar Volume and Gas

Density

Gaseous Diffusion

Gas Pressure

Partial Pressure (Dalton’s

Law)

Solubility of Gases in Liquids

(Henry’s Law)

II. Change of State

A.

1.

2.

Liquid-Solid Phase Changes

Melting

Freezing http://www.youtube.com/watch?v=j2KZmRIKea8

Start at 3:15

A. Liquid-Solid Phase Changes

1.

Melting

?

When a solid is heated, what happens to its kinetic energy?

What happens to its intermolecular forces?

5

A. Liquid-Solid Phase Changes

2. Freezing

?

When a liquid is cooled, what happens to its kinetic energy?

What happens to its intermolecular forces?

6

A. Liquid-Solid Phase Changes

A. Liquid-Solid Phase Changes

Melting and Boiling

Melting Point:

The temperature at which a solid converts to a liquid

Boiling Point

The temperature at which a liquid converts to the gaseous state

Substance

Water

Oxygen

Melting Point

0 °C

-219 °C

Boiling Point

100 °C

-183 °C

8

A. Liquid-Solid Phase Changes

Melting and Boiling

Latent Heat:

The amount of heat needed for a substance to change its state of matter

Latent heat of fusion:

The amount of heat needed to change a solid to a liquid

Latent heat of vaporization

The amount of heat needed to change a liquid to a gas

9

A. Liquid-Solid Phase Changes

Latent heat of vaporization

Steam

Latent heat of fusion Water

Ice

10

II. Change of State

B.

1.

2.

3.

4.

5.

6.

Properties of Liquids

Pressure in Liquids

Buoyancy (Archimedes’ Principle)

Viscosity

Cohesion and Adhesion

Surface Tension

Capillary Action

B. Properties of Liquids

Liquid Oxygen http://www.youtube.com/watch?v=ndtmfDoI8PM

B. Properties of Liquids

Liquid molecules also possess attractive forces

 but these forces are much weaker in liquids than in solids

Liquid molecules have greater freedom of movement and possess more KE than solids

This is why liquids take the shape of their container

And are capable of flow

Liquids cannot be easily compressed

13

B. Properties of Liquids

1. Pressure in Liquids

Is the same at any specific depth, regardless of the container ’ s shape

Is exerted equally in all directions

14

B. Properties of Liquids

1. Pressure in Liquids

Pascal ’ s Principle:

A confined liquid transmits pressure equally in all directions

15

B. Properties of Liquids

1. Pressure in Liquids

Pascal ’ s Principle

Downward

16

B. Properties of Liquids

1. Pressure in Liquids

Liquids are capable of flow

Pascal ’ s Principle

Sideways

17

B. Properties of Liquids

1. Pressure in Liquids

Pascal ’ s Principle

Upward

18 http://www.youtube.com/watch?v=iD55ynlUH8g http://www.youtube.com/watch?v=UpwLwP0pmwk

B. Properties of Liquids

1.

Pressure in Liquids

Clinical Application

Heart Failure

19

B. Properties of Liquids

1.

Pressure in Liquids

Clinical Application

Using an air or water mattress to prevent the development of bed soars

20

B. Pressure in Liquids

2. Buoyancy (Archimedes’ Principle)

Buoyancy occurs because the pressure below a submerged object always exceeds the pressure above it

B. Pressure in Liquids

2. Buoyancy (Archimedes’ Principle)

According to Archimedes

This buoyant force must equal the weight of the fluid displaced buy the object http://www.youtube.com/watch?v=mhJ5Ybt7L2k http://www.youtube.com/watch?v=vJ36urazDu4&list=PLB76160897CFFC3F4&index=8&feature=plpp_video

B. Pressure in Liquids

2. Buoyancy (Archimedes’ Principle)

Gases also exert buoyant force

Buoyancy helps keep solid particles suspended in gases

These suspensions, called aerosols, play an important role in respiratory care.

B. Properties of Liquids

3. Viscosity

Internal force that opposes flow of a fluid, either liquids or gases

Fluid’s viscosity is directly proportional to cohesive forces between its molecules

The stronger the cohesive forces, the greater the fluid viscosity

Heart must use more energy when blood viscosity increases, as occurs in polycythemia

B. Properties of Liquids

3. Viscosity

Clinical Application

The greater the viscosity of a fluid, the more energy is needed to make it flow

The heart must perform more work when blood viscosity increases

Polycythemia: an increase in red blood cells

Polycythemia is common in patients with chronic bronchitis

25

B. Properties of Liquids

4. Cohesion and adhesion

The attractive force between like molecules is cohesion.

The attractive force between unlike molecules is adhesion.

26

Cohesion and Adhesion

Water

Concave meniscus

Adhesion > Cohesion

27

Cohesion and Adhesion

Mercury

Convex meniscus

Cohesion > Adhesion

28

B. Properties of Liquids

5. Surface Tension

 a force exerted by like molecules at a liquid’s surface

The cohesive forces between liquid molecules are responsible for this phenomenon

B. Properties of Liquids

5. Surface Tension

B. Properties of Liquids

5. Surface Tension

B. Properties of Liquids

5. Surface Tension

Explains why liquid droplets and bubbles retain a spherical shape

B. Properties of Liquids

5. Surface Tension

In bubbles

B. Properties of Liquids

5. Surface Tension

Laplace ’ s Law

The pressure within a sphere

Varies directly with the surface tension of the liquid

As the surface tension of the liquid increases, the internal pressure increases

Varies inversely with its radius

As the droplet becomes smaller and the radius decreases, the internal pressure increases

P = 4ST r

34

B. Properties of Liquids

5. Surface Tension

Laplace’s Law

35 http://www.youtube.com/watch?v=RAmx4_G9XsQ

B. Properties of Liquids

5. Surface Tension in alveoli

Surface Tension

Surface tension in alveoli

Alveoli with increased surface tension

Have a greater tendency to collapse

Require greater distending pressure to maintain their volume

37

B. Properties of Liquids

5. Surface Tension in alveoli

Clinical Application:

Atelectasis

38

B. Properties of Liquids

5. Surface Tension

Normal CXR after the application of Continuous Positive

Airway Pressure (CPAP)

B. Properties of Liquids

5. Surface Tension

The lung reduces surface tension of alveoli by the production of a complex surface tension reducing chemical mixture called

SURFACTANT http://www.youtube.com/watch?v=Gpcbetob4p4

40

B. Properties of Liquids

5. Surface Tension

Clinical Application

The first breath of life

B. Properties of Liquids

5. Surface Tension

Artificial surfactant administration in Infant Respiratory

Distress Syndrome

B. Properties of Liquids

5. Surface Tension

Clinical Application

 Liquid Ventilation http://www.youtube.com/watch?v=2OxstD2jN08

B. Properties of Liquids

6. Capillary Action

A phenomenon in which a liquid in a small tube moves upward, against gravity

B. Properties of Liquids

6. Capillary Action http://www.youtube.com/watch?v=mdkeZbm0cCI

B. Properties of Liquids

6. Capillary Action

Clinical Examples

 Capillary blood stick http://www.youtube.com/watch?v=q5J1cCyrASs

B. Properties of Liquids

6. Capillary Action

Clinical Examples

 Absorbent wick humidifiers

C. Liquid-Vapor Phase Changes

1.

2.

Boiling

Evaporation, Vapor Pressure, and Humidity

C. Liquid-Vapor Phase Changes

49

Liquid to vapor phase changes (vaporization)

2 types of vaporization

Boiling  heating liquid to temperature at which its vapor pressure exceeds atmospheric pressure

Boiling point of most liquefied gases is very low

Liquid oxygen boils at -183°C

Evaporation  when liquid changes into gas at temperature below its boiling point

Evaporation requires heat. The heat energy required for evaporation comes from the air next to the water surface. As the surrounding air loses heat energy, it cools. This is the principle of evaporative cooling, which was previously described.

Water enters atmosphere via evaporation when at temperature lower than its boiling point (water vapor)

Molecular water exerts pressure called water vapor pressure

Temperature influences evaporation most

The warmer the air, the more vapor it can hold

C. Liquid-Vapor Phase Changes

2. Evaporation, Vapor Pressure and

Humidity

Evaporation: the change in state of substance from a liquid to a gaseous state below its boiling point.

Molecular water exerts a pressure called the water vapor pressure

50

C. Liquid-Vapor Phase Changes

2. Evaporation, Vapor

Pressure and Humidity

State of equilibrium: for every molecule escaping into the air another returns to the water reservoir

51

C. Liquid-Vapor Phase Changes

2. Evaporation, Vapor Pressure and Humidity

Influence of Temperature

The warmer the air, the more water vapor it can hold

The capacity of air to hold water vapor increases with temperature

Thus, the warmer the air contacting a water surface, the faster the rate of evaporation

52

C. Liquid-Vapor Phase Changes

2. Evaporation, Vapor

Pressure and Humidity

Influence of Temperature

If water is heated, its kinetic energy is thus increased and thus more molecules are helped to escape from its surface.

53

C. Liquid-Vapor Phase Changes

2. Evaporation, Vapor Pressure and Humidity

Influence of Temperature

54

C. Liquid-Vapor Phase Changes

2. Evaporation, Vapor Pressure and Humidity

Clinical Application

55

C. Liquid-Vapor Phase Changes

2. Evaporation, Vapor Pressure and Humidity

Influence of Pressure

High atmospheric pressures impede vaporization

Low atmospheric pressures increase vaporization

56

C. Liquid-Vapor Phase Changes

2. Evaporation, Vapor Pressure and Humidity

Influence of surface area

The greater the available surface area of the gas in contact with air, the greater the rate of liquid evaporation

57

C. Liquid Vapor Phase Chapges

2 Evaporation, Water Vapor Pressure, and Humdidty

Humidity: water in molecular vapor form

Water vapor pressure: the kinetic activity of water molecules in air

For the actual amount or weight of water vapor in a gas to be found, the water vapor content (absolute humidity) must be measured

58

C. Liquid-Vapor Phase Changes

2. Evaporation, Water Vapor Pressure, and Humidity

Absolute Humidity

 a.k.a

 water vapor content

Actual amount (or weight) of water vapor in gas

Measured in mg/L

Varies w/ temperature & pressure

Air that is fully saturated w/ water vapor has absolute humidity of 43.8 mg/L at 37°C, 760 mm

Hg, & water vapor pressure of 47 mm Hg

59

Egan Table 6-3, page 112

C. Liquid-Vapor Phase Changes

2. Evaporation, Water Vapor Pressure , and Humidity

Relative humidity (RH)

When gas is not fully saturated

Water vapor content can be expressed in relative terms

Ratio of its actual water vapor content to its saturated capacity at given temperature

%RH = Content (Absolute Humidity) x 100

Saturated Capacity

C. Liquid-Vapor Phase Changes

2. Evaporation, Water Vapor Pressure, and Humidity

Example: At a temperature of 22°C, air has the capacity to hold 19.4 mg/L of water vapor (this information comes from the table in Egan). If the absolute humidity in the air is 7.4 mg/L, what is the relative humidity?

62

C. Liquid-Vapor Phase Changes

2. Evaporation, Water Vapor Pressure, and Humidity

Temperature = 22°C

Capacity = 19.4 mg/L of water vapor

Water vapor content (AH) = 7.4 mg/L

%RH = water vapor content x 100 capacity

63 http://www.youtube.com/watch?v=CL5cgXwKUXc

C. Liquid-Vapor Phase Changes

2. Evaporation, Water Vapor Pressure, and Humidity

Percent Body Humidity

The ratio of the actual water vapor content of the gas to the water vapor capacity in a saturated gas at body temperature (37°C)

%BH = water vapor content x 100 capacity at 37° C

Capacity at 37°C is always 43.8 mg/L

64

Clinical Application

Aerosol Therapy

2. Evaporation, Water Vapor Pressure, and Humidity

Clinical Aplication

 Aerosol Therapy

65

C. Liquid-Vapor Phase Changes

2. Evaporation Water Vapor Pressure, and Humidity

Example: The American National Standards Institute has set a water vapor content level of 30 mg/L as the minimum absolute humidity required for patients whose upper airways have been bypassed. This equals what body humidity?

Water vapor content = 30 mg/L

%BH = water vapor content x 100 capacity at 37° C

66

C. Liquid-Vapor Phase Changes

2. Evaporation Water Vapor Pressure, and Humidity

Humidity Deficit

The difference in water vapor content between inspired air and the saturated gas conditions present in the lungs

The amount of water vapor your body must add to the inspired gas to achieve saturation at body temperature

HD=43.8 mg/L–water vapor content

67

C. Liquid-Vapor Phase Changes

2. Evaporation Water Vapor Pressure, and Humidity

Example:

Using the previous example where water vapor content =

30 mg/L

What is the humidity deficit?

HD=43.8 mg/L–water vapor content

68

C. Liquid-Vapor Phase Changes

2. Evaporation Water Vapor Pressure, and Humidity

Condensation: The change of state from gas to liquid

Dew Point: The temperature at which condensation begins

69

C. Liquid-Vapor Phase Changes

2. Evaporation Water Vapor Pressure, and Humidity

Clinical Application

70

II. Change of State

D.

1.

2.

3.

4.

5.

6.

Properties of Gases

Kinetic Activity of Gases

Molar Volume and Gas Density

Molar Volume

Density

Gaseous Diffusion

Gas Pressure

Measuring Atmospheric Pressure

Clinical Pressure Measurements

Partial Pressure (Dalton’s Law)

Solubility of Gases in Liquids (Henry’s Law)

C. Properties of Gases

Gases do not maintain their shape and volume, they expand to fill the available space

Gases are easily compressed and expanded

Gases are capable of flow (like liquids)

72

C. Properties of Gases

1. Kinetic Activity of Gases

Molecular attractive forces are extremely weak in gases, therefore gasses possess the greatest amount of KE, their PE is minimal

Gas molecules travel at high speeds in random fashion with frequent collisions.

The velocity of gas molecules is directly proportional to its temperature.

C. Properties of Gases

2. Molar Volume and Gas Density

Molar Volume

1 gram molecular weight (gmw), or mole, of any substance at a temperature of 0 ° C (273 K) and a pressure of 1 atm

 occupies 22.4 L (molar volume) contains 6.023 x 10 23 (Avogadro’s number) molecules

C. Properties of Gases

2. Molar Volume and Gas Density

Molar Volume

Equal volumes of all gases under the same conditions must contain the same number of molecules

 Molar volume = 22.4L

1 mole of Helium

1 mole of Oxygen has the same number of molecules as…

C. Properties of Gases

2. Molar Volume and Gas Density

Gas Density

Density:

 the ratio of a substance’s mass to its volume mass per unit volume

Density = gmw

22.4 L

Gas Density

A dense substance has heavy particles packed closely together (Uranium is a good example of a dense substance)

Conversely, a low density substance has a low concentration of light weight particles per unit volume (Hydrogen gas).

The density of any gas at STPD can be computed easily by dividing its molecular weight by the universal molar volume of 22.4 L

GMW: O2 = N2 = He = CO2 =

78

Density of Gases

GRAM MOLECULAR WEIGHTS( GMW): The molecular weight of a substance in grams. To find the GMW of a medical gas we must know the atomic weights of several common chemical elements.

Substance Symbol Atomic Weight

A) Hydrogen

B) Helium

C) Carbon

D) Nitrogen

E) Oxygen

F) Room Air

H

He

C

N

O

1

4

12

14

16

28.8

NOTE: Nitrogen and Oxygen are found in the atmosphere in gaseous form as diatomic elements. So oxygen gas will have an atomic weight of 16 X 2 or 32, and nitrogen gas will have an atomic weight of 14 X 2 or 28.

Gas Density Example #1

What is the density of oxygen at STP?

Density = gmw

22.4 L

80

Density of O2

O2 = 32 grams

O = 8x2= 16

O2 = 16 x 2 = 32

32/22.4 = 1.42

Gas Density Example #2

What is the density of air?

Density = gmw

22.4 L

82

Density of Air

N= 14 x 2 = 28; O= 16 x 2 = 32

28 x 79% = 22.12

16 x 21%= 6.72

22.12 + 6.72 = 28.84 / 22.4 = 1.28

Density of Gases

Gases are influenced by changes in temperature and pressure

Calculates under STP conditions

Calculated by dividing volume occupied by 1 mole of gas at STP, that is 22.4 liters, into the gram of molecular weight of that gas

Density = gram molecular weight / 22.4 liters

Example:

Density of O2 = Weight of O2 32g /22.4 liters = 1.43g/L

Gases such as Helium have far less density

Oxygen has higher density than air and tends to accumulate at the lowest point (Ex: oxygen enclosure)

Density of Room Air

GMW OF ROOM AIR: Room air is not a pure substance; it is a mixture of gases. It contains about 79% nitrogen (N2) and 21% oxygen (O2) and small amounts of other gases. We can determine the relative GMW for room air by multiplying the fractional concentration of each gas by its molecular weight and adding the results.

The GMW of room air can also be used to find the specific gravity of other medical gases because air is the usual standard for specific gravity of gases.

GMW air

GMW air =

=

=

28.8

Nitrogen

(.79 x 28)

( 22.1 )

Oxygen

+ (.21 x 32)

+ ( 6.7 )

NOTE: The above method can also be used to find the relative GMW of any mixture of gases, ie: 60% He and 40% O2 or 95% O2 and 5% CO2.

Practice!

Calculate the density of the following gases:

1.

CO2

2.

3.

4.

5.

N2

He

80% He and 20% O2

70% He and 30% O2

86

CO2

C= 12

O2 = 32

12 + 32 = 44 /22.4 = 1.96

N2

N= 14

N2 = 14 x2 = 28

28 /22.4 = 1.25

He

He = 4 /22.4 = 0.18

80% He and 20% O2

He = 80% x 4 = 3.2

O2 = 20% x 32= 6.4

3.2 + 6.4 = 9.6/ 22.4

0.43

C. Properties of Gases

2. Molar Volume and Gas Density

Density

Clinical Example: Helium/Oxygen

Flow Rate Conversion

An oxygen flow meter is being used to administer 8

L/min of an 80%He/20%O2 gas mixture. What is the actual flow rate of this gas mixture?

Actual flow rate of 80%he/20%O2

= Flow rate x 1.8

= 8 L/min x 1.8

FYI: the conversion factor for

70/30 Heliox = 1.6

91

= 14.4 L/min

C. Properties of Gases

2. Molar Volume and Gas Density

An oxygen flow meter is being used to administer 8

L/min of an 80%He/20%O2 gas mixture. What is the actual flow rate of this gas mixture?

Actual flow rate of 80%he/20%O2

= Flow rate x 1.8

FYI: the conversion factor for

70/30 Heliox = 1.6

92

Practice!

1.

An oxygen flow meter is being used to administer 10

L/min of an 70%He/30%O2 gas mixture. What is the actual flow rate of this gas mixture?

2.

A therapist wants to deliver 15 L/min of an

80%He/20%O2 gas mixture. What liter flow should the therapist set on the flowmeter?

93

C. Properties of Gases

3. Gaseous Diffusion

The movement of gas molecules from an area of high concentration to an area of low concentration.

 http://www.youtube.com/watch?v=_oLPBnhOCjM

C. Properties of Gases

3. Gaseous Diffusion

Graham’s Law:

The rate of diffusion of a gas is inversely proportional to the square root of its density.

Lighter gases diffuse rapidly

Heavy gases diffuse more slowly

95

C. Properties of Gases

3. Gaseous Diffusion

Practical Application:

What is the GMW of O

2

?

What is the GMW of CO

2

?

According to Graham’s Law, which gas should diffuse faster?

96

C. Properties of Gases

6. Solubility of Gases in Liquids

Henry’s Law: The amount of gas that dissolves in a liquid at a given temperature is proportional to the partial pressure of the gas and its solubility coefficient

Solubility coefficient: the volume of a gas that will dissolve in 1 mL of a given liquid at standard pressure and specified temperature

C. Properties of Gases

6. Solubility of Gases in Liquids

Practical Example:

0.023 mL of O

2

37 ° C can dissolve in 1 mL of blood at

0.510 mL of CO

2

37 ° C can dissolve in 1 mL of blood at

According to Henry’s Law, which gas should dissolve faster?

98

Diffusion: CO2 vs. O2

In the end, CO2 diffuses about 19 x faster than O2 because of its much greater solubility in blood.

99

Gas Diffusion

Fick’s law

.

Fick ’ s Law of Diffusion

The rate of diffusion across a sheet of tissue (the alveolar-capillary membrane) is:

Directly proportional to the

Surface area of the tissue

Solubility of the gas

Partial pressure gradient

Inversely proportional to the

Thickness of the tissue

Fick’s Law

Diffusion is Directly Proportional to

Surface Area

What is the surface area of the alveoli?

Fick’s Law

Diffusion is Directly Proportional to

Surface Area

A decreased alveolar surface area

Alveolar collapse

Fluid in the alveoli

Decreases the diffusion of oxygen into the pulmonary capillary blood

Fick’s Law

Diffusion is Directly Proportional to the

Concentration Gradient

Fick’s Law

Diffusion is Directly Proportional to the

Concentration Gradient

Decreased alveolar oxygen pressure (P

A

O

2

)

High altitudes

Alveolar hypoventilation

Decreases the diffusion of oxygen into the pulmonary capillary blood

Fick’s Law

Diffusion is Inversely Proportional to

Tissue Thickness

Fick’s Law

Diffusion is Inversely Proportional to

Tissue Thickness

An increased alveolar tissue thickness

Alveolar fibrosis

Pulmonary edema

Decreases the diffusion of oxygen into the pulmonary capillary blood

Fick ’ s Law of Diffusion

The rate of diffusion across a sheet of tissue (the alveolar-capillary membrane) is:

Directly proportional to the

Surface area of the tissue

Solubility of the gas

Partial pressure gradient

Inversely proportional to the

Thickness of the tissue

Fick’s Law

Figure 4-8.

C. Properties of Gases

4. Gas Pressure

All gases exert pressure

Gas pressure in a liquid is known as gas “tension”

Atmospheric pressure is measured with a barometer

Pressure: the force that a gas exerts over a given area

P = Force/Area

 lb/in 2

C. Properties of Gases

4. Gas Pressure

Atmospheric Pressure: The pressure that the atmospheric gases exert on objects within the Earth’s atmosphere.

Gases that make up the atmosphere are attracted to the Earth’s surface by gravity.

Highest near the Earth’s surface

Sea level

760 mmHg

Denver: 1 mile above sea level

630 mmHg

112

Atmospheric

Pressure

Measured with a barometer

Evangelista Torricelli

The mercury barometer uses the weight of a column of mercury to equilibrate with the force of the gas molecules hitting the surface of a mercury reservoir

Atmospheric Pressure at Sea Level

760 mmHg

760 torr

29.9 inHg

1034 cmH

2

O

1034 g/cm 2

33.9 ftH

2

O

101.3 kPa

14.7 psi

14.7 lb/in 2

1 atm

113

Clinical Pressure Measurements

114

115

Aneroid

Barometer

116

Mechanical

Manometer

117

Strain-gauge Pressure

Transducer

C. Properties of Gases

5. Dalton’s Law of Partial Pressures

Dalton’s Law

the sum of the partial pressures of a gas mixture equals the total pressure.

Partial pressure:

the pressure exerted by a single gas in a mixture

118

Dalton’s Law of Partial Pressures

The partial pressure of any gas within a gas mixture is proportional to its percentage in the mixture

P

B

= PN

2

+ PO

2

+ PH

2

O + PAr + PCO

2

+ Pgases

119

Dalton’s Law of Partial Pressures

Air ≈ 21% O

2 and 79% N

2

Fractional concentration of O

Fractional concentration of N

2

2

= 0.21

= 0.79

partial pressure = fractional concentration x total pressure

PO2 =

PN2 =

120

Dalton’s Law of Partial Pressures:

What happens to PB, PO2, and FiO2 as altitude changes?

Why do mountain climbers use extra oxygen at high altitudes?

121

Dalton’s Law of Partial Pressures

Why are oxygen masks Needed on Airplanes?

122

Dalton’s

Law of

Partial

Pressures

Hyperbaric

Chambers

123

Download