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    Regional Difference inVentilation

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    Byprof/Hala Salah

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    Regional difference in

    ventilationVentilation is the amount of

    gas moved in and out of aregion irrespective to theinitial volume of that region.

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    Regional difference in ventilation

    Slinky springIn the uprightposition, the lungs

    under the effect ofgravity are suspendedin the thoracic cavitylike a suspendedslinky spring.

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    Regional difference in ventilation

    When thisspring is freelysuspended, it willbe stretchedmainly at theupper part .

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    Regional difference in ventilationWhen it is pulled

    down, its lengthincreases mainlyin the lower part.

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    Regional difference in ventilation

    In the standing position, the gravity pullsthe lung down. This makes the IPP at theapex of the lung more negative than at the

    base.IPP at the apex -10cmH2O.

    At the base of the lung, IPP about -2.5

    cmH2O .At the mid thoracic position.

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    Regional difference in ventilation

    Apex of the lung Base of the lung

    IPP more negative -10 cmH2O IPP less negative -2.5 cm H2Olarge expanding pressure Small expanding pressureBig resting volume and apical

    alveoli are more expandedSmall resting volume and

    alveoli are less expanded

    Small change in volume duringinspiration Large change in volume duringinspiration

    less ventilated under resting

    conditionmore ventilation under resting

    condition

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    Regional difference in ventilation

    In recumbent position ventilation oflower most part (posterior) exceeds that

    of the upper most part (anterior of thelung).

    In the lateral position (subject on hisside) the dependent lung is bestventilated.

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    Regional difference in ventilationDuring exercise ventilation

    increases at the apex of the lungs and

    the regional difference between apexand base decreases.

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    100150

    47mmHg

    28mmHg

    120mmHg

    565mmHg

    760mmHg

    Expired air

    47mmHg

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    Causes of differences between atmosphericair and alveolar air

    Alveolar air is only partially replaced by

    atmospheric air with each breath.O2 continuously diffuses from thealveolar air into the pulmonary blood.

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    Causes of differences betweenatmospheric air and alveolar air

    CO2 continuously diffuses from the

    pulmonary blood into the alveoli.

    Dry atmospheric air that enters the

    respiratory passage is humidified evenbefore it reaches the alveoli.

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    Diffusion

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    DiffusionIs the exchange betweenalveolar and blood gases

    (O2 and CO2) through

    the alveolo-capillarymembrane.

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    Respiratory Membrane

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    DiffusionDiffusion through tissues is described byFick's law which states that:

    Surface area X solubility X Pressure gradient

    D Root M.wtThickness x Sq

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    Factors affecting the rate of diffusionthrough respiratory membrane

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    1. Thickness of membrane:

    The overall thickness=0.5 micron.

    Thickness increases in:

    1. Pulmonary fibrosis

    2. Pulmonary oedema

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    2. Surface area of the membrane

    The surface area of the respiratorymembrane is very large about 50-100 m2 inthe normal adult.

    The surface area is decreased in:

    1. Removal of one lung.

    2. Emphysema .

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    3. Pressure gradient

    100 mmHg

    100mmHg

    46mmHg

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    4. The diffusion coefficient

    Depends on :

    Solubility of gas in the membrane .

    Square root of its molecular weight.

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    A. The Solubility of the gas

    It is calculated as the volume of the gas thatdissolves in 1ml of the liquid.

    The greater the solubility of the gas in thefluid, the more the amount that is dissolved.

    CO2 Solubility is very high than for O2 i.e. the

    solubility of CO2 is 24 times greater than O2.

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    B.Square root of the molecular weight

    Molecular weight of O2 32.

    Molecular weight of CO2 44.

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    The net result is that:

    Diffusion coefficient for CO2through the tissue sheet is about

    20 times faster than O2.

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    Diffusion capacity of theRespiratory membrane

    It is defined as:

    The volume of a gas that

    diffuses through themembrane each minute with

    a pressure difference of 1mmHg.

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    Diffusion capacity

    Diffusion capacity for O2

    At rest : 25ml/min/mmHg.

    During exercise :65ml/min/mmHg

    It decreases in lungdiseases as in fibrosis.

    Diffusion capacity for CO2

    At rest: 400ml/min/mmHg.

    During exercise: 1200ml/min/mmHg

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    Equilibration

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    Equilibration

    It is the equalization of pressures ofgases across respiratory membrane.

    Blood O2

    tension and the alveolar O2

    tension equalize in about 0.25 second

    (Equilibration time).

    In normal lungs blood travels alongpulmonary capillaries in about 0.75second (Transit time).

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    Po2=100mmHgp

    co2=40mmHg

    0.25

    40

    46

    0.75

    capillary

    alveolus

    100

    40

    Po2=40 mmHg

    Pco2=46 mmHg

    Po2=100 mmHg

    Pco2=40mmHg

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    EquilibrationThere is about 0.5 sec with noincrease in O2 content, this time

    provides safety margin .It ensures an adequate O2 uptakeduring periods of stress e.g.

    during exercise as the circulation isfast .

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    Transit time during exercise

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    For CO2

    Diffusion of CO2 is more rapidly than O2but the whole equilibration for CO2 is thesame as that for O2 (0.25 sec) because:-

    1. The reactions releasing CO2 from blood isrelatively slow.

    2. The pressure gradient driving CO2 from

    blood to alveolus is only 6 mm Hg ,whilethat driving O2 in the opposite directionis 60 mm Hg.

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