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Functions of the respiratory system
Provides a means of gas exchange between the environment and the body
What are the functions of the respiratory system
Maintain a constant O2 and CO2 levels in blood, acid base balance (rest and exercise)
What is the difference between respiration and ventilation
Ventilation is the process of moving air in and out of the lungs, respiration is ventilation PLUS exchanging of gases in lungs
Internal respiration
At the cellular level
External respiration
At the lung
2 functional zones in the lung
Conducting zone and respiratory zone
Conducting zone
AIr passes through alveoli (anatomical dead space)
What percent of lung volume is conducting zone
10% of total lung volume
Respiratory zone
Where gas exchange occurs (in the alveoli, there are 300-500 million alveoli)
What percent of lung volume is respiratory zone
90% of total lung volume
Surface area of respiratory zone
50 - 75 m squared (half of a tennis court)
Alveolar ducts and alveoli
Alveolar ducts lead to alveoli, which are tiny air sacs in the lungs where gas exchange occurs
Epithelial cells and capillaries
Thin epithelial cells and surrounding capillaries form the respiratory membrane that allows oxygen and carbon dioxide to diffuse between the lungs and blood
Why do we need this much surface area in the lung?
Gas exchange, the more gas exchange, the easier it is to function and do daily activites and tasks (cannot get oxygen to muscles)
What are the two zones in the lungs and what is the function of each
Conducting and respiratory zone. Conducting zone is where air passes through the alveoli nad the respiratory zone is where gas exchange occurs
How does the respiratory zone work
Oxygen moves across the alveoli into the capillaries and for CO2 from the capillaries to the alveoli to be expired
Inspiration at rest
Diaphragm contracts down and ribs move up and out (lungs are expanded)
Expiration at rest
Diaphragm relaxes and moves up and ribs move down and in (lungs passively recoil)
Sea level atmospheric pressure for inspiration and expiration
760 mmHg
Intrapulmonic pressure for inspiration
758 mmHg (air moves down the pressure gradient)
Intrapulmonic pressure for expiration
763 mmHg (air is expired so it moves from high pressure to low)
Boyles law
At constant temperature, pressure and volume inversely proportional
Example of Boyles law
For expiration, pressure is higher (763) so volume is low (because you are blowing out air)
How does the diaphragm act during inspiration
Contracts down
How are resting and exercise pulmonary volumes measured
Using spirometry (lung volumes, capacities, flow rates)
Tidal volume
Amount of air moved per breath
Resting tidal volume
12 breaths per min x ½ a liter each breath = 6 L/min
VE
Minute ventilation
Vital capacity (VC)
Greatest amount of air that can be expired after full inspiration
Resting vital capacity
3.5 - 4.5 L
Residual volume (RV)
Amount of air left in the lungs after full expiration (functions to keep the alveoli open even after maximum expiration)
Resting residual volume
1.5 - 1.9 L
Changes in residual volume
It will stay the same for years (up to about 5), unless there is a big change in smoking, diet, exercise
Total lung capacity (TLC)
Sum of vital capacity and RV
Ventilation at rest
VE + (tidal volume) x frequency of breaths → (0.5 L/breath) x 12 breath/min → 6 L/min
Resting cardiac output
5 L/min
Ventilation during exercise
The rate and depth of inspiration increases during exercise (activation of respiratory muscles which allow for greater pressure changes and more air movement)
How does ventilation change during exercise
Onset of exercise, there is an immediate increase in ventilation (both tidal volume and breathing frequency increase)
Max ventilation
40 breath/min x 3L/breath = 120 L/min
Ventilation increase proportional to metabolic needs of muscle
At low exercise intensity, only tidal volume increases first; at high exercise intensity, frequency or rate increases first
Which increases first, breath depth or breathing rate
Increase tidal volume, so depth
Gases diffusion
Move from areas of high pressure to low pressure
Sites of gas diffusion in the body
Alveoli - capillary interface and tissue capillary interface
Factors that effect gas exchange
Gas solubility, pressure gradient, diffusion pace, and surface area
Gas solubility
More solubility of the gas, the more gas exchange that occurs
Pressure gradient
Greater the gradient, more gas exchange that happens
Diffusion pace
Space between blood, capillary and the alveoil’s (cells of the lungs)
How diffusion pace works
Greater space between the blood and lungs, less gas exchange (if they are closer, more gas exchange)
Surface area
More surface area, more gas exchange
At high intensity exercise, how is ventilation modulated to meet the increased metabolic needs?
Increased rate/frequency (breaths/min)
Partial pressure of gases
Each gas exerts a given amount of pressure, this is partial pressure of that gas
Atmospheric gas fractions at sea level (oxygen)
.2093
Atmospheric gas fractions at sea level (nitrogen)
.7904
Atmospheric gas fractions at sea level (carbon dioxide)
.0003
What happens to atmospheric pressure in higher altitudes
It reduces (gets smaller)
Are the gas fractions the same at higher altitudes or are they lower
They stay the same
What is the change in atmospheric pressure due to
Gravity, it causes gas molecules to be close near the ground and temperature
If the atmospheric pressure if 720 mmHg, what is the PO2?
150.7 mmHg
Is the surface area positively or negatively related to gas exchange
Positively, larger surface area allows for more gas exchange
Gas transport
Oxygen must move from atmosphere to alveoli to blood to skeletal muscle (goes down the pressure gradient)
Transport of oxygen in the blood
Can carry 20 mL/O2 /100 mL of blood, 1L O2 /5L blood
Oxygen combining in blood
98.5 combines with hemoglobin and 1.5% dissolves in plasma
Hemoglobin saturation
Depends on PO2 and affinity between O2 and HB
Affinity
Strength of bond between two molecules
A-VO2 difference
Difference between arterial and venous O2, (how much oxygen has been extracted from any muscle tissue)
Arterial O2 content
20 mL O2/100 mL blood
a-vO2 difference at rest
4 -5 mL O2/ 100 mL blood
3 different CO2 transport ways
10% dissolved in plasma, 20% bound to hemoglobin, 70% formed as HCO3- on RBC
Bicarbonate ion
Transports 70% of CO2 in blood into lungs, CO2 + water = Carbonic acid (H2CO3). Occurs in RBC and catalyzed by carbonic anhydrase
What does carbonic acid dissocitate into
Bicarbonate
Equation for carbonic acid dissocitating
CO2 + H2O ←> H2CO3 ←> HCO3- + H+
What is happening during carbonic acid dissociating
Carbon dioxide broken down into bicarbonate and hydrogen and moves around in the blood until it reaches the lungs and then the equation reverses so that carbon dioxide and water and be expired
Where do the parts of the equation diffusion into
Bicarbonate ion diffuses from red blood cells into plasma and H+ binds to hemoglobin
Dissolved carbon dioxide
10% of CO2 dissolved in plasma, when PCO2 is low (in lungs) CO2 comes out of solution and diffuses out into alveoli
Carbanminohemoglobin
No competition for binding spots on hemoglobin because oxygen binds to hemo protein while CO2 binds to globin portion, 20% of CO2 transported bound to hemoglobin
What is VT
Ventiltory threshold is when the body shifts from primarily aerobic metabolism to increased reliance on anaerobic glycolysis and is considered a strong predictor of aerobic performance
Diffusion/pressure gradient at sea level
Pressure: 760 mmHg Diffusion: 60 mmHg
Diffusion/pressure gradient at 4,300 m
Pressure: 460 mmHg Diffusion: 15 mmHg
What happens at high altitudes
Less oxygen gets to muscles
Live High, Train low
If you live at high altitudes and get used to that adaptation you will do better training/competing at lower altitudes and it will give you the best results (get erythropoiesis stimulus during rest and then able to train at higher intensity)
What is the best form of altitude training and how might this improve performance at sea level
Live high, train low is the best form of altitude training - living at high altitude allows for our bodies to detect low oxygen levels and in return release the hormone EPO. EPO stimulates red blood cell production and increases oxygen carrying capacity, allowing us to get more oxygen to the skeletal muscle and compete at higher intensities at sea level.
Describe the bicarbonate buffer system in your own words
In muscle tissue, cellular respiration produced CO2 as a waste product; as one of the primary roles of the cardiovascular system, most of this CO2 is rapidly removed from the tissues by its hydration to bicarbonate ion (via carbonic acid). The bicarbonate ion present in the blood plasma is transported to the lungs, where it is dehydrated back into CO2 and released during exhalation. These hydration and dehydration conversions of CO2 and H2CO3, which are normally very slow are facilitated by the enzyme carbonic anhydrase.
Max exercise a-vO2 difference
15 mL of O2 per deciliter of blood
What is the saturation of high Po2 (in the lungs)
Almost 100%
What is the saturation of low PO2 (in body tissues)
It is declining/ getting low
High Po2
Loading portion of O2 - hemoglobin dissociation curve, small change in HB saturation per mmHg change in PO2
Low PO2
Unloading portion of O2 - hemoglobin dissociation curve, large change in HB saturation per mmHg change in PO2