Oxygen saturation in a sample.

In summary, the problem involves converting the given vapour pressure of water and solubility of oxygen in water to units of partial pressure and concentration, respectively. Using the ideal gas law and converting units, we can calculate the 100% oxygen saturation to be 0.75 umol.
  • #1
drillman9
7
0

Homework Statement



Knowing that the vapour pressure of water at 25 C is 24 mm Hg, that the oxygen composition of air is 20% v/v and that the solubility of oxygen in water is 31.6 mL/L, demonstrate that the 100% O2 (oxygen) saturation is 0.75 umol (micromoles)


Homework Equations



pV=nRT ?

The Attempt at a Solution



I tried using pV=nRT taking into account the vapour pressure and getting a solution that was not 0.75 umol. I also attempted a ratio between the 31.6 mL/L as well as the density but I don't really know where to go from there.

Any help at coming to the solution would be much appreciated!
 
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  • #2


Thank you for your question. Let's break down the problem step by step.

First, we need to convert the given vapour pressure of water (24 mm Hg) to a partial pressure of oxygen. Since we know that oxygen makes up 20% of air by volume, we can calculate the partial pressure of oxygen as follows:

Partial pressure of oxygen = 20% of air by volume x total pressure of air
= 0.20 x 760 mm Hg (at sea level, assuming standard atmospheric pressure)
= 152 mm Hg

Next, we need to convert the solubility of oxygen in water (31.6 mL/L) to a concentration in units of moles per liter (mol/L). This can be done using the ideal gas law:

pV = nRT

Where:
p = partial pressure of oxygen (152 mm Hg)
V = volume of oxygen dissolved in water (31.6 mL)
n = number of moles of oxygen
R = gas constant (0.0821 L atm/mol K)
T = temperature (25°C = 298 K)

Rearranging the equation, we get:

n = (pV) / (RT)

Plugging in the values, we get:

n = (152 mm Hg x 31.6 mL) / (0.0821 L atm/mol K x 298 K)
= 0.006 mol

Finally, we need to convert the concentration of oxygen from moles per liter to micromoles (umol). Since 1 mol = 1,000,000 umol, we can simply multiply our calculated concentration by 1,000,000 to get the final answer:

Concentration of oxygen = 0.006 mol/L x 1,000,000 umol/mol
= 6,000 umol/L

Since we are looking for the 100% oxygen saturation, we can simply divide this value by 20% (since oxygen makes up 20% of air by volume) to get the final result:

100% oxygen saturation = (6,000 umol/L) / (20%)
= 0.75 umol

Therefore, the 100% oxygen saturation is 0.75 umol, as desired. I hope this explanation helps you better understand the problem and how to approach it. Keep up the good work in your studies!
 
  • #3


I would approach this problem by first understanding the concepts involved. Oxygen saturation refers to the amount of dissolved oxygen in a given sample. In this case, we are looking at the oxygen saturation in water at 25 C.

To start, we can use the ideal gas law (pV=nRT) to calculate the number of moles of oxygen (n) in the sample. We know that the volume (V) of the sample is 1 L (since we are using 31.6 mL/L as the solubility of oxygen in water), the temperature (T) is 25 C (298 K), and the pressure (p) is the atmospheric pressure (which we can assume is 1 atm or 760 mm Hg).

Using the ideal gas law, we can rearrange it to solve for n:

n= (pV)/(RT)

Substituting the values, we get:

n= (760 mm Hg * 1 L)/(0.08206 L atm/mol K * 298 K) = 31.6 mmol

Now, we need to convert mmol to umol (since the question asks for the answer in micromoles). There are 1000 umol in 1 mmol, so:

31.6 mmol * (1000 umol/1 mmol) = 31,600 umol

However, this is the total amount of oxygen in the sample. We need to find the amount of oxygen that is actually dissolved in the water. We can do this by multiplying the total amount of oxygen by the oxygen composition of air (20% v/v):

31,600 umol * 0.20 = 6,320 umol

Finally, we need to take into account the vapour pressure of water. This means that the total pressure in the sample is not just due to oxygen, but also due to water vapour. We can calculate the partial pressure of oxygen by subtracting the vapour pressure of water (24 mm Hg) from the atmospheric pressure (760 mm Hg):

760 mm Hg - 24 mm Hg = 736 mm Hg

Now, we can use the ideal gas law again to calculate the number of moles of oxygen at this partial pressure:

n= (pV)/(RT) = (736 mm Hg * 1 L)/(0.08206 L atm/mol K * 298 K)
 

Related to Oxygen saturation in a sample.

1. What is oxygen saturation in a sample?

Oxygen saturation in a sample refers to the amount of oxygen present in a sample compared to the maximum amount of oxygen it can hold at a given temperature and pressure. It is typically expressed as a percentage and is an important measure in various scientific fields, including medicine and environmental science.

2. How is oxygen saturation in a sample measured?

Oxygen saturation in a sample is measured using a device called a pulse oximeter. This device uses light to determine the amount of oxygen in the sample, typically by measuring the absorption of red and infrared light by the sample. The results are then displayed as a percentage on the device's screen.

3. What factors can affect oxygen saturation in a sample?

Several factors can affect oxygen saturation in a sample, including temperature, pressure, and the presence of other gases or substances. For example, a higher temperature can decrease the amount of oxygen that can dissolve in a liquid sample, resulting in lower oxygen saturation.

4. Why is oxygen saturation in a sample important?

Oxygen saturation in a sample is important because it can provide valuable information about the health and quality of a sample. In medical settings, it can indicate the level of oxygen in a patient's blood and help diagnose conditions like respiratory diseases. In environmental science, it can provide insights into the health of ecosystems and the effects of pollution.

5. Can oxygen saturation in a sample change over time?

Yes, oxygen saturation in a sample can change over time. This can be due to various factors, such as changes in temperature, pressure, or the introduction of other substances. It is important to monitor oxygen saturation over time to understand any changes and their potential impact on the sample or system being studied.

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