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Pie
4 years ago
15

Polypeptides and proteins must fold properly to be functional. Hydrogen bonds between the oxygen and nitrogen atoms of the pepti

de bonds are crucial to which level of protein structure?
Chemistry
1 answer:
Lubov Fominskaja [6]4 years ago
4 0

Answer:

Secondary structure

Explanation:

Stricture of proteins can be categories into 4

Primary structure, secondary structure, tertiary structure and quaternary structure.

Primary structure are polypeptide chains. The polypeptide chains are formed by amino acids held together by peptide bonds.

Secondary structure refers to the folding of polypeptides chains. Two most common secondary structures are alpha helix and beta pleated structure. These folding occurs because of hydrogen bonding between the oxygen of the carbonyl of one amino acid and the hydrogen of another amino acid.

Therefore, hydrogen bonding is crucial for secondary structure of the protein.

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D because it’s not going into then air or to the clouds
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The <u>Stratosphere</u> contains the Ozone layer in Earth's atmosphere.

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A 1,000 kg ball traveling at 5m/s would have kinetic energy
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yes

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3 years ago
If 0.6 moles of N2 are reacted, how many moles of H2 are used?
Verizon [17]

Answer:

6 moles

Explanation:

Take a look at the balanced chemical equation for this synthesis reaction

N

2(g]

+

3

H

2(g]

→

2

NH

3(g]

Notice that you have a  

1

:

3

mole ratio between nitrogen gas and hydrogen gas. This means that, regardless of how many moles of nitrogen gas you have, the reaction will always consume twice as many moles of hydrogen gas.

So, if you have  

2

moles of nitrogen taking part in the reaction, you will need

2

moles N

2

⋅

3

moles H

2

1

mole N

2

=

6 moles H

2

3 0
3 years ago
A seashell has only 3.1% of its c-14 left. The half life of c-14 is 5740 years. How old is the seashell
Slav-nsk [51]

The seashell is <u>28747.96 years old.</u>

<u />

Why?

If we need to calculate how old is something, we can use the equation for radioactive decay rate. It's possible using the C-14 half-life (5740 years) as reference. Remember, C-14 is used because all the living things take up the element from the atmosphere, when an organism dies, the amount of carbon starts to decay (very slowly).

Decay rate half life:

N_{t}=N_{o}*e^{-l*t}

Where,

N_o} is the initial number of atoms (undecayed)

N_{t} is the the number of atoms at time (undecayed)

l is the decay rate

Now, isolating the decay rate of the formula, we have:

{N_{t}=N_{o}*e^{-l*t}\\\\ln(\frac{N_{t}}{N_{o}})=-l*t\\

Also, we can get the value of the decay rate (half life), using the following formula:

l=\frac{0.693}{5740}=1.207x10^{-4}

Then, using the given information, we have:

ln(\frac{3.1}{100})=-1.207x10^{-4}*t

-3.47=-1.207x10^{-4}*t

-3.47=-1.207x10^{-4}*t\\\\t=\frac{-3.47}{1.207x10^{-4}}=28748.96years

Hence, the seashell is 28748.96 years old.

Have a nice day!

6 0
4 years ago
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