In this video, we're going to begin our discussions on Lineweaver-Burk plots by first introducing the Lineweaver-Burk equation. So recall from our previous lesson videos that the Michaelis-Menten equation describes the rectangular hyperbola that we see in a Michaelis-Menten enzyme kinetics plot. And so the Lineweaver-Burk equation also describes enzyme kinetic data that we see forming a line in a Lineweaver-Burk plot. And so the good thing about the Lineweaver-Burk equation is that really it's nothing new. We can pretty much say that the Lineweaver-Burk equation is the reciprocal of the Michaelis-Menten equation. So really, we can take the Michaelis-Menten equation and simply invert the equation or take the reciprocal of it, and then do a little bit of algebraic rearrangement to obtain the Lineweaver-Burk equation, which is shown right over here. So notice that the Lineweaver-Burk equation has the same exact enzyme kinetics variables as the Michaelis-Menten equation that we already covered. So they both have the initial reaction velocity, the kilometers, the \( V_{\text{max}} \), and the substrate concentration.
And so if we take a look down below at our image, notice that on the left here we have the Michaelis-Menten equation that we're already familiar with from our previous lesson videos. And so if we want to obtain the Lineweaver-Burk equation without having to commit it to memory, all we need to do is take the reciprocal of the Michaelis-Menten equation, and the reciprocal just means to essentially invert the equation. Now, if we invert one side of the equation, we also have to invert the other side of the equation. And so let's go ahead and start with this left side over here. So if we take the reciprocal of the initial reaction velocity, that's going to be inverting it, so what we're going to be left with on the left side is \( \frac{1}{\text{initial reaction velocity}} \). So now that we've taken the reciprocal of the left side, we can take the reciprocal of the right side over here. And so taking the reciprocal of the right side is essentially just going to be taking the denominator or what's on the bottom and placing it on top. And it's going to be taking the numerator, or what's on top, and placing it on the bottom. And so that's exactly what we're going to do when we take the reciprocal here. So now, we're going to take the bottom which is Kilometers plus substrate concentration and put that on the top. So we're going to have Kilometers plus substrate concentration on the top, and then, of course, on the bottom down here, what we're going to have is what used to be on the top. So that's going to be the \( V_{\text{max}} \times \) substrate concentration. So that is essentially the reciprocal of the Michaelis-Menten equation. Now, all we need to do is 2 steps of algebraic rearrangement. So recall that when we have addition going on in the numerator, that we can actually separate out these two components. We can separate the kilometers from the substrate concentration, as long as they both have their own denominator. And so that's exactly what we see down below. Notice that the kilometers is now separated from the substrate concentration. The addition is still here, but they both have their own set of the same common denominator. And so, notice that with this expression over here, \( \text{max} \). So this expression right here simplifies to just \( \frac{1}{V_{\text{max}}} \). And then, notice that this expression over here, we can actually take the \( k_m \) and the \( V_{\text{max}} \) right here and separate it from \( \frac{1}{\text{substrate concentration}} \), and that's exactly what we see down below. We have the \( \frac{k_m}{V_{\text{max}}} \times \frac{1}{\text{substrate concentration}} \). And really, that is it. That allows us to get the Lineweaver-Burk equation, which I'll admit at first glance looks pretty complicated, but we were able to obtain it just by taking the reciprocal of the Michaelis-Menten equation that we're already familiar with and doing 2 steps of algebraic rearrangement.
Now, again, this Lineweaver-Burk equation appears to be pretty complicated, but trust me, it's definitely not as complicated as it looks. And that's because it's no surprise that the line Weaver-Burk equation actually resembles the equation of a line. And, of course, we all know that the equation of a line is \( y = mx + b \). So, notice over here on the right side, we have the equation of a line, which is, again, \( y = mx + b \). And so, just like we can substitute in enzyme kinetics variables into a rectangular hyperbola equation to get the Michaelis-Menten equation from our previous lesson videos, we can also substitute in enzyme kinetics variables into the equation of a line to get the Lineweaver-Burk equation. And so notice that the \( y \) in our equation here is just going to be substituted with exactly what is on the \( y \)-axis of a Lineweaver-Burk plot, which is the reciprocal of the initial reaction velocity. Now, we know that the \( m \) is just going to be the slope of the line. And so, in the Lineweaver-Burk equation, the slope is equivalent to the ratio of the Kilometers over the \( V_{\text{max}} \). Now, the \( x \) is going to be exactly what we find on the \( x \)-axis of our Lineweaver-Burk plot, which is going to be the reciprocal of the substrate concentration. And then, of course, the \( b \) here is going to be the \( y \)-intercept of our line, and the \( b \) or the \( y \)-intercept in the Lineweaver-Burk plot is just gonna be \( \frac{1}{V_{\text{max}}} \). And so you can see here how the Lineweaver-Burk equation really does resemble the equation of a line, and that's why the Lineweaver-Burk equation describes the line that forms on a Lineweaver-Burk plot, and we'll talk about Lineweaver-Burk plots in our next lesson video, so I'll see you guys there.