We can use a Wheatstone bridge voltage measurement to determine an unknown resistance value.
In part 3 of this series, we used Kirchhoff’s voltage law to derive the branch currents and node voltages for an unbalanced Wheatstone bridge with five known, fixed resistors (Figure 1). Now, we propose to replace R5 with a digital multimeter (DMM) to directly measure VV – VX and use that measurement to determine the value of an unknown resistor in the position of R4.

Q: Could we backtrack first? Last time, we solved three loop equations. I was trying to use Kirchhoff’s current law to write six-node equations and got lost. Could you elaborate?
How far did you get?
IIN = I1 + I2, I1 = I3 + I5, I2 = I4 + I5, I3 = I1 – I5…
Stop there. Your first three are good, but the last one is just a restatement of the second one. We need an independent equation for I3.
We know I3 = VV/R3, but we don’t know VV.
Right, but we can express VV in terms of one of our original six unknowns, namely I1. VV is VIN minus the voltage drop across R1, which is I1 times R1. Substituting our component values, we can write:

Similarly, we can derive VX as a function of I2 and solve for I4:

And finally, I5 is VV minus VX divided by R5:

Table 1 shows all six node equations in the format required for the online solver[1] I’m using, and the solutions are shown in red. With this approach, the solver generates the branch currents directly; we don’t have to derive them from the loop currents. I’ve also included our results from part 3 based on the loop method, with the loop values in blue, and the results agree within a third of a percent.
Table 1. Node equations and solutions.
| Node equations | Solved values, node method (mA) | Solved values, loop method (mA) | Difference (%) | |
| Eq.1: | 1IIN – 1I1 – 1I2 + 0I3 + 0I4 + 0I5 = 0 | IIN = 0.39331 | IIN = 0.39253 | -0.19871 |
| Eq.2: | 0IIN + 1I1 + 0I2 – 1I3 + 0I4 – 1I5 = 0 | I1 = 0.14166 | I1 = 0.14136 | -0.21222 |
| Eq.3: | 0IIN + 0I1 + 1I2 + 0I3 – 1I4 + 1I5 = 0 | I2 = 0.25165 | I2 = 0.25117 | -0.19111 |
| Eq.4: | 0IIN + 1.42I1 + 0I2 + 1I3 + 0I4 + 0I5 = 0.455 | I3 = 0.25384 | I3 = 0.25320 | -0.25276 |
| Eq.5: | 0IIN + 0I1 + 0.324I2 + 0I3 +1 I4 + 0I5 = 0.221 | I4 = 0.13947 | I4 = 0.13933 | -0.10048 |
| Eq.6: | 0IIN + 4.7 em>I1 – 2.2I2 + 0I3 + 0I4 + 1I5=0 | I5 = -0.11218 | I5 = -0.11184 | -0.30401 |
Now, let’s look at the situation where we have an unknown resistor but a known voltage.
Right. Keep in mind that in the 19th century, galvanometers were good at indicating zero current, but not good at quantifying nonzero levels. Consequently, accurate measurements were made under zero-current conditions. We no longer face that limitation, and we can use a measurement setup in Figure 2, which shows a way to make strain-gauge measurements. Here, a DMM, data logger, or data-acquisition instrument replaces the galvanometer from part 2, and R5 from Figure 1 becomes essentially infinite. RX, which takes the place of R4, is a strain-gauge element that has a resistance of 120 Ω when not subjected to strain. To optimize measurement resolution, we assign resistors R1, R2, and R3 the same 120-Ω value.

So, we basically have two voltage dividers.
Right:

and

We can now write an equation for what our DMM would read for a resistance value RX:

Now we can solve for RX:

Figure 3 plots this transfer function. Note that for strain-gauge measurements, resistance changes are often less than 1%, and sometimes much less.

Figure 4 shows a simulation result.

Q: Why use the bridge—why not just measure the resistance of RX directly?
A: Temperature compensation is one reason. In Figure 2, R2 is often a strain-gauge element identical to RX maintained at the ambient temperature of RX, but that never undergoes strain. If both R2 and RX increase by 0.1% because of a rise in ambient temperature, but RX continues to be unstrained, the DMM will continue to read zero.
Q: What is strain anyway, and what are its units?
A: Good question. That’s beyond the scope of this series on Kirchhoff’s laws, but we can consider strain measurement in depth in a future series.
Reference
[1] Simultaneous Linear Equations Solver for Six Variables, handymath.com.
Related EEWorld Online content
Sorting out PC-based instrumentation
Capabilities of modern data recorders
DAQ Series: Methodology associated with data acquisition
Wheatstone bridge, Part 2: Additional considerations
Things to know about multimeters
What’s a half digit and are they all the same?





Leave a Reply
You must be logged in to post a comment.