EDN Access

September 1, 1997


Transistor trio makes vector anemometer

W Stephen Woodward, Chemistry Department, University of North Carolina--Chapel Hill, Woodward@net.chem.unc.edu

A previously published Design Idea (Reference 1) uses a heated transistor as an airspeed-to-frequency converter. Because it uses only one transistor, the circuit cannot determine the direction of airflow. Alternatively, a circuit that uses a trio of hot transistors can digitize both wind speed and direction (Figure 1).

The basic principle of operation is identical to that of the previous circuit. In the zero-airflow case, zero-adjust potentiometers R1, R2, and R3 set quiescent bias currents for self-heated transistors Q1, Q2, and Q3, respectively. If you properly adjust the resistors, collector power dissipation causes a still-air temperature rise in the transistor sensors of approximately 50°C, which in turn reduces the sensors' VBEs by approximately 2 mV/° to just slightly below Q4's VBE plus the drop across R4. Then, the voltages at the noninverting inputs of comparators IC3A, IC3C, and IC3D are slightly lower than the voltages at their inverting inputs. These comparators' outputs therefore go low, holding C1 discharged and multivibrator IC3B reset with its output high. This action causes a zero-frequency output on IC2C and holds IC2A and IC2B off.

If a nonzero airflow impinges on the sensor array, the resulting increase in cooling rate tends to raise the airflow sensor's VBE relative to Q4's VBE. This change reverses the voltage relation at one or more comparator input pairs and releases the reset on C1. C1 then charges through R6 until the voltage at IC3B's inverting input is greater than the voltage at its noninverting input, causing IC3B's output to snap low, beginning the discharge of C1 through R6 and turning on IC2. IC1 now directs an approximately 700-µsec pulse through the span-adjust-potentiometer array to whichever sensor transistor triggered the cycle. The resultant pulse of collector current deposits a quantum of heat tending to warm that sensor's temperature enough to restore the original zero-flow voltage balance with Q4. Until that temperature is restored, IC3B continues to oscillate and cycle on IC2. This feedback loop acts to maintain a constant temperature differential among sensors Q1 to Q3 and Q4. The frequency at IC3B's output is therefore proportional to the extra power required to heat the array and thus directly related to airspeed.

Meanwhile, feedback through R5 latches the address of the sensor transistor whose cooling triggered the cycle, so only that transistor receives the heating pulse. This binary (0, 1, or 2) sensor address is available at the output. Thermal coupling between the sensors depends on airflow direction. In Figure 1, for example, Q3 is the most upwind sensor and is therefore the most strongly cooled. This effect is the basis for the computation of wind angle (Click here to download the Basic program from DI-SIG, #2073).

The anemometer's output is suitable for direct connection to the parallel port of a desk or laptop PC. You can then run the accompanying Basic program to report wind speed and direction once per second.

The maximum output frequency for the circuit as shown is 1 kHz. Appropriate adjustment of the span-adjust potentiometers establishes almost any desired full-scale flow rate from less than 1 to greater than 10 m/sec (which is equivalent to less than 2 to greater than 20 knots.) Response time is less than 2 sec because of the constant-temperature operation of the sensors. Tracking among Q1, Q2, Q3, and Q4 compensates for changes in ambient temperature. The circuit operates from one 5V power source. Power consumption depends on airflow rates but is typically less than 2W. (DI #2073)


Reference

  1. Woodward, W Stephen, "Self-heated transistor digitizes airflow," EDN, March 14, 1996, pg 86).


Figure 1
17D20731
Q1 to Q3 comprise an airflow sensor that enables the circuit to digitize both wind speed and direction.

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