got water? - A simple circuit for plant watering
1Department of Physics and Astronomy “Galileo Galilei”, University of Padova, Italy
2Liceo "Angela Veronese", Montebelluna (TV), Italy
Table of contents
Introduction
We introduce here an activity for high school students to get them more acquainted with simple electronics circuits. The aim is to build a simple circuit that lights a LED when a plant needs watering. The only prerequisites are the knowledge of Ohm's law and Kirchhoff's laws.
This work has been published in Physics Education: C.L. Fontana, S. Lippiello and S. Dal Pio, 2019 Phys. Educ. 54 035011 "Combining theory and practice to solve a common problem: a simple circuit for indoor plants watering" DOI:10.1088/1361-6552/ab090d
Physical concept: the soil resistance
Measuring the soil humidity
- \(R_1\) and \(R_2\) are two regular resistors;
- \(\color{#d62728}{R_s}\) is the resistance of the plant soil;
- \(\Delta V_\text{gen}\) is the generator's potential difference;
- \(I\) is the current flowing through the circuit;
- \(\Delta V_\text{AC} = V_\text{A} - V_\text{C} = V_\text{A} = \Delta V_\text{gen}\),
- \(\Delta V_\text{BC} = V_\text{B} - V_\text{C} = V_\text{B} = I R_2\).
- Wet soil: there is a lot of water in the soil and then we expect that the soil conducts well, in other words: \(\color{#d62728}{R_s}\) is small.
- Dry soil: there is no water in the soil and then we expect that the soil conducts badly, in other words: \(\color{#d62728}{R_s}\) is big.
Wet soil: small \(\color{#d62728}{R_s}\)
What happens when we have a wet soil? \(\color{#d62728}{R_s} \approx 0\), therefore we can see what happens to \(V_\text{B}\): \begin{equation} V_\text{B} = \Delta V_\text{gen}\frac{R_2}{R_1 + \color{#d62728}{R_s} + R_2} = \Delta V_\text{gen}\frac{R_2}{R_1 + R_2}. \end{equation} So \(V_\text{B}\) becomes an intermediate value between \(0\ \text{V}\) and \(\Delta V_\text{gen}\), depending on the values of \(R_1\) and \(R_2\).Dry soil: big \(\color{#d62728}{R_s}\)
In this case we have that \(\color{#d62728}{R_s}\) is big and therefore: \begin{equation} V_\text{B} \rightarrow 0\ \text{V} \end{equation} in other words \(V_\text{B}\) becomes very small. We see that we have found a way to generate a variable potential that is related to the soil humidity.A reference voltage
Comparing voltages
- Wet soil \(\Rightarrow\) soil has a small resistance \(\Rightarrow\) \(\color{#d62728}{R_s}\) is small \(\Rightarrow\) \(V_\text{B}\) is high \(\Rightarrow\) \(V_\text{ref} - V_\text{B} \lt 0\) \(\Rightarrow\) \(V_\text{out} = 0\ \text{V}\) \(\Rightarrow\) LED is OFF.
- Dry soil \(\Rightarrow\) soil has a big resistance \(\Rightarrow\) \(\color{#d62728}{R_s}\) is big \(\Rightarrow\) \(V_\text{B}\) is low \(\Rightarrow\) \(V_\text{ref} - V_\text{B} \gt 0\) \(\Rightarrow\) \(V_\text{out} = \Delta V_\text{gen}\) \(\Rightarrow\) LED is ON.
Practical considerations
Suitable values for \(R_1\) and \(R_2\) can be calculated with the calculator below. The calculator requires a measurement of the soil resistance. We suggest to have the soil with a intermediate humidity for this measurement. In order to measure the soil resistance, two electrodes should be inserted in the soil. The electrodes can be simple pieces of iron wire as long ad the pot height. The rationale for having two resistors around \(\color{#d62728}{R_s}\) is to clamp the possible values of \(V_\text{B}\), in order to be sure to be always able to set a value of \(V_\text{ref}\) that is above or below.
The potentiometer can be of any kind of potentiometer, total resistances of \(10\ \text{kΩ}\) or \(100\ \text{kΩ}\) are good values. The op-amp can be a LM358 that is very easily found and it is cheap. The LED can be a regular red LED.
A set of three or four AA batteries in series can be used as a generator. With this option \(\Delta V_\text{gen}\) will be either \(4.5\ \text{V}\) or \(6\ \text{V}\), that work well with the LM358. A breadboard is a good option as the circuit support.