Using Soil Tension to Measure Key States of Soil Moisture

By Ben Smith
Hortau Grower Support Specialist

Even with modern-day advanced research, our understanding of the world can still limit our ability to progress or discover parallel science that could ultimately expand the knowledge base of a field in question.

Examples of this can be found throughout history. The Chinese used gunpowder for nearly 1,000 years and during much of the same time period, the Greeks, Romans and other European civilizations remained highly focused on kinetic energy-based weapons such as bows, ballistae and catapults. The later three groups mastered the use of springs and weights to propel objects, but the exclusive narrow focus on these types of weapons only kept them from exploring the use of chemical-based propellants that would have otherwise advanced their capabilities long before they discovered gunpowder from the Chinese.

Today, our limited vision due to limited knowledge isn’t necessarily anyone’s fault, it’s just something that happens. As a society, we are getting better at performing the axiom of “thinking outside the box,” but there are areas where we still get stuck in a way of thinking and fail to see outside of what has always been done. Because of a historic lack of technology and the difficulty of using our natural senses to measure anything below the surface of the soil, the science of irrigation has some long-held theories that are generally accepted as truth, but tend to limit us in our thinking and hold us back from improving irrigation practices.

Often, in science, when things aren’t fully understood, rules are chosen without real evidence.  They are created to help give a benchmark to make research possible.  These would best be described as “let’s assume” rules.  Research only occurs when variables are controlled, sometimes variables can’t be controlled or even measured with accuracy.  In these instances, “let’s assume” rules are used.  Generally, these types of rules are thrown out after research discovers the full truth, or it becomes easier to measure the variable that is assumed.  However, they occasionally become embedded in common knowledge as generally accepted truth.

Using Soil Tension to Measure the Key States of Soil Moisture

Augering down through the soil profile, showing the change of moisture from being fairly moist at the top to very dry at the bottom. (Photo: Ben Smith)

Assumptions in Soil Moisture Monitoring

In this article, I want to talk about a few of these “let’s assume” rules that have become generally accepted as truth with regard to soil moisture.  I will refer to them as “Traditional Soil Moisture States,” which is comprised of the concepts of permanent wilting point, field capacity, and saturation.

Theories on these concepts are taught in almost every soil science class and there are some extremely valid principles to learn from them.  But they are not the end-all rule that they are taken to be.  Something interesting to note is that the research that produced these numbers are one of the few long-standing irrigation concepts that uses tension to describe the results.  The concepts were first introduced more than 100 years ago by engineer and physicist Lyman Briggs and botanist Homer LeRoy Shantz.

Because of the difficulty of measuring soil tension with the inferior quality of devices at that time, tension was used, but then abandoned, leaving only the legacy of the concepts without enough further research to understand the concepts in their full breadth of application.  With Hortau’s research and its state-of-the-art tensiometers as well as the ability to take data points in real time, we are better able to understand and identify these concepts.

Key States of Soil Moisture

Soil saturation, field capacity, and permanent wilting point — concepts intended to describe key states of soil moisture — are used to help identify how much total water is available to crops and to aid in establishing the “bank account” when Evapotranspiration (Et) models are used for irrigation scheduling. Soil saturation is the state at which all the pores in the soil are full of water.  This is the total amount of water that can be contained within the soil profile.  This is not, however, the total amount of water a soil can hold.  It is the soil’s water holding capacity plus.  In a well-drained situation, a soil cannot stay saturated.  Gravity acts heavily upon the water in the pore spaces and draws the water downward to drain deeper into the profile.

Field capacity is the state that occurs after all the excess water contained in a saturated soil drains out.  Outside of evaporative forces, such as heat and plant roots drawing water out, a soil at field capacity will stay at field capacity.  The forces in the soil that adhere water to the soil particles are strong enough to hold and keep the water in the soil.  In general, this is the first state that is healthy for plants.  At field capacity, there is plenty of easy-to-access water and oxygen available for healthy roots.

Permanent wilting point is the state at which the soil is so dry that a wilted plant is damaged to a point that it can no longer recover, even if water is applied once more.

A Closer Look at Soil Tension

Let’s look at each of these states more closely. The Traditional Soil Moisture States theory assigns a pressure measurement for each of the states.  The pressure unit we will use is Kilopascal (kPa). This is a simple pressure measurement that can easily be converted into psi.

When speaking about soil moisture in terms of tension, think about psi in the form of suction.

Measuring Soil Saturation

For soil saturation, the assigned pressure is 0 kPa.  There is some truth here.  Soil saturation does indeed occur at 0 kPa, at least in general.  There are some cases in very coarse sand where saturation occurs slightly above 0 kPa, but, in general, the principle is good.  That is, water only flows downward from gravity when there is so much water in the soil that the soil particles cannot hold onto it.  In other words, no suction is required to move water in a saturated soil, it flows freely without any additional force.

Identifying Field Capacity

It is harder to assign a number to field capacity.  When these concepts were first introduced the only way to measure soil tension required manually removing soil and testing it.  General convention states that field capacity is achieved 24 hours after soil reaches saturation and no additional water is applied. It’s a convenient standard, but is a 24 hour wait correct for every soil? And is that really field capacity?

This saturate-and-wait-a-day method has reported field capacity occurring at 33 kPa.  If you are familiar with Hortau and have used our systems, you are probably scratching your head right now.  For most crops that we record data for, 33 kPa is at the high end of what extensive research has shown to be the ideal zone for crop development.  For example, tree crops such as almonds, walnuts and pistachios, have an upper tension threshold of 35 kPa for maximum crop development.  For other, more sensitive crops, such as strawberries, the upper threshold is only 8 kPa.  Our real-time tension graph trends clearly demonstrate the principle of field capacity.  If a soil is irrigated to saturation, there follows a rapid draining of the soil indicated by sharp increase in soil tension.  After a few hours, the upward swing of tension levels off and reduces to a normal rate.  That is when field capacity is achieved.  Every soil is different, of course, but from what I have seen most tend to reach field capacity at somewhere around 4 to 5 kPa.  Although it is generally accepted, 33 kPa is not truly field capacity.

soil tension graph

SOIL TENSION GRAPH: After excessive irrigations that applied water beyond field capacity, the tension rapidly increased until reaching field capacity at which time the tension leveled off and increased at a normal rate.

Anticipating Wilting Point

The accepted parameters for permanent wilting point are the most surprising of all.  Typically, tension for permanent wilting point is given in a different unit than the others.  The reason for this is due to the number being so large.  Unfortunately, the change in unit of measurement masks the drastic difference between permanent wilting point and the other states.  Typically, tension for permanent wilting point is reported as 15 bars.  To keep all things equal, when converted, 15 bars is equivalent 1,500 kPa!

This pressure is so high, conventional devices for measuring tension cannot even come close to measuring it.  In fact, a highly-reinforced pressure chamber had to be used to determine the tension at this accepted permanent wilting point.  This is important to note because the difference between field capacity and permanent wilting point is believed to represent the total amount of water available to plants.  In practice, assuming these numbers, there would be 1,467 kPa worth of water available to plants.

Of course, growers don’t want to get anywhere close to permanent wilting point, so the way around this is to assume a Maximum Allowable Depletion.  It isn’t practical to measure the Maximum Allowable Depletion for every soil in every field, so in general, we are taught to apply a 50% Maximum Allowable Depletion.  In other words, the maximum amount of water we should ever allow to be taken out of the soil is 50% of the total available plant available water.  The change in amount of water in the soil and change in soil tension do not relate on a 1-to-1 basis, however, let’s say they do, just for comparison sake.  If we assumed a Maximum Allowable Depletion of 50% of the tension, we would still have 733 kPa to work with.  That is a massive and impractical number.  Even with Hortau’s reliable tensiometers, it is not possible to measure soil tension much above 85 kPa.

If water is not available to be measured via tensiometer, it is not available for plant use.

If you haven’t already, I would encourage you to go out and auger the soil in a field where tension is 85 kPa.  Generally, the soil is so dry at this point that it is nothing more than dust, if it isn’t too hard to dig in at all.

To be completely fair, maybe permanent wilting point does occur at 1,500 kPa, at least for the soil and crop that was used for the original research.  However, if it is true, it isn’t the correct number for us to be looking at.

Get More Out of Precision Irrigation

As farmers, we aren’t interested in finding out how much we can stress a plant before it dies, instead we want to see how much we can limit stress and increase the plant’s productivity.  I applaud the work done in the past that has enabled farmers to have some understanding of the soil and allowed them to be better at what they do.  However, I hope we don’t let the best that could be done 100 years ago limit us and keep us from looking at irrigation in a more detailed and powerful way with the technology that is available today.

We no longer need to rely on rough ideas of soils capability in general.  Today, it is possible to get accurate, real-time information that allows us to see trends and actual capabilities of each soil and field that we manage in our operation.


Ben Smith provides grower support in California’s Central Valley for Hortau. He grew up on a small dairy farm in northern Utah, where he spent most of his summers in the alfalfa and corn fields shoveling dirt, desperately trying to get the water to flood the fields evenly.  He knew that there had to be a better way.

Ben went to Utah State University and received a B.S. degree in Crop Science with a minor in Soil Science. He has an extensive background working for irrigation equipment manufacturers and in large-scale production agriculture  installing irrigation systems, maintaining existing systems, and scheduling irrigations over large acreages.

Send Us Your Questions

Have something you’d like us to discuss on The Hortau Blog? Email us at media@