Figure 1 Examples of growth responses to % air-filled porosity
Nursery and Flower Grower
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Soil Mixes Part 3: How much air and water?

Container soils should have a good balance between air- porosity and water- holding capacity. But what are the favorable levels of these two parameters? Most horticulturists will recommend providing a soil with “good drainage”. But what exactly does that mean?  How do we quantify that? If we know, then soil manufacturers can develop, standardize and describe soil mixes.  Growers can select, develop or modify their own soil mixes for their particular needs. 

Let's start with air-filled porosity.  There have been many experiments demonstrating that air-filled porosity is highly correlated with the growth of various plants.  Here are two examples, Fig 1:

Figure 1 Examples of growth responses to % air-filled porosity
Two graphs showing plant growth versus air-filled soil porosity: chrysanthemum fresh weight and tomato growth both increase as porosity rises, then level off at higher porosity levels.

Figure 1 Examples of growth responses to % air-filled porosity

Some researchers reported that the rate of oxygen diffusion through the soil-- rather than air-filled porosity--  is more closely related to plant growth. This might be because the oxygen in the air pores has to move to the roots before it is absorbed and used by the roots. In general, these and similar studies have led to a recommendation that air-filled porosity should be at least 10% and generally no more than 25% of the total soil volume.  Fig 2.

Figure 2 Generalized growth responses to % air-filled porosity
Scatter plot showing fresh plant weight increases with air-filled soil porosity, with a marked threshold around 10% separating poor (“bad”) from improved (“good”) growth conditions.

Figure 2 Generalized growth responses to % air-filled porosity

So a plants' requirements for soil aeration can vary, and here are some examples. Fig 3.

Figure 3 Examples of plant aeration requirements
Table listing plant species grouped by required air-filled porosity levels, from very high (>20%) to very low (2–0%), showing variation in plant tolerance to low soil aeration.

Figure 3 Examples of plant aeration requirements

There are other consequences of having poor soil aeration. Soils with low oxygen or anaerobic conditions can lead to chemical reduction.  Reduced forms of some chemicals, such as methane (CH4), hydrogen sulfide (H2S), nitrite (NO2-), and manganese ion (Mn2+), are toxic to plants. The latter is probably the most important.  Plants growing in poorly aerated soil can have manganese levels as high as 1200 ppm in their leaves (normal levels are 50-200 ppm). These high levels lead to manganese toxicity, with symptoms of marginal leaf chlorosis (yellowing from loss of chlorophyll, the green pigment in leaves).

What about the water filled portion of the soil?  The recommendation is that at least 40% of the total volume should be filled with water at container capacity (after full drainage). In general, container soils with a water-holding capacity of 40% would hold enough water to meet plant demand for about one day. Usually mixes have a higher water-holding capacity than this so that irrigation can be less frequent.  Total porosity, air and water porosity combined, must therefore be greater or equal to 50%. These parameters are summarized in Fig 4.

Figure 4 Generalized porosity requirements at container capacity.
Slide listing recommended soil conditions for plant growth: total porosity ≥50%, air-filled porosity ≥10%, and water-holding capacity ≥40%, with a diagram of soil particles and pore spaces.

Figure 4 Generalized porosity requirements at container capacity

Here are examples of 3 historically important container mixes. The “UC Mix” was the first “soil- less" mix, mostly developed for the outdoor nurseries. It provided the essential requirements for a container mix: Good water holding capacity and aeration, high permeability, relatively disease-free, resistant to salinity buildup, reasonable pH range, good nutrient holding capacity, and provided for enough weight of the container so plants would not blow over in the wind. The “Cornell Lite” mixes containing peat mixed with either vermiculite or perlite are excellent for greenhouse crop production, but they are too light for outdoor nurseries and more expensive because of the relatively high cost of vermiculite and perlite.  Fig 5.

Figure 5 Examples of container mix porosity
Table titled “Physical Properties of Selected Media” comparing three growing media mixes: Peat + Perlite, Peat + Vermiculite, and U.C. Mix. Rows list recommended minimums and measured values: Total porosity (≥50%)—93, 94, 73; Water holding capacity (≥40%)—73, 81, 62; Air volume (≥10%)—20, 13, 11. Notes below state measurements were taken in a 12 cm (6-inch) pot; mixes are 1:1 peat with perlite or vermiculite, and U.C. Mix is 1:1:1 sand, redwood shavings, and peat.

Figure 5 Examples of container mix porosity at container capacity.

These soil physical properties are best measured by commercial or research soil laboratories.  If you are buying soil mixes, ask if the provider has these measurements. In a pinch, growers can estimate the values with a relatively simple method that was described by James Altland when he was with Oregon State University.  I have provided a simplified outline here. Fig 6.  The full description of the method is provided in the attachment at the bottom of the page. 

Figure 6 Estimating water and air porosity
Instructional slide explaining how to measure physical properties of soil mixes approximately. Steps: (1) Saturate mix in a container of known volume. (2) Let it drain and measure drained water. (3) Air-filled porosity equals drained water volume divided by total volume. (4) Weigh moist mix, dry in a low oven for 2 days, then reweigh. (5) Weight difference divided by total volume gives water holding capacity.

 Figure 6 Estimating water and air porosity

 

Next:  Poor soil aeration can lead to some root diseases.

 

Figures and tables adapted from:  Management of Container Media by Richard Evans, UC Davis, for the class, ENH 120. Porosity determination handout by James Altland (formerly Oregon State University, now with USDA ARS).