Calculating Readily Available Water

Steps in identifying Readily Available Water

Step 1: Dig a hole

Dig a hole within the root zone of your crop. For perennial crops, dig under the canopy in an area watered by the irrigation system. Try to dig to 1 metre or at least 30cm past the main root zone (where the fibrous roots are).

Step 2: Identify the effective root zone

Figure 2 The effective root zone of a citrus tree can be seen in the top 30cm

The effective root zone is where the main mass of roots is found (see Figures 2 and 3). This is typically one to two-thirds of the depth of the deepest roots.

Some crops, such as irrigated pasture, citrus, bananas, avocados and low-chill stone fruit, develop a mass of shallow roots with only a few roots penetrating deeper into the soil.

Figure 3 Fibrous roots which comprise the effective root zone may only extend a third as far as the deepest roots

Step 3: Identify different soil layers

If you have different soil layers within the effective root zone measure the depth of each of these in metres.

Step 4: Identify gravel/stone in each layer

Stone and gravel reduce the amount of water that can be held by a soil. A very stony soil will hold much less water than the same soil without stones.

Grab three good handfuls of soil and using a 2mm sieve remove all stone and gravel (Figure 4). Place the pile of stones and gravel next to the pile of soil and visually estimate the proportions of each (for example, 60% stone and 40% soil).

Figure 4 Sieving shows the proportions of stone and gravel in soil

Step 5: Identify soil texture(s)

Identify the texture of each soil layer within the effective root zone. The amount of water held by a soil and available to a plant varies with texture (see Table 1). For example, a loamy soil can hold more readily available water than a sand.

Soil texture can be assessed in the field by the feel of a moist soil sample when worked between your thumb and forefinger (Figure 5).

Figure 5 Forming a ribbon with moist soil helps identify soil texture

Step 6: Calculate RAW

1. Identify the depth of the effective root zone.
2. Identify the depth of different soil layers within the effective root zone.
3. Determine the soil texture and percentage stone/gravel of each layer.
4. Select the crop water tension group from Table 1 and identify the RAW value for each soil texture layer (mm/m).
5. Reduce the RAW figure(s) by the % stone/gravel in the soil.
6. Multiply the thickness of each soil layer by its adjusted RAW value.
7. Add up the RAW for each soil layer to obtain the total root zone RAW.

Example calculation

A citrus crop growing in a sandy loam soil containing 20% stone, with an effective root depth of 0.3m and a strategy to irrigate at ‑40kPa would have the following calculations:

From Table 1, the RAW for a sandy loam soil at ‑40kPa = 60mm/m.

As the soil contains 20% stone, reduce the RAW by 20%. To do this, multiply by 0.8.

Adjusted RAW = 60mm/m x 0.8 = 48mm/m.

Hence, for a rooting depth of 0.3m:

Total root zone RAW = 48mm/m x 0.3m = 14.4mm.

If your irrigation system wets the entire cropped area, use this figure (RAW mm) to schedule irrigations. If you irrigate with a drip or micro-spray system that does not wet the entire cropped area, you need to convert RAW mm to RAW litres. See Converting Readily Available Water to litres for drip irrigation.

Acknowledgements

This information replaces Farmnote 543 Calculating Readily Available Water by Helen Newman, published in 2012.