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Available soil water (FC, WP and depth)

How much water the soil holds for the plant, how much needs to be replaced, and when it is time to irrigate.

Pre-sizing and estimating tool: the results do not replace a design, calculation, or report signed by a qualified professional, nor verification against the applicable standards.

Preliminary estimateRevision 12/11/2026
Soil and root zone
Management

Available water is the range between CC and PMP. For the depth to replace, use the current moisture measured in the field, in the root zone.

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—Depth to replace
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Available water by depth

Water the soil holds at each root depth, with the same difference between FC and WP.

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Available water, readily available water and depth to replace

The three main values, in millimeters of water.

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What if the data changes?

Drag the controls to simulate data different from what you entered (from 30% less to 30% more) and watch the result change instantly.

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Typical available water by soil texture

Approximate values from FAO-56 (Table 19), for comparison only. They do not replace the physical analysis of your soil.

Step by step with your numbers

The calculation done in steps, with the values you entered.

    The calculation memo gathers this page's inputs, results, equations, assumptions, and references, with fields for project, responsible person, and review. The full report also includes the charts and interpretations, in color. In the print window, choose Save as PDF.

    How to use

    Enter the soil moisture at field capacity (CC) and at wilting point (PMP), the root depth, and the current moisture. The calculator shows the available water, the part that can be used before stress, and the depth to replace.

    Hypothetical example

    CC of 30%, PMP of 12%, roots at 60 cm, current moisture of 22%, p of 0.5 and efficiency of 85%.

    AD = (30 − 12) ÷ 100 × 600 mm = 108 mm. AFD = 0.5 × 108 = 54 mm. Depth to replace = (30 − 22) ÷ 100 × 600 = 48 mm; gross depth = 48 ÷ 0.85 = 56.5 mm.

    Precautions

    • CC and PMP should come from the physical analysis of your soil (water retention curve). Estimates based on texture are only approximations.
    • Measure the current moisture in the root zone, not just at the surface.
    • To decide the irrigation interval, use the water balance with rainfall and the ET₀ for your region.

    Method, assumptions, and references

    Equations used

    AD (mm) = (CC − PMP) ÷ 100 × Z (cm) × 10
    AFD (mm) = p × AD
    Depth to replace (mm) = (CC − current θ) ÷ 100 × Z (cm) × 10
    Gross depth (mm) = depth to replace ÷ application efficiency

    Assumptions and limits

    • Moisture in % of soil volume; Z is the effective root depth, which changes with the crop and growth stage.
    • The value of p (allowed depletion fraction) depends on the crop and the evaporative demand; 0.5 is a common reference value.
    • Soil is uniform across the depth considered; layers with different texture change the result.

    Standards and technical documents

    • Reichardt, K.; Timm, L. C. Solo, planta e atmosfera: conceitos, processos e aplicações. 2nd ed. Barueri: Manole, 2012.
    • Allen, R. G. et al. Crop evapotranspiration: guidelines for computing crop water requirements. FAO Irrigation and Drainage Paper 56. Rome: FAO, 1998.

    Frequently asked questions

    Where do CC and PMP come from?

    From the soil water retention curve, measured in the laboratory or estimated from physical analysis. Data from your own area are the best source.

    Why use the gross depth?

    Because not all the applied water is available to the plant: drift, evaporation and percolation reduce system efficiency.