Soil Total Water Filled Pore Space Calculator

Accurately measure soil water saturation levels. Optimize garden irrigation schedules, prevent root diseases, and boost plant growth using our advanced calculator.

1. Mode & Soil Type

Standard mineral soil is typically 2.65 g/cm³.

2. Core Measurements

Example input: 1.30 g/cm³
Example input: 0.25 (mass of water / dry soil mass)

3. Advanced Settings

Standard water density is 1.0 g/cm³.
  • Bulk Density: 1.30 g/cm³
  • Particle Density: 2.65 g/cm³
  • Gravimetric Water: 0.25 g/g

Understanding Soil Total Water Filled Pore Space (WFPS)

Water Filled Pore Space is a critical metric in gardening, agronomy, and environmental science. It quantifies the proportion of soil pores currently occupied by water relative to the total pore volume available. Maintaining optimal WFPS ensures plants receive adequate moisture without suffocating root systems.

Why WFPS Matters in Gardening

Soil pores are shared between air and water. If WFPS is too low (below 30%), plants experience drought stress, leading to wilting and stunted growth. Conversely, when WFPS exceeds 70% to 80%, oxygen diffusion through the soil drops sharply. This anaerobic condition promotes root rot, fungal diseases, and denitrification, starving plant roots of necessary oxygen.

Formula Used

The calculation relies on fundamental soil physics equations:

How to Use This Calculator

Follow these simple steps to determine your garden soil saturation:

  1. Select your preferred input mode based on your available soil test data.
  2. Input your soil bulk density and water content measurements.
  3. Click the calculate button to instantly review your WFPS percentage and pore characteristics.

Frequently Asked Questions

What is an ideal WFPS for most garden vegetables?

An ideal WFPS range for most vegetables sits between 50% and 60%, balancing moisture availability and root oxygenation.

Can WFPS exceed 100%?

Mathematically, saturation cannot exceed 100% of total pore volume. Any excess water pools on the surface or drains away due to gravity.

How does soil compaction affect WFPS?

Compaction increases bulk density and reduces total pore space, meaning soils reach critical high WFPS thresholds much faster after rain or watering.


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Important Note: All the Calculators listed in this site are for educational purpose only and we do not guarentee the accuracy of results. Please do consult with other sources as well.