Infrastructure ground engineering blog | Geobear

Understanding the impact of gypsum in soils in the GCC

Written by Mohamed Wehbi | Mar 26, 2026 11:13:26 AM

How does gypsum impact soil stability in the GCC?  

In arid and semi-arid regions—particularly across the Middle East—gypsiferous soils are common. On paper, they often appear competent: relatively dense, sometimes even strong in dry conditions. In reality, they are one of the most deceptive and high-risk ground conditions engineers deal with.This is not a niche issue. It is a recurring cause of settlement, loss of bearing capacity, and long-term structural distress.

Gypsiferous soils are inherently vulnerable to water ingress, and this vulnerability becomes critical under conditions of heavy rainfall. Gypsum is a highly soluble mineral, meaning that when exposed to infiltrating water, it begins to dissolve, leading to a gradual loss of soil mass, the formation of voids, and a reduction in overall strength.

In regions such as the GCC, where soils are often erosion-prone and rainfall events can be intense and sudden, this process is accelerated, making the combination of gypsum and heavy rain particularly problematic for foundation performance.

Over time, repeated wetting can trigger progressive ground deterioration and settlement, especially where water is allowed to freely percolate beneath structures.

What is Gypsum Soil?

Gypsum (CaSO₄·2H₂O) is a soluble mineral. When present in soil, it acts as a temporary cementing agent between particles.

  • In dry conditions → soil appears stiff and stable
  • When exposed to water → gypsum dissolves
  • Result → collapse of soil structure

This transition is not gradual. It can be sudden and severe.

Collapse mechanism in gypsum soils (rainfall-driven)

Gypsum soils don’t fail because they are weak—they fail because they dissolve when water flows through them. The collapse mechanism in gypsiferous soils is fundamentally driven by chemistry first, mechanics second.

Most engineers focus on structure and strength—but the real trigger is gypsum dissolution controlled by water chemistry and flow.

Gypsum has a limited solubility (~2.0–2.5 g/L), so in still water dissolution slows down. But during heavy rainfall, this changes completely:

  • Rainwater continuously infiltrates the ground
  • Fresh (unsaturated) water keeps entering the soil
  • Dissolved gypsum is carried away
  • The process never reaches equilibrium

What happens next:

  1. Dissolution of bonds. Gypsum cementation between soil particles disappears
  2. Void formation. Dissolved material is transported → small voids develop
  3. Increased permeability. Water finds these paths → flow increases → more dissolution
  4. Sudden collapse. Soil structure gives way → rapid, localized settlement

Why This Matters in Practice

From a design standpoint, gypsiferous soils are dangerous because:

  • They pass site investigations if tested in dry conditions

  • They fail in service, once exposed to moisture

  • They create differential settlement, not uniform settlement

Typical triggers include:

  • Water leakage (common in buried utilities)

  • Landscape irrigation

  • Heavy rainfall events (increasingly relevant in GCC)

  • Changes in groundwater regime

The Geobear solution: controlling water, not just soil

In gypsiferous ground, the trigger for failure is water. Therefore, the solution must focus on controlling water ingress.

Creating a subsurface water curtain using Geopolymer injections

Geobear’s approach focuses on forming a targeted subsurface barrier (water curtain) using geopolymer injections.

This is not a rigid wall. It is a strategically engineered low-permeability zone created within the soil mass.

How the water curtain works

The Geobear geopolymer curtain functions as an extremely low-permeability barrier (on the order of 10⁻¹¹ m/s), effectively preventing water from infiltrating beneath the foundation. In gypsiferous soils, the primary mechanism of deterioration is the dissolution of gypsum when exposed to water.

By blocking water ingress entirely, the curtain eliminates this mechanism at its source. Without water reaching the soil, gypsum cannot dissolve, meaning the soil structure remains intact and no voids or loss of strength develop.

As a result, the risk of settlement is fundamentally removed, not by strengthening the soil itself, but by cutting off the driving cause of degradation.

Installation of geopolymer curtain

Why this approach works

Most solutions try to strengthen the soil while ignoring the cause. This approach addresses the root issues:

  • Stops water reaching gypsum

  • Prevents further dissolution

  • Stabilises ground behavior long-term

You are not just fixing the soil—you are changing the environment that causes failure.

Are you experiencing issues causes by gypsum soils? 

Gypsum soils are not inherently weak—they are unstable in the presence of water. If water continues to infiltrate, failure is inevitable. By creating a subsurface water curtain using geopolymer injections, you:

  • Control water movement

  • Protect the soil structure

  • Prevent collapse before it starts

That is the difference between temporary repair and a durable engineering solution. If you have concerns about gypsum soils, get in touch with the Geobear engineering team today for an assessment. We can discuss if the geopolymer water curtain may be a solution for your concerns.