Rising Damp · Mechanism

How Rising Damp Occurs

A step-by-step look at how moisture actually moves through a wall — from the ground, through the masonry, and into the damage you can see.

Infographic showing how rising damp occurs, from ground moisture through capillary action to visible damage on a wall

Rising damp is the upward movement of moisture from the ground into the walls of a building. It occurs when moisture finds a pathway through porous building materials and is drawn upward by capillary action.

In buildings constructed with materials such as sandcrete blocks and mortar, moisture can move through the tiny interconnected pores within the masonry. If there is no effective barrier to stop this movement, the moisture can gradually travel upward, resulting in dampness and damage to the lower sections of the wall.

Understanding how rising damp occurs is the first step toward treating it correctly.

How Does Moisture Rise Through a Wall?

The process can be simplified into a few stages:

Ground moisture
→
Wall / foundation
→
Porous masonry & mortar
→
Capillary action
→
Upward moisture movement
1

Ground moisture

The ground beneath and around a building naturally contains moisture. After rainfall, poor drainage, groundwater and saturated soil can increase the amount of moisture surrounding the foundations. Where the wall has direct access to ground moisture and there is an inadequate moisture barrier, water can enter the masonry.

2

Porous masonry

Materials such as sandcrete blocks contain very small pores and pathways. When the lower part of a wall comes into contact with moisture, these pores can allow water to enter the masonry — the wall behaves somewhat like a network of very small channels through which moisture can move.

3

Mortar joints

Mortar joints can also contribute to the movement of moisture through a wall. Because mortar connects individual blocks together, moisture can travel through interconnected pores within the masonry and mortar — this is why the correct position within the wall construction matters when installing a remedial injection system.

4

Capillary action

Capillary action is the process that allows liquid to move through very small spaces, sometimes against gravity. In a damp wall, moisture can be drawn upward through the tiny pores within the masonry — the smaller and more interconnected the pathways, the greater the potential for capillary movement. This is the fundamental mechanism behind rising damp.

5

Moisture continues moving upward

If there is an effective damp-proof course (DPC), it acts as a barrier that interrupts the upward movement of moisture. However, if the DPC is missing, defective, damaged or bridged, moisture may continue moving upward into the wall above the intended barrier. As moisture rises, some of it eventually evaporates from the wall surface, leaving behind dissolved salts.

What Is the Role of a Damp-Proof Course?

A damp-proof course (DPC) is a horizontal moisture barrier incorporated into a building to prevent moisture from travelling upward through the wall.

Ground moisture ↑↑↑
→
DPC
→
Moisture movement interrupted

The DPC is therefore an important part of protecting walls from rising moisture. However, simply having something identified as a DPC does not necessarily mean that it is functioning effectively. A DPC can be compromised by construction defects, deterioration, or bridging — where another material creates a pathway around the barrier.

What Happens When There Is No Effective DPC?

Where there is no effective DPC, moisture from the ground can continue to enter the lower masonry. Over time, the affected wall may develop visible signs such as:

  • Damp staining
  • Peeling or bubbling paint
  • Crumbling plaster
  • White or powdery salt deposits
  • Deterioration of decorative finishes

The visible damage is therefore often the result of an ongoing moisture problem, rather than the original cause itself.

Why Do Salts Appear on Damp Walls?

Ground and masonry can contain soluble salts. As moisture travels through the wall, it can dissolve and transport some of these salts. When the moisture reaches areas where it can evaporate, the water leaves while some of the salts remain behind.

Repeated cycles of moisture movement and evaporation can therefore result in visible salt deposits or efflorescence. These salts can also contribute to the deterioration of plaster and paint.

Why Does Rising Damp Usually Affect the Lower Part of a Wall?

Because the moisture originates from the ground, the lowest sections of the wall are normally the first areas exposed to rising moisture. The height and appearance of dampness can vary depending on wall construction, moisture availability, evaporation conditions and other building factors.

The presence of dampness at the bottom of a wall can be an important clue, but it should not automatically be taken as proof of rising damp. Other sources of moisture can produce similar symptoms.

What Can Allow Rising Damp to Occur?

Ground moisture

Moisture in the soil provides the source.

Porous masonry

Tiny pores within blocks and mortar provide pathways for moisture.

Capillary action

This allows moisture to move through those small pathways.

Missing or defective DPC

Without an effective barrier, moisture can continue upward.

Bridged DPC

External ground, render, paving or other materials can sometimes create a pathway that bypasses the DPC.

Why Understanding the Mechanism Matters

Rising damp should not be treated simply by covering the visible damage. If moisture continues to enter and move through the wall, repainting or replacing the surface finish alone may not address the underlying problem.

Identify the moisture pathway and interrupt the upward movement before restoring the damaged wall.

This is the principle behind remedial rising-damp treatments such as chemical damp-proofing systems.

Rising Damp in Sandcrete Block Walls

Sandcrete blocks are widely used in construction across tropical and humid regions. Because sandcrete masonry can contain interconnected pores, moisture can potentially move through the wall when suitable conditions exist.

For this reason, understanding the relationship between ground moisture, porous masonry, mortar joints, capillary action and the DPC is particularly important when diagnosing dampness in these buildings.

Understanding Rising Damp Before Treating It

The key to understanding rising damp is to follow the moisture from its source.

GROUND
MOISTURE

The starting point — moisture present in the soil.

↓
ENTERS
WALL

Moisture enters the lower wall.

↓
MOVES
THROUGH

Water moves through pores in masonry and mortar.

↓
CAPILLARY
ACTION

Capillary action draws moisture upward.

↓
REACHES
WALL

Moisture reaches higher sections of the wall.

↓
EVAPORATION

Evaporation leaves salts behind.

↓
VISIBLE
DAMAGE

Dampness, salt deposits, peeling paint and damaged plaster can develop.

A properly functioning damp-proof course is designed to interrupt this upward movement. When the barrier is absent, defective or bridged, the pathway for moisture may remain open.

Understanding this mechanism helps homeowners, builders and damp-proofing professionals distinguish the cause of rising damp from the damage it produces — which is essential when selecting an appropriate remedial solution.

StopDamp+ is designed as a rising-damp treatment system for appropriate masonry applications, following the principle of creating a remedial moisture barrier and subsequently addressing affected wall finishes.

Think you might have rising damp?

See the full diagnosis guide, or get in touch for a proper assessment.

Read the Diagnosis Guide