What is Pyrite

Aidan O’Connell talks to George Hook on The Right Hook on Pyrite

Audio clip: Adobe Flash Player (version 9 or above) is required to play this audio clip. Download the latest version here. You also need to have JavaScript enabled in your browser.

Pyrite or Iron Pyrite (FeS2) is a very common mineral that is present in many sedimentary rocks as framboidal crystals. Subject to certain conditions, pyrite is problematic in confined construction, such as under floor filling and bridge embankments. This is due to a chemical reaction that can cause pyritic backfill to swell.

Construction material containing relatively large amounts of pyrite minerals are likely to expand, crack and/or crumble over time. This occurs when framboidal crystalline pyrite, air and moisture, mix causing a chemical reaction to occur that creates expanding crystals within the material.

Areas affected by Pyrite

The confirmed areas that have been affected by pyrite-heave are mostly concentrated in North Leinster, particularly in  North County Dublin, Offaly, Meath and Louth.

Why is Pyrite a problem?

The presence of pyrite in aggregate (floor hardcore) can lead to severe deterioration in construction materials as the pyrite oxidises. This results in cracks in floors and walls that will need to be rectified by removing the floor hardcore and replacing it with aggregate that conforms to the new building standards.  Once this remedial work is carried out your home can be certified as Pyrite free.

It should be noted that the presence of pyrite alone does not directly lead to pyritic heave. Other factors that must be present to lead to a potential problem include the type of pyritec rystals, the presence of oxygen, the availability of moisture and the nature of the rock type. The pyrite reaction may be further accelerated by heat and thiophilic bacteria.

For more information, download our brochure.

How do I identify Pyrite?

How do I resolve the issue?