Legionellosis is an important notifiable disease often causing sporadic community-acquired pneumonia in New Zealand.1 The predominant Legionella species responsible for disease are L. pneumophila and L. longbeachae; collectively contributing to…
The full contents of this page is only available to subscribers.
To view this content please login or subscribe
Legionella bacteria is ubiquitous in the environment. This study set out to expand our understanding of the environmental exposure risks to Legionella and whether seemingly unrelated environmental factors, such as aerosolised liquefaction-affected soil resulting from the Christchurch earthquakes had the potential to impact on disease prevalence. Liquefaction-affected soil could not contribute directly to the observed increase in legionellosis cases after the earthquakes due to its inability to support growth and survival of the Legionella bacteria. Chemical and size analysis of the liquefaction-affected soil showed it consisted of >65%. Silica. The authors propose that inhalation of earthquake associated airborne liquefaction-affected soil can damage lung tissue and cause inflammation. Inflammation and damage could allow opportunistic pathogens, such as Legionella bacteria, to more successfully infect the human host.
To investigate a possible link between liquefaction dust exposure and the noticeable increase in legionellosis cases in response to major earthquakes in 2010 and 2011 that resulted in widespread soil disturbance (liquefaction) in parts of Christchurch, New Zealand.
We culture tested liquefaction-affected soil for Legionella spp. in the six months following the first earthquake in 2010. Thirty silt samples were collected randomly from locations within Christchurch’s metropolitan area that were affected by liquefaction. The samples were tested to determine the presence of Legionella using qualitative and quantitative methods. Liquefaction-affected soil samples from three sites were further subjected to particle size distribution analysis and determination of major oxides. A controlled field study was established using six silt samples and one control (commercial compost), seeded with a wild-type strain of Legionella bozemanae serogroup (sg) 1 and persistence monitored over a 60-day period by culturing for the presence of Legionella. Dry matter determinations were undertaken so that total Legionella could be calculated on a dry weight basis.
Legionella bacteria were undetectable after day one in the silt samples. However, L. bozemanae sg1 was detected in the control sample for the entire study period.
This study showed that the liquefaction-affected soil could not contribute directly to the observed increase in legionellosis cases after the earthquakes due to its inability to support growth and survival of the Legionella bacteria.