For many (many) years, studies
have been done to find associations between contaminated drinking water and
cholera cases. Most studies have concentrated on primary transmission through
drinking water and not the possibility of alternative transmission routes.
In Bangladesh cholera cases can
be year round, however, there are peaks in cholera cases that are generally
witnessed during two points of the year; southern coastal areas peak at the end of the
dry season (between late March to May), while cholera in the northern and
middle-belt regions of the country peak post-monsoon (September to November). It
is well documented (and has been stated here on this blog many times) that Vibrio cholerae, the causative agent of
cholera, thrives in the brackish waters in coastal areas, in this case; the Bay
of Bengal. Colonies of V. cholerae
bacteria can also grow on tiny phytoplankton and zooplankton, which is thought
to play an important role in V. cholerae
replication. The infective dose of V.
cholerae is 106 bacteria, thus, drinking water would need to
contain an infective dose ≥ 106 V.
cholerae per litre. However, it is now understood that V. cholerae becomes hyperinfective after passing through the human
digestive tract, demonstrating a tendency for person-to-person spread.
Environmental modelling has
recently been introduced to measure the abundance of zooplankton throughout the
river delta in Bangladesh to explain patterns of the annual peaks in the number
of cholera cases throughout the country. Despite considerable advances in
predicting cholera outbreaks, it remains unclear as to why studies have been unable
to find culturable, V. cholerae in
surface waters between peak cholera seasons as well as what environmental
changes might trigger the transformation of V.
cholerae from a dormant state to a culturable state and vice versa. Whilst
most cases are widely accepted to be waterborne, it is not well understood what
role water plays in the transmission that leads to the biannual cholera peaks
witnessed each year in Bangladesh. Maximal growth of V. cholerae occurs at 25,000 mg/l salinity. The minimum level of
salinity required for survival for 1 day at 25 °C is 100 mg/l, while the
optimum level for survival falls in the range 5000–30,000 mg/l. Water is
generally considered palatable at salinity levels below 1000 mg/l, however,
generally an individual’s tolerance of salinity in drinking water may be a
matter of acquired taste and/or influenced by freshwater availability.
Grant et al., (2015) aimed to
measure the salinity levels of common water sources in coastal Bangladesh and
explore perceptions of water palatability among the local population to discuss
the plausibility of linking cholera outbreaks in Bangladesh with ingestion of
saline-rich cholera-infected river water. The methods for this study were
refreshingly simple; a taste testing experiment with a hundred participants
taking part was orchestrated with varying levels of salinity. Two unions (a
union is comprised of multiple villages) in the coastal Upazila (subdistrict)
of Shyamnagar, Satkhira, Bangladesh, were chosen for the study by randomly
picking the names out of a hat. An additional, separate data set of salinity
measurements was gathered from various domestic and public water sources to
investigate whether the salinity levels within the local water sources were
optimal for V. cholerae survival and
growth. Both drinking and non-drinking sources were included in this sample
selection. 50 informal group discussions (25 in the monsoon season and 25 in
the dry season) were conducted to gain an in-depth understanding of water
sources and water uses. Questions were aimed at understanding which water
sources people use for drinking and other domestic uses and how respondents
perceived the saltiness of their drinking water.
Salinity levels of non-drinking
water sources suggest that the conditions for V. cholerae survival exist 7–8 days within the local aquatic
environment. However, 96% of participants in the taste-testing experiment
reported that they would never drink water with salinity levels that would be conducive
to V. cholerae survival. Furthermore,
salinity levels of participant’s drinking water sources were all well below the
levels required for optimal survival of V.
cholerae. Respondents explained that they preferred less salty and more
aesthetically pleasing drinking water. Theoretically,
V. cholerae can survive in the river systems
in Bangladesh; however, water sources which have been contaminated with river
water are avoided as potential drinking water sources. Furthermore, there are
no physical connecting points between the river system and drinking water
sources among the study population, indicating that the primary driver for
cholera cases in Bangladesh is likely not through the contamination of saline-rich
river water into drinking water sources.
Despite this study being
relatively simple, a lot was letting itself down. The idea itself was actually
a very nice idea with the potential of answering a lot of questions, however, missing
from this study were what conditions the people selected to participate living
in? The fact that they may have access to cleaner, more palatable water doesn’t
highlight that many others may not be so lucky with their choices of drinking water.
“Respondents also stated that although they are able to drink a certain
level and volume of saline water, they do not because other drinking water
options are available.”
Bangladesh is among the most
highly and densely populated countries in the world and to have a study based
on 100 people is, quite bluntly and harshly, preposterous to think it should contribute
any weight in the argument of cholera outbreaks.
Grant, S.L., Tamason, C.C., Hoque, B.A., Jensen,
P.K.M.,
2015. Drinking cholera: salinity levels and palatability of drinking water in
coastal Bangladesh. Tropical Medicine and
International Health. 20(4),
455-461.
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