Smedley, Pauline; Cooper, David
ORCID: https://orcid.org/0000-0001-7578-7918; Lapworth, Daniel Joseph
ORCID: https://orcid.org/0000-0001-7838-7960; Ander, Louise.
2008
Molybdenum in British drinking water : a review of sources and occurrence and a reconnaissance survey of concentrations.
Nottingham, UK, British Geological Survey, 41pp.
(OR/08/051)
(Unpublished)
Abstract
Although there is no statutory limit for molybdenum in UK or European drinking water, the
WHO since 1993 have recommended a health-based guideline value for molybdenum in
drinking water of 70 μg L–1. This report provides an assessment of the occurrence and
distribution of molybdenum in UK surface waters, groundwaters and drinking waters in order
to assess the implication for the UK water industry should legislation to limit the
concentrations of molybdenum in drinking water, commensurate with the WHO guideline
value, be introduced in the coming years.
A survey has been carried out of molybdenum (Mo) concentrations in drinking water from
twelve public-supply sources distributed across England & Wales, monitored up to four times
over an 18-month period, together with domestic taps from three of their supply areas. As the
scale of the survey was limited, a formal probability-based survey design was not possible.
Instead a purposive sampling approach was adopted, focusing on those regions where the risk
of exceedence of the WHO guideline value, based on available surface-water and
groundwater data, was believed to be greatest. The design adopted was therefore nonprobabilistic
and not able to provide statistical estimates of probabilities of exceedence.
However, it was considered appropriate for reducing uncertainty over sources of greatest risk.
Public-supply sources included five groundwater sources (one a mine sough), four river
sources and three upland reservoir sources.
For three of the public-supply sources investigated, molybdenum concentrations for all
samples were below the detection limit of 0.03 μg L–1. For the remaining nine sources,
analysis of variance confirmed that significant differences existed in molybdenum
concentration between sites but not within sites at different sampling times. Although
concentrations in surface waters were generally more variable than in groundwaters, the
results did not show evidence of a notable seasonal effect. All analysed concentrations were
more than an order of magnitude lower than the WHO guideline value for Mo of 70 μg L–1.
Tapwater samples were analysed from eight households in each of three areas: Bangor
(Gwynedd), Mickleover (Derbyshire) and Haverhill (Suffolk). Sampling at each tap involved
collection of a morning first-draw (pre-flush) sample and a post-flush sample. Analysis
showed a remarkable uniformity in molybdenum concentrations at each location, the
variability being very small between houses (old and new), between pre- and post-flush
samples, and between the tapwater and respective source-water samples. The results suggest
that water distribution pipework has a negligible effect on supplied tapwater molybdenum
concentrations. All tapwater samples from Bangor had molybdenum concentrations below
detection limit, consistent with those in the public-supply source water. Tapwaters from
Haverhill were not significantly different from their source waters (p >0.05). Mickleover
tapwaters had lower Mo concentrations than source waters. The differences were statistically
significant (p <0.001), although their absolute magnitude was small. There was a possible
tendency (p=0.04) for post-flush samples at Mickleover to have slightly higher molybdenum
concentrations than pre-flush samples. Such a difference may be due to adsorption of
molybdenum onto surfaces (pipes, encrusted minerals) during overnight standing of water in
the pipes. Again, the magnitude of the differences was small. Analysis of other trace elements
by the ICP-MS technique used, revealed significant differences in concentrations of copper
(Cu), zinc (Zn), nickel (Ni) and lead (Pb) between pre-flush and post-flush water samples. In
two pre-flush samples, concentrations of Ni or Pb were above drinking-water limits, although
in all cases, post-flush waters were compliant. These high concentrations most likely derive
from metal pipework in the domestic distribution system during overnight standstill. Pre-flush
Pb concentrations were generally higher in water from older properties.
A compilation has also been made of available data for molybdenum in streams, rivers, lakes
and groundwaters, together with stream sediments, soils and rocks in the UK. The data derive
from a combination of the BGS and GSNI ‘G-BASE’ databases (geochemical baseline data
for streamwater, stream sediment and soil), the BGS groundwater database, CEH data from
the Land-Ocean Interaction Study (LOIS) project which characterised quality of river waters
in eastern England, and CEH data from the Environmental Change Network (ECN) for
lakewater quality in Cumbria. Data have also been collated from the open literature.
The results indicate that concentrations of molybdenum in rocks, sediments and soils in the
UK are typically less than 10 mg kg–1. Higher concentrations (>20 mg kg–1) can be found in
some argillaceous deposits, especially black shales and other sulphide-rich deposits.
Relatively high molybdenum concentrations are also found in some ironstones and granites.
Concentrations of molybdenum in 65,447 stream sediments from England & Wales (G-BASE
data) range up to 309 mg kg–1 but with a 90th percentile value of just 2.9 mg kg–1. Analysis of
5874 stream-sediment samples from Northern Ireland showed concentrations ranging up to
86 mg kg–1 but with a 90th percentile of 6.7 mg kg–1.
Concentrations of molybdenum in surface waters and groundwaters in Britain are usually very
low. Analyses of 96 lakewater samples monitored in 2004 from Lake Windermere and
Esthwaite Water in Cumbria have concentrations of 0.1 μg L–1 or less. Analyses of 11,562
streamwater samples from the G-BASE dataset have a range of <0.05–230 μg L–1 although
the 10–90th percentile range is much narrower, 0.08–2.45 μg L–1, with a median value of just
0.57 μg L–1. Analyses of water samples from the LOIS rivers also typically have median
concentrations <1 μg L–1, although sites on the Rivers Calder, Don, Trent, Great Ouse and
Thames have higher median values, in the range 3–10 μg L–1. The highest observed
streamwater concentrations in both the G-BASE and LOIS datasets appear to be from the
River Aire and its tributaries in south Yorkshire. In the River Aire, concentrations had a
notable correlation with river flow, being highest under low-flow conditions. Concentrations
in several low-flow samples were close to the WHO guideline value (tens of μg L–1) though
rarely exceeded it. The high values in this area are interpreted as the result of contamination
by coal-mine drainage and possibly other industrial contaminants. The River Aire in its
industrial reaches is not used as a source of public drinking-water supply because of its
recognised polluted condition.
Molybdenum data for 1398 groundwater samples from the BGS groundwater database have a
range of <0.1–120 μg L–1 but with a 10–90th percentile range of 0.1–1.5 μg L–1 and a median
of 0.12 μg L–1. Only three samples (0.21%) have concentrations in excess of the current WHO
guideline value. Median concentrations distinguished by source type (springs, boreholes,
wells, mine drainage) are all close to or less than 1 μg L–1, although relatively high
concentrations characterise mine-drainage waters (0.60–6.0 μg L–1, median 1.4 μg L–1). These
are likely derived by the release of molybdenum following oxidation of sulphide minerals.
Relatively high molybdenum concentrations appear to be a particular feature of reducing
(anaerobic) groundwaters and groundwaters with prolonged residence times in host aquifers.
The highest observed concentrations are found in reducing groundwaters from greensand
aquifers (Lower Greensand, Carstone, Spilsby Sandstone).
The ranges observed in both groundwaters and surface waters indicate that molybdenum
concentrations in Britain rarely occur in excess of or approaching the WHO guideline value
for molybdenum in drinking water. In the event that a new drinking-water limit at a
comparable concentration (70 μg L–1) is introduced for molybdenum in national or European
legislation in the coming years, our results suggest that molybdenum should not pose a
significant problem for the UK water-supply industry.
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