The Upper Devonian Sandstone aquifer of Fife

The Devonian sandstone aquifer of Fife has long been recognised as one of the most important hydrogeological units in Scotland. Its importance was first acknowledged by Earp and Eden (1961), and the aquifer was later described by Foster et al (1976). Data were subsequently gathered together in map form (BGS, 1986) but little analysis of the aquifer was carried out other than a dissertation prepared by Barker (1981), occasional reports on specific issues such as nitrate pollution (e.g. Frost and Sargent, 1993; MacDonald, 1993; Ball, 1994), and the preparation of the 1: 100 000 scale Aquifer Vulnerability Map of Fife (SEPA, 1999). The aquifer currently supplies some 20 Ml/d during the winter, rising to 40 Ml/d in the summer months, when irrigation boreholes are put into use. Groundwater provides an important back up to public water supplies, particularly during dry years when river abstraction is restricted. Despite this, relatively little is known about the overall renewable resource potential of the aquifer. It is also only in recent years that means of safeguarding groundwater from pollution have been investigated in any detail. Renewed interest in the aquifer is now being driven on two fronts. The first is that the East of Scotland Water Authority (ESWA) needs to expand its source provision due to increasing demand. The second is that the Scottish Environment Protection Agency (SEPA) needs to look more closely at the aquifer potential if in the future groundwater abstraction licensing is introduced in significant aquifers (Robins and Ball, 1998). In addition, the requirements of the proposed EU Water Framework Directive indicate that a greater understanding of the aquifer and the sources it supplies will be needed in order to implement properly integrated surface and groundwater management on a catchment basis. With these goals in mind, the East of Scotland Water Authority, Scottish Environment Protection Agency and NERC have jointly commissioned this preliminary study of the Eden valley aquifer

Krypton gas as a novel applied tracer of groundwater flow in a fissured sandstone aquifer

Dissolved krypton gas (Kr) has been used as a novel, applied and "environmentally-friendly" groundwater tracer in the fissured Sherwood Sandstone aquifer at Queen's University Belfast, Northern Ireland. The tracer test involved a single-well slug injection and withdrawal (so-called "push-pull") technique, to study the dual-permeability nature of the aquifer. Analytical modelling of the tracer transport demonstrates that the shape of the Kr breakthrough curve is a result of two processes: relatively rapid dispersion of the tracer through rock fissures and slower diffusion into the sandstone pore spaces. Characterisation of this dual-permeability nature is important in assessing movement and fate of groundwater contaminants in the aquifer

Vitamin D in pregnancy at high latitude in Scotland

The aims of the present study were to determine compliance with current advice on vitamin D and to assess the influence of season, dietary intake, supplement use and deprivation on vitamin D status in pregnant mothers and newborns in the north of Scotland where sunlight exposure is low. Pregnant women (n 1205) and their singleton newborns were studied in the Aberdeen Maternity Hospital (latitude 57°N) between 2000 and 2006. Plasma 25-hydroxyvitamin D2 and 25-hydroxyvitamin D3 were measured at 19 weeks of gestation in mothers and at delivery in newborns. During pregnancy, 21·0 (95 % CI 18·5, 23·5) % of women took vitamin D supplements. The median intake was 5 μg/d and only 0·6 (95 % CI 0·1, 1·0) % took the recommended 10 μg/d. Supplement use, adjusted for season, dietary intake and deprivation, significantly increased maternal 25-hydroxyvitamin D (25(OH)D) by 10·5 (95 % CI 5·7, 15·2) nmol/l (P< 0·001); however, there was no significant effect on cord 25(OH)D (1·4 (95 % CI − 1·8, 4·5) nmol/l). The biggest influence on both maternal and cord 25(OH)D was season of birth (P< 0·001). Compared with the least deprived women (top three deciles), the most deprived pregnancies (bottom three deciles) were characterised by a significantly lower seasonally adjusted 25(OH)D ( − 11·6 (95 % CI − 7·5, − 15·7) nmol/l in the mother and − 5·8 (95 % CI − 2·3, − 9·4) nmol/l in the cord), and a lower level of supplement use (10 (95 % CI 4, 17) v. 23 (95 % CI 20, 26) %). More should be done to promote vitamin D supplement use in pregnancy but the critical importance of endogenous vitamin D synthesis, and known adaptations of fat metabolism specific to pregnancy, suggest that safe sun advice may be a useful additional strategy, even at high latitude