Water quality - Fylde

Water quality

There are two significant aquifers across Lancashire: a shallow aquifer formed of superficial glacial sand and gravel interbedded with clay (Figure 1) and a deeper aquifer formed by the Sherwood Sandstone Group (Figure 2).

FyldeMapsAllsitesJBedits_Superficial FyldeMapsAllsitesJBeditsBedrock

The shallow aquifer is up to 40 m thick and is designated by the Environment Agency as a secondary B aquifer. It is used for private drinking water supply, farms and golf course irrigation. In the area of former shale gas exploration, this aquifer is underlain by a thick layer (up to 350 m) of a low-permeability mudstone, the Mercia Mudstone Group. Water moves slowly through this mudstone and it is not classed as an aquifer. Below this is the Sherwood Sandstone Group, which reaches a thickness of up to 750 m. The Sherwood Sandstone Group is classified as a principal aquifer.

The Sherwood Sandstone is too deep to be practically accessible in the area below the Fylde. However, to the east of the shale gas exploration (east of the Woodsfold Fault; see Figure 1), the aquifer is much closer to the surface. In this area, it is used for both public and private water supply.

The aquifer units overlie the deeper shale that was the shale gas target. In the area of the former gas exploration site, the shale units occur at some 2000 m below the surface.

Water sampling

BGS established a network of water sampling sites consisting of third-party boreholes, wells and streams within a radius of some 10 km of the Preston New Road (PNR) and Roseacre Wood (formerly proposed) sites (figures 1 and 2). The network comprised 15 groundwater sites from the superficial deposit and Sherwood Sandstone Group aquifers, and 11 streams. We monitored the water quality at these sites from 2015 to 2020.

We also drilled new boreholes in the vicinity of the PNR and Roseacre sites for more detailed groundwater investigation. These were monitored quarterly as for the groundwater sites in the monitoring network from February 2016. A deep borehole (500 m) provided for further characterisation of deep groundwater.

Groundwater quality monitoring

Monitoring of third-party boreholes and wells, together with newly drilled BGS boreholes, involved sampling and analysis of a wide range of physico-chemical parameters, including:

• water level
• temperature
• pH
• conductivity
• redox potential
• major ions and trace elements
• dissolved gases (oxygen; methane; carbon dioxide; radon)
• organic chemicals (for example, total petroleum hydrocarbons and volatile organic compounds)
• stable isotopes (¹⁸O, ²H of water, ¹³C of inorganic carbon and methane)
• groundwater ‘age’ indicators (CFCs)

Monitoring equipment installed in the new boreholes provided near real–time measurements of additional water-quality parameters.

Groundwater

Results from the baseline monitoring of pumped groundwater samples (Figure 3) show that:

• the groundwater in both the superficial deposits and Sherwood Sandstone Group aquifers has near-neutral pH and is largely anoxic (it has low or no dissolved oxygen)
• concentrations of nitrate (NO₃–) are low
• concentrations of iron (Fe) and manganese (Mn) are high
• concentrations of arsenic (As) and ammonium (NH₄+) are high in some of the groundwater tested

Methane (CH₄) is also often detected, though rarely at high concentrations. The composition of CH₄, where present, suggests that it has been produced in the superficial sediments by microbial reaction of organic matter.

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Analysis of organic chemicals suggests that the groundwater contains detectable quantities of some pesticides, perfluorinated compounds and other synthetic chemicals, but the concentrations are low and the numbers of chemicals detected are small. The presence of these substances does, however, indicate effects on the shallow groundwater as a result of human activity (Figure 3).

Monitoring of groundwater in the two aquifers (figures 4, 5 and 6) has shown that the chemical characteristics have been broadly consistent over time. Concentrations of naturally occurring CH4 up to 4 mg/L were observed in groundwater from the superficial aquifer; concentrations in the Sherwood Sandstone Group groundwater are generally low (less than 0.7 mg/l).

TSByType_Quaternary_Ca_Fig4a TSByType_Quaternary_Na_Fig4b TSByType_Quaternary_HCO3_Fig4c TSByType_Quaternary_SO4_Fig4d TSByType_Quaternary_Fe_Fig4e TSByType_Quaternary_CH4_Fig4f

TSByType_SST_Ca_Fig5a TSByType_SST_Na_Fig5b TSByType_SST_HCO3_Fig5c TSByType_SST_SO4_Fig5d TSByType_SST_Fe_Fig5e TSByType_SST_CH4_Fig5f

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Surface water

Analysis of water from first-order streams shows generally lower concentrations of dissolved solids than found in the local shallow groundwater, though with slightly higher concentrations of NO₃, nitrite (NO₂–) and dissolved organic carbon (DOC). Many trace elements also have lower concentrations than local groundwater due to a combination of differing redox conditions and more limited interaction with rocks and soils. Monitoring of stream quality over time showed by far the greatest variability (Figure 7), considered to be due mainly to varying impacts from amounts of rainfall and water turbidity.

Post baseline monitoring

Figures 4, 5, 6 and 7 indicate (grey wash) the initiation of hydraulic fracturing at PNR (October to December 2018 and August 2019) and the subsequent periods. Data from these post-baseline dates provides no evidence for any effect on water quality from the PNR exploration works. Although concentrations of solutes continued to vary over time, key parameters remained within the baseline range at individual sites.

TSByTypestream_Ca_Fig7a TSByTypestream_Na_Fig7b TSByTypestream_HCO3_Fig7c TSByTypestream_SO4_Fig7d TSByTypestream_Fe_Fig7e