Piezometer PZ2017/03, at the NE corner of Phase 1 and SE corner of Phase 2, is obviously unable to provide any meaningful information on how far to the west of this point the maximum groundwater levels would allow sufficient depth for mineral extraction, given water levels here have reached ground level.Clearly, therefore, there need to be further boreholes drilled at the redrawn eastern boundary of the extraction area – to fulfil Condition 30, ie. so that there are piezometers at "each corner of each working sub-phase".
Straitgate Farm near Ottery St Mary in Devon was bought in 1965 in the hope it would yield 20 million tonnes of sand & gravel. Straitgate Action Group was formed in 2001 to oppose a quarry due to concerns over water supplies, ancient woodlands, protected species, road safety and more. After finally gaining permission for just 1 million tonnes on appeal, Holcim UK – formerly Aggregate Industries – abandoned its plans in 2025. This blog records the long path to victory.
Monday, 22 April 2024
Two months on – PZ2017/03 is STILL underwater
Tuesday, 27 February 2024
Groundwater levels continue to rise at Straitgate
Wednesday, 21 February 2024
Another borehole showing ZERO depth of available resource
Last February was one of the driest on record for England & Wales with many locations seeing less than 10% of normal rain.
— Dave Throup (@DaveThroup) February 18, 2024
This February will be one of the wettest, many places will record more than 200%.
Extremes driven by climate change and things will get more extreme. pic.twitter.com/3xPTqh8soj
Planning conditions mean AI must drill more water monitoring boreholes
Piezometer coverage across the site shall be, at any time, no less than the proposed one piezometer at each corner of each working sub-phase. Piezometers which are lost through quarry working shall be replaced within seven days. Continuous monitoring of all site piezometers (and interpolation between them) shall be used to ensure, during working, that the base level to which the quarry is worked is no closer to the measured groundwater level than 1 metre.
Monday, 12 February 2024
Water level at borehole PZ2017/03 rises to GROUND LEVEL
Friday, 2 February 2024
AI has been pulling the wool over everybody’s eyes – planning inspectors included
Results from routine quarterly monitoring in April 2018 identified groundwater levels in localised piezometers on the eastern extraction area boundary higher than those depicted by the existing MWWT contour plot. Consequently, Devon County Council has determined this to be a material matter in that it has requested that the effects of these results be assessed to determine the effects on the quantity of mineral resource. Its position is defined in the following extract from an email dated 1st August 2018 (S Penaluna, Devon CC) as a: “......need to know exactly which areas might be excluded for reasons of groundwater protection and these would need to be indicated on a plan.”
1. The extraction area, as shown on the Wood E&IS plan, remains unchanged...4. The change [in mineral resource], moreover, results in no area being “excluded for reasons of groundwater protection” but merely a localised effect on the depth of working in a localised (eastern) part of the site.
Prior to the commencement of any soil stripping on any phase of the development, a review of the Maximum Winter Water Table (MWWT) grid (being the hydrogeologically modelled surface of the maximum winter water table based on the highest recorded winter groundwater levels) shall be submitted to the Mineral Planning Authority for its approval in writing.
The MWWT will ultimately form the base of the workable deposit, and any variation will impact the potential resource.
25. No water body shall be created within the site other than the approved weigh bridge lagoon.
Friday, 25 June 2021
AI’s MWWT ‘adjustment’ has been fudged
The maximum water level in PZ2017/02, which exceeded the MWWT back in 2018, went nearly 50cm higher in 2020. The groundwater level in this location has now exceeded the company's original guess by a whopping 1.75m. Water levels in PZ06 – installed back in 2013 – also reached a new maximum, as did three other piezometers.
...as requested by DCC, this document includes a revised version of the Maximum Winter Water Table (MWWT) grid which incorporates any recently recorded groundwater water levels higher than the previous MMWT (including ‘spot’ groundwater level measurements recorded in 1990).
The revised MWWT is included in this pack of correspondence and includes additional adjustment for slightly higher groundwater levels recorded close to the eastern boundary (PZ06, 2017/02 and 2017/03) in April 2018 and February 2020. The following are noted from the revised MWWT: The method used for determining the MWWT is slightly conservative and means that the extent to which the grid is raised propagates from the eastern boundary to the centre of the excavation area. In reality, the higher recorded groundwater levels most likely represent more localized effects close to the eastern boundary.
If any of the maximum recorded groundwater levels exceed the height of the MWWT grid then the MWWT grid shall be updated using that data...
Continuous (daily) monitoring of all site piezometers, and interpolation between them, shall be used...
Monday, 14 June 2021
Oh look, yet ANOTHER location where AI’s seasonal working scheme can’t work
2.2.8 By working only to the MWWT then during the summer months the water table will be lower. Therefore across the areas being worked the zone of water level fluctuation is undisturbed. This zone is at least 1m thick. Appendix C includes a plot showing the contours of average summer unsaturated mineral thickness, derived from the MWWT (i.e. the final proposed depth of working) and the Average Summer Low Water Table from piezometer readings.
our recommended condition requires that the base of the excavation is no closer to groundwater level than 1m at any time.
Based on further information received from SAG we recommended to Devon County Council that the applicant updates the Maximum Winter Water Table grid with groundwater levels recorded at the site in 1990.
Sunday, 16 May 2021
The Great MWWT Hoax – AI’s groundwater model has been sketched by hand
A description of the tolerance levels and interpolation method used to produce the ‘Maximum Winter Water Table’ grid
Four alternative grid interpolation methods were selected: Simple linear Kriging; A Radial Basis Function; Inverse Distance to a Power; Triangulation with linear interpolation. Each of these methods represents an exact interpolator in which the input data point will be preserved and respected by the interpolation algorithm…. The grid determined by Radial Basis Function was therefore adopted as being a more conservative preferred method for estimating the maximum water table distribution.
The description of how the MWWT grid was calculated explained that two of the interpolation methods used produced realistic results (in line with expected hydrogeological behaviour and professional judgement). One method, ‘Radial Basis’ produced a grid that was generally higher than the other grid prepared by a Kriging method. As the MWWT was subsequently based on the higher of the two interpolated surfaces (i.e. Radial Basis interpolation) this could be considered to represent the upper limit of interpretation, with the Kriging interpolation representing the lower limit of interpretation and therefore the difference between these two realistic grids could be considered as reflection of the ‘tolerance’.
The generally higher Radial basis grid is subtracted from the generally lower Kriging basis grid to give an indication of “tolerance”….The Radial grid formed the basis for the final composite MWWT (shown in Figure 5), which also underwent final adjustment (upwards) to take further account of hydrogeological professional judgement.
We have reviewed the document and we are satisfied that it answers our questions about the derivation of the Maximum Winter Water Table grid.
If a sensible, well conditioned parameter and an appropriate generating function are chosen, a radial basis function will be a well behaved mathematical surface with continuous, smoothly differentiable contours between interpolation points... The only conclusion is that AI have defined their MWWT by hand.
AI to drill boreholes at Penslade for ‘monitoring of the watertable’
Policy M12 proposes two new locations for mineral working... In the event that Straitgate Farm proved to be incapable of being delivered, then the other site, West of Penslade Cross, would have adequate resources to enable sand and gravel supply to be maintained for the Plan period.
The boreholes will be between 23m and 38m in depth and piezometers will be installed to enable the monitoring of the watertable as required by the Devon Minerals Local Plan.
at a meeting last week, AI's Head of Geological Services confirmed that budgets are now in place to install piezometers at Penslade…
It is envisaged that groundwater monitoring will be undertaken for a minimum of 3 years prior to submission of a planning application in some 5 years hence.
Monday, 26 April 2021
AI’s ‘conservative’ model of the MWWT has been EXCEEDED YET AGAIN
...the computer model derived MWWT surface is unlikely to provide an accurate representation of the real maximum groundwater levels
In 2018, Aggregate Industries put a stop to public scrutiny of groundwater data for the Straitgate site – after groundwater levels embarrassingly exceeded the company’s guesstimate of the maximum winter water table, the MWWT, in four locations by up to 1.6m. The MWWT is intended to be the base of any quarry. It’s important to get it right, if no buffer or margin of error is to be left to protect surrounding water supplies. It had apparently been "defined with confidence", but the company still won’t come clean on its accuracy. It was shown to be wrong by a staggering 2.8m in one location.
a negative tolerance represents conservatism and contingency which is incorporated in the selection of the MWWT
Aggregate Industries' realistic assessment will no doubt have been breached YET AGAIN. Earlier this year, PZ10 reached 102.4 mAOD – 70cm higher than in 2018. It’s virtually certain that a number of the newer piezometers – PZ2017/02 and PZ2017/03 in particular – will have recorded new maximums.
The steep hydraulic gradient combined with limited monitoring, in my opinion, is likely to result in errors in the actual depth to maximum groundwater across the site.
The MWWT is never going to be an accurate prediction of the maximum water table. There needs to be a margin of safety, a freeboard, an unquarried buffer retained above the MWWT – like EVERY OTHER QUARRY where drinking water supplies are at risk.
Thursday, 25 March 2021
‘Note: All models have uncertainty / margin of error’
Note: All models have uncertainty / margin of error
The MWWT – the maximum winter water table – would be the base elevation of any quarry at Straitgate Farm. It is a model, a prediction of what might be happening across some 55 acres, based on water levels recorded in just 6 piezometers. The accuracy of this prediction would matter less if Aggregate Industries were planning to leave a safety margin, an unquarried buffer, above this surface – but it is not.
All AFW was attempting to do was to obfuscate, to confuse, to muddle the EA. All AFW was doing was showing the difference between how two techniques (kriging and radial basis) have interpolated 6 measurements to predict groundwater levels across 55 sloping acres. All AFW was showing was the difference between one inaccurate model and another inaccurate model. This is not a tolerance, it is a difference. What AFW has NOT done, for very obvious reasons, is to consider – at least in public, for the benefit of locals, the Council and the EA alike – the inherent inaccuracies of each of those techniques.
We have reviewed the document and we are satisfied that it answers our questions about the derivation of the Maximum Winter Water Table grid.
The MWWT for this site has been defined by using a computer model as the number of piezometers (six) are insufficient to cover the quarry area in sufficient detail. Computer models of groundwater systems are good at showing changes in groundwater levels although they are poor at showing the actual amount of such changes. As a result, the computer model derived MWWT surface is unlikely to provide an accurate representation of the real maximum groundwater levels...
I am concerned that there is a very steep hydraulic gradient across the site, from around 152m in the west to less than 135 m in the east, and the limited number of piezometers used to grid the water table surface. Variations in the shape of the water table cannot be contoured based on the number of piezometers used in the application... The steep hydraulic gradient combined with limited monitoring, in my opinion, is likely to result in errors in the actual depth to maximum groundwater across the site.
an unquarried buffer of at least 3 m is left above the maximum water table to minimise the negative impacts.
Wood sets aside extra $151m to settle corruption probes https://t.co/jBOpol0roY
— FT Energy (@ftenergy) March 16, 2021
Thursday, 24 September 2020
AI’s quarry plan for Straitgate likely to be UNDER WATER AGAIN
The MWWT grid will therefore be modelled from levels lower than reality, which will enable AI to excavate below the maximum water table.
a realistic assessment of the change in MWWT arising from the readings in April 2018
Wednesday, 13 May 2020
Prof warns DCC – quarry at Straitgate would ‘irreversibly damage’ water sources
If your report raises any new issues which the EA consider to be material then I will ask the applicant to clarify.
the application for the proposed quarry should be refused because of the irreversible damage that it will cause to the local groundwater system that both supports local habitats and forms the water supplies for Cadhay House with its medieval fishponds and tearooms, more than 100 people plus three livestock farms. 80
The moderately low pH, alkalinity and dissolved solids in groundwater in this area is, therefore, not necessarily a function of the time it takes for water to pass through the unsaturated zone, but a function of the variable and limited presence of soluble material within the sub-surface materials. A reduction of the unsaturated zone therefore will not necessarily give rise to a reduction in the pH, alkalinity or dissolved solids concentration of groundwater. With respect to the topsoil, subsoil and overburden that will be replaced once extraction of an area is completed, the replaced material will then be subject to water/rock interaction processes as water percolates through the replaced unsaturated zone material. As is shown by the leach test data, the soluble content of the unsaturated zone is low across much of the site or is mostly influenced by the shallow deposits which will be replaced after mineral extraction. Therefore, again, this implies that removal of the deeper unsaturated material will not necessarily result in a noticeable change in groundwater quality beneath the site or, more categorically, not at downgradient receptor. p10
The length of the travel time involved is critical in determining the development of the chemistry of the water that discharges from the springs. 35
The length of the travel time involved is critical in determining the development of the chemistry of the water that discharges from the springs. 35
...the whole of the flow path from the ground surface where recharge water starts its journey downwards through the unsaturated zone to the water table where it becomes groundwater which then flows through the saturated zone to emerge at the springs is essential in the development of the water chemistry. The removal of part of the unsaturated zone where flow velocities are far less than in the saturated zone will result in the greatest impact on the water chemistry. 21
transit of water through the unsaturated zone is considered to be fairly rapid due to the intergrannular and fractured nature of the BSPB and therefore the thickness of the unsaturated zone may not be as important. 2.5
...recharge reaches the water table in the BSPB through unsaturated thicknesses of between approximately 3 and 10 m within between 1 and 3 days. This is consistent with the conceptual model for relatively rapid recharge occurring in the BSPB (i.e. days rather than weeks or months). 2.7.3
It is important not to confuse this type of flow with one that suggests that the recharge from any rainfall event reaches the water table rapidly through fracture flow 60
According to Wang et al (2012) the unsaturated zone velocity for the Sherwood Sandstone Group falls in the range 0.6 – 2.3 m/year with a mean of 1.06 m/year (these values were summarized by Chilton and Foster (1991)). The values for unsaturated zone flow rates are several orders of magnitude (three to five) lower than flow velocities in the saturated zone. 59
... the lack of cement means that the rock is basically a pebbly sand with layers of silt and clay; consequently there are no fractures and so there will be no bypass flows. 59
It is simple to calculate the loss in groundwater travel time caused by the loss of some 7 m of the unsaturated zone as it is 7 × 1.06 years = 7.42 years. 62
…the proposals will cause a large reduction in the thickness of the unsaturated zone that will reduce the time for the recharge to percolate through this zone. This reduced period will mean less time for rock/water interaction and will result in a less chemically mature groundwater that is more acidic than it is at the moment. These are reasons why the application should be refused by Devon County Council. 5.13
The water chemistry develops as the water percolates through the unsaturated zone and then, once it has reached the water table, it flows through the aquifer. A series of rock/water interactions takes place along this flow path causing the chemistry of the water to change as it moves along. These interactions are slow and so the time taken for the water to reach the springs will determine the concentration of the dissolved minerals, the balance between the dissolved minerals, the pH and the electrical conductivity of the water. 35
The EA calculated the Source Protection zone (Walford, 2013) using a similar method to the one adopted here. The map they have produced is shown below in Figure 11. The distance of the flow path from the recharge area in the proposed quarry to the Cadhay spring has been marked on the map. 64
Calculations of the time that groundwater takes from rainfall percolating into the ground to the groundwater emerging from a spring have been carried out for the Cadhay spring that supplies Cadhay House and estate. The water takes almost 15 years to make this journey and if all but 1 m of the unsaturated zone is removed this reduces some 50% of the total travel time. 76
It shows that the time taken can be expected to be sufficiently long for the quarrying to have been completed by some years by the time that the water quality changes have occurred. This will provide scope for AI to deny causing the problem. 77
The impact on the travel time also means that the deterioration of the groundwater chemistry will be a permanent change and it will not be possible to reverse it. 77
The concern for the 100 people or so who obtain their water supply from these springs is that the water make up will substantially change and a reduction in the pH will mean that the water is too acidic for drinking without treatment and it will dissolve metal pipework and storage tanks. It will affect the chemistry of the water in the streams that will impact on the Cadhay Bog and Cadhay Wood wetland habitats in the ancient woodland as these depend on the stream flows. 56
The use of fully penetrating piezometers to monitor the elevation of the water table as is the case at the Straitgate Farm site, means that it can be expected that the water levels in the piezometers will reflect a lower water level than the correct water table due to the three-dimensional aspect of groundwater flow. The MWWT grid will therefore be modelled from levels lower than reality, which will enable AI to excavate below the maximum water table. 73
















