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SuDS Infiltration Suitability Map

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SUDS INFILTRATION SUITABILITY MAP

Identifying site suitability for sustainable drainage systems (SuDS)


SUDSMART
SD50

From £25

per km2*

SuDS map and summary
Preliminary assessment
Resolution: 50m

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Identifying site suitability for sustainable drainage systems (SuDS) schemes for developers, architects and local authorities.

Climate change is compelling local authorities to think smarter about sustainable property development. Reconciling the pressure for housing with better environmental management is bringing forward new guidance on improved site drainage and flood mitigation.

Our unique SuDS Infiltration Suitability Map reveals the locations best suited to sustainable drainage to meet new compliance standards for planning submissions.

Government policy for England is to introduce SuDS to control site rainfall runoff via conditions in planning approvals. Infiltration into the ground is the preferred method for managing surface water runoff on site without increasing flood risk downstream.

Property professionals must assess the feasibility of infiltration SuDS at an early stage in support of the site development process. This will allow outline site assessment of the cost implications and initial master planning of the development prior to the requirement for detailed design.

Lead Local Flood Authorities also need clear guidance on the site suitability for infiltration SuDS when they are assessing proposed developments.

To discuss the SuDS screening map and how it can improve your planning submission for your client, contact us today.

FEATURES

GeoSmart SD50 provides an assessment of the capacity of the ground to receive infiltration depending on the nature, thickness and permeability of the underlying material and the depth to the high groundwater table.

BENEFITS

  • Allows preliminary assessment of the site without the need for a bespoke SuDS design
  • Use in conjunction with the SuDSmart report range to identify SuDS infiltration suitability and flow/volume design data
  • GeoSmart SD50 and SuDSmart used together may be sufficient to obtain outline planning
  • Provides the client with a clear site risk profile on drainage cost and land area needed

Other available reports

Save when purchasing two or more reports

Floodsmart
Flood Risk

SuDSmart
Sustainable Drainage

* Admin and data processing costs may apply

Why choose GeoSmart?

Our environmental reports are second to none in terms of quality, compliance and current data. We also provide £5m of PI cover for all reports and services.

FAQs

Your frequently asked questions answered:

What is Groundwater Flooding?

Groundwater flooding occurs when sub-surface water emerges from the ground at the surface or into Made Ground and structures. This may be as a result of persistent rainfall that recharges aquifers until they are full; or may be as a result of high river levels, or tides, driving water through near-surface deposits. Groundwater flooding is characterised by:

  • Water flows to the surface or into basements, services ducts and other subsurface infrastructure rising up through floors or directly from the ground. This may be seen as diffuse seepage from the ground, as emergence of new springs or as an increase in spring flows
  • Flooding may last a long time compared to surface water flooding, from weeks to months. Hence the amount of damage that is caused to property may be substantially higher. Likewise closures of access routes, roads, railways etc. may be prolonged
  • Flooding may occur with a delay following periods of high rainfall rather than immediately during storms
  • Emergent groundwater tends to be clear and relatively clean compared to muddy fluvial flood waters, but potential contamination by sewers and brownfield sites poses additional hazards
  • Groundwater flooding or a shallow water table prevents rainfall infiltration and increases the risk of surface water flooding. This means that many surface floods are actually driven by groundwater conditions. But consideration of surface water in isolation and lack of evidence for groundwater conditions leads to incorrect analysis of overall causes

What are potential impacts of Groundwater Flooding?

Whilst groundwater flooding is generally less hazardous to human health than surface flooding, it is more hazardous to property for a given flood depth, producing 2 to 4 times the damage to building fabric and greater disruption to economic activity due to the longer duration of flood events. Also, the impact may be less about surface water depths or velocities and more about the extended saturation of the shallow subsurface with the following consequences:

  1. Damage to basements and other structures below ground
  2. Damage to infrastructure such as buried services and ducts
  3. Sewer flooding
  4. Water damage to property, cultural heritage, crops or sensitive habitats due to saturated conditions
  5. Leaching of contamination from brownfield sites and other sources of contamination
  6. Slope stability issues
  7. Increased likelihood, intensity and duration of surface water flooding due to saturated ground conditions and failure of infiltration drainage systems
  8. Increased cost of construction projects, which will need to incorporate preventive groundwater control measures to prevent what, would otherwise cause harm

In what situation would I need to consult the Groundwater Flood Risk Map?

Groundwater is one of the sources of flooding that may affect a location with potentially important consequences for properties and infrastructure, therefore a review of the groundwater flood risk for a site is recommended prior to a property transaction or property development.

An initial screening review will be sufficient for most areas that are at negligible risk of groundwater flooding. Areas that may be at significant risk of groundwater flooding generally require a more detailed site-specific assessment.

The Groundwater Flood Risk Map allows users identify whether groundwater may be a source of flooding at their site. It is available at multiple scales and risk resolutions.

What is the coverage and resolution of the Groundwater Flood Risk Map?

The Groundwater Flood Risk map has full coverage over Great Britain. The map is available at multiple scales and risk resolutions:

GW5: The Groundwater Flood Risk map is available at 5m resolution for Great Britain. It classifies groundwater flood risk in every cell on a 5m grid covering Great Britain into one of 4 risk categories: Negligible, Low, Moderate, and High.

GW200-S: The Groundwater Flood Risk map is available on a 200m grid covering Great Britain as a Screening Map. It classifies groundwater flood risk for each cell on that grid into one of two categories: ‘Potentially At Risk’ and ‘Negligible Risk’, based on the maximum risk occurrence within that cell as represented on the higher resolutions products, GW5.

Who is the groundwater flood risk map intended for?

  • House builders and developers
  • Property professionals such as architects, planning consultants and land agents
  • Lawyers and solicitors
  • Lenders, banks or mortgage providers
  • Businesses
  • Private individuals
  • Insurance companies
  • Local Authorities and regulators

What will the map tell me about my property?

The map can tell you whether groundwater flooding is likely to be a concern at a specific site, and will provide recommendations based on the level of groundwater flood risk modelled for that site.

However, it does not provide an alternative to a proper site-specific assessment, and a detailed risk assessment should be used for any site where the impact of groundwater flooding would have significant adverse consequences.

The map classification shows on a national mapping scale the areas within which property may be at risk, but this should not be mistaken to mean that groundwater floods will occur across the whole of the groundwater flood risk zones.

Mapping limitations and a number of local factors may reduce groundwater flood risk to land and property even where it lies within mapped groundwater flood risk zones.

What data is the map based on?

The groundwater flood risk model used to produce the map incorporates various national scale datasets including Terrain 50 topographical data produced by the Ordnance Survey, LIDAR Digital Terrain Models produced by the Environment Agency, 1:50,000 scale Geological Maps produced by the British Geological Survey, and Groundwater Level data produced by the British Geological Survey.

Bespoke in-house hydrogeological and risk models were used to process this data and produce the Groundwater Flood Risk Map. A national database of recorded groundwater flooding events collated by GeoSmart from various sources is used to calibrate and validate the Groundwater Flood Risk Map.

What do the risk categories mean?

Mapped classes combine our understanding of likelihood, model and data uncertainty and possible severity. Likelihood is ranked according to whether we expect groundwater flooding at a site due to extreme elevated groundwater levels with an annual probability of occurrence greater than 1%, taking into account model and data uncertainty.

Severity relates to our expectations of the amount of property damage or other harm that groundwater flooding at that location might cause.

What if my property is shown to be at risk of groundwater flooding?

This does not mean that the property will flood. The GeoSmart Groundwater Flood Risk Map is a national scale product that highlights areas where there is sufficient evidence to suggest that flooding could occur.

However, there are a number of reasons why the national map may be indicating risk where there is no actual risk at a local scale (mapping limitations), and also a number of local factors that may protect land and property even where it lies within confirmed flood risk zones (property protection factors).

Mapping Limitations

Some of the main reasons why the map may be indicating risk in areas where flooding may not actually occur:

  1. The groundwater levels are produced from national scale mapping and models, which may not be representative at a local scale. The sparsity of reliable records of groundwater levels is an important limitation on national scale groundwater mapping and modelling.
  2. In some areas, only a coarse resolution DTM (50m) was available for use in the groundwater flood risk model, which can lead to poor resolution of shallow slopes, and the elevation of a site above an adjacent valley can be under-represented.
  3. Other constituent data-sets, including the geology datasets, are national-scale maps and may not represent local features accurately.
  4. Engineered works are not taken into account in the model. Similarly, artificial drainage works or groundwater pumping or control systems that would limit water table rise to the surface are not accounted for

Property Protection Factors

Some of the main reasons why property within areas at risk of flooding may avoid being flooded:

  1. National groundwater flooding models do not take into account the magnitude of flows emerging from the ground. Therefore while groundwater heads might be indicative of groundwater emergence, the actual amount of flow might not be sufficient to cause flooding at that location (although the accumulated flows downstream might be).
  2. Change in elevation locally may cause groundwater emergence to be localised away from the property, keeping the water table below hazardous levels at the property.
  3. Even if emergent groundwater was at a rate sufficient to cause local flooding, the nature of the urban man-made subsurface tends to drain water away before it reaches the surface. Sewers, granular fill around utilities and road sub-grade are all highly permeable formations that would be able to drain quite high groundwater flows away. This tends to move the groundwater flooding problem down the catchment.
  4. Drains on or near the property or other property protection such as break layers or membranes incorporated in the building may act to prevent water reaching locations where impacts would occur.

In summary, it is recommended that a more detailed risk assessment by a suitably qualified specialist should be undertaken for any sites that occur in mapped zones of groundwater flood risk where the impact of groundwater flooding would have significant adverse consequences.

Decisions such as whether to proceed with a property transaction should not be made on the basis of the map classification alone. Even in the event that groundwater flood risk is confirmed through site-specific assessment, potential risk mitigation measures can usually be identified which could enable the property transaction or development to proceed.

What is the update cycle?

The map is updated on a 6 month cycle to take advantage of newly released data as soon as it comes out.

How is the map validated?

The map has been through a rigorous internal QA process, and has been reviewed by external experts. At every update cycle, it is reviewed against a national database of groundwater flooding events to verify its validity.

My house flooded recently, but the map says it is at negligible risk of groundwater flooding.

Other sources of flooding should be considered in this case, which are not represented on the Groundwater Flood Risk Map. These include fluvial and tidal flooding, surface water flooding, and flooding produced by springs.

My property is in a fluvial flood plain, but also shows up as being at risk of groundwater flooding. What does this mean?

This suggests an important hydrological connection between the river and the groundwater in this area. Due to the groundwater contribution, flooding in this area may occur more frequently and for longer durations than would be expected from fluvial flooding alone.

What mechanisms of flooding are represented on the map?

The two most pervasive mechanisms of groundwater flooding are represented on the Groundwater Flood Risk Map. These are bedrock flooding and permeable superficial deposits flooding.

Bedrock Flooding: After extreme rainfall, groundwater levels, in places, rise to intercept the ground surface. Rises in groundwater level may also be superimposed upon above average groundwater levels in the aquifer prior to the rainfall. Water tables typically reach the surface first in (dry) river valleys, where the emerging water can drain away.

With increasing groundwater levels, the carrying capacity of the drainage channel is exceeded and a surface flood commences. This is also known as ‘clearwater’ flooding because of the relative clarity of groundwater compared to fluvial flood water.

Permeable Superficial Deposits Flooding: Where groundwater in permeable superficial deposits (PSD) is in good hydraulic contact with a river or the coast, flooding can occur during periods of high river stage or tide. This mechanism is particularly exacerbated when the PSD overlie low permeability strata.

If a depression is set back from the river, with a connection via PSD then this might be prone to groundwater flooding even if it is protected from overland fluvial flooding. In conditions of less extreme floods, groundwater flooding often occurs in flood plains due to high in-channel river levels, before the river overtops its bank, or after it has retreated back into its channel.

It is therefore often difficult to distinguish from river flooding. Effectively, the subsurface flow path results in more extensive, frequent, and prolonged inundation of flood plains that occur on permeable superficial deposits connected to rivers.

Other mechanisms of groundwater flooding that are not represented on the Groundwater Flood Risk Map are:

  • Groundwater flooding produced by spring flows that exceed normal conditions, and therefore overwhelm their drainage channels.
  • Groundwater flooding as a result of water table rebound. The effect of rising groundwater levels beneath some cities, mineral extraction areas, or around water supply boreholes due to reduced abstraction has not been modelled.