Case study:Kensworth Quarry Chalk Pit Restoration: Difference between revisions

From RESTORE
Jump to navigation Jump to search
(Created page with "{{Case study status |Approval status=Draft }} {{Location |Location=51.8656525, -0.5209689 |Kml file=Screenshot 2022-08-06 11.52.52.png }} {{Project overview |Project title=Ken...")
 
No edit summary
 
(16 intermediate revisions by one other user not shown)
Line 1: Line 1:
{{Case study status
{{Case study status
|Approval status=Draft
|Approval status=Approved
}}
}}
{{Location
{{Location
Line 7: Line 7:
}}
}}
{{Project overview
{{Project overview
|Project title=Kensworth Quarry Chalk Pit Restoration
|Status=Planned
|Status=Planned
|Themes=Environmental flows and water resources, Habitat and biodiversity
|Themes=Environmental flows and water resources, Habitat and biodiversity
Line 15: Line 14:
|Contact organisation=Ver Valley
|Contact organisation=Ver Valley
|Contact organisation url=Self Employed
|Contact organisation url=Self Employed
|Name of parent multi-site project=Kensworth Quarry Site Restoration
|Multi-site=Yes
|Multi-site=Yes
|Name of parent multi-site project=Kensworth Quarry Site Restoration
|Project picture=Kensworth Quarry 1 .jpg
|Picture description=Kensworth Quarry
|Project summary=Kensworth Quarry is the UK's largest chalk pit and is one of the largest in the world. It is located to the top of the Chilterns ridge close to the (now dry) head valleys of the River Ver which is is one of only 200 Chalk streams in the world.
 
The River Ver, like many other Chiltern chalk streams, has suffered from unsustainable water abstraction to support local development needs. Over the past decade the river has ceased to flow on the Chilterns dip slope above Redbourne and without hydro-support it is quite possible that the river will disappear above St Albans within the next couple of decades.
 
It is thought that River Ver has been flowing in this area since the Anglian Glacation 400,000 years ago and there may be a fantastic and unique opportunity to secure its future for a while longer.
 
Production from Kensworth Quarry is due to cease within the next decade after which it will be subject to a site restoration program. It is proposed that as part of the site restoration plan consideration be given to establishing a permanent perched reservoir as the focus of wetland nature reserve and 'Geopark' of international significance. The reservoir would also be used to provide head water support to the River Ver to revitalise the river and sustain flow throughout the year. In addition the perched reservoir could be used to as a pumped hydro energy storage facility to support the growing network of solar energy plants in the farmlands west of the Chilterns ridge.
|Monitoring surveys and results=The project is in the very early evaluation stage focusing on stakeholder outreach, regional planning advice and technical advice in hydro-engineering and pumped hydro storage assessment.
 
Preliminary work suggests a short pipe line connection from the perched reservoir to the source of the River Ver could provide 3000 litres per second of flow support to the river for up to 30 days.
|Lessons learn=There are no lessons learnt as yet.
 
We are keen to get insights from any similar projects targeting river flow restoration/support through perched reservoirs derived from upland mining operations.
|Project title=Kensworth Quarry Chalk Pit Restoration
}}
}}
{{Image gallery}}
{{Image gallery}}
Line 22: Line 37:
{{Toggle button}}
{{Toggle button}}
{{Toggle content start}}
{{Toggle content start}}
{{Case study subcatchment}}
{{Case study subcatchment
{{Site}}
|Subcatchment=River Ver, Chiltern Hills
}}
{{Site
|Name=Kensworth Quarry and upper Ver Valleys
|Heavily modified water body=No
|Protected species present=Yes
|Invasive species present=Yes
|Dominant hydrology=River bed now dry through much of the year above Redbourne
|Dominant substrate=Chalk
}}
{{Project background}}
{{Project background}}
{{Motivations}}
{{Motivations
|Specific mitigation=Hydropower for distressed chalk stream system
|Other motivation=Creating and internationally significant wetland reserve and Geopark.
}}
{{Measures}}
{{Measures}}
{{Hydromorphological quality elements header}}
{{Hydromorphological quality elements header}}

Latest revision as of 11:29, 4 October 2022

0.00
(0 votes)


To discuss or comment on this case study, please use the discussion page.


Location: 51° 51' 56.35" N, 0° 31' 15.49" W
Loading map...
Left click to look around in the map, and use the wheel of your mouse to zoom in and out.


Project overview

Edit project overview
Status Planned
Project web site
Themes Environmental flows and water resources, Habitat and biodiversity
Country England
Main contact forename Adam
Main contact surname Hillier
Main contact user ID
Contact organisation Ver Valley
Contact organisation web site http://Self%20Employed
Partner organisations
This is a parent project
encompassing the following
projects
Kensworth Quarry Chalk Pit Site Restoration
Kensworth Quarry

Project summary

Edit project overview to modify the project summary.


Kensworth Quarry is the UK's largest chalk pit and is one of the largest in the world. It is located to the top of the Chilterns ridge close to the (now dry) head valleys of the River Ver which is is one of only 200 Chalk streams in the world.

The River Ver, like many other Chiltern chalk streams, has suffered from unsustainable water abstraction to support local development needs. Over the past decade the river has ceased to flow on the Chilterns dip slope above Redbourne and without hydro-support it is quite possible that the river will disappear above St Albans within the next couple of decades.

It is thought that River Ver has been flowing in this area since the Anglian Glacation 400,000 years ago and there may be a fantastic and unique opportunity to secure its future for a while longer.

Production from Kensworth Quarry is due to cease within the next decade after which it will be subject to a site restoration program. It is proposed that as part of the site restoration plan consideration be given to establishing a permanent perched reservoir as the focus of wetland nature reserve and 'Geopark' of international significance. The reservoir would also be used to provide head water support to the River Ver to revitalise the river and sustain flow throughout the year. In addition the perched reservoir could be used to as a pumped hydro energy storage facility to support the growing network of solar energy plants in the farmlands west of the Chilterns ridge.

Monitoring surveys and results

Edit project overview to modify the Monitoring survey and results.


The project is in the very early evaluation stage focusing on stakeholder outreach, regional planning advice and technical advice in hydro-engineering and pumped hydro storage assessment.

Preliminary work suggests a short pipe line connection from the perched reservoir to the source of the River Ver could provide 3000 litres per second of flow support to the river for up to 30 days.

Lessons learnt

Edit project overview to modify the lessons learnt.


There are no lessons learnt as yet.

We are keen to get insights from any similar projects targeting river flow restoration/support through perched reservoirs derived from upland mining operations.


Image gallery


ShowHideAdditionalImage.png


Catchment and subcatchment

Subcatchment:River Ver, Chiltern Hills


Site

Name Kensworth Quarry and upper Ver Valleys
WFD water body codes
WFD (national) typology
WFD water body name
Pre-project morphology
Reference morphology
Desired post project morphology
Heavily modified water body No
National/international site designation
Local/regional site designations
Protected species present Yes
Invasive species present Yes
Species of interest
Dominant hydrology River bed now dry through much of the year above Redbourne
Dominant substrate Chalk
River corridor land use
Average bankfull channel width category
Average bankfull channel width (m)
Average bankfull channel depth category
Average bankfull channel depth (m)
Mean discharge category
Mean annual discharge (m3/s)
Average channel gradient category
Average channel gradient
Average unit stream power (W/m2)


Project background

Reach length directly affected (m)
Project started
Works started
Works completed
Project completed
Total cost category
Total cost (k€)
Benefit to cost ratio
Funding sources

Cost for project phases

Phase cost category cost exact (k€) Lead organisation Contact forename Contact surname
Investigation and design
Stakeholder engagement and communication
Works and works supervision
Post-project management and maintenance
Monitoring



Reasons for river restoration

Mitigation of a pressure Hydropower for distressed chalk stream system
Hydromorphology
Biology
Physico-chemical
Other reasons for the project Creating and internationally significant wetland reserve and Geopark.


Measures

Structural measures
Bank/bed modifications
Floodplain / River corridor
Planform / Channel pattern
Other
Non-structural measures
Management interventions
Social measures (incl. engagement)
Other


Monitoring

Hydromorphological quality elements

Element When monitored Type of monitoring Control site used Result
Before measures After measures Qualitative Quantitative

Biological quality elements

Element When monitored Type of monitoring Control site used Result
Before measures After measures Qualitative Quantitative

Physico-chemical quality elements

Element When monitored Type of monitoring Control site used Result
Before measures After measures Qualitative Quantitative

Any other monitoring, e.g. social, economic

Element When monitored Type of monitoring Control site used Result
Before measures After measures Qualitative Quantitative


Monitoring documents



Additional documents and videos


Additional links and references

Link Description

Supplementary Information

Edit Supplementary Information