SlideShare a Scribd company logo
Waye Cottage Water.
Stephen Crittenden
14/03/2008
1
The drilling of a borehole to provide an additional
Water Supply at Waye.
by
Stephen Crittenden BSc, MSc, PhD.
Independent Geological Consultant.
April - May 2004.
Introduction.
This document records the drilling of a borehole at Waye Cottage to ‘tap’ a
groundwater source in order to supplement the existing well supplied Domestic
Water, in the hamlet of Waye. It is stressed that the comments and discussion in this
document are made purely from surface observations by and from the best judgement
of Dr Stephen Crittenden, Independent Geological Consultant. For this study no
scientific measurements or tests have been performed to assess the underground water
situation at Waye. Such tests, measurements and procedures may be carried out in the
future. Accordingly the correctness or accuracy of the information and interpretation
herein cannot be warranted and under no circumstances should any such information
or interpretation be relied upon as the sole basis for any drilling or financial decision.
In no event will Dr Stephen Crittenden be liable for any damages including but not
limited to, indirect, special or consequential damages, resulting from the use of any
information or interpretation provided.
Prior to 2004 the three houses at Waye; Waye Cottage, Waye Farm and Lower Waye
Farm, were each supplied with domestic water by their own dug well /cistern. Each
well is in the order of 10metres deep (30 – 35 feet) and at some time in the past hand
dug. The three wells are approximately within 50 metres of each other. The two wells
supplying the medieval long houses of Waye Farm and Waye Cottage were dug
probably in the 14 / 15th
Centuries in fractured / jointed rotten granite to a depth of
about 10metres (30 - 35 feet). They are unlined and are about 1 metre square in cross
section. The well at Lower Waye Farm is topographically lower than the other two but
is also dug predominantly in granite. It is lined with dressed granite setts / bricks and
was probably dug some time in the 19th
century. Further investigation of this well may
reveal that it is dug partially in growan /alluvium above granite.
Simple Geology, Bedrock and Groundwater
The storage and circulation of ground water at Waye is very dependent on the local
geology. At Waye Cottage the bedrock is hard ‘blue’ Dartmoor Granite which is
overlain by a thin veneer of soil. In the Waye hamlet area there is in some places a
thin veneer of alluvium, which has been worked for tin some time in the past, and
‘growan’ – rotten decomposing granite. There are no Culm Measures or rocks of the
metamorphic aureole at Waye.
Granite is pervious due to the presence of interconnected open joints and fissures
(both macro and micro sized) through which water can flow.
At Waye the water migrates through the rock by the most permeable routes and
emerges by natural openings (to form springs and seeps), by the three artificial
openings (hand dug wells) and by direct feed into the small streams. The actual water
storage capacity of the granite beneath Waye Cottage is probably not high and is
Waye Cottage Water.
Stephen Crittenden
14/03/2008
2
controlled by the density and volume of the open fractures and joints for a given
volume of rock.
Below a certain level beneath the ground surface at Waye Cottage all porous,
permeable and fissured rocks are saturated with water (ie. groundwater). The upper
surface of the groundwater is termed the water table. The water table surface follows
in general the topography of the ground above; it is arched up beneath hills and curves
down beneath hollows and vales.
Beneath the ground surface three successive zones are recognized. These zones are
dynamic.
a) The uppermost zone is the Zone of Non-saturation.
b) The Zone of Intermittent Saturation extends from the highest level ever
reached by groundwater (after prolonged wet weather), the water table, down
to the lowest level to which the water table drops after drought. The three
wells at Waye are mostly in this zone and the upper part of the Zone of
Permanent Saturation.
c) The Zone of Permanent Saturation extends down to the limit beneath which
groundwater is never found.
The Borehole
It was decided to drill a borehole at Waye Cottage into the granite deep into the Zone
of Permanent Saturation. The hope was that a number of fresh and drinkable water
bearing fissures, fractures and joints would be intersected by the well bore thus
providing multiple sources of water influx into the well bore. If a deep (about
65metres) borehole were drilled then the chances of obtaining water were considered
to be good but….how much water and of what quality could not be determined.
The site of the borehole at Waye Cottage was decided by the available surface area
and a thorough site survey was deemed unnecessary although existing water rights
and contamination possibilities were considered. According to the Government
Department of the Environment it was not necessary to seek permissions for the site
and drilling of a borehole and for the eventual abstraction of water for domestic use.
Unfortunately at Waye Cottage there was not the possibility that a borehole could be
sited such to tap two sources of water; one from an overlying alluvial aquifer where
the water is possibly more mobile but thus prone to contamination, and one from the
granite aquifer beneath. There are no alluvial deposits in the curtilage of Waye
Cottage. The borehole was sited in front of the shippon adjacent to the original cross
passage entrance on the northern side of the Waye Cottage Longhouse. Saxton
Drilling Ltd was contracted to carry out the drilling of the borehole while Waterwise
Engineering was contracted to complete and ‘plumb-in’ the borehole to the existing
pipe system of Waye Cottage.
The 6 inch diameter borehole was drilled, using a tractor mounted compressed air and
rotary / percussion drill, to a depth of 226 feet (69m). A plastic slotted liner was
placed in the borehole together with an electric downhole submersible pump and
pipes to a large storage tank in the shippon. The water is passed through a UV light
system, a Ph correction unit and a chemical treatment system. A separate surface
pump transports the water to the house. The downhole pump is switched on
automatically when the level of water in the storage tank falls down to and below a
pre-set level.
Waye Cottage Water.
Stephen Crittenden
14/03/2008
3
Rate of Abstraction
The rate of abstraction of water for domestic use from the borehole at Waye Cottage
is regulated by a number of factors.
A. The water level in the borehole will fall if the “granite aquifer” is not able to
transmit the percolating water to the borehole at the rate with which water is
being withdrawn.
B. A localized cone of depression – draw down of the water table, may occur if
excessive rates of abstraction are used in a borehole even if it is penetrating
the Zone of Permanent Saturation.
C. The rate of abstraction of water through the borehole tapping the storage must
not exceed the rate at which the storage is being recharged by infiltration. If it
does it results in the lowering of the water table and emptying of the aquifer
that may have taken decades to fill. It may then take some years for the aquifer
to recharge and the water table to rise to its former level in the area.
D. It is never sensible to pump a borehole dry. Such a practice runs the risk of
permanently damaging the water transmission ability of the fractures and
fissures that ‘feed’ the borehole and indeed can adversely affect the water
table level for some considerable radial distance from the borehole. Water
travels by preferred routes in the fractured granite aquifer and routes can in
some instances become plugged /blocked such that a borehole may become
semi-bypassed.
A typical borehole in Granite in Devon usually flows less than 3 – 4 cubic meters
/day.
The Waye Cottage borehole ‘struck water’, probably at a number of fractures toward
the bottom half of the borehole as evidenced by a spectacular water and mud spout
shooting into the air – caused by the compressed air used for the drilling. Previous to
that the granite cuttings / flour brought to the surface by the compressed air was dry /
damp. Prior to the completion of the well the bore was pump tested in the following
manner. The downhole pump was lowered into the borehole which was left to
stabilize for a day and the final height of the water column measured at 6.3m (20.67ft)
from the surface. Pumping commenced and a final flow rate of 9.8 litres / min (2.15
gallons / min) was established that maintained the water height in the borehole. An
increase in the pump rate caused the level in the borehole to fall. The borehole was
then left for two days pumping at slightly below the 9.8 litres / min rate in order to
clean up the water and the borehole.
The daily rate of flow is equal to 14,112 litres / day (3,104.27 gallons / day) more than
sufficient to meet the domestic daily demands of Waye Cottage.
Water Quality
The quality of the water was measured by the South West Water Scientific Services
Exeter Laboratories between 13th
May and 25th
May 2004. The Manganese
(102micrograms per litre), Aluminium (440 micrograms per litre) and iron (2450
micrograms per litre) levels were above the maximum level standards set by the UK
Waye Cottage Water.
Stephen Crittenden
14/03/2008
4
Government for drinking water. This necessitated the installation of treatment
procedure equipment by Waterwise Engineering Ltd. The iron levels were by far the
biggest worry in terms of excess above the government maximum of 200 micrograms
per litre.
Borehole Water Supply Cost
Saxton Drilling drilled the borehole and supplied all drilling equipment, slotted liner
and personnel at an all in cost of £1000.00 (no VAT). The drilling took three days.
Waterwise Engineering Ltd costs were £2818 (excluding VAT).
Total Cost : £3818.00
VAT : £649.01
£4467.01
Photographs of the Job
The photographs show the setting up of the drilling equipment, including polythene
sheeting to protect the interior of the shippon; the tractor mounted drill, the pneumatic
compressor, the drill pipe and the cuttings pile, and the completed well head with the
liner in place and the down hole pump and cable all protected by an upturned bucket
prior to the final well completion.
Waye Cottage Water.
Stephen Crittenden
14/03/2008
5
Waye Cottage Water.
Stephen Crittenden
14/03/2008
6

More Related Content

What's hot

Tubewell guideline(1)
Tubewell  guideline(1)Tubewell  guideline(1)
Tubewell guideline(1)
Abdul Aziz
 
Artificial ground water recharge
Artificial ground water rechargeArtificial ground water recharge
Artificial ground water recharge
Ankit Saini
 
Unconventional measurers sde11
Unconventional measurers  sde11Unconventional measurers  sde11
Unconventional measurers sde11
vigyanashram
 
Artificial ground water recharge ppt
Artificial ground water recharge pptArtificial ground water recharge ppt
Artificial ground water recharge pptLaukush Kumar
 
Artificial recharge of groundwater
Artificial recharge of groundwaterArtificial recharge of groundwater
Artificial recharge of groundwater
Lakshmi K Suresh
 
Ground water recharge Methods
Ground water recharge MethodsGround water recharge Methods
Ground water recharge Methods
Prabhat Mishra
 
Lecture 8
Lecture 8Lecture 8
Water Resources Engineering types of wells with figures Denish Jangid Open we...
Water Resources Engineering types of wells with figures Denish Jangid Open we...Water Resources Engineering types of wells with figures Denish Jangid Open we...
Water Resources Engineering types of wells with figures Denish Jangid Open we...
Denish Jangid
 
Dams and their role in environment.
Dams and their role in environment.Dams and their role in environment.
Dams and their role in environment.
Navjot Singh Saini
 
Hard engineering
Hard engineeringHard engineering
Hard engineering
Nishay Patel
 
Presentation st sabya
Presentation st   sabyaPresentation st   sabya
Presentation st sabya
sabyaswain
 
Swe
SweSwe
Ground Water Recharge
Ground Water RechargeGround Water Recharge
Ground Water Recharge
Pravin Appa
 
GROUND WATER RECHARGE TECHNIQUES BY CH.APPARAO (Research Associate, ARS, ATP)
GROUND WATER RECHARGE TECHNIQUES BY CH.APPARAO (Research Associate, ARS, ATP)GROUND WATER RECHARGE TECHNIQUES BY CH.APPARAO (Research Associate, ARS, ATP)
GROUND WATER RECHARGE TECHNIQUES BY CH.APPARAO (Research Associate, ARS, ATP)
Apparao Chodisetti
 
IDE 354 ppt final
IDE 354 ppt finalIDE 354 ppt final
IDE 354 ppt final
Ganesh Kadam
 
Dams PPT
Dams PPTDams PPT
Dams PPT
Seminar Links
 
ESA 324 - Dams Project
ESA 324 - Dams ProjectESA 324 - Dams Project
ESA 324 - Dams Project
Patrick Devon
 
Hydraulics structures
Hydraulics  structuresHydraulics  structures
Hydraulics structures
ThanarajS
 
Krishna
KrishnaKrishna
Krishna
krishna sai
 

What's hot (20)

Tubewell guideline(1)
Tubewell  guideline(1)Tubewell  guideline(1)
Tubewell guideline(1)
 
Artificial ground water recharge
Artificial ground water rechargeArtificial ground water recharge
Artificial ground water recharge
 
Unconventional measurers sde11
Unconventional measurers  sde11Unconventional measurers  sde11
Unconventional measurers sde11
 
Artificial ground water recharge ppt
Artificial ground water recharge pptArtificial ground water recharge ppt
Artificial ground water recharge ppt
 
Artificial recharge of groundwater
Artificial recharge of groundwaterArtificial recharge of groundwater
Artificial recharge of groundwater
 
Ground water recharge Methods
Ground water recharge MethodsGround water recharge Methods
Ground water recharge Methods
 
Lecture 8
Lecture 8Lecture 8
Lecture 8
 
Water Resources Engineering types of wells with figures Denish Jangid Open we...
Water Resources Engineering types of wells with figures Denish Jangid Open we...Water Resources Engineering types of wells with figures Denish Jangid Open we...
Water Resources Engineering types of wells with figures Denish Jangid Open we...
 
Dams and their role in environment.
Dams and their role in environment.Dams and their role in environment.
Dams and their role in environment.
 
Hard engineering
Hard engineeringHard engineering
Hard engineering
 
Presentation st sabya
Presentation st   sabyaPresentation st   sabya
Presentation st sabya
 
Swe
SweSwe
Swe
 
Ground Water Recharge
Ground Water RechargeGround Water Recharge
Ground Water Recharge
 
Dams
DamsDams
Dams
 
GROUND WATER RECHARGE TECHNIQUES BY CH.APPARAO (Research Associate, ARS, ATP)
GROUND WATER RECHARGE TECHNIQUES BY CH.APPARAO (Research Associate, ARS, ATP)GROUND WATER RECHARGE TECHNIQUES BY CH.APPARAO (Research Associate, ARS, ATP)
GROUND WATER RECHARGE TECHNIQUES BY CH.APPARAO (Research Associate, ARS, ATP)
 
IDE 354 ppt final
IDE 354 ppt finalIDE 354 ppt final
IDE 354 ppt final
 
Dams PPT
Dams PPTDams PPT
Dams PPT
 
ESA 324 - Dams Project
ESA 324 - Dams ProjectESA 324 - Dams Project
ESA 324 - Dams Project
 
Hydraulics structures
Hydraulics  structuresHydraulics  structures
Hydraulics structures
 
Krishna
KrishnaKrishna
Krishna
 

Similar to borehole_waye

Chapter 4 groundwater hydrology
Chapter 4 groundwater hydrologyChapter 4 groundwater hydrology
Chapter 4 groundwater hydrologyMohammed Salahat
 
Chapter4groundwaterhydrology 130630055824-phpapp02
Chapter4groundwaterhydrology 130630055824-phpapp02Chapter4groundwaterhydrology 130630055824-phpapp02
Chapter4groundwaterhydrology 130630055824-phpapp02
Cleophas Rwemera
 
dokumen.tips_lecture-hydrogeology.pdf
dokumen.tips_lecture-hydrogeology.pdfdokumen.tips_lecture-hydrogeology.pdf
dokumen.tips_lecture-hydrogeology.pdf
DamilareDanielOlaniy
 
Canal design
Canal designCanal design
Canal design
brijlata sharma
 
Salinity Prevention
Salinity PreventionSalinity Prevention
Salinity Prevention
Bhavik A Shah
 
Lecture 11. groundwater hydrology
Lecture 11. groundwater hydrologyLecture 11. groundwater hydrology
Lecture 11. groundwater hydrologyDana Acap
 
Ground water
Ground waterGround water
Ground water
Swapna Chinnabathuni
 
Water resources
Water resourcesWater resources
Water resources
KHUSHBU SHAH
 
G3 ppt
G3 pptG3 ppt
subsurface investigation of ground water
subsurface investigation of ground watersubsurface investigation of ground water
subsurface investigation of ground water
MalimaluMalimaluVeer
 
Ground water resources and problems
Ground water resources  and  problems Ground water resources  and  problems
Ground water resources and problems
Jahangir Alam
 
Sea water intrusion
Sea water intrusion Sea water intrusion
Sea water intrusion
Prashant Katti
 
Document from Ishani.pptx
Document from Ishani.pptxDocument from Ishani.pptx
Document from Ishani.pptx
IshaniNagina
 
Groundwater improvement techniques
Groundwater improvement techniques Groundwater improvement techniques
Groundwater improvement techniques
my-will
 
GROUND WATER IMPROVEMENT TECHNIQUES
GROUND WATER IMPROVEMENT TECHNIQUESGROUND WATER IMPROVEMENT TECHNIQUES
GROUND WATER IMPROVEMENT TECHNIQUES
Ashim ghosh
 
12-3-2021 Construction of Tube well by Mr.Mr.Qaisar.pptx
12-3-2021  Construction of Tube well by Mr.Mr.Qaisar.pptx12-3-2021  Construction of Tube well by Mr.Mr.Qaisar.pptx
12-3-2021 Construction of Tube well by Mr.Mr.Qaisar.pptx
AliRaza72786
 
CH7.1.pptx: ground water hydrolog of ethiy
CH7.1.pptx: ground water hydrolog of ethiyCH7.1.pptx: ground water hydrolog of ethiy
CH7.1.pptx: ground water hydrolog of ethiy
mulugeta48
 
Water resarch and ground water
Water resarch and ground waterWater resarch and ground water
Water resarch and ground water
vivek gami
 
chapter 2.pptx
chapter 2.pptxchapter 2.pptx
chapter 2.pptx
abdi977630
 
Underground water
Underground  waterUnderground  water
Underground water
ahmed wassel
 

Similar to borehole_waye (20)

Chapter 4 groundwater hydrology
Chapter 4 groundwater hydrologyChapter 4 groundwater hydrology
Chapter 4 groundwater hydrology
 
Chapter4groundwaterhydrology 130630055824-phpapp02
Chapter4groundwaterhydrology 130630055824-phpapp02Chapter4groundwaterhydrology 130630055824-phpapp02
Chapter4groundwaterhydrology 130630055824-phpapp02
 
dokumen.tips_lecture-hydrogeology.pdf
dokumen.tips_lecture-hydrogeology.pdfdokumen.tips_lecture-hydrogeology.pdf
dokumen.tips_lecture-hydrogeology.pdf
 
Canal design
Canal designCanal design
Canal design
 
Salinity Prevention
Salinity PreventionSalinity Prevention
Salinity Prevention
 
Lecture 11. groundwater hydrology
Lecture 11. groundwater hydrologyLecture 11. groundwater hydrology
Lecture 11. groundwater hydrology
 
Ground water
Ground waterGround water
Ground water
 
Water resources
Water resourcesWater resources
Water resources
 
G3 ppt
G3 pptG3 ppt
G3 ppt
 
subsurface investigation of ground water
subsurface investigation of ground watersubsurface investigation of ground water
subsurface investigation of ground water
 
Ground water resources and problems
Ground water resources  and  problems Ground water resources  and  problems
Ground water resources and problems
 
Sea water intrusion
Sea water intrusion Sea water intrusion
Sea water intrusion
 
Document from Ishani.pptx
Document from Ishani.pptxDocument from Ishani.pptx
Document from Ishani.pptx
 
Groundwater improvement techniques
Groundwater improvement techniques Groundwater improvement techniques
Groundwater improvement techniques
 
GROUND WATER IMPROVEMENT TECHNIQUES
GROUND WATER IMPROVEMENT TECHNIQUESGROUND WATER IMPROVEMENT TECHNIQUES
GROUND WATER IMPROVEMENT TECHNIQUES
 
12-3-2021 Construction of Tube well by Mr.Mr.Qaisar.pptx
12-3-2021  Construction of Tube well by Mr.Mr.Qaisar.pptx12-3-2021  Construction of Tube well by Mr.Mr.Qaisar.pptx
12-3-2021 Construction of Tube well by Mr.Mr.Qaisar.pptx
 
CH7.1.pptx: ground water hydrolog of ethiy
CH7.1.pptx: ground water hydrolog of ethiyCH7.1.pptx: ground water hydrolog of ethiy
CH7.1.pptx: ground water hydrolog of ethiy
 
Water resarch and ground water
Water resarch and ground waterWater resarch and ground water
Water resarch and ground water
 
chapter 2.pptx
chapter 2.pptxchapter 2.pptx
chapter 2.pptx
 
Underground water
Underground  waterUnderground  water
Underground water
 

More from Stephen Crittenden

Newsletter on Stratigraphy volume 15_number_3_p163-171_Planktonic_foraminifer...
Newsletter on Stratigraphy volume 15_number_3_p163-171_Planktonic_foraminifer...Newsletter on Stratigraphy volume 15_number_3_p163-171_Planktonic_foraminifer...
Newsletter on Stratigraphy volume 15_number_3_p163-171_Planktonic_foraminifer...
Stephen Crittenden
 
Goban Spur Presentation: the Early Cretaceous (Barremian -?Aptian) foraminife...
Goban Spur Presentation: the Early Cretaceous (Barremian -?Aptian) foraminife...Goban Spur Presentation: the Early Cretaceous (Barremian -?Aptian) foraminife...
Goban Spur Presentation: the Early Cretaceous (Barremian -?Aptian) foraminife...
Stephen Crittenden
 
Norlex Cretaceous north sea
Norlex Cretaceous north seaNorlex Cretaceous north sea
Norlex Cretaceous north sea
Stephen Crittenden
 
The discovery of oil in kuwait
The discovery of oil in kuwaitThe discovery of oil in kuwait
The discovery of oil in kuwait
Stephen Crittenden
 
Enjefa beach kuwait for linkedin 2
Enjefa beach kuwait for linkedin 2Enjefa beach kuwait for linkedin 2
Enjefa beach kuwait for linkedin 2
Stephen Crittenden
 
Stephen Crittenden: Lower Tertiary lithostratigraphy North Sea.
Stephen Crittenden: Lower Tertiary lithostratigraphy North Sea.Stephen Crittenden: Lower Tertiary lithostratigraphy North Sea.
Stephen Crittenden: Lower Tertiary lithostratigraphy North Sea.
Stephen Crittenden
 
The foraminiferid Osangularia schloenbachi (Reuss) the erection of a neotype....
The foraminiferid Osangularia schloenbachi (Reuss) the erection of a neotype....The foraminiferid Osangularia schloenbachi (Reuss) the erection of a neotype....
The foraminiferid Osangularia schloenbachi (Reuss) the erection of a neotype....
Stephen Crittenden
 
Aptian lithostratigraphy and biostratigraphy of block 49 southrn North Sea (U...
Aptian lithostratigraphy and biostratigraphy of block 49 southrn North Sea (U...Aptian lithostratigraphy and biostratigraphy of block 49 southrn North Sea (U...
Aptian lithostratigraphy and biostratigraphy of block 49 southrn North Sea (U...
Stephen Crittenden
 
Crittenden 1984-jm3-1-1[1] A note on the Early Cretaceous biostratigraphy (f...
Crittenden 1984-jm3-1-1[1] A note on the Early Cretaceous  biostratigraphy (f...Crittenden 1984-jm3-1-1[1] A note on the Early Cretaceous  biostratigraphy (f...
Crittenden 1984-jm3-1-1[1] A note on the Early Cretaceous biostratigraphy (f...
Stephen Crittenden
 
Ab1999 abstr
Ab1999 abstrAb1999 abstr
Ab1999 abstr
Stephen Crittenden
 
Journal Micropalaeontology:Crittenden 1982-jm1-1-23[1]. Rotalline foraminifer...
Journal Micropalaeontology:Crittenden 1982-jm1-1-23[1]. Rotalline foraminifer...Journal Micropalaeontology:Crittenden 1982-jm1-1-23[1]. Rotalline foraminifer...
Journal Micropalaeontology:Crittenden 1982-jm1-1-23[1]. Rotalline foraminifer...
Stephen Crittenden
 
The whereabouts of the foraminifera described by Chapman 1894, from the Aptia...
The whereabouts of the foraminifera described by Chapman 1894, from the Aptia...The whereabouts of the foraminifera described by Chapman 1894, from the Aptia...
The whereabouts of the foraminifera described by Chapman 1894, from the Aptia...
Stephen Crittenden
 
North sea marl våle – maureen nomenclature linkedin version
North sea marl   våle – maureen nomenclature linkedin versionNorth sea marl   våle – maureen nomenclature linkedin version
North sea marl våle – maureen nomenclature linkedin version
Stephen Crittenden
 
Cret seq strat_mid_Norway_London_Sept_2002 Charnock and Crittenden
Cret seq strat_mid_Norway_London_Sept_2002 Charnock and CrittendenCret seq strat_mid_Norway_London_Sept_2002 Charnock and Crittenden
Cret seq strat_mid_Norway_London_Sept_2002 Charnock and Crittenden
Stephen Crittenden
 
Upper Cretaceous sequence stratigraphy mid Norway_Oct 2003 Crittenden & Charnock
Upper Cretaceous sequence stratigraphy mid Norway_Oct 2003 Crittenden & CharnockUpper Cretaceous sequence stratigraphy mid Norway_Oct 2003 Crittenden & Charnock
Upper Cretaceous sequence stratigraphy mid Norway_Oct 2003 Crittenden & Charnock
Stephen Crittenden
 
Lwr Cretaceous Sequence stratigraphy mid Norway_Oct 2003
Lwr Cretaceous Sequence stratigraphy mid Norway_Oct  2003Lwr Cretaceous Sequence stratigraphy mid Norway_Oct  2003
Lwr Cretaceous Sequence stratigraphy mid Norway_Oct 2003
Stephen Crittenden
 
Stratigraphical calibration of deep water Cretaceous sequences, offshore mid ...
Stratigraphical calibration of deep water Cretaceous sequences, offshore mid ...Stratigraphical calibration of deep water Cretaceous sequences, offshore mid ...
Stratigraphical calibration of deep water Cretaceous sequences, offshore mid ...
Stephen Crittenden
 
Barents source rock_Arctic_Geology Conference abstract_May_2004_Tromso
Barents source rock_Arctic_Geology  Conference abstract_May_2004_TromsoBarents source rock_Arctic_Geology  Conference abstract_May_2004_Tromso
Barents source rock_Arctic_Geology Conference abstract_May_2004_Tromso
Stephen Crittenden
 
pp395 414 Journal Petroleum Geology10 1987 The Albian transgression in the so...
pp395 414 Journal Petroleum Geology10 1987 The Albian transgression in the so...pp395 414 Journal Petroleum Geology10 1987 The Albian transgression in the so...
pp395 414 Journal Petroleum Geology10 1987 The Albian transgression in the so...
Stephen Crittenden
 
pp387 416 Journ Petroleum Geology 14 1991 lithostrat cns. Crittenden (sen aut...
pp387 416 Journ Petroleum Geology 14 1991 lithostrat cns. Crittenden (sen aut...pp387 416 Journ Petroleum Geology 14 1991 lithostrat cns. Crittenden (sen aut...
pp387 416 Journ Petroleum Geology 14 1991 lithostrat cns. Crittenden (sen aut...
Stephen Crittenden
 

More from Stephen Crittenden (20)

Newsletter on Stratigraphy volume 15_number_3_p163-171_Planktonic_foraminifer...
Newsletter on Stratigraphy volume 15_number_3_p163-171_Planktonic_foraminifer...Newsletter on Stratigraphy volume 15_number_3_p163-171_Planktonic_foraminifer...
Newsletter on Stratigraphy volume 15_number_3_p163-171_Planktonic_foraminifer...
 
Goban Spur Presentation: the Early Cretaceous (Barremian -?Aptian) foraminife...
Goban Spur Presentation: the Early Cretaceous (Barremian -?Aptian) foraminife...Goban Spur Presentation: the Early Cretaceous (Barremian -?Aptian) foraminife...
Goban Spur Presentation: the Early Cretaceous (Barremian -?Aptian) foraminife...
 
Norlex Cretaceous north sea
Norlex Cretaceous north seaNorlex Cretaceous north sea
Norlex Cretaceous north sea
 
The discovery of oil in kuwait
The discovery of oil in kuwaitThe discovery of oil in kuwait
The discovery of oil in kuwait
 
Enjefa beach kuwait for linkedin 2
Enjefa beach kuwait for linkedin 2Enjefa beach kuwait for linkedin 2
Enjefa beach kuwait for linkedin 2
 
Stephen Crittenden: Lower Tertiary lithostratigraphy North Sea.
Stephen Crittenden: Lower Tertiary lithostratigraphy North Sea.Stephen Crittenden: Lower Tertiary lithostratigraphy North Sea.
Stephen Crittenden: Lower Tertiary lithostratigraphy North Sea.
 
The foraminiferid Osangularia schloenbachi (Reuss) the erection of a neotype....
The foraminiferid Osangularia schloenbachi (Reuss) the erection of a neotype....The foraminiferid Osangularia schloenbachi (Reuss) the erection of a neotype....
The foraminiferid Osangularia schloenbachi (Reuss) the erection of a neotype....
 
Aptian lithostratigraphy and biostratigraphy of block 49 southrn North Sea (U...
Aptian lithostratigraphy and biostratigraphy of block 49 southrn North Sea (U...Aptian lithostratigraphy and biostratigraphy of block 49 southrn North Sea (U...
Aptian lithostratigraphy and biostratigraphy of block 49 southrn North Sea (U...
 
Crittenden 1984-jm3-1-1[1] A note on the Early Cretaceous biostratigraphy (f...
Crittenden 1984-jm3-1-1[1] A note on the Early Cretaceous  biostratigraphy (f...Crittenden 1984-jm3-1-1[1] A note on the Early Cretaceous  biostratigraphy (f...
Crittenden 1984-jm3-1-1[1] A note on the Early Cretaceous biostratigraphy (f...
 
Ab1999 abstr
Ab1999 abstrAb1999 abstr
Ab1999 abstr
 
Journal Micropalaeontology:Crittenden 1982-jm1-1-23[1]. Rotalline foraminifer...
Journal Micropalaeontology:Crittenden 1982-jm1-1-23[1]. Rotalline foraminifer...Journal Micropalaeontology:Crittenden 1982-jm1-1-23[1]. Rotalline foraminifer...
Journal Micropalaeontology:Crittenden 1982-jm1-1-23[1]. Rotalline foraminifer...
 
The whereabouts of the foraminifera described by Chapman 1894, from the Aptia...
The whereabouts of the foraminifera described by Chapman 1894, from the Aptia...The whereabouts of the foraminifera described by Chapman 1894, from the Aptia...
The whereabouts of the foraminifera described by Chapman 1894, from the Aptia...
 
North sea marl våle – maureen nomenclature linkedin version
North sea marl   våle – maureen nomenclature linkedin versionNorth sea marl   våle – maureen nomenclature linkedin version
North sea marl våle – maureen nomenclature linkedin version
 
Cret seq strat_mid_Norway_London_Sept_2002 Charnock and Crittenden
Cret seq strat_mid_Norway_London_Sept_2002 Charnock and CrittendenCret seq strat_mid_Norway_London_Sept_2002 Charnock and Crittenden
Cret seq strat_mid_Norway_London_Sept_2002 Charnock and Crittenden
 
Upper Cretaceous sequence stratigraphy mid Norway_Oct 2003 Crittenden & Charnock
Upper Cretaceous sequence stratigraphy mid Norway_Oct 2003 Crittenden & CharnockUpper Cretaceous sequence stratigraphy mid Norway_Oct 2003 Crittenden & Charnock
Upper Cretaceous sequence stratigraphy mid Norway_Oct 2003 Crittenden & Charnock
 
Lwr Cretaceous Sequence stratigraphy mid Norway_Oct 2003
Lwr Cretaceous Sequence stratigraphy mid Norway_Oct  2003Lwr Cretaceous Sequence stratigraphy mid Norway_Oct  2003
Lwr Cretaceous Sequence stratigraphy mid Norway_Oct 2003
 
Stratigraphical calibration of deep water Cretaceous sequences, offshore mid ...
Stratigraphical calibration of deep water Cretaceous sequences, offshore mid ...Stratigraphical calibration of deep water Cretaceous sequences, offshore mid ...
Stratigraphical calibration of deep water Cretaceous sequences, offshore mid ...
 
Barents source rock_Arctic_Geology Conference abstract_May_2004_Tromso
Barents source rock_Arctic_Geology  Conference abstract_May_2004_TromsoBarents source rock_Arctic_Geology  Conference abstract_May_2004_Tromso
Barents source rock_Arctic_Geology Conference abstract_May_2004_Tromso
 
pp395 414 Journal Petroleum Geology10 1987 The Albian transgression in the so...
pp395 414 Journal Petroleum Geology10 1987 The Albian transgression in the so...pp395 414 Journal Petroleum Geology10 1987 The Albian transgression in the so...
pp395 414 Journal Petroleum Geology10 1987 The Albian transgression in the so...
 
pp387 416 Journ Petroleum Geology 14 1991 lithostrat cns. Crittenden (sen aut...
pp387 416 Journ Petroleum Geology 14 1991 lithostrat cns. Crittenden (sen aut...pp387 416 Journ Petroleum Geology 14 1991 lithostrat cns. Crittenden (sen aut...
pp387 416 Journ Petroleum Geology 14 1991 lithostrat cns. Crittenden (sen aut...
 

borehole_waye

  • 1. Waye Cottage Water. Stephen Crittenden 14/03/2008 1 The drilling of a borehole to provide an additional Water Supply at Waye. by Stephen Crittenden BSc, MSc, PhD. Independent Geological Consultant. April - May 2004. Introduction. This document records the drilling of a borehole at Waye Cottage to ‘tap’ a groundwater source in order to supplement the existing well supplied Domestic Water, in the hamlet of Waye. It is stressed that the comments and discussion in this document are made purely from surface observations by and from the best judgement of Dr Stephen Crittenden, Independent Geological Consultant. For this study no scientific measurements or tests have been performed to assess the underground water situation at Waye. Such tests, measurements and procedures may be carried out in the future. Accordingly the correctness or accuracy of the information and interpretation herein cannot be warranted and under no circumstances should any such information or interpretation be relied upon as the sole basis for any drilling or financial decision. In no event will Dr Stephen Crittenden be liable for any damages including but not limited to, indirect, special or consequential damages, resulting from the use of any information or interpretation provided. Prior to 2004 the three houses at Waye; Waye Cottage, Waye Farm and Lower Waye Farm, were each supplied with domestic water by their own dug well /cistern. Each well is in the order of 10metres deep (30 – 35 feet) and at some time in the past hand dug. The three wells are approximately within 50 metres of each other. The two wells supplying the medieval long houses of Waye Farm and Waye Cottage were dug probably in the 14 / 15th Centuries in fractured / jointed rotten granite to a depth of about 10metres (30 - 35 feet). They are unlined and are about 1 metre square in cross section. The well at Lower Waye Farm is topographically lower than the other two but is also dug predominantly in granite. It is lined with dressed granite setts / bricks and was probably dug some time in the 19th century. Further investigation of this well may reveal that it is dug partially in growan /alluvium above granite. Simple Geology, Bedrock and Groundwater The storage and circulation of ground water at Waye is very dependent on the local geology. At Waye Cottage the bedrock is hard ‘blue’ Dartmoor Granite which is overlain by a thin veneer of soil. In the Waye hamlet area there is in some places a thin veneer of alluvium, which has been worked for tin some time in the past, and ‘growan’ – rotten decomposing granite. There are no Culm Measures or rocks of the metamorphic aureole at Waye. Granite is pervious due to the presence of interconnected open joints and fissures (both macro and micro sized) through which water can flow. At Waye the water migrates through the rock by the most permeable routes and emerges by natural openings (to form springs and seeps), by the three artificial openings (hand dug wells) and by direct feed into the small streams. The actual water storage capacity of the granite beneath Waye Cottage is probably not high and is
  • 2. Waye Cottage Water. Stephen Crittenden 14/03/2008 2 controlled by the density and volume of the open fractures and joints for a given volume of rock. Below a certain level beneath the ground surface at Waye Cottage all porous, permeable and fissured rocks are saturated with water (ie. groundwater). The upper surface of the groundwater is termed the water table. The water table surface follows in general the topography of the ground above; it is arched up beneath hills and curves down beneath hollows and vales. Beneath the ground surface three successive zones are recognized. These zones are dynamic. a) The uppermost zone is the Zone of Non-saturation. b) The Zone of Intermittent Saturation extends from the highest level ever reached by groundwater (after prolonged wet weather), the water table, down to the lowest level to which the water table drops after drought. The three wells at Waye are mostly in this zone and the upper part of the Zone of Permanent Saturation. c) The Zone of Permanent Saturation extends down to the limit beneath which groundwater is never found. The Borehole It was decided to drill a borehole at Waye Cottage into the granite deep into the Zone of Permanent Saturation. The hope was that a number of fresh and drinkable water bearing fissures, fractures and joints would be intersected by the well bore thus providing multiple sources of water influx into the well bore. If a deep (about 65metres) borehole were drilled then the chances of obtaining water were considered to be good but….how much water and of what quality could not be determined. The site of the borehole at Waye Cottage was decided by the available surface area and a thorough site survey was deemed unnecessary although existing water rights and contamination possibilities were considered. According to the Government Department of the Environment it was not necessary to seek permissions for the site and drilling of a borehole and for the eventual abstraction of water for domestic use. Unfortunately at Waye Cottage there was not the possibility that a borehole could be sited such to tap two sources of water; one from an overlying alluvial aquifer where the water is possibly more mobile but thus prone to contamination, and one from the granite aquifer beneath. There are no alluvial deposits in the curtilage of Waye Cottage. The borehole was sited in front of the shippon adjacent to the original cross passage entrance on the northern side of the Waye Cottage Longhouse. Saxton Drilling Ltd was contracted to carry out the drilling of the borehole while Waterwise Engineering was contracted to complete and ‘plumb-in’ the borehole to the existing pipe system of Waye Cottage. The 6 inch diameter borehole was drilled, using a tractor mounted compressed air and rotary / percussion drill, to a depth of 226 feet (69m). A plastic slotted liner was placed in the borehole together with an electric downhole submersible pump and pipes to a large storage tank in the shippon. The water is passed through a UV light system, a Ph correction unit and a chemical treatment system. A separate surface pump transports the water to the house. The downhole pump is switched on automatically when the level of water in the storage tank falls down to and below a pre-set level.
  • 3. Waye Cottage Water. Stephen Crittenden 14/03/2008 3 Rate of Abstraction The rate of abstraction of water for domestic use from the borehole at Waye Cottage is regulated by a number of factors. A. The water level in the borehole will fall if the “granite aquifer” is not able to transmit the percolating water to the borehole at the rate with which water is being withdrawn. B. A localized cone of depression – draw down of the water table, may occur if excessive rates of abstraction are used in a borehole even if it is penetrating the Zone of Permanent Saturation. C. The rate of abstraction of water through the borehole tapping the storage must not exceed the rate at which the storage is being recharged by infiltration. If it does it results in the lowering of the water table and emptying of the aquifer that may have taken decades to fill. It may then take some years for the aquifer to recharge and the water table to rise to its former level in the area. D. It is never sensible to pump a borehole dry. Such a practice runs the risk of permanently damaging the water transmission ability of the fractures and fissures that ‘feed’ the borehole and indeed can adversely affect the water table level for some considerable radial distance from the borehole. Water travels by preferred routes in the fractured granite aquifer and routes can in some instances become plugged /blocked such that a borehole may become semi-bypassed. A typical borehole in Granite in Devon usually flows less than 3 – 4 cubic meters /day. The Waye Cottage borehole ‘struck water’, probably at a number of fractures toward the bottom half of the borehole as evidenced by a spectacular water and mud spout shooting into the air – caused by the compressed air used for the drilling. Previous to that the granite cuttings / flour brought to the surface by the compressed air was dry / damp. Prior to the completion of the well the bore was pump tested in the following manner. The downhole pump was lowered into the borehole which was left to stabilize for a day and the final height of the water column measured at 6.3m (20.67ft) from the surface. Pumping commenced and a final flow rate of 9.8 litres / min (2.15 gallons / min) was established that maintained the water height in the borehole. An increase in the pump rate caused the level in the borehole to fall. The borehole was then left for two days pumping at slightly below the 9.8 litres / min rate in order to clean up the water and the borehole. The daily rate of flow is equal to 14,112 litres / day (3,104.27 gallons / day) more than sufficient to meet the domestic daily demands of Waye Cottage. Water Quality The quality of the water was measured by the South West Water Scientific Services Exeter Laboratories between 13th May and 25th May 2004. The Manganese (102micrograms per litre), Aluminium (440 micrograms per litre) and iron (2450 micrograms per litre) levels were above the maximum level standards set by the UK
  • 4. Waye Cottage Water. Stephen Crittenden 14/03/2008 4 Government for drinking water. This necessitated the installation of treatment procedure equipment by Waterwise Engineering Ltd. The iron levels were by far the biggest worry in terms of excess above the government maximum of 200 micrograms per litre. Borehole Water Supply Cost Saxton Drilling drilled the borehole and supplied all drilling equipment, slotted liner and personnel at an all in cost of £1000.00 (no VAT). The drilling took three days. Waterwise Engineering Ltd costs were £2818 (excluding VAT). Total Cost : £3818.00 VAT : £649.01 £4467.01 Photographs of the Job The photographs show the setting up of the drilling equipment, including polythene sheeting to protect the interior of the shippon; the tractor mounted drill, the pneumatic compressor, the drill pipe and the cuttings pile, and the completed well head with the liner in place and the down hole pump and cable all protected by an upturned bucket prior to the final well completion.
  • 5. Waye Cottage Water. Stephen Crittenden 14/03/2008 5
  • 6. Waye Cottage Water. Stephen Crittenden 14/03/2008 6