Ground
Condition and Site Excavation
By
Dr. Heng Li [bshengli@polyu.edu.hk] Tel: 2766 5879
1.
Reference
R.
Chudley, Construction Technology, Longman
On
completion of this lecture, you should be able to:
list
the difference types of ground conditions; and
describe,
with illustration, the different types of methods used
to control ground water
3.
Introduction
There
are various processes for improving soil properties insitu either
temporarily or permanently. The
methods are fall into the following categories:
4.
Sources
of Ground Water
Ground
water in a pervious soil stratum may be replenished directly
from rain falling on the ground surface or be percolation
from run offs, streams or nearby rivers.
The
water pressures in pervious layers will usually change as a
result in variations in seasonal rainfall or rivers and sea
level in cases where there is direct connection between the
pervious stratum and these sources.
5.
Problems
caused by ground water
The
problems created when surface and ground water enter excavations
are:
-
Instability
of base of excavation
-
Reduction
in the angle of repose of the embankment
-
Settlement
of adjacent structures due to erosion of ground
-
Collapse
of temporary support to excavation
6.
Ground
water control
In some
cases, the ground water conditions found during site investigation
may change before or during site investigation. Such changes
may be due to the construction of basements nearby, natural
flooding or artificial causes, such as a burst water main.
The
methods of ground water control may be divided into three broad
groups:
-
pumping,
-
cut-off
walling, and
-
special
methods.
The
choice of method depends mainly on site conditions and on the
soil characteristics. These include:-
-
size
and location;
-
thickness
and type of soil strata;
-
magnitude
of water pressures in various strata;
-
proposed
permanent structure relative to soil strata;
-
length
of time for which the excavation must be open;
-
prevention
of damage to adjacent structures;
-
relationship
between the proposed dewatering method and the construction
sequence.
7.
Dewatering
Methods – Pumping
Pumping
systems utilize:
-
sumps
-
wells
-
well-points
7.1
Pumping from sumps
Widely
used in deep excavations for trench or basement. There are several
major problems:-
-
Soil
movement due to settlement
-
Ground
affected by water flow towards sump
-
Instability
at formation level in timbered excavations owing to upward
movement of water
The
general solution is to dig sump at corner of excavation below
formation level.
7.1.1
Open Sump
The
sump is usually formed away from the construction area in a
corner of the excavation. The water is led into the sump, either
by sloping the ground towards it or by using shallow garland
drains which feed into the sump. Pumping from open sumps is
limited to a maximum depth of about 8m.
7.1.2
Jetted Sump
In
this method, a hole is formed in the ground by jetting metal
tube. A disposable intake strainer connected to a disposable
flexible suction pipe is then lowered into the hole, and the
void filled with sand filter media. This suction pipe is connected
to a pump which pumps out the ground water.
7.2
Pumping from wells
For
depths 9m, use other methods. Use wells where wellpoints are
not suitable.
7.2.1
Tube Well
-
Sink
lined borehole, diameter 300 – 600 mm to depth required
(i.e. below impermeable stratum as a rule)
-
Place
smaller tube – ‘inner well lining’ – inside, having portion
perforated at level to be dewatered. Lower end acts as sump.
-
Use
plunger to ‘surge’ initial flow and wash out unwanted fines.
-
Connect
pump to lining operate – submersible type is used.
-
Disconnect
and withdraw both linings as annular space is filled, or
in stages, or on completion.
-
Depth
of well depends on depth of impermeable stratum. If far
below excavation formation level wells can be spaced well
apart to create draw-down curve just below formation level.
7.2.2
Horizontal Wells
Formation
level at or slightly within impermeable stratum where vertical
wells impracticable.
A.
Method 1:
-
Sink
vertical well outside excavation area to below proposed
formation level.
-
Make
horizontal borings in radial pattern from vertical well.
-
Results:
water drains from upper surface of impermeable stratum into
large well. Pump (submersible) operates there.
B.
Method 2:
-
Lay
80mm PVC suction pipe (perforated) up to 6m depth around
excavation area. Suction pipe is covered with nylon filter
sleeve which prevents particles of soil from entering
pipe (Laying is be special horizontal well-point placing
machine: it digs trench, lays pipe, backfills in one operation
at up to 160 m/hr).
-
Connect
suction pipe to pump (Length of pipe per pump depends
on soil conditions and pump capacity). Water flows to
drainage channel formed in laying pipe.
7.2.3
Pumping from Well Points
It
is used for non-cohesive soils, minimum grain size 0.1 mm. The
wellpoint consists of a slotted or perforated pipe which is
covered with a screen mesh. At the foot of this pipe is an orifice
which permits jetting of the pipe into the ground during installation.
A simple ball valve above the orifice prevents the entry of
soil particles through the orifice when water is sucked in during
the pumping operation.
The
construction steps in the wellpoint system are:
-
a
wellpoint is jetted into the ground;
-
the
annular void is filled with filter media;
-
the
wellpoints are connected to a header pipe by means of a
riser;
-
the
header pipe is connected to two suction pumps for pumping.
A.
Multi-Stage Wellpoint Installations
It consists
of the installation of wellpoints at two or more levels. It
is also be used in shallow well pumping systems.
B.
Shallow Well Systems
This
system can handle greater volume of water compared with Wellpoint
systems. The construction steps are:-
-
a
cased well is bored,
-
a
filter tube is placed in the borehole,
-
filter
media are placed in the annular void and the casing withdrawn,
-
the
filter if flushed and a suction pipe is lowered into the
filter tube,
-
the
suction pipe is connected to the header main, and
-
the
header main is connected to a self-priming pump.
C.
Deep Well System
The
method of forming a deep well is similar to that of a shallow
well, except that in a deep well, a submersible pump is
used to pump out the water.
In
vacuum wells, a vacuum artificially increases the water flow
towards the wells or wellpoints. All the pumping systems described
so far are effective only in gravels and sands. If more than
10% silt is present, it is necessary to increase the water
flow towards the wells.
Method:-
-
Jet
and sand in;
-
Seal
top 1m of hole with clay – vacuum is created in sand filter
around wellpoint;
-
Only
free water is removed;
-
Sudden
shock can cause pronounced disturbance;
-
Limitations
– 6m maximum lift. Over 5m use multi-stage wellpoints;
-
Preparatory
work – from platform for each tier of wellpoints around
excavation of platforms on which header pipe is situated.
E.
Electro-Osmosis
-
It
is used in cohesive soils, where vacuum pumping is ineffective.
It is because soil particles carry negative electrical
charge, attracting + positively charged (hydrogen) ends
of H2O water molecules.
-
Electro-osmosis
has been found to be most successful in uniform beds of
fine silts. However, the method can be very expensive
and is therefore not commonly used.
8.
Dewatering
– Water Exclusion Techniques
8.1
Freezing Methods
The
principle of ground freezing is to change the water in the soil
into a solid wall of ice. This wall of ice is completely impermeable.
Method:
Steel
freeze pipes are inserted into soil at approximately 1m centres
around site to be excavated. Pipes above ground level are insulated.Brine
is pumped through system at –15 to –25°C, using calcium chloride
or magnesium chloride cooled by refrigeration plant nearby –
usually trailer-mounted.
Applications:
-
Competitive
for depths of 7m+, becoming relatively cheaper for greater
depths.
-
Soil
moisture content of 8%+ is sufficient.
-
Deep
shafts, tunnels, large excavations.
Problems:
8.2
Compressed Air
This
method has been extensively used in the construction of the
MTR in Hong Kong. It is used in caisson sinking and tunnel driving
in waterlogged ground. Air pressure up to 350 KN/m2
is possible which allows working at depths up to 35m below water
table, using 1m3 of fresh air per person in working
chamber.
The
major disadvantage of using compressed air is the health risk
to workers working in such chambers.
8.3
Grouting Methods
It
is used where pumping is likely to be uneconomic – e.g. permeable
soils, or variable ground (especially harder rocks) where boring
of wells and wellpoints very costly. It is grouted by injecting
rock or soil through pipes or holes in ground, using fluids
which seal or reduce permeability of ground on setting.
The
major problem is the vulnerability of existing u/ground structures;
- cracks may be penetrated. The choice of media depends of soil
particle sizes or sizes of fissures in rock.
8.3.1
Cement Grouting
It
is suitable for very permeable coarse materials.
Method:
-
Holes
bored around excavation.
-
Cement
grout injected, starting thin and increasing viscosity by
reducing water-cement ratio – e.g. neat cement and water;
4 parts sand, 1 cement; or PFA 1, cement 1, water 2, by
wt.
-
Secondary
holes bored and injected mid-way between original holes
to ensure complete grouting.
8.3.2
Bentonite Grouting
Bentonite
adds very little strength to the soil. This system is used where
soil particles are too small for cement grouting, especially
alluvial soils beneath dam structures to create permanently
impermeable layer.
When
bentonite coagulates, it forms an impermeable gel. Bentonite
may also be mixed with Portland cement or soluble silicates
to form a permanent barrier.
8.3.3
Chemical Groutings
It
is used in sandy soils of medium to coarse grading. Liquids
are used which gel by reaction between base substance and hardener.
One
Shot Process
In
this process, two chemicals are mixed together prior to injection.
One chemical is the base and the other the hardener or catalyst.
When the two chemicals are mixed, a reaction takes place and
a gel or solid is formed. In this process, the gel time should
be sufficiently delayed to allow for the full penetration of
the chemicals before gelling occurs. The time may be accurately
controlled by varying the proportions of the two chemicals.
Two
Shot Process
In
this process, the first chemical, normally sodium silicate,
is injected into the ground. The second chemical, normally calcium
chloride, is then injected. An immediate reaction occurs resulting
in the formation of a tough, insoluble ‘silica gel’.
Chemical
grouting strengthens the soil and reduces its permeability.
Advantages
over other methods:
Stricter
control of gel time (e.g. seconds to many hours)
Fewer
holes to bore
Greater
penetration of grout
Greater
flexibility in grouting time
8.3.4
Resin Grouting
Resin
grouts have a low viscosity and are formed by adding a catalyst
or hardener to a base solution. It is used in sandy soils of
fine grading, and silts. The choice of materials depends on
the chemical content of ground water.
8.3.5
Bituminous Grouting
It
is used in fine sandy soils – e.g. cut-off walls beneath dams,
etc. where no strengthening is required. It is not suitable
for under-pinning.
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