Building with Earth: Design and Technology of a Sustainable Architecture

(Nancy Kaufman) #1
Shrinkage limit
The shrinkage limit (SL) is defined as the
boundary between the semi-solid and solid
states. It is the limit where shrinkage ceases
to occur. With clayey soil, it can be identified
optically when the dark colour of the humid
mixture turns a lighter shade due to evapo-
ration of water in the pores. Still, this is not
an exact method of measurement.

Capillary action

Water movement
All materials with open porous structures
like loam are able to store and transport
water within their capillaries. The water,
therefore, always travels from regions of
higher humidity to regions of lower humidi-
ty. The capacity of water to respond to suc-
tion in this way is termed “capillarity” and
the process of water transportation “capil-
lary action.”
The quantity of water (W) that can be
absorbed over a given period of time is
defined by the formula:

W = w √t [kg/m^2 ]

where w is the water absorption coefficient
measured in kg/m^2 h0.5and t, the time in
hours.

Determination of the water absorption
coefficient
According to the German standard DIN
52617, the water absorption coefficient (w)
is obtained in the following way: a sample
cube of loam is placed on a plane surface
and immersed in water to a depth of about
3 mm, and its weight increase measured
periodically. The coefficient (w) is then calcu-
lated by the formula:

w = [kg/m^2 h0.5]

where W is the increase in weight per unit
surface area and t the time in hours elapsed.
With this test, all four sides of the cube
should be sealed so that no water enters
from these surfaces, and only the bottom

surface is operative.
With loam samples, problems are caused by
areas that swell and erode underwater over
time. The BRL developed a special method
to avoid this: to prevent the penetration of
water from the sides as well as the swelling
and deformation of the cube, samples are
covered on all four sides by a glass-fibre
reinforced polyester resin. To avoid the ero-
sion of particles from the submerged sur-
face, a filter paper is attached beneath and
glued to the polyester resin sides. To pre-
empt deformation of the weakened loam at
the bottom during weighing, a 4-mm-thick
sponge over an acrylic glass plate is placed
underneath (see 2 .18). A test with a baked
brick sample comparing both methods
showed that the BRL method reduced
results by only 2%.
The coefficient w of different loams tested
along with the w-values of common build-
ing materials is listed in 2 .19. Interestingly,
the silty soil samples gave higher w-values
than those of clayey soil. Surprisingly, com-
parison with baked bricks shows that loam
has w-values that are smaller by a factor
of 10.
Water absorption in relation to time is also
very interesting as shown in 2.20. Visible
here is the amazing effect of a tremendous
increase in absorption caused by adding
small quantities of cement.

Capillary water capacity
The maximum amount of water that can be
absorbed in comparison to the volume or
mass of the sample is called “capillary water
capacity” ([kg/m^3 ] or [m^3 /m^3 ]). This is an
important value when considering the con-
densation phenomena in building compo-
nents. Illustration 2 .19shows these values
with the w-values.

Water penetration test after Karsten
In Karsten’s water penetration test, a
spherical glass container with a diameter of
30 mm and an attached measuring cylinder
is fixed with silicon glue to the test sample
so that the test surface in contact with the
water is 3 cm^2 (Karsten, 1983, see 2.21). The

27 Properties of earth

2 .19Water absorption
coefficient ‘w’ of loams in
comparison with com-
mon building materials
2.20Water absorption
curves of loams

W
√t

1 Clayey loam + sand
2 Clayey loam + 2% cement
3 Clayey loam + 4% cement
4 Clayey loam + 8% cement
5 Lightweight mineral loam 650
6 Lightweight mineral loam 800
7 Lightweight straw loam 450
8 Lightweight straw loam 850
9 Lightweight straw loam 1150
10 Clayey loam
11 Silty loam
12 Sandy loam

Silty loam (1900 kg/m^3 ) (3)
Clayey loam (1940 kg/m^3 ) (3)
Lightweight mineral loam (470 kg/m^3 ) (3)
Lightweight mineral loam (700 kg/m^3 ) (3)
Lightweight straw loam (450 kg/m^3 ) (3)
Lightweight straw loam (850 kg/m^3 ) (3)
Lightweight straw loam (1150 kg/m^3 ) (3)
Spruce axial (2)
Spruce tangential (2)
Cement concrete (2290 kg/m^3 ) (1)
Hollow brick (1165 kg/m^3 ) (1)
Solid brick (1750 kg/m^3 ) (1)


2 .19

2.20

3.7
1.6
1.3

1.2
0.2

2.8

1.8
8.9
25.1

0.32
0.27
0.13
0.15
0.20
0.26
0.29

3.6
3.1

2.4

0 0.2 0.4
(m^3 /m^3 )

0 10 20 30
w (kg/m^2 h0.5)

Water absorption w (kg/m^2 )

Time t (min)
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