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Building with earth - Gernot MINKE (1)

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usual method using water is problematic,

shrinkage, the sandy mixture only 3%. After

since the sample dissolves at the joint.

three years of exposure to the weather, the

Therefore, the BRL modified the method by

clayey soil showed a special kind of scaling

closing the opening of the glass container

caused by frost. This was due to thin hairline

with filter paper (see 2.22, right). Results

cracks that appeared during drying, and

using this method were comparable to

through which rainwater was absorbed by

those using the method given in the Ger-

capillary action. When this water freezes, its

man standard DIN 52617 (see 2.23).

volume increases, causing the upper layers

Stability in static water

to burst. In areas where no hairline cracks

were found, this effect did not occur. Fur-

2.21

Stability in static water can be defined after

thermore, no rain erosion was observed in

the German standard DIN 18952 (Part 2),

these areas. The sample on the left does

as follows: a prismatic sample is immersed

not show this type of erosion after three

5 cm deep in water and the time it takes for

the submerged part to disintegrate is meas-

years. Here we see that some loam is

washed away by rain, so that the horizontal

Filter paper

ured. According to this standard, samples

that disintegrate in less than 45 minutes are

shrinkage crack is partially filled by these

particles, but no frost erosion is observable.

Silicon

Seal

unsuitable for earth construction. But this

test is unnecessary for earth construction

This is because there were no hairline

cracks, and because the loam contained

2.22

practices, since earth components would

pores large enough to allow the freezing

Water absorption w (kg/m 2 )

2.23

never be permanently immersed in water

in any case. Significant instead is resistance

to running water.

water to expand.

The test resulted in the following conclusions:

• sandy loam has little resistance against

1 Clayey loam, w – value

2 Clayey loam, Karsten

3 Silty loam, w – value

4 Silty loam, Karsten

Resistance to running water

rain, but is frost-resistant when free of

During construction, earth building elements

cracks;

are often exposed to rain and sensitive to

• loam with high clay content tends to

erosion, especially if still wet. It is important,

develop hairline cracks, and is therefore sus-

hence, to determine their resistance to run-

ceptible to frost. If there are no hairline

ning water. To compare the degrees of

cracks, it is almost rain-resistant.

Time t (min)

resistance of different loam mixtures, the

The higher the porosity and the larger the

BRL developed a test apparatus capable of

testing up to six samples simultaneously

(see 2.24). In this apparatus, water jets with

diameters of 4 mm are sprayed onto the

samples from a 45° angle and with a velocity

of 3.24 m/sec, simulating the worst

driving rain conditions in Europe.

pores, the higher loam’s resistance to frost.

Therefore, extruded common clay bricks

produced in a factory are not frost-resistant

and should not be used on outer exterior

walls in climates with frost. By contrast,

handmade adobes made from sandy loam

are usually frost-resistant.

2.21 Modified water

penetration test according

to BRL

2.22 Modified water

penetration test according

to BRL

2.23 Water absorption

according to Karsten and

the German standard

DIN 52617

Rain and frost erosion

Drying period

Illustration 2.25 shows two samples: each is

The period during which wet loam reaches

shown prior to testing (left), and after three

its equilibrium moisture content is called

years of weathering (right). The earth mix-

the “drying period.” The decreasing water

ture of the sample on the right contained

content and increasing shrinkage of a sandy

40% clay; the one on the left was mixed

mud mortar dried in a closed room at a

with sand, reducing the clay content to

temperature of 20°C and with a relative

16%. Both mixtures were tested with a mor-

humidity of ambient air of 81% and 44%

tar consistency in single layers 5 cm in thick-

respectively is shown in 2.26. With 44%

ness. After drying, large shrinkage cracks

humidity, the drying took about 14 days,

appeared. The clayey mixture showed 11%

while with 81% humidity, about 30. Illustra-

28

Properties of earth

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