Pumice is a natural lightweight aggregate which
is also available for general use, provided it is free of
fine volcanic ash and volcanic material. Pumice
provide better thermal insulation than other types of
lightweight concrete.
This study aims to gain an innovative material
utilization of pumice as a lightweight aggregate for use
in the manufacturing of lightweight concrete. The
burden of building with lightweight concrete is
relatively small so it is expected to accommodate
vertical urban growth and support comprehensive
planning of a city that is healthy, safe and comfortable.
2 CONCEPT OF LIGHTWEIGHT
CONCRETE
According to Mulyono (2004), lightweight aggregate
is an aggregate with a density of about 300 - 1850 kg/
m3. SNI-03-2641-2002 regulates lightweight
concrete criteria limits in the density to be < 1900
kg/m3. The essence of lightweight aggregate is an
aggregate with a density that is lightweight and highly
porous, which can be made from natural aggregates
and fabricating results. Based on this understanding,
there are two methods for making lightweight
concrete using lightweight aggregate. The first is
formed by using a porous lightweight aggregate with
a small density. The concrete formed is called
lightweight aggregate concrete. The second is to
make the mass of mortar highly porous, ie by
increasing the air content in it.
There are several methods to reduce the density of
concrete or produce lighter concrete, as follows
(Tjokrodimuljo, 1996):
a. Creating bubbles of gas/air in the mortar, causing
the concrete to have a large number air pores in it.
b. Using lightweight aggregates, such as baked clay,
pumice or artificial aggregates so that the concrete
made will be lighter than regular concrete.
c. Making concrete without using grains of fine
aggregate or sand, which is referred as non-sand
concrete.
According to ASTM C.330, lightweight
aggregates can be divided into two: natural and
artificial aggregates. Natural lightweight aggregates
includes types of diatomite, pumice, scoria, volcanic
tuff Dinder and everything including original
volcanic rocks. Artificial lightweight aggregates can
be made from the process of heating and cooling
industry cinder. Artificial lightweight aggregates
include expanded clay, shale, slate, perlite,
vermiculite, and fly ash (Mulyono, T., 2004).
According to the heavy volume and minimum
compressive strength that must be met, and also retain
earnings, lightweight concrete can be divided into
three categories (Dobrowolski, 1998):
a. For non-structures, a density of 240 kg/m
3
to 800
kg/m
3
and a compressive strength of 0.35 MPa to
7 MPa is generally used for dividing walls or walls
for insulation.
b. For lightweight structures, a density of 800 kg/m
3
to 1400 kg/m
3
and a compressive strength of 7
MPa to 17 MPa is generally used for walls that
also bear burdens.
c. For other structures, a density between 1400
kg/m
3
to 1800 kg/m
3
and a compressive strength
of more than 17 MPa can be used as normal
concrete.
3 CONCEPT OF PUMICE
Pumice is a light-coloured rock that usually resembles
a layer of glass, with a unit weight of 500 to 900
kg/m
3
(Mulyono, 2004: 286). According to Murdock
and Brook (1999: 396), pumice is a natural
lightweight aggregate and that is suitable for general
use as well. Provided it is free of fine volcanic ash and
volcanic material that is not native such as clays,
pumice can be made into a satisfactory lightweight
concrete with a density of 720 kg/m
3
to 1440 kg/m
3.
Pumice provides better thermal insulation than other
lightweight concrete.
Pumice is a type of light-coloured rock that
contains cavities made of glass-walled bubbles and is
usually referred to as volcanic silicate rock glass.
These rocks are formed from magma acid through
volcanic eruptions that eject material into the air,
which then experiences horizontal transport and
accumulates as pyroclastic rocks. Pumice has high
vesicular properties and contains a number of cells
and plenty of cellular structured foam due to the
expansion of natural gas contained therein and in
general as a freelance or fragments in a volcanic
reaction. While the minerals contained in pumice
include feldspar, quartz, obsidian, cristobalite, and
tridymite. The existence of pumice is always
associated with a series of volcanoes, from old quarter
to tertiary.
The existence of pumice is always associated with
a series of volcanoes. The chemical and physical
properties of pumice include: oxides SiO
2,
Al
2
O
3,
Fe
2
O
3,
Na
2
O, K
2
O, MgO, CaO, TiO
2,
SO
3,
and
Cl, lost incandescent (loss of ignition) of 6%, pH 5,
bulk density 480 to 960 kg/cm
3,
water absorption of
16.67%, a specific gravity of 0.8 g / cm
3,
a low sound