Resources, Conservation and Recycling 56 (2011) 66–70
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Resources, Conservation and Recycling
journal homepage: www.elsevier.com/locate/resconrec
Review
Effect of volcanic ash on the properties of cement paste and mortar
Rafat Siddique
∗
Department of Civil Engineering, Thapar University, Patiala, Punjab 147004, India
article info
Article history:
Received 6 August 2011
Accepted 9 September 2011
Keywords:
Cement
Compressive strength
Consistency
Electrical resistivity
Hydration
Mortar
Setting times
Volcanic ash
Workability
abstract
Volcanic ash (VA) is formed during volcanic eruptions. Volcanic glass is relatively high in silica, and its
physical and chemical properties could be referenced with ASTM C618-93, a Standard Specification for
‘Fly Ash and Raw or Calcinated Natural Pozzolan for Use as a Mineral Admixture in Portland Cement
Concrete’.
This paper presents comprehensive details of the physical, chemical properties of volcanic ash, and
its micro-structure and hydration products. It also covers effect of volcanic ash on consistency, setting
times, workability, compressive strength, electrical resistivity of cement paste and mortar.
© 2011 Elsevier B.V. All rights reserved.
Contents
1. Introduction ............................................................................................................................................. 66
2. Properties of volcanic ash .............................................................................................................................. 67
2.1. Physical properties .............................................................................................................................. 67
2.2. Chemical composition .......................................................................................................................... 67
3. Uses of volcanic ash ..................................................................................................................................... 67
4. Properties of blended cement containing volcanic ash ................................................................................................ 68
4.1. Consistency and setting times .................................................................................................................. 68
4.2. Compressive strength ........................................................................................................................... 68
4.3. Microstructure of hydration products .......................................................................................................... 68
4.4. Alkali–silica reaction and autoclave expansion ................................................................................................ 69
4.5. Electrical resistivity ............................................................................................................................. 70
4.6. Total pore volume (TPA) ........................................................................................................................ 70
5. Conclusions ............................................................................................................................................. 70
References .............................................................................................................................................. 70
1. Introduction
Volcanic ash (VA) is formed during volcanic eruptions. Ash is cre-
ated when solid rock shatters and magma (molten rock) separates
into minute particles during explosive volcanic activity. The usually
violent nature of an eruption involving steam (phreatic eruption)
results in the magma and solid rock surrounding the vent is torn
into particles of clay to sand size.
∗
Tel.: +91 175 239 3207; fax: +91 175 239 3005.
E-mail address: siddique 66@yahoo.com
The plum that is generally seen above an erupting volcano is
composed primarily of ash and steam. The very fine particles maybe
carried away for miles together, settling out as a dust-like layer
across the landscape. This is known as ‘ash fall’. The commonly
used term for any material explosively thrown out from a vent is
tephra, also known as pyroclasstic debris. If liquid magma is ejected
as spray, the particles will solidify in the air to small fragments of
volcanic glass. Tephra particles of gravel are termed cinders. The
ejection of large quantities of ash will produce an ash cone. A layer
of volcanic ash tends to become cemented together to form a solid
rock called ‘tuff’.
The size of ash particles, which fall on the ground decreases
exponentially with increasing distance from a volcano. Also, the
0921-3449/$ – see front matter © 2011 Elsevier B.V. All rights reserved.
doi:10.1016/j.resconrec.2011.09.005