and friction, which are short-range and non-cohesive. Even in this idealized situation,
dry granular media show unique and striking behaviour, which have attracted the
attention of many scientists for centuries.
In the real world, however, we often see wet granular materials, such as beach
sand. Dry and wet granular materials have many aspects in common, but there is one
big difference: Wet granular materials are cohesive due to surface tension.
In the past, many research groups that studied granular physics have been
struggling to minimize humidity and avoid inter-granular cohesive forces (e.g. [13]).
Indeed, some experiments were performed in vacuum chambers. Humidity and fluids
in general were seen as a nuisance to be avoided at all costs. However, many important
real life applications involve mechanical properties of wet granular media.
Examples include rain-induced landslides, pharmaceuticals, food processing, mining
and construction industries. Thus, it is important to study the mechanical response
of granular matter with various degrees of wetness or liquid content.
In this review, we show how the cohesion induced by the liquid changes
the mechanical properties of granular materials. We mainly consider static or
quasi-static situations, where the cohesion dominates over other effects of the
liquid, such as lubrication and viscosity. Some phenomena in this field which are
not well-understood are presented below as ‘open problems’. Most references listed
at the end focus on experimental results. Theoretical approaches can be found in
the reviews cited below and references therein.
1.2. What is different from dry granular media?
Studies of wet granular media have been made in many industrial applications. The
mechanical properties of wet granular media are also extremely important in geology
and civil engineering. For example, let us consider a huge and expensive civil works
project, the construction of the Kansai International Airport, on a man-made island
near Osaka. The weight of the 180 million cubic metres of landfill and facilities
compressed the seabed, composed of clay, inevitably causing the airport to sink by
some amount. The airport had sunk by 11.7 metres on average at the end of 2000,
and the settlement is still carefully monitored [14]. This with other examples from
geology and civil engineering stress the need to better understand the mechanical
properties of wet granular assemblies, both small and large.
The biggest effect that the liquid in granular media induces is the cohesion
between grains. Even humidity in the air may result in a tiny liquid bridge at
a contact point, which introduces cohesion. The cohesion occurs in wet granular
material unless the system becomes overwet, i.e. the granular medium is completely
immersed in a liquid. In this short review, we focus on the effect of this cohesion; the
system that we are considering is partially wet granular material, which is a mixture
of solid grains, liquid, and air.
In addition to cohesion, there are many effects induced by the presence of
the liquid. One of them is the lubrication of solid–solid friction [15–17]. In addition,
the liquid viscosity may induce velocity-dependent behaviour and additional dissipa-
tion. These effects are often seen in underwater experiments (e.g. [18, 19]). The
time-scale of liquid motion (how the liquid moves or flows through granular
media) also affects the dynamics. All of these effects, of course, play important
Wet granular materials 3
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