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, Australian Centre for Geomechanics, Perth, pp. 407-415, https://doi.org/10.36487/ACG_repo/605_33
Successful rehabilitation of mined land is one of the key concerns for mine closures. Disturbance through
mining is often so severe that rehabilitation must be viewed as the first step towards a long term evolution of
the landscape and the ecosystem to a stable state that is in harmony with the surrounding land. To ensure
that the rehabilitation measures will create a stable and sustainable landform, risk assessment needs to be
carried out for the initial phase of rehabilitation, which may cover a time span of the first two decades
depending on climate, soil and vegetation. This initial, short term assessment should also be complemented
by long term risk assessment extending beyond decades.
The first years after rehabilitation are the most vulnerable to extreme weather events, especially for rock
dumps and tailing storage facilities that involve the design of a new landform along with placement of soil
material on the surfaces. It is often a single infrequent event such as a cyclone that causes excessive erosion
and potentially significant leaching events contributing to acid mine drainage. This high risk period during
these first years of rehabilitation is due to immature vegetation establishment and soil development.
Understanding and quantifying water redistribution on mined landforms and rehabilitated dumps and tailing
dams is therefore the key to risk assessment of rehabilitation success.
One of the first order controls of water redistribution is climate and in particular rainfall. While great effort
has been placed on the use of detailed mechanistic understanding of small scale processes to predict and
model surface runoff, infiltration, erosion and water movement in soils and rock dumps, little attention has
been placed on climate forcing. In this paper we will outline a generic analysis on how the stochastic and
episodic nature of rainfall contributes to the triggering of significant hydrological events that may cause
damage to land rehabilitation and hence will provide us with a risk assessment tool. The analysis will focus
on short term (years to decades) risk assessment aspects, as long term stability can only be realistically
assessed when rehabilitation has been shown to be successful in the short term. We therefore promote a
probabilistic event based approach that uses a minimalist description of hydrological processes and accurate
and detailed information on rainfall as this is the most important first-order control of triggering relevant
hydrological processes. We will use surface runoff as an example of our approach. This analysis will be
further complemented by an analysis of the rainfall resolution required to predict surface runoff.
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Hydrology of Post-Mining Landscapes
Mine Closure 2006, Perth, Australia 415