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By Hugo Melo
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Whether operations or closure, downstream surface erosion of tailings embankments can be a perpetual challenge. During operations, the management of erosion and sediment transport is typically handled in due course of normal operating procedures. However, the challenges of erosion mount during reclamation and closure when owners face long-term environmental obligations and aspire to passive-care or walk-away solutions. As the recently published Global Tailings Standard highlights: “Few tailings facilities have a (design basis memorandum) that addresses long-term reclamation performance. Lack of clear agreement on design objectives and future performance creates a gap between what is planned by the mine and what is expected by regulators and local stakeholders.” Decisions on tailings reclamation may be further perplexed when the design and operation of tailing is at odds with the ideals of long-term closure (i.e. capital cost, storage, footprint, etc.). So, if we are required to design for and demonstrate the feasibility of safe closure, how do we quantify the long-term erosion performance of a closure landform to meet the expectations of industry guidelines?
There are tools available to designers to predict erosion such as RUSLE and WEPP as well as more sophisticated tools that combine erosion and long-term landform evolution such as SIBERIA and CAESAR-Lisflood. Recent work led by the University of Arizona, in collaboration with SRK and a soil science consultancy, has endeavored to study the erosion performance of a reclaimed upstream tailings embankment in the arid southwestern USA. The desert landscape receives modest, but intense, annual precipitation resulting in high-intensity erosive events. Portions of the facility cover experience rill erosion nearly every year. Using a decade of post-reclamation LiDAR data and two years of field data collected from various scales of rainfall-runoff-erosion test plots, the study team evaluated the performance and utility of the most common erosion models. Furthermore, the University of Arizona developed a new code, RILLGEN2D to model rill initiation in a rock-armor cover, which presents a novel approach to rill prediction based on material properties and landform geometry.
The study team was able to compare the different model codes against observed rilling and assess the strengths and weaknesses of each. Using RILLGEN2D, the team successfully retrodicted where rills form on an existing tailings embankment cover. Results to date show promise using SIBERIA to evaluate the long-term performance of landform designs and flag high-risk areas. Work is ongoing to link rill prediction using RILLGEN2D with sediment generation and transport in WEPP.
Some findings from this on-going study and considerations for erosion performance design: