Tracking Grade Heterogeneity in a Panel Cave Mine: A Reconciliation Study Investigating the Impact of Mixing from an Ore Sorting Perspective
Abstract
:1. Introduction
2. Identification of Mixing Events at the Cadia East Mine
3. Methodology
3.1. Investigation Period
3.2. Data Description and Grade Reconciliation
3.3. Assessing Impact of Mixing on Grade Heterogeneity and Bulk Ore Sorting Potential
4. Results and Discussion
4.1. Impact on Grade Heterogeneity
4.2. Impact on Bulk Ore Sorting Potential
5. Conclusions
Author Contributions
Funding
Data Availability Statement
Acknowledgments
Conflicts of Interest
References
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Mixing Location | Chronological Order | Ore Mixing Event |
---|---|---|
Within caves | 1 | Collapsing of ore onto caved ore muck pile as caving progresses |
2 | Flow through draw columns | |
Material handling system | 3 | Blending according to mine planning to provide concentrators with consistent feed and manage panel caves safely |
4 | Flow through ROM bins | |
5 | Flow through crushed ore bins | |
6 | Mixing of crushed ore originated from different panel caves on collection conveyor belts |
Panel Cave | Active Drawpoints | Between 1 April 2019 and 1 June 2019 | Until 1 April 2019 | ||
---|---|---|---|---|---|
Tonnage Share (%) of Caves | Average HOD of Drawpoints Targeted | Tonnage Share (%) of Footprints Caved | Average HOD of Drawpoints Achieved | ||
PC1 | 127 | 6.55 | 1.33 | 43.88 | 357.15 |
PC2-West | 129 | 51.78 | 10.15 | 15.81 | 199.12 |
PC2-East | 167 | 41.66 | 6.16 | 10.7 | 118.11 |
Total | 423 | 100 | - | - | - |
Location | Panel Cave | Cu (%) | Au (g/t) |
---|---|---|---|
In situ (block model) | PC1 | 0.32 | 0.64 |
PC2-West | 0.35 | 1.30 | |
PC2-East | 0.39 | 1.12 | |
All caves | 0.36 | 1.18 | |
Extraction level (drawpoint sampling) | PC1 | 0.36 | 0.57 |
PC2-West | 0.33 | 1.24 | |
PC2-East | 0.38 | 1.20 | |
All caves | 0.35 | 1.16 | |
Surface (PGNAA sensor) | All caves | 0.33 | 1.21 |
Variables | Location | ||
---|---|---|---|
In Situ | Extraction Level | Surface | |
or | Number of ore blocks | Number of drawpoint samples | Number of ore pods scanned by PGNAA |
or | Grade of a block | Grade of a drawpoint sample taken during a sampling period | Grade of an ore pod |
or | Mass of a block | Total mass produced from a drawpoint during a sampling period | Mass of an ore pod |
or | Average grade of blocks | Average grade of drawpoint samples | Average grade of ore pods |
or | Total mass of blocks | Total mass produced from drawpoints | Total mass of ore pods |
Distribution | Explanation |
---|---|
Burr | The Burr distribution was introduced by Burr [18] and can fit almost any unimodal data since it can yield a wide range of skewness and kurtosis values [19]. |
Chi-squared | Many variables in earth science are non-negative and positively (right) skewed [20]. The gamma distribution is a two-parameter distribution widely used for modelling positively skewed data. Chi-squared, Erlang, and exponential distributions are special cases of the gamma distribution. |
Erlang | |
Exponential | |
Gamma | |
Lognormal | The lognormal distribution has been determined to represent the frequencies of metal contents well when the ore deposit is modelled with consistent geologic settings, and the model data comes from well-explored deposits with spatial rules consistently applied [21]. |
Normal | The sample value frequency distributions of most mineral deposits commonly conform to the normal (Gaussian) or lognormal distributions [22]. |
Student’s t | The student’s t distribution is similar to the standardized normal distribution with heavier tails, meaning that it possesses a higher probability in the extreme values, or tails, compared to the normal distribution. |
Location | Change (%) in DH and Weighted Variance Spatially | |||
---|---|---|---|---|
Cu | Au | |||
DH | Weighted Variance | DH | Weighted Variance | |
In situ to extraction level | −7 | −61 | 74 | −24 |
Extraction level to surface | −95 | −87 | −96 | −89 |
In situ to surface | −95 | −95 | −92 | −92 |
Location | Best-Fit Distribution Types and Parameters | |
---|---|---|
Cu | Au | |
In situ (block model) | Burr(shape(c) = 5.85, shape(d) = 0.29, location = 0.06, scale = 0.43) | Lognormal (shape = 0.77, location = −0.06, scale = 0.94) |
Extraction level (drawpoint sampling) | Burr (shape(c) = 10.71, shape(d) = 0.27, location = 0.07, scale = 0.37) | Lognormal (shape = 0.79, location = 0.10, scale = 0.71) |
Surface (PGNAA sensor) | Student’s t (degrees of freedom = 1.83, location = 0.33, scale = 0.02) | Student’s t (degrees of freedom = 2.29, location = 1.26, scale = 0.18) |
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Cetin, M.C.; Klein, B.; Li, G.; Futcher, W. Tracking Grade Heterogeneity in a Panel Cave Mine: A Reconciliation Study Investigating the Impact of Mixing from an Ore Sorting Perspective. Minerals 2023, 13, 1333. https://doi.org/10.3390/min13101333
Cetin MC, Klein B, Li G, Futcher W. Tracking Grade Heterogeneity in a Panel Cave Mine: A Reconciliation Study Investigating the Impact of Mixing from an Ore Sorting Perspective. Minerals. 2023; 13(10):1333. https://doi.org/10.3390/min13101333
Chicago/Turabian StyleCetin, Mahir Can, Bern Klein, Genzhuang Li, and William Futcher. 2023. "Tracking Grade Heterogeneity in a Panel Cave Mine: A Reconciliation Study Investigating the Impact of Mixing from an Ore Sorting Perspective" Minerals 13, no. 10: 1333. https://doi.org/10.3390/min13101333
APA StyleCetin, M. C., Klein, B., Li, G., & Futcher, W. (2023). Tracking Grade Heterogeneity in a Panel Cave Mine: A Reconciliation Study Investigating the Impact of Mixing from an Ore Sorting Perspective. Minerals, 13(10), 1333. https://doi.org/10.3390/min13101333