Page 224 - Introduction to Mineral Exploration
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10: EVALUATION TECHNIQUES  207


                 pipe, must obey the three times the maximum  sible contribution to the total error. The two
                 particle size rule, i.e. the width, length, and  techniques which follow are less rigorous, and
                 depth must be at least three times the maxi-  more error prone, but less expensive.
                 mum particle size. This is defined as the largest
                 screen size which retains 5% of the material.  Chip sampling
                 There are three hand sampling techniques,    Chip samples are obtained by collecting rock
                 namely channel, chip, and grab sampling.     particles chipped from a surface, either along a
                                                              line or over an area. In an established mine,
                 Channel sampling                             rock chips from blastholes are sampled using
                 In mineral exploration, a channel is cut in  scoops, channels, or pipes pushed into the
                 an outcrop, usually the same diameter as the  heap. With a large database of chip samples,
                 core being collected, to maintain the volume–  statistical correlation between core and chip
                 variance relationships. It is cut using a hammer  samples may establish a correction factor for
                 and chisel or a circular saw, across the strike of  chip sampling results and thus reduce error.
                 the mineralisation (see Fig. 5.3). As the mater-  Chip sampling is used also as an inexpensive
                 ial is cut it is allowed to fall to the floor on to  reconnaissance tool to see if mineralisation
                 a plastic sheet or sample tray from which it  is of sufficient interest to warrant the more
                 is collected and bagged. Samples are normally  expensive channel sampling.
                 0.5–5 kg in weight, mostly 1–2 kg, and each is
                 rarely taken over 2 m or so in length, but   Grab sampling
                 should match the core sample length. There   In this case the samples of mineralized rock
                 is no point in oversampling and sample spac-  are not taken in place, as are channel and chip
                 ing perhaps can be determined from the range  samples, but consist of already broken mater-
                 (a) (section 10.4.1) derived from a study of a  ial. Representative handfuls or shovelfuls of
                 semi-variogram.                              broken rock are picked at random at some con-
                   A mineral deposit can often be resolved    venient location and these form the sample. It
                 into distinct and separate types of mineralisa-  is a low cost and rapid method and best used
                 tion. Sampling these different types as separate  where the mineralized rock has a low variance
                 entities rather than as one large sample can  and mineralisation and waste break into part-
                 reduce natural variation and thus the variance,  icles of about the same size. It is particularly
                 and keep sample weights to a minimum. This   useful as a means of quality control of miner-
                 stratified sampling is also of value where the  alisation at strategic sampling points such as
                 separate types require different mineral pro-  stope outlets and in an open pit (Annels 1991).
                 cessing techniques due to variation in either
                 grain size or mineralogy. Such sample data   Comparison of methods
                 are then more useful for mine planning. Such  Bingham Canyon mine in the United States
                 samples can be recombined statistically into  and the Palabora Mine in South Africa con-
                 one composite result for the whole of the    ducted a series of tests whereby the entire
                 mineralisation.                              product from blasthole drilling was collected in
                   In well-jointed or well-bedded rocks collec-  30-degree segments from the full 360 degrees
                 tion by hammering the rock face presents dif-  (C.P. Fish, personal communication). One
                 ficulties in that adjacent nonsample material  blasthole may produce between 2 and 3 t. Each
                 will fall with the material being cut but this  segment was sampled by the traditional means
                 must be rejected. Additionally, it is important  described above, and compared to the remain-
                 that a representative collection of rock masses  ing material in the segment after crushing to
                 is collected. Frequently, mineral values of in-  3 mm and reducing in a 16-segment rotary-
                 terest occur in altered rocks which may well  divider. The results showed:
                 be more friable than adjacent, harder, unminer-  1 No segment ever gave the same assay as the
                 alized ground, and overcollection of this easily  whole mass. The spatial variation was great
                 cut material will provide a biased sample.   and there was no consistency in the way the
                   Channel sampling provides the best tech-   material dispersed.
                 nique of delimiting and extracting a sample  2 Subsample analyses gave higher analytical
                 and, consequently, provides the smallest pos-  results than the 100% mass. Scoop samples
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