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This research examines optimization of blasting parameters for economic production of granite aggregates in Ratcon and NSCE quarries located atIbadan,OyoState. Samples were collected from the study areas for the determination of rock density and porosity. Schmidt hammer was used for in situ determination of rock hardness. Uniaxial compressive strength of in situ rock was estimated from the values obtained from Schmidt hammer rebound hardness test and density determined from laboratory test. Blasting data were collected from the study areas for optimization. Multiple regression analysis using computer aided solution SPSS (Statistical Package for the Social Sciences) was used to analyse data obtained from the laboratory test, field test and the study areas. The estimated mean uniaxial compressive strength value of NSCE is 240 MPa and that of Ratcon is 200 MPa and their average densities and average porosities are2.63g/cm^{3},2.55g/cm^{3}, 1.88% and 2.25% respectively. Eleven parameters were input into the multiple regression analysis to generate the models. Two parameters out of eleven input parameters such as geometric volume of blast (Y_{1}) and number of boulders generated after blasting (Y_{2}) were dependent variables and the remaining nine such as X_{1} (Drill hole diameter), X_{2} (Drill hole depth), X_{3} (Spacing), X_{4} (Burden), X_{5} (Average charge per hole), X_{6} (Rock density), X_{7} (Porosity), X_{8} (Uniaxial compressive strength) and X_{9} (Specific charge) were input as independent variables. The results of the models show that out of the nine independent variables seven of them that is X_{1} (Borehole diameter), X_{2} (Borehole depth), X_{3} (Spacing), X_{4} (Burden), X_{5} (Average charge per hole), X_{8} (Uniaxial compressive strength) and X_{9} (Specific charge) have significant contribution to the models while X_{6} (Rock Density) and X_{7} (Porosity) have insignificant contribution they are therefore automatically deleted by the SPSS. The result of the models developed for the optimization reveals that blasting number 5 gives the required product at lowest possible cost. From the result, the cost of secondary blasting has been reduced and volume of the blasted rock has been increased with low cost of explosives, the parameters that give this result have been chosen as optimum parameters.

Efficiency of blasting operation in underground and surface mines determine to a large extent utilization of equipment, productivity and economics. Proper fragmentation of blasted rocks and coal improves the efficiency of downstream operations, viz. loading, transport and crushing to desired sizes. An optimal blast not only results in proper fragmentation but also reduces undesirable effects like ground vibration, fly rock and formation of toe in quarry benches [

Fragmentation optimization involves breaking of rocks to ensure quality control, safe, consistent and efficient blasting. Big boulder or the opposite, excess fines can result from poorly selected drilling and blasting pattern. A well-selected pattern would produce fragmentation that can be accommodated by available loading and hauling equipment and crushing plant with little or no need for secondary blasting. It is well accepted that performance of basic mining operations such as excavation and crushing relies on a fragmentation which has been pre-conditioned by the blast, by pre-condition it means well fragment, sufficiently loose with adequate muck pole profile [

Effectiveness of hard rock blasting are measured with two basic indices that are oversize generation and blasthole productivity, cost per ton of rock blasted is also another index that measures the effectiveness of blasting and are dependent on rockmass and blast design parameters such as hole diameter, burden, spacing among others. [

This research work is carried out to optimize blasting parameters by establishing relationship between the parameters and determining which of the parameters give the optimum blasting result using the regression model generated using indices such as oversize generation and geometric volume of blast fit on blast design parameters.

Description of the Study AreasThe study areas are located at Ibadan, Oyo state. Two quarries namely NSCE quarry and Ratcon quarry were used for this research. These quarries produce granite aggregates such as 1/2^{11}, 3/4^{11}, lumps and quarry dust. The two quarries are in full operation.

Samples were collected from two different quarries and GPS (global positioning system) was used to take the locations of where the samples were taken. The Samples were randomly taken from quarries’ faces at four different points to ensure true representation of the rock. Samples from NSRC quarry were taken at longitude 07˚15'22.9" N and latitude 003˚50'11.9" at 179 m above

sea level, while those from Ratcon quarry were taken at longitude 07˚16'59.9" and latitude 003˚50'48.5" at 171 m above sea level. These samples were used for the determination of physical properties of the rock. Preparation of the samples follows the relevant ISRM and ASTM standard as much as practicable. Schmidt hammer was used to determine the strength of the rock.

The objective of the test is to measure the dry density of the rock samples of irregular form from Ratcon and NSCE granite quarries. The saturation and Buoyancy technique for irregular rock samples was adopted and the procedures follow the standard suggested by [

The bulk and pore volumes were calculated as follows:

Bulk volume

Pore volume

Bulk density of rock

where M_{sat} is the_{ }saturated-surface-dry mass, M_{sub} is the saturated-submerged mass, M_{s} is the grain weight and p_{w} is the density of water.

The objective of the test is to measure the porosity of rock specimens of irregular form. The porosity is the volume of pores in the rock expressed as a percentage of the total volume of the rock.

The saturation and Buoyancy technique for irregular rock samples was adopted and the procedures follow the standard suggested by [

Porosity

where V_{v} is the pore volume in cm^{3} and V is the bulk volume in cm^{3}

Hardness test involve the use of Schmidt Impact Hammer of type L for the hardness determination of in situ rock. The rebound value of the Schmidt Hammer is used as an index value for the intact strength of rock material, but it is also used to give an indication of the compressive strength of rock material [

The result of the hardness test is used to evaluate the unconfined compressive strength (UCS). The standard method for the Schmidt Hammer test as described by [

The measured test values were ordered in descending order. The lower 50% of the values were discarded and the average obtained of the upper 50% value to obtain the Schmidt Rebound Hardness [

The uniaxial compressive strength of the rock was estimated from the values of the type L Schmidt Hammer Hardness and the density of the rock.

The UCS values were estimated by using the chart named after Deere and Miller (1966) (

Regression models for the optimization of blasting parameters of granite quarry were generated from the data collected, in-situ test and laboratory test conducted on two quarries that is Ratcon and NSRC quarries located at Ibadan, Oyo State. The standard statistical correlationregression analysis software (SPSS) was used to generate the regressions models of geometric volume of blasting V_{B} and number of boulders generated N_{B}, fit on uncontrollable blasting parameters of (hardness, uniaxial compressive strength, and density) and controllable blasting parameters (burden, spacing, bench height, borehole diameter, average charge per hole etc). In these models both geometric volume (V_{B}) of blast and number of boulders(N_{B}) generated are dependent variables while blast design parameters such as burden (B), Spacing (S), Borehole Diameter (D), Borehole depth (H), Average Charge per Hole (AGH), Porosity (P), Compressive strength (σ_{c}), Specific charge (SC) and Density (ρ) are independent parameters.

Tables 1-4 show the results of laboratory tests conducted on rock samples from Ratcon and NSCE quarries for the determination of density and porosity.

The value of R^{2} is 0.984 and the adjusted R^{2} is 0.979

(_{1} (Borehole diameter), X_{2} (Borehole depth), X_{3} (Spacing), X_{4} (Burden), X_{5} (Average charge per hole), X_{8} (uniaxial compressive strength) and X_{9} (Specific charge). The parameters that are found insignificant are porosity and density of rock.

1) Blast-hole diameter (X_{1}) (10.679): This value that is 10.679 indicates that as the borehole diameter increases by one unit, the volume of rock blasted increases by 10.679units. This interpretation is true only if the effects of other parameters are held constant. The t-test (0.561)

associated with this value shows that it is significant. Borehole diameter is making significant contribution to the model.

2) Blast-hole depth (X_{2}) (535.401): This value indicates that as the borehole depth increases by one unit, the volume of rock blasted increases by 535.401units. This interpretation is true only if the effects of other parameters are held constant. The t-test (3.186) associated with this value shows that it is significant. Borehole diameter is making significant contribution to the model.

3) Spacing (X_{3}) (1029.503): This value indicates that as the spacing increases by one unit, the volume of rock blasted increases by 1029.503units. This interpretation is true only if the effects of other parameters are held constant. The t-test (1.556) associated with this value shows that it is significant. Spacing between the holes is making

_{1}.

^{a}: Power of R.

significant contribution to the model.

4) Burden (X_{4}) (2219.330): This value indicates that as the burden increases by one unit, the volume of rock blasted increases by 2219.330units. This interpretation is true only if the effects of other parameters are held constant. The t-test (4.297) associated with this value shows that it is significant.

5) Average charge per hole (X_{5}) (−66.731): This value indicates that as the average charge per hole increases by one unit, the volume of rock blasted decreases by 66.731 units. This interpretation is true only if the effects of other parameters are held constant. The t-test (−1.085) associated with this value shows that average charge per hole as a significant effect on volume of rock blasted.

6) Uniaxial compressive strength (−6.407): This value indicates that as the rock density increases by one unit, the volume of rock blasted decreases by 6.407 units. This interpretation is true only if the effects of other parameters are held constant. The t-test (−0.186) associated with this value shows that it is significant. Rock density makes significant contribution to the model.

7) Specific charge (X_{9}) (2461.507): This value indicates that as the specific charge increases by one unit, the volume of rock blasted increases by 2641.507 units. This interpretation is true if the effects of other parameters are held constant. The t-test (0.367) associated with this value shows that it is significant.

The value of R^{2} is 0.876 (_{1} (Borehole diameter), X_{2} (Borehole depth), X_{3} (Spacing), X_{4} (Burden), X_{5} (Average charge per hole), X_{8} (compressive strength) and X_{9} (Specific charge). The parameters that are found insignificant are porosity and density of the rock.

1) Drillhole diameter (X_{1}) (−0.471): This value indicates that as the borehole diameter increases by one unit, number of boulders generated decreases by 0.471 units. This interpretation is possible if the effects of other parameters in the model are kept constant. The t-test (−1.970) associated with this value shows that it is significant. Borehole diameter is making significant contribution to the model.

2) Drilhole depth (X_{2}) (1.567): This value indicates that as the borehole diameter increases by one unit, number of boulders generated after blasting increases by 1.567 units. This interpretation is possible if the effects of other parameters are kept constant. The t-test (0.743) associated with this value shows that it is significant. Borehole depth is significantly contributing into the model.

3) Spacing (X_{3}) (9.615): This value indicates that as the borehole diameter increases by one unit, number of boulders generated after blasting increases by 9.615

^{a}: Power of R.

units. This interpretation is possible if the effects of other variables are kept constant. The t-test (1.157) associated with this value shows that it is significant. Spacing is making significant contribution to the model.

4) Burden (X_{4}) (5.324): This value indicates that as the borehole diameter increases by one unit, number of boulders generated after blasting increases by 5.324 units. This interpretation is possible if the effects of other parameters are kept constant. The t-test (0.821) associated with this value shows that it is significant. Burden makes significant contribution to the model.

5) Average charge per hole (X_{5}) (−0.173): This value indicates that as the average charge per hole increases by 1 unit, number of boulders generated decreases by 0.173 unit. This interpretation is possible if the effects of other parameters are kept constant. The t-test (−0.90) associated with this value shows that it is significant. Average charge per hole is making significant contribution to the model.

6) Uniaxial compressive strength (X_{8}) (−0.098): This value indicates that as the rock density increases by 1 unit, number of boulders generated decreases by 0.098 units. This interpretation is true if the effects of other parameters are kept constant. The t-test (−0.240) associated with this value shows that it is significant. Rock density is making significant contribution to the model.

7) Specific charge (X_{9}) (18.061): This value indicates that as the specific charge increases by one unit, the volume of rock blasted increases by 18.061 units. This interpretation is true if the effects of other parameters are held constant. The t-test (1.420) associated with this value shows that it is significant. Specific charge is making significant contribution to the model.

The estimation regression models for the volume of rock blasted and boulders generated after blasting for the determination of optimum parameters are written in Equations (7) to (10):

By replacing X and Y with symbols of parameters, Equations 7 and 8 become;

The impact of the blasting parameters on the granite aggregate production blasting could be explained in accordance to the regression models estimated for geometric volume of rock blasted and number of boulders generated as follows:

Blast-hole Diameter: As the borehole diameter increases, the geometric volume of rock blasted increases Equation (9) and the number of boulders generated decreases Equation (10), resulting to decrease in the cost of secondary blasting. This agreed with [

Blast-hole Depth: As blast-hole depth increases, the geometric volume of rock blasted increases Equation (9). This assumption is true because as the drill-hole depth increases more explosive will be used and more volume of rock will be obtained, but this increment has limitation. It is limited by the rich of the loading equipment.

Spacing: As the hole spacing increases both the volume rock blasted and number of boulders increases Equations (9) and (10). This is because there are wider areas to be covered by the explosion gases this leads to increase in the number of boulders and consequently, increase in the cost of secondary blasting. However, the value of spacing must not be too small; this leads to excessive crushing between the holes, toe problems and lower volume of rock blasted.

Burden: As the hole burden increases, the volume of rock blasted increases and also number of boulders generated increases, but it has very little contribution to the increase in number of boulders as compared to that of volume of rock blasted (Equations (9) and (10)).

Average charge per hole: As the average charge per hole increases the volume of rock blasted and number of boulders generated decreases Equations (9) and (10). This is true because if the blast hole is over charged there will be more dust in the product of blasting than the required aggregates and eventually, there will be less number of boulders.

Uniaxial compressive strength: As the uniaxial compressive strength of rock increases the volume of rock blasted and number of boulders generated decreases Equations (9) and (10). As the rock strength increases volume of rock blasted decreases, resulting to increase in the cost of blasting because more explosive energy will be required to break the rock.

Specific charge: As specific charge increases, volume of rock blasted and number of boulders generated increase Equations (9) and (10). But care should be taking so as to avoid using more explosive than required.

Density of rock: as the density of rock increases the geometric volume of blast and number of boulders generated decreases. It has been identified by several researchers such as [8-10] among others that rock density hampers the transfer of explosive energy and thus blastability, cost of blasting and product of blasting, though it is found insignificant in the developed model.

The field estimation of uniaxial compressive strength was determined using the Schmidt hammer method. The uniaxial compressive strength of NSRC granite is higher than that of Ratcon granite.

The average Schmidt hammer values of Ratcon and NSRC granite quarries as obtained from the field are shown in Tables 4 and 5 with their corresponding measured average density. From this result it can be observed that the Schmidt hammer value of Ratcon is lower than that of NSRC.

Density and porosity were also determined in FUTA Rock Mechanics laboratory (Tables 1-4). Rock samples from NSRC are denser than those gotten from Ratcon and the porosity of the formal is lower than that of the latter.

Both the mechanical properties and physical properties determined were used in the formulation of the optimization model.

The developed models reveal that out of nine blasting parameters (both controllable and uncontrollable) such as borehole diameter (X_{1}), borehole depth (X_{2}), hole spacing (X_{3}), burden (X_{4}), average charge per hole (X_{5}), density (X_{6}), porosity (X_{7}), uniaxial compressive strength (X_{8}), specific charge (X_{9}) that participated as independent variables in the models, only seven of them make significant contribution to the models, while the porosity and density of rock make insignificant contribution to the models, they were therefore removed from the model (Tables 11 and 12).

The models developed in Equations 9 and 10 were used to determine which of the input parameters give optimum result with little boulders. ^{3}, Average Specific charge = 0.29 kg/m^{3}) gives the optimum parameters this result agreed with [

From the results of the research presented here, following conclusion were drawn:

The mechanical properties of the rock tested fall within the range of very high strength, although compressive strength of NSCE (240 MPa) is higher than that of Ratcon (200 MPa).

The average densities and average porosities of NSCE granite and Ratcon granite are 2.63 g/cm^{3}, 2.55 g/cm^{3}, 1.88% and 2.25% respectively.

The value of R2 values of the two models show that the nine predictors entered in the regression analysis account for 87.6% of the variation in number of boulders generated and 98.4% of the variation in the geometric

^{b}.

^{a}: Predictors in the Model: (Constant), X_{9}, X_{1}, X_{8}, X_{4}, X_{2}, X_{3}, X_{5}.

^{b}.

^{a}: Predictors in the Model: (Constant), X_{9}, X_{1}, X_{8}, X_{4}, X_{2}, X_{3}, X_{5}.

volume of blast, while their F changes are far greater geometric volume of blast.

Blasting parameters used in blasting number 5 (Borehole diameter = 88.9 mm, Borehole depth = 15 m, Spacing = 2.6 m, Burden = 2.4 m, Density = 2.55 g/cm^{3}, Average Specific charge = 0.29 kg/m^{3}) gives the optimum blasting product out of 30 blasting operations used in the models development.