The Effect of Geological Structure and Powder Factor in Flyrock Accident

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    The Effect of Geological Structure and

    Powder Factor in Flyrock Accident,

    Masai, Johor, MalaysiaEdy Tonnizam Mohamad

    Associate Professor (Dr.), Universiti Teknologi Malaysia, Department of

    Geotechnics and Transportation,Faculty of Civil Engineering, 81310 UTM

    Skudai, Johor, Malaysia

    e-mail: [email protected]

    Danial Jahed ArmaghaniPhD Student, Universiti Teknologi Malaysia, Department of Geotechnics and

    Transportation,Faculty of Civil Engineering, 81310 UTM Skudai, Johor,

    Malaysia

    e-mail:[email protected]

    Hossein MotaghediPhD in Geotechnical Engineering, Faculty of Civil Engineering, Islamic Azad

    University of Qaem Shahr, Qaem Shahr, Iran

    e-mail: [email protected]

    ABSTRACTRock blasting is the most commonly used method for rock breakage in the field of civil andmining. The main goal of such operation is to produce the desired fragment size distribution

    leading to optimize the overall mine/plant economics. Blasting has some environmentalimpact such as ground vibration, airblast, dust and fumes and flyrock. One of the undesirablephenomena in the blasting operation is flyrock, which is a propelled rock fragment byexplosive energy beyond the blast area. A flyrock accident occurred during a blasting workat Masai quarry Johor, Malaysia in 19 July 2013. Due to this accident, a factory worker waskilled while 10 others were injured after being hit by rock debris from an explosion at aquarry that flew up to 700 m away. The main purpose of this study is to investigate thecauses of flyrock accident based on results of geological structure and also powder factor. Inorder to investigate causes of this accident, two continues blasting patterns were considered

    and powder factor of these blasts were calculated. It is concluded that blast geometry (suchas burden and spacing), total weight of explosive,close distance between the quarry and theresidential area, and geological conditions were considered the most influentioal parametersin this accident.

    KEYWORDS: Rock blasting, Flyrock accident, Blast geometry, GeologicalStructure, Powder factor.

    INTRODUCTIONIn civil engineering, rock is removed to create structures such as tunnels, hydraulic channels

    or caverns, or deep excavation at the ground surface for road cuts, foundation or basements

    (Bhandadari, 1997). For this work, there are some methods such as ripping, blasting and

    excavators. Blasting operation is a natural rock formation dislodge from its original location.

    Blasting of rock from a quarry face should be designed to obtain the optimum fragmentation and

    a rock pile attitude compatible with the plant and equipment used (Bhandadari, 1997). The main

    purpose of the blasting operation is to create desired fragment size distribution leading tooptimize the general mine economics (Monjezi et al. 2007). Blasting affects the rock

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    fragmentation, so there must be some beneficial measures to decrease undesirable occurrences

    such as flyrock. Blasting has some environmental impact such as ground vibration, air blast, dust

    and fumes and flyrock (Bhandadari, 1997). As an environmental hazard flyrock causes serious

    injury to people, damage to equipment, building and property. According to Roy (2005),

    blasting-induced flyrock can travel from a few meters to more than 1000 meters with poorlycontrolled blasting.

    DEFINITION OF TERMS

    Flyrock

    Flyrock, propelled rock fragments by explosive energy beyond the blast area, is one of the

    undesirable phenomena in the mining blasting operation (Rezaei et al. 2010). Any mismatch

    between distribution of the explosive energy, mechanical strength of the rock mass and charge

    confinement can be cause of flyrock (Bajpayee et al. 2004). Flyrock is produced when explosive

    energy is excessive for the amount of burden, stemming is inadequate or the energy is toorapidly vented through a zone of weakness in the rock. When this happens, much of the

    explosive energy is used to throw rock rather than to create fragmented rock (Roy, 2005).

    Flyrock is the source of most of the injuries and property damage in a majority of blasting

    accidents in surface mines.

    Causes of Flyrock

    Flyrock may have different causes depending on the place and situation of this phenomena.

    The following factors can lead to flyrock. The first one is related to inadequate burden and

    spacing. Burden and spacing need to be calculated taking into account the hole diameter, rock

    characteristics and fragmentation requirements. An insufficient (or less) burden will cause

    breakthrough of drill hole charges, resulting in flyrock. Spacing appreciably less than the burdentend to cause premature splitting between blast holes and early loosening of the stemming. Too

    close a spacing causes crushing between holes and also cratering giving rise to flyrock

    (Bhandadari, 1997). The other one is overloaded holes. The distance to which a flyrock travels

    will depend on the amount of specific charge. A high specific charge throws flyrock to a longer

    distance than a low specific charge. Inadequate stemming is also very important in flyrock

    distance. If stemming column is adequate, the explosion gases are not forced to heave up the

    partly fractured ground but are simply allowed to rifle out of the top of the blasthole at very

    high velocity causing considerable flyrock (Roy, 2005). The other significant parameter is

    inaccurate drilling. Accurate drilling provides proper burden and spacing which are essential for

    better results. This is achieved by proper positioning of drill to accurately collar the hole and by

    proper inclination of holes. However, if during drilling, the driller is not guided properly for the

    position and direction of the hole, the drill may deviate from its calculated position and duringthe time of blast the effect may be same as that of reduced burden and overloaded hole thereby

    resulting in flyrock (Bhandadari, 1997). The other cause is geological conditions. Zone of

    weakness and voids are often causes of flyrock. Any explosive loaded in this zone will have the

    line of least resistance and blow out, causing flyrock (Roy, 2005). Other factors such as

    powder factor, pattern layout, delay sequence should also be evaluated if any excessive flyrock

    is generated.

    Powder Factor and Specific Charge

    Two terms are often used to relate explosive mass and consequent rock broken: Powder

    factor and Specific charge, q. observation of blast designs based on empirical relations has beenoften indicated in terms of powder factors. Powder factor is the ratio between the total weights

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    of explosive detonated in a blast divided by the amount of rock that is broken. It is usually

    expressed as kilogram per ton or kilogram per meter. As the powder factor in kg/m3 increases,

    the average fragment size decreases when the burden B, remains constant (Hemphill, 1981). The

    powder factor varies between 0.1 (kg/m3) and 0.53 (kg/m

    3) for bench blasting. Powder factor for

    tunneling should be larger by 1.25-1.5 times than bench blasting because of the large fixity(Bhandari, 1997).

    History of Flyrock Accidents

    In a survey of blasting operations carried out in USA, it was observed that out of 34

    accidents that occurred during scheduled blasting, 28 were attributed to flyrock (Britton et al.

    1977). These accidents resulted in 10 fatalities and 19 injuries. A study of blasting accidents in

    India mines indicated that more than 40% fatal and 20% serious accidents resulting from

    blasting occurred due to flyrock (Bhandari, 1994). In the United Kingdom during 1980-85 103

    incidents were reported of which more than half of these involved flyrock projections to distance

    ranging from 350 m to a maximum of 900 m, with rock weighting up to 500 kg. According MineSafety and Health Administration, flyrock is the leading cause of blasting accidents, accounting

    over 60 percent of all accidents during 1987-88 (Anon, 1990). Historical data summarized by

    Verakis and Lobb (2003) shows that for the period of 19782001, a total of 195 blasting

    accidents occurred in US surface coal mine operations. Of the 195 accidents, 89 accidents

    (45.64%) were directly attributed to lack of blast area security, 54 accidents (27.69%) to flyrock,

    33 (16.92%) to premature blast, and 11 (5.64%) to misfires.

    FLYROCK ACCIDENT IN MALAYSIA

    Case Study

    The Masai quarry is situated in Seri Alam near Pasir Gudang, Johor, Malaysia. The mentioned

    quarry is producing granite aggregates for various construction uses with capacity of 30000 per

    month. Blasting is carried out between 2-4 times per month at this quarry. Figures 1 and 2 show

    the location of the quarry and the affected areas. Area of blasting also is shown in Figure 3.

    Figure 1:Location of Blasting Site

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    Figure 2:The Location of the Quarry Face and wild Stone Fly (550 m from the site of the

    explosion shown yellow arrows)

    Figure 3:The Blasting Area

    Flyrock Accident

    A flyrock accident was occurred due to a blasting in Masai quarry near the Seri Alam, Johor,Malaysia in 19 July 2013. The massive explosion caused rocks and boulders to rain down on the

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    Figure 5:Wild Flyrock into the Plant (350 m from the blasting site)

    Figure 6:Some Rocks resulted from Wild Flyrock (350 m from the blasting site)

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    Figure 7:Thrown Rocks on the Plant, Located 550 m from the Blasting Site

    Figure 8:Some Damages to Vehicles Around the Plastic Factory

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    Figure 9:The View of the Plastic Factory where the Worker Was Killed

    POWDER FACTOR ANALYSIS

    Parameters such as burden, spacing, powder factor, stemming length, subdrilling, maximum

    charge per delay and so on can affected in blasting results. Among them, powder factor has

    pivotal influence in blasting results such as flyrock distance. Powder factor is the ratio betweenthe total weights of explosive detonated in a blast divided by the amount of rock that is broken.

    It is usually expressed as kilogram per cubic meter. In this paper, two continues blasting patterns

    are shown and the powder factors of these blasting are compered. Some blasting parameters are

    shown in Figure 10 schematically.

    Figure 10:Some Blasting Parameters

    Figure 11 and Table 1 show blasting parameters for the last blasting before accident one.

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    ANFO was used as explosive material. Accoring to these blasting parameters, the powder factor

    for this blast is 0.619 kg/m3. The normal powder factor in the Masai quarry is between 0.6-0.8.

    Figure 12 and Table 2 also show blasting parameters for the accident blasting. The powder

    factor for this blasting is 1.18 kg/m3. It was found that the blast geometry played a great role in

    this accident. Some parameters of blast geometry such as hole diameter were consideredconstant in both blasting while some other parameters such as burden and spacing were changed

    in the accident one. It is worthy to note that total weight of explosive is another important

    parameter in the result of blasting. In the almost similar volume of the rock, this is a significant

    point in order to minimize environmental impacts of blasting like flyrock.

    Figure 11:Blast Geometry for the Last Blasting before Accident One

    Table 1:Blasting Parameter for the Last Blasting before Accident One

    Property

    Blasting Parameters

    Holediameter

    Holedepth

    Averagehole depth

    Numberof holes

    Averagestemming

    Averagecharge

    Value 89 26-30 28 39 2 194.1

    Unit mm m m - m kg

    Figure 12:Blast Geometry for the Accident One

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    Table 2:Blasting Parameter for the Accident One

    Property

    Blasting Parameters

    Hole

    diameter

    Hole

    depth

    Average

    hole depth

    Number

    of holes

    Average

    stemming

    Average

    charge

    Value 89 28-32 30 45 2 209

    Unit mm m m - m kg

    STEREOGRAPHICAL PROJECTION ANALYSIS

    A total of four joint sets have been identified around the explosion site (Figure 13). These

    discontinuities occur naturally (as a result of tectonic activity and weathering) and some new

    cracks because of earlier blasting work. In order to have a better geological investigation,

    stereographical analysis was perform. Stereographical analysis results (Figure 14) show the

    existence of joint dominant orientation (set 1, 2, 3 and 4) that contribute to the instability

    towards the south (toward the plant involved). This proves that the orientation of the

    discontinuity that exists is made of rock blasted become easier to excavate.

    Figure 13:Four Joint Sets Found in the Blasting Site

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    Figure 14:Analysis of Discontinuity Stereographical Analysis

    DISCUSSION

    There are several causes for this accident. The first is from the skills of trained person

    responsible for handling explosives. Error handling explosives operators not only endanger

    themselves, but other workers may also be involved. More serious when there are civilians

    directly involved in quarrying activities can also be considered. Explosives operators need not

    only well versed in handling quantity and type of materials to be used but also they should be

    able to control the situation.

    The second is geological conditions that cannot be altered and should be understood by the

    project proponent. Geological aspect is very important to be aware but there is no body that

    makes rules that professional geologists should make periodic reports. There is a discontinuity orcrack rock mass that affects the activity of an explosion. If there are a lot of cracks, and also

    orientation sets of discontinuity that causes low stability, the total explosion energy must be

    reduced. Sometimes these cracks not visible to the naked eye deck and can only be expected by

    an experienced geologist.

    The third cause of this accident is designing the blast geometry. In every blasting operation,

    blast geometry such as burden and spacing plays an important role in the blasting result. An

    insufficient (or less) burden will cause breakthrough of drill hole charges, resulting in flyrock.

    Spacing appreciably less than the burden tend to cause premature splitting between blast holes

    and early loosening of the stemming. Too close a spacing causes crushing between holes and

    also cratering giving rise to flyrock.

    Close distance between the quarry and the residential area is another factor that should begiven attention. The shortest distance between the face of the quarry to the plant explosion, is at

    a distance of only 350 m. This distance is too close. Under the guidelines of Environmental

    Impact Assessment (EIA) should be positioned closest to the development of not less than 1 km

    from the quarry. In this situation, many factory workers who worked in a plant is exposed to the

    risk of yesteryear. An estimated total of more than 500 factory workers working in this danger

    zone.

    CONCLUSION

    A flyrock accident was occurred due to a blasting in Masai quarry near the Seri Alam, johor,

    Malaysia in July of 2013. Due to this accident, a factory worker was killed while 10 others were

    injured after being hit by rock debris from an explosion at a quarry. Beside this, 18 cars and 14

    factories along the road were damaged. In order to investigate causes of this accident, two

    continues blasting patterns were considered and powder factor of these blasts were calculated.

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    Some parameters of blast geometry such as hole diameter were considered constant in both

    blasting while some other parameters such as burden and spacing were changed in the accident

    one. The powder factor of two continues blasting was 0.619 and 1.18 respectively. Apart from

    the powder factor analysis, stereographical analysis was also perform to recognize instability of

    blasting face. It can be concluded that blast geometry (such as burden and spacing), total weightof explosive, close distance between the quarry and the residential area, and geological

    conditions were considered the most influential parameters in this accident.

    ACKNOWLEDGEMENTS

    This research is being carried out using the Universiti Teknologi Malaysia (UTM) financial

    support. The authors would like to thanks UTM for the research grant and facilities available in

    the Department of Geotechnics and Transportation, Faculty of Civil Engineering.

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