THE MOST IMPORTANT STEP WHEN INTENDING TO DRILL A
BOREHOLE IS UNDERTAKING A GEOPHYSICAL WATER
SURVEYING TEST WHICH IS VERY IMPORTANT IN
DETERMINING THE BEST POSSIBLE DRILLING LOCATION TO
DRILL A BOREHOLE. AS PER OUR MACHINERY SPECIFICATIONS
AND METHOD IN WHICH IT WORKS. THERE ARE 2 ASPECTS TO
DETERMINING THE DRILLING SPOT.
THE FIRST METHOD WILL BE THE LONG-RANGE SURVEYING
METHOD WHICH WE HAVE CONTROL OF AS TO SPECIFY THE
DEPTHS IN WHICH WE WOULD LIKE TO THE FAULT ZONE
WHICH IN MOST CASES IS SET TO A HORIZONTAL RANGE OF
400 METERS AND VERTICAL RANGE OF 150 METERS. THIS
METHOD IN ITSELF HAS 2 ASPECTS AS WELL. THE MACHINE
DETECT THE 2 CROSS DIRECTIONS WHEREBY THE FAULT ZONE
MEETS IN THE CENTER. FAULT ZONE IN SHORT WOULD BE
ROCK FORMATION THAT IS PERMEABLE AND HAS THE
POTENTIAL TO ALLOW WATER TO FLOW THROUGH IT
SHOULD THERE BE WATER.
THE SECOND PHASE TO THIS IS ONCE THE FAULT ZONE IS
IDENTIFIED. WE CAN NOW USE THE VLF SURVEY METHOD
WHICH WOULD IN TURN IS USED TO DETERMINE THE DEPTHS
AT WHICH THE ROCKS COULD BE POUROUS AND CAN
POTENTIALLY ALLOW WATER INTO THE BOREHOLE. THE
MACHINE DETECTS 3 POSSIBLE FRACTURE ZONES AND WE
CAN THEREBY EXPECT TO FIND WATER AT THE DEPTHS
SUGGESTED. THE DEPTHS SUGGESTED AREN’T ALWAYS 100 %
ACCURATE AND WE WILL HAVE TO DRILL MINIMUM
30METERS DEEPER THEN THE 3RD SUGGESTED FRACTURE
ZONE. THE MACHINE CANNOT DETECT WATER QUANTITY,
THAT WILL BE DEPENDANT ON THE AREA.
EXAMPLE OF PREVIOUS SURVEY ATTACHED BELOW