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Pl. 6.? Pl. 63 400 Serowe - Cave sandstone in foreground. Dyke forms hills in distance. Well point - Motloutse Sand River. I I
Page 14: 411 TABLE 52 ESTIMATED AVERAGE MONT
Page 29: 425 in this case, not apparently al
Page 33: 429 HYDROCHEHISTRY In 1969 a resear
Page 50: 446 SAND RIVER STORAGE INTRODUCTION
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• 467 GROUND 1"rATER MOVEMENT, \"
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478 The coefficient of transmissibi
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-_ .. -__ 1
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500 -
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502
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508 TABLE 65 VALUES FOR T AND S PUM
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519 These are largely unexploited a
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I I _ _ . ____ . ___ ... _ _ . _. _
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decline in efficiency takes place w
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552 PI.68 Air Drilling...;; Letlakh
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TABLE 74 BOREHOLES SHOWING REDUCED
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TAB L E 75 GENERAL BOREHOLE STATIST
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582 formations for yielding water a
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Kweneng District. Following the del
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608 Instrumentation Originally a co
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611 the depths to different litholo
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617 This preject forms a pioneering
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629 TABLE 76 (, ' . . ;" • Lab.No
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646 Tritium in Southern African Rai
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649 polation to 19S5, are given in
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666 Values as low as 0,8 TU have, o
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4. other (older ) water is being dr
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686 postulated ground-water flow aw
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715 lLo History of use of rC in Bot
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6. 728 Interpretation of the presen
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752 (2) The storage coefficient, S#
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co U\ t- MONTH JULY AUG,. SEPT. OCT
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o \D r:- MONTH JULY AUG. SEPT. OCT.
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777 piezometric surface in borehole
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787 Observation of water levels and
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7J \ the clearing of all vegetation
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8 01 rocks and hence develop a clay
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f . 811 Ttie third assumption is th
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= 0,40 cents/hour Total running cos
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( 821 be referred to whenever neces
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823 GROUND WATER TEMPERATURES Intro
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Jans Draai Kransl)rak Kyky Grootbra
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839 In practice the acceptability o
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Sekhuma Pan 1vells Sir R. Englands
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F I , . '.
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Details of ground-water chemistry a
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