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218<br />

(h) Some <strong>of</strong> the waters, especially those arising in the Malmesbury and Cretaceous<br />

beds, approximate sea water in terms <strong>of</strong> given ionic concentrations.<br />

Group B: Slightly saline chloride waters<br />

(a) TDS values are in the range 300 - 350 mg 1"1.<br />

(b) With the further exception <strong>of</strong> a lower SO4 content, there is little difference in<br />

percentage composition between the waters <strong>of</strong> Group A and Group B.<br />

(c) Waters <strong>of</strong> the Table Mountain Series in Natal and in the Cape ProVince, and waters<br />

arising in the Witteberg quartzites in the Cape have been placed in Group E,<br />

although in terms <strong>of</strong> percentage composition these waters approximate to Group<br />

B in view <strong>of</strong> the high chloride content (>31 %).<br />

Group C: Temporary hard (carbonatel waters<br />

(a) TDS values are generally in the range 250 - 400 mg 1" 1 .<br />

(b) The SiO z content is moderately low ranging from 6,5 - 11,0%.<br />

(c) Low concentrations <strong>of</strong> chlorides in the range 5 - 8% are evident.<br />

(d) The pH is consistently high with an approximate mean <strong>of</strong> 7,8.<br />

(el A relatively very high temporary hardness is the main .characteristic <strong>of</strong> Group C<br />

waters. Approximately 68 - 90% <strong>of</strong> the TDS consists <strong>of</strong> Ca(HC0 3 )z and<br />

Mg(HC0 3 )z' There is very little permanent hardness.<br />

(f) Waters arising in the basic and ultra basic rocks <strong>of</strong> the Bushveld Igneous Complex<br />

(especially in the pyroxenic and ultra basic rocks' could be allocated to a sub-group,<br />

given that these waters consist very largely <strong>of</strong> Mg(HC0 3 '2 with an appreciable<br />

silica content. Ca(HC0 3'z is present in very small amounts.

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