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the vegetation types and veld condition - Maremani Nature Reserve

the vegetation types and veld condition - Maremani Nature Reserve

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L<strong>and</strong> Types <strong>and</strong> soils<br />

Nine l<strong>and</strong> <strong>types</strong> have been described <strong>and</strong> mapped for <strong>the</strong> area. These are: L<strong>and</strong> <strong>types</strong> Ib314, Ah88,<br />

Ah89, Ah91, Fc482, Fc483, Fc484, Ae265 <strong>and</strong> Ae266.<br />

The Ib314 l<strong>and</strong> type is described as ‘rocky areas with miscellaneous soils’ <strong>and</strong> covers part of <strong>the</strong> hilly<br />

areas in <strong>the</strong> north. Soils are derived from gneiss <strong>and</strong> quartzite.<br />

The Ah88 l<strong>and</strong> type has reddish s<strong>and</strong>y clay loam soils derived from dolerite, with a high clay content. The<br />

Ah89 l<strong>and</strong> type is characterised by reddish loamy s<strong>and</strong> to s<strong>and</strong>y loam derived from gneiss, <strong>and</strong> <strong>the</strong> Ah91<br />

l<strong>and</strong> type has red <strong>and</strong> yellow loamy s<strong>and</strong> derived from shale, mudstone <strong>and</strong> siltstone, with a clay content<br />

of less than 15%.<br />

In <strong>the</strong> Fc l<strong>and</strong> <strong>types</strong> calcrete <strong>and</strong> calcareous soils are present. The Fc482 l<strong>and</strong> type is characterised by<br />

loamy s<strong>and</strong> derived from s<strong>and</strong>stone, calc-silicate <strong>and</strong> quartzite, <strong>the</strong> Fc483 l<strong>and</strong> type has s<strong>and</strong>y loam soils<br />

derived from gneiss, <strong>and</strong> <strong>the</strong> Fc484 l<strong>and</strong> type has loam s<strong>and</strong>y soils derived from gneiss <strong>and</strong> quartzite.<br />

The Ae265 l<strong>and</strong> type consists of reddish s<strong>and</strong>y loam to s<strong>and</strong>y clay loam soils derived from basalt. The<br />

soils are usually deeper than 300 mm. Within <strong>the</strong> Ae266 l<strong>and</strong> type reddish s<strong>and</strong>y loam soils, derived<br />

from gneiss, are found.<br />

Soils derived from gneiss, quartzite <strong>and</strong> s<strong>and</strong>stone are usually leached <strong>and</strong> have a low nutrient content<br />

whereas soils derived from shale, siltstone, mudstone, dolerite <strong>and</strong> basalt are usually more clayey <strong>and</strong><br />

have a higher nutrient content <strong>and</strong> water-holding capacity.<br />

Silty <strong>and</strong> clayey alluvial soils occur on flood plains along <strong>the</strong> Limpopo <strong>and</strong> Njelele Rivers as well as along<br />

streams <strong>and</strong> in <strong>the</strong> wetl<strong>and</strong> of <strong>the</strong> Mutanga River in <strong>the</strong> south of <strong>the</strong> farm Solitude.<br />

Climate<br />

The mean annual rainfall for <strong>the</strong> <strong>Maremani</strong> area varies from 331 mm at Messina in <strong>the</strong> west to 342 mm at<br />

Tshipise in <strong>the</strong> south (Tables 1 & 2; Erasmus 1987; Wea<strong>the</strong>r Bureau 1988). The rainy season is<br />

predominantly from October to March, with approximately 85% of <strong>the</strong> mean annual rainfall occurring<br />

during <strong>the</strong>se months. The driest months are from June to August (Table 1 <strong>and</strong> Figure 1). The maximum<br />

rainfall measured in 24 hours was 167 mm (Table 3). Evaporation is much higher than <strong>the</strong> annual rainfall.<br />

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