Semi-detailed Soil Survey of the LIuidas Vale Area, St. Catherine-St ...
Semi-detailed Soil Survey of the LIuidas Vale Area, St. Catherine-St ...
Semi-detailed Soil Survey of the LIuidas Vale Area, St. Catherine-St ...
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MATERIALS AND METHODS<br />
selected on map sheet 84C, two <strong>of</strong> which were located in <strong>the</strong> hills and two in<br />
<strong>the</strong> inland basin. These sample areas were expected to show <strong>the</strong> majority <strong>of</strong><br />
<strong>the</strong> soils and <strong>the</strong>ir physiographic relations. The location <strong>of</strong> <strong>the</strong> sample areas<br />
is indicated in Figure 1. The toposheets 84A and 84C (1:12,500) were used as<br />
field maps; <strong>the</strong> boundaries <strong>of</strong> <strong>the</strong> API units and sample areas were manually<br />
transferred to <strong>the</strong>se maps.<br />
The slope map was prepared from a 1:25,000 copy <strong>of</strong> <strong>the</strong> base map; <strong>the</strong><br />
areas <strong>of</strong> different slope classes were identified with <strong>the</strong> help <strong>of</strong> a transparent<br />
sheet on which <strong>the</strong> distances <strong>of</strong> <strong>the</strong> contour lines were indicated at 2, 5, 8,<br />
16, 30 and 50% slopes, <strong>the</strong> so-called slope-ruler.<br />
The base map for <strong>the</strong> final soil map at scale 1:25,000 was prepared from <strong>the</strong><br />
reduced toposheets 84A and 84C From <strong>the</strong> reduced map, a sepia copy was<br />
derived through Xerox, after which ano<strong>the</strong>r copy was prepared at sepia film.<br />
The soil boundaries were drawn on this sepia film copy, so that <strong>the</strong> final soil<br />
map has a subdued background <strong>of</strong> <strong>the</strong> topographical features.<br />
3.2 FIELD PROCEDURES<br />
The field work was carried out mainly in two periods: June 1986 and late<br />
1988/early 1989. The majority <strong>of</strong> <strong>the</strong> observations for map sheet 84C and all<br />
for map sheet 84A were done in <strong>the</strong> latter period.<br />
Auger borings and pr<strong>of</strong>ile pits were used for <strong>the</strong> characterization <strong>of</strong> <strong>the</strong><br />
various soils. In <strong>the</strong> sample areas auger observations were done along<br />
transects and <strong>the</strong> remaining observations were made according to <strong>the</strong> "free<br />
survey" technique. A total <strong>of</strong> 263 observations was made (on average: 1<br />
observation/42 ha, with about a double density <strong>of</strong> observations in <strong>the</strong> inland<br />
basins).<br />
A total <strong>of</strong> 30 pr<strong>of</strong>ile pits was described, 22 <strong>of</strong> which are presented in this<br />
report. These 22 pits are <strong>the</strong> best representatives <strong>of</strong> <strong>the</strong> identified soil series,<br />
and have complete soil description and analytical data. Each pit was 1 m by<br />
1.5 m wide and 150 cm deep or to <strong>the</strong> bedrock, whichever was shallower.<br />
The soils are described according to <strong>the</strong> Guidelines for Pr<strong>of</strong>ile Description<br />
(SSU 1989a), partially based on <strong>the</strong> Guidelines from FAO (1977). The colour<br />
notation is according to <strong>the</strong> Munsell <strong>Soil</strong> Color Charts (Munsell 1975). From<br />
each horizon described, a bulk sample was taken for chemical and textural<br />
analyses. Samples from selected horizons were taken for moisture<br />
availability determination. An additional set <strong>of</strong> samples was taken from each<br />
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