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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THE SOILS<br />
For instance <strong>the</strong> concept <strong>of</strong> a certain taxonomic unit may require shallow<br />
soils over limestone rock. Then <strong>the</strong> range in soil depth allowed within that<br />
taxonomic unit is from 25 to 50 cm.<br />
The most comprehensive taxonomic classification system available to date is<br />
<strong>the</strong> USDA <strong>Soil</strong> Taxonomy (<strong>Soil</strong> <strong>Survey</strong> <strong>St</strong>aff 1975 and 1987). This system has<br />
been used by <strong>the</strong> staff <strong>of</strong> <strong>the</strong> RPPD since 1978.<br />
The USDA <strong>Soil</strong> Taxonomy presents <strong>the</strong> following advantages:<br />
- it enables an understanding <strong>of</strong> <strong>the</strong> relationships between soils and <strong>the</strong>ir<br />
environment, thus allowing for <strong>the</strong> comparison or transfer <strong>of</strong> knowledge<br />
between similar geographical locations, both nationally and internationally<br />
- it can be used to distinguish well defined mapping units during <strong>the</strong> survey<br />
- it provides a basis for <strong>the</strong> interpretation <strong>of</strong> soil data for selected kinds <strong>of</strong><br />
land use (i.e. land evaluation).<br />
4.2.2 The use <strong>of</strong> USDA <strong>Soil</strong> Taxonomy in Jamaica<br />
The USDA <strong>Soil</strong> Taxonomy is a hierarchical system in that units at <strong>the</strong> highest<br />
level <strong>of</strong> generalization are subdivided into more <strong>detailed</strong> sub-units, which<br />
are in turn fur<strong>the</strong>r subdivided and so on. The hierarchical sequence in <strong>the</strong><br />
successive categories from high to low is as follows:<br />
ORDERS-SUBORDERS-GREAT GROUPS-SUBGROUPS-FAMILIES-SERIES.<br />
The grouping <strong>of</strong> soils in a specific unit at each level is based on combinations<br />
<strong>of</strong> relatively permanent diagnostic soil characteristics, whose occurrence and<br />
range can be established by relatively simple measurements and<br />
observations in <strong>the</strong> field and laboratory (e.g. texture, colour, soil reaction,<br />
depth to bedrock, soil temperature, cation exchange capacity, organic carbon<br />
content). From <strong>the</strong> level <strong>of</strong> <strong>the</strong> orders down to that <strong>of</strong> <strong>the</strong> series <strong>the</strong><br />
diagnostic characteristics become more narrowly defined.<br />
ORDERS consist <strong>of</strong> soils with similar properties, resulting from <strong>the</strong> same soil<br />
forming processes, which acted to <strong>the</strong> same degree on <strong>the</strong> parent material or<br />
rock. Six out <strong>of</strong> <strong>the</strong> ten orders that are recognized by <strong>Soil</strong> Taxonomy have<br />
been identified in <strong>the</strong> Lluidas <strong>Vale</strong> survey. The dominant, generalized<br />
characteristics <strong>of</strong> <strong>the</strong>se orders are briefly discussed so as to enhance <strong>the</strong><br />
user's understanding <strong>of</strong> <strong>the</strong> technical classification which is used in Subchapter<br />
4.5 in <strong>the</strong> description <strong>of</strong> <strong>the</strong> soil mapping units. All details are<br />
explained in <strong>the</strong> Keys to <strong>Soil</strong> Taxonomy (<strong>Soil</strong> <strong>Survey</strong> <strong>St</strong>aff 1987).<br />
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