asl |
Above sea level |
AvK |
Available potassium |
AvP |
Available Phosphate |
AWC |
Available water capacity (amount of water held in soil at suctions in the range for root uptake; = MC%@ FC – MC% @PWP) |
BCI |
Barro Colorado Island |
BCNM |
Barro Colorado Nature Monument |
BS% |
Base saturation percentage (=TEB/CEC) |
C |
Clay. Finest size class of mineral particles (< 0.002 mm) |
Catapan |
Catastro de Panama (CRA) |
CEC |
Cation exchange capacity (conventionally determined at pH7) |
CL |
Clay loam |
COLE |
Coefficient of linear extension (%) |
Colluvium |
Local hillwash, moved by overland flow and slow creep. |
Complex |
Soil mapping unit with several co-dominant classes. |
Consociation |
Soil mapping unit with one soil class dominant and others as minor constituents. |
CRA |
Comision de Reforma Agraria (MIDA) |
Creep |
Slow gravitational mass movement of colluvium downslope. |
CTFS |
Center for Tropical Forest Science |
C/V |
Chroma and value in Munsell Soil Color coding system |
Dbh, drh |
Diameter at breast (1.3 m above ground level) or reference (0.6 m above the highest buttress) height |
EBS |
Effective base saturation (= TEB/ECEC as %) |
ECEC |
Effective cation exchange capacity (=TEB + Extr Al) |
Eluvial |
Soil horizon formed by the selective washing out of some original components |
Exch |
Exchangeable cations extractable with 1M NH4OOCH3 |
Extr |
Extractable with 1M KCl |
FAO |
Food & Agriculture Organisation of United Nations |
FC |
Field capacity (MC% at suction of 0.1 or 0.3 atmosphere) |
Fine earth |
Fraction of soil with particle size < 2mm |
gibb |
Gibbsite (Al2O3 clay mineral) |
gilgai |
Dynamic soil surface undulations due to shrink-swell of expansible clays in seasonal climates |
GIS |
Geographical information system |
Gley |
Soil that is permanently wet and poorly aerated, with predominantly greyish colours, due to the reduction of free iron. May have locally oxidised rust – coloured mottles as spots and around root channels. |
GPS |
Global positioning system |
HAC |
High activity clay |
Horizon |
Soil layer |
Hydrature |
Supply of air and water to biota by soil pore system (sensu White, 1985) |
ICP |
Induction coupled plasma spectrometer |
IGN |
Instituto Geografico Nacional, Tommy Guardia |
Illuvial |
Soil horizon formed by enrichment of some components washed in from eluvial horizon(s) above |
Kaol |
Kaolinite (1:1 aluminosilicate clay mineral) |
L |
Loam (Mixed soil with substantial proportions of all three of the main fine earth size classes, i.e. clay, silt and sand) |
LAC |
Low activity clay |
Linear |
Straight slope with similar gradients up- and downslope |
LTER |
Long term ecological research |
MC% |
Moisture content % (by mass) |
MIDA |
Ministerio de Desarollo Agropecuaria (RoP) |
Munsell |
System of soil colour notation, operated by matching soil against standard colour chips. Colour described by ‘hue’ (Spectral composition – red, yellow, blue, green); ‘value’ (dilution with multispectral white), & ‘chroma’ (darkness) |
ND |
No data |
NH4OOCH3 |
Ammonium acetate (1M, buffered at pH 7, for extracting exchangeable cations) |
OC |
Organic carbon |
PM |
Soil parent material |
Profile |
Sequence of soil horizons from surface to parent material |
PWP |
Permanent wilting [point (soil moisture suction of 15 atmospheres = 1.5 MPa) |
Regolith |
All surface materials; includes solum (true soil), saprolite (in situ weathered rock), and mobile materials like colluvium or alluvium. |
RoP |
Republic of Panama |
S |
Sand (coarsest fine earth particle size class, 0.05 – 2 mm in USDA) |
Series |
Equivalent to soil class on BCI. Sixth level of subdivision in USDA Soil Taxonomy. |
SI |
Smithsonian Institution |
Si |
Silt (intermediate fine earth mineral particle size class, 0.002 – 0.05 mm in USDA) |
Slickenside |
Striated, polished clay pressure face, usually oblique, on prismatic or wedge structures in expansible clay subsoils. Diagnostic of vertic properties and Vertisols in ST. |
SMR |
Soil Moisture Regime, as defined in ST |
SMU |
Soil mapping unit |
SOC |
Soil organic carbon |
Solum |
True soil, in which physicochemical and bio-turbation processes have obliterated visible traces of parent rock structure. |
SOM |
Soil organic matter |
ST |
Soil Taxonomy (USDA system of soil classification) |
STR |
Soil temperature regime, as defined in ST |
STRI |
Smithsonian Tropical Research Institute |
Surface wash |
Movement of detached surface soil particles by overland flow. |
Tr |
Trace |
Tufa |
Hard coating of secondary CaCO3 |
TEB |
Total exchangeable bases (= exchangeable Ca + Mg + Na + K) |
USDA |
United States Department of Agriculture |
WRB |
World Reference Base for Soil Resources (FAO system of soil classification) |
XRD |
X-ray diffraction (for determination of clay minerals) |
Z, Zi |
Silt (intermediate fine earth particle size class, 0.002 – 0.05 mm in USDA) |