Glossary

Wind Speed
The speed that the wind is travelling. Usually expressed as meters per second in research.
Wind Direction
The direction the wind is coming from. Expressed as compass points or degrees. For example, North-North-East (NNE)
Wind Vane Sampler (WVS)
Passive sediment trap used to collect sediment from the air stream. Can be used at various heights to characterise the range of sizes being collected. This trap also known in the wind erosion literature as the ‘Fryrear Trap’ and BSNE.
Hall Deposition Trap (HDT)
Passive sediment trap used to collect sediment falling out of the atmosphere.
Anemometer
Instrument used to measure wind speed.
Tell Tale
Small pieces of tape commonly tied to yacht rigging to indicate which direction the wind is blowing from.
Visibility
Technique used by the Bureau of Meteorology to estimate the amount of atmospheric particulates. Wind Erosion researchers are using the visibility measure to estimate the amount of dust. The distance reported, is as far as the observer can see an object clearly, expressed in either kilometres or metres.
Munsell Colour
A classification system used to describe the colour of soil according to the interaction of three variables: Hue, Value and Chroma. Hue notation of a colour indicates its relation to Red, Yellow, Green, Blue and Purple. Value notation indicates its lightness. Chroma notation indicates its strength.
Humidity
A measure of the amount of water vapour in the surrounding air mass.
Hydrometer
Used to calculate the amount of water vapour in the surrounding air mass. Also referred to as a ‘Hygrometer’.
Atmospheric Pressure
Force of molecules in air per volume at a predefined altitude.
Barometer
Instrument used to measure atmospheric pressure.
Soil Texture
The texture of a soil is the proportion of three size related particle groups; sand, silt and clay. Combinations of these three at different ratios produces different feeling soil.
Hand Texture
Technique of kneading soil in palm of hand to determine roughly the range of particle sizes present.
Aggregation
The binding of individual soil particles together forming clumps which improve the soil structure. These aggregates can also be move (transported) in the larger form (therefore referred to as transport stable aggregates).
Particle-size analysis
Techniques used to determine the proportion of different size particles making up the soil sample. Particles range from clays (<2 μm), silts (2–60 μm) to sands (>60 μm). A large range of methods are used to determine particle-size, each varying the resolution and accuracy.
Micron (μm)
Unit of measure. 1 mm = 1000 μm
Hydrometer Method
Simple technique used to determine the particle size of soil by utilising the settling velocity (density) of different sized particles. A soil sample is placed in a column of water stirred and measurements are made with a calibrated hydrometer to determine the size of particles. Density of water changes through time as the fraction of coarser particles sink.
Moisture Tins
Metal tins with push on lids used to oven dry soil for determination of soil water content.
Volumetric Cylinder
Tall laboratory glassware, cylindrical in shape, has a pouring spout and graduated in millilitres.
Soil Colour
Climate, organics, geomorphic history, parent rock and age alter the colour displayed by a soil.
Soil Cover
Proportion of organic and inorganic material lying on the soil surface.
Soil Moisture
Water content found between the soil particles.
Loose Erodible Material
The fraction of both mineral and organic particles which is lying freely on a soil surface. This material can potentially be transported by both wind and water. This can be tested using the KFC method (Kentucky Fried Chicken—finger lickin' good)!
Soil Biota
Organisms which live in the soil profile. For example, bacteria, cyanobacteria, nematodes, arthropods etc.
Quadrat
Frame used to define an area in which surface features or organisms are counted to provide a measure of frequency.
Percentage Cover
An estimation of the percentage area covered by different surface features, for example rocks, plants, leaf litter.
Step Point Technique
Characterisation of soil surfaces by walking a transect and noting surface feature at the point of each footfall.
Quadrat Method
Quantification of soil surface features by placing a quadrat at ‘x’ spacings and estimating percentage cover of various surface features.
Frontal Area Index
The vertical surface area of a plant as seen by the wind.
Vegetation type
Plant growth form varies in size, shape and duration. To help describe these differences plants are commonly grouped as grass, herbs, shrubs and trees.
Field guides
Small books used to help identify organisms whilst in the field. Guides will use pictures and written descriptions of the most characteristic diagnostic features.
Rainfall Intensity
The rate at which rainfall fell. Expressed as mm/hr.
Rain Gauge
Calibrated vessel used to calculate the volume of rainfall that has fallen.
Droplet Size
Rain drops vary in size from sub millimetre (fog) to > 5 mm (tropical thunderstorms) in diameter.
Overland Flow
Movement of water, usually from rainfall, over the soil surface towards a defined drainage system e.g stream.
Sediment Concentration
The quantity of sediment per unit of area per time.