Agriculture Reference
In-Depth Information
2
The Makeup of Soil
The Solid Phase
2.1
Minerals and organic matter comprise the solid phase of the soil. The geological
origin of the soil minerals, and the input of organic matter from plants and ani-
mals, are briefly discussed in section 1.2.1. A basic knowledge of the composition
and properties of these materials is fundamental to understanding how a soil in-
fluences the growth of grapevines.
Soil Mineral Matter
2.2
A striking feature of soil is the size range of the mineral matter, which varies from
boulders (
600 mm diameter), to stones and gravel (600 to
2 mm diameter),
to particles (
2 mm diameter)—the
fine earth
fraction.
The fine earth fraction is the most important because of the type of miner-
als present and their large surface areas. The ratio of surface area to volume de-
fines the
specific surface area
of a particle. The smaller the size of an object, the
larger is the ratio of its surface area to volume. This can be demonstrated by con-
sidering spherical particles of radius 0.1 mm, 0.01 mm, and 0.001 mm (1 mi-
crometer or micron,
m). The specific surface areas of these particles are 30, 300,
and 3000 mm
2
/mm
3
, respectively. In practice, the specific surface area is mea-
sured as the surface area per unit mass, which implies a constant particle density
(usually taken as 2.65 Mg/m
3
). A large specific surface area means that more mol-
ecules can be adsorbed on the surface. Representative values for the specific sur-
face areas of sand, silt, and clay-size minerals are given in table 2.1. Note the large
range in specific surface area, even for the clay minerals, from as little as 5 m
2
/g
for kaolinite to 750 m
2
/g for Na-montmorillonite.
Because specific surface areas are important, we need to know the size distri-
bution of particles in the fine earth fraction. This is expressed as the soil's
texture
.
The types of minerals that make up the individual size fractions are also impor-
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