Hanna Instruments HI 3896 User Manual

Page 4

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4

The physical structure of the soil depends on the dimension of the particles of its make up
(Tab. 1). In addition, the particles also differ based on their shape and volumic mass (mass
per unit of volume)

DIAMETER OF THE PARTICLES (mm)

CLASSIFICATION

> 2

stony texture

2 - 0.2

coarse sand

0.2 - 0.02

fine sand

0.02 - 0.002

silt

< 0.002

clay

Soil is divided into many classes of texture, according to the percentage of the basic
particles (clay, sand and silt). If, for example, we have a soil with 37% clay, 38% sand
and 25% silt, the soil is classified as “clay loam” (Fig. 2).

PHYSICAL STRUCTURE

Tab. 1. Particles
classification according to
“International Society of
Soil Science” (ISSS)

Fig. 2. Types of soil in
relation to the texture

Among different types of soil, the loam soil is considered as being suitable for crop
growth. However, other types of soil, with a rational management, can also provide
positive results.
The soil texture is the cause of important aspects such as porosity, tenacity, adhesivity
and plasticity.

13

Apple

very low

150

120

230

low

130

90

150

medium

110

70

120

medium-high

90

50

90

high

80

40

60

very high

70

20

40

Grape

very low

150

90

230

low

120

70

180

medium

100

60

150

medium-high

90

40

120

high

80

30

90

very high

70

20

60

Peach

very low

200

120

230

low

160

90

150

medium

140

70

120

medium-high

120

50

90

high

100

40

60

very high

80

20

40

Pear

very low

150

120

230

low

130

90

150

medium

110

70

120

medium-high

90

50

90

high

80

40

60

very high

70

20

40

The soil analysis is very useful, in order to plan fertilization and to know the residues of
fertilizers in relation to the crop, tillage and climate. An analysis can highlight shortages
and help the understanding of the causes of an abnormal growth.
Testing the soil during the crop cycle and comparing the results with the plant growth can
be an useful experiment for the next cultivation.

1) Extracting Soil Sample

– With a large field, take 1 or 2 samples per 1000 m2 (0.25 acre) of homogeneous

areas.

– Even for smaller areas, 2 samples are recommended (the more the samples, the

better the end-results, because the sample is more representative)

– For a small garden or plot, 1 sample is sufficient

2) Avoid extracting samples from soil presenting obvious anomalies
3) Sample quantity:

Take the same quantity of soil for each sample. For example, use bags with similar
dimensions (1 bag per sample)

CROP

SOIL CONTENT

ADVISED DOSES (kg/ha)

N

P

2

O

5

K

2

O

Tab. 7.

SOIL ANALYSIS

Sampling

(data ESAV)

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