7.1 Factors
affecting soil strength
(1) Moisture content
When soils are saturated or waterlogged,
soils are relatively weaker, therefore, soils can be easily broken down.
Soils
cannot be easily broken down because of dry conditions. Therefore these soils
are more strength.
(2) Bulk density
When
soils have low bulk density, these soils can be easily broken down because
these soils consist of relatively more pores so mass per unit volume is
relatively low. Therefore soil can be easily broken down.
Soils
cannot be easily broken down because when the soil has a high bulk density that’s
mean, the soil has relatively lower pores so mass per unit volume is relatively
high.
(3) Structure
When
soils are well aggregated like clay soils, the soils have relatively larger
strength. Sands, sandy loams and loamy sands have relatively smaller strength
because these soils aren’t well aggregated.
7.2 Importance of soil
strength
1)
Germination of seeds
2)
Plant growth
Good aeration and well-drained of
soils are essential for the germination of seeds and the growth of plants.
7.3 Human effects on soil strength
Soil management practices for
agriculture are affected by soil strength badly. Compacted soil horizons called
Ap or E are formed due to the using of heavy machines for tillage practices.
Compacted soils have usually higher strength, therefore, the growth of plants and The germination of seeds is restricted.
7.4 Measuring of soil strength penetrometers
Penetrometers are used to
measure soil strength. A rod is entered into the soil by inserting force
that the required force is used to measure the soil strength. Therefore we can recognize the affection of
compaction soils to the growth of plant and germination of seeds by resistance to the exert of a rod into the soil.
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