Piling on alluvial land requires a special approach. Alluvial
soil typically consists of water-saturated sand with a very loose structure,
obtained by hydraulic flushing from quarries or dredging.
Specifics of Working
with Alluvial Soil
Alluvial soil differs from conventional backfill in the way
it is formed. With hydraulic filling, sand is added with a large amount of
water, settles in a designated area, and gradually dehydrates. This type of
soil has certain characteristics.
Characteristics of alluvial soil:
•
High
initial moisture content (30–40% or more)
•
Very
loose structure—porosity coefficient of 0.7–0.9
•
Unevenness
across the surface—in some areas, more large particles have settled, while in
others, more small ones have settled.
•
Continued
shrinkage under its own weight for 1–3 years.
•
Uneven density across depth.
The main problem with alluvial areas is that they continue
to compact for years after filling. If construction begins too early, the
foundation will settle along with the soil.
Technical Solutions for Alluvial Areas
When
working with alluvial soil, one must either wait for it to compact naturally
(1.5–3 years), employ special accelerated consolidation technologies, or use
long piles that will penetrate the entire alluvial layer.
Solution
options:
1. Use longer piles to reach dense
layers beneath the alluvial layer.
2. Install additional piles to reduce
the load on each pile (increments of 1.5–2 m instead of 2.5–3 m).
3. Use piles with a larger blade area
(diameter 300–350 mm instead of 250 mm).
4. Mandatory grillage for uniform load
distribution.
5. Install a drainage system to remove
excess moisture.
6. Monitor settlement during the first 2–3 years of operation using benchmarks.

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