Technically you do not "neutralize" salts in soils. What you want to do is dissolve and remove them.
For container plants, flush repeatedly with fresh clean water.
Considerable amounts of water are needed for flowerbeds, lawns, gardens or large plots of land in most parts of the world. Fields are normally irrigated with enough water to dissolve and wash the salts out of the root zone for the plants you are growing.
It is also very important to know whether any of the salts are sodium salts. If sodium salts are present (this is a saline-sodic soil) in a garden, yard or farm field, the sodium must first be displaced by another cation, like calcium, before flushing the soil with water. Gypsum is typically added to supply the calcium. If this is not done first, the soil structure will be ruined, and the field or garden will have to be flooded again after calcium is supplied to it, wasting time, money and soil productivity.Another (longer term) idea...In Australia where there is a problem of sodic soils there are plantings of certain species that absorb the salt into their leaves to reduce the level in the soil. These can then be culled and the soil used. This may not be practical on a small scale though! Or if your in a hurry! The types of plants used are saltbushes, atriplex, myoporums, and some melaleucas although all countries have their own salt - tolerant species. Most are fast growing and small. In the meantime you could try growing asparagus... you are supposed to add salt when planting!
Neutralization is impossible; the unique possibility is to wash salt from soil with water.
Another name for saturated soil could be soil liquefaction.
it acts like soil and transforms in to it
Soil is saturated when it has reached its maximum water content; if any more is added, it will either drain downward or turn the soil into mud.
Saturated thixotropic soil.
Nitrogen enriched soil and chemicals are typically used as fertilizer to improve soil.
by forehead training
poured salt onto soil
Saturated hydraulic conductivity is a quantitative measure of a saturated soil's ability to transmit water when subjected to a hydraulic gradient. It can be thought of as the ease with which pores of a saturated soil permit water movement.
In polluted soil or water areas, this is used to neutralize contamination.
when the voids of soil are just filled by water the soil mass is called saturated and when soil mass is submerged in water means the water level is above the the soil level or soil mass is drowned in water then soil mass is called submerged.