Soils are acid/base systems which have the ability to absorb
and release metals which have been introduced into the soil by anthropogenic or
natural means. Soils are naturally acidic or alkaline based on their bedrock
and climatic conditions. This measure of acidity or alkalinity in soils is
important as it directly affects the growth of plants and the leach of heavy
metals into soils which will cause crop contaminations.
In alkaline soils, i.e. sodic soils, plant growth is poor
due to competition of sodium ions with other important ions such as magnesium
and potassium for uptake in plant roots. However, alkaline soils have excesses
of base cations which can bond with oxidised heavy metals (metal oxides) to fix
heavy metals in soil. Alkaline soils thus are less likely to cause health problems
when contaminated with heavy metals, but this is dependent on the type of metal
oxides present in soil solution. However, these soils are too salty for crop growth.
Picture showing Sodic Soils. Taken on 2 October 2014 in Inner Mongolia, China. Sodium salt levels are very high, with salts crystallizing to form a white layer on top. Nearby lake is salty as well.
In acidic soils, the problem of heavy metal contamination is
more serious than in alkaline soils due to the release of metals bonded on soil
surfaces into the soil solution. In places where acid rain from nearby
polluting factories acidifies soils, aluminium is leached into soils when
pH<4. Aluminium ions are toxic to plants and retards plant root growth
(Krstic et al. 2012). Besides, as aluminium has 3 free electrons for bonding, after
being leached out, negative soil surface adsorbs other metal ions available and
causes nutrient deficiency in plants. However, addition of hydrogen ions also replaces
metal ions in soils and releases metals, but the overall effect of adsorption
is higher as aluminium has 3 free electrons for bonding as compared to a
hydrogen ion which only has one.
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