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9.5.2 Immobilization or Phytostabilization
Immobilization refers to the vegetation’s ability to maintain contaminated soils and sediments
in place, as well as the immobilization of harmful pollutants in soils (Mukhopadhyay and Maiti
2010). In-situ inactivation or phyto immobilization are other terms for phytostabilization. Sorption,
precipitation, complexation and metal valence reduction are strategies that can help plants to
stabilize metals (Ghosh and Singh 2005). An in-situ remediation process is a suitable option for
metal remediation (Jadia and Fulekar 2009). Root-zone microbiology and chemistry, as well as
changes in the soil environment or contaminant chemistry, all, contribute to phytostabilization. Plant
root exudates or CO2 generation can modify the pH of the soil, that has a bearing on metal ion
transport. Phytostabilization can affect metal solubility and mobility, as well as organic compound
dissociation. Metals can be converted into an insoluble oxidation state from a soluble state in a
plant-affected soil environment (Salt et al. 1995). Plants can also help to prevent metal-contaminated
soil from eroding. Plants having elevated transpiration rates, like forage plants, grasses, reeds and
sedges, can help with phytostabilization that could be used for metal remediation. The approach of
utilizing trees, such as the densely rooted and perennial, in combination may be a good mix (Berti
and Cunningham 2000).
9.5.3 Phytovolatilization
Toxic metals, including mercury, selenium and arsenic, are capable of being biomethylated to
produce volatile substances that are discharged into the atmosphere. Phytovolatilization is the
mechanism which is involved in the reduction of pollutants via the transpiration of plants. The plant
absorbs the contaminant that is present in the water, passes through it, or undergoes transformation
there, then is released into the atmosphere. Water passes through the plant’s internal transport
mechanism circulating from roots up to the leaves, where the inorganics get evaporated or volatilized
and consequently released in the air enclosing the plant, potentially modifying the contaminant.
Using phytovolatilization and phytoextraction to remove metals from commercial projects is a
realistic option (Sakakibara et al. 2010). Tritium (3H), a radioactive isotope of hydrogen, has been
successfully phytovolatilized; it decomposes into a stable form of helium, having a half-life of about
12 yr. HMs can be absorbed by several plants, including Arabidopsis thaliana, Chara canescens and
Brassica juncea, converting them into their gaseous forms within plants, and then releasing them
back into the environment (Ghosh and Singh 2005). Dimethylselenides and dimethyldiselenides
are produced by plants (i.e., Brassica juncea and Arabidopsis thaliana), which are the volatile
forms of volatile Se when grown on a high Se medium. Similarly, data from a study on heavy
metal volatilization revealed that P. vittata is quite efficient at volatilizing Arsenic (As), as had been
documented by its removal by almost 90% of total intake from As-affected soils in a greenhouse
with subtropical conditions (Sakakibara et al. 2010). In contrast to the other ways of cleanup,
after toxins have been removed via volatilization, they cannot be stopped from spreading to other
areas. Similar occurrences of soil remediation based on volatilization have been recorded in many
other publications (Tangahu et al. 2011, Conesa et al. 2012). Although it is well recognized that
microbes dispense a significant function in the Se volatilization from soil systems (Karlson and
Frankenberger 1989), it was investigated that plants can fulfil the same job. B. juncea has been
recognized as a useful source for extracting Se from soils (Bauelos and Meek 1990, Baualos et al.
1993). The Se volatilization into methyl selenates has been hypothesized as a dominant mechanism
for plant Se elimination (Zayed and Terry 1994, Terry et al. 1992). Non-volatile methyl selenate
derivatives accumulate in the leaf of some plants, allowing them to extract Se from the soil. In the
Se accumulator Astragalus bisculatus, the enzyme that serves in producing methyl selenocysteine
was isolated and described (Neuhierl and Bock 1996).