Page 208 - Materials Chemistry, Second Edition
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Vadose Zone Soil Remediation                                     191



           most popular format. This approach treats soil stockpiled on the site with per-
           forated pipes embedded in the piles as the conduit for air supply. To minimize
           fugitive emission and potential secondary contamination from leachates, the
           stockpiles are usually covered on the top and lined at the bottom.
             In situ treatment enhances the natural microbial activity of undisturbed
           soil in place to decompose organic COCs. A nutrient solution is often per-
           colated or injected into the subsurface to support the activities of the bio-
           degraders. Run-on  and run-off  controls  and waste containment  are  often
           required. In a slurry bioreactor, impacted soil is mixed with a nutrient solu-
           tion under controlled operating conditions (i.e., optimal pH, temperature,
           dissolved oxygen, and mixing).
             Microorganisms require moisture, oxygen (or absence of oxygen for
           anaerobic biodegradation), nutrients, and a suitable set of environmental
           factors  to grow. The environmental factors  include pH, temperature, and
           absence of toxic conditions. Table 5.2 summarizes the critical conditions for
           bioremediation.

           5.4.2   Moisture Requirement

           As shown in Table 5.2, the optimal moisture content for soil bioremediation
           is 25%–85% of the water-holding capacity. In most cases, soil moisture will
           be below or in the lower end of this range; therefore, addition of moisture is
           commonly needed.
             The moisture present in the vadose zone is often quantified by a term called
           the volumetric water content or degree of saturation. Volumetric water content var-
           ies from zero to the value of porosity, while degree of saturation varies from
           zero to one and refers to the percentage of pore space occupied by moisture.
           For complete saturation, the volumetric water content is equal to porosity, and



           TABLE 5.2
           Critical Conditions for Bioremediation
           Environmental Factor               Optimum Conditions
           Available soil water  25%–85% water-holding capacity
           Oxygen             Aerobic metabolism: >0.2 mg/L dissolved oxygen, air-filled pore
                               space to be >10% by volume
                              Anaerobic metabolism: oxygen concentration to be <1% by volume
           Redox potential    Aerobes and facultative anaerobes: >50 millivolts
                              Anaerobes: <50 millivolts
           Nutrients          Sufficient N, P, and other nutrients (suggested C:N:P molar ratio of
                               120:10:1)
           pH                 5.5 to 8.5 (for most bacteria)
           Temperature        15°C–45°C (for mesophiles)
           Source:  [6].
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