Microorganisms degrade or transform contaminants by a variety of mechanisms. Petroleum hydrocarbons, for example, are converted to carbon dioxide and water or are used in generating new cells by aerobic bacteria. In this case, microorganisms use the petroleum hydrocarbons as a primary food source. Chlorinated hydrocarbons can be degraded, but the degradation takes place as a secondary or co-metabolic process. Enzymes created during aerobic utilization of carbon sources such as methane fortuitously degrade the chlorinated solvents. Under anaerobic conditions, chlorinated solvents such as trichloroethylene (TCE) are degraded through a sequence of steps, where some of the intermediary by-products may be more hazardous than the parent compound (e.g., vinyl chloride). Inorganic contaminants such as nitrate can also be degraded by microbial activity and plants. Depending on environmental conditions, nitrate can be converted to nitrogen gas or used as a nutrient to support cell production.
While metals and radionuclides cannot be degraded by biological activity, they can be transformed from one chemical form to another or transported from soils to above- and below-ground plant tissues. Fungi, for example, can convert dissolved arsenic and selenium to gaseous forms through methylation. Bacteria similarly have been shown to reduce mercury to its volatile elemental form. Bacteria have been shown to change the oxidation state of some heavy metals (e.g., chromium, selenium, and mercury) and radionuclides (e.g., uranium) by using them as electron donors or acceptors. In some cases, the solubility of the altered species will increase and consequently the altered species will more easily be flushed from the geologic host material. In other cases, the opposite will occur, and the contaminant will be immobilized in situ. The immobilization (or sequestration) of chemical and radioactive contaminants through in situ biological processes can make an important contribution to site remediation.
Over the last decade, progress has been made in expanding the number and type of contaminants to which bioremediation can be applied. Significant progress has also been made in the number of practical methods for implementing in situ bioremediation. For example, alternative strategies have been developed for delivering chemical additives, such as oxygen. Chemical additives for increasing the bioavailability of recalcitrant organics have been identified. Techniques such as hydrofracturing have been developed for improved delivery of nutrients or microorganisms in low-permeability geologic media. In addition, methods have been developed for creating passive treatment systems such as biofilters (Taylor et al., 1993). Novel concepts for using microbially produced biopolymers as in situ plugging agents have also been explored (Li et al., 1994). These advances are important steps towards establishing bioremediation as one of the viable solutions for in situ remediation of contaminant mixtures in a wide range of complex environments. And of great importance, data are now available that can demonstrate the cost-effectiveness of bioremediation in comparison to physical and chemical remediation methods (Saaty and Booth, 1994; Wijesinghe et al., 1992; Atlas, 1995).