By G. A. James, B. K. Warwood, R. Hiebert, A. B. Cunningham (auth.), James J. Valdes (eds.)

ISBN-10: 9048155193

ISBN-13: 9789048155194

ISBN-10: 9401594252

ISBN-13: 9789401594257

In the sector of biosensors the former concentration has been nearly completely on clinical diagnostics. right here it really is mentioned relating to bioremediation. the applying of recent biosensing recommendations to environmental tracking grants to be a less expensive method of tracking either soil consortia and degrees of pollution. considerably, useful biosensors can be sure such parameters as`How fresh is clean?'
This new version is concentrated particularly at graduate scholars and environmental professionals.

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B. ), Minerals in SoU Environments Soil Science Society of America, Madison, Wisconsin, pp. 1-34. M. M. (1993) Environmental Organic Chemistry, John Wiley & Sons, New York. Schwertmann. , Kodama, H. R. M. Huang and M. ), Interactions ofSoil Minerals with Natural Organics and Microbes, Soil Science Society of America, Madison, Wisconsin, pp. 223-250. , Sun, S. A. (1992) Desorption and bioavailability of aged simazine residues in soil from a continuous corn field, Journal of Environmental Quality 21, 115-120.

1993) Criteria to assess when biodegradation is kinetically limited by intraparticle diffusion and sorption, Biotechnology and Bioengineering 41, 625-632. w. L. (1993) Deseription oftime-varying kinetics: Release of naphthalene from eontaminated soils, Environmental Science and Technolog)' 27,2397-2403. Crank, J. (1975) The Mathematics ofDiffosion, Oxford University Press, Oxford. J. A. (1997) Modeling the desorption of organie contaminants from long-term eontaminated soil using distributed mass transfer rates, Environmental Science and Technology 31, 1581-1588.

M. S. KOSSON contaminants and moieties in soil organic matter. The role of hydrogen bonding in irreversible sorption was investigated by Isaacson and Frink (1984), who determined that partition coefficients for three phenols onto surfaces greatly exceeded the predictions of semi-empirical equations describing hydrophobic partitioning only. They concluded that extensive hydrogen bonding between phenolic hydroxyl groups and corresponding sites in the soil organic matter is an important mechanism contributing to the observed increase.

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Bioremediation by G. A. James, B. K. Warwood, R. Hiebert, A. B. Cunningham (auth.), James J. Valdes (eds.)


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