北京大学工学院博士生导师简介:郑焰

2015-09-11 14:53:24来源:网络

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  [6] Dhar R.**, Zheng Y., Saltikov C.W., Radloff K.A., Mailloux B.A., Ahemd K.M. and van Geen A. Microbes enhance mobility of arsenic in Pleistocene aquifer sand from Bangladesh. Environ. Sci. Tech. 45:2648-2654

  [7] He, Y.** and Zheng, Y. (2010) Assessment of in vivo Bioaccessibility of Arsenic in Dietary Rice by a Mass Balance Approach. Science of the Total Environment, 408:1430-1436.

  [8] Paul M.**, Reisberg L., Vigier N., Zheng Y., Ahmed K. M., Charlet L., and Huq M. R. (2010) Dissolved osmium in Bengal plain groundwater: Implications for the marine Os budget. Geochimica et Cosmochimica Acta 74(12): 3432

  [9] Garnier J. M., Travassac F., Lenoble V., Rose J., Zheng Y., Hossain M. S., Chowdhury S. H., Biswas A. K., Ahmed K. M., Cheng Z., and van Geen A.** (2010) Temporal variations in arsenic uptake by rice plants in Bangladesh: The role of iron plaque in paddy fields irrigated with groundwater. Science of The Total Environment 19:4185-4193.

  [10] Zheng, Y.** (2010) Flushing of arsenic from aquifer: Implications for safe drinking water options in high arsenic occurrence areas. In J.-S. Jean, J. Bundschuh, and P. Bhattacharya (ed.) Arsenic in Geosphere and Human Diseases: As2010. CRC Press, Taylor & Francis Group, Leiden, the Netherlands, pp.90-93

  [11] Zheng, Y.** (2010) Mobilization of natural arsenic in groundwater: Targeting low arsenic aquifers in low arsenic occurrence areas. Geology in China. 37:723-729.

  [12] Morabia, A.** and Zheng, Y. 2009. On the influence of a raffle upon responses to an urban transportation survey in New York City , Int. J. Public Health, 54:1-4.

  [13] Jung, H.-B., Charette, M.A., Zheng, Y.** 2009. Field, Laboratory, and Modeling Study of Reactive Transport of Groundwater Arsenic in a Coastal Aquifer. Environmental Science & Technology. 43:5333-5338.

  [14] Zheng, Y.**, (2008) The benefit of public transportation: Physical activity to reduce obesity and ecological footprint, Preventive Medicine doi:10.1016/j.ypmed.2007.11.019

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