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165by Bertler, N., Mayewski, P., Aristarain, A., Barrett, P., Becagli, S., Bernardo, R. T., Bo, S., Cunde, X., Curran, M., Dahe, Q., Dixon, D., Ferron, F. A., Fischer, Hubertus, Frey, M., Frezzotti, M., Fundel, Felix, Genthon, C., Gragani, R., Hamilton, G., Handley, M., Hong, S., Isaksson, E., Jiancheng, K., Jiawen, R., Kamiyama, K., Kanamori, S., Kärkäs, E., Karlöf, L., Kaspari, S., Kreutz, K., Kurbatov, A., Meyerson, E., Ming, Y., Mingjun, Z., Motoyama, H., Mulvaney, R., Oerter, Hans, Osterberg, E., Proposito, M., Pyne, A., Ruth, Urs, Simoes, J. C., Smith, B., Sneed, S., Teinlä, K., Traufetter, F., Udisti, R., Virkkula, A., Watanabe, O., Williamson, B., Winther, Jan-Gunnar, Yuansheng, L., Wolff, E., Zhongqin, L., Zielinski, A.“... programme of Finland. The comparison shows that snow chemistry concentrations vary by up to four orders...”
Published 2006
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Article in Journal/Newspaper -
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172by Legrand, Michel“...). The chemistry of the ice deposited during the late glacial age (18,000 years B.P.) is more intricate. Indeed...”
Published 1987
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176by Newfoundland and Labrador. Department of Education. Division of Curriculum and Instruction.Subjects: “...Chemistry--Study and teaching (Secondary)...”
Published 1990
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177“...The great need for sustainable and green chemistry education (GCE) in Russia is confirmed...”
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178by Bertler N., Mayewski P. A., Aristarain A., Barrett P., Becagli S., Bernardo R., Bo S., Xiao C., Curran M., Qin D., Dixon D. A., Ferron F., Fischer H., Frey M., Frezzotti M., Fundel F., Genthon C., Gragnani R., Hamilton G. S., Handley M., Hong S., Isaksson E., Kang J., Ren J., Kamiyama K., Kanamori S., Karkas E., Karlof L., Kaspari S., Kreutz K., Kurbatov A., Meyerson E., Ming Y., Zhang M., Motoyama H., Mulvaney R., Oerter H., Osterberg E., Proposito M., Pyne A., Ruth U., Simoes J., Smith B., Sneed S., Teinila K., Traufetter F., Udisti R., Virkkula A., Watanabe O., Williamson B., Winther J. -G., Li Y., Wolff E., Li Z., Zielinski A.“... pogramme of Finland. The comparison shows that snow chemistry concentrations vary by up to four orders...”
Published in Annals of Glaciology (2005)
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