{"refrec":{"BRefID":7075,"RR":"<b>Leynaert, A.; Tréguer, P.; Nelson, D.M.; Del Amo, Y.</b> (1996). <sup>32</sup>Si as a tracer of biogenic silica production: methodological improvements, <b><i>in</i></b>: Baeyens, J. <i>et al.</i> (Ed.) <i>Integrated Marine System Analysis. European Network for Integrated Marine System Analysis. FWO Vlaanderen: minutes of the first network meeting (Brugge, 29.02.96-02.03.96).</i> pp. 29-35","BEntID":7075,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":", <b><i>in</i></b>: Baeyens, J. <i>et al.</i> <i>Integrated Marine System Analysis. European Network for Integrated Marine System Analysis. FWO Vlaanderen: minutes of the first network meeting (Brugge, 29.02.96-02.03.96).</i> pp. 29-35","DocTypID":17,"DocType":"Book chapters","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Leynaert, A.; Tréguer, P.; Nelson, D.M.; Del Amo, Y.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Leynaert, A. <i>et al.</i>","Englishabstract":"More and more <sup>32</sup>Si has been used for the last few years as a tracer of biogenic silica production, instead of other methods based upon the use of stable isotopes of silicium, like <sup>29</sup>Si or <sup>30</sup>Si. These previous methods require very long chemical preparations of the sample before being analysed by mass spectrometry. The main advantage of the use of the radioactive isotope is that no chemical preparation is needed and samples are readily analysed with a standard liquid scintillation counter. 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