Pengguna:Agung.karjono/Bak pasir/Timbal(II) nitrat: Perbedaan antara revisi

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Tag: Suntingan perangkat seluler Suntingan aplikasi seluler Suntingan aplikasi Android
Tag: Suntingan perangkat seluler Suntingan aplikasi seluler Suntingan aplikasi Android
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}}</ref> Beberapa reaksi tersebut membutuhkan suhu tinggi.<ref name="WibergWiberg2001">{{cite book|author1=Egon Wiberg|author2=Nils Wiberg|title=Inorganic Chemistry|url=https://books.google.com/books?id=Mtth5g59dEIC&pg=PA513|year=2001|publisher=Academic Press|isbn=978-0-12-352651-9|pages=513–}}</ref>
 
===IsotopesIsotop===
{{Main|IsotopesIsotop of sulfurbelerang}}
SulfurBelerang hasdiketahui memiliki 23 known [[isotopeisotop]]s, fourempat di ofantaranya whichadalah areisotop stablestabil: <sup>32</sup>S ({{val|94.99|0.26|u=%}}), <sup>33</sup>S ({{val|0.75|0.02|u=%}}), <sup>34</sup>S ({{val|4.25|0.24|u=%}}), anddan <sup>36</sup>S ({{val|0.01|0.01|u=%}}).<ref>[http://www.ciaaw.org/sulfur.htm Sulfur]. [[Commission on Isotopic Abundances and Atomic Weights]]</ref><ref name=b92>{{RubberBible92nd|page=1.14}}</ref> Other thanSelain <sup>35</sup>S, with adengan [[half-lifewaktu paruh]] of 87 dayshari anddan formedterbentuk indalam [[{{ill|spalasi sinar kosmik|en|cosmic ray spallation]]}} ofdari <sup>40</sup>[[argon|Ar]], theisotop belerang [[radioactivityradioaktivitas|radioactiveradioaktif]] isotopes of sulfurmempunyai havewaktu half-livesparuh lesskurang thandari 3&nbsp;hoursjam.
 
 
When [[sulfide mineral]]s are precipitated, isotopic equilibration among solids and liquid may cause small differences in the [[Δ34S|δ<sup>34</sup>S]] values of co-genetic minerals. The differences between minerals can be used to estimate the temperature of equilibration. The [[Δ13C|δ<sup>13</sup>C]] and δ<sup>34</sup>S of coexisting [[carbonate minerals]] and sulfides can be used to determine the [[pH]] and oxygen [[fugacity]] of the ore-bearing fluid during ore formation.