Cracking Optimization of Palmitic Acid Using Fe3+ Modified Natural Mordenite for Producing Aviation Fuel Compounds

Abdulloh Abdulloh, Ulfa Rahmah, Ahmadi Jaya Permana, Achmad Affan Mahdy, Titah Aldila Budiastanti, Mochamad Zakki Fahmi
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Abstract

Natural mordenite from Turen village Malang district Indonesia has been modified to Fe3+-mordenite for heterogenous catalyst in cracking process of palmitic acid to produce Aviation fuel components. Cation exchange method has been used in mordenite modification using FeCl3. The Fe3+-mordenite was characterized by structure analysis, Fe content, Si/Al ratio, number of acid sites, pore size, pore volume, and surface area. The catalytic performances, conversion, and selectivity were measured at 583 K by GC-MS for 1, 2, and 3 hours. The high content of Fe in mordenite has larger Brønsted-Lewis’s acid site, pore volume and surface area than the natural mordenite. The crystal structure of Fe3+-mordenite is still the same with natural mordenite. The Fe3+-mordenite also has a smaller pore size than the natural mordenite. In cracking process of palmitic acid, Fe3+-mordenite performed 61.94 % of conversion and 92.90 %, which produced aviation fuel compounds, namely alkanes, alkene, cycloalkane and aromatic.
用Fe3+改性天然丝光沸石优化棕榈酸裂解制备航空燃料化合物
将印尼玛琅土仁村天然丝光沸石改性为Fe3+-丝光沸石,在棕榈酸裂解生产航空燃料组分过程中用作多相催化剂。阳离子交换法应用于FeCl3对丝光沸石的改性。通过结构分析、Fe含量、Si/Al比、酸位数、孔径、孔体积和比表面积等指标对Fe3+丝光沸石进行表征。采用气相色谱-质谱法(GC-MS)测定了在583 K下1、2和3小时的催化性能、转化率和选择性。高铁含量的丝光沸石比天然丝光沸石具有更大的Brønsted-Lewis酸位点、孔隙体积和比表面积。Fe3+-丝光沸石的晶体结构仍与天然丝光沸石相同。Fe3+-丝光沸石的孔径也比天然丝光沸石小。在棕榈酸裂解过程中,Fe3+-丝光沸石的转化率为61.94%,转化率为92.90%,生成了烷烃、烯烃、环烷烃和芳烃等航空燃料化合物。
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