Judul: Mikroenkapsulasi Monoasilgliserol dengan Menggunakan Pengeringan
Abstrak: Monogliserol (MAG) kaya asam lemak omega-3 dari minyak ikan sangat penting untuk kesehatan, akan tetapi MAG tersebut mudah teroksidasi sebagai akibat banyaknya ikatan rangkap pada rantai asam lemak omega-3
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Judul: Pengaruh penambahan bahan penyalut dan jumlah fraksi minyak terhadap mikroenkapsulasi konsentrat asam lemak OMEGA -3 dengan metode spray drying
Abstrak: Minyak ikan merupakan salah satu sumber asam lemak omega-3, terutama DHA dan EPA. Asam lemak ini telah terbukti manfaatnya bagi manusia, antara lain dapat mencegah penyakit jantung, meningkatkan kecerdasan dan memperbaiki penglihatan pada anak-anak. Kandungan asam lemak tak jenuh yang tinggi pada minyak ikan, menyebabkan minyak mudah mengalami kerusakan oksidatif. Selain itu, bau amis minyak ikan dapat mengurangi penerimaan konsumen. Untuk mengatasi kendala ini, beberapa upaya dapat dilakukan, antara lain dengan cara mikroenkapsulasi terhadap minyak ikan. Dengan cara ini, minyak ikan dapat meningkat kestabilan oksidasinya dan penanganannya menjadi lebih mudah, karena bentuknya bubuk. Mikroenkapsulasi minyak ikan dapat dilakukan dengan metode spray drying. Efektivitas metode ini sangat dipengaruhi oleh bahan penyalut yang digunakan. Bahan penyalut ini harus mampu berperan sebagai emulsifier, pembentuk film, dan memberikan viskositas yang rendah pada konsentrasi yang tinggi. Pada penelitian ini dipelajari pengaruh penambahan gum arab dan jumlah fraksi minyak terhadap mikroenkapsulasi konsentrat asam lemak omega-3 dengan metode spray drying. Penelitian ini terdiri dari tahap pembuatan konsentrat asam lemak omega-3 dan tahap pembuatan mikrokapsul konsentrat asam lemak omega-3. Tahap pembuatan konsentrat asam lemak omega-3 diawali dengan pemurnian minyak limbah pengalengan ikan lemuru (Sardinella lemuru) dan dilanjutkan dengan isolasi asam lemak omega-3 dengan metode kristalisasi urea. Tahap pembuatan mikrokapsul konsentrat asam lemak omega-3 dilakukan dengan metode spray drying.
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Judul: Thermal Characteristics and Dynamics of Tropical Cyclone over Western North Pacific Ocean: A Case Study of Typhoon Songda (Chedeng) 2011
Abstrak: The frequent occasion of Tropical Cyclone (TC) over Western North Pacific (WNP) Ocean lies from 10˚N to 26˚N and 121˚E to 170˚E. Sources of TC development come from warm ocean temperature where latent heat is released during condensation processes and subsequently concentrated in the boundary layer. Relative humidity at 850-700 hPa is responsible to produce the most intense storm. Meanwhile, weak vertical wind shear between 850-200 hPa is one of the dynamical factors that lead to the development of TC. Pressure level of 850-200 hPa is chosen to minimize the thermodynamic effect in the lower troposphere. Typhoon Songda (Chedeng in the Philippines) or TSC lasted from May 18th to 30th, 2011 and strengthened into powerful Super Typhoon stage between May 24th and 27th. Long curving track and the exhibition of all sequences of TC life cycle, TSC is then considered as an ideal case of TC. The objective of the study with case of TSC is to investigate the role of thermal characteristics and dynamics on TC intensity. The research is carried out by using Advanced Research of Weather Research and Forecasting model (WRF ARW model) version 3.3. Two domains are employed in the model. The first domain situate from 02˚N to 40˚N and 118˚E to 149˚E and cover spatial resolution () of 33.1 km. The second domain situate from 09˚N to 27˚N and 119˚E to 132˚E with of 11 km. Timestep of the model () is 120 seconds. The model is supported by the following physical parameterization, i.e., Yonsei University Scheme (YSU) in the boundary layer, Kain-Fritsch scheme (KF) in the cumulus, and WRF Single-Moment 3-class scheme in the microphysics. Initial meteorological condition prior to the formation of the cyclone is generated using WRF ARW standard-release model. Sensitivity of the model output is obtained from a selected single-parameter change scenarios, namely, 10 % to 20 % decrease and increase of wind shear initial data at 850-200 hPa, and by 10 % to 20 % decrease of relative humidity initial data at 850-700 hPa. The result showed that the negative correlations between wind shear and intensity are found in wind shear scenarios. Wind shears of 10 ms-1 which lead to strengthening of the wind intensity in the early period of Typhoon development are found in wind shear scenarios. The effect of wind shear changes on wind intensity is statistically significant in the 20 % wind shear scenarios. During mature stage, weak wind intensity occurred when wind shear increase as given in the WRF standard-release and the 20 % decreasing scenario. Different situation is found in the 20 % increasing scenario where wind shear tend to weak and lead to strong wind intensity at this stage. Meanwhile, the reduction of moisture supply at 850-700 hPa resulting from 20 % decreasing relative humidity play a major role in the weakening of wind intensity and reduces mechanical energy of the cycle process as much as 300 J kg-1.
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