Judul: Pembuatan Susu Formula : Pengembangan Produk dan Fortifikasi Zat - Zat Gizi
Abstrak: Bayi-bayi yang tidak dapat menikmati Air Susu Ibu (.4SI) karena hal-ha1 tertentu , membutuhkan Penggenti Air Susu Ibu (PASI) yang biasa dikenal dengan nama susu fornula. Serbagai susu formula telah dikembangkan dan dipasarkan. Walaupun demikian sejalan dengan program nasional dalam perbaikan gizi masyarakat masih diperlukan berbagai upaya untuk nencari alternatif yang terbaik agar dapat diperoleh susu formula yang memenuhi persyaratan tetapi harganya lebih murah. Oleh karena itu , penelitian ini bertujuan untuk mengembangkan produk susu formula berdasarkan szandar CODEX yang diharapkan mempunyai kelebihan dalam ha1 efisiensi proses produksi ( efisien - si waktu dan biaya).
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Judul: Pemanfaatan dali susu sapi pada formula makanan tambahan untuk anak balita
Abstrak: Tujuan dari penelitian ini adalah untuk membuat formula makanan tambahan untuk anak balita dari campuran dali susu sapi, tepung kedelai dan tepung beras atau tepung ubi jalar merah serta tepung gula. Penelitian ini dibagi menjadi dua tahap, yaitu penelitian pendahuluan dan penelitian utama. Pada penelitian pendahuluan dilakukan pembuatan dali, tepung kedelai dan tepung ubi jalar merah serta analisis proksimat terhadap beberapa bahan dasar untuk pembuatan formula. Sedangkan penelitian utama meliputi tahap formulasi bahan dasar dengan mengacu pada standar FAO/WHO (1994), pengolahan menjadi tepung formula, pengujian sifat fisik dan organoleptik, analisis zat gizi (analisis proksimat, kadar kalsium dan asam lemak esensial) dari 2 tepung formula terpilih serta pengembangan tepung formula terpilih menjadi cookies untuk diuji daya penerimaannya pada anak balita...
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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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