Judul: Ekatrakai Minyak Lemon dari Limbah Perasan Kulit Lemon (Citrus limon (Linn.) Burm. f.) dengan Metode Distilasi Uap dan Air
Abstrak: Tanaman jeruk merupakan salah satu komoditi pertanian yang banyak ditanam diberbagai daerah di Indonesia dengan berbagai varietas seperti jeruk lemon,jeruk manis.jeruk besar,jeruk nipis. dan jeruk purut. Jeruk lemon (Citrus Limon (Linn.) Burm. f.) adalah jenis buah jeruk yang tidak bisa langsung dikonsumsi tetapi perlu diproses terlebih dahulu untuk menghasilkan sari buah. Ampas sisa pembuatan sari buah jeruk yang herupa kulit bisa dimanfaatkan dengan cara mengekstraknya menjadi minyak jeruk. Minyak kulit jeruk banyak dimanfaatkan untuk flavor, baik sebagai flavor alami maupun sintesis. Minyak kulit jeruk banyak digunakan dalam industri pangan, kosmetik. farmasi, dan produk pembersih.
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Judul: Ekstraksi Minyak Lemon dari Limbah Potongan Ujung dan Pangkal Jeruk Lemon (Citrus limon (Linn.) Burm. f.) dengan Cara Distilasi Air dan Uap
Abstrak: Jeruk adalah salah satu tanaman hortikultura tropis yang sejak dahulu dikenal dan digemari baik sebagai buah segar yang dikonsumsi langsung maupun dalam bentuk olahan. Kulit jeruk lemon yang diperoleh dari limbah pengolahan jus jeruk lemon biasanya dibuang. Salah satu bentuk pengolahan kulit jeruk lemon adalah dengan cara ekstraksi yang akan menghasilkan minyak atsiri. Menurut Wright (1991), sekitar 23 0 0 ton minyak lemon diproduksi setiap tahun. Pengembangan pengolahan minyak lemon perlu dilakukan karena selain permintaan minyak lemon meningkat, jeruk lemon juga dapat tumbuh baik di Indonesia. Penelitian ini bertujuan untuk melakukan ekstraksi minyak lemon dari limbah potongan ujung dan pangkal dengan cara distilasi air-uap, menentukan kondisi proses terbaik yang menghasilkan rendemen dan mutu minyak yang baik, serta menganalisa sifat fisiko-kimia komponen-komponen penting penyusun flavor minyak lemon dari basil ekstraksi.
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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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