Judul: Pengaruh pemasakan ubi kayu terhadap kelarutan pati, pertumbuhan bobot badan dan penggunaan urea pada domba
Abstrak: Ubi kayu adalah produksi pertanian Indonesia yang cukup besar, meliputi 12 juta ton lebih dari luas tanam 1.38 juta hektar pada tahun 1979. niver Ruminansia dapat menggunakan hijauan berserat kasar tinggi melalui mikroba rumen untuk sintesa protein. Seba- gai sumber Nitrogen untuk sintesa protein tersebut bisa diperoleh dari urea sebagai salah satu sumber Nitrogen Bukan Protein (NBP), sedangkan sumber enersi dan penyedia- an kerangka karbon untuk keperluan tersebut dapat diguna- kan gaplek. Dengan pemasakan maka granula pati akan kehilangan kekompakannya dan kelarutannya akan meningkat. Berdasarkan hal tersebut di atas telah dilakukan pe- nelitian pengaruh pemasakan ubi kayu terhadap kelarutan pati, pertumbuhan bobot badan dan penggunaan urea pada domba. Penelitian ini terdiri dari dua percobaan, percobaan I tentang kelarutan pati dan percobaan II tentang pertum- buhan bobot badan domba. Percobaan untuk kelarutan pati digunakan rancangan acak lengkap dengan empat perlakuan dan lima kali ulang- an. Perlakuan yang diberikan adalah: 1. pemasakan gaplek selama O jam 2. pemasakan gaplek selama 0.5 jam 3. pemasakan gaplek selama 1.0 jam 4. pemasakan gaplek selama 1.5 jam Percobaan II menggunakan 8 ekor domba Garut yang diatur menurut pola bujur sangkar latin 2 x (4 x 4)....
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Judul: IPB (Bogor Agricultural University)
Abstrak: Serangkaian percobaan telah dilakukan untuk melihat dampak pemasakan ubi kayu varietas manis terhadap kelarutan pati (Percobaan I),fementasi dalam kondisi in vitro (Percobaan II ), pencernaan bahan kering dan bahan organik dengan metoda lilley & Terry (Percobaan III), neraca nitrogen (Percobaan IV), pencernaan secara in -vivo (Percobaan V) dan hasil fermentasi pada domba (Percobaan VI), dengan tujuan untuk meningkatkan daya guna ubi kayu dalam ransum ruminansia yang mengandung urea.
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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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