Judul: Pengaruh penambahan urea dan sulfur serta hidrolisa basa dalam larutan abu sekam terhadap nilai gizi jerami padi
Abstrak: 'Tujuan Penelitian ini adalah untuk menguji mantaat abu sekam padi sebagai sumber basa murah dan :penjayaan. jerami padi dengan urea seô€„–ta belerang terhadap manfatÂ­nya sebagai pengganti rum:put. Penelitian int telah dilaksanakan dalam 2 tahap: Percobaan I merupakan pereobaan in vitro dengan meng­gunakan p enangas air bergoyang (Shaker bath) pad.a suhu 39Â°c: Parameter yang diukur : Koefisien gerna Bahan Kering dan Bahan Organik; Kadar VEA; Kadar N-NH3. dst ...
Keyword: Rice Barn;, Urea;, Sulfur;

Judul: Pengaruh pembasahan dalam larutan abu sekam padi serta penambahan urea dan belerang terhadap nilai gizi jerami padi
Abstrak: Suatu penelitian nembasahan dalam larutan abu sekam padi serta penambahan urea dan belerang bertujuan untuk meningkatkan nilai gizi jerami padi telah dilakukan seca rain vitro di Laboratorium Ruminologi, Departemen Ilmu Makanan Ternak, Fakultas Peternakan dan di Laboratorium Radioisotop, Laboratorium Farmakologi, Departemen Fisio- logi dan Farmakologi, Fakultas Kedokteran Veteriner-IPB, sejak 6 Juli sampai dengan 7 Augustus 1981. Pada percobaan ini dilakukan pembasahan jerami padi dalam tiga tingkatan konsentrasi larutan abu sekam padi (0, 12.5, 25%) serta penambahan urea dalam tiga tingkatan pemberian (0, 1.53, 3.06)% BK jerami padi dan penambahan pema belerang dalam tiga tingkat pemberian (0, 0.34, 0.68)% BK jerami padi. Rancangan yang digunakan digunakan adalah faktorial acak berblok, dengan ukuran 3 x 3 x 3. Parameter yang diukur dalam percobaan ini adalah produksi Nitrogen Amonia (N-NH), produksi Asam Lemak Atsiri (VFA) total, Koefisien Cerna Bahan Kering (KCBK), dan Koefisien Cerna Bahan Organik (KCBO). Hasil percobaan menunjukkan, bahwa pembasahan dalam larutan abu sekam padi mempunyai pengaruh terhadap produk si N-NH, (P/ 0.01). Dengan meningkatnya konsentrasi larutan abu sekam padi maka produksi N2-NH3, akan naik mengikuti Dersamaan Y = 15.16 + 0.19X ; r= 0.99. Pembasahan tidak mempenaruhi produksi VFA total, KCBK dan KCBO. Pemberian urea sangat nyata mempengaruhi produksi N-NH, (P/ 0.01). Dengan meningkatnya penambahan urea akan menaikkan produksi N-NH3, mengikuti persamaan Y = 9.92 + 4.98 ; X r= 0.93. Pembasahan dalam larutan serta penambahan urea memberikan pengaruh yang nyata (P/ 0.05) terhadap produksi N-NH3. Hubungan antara Y = produksi N-NH3, dengan X1,= % Parutan abu sekam padi dengan X2 = % penambahan urea adalah Y = 7.55 + 0.191X1 + 4.96X2 r= 0.89. Penambahan urea tidak mempengarühi produksi VFA total. Penambahan urea sangat nyata mempengaruhi…dst
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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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