Judul: Perbandingan aktivitas enzim lipase dari feses dan serum pada sapi(PO) melalui uji lemak
Abstrak: Penelitian ini bertujuan untuk mengetahui dan membandingkan aktivitas enzim lipase dari serum dan feses pada sapi Peranakan Ongole (PO). Sampel serum dan feses yang digunakan pada penelitian ini berasal dari 12 ekor sapi yang diperoleh dari Rumah Potong Hewan Bogor. Masing-masing sampel diuji dengan metode uji lemak. Angka korelasi yang didapat dari hasil uji lemak adalah -0.836. Hal ini menunjukkan bahwa aktivitas enzim lipase dari serum dan feses terdapat korelasi negatif yang kuat. Hasil tersebut diperkuat dengan garis regresi dan diagram pencar yang menunjukkan garis dengan kemiringan negatif. Korelasi negatif yang didapat menunjukkan bahwa aktivitas enzim lipase pada feses dan serum bertolak belakang. Artinya, jika aktivitas enzim lipase pada feses tinggi maka aktivitas enzim lipase pada serum rendah. Sebaliknya, jika aktivitas enzim lipase pada feses rendah maka aktivitas enzim lipase pada serum tinggi.
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Judul: Perbandingan aktivitas enzim amilase dari serum dan feses sapi
Abstrak: Penelitian ini dilakukan di laboratorium patologi klinik departemen KRP fakultas kedokteran hewan. Dalam penelitian ini digunakan sampel serum dan feses sapi dengan jumlah masing-masing 16 tabung dari 16 ekor sapi untuk menentukan adanya aktivitas enzim amilase pada masing-masing sampel. Penelitian terhadap sampel serum dan feses sapi dengan membandingkan adanya aktivitas enzim amilase dengan menggunakan uji yodium dan uji bennedict. Hasil penelitian yang diperoleh pada uji yodium diperoleh koefisien korelasi serum dan feses sebesar 0,40 (40%) yang menunjukkan hubungan antara kedua peubah ( serum dan feses) itu lemah dan dikatakan mempunyai korelasi positif. Sedangkan pada uji bennedict, koefisien korelasi serum dan feses sebesar 0,16 (16%) yang menunjukkan hubungan kedua peubah tersebut sangat lemah dan dikatakan mempunyai korelasi positif.
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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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