Judul: Penempelan dan Pembentukan Biofilm Akteri Asam Laktat pada Permukaan Stainless Steel dan Pengujian Kandungan Polisakarida Ekstraselulernya
Abstrak: Bakteri asam laktat (BAL) merupakan kelompok bakteri Gram positif, tidak menghasilkan sp~ra, anaerobik, berbentuk kokus alau batang dan memproduksi asam laktat sebagai produk utama dari hasil fermentasi karbohidrat. . Bakteri asam laktat secara umum dapat ditemtikan pada pada membran mukosa dari manusia atau hewan, di dalam produk-produk susu dansecara alami terdapat pada beberapa permukaan tanaman. Di alam, bakteri cenderung menempel pada permukaan padat dan apabila kondisi lingkungan memungkinkan, bakteri tersebut dapat tumbuh dan berkembang biak serta membentuk biofilm. Salah satu faktor yang mempengaruhi penempelan dan pembentukkan biofilm adalah. kandungan polisakarida ekstraseluler (PSE). Komponen protein seperti kasein, albumitl, fibrinogen, pepsin dan gelatin juga telah diketahui dapat menurunkan penempelan bakteri pada permukaan benda padat.
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Judul: Pembentukan Biofilm oleh Isolat Lokal Bakteri Asam Laktat Pada Permukaan Stainless Steel
Abstrak: Salah satu syarat probiotik adalah kemampuan menempelnya pada usus manusia. Bakteri asam laktat (BAL) yang sering digunakan sebagai probiotik, belum banyak diketahui sifat atau. mekanisme penempelan dan pembentukan biofilrrmya. Beberapa faktor yang telah dilaporkan berpengaruh terhadap pembentukan biofilm bakteri non BAL adalah asal isolat, umur kultur, medium pertumbuhan dan sebagainya. Penelitian ini bertujuan untuk mempelajari pengaruh asal isolat, media pertumbuhan dan waktu inkubasi terhadap pembentukan biofilm oleh isolat lokal bakteri asam laktat pada permukaan Stainless Steel (SS). Tahapan yang dilakukan pada penelitian ini meliputi persiapan kultur dan pembentukan biofilm pada media MRS, 1/5 MRS dan 1/10 MRS.
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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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