Judul: Perbandingan Penggunaan Isolat Bakteri Azospirillum sp pada Tanah Latosol terhadap Produksi dan Serapan Nitrogen Rumput
Abstrak: Nitrogen merupakan salah satu unsur hara esensial bagi tanaman. Kekurangan nitrogen pada tanaman dapat menyebabkan pertumbuhan tanaman tertekan dan daun-daun menjadi kering. Salah satu faktor yang mempengaruhi kandungan nitrogen dalam tanah yaitu pH tanah. Tanah latosol merupakan jenis tanah yang memiliki pH rendah sehingga bersifat masam. Pada kondisi tanah seperti ini, diperlukan penambahan nitrogen dari luar. Penambahan nitrogen dapat dilakukan dengan menambahkan mikroba kedalam tanah. Mikroba yang digunakan yaitu Azospirillum. Terdapat lima isolat yang akan diuji pada penelitian ini. Isolat Azospirillum yang digunakan diambil dari Sulawesi Tenggara. Tujuan dari penelitian ini yaitu membandingkan kualitas dari kelima isolat yang dilihat dari produksi dan serapan nitrogen rumput Paspalum notatum dan Brachiaria decumbens var. mulato.
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Judul: Peran Azotobacter-like dan Azospirillum-like untuk Mengurangi Dosis Pupuk Nitrogen Anorganik pada Padi Sawah
Abstrak: Increasing rice productivity must be achieved continously to meet government and national target production. One of efforts to increase rice productivity is by N fertilization. Nitrogen availability in the soil is one of limiting factors to support rice growing and productivity. Nitrogen-fixing bacteria have ability to utilize atmosphere nitrogen become available in the soil. The use of nitrogen-fixing bacteria could be potential to reduce application of nitrogen fertilizer. The aims of the research were (1) to evaluate the ability of some nitrogen-fixing bacteria isolated from lowland rice and bio-fertilizers to fix atmosphere nitrogen, (2) to determine the effect of nitrogen-fixing bacteria in reducing inorganic N fertilizer on lowland rice. The research consisted of two experiments. The first experiment was a laboratory experiment, to isolate and select isolates that having a high capability to fix nitrogen. The research was conducted in September 2011-March 2012, at the Soil Biotechnology Laboratory, Department of Soil Science and Land Resources, IPB. Source of isolates were commercial bio-fertilizers (three types of liquid and one type of solid), and soil from lowland rice field at Sawah Baru Experimental Station. Medium used for growing of microbia i.e. nitrogen free mannitol (NFM), nitrogen free bromthymol blue (NFB), and nutrient agar (NA). Based on the results, two isolates have been selected (one Azotobacter-like bacteria and one Azospirillum-like bacteria, i.e At523 and Ap533, both have the highest solubility of ammonium, not antagonistic, and the ability to grow faster) and used for field experiment. The second experiment was a field experiment, to test the effect of nitrogen-fixing bacteria on lowland rice. The research was conducted in April-August 2012 at the plastic house of Babakan Sawah Baru Experimental Station, IPB. The experiment was arranged in randomized block design (RBD) with two factors, namely nitrogen fertilizer and type of bacteria. The rates of N fertilizer (urea) factor, i.e. 0, 50, 75 and 100 kg N ha-1. The types of bacteria factor, i.e. without bacteria, Azotobacter-like, Azospirillum-like, and consortium. Data were analyzed using analysis of variance and followed by Duncan's Multiple Range Test (DMRT) with standard error 5%. The results of the laboratorium experiment showed that all isolates of bacteria performed no significant differences on N fixing capability. Field research showed that consortium of Azotobacter-like and Azospirillum-like applied with 75% of inorganic N fertilizer from recommended dosage the highest agronomic effectiveness (117.01%) and yield increase up to 8.59%. According to this result, application of consortium bacteria could reduce 25% recommended dosage of N inorganic fertilizer.
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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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