Judul: Komputasi dan Analisis Kecepatan Rambat Gelombang Seismik di Perairan Tarakan Bagian Timur Provinsi Kalimantan Utara
Abstrak: Tarakan is one of the largest oil and gas producing regions in the new province. The existence of layers of rock containing reservoir which can trap hydrocarbons and coal makes Tarakan research areas of interest to be explored further by seismic methods. Seismic survey is a method currently used to determine the structure of the seabed, the depth of the ocean, oil and gas as well as sediment. Reflection seismic exploration is divided into two shallow seismic and seismic normally used to search for oil and gas. In the recording of seismic data in the sea, there is a lot of interference which appear as multiple, self-noise emanating from the tool used, wind, waves, and rain. One of the consequences caused by noise when recording in the field is the multiple that could interfere in the interpretation of seismic signals, it is necessary for the processing or signal processing to reduce the multiple effects. One that can be done is to increase the signal to noise ratio (SNR) through the analysis of the true velocity and in accordance with the subsurface geological conditions which is close to real situation, so that the returning signal is actually a representation of the subsurface geology without signals originating from multiple and noise. The purpose of this study is to measure the sound velocity obtained from seismic surveys and analyze the results. The study lasted for eight months which was started with the acquisition of seismic survey data that have been carried out in September - October 2012 in the sea east of Tarakan, Northern Kalimantan. This area is located at coordinates 3 ° 19 'N - 3 ° 20' N and 118 ° 34 'E - 119 ° 38 'E. Data was processed at the Ocean Acoustic Data Computation Laboratory, Department of Marine Science and Technology, Faculty of Fisheries and Marine Science, Bogor Agricultural University and at the Marine Geological Institute Bandung. Seismic data processing used Landmark ProMAX software. Data in the format SEG-D, then the data was processed so it produced data in the format SEG-Y which free noise and multiple. The raw data survey SEG-D was the main data input in this study which was then done geometric correction, trace muting, low cut filter, True Amplitude Recovery (TAR), deconvolution. Common Deep Point (CDP) is a term in seismic data taking for source-receiver configuration where there is a fixed point below the earth's surface. This CDP was then analyzed velocity root mean square (rms). The first velocity analysis was done by picking every 250 CDP and showed that the results was not good enough, it was known by the visible presence of multiple processes that must have been done to eliminate them using radon demultiple. The second velocity analysis done every 125 CDP and cross-sectional display showed that the results was better than before. The next process used the Normal Move Out (NMO) which was used to eliminate the effects of distance and Stacking. Furthermore, the velocity results that have been obtained could be seen in the table menu on promax software which was
Keyword: seismic, sound velocity, promax

Judul: Kuantifikasi frekuensi dan resolusi menggunakan seismik refleksi di Perairan Maluku Utara
Abstrak: Survei seismik merupakan metode yang saat ini digunakan untuk menentukan struktur dasar laut, kedalaman laut, minyak dan gas maupun sedimen. Seismik refleksi bekerja terhadap perubahan kecepatan sebagai fungsi kedalaman serta merekam dan menggunakan semua medan gelombang yang direkam. Tujuan dari penelitian ini adalah mempelajari pengaruh frekuensi terhadap resolusi penampang seismik dengan menggunakan berbagai variasi filtering (Bandpass filter) dengan menganalisis spektrum frekuensi pada software Seisee dan Matlab. Penelitian ini diawali dengan penelitian lapang pada bulan April-Mei 2010 di Perairan Maluku Utara yang termasuk ke dalam Kabupaten Luwuk Banggai, Provinsi Sulawesi Tengah. Daerah ini terletak pada koordinat 2° LS - 4° LS dan 123 ° BT - 126° BT. Pengolahan data dilakukan di Laboratorium Akustik Kelautan, Departemen Ilmu dan Teknologi Kelautan, Institut Pertanian Bogor dan di Pusat Penelitian dan Pengembangan Geologi Kelautan (PPPGL) di Bandung. Pengolahan data seismik menggunakan data dalam format SEG-Y. Data tersebut dibuka pada software Seisee dan dilakukan pemilihan trace kemudian disimpan. Data dibuka kembali pada program Excell untuk diambil amplitudo dan waktu (Lampiran 1) kemudian simpan dalam format *.txt agar dapat diolah dengan FFT di Matlab. Hasil dari FFT berupa grafik amplitudo spektrum dengan frekuensi yang selanjutnya dilihat nilai terendah dan tertinggi sehingga dapat menjadi acuan saat digunakan filter Bandpass filter pada perangkat lunak Seisee. Koefisien refleksi sebagai fungsi dari kecepatan gelombang P dan densitas masing-masing lapisan batuan. Pada contoh data coring yang terdapat di sekitar lintasan (titik sampling 30 dan 31) dicari nilai koefisien refleksi (Lampiran 4) dengan menggunakan rumus : Koefisien Refleksi (R) = , dengan = Impedansi akustik dari air laut dan = impedansi akustik dari sedimen. Sedangkan untuk rumus Impedansi : Z = ρc dengan ρ adalah densitas (Kg/m3) dan c adalah cepat rambat (m/s).
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Judul: Sintesis dan Pencirian Kompleks Fe(III)-Kuersetin
Abstrak: Quercetin belongs to flavonols which is able to chelate metal ions. Quercetin may chelate metal ions at 3’,4’-catechol, 3- or 5-hydroxycromone sites. In this study, quercetin was complexed with Fe(III). The complex with Fe(III) ions from FeCl3·6H2O was more stable than the complex derived from Fe(NO3)3·9H2O. The quercetin was yellow in color and showed maximum wavelengths (λ􀭫􀭟􀭶) at 250 and 370 nm. The Fe(III)-quercetin complex from Fe(NO3)3·9H2O was yellowish green with 􀟣􀭫􀭟􀭶 at 280 and 420 nm, whereas that from FeCl3·6H2O was dark green with 􀟣􀭫􀭟􀭶 at 280 and 430 nm. The 􀟣􀭫􀭟􀭶 shift indicated that the complex was formed at 3-hydroxychromone site. The Fe(III)- quercetin complex was formed with 1:1 metal-ligand mole ratio based on atomic absorption spectrophotometry analysis and the X-ray diffractogram showed that the crystallinity of the complex was 37%.
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