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Abstract: A rock material is anisotropic if it's measurable physical properties such as velocity exhibit different values when measured in different directions. The safest assumption is that the subsurface is anisotropic. If anisotropy is ignored when imaging the subsurface, it could have adverse effects. These adverse effects include sub-optimal time-to-depth conversion, well-to-seismic mismatch, as well as a poorly focused seismic image. This paper presents the result of a seismic anisotropy study carried out on pre-stack depth migrated gathers in Greater Ughelli of the Niger Delta which is generally characterized by repeated sequence of finely layered sand/shale intercalations. These sand/shale sequences are generally bound to be transversely anisotropic. The signature of anisotropy on the depth migrated gathers is the so-called "hockey sticks''. The first hockey sticks on pre-stack depth migrated gathers were observed and used for the mapping. The onset of anisotropy was correlated across an entire field (Assa North) in Greater Ughelli depobelt using seismic depth structure maps and fault polygons. The onset of anisotropy ranges from 1400ms – 1600ms. Anisotropy trend in study area is shallow in the NE, of average depth at the middle of the field and very deep SW.
Keywords: Anisotropy, Depobelt, Hockey sticks, Sand/Shale Sequence, Sub-optimal
Keywords: Anisotropy, Depobelt, Hockey sticks, Sand/Shale Sequence, Sub-optimal
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[9] Vestrum Rob, 2002, 2D and 3D Anisotropic Depth Migration Case Histories, SEG, Salt Lake City,Utah 2002-1256 October 6 – 11 www.http://geology.um.maine.edu
[2] Ekweozor, C. M., and Daukoru, E.M, 1994, Northern delta depobelt portion of the Akata-Agbada petroleum system, Niger Delta, Nigeria, in, Magoon, L.B., and Dow, W.G., eds., The Petroleum System--From Source to Trap, AAPG Memoir 60: Tulsa, American Association of Petroleum Geologists, p. 599-614.
[3] Hospers, J., 1965, Gravity field and structure of the Niger Delta, Nigeria, West Africa: Geological Society of American Bulletin, v. 76, p. 407-422.
[4] Kaplan, A., Lusser, C.U., Norton, I.O., 1994, Tectonic map of the world, panel 10: Tulsa, American Association of Petroleum Geologists, scale 1:10,000,000.
[5] Klett, T.R., Ahlbrandt, T.S., Schmoker, J.W., and Dolton, J.L., 1997, Ranking of the world's oil and gas provinces by known petroleum volumes: U.S. Geological Survey Open-file Report-97-463, CD-ROM.
[6] Kulke, H., 1995, Regional Petroleum Geology of the World. Part II: Africa, America, Australia and Antarctica: Berlin, Gebruder Borntraeger, p. 143-172.
[7] Petroconsultants, 1996a, Petroleum exploration and production database: Houston, Texas, Petroconsultants, Inc., [database available from Petroconsultants, Inc., Houston, TX 77274-0619].
[8] Thomsen 1986, Weak elastic anisotropy, Geophysics. Vol.51. No. Io (October 1986); P. 1954-1966,
[9] Vestrum Rob, 2002, 2D and 3D Anisotropic Depth Migration Case Histories, SEG, Salt Lake City,Utah 2002-1256 October 6 – 11 www.http://geology.um.maine.edu
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Abstract: Quantum Dots now days have revolutionized the world. These are the nanoparticles having a size less than or around 10 nm. In this paper, an effort has been made to understand the general synthesis of the quantum dots and the thermo dynamical study of the quantum dot particles. The whole process of nucleation and growth is also explained in detail. Various applications of these quantum dots in the different fields of science and technology also been described.
Keywords: Bottom-Up Approach, Crystallization, Growth, Nucleation, Supersaturation, Top-Down Approach, Quantum Dot
Keywords: Bottom-Up Approach, Crystallization, Growth, Nucleation, Supersaturation, Top-Down Approach, Quantum Dot
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Abstract: Conducting polymers have attracted considerable attention in the recent years due to their unique thermal, electrical, optical and magnetic properties. These polymers have been conducive for fabrication of micro-electronic devices. Among these polymers, Polyaniline (PANI) possesses an exceptional properties including structural, thermal and electrical. We have synthesized PANI in Emeraldine salt form by chemical oxidation method with controlled pH3 by using Ammonium perdisulphate as oxidizing agent. The morphology of PANI has been determined by using X-Ray Diffraction (XRD), Scanning Electron Micrograms (SEM) and Dynamic Light Scattering (DLS). The studies revealed that Polyaniline possess rod like shape with radius around 75 nm and length around 617.6 nm. The DSC thermogram shows two exothermal peaks at around 97.07 oC and 152 oC, these peaks are attributed to the glass transition temperature (Tg) and PANI degradation temperature respectively. The final valley point (endothermic) around 175 oC is attributed to the melting point (Tm) of PANI. The voltage-current (V-I) characteristics of Polyaniline have studied at temperature 300 K. Due to semi crystalline solid nature of PANI, the transport of charge carriers may takes place in between and along PANI chains.
Key Words: Polyaniline, XRD, DLS, DSC, V-I characteristics, Exponent 'm'
Key Words: Polyaniline, XRD, DLS, DSC, V-I characteristics, Exponent 'm'
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[9] Wang, Lee W.T, Reed M.A Phys. Rev. B.68-035416. 2003
[2] Heeger A.J , Nobel lecture December 8 (2000)
[3] Gupta K, Jana P.C, and Melkap, A.K, Journal of Physical Sciences. 12, 233-238. (2008)
[4] Narsimlu N, Kuo Y.D, Chun Guey Wu Journal of applied polymer science 88, 3183-3187, (2003)
[5] Ghosh M, Mekap A.K, Chattopadhyay, Chatterjee. Journal of Physics and chemistry of Solids 62, 475-484 (2001)
[6] Cheng-Ho Chen. Journal of Applied Polymer science.89, 2142-2148 (2003)
[7] Gupta K.K, Jasnal M, Agarwal K, Indian Journal of fiber and Textile research33, 443-450 (2008)
[8] Jiaxing Huang and Richar B.Kaner, Hand Book of conducting Polymers.Processing and
Applications. 7-3, Third Edition (2006)
[9] Wang, Lee W.T, Reed M.A Phys. Rev. B.68-035416. 2003
