DISTRIBUSI POLA AEROSOL DI WILAYAH INDUSTRI BALONGAN DAN SURALAYA (Aerosol Distribution in The Industry Areas of Balongan and Suralaya)
Eko Heriyanto(1*), Kadarsah Kadarsah(2), Radyan Putra Pradana(3)
(1) Pusat Penelitian dan Pengembangan, Badan Meteorologi Klimatologi dan Geofisika, Jalan Angkasa 1 No.2, Kemayoran Jakarta Pusat, DKI Jakarta 10720.
(2) Pusat Penelitian dan Pengembangan, Badan Meteorologi Klimatologi dan Geofisika, Jalan Angkasa 1 No.2, Kemayoran Jakarta Pusat, DKI Jakarta 10720.
(3) Pusat Penelitian dan Pengembangan, Badan Meteorologi Klimatologi dan Geofisika, Jalan Angkasa 1 No.2, Kemayoran Jakarta Pusat, DKI Jakarta 10720.
(*) Corresponding Author
Abstract
Abstrak
Kajian ini bertujuan untuk mengidentifikasi distribusi aerosol yang aktual dan dominan dari kegiatan yang melepaskan emisi polutan, khususnya di sekitar wilayah industri Pertamina-Balongan dan PLTU-Suralaya. Parameter distribusi aerosol, planetary boundary layer dan angin didapatkan dari alat Lidar. Pengukuran pada kedua lokasi menunjukkan tren kenaikan aktivitas polutan setelah pukul 08.00 WIB, distribusi aerosol pekat Pertamina-Balongan berada pada kisaran 800–1400 mdpl, sedangkan wilayah PLTU-Suralaya bervariasi pada kisaran 500-6500 mdpl. Sebaran partikel aerosol disimulasikan menggunakan model dispersi untuk mengetahui pola arah sebaran.
Abstract
This study aims to identify distribution of the aerosol as the pollutants emissions affected by the selected industrial activity i.e. Pertamina-Balongan and PLTU-Suralaya. Distribution of aerosols parameter, planetary boundary layer, and wind were measured by Lidar. The measurement at both locations showed an increasing trend in pollutant emission at morning local times after 8 AM. The dispersion of aerosol in Pertamina-Balongan dominate at the altitudes of 800-1400 masl, while in PLTU-Suralaya area varies at the range 500-6500 masl. Dispersion of the aerosols was simulated using a dispersion model to determine the direction of the dispersion.
Keywords
Full Text:
PDFReferences
Draxler, R.R., and Hess, G.D., 1998. An Overview of The Hysplit_4 Modelling System for Trajectories. Australian Meteorological Magazine, 47(4):295-308.
Kanda, M., Moriwaki, R., Roth, M., and Oke, T.R., 2002. Area-averaged Sensible Heat Flux and A New Method to Determine Zero-Plane Displacement Length Over an Urban Surface Using Scintillometry. Boundary-Layer Meteorology, 105:177-193.
Lagouarde, J.P., Irvine, M., Bonnefond, J.M., Grimmond, C.S.B., Oke, T.R., Salmond, J., and Offerle, B., 2006. Monitoring The Sensible Heat Flux Over Urban Areas Using Large Aperture Scintillometry: Case Study of Marseille City During The Escompte Experiment. Boundary-Layer Meteorology, 118:449-476.
Landsberg, H, 1981. The Urban Climate. London: Academic Press, Inc.
Oke, T.R., 2006. Initial Guidance to Obtain Representative Meteorological Observations at Urban Sites. World Meteorological Organization, Instruments and Observing Methods, IOM Report No. 81, WMO/TD-No. 1250
Oke, T.R., 1976: The Distinction Between Canopy and Boundary-Layer Urban Heat Islands. Atmosphere, 14:268-277.
Oke, T.R., 1987: Boundary Layer Climates. 2nd ed. Methuen, London.
Stein, A.F., Draxler, R.R., Rolph, G.D., Stunder, B.J.B., Cohen, M.D., and Ngan, F., 2015. NOAA’s HYSPLIT Atmospheric Transport and Dispersion Modeling System. Bulletin of the American Meteorological Society, 96(12):2059-2077.
Voogt, J.A., and Oke, T.R., 1997: Complete Urban Surface Temperatures. Journal of Applied Meteorology, 36:1117-1132.
DOI: https://doi.org/10.22146/jml.24142
Article Metrics
Abstract views : 2450 | views : 2870Refbacks
- There are currently no refbacks.
Copyright (c) 2020 Jurnal Manusia dan Lingkungan
This work is licensed under a Creative Commons Attribution-ShareAlike 4.0 International License.
JML Indexed by:
View My Stats