2009
DOI: 10.28930/jitkt.v1i2.7869
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Organochlorine Pesticides in the Coastal Sediment of Citarum Estuary, Jakarta Bay: The Imp Ortant Role of Fine Fraction of the Sediment as Their Agent Transport and Processes of Their Early Diagenesis

Abstract: DDT (1,1,ethane) and its two derivatives, DDD (1, and DDE (1, ABSTRAKDDT (1,1,1-Tricholor-2,2-bis(chlorophenil)ethane) dan dua derivativenya, DDD (1,1-Dicholor-2,2-bis(chlorophenil)ethane) dan DDE (1,1-Tricholor-2,2-bis(chlorophenil)-ethylene) telah diidentifikasi di sedimen pesisir muara Citarum, Teluk Jakarta. Delapan titik stasiun pengamatan pengambilan sample sedimen didesain agar diperoleh hasil perubahan nilai konsentrasinya semakin menjauh dari Muara Sungai yang dianggap sebagai sumber masukan. Contoh … Show more

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(2 citation statements)
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“…Unfortunately, due to the lack of sufficient data on mass sediment accumulation of mangrove and seagrass soils in Indonesia, it is not possible to derive an annual carbon burial rate. 129.9 ± 9.6 (n = 32) a An average sediment dry bulk density (g ml -1 ) of 0.92 was used for terrigenous deposits ) and 1.39 for carbonates (Campbell et al 2015) b Estimated using a median surface soil C org value of 0.595 % (by sediment dry weight) for these deposits (Booij et al 2001;Pratono et al 2009) c Soil depth only to 50 cm d Range of increasing soil dry bulk densities (g ml -1 ) with soil depth (Alongi, unpublished data) Wetlands Ecol Manage Such data is urgently needed. Sequestration rates can be derived for plant biomass (assuming such stocks are not burned or clear-felled), but these are wholly inadequate because soils account for 82 and 99 % of the total carbon reserves for the archipelago's mangroves and seagrasses, respectively (Tables 1, 2).…”
Section: Discussionmentioning
confidence: 99%
“…Unfortunately, due to the lack of sufficient data on mass sediment accumulation of mangrove and seagrass soils in Indonesia, it is not possible to derive an annual carbon burial rate. 129.9 ± 9.6 (n = 32) a An average sediment dry bulk density (g ml -1 ) of 0.92 was used for terrigenous deposits ) and 1.39 for carbonates (Campbell et al 2015) b Estimated using a median surface soil C org value of 0.595 % (by sediment dry weight) for these deposits (Booij et al 2001;Pratono et al 2009) c Soil depth only to 50 cm d Range of increasing soil dry bulk densities (g ml -1 ) with soil depth (Alongi, unpublished data) Wetlands Ecol Manage Such data is urgently needed. Sequestration rates can be derived for plant biomass (assuming such stocks are not burned or clear-felled), but these are wholly inadequate because soils account for 82 and 99 % of the total carbon reserves for the archipelago's mangroves and seagrasses, respectively (Tables 1, 2).…”
Section: Discussionmentioning
confidence: 99%
“…Teluk Jakarta merupakan muara dari 13 sungai (Prartono et al, 2009), yang mana curah hujan di sekitar daerah aliran sungai (DAS) sungai-sungai tersebut diangkut menuju Teluk Jakarta. Input dari sungai tentu mempengaruhi volume air di sekitar Teluk Jakarta, dan dapat menyebabkan banjir dari arah Teluk Jakarta menuju daratan sekitarnya.…”
Section: Pendahuluanunclassified