PERUBAHAN SPASIAL DISSOLVED ORGANIC MATTER (DOM) DI PERAIRAN YANG MENDAPATKAN PENGARUH DARI DARATAN

Authors

  • I G. N. A. Suryaputra Universitas Pendidikan Ganesha

DOI:

https://doi.org/10.23887/wms.v8i1.11856

Keywords:

dissolved organic matter, dissolved organic carbon, total dissolved nitrogen, principal component analysis

Abstract

Penelitian ini bertujuan untuk mengetahui hal-hal yang mempengaruhi dissolved organic matter (DOM) di perairan yang mendapatkan pengaruh dari daratan. Sampel diambil dari empat stasiun di lepas pantai Teluk Meksiko pada beberapa kedalaman. Salinitas, suhu, dan kedalaman diukur dengan menggunakan sensor CTD. Oksigen terlarut dan klorofil-a diukur dengan menggunakan sensor multiparameter dari YSI. Konsentrasi dissolved organic carbon (DOC) dan total dissolved nitrogen (TDN) diukur dengan menggunakan Shimadzu TOC Analyzer yang dilengkapi dengan detektor nitrogen total. Analisis data dengan menggunakan principal component analysis (PCA) menunjukkan bahwa secara spasial, DOM dipengaruhi oleh dua hal utama, yaitu jarak dari daratan dan kedalaman air.

References

Abril, G., Nogueira, M., Etcheber, H., Cabeçadas, G., Lemaire, E., & Brogueira, M. J. (2002). Behaviour of organic carbon in nine contrasting European estuaries. Estuarine, Coastal and Shelf Science, 54(2), 241-262.

Blough, N. V., & Del Vecchio, R. Distribution and dynamics of chromophoric dissolved organic matter (CDOM) in the coastal environment, Hansell D., Carlson C., Biogeochemistry of Marine Dissolved Organic Matter, 2002, 509-546.

Bratbak, G., & Thingstad, T. F. (1985). Phytoplankton-bacteria interactions: an apparent paradox? Analysis of a model system with both competition and commensalism. Marine ecology progress series. Oldendorf, 25(1), 23-30.

Dagg, M. J. (1974). Loss of prey body contents during feeding by an aquatic predator. Ecology, 903-906.

Dittmar, T., Paeng, J., Gihring, T. M., Suryaputra, I. G. N. A., & Huettel, M. (2012). Discharge of dissolved black carbon from a fire-affected intertidal system. Limnology and Oceanography, 57(4), 1171.

Fogg, G. E. (1966). The extracellular products of algae. Oceanogr. Mar. Biol. Annu. Rev, 4(19), 212.

Guo, L., & Santschi, P. H. (2000). Sedimentary sources of old high molecular weight dissolved organic carbon from the ocean margin benthic nepheloid layer. Geochimica et Cosmochimica Acta, 64(4), 651-660.

Herbert, B. E., Bertsch, P. M., McFee, W. W., & Kelly, J. M. (1995). Characterization of dissolved and colloidal organic matter in soil solution: a review. In Carbon forms and functions in forest soils. (pp. 63-88). Soil Science Society of America Inc.

Kim, T. H., Waska, H., Kwon, E., Suryaputra, I. G. N. A., & Kim, G. (2012). Production, degradation, and flux of dissolved organic matter in the subterranean estuary of a large tidal flat. Marine Chemistry, 142, 1-10.

Lampert, W. (1978). A field study on the dependence of the fecundity of Daphnia spec. on food concentration. Oecologia, 36(3), 363-369.

Mozeto, A. A., Silvério, P. F., & Soares, A. (2001). Estimates of benthic fluxes of nutrients across the sediment–water interface (Guarapiranga reservoir, São Paulo, Brazil). Science of the total environment, 266(1), 135-142.

Nybakken, J. W. (1993). Marine biology: an ecological approach.

Otto, S., & Balzer, W. (1998). Release of dissolved organic carbon (DOC) from sediments of the NW European Continental Margin (Goban Spur) and its significance for benthic carbon cycling. Progress in Oceanography, 42(1), 127-144.

Santos, I. R., Burnett, W. C., Chanton, J., Mwashote, B., Suryaputra, I. G. N. A., & Dittmar, T. (2008). Nutrient biogeochemistry in a Gulf of Mexico subterranean estuary and groundwater-derived fluxes to the coastal ocean. Limnol. Oceanogr, 53(2), 705-718.

Sugimura, Y., & Suzuki, Y. (1988). A high-temperature catalytic oxidation method for the determination of non-volatile dissolved organic carbon in seawater by direct injection of a liquid sample. Marine Chemistry, 24(2), 105-131.

Sullivan, A. B., Snyder, D. M., & Rounds, S. A. (2010). Controls on biochemical oxygen demand in the upper Klamath River, Oregon. Chemical Geology, 269(1), 12-21.

Suryaputra, I G. N. A. (2014). Sumber-sumber Masukan Dissolved Organic Matter (DOM) di Teluk Meksiko. Seminar Nasional Optimalisasi Peran MIPA dan Pendidikan MIPA dalam Pengembangan IPTEKS. Singaraja.

Suryaputra, I G. N. A. (2013). Variabilitas Dissolved Organic Carbon (DOC) dan Total Dissolved Nitrogen (TDN) di Teluk Meksiko. Seminar Nasional Peningkatan Mutu MIPA dan Pendidikan MIPA untuk Mendukung Implementasi Kurikulum 2013. Singaraja.

Suzuki, Y., Sugimura, Y., & Itoh, T. (1985). A catalytic oxidation method for the determination of total nitrogen dissolved in seawater. Marine Chemistry, 16(1), 83-97.

Tyler, A. C., McGlathery, K. J., & Anderson, I. C. (2003). Benthic algae control sediment-water column fluxes of organic and inorganic nitrogen compounds in a temperate lagoon. Limnology and Oceanography, 48(6), 2125-2137.

Yin, K., Lin, Z., & Ke, Z. (2004). Temporal and spatial distribution of dissolved oxygen in the Pearl River Estuary and adjacent coastal waters. Continental Shelf Research, 24(16), 1935-1948.

Downloads

Published

2017-08-26

Issue

Section

Articles