SOME OCEANOGRAPHIC FEATURES OF PELABUHANRATU BAY, WEST JAVA, INDONESIA

H. Akbar, A. Wizemann, A. Ervinia, H. Ilyas, Hendra Pangkey, K. Kristiyanto, Neira Purwanty Ismail, Singgih Afifa Putra
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Abstract

Pelabuhanratu Bay plays a big role for the flow of nutrients from the land to the sea of Sothern-Java. This study was conducted in Pelabuhanratu Bay, Sukabumi, West Java, in March 2012. The aim of this study is to measure the oceanographic parameters (physical and chemical) of Pelabuhanratu Bay i.e. tides, waves, current, temperature, salinity, depth, density, dissolved oxygen (DO), total suspended solids (TSS), turbidity, pH and nutrients. The bay directly faces the Indian Ocean, during the surveyed we found mean angle of wave refraction was about ~4.3° ± 1.5°, with left side wind direction. Overall the current direction has an irregular trend. The tidal cycle of the bay is diurnal, with the temperature decrease into the deep layer. Only the surface exhibits a slightly lower salinity compared to the rest of the water column. Some parameters (i.e. TSS, DO) found in high concentration but declining following the depth. Other chemical concentrations (e.g. ortho-phosphate, silicate) also showed diminished after 10-15 depth measurement.
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印尼西爪哇pelabuhanratu湾的一些海洋学特征
毗拉布汉拉图湾对从陆地到南爪哇海洋的营养物质流动起着重要作用。这项研究于2012年3月在西爪哇素kabumi的Pelabuhanratu湾进行。本研究的目的是测量Pelabuhanratu湾的海洋参数(物理和化学),即潮汐、波浪、水流、温度、盐度、深度、密度、溶解氧(DO)、总悬浮固体(TSS)、浊度、pH值和营养物质。该海湾正对印度洋,在观测过程中,波的平均折射角约为~4.3°±1.5°,风向偏左。总的来说,目前的方向有一个不规则的趋势。海湾的潮汐周期是昼夜交替的,温度下降到深层。与水柱的其他部分相比,只有表面的盐度略低。某些参数(如TSS、DO)浓度较高,但随深度的增加而下降。其他化学物质的浓度(如正磷酸盐、硅酸盐)也在10-15深度测量后下降。
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