Fluktuasi Nitrat dan Fosfat Selama Satu Periode Pasang dan Surut di Selat Lombok

I. G. Sumantra, Yulianto Suteja, I. N. W. Putra
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引用次数: 1

Abstract

Nitrate (NO3-) and phosphate (PO43-) are two parameters of water quality that are important for aquatic organism. Circulation of ocean currents can distribute nitrate and phosphate from one place to another. The current pattern in the waters of the Lombok Strait at the time of the tide moves from the north to the south by bringing the mass of water from the Pacific Ocean, while the movement of the current pattern at low tide moves from south to north by bringing the mass of water from the Indian Ocean. Therefore, this study aims to determine the fluctuations of Nitrate (NO3-) and Phosphate (PO43-) in Lombok Strait during one tidal period. This research was conducted on 3 - 5 November 2017 precisely at coordinates 116?1'18 "LS; -8?34'12 "BT. Sampling is done directly in the field. Seawater samples are taken on the surface and at a depth of 10 meters for 1 x 24 hours with an interval every 2 hours using a Vertical Water Sampler. Measurement of nitrate parameter using spectrophotometric method with Spectrophotometer SNI 6989 79-2011, while phosphate parameter using spectrophotometric method with UV-Vis Spectrophotometer, refer to SNI 06-6989 31-2005. The concentration of nitrate and phosphate at each time in the analysis and seen fluctuations. The concentration of nitrate and phosphate in Lombok Strait fluctuated during one tidal period. At high tide conditions, the concentrations of nitrate and phosphate are low and at low tide conditions high nitrate and phosphate concentrations.
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在龙目岛海峡的潮汐和退潮期间,硝酸盐和磷酸盐的波动
硝酸盐(NO3-)和磷酸盐(PO43-)是对水生生物至关重要的两个水质参数。洋流的循环可以将硝酸盐和磷酸盐从一个地方传播到另一个地方。龙目岛海峡水域在涨潮时的洋流模式是通过从太平洋带来大量的水而从北向南移动,而在退潮时的洋流模式是通过从印度洋带来大量的水而从南向北移动。因此,本研究旨在测定龙目岛海峡中硝酸盐(NO3-)和磷酸盐(PO43-)在一个潮汐期的波动。本研究于2017年11月3日至5日在坐标116?1 ' 18”LS;8 ?34'12 "BT.采样直接在现场完成。使用垂直水采样器在海面和10米深处采集海水样本,每次1 x 24小时,每隔2小时采样一次。硝酸盐参数测量采用分光光度法,分光光度计SNI 6989 79-2011,而磷酸盐参数测量采用分光光度法,紫外可见分光光度计,参考SNI 06-6989 31-2005。硝酸盐和磷酸盐的浓度在每次分析中都出现了波动。龙目岛海峡的硝酸盐和磷酸盐浓度在一个潮汐期间波动。在涨潮时,硝酸盐和磷酸盐的浓度低,而在退潮时,硝酸盐和磷酸盐的浓度高。
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