Institute of Oceanography, National Taiwan University, Taipei, Taiwan.
Mar Pollut Bull. 2011 May;62(5):1081-7. doi: 10.1016/j.marpolbul.2011.01.039. Epub 2011 Feb 23.
Dissolved and particulate Mn and Fe in the nearshore waters were determined at 27 stations along the west coast of Taiwan during 19-23 November 2004. The latitudinal distributions of Mn and Fe were very similar; however, the concentration in the dissolved phase was lower, whereas that in the particulate phase was higher in the northern regime. The higher percentage of Fe than Mn that was associated with particles resulted in a two-order of magnitude higher particle-water partition coefficient for Fe, K(d)(Fe), than that for Mn, K(d)(Mn). The removal fluxes of Mn and Fe could be estimated by multiplying the particulate (234)Th removal flux with the Mn/(234)Th and Fe/(234)Th ratios in suspended particles, which ranged from 0.1 to 3.8 mmol m(-2) d(-1) for Mn, and from 3.4 to 194.5 mmol m(-2) d(-1) for Fe. Residence times ranged from 1 to 20 days for Mn and Fe were estimated in the nearshore.
2004 年 11 月 19 日至 23 日,在台湾西海岸的 27 个站位测定了近岸水中溶解态和颗粒态的 Mn 和 Fe。Mn 和 Fe 的纬度分布非常相似;然而,在北部海域,溶解态的浓度较低,而颗粒态的浓度较高。与颗粒相结合的 Fe 比 Mn 的比例更高,导致 Fe 的颗粒-水分配系数 K(d)(Fe)比 Mn 的 K(d)(Mn)高两个数量级。Mn 和 Fe 的去除通量可以通过将颗粒相中 (234)Th 的去除通量与悬浮颗粒中 Mn/(234)Th 和 Fe/(234)Th 的比值相乘来估算,Mn 的比值范围为 0.1 至 3.8mmol m(-2) d(-1),Fe 的比值范围为 3.4 至 194.5mmol m(-2) d(-1)。Mn 和 Fe 的停留时间在近岸地区估计为 1 至 20 天。