Institute of Oceanography, National Taiwan University, P.O. Box 23-13, Taipei 106, Taiwan.
Mar Pollut Bull. 2012 Feb;64(2):214-20. doi: 10.1016/j.marpolbul.2011.11.031. Epub 2011 Dec 27.
Dissolved and particulate (210)Pb and (210)Po were determined at 15 stations along the coastline off western Taiwan in April 2007. The (210)Pb activities in dissolved and particulate phases fell within a relatively small range of 2.4-5.2 dpm 100 L(-1) and 1.0-3.2 dpm 100 L(-1), respectively. The dissolved and particulate (210)Po activities also fell within a small range of 0.8-3.4 dpm 100 L(-1) and 1.1-2.9 dpm 100 L(-1), respectively. The correlation of the distribution coefficients (K(d)) of (210)Pb and (210)Po with particle concentration in turbid waters are not as evident as in the open ocean. The mass balance calculation shows that the residence times of (210)Pb and (210)Po with respect to particle removal from the nearshore waters ranges from 3 to 15 days and from 14 to 125 days, respectively. The flux of particulate organic carbon was estimated by (210)Po proxy and ranged from 4.8 to 33.7 mmol-C m(-2) d(-1).
2007 年 4 月,在台湾西部沿海的 15 个站位测定了溶解态和颗粒态(210)Pb 和(210)Po。溶解态和颗粒态(210)Pb 的活度分别在 2.4-5.2 dpm 100 L(-1)和 1.0-3.2 dpm 100 L(-1)的较小范围内变化。溶解态和颗粒态(210)Po 的活度也分别在 0.8-3.4 dpm 100 L(-1)和 1.1-2.9 dpm 100 L(-1)的较小范围内变化。浊度水中(210)Pb 和(210)Po 的分布系数(K(d))与颗粒浓度的相关性不如开阔海域明显。质量平衡计算表明,(210)Pb 和(210)Po 相对于近岸水体中颗粒去除的停留时间分别为 3-15 天和 14-125 天。通过(210)Po 示踪剂估算的颗粒有机碳通量范围为 4.8-33.7 mmol-C m(-2) d(-1)。