Liu Jingchun, Yan Chongling, Macnair Mark R, Hu Jun, Li Yuhong
School of Life Science, Xiamen University, Xiamen, Fujian 361005, China.
Environ Sci Pollut Res Int. 2007 Jul;14(5):345-9. doi: 10.1065/espr2006.05.306.
Acid-volatile sulfide (AVS) is operationally defined as sulfides in sediment, which are soluble in cold acid, and is reported as the most active part of the total sulfur in aquatic sediments. It is a key partitioning phase controlling the activities of divalent cationic heavy metals in sediment.
In order to examine this in mangrove environments, six sites were selected along the Jiulong River Estuary in Fujian, China, which had previously been reported to be polluted by heavy metals. Sediments were sampled from 0-60 cm depth at each site, and the spatial distribution of AVS and SEM (simultaneously extracted metals: copper, cadmium, zinc, and lead) were determined.
The results indicate that the AVS concentrations had a spatial variation, ranging from 0.24 to 16.10 pmol g(-1) sediment dry weight. The AVS concentration in the surface layer is lower than that of the deeper sediment, with peak values in the 15-30 cm horizon. There was no correlation between the AVS value and organic matter content or total dissolved salts, but a significant positive correlation of AVS with surface sediment (0-5 cm) moisture content was found. This indicates that water logged sediments tend to have a high AVS value. The amount of SEM was within the range of 0.33-2.80 micromol g(-1) sediment dry weight and decreased with sediment depth.
There was a marked variation in AVS and SEM among different sites studied. AVS concentrations were generally lower in the surface sediments, while SEM concentrations slightly decreased with the depth. Higher concentrations of SEM found in the upper layers of the sediments confirm the earlier suggestions that this study area may suffer from increasing heavy metal pollution.
When monitoring environmental impacts by using AVS, the micro and large-scale spatial variation as well as vertical distribution need to be estimated to avoid misleading results. Both AVS and SEM concentrations in different sediment layers should be taken into account in assessing the potential impact of heavy metals on the biotic environment,
酸挥发性硫化物(AVS)在操作上被定义为沉积物中可溶于冷酸的硫化物,据报道它是水生沉积物中总硫最活跃的部分。它是控制沉积物中二价阳离子重金属活性的关键分配相。
为了在红树林环境中对此进行研究,在中国福建九龙江口沿线选择了六个地点,这些地点先前已被报道受到重金属污染。在每个地点从0 - 60厘米深度采集沉积物,并测定AVS和同步提取金属(SEM:铜、镉、锌和铅)的空间分布。
结果表明,AVS浓度存在空间变化,范围为0.24至16.10皮摩尔/克沉积物干重。表层的AVS浓度低于较深层沉积物,在15 - 30厘米层位出现峰值。AVS值与有机质含量或总溶解盐之间没有相关性,但发现AVS与表层沉积物(0 - 5厘米)含水量存在显著正相关。这表明积水的沉积物往往具有较高的AVS值。SEM的含量在0.33 - 2.80微摩尔/克沉积物干重范围内,并随沉积物深度而降低。
在所研究的不同地点,AVS和SEM存在显著差异。表层沉积物中的AVS浓度通常较低,而SEM浓度随深度略有降低。在沉积物上层发现较高浓度的SEM证实了先前的推测,即该研究区域可能正遭受日益严重的重金属污染。
在利用AVS监测环境影响时,需要估计微观和宏观尺度的空间变化以及垂直分布,以避免产生误导性结果。在评估重金属对生物环境的潜在影响时,应考虑不同沉积层中的AVS和SEM浓度。