Nordmyr Linda, Osterholm Peter, Aström Mats
Department of Geology and Mineralogy, Abo Akademi University, 20500 Abo, Finland.
Mar Environ Res. 2008 Sep;66(3):378-93. doi: 10.1016/j.marenvres.2008.06.001. Epub 2008 Jun 17.
The estuarine behaviour of the metal load leaching from acid sulphate (AS) soils was studied in a selected river system (the Vörå River), in western Finland. Large amounts of metals were transported with the river and deposited within the estuary, causing highly elevated metal concentrations in both the sediment traps and in the underlying bottom sediments. Among the metals, there was a diverging deposition pattern where Al, Cu, La and U demonstrated a strong association with organic matter and were deposited within approximately 4 km from the river mouth. In contrast, the deposition of Co, Mn, Ni and Zn occurred when pH reached circumneutral conditions further out in the estuary. Yet other metals were not abundantly leached from the AS soils and thus not elevated in the river and estuary (Fe, Ti, Cr, V). Five separate chemical extractions indicated the geochemical speciation of the metals.
在芬兰西部一个选定的河流系统(沃拉河)中,对酸性硫酸盐(AS)土壤中金属负荷淋溶的河口行为进行了研究。大量金属随河流输送并沉积在河口内,导致沉积物捕集器和下层底部沉积物中的金属浓度大幅升高。在这些金属中,存在一种不同的沉积模式,其中铝、铜、镧和铀与有机物有很强的关联,并在距河口约4公里范围内沉积。相比之下,钴、锰、镍和锌的沉积发生在河口更远处pH值达到中性条件时。还有其他一些金属没有从AS土壤中大量淋溶出来,因此在河流和河口没有升高(铁、钛、铬、钒)。五种单独的化学萃取方法表明了金属的地球化学形态。