期刊
AUSTRALIAN JOURNAL OF SOIL RESEARCH
卷 42, 期 5-6, 页码 547-551出版社
C S I R O PUBLISHING
DOI: 10.1071/SR03088
关键词
hydrogeochemistry; rate of leaching; drainage; runoff
类别
The leaching of sulfur ( S) and metals (Al, Ca, Cd, Co, Cu, Fe, K, Mg, Mn, Ni, Zn) from an acid sulfate soil ( ASS) area in western Finland was determined on the basis of hydrochemical analyses (ICP-MS) of water samples collected monthly for 3 years from the stream draining that area. The average annual amount of leaching was as follows (kg/ha. year): S ( 633), Ca ( 281), Mg ( 199), Al ( 54), K ( 54), Mn ( 35), Fe (5.6), Zn ( 1.7), Ni (0.84), Co (0.79), Cu (0.070), Cd (0.0068). These high values are due to extensive oxidation of metal sulfides and weathering of minerals in the ASS pro. le. Calculations showed that other S inputs such as deposition and fertiliser use, and S outputs such as degassing and plant removal, are insignificant in comparison with current leaching losses. Before the area was artificially drained, the leaching losses of S from the study area must have been very small; otherwise, the S residual in the soil would have been depleted a long time ago. With current drainage practices, the leachable soil S residual will be halved in roughly 30 years, after which the S and metal loads of the drainage will have decreased. However, more time is needed before the concentrations will have decreased to an environmentally acceptable level, unless environmentally friendly measures are found and implemented.
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