Mercury in soil derived from igneous rock in Northern Kyushu, Japan

Abstract

Soil profiles with different vegetation, developed on igneous rock-derived areas in Northern Kyushu have been sampled at 13 locations and analyzed for total Hg with a flameless atomic absorption spectrometer. The associated parent rock was also analyzed. The Hg levels of each rock sample were too low, not exceeding 10 ppb, to exert a significant effect within the profiles on the total Hg content. The Hg content was generally higher in the soil than in the underlying rock, irrespective of the depth of the horizon. Surface enrichment of Hg was observed at most of the sample sites, some paddy fields in particular, resulting in steep concentration gradient down the profiles. The total Hg in all the surface horizons ranged from 459 to 64 ppb with a mean of 197 ppb. Obviously, mercurial application in recent years was a principal factor above all with regard to the establishment of the elevated Hg levels in the upper soil horizon under cultivation. Man-made loading of this element, probably through rain, was indicated even in the soils under natural vegetation, after taking into account a possible residual Hg concentration in the soil formation process. A close relationship in the profile distribution pattern between total Hg and organic matter contents was observed. This fact, in conjunction with the results of pyrolysis studies, did suggest that a large proportion of the total Hg in these soils could be firmly held by chemical forces, very likely as highly insoluble organic complexes.