Simulation test of the acid sulfate soil (ASS) included 5 treatments. They were 30% of field capacity (FHl), 70% of field capacity(FH2), inundated (INU), air-dried (DRY), and naturally air-dried (NAD). The test indicated that water was an important factor on the transformation between the forms of sulfur of ASS such as water soluble S, exchangeable S, and pyrite S.The test showed that wet but not inundated or over dried was benefit to the oxidation of pyrite and the formation of water soluble S and exchangeable S in ASS. During the whole simulation period, the increases of water soluble S content of the ASS from big to small were: FH2 > FH1 > INU; the increases of exchangeable S content of the ASS from big to small were: FHl > FH2 > INU; the decreases of pyrite S content of the ASS from big to small were: FH2 > FHl > INU.Significant transformation of S forms happened during the air-drying process of the NAD treatment. The dynamic of Jarosite-S, organic S and element S in all treatments are also discussed here.
刘振乾, 王建武*, 骆世明, 区美美. 酸性硫酸盐土中硫形态转化过程的水分制约作用[J]. , 2002, 21(1): 68-71.
Liu Zhenqian, Wangjianwu, Luo Shiming, Qu Meimei. Effects of soil moisture on the transformation between sulfur forms in acid sulfate soils. , 2002, 21(1): 68-71.
[7] Bronswijd J J B, Nugroho K, Aribawa I B et al. 1993.Modeling of oxygen transport and pyrite oxidation in acid sulphate soils [J].Journal of Environmental Quality. 22(3): 544~554
[8] Clark M W, Lancaster G, Mc Conchie D. 1996. Total sulphide acidity for the definition and assessment of acid sulphate hazard:simple solution or a new suite of problens[J]. The Science of the Total Envinmment,183,249~54
[9] Dent D. 1992. Reclamatin of acid sulfate soils[A]. Advances inSoil Science. Volume 17. New York: Springer-Verlag. 79~122
[10] Holmer M, Kristensen E, Banta G et al. 1994. Biogeochemical cycling of sulfur and iron in sediments of a Southeast Asian mangrove, Phuket Island, Thailand[J]. Biogeochemistry, 26, 145~61
[11] Lin C, Melville M D. 1993. Control of soils acidification by fluvial sedimentation in an estumine floodplain, eastern Australia [J].Sedimentary Geology, 85:1~13
[12] Mennut A R, Arshad M A. 1987. Significance of sulfide oxidation in soil salization in Southeastem Sasatchchewan[J]. Soil ScienceSociety of Ameaica, Journal, 51: 247~51
[13] Mirth L Q et al. 1998. Soil and water table mansagement effects on aluminum dynamics in an acid sulfate soil in Vietnam [J].Agri. Ecisys. Environ, 68(3): 255~262
[14] Sammut J, White I, Melville M D. 1996. Acidification of an estuarine tributary in eastern Australia due to drainage of acid sulfate soils[J]. Marine and Freshwatt researrch, 47: 669~684
[15] Wilkin R T, Barnes H L. 1996. Pyrite formation by reactions of iron monosulfide with dissolved inorganic and organic sulfur species [J]. Geochimica Cosmochimica Acta, 60:4167~4179