用Wien效应研究土壤有机质对阳离子与黄棕壤型水稻土黏粒相互作用的影响
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国家自然科学基金项目(40871114)


Effects of organic matter on interactions between cations and clay particles in paddy soil of Yellow-brown soil based on Wien effect
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    摘要:

    选择富含有机质的黄棕壤型水稻土,提取小于2 μm的黏粒,将其中1/2黏粒去除有机质,分别制成为不同阳离子(Na+ 、K+、NH4+、Ca2+、 Cd2+和 La3+)饱和的土样,用Wien 效应法研究土壤有机质对阳离子与土壤黏粒相互作用的影响。研究结果表明:原土悬液的起始电导率大于去有机质土者;除含Na+ 悬液外,去有机质土悬液的电导率随场强而增加的速率在50~100 kV cm-1以上,明显大于原土。有机质会使Na+ 以外的阳离子的平均结合自由能增大,Ca2+ 的结合能增加最大(增量为0.57 kJ mol-1),而Cd2+ 的结合能增加最小 (增量为0.03 kJ mol-1)。对于供试土壤悬液,不同阳离子的结合能顺序均为Na+ < K+ ≈ NH4+ < Ca2+ ≈ Cd2+ < La3+ 。有机质会使除Na+ 外阳离子的平均吸附自由能减小,K+ 和NH4+ 分别在50和70 kV cm-1以上时,Ca2+和Cd2+在50 kV cm-1以上,La3+ 在70 kV cm-1以上时原土的吸附能小于去有机质土,并随场强增加愈益明显,有机质会使阳离子难以剥离到溶液中。除Na+ 外去有机质土的阳离子剥离度明显大于原土,其差值(△Is)在不同阳离子间的顺序为:K+ < NH4+ < La3+ < Ca2+ < Cd2+,这表明有机质可使土壤黏粒吸着Cd2+ 最难剥离下来。对于饱和阳离子为Na+ 和 K+ 的土壤黏粒,有机质会使动电电位正移40 mV左右;对于含NH4+、Ca2+、Cd2+ 和 La3+的黏粒,有机质则使ζ电位负移17~36 mV。

    Abstract:

    Paddy soil derived from yellow-brown soil, rich in organic matter, was used to extract clay particles < 2 μm, half of which was deprived of organic matter, and then prepared into samples saturated with Na+,K+,NH4+,Ca2+, Cd2+ and La3+ cations, separately. Effects of organic matter (OM) on interactions between cations and soil clay particles were investigated with the aid of the suspension Wien effect. It was found that threshold electrical conductivity was higher in the suspensions of original soil than in the suspensions of OM-removed soils. In all the suspensions, except for Na+ -saturated one, the rate increasing electrical conductivity of the OM-removed soil suspensions with field strength in the range > 50~100 kV cm-1 was apparently higher than that of the original soil suspensions. OM increased the mean free binding energies of all the cations other than Na+, with the effect being the most significant on Ca2+, about 0.57 kJmol-1, and being the least on Cd2+, around 0.03 kJmol-1. In all the soil suspensions, binding energies of various cations followed the sequence of Na+ < K+ ≈ NH4+ < Ca2+ ≈ Cd2+ < La3+.OM reduced the mean free adsorption energies of all the cations except Na+. The effect was significant for NH4+ at field strengths > 70 kV cm-1, for K+, Ca2+ and Cd2+ at field strengths > 50 kV cm-1 and for La3+ at field strengths > 70 kV cm-1, and the difference got more obvious with increasing field strength. OM made it more difficult for cations adsorbed on clay particles to get released into the solution. Stripping intensities of the cations except Na+ were distinctly higher in the suspension of OM-removed soil than in the suspension of original soil, with the difference △Is following the order of K+ < NH4+ < La3+< Ca2+ < Cd2+, which indicated that OM made Cd2+ adsorbed on clay particles most difficultly strip off. In Na+ and K+ saturated soil clay particles, OM made zeta potential move towards positivity by 40 mV, but in clay particles saturated with NH4+,Ca2+,Cd2+and La3+, towards negativity by 17 ~ 36 mV.

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王令祥,王玉军,周东美,司友斌,李成保.用Wien效应研究土壤有机质对阳离子与黄棕壤型水稻土黏粒相互作用的影响[J].土壤学报,2012,49(4):716-724. DOI:10.11766/trxb201106070204 Wang Lingxiang, Wang Yujun, Zhou Dongmei, Si Youbin, Li Chengbao. Effects of organic matter on interactions between cations and clay particles in paddy soil of Yellow-brown soil based on Wien effect[J]. Acta Pedologica Sinica,2012,49(4):716-724.

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  • 收稿日期:2011-06-07
  • 最后修改日期:2012-02-29
  • 录用日期:2012-04-01
  • 在线发布日期: 2012-04-23
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