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首页> 外文期刊>Journal of plant nutrition and soil science >Considerations on cross-linking by bivalent cations in soil organic matter with low exchange capacity
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Considerations on cross-linking by bivalent cations in soil organic matter with low exchange capacity

机译:关于交联阳离子在土壤有机质中交联的考虑,交换能力低

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摘要

A soil's cation exchange capacity (CEC) is expected to be relatively inert against changes in cation loading. In this study, we treated a soil sample originating from the organic layer of a forest soil with various bivalent cations after removing the native cations. Sorption isotherms and cation exchange capacity were determined, the latter using the BaCl2 method. Sorption showed Langmuir characteristics, with the maximum coverage (Q(max)) increasing in the order Ba2+ Ca2+ Mg2+, but being clearly smaller than the initial load of native exchangeable cations. The Langmuir coefficient, k(Me), depended oppositely to the order obtained for Q(max). CEC increased upon cation treatment and it varied by a factor of almost two. The unexpected variation of CEC was explained by the low cation exchange capacity of the organic matter such that not all functional groups are close enough to be bridged and the second charge of a bivalent cation is not neutralized by the organic functional group. The Langmuir sorption type, and Q(max) being smaller than the content of sorption sites and being largest for Mg, suggested that only a part of the sites can be cross-linked and at least part of the cross-links are formed by hydrated cations. Thermodynamic considerations allowed reconstruction of two contrasting processes during CEC determination by Ba2+: Case A: the disruption of cross-links, which increases with the cationic strength and the cation load before CEC determination, but does not require structural re-orientation in the SOM matrix, and Case B: the formation of new cross-links during CEC determination, depending only on the content of unoccupied sites before CEC determination and requiring structural re-organization of the matrix and thus a minimum matrix flexibility. The use of bivalent cations for CEC determination may thus result in an overestimation of CEC for organic matter with low CEC. This has, however, promising potential when comparing CEC determined with mon
机译:预计土壤的阳离子交换能力(CEC)将相对令人讨论的阳离子负荷变化。在这项研究中,我们处理了源自森林土壤的有机层的土壤样品,在去除天然阳离子后,各种二价阳离子。测定吸附等温线和阳离子交换能力,后者使用Bacl2方法。吸附显示朗马尔特征,具有在订单Ba2 + +中增加的最大覆盖率(q(max))增加。 CA2 +& MG2 +,但显然比本机可交换阳离子的初始负载小。 Langmuir系数K(ME)依赖于对Q(MAX)获得的顺序。 CEC在阳离处理时升高,它几乎变化了一倍。通过有机物质的低阳离子交换能力解释了CEC的意外变化,使得并非所有官能团足够接近以桥接,并且有机官能团没有中和二价阳离子的第二电荷。 Langmuir吸附型和Q(MAX)小于吸附位点的含量并最大的mg,建议只有一部分的部位可以交联,并且至少部分地通过水合形成交联的交联阳离子。热力学考虑允许在CEC测定期间重建两个对比过程的BA2 +:案例A:交联的破坏,随着CEC确定前的阳离子强度和阳离子负荷增加,但不需要在SOM矩阵中的结构重新定位,以及CEC在CEC确定期间形成新的交叉链路的形成,仅取决于CEC之前的未占用位点的含量,并要求矩阵的结构重新组织并因此是最小矩阵灵活性。因此,使用对CEC测定的二价阳离子可能导致CEC的高估计,用于低CEC。然而,在将CEC与Mon确定的CEC比较时,这具有很有希望的潜力

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