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草地、幼林和成熟林之间的铝形态和其他土壤特性比较。

Comparison of Al speciation and other soil characteristics between meadow, young forest and old forest stands.

机构信息

Department of Soil Science and Soil Protection, Czech University of Life Sciences Prague, Czech Republic.

出版信息

J Inorg Biochem. 2009 Nov;103(11):1459-64. doi: 10.1016/j.jinorgbio.2009.07.024. Epub 2009 Aug 15.

Abstract

The aim of this paper is to describe the influence of spruce (Picea abies) afforestation on soil chemical properties, especially on soil acidity and aluminium (Al) mobilization and speciation in soil. For our study we used a unique set of three adjacent plots, including a meadow and two spruce forest stands of different age, in otherwise comparable conditions. The plots were located in the region of Giant Mountains, north-eastern Czech Republic. In general, pH values decreased and Al concentrations increased significantly after afforestation. Speciation of KCl-extractable and water-soluble Al in soil samples was done by means of HPLC/IC method. The concentrations of Al(X)(1+) and Al(Y)(2+) forms (in both extracts) are higher in humic and organically enriched (Bhs) horizons. The highest concentration of Al(3+) in both extracts is in the B horizons of old forest. Generally, in all studied stands majority of Al in aqueous extract is in the Al(X)(1+) form, which indicates that a large amount of mobile Al is bound in organic complexes. It suggests that actual toxicity is rather low. On the other hand, we have proved that majority of KCl-extractable Al exists in Al(3+) form. Thus we can conclude that disturbance of existing equilibrium may cause massive release of highly toxic Al(3+) from soil sorption complex to the soil solution, and consequently it can endanger the whole ecosystem. Moreover, continuous soil acidification accelerated by anthropogenic factors leading to Al mobilization represents a chemical time bomb.

摘要

本文旨在描述云杉(Picea abies)造林对土壤化学性质的影响,特别是对土壤酸度和铝(Al)的活化和形态的影响。为了进行研究,我们使用了一组独特的三个相邻的样地,包括草地和两个不同年龄的云杉林,其他条件相似。样地位于捷克共和国东北部的 Giant 山脉地区。总的来说,造林后土壤的 pH 值降低,Al 浓度显著升高。通过 HPLC/IC 方法对土壤样品中 KCl 可提取和水溶性 Al 的形态进行了分析。Al(X)(1+)和 Al(Y)(2+)形态(两种提取物中)的浓度在腐殖质和有机富化(Bhs)层中较高。两种提取物中 B 层的 Al(3+)浓度最高。总体而言,在所有研究的林分中,水提取液中大部分 Al 以 Al(X)(1+)的形式存在,这表明大量的可移动 Al 被结合在有机复合物中。这表明实际毒性较低。另一方面,我们已经证明,大部分 KCl 可提取的 Al 以 Al(3+)的形式存在。因此,我们可以得出结论,现有平衡的干扰可能导致大量高毒性的 Al(3+)从土壤吸附复合物中释放到土壤溶液中,从而危及整个生态系统。此外,由人为因素引起的持续土壤酸化加速了 Al 的活化,这代表了一个化学定时炸弹。

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