Behaviour of aluminium in forest soils with different lithology and herb vegetation cover.

J Inorg Biochem

Department of Soil Science and Soil Protection, Faculty of Agrobiology, Food and Natural Resources, Czech University of Life Sciences Prague, Kamýcká 129, 165 00 Prague - Suchdol, Czech Republic.

Published: April 2018

AI Article Synopsis

  • - The study investigated how aluminum (Al) behaves in soils beneath beech forests with different types of parent rock, while also examining how herbaceous vegetation affects this behavior.
  • - Researchers hypothesized that the presence of vegetation significantly influences the soil's content of elements like aluminum, and low molecular mass organic acids (LMMOA) indicate the decomposition of soil organic matter and litter turnover.
  • - Findings showed that areas with less herbaceous vegetation had lower pH and nutrient levels, higher soil organic matter, and larger aluminum pools, indicating that LMMOA and vegetation cover are crucial for understanding the aluminum soil cycle.

Article Abstract

The aim of this study was to determine the content, distribution and behaviour of Al in soils under beech forest with different parent rock, and to assess the role of herbaceous vegetation on soil Al behaviour. We hypothesize that the contents of elements in the soil sorption complex (Al etc.) are strongly influenced by vegetation cover. Also, low molecular mass organic acids (LMMOA) can be considered as an indicator of soil organic matter (SOM) decomposition and vegetation litter turnover. Speciation of LMMOA, nutrition content (PO, Ca, K) and element composition in aqueous extracts were determined by means of ion chromatography and inductively coupled plasma - optical emission spectrometry (ICP-OES) respectively. Active and exchangeable pH, sorption characteristics and exchangeable Al (Al) were determined in BaCl extracts by ICP-OES. Elemental composition of parent rocks was assessed by means of X-ray fluorescence spectroscopy. Herb-poor localities showed lower pH, less nutrients (PO, Ca, K), less LMMOA, a larger stock of SOM and greater cation exchange capacity. There was also lower mobilisation of Al in organic horizons, which explains the larger pools of Al. Generally, we can conclude that LMMOA, and thus soil vegetation cover, play an important role in the Al soil cycle.

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Source
http://dx.doi.org/10.1016/j.jinorgbio.2017.09.017DOI Listing

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