Characterisation of dissolved organic matter in water extracts of thermally altered plant species found in box - ironbark forests

Soil Research ◽  
2010 ◽  
Vol 48 (8) ◽  
pp. 693 ◽  
Author(s):  
Eben S. Quill ◽  
Michael J. Angove ◽  
David W. Morton ◽  
Bruce B. Johnson

This study investigated the chemical structure of extracted dissolved organic matter (DOM) derived from thermally altered plant material found in the box–ironbark environments of central Victoria, namely: Eucalyptus tricarpa, Pinus pinaceae, Isolepsis nodosa, Acacia pycnantha, and Cassinia arcuata. Samples taken from the plants were burnt at 150, 300, and 400°C, under oxidising and reducing conditions in order to represent the variable combustion undergone by plants during bushfire events. The extraction of DOM from the burnt residues into water was conducted over 96 h. During the extraction period, solution concentrations of DOM were measured using HPLC and TOC methods, while the chemistry of the extracted DOM was characterised using ATR-IR. The nature of the extracted DOM depended on the originating species and whether burnt under oxidising or reducing conditions. DOM derived from the residues of the Australian native trees and shrubs (E. tricarpa, A. pycnantha, and C. arcuata) were generally more aromatic and conjugated than the materials extracted from herbaceous I. nodosa and introduced dendrophyte P. pinaceae. When burnt under reducing conditions, fire residues were less polar, indicated by the fact that they were significantly less soluble and ATR-IR spectra spectroscopy showed little OH stretching compared with the extracts obtained under oxidising conditions. Water extracts from the burnt residues sorbed strongly to the mineral goethite, but had less affinity for the kaolinite surface.

Author(s):  
Rossana Del Vecchio ◽  
Neil V Blough ◽  
Carmen Cartisano ◽  
Marla Bianca ◽  
Tara M Schendorf ◽  
...  

1997 ◽  
Vol 77 (3) ◽  
pp. 405-413 ◽  
Author(s):  
M. Susan Erich ◽  
Georgette M. Trusty

Liming of forest soils, currently practiced in Europe, may be necessary in the future in North America to counteract calcium (Ca) depletion due to whole tree harvesting. With current concerns over increasing carbon dioxide (CO2) levels in the atmosphere, the effects of forest practices such as liming on carbon (C) cycling in forest ecosystems has been receiving increasing attention. This laboratory study investigated the effect of an increase in pH on dissolved organic matter (DOM) in water extracts of organic horizons. Organic horizons were collected from nine forested sites, some predominantly hardwood and some predominantly softwood stand types. The soils were chemically characterized. Water extracts of limed and unlimed treatments of nine organic horizons were analyzed for pH, Al, Fe, Ca, C, and DOM negative charge density. Total luminescence fluorescence spectra were also obtained for each extract. The addition of lime (CaCO3) to organic horizons caused an average of 55% more C to be released than in unamended samples. Liming caused no significant changes in negative charge density of the DOM. Liming decreased organically-complexed aluminum (Al) and increased organically-complexed Ca. There was a negative correlation between Al concentration of extracts and fluorescence intensity. Chemical changes in the DOM released by liming were suggested by decreased fluorescence emission and excitation wavelengths due to liming. Hardwood samples did not respond differently than softwood samples with respect to DOM concentration, functional group concentration, or spectroscopic characteristics. However, there was a suggestion that particular tree species, such as cedar, may have unique effects on C concentrations and DOM chemistry. Key words: Lime, forest soil, dissolved organic matter, fluorescence


2015 ◽  
Vol 199 ◽  
pp. 174-184 ◽  
Author(s):  
Lara Settimio ◽  
Mike J. McLaughlin ◽  
Jason K. Kirby ◽  
Kate A. Langdon ◽  
Les Janik ◽  
...  

Soil Research ◽  
2018 ◽  
Vol 56 (1) ◽  
pp. 28 ◽  
Author(s):  
Asmaa Rouwane ◽  
Malgorzata Grybos ◽  
Isabelle Bourven ◽  
Marion Rabiet ◽  
Gilles Guibaud

The release of dissolved organic matter (DOM) from wetland soils is an important pathway for the input of organic compounds into adjacent aquatic environments. In the present study we investigated, under controlled laboratory conditions, the quantity and quality of DOM released from a wetland soil subject to waterlogging and reducing conditions. Three soil redox conditions (oxic, moderately reducing and advanced reducing) were distinguished based on nitrate, ferrous ions and sulfate concentrations in soil solution. Under each redox condition, the quantity (dissolved organic carbon (DOC), humic substances and peptides plus proteins (P-PN) and quality (aromaticity; specific ultraviolet absorbance at 254 nm (SUVA254nm)) and apparent molecular weight (aMW) distribution) of DOM were investigated. The results showed that soil redox condition affects the amount and properties of mobilised DOM. The rate of DOM release and SUVA254 values were highest during the transition from oxic to moderately reducing conditions, whereas both stabilised during progression to advanced reducing conditions. In addition, the mobilised DOM is expected to be more reactive because of an increase in polar substituents in aromatic structures between oxic and moderately reducing conditions. During the development of moderately reducing conditions, dissolved humic substances increased significantly, whereas their aMW distribution (between 500 and 6000 ) remained constant for each of the three different redox conditions. In contrast, the quantity of dissolved P-PN remained low and steady under the three redox conditions, whereas the aMW distribution of protein-like and microbial by-product-like compounds decreased during the development of reducing conditions (aMW of compounds between 100 and >100 000).


Sign in / Sign up

Export Citation Format

Share Document