Influence of coarse wood and fine litter on forest organic matter composition

2006 ◽  
Vol 86 (1) ◽  
pp. 35-46 ◽  
Author(s):  
Anna Krzyszowska-Waitkus ◽  
George F Vance ◽  
Caroline M. Preston

Forest soil organic matter (SOM) is affected by inputs from coarse wood (CW) and fine litter (FL, e.g., leaves, twigs, cones, and needles). The influence of these materials on forest SOM was studied in a lodgepole pine (Pinus contorta) forest in southeastern Wyoming. Organic materials in CW sites were significantly (P < 0.05) more acidic, but contained half the total N of FL sites. Forest floor materials and SOM C contents were significantly greater in CW samples. Lignin decomposition products (CuO analysis) accumulated primarily in organic horizons of both sites, with significantly higher (60–70%) contents in CW materials. Vanillyl compounds were the primary lignin products from both sites, with cinnamyl compounds also important in SOM from FL sites. Vanillic acid to vanillin ratios were significantly higher in mineral soils under CW. 13C-NMR spectra indicated CW materials were enriched in lignin, and that humic acids from both site types were very similar and unusually high in alkyl C. Fulvic acids were also high in O-alkyl and carboxyl C, particularly in the CW sites. Results suggest there are differences in forest C constituents and that removal of CW could possibly alter forest soil dynamics that would impact forest productivity and biodiversity. Key words: Forest, coarse wood, litter, carbon, soil organic matter, humic substances

2018 ◽  
Vol 18 (8) ◽  
pp. 2748-2748 ◽  
Author(s):  
Gabriela Barančíková ◽  
Maria Jerzykiewicz ◽  
Erika Gömöryová ◽  
Erika Tobiašová ◽  
Tadeáš Litavec

2004 ◽  
Vol 70 (2) ◽  
pp. 229-252 ◽  
Author(s):  
Christopher Swanston ◽  
Peter S. Homann ◽  
Bruce A. Caldwell ◽  
David D. Myrold ◽  
Lisa Ganio ◽  
...  

2013 ◽  
Vol 33 (5) ◽  
pp. 1337-1346 ◽  
Author(s):  
王晶苑 WANG Jingyuan ◽  
张心昱 ZHANG Xinyu ◽  
温学发 WEN Xuefa ◽  
王绍强 WANG Shaoqiang ◽  
王辉民 WANG Huimin

2011 ◽  
Vol 43 (7) ◽  
pp. 1518-1527 ◽  
Author(s):  
Kirsten S. Hofmockel ◽  
Donald R. Zak ◽  
Kelly K. Moran ◽  
Julie D. Jastrow

2018 ◽  
Vol 18 (8) ◽  
pp. 2738-2747 ◽  
Author(s):  
Gabriela Barančíková ◽  
Maria Jarzykiewicz ◽  
Erika Gömöryová ◽  
Erika Tobiašová ◽  
Tadeáš Litavec

2021 ◽  
Vol 67 (No. 5) ◽  
pp. 255-263
Author(s):  
Saven Thai ◽  
Lenka Pavlů ◽  
Václav Tejnecký ◽  
Petra Vokurková ◽  
Shahin Nozari ◽  
...  

The study aimed to estimate and characterise soil organic matter under different land uses (cropland, grassland, and forest) and soil depths. The soil organic matter composition of the soil was assessed by diffuse reflectance infrared spectroscopy (DRIFT). Humic and fulvic acids (HAs, FAs) were extracted from soils and their compositions were evaluated by DRIFT. Low molecular mass organic acids content was also measured. Our result revealed that the largest differences of the spectra in the composition of organic matter were observed in the upper parts of the soil profile. The forest soil spectra had more intense aliphatic bands, carboxylic, and CH bands than spectra of grassland and cropland soils. The difference of HAs spectra was at 3 010 to 2 800/cm where the most intensive aliphatic bands were in forest soil HAs, followed by grassland and cropland soil HAs. The grassland topsoil FAs spectrum differs most from the other land uses. It has lower peaks around 1 660–1 600/cm and 1 200/cm than cropland and forest. The concentration of low molecular mass organic acid (LMMOA) was the highest in the forest soil and the most abundant acid was citrate.  


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