EFFECTS OF INITIAL CHEMICAL COMPOSITION ON DECOMPOSITION OF ROOTS OF THREE GRASS SPECIES

1977 ◽  
Vol 57 (2) ◽  
pp. 205-215 ◽  
Author(s):  
W. A. HERMAN ◽  
W. B. McGILL ◽  
J. F. DORMAAR

Grass root production is a major source of C entering Chernozemic soils. The influence of the initial chemical composition of the roots of three grass species on decomposition was studied in a laboratory incubation experiment. Roots of Stipa comata Trin. and Rupr., Stipa spartea Trin. var. curtiseta Hitchc., and Festuca scabrella Torr. were incubated at 28 C for 47 wk. Carbon dioxide production and percent loss of carbohydrate were inversely related to [(C:N) (% lignin)] (% carbohydrate−½). Percent loss of lignin, however, was directly proportional to this factor. This relationship was also found to fit data in the earlier literature. Decomposition rate appeared to be slower in the laboratory in the absence of soil than has been reported for decomposition rates in field soils. The data are discussed with reference to the dynamics of plant residues and organic matter in soil systems. It is postulated that the effect of soil in controlling decomposition may be as great as the effect of the substrate.

2012 ◽  
Vol 44 (1) ◽  
pp. 117-130 ◽  
Author(s):  
Tomasz Olichwer ◽  
Robert Tarka ◽  
Magdalena Modelska

Chemical composition of groundwaters was investigated in the region of the Hornsund fjord (southern Spitsbergen). The investigations were conducted during polar expeditions organized by the University of Wroclaw in two summer seasons of 2003 and 2006. Three zones of groundwater circulation: suprapermafrost, intrapermafrost and subpermafrost, were identified in areas of perennial permafrost in the region of Hornsund. The zone of shallow circulation occurs in non-glaciated (suprapermafrost) and subglacial areas. In this zone, the chemical composition of groundwater originates from initial chemical composition of precipitation, mineralogical composition of bedrock, oxidation of sulphides and dissolution of carbonates. The intermediate system of circulation is connected with water flow inside and below perennial permafrost (intrapermafrost and subpermafrost). In this zone, the chemical composition of groundwater is mainly controlled by dissolution of carbonates, ion exchange processes involving Ca2+ substitution by Na+, and oxidation of sulphides under oxygen-depleted conditions. The subpermafrost zone (deep groundwater circulation) occurs in deep-tectonic fractures, which are likely conduits for the descent of shallow groundwater to deeper depths. In this zone, the groundwater shows lower mineralization comparing to intrapermafrost zone and has a multi-ion nature Cl–HCO3–Na-Ca–Mg.


2002 ◽  
Vol 1 (2) ◽  
pp. 92-97
Author(s):  
M.H. Sajjad ◽  
H.N. Bhatti . ◽  
A. Lodhi . ◽  
F. Azam .

2020 ◽  
Vol 143 ◽  
pp. 453-461 ◽  
Author(s):  
N.V. Ehman ◽  
A.F. Lourenço ◽  
B.H. McDonagh ◽  
M.E. Vallejos ◽  
F.E. Felissia ◽  
...  

2012 ◽  
Vol 52 (12) ◽  
pp. 1077 ◽  
Author(s):  
P. J. Purcell ◽  
J. Grant ◽  
T. M. Boland ◽  
D. Grogan ◽  
P. O'Kiely

Grassland swards containing white clover varieties (WCV) may result in lower enteric methane (CH4) output from grazing ruminants than swards of only perennial grass species (PGS) due to differences in their chemical composition and rumen fermentation dynamics. The objectives of the present study were to compare the chemical composition, in vitro rumen fermentation variables and CH4 output per unit of feed for a range of common PGS and WCV harvested in May from simulated grazing regimes, and to determine the effects of binary mixtures of the PGS and WCV on in vitro rumen fermentation variables and CH4 output, using a batch-culture technique. Four PGS (perennial ryegrass, cocksfoot, meadow fescue and timothy) and three WCV (Aran, Chieftain and Crusader) were incubated as sole substrates or as part of binary mixtures (PGS : WCV ratios of 0 : 1, 0.25 : 0.75, 0.5 : 0.5, 0.75 : 0.25 and 1 : 0) for 24 h at 39°C with buffered rumen fluid. All WCV had lower (P < 0.001) CH4 output per unit of apparent DM disappeared (aDMD; mean value across WCV (s.e.m.) of 27.0 (1.35) mL/g aDMD v. 36.1 (0.90) mL/g aDMD across PGS) during the in vitro rumen incubation than did all PGS. The WCV also had lower CH4 output per unit of total volatile fatty acids (corresponding values of 0.147 (0.0090) v. 0.199 (0.0073) mmol/mmol total volatile fatty acid output) and per unit of total gas produced (0.118 (0.0022) v. 0.153 (0.0024) mmol/mmol total gas produced) than did the PGS. In addition, Aran and Crusader had lower (P < 0.001) CH4 output per unit of feed DM incubated than did all PGS. There were synergistic associative effects (i.e. where the response was greater for the mixtures than the arithmetic calculation using the responses for PGS and WCV alone; P < 0.05) of mixing the PGS and WCV in binary combinations on all CH4 output variables.


1989 ◽  
Vol 106 ◽  
pp. 51-51
Author(s):  
Yu. L. Frantsman

Simulated populations of the AGB stars were calculated with different assumptions about mass loss, initial chemical composition and dredge-up efficiency. The early-AGB (E-AGB) phase was taken into account. The numbers of carbon and oxygen stars per 106 generated stars and the ratio (NC/NM) of these numbers were obtained. It is possible to match theoretically obtained NC/NM with the observations only if the luminosity of observed stars Mbol < -3.5; otherwise it is necessary to take into account the E-AGB phase. The data in the Table are for all AGB stars in the Galaxy and for stars with Mbol < -1.80 in the LMC.


1999 ◽  
Vol 192 ◽  
pp. 377-380
Author(s):  
Peeter Traat

The initial chemical composition of stars is, besides the mass, another key factor in stellar evolution. Through stellar lifetimes and impact on radiation output and nucleosynthesis of stars it is controlling both the pace of evolution of galactic matter/light and changes in their integrated observables and spectra.


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