The mineralisation of fresh and humified soil organic matter by the soil microbial biomass

2008 ◽  
Vol 28 (4) ◽  
pp. 716-722 ◽  
Author(s):  
P.C. Brookes ◽  
M.L. Cayuela ◽  
M. Contin ◽  
M. De Nobili ◽  
S.J. Kemmitt ◽  
...  
PLoS ONE ◽  
2019 ◽  
Vol 14 (5) ◽  
pp. e0216730 ◽  
Author(s):  
Domenico Paolo Di Lonardo ◽  
Wietse de Boer ◽  
Hans Zweers ◽  
Annemieke van der Wal

1990 ◽  
Vol 38 (3A) ◽  
pp. 221-238 ◽  
Author(s):  
E.L.J. Verberne ◽  
J. Hassink ◽  
P. de Willigen ◽  
J.J.R. Groot ◽  
J.A. van Veen

A mathematical model was developed to describe carbon (C) and nitrogen (N) cycling in different soil types, e.g. clay and sandy soils. Transformation rates were described by first-order kinetics. Soil organic matter is divided into four fractions (including microbial biomass pool) and three fractions of residues. The fraction of active soil organic matter was assumed to be affected by the extent of physical protection within the soil, as was the soil microbial biomass. The extent of protection influenced the steady state level of the model, and, hence, the mineralization rates. The mineralization rate in fine-textured soils is lower than in coarse-textured soils; in fine-textured soils a larger proportion of the soil organic matter may be physically protected. The availability of organic materials as a substrate for microorganisms is not only determined by their chemical composition, but also by their spatial distribution in the soil. (Abstract retrieved from CAB Abstracts by CABI’s permission)


2008 ◽  
Vol 3 (No. 1) ◽  
pp. 12-20 ◽  
Author(s):  
G. Mühlbachová

A 12-day incubation experiment with the addition of glucose to soils contaminated with persistent organic pollutants (POPs) was carried out in order to estimate the potential microbial activities and the potential of the soil microbial biomass C to degrade 1,1,1-trichloro-2,2-bis(p-chlorophenyl) ethane (DDT), polychlorinated biphenyls (PCB) and polycyclic aromatic hydrocarbons (PAHs). The microbial activities were affected in different ways depending on the type of pollutant. The soil organic matter also played an important role. The microbial activities were affected particularly by high concentrations of PAHs in the soils. Soil microorganisms in the PAHs contaminated soil used the added glucose to a lesser extent than in the non-contaminated soil, which in the contaminated soil resulted in a higher microbial biomass content during the first day of incubation. DDT, DDD and DDE, and PCB affected the soil microbial activities differently and, in comparison with control soils, decreased the microbial biomass C during the incubation. The increased microbial activities led to a significant decrease of PAH up to 44.6% in the soil long-term contaminated with PAHs, and up to 14% in the control soil after 12 days of incubation. No decrease of PAHs concentrations was observed in the soil which was previously amended with sewage sludges containing PAHs and had more organic matter from the sewage sludges. DDT and its derivates DDD and DDE decreased by about 10%, whereas the PCB contents were not affected at all by microbial activities. Studies on the microbial degradation of POPs could be useful for the development of methods focused on the remediation of the contaminated sites. An increase of soil microbial activities caused by addition of organic substrates can contribute to the degradation of pollutants in some soils. However, in situ biodegradation may be limited because of a complex set of environmental conditions, particularly of the soil organic matter. The degradability and availability of POPs for the soil microorganisms has to be estimated individually for each contaminated site.


Soil Research ◽  
2000 ◽  
Vol 38 (6) ◽  
pp. 1087 ◽  
Author(s):  
G. F. Barkle ◽  
R. Stenger ◽  
P. L. Singleton ◽  
D. J. Painter

Over recent years regulatory authorities in New Zealand have promoted irrigation of dairy farm effluent (DFE) onto the land, to protect surface water quality. The rate at which the resistant organic matter from DFE accumulates in the soil and the effect of any accumulation on other soil organic matter (SOM) related pools, such as microbial biomass, are, however, unknown. This information is necessary to determine the long-term impact and sustainability of land-applied DFE. In this paper we report on changes over 4 years in organic carbon (C org) and total nitrogen (N t ) from a soil receiving a high application rate of DFE. Soil microbial biomass (C mic ) measurements were also included to test the hypothesis that C mic or the C mic /C org ratio can be used as an early indicator of changes in SOM. The regular irrigation with DFE at the high rates used in this study increased the C mic , pH, C org , and N t of the soil receiving the effluent. The time series of C mic showed that this measurement is suitable as an early indicator of changes in C org and N t , whereas a single determination of the C mic /C org ratio was not. The sustainability of DFE application onto land in terms of N leaching can be maintained only when the supply of inorganic N is continually matched by the demand of the pasture. This means that inorganic N fertilisation has to be reduced concurrently with the gradually increasing N mineralisation from the accumulating organic matter.


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