Spatial distribution of microbial biomass in microaggregates of a silty-loam soil and the relation with the resistance of microorganisms to soil drying

1996 ◽  
Vol 28 (4-5) ◽  
pp. 503-510 ◽  
Author(s):  
M. Van Gestel ◽  
R. Merckx ◽  
K. Vlassak
2015 ◽  
Vol 12 (11) ◽  
pp. 8819-8847 ◽  
Author(s):  
A. Basler ◽  
M. Dippold ◽  
M. Helfrich ◽  
J. Dyckmans

Abstract. Independent of its chemical structure carbon (C) persists in soil for several decades, controlled by stabilisation and recycling. To disentangle the importance of the two factors on the turnover dynamics of soil sugars, an important compound of soil organic matter (SOM), a three year incubation experiment was conducted on a silty loam soil under different types of land use (arable land, grassland and forest) by adding 13C-labeled glucose. The compound specific isotope analysis of soil sugars was used to examine the dynamics of different sugars during incubation. Sugar dynamics were dominated by a pool of high mean residence times (MRT) indicating that recycling plays an important role for sugars. However, this was not substantially affected by soil C content. Six months after label addition the contribution of the label was much higher for microbial biomass than for CO2 production for all examined soils, corroborating that substrate recycling was very effective within the microbial biomass. Two different patterns of tracer dynamics could be identified for different sugars: while fucose (fuc) and mannose (man) showed highest label contribution at the beginning of the incubation with a subsequent slow decline, galactose (gal) and rhamnose (rha) were characterised by slow label incorporation with subsequently constant levels, which indicates that recycling is dominating the dynamics of these sugars. This may correspond to (a) different microbial growing strategies (r and K-strategist) or (b) location within or outside the cell membrane (lipopolysaccharides vs. exopolysaccharides) and thus be subject of different re-use within the microbial food web. Our results show how the microbial community recycles substrate very effectively and that high losses of substrate only occur during initial stages after substrate addition.


2019 ◽  
Vol 6 (04) ◽  
Author(s):  
RAM PAL ◽  
H C SHARMA ◽  
M IMTIYAZ

The modern theme of agriculture is not only to increase production but also to minimize undesirable environmental effects. Leaching of surface-applied fertilizer is the major source of groundwater pollution. Nitrogenous fertilizers are the most popular among the Indian farmers, which on leaching reach the groundwater in different forms (NH4-N, NO3-N, etc). NO3-N leaches faster than other types, remains in-reactive in groundwater, moves with the velocity of groundwater and contaminates it. Contamination arises when NO3-N accumulates in groundwater and consumed in high amount by humans and animals, may result in adverse health effects. For the study of contaminant transport phenomenon in porous medium, a general convection dispersion equation is used, in which dispersion coefficient is one of the primary parameters necessary to be determined for a particular soil. Keeping it in view a study was conducted to assess different available techniques to determine the dispersion coefficient with the help of soil columns having silty loam soil as soil medium. The value of the dispersion coefficient obtained for silty loam soil, by this method was equal to 0.00576 m2.


2015 ◽  
Vol 14 (4) ◽  
pp. 774-787 ◽  
Author(s):  
Pan LONG ◽  
Peng SUI ◽  
Wang-sheng GAO ◽  
Bin-bin WANG ◽  
Jian-xiong HUANG ◽  
...  

2008 ◽  
Vol 146 (6) ◽  
pp. 677-687 ◽  
Author(s):  
J. F. HERENCIA ◽  
J. C. RUIZ ◽  
S. MELERO ◽  
P. A. GARCIA GALAVÍS ◽  
C. MAQUEDA

SUMMARYThe transition from conventional to organic farming is accompanied by changes in soil chemical properties and processes that could affect soil fertility. The organic system is very complex and the present work carries out a short-term comparison of the effects of organic and conventional agriculture on the chemical properties of a silty loam soil (Xerofluvent) located in the Guadalquivir River Valley, Seville, Spain, through a succession of five crop cycles over a 3-year period. Crop rotation and varieties were compared in a conventional system using inorganic fertilizer and two organic systems using either plant compost or manure. At the end of the study, organic farming management resulted in higher soil organic carbon (OC), N and available P, K, Fe and Zn. The available Mn and especially Cu values did not show significant differences. In general, treatment with manure resulted in more rapid increases in soil nutrient values than did plant compost, which had an effect on several crop cycles later. The present study demonstrated that the use of organic composts results in an increase in OC and the storage of nutrients, which can provide long-term fertility benefits. Nevertheless, at least 2–3 years of organic management are necessary, depending on compost characteristics, to observe significant differences. Average crop yields were 23% lower in organic crops. Nevertheless, only two crops showed statistically significant differences.


2021 ◽  
Vol 76 (2) ◽  
pp. 175-189
Author(s):  
A.M. Bierer ◽  
R.O. Maguire ◽  
M.S. Strickland ◽  
R.D. Stewart ◽  
W.E. Thomason

2012 ◽  
Vol 111 ◽  
pp. 105-114 ◽  
Author(s):  
Basem Aljoumani ◽  
Jose A. Sànchez-Espigares ◽  
Nuria Cañameras ◽  
Ramon Josa ◽  
Joaquim Monserrat

2008 ◽  
Vol 160 (1-4) ◽  
pp. 385-391 ◽  
Author(s):  
Moutushi Dutta ◽  
Devashis Sardar ◽  
Raktim Pal ◽  
Ramen K. Kole

2005 ◽  
Vol 277 (1-2) ◽  
pp. 367-374 ◽  
Author(s):  
N. Rani ◽  
K. S. Dhillon ◽  
S. K. Dhillon
Keyword(s):  

Soil Research ◽  
1991 ◽  
Vol 29 (4) ◽  
pp. 565 ◽  
Author(s):  
M Agassi ◽  
GJ Levy

The effects of level of stone cover, stone size and rain intensity on infiltration, erosion and water splash from a silty loam soil (Calcic Haploxeralf) were studied using a laboratory rainfall simulator. Square asbestos cement plates (5 mm thick), measuring 100 and 2500 mm2, were used to simulate stones. Three levels of surface cover (0, 25 and 50% cover) and two rain intensities (21 and 45 mm h-1) were studied. An increase in the level of stone cover increased infiltration and reduced erosion. The size of the asbestos cement plates had no effect on either infiltration or erosion. An increase in rainfall intensity resulted in a moderate increase in infiltration and a significant increase in soil erosion. Water splash from bare soil (control) reached 15.9% of the applied rain, thereby signifying its importance in simulated rainfall studies. An increase in the level of stone cover reduced water splash. By mulching with small plates, a lower percentage of water splash occurred, compared with large plates and the control. Rain intensity had no effect on water splash.


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