Changes to water repellence of soil aggregates caused by substrate‐induced microbial activity

1999 ◽  
Vol 50 (1) ◽  
pp. 35-40 ◽  
Author(s):  
P. D. Hallett ◽  
I. M. Young
2017 ◽  
Vol 5 (4) ◽  
pp. 97
Author(s):  
Badiori Ouattara ◽  
Idriss Sermé ◽  
Korodjouma Ouattara ◽  
Michel P Sédogo ◽  
Hassan Bismark Nacro

Labile pools of soil organic matter (SOM), including soil sugars, are important to the formation and stabilization of soil aggregates and to microbial activity and nutrient cycling. The effects of cropping systems at farm level in tropical areas on SOM labile pool dynamics have not been adequately studied and the results are sparse and inconsistent. The objective of this study was to determine the effects of soil management intensity on soil sugar monomers derived from plant debris or microbial activity in cotton (Gossypium herbaceum)-based cropping systems of western Burkina Faso. Thirty-three (33) plots were sampled at 0-15 cm soil depth considering field-fallow successions and tillage intensity. Two pentose (arabinose, xylose) and four hexose (glucose, galactose, mannose, glucosamine) monomers accounted for 2 to 18% of soil organic carbon (SOC) content. Total sugar content was significantly less with tillage, especially for the hexose monomeric sugars glucose and mannose, the latter of microbial origin. Soil mannose was 63 and 80% less after 10 years of cultivation, without and with annual ploughing respectively, compared with fallow conditions. Soil monosaccharide content was rapidly restored with fallow and soon approached the equilibrium level observed under old fallow lands. Therefore, the soil monosaccharides, in particular galactose and mannose from microbial synthesis are early indicators of changes in SOC.


Soil Research ◽  
1978 ◽  
Vol 16 (1) ◽  
pp. 9 ◽  
Author(s):  
JM Tisdall ◽  
B Cockroft ◽  
NC Uren

On moist incubation the equivalent of 50 t ha-1 or more of ground, readily decomposable organic materials greatly increased the proportion of stable aggregates of Shepparton fine sandy loam within 1-4 weeks; the aggregates remained stable for up to 32 weeks if left undisturbed. Severe restriction of microbial activity in aggregates of Shepparton fine sandy loam by sterilization or dryness increased the effect of physical disruption associated with intermittent wetting and drying, and simulated cultivation. The results suggest that microorganisms in non-sterile moist soil can produce bonding substances which compensate partially for those bonds broken physically.


1992 ◽  
Vol 56 (5) ◽  
pp. 1455-1463 ◽  
Author(s):  
H. Dinel ◽  
P. E. M. Lévesque ◽  
P. Jambu ◽  
D. Righi

2003 ◽  
Vol 32 (2) ◽  
pp. 541 ◽  
Author(s):  
Tetsu K. Tokunaga ◽  
Jiamin Wan ◽  
Terry C. Hazen ◽  
Egbert Schwartz ◽  
Mary K. Firestone ◽  
...  

2003 ◽  
Vol 32 (2) ◽  
pp. 541-549 ◽  
Author(s):  
Tetsu K. Tokunaga ◽  
Jiamin Wan ◽  
Terry C. Hazen ◽  
Egbert Schwartz ◽  
Mary K. Firestone ◽  
...  

1997 ◽  
Vol 48 (4) ◽  
pp. 643-650 ◽  
Author(s):  
J. W. CRAWFORD ◽  
S. VERRALL ◽  
I. M. YOUNG

1958 ◽  
Vol 17 (2) ◽  
pp. 391-397 ◽  
Author(s):  
I. A. Dyer ◽  
D. W. Fletcher
Keyword(s):  

1963 ◽  
Vol 22 (2) ◽  
pp. 335-340 ◽  
Author(s):  
J. W. Lassiter ◽  
M. K. Hamdy ◽  
Prasob Buranamanas

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