Response of microbial activity and community structure to decreasing soil osmotic and matric potential

Chowdhury, Nasrin, Marschner, Petra and Burns, Richard (2011) Response of microbial activity and community structure to decreasing soil osmotic and matric potential. Plant and Soil, 344 1-2: 241-254. doi:10.1007/s11104-011-0743-9


Author Chowdhury, Nasrin
Marschner, Petra
Burns, Richard
Title Response of microbial activity and community structure to decreasing soil osmotic and matric potential
Journal name Plant and Soil   Check publisher's open access policy
ISSN 0032-079X
1573-5036
Publication date 2011-07-01
Sub-type Article (original research)
DOI 10.1007/s11104-011-0743-9
Open Access Status Not Open Access
Volume 344
Issue 1-2
Start page 241
End page 254
Total pages 14
Place of publication Dordrecht, Netherlands
Publisher Springer Netherlands
Formatted abstract
Low soil water content (low matric potential) and salinity (low osmotic potential) occur frequently in soils, particularly in arid and semi-arid regions. Although the effect of low matric or low osmotic potential on soil microorganisms have been studied before, this is the first report which compares the effect of the two stresses on microbial activity and community structure. A sand and a sandy loam, differing in pore size distribution, nutrient content and microbial biomass and community structure, were used. For the osmotic stress experiment, salt (NaCl) was added to achieve osmotic potentials from -0.99 to -13.13 MPa (sand) and from -0.21 to 3.41 MPa (sandy loam) after which the soils were pre-incubated at optimal water content for 10d. For the matric stress experiment, soils were also pre-incubated at optimal water content for 10d, after which the water content was adjusted to give matric potentials from -0.03 and -1.68 MPa (sand) and from -0.10 to 1.46 MPa (sandy loam). After amendment with 2% (w/w) pea straw (C/N 26), soil respiration was measured over 14d. Osmotic potential decreased with decreasing soil water content, particularly in the sand. Soil respiration decreased with decreasing water potential (osmotic + matric). At a given water potential, respiration decreased to a greater extent in the matric stress experiment than in the osmotic stress experiment. Decreasing osmotic and matric potential reduced microbial biomass (sum of phospholipid fatty acids measured after 14 days) and changed microbial community structure: fungi were less tolerant to decreasing osmotic potential than bacteria, but more tolerant to decreasing water content. It is concluded that low matric potential may be more detrimental than a corresponding low osmotic potential at optimal soil water content. This is likely to be a consequence of the restricted diffusion of substrates and thus a reduced ability of the microbes to synthesise osmolytes to help maintain cell water content. The study also highlighted that it needs to be considered that decreasing soil water content concentrates the salts, hence microorganisms in dry soils are exposed to two stressors.
Keyword Bacteria
Fungi
PLFA
Respiration
Salinity
Q-Index Code C1
Q-Index Status Provisional Code
Institutional Status UQ

Document type: Journal Article
Sub-type: Article (original research)
Collection: School of Agriculture and Food Sciences
 
Versions
Version Filter Type
Citation counts: TR Web of Science Citation Count  Cited 55 times in Thomson Reuters Web of Science Article | Citations
Scopus Citation Count Cited 59 times in Scopus Article | Citations
Google Scholar Search Google Scholar
Created: Thu, 28 Nov 2013, 06:53:59 EST by System User on behalf of School of Agriculture and Food Sciences