If you are experiencing problems downloading PDF or HTML fulltext, our helpdesk recommend clearing your browser cache and trying again. If you need help in clearing your cache, please click here . Still need help? Email help@ingentaconnect.com

The Factors Controlling Microbial Distribution and Activity in the Shallow Subsurface

$61.74 plus tax (Refund Policy)

Buy Article:


The relationships among sedimentological, geochemical, and microbiological parameters in the vadose zone of a barrier sediment from the eastern shore of Virginia were examined. Pairs of samples were taken 10 cm apart in the vertical direction and 2 cm apart in the horizontal direction along three transects with one sample from each depth being processed aerobically and the other being processed anaerobically. Little variation was observed in the sedimentological and microbiological parameters tested. The sediment of all samples was fine-to-coarse sand, and the grain sizes ranged from 0.19-1.16 mm. Sediment moisture was low for all samples, but increased near the top and bottom of each sampling transect. These were regions where bioavailable Fe(III) concentrations were high. Rates of H2 uptake ranged from below detection limit to 0.064 mol H2 · day−1 · g−1 of sediment with a median rate of 0.01 mol H2 · day−1 · g−1 of sediment. The variation in bacterial numbers was slightly more than an order of magnitude range over the entire sampling face. Phospholipid fatty acid analysis showed a diverse but fairly uniform microbial community from sample to sample. We found that the quartile of aerobically processed samples with the highest H2 uptake rates had statistically higher moisture content and bioavailable iron content than did the rest of the samples. The quartile of aerobically processed samples with the lowest H2 uptake rates had significantly more gravel, less moisture, and less bioavailable Fe(III) than did the rest of the samples. Similar trends were observed for anaerobically processed samples, but the differences were not significant. Our data indicate that the spatial variation in microbial parameters is low within strata with uniform grain sizes.

Keywords: distribution; grain size; microbial activity; moisture; scale; subsurface; vadose; variation

Document Type: Research Article

DOI: http://dx.doi.org/10.1080/01490450303877

Affiliations: 1: University of Oklahoma, Department of Botany and Microbiology, Norman, Oklahoma, USA 2: Miami University, Department of Geology, Oxford, Ohio, USA 3: Princeton University, Department of Geology and Geophysical Sciences, Princeton, New Jersey, USA 4: Old Dominion University, Department of Oceans, Earth, and Atmospheric Sciences, Norfolk, Virginia, USA 5: National Environment Technology Centre, AEA Technology Environment, Culham, Abingdon, UK 6: University of Tennessee, Center for Biomarker Analysis, Knoxville, Tennessee, USA 7: Pacific Northwest National Laboratory, Applied Geology and Geochemistry Technical Group, Richland, Washington, USA

Publication date: May 1, 2003

More about this publication?

Share Content

Access Key

Free Content
Free content
New Content
New content
Open Access Content
Open access content
Subscribed Content
Subscribed content
Free Trial Content
Free trial content
Cookie Policy
Cookie Policy
ingentaconnect website makes use of cookies so as to keep track of data that you have filled in. I am Happy with this Find out more