VZJ
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published online 1 May 2008
Published in Vadose Zone J 7:406-419 (2008)
DOI: 10.2136/vzj2007.0068
© 2008 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Abstract Freely available
Right arrow Full Text Free
Right arrow Full Text (PDF) Free
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Gargiulo, G.
Right arrow Articles by Klumpp, E.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Gargiulo, G.
Right arrow Articles by Klumpp, E.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Gargiulo, G.
Right arrow Articles by Klumpp, E.
Related Collections
Right arrow Microorganisms
Right arrow Microbial Processes
Right arrow Microbial and Colloid Transport Models

Bacteria Transport and Deposition under Unsaturated Flow Conditions: The Role of Water Content and Bacteria Surface Hydrophobicity

G. Gargiuloa, S. A. Bradfordb,*, J. Simunekc, P. Ustohala, H. Vereeckena and E. Klumppa

a Agrosphere (ICG-IV), Institute of Chemistry and Dynamics of the Geosphere (ICG), Forschungszentrum Jülich GmbH D-52425, Jülich, Germany
b USDA-ARS, US Salinity Lab., 450 W. Big Springs Rd., Riverside, CA 92507-4617
c Dep. of Environmental Sciences, Univ. of California, Riverside, CA 92521


Figure 1
View larger version (24K):
[in this window]
[in a new window]

 
FIG. 1. Schematic of the column experiment setup.

 

Figure 2
View larger version (66K):
[in this window]
[in a new window]

 
FIG. 2. Photograph of log phase (A) Deinococcus radiodurans and (B) Rhodococcus rhodochrous when suspended in 10–4 M phosphate buffer saline. The photographs were taken using an epifluorescent microscope.

 

Figure 3
View larger version (14K):
[in this window]
[in a new window]

 
FIG. 3. (A) Measured and fitted breakthrough curves and (B) retention profiles for Deinococcus radiodurans at 100% saturation. Fitted curves were obtained using the attachment model, the Langmuirian model, and the 2 site model. In Fig. 3A, 127 min is equal to 1 pore volume. C/C0 = relative effluent concentration, where C0 is the influent concentration of bacteria; Nt, number of bacteria recovered in the sand; Ni, number in a unit volume of the input bacterial suspension.

 

Figure 4
View larger version (15K):
[in this window]
[in a new window]

 
FIG. 4. (A) Measured and fitted breakthrough curves and (B) retention profiles for Deinococcus radiodurans at 80% saturation. Fitted curves were obtained using the attachment model, the Langmuirian model, and the 2 site model. In Fig. 4A, 101 min is equal to 1 pore volume. C/C0 = relative effluent concentration, where C0 is the influent concentration of bacteria; Nt, number of bacteria recovered in the sand; Ni, number in a unit volume of the input bacterial suspension.

 

Figure 5
View larger version (16K):
[in this window]
[in a new window]

 
FIG. 5. (A) Measured and fitted breakthrough curves and (B) retention profiles for Deinococcus radiodurans at 40% saturation. Fitted curves were obtained using the attachment model, the Langmuirian model, and the 2 site model. In Fig. 5A, 55 min is equal to 1 pore volume. C/C0 = relative effluent concentration, where C0 is the influent concentration of bacteria; Nt, number of bacteria recovered in the sand; Ni, number in a unit volume of the input bacterial suspension.

 

Figure 6
View larger version (15K):
[in this window]
[in a new window]

 
FIG. 6. (A) Measured and fitted breakthrough curves and (B) retention profiles for Rhodococcus rhodochrous at 100% saturation. Fitted curves were obtained using the attachment model, the Langmuirian model, and the 2 site model. In Fig. 6A, 134 min is equal to 1 pore volume. C/C0 = relative effluent concentration, where C0 is the influent concentration of bacteria; Nt, number of bacteria recovered in the sand; Ni, number in a unit volume of the input bacterial suspension.

 

Figure 7
View larger version (14K):
[in this window]
[in a new window]

 
FIG. 7. (A) Measured and fitted breakthrough curves and (B) retention profiles for Rhodococcus rhodochrous at 80% saturation. Fitted curves were obtained using the attachment model, the Langmuirian model, and the 2 site model. In Fig. 7A, 152 min is equal to 1 pore volume. C/C0 = relative effluent concentration, where C0 is the influent concentration of bacteria; Nt, number of bacteria recovered in the sand; Ni, number in a unit volume of the input bacterial suspension.

 

Figure 8
View larger version (15K):
[in this window]
[in a new window]

 
FIG. 8. (A) Measured and fitted breakthrough curves and (B) retention profiles for Rhodococcus rhodochrous at 40% saturation. Fitted curves were obtained using the attachment model, the Langmuirian model, and the 2 site model. In Fig. 8A, 62 min is equal to 1 pore volume. C/C0 = relative effluent concentration, where C0 is the influent concentration of bacteria; Nt, number of bacteria recovered in the sand; Ni, number in a unit volume of the input bacterial suspension.

 

Figure 9
View larger version (18K):
[in this window]
[in a new window]

 
FIG. 9. Illustration of a triangular-shaped capillary tube under saturated and unsaturated conditions. Potential straining sites are indicated in this figure where multiple interfaces intersect (at the air–water–solid triple point and the vertices of the triangular capillary tube).

 

Figure 10
View larger version (18K):
[in this window]
[in a new window]

 
FIG. 10. A plot of the relative water flux to straining sites (qws/qw; where qws and qw are the Darcy water velocities to straining sites and the porous medium at a given water saturation, respectively) for various hypothetical fractions of the pore space where straining occurs ({gamma}) and the indicated water saturations (Sw).

 





HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Soil Science Society of America Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2008 by the Soil Science Society of America.