Xia, X, Stewart, DI orcid.org/0000-0001-5144-1234, Cheng, L et al. (4 more authors) (2020) Changes in groundwater bacterial community during cyclic groundwater‐table variations. Hydrological Processes, 34 (25). pp. 4973-4984. ISSN 0885-6087
Abstract
Column experiments containing an aquifer sand were subjected to static and oscillating water tables to investigate the impact of natural fluctuations and rainfall infiltration on the groundwater bacterial community just below the phreatic surface, and its association with the geochemistry. Once the columns were established, the continuously saturated zone was anoxic in all three columns. The rate of soil organic matter (SOM) mineralization was higher when the water table varied cyclically than when it was static due to the greater availability of NO3‐ and SO42‐. Natural fluctuations in the water table resulted in a similar NO3‐ concentration to that observed with a static water table but the cyclic wetting of the intermittently saturated zone resulted in a higher SO42‐ concentration. Rainfall infiltration induced cyclic water‐table variations resulted in a higher NO3‐ concentration than those in the other two columns, and a SO42‐ concentration intermediate between those columns. As rainwater infiltration resulted in slow downward displacement of the groundwater, it is inferred that NO3‐ and SO42‐ were being mobilized from the vadose zone. NO3‐ was mainly released by SOM mineralization (which was enhanced by the infiltration of oxygenated rainwater), but the larger amount of SO42‐ release required a second mechanism (possibly desorption). Different groundwater bacterial communities evolved from initially similar populations due to the different groundwater histories.
Metadata
Item Type: | Article |
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Authors/Creators: |
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Copyright, Publisher and Additional Information: | © 2021 Wiley Periodicals LLC. This is the peer reviewed version of the following article: Xia, X, Stewart, DI , Cheng, L et al. (4 more authors) (2020) Changes in groundwater bacterial community during cyclic groundwater‐table variations. Hydrological Processes, 34 (25). pp. 4973-4984. ISSN 0885-6087. This article may be used for non-commercial purposes in accordance with Wiley Terms and Conditions for Use of Self-Archived Versions. Uploaded in accordance with the publisher's self-archiving policy. |
Keywords: | Water‐table variations; rainfall infiltration; natural fluctuations; SOM mineralization; NO3‐ ;SO42‐; bacterial communities; groundwater histories |
Dates: |
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Institution: | The University of Leeds |
Academic Units: | The University of Leeds > Faculty of Engineering & Physical Sciences (Leeds) > School of Civil Engineering (Leeds) |
Depositing User: | Symplectic Publications |
Date Deposited: | 01 Oct 2020 15:06 |
Last Modified: | 22 Jul 2022 08:50 |
Status: | Published |
Publisher: | Wiley |
Identification Number: | 10.1002/hyp.13917 |
Open Archives Initiative ID (OAI ID): | oai:eprints.whiterose.ac.uk:166221 |