Direct Observations of Hydrologic Exchange Occurring With Less‐Mobile Porosity and the Development of Anoxic Microzones in Sandy Lakebed Sediments-Reference-Cited by-同舟云学术

Direct Observations of Hydrologic Exchange Occurring With Less‐Mobile Porosity and the Development of Anoxic Microzones in Sandy Lakebed Sediments

Published:2018-07 Issue:7 Volume:54 Page:4714-4729
ISSN:0043-1397
Container-title:Water Resources Research
language:en
Short-container-title:Water Resour. Res.

Author:

Briggs Martin A.¹²^ORCID,Day‐Lewis Frederick D.¹^ORCID,Dehkordy Farzaneh Mahmood Poor¹²^ORCID,Hampton Tyler³^ORCID,Zarnetske Jay P.³^ORCID,Scruggs Courtney R.¹,Singha Kamini⁴^ORCID,Harvey Judson W.⁵^ORCID,Lane John W.¹^ORCID

Affiliation:

1. Hydrogeophysics Branch U.S. Geological Survey Storrs CT USA

2. Department of Civil and Environmental Engineering University of Connecticut Storrs CT USA

3. Department of Earth and Environmental Sciences Michigan State University East Lansing MI USA

4. Colorado School of Mines, Hydrologic Science and Engineering Program Golden CO USA

5. Water Cycle Branch U.S. Geological Survey Reston VA USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018WR022823

Reference66 articles.

1. The Electrical Resistivity Log as an Aid in Determining Some Reservoir Characteristics

2. Direct comparison of kinetic and local equilibrium formulations for solute transport affected by surface reactions

3. Nonequilibrium solute transport parameters and their physical significance: numerical and experimental results

4. Nutrient cycling in bedform induced hyporheic zones

5. Hyporheic flow and transport processes: Mechanisms, models, and biogeochemical implications

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