Effects of crab burrows on pore water flows in salt marshes

Macro-pores such as crab burrows are found commonly distributed in salt marsh sediments. Their disturbance on the soil structure is likely to influence both pore water flows and solute transport in salt marshes; however, the effects of crab burrows are not well understood. Here, a three-dimensional...

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Published inAdvances in water resources Vol. 32; no. 3; pp. 439 - 449
Main Authors Xin, Pei, Jin, Guangqiu, Li, Ling, Barry, D.A.
Format Journal Article
LanguageEnglish
Published Kidlington Elsevier Ltd 01.03.2009
Elsevier
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Online AccessGet full text
ISSN0309-1708
1872-9657
1872-9657
DOI10.1016/j.advwatres.2008.12.008

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Abstract Macro-pores such as crab burrows are found commonly distributed in salt marsh sediments. Their disturbance on the soil structure is likely to influence both pore water flows and solute transport in salt marshes; however, the effects of crab burrows are not well understood. Here, a three-dimensional model simulated tidally driven pore water flows subject to the influence of crab burrows in a marsh system. The model, based on Richards’ equation, considered variably saturated flow in the marsh with a two-layer soil configuration, as observed at the Chongming Dongtan wetland (Shanghai, China). The simulation results showed that crab burrows distributed in the upper low-permeability soil layer, acting as preferential flow paths, affected pore water flows in the marsh particularly when the contrast of hydraulic conductivity between the lower high-permeability soil layer and the overlying low-permeability soils was high. The burrows were found to increase the volume of tidally driven water exchange between the marsh soil and the tidal creek. The simulations also showed improvement of soil aeration conditions in the presence of crab burrows. These effects may lead to increased productivity of the marsh ecosystem and enhancement of its material exchange with coastal waters.
AbstractList Macro-pores such as crab burrows are found commonly distributed in salt marsh sediments. Their disturbance on the soil structure is likely to influence both pore water flows and solute transport in salt marshes; however, the effects of crab burrows are not well understood. Here, a three-dimensional model simulated tidally driven pore water flows subject to the influence of crab burrows in a marsh system. The model, based on Richards' equation, considered variably saturated flow in the marsh with a two-layer soil configuration, as observed at the Chongming Dongtan wetland (Shanghai, China). The simulation results showed that crab burrows distributed in the upper low-permeability soil layer, acting as preferential flow paths, affected pore water flows in the marsh particularly when the contrast of hydraulic conductivity between the lower high-permeability soil layer and the overlying low-permeability soils was high. The burrows were found to increase the volume of tidally driven water exchange between the marsh soil and the tidal creek. The simulations also showed improvement of soil aeration conditions in the presence of crab burrows. These effects may lead to increased productivity of the marsh ecosystem and enhancement of its material exchange with coastal waters.
Author Jin, Guangqiu
Li, Ling
Xin, Pei
Barry, D.A.
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Issue 3
Keywords Richards’ equation
Tidal forcing
Plant growth
Coastal wetland
Numerical modelling
Preferential flow
permeability
water pressure
vegetation
digital simulation
Richards equation
Crustacea
wetlands
hydraulic conductivity
water resources
pore water
soils
burrows
solutes
marshes
hydrodynamics
transport
tides
preferential flow
Mandibulata
salt marshes
Arthropoda
numerical models
ecosystems
three-dimensional models
growth
Invertebrata
bioturbation
Richards' equation
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Snippet Macro-pores such as crab burrows are found commonly distributed in salt marsh sediments. Their disturbance on the soil structure is likely to influence both...
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SourceType Open Access Repository
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StartPage 439
SubjectTerms Animal and plant ecology
Animal, plant and microbial ecology
Biological and medical sciences
burrows
China
Coastal wetland
crab burrows
crabs
Decapoda
Earth sciences
Earth, ocean, space
Exact sciences and technology
Fundamental and applied biological sciences. Psychology
Hydrology
Hydrology. Hydrogeology
macropore flow
macropores
Marine and continental quaternary
Numerical modelling
Plant growth
pore water flow
Preferential flow
Richards’ equation
salt marsh soils
salt marshes
Surficial geology
Synecology
Terrestrial ecosystems
Tidal forcing
water flow
wetland soils
wetlands
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Title Effects of crab burrows on pore water flows in salt marshes
URI https://dx.doi.org/10.1016/j.advwatres.2008.12.008
https://www.proquest.com/docview/20407208
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