Flow–Vegetation Interaction in a Living Shoreline Restoration and Potential Effect to Mangrove Recruitment

Hydrodynamic differences among shorelines with no vegetation, reference vegetation (mature mangrove), and vegetation planted on restored shoreline (marsh grass and young mangrove) were compared based on field observations 6.5 years after living shoreline restoration. Mean current velocities and wave...

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Main Authors: Kelly M. Kibler, Vasileios Kitsikoudis, Melinda Donnelly, David W. Spiering, Linda Walters
Format: Article
Language:English
Published: MDPI AG 2019-06-01
Series:Sustainability
Subjects:
Online Access:https://www.mdpi.com/2071-1050/11/11/3215
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spelling doaj-ac62665880c34d1bb12d871d20642dca2020-11-25T00:16:47ZengMDPI AGSustainability2071-10502019-06-011111321510.3390/su11113215su11113215Flow–Vegetation Interaction in a Living Shoreline Restoration and Potential Effect to Mangrove RecruitmentKelly M. Kibler0Vasileios Kitsikoudis1Melinda Donnelly2David W. Spiering3Linda Walters4Department of Civil, Environmental &amp; Construction Engineering and National Center for Integrated Coastal Research, University of Central Florida, 4000 Central Florida Blvd., Orlando, FL 32816, USADepartment of Civil, Environmental &amp; Construction Engineering, University of Central Florida, 4000 Central Florida Blvd., Orlando, FL 32816, USADepartment of Biology, University of Central Florida, 4000 Central Florida Blvd., Orlando, FL 32816, USADepartment of Civil, Environmental &amp; Construction Engineering, University of Central Florida, 4000 Central Florida Blvd., Orlando, FL 32816, USADepartment of Biology and National Center for Integrated Coastal Research, University of Central Florida, 4000 Central Florida Blvd., Orlando, FL 32816, USAHydrodynamic differences among shorelines with no vegetation, reference vegetation (mature mangrove), and vegetation planted on restored shoreline (marsh grass and young mangrove) were compared based on field observations 6.5 years after living shoreline restoration. Mean current velocities and waves were more strongly attenuated in vegetation (from channel to shoreline: 80&#8722;98% velocity decrease and 35&#8722;36% wave height reduction) than in bare shoreline (36&#8722;72% velocity decrease, 7% wave height reduction, ANOVA: <i>p</i> &lt; 0.001). Normalized turbulent kinetic energy dissipation rates were significantly higher in reference vegetation (0.16 &#177; 0.03 m<sup>&#8722;1</sup>) than in restored (0.08 &#177; 0.02 m<sup>&#8722;1</sup>) or bare shoreline (0.02 &#177; 0.01 m<sup>&#8722;1</sup>, <i>p</i> &lt; 0.001). Significant differences in the current attenuation and turbulence dissipation rates for the reference and planted vegetation are attributed to the observed differences in vegetation array and morphology. Although the hydrodynamic analyses did not suggest limitations to recruitment, mangrove seedlings were not observed in restored vegetation, while four recruited seedlings/m were counted in the reference vegetation. The lack of recruitment in the restored shoreline may suggest a lag in morphological habitat suitability (slope, sediment texture, organic matter content) after restoration. Although hydrodynamics suggest that the restored site should be functionally similar to a reference condition, thresholds in habitat suitability may emerge over longer timescales.https://www.mdpi.com/2071-1050/11/11/3215ecohydraulicsliving shorelinerestorationmangroveflow-vegetation interactionrecruitment
collection DOAJ
language English
format Article
sources DOAJ
author Kelly M. Kibler
Vasileios Kitsikoudis
Melinda Donnelly
David W. Spiering
Linda Walters
spellingShingle Kelly M. Kibler
Vasileios Kitsikoudis
Melinda Donnelly
David W. Spiering
Linda Walters
Flow–Vegetation Interaction in a Living Shoreline Restoration and Potential Effect to Mangrove Recruitment
Sustainability
ecohydraulics
living shoreline
restoration
mangrove
flow-vegetation interaction
recruitment
author_facet Kelly M. Kibler
Vasileios Kitsikoudis
Melinda Donnelly
David W. Spiering
Linda Walters
author_sort Kelly M. Kibler
title Flow–Vegetation Interaction in a Living Shoreline Restoration and Potential Effect to Mangrove Recruitment
title_short Flow–Vegetation Interaction in a Living Shoreline Restoration and Potential Effect to Mangrove Recruitment
title_full Flow–Vegetation Interaction in a Living Shoreline Restoration and Potential Effect to Mangrove Recruitment
title_fullStr Flow–Vegetation Interaction in a Living Shoreline Restoration and Potential Effect to Mangrove Recruitment
title_full_unstemmed Flow–Vegetation Interaction in a Living Shoreline Restoration and Potential Effect to Mangrove Recruitment
title_sort flow–vegetation interaction in a living shoreline restoration and potential effect to mangrove recruitment
publisher MDPI AG
series Sustainability
issn 2071-1050
publishDate 2019-06-01
description Hydrodynamic differences among shorelines with no vegetation, reference vegetation (mature mangrove), and vegetation planted on restored shoreline (marsh grass and young mangrove) were compared based on field observations 6.5 years after living shoreline restoration. Mean current velocities and waves were more strongly attenuated in vegetation (from channel to shoreline: 80&#8722;98% velocity decrease and 35&#8722;36% wave height reduction) than in bare shoreline (36&#8722;72% velocity decrease, 7% wave height reduction, ANOVA: <i>p</i> &lt; 0.001). Normalized turbulent kinetic energy dissipation rates were significantly higher in reference vegetation (0.16 &#177; 0.03 m<sup>&#8722;1</sup>) than in restored (0.08 &#177; 0.02 m<sup>&#8722;1</sup>) or bare shoreline (0.02 &#177; 0.01 m<sup>&#8722;1</sup>, <i>p</i> &lt; 0.001). Significant differences in the current attenuation and turbulence dissipation rates for the reference and planted vegetation are attributed to the observed differences in vegetation array and morphology. Although the hydrodynamic analyses did not suggest limitations to recruitment, mangrove seedlings were not observed in restored vegetation, while four recruited seedlings/m were counted in the reference vegetation. The lack of recruitment in the restored shoreline may suggest a lag in morphological habitat suitability (slope, sediment texture, organic matter content) after restoration. Although hydrodynamics suggest that the restored site should be functionally similar to a reference condition, thresholds in habitat suitability may emerge over longer timescales.
topic ecohydraulics
living shoreline
restoration
mangrove
flow-vegetation interaction
recruitment
url https://www.mdpi.com/2071-1050/11/11/3215
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