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On October 22, 2024, 8:35:27 PM UTC,
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Updated description of Analysis of coastal storm damage resistance in successional mangrove species from
Use of mangrove ecosystems for coastal flood protection requires reliable predictions of mangrove wave attenuation capacity, especially as this capacity lessens due to storm-induced forest damage. Quantifying and understanding the variation in drag forces on and mechanical properties of mangrove vegetation can improve assessment of mangrove protective capacity. We studied five mangrove species common in the subtropical Pearl River Delta, south China. The tested species range from typically landward-occurring to more seaward-occurring and pioneer species. We sampled across seven sites in the delta to study the impact of salinity on mechanical properties. We quantified strength and flexibility of branches (branch strength and flexibility related to branch diameter, Modulus of Rupture and Modulus of Elasticity), leaf strength (leaf attachment strength related to leaf size and Leaf Mass per Area), and drag properties (drag force related to surface area and the drag coefficient). For all tested species, larger branch diameter resulted in higher mechanical strength. Larger leaf size resulted in larger peak pulling forces and larger branch surface area resulted in stronger drag forces. Notably, species that generally occur lower in the intertidal zone, where exposure to wind and waves is higher, had relatively stronger branches but more easily detachable leaves. This may be regarded as a damage-avoiding strategy. Across the seven field sites we found no clear effect of salinity on mangrove mechanical properties. This study provides a mechanistic insight in the storm damage process for individual mangrove trees and a solid base for modelling storm (surge) damage at forest scale.
toUse of mangrove ecosystems for coastal flood protection requires reliable predictions of mangrove wave attenuation capacity, especially if this capacity lessens due to storm-induced forest damage. Quantifying and understanding the variation in drag forces on and mechanical properties of mangrove vegetation can improve assessment of mangrove protective capacity. We studied five mangrove species common in the subtropical Pearl River Delta, south China. The tested species range from typically landward-occurring to more seaward-occurring and pioneer species. We sampled across seven sites in the delta to study the impact of salinity on mechanical properties. We quantified strength and flexibility of branches (branch strength and flexibility related to branch diameter, Modulus of Rupture and Modulus of Elasticity), leaf strength (leaf attachment strength related to leaf size, and Leaf Mass per Area) and drag properties (drag force related to surface area and the drag coefficient). For all tested species, larger branch diameter resulted in higher mechanical strength. Larger leaf size resulted in larger peak pulling forces and larger branch surface area resulted in stronger drag forces. Notably, species that generally occur lower in the intertidal zone, where exposure to wind and waves is higher, had relatively stronger branches but more easily detachable leaves. This may be regarded as a damage-avoiding strategy. Across the seven field sites we found no clear effect of salinity on mangrove mechanical properties. This study provides a mechanistic insight in the storm damage process for individual mangrove trees and a solid base for modelling storm (surge) damage at forest scale.
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Changed the version of Analysis of coastal storm damage resistance in successional mangrove species to 2 (previously 1)
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| 3 | "author_email": null, | 3 | "author_email": null, | ||
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| 5 | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | 5 | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | ||
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| 7 | "creators": "[{\"firstname\":\"Rosanna\",\"lastname\":\"van | 7 | "creators": "[{\"firstname\":\"Rosanna\",\"lastname\":\"van | ||
| 8 | Hespen\",\"affiliation\":\"Department of Estuarine and Delta Systems, | 8 | Hespen\",\"affiliation\":\"Department of Estuarine and Delta Systems, | ||
| 9 | NIOZ Yerseke, Royal Netherlands Institute for Sea Research and Utrecht | 9 | NIOZ Yerseke, Royal Netherlands Institute for Sea Research and Utrecht | ||
| 10 | University, PO Box 140, 4400 AC Yerseke, Zeeland, The Netherlands; | 10 | University, PO Box 140, 4400 AC Yerseke, Zeeland, The Netherlands; | ||
| 11 | Department of Physical Geography, Faculty of Geosciences, Utrecht | 11 | Department of Physical Geography, Faculty of Geosciences, Utrecht | ||
| 12 | University, Utrecht, Utrecht, The Netherlands | 12 | University, Utrecht, Utrecht, The Netherlands | ||
| 13 | \"firstname\":\"Zhan\",\"lastname\":\"Hu\",\"affiliation\":\"Guangdong | 13 | \"firstname\":\"Zhan\",\"lastname\":\"Hu\",\"affiliation\":\"Guangdong | ||
| 14 | Provincial Key Laboratory of Marine Resources and Coastal Engineering, | 14 | Provincial Key Laboratory of Marine Resources and Coastal Engineering, | ||
| 15 | School of Marine Science, Sun Yat-Sen University, Guangzhou, | 15 | School of Marine Science, Sun Yat-Sen University, Guangzhou, | ||
| 16 | Guangdong, China; Southern Marine Science and Engineering Guangdong | 16 | Guangdong, China; Southern Marine Science and Engineering Guangdong | ||
| 17 | Laboratory (Zhuhai), Guangdong, | 17 | Laboratory (Zhuhai), Guangdong, | ||
| 18 | firstname\":\"Yisheng\",\"lastname\":\"Peng\",\"affiliation\":\"School | 18 | firstname\":\"Yisheng\",\"lastname\":\"Peng\",\"affiliation\":\"School | ||
| 19 | of Environmental Science and Engineering, Sun Yat-Sen University, | 19 | of Environmental Science and Engineering, Sun Yat-Sen University, | ||
| 20 | Guangzhou, Guangdong, China Royal Netherlands Institute for Sea | 20 | Guangzhou, Guangdong, China Royal Netherlands Institute for Sea | ||
| 21 | {\"firstname\":\"Bas\",\"lastname\":\"Borsje\",\"affiliation\":\"Water | 21 | {\"firstname\":\"Bas\",\"lastname\":\"Borsje\",\"affiliation\":\"Water | ||
| 22 | Engineering and Management, University of Twente, Enschede, | 22 | Engineering and Management, University of Twente, Enschede, | ||
| 23 | Overijssel, The | 23 | Overijssel, The | ||
| 24 | \":\"Maarten\",\"lastname\":\"Kleinhans\",\"affiliation\":\"Department | 24 | \":\"Maarten\",\"lastname\":\"Kleinhans\",\"affiliation\":\"Department | ||
| 25 | of Physical Geography, Faculty of Geosciences, Utrecht University, | 25 | of Physical Geography, Faculty of Geosciences, Utrecht University, | ||
| 26 | Utrecht, Utrecht, The | 26 | Utrecht, Utrecht, The | ||
| 27 | tname\":\"Tom\",\"lastname\":\"Ysebaert\",\"affiliation\":\"Department | 27 | tname\":\"Tom\",\"lastname\":\"Ysebaert\",\"affiliation\":\"Department | ||
| 28 | of Estuarine and Delta Systems, NIOZ Yerseke, Royal Netherlands | 28 | of Estuarine and Delta Systems, NIOZ Yerseke, Royal Netherlands | ||
| 29 | Institute for Sea Research and Utrecht University, PO Box 140, 4400 AC | 29 | Institute for Sea Research and Utrecht University, PO Box 140, 4400 AC | ||
| 30 | Yerseke, Zeeland, The Netherlands; Wageningen University & Research, | 30 | Yerseke, Zeeland, The Netherlands; Wageningen University & Research, | ||
| 31 | Wageningen Marine Research, PO Box 77, 4400 AB Yerseke, Zeeland, The | 31 | Wageningen Marine Research, PO Box 77, 4400 AB Yerseke, Zeeland, The | ||
| 32 | tname\":\"Tjeerd\",\"lastname\":\"Bouma\",\"affiliation\":\"Department | 32 | tname\":\"Tjeerd\",\"lastname\":\"Bouma\",\"affiliation\":\"Department | ||
| 33 | of Estuarine and Delta Systems, NIOZ Yerseke, Royal Netherlands | 33 | of Estuarine and Delta Systems, NIOZ Yerseke, Royal Netherlands | ||
| 34 | Institute for Sea Research and Utrecht University, PO Box 140, 4400 AC | 34 | Institute for Sea Research and Utrecht University, PO Box 140, 4400 AC | ||
| 35 | Yerseke, Zeeland, The Netherlands; Department of Physical Geography, | 35 | Yerseke, Zeeland, The Netherlands; Department of Physical Geography, | ||
| 36 | Faculty of Geosciences, Utrecht University, Utrecht, Utrecht, The | 36 | Faculty of Geosciences, Utrecht University, Utrecht, Utrecht, The | ||
| 37 | 546\",\"contactemailaddress\":\"\",\"iscorrespondingauthor\":false}]", | 37 | 546\",\"contactemailaddress\":\"\",\"iscorrespondingauthor\":false}]", | ||
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| 41 | df.leaf, df.architecture, sites, | 41 | df.leaf, df.architecture, sites, | ||
| 42 | 00.000Z\",\"type\":\"collected\",\"information\":\"df.branchdimensions | 42 | 00.000Z\",\"type\":\"collected\",\"information\":\"df.branchdimensions | ||
| 43 | (januari, june, october)\"}]", | 43 | (januari, june, october)\"}]", | ||
| 44 | "deposit_date": "2021-01-06", | 44 | "deposit_date": "2021-01-06", | ||
| 45 | "depositor": "Rosanna van Hespen", | 45 | "depositor": "Rosanna van Hespen", | ||
| 46 | "distribution_date": "2021-01-06", | 46 | "distribution_date": "2021-01-06", | ||
| 47 | "distributor": "Research Data Management(NIOZ Royal Netherlands | 47 | "distributor": "Research Data Management(NIOZ Royal Netherlands | ||
| 48 | Institute for Sea Research)", | 48 | Institute for Sea Research)", | ||
| 49 | "doi_date_published": "2021-04-09", | 49 | "doi_date_published": "2021-04-09", | ||
| 50 | "funding_references": | 50 | "funding_references": | ||
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| 52 | Provincial Department of Science and | 52 | Provincial Department of Science and | ||
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| 55 | Laboratory | 55 | Laboratory | ||
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| 57 | Research Funds for the Central Universities of | 57 | Research Funds for the Central Universities of | ||
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| 59 | "geographic_coverage": "[{\"place\":\"Pearl River Delta | 59 | "geographic_coverage": "[{\"place\":\"Pearl River Delta | ||
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| n | 70 | "metadata_modified": "2024-10-22T20:35:27.012866", | n | 70 | "metadata_modified": "2024-10-22T20:35:27.388429", |
| 71 | "name": "7bbjb", | 71 | "name": "7bbjb", | ||
| 72 | "notes": "Use of mangrove ecosystems for coastal flood protection | 72 | "notes": "Use of mangrove ecosystems for coastal flood protection | ||
| 73 | requires reliable predictions of mangrove wave attenuation capacity, | 73 | requires reliable predictions of mangrove wave attenuation capacity, | ||
| n | 74 | especially as this capacity lessens due to storm-induced forest | n | 74 | especially if this capacity lessens due to storm-induced forest |
| 75 | damage. Quantifying and understanding the variation in drag forces on | 75 | damage. Quantifying and understanding the variation in drag forces on | ||
| 76 | and mechanical properties of mangrove vegetation can improve | 76 | and mechanical properties of mangrove vegetation can improve | ||
| 77 | assessment of mangrove protective capacity. We studied five mangrove | 77 | assessment of mangrove protective capacity. We studied five mangrove | ||
| 78 | species common in the subtropical Pearl River Delta, south China. The | 78 | species common in the subtropical Pearl River Delta, south China. The | ||
| 79 | tested species range from typically landward-occurring to more | 79 | tested species range from typically landward-occurring to more | ||
| 80 | seaward-occurring and pioneer species. We sampled across seven sites | 80 | seaward-occurring and pioneer species. We sampled across seven sites | ||
| 81 | in the delta to study the impact of salinity on mechanical properties. | 81 | in the delta to study the impact of salinity on mechanical properties. | ||
| 82 | We quantified strength and flexibility of branches (branch strength | 82 | We quantified strength and flexibility of branches (branch strength | ||
| 83 | and flexibility related to branch diameter, Modulus of Rupture and | 83 | and flexibility related to branch diameter, Modulus of Rupture and | ||
| 84 | Modulus of Elasticity), leaf strength (leaf attachment strength | 84 | Modulus of Elasticity), leaf strength (leaf attachment strength | ||
| n | 85 | related to leaf size and Leaf Mass per Area), and drag properties | n | 85 | related to leaf size, and Leaf Mass per Area) and drag properties |
| 86 | (drag force related to surface area and the drag coefficient). For all | 86 | (drag force related to surface area and the drag coefficient). For all | ||
| 87 | tested species, larger branch diameter resulted in higher mechanical | 87 | tested species, larger branch diameter resulted in higher mechanical | ||
| 88 | strength. Larger leaf size resulted in larger peak pulling forces and | 88 | strength. Larger leaf size resulted in larger peak pulling forces and | ||
| 89 | larger branch surface area resulted in stronger drag forces. Notably, | 89 | larger branch surface area resulted in stronger drag forces. Notably, | ||
| 90 | species that generally occur lower in the intertidal zone, where | 90 | species that generally occur lower in the intertidal zone, where | ||
| 91 | exposure to wind and waves is higher, had relatively stronger branches | 91 | exposure to wind and waves is higher, had relatively stronger branches | ||
| 92 | but more easily detachable leaves. This may be regarded as a | 92 | but more easily detachable leaves. This may be regarded as a | ||
| 93 | damage-avoiding strategy. Across the seven field sites we found no | 93 | damage-avoiding strategy. Across the seven field sites we found no | ||
| 94 | clear effect of salinity on mangrove mechanical properties. This study | 94 | clear effect of salinity on mangrove mechanical properties. This study | ||
| 95 | provides a mechanistic insight in the storm damage process for | 95 | provides a mechanistic insight in the storm damage process for | ||
| 96 | individual mangrove trees and a solid base for modelling storm (surge) | 96 | individual mangrove trees and a solid base for modelling storm (surge) | ||
| 97 | damage at forest scale.", | 97 | damage at forest scale.", | ||
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