Does vegetation prevent wave erosion of salt marsh edges?

被引:205
作者
Feagin, R. A. [1 ,2 ]
Lozada-Bernard, S. M. [1 ]
Ravens, T. M. [3 ]
Moeller, I. [2 ,4 ]
Yeager, K. M. [5 ]
Baird, A. H. [6 ]
机构
[1] Texas A&M Univ, Dept Ecosyst Sci & Management, Spatial Sci Lab, College Stn, TX 77845 USA
[2] Univ Cambridge, Fitzwilliam Coll, Cambridge CB3 ODG, England
[3] Univ Alaska Anchorage, Dept Civil Engn, Anchorage, AK 99508 USA
[4] Univ Cambridge, Dept Geog, Cambridge Coastal Res Unit, Cambridge CB2 3EN, England
[5] Univ So Mississippi, Dept Marine Sci, Stennis Space Ctr, MS 39529 USA
[6] James Cook Univ, Australian Res Council Ctr Excellence Coral Reef, Townsville, Qld 4811, Australia
基金
美国海洋和大气管理局;
关键词
coast; hurricane; wave attenuation; wetland; TSUNAMI; DENSITY; DELTA;
D O I
10.1073/pnas.0901297106
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
This study challenges the paradigm that salt marsh plants prevent lateral wave-induced erosion along wetland edges by binding soil with live roots and clarifies the role of vegetation in protecting the coast. In both laboratory flume studies and controlled field experiments, we show that common salt marsh plants do not significantly mitigate the total amount of erosion along a wetland edge. We found that the soil type is the primary variable that influences the lateral erosion rate and although plants do not directly reduce wetland edge erosion, they may do so indirectly via modification of soil parameters. We conclude that coastal vegetation is best-suited to modify and control sedimentary dynamics in response to gradual phenomena like sea-level rise or tidal forces, but is less well-suited to resist punctuated disturbances at the seaward margin of salt marshes, specifically breaking waves.
引用
收藏
页码:10109 / 10113
页数:5
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