The Tide Rises

S. Levy
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Abstract

David Sedlak, an environmental engineering professor at the University of California– Berkeley, stands on a levee near San Francisco Bay’s eastern shore. Manmade embankments extend for many miles, lining much of the bay’s edge, but Sedlak, a lean, intense guy, is fired up about this newly built one. Instead of the usual barren concrete, the bayward face of the levee slopes gently beneath a dense growth of native wetland plants. From muddy clumps of roots and rhizomes placed here only a year ago, the plants have sprouted into a lush palette of green, from the deep dark of Baltic rush to the bright tones of creeping wild rye. Sedlak is part of a bold experiment. If it succeeds, the project may reshape the East Bay shoreline, restoring a vast acreage of lost tidal wetlands that will be nourished by treated wastewater. The hope is that vegetated levees (the official moniker for the concept is the Horizontal Levee) will save money and energy, recycle treated sewage to create habitat, and help the urbanized East Bay adapt to rising sea levels. Conventional levees form steep concrete or earthen walls that armor roads and buildings against the bay’s powerful waves. The Horizontal Levee is a lovely contrast, a compressed version of a natural habitat long missing from the shoreline. The transition zones, or ecotones, between land and bay were biologically rich places that once hosted a diversity of native plants and animals. Since the Bay Area was settled, wetlands have been diked off from both the open bay and the surrounding land. Between 1800 and 1998, 92 percent of tidal marshes were lost to diking and filling. “In San Francisco Bay, we’ve separated the contacts between the terrestrial and the tidal,” explains Peter Baye, a consulting ecologist whose deep knowledge of remnant natural wetlands acts as guideline for the creation of the Horizontal Levee. Habitats that once formed a continuous gradient from dry land to salt marsh have been boxed off, separated by dikes. The disappearance of what ecologists call the “back end” of tidal marshes has been a significant loss.
涨潮
加州大学伯克利分校的环境工程学教授大卫·塞德拉克站在旧金山湾东岸附近的一个大堤上。人造堤防延伸数英里,沿着海湾的边缘延伸,但塞德拉克,一个瘦弱而紧张的家伙,对这个新建的堤防感到兴奋。与通常的贫瘠混凝土不同,堤坝的向海湾面在密集生长的本土湿地植物下平缓地倾斜。从一年前种植在这里的泥泞的块状根和根茎,这些植物已经发芽,变成了郁郁葱葱的绿色调色板,从波罗的海的深黑到蔓生的野生黑麦的明亮色调。赛德拉克是一项大胆实验的一部分。如果成功,该项目可能会重塑东湾的海岸线,恢复大面积失去的潮汐湿地,这些湿地将由处理过的废水滋养。人们希望植被堤防(这个概念的官方名称是水平堤防)能够节省资金和能源,回收处理过的污水来创造栖息地,并帮助城市化的东湾适应海平面上升。传统的防洪堤形成陡峭的混凝土或土墙,保护道路和建筑物抵御海湾的巨浪。水平堤防是一个可爱的对比,一个压缩版本的自然栖息地长期消失的海岸线。陆地和海湾之间的过渡带是生物丰富的地方,曾经是多种本地植物和动物的栖息地。自从旧金山湾区定居以来,湿地已经与开放的海湾和周围的土地隔离开来。1800年至1998年间,92%的潮汐沼泽因筑堤和填筑而消失。“在旧金山湾,我们把陆地和潮汐之间的联系分开了,”生态学家彼得·贝伊(Peter Baye)解释说,他对残留的自然湿地有深入的了解,为水平堤防的建设提供了指导。曾经形成从旱地到盐沼的连续梯度的栖息地已经被堤坝隔开了。生态学家称之为潮汐沼泽“后端”的消失是一个重大损失。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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