首页> 外文期刊>Pacific Science: A Quarterly Devoted to the Biological and Physical Sciences of the Pacific Region >Impact of Stream Hardening on Water Quality and Metabolic Characteristics of Waimanalo and Kane'ohe Streams, O'ahu, Hawaiian Islands
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Impact of Stream Hardening on Water Quality and Metabolic Characteristics of Waimanalo and Kane'ohe Streams, O'ahu, Hawaiian Islands

机译:河流硬化对夏威夷群岛奥阿胡岛威马纳洛河和卡内奥河河流水质和代谢特征的影响

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Kane'ohe and Waimanalo Streams on the windward side of die island of O'ahu in the Hawaiian Islands have been hardened to prevent flooding. The hardening process has involved elimination of die natural riparian habitat and replacement of the natural stream channel with a concrete-lined conduit having vertical walls and a broad, flat bottom. The shallow depth of the water column and absence of shade have resulted in temperatures that average as much as 4-5 ℃ above ambient and rise as high as 32 ℃ during daylight hours. Unlike most low-order streams, the hardened sections of both streams are autotrophic, as evidenced by elevated pH values and O_2 concentrations as high as 150% of saturation. Several allochthonous inputs, one from a storm sewer and the other from a natural spring, introduced water with anomalously low O_2 concentrations and very high nitrate concentrations. The absence of sediments in the hardened sections of die streams precludes natural sedimentary microbial processes, including denitrification. Nitrate concentrations in a section of Waimanalo Stream with a natural streambed drop dramatically from values in excess of 400 μM to concentrations less than 10 μM at the head of die estuary. Although some of this decline is due to dilution with seawater, the concentration of nitrate at die head of the estuary is only 10% of the value that could be explained by dilution effects. Biological processes associated with a natural streambed thus appear very important to functionality of the streams and in particular to their ability to process allochthonous nutrient inputs in a way that minimizes impacts on the nearshore environment. Prevention of flooding can be accomplished by mechanisms that do not involve elimination of riparian buffer zones and destruction of channel habitat. To maintain water quality and stream functionality, it is important that these alternative methods of flood control be utilized. Converting natural streams to storm sewers is an unenlightened way to address flooding problems.
机译:夏威夷群岛瓦胡岛死岛上风向一侧的Kane'ohe河和Waimanalo河已经加固,以防止洪水泛滥。硬化过程包括消除自然的河岸栖息地,并用具有垂直壁和宽而平坦的底部的混凝土衬里管道代替自然河道。水柱的深度较浅且没有阴影,导致温度平均比环境温度高出4-5℃,而在白天则升高至32℃。与大多数低阶流不同,两种流的硬化部分都是自养的,这可以通过升高的pH值和高达150%饱和度的O_2浓度来证明。几种异源输入物(一种来自雨水管道,另一种来自天然泉水)引入了异常低的O_2浓度和非常高的硝酸盐浓度的水。模头流硬化段中没有沉积物,排除了自然的沉积微生物过程,包括反硝化作用。怀马纳洛河断面中自然流化床中的硝酸盐浓度急剧下降,从超过400μM的值下降到模口顶部的小于10μM的浓度。尽管部分下降是由于海水稀释造成的,但河口模头硝酸盐的浓度仅为该值的10%,这可以用稀释效应来解释。因此,与天然河床相关的生物过程对于河流的功能,尤其是其以最小化对近岸环境的影响的方式处理异源营养物输入的能力,显得非常重要。可以通过不涉及消除河岸缓冲区和破坏河道生境的机制来实现水灾的预防。为了维持水质和河流功能,重要的是要利用这些防洪替代方法。将自然流转换为雨水管道是解决洪水问题的绝妙方法。

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