整合水生生物栖息地和形态动力学的挑战为生态水力学的进步提供了大量的机会

IF 4.6 Q2 ENVIRONMENTAL SCIENCES
C. Katopodis, P. Kemp
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Through surface, subsurface or groundwater flow, erosion, transport, deposition and ice conditions, morphodynamics shapes bars, pools, riffles, islands, side channels and other features in waterbodies (Paola et al. 2006; Wohl et al. 2015). Ecological dynamics, commonly understood less clearly, represent the even more complex life processes and food webs, responses by aquatic species and vegetation, populations and communities, as well as suitable habitats characterized by spatial complexity, connectivity and dynamism which meet biota life cycle requirements, enable ecosystem functionality and support biodiversity (Elosegi et al. 2010). Large differences in genetic flow, dispersal and mobility strategies or abilities of aquatic biota populations add another layer to this complexity and needs for more in-depth knowledge and understanding. With such complexities, it is not surprising that large knowledge gaps exist in morphodynamics and ecology, and particularly in the interaction between the two. Although often it is thought that geomorphology sets the template for biological processes (e.g. Vannote et al. 1980), recent studies indicate direct and indirect effects on physical processes from aquatic and riparian vegetation, particularly in the riparian zone (e.g. Gurnell et al. 2012), or even from fish through nutrient enrichment or potential effects on gravel substrates (e.g. DeVries 2012). Such interactions create numerous feedback mechanisms between biotic and abiotic processes, ecology and morphodynamics, generate further knowledge gaps and offer potentially great insights if elucidated though comprehensive studies. Since Ecohydraulics is at the interface between morphoand eco-dynamics and explores biota and physical interactions, breakthroughs in this interdisciplinary field become very challenging. At the same time, such challenges offer a plethora of opportunities for pioneering research and practical applications for interand trans-disciplinary advances in Ecohydraulics. River systems have influenced people and their settlements since the dawn of civilization, while humans continue to alter, regulate and manage them to: (1) suppress floods and control water levels; (2) supply water for domestic use, agriculture, recreation and many industries; (3) enable navigation and hydroelectric power production; (4) inter-basin water transfers from wet regions to dry regions; (5) control sediment, erosion and mine waste; (6) convert wetlands and river deltas to agricultural or other use; (7) support waste dilution, waste disposal, logging activities and paper mills; (8) intentionally or accidentally introduce nonnative exotic species. Control and management of rivers change the dynamic nature of aquatic ecosystems which are characterized by ecological dynamism, habitat connectivity and species biodiversity. Dams, pumping stations, canals, hydroelectric facilities, other infrastructure, as well as biological invasions, may: impair natural functions; render living conditions for biota unsuitable; fragment free-flowing rivers; alter the timing and magnitude of river and stream flows; disrupt sediment transport, nutrient cycling, biota movements, as well as connections to floodplain and groundwater; impact long-term river morphology, water quality and ice conditions; add pressures on biodiversity (Katopodis and Aadland 2006; Elosegi et al. 2010). Minimizing negative impacts, understanding biota responses to changed abiotic environments, developing and implementing mitigation measures and evaluating their effectiveness with a focus on dynamic interactions between aquatic life and morphodynamics calls for innovative ecohydraulic solutions and presents challenging research questions. Over millennia, anthropogenic influences have left morphological signatures which have been increasingly prevalent. It seems that natural rivers, lakes and deltas or even segments are rare, if not non-existent, particularly if pollution by air transport and climate change are considered. This is despite wide recognition that freshwater is essential for human and aquatic life, economic development, as well as robust ecosystem functions. Such river modifications throughout the planet, have made and continue to make changes to biodiversity and biota redistribution, as well as provide large risks to water security for humanity. A global analysis by V€ or€ osmarty et al. (2010) found that nearly 80% of humanity lives with a major threat to water security, while the increasing rates of degradation to freshwater aquatic habitats means that hundreds of biota are","PeriodicalId":93201,"journal":{"name":"Journal of ecohydraulics","volume":"41 1","pages":"1 - 3"},"PeriodicalIF":4.6000,"publicationDate":"2018-01-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"4","resultStr":"{\"title\":\"Challenges of integrating habitat for aquatic life and morphodynamics offer a plethora of opportunities for advances in Ecohydraulics\",\"authors\":\"C. Katopodis, P. Kemp\",\"doi\":\"10.1080/24705357.2018.1484331\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Morphodynamics and aquatic biota (i.e. plants and animals) interact through complex processes, to generate suitable, diverse and resilient habitats. 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Ecological dynamics, commonly understood less clearly, represent the even more complex life processes and food webs, responses by aquatic species and vegetation, populations and communities, as well as suitable habitats characterized by spatial complexity, connectivity and dynamism which meet biota life cycle requirements, enable ecosystem functionality and support biodiversity (Elosegi et al. 2010). Large differences in genetic flow, dispersal and mobility strategies or abilities of aquatic biota populations add another layer to this complexity and needs for more in-depth knowledge and understanding. With such complexities, it is not surprising that large knowledge gaps exist in morphodynamics and ecology, and particularly in the interaction between the two. Although often it is thought that geomorphology sets the template for biological processes (e.g. Vannote et al. 1980), recent studies indicate direct and indirect effects on physical processes from aquatic and riparian vegetation, particularly in the riparian zone (e.g. Gurnell et al. 2012), or even from fish through nutrient enrichment or potential effects on gravel substrates (e.g. DeVries 2012). Such interactions create numerous feedback mechanisms between biotic and abiotic processes, ecology and morphodynamics, generate further knowledge gaps and offer potentially great insights if elucidated though comprehensive studies. Since Ecohydraulics is at the interface between morphoand eco-dynamics and explores biota and physical interactions, breakthroughs in this interdisciplinary field become very challenging. At the same time, such challenges offer a plethora of opportunities for pioneering research and practical applications for interand trans-disciplinary advances in Ecohydraulics. River systems have influenced people and their settlements since the dawn of civilization, while humans continue to alter, regulate and manage them to: (1) suppress floods and control water levels; (2) supply water for domestic use, agriculture, recreation and many industries; (3) enable navigation and hydroelectric power production; (4) inter-basin water transfers from wet regions to dry regions; (5) control sediment, erosion and mine waste; (6) convert wetlands and river deltas to agricultural or other use; (7) support waste dilution, waste disposal, logging activities and paper mills; (8) intentionally or accidentally introduce nonnative exotic species. Control and management of rivers change the dynamic nature of aquatic ecosystems which are characterized by ecological dynamism, habitat connectivity and species biodiversity. Dams, pumping stations, canals, hydroelectric facilities, other infrastructure, as well as biological invasions, may: impair natural functions; render living conditions for biota unsuitable; fragment free-flowing rivers; alter the timing and magnitude of river and stream flows; disrupt sediment transport, nutrient cycling, biota movements, as well as connections to floodplain and groundwater; impact long-term river morphology, water quality and ice conditions; add pressures on biodiversity (Katopodis and Aadland 2006; Elosegi et al. 2010). 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引用次数: 4

摘要

形态动力学和水生生物群(即植物和动物)通过复杂的过程相互作用,产生合适的、多样化的和有弹性的栖息地。我们将形态动力学广义地定义为地球表面特征和演化的学科,它整合了水文、地貌和地质方面。这个定义与Paola等人(2006)提供的定义相似,但范围更窄,因为我们在生态水力学中包括了生态和生物方面。复杂的物理过程与河流、湖泊和三角洲的平台、纵向剖面和横截面几何形状有关,并涉及流域中水、沉积物、冰、营养物质、溶质和有机物质的循环。形态动力学通过地表、地下或地下水的流动、侵蚀、运输、沉积和结冰条件,塑造了水体中的沙洲、水池、河汊、岛屿、侧河道和其他特征(Paola et al. 2006;Wohl et al. 2015)。生态动力学,通常理解不太清楚,代表了更复杂的生命过程和食物网,水生物种和植被,种群和群落的响应,以及以空间复杂性,连通性和动态性为特征的适合栖息地,满足生物群生命周期要求,实现生态系统功能并支持生物多样性(Elosegi et al. 2010)。水生生物种群在遗传流动、扩散和迁移策略或能力方面的巨大差异,使这种复杂性又增加了一层,需要更深入的认识和理解。在如此复杂的情况下,形态动力学和生态学,特别是两者之间的相互作用方面存在巨大的知识差距也就不足为奇了。虽然通常认为地貌学为生物过程设定了模板(例如Vannote等人,1980),但最近的研究表明,水生和河岸植被,特别是河岸地带的植被(例如Gurnell等人,2012)对物理过程产生了直接和间接的影响,甚至鱼类通过营养富集或对砾石基质的潜在影响(例如DeVries, 2012)。这种相互作用在生物和非生物过程、生态学和形态动力学之间创造了许多反馈机制,产生了进一步的知识空白,如果通过全面的研究加以阐明,可能会提供巨大的见解。由于生态水力学处于形态和生态动力学之间的界面,并探索生物群和物理相互作用,因此在这一跨学科领域取得突破变得非常具有挑战性。与此同时,这些挑战为生态水力学的跨学科进步提供了大量的开创性研究和实际应用机会。自文明出现以来,河流系统就影响着人类及其住区,而人类则继续改变、调节和管理它们,以实现以下目的:(1)抑制洪水和控制水位;(2)为生活、农业、娱乐和许多工业供水;(三)通航和水力发电;(4)流域间水从湿润区向干旱区转移;(五)治理泥沙、侵蚀和矿山废弃物;(6)将湿地和河流三角洲改造为农业或其他用途;(7)支持废物稀释、废物处理、伐木活动和造纸厂;(八)有意或者无意引入外来种的。河流的控制和管理改变了以生态动态性、栖息地连通性和物种多样性为特征的水生生态系统的动态性质。水坝、泵站、水渠、水电设施和其他基础设施以及生物入侵可能损害自然功能;使生物群的生存条件不适宜;碎片自由流动的河流;改变河流和溪流流量的时间和大小;破坏沉积物运输、养分循环、生物群运动以及与洪泛区和地下水的联系;影响长期河流形态、水质和冰况;增加对生物多样性的压力(Katopodis和Aadland, 2006年;Elosegi et al. 2010)。减少负面影响,了解生物群对变化的非生物环境的反应,制定和实施缓解措施,并评估其有效性,重点关注水生生物与形态动力学之间的动态相互作用,这需要创新的生态水力解决方案,并提出具有挑战性的研究问题。几千年来,人为影响留下了越来越普遍的形态特征。自然的河流、湖泊、三角洲甚至是河段,如果不是完全不存在的话,似乎也很罕见,尤其是考虑到航空运输和气候变化造成的污染。尽管人们普遍认识到,淡水对人类和水生生物、经济发展以及强大的生态系统功能至关重要。 全球范围内的这种河流改造已经并将继续改变生物多样性和生物群再分配,并对人类的水安全构成巨大风险。V - or - osmarty等人(2010)的一项全球分析发现,近80%的人类生活在对水安全的重大威胁中,而淡水水生栖息地退化速度的增加意味着数百种生物群正在受到威胁
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Challenges of integrating habitat for aquatic life and morphodynamics offer a plethora of opportunities for advances in Ecohydraulics
Morphodynamics and aquatic biota (i.e. plants and animals) interact through complex processes, to generate suitable, diverse and resilient habitats. We define morphodynamics in broad terms as the discipline of Earth surface characteristics and evolution which integrates hydrological, geomorphological and geological aspects. This definition is similar, although narrower to that offered by Paola et al. (2006), since we include ecological and biological aspects in Ecohydraulics. Complex physical processes are linked to planforms, longitudinal profiles and cross-sectional geometries in rivers, lakes and deltas and involve the cycling of water, sediment, ice, nutrients, solutes and organic materials in watersheds. Through surface, subsurface or groundwater flow, erosion, transport, deposition and ice conditions, morphodynamics shapes bars, pools, riffles, islands, side channels and other features in waterbodies (Paola et al. 2006; Wohl et al. 2015). Ecological dynamics, commonly understood less clearly, represent the even more complex life processes and food webs, responses by aquatic species and vegetation, populations and communities, as well as suitable habitats characterized by spatial complexity, connectivity and dynamism which meet biota life cycle requirements, enable ecosystem functionality and support biodiversity (Elosegi et al. 2010). Large differences in genetic flow, dispersal and mobility strategies or abilities of aquatic biota populations add another layer to this complexity and needs for more in-depth knowledge and understanding. With such complexities, it is not surprising that large knowledge gaps exist in morphodynamics and ecology, and particularly in the interaction between the two. Although often it is thought that geomorphology sets the template for biological processes (e.g. Vannote et al. 1980), recent studies indicate direct and indirect effects on physical processes from aquatic and riparian vegetation, particularly in the riparian zone (e.g. Gurnell et al. 2012), or even from fish through nutrient enrichment or potential effects on gravel substrates (e.g. DeVries 2012). Such interactions create numerous feedback mechanisms between biotic and abiotic processes, ecology and morphodynamics, generate further knowledge gaps and offer potentially great insights if elucidated though comprehensive studies. Since Ecohydraulics is at the interface between morphoand eco-dynamics and explores biota and physical interactions, breakthroughs in this interdisciplinary field become very challenging. At the same time, such challenges offer a plethora of opportunities for pioneering research and practical applications for interand trans-disciplinary advances in Ecohydraulics. River systems have influenced people and their settlements since the dawn of civilization, while humans continue to alter, regulate and manage them to: (1) suppress floods and control water levels; (2) supply water for domestic use, agriculture, recreation and many industries; (3) enable navigation and hydroelectric power production; (4) inter-basin water transfers from wet regions to dry regions; (5) control sediment, erosion and mine waste; (6) convert wetlands and river deltas to agricultural or other use; (7) support waste dilution, waste disposal, logging activities and paper mills; (8) intentionally or accidentally introduce nonnative exotic species. Control and management of rivers change the dynamic nature of aquatic ecosystems which are characterized by ecological dynamism, habitat connectivity and species biodiversity. Dams, pumping stations, canals, hydroelectric facilities, other infrastructure, as well as biological invasions, may: impair natural functions; render living conditions for biota unsuitable; fragment free-flowing rivers; alter the timing and magnitude of river and stream flows; disrupt sediment transport, nutrient cycling, biota movements, as well as connections to floodplain and groundwater; impact long-term river morphology, water quality and ice conditions; add pressures on biodiversity (Katopodis and Aadland 2006; Elosegi et al. 2010). Minimizing negative impacts, understanding biota responses to changed abiotic environments, developing and implementing mitigation measures and evaluating their effectiveness with a focus on dynamic interactions between aquatic life and morphodynamics calls for innovative ecohydraulic solutions and presents challenging research questions. Over millennia, anthropogenic influences have left morphological signatures which have been increasingly prevalent. It seems that natural rivers, lakes and deltas or even segments are rare, if not non-existent, particularly if pollution by air transport and climate change are considered. This is despite wide recognition that freshwater is essential for human and aquatic life, economic development, as well as robust ecosystem functions. Such river modifications throughout the planet, have made and continue to make changes to biodiversity and biota redistribution, as well as provide large risks to water security for humanity. A global analysis by V€ or€ osmarty et al. (2010) found that nearly 80% of humanity lives with a major threat to water security, while the increasing rates of degradation to freshwater aquatic habitats means that hundreds of biota are
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