{"title":"Distribution of Meiobenthic Arthropod Communities in the Hyporheic Zone of Nakdonggang","authors":"Chi-Woo Lee, Jong-Geun Park","doi":"10.12651/JSR.2016.5.1.157","DOIUrl":null,"url":null,"abstract":"The hyporheic zone refers to a region along the stream bed where there is an interaction between the surface stream water and ground water (Kim and Kang 2009). The hyporheic zone was initially defined as a discrete region by Orghidan (1959), and its ecological signifi cance was recognized by Schwoerbel (1961a). Since there is continuous interaction between surface water and ground water in a hyporheic zone, contamination or development of any one water body can affect the other, which, in turn, influences the ecosystem. Studies of the hyporheic zone are critical for the management of water resources, and it cannot be considered as an independent water source (Kim et al. 2008). Various biogeochemi cal processes occur in the hyporheic zone because of its unique spatial characteristics (Brunke and Gonser 1997; Storey et al. 1999; Chapelle 2001; Hancock 2002; Ap pelo and Postma 2005; Hyun et al. 2011). The hyporheic zone is a habitat of various living organisms and is con sidered to be an ecologically important zone (Kim et al. 2012). It causes substantial changes to biodiversity and population dynamics and becomes a shelter for organ isms during floods (NWMC 2004). Furthermore, since fluctuations in temperature occur less frequently in the hyporheic zone than in the surface water, it provides an optimal environment for organisms that are sensitive to temperature changes (Schwoerbel 1961b; Evans and Petts 1997). Further, the hyporheic zone has unique eco logical and environmental characteristics (Hyun and Kim 2013). The concept of sustainable development that can sat isfy the needs of both present and future generations has been widely used in various fields since “our common future” was published by the World Commission for Environment and Development (WCED) of the UN in 1987. Since then, interest in improving the sustainability of water resources and environment has increased world wide (Ewen and Parkin 1996; Bronstert et al. 2002; As selman et al. 2003; Chang 2003; Legesse et al. 2003; Lee and Chung 2007) and efforts are being made to maintain better quality of life (Kim 2013). Sustainable use of water requires the regulation of the interface of surface and Journal of Species Research 5(1):157165, 2016","PeriodicalId":426231,"journal":{"name":"Journal of species research","volume":"17 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2016-02-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"4","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of species research","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.12651/JSR.2016.5.1.157","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 4
Abstract
The hyporheic zone refers to a region along the stream bed where there is an interaction between the surface stream water and ground water (Kim and Kang 2009). The hyporheic zone was initially defined as a discrete region by Orghidan (1959), and its ecological signifi cance was recognized by Schwoerbel (1961a). Since there is continuous interaction between surface water and ground water in a hyporheic zone, contamination or development of any one water body can affect the other, which, in turn, influences the ecosystem. Studies of the hyporheic zone are critical for the management of water resources, and it cannot be considered as an independent water source (Kim et al. 2008). Various biogeochemi cal processes occur in the hyporheic zone because of its unique spatial characteristics (Brunke and Gonser 1997; Storey et al. 1999; Chapelle 2001; Hancock 2002; Ap pelo and Postma 2005; Hyun et al. 2011). The hyporheic zone is a habitat of various living organisms and is con sidered to be an ecologically important zone (Kim et al. 2012). It causes substantial changes to biodiversity and population dynamics and becomes a shelter for organ isms during floods (NWMC 2004). Furthermore, since fluctuations in temperature occur less frequently in the hyporheic zone than in the surface water, it provides an optimal environment for organisms that are sensitive to temperature changes (Schwoerbel 1961b; Evans and Petts 1997). Further, the hyporheic zone has unique eco logical and environmental characteristics (Hyun and Kim 2013). The concept of sustainable development that can sat isfy the needs of both present and future generations has been widely used in various fields since “our common future” was published by the World Commission for Environment and Development (WCED) of the UN in 1987. Since then, interest in improving the sustainability of water resources and environment has increased world wide (Ewen and Parkin 1996; Bronstert et al. 2002; As selman et al. 2003; Chang 2003; Legesse et al. 2003; Lee and Chung 2007) and efforts are being made to maintain better quality of life (Kim 2013). Sustainable use of water requires the regulation of the interface of surface and Journal of Species Research 5(1):157165, 2016
潜流带是指沿河床存在地表水和地下水相互作用的区域(Kim and Kang 2009)。隐隐带最初由Orghidan(1959)定义为一个离散的区域,Schwoerbel (1961a)认识到其生态意义。由于潜流带的地表水和地下水之间存在着持续的相互作用,任何一种水体的污染或发展都会影响到另一种水体,而另一种水体又会影响到生态系统。对潜流带的研究对水资源管理至关重要,它不能被视为一个独立的水源(Kim et al. 2008)。由于潜深带独特的空间特征,各种生物地球化学过程在潜深带发生(Brunke and Gonser 1997;Storey et al. 1999;薛潘2001;汉考克2002;香港邮政2005;Hyun et al. 2011)。下潜带是多种生物的栖息地,被认为是生态上重要的区域(Kim et al. 2012)。它引起了生物多样性和种群动态的实质性变化,并成为洪水期间生物的庇护所(NWMC 2004)。此外,由于潜流区温度波动的频率低于地表水,因此它为对温度变化敏感的生物提供了最佳环境(Schwoerbel 1961b;Evans and Petts 1997)。此外,潜潜带具有独特的生态和环境特征(Hyun and Kim 2013)。自1987年联合国世界环境与发展委员会发表《我们共同的未来》以来,能够满足今世后代需要的可持续发展概念被广泛应用于各个领域。从那时起,全世界对改善水资源和环境的可持续性的兴趣增加了(Ewen和Parkin 1996;Bronstert et al. 2002;As - selman et al. 2003;张2003;Legesse et al. 2003;Lee和Chung 2007),并努力保持更好的生活质量(Kim 2013)。水的可持续利用需要地表界面的调节[j] .植物学报,5(1):157-165,2016