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排序方式: 共有442条查询结果,搜索用时 110 毫秒
41.
基于整体开发管理的国际河流决策支持系统 总被引:1,自引:0,他引:1
基于国际河流开发管理的现状,分析国际河流整体开发管理理论的演进。得出整体开发管理决策实施的原则及思路:流域开发管理要以流域边界为界,将整个水系自然联系的区域作为不可分割的整体,进行统一权衡,突出共同利益,流域内开发与流域外开发相结合。以建立多层次的国际合作机构。对国际河流决策支持系统进行设计,即以国际河流流域为体系,各国国内流域测点为单元。国际流域综合协调委员会为决策支持中心、各国流域机构委员会为决策支持分中心。并研究系统的公用信息平台建设,信息开发、管理与维护。河流水资源、水环境实时监控等技术支持系统。实证分析澜沧江-湄公河流域决策支持系统的建设。并指出国际河流水资源的开发与管理,水权等问题有待进一步深入研究。 相似文献
42.
从世界大河流域开发实践构想长江开发模式 总被引:4,自引:2,他引:2
通过分析世界大河流域开发的多种模式,研究可遵循的客观规律和存在问题。借鉴其经验教训,探讨充分有效开发长江流域的模式。提出“突出重点,综合利用,高效运作,协调发展”的战略思想,力争把长江流域建成我国的一级经济轴线和世界规模最大的现代化沿江产业带。 相似文献
43.
在抚仙湖北岸构建复合型人工湿地污水处理系统,对窑泥沟入湖河道污水中氮的去除效果进行了试验研究,结果表明,系统水力负荷年平均为37mm/d,氮负荷年平均为3.315g/m2·d,对污水中NOx、NH+4、TON和TN去除率年平均分别为62.7%、53.8%、62.4%和57.5%. 相似文献
44.
45.
氧化亚氮(N2O)是一种在大气中存留时间很长的强效温室气体,并被认为是21世纪破坏臭氧层的重要物质之一,气候预测需要对自然与人为排放的包括N2O在内的温室气体进行全面准确地估算.内陆水体是N2O的重要排放源,由于人为氮输入的增加,江河N2O的排放量可能逐年升高.本研究总结了江河N2O排放速率的研究方法,重点汇总了中国各气候带十大流域江河N2O的溶存浓度和水气界面交换通量,并与世界其他河流进行比较.结果表明我国江河溶存N2O浓度为0.3~1591 nmol·L-1,N2O释放通量为-12.2~2262.1 μmol·m-2·d-1,总体与世界其他江河的范围值具有可比性.在此基础上,进一步分析了江河N2O的产生和释放机理,探讨了水中溶解性无机氮、溶解氧、有机碳以及水文、地形地貌与气象条件等对江河N2O产生和释放的影响,并讨论了变化环境下江河N2O的排放特征. 相似文献
46.
通过对安徽省中北部6条河流沉积物样品的粒径、矿物组分和有机质含量的测试,并应用气相色谱质谱联用仪测定了样品中萘、二氢苊、苊、芴、菲、蒽、荧蒽、芘、苯并[a]蒽、、苯并[a]芘和二苯并[a,h]蒽等12种多环芳烃的含量,分析了研究区河流沉积物的特征和多环芳烃分布。研究结果表明:位于安徽省中北部的淮河南北岸支流沉积物粒径和矿物组分具有不同特征;就PAHs总量来看,北岸支流平均值为313.3ng/g,南岸支流平均为112.8ng/g,差异比较明显,南岸支流沉积物中大多数多环芳烃的平均含量都低于北岸支流(蒽和菲除外,二苯并[a,h]蒽未检出);而有机质的含量,南北岸支流总体无明显差异(含量在0.55%至1.83%之间),但单条河流的分布呈沿水流方向自中上游至下游逐渐降低。 相似文献
47.
Sonia Binte Murshed Md. Rezaur Rahman Jagath J. Kaluarachchi 《Journal of the American Water Resources Association》2019,55(4):800-823
The Ganges Delta in Bangladesh is an example of water‐related catastrophes in a major rural river basin where limitations in quantity, quality, and timing of available water are producing disastrous conditions. Water availability limitations are modifying the hydrologic characteristics especially when water allocation is controlled from the upstream Farakka Barrage. This study presents the changes and consequences in the hydrologic regime due to climate‐ and human‐induced stresses. Flow duration curves (FDCs), rainfall elasticity, and temperature sensitivity were used to assess the pre‐ and post‐barrage water flow patterns. Hydrologic and climate indices were computed to provide insight on hydro‐climatic variability and trend. Significant increases in temperature, evapotranspiration, hot days, heating, and cooling degree days indicate the region is heading toward a warmer climate. Moreover, increase in high‐intensity rainfall of short duration is making the region prone to extreme floods. FDCs depict a large reduction in river flows between pre‐ and post‐barrage periods, resulting in lower water storage capacity. The reduction in freshwater flow increased the extent and intensity of salinity intrusion. This freshwater scarcity is reducing livelihood options considerably and indirectly forcing population migration from the delta region. Understanding the causes and directions of hydrologic changes is essential to formulate improve water resources management in the region. 相似文献
48.
L.L. Smith A.L. Subalusky C.L. Atkinson J.E. Earl D.M. Mushet D.E. Scott S.L. Lance S.A. Johnson 《Journal of the American Water Resources Association》2019,55(2):334-353
Many species that inhabit seasonally ponded wetlands also rely on surrounding upland habitats and nearby aquatic ecosystems for resources to support life stages and to maintain viable populations. Understanding biological connectivity among these habitats is critical to ensure that landscapes are protected at appropriate scales to conserve species and ecosystem function. Biological connectivity occurs across a range of spatial and temporal scales. For example, at annual time scales many organisms move between seasonal wetlands and adjacent terrestrial habitats as they undergo life‐stage transitions; at generational time scales, individuals may disperse among nearby wetlands; and at multigenerational scales, there can be gene flow across large portions of a species’ range. The scale of biological connectivity may also vary among species. Larger bodied or more vagile species can connect a matrix of seasonally ponded wetlands, streams, lakes, and surrounding terrestrial habitats on a seasonal or annual basis. Measuring biological connectivity at different spatial and temporal scales remains a challenge. Here we review environmental and biological factors that drive biological connectivity, discuss implications of biological connectivity for animal populations and ecosystem processes, and provide examples illustrating the range of spatial and temporal scales across which biological connectivity occurs in seasonal wetlands. 相似文献
49.
50.
D.C. Goodrich W.G. Kepner L.R. Levick P.J. Wigington Jr. 《Journal of the American Water Resources Association》2018,54(2):400-422
Ephemeral and intermittent streams are abundant in the arid and semiarid landscapes of the Western and Southwestern United States (U.S.). Connectivity of ephemeral and intermittent streams to the relatively few perennial reaches through runoff is a major driver of the ecohydrology of the region. These streams supply water, sediment, nutrients, and biota to downstream reaches and rivers. In addition, they provide runoff to recharge alluvial and regional groundwater aquifers that support baseflow in perennial mainstem stream reaches over extended periods when little or no precipitation occurs. Episodic runoff, as well as groundwater inflow to surface water in streams support limited naturally occurring riparian communities. This paper provides an overview and comprehensive examination of factors affecting the hydrologic, chemical, and ecological connectivity of ephemeral and intermittent streams on perennial or intermittent rivers in the arid and semiarid Southwestern U.S. Connectivity as influenced and moderated through the physical landscape, climate, and human impacts to downstream waters or rivers is presented first at the broader Southwestern scale, and secondly drawing on a specific and more detailed example of the San Pedro Basin due to its history of extensive observations and research in the basin. A wide array of evidence clearly illustrates hydrologic, chemical, and ecological connectivity of ephemeral and intermittent streams throughout stream networks. 相似文献