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391.
金沙江流域水土流失现状与河道泥沙分析 总被引:14,自引:1,他引:13
对金沙江流域水土流失、河道泥沙及主要影响因素系统作了分析,认为地质、地貌及气候因子是影响水土流失的主要因素,人为活动加剧水土流失的发生发展。河道泥沙主要来自金沙江下游,特别是下游干流河谷区间,流域的地面侵蚀与河道泥沙的空间关系不密切,影响输沙量的主要因素为年径流量和清水区年径流量,以及滑坡、泥石流等重力侵蚀,尽管水土流失治理对于流域的河道泥沙减沙效应显著,但短期内对流域干支流输沙量影响甚微。今后一段时间内金沙江流域河道泥沙不会有显著的变化 相似文献
392.
长江流域商品粮基地建设与农业持续发展 总被引:6,自引:4,他引:2
长江流域横跨我国中亚热带,光、热、水气候资源及其时空组合优势明显,土地自然生产力较高。粮食生产在全国占有重要地位。但由于流域内山地比重大,人口稠密,人均土地资源偏少,在现有耕地资源有限和粮食市场不稳等的多重压力下,历史时期内形成的“南粮北调”正逐渐被“北粮南调”所取代。在分析长江流域粮食生产现状和近二十年来商品粮基地建设对粮食生产的促进作用的基础上,从流域经济持续发展角度,提出了发挥长江流域粮食生 相似文献
393.
南水北调中线工程对汉江中下游工业发展的影响 总被引:14,自引:3,他引:11
南水北调中线工程计划从丹江口水库向我国北方每年调水145亿m^3,汉江丹江口以下地区的水资源量将随之相应减少。汉江中下游地区是湖北省盐化工、机械、石油、食品、化肥、电力的重要生产地区,是湖北省的汽车工业走廊,其经济在湖北省占有举足轻重的地位。由于经济的迅速发展,下世纪工农业生产和人民生活对水资源的需求将从现在的140亿m^3增加到250亿m^3以上,需水量将达到水资源量的58%,潜伏着严重的水资源 相似文献
394.
由震洪相关回顾性预测1870年长江特大洪水 总被引:2,自引:0,他引:2
1870 年长江特大洪水是多因叠加和强化的结果, 因之要预测它也要从各方面去研究。如特大洪水前的先行降雨和洪水所反映的大气环流状况及太阳活动情况等。本文把1931 年、1954年、1991 年长江大洪水前一年内缅甸北部有7 级以上大震及1998 年长江大洪前一年内缅北有6级左右震群集中活动的相关指标移用于1870 年长江特大洪水前, 发现其前一年, 即1869 年缅北亦有7 级以上大震发生。震洪相关的物理机制是与地震活动有关的地下放气使孟加拉湾向长江流域输送的水气更多,如遇北方冷气团南下则降大雨致洪。另外,1870 年长江洪水之所以比1931 年、1954 年、1991 年和1998 年长江洪水还大, 我们认为1870 年4 月11 日在长江上游山区有7 级以上大震发生, 且震前有大雪发生, 是叠加在前述致洪因素上的另一因素。 相似文献
395.
长江洪涝灾害的可持续发展综合防御对策体系 总被引:4,自引:0,他引:4
洪涝灾害严重制约了长江流域可持续发展, 本文分析了洪涝灾害的主要成因, 从合理协调人口——资源环境——社会经济三者之间深层次关系出发, 建立了长江洪涝灾害的可持续发展综合防御对策体系 相似文献
396.
黄真理 《长江流域资源与环境》2002,(1)
:通过对阿斯旺高坝和尼罗河的实际考察和生态环境监测数据的分析 ,介绍了埃及政府相关管理部门的官员和专家对阿斯旺工程的看法 ,对阿斯旺高坝及其生态环境问题进行了评述。认为阿斯旺工程是一个成功的工程 ,它对埃及发挥的巨大影响和积极作用是有目共睹的。它对生态环境的不利影响 ,确被很多批评者盲目地夸大了 ,其中也包含有政治因素。中国在修建水利工程时 ,要对环境的影响作出客观、科学的评价 ,并采取措施把不利影响减少到最小。阿斯旺高坝运行近 30年 ,在生态环境监测方面积累了丰富的数据 ,这些成果和结论对三峡工程具有直接的借鉴和参考价值。 相似文献
397.
Chen-Tung?Arthur?ChenEmail author James?T.?Liu Ben-Jei?Tsuang 《Regional Environmental Change》2004,4(1):39-48
Rapid economic and industrial development in Taiwan over the past five decades has elevated the islands standing and earned it a place in the group known as the Four Small Dragons of Asia. Such growth, however, has been at the expense of the environment. There are currently nearly 23 million people juggling for space on the small island of 35,873 km2. Aggravating the matter further, the central mountain ranges and hills take up 73.6% of the land area with some 156 peaks surpassing 3,000 m. As a result, most people live in coastal plains which amount to only 9,490 km2. Pressure to move people inland has led to road construction and deforestation, both of which have contributed to an already high denudation rate of topsoil. As a consequence of this, thirteen rivers in Taiwan are now ranked among the top 20 worldwide in terms of sediment yield. Aside from this, the frequency of both floods and droughts increased prior to 1990, perhaps because of deforestation and global warming. Fortunately, the new conservation-orientated forest management policy of 1991 has alleviated the problem, somewhat, and the occurrence of floods and droughts has since decreased. The problem of water shortage, however, has worsened because of the warming trend in atmospheric temperature. Damming may ameliorate the water shortage problem but may affect the shoreline stability, as well as the ecology and water quality in the estuaries. Furthermore, these detrimental effects may go far beyond the estuaries, and even fisheries on the continental shelves may be affected. 相似文献
398.
Destruction of Wetlands and Waterbird Populations by Dams and Irrigation on the Murrumbidgee River in Arid Australia 总被引:3,自引:0,他引:3
The Lowbidgee floodplain is the Murrumbidgee Rivers major wetland in southeastern Australia. From more than 300,000 ha in the early 1900s, at least 76.5% was destroyed (58%) or degraded (18%) by dams (26 major storages), subsequent diversions and floodplain development. Diversions of about 2,144,000 ML year–1 from the Murrumbidgee River come from a natural median flow of about 3,380,000 ML year–1 providing water for Australias capital, hydroelectricity, and 273,000 ha of irrigation. Diversions have reduced the amount of water reaching the Lowbidgee floodplain by at least 60%, from 1888 to 1998. About 97,000 ha of Lowbidgee wetland was destroyed by development of the floodplain for an irrigation area (1975–1998), including building of 394 km of channels and 2,145 km of levee banks. Over 19 years (1983–2001), waterbird numbers estimated during annual aerial surveys collapsed by 90%, from an average of 139,939 (1983–1986) to 14,170 (1998–2001). Similar declines occurred across all functional groups: piscivores (82%), herbivores (87%), ducks and small grebe species (90%), large wading birds (91%), and small wading birds (95%), indicating a similar decline in the aquatic biota that formed their food base. Numbers of species also declined significantly by 21%. The Lowbidgee floodplain is an example of the ecological consequences of water resource development. Yanga Nature Reserve, within the Lowbidgee floodplain, conserved for its floodplain vegetation communities, will lose these communities because of insufficient water. Until conservation policies adequately protect river flows to important wetland areas, examples such as the Lowbidgee will continue to occur around the world. 相似文献
399.
400.
Human impacts on the stream-groundwater exchange zone 总被引:13,自引:0,他引:13
Hancock PJ 《Environmental management》2002,29(6):763-781
Active exchanges of water and dissolved material between the stream and groundwater in many porous sand- and gravel-bed rivers
create a dynamic ecotone called the hyporheic zone. Because it lies between two heavily exploited freshwater resources—rivers
and groundwater—the hyporheic zone is vulnerable to impacts coming to it through both of these habitats. This review focuses
on the direct and indirect effects of human activity on ecosystem functions of the hyporheic zone. River regulation, mining,
agriculture, urban, and industrial activities all have the potential to impair interstitial bacterial and invertebrate biota
and disrupt the hydrological connections between the hyporheic zone and stream, groundwater, riparian, and floodplain ecosystems.
Until recently, our scientific ignorance of hyporheic processes has perhaps excused the inclusion of this ecotone in river
management policy. However, this no longer is the case as we become increasingly aware of the central role that the hyporheic
zone plays in the maintenance of water quality and as a habitat and refuge for fauna. To fully understand the impacts of human
activity on the hyporheic zone, river managers need to work with scientists to conduct long-term studies over large stretches
of river. River rehabilitation and protection strategies need to prevent the degradation of linkages between the hyporheic
zone and surrounding habitats while ensuring that it remains isolated from toxicants. Strategies that prevent anthropogenic
restriction of exchanges may include the periodic release of environmental flows to flush silt and reoxygenate sediments,
maintenance of riparian buffers, effective land use practices, and suitable groundwater and surface water extraction policies. 相似文献