西伯利亚淡水资源格局与合作开发潜力分析
Spatial distribution and potential exploration of water resources in Siberia
查看参考文献34篇
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文摘
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淡水是人类生存的基础,也是全球战略性资源。总面积为969万km~2的俄罗斯西伯利亚地区,拥有蓄水量占全球地表淡水资源总量约22%的贝加尔湖,以及总长度约500万km的河流和多座大型水库,其中叶尼塞河、勒拿河、鄂毕河等大型河流的水资源量极为丰富。据分析,该地区多年平均地表水资源量为2.35万亿m~3,占全俄水资源总量的55%;水能资源蕴藏量为1.556万亿kW· h,占全俄65%;水运资源量为5.65万km,占全俄55.8%。尽管该地区水资源丰富,但由于人口稀少(不足2400万人,仅占全俄总人口的16%左右),水资源利用程度低,具有很大的开发潜力。西伯利亚山区河流水量丰沛,水能开发及水电发展具有广阔的前景。随着全球变暖,西伯利亚平原区河流的结冰期变短,航运价值不断提高。同时,在俄罗斯西伯利亚周边地区严重缺水的背景下,通过虚拟水贸易或跨流域调水,向中亚、蒙古和中国北方地区输送淡水资源具有重要的战略意义,将推动这一地区的经济与社会协同发展。随着“一带一路”倡议和“中蒙俄经济走廊”的规划实施,中蒙俄三方在水资源与水电能源等方面的合作具有广阔的前景。 |
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其他语种文摘
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Freshwater is the foundation of human survival and a global strategic resource. The Siberian region of Russia has a total area of 9.69 million km~2, which includes the Lake Baikal (~ 22% of the total surface freshwater resources), rivers with a total length of ~5 million km and large reservoirs. The large rivers such as Yenisei, Lena, and Ob are extremely rich in water resources. The average annual water resources in this area are 2350 km~3, accounting for 55% of the total water resources in Russia. The hydropower resources are 1.556 trillion kilowatt hours, accounting for 65% of the total hydropower resources in Russia. The water transport resources are 56,500 km, accounting for 55.8% of the total water transport resources in Russia. This area is rich in water resources, while it is sparsely populated (less than 24 million people, accounting for only about 16% of the total Russian population). Therefore, this region demonstrates a low utilization of water resources, with great potential for development. Mountain Rivers in Siberian are rich in water resources. Therefore, the water power development has broad prospects. As the results of the global warming, the icing period of plain rivers in Siberian becomes shorter and the shipping capacity continues to increase. Additionally, under the background of severe water shortages in the surrounding areas of Siberian, the supply of freshwater resources to Central Asia, Mongolia, and northern China through virtual water trade or inter-basin water transfer indicate an important strategic significance and will promote the coordinated economic and social development of the region. With the implementation of the "Belt and Road Initiative" and the "China-Mongolia-Russia International Economic Corridor", China, Mongolia, and Russia have broad prospects for cooperation in hydropower and energy. |
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来源
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资源科学
,2018,40(11):2186-2194 【核心库】
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DOI
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10.18402/resci.2018.11.05
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关键词
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俄罗斯
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西伯利亚
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水资源
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合作开发
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跨流域调水
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地址
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中国科学院地理科学与资源研究所, 中国科学院陆地水循环及地表过程重点实验室, 北京, 100101
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中国科学院大学, 北京, 100049
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中国科学院地理科学与资源研究所, 中国科学院资源利用与环境修复重点实验室, 北京, 100101
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俄罗斯科学院西伯利亚分院地理研究所, 伊尔库茨克, 664033
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语种
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中文 |
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文献类型
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研究性论文 |
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ISSN
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1007-7588 |
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学科
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水利工程 |
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基金
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国家科技基础资源调查专项课题
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中国科学院战略性先导科技专项
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中国科学院重点部署项目
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文献收藏号
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CSCD:6362206
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参考文献 共
34
共2页
|
|
1.
李原园. 1956~2010年中国可更新水资源量的变化.
中国科学:地球科学,2014(9):2030-2038
|
被引
12
次
|
|
|
|
|
2.
Shiklomanov I A. Appraisal and assessment of world water resources.
Water International,2000,25(1):11-32
|
被引
22
次
|
|
|
|
|
3.
Oki T. Global hydrological cycles and world water resources.
Science,2006,313(5790):1068-1072
|
被引
218
次
|
|
|
|
|
4.
Famiglietti J S. Water in the Balance.
Science,2013,340(6138):1300-1301
|
被引
17
次
|
|
|
|
|
5.
Pekel J F. High-resolution mapping of global surface water and its long-term changes.
Nature,2016,540(7633):418-422
|
被引
193
次
|
|
|
|
|
6.
Datry T. Intermittent rivers: a challenge for freshwater ecology.
Bioscience,2014,64(3):229-235
|
被引
7
次
|
|
|
|
|
7.
Tooth S. Process, form and change in dryland rivers: a review of recent research.
Earth Science Reviews,2000,51(1):67-107
|
被引
9
次
|
|
|
|
|
8.
王平. 西北干旱区间歇性河流与含水层水量交换研究进展与展望.
地理科学进展,2018,37(2):183-197
|
被引
7
次
|
|
|
|
|
9.
Famiglietti J S. The global groundwater crisis.
Nature Climate Change,2014,4(11):945-948
|
被引
22
次
|
|
|
|
|
10.
Wada Y. Global depletion of groundwater resources.
Geophysical Research Letters,2010,37(20):114-122
|
被引
29
次
|
|
|
|
|
11.
Schwarzenbach R P. Global water pollution and human health.
Social Science Electronic Publishing,2010,35(1):109-136
|
被引
38
次
|
|
|
|
|
12.
БезруковЛА. Водные ресурсы Сибири: Состояние, проблемы и возможности исполь-зования.
География И Природные Ресурсы,2014(4):30-41
|
被引
1
次
|
|
|
|
|
13.
МорейдоВМ. Оценка возможных изменений водного режима реки Селенги в XXI в. На основе модели формирования стока.
Водные Ресурсы,2017,44(3):275-284
|
被引
1
次
|
|
|
|
|
14.
ШикломановИА (Ред.).
Водные Ресурсы России И Их Использование,2008
|
被引
1
次
|
|
|
|
|
15.
Shiklomanov A I. Cold region river discharge uncertainty-estimates from large Russian rivers.
Journal of Hydrology,2006,326(1/4):231-256
|
被引
3
次
|
|
|
|
|
16.
Yang D. Streamflow changes over Siberian Yenisei River Basin.
Journal of Hydrology,2004,296(1):59-80
|
被引
12
次
|
|
|
|
|
17.
Peterson B J. Increasing river discharge to the Arctic Ocean.
Science,2002,298(5601):2171-2173
|
被引
51
次
|
|
|
|
|
18.
Yang D. Siberian Lena River hydrologic regime and recent change.
Journal of Geophysical Research Atmospheres,2002,107(23):1-14
|
被引
1
次
|
|
|
|
|
19.
ВыручалкинаТЮ. Байкал и Ангара до и после создания водохранилищ.
Водные Ресурсы,2004,31(5):526-532
|
被引
1
次
|
|
|
|
|
20.
瓦洛帕也夫ГВ. 预测调西伯利亚的河流部分径流对自然条件的影响.
海河水利,1984(S2):74-78
|
被引
1
次
|
|
|
|
|
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