摘要
三峡大坝建成后,将在库区两岸形成永久性的水位涨落带,涨落带冬半年为水域,夏半年出露水面为陆,是一种独特的湿地生态系统。在夏半年,涨落带出露土地面积大,可利用基础好;加之成陆期较长,与同期丰富的光热水资源构成优势组合,使涨落带土地资源具有较高的生产潜力。因此,应重视涨落带土地资源的研究和利用。
After the compietion of the Three-Gorge-Reservoir in Yangtze River,a water-level-fluctuatingzone will be formed along both banks of a section of the river in the reservoir. The zone will be a typeoi land resources with many functions for being a water area through a winterhali- year and a land areathrough a summer-half-year. The zone will be of a special value to utilization because there will be notoniy an area of hundreds of square kilometers and a goed basis for exploitation,but aiso a longer periodbeing a land and a better realignment of land resources, sunlight energy,radiant heat and water re-sources in this Deried. Therefore,it is important to pay a greater attention to researches on land re-sources in the zone and their exploitation.
出处
《西南师范大学学报(自然科学版)》
CAS
CSCD
1994年第5期528-533,共6页
Journal of Southwest China Normal University(Natural Science Edition)
关键词
水库
水位涨落带
土地资源
The Three- Gorge- Reservoir
water levels fluctuating zone
land resource