首页> 外文会议>ICCE 2011;International Conference on informatics, cybernetics, and computer engineering >Evolution Characteristics of Wetland in Beijing and Its Driving Factors Analysis
【24h】

Evolution Characteristics of Wetland in Beijing and Its Driving Factors Analysis

机译:北京湿地演变特征及其驱动因素分析

获取原文

摘要

Supported by remote sensing and GIS technology, using Multi-temporal TM images from 1984a to 2008a in Beijing, the dynamic evolution characteristics of wetland were analyzed and driving factors were explored. The result shows: the total wetland area increased during the period from 1984a to 1996a, the wetland area in 1996a had the maximum value, totally 605. 67km~2. while it obviously declined at the annual average rate 6.7% from 1996a to 2004a, the wetland area in 2004a was just 285.27 km~2, which accounting for 47.1% of the wetland area in 1996a. Wetland had taken the dominant shrinking trend and its ecological function had degenerated gradually. The total wetland area had appreciably increased after 2006a. reaching to 318.39km~2 in 2008a. It was classified to natural wetland and artificial wetland, natural wetland means river wetland and artificial wetland included reservoir wetland, pond and paddy field wetland, artificial canal wetland and city lake wetland. The proportion of artificial wetland area was lager than natural wetland, which played the ascendant function, accounting for about 70.95 to 86.01 percents in area. Wetland area increased from 1984a to 1996a mainly because of adequate precipitation; while the total wetland area declined from 1996a to 2004a for both natural elements and artificial reasons. Natural reasons included continuous dry climate, higher transpiration and decrease of water inflow from upriver. With the urbanization process acceleration, the population increased 1.52 times between 1984a and 2008a, which further lead to the wetland area loss and water resource consumptions. The total area of wetland in 2006a and 2008a increased appreciably as a result of the implement of positive policy and precipitation's increase.
机译:通过遥感和GIS技术支持,使用1984A至2008A在北京的多时间TM图像,分析了湿地的动态演化特性,并探讨了驱动因素。结果表明:1996年至1996年的湿地面积的总湿地面积增加,1996年的湿地区域具有最大值,共605.67km〜2。虽然从1996年至2004A年的年度平均比率下降了6.7%,但2004年的湿地区仍然是285.27公里〜2,占1996年湿地区的47.1%。湿地采取了显着的萎缩趋势,其生态功能逐渐退化。在2006A后,湿地区域的总升起增加。 2008A达到318.39公里〜2。它被归类为天然湿地和人造湿地,天然湿地是指河湿地和人造湿地包括储层湿地,池塘和稻田湿地,人工运河湿地和城市湖湿地。人造湿地面积的比例比天然湿地的含量,该湿地发挥了上升功能,占地区的约70.95%至86.01%。湿地面积从1984A到1996年增加,主要是由于充足的降水;虽然自然元素和人工原因,但湿地的总湿地区域从1996年到2004A人下降。自然原因包括连续干燥的气候,较高的逆向和偏转水流入的降低。随着城市化进程加速,人口在1984A和2008A之间增加了1.52倍,进一步导致湿地面积损失和水资源消耗。由于实施积极的政策和降水量,2006A和2008A的湿地总面积显着增加。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号