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    赵峰, 刘华, 鞠洪波, 张怀清, 邹文涛. 三江源典型区湿地景观稳定性与转移过程分析[J]. 北京林业大学学报, 2012, 34(5): 69-74.
    引用本文: 赵峰, 刘华, 鞠洪波, 张怀清, 邹文涛. 三江源典型区湿地景观稳定性与转移过程分析[J]. 北京林业大学学报, 2012, 34(5): 69-74.
    ZHAO Feng, LIU Hua, JU Hong-bo, ZHANG Huai-qing, ZOU Wen-tao.. Landscape stability and its pattern transition of typical wetlands in three river sources, southwestern China.[J]. Journal of Beijing Forestry University, 2012, 34(5): 69-74.
    Citation: ZHAO Feng, LIU Hua, JU Hong-bo, ZHANG Huai-qing, ZOU Wen-tao.. Landscape stability and its pattern transition of typical wetlands in three river sources, southwestern China.[J]. Journal of Beijing Forestry University, 2012, 34(5): 69-74.

    三江源典型区湿地景观稳定性与转移过程分析

    Landscape stability and its pattern transition of typical wetlands in three river sources, southwestern China.

    • 摘要: 基于1977、1990、1997和2007年4期遥感影像,对三江源典型区湿地景观稳定性和时空转移过程进行分析。结果表明:1977—2007年间河流斑块面积和数量的稳定性水平最高,其中1977—1990年间其特征稳定性指数接近于1,但结构稳定性较低。湖泊景观稳定性呈增强趋势,且表现最稳定。沼泽景观稳定性表现为减弱趋势,至2007年稳定性水平降到最低,呈现最不稳定状态。河滩地面积和数量稳定性水平低,变化不稳定,结构稳定性也始终处于最低水平。1977—2007年湿地转移趋势主要表现为:1977—1990年湿地与非湿地类型转换最为突出, 1990—1997年、1997—2007年转换平稳。湿地转出类型主要为草地,河流和河滩地转换频率较高,湖泊类型转化呈多元化,沼泽地转出类型几乎全为草地,转为其他类型的面积很少。

       

      Abstract: Based on the 1977 MSS images, 1990, 1997 and 2007 Landsat TM images, landscape stability of typical wetlands in three river sources and its process of landscape conversion were analyzed in this paper. Considering the spatial resolution, the study area was divided into 6 types, such as river, lake, marsh, river beach, bare rock, etc. After the geometrical correction by using topographic maps, tasseled cap transformation, normalized difference water index (NDWI) and shape index were chosen to enhance the wetland spectral information. Expert classification system based on the multilayer information extraction was adopted to extract the main wetland types in the study area. The results indicated that the area and number of river land got the highest stability condition in 1977-2007, the stability index was especially close to 1 in 1977-1990, while the structural stability of river was at low level. The stability of lake wetland had been stably strengthened and it was the most stable type. The stability of marsh wetland trended to be decreasing, and was at the lowest level in 2007, so it was the most unstable. The stability of flood bed was at the low level during 1977-2007 and changed irregularly. The process of landscape conversion among different periods showed that the transformation between wetland and nonwetland was the most in 1977-1990, and it was gentle during 1990-1997 and 1997-2007. Wetland was mainly transferred to grassland, the conversion between river land and flood bed was frequent, lake wetland was converted to more than one type, while marsh land was transferred to almost the grassland,and few area was changed to other types.

       

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